gis.geosurv.gov.nl.cagis.geosurv.gov.nl.ca/geofilePDFS/ReceivedBatch63/013J_0285.pdf · 2008...

2008 Assessment Report on the

Geochemical and Diamond Drilling Investigations on the Jacques Lake Property

of the CMB Project, Labrador, Canada

Year 5 Supplementary Assessment Report

Includes work on licence: 10051M

NTS Sheet: 13J12E; 13J13E

Submitted by: P. McNeill, P.Geo, C. McLean, P. Geo.,

L. Hansen, S. Savidant

For

Aurora Energy Resources Inc. Suite 303, 10 Fort William Place, St. John's, NL A1C 1K4

June 11, 2009

Work Year: 2008 Total Claims: 220

Total Expenditure: $ 4,475,761.61

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TABLE OF CONTENTS

Page LIST OF FIGURES.......................................................................................................................................3 LIST OF TABLES.........................................................................................................................................3 LIST OF PLATES.........................................................................................................................................3 LIST OF APPENDICES...............................................................................................................................3 1.0 INTRODUCTION...........................................................................................................................4

1.1 PROPERTY DESCRIPTION AND LOCATION ......................................................................................4 1.2 STATEMENT OF EXPENDITURES.....................................................................................................9

2.0 JACQUES LAKE TARGET ........................................................................................................12 2.1 DIAMOND DRILLING....................................................................................................................12

2.1.1 Introduction ...........................................................................................................................12 2.1.2 Drill Hole Summaries ............................................................................................................14 2.1.3 Discussion of Drill Hole Results Introduction.......................................................................20

2.2 SPECIFIC GRAVITY SAMPLING.....................................................................................................24 3.0 SAMPLING PROTOCOLS .........................................................................................................24

3.1 CORE SAMPLES ...........................................................................................................................24 3.2 SHIPPING PROTOCOL ...................................................................................................................24 3.3 DIAMOND DRILLING....................................................................................................................25

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LIST OF FIGURES Figure 1.1: Location Map – CMB Project .......................................................................... 6 Figure 2.1: Jacques Lake Target Area – 2008 Diamond Drilling Plan Map .................... 14 Figure 2.2: Jacques Lake Long Section Showing 2008 DDH .......................................... 23 Figure 2.3: Jacques Lake Representative Drill Section L1000mE ................................... 24

LIST OF TABLES Table 1.1: Aurora’s Mineral Holdings................................................................................ 8 Table 1.2: Accepted Expenditures on Mineral Licence 10051M ....................................... 9 Table 1.3: Tenure Information for Jacques Lake property ............................................... 10 Table 1.4: List of personnel and days worked on the CMB Project in 2008.................... 11 Table 1.5: List of Contractors that worked on the CMB Project in 2008......................... 12 Table 2.1: Summary of Summer 2008 Jacques Lake Drilling.......................................... 15 Table 2.2: Summary of Summer 2008 Jacques Lake Assay Composites......................... 22

LIST OF PLATES Plate 1.1: Aerial View of Postville, Labrador..................................................................... 4

LIST OF APPENDICES Appendix I Certificate of Author ……………………………………………….... 16 Appendix II Expenditure Summary ………………………………………………. . 18 Appendix III Analytical Methods …………………………………………………... 20 Appendix IV Drill Sections ………………………………………………………… 34 Appendix V Drill Data ……………………………………………………………. 42 Appendix VI Assay Certificates ……………………………………………………. 128 Appendix VI Drill Section Lithology Key Code …………………………………… 230 Appendix VII Sample Info ………………………………………………………….. 232

LIST OF DIGITALFILES (.txt,.MDB,.xls files) Downhole Gamma Probe Downhole Magnetic Susceptibility Downhole RQD Downhole Deviation Survey

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1.0 INTRODUCTION This report details the diamond drilling, associated geochemical sampling activities, and specific gravity sampling carried out on the Jacques Lake property by Aurora Energy Resources Inc. from the month of May up to, and including, the month of August in the 2008 work year. Drilling activities conducted from January to March of 2008 on the Jacques Lake property have been submitted in an early report. Other exploration activities carried out on this property but not contained within this assessment report include mapping and prospecting.

1.1 Property Description and Location The Jacques Lake property is part of the CMB Project, located southeast of Kaipokok Bay on the northeast coast of Labrador, Canada (Figure 1.1). The nearest community is the town of Postville located approximately 24 km north of the project boundary (Plate 1.1). The community of Happy Valley-Goose Bay lies 180 km south of Postville. The project straddles two UTM zones (Zone 20, 21) and seven NTS map sheets (13J/11, 13J/12, 13J/13, 13J/14, 13K/03, 13K/06, 13K/09). The northern and southern limits of the project area are 6094000mN (Zone 21) and 6048500mN (Zone 21) respectively, while the western and eastern limits of the project area are 681000mE (Zone 20) and 345000mE (Zone 21) respectively. Most of the licenses are contiguous and are located 5 to 40 kilometres south of Postville (Figure 1.2) though some licenses which make up the Croteau and Storm properties are located further west in the Central Mineral Belt and the interior of Labrador. Aurora staked another four Mineral Licences located along the proposed road corridor in June 2008.

Plate 1.1: Aerial View of Postville, Labrador

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Figure 1.1: Location Map – CMB Project

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1.2 Mineral Tenure The CMB Uranium Property consists of 32 map staked licenses registered in the name of Aurora Energy Resources Inc. (TSX-AXU) totaling 3660 claims or 91,500 ha. (Figure 1.2 and Table 1.1). Twenty-eight of these licenses totaling 3248 claims or 81,200 ha were originally subject to a letter of agreement dated February 5th, 2003, between Fronteer Development Group Inc. (TSX-FRG) of Vancouver, Canada and Altius Resources Inc. (TSX-ALS) regarding an Area of Interest made up of eighteen 1:50,000 scale NTS map sheets. This agreement formed the basis for a 50:50 strategic alliance between Fronteer and Altius Resources Inc. of St. John’s, Newfoundland to explore for iron oxide-copper-gold mineralization in the Central Mineral Belt of Labrador. A further agreement was signed on June 3rd, 2005 allowing for the formation of a jointly owned private company called Aurora Energy Inc. to hold the assets of the CMB Uranium Property. The name of Aurora Energy Inc. was subsequently changed to Aurora Energy Resources Inc. during an initial IPO on the Toronto Stock Exchange on March 22nd, 2006. Four additional map licences totaling 412 claims or 10,300 ha (Table 1.1) were staked in June; these located between the Town of North West River and the Michelin Project.

Figure 1.2: CMB Project - Mineral Tenure with outline of LISA and LIL Lands

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Table 1.1: Aurora’s Mineral Holdings

Property Licence Claims Issued Long Point Pond 009411M 128 27-Mar-03 Michelin Main 009412M 190 27-Mar-03 White Bear 009413M 42 27-Mar-03 Otter Lake 009414M 63 27-Mar-03 Croteau 009415M 40 27-Mar-03 Storm 010726M 16 27-Mar-03 Inda 014457M 145 27-Mar-03 Melody Hill 009482M 32 28-Apr-03 Goulou Pond 009719M 32 24-Oct-03 Post Hill West 009720M 60 24-Oct-03 East Micmac Lake 009721M 36 24-Oct-03 Morgan’s Pond 009722M 100 24-Oct-03 Michelin Northwest 009723M 42 24-Oct-03 Melody West 010022M 190 2-Apr-04 Witch Doctor Lake 010046M 181 12-Apr-04 Mustang Lake South 010047M 120 12-Apr-04 Mustang Lake Northwest 010048M 137 12-Apr-04 Tom Hill Pond 010049M 166 12-Apr-04 Bear Trap 010050M 147 12-Apr-04 Jacques Lake 010051M 220 12-Apr-04 Micmac Hill 010052M 127 12-Apr-04 Porcupine Lake South 010053M 111 12-Apr-04 Porcupine Lake North 010054M 170 12-Apr-04 Eastern Boundary 010055M 136 12-Apr-04 Pond of Islands Lake 010056M 126 12-Apr-04 Kaipokok Bay 010059M 54 12-Apr-04 Aurora Corridor 010343M 175 29-Oct-04 Melody Lake 010344M 120 29-Oct-04 5460 015222M 25 25-Jul-08 Mulligan River 015223M 131 25-Jul-08 Seabaskachu River 015237M 165 25-Jul-08 Lake Melville 015237M 91 25-Jul-08

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Mineral Licence 10051M was staked on March 3, 2004 and issued on April 12, 2004. The licence contains 220 claims and is located at the East end of Jacques Lake (see Figure 1.3). The licence overlaps Labrador Inuit Lands (LIL 36.59%). Exploration work on the licence has been continuous since 2004 with expenditures totaling $15,060,109.11 (see Table 1.1). An expenditure of $124,474.55 is required on this license by 2018/04/12.

Figure 1.3: Mineral Licence 10051M Location Map

Table 1.2: Accepted Expenditures on Mineral Licence 10051M

Year Submittal Date Expenditure 1 2/25/2005 $178,773.94 2 2/20/2006 $1,080,552.78 3 7/5/2007 $2,767,990.24 4 3/10/2008 $10,959,266.70 5 4/6/2009 $73,525.45

Total $15,060,109.11

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1.2 Statement of Expenditures The total eligible expenditures on the Jacques Lake property from May through September, 2008, contained within licence 10051M, was $4,475,761.61. Table 1.2 summarizes tenure information for the eligible 2008 expenditures applied to licence 10051M. Table 1.2 gives a Division Allocation Summary detailing the cost breakdown within licence 10051M. Table 1.3 lists Aurora’s personnel who worked on the CMB Project during 2008 with total number of field man days worked. Table 1.4 lists the contractors that worked the prospecting program. Also, note that excess expenditures will be carried forth to the following assessment years.

Further details can be found in Appendix II including: the 2008 Division

Allocation Summary from the accounting department of Aurora Energy Resources Inc.

Table 1.3: Tenure Information for Jacques Lake property

Property Licence Claims Ha. NTS Issued Work Due 2008 Total

Jacques Lake 10051M 220 5500 13J/12E; 13J13E 12/4/2004 6/11/2009 $4,475,761.61

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Table 1.4: List of personnel and days worked on the CMB Project in 2008

Department Services Provided Personnel Days Worker VP Exploration Paul McNeil 174 Exploration Manager Cameron McLean 348 Project Geologist Lyle Hanson 217 Project Geologist Liane Boyer 177 Geologist Jean Bernard 117 Geologist Martin Taiani 212 Geologist Jean Francois 59 Geologist Kanan Sarioglu 188 Geologist Stephanie Savidant 315 Geotechnician David Winters 84 Geotechnician Holly Andersen 124 Geotechnician Jenna Penney 85 Geotechnician Lukas Ittulak 70 Geotechnician Russell Palliser 50 Junior Geologist Sarah Nicholson 53 Junior Geologist Matthew Tracey 66 Junior Geologist Byron Kelly 54

Geo

scie

ntifi

c S

taff

Junior Geologist Robyn Dicks 53 Field Tech Matthew Gould 145 Enviro Technician Sheldon Anderson 88 Pad Builder Chris LA Combdon 69 Pad Builder Brendan Lethbridge 99 Fi

eld

Cre

w

Pad Builder Don Gear 99 Logistics Manager Wayne Broomfield 323 Logistics Manager Lisa Holleman 190 First Aid Attendant/Logistics Angelina Dragani 69 Ground Support Don Colbourne 83 Facilities Assistant Aubrey Paul 205 Lo

gist

ics

Logistics Coordinator Cal Priddle 239 Camp Maintenance Wayne Curl 51 Camp Maintenance Eric Lane 61 Camp Maintenance Trevor Edmunds 64 C

amp

Mai

nten

ance

Camp Maintenance Stanley Wolfrey 67 Head Cook Stella Bird 64 Head Cook Elizabeth Blois 57 Head Cook Dianne Peterson 19 Kitchen Assistant Sharon Hamel 67 Kitchen Assistant Voilet Ward 42 Kitchen Assistant Mary Ann Andersen 77 Kitchen Assistant Margaret Martin 34 Kitchen Assistant Myrtle Groves 61 Assistant Cook Donna Sheppard 61

Kitc

hen

Sta

ff

Housekeeper Maxine Andersen 74 Lands Manager John Stephen Ash 348 Office Coordinator Judy Manak 206

Offi

ce

Administrative Assistant Zena Sheppard 162 Total 5570

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Table 1.5: List of Contractors that worked on the CMB Project in 2008

Courier Air Labrador, Blizzard Corporation Limited, Bugden's Taxi Ltd., Dynamex Canada Corp., Express Havre St Pierre, Federal Express Canada Ltd., Innu Mikun Airlines, Moktech 2000 Limited, Neopost Canada Ltd., Pik-Fast Express Inc., Provincial Airlines, RBC Visa, RST Instruments Ltd., U.T.V. International Inc., UPS Canada

Field Supplies

First Copy Duplicating Centre Ltd., Moktech 2000 Limited, Target Marketing&Communications Inc, Tosss Signs Inc.

Equipment Supplies

ACM Investments Ltd, Acklands-Grainger Inc., Bell ExpressVU, Blizzard Corporation Limited, Canex Supermart, Deakin Industries, Eastern Medical Supplies, Enviro Safe Fuel Systems Ltd., Executive Coffee Services Ltd., Frenchie's Service Centre, Goose Bay Motors Ltd., Goose Bay Sports Ltd, Goose Bay Wholesalers Limited, Goose Sales & Service Ltd., Guillevin International Co., Hamilton Drugs Ltd., Hamilton Systems & Sales Ltd, Hamilton Wholesalers, Hillcrest Automotive, Hillier's Trades Limited, Hoskin Scientific Limited, Hotel North, Iglutek Computers Inc., Innu Mikun Airlines, Joe's Autobody Shop Ltd., Labrador Specialty Services Inc., Labradorian Printers, Mealy Mountain Contracting Ltd., Mettler Toledo Inc., Minipi Outfitters 2006, Moktech 2000 Limited, Moore's Handicrafts Ltd., Multitrends, Naskaupi Woodworkers Inc., National Safety Equipment, National Shoe, Neopost Canada Ltd., Northern Lights, Northmart, Notre Dame Agencies, Per-mit Enterprises Ltd., Postmill Lumber Inc., ProFire Sales & Services Inc., Project allocation adjustment, Reflex Instrument North America, Riff's Limited, Rogers Payment Centre 265-028493508, RST Instruments Ltd., Sheppard's Skiddo Variety Shop Inc, Staples Business Depot, Star Choice Television, Switch Electrical Inc., Terraplus Inc., Terry's Tents and Shoe Repair Ltd., The Carpet Man Limited, The North West Co. Inc., Tosss Signs Inc., Transport Sego, U.T.V. International Inc., Ulu Industrial Services, United Rentals, Universal Helicopters Newfoundland, Valley Business Equipment Inc., Warr's Pharmacy Ltd., Westland Environmental Services Inc

Aircraft Universal Helicopters Newfoundland, Air Labrador, Innu Mikun Airlines

Fuel Facility Goose Sales & Service Ltd., Keller Equipment Supply Ltd., Postmill Lumber Inc., Enviro Safe Fuel Systems Ltd., ProFire Sales & Services Inc.

Crew Care Bell ExpressVU, Blizzard Corporation Limited, Goose Bay Sports Ltd, Goose Sales & Service Ltd., Hamilton Drugs Ltd., Newfoundland & Labrador Hydro 58133, Northmart, Setanta Sports Canada, Star Choice Television, The North West Co. Inc.

Lodging Goose Sales & Service Ltd., Hamilton Wholesalers, Hotel North, Newfoundland & Labrador Hydro 58133, Northcoast Hospitality Ltd., Northmart, The Fairmont Newfoundland, The Labrador Inn

Drilling Air Liquide Canada Inc., Enviro Safe Fuel Systems Ltd., Falcon Drilling Ltd., Frenchie's Service Centre, Goose Sales & Service Ltd., Major Drilling Int'l. Group Inc., Notre Dame Agencies, Postmill Lumber Inc., Reflex Instrument North America, Royal Inn & Suites, RST Instruments Ltd., Springdale Forest Resources Inc., Woodward's Oil Limited

Vehicle Maintenance

All Season Recreation, Goose Bay Motors Ltd., Hillcrest Automotive, Labrador Motors Ltd., Remote Camp Services, U.T.V. International Inc.

Equipment Rental

Air Liquide Canada Inc., Blizzard Corporation Limited, Canada Wide Communications, Dewy's Gas Bar, Falcon Research, Gemcom Software International Inc., GMAC - Montana 056-9120-96337, GMAC - Silverado 056-9114-72742, Goose Bay Motors Ltd., Goose Sales & Service Ltd., Innu Mikun Airlines, Labrador Specialty Services Inc., Postmill Lumber Inc.

Property Rental

56539 Newfoundland and Labrador Inc., Adlavik Inn Ltd., Baine Johnston Centre Limited, Fortis Properties Corporation, Fronteer Development Group Inc.

Survey Topographic Aero Geometrics, EnFor Consulting Services

Expediting Freight

Air Canada Cargo, Air Labrador, Blizzard Corporation Limited, Department of Transporation, Government of Newfoundland and Labrador, Innu Mikun Airlines, Provincial Airlines, United Rentals, Woodward's Oil Limited

Geological Services Activation Laboratories Ltd., ALS Chemex, Fugro Airborne Surveys Corp., Technetium Consulting Ltd.

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2.0 JACQUES LAKE TARGET

2.1 Diamond Drilling

2.1.1 Introduction

The Jacques Lake Area is located 31 km northeast of the Michelin deposit and approximately 25 km southeast of Postville at the eastern end of Jacques Lake. A diamond drilling program consisting of approximately 6,000 metres was proposed for the Jacques Lake deposit in the summer of 2008. The focus of the proposed program was to infill the known regions of the deposit and upgrade inferred and indicated resources.

A total of 17 drill holes, comprised of 14 completed infill drill holes (one of

which was started during the winter program), 2 completed metallurgical/geotechnical holes, and one aborted infill drill hole (which was started during the winter program), totalling 6482.5 m were drilled on the Jacques Lake deposit between May 17th and August 3rd, 2008 (Figure 2.1 and Table 2.1). The infill drill program used up to 2 helicopter-supported drill rigs from Major Drilling Group International Inc. of Suite 100, 111 St. George Street, Moncton, NB E1C 1T7, and one helicopter-supported drill rig from Springdale Forest Resources of PO Box 387, Springdale, NL A0J 1T0; while the metallurgical/geotechnical drill program used one helicopter-supported drill rig from Dorado Drilling of 1236 Mabel Lake Rd., Box 1344, Vernon, BC V1T 6N6.

Infill drilling targeted the central region of the deposit through to the southwestern edge at depth. Drill hole orientations ranged from 305° to 319° azimuth to intercept mineralization at a roughly perpendicular orientation. Metallurgical drilling targeted the length of the main ore zone with vertical drill holes.

Details concerning the individual holes are listed in Table 2.1 and represented in

the following DDH plan map Figure 2.1.

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Figure 2.1: Jacques Lake Target Area – 2008 Diamond Drilling Plan Map Summer 2008 ddh are shown in green; previous ddh are shown in red

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Table 2.1: Summary of Summer 2008 Jacques Lake Drilling # Holes Hole ID UTM East UTM North Elev.

(m) Azimuth Dip Status Meterage (m)

Jacques Lake Data = NAD83, zone 21

1 JL08-085** 333008.2 6065866.7 230 310 -55 completed 172

2 JL08-086** 333139.3 6065857.2 242 305 -47 aborted 138

3 JL08-088 333029.3 6065962 239 311 -60 completed 447

4 JL08-089 333007.9 6065867.2 255.1 314 -46 completed 534

5 JL08-090 333102.6 6065959.3 244.4 314 -55 completed 499

6 JL08-091 333029.3 6065962.3 230 315 -53 completed 419

7 JL08-092 333008.9 6065866.4 239 315 -65 completed 583

8 JL08-093 333103 6065958.8 255.1 313 -62 completed 517

9 JL08-094 332998.7 6066070.6 230 312 -60 completed 395

10 JL08-095 332763.3 6065836.8 211 319 -68 completed 492

11 JL08-096 333103.5 6065958.8 255.1 318 -72 completed 634

12 JL08-097 332998.2 6066070.9 244 310 -49 completed 353

13 JL08-098 332762.8 6065837.7 208 313 -49 completed 439

14 JL08-099 332999 6066070.4 244 310 -63 completed 367

15 JL08-100 332945 6066325 190 315 -45 completed 219 Infill Drill Total 6208

16 JLM08-001* 333030.2 6066396.5 190.6 0 -90 completed 142

17 JLM08-002* 333030 6066396.8 190.6 0 -80 completed 132.5 Metallurgical Drilling Total 274.5

Overall Drilling Totals 6482.5

* denotes geotechnical/metallurgical drill hole ** denotes drill holes continued from the 2008 winter drill program. Only lists meterage pertaining to the summer drill program.

2.1.2 Drill Hole Summaries JL08-085 Azimuth: 310° Dip:-55° E: 333006 N: 6065856 EOH: 517 m

JL08-085 commenced drilling March 6th and subsequently shut down March 14th, 2008 as the winter DDH program came to a close. The hole was re-started May 17th and reached a final depth of 517m on May 20th, 2008. The core displayed frequent intervals of fine grained intermediate metavolcanics along with the usual metamorphosed polylithic conglomerate cut by frequent mafic dykes; however, it showed little mineralization. A spot high of 315 cps occured at approximately 357.29 m hosted in typical carbonate +/- biotite +/- pyrite +/- hornblende veined, fine grained intermediate metavolcanics. Another thin zone approximately 0.25 m thick and hosted in intermediate metavolcanics returned elevated scint values peaking at 696 cps at a depth of approximately 362 m. No further mineralization was recorded. The hole passed through 2 felsic porphyry horizons, and ended in barren intermediate volcanics at a depth of 517m.

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JL08-086 Azimuth: 305° Dip:-47° E: 333143 N: 6065858 EOH: 317 m

JL08-086 began drilling March 9th, 2008 on the same site as JL08-081A and -084. The hole was shut down with the winter program on March 14th, 2008 and was re-started May 18th, 2008. The drill cored typical Jacques Lake hanging wall lithologies consisting of chlorite-actolite altered porphyritic to non-porphyritic mafic intrusives, variably strained polylithic metaconglomerate and occasional fine grained to aphanitic, felsic to intermediate dykes. The hole was eventually shut down on May 22nd, 2008 due to unexpected deviation and poor drilling conditions resulting from the fractured rock. The hole was aborted at a depth of 317 meters in barren intermediate volcanics short of the main ore zone. As a result, no anomalous uranium mineralization was encountered. JL08-087 Completed in March 2008 – see previous assessment report

JL08-088 Azimuth: 311° Dip: -60° E: 333032 N: 6065970 EOH: 438 m

Drill hole JL08-088 commenced on May 20th, 2008 and reached a final depth of 447m on June 3rd, 2008. Typical Jacques Lake polylithic, moderately strained metaconglomerate was encountered up to a depth of 258.56 m, frequently cut by syn to post kinematic mafic dykes. Jacques Lake fine grained, maroon coloured, carbonate +/- biotite+/- hornblende +/- pyrite veined, intermediate metavolcanics were intersected at a depth of 263.7 m. The contact between the intermediate volcanic and overlying conglomerate is defined by an intersection of mafic dyke. Patchy, moderate uranium mineralization was hosted in the intermediate volcanics, occurring from approximately 300-332 m, and averaging 275 cps throughout with a maximum of 1600 cps in hand. Trace chalcopyrite occured between 409.8 and 424.86 m. The drill hole was shut down in a thick, unmineralized syn-kinematic mafic intrusive. JL08-089 Azimuth: 314° Dip: -46° E: 333006 N: 6065856 EOH: 522 m

Drill hole JL08-089 was drilled off of the same pad as JL08-085. Drilling commenced on May 21st, 2008 and reached a final depth of 522 m on June 3rd, 2008. Typical Jacques Lake hanging wall lithologies of fine grained intermediate metavolcanics and polylithic metaconglomerate were cut by intermittent pre to post kinematic mafic dykes up to a depth of 299.84 m. Intermediate metavolcanics were intersected from a depth of 299.84 to 367.95 m hosting patchy moderate uranium mineralization with scint highlights as follows: 311 to 323 m averaging 535 cps with a maximum of 3100 cps; 350 to 357 m averaging 400 cps with a maximum of 1070 cps; 388 to 390 m with an average of 625 cps and a maximum of 2655 cps; 440 to 456 m averaging 550 cps with a maximum of 3700 cps. The contact between the conglomerate and underlying intermediate metavolcanic rocks is described as gradational. The drill was stopped in barren transitional felsic volcanics.

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Drill hole JL08-090 commenced on May 27th, 2008 and reached a final depth of 499m on June 7th, 2008. The drill hole cored typical metamorphosed polylithic conglomerate, intermittent pre to post kinematic mafic dykes and quartz-feldspar porphyritic felsic volcanics to a depth of 279.24 m. Net biotite +/- hornblende +/- carbonate +/- pyrite veined, fine grained intermediate volcanics were intersected from 297.40 to 406.21 m with moderate patchy uranium mineralization occurring from 360 to 382 m averaging 600 cps with a spot high of 5058 cps in hand. The drill then cored coarse feldspar porphyritic felsic intrusives, unmineralized intermediate metavolcanics and porphyritic to non-porphyritic mafic dykes. The drill hole ended in unmineralized coarsely feldspar porphyritic felsic intrusive. JL08-091 Azimuth: 315° Dip: -53° E: 333032 N: 6065970 EOH: 419 m

Drilling of hole JL08-091 started on June 4th, 2008 and reached a final depth of 419m on June 14th, 2008. Typical Jacques lake hanging wall sequences of polylithic metaconglomerate, porphyritic felsic intrusives and pre to post kinematic mafic dykes were intersected to a depth of approximately 241.86 m where a gradational contact with underlying intermediate metavolcanics was present. Patchy, weak uranium mineralization was encountered between approximately 287 m and 310 m depth with spot highs in hand up to 2200 cps. This mineralization was hosted in typical carbonate +/- biotite +/- hornblende +/- pyrite veined, fine grained intermediate volcanics. The drill then cored coarsely feldspar porphyritic felsic intrusives cut by minor porphyritic to non-porphyritic mafic dykes. The drill hole was shut down in a fine grained mafic intrusive unit. JL08-092 Azimuth: 315° Dip: -65° E: 333006 N:6065858 EOH: 583 m

Drill hole JL08-092 was collared on June 4th, 2008 and completed on June 17th, 2008. The hole was dominated by typical polylithic metaconglomerate and thin pre to post kinematic mafic dykes up to a depth of 466.5 m where a sharp contact with underlying intermediate metavolcanic rocks is found. Weak uranium mineralization occurs between 463 and 481 m with the best interval from 473-478 m returning an average of 330 cps and max value of 926 cps. From 502 m to EOH, the hole was dominantly coarse felsic feldspar porphyry cut by occasional mela-gabbro dykes. The drill hole was stopped at a final depth of 583 in barren metamorphosed mafic intrusives. JL08-093 Azimuth: 313° Dip: -62° E: 333102 N: 6065959 EOH: 517 m

JL08-093 was drill from June 8th to 19th, 2008. The top of the hole was mainly metamorphosed polylithic conglomerate with intermittent mafic dykes and coarse felsic feldspar porphyries. The first interval of intermediate metavolcanics was intersected at a depth of 408.85 m. Patchy & weak uranium mineralization was cored between a depth of approximately 420 and 440 m and hosted in intermediate metavolcanics. Highlights are as follows: 421.25 to 421.6 m with an average of 500 cps and maximum of 941 cps;

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435.2 to 435.7 m with an average of 400 cps and maximum of 573 cps; 440.2 to 441.2 m with an average of 390 cps and maximum of 495 cps. The hole ended at a depth of 517 m in barren coarse grained felsic intrusives.


Drill hole JL08-094 was initiated on June 14th, 2008 and completed June 23rd, 2008 at a final depth of 395m. The top of the hole encountered typical Jacques Lake hanging wall sequences of metamorphosed polylithic conglomerate, intermediate fine grained metavolcanics; all of which were cut by porphyritic to non-porphyritic mafic and felsic dykes to a depth of 139.72 m. From a depth of 139.72 to 252.52 m typical Jacques Lake host rock (carbonate +/- biotite +/- hornblende +/- pyrite veined, fine grained intermediate volcanics) was intersected. Uranium mineralization within the intermediate volcanics occured in several zones as follows: from 222.10 to 226.15 m with an average of 1825 cps and a high of 4000 cps; from 234.5 to 238.25 m with a high of 3250 cps and an average of 1118 cps; and from 242.13 to 242.87 m with a high of 280 cps and an average of 270 cps. JL08-095 Azimuth: 319° Dip: -68° E: 332765 N: 6065848 EOH: 492 m

JL08-095 was drilled between June 18th and June 28th, 2008. The drill hole intersected typical hanging wall lithologies of variably strained intermediate volcanics and polylithic metaconglomerate cut by pre to post kinematic mafic dykes up to a depth of 311.5 m. The contact between the overlying metaconglomerate and underlying intermediate metavolcanic rocks is defined by a pre kinematic mafic dyke. Intervals of weak uranium mineralization were intersected from a depth of 367.38 to 368.52 m with scint readings up to 510 cps in hand, and from 372.69 to 375.00 m with a maximum of 397cps in hand. The footwall mineralized zone occurred from a depth of 452.0 to 452.4 m with a spot high of 609 cps in hand. All mineralization was hosted in typical fine grained carbonate +/- biotite +/- hornblende +/- pyrite veined, intermediate metavolcanics. The drill hole was stopped at a depth of 492m in barren, fine grained intermediate volcanics. JL08-096 Azimuth: 318° Dip: -72° E: 333102 N: 6065959 EOH: 634 m

JL08-096 started on June 19th, 2008 and was terminated on July 3rd, 2008. The drill cored a sequence dominated by polylithic metaconglomerate, porphyritic mafic intrusives and metamorphosed felsic to intermediate volcanics up to a depth of 551.48 m. Typical Jacques Lake host rock (carbonate +/- biotite +/- hornblende +/- pyrite veined intermediate metavolcanics) was intersected from a depth of approximately 551.48 to 621.8 m. Many thin, moderately mineralized zones within the intermediate volcanics occurred at the following depths: 571.94 to 573.2 m with a high of 1110 cps and an average of 390 cps; 578.78 to 579.12 m with a high of 860 cps and an average of 374 cps; 593.58 to 594.06 m with a high of 410 cps and an average of 280 cps; 595.92 to 601 m with a high of 710 cps and an average of 258 cps; 602.10 to 603.25 m with a high

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of 620 cps and an average of 248 cps, and 605.50 to 606.02 m with a high of 430 cps and an average of 310 cps. No other anomalous uranium mineralization was intersected and the drill hole was stopped at a final depth of 634 m in barren, fine grained intermediate volcanics. JL08-097 Azimuth: 310° Dip:-48.5° E: 332998 N: 6066069 EOH: 353 m

JL08-097 was collared on June 24th, 2008 and completed July 3rd, 2008 at a depth of 353m. The hanging wall portion of the hole was dominated by polylithic metaconglomerate cut by several generations of mafic dyke up to a depth of approximately 84 m. Intermediate metavolcanics, hosting a 90 m thick interval of patchy uranium mineralization, were intersected at 113.60 m. Highlights from the mineralized zone are as follows: 197 to 219 m averaging 570 cps with a maximum of 3000 cps in hand; 220 to 243 m averaging 410 cps, with a maximum of 2400 cps in hand; and 280 to 304 m averaging 320 cps with a maximum of 1700 cps. The drill hole was stopped in barren fine grained intermediate volcanic. JL08-098 Azimuth: 313° Dip: -49° E: 332765 N: 6065848 EOH: 439 m

Drill hole JL08-098 was drilled between June 29th and July 8th, 2008 to a final depth of 439 m. The drill intersected a thick sequence of fine grained intermediate metavolcanics with lesser variably strained polylithic metaconglomerate and fine grained porphyritic felsic and mafic intrusives. A thin mineralized lens was first intersected in the intermediate metavolcanics from a depth of 77 to 78.73 m with a peak value of 603 cps and an average of 295 cps. Uranium mineralization also occurred intermittently from 299.84 through to 402.90 m depth with spot highs up to 2100 cps in hand. A second mineralized zone (footwall) was encountered from 420m to 466.14 m with an average of 600 cps and a maximum of 3700 cps. JL08-099 Azimuth: 310° Dip: -63° E: 332998 N: 6066069 EOH: 367 m

JL08-099 was started on July 3rd, 2008 and completed on July 14th, 2008 at a final depth of 367 m. Hanging wall sequences of polylithic metaconglomerate, plagioclase porphyritic intermediate volcanics, porphyritic felsic metavolcanics, and altered mafic dykes were intersected to a depth of 226.55 m. Uranium mineralization was intersected in several zones and hosted in typical carbonate +/- biotite +/- hornblende +/- pyrite veined intermediate volcanics. Highlights from the mineralized zones are as follows: 230 to 237 m depth averaging 1600 cps with a maximum of 5000 cps in hand; 268 to 276 m averaging 800 cps with a max of 7044 cps; and 321 to 324 m averaging 996 cps with a maximum of 1453 cps. Patchy uranium mineralization was also present from 324 to 354.53 m with several spots reaching up to 1000 cps. The drill hole ended in barren intermediate metavolcanics.

19

JL08-100 Azimuth: 315°Dip: -45° E: 332945 N: 6066325 EOH: 219 m

JL08-100 was started on July 7th, 2008 and completed on July 11th, 2008. The drill cored a 38.9 m thick hanging wall sequence of fine grained, chloritic intermediate volcanics along with a dark green, fine grained post kinematic mafic dyke. Moderate, patchy uranium mineralization, hosted in typical Jacques Lake carbonate +/- biotite +/- hornblende +/- pyrite veined intermediate volcanics, was first intercepted from a depth of 46.35 to 62.12 m averaging approximately 300 cps with spot highs of up to 2000 cps in hand. Several other mineralized zones were intercepted with highlights as follows: 105 to 121 m depth with an average scint value of 287 cps and a maximum of 3159 cps in hand; and 189 to 193 m depth averaging 808 cps with a maximum of 2681 cps. The drill hole was shut down at a final depth of 219 m in barren, medium grained feldspar porphyritic granitoid. JLM08-001 Azimuth: 0° Dip: -90° E: 333026 N: 6066400 EOH: 142 m

JLM08-001 was a metallurgical and geotechnical hole collared on July 21st, 2008 with an orientation 360˚/-90 targeting the length of the main ore zone. It was completed on July 23rd, 2008 at a final depth of 142 m. The drill then intersected the main Jacques Lake mineralized zone of carbonate +/- biotite +/- hornblende +/- pyrite veined, maroon coloured, fine grained intermediate metavolcanics cut by multiple thin, syn to post kinematic mafic dykes. Strong uranium mineralization was intercepted from a depth of: 47.93 to 73.01 m with an average of 587 cps and a maximum of 3373 cps; 83.15 to 89.50 m with an average of 400 cps and a maximum of 1500 cps; and 91.75 to 96.47 m with an average of 330 cps and a maximum of 1630 cps. A final mineralized zone was intersected from 110.50 to 131.50 m with an average of 724 cps and a maximum of 5000 cps. The drill hole was stopped in a barren post kinematic mafic dyke. JLM08-002 Azimuth: 0° Dip: -80° E: 333026 N: 6066400 EOH:132.5 m

JLM08-002, the second metallurgical drill hole, was collared on July 28th, 2008 with orientation of 360˚/-80˚ targeting the length of the main ore body. It was completed on August 3rd, 2008 at a final depth of 132.5 m. The first 19.2 m of the drill hole consisted of fine grained intermediate metavolcanics cut by a syn kinematic mafic dyke. Mineralization, which was first intercepted at a depth of 29 m and continued to 55 m, was hosted in typical carbonate +/- biotite +/- hornblende +/- pyrite veined intermediate metavolcanics. Throughout this interval the average scint reading was approximately 691.51 cps with a maximum of 6383 cps including highs of 1382, 3064, 2646, 483, 2163 and 1126 cps in hand. A second mineralization zone was encountered (again in intermediate metavolcanics) from 74 to 109 m depth with an average of 416.14 cps, a maximum of 3559 cps including highs of 1207, 1155, 1858, 1218, 2079cps in hand. The hole was stopped in a barren syn kinematic mafic dyke.

20

2.1.3 Discussion of Drill Hole Results Introduction

The 2008 summer drill program was successful in terms of infilling “inferred & indicated” areas with drill pierce-points that convert segments of the deposit to a status of “measured and indicated.” The 2008 drill program also reinforced the idea of the fold interference causing thickening of the mineralized zone. Intervals of uranium mineralization intersected to date continue to be of comparable width and grade to those cut in 2006, 2007, and the winter of 2008.

Highlights from the 2008 summer drilling program include:

- 0.05% U3O8 over 19.00 m including 0.09% U3O8 over 6.00 metres in JL08-088


- 0.22% U3O8 over 7.00 metres in JL08-094


- 0.28% U3O8 over 7.00 metres and 0.14% U3O8 over 8.00 metres in JL08-099

- 0.11% U3O8 over 4.00 metres and 0.05% U3O8 over 12.5 metres in JL08-100

Work in 2009 should continue adding additional infill holes in order to upgrade resource to indicated & measured for the pre-feasibility & feasibility studies.

A summary of assay composites from 2008 drilling is listed in Table 2.2, with a deposit long section shown in Figure 2.2, and a representative cross-section shown in Figure 2.3. Further details on drill holes of the Jacques Lake Property can be found in Appendix IV: Drill Sections; Appendix V: Drill Data including a) drill logs and b) geochemical sampling summaries and; Appendix VI: Assay Certificates.

All Aurora Jacques Lake drill core, both past and present (from JL05-001 to

JL08-100), and including the ½ and ¼ split sampled core, has been relocated from its respective locations to a central core storage area uphill from the old Jacques Lake Core Shack. The coordinates for the new core storage area are UTM 333550 mE, 6066350 mN; NAD83, zone 21.

21

Table 2.2: Summary of Summer 2008 Jacques Lake Assay Composites

Hole ID From (m) To (m) Length % U3O8

cut off grade 0.03% U3O8

JL08-085 361.45 362.45 1.00 0.05

JL08-086 No results – aborted drill hole

JL08-088 314.00 333.00 19.00 0.05 incl. 314.00 319.00 5.00 0.06

and incl. 327.00 333.00 6.00 0.09

JL08-089 388.00 390.00 2.00 0.07

and 313.00 318.00 5.00 0.07

and 353.00 357.00 4.00 0.08

and 447.00 455.00 8.00 0.07

JL08-090 360.00 382.00 22.00 0.06 incl. 360.00 361.87 1.87 0.08

and incl. 365.00 370.00 5.00 0.09

and incl. 378.00 382.00 4.00 0.12

JL08-091 293.00 295.00 2.00 0.05

and 298.00 302.00 4.00 0.09

JL08-092 476.00 478.00 2.00 0.06

JL08-093 435.00 436.00 1.00 0.04

and 440.20 441.25 1.05 0.05

JL08-094 222.00 229.00 7.00 0.22 and 234.50 238.00 3.50 0.19

and 271.90 274.00 2.10 0.07

and 356.69 359.69 2.70 0.03

JL08-095 372.48 373.48 1.00 0.04

JL08-096 597.51 598.51 1.00 0.06

JL08-097 201.96 237.29 35.33 0.07 incl. 207.04 219.60 12.56 0.14

and incl. 234.28 237.29 3.01 0.13

and 281.44 298 16.56 0.05

JL08-098 342.00 343.00 1.00 0.11

JL08-099 230.00 237.00 7.00 0.28 and 240.00 245.00 5.00 0.05

and 268.00 276.00 8.00 0.14

JL08-100 41.00 61.50 12.50 0.05 incl. 41.00 41.75 0.75 0.11

and incl. 60.50 61.50 1.00 0.11

and 104.00 106.00 2.00 0.17

and 116.00 119.00 3.00 0.04

and 189.00 193.00 4.00 0.11

JLM08-001 No results – metallurgical drill hole

JLM08-002 No results – metallurgical drill hole

22

Figure 2.2: Jacques Lake Long Section Showing 2008 DDH

Generated September 25th, 2008

23

Figure 2.3: Jacques Lake Representative Drill Section L1000mE

24

2.2 Specific Gravity Sampling A specific gravity (SG) sample program was carried out from June through September, 2008. 460 SG samples were taken from 2006 & 2007 drill holes, including JL06-010 through to JL07-072, on the Jacques Lake Deposit. Specific gravity samples were collected from most major units greater than 5m in length, with the noted exception of split mineralized core. For extensive units, samples were taken approximately every 25 metres. Samples ranged from 10 to 20 cm in size. Samples were weighed dry and then wet. Data was directly entered into an Excel spreadsheet where the specific gravity calculations were done. All samples were baked in an oven for 12 to 14 hours at 60°C prior to any measurements being taken.

3.0 Sampling Protocols All samples were collected according to the safety methods established by the

company. UTM coordinates were recorded in NAD83, zone 21 using a Trimble DGPS. Sample descriptions and UTM coordinates (or depth interval in the case of core) were entered into the appropriate Excel file. Assays were added upon receipt and QAQC was completed on standard, blank and duplicate samples.

3.1 Core Samples Drill core sampling was done based on visual indications of mineralization and

radioactivity readings from the scintillometer. Sampling intervals were predominantly in the 1.0 m range; although in areas of homogenous lithology, samples were collected in 1.5 m intervals. In addition, narrow zones of mineralization were broken out to a minimum width of 0.1 m.

Samples were split using a manual core splitter; with one-half of the core sent to the

lab and the remaining half returned to the core box for reference. Samples were placed in a polyvinyl sample bag with a reference sample tag and then sealed with a plastic zip tie. Every twenty-five samples a duplicate of one-quarter of the sample interval, as well as a geochemical blank and a geochemical standard, were inserted into the sequence at pre-designated locations in the sample series. Prior to shipping, the bagged samples were individually scanned with Exploranium GR-110 G Portable Gamma Ray scintillometer for data correlation purposes.

The samples were analysed for delayed neutron counting (DNC) and a multi

element suite of 32 elements (ICP/OES aqua regia extraction). For more details of analytical procedures see Appendix III.

3.2 Shipping Protocol

As per regulations for the Transportation of Dangerous Goods Act, all containers were labelled “UN2910” on the outside, with signage indicating “Excepted Package: Radioactive Material” placed within each container. The individual containers were then scanned with a S.E. International Inc. “Inspector” contamination meter to ensure

25

compliance with the maximum allowable limit of 5 µSv/hr measured at a distance of one meter from the package.

Samples were shipped in lidded pails and sealed with numbered security zip ties.

The first and last sample numbers were written on the pail. Analytical request forms from Activation Laboratories Ltd. (“ActLabs”) were

completed, copied, and placed in the designated container. Pails were then sealed with numbered security “zip-tie” tags, which were previously recorded on the laboratory forms. Chain of custody forms were signed in Postville and forwarded to the lab for verification upon receipt of intact sample shipments. Containers were shipped from Postville to ActLabs’ sample prep facility in Goose Bay, who arranged shipment to the laboratory in Ancaster, Ontario.

3.3 Diamond Drilling Drilling was done by Major Drilling Group International Inc. of Suite 100, 111

St. George Street, Moncton, NB E1C 1T7 , Springdale Forest Resources of PO Box 387, Springdale, NL A0J 1T0 and Dorado Drilling of 1236 Mabel Lake Rd., Box 1344, Vernon, BC V1T 6N6 to the standards set by “Saskatchewan Guidelines for Uranium Exploration”. A Polydrill system and a connected series of plastic tubs were employed during the course of drilling to contain drill cuttings and to prevent cloudy drill water from entering nearby watercourses. Drill cuttings from the radioactive zones were collected and buried on site. All drill holes were cemented after completion to prevent any artesian water flow from exiting onto the surface after the program was finished.

26

2008 Assessment Report on the Geochemical and Diamond Drilling Investigations on the

Jacques Lake Property of the CMB Project, Labrador, Canada

APPENDIX I

CERTIFICATE OF AUTHOR


sash

Typewritten Text

sash

Typewritten Text

27

28


APPENDIX II

EXPENDITURE SUMMARY


29

Jacques Lake 010051M Expenditures3rd Party environmental monitoring $36,618.01 Accommodation $5,451.58 Bulk fuel $113,632.95 Contract Salaries $12,117.68 Crew Care Food $121,501.12 Drilling - Diamond $1,683,716.71 Drafting Digitizing Plotting Printing $2,208.66 Equipment Rental $69,054.93 Field Materials & Supplies $61,112.88 Fixed wing charter $71,142.99 Freight courier and postage $7,922.27 Geochemical analysis $43,786.32 Geological Services $2,858.65 Helicopter charter $832,436.68 Postville Fuel Farm $45,626.43 Telecommunications/Utilities $23,865.06 Travel expenses food & lodging $8,775.64 Travel expenses transportation $83,821.48 Wages and benefits $666,316.58 Sub Total $3,891,966.62 Overhead (15%) $583,794.99 Totals $4,475,761.61

30



APPENDIX III

ANALYTICAL METHODS


31

Actlabs Analytical Methods – Rock Sample Preparation (RX-1) Rock Sample Preparation Procedure (www.actlabs.com)

To obtain meaningful analytical results, it is imperative that sample collection and preparation be done properly. ACTLABS can advise on sampling protocol for your field program if requested. Once the samples arrive in the laboratory, ACTLABS will ensure that they are prepared properly. As a routine practice with rock and core, the entire sample is crushed to a nominal minus 10 mesh (1.7 mm), mechanically split (riffle) to obtain a representative sample and then pulverized to at least 95% minus 150 mesh (106 microns).

As a routine practice, we will automatically use cleaner sand between each sample at no cost to the customer. Quality of crushing and pulverization is routinely checked as part of our quality assurance program. Randomization of samples in larger orders (>100) provides an excellent means to monitor data for systematic errors. The data is resorted after analysis according to sample number. Please request Code Random (additional $1.25/sample) if you prefer randomization.

Note: Larger sample sizes than listed above can be pulverized at additional cost.

Pulverization Contaminants Added (amount added depends on hardness of material and particle size required)

Mill Type Contaminant Added Mild Steel (best choice) Fe (up to 0.2%) Hardened Steel Fe (up to 0.2%), Cr (up to 200 ppm), trace Ni, Si, Mn and C Ceramic Al (up to 0.2%), Ba, trace REE Tungsten Carbide W (up to 0.1%), Co, C, Ta, Nb and Ti Agate Si (up to 0.3%), Al, Na, Fe, K, Ca, Mg, Pb

Rock, Core and Drill Cuttings Code

Description Price (CDN)

Code RX1 crush up to 75% passing 2 mm, split (250 g) and pulverize

(hardened steel) to 85% passing 75m (< 5 kg) $8.50

Code RX1 Terminator

crush up to 90% passing 2 mm, split (250 g) and pulverize (hardened steel) to 85% passing 75m (< 5 kg)

$9.50

Code RX2 crush, split and pulverize with mild steel (100 g) (best for low contamination)

$9.00

Code RX3 oversize charge per kilogram (if required) $2.00 Code RX4 pulverization only (mild steel) (coarse pulp or crushed rock) $6.50 Code RX5 pulverize ceramic (100 g) $15.50 Code RX6 hand pulverize small samples (agate mortar and pestle) $15.50 Code RX7 crush only (split) $4.50 Code RX8 sample prep only surcharge, no analyses $3.50 Code RX9 compositing (per composite) $2.25 Code RX10 dry drill cuttings in plastic bags $2.00 Code RX11 checking quality of pulps or rejects prepared by other labs and

issuing report $8.25

32

Actlabs Analytical Methods – Uranium Analysis (5D-U) Code 5D – Miscellaneous Elements Requiring Specific Methods (www.actlabs.com) Analysis Method Detection Limit Upper Limit C-Total Infrared 0.01% C-Graphitic Infrared 0.05% C-Organic Infrared 0.05% F ISE 100 ppm 10,000 ppm Li Total Digestion ICP 1 ppm 10,000 ppm Sn Fusion ICP 1 ppm 10,000 ppm U DNC 0.1 ppm 10,000 ppm B-Total PGNAA 0.5 ppm 10,000 ppm B-Total PGNAA 2 ppm 10,000 ppm Tl Total Digestion ICP-MS 0.2 ppm 10,000 ppm

Code 5D – C (Organic)

0.5 g of sample is titrated with 25% HCl to drive off the CO2 (inorganic C). The sample is neutralized with ammonium hydroxide and dried on a hot plate. Sample residue is analyzed by LECO Combustion-IR technique to provide a value for total carbon, which is composed of organic C and graphitic C. The graphitic C content is subtracted to provide the organic C content.

Code 5D – C (Graphitic)

0.5 g of sample is ignited at 1,000°C to drive off organic and inorganic carbon (CO2). The residue is analyzed by LECO Combustion-IR t o provide a graphitic carbon value.

Code 5D - F

0.5 g samples are fused with sodium hydroxide in an oven at 580°C for 1 hour to release the fluoride ions from the sample matrix. The fuseate is dissolved in sulphuric acid with ammonium citrate buffer. The fluoride-ion electrode is immersed in this solution to measure the fluoride-ion activity directly.

Code 5D - B

1 g samples are encapsulated in a polyethylene vial and placed in a thermalized beam of neutrons produced from a nuclear reactor. Samples are measured for the doppler broadened prompt gamma ray at 478 KeV using a high purity GE detector. Samples are compared to certified reference materials used to calibrate the system.

33

Actlabs Analytical Methods – Multi-element analysis (1E3) Code 1E1/1E3** – Aqua Regia - ICP-OES (www.actlabs.com)

0.5 g of sample is digested with aqua regia (0.5 ml H2O, 0.6 ml concentrated HNO3 and 1.8 ml concentrated HCl) for 2 hours at 95°C. Sample is cooled then diluted to 10 ml with deionized water and homogenized. The samples are then analyzed using a Perkin Elmer OPTIMA 3000 Radial ICP for the 30 element suite. A matrix standard and blank are run every 13 samples. For vegetation a 0.25 g sample is used.

A series of USGS-geochemical standards are used as controls. This digestion is near total for base metals however will only be partial for silicates and oxides.

Code 1E1 Elements and Detection Limits (ppm) Element Detection Limit Upper Limit Ag* 0.2 100 Al* 0.01% As* 10 Ba* 1 Be* 1 Bi 10 Ca* 0.01% Cd 0.5 2,000 Co* 1 Cr* 2 Cu 1 10,000 Fe* 0.01% K* 0.01% Mg* 0.01% Mn* 2 10,000 Mo* 2 10,000 Na* 0.01% Ni* 1 10,000 P* 0.001% Pb* 2 5,000 S* 100 Sb* 10 Sc* 1 Sn* 10 Ti* 0.01% V* 1 W* 10 Y* 1 Zn* 1 10,000 Zr* 1

Notes:

* Element may only be partially extracted. ** 1E3 includes B, Ga, Hg, La, Sb, Sr, Tl and U but includes Sn, Y, and Zr. *** Assays are recommended for values which exceed the upper limits.

34



APPENDIX IV

DRILL SECTIONS


Document Page 34

JL06

-042

JL06

-042

JL06

-046

JL06

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JL07

-076

JL07

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JL08

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JL08

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JL08

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Viewport1

JL06

-042

JL08

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JL06-046

JL07-076

JL08-095

500.

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600.

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700.

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Viewport3

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LITH_SRS: Jacques Lake Lithologies

Viewport5

Aurora Energy ResourcesJaques Lake

Vertical section 625 NE.Scale 1:2500

Projection: Non Earthe Meters Date: 01/07/2009 Document Page 35

JL06

-039

JL06

-039

JL06

-041

JL06

-041

JL06

-046

JL06

-046

JL07

-074

JL07

-074

JL07

-076

JL07

-076

JL08

-095

JL08

-095

600.

00 m

700.

00 m

800.

00 m

900.

00 m

1000

.00

m

-300.00 m

-200.00 m

-100.00 m

0.00 m

100.00 m

200.00 m

300.00 m

400.00 m

JL08-095

JL07-076

JL06

-039

JL06-041

JL06-046

JL07-074

600.

00 m

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800.

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900.

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1000

.00

m

-400.00 m

-300.00 m

-200.00 m

-100.00 m

0.00 m

100.00 m

200.00 m

Jaques LakeVertical section 675 NE.

Scale 1:2500

Aurora Energy Resources

Projection: Non Earth Meters Date: 01/07/2009

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Document Page 36

JL07

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JL07

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JL07

-065

JL07

-065

JL07

-067

JL07

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JL07

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JL07

-072

JL07

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JL07

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JL07

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JL07

-077

JL07

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JL07

-078

JL07

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JL07

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JL08

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JL08

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JL08

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JL08

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JL08

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JL08

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Viewport1

JL07-072

JL07-065

JL08-085

JL07-067JL

08-0

89

JL07-0

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JL07

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JL08-092

JL07

-077

JL07-079

JL07-078

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Viewport2



Projection: Non Earthe Meters Date: 01/07/2009

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Document Page 37

JL06

-022

JL06

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AJL

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JL06

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JL06

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JL06

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JL06

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JL06

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JL06

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JL07

-059

JL07

-059

JL0 7

-060

JL07

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JL07

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JL07

-061

JL07

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JL07

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JL07

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JL07

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JL07

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JL07

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JL07

-077

JL07

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JL07

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JL07

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JL08

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AJL

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81AJL

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84

JL08

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JL08

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JL07

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JL06-035

JL07

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JL08

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JL06-032

JL06-034

JL06

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JL07

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JL07-070

JL08

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JL07-062

JL07-061

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JL07-078

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Document Page 38

JL06

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JL06

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JL06

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JL07

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JL07

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AJL

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JL07

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JL07

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LITH_SRS: Jacques Lake LithologiesFI.dk

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Document Page 39

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Document Page 40

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Document Page 41

42



APPENDIX V

DRILL DATA


Document Page 42

Hole ID From (m) To (m) Lithology Code DescriptionJL08-085 0 4.28 OVBD Overburden and casingJL08-085 4.28 13.72 MI.dk.pk Hornblende-phyric mafic dyke, very broken, blocky. Slightly magnetic throughout. Minor to locally

moderate pervasive chlorite alteration. Abundant hornblende phenos throughout to ~3 mm size. ~1.5m of core missing. Majority of core is rubble. Some flowing pyroxene. Very biotite rich. Small interval of cooked mudstone from 8.93 to 7.52. As depth increases, intrusive mudstone abundance increases dramatically, with feldspar phenos appearing as well. Chlorite abundance increases as well. Biotite/hornblende matrix decreases.

JL08-085 13.72 16.16 MT-CO.plMetamorphic intermediate conglomerate. Subangular maroon intermediate volcanics, quartz, fleshy felsic volcanics, multicolored mudstone and blebby albite and actinolite. Patchy sections are relatively clast free and are made up of fine to medium grained dirty yellow-brown to green material. Green clasts have clay texture. Veining is intense throughout the unit, typically as dark green chlorite, buff carbonate, pistachio epidote and dull green actinolite. Weak hematite alteration, fleshy feldspar alt as rims along veinlets. Weak to absent magnetism.

JL08-085 16.16 20.83 MI.dk 6 feet of core missing. Typical Mafic dyke with biotite and hornblende rich matrix. Some feldspar phenos, calcite veins, pyrite veins. Weakly magnetic

JL08-085 20.83 34.86 MT-IVPink to grey, fine grained, moderately strained felsic volcanic. Streaky mafic minerals (hornblende +/- biotite) throughout. Slickenslides visible. Occasional green epidote, buff carbonate and smokey quartz veins cutting across foliation. Hematite alteration is patchy and weak. Kspar and hematite alteration become progressively stronger with depth as does epidote veining which is quite pervasive.

JL08-085 34.86 37.76 MT-CO.pl Mafic dyke with prominent mudstone inclusionJL08-085 37.76 39.46 MT-IV Return to felsic metamorphosed volcanic. Red k feldspar with some quartz veining. Alteration

between mafic minerals and red feldspathics.JL08-085 39.46 45.28 MT-CO.pl Mafic dyke with large clasts of pale mudstone. Also present are large chlorite and feldspar "blobs".

Typical calcite veins seen throughout. Weakly hematized, little to no magnetismJL08-085 45.28 47.49 MT-CO.pl Moderately strained metamorphic porphyritic felsic volcanic. Chlorite veinlets visible throughout.

Moderately hematized with little alteration. Moderately magnetic. Feldspar prominent throughout, with small amounts of quartz. Overall colour is dark red/grey. Appears highly mafic. Low hematite intensity

JL08-085 47.49 49.06 MT-IV Salmon coloured feldspar with blebby chlorite. Some mudstone visible as well. Slightly strained. Weakly magnetic, though increasingly hematized with depth. Wavy alteration between feldspar and chlorite towards end of section. Borders at a 30 degrees to core axis.

JL08-085 49.06 52.32 MT-IV Metamorphosed intermediate volcanic, high levels of feldspar. Weakly hematized, with prominent alteration between feldspar and mafics. Appears to be moderately strained. Some chlorite veinlets and smokey quartz also present. Some chlorite still present. Alteration appears in "flow" form. Moderately magnetic. Occasional carbonate veinlets.

Page 1Document Page 43

Hole ID From (m) To (m) Lithology Code DescriptionJL08-085 52.32 64.02 MI.dk.por Mafic dyke, fine grained towards margins, with coarsening towards centre of unit. Prominent feldspar

and quartz phenos up to 1.5 cm found in centre of unit. No deformation. Epidote and carbonate veinlets are common. Weakly magnetic.

JL08-085 64.02 68.29 MT-IV Return to dark grey and maroon alternating felsic volcanics. Much darker this times, though still prominent alteration. Increase in carbonate veinlets. Smokey quartz still present. Small amounts of biotite visible as well. Borders at 30 degrees to core axis on top and 35 on bottom. Moderately magnetic. Strong hematite presence.

JL08-085 68.29 69.33 MT-CO.pl Small metamorphosed conglomerate prominent chlorite. Undeformed. Some mudstone present as well. Non magnetic. Feldspar phenos present.

JL08-085 69.33 81.46 MT-IV.por.fp Return to previously mentioned metamorphosed felsic volcanic. Period of predominantly mafic sections seen from 76.34 to 77.24, however meta-felsic presence still visible.

JL08-085 81.46 82.02 MI.dk Small mafic dyke. Some carbonate veins with typical chloritic presence. Non magneticJL08-085 82.02 83.61 MT-IV.por.fp

Metamorphic Intermediate volcanic. Begins with prominent mafics, though feldspar presence increases with depth. Moderately altered. Weakly magnetic. Grey to maroon fine grained feldspar porphyritic intermediate intrusive. Fine mm scale phenos of fleshy feldspar and smokey quartz.. Pink to buff carbonate veins, epidote, green chlorite and dirty yellow sericite common.Fabric is oriented 15 degrees to the core axis. Actinolite as blebby clots. Appears highly siliceous.

JL08-085 83.61 89.19 MT-CO.plTypical metaconglomerate. Moderately strained. Shows typical quartz vines, carbonate scour and fill structures. Moderately magnetic. Mineralogy mainly consists of epidote and k-feldspar.

JL08-085 89.19 90.79 MI.dk.pk Dark green-grey medium grained porphyritic mafic dyke. Common vein/fabric orientation of 40-45 degrees to the core axis. Chlorite alteration is pervasive throughout and occurs as blebs and veinlets. Dull green actinolite and epidote veinlets. Typical flowing pyroxene. Upper and lower contacts 15 degrees to core axis.

JL08-085 90.79 93.28 MT-CO.plHighly strained grey to salmon red metaconglomerate. Clasts have been stretched almost beyond recognition. Prominent feldspar phenos are visible throughout unit, along with some quartz phenocrysts. Unit is grey-maroon in colour and is largely matrix supported coarse grained material with few subangular mudstone, fleshy felsic volcanic and fine grained maroon intermediate volcanic clasts, though extremely stretched. Veining is typically rosy carbonate with lesser dark green to black chlorite, hornblende +/- biotite and dull green actinolite. Weakly magnetic.

JL08-085 93.28 97.53 MT-IV Very mylonitized metaconglomerate with lenses and clasts of felsic to intermediate volcanics. Hematite is trace throughout. Highly altered in areas. Medium to fine grained pink-grey variably altered metamorphosed felsic/intermediate volcanics. Felsic lens seen at 94.97. Patchy hematite alteration. Actinolite as blebs and veins, epidote stringers, quartz+/-carbonate veins viewed, but not common. Hornblende occurs as small black-green blebs and veins as well. Weak fabric developed at approx 40 degrees to the CA


Hole ID From (m) To (m) Lithology Code DescriptionJL08-085 97.53 101.53 MT-CO.pl

Return to grey coloured clast poor metaconglomerate. Usual mudstone seen, along with previously mentioned epidote, chlorite, hornblende and calcitic veins. Weakly hematitic, moderately magnetic. Usual quartz, feldspar phenocrysts. Large feldspar lenses from 100.92 to 101.03, again from 101.18 to 101.34. Very mylonitized metaconglomerate with lenses and clasts of felsic to intermediate volcanics. Hematite is trace to moderate throughout unit.

JL08-085 101.53 103.83 MT-IVReturn to previously mentioned intermediate volcanics. Continues to be very mylonitized with lenses and cla sts of felsic to intermediate volcanics. Hematite is trace to moderate throughout. Highly altered locally, although overall alteration is weak. Medium to fine grained pink-grey variably altered metamorphosed felsic/intermediate volcanics. Actinolite as blebs and veins, epidote stringers, quartz+/-carbonate veins viewed, but not common. Fabric developed at approx 30 degrees to the CA

JL08-085 103.83 107.2 MI.dk Mafic dyke with prominent chlorite veins and phenos. Plagioclase porphyritic mafic dyke. Also felsic phenos viewed throughout. Some pyroxene and calcite veins.

JL08-085 107.2 141.85 MT-IV Return to aforementioned Intermediate volcanic with small mafic dyke at 124.56 and small sections of MT-CO from 130.52 to 130.75, and 138.2 to 138.38. Continues to be clast poor. Weakly hematitic, with small sections of high alteration. Phenos of feldspar and quartz still visible in sections. Periodic "blob" of mudstone and chlorite.

JL08-085 141.85 143.61 MT-CO.plReturn to metaconglomerate, however this time much more clast rich. Heterolithic, subangular clast rich metamorphosed conglomerate. Range of colors, typically brown to green to red. Typical clast assemblage of multicoloured mudstones, quartz, intermediate and felsic volcanics and blebby dull medium green actinolite (?) +/- chlorite. Clast size varies throughout the unit from >3cm fleshy felsics to locally sections where size is <0.5cm. Veining is typically a combination of medium - dark green epidote, chlorite, actinolite and smokey quartz with trace buff carbonate. Weak fabric developed, oriented ~35 degrees to the core axis. Moderately magnetic.

JL08-085 143.61 145.28 FI.por.fp Coarse porphyritic felsic intrusive. Moderate hematite presence. Moderately magnetic. Almost primarily cm feldspar phenos. Matrix abundant with biotite and hornblende. Low alteration. Cross cutting, fracture fill calcite. Bright red, fine grained felsic intrusive -- quartz-feldspar porphyritic. Fleshy tabular to subrounded feldspar phenos <0.5cm in width, finer smokey to dull quartz . Some quartz eyes visible. Weak strain evident in some grains -- elongated. Intensely veined (to net textured) by dull green actinolite. Trace black veins and disseminations of hornblende . Hematite alteration is weak to moderate throughout the unit. Moderately magnetic. Locally bleached to a fleshy pink. . �Near the upper border, he felsic intrusive is also becomes intensely fractured to the point of being an angular clast rich breccia of felsic intrusive and mafic dyke material. Colour varies towards bottom of the unit from fleshy pink to deep red.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-085 145.28 147.15 MT-IV

Return to weakly altered/hematized clast poor, intermediate volcanics as seen 107.2 to 141.85JL08-085 147.15 169.76 MT-CO.pl

Fine grained to locally aphanitic dark red to grey mylonitic intermediate volcanic. Mm scale phenos of quartz, feldspar, mudstone, chlorite milled shape in mylonitic zones. Fabric is approx 30-40 degrees to the core axis though increases to 50-60 with depth. Hematite alteration is weak in upper portion of the unit from moderate to intense in lower sections. Intense blebby dull green to dark green actinolite +/- epidote +/- chlorite throughout the unit up to 2cm in width as rounded clasts. Kspar alteration as fleshy blebs and wispy bands often around actinolite blebs. Veining cuts fabric and is intense locally (vein breccia) typically comprised of vuggy rosy carbonate, epidote, chlorite and actinolite and can range from hairline thickness to several cm. �Borders on mafic dyke parallel to core axis.

JL08-085 169.76 179.83 MI.dk.pk Typical mafic dyke, occasional felsic lens. Dark green-grey medium grained. Chlorite alteration is weak throughout. Chlorite veins common. Dull green actinolite and epidote veinlets. Typical high biotite and hornblende matrix

JL08-085 179.83 234.38 MI.dk.por Mafic dyke, feldspar porphyritic. Biotite rich matrix, typical chlorite. Tabular black hornblende and biotite with needle shaped lathes of white feldspar. Chlorite alteration is pervasive throughout the unit. Non-magnetic. Prominent chill margin visible at lower end. Very slightly hematized. Pyrite also visible.

JL08-085 234.38 285.93 MT-CO.pl Continuation of previously mentioned metaconglomerate. Periodic mafic dykes visible from 235.31 to 235.76, and 251.39 to 259.80. Large felsic lenses visible towards middle of unit. Strain remains weak throughout, until roughly 274 where it increases dramatically. Fabric is oriented roughly 30 degrees to core axis, with highly strained bands of conglomerates.

JL08-085 285.93 295.49 MT-CO.pl Metamorphosed conglomerate as seen prior to dyke. Appears to be moderately strained.JL08-085 295.49 296.71 MI.dk.por Small mafic dyke. Borders at 60 degrees to core axis, fine grained, though coarsens with depth.

Some alteration towards lower contact. Typical chlorite alteration. Non magnetic.JL08-085 296.71 298.49 MT-CO.pl Return to metaconglomerate. Usual mis-mash of mudstone +/- actinolite +/- epidote +/- chlorite.

Slightly strained. Moderately magnetic. Some feldspar visible as well.JL08-085 298.49 334.14 MI.dk Large porphyritic mafic intrusion. Very feldspar rich, with occasional lens. Matrix primarily biotite.

Some flowing pyroxene visible, as well as chlorite alteration, though patchy. Matrix also abundant in hornblende. Non-magnetic. Some carbonate veins also visible.

JL08-085 334.14 343.01 MT-CO.plReturn to typical metaconglomerate. Usual moderate magnetism. Low strained. Low alteration.

JL08-085 343.01 345 FI.por.fp Coarse grained felsic intrusive, predominant quartz eyes. Pinkish red felsic intrusive with fleshy cm scale phenos of feldspar and smokey-blue quartz eyes. Weak fabric resulting in elongation of phenos. Fine grained matrix with disseminated hornblende.

JL08-086 0 3.36 OVBD Overburden


Hole ID From (m) To (m) Lithology Code DescriptionJL08-086 3.36 73.6 MI.dk.por Metamorphosed porphyritic mafic intrusion. This unit is a dark-brown apossed dark green unit (brown

spots/ dark green matrix). Composed of 40 to 75% phenocrysts of hbl and biotite books. Hbl crystals are distinguished by their hardness, black colour and more glassy luster. Biotite is very soft, and brown and appears to be replacing the hbl and whatever other mafic phenocrysts that may have been present. Hbl crystals tend to be larger, but partially replaced. There are clear examples of biotite pseudomorphs of biotite in this rock. The phenocrysts are generally >1mm and <10mm and euhedral to anhedral. They are often rimed by a whitish/greyish mineral (poss sericite). The unit is moderately magnetic. Green colour is from strong chl and act altn. In many places the broken core can take on a waxy luster and is very soft, especially around 58 m depth (poss some serpentine and talc present?). Locally, there is a weak foliation imprinted on the rock as defined by alignment of biotite and hbl in places (bio altn after deformation?). A few silica, hematite veins cut the unit at 30 m depth (75 to 90 degrees to c/a).

JL08-086 73.6 83.5 MT-IV Fine Grained intermediate dyke (THIS IS AN INTERMEDIATE DYKE) - Unit is composed of equigranular feldspar (50-30%) and mafic material (can't tell what the mineral is). Unit is dark green to dark brown from alteration of chl and/or biotite. The upper contact is sharp and is about 45 degrees to c/a. Lower contact is difficult to pinpoint. Unit is cut by minor carbonate and the odd qtz/hem veins. Carb veins tend to be oriented roughly 40 degrees to c/a.

JL08-086 83.5 101 MI.dk.por Metamorphosed porphyritic mafic intrusion. Same as the above. Unit includes a few minor shear zones a few cm to 20 cm thick. The lower contact is approximate and defines the start of a large shear zone, though the rock type is the same. The minor shears are about 30 to 50 degrees to c/a. Alteration and veining are the same as the unit above.

JL08-086 101 126.2 MI.dk.por Sheared Metamorphosed porphyritic mafic intrusion. Same unit a as the above but sheared. All crystals milled to some degree in the shear zone and the unit here displays a strong foliation. The foliation is mostly 40 to 50 degrees to c/a though there are some exceptions. There is a soft white mineral which forms spots in the more sheared areas. Appears to be sericite. Minot veining similar to above.

JL08-086 126.2 127.5 MI.dk.pskFine Grained intermediate dyke (THIS IS AN INTERMEDIATE DYKE) - Unit same as the f.g. dyke just above. Unit has two sharp contacts, the upper at 40 degrees to c/a and the lower is at 25 degrees to c/a. The unit is moderately magnetic and displays some hem staining. Unit is cut by green/carbonate filled fractures and white silica filled fractures. The green fractures tend to be oriented mostly about 60 degrees to c/a and qzt are more broken up and 70 - 80 degrees.

JL08-086 127.5 130.5 MI.dk.por Sheared Metamorphosed porphyritic mafic intrusion. Same unit a as the above but sheared. All crystals milled to some degree in the shear zone and the unit here displays a strong foliation. The foliation is mostly 30 to 40 degrees to c/a though there are some exceptions. There is a soft white mineral which forms spots in the more sheared areas. Appears to be sericite. Minot veining similar to above.



Fine Grained intermediate dyke (THIS IS AN INTERMEDIATE DYKE) - Unit same as the f.g. dyke just above. The upper contact is broken and the lower is sharp but somewhat irregular and clearly intrusive (50-60 degrees to c/a). The unit is moderately magnetic and displays some hem staining. Unit is cut by green/carbonate filled fractures and white silica filled fractures. This dyke contains two ~10cm thick zones that are quite magnetic and one is quite radioactive while the other is more of a broken up vein of hem, qzt mag and moly. This unit, and the other f.g. intermediate volcs above may be feeder dykes to the mineralized int volcs of the area (?).

JL08-086 131.4 134.7 MT-IVMetamprphosed mafic intrusion. Not sure if this is the same unit as above. It is coarse grained and equigranular with about 30-35% plagioclase laths and the rest elongate mafic (mostly hbl) grains. The minerals appear metamorphic and create a amphibolite rocks. Biotite and chl effect the mafic minerals while the plag is epidote and sericite altered. The lower contact is fairly sharp and is about 35 degrees to c/a. Also some strong blebby magnetite.

JL08-086 134.7 159.5 MT-CO.plMetamorphosed and tectonized conglomerate. Unit is multi-coloured, kinda patchy but sheared w elongate patches to mylonitic. There are 0.5 mm to 10 cm or so long elongate clasts of various f.g. volcanic units which are anywhere from pale green to pinkish to dark brown in colour within a f.g. sheared pale green (mostly) matrix which is dark brown in places. The unit has undergone various states of alteration and metamorphism (different clasts are altered/metamorphosed differently. Many are chl/ep/act (green) some are pink (ser/si/hem) etc. The pale green groundmass is soft and appears to be ep + ser and carbonate. The browner is biotite + silica (?) (hard). Up to about 137m the unit is quite mylonitic but is still the conglomerate. Unit is cut my minor late carbonate veins mostly forming at 50 - 55 degrees to c/a.

JL08-086 159.5 161.1 MI.dk.psk Fine Grained dark green metamorphosed mafic dyke. Unit is composed of strongly altered chl + ep + act +/- bio altered material. Very difficult to identify the original mineralogy and texture, but appears to have contained at least some hbl and plag. Both contacts are sharp and are at 45 and 70 degrees to c/a respectively. Unit is weakly magnetic and does not react with HCl. There is not an identifiable foliation.

JL08-086 161.1 166.8 MT-IVFine Grained Brown/green Intermediate Dyke - Unit is almost sand-stone in texture and is composed of 35 - 40 % plag and the rest similar sized mafic material, some of which loks to be hbl, but a bunch could be px. Unit reacts well with HCl (not strongly though). Unit is non-magnetic. Both contacts are fairly sharp, butr the lower is broken and hard to tell for sure what the angle is. The unit is cut by weak carbonate veins, all < 1 mm thick and tend to be oriented at 45 degrees to c/a.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-086 166.8 169.8 MT-CO.pl Medium grained clastic unit which appears to be a finer grained layer within the conglomerate unit. Is

composed of 30 - 40% white-pink-orange spots (0.5 - 1.5 mm) within a fg dark brown groundmass. The unit also contains 1 - 5% clasts of volcanic material (up to 3 cm). The unit is sheared to some extent (~45 degrees to c\a). The unit does not react with HCl other than the weak carbonate veining (~45 degrees but not same orientation as foliation). Unit weakly magnetic. Lower contact ~40 degrees to c/a.

JL08-086 169.8 170.5 MI.dk.psk Fine Grained dark green metamorphosed mafic dyke - Same as unit above. This one less altered and clearly contains 15 - 20% plag, and the rest mafics, some of which is hbl. Unit green due to ser + chl + act + ep altn. Contacts sharp and at 40 degrees to c/a. Unit weakly magnetic and does not react with HCl.

JL08-086 170.5 173.5 MT-CO.pl Metamorphosed conglomerate - exact same unit as the stuff at 134.7 m. Lower contact fairly sharp, but not razor sharp. Unit highly tectonised with foliation at 60 degrees to c/a. Lower contact at ~60 degrees (same as foliation).

JL08-086 173.5 197.15 MT-CO.plSmall sections of moderately sheared traditional "fruit cake" conglomerate as seen above within a dk gy to maroon coloured, silicified, fgr indistinct unit - possibly a low to no clast transition from the conglomate w subtle white alteration spots trgt. (or extrememely fgr dykes with very small white phenos?) Linear features (probably veining) being crosscut and altered by chl w hem selvages. Spidering hairline fractures filled with chl, carb & mnr epidote trgt. Mnr, micro-scale, extensional fracturing filled w carb. Non-mtc. Last meter of unit is conglomerate w moderate carb vts & mnr carb trgt; angualr clasts up to @ 196.14m w small, angular clasts generally less than 3mm but up to 3cm in size. LCT irregular w alteration encrouching on the dyke below.

JL08-086 197.15 199.22 MI.dk Dk gy, fgr mafic dyke with very small spotting trgt (possibly phenocrystic) & a slightly felty texture. Occasional blebs of qtz-carbonate material. Late hairline carb vts trgt. Non-mtc.

JL08-086 199.22 216.35 MT-IVGy, extremely fgr to aphanitic, massive intermediate volcanic; Moderate to abndt carb-chl vnng & stockworking w biotite selvages; Moderate, mico-scale extensional fractures filled w carb & occ clasts of surrounding MT-IV. Bleaching alteration from 200.45-201.4m. Non-mtc. Intruded by multiple small, sublte, very fgr mafic dykes. Mnr epidote & hemative selvages on vnng downhole toward LCT (same alteration found in the conglomerate unit below). LCT irregular.

JL08-086 216.35 222.07 MT-CO.pl Typical multi-coloured, moderately sheared, 'fruit cake' conglomerate; Abndt hem & epidote alteration of matrix w aprx 30% sub-angular to subrndd clasts of MT-IV & qtz generally less than 2cm but ranging up to 5cm in size. Patchy, weak magnetics.

JL08-086 222.07 227 MT-CO.pl Gy, ambiguous unit - probably low to no clast conglomerate sheared out with mnr remenant clasts; Epidote altered nodules with hematite selvages - probably crosscut veins. Thin white bands trgt appearing to be squeezed out clasts. Non-mtc. Late carbonate fracture fill w occasional stockwork of carbonate.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-086 227 233.15 MT-CO.pl Multi-coloured 'fruit cake' conglomerate with intense hem & epidote alteration; also a tan-coloured

alteration trgt - poss albite? Abndt sub-angular to subrndd clasts of qtz, jasper, & volcanics ranging up to 7cm in size. Shearing is variable from weak to moderate trgt. Small micro-fracturing causing mnr displacement w/I clasts. Late hairline carbonate fracture fill & occasional section of intense carb altn (<10cm). LCT @ 45 deg tca.

JL08-086 233.15 243.82 MT-CO.pl.my Pinky-maroon, silicified, hem-dusted unit containing small qtz pieces up to a few mm in size; qtz have small foliation tails. Possibly the mylonitized conglomerate with remnant qtz clasts, or foliated qtz porphyritic unit. Occasional bands of bright orange-pink, hem-dusted albite alteration. Non-mtc. Micro-faulting trgt & hairline carbonate fracture fill.

JL08-086 243.82 247.4 MT-CO.pl Multi-coloured 'fruit cake' conglomerate with predominant epidote & tan-coloured (possibly albite?) alteration trgt the matrix. Clasts are subrndd to sub-angular jasper, volcanics and occasional felsic. Clasts generally less than 3cm but ranging up to 7cm. Foliation genreally weak w a few sections of strongly sheared conglomerate squeezing out the clasts. Patches of weak magnetics. Spidering hairline carb fracture fill & occasional 10cm section of intense carb alteration. LCT wavy @ 70 deg tca. Alteration encrouches aprx 1ft into the lower unit.

JL08-086 247.4 255.65 MT-FV.por Pinky to maroon, hem-dusted, aphanitic qtz-fsp porphyritic felsic metavolanic; Moderately foliated trgt with increased, strong foliation near the UCT. Qtz & fsp tend to be slightly elongate in the plane of foliation & some have tails indicating mnr dextral rotation. Aprx 2% phenos genrally 1-2 mm but up to 5 mm in size. Hematite alteration as phenocryst selvages & along filled, hairline fractures. Occasional chl replacement vns. Contains 2 small chlzd & foliated mafic dykes less than 50 cm in size w one at LCT; LCT fairly gradual.

JL08-086 255.65 266.95 MT-FV.por Typical qtz-fsp porphyritic felsic volcanic w aprx 20% fsp & blue qtz phenos. Pervasive disseminated hematite trgt. Fsp phenos tend to take up mnr hematite alteration. Qtz phenos tend to be smaller ranging up to 5mm in size & fsp phenos range up to 1cm. Mnr qtz vnng & chl vts trgt. Spidering, hairline carb fracture fill trgt. Weakly to moderately mtc trgt. Two small moderiatly foliated & chltzd mafic dykes less than 30 cm in size. LCT gradual & marked by change in alteration. Last meter or so by LCT non-mtc.

JL08-086 266.95 279.4 MT-FV.porQtz-feldspar porphyritic felsic volcanic w strong foliation squeezing out the phenos & leaving only a few small qtz phenos. Weak to moderate epidote, hematite, & tan-coloured albite (?) alteration along foliation. Nodules of epidote-chl slightly stretched along foliation & ranging up to 4 cm in size - possibly crosscut veins (?). Carb filled hairline fractures & healed fractures trgt. Unit becomes very stongly foliated, almost mylonitized, downhole - phenos are almost completely squeezed out; Epidotized vnng still present & slightly more elongate. Mnr dyking trgt - fg chtzd mafic dykes crosscutting foliation - aprx perpendicular tca. Non-mtc. LCT sharp & irregular.



Multi-coloured, weakly foliated, heterolithic conglomerate with variable patchy & occasional clast epidote alteration uphole & sections of pervasive epidote alteration of the matrix trgt. Variable sub-angular to subrndd clasts of japser, qtz, felsic & intermediate volcanics, & mgr intermediate intrusive, ranging from a few mm up to 10 cm in size. Size & distribution of clasts varies trgt possibly representing a fining upward sequence. Aprx 30-40% clasts. Abdnt carb & epidote hairline fracture fill & alteration on jts & fractures. Calcite, siderite (oh my god! The tan-coloured mineral is siderite!), epidote & chl vts trgt. Occasional very small, heavily chloritized, fgr, porphytitic mafic dyke. Becomes weakly magnetic downhole. ��Pervasive hematite alteration of matrix & clasts w spot high mineralization @ LCT. Spot high of 473 cps @ LCT. Mineralized & hematized fluids probably exploiting the conglomerate-dyke contact.

JL08-086 309.7 311.12 MI.dk.psk Fgr intermediate dyke with amphibole & lathy fsp. Relatively unfoliated. Weak patchy mtc. Trace cpy.��UCT has a spot high of 302 cps.

JL08-086 311.12 315.73 MI.dk Pervasively chltzd fgr mafic dyke. Non-mtc. Calcite along jts & fractures. LCT @ 65 deg tca.JL08-086 315.73 317 MT-IV Med gy, very fgr intermediate volcanic. Unfoliated. Moderately mtc trgt. Hairline carbonate fracture

fill. Trace pyrite.��E.O.H. @ 317 m.

JL08-088 0 3.52 OVBD Overburden. Hole started on May 20th.JL08-088 3.52 5.77 MI.dk Dark green/grey, heavily chloritized porphyritic mafic intrusion. No fabric visible. 0.2 to 1.0 cm

euhedral feldpsar phenocrysts (1%) and fine (<2mm) relicts of fps phenos (2%). Minor ct vts stockwork. Contacts are broken up.

JL08-088 5.77 13.87 MT-IV Dark purple/grey, very fine to fine grained metamorphosed intermediate volcanics. Core is extremely broken up (sitting right below ovbd). Non-magnetic, unmineralized. Very weak foliation defined by thin bands of dark material and by set of aligned carbonate veinlets (minor). A few chloritized undifferentiated mafic dykes intrude the units (all in pieces and less than 15 cm). Ct +/-hm alteration throughout. LCT (w/ MT-CO) is irregular but sharp (over 1cm).

JL08-088 13.87 23.44 MT-CO.pl Dark green to pink moderately sheared conglomerate unit. Clasts sizes range from 0.2 to 2cm. Number of clasts decreases downhole. About 10% elongated clast at top of unit. Only rare clasts after 19.50m. Groundmass is similar to MT-IV unit above: dark purple/grey, very fine to fine grained material (could the MT-IV be a clastless MT-CO?). Clasts are polylithic, brown, green, pink… but most clasts are light to dark green with ct +ap +/-ac +/-fps. Med hm alteration throughout unit. Several sets of micro-fractures with approx 1mm bleaching on each side. Non to weakly magnetic wk folation defined by elongated clasts. LCT sharp at 45tca.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-088 23.44 37.96 MT-IV Dark green very fine to fine grained metamorphosed intermediate volcanics. Mod to stgrongly

magnetic. Soft with weak ct alteration. About 15% cb veinlets (stockwork). Weak foliation defined by alignment of fine grained light colored minerals (clays, fps, mt, leucoxene). Sporadic 5-20cm soft, chloritized post kinematic mafic dykes. LCT is gradational, over approx 20 cm: stockwork veining goes down to <1%, mt drop to close to nil, ct alteration goes down and hm alteration goes up (about 2-3%).

JL08-088 37.96 52.05 MT-CO.pl.mypink/red to dark red, aphanitic, strongly altered, mod sheared, metamorphosed conglomerate. Low content of clasts. Non magnetic, hm alteration increases downhole. Mod silicified. Minor elongated chloritized clasts (1-2%). Some rounded fine grained ep+ct-rich ppb (ppb relicts?). Minor cb vts (<1%). Minor veins (<1%) filled with bt, mt +/- ct. Some bleaching occurs around vts.��1 undiff ct altered undiffirentiated MI.dk at 41.37m. Broken up with some gouge (FLT ZONE). Ct obscured by broken core.�2 short, mod ct altered syn to post-kinematic II.dk at 49.83 (37cm) and 50.07m (80cm).

JL08-088 52.05 55.39 Light green, pink and cream colored, very fine grained syn- to post kinematic II.dk (INTERMEDIATE DYKE). Weak fol defined by colored bands with blurry con in between. UPC lost in broken core. LCT with MT-CO sharp at 65tca.

JL08-088 55.39 61.26 MT-CO.pl Similar to unit above II.dk. Strong hm alteration with minor ct altn. Mod sheared. Fol defined by colored bands and minor aligned elongated clasts. LCT obscured by broken core. Minor cb vts (<1%). Groundmass is non-mag. Some mag vts (mt +bt +/-ct).

JL08-088 61.26 65.5 MI.dk.pk Dark green, post-kinematic mafic intrusion. Most of the minerals have been replaced by ct. Remnants of possible fps phorphyroclast replaced by light green clays +ct. No visible fabric. Some <10cm sections are highly broken up with some gouge (FLT zones). Non-mag.

JL08-088 65.5 70.65 MT-CO.pl Conglomerate? To be continued. Waiting for rest of unit before write-up.JL08-088 191.6 203.9 MT-CO.pl Unit is Dark grey/green to lighter grey/green. Grain size changes from a coarse grained (~1.0-5.0cm

and <) conglomerate to a finer grained (~0.5-1.0cm) at ~197.90m and back to the coarser grained conglom at ~201.60m. Contains angular-subrounded clasts containing epidote, quartz, chlorite, and hematite . Mild to medium deformation towards ends of unit with very little deformation in center at finer grained section.

JL08-088 203.9 205.23 MI.dk.psk contains relict hornblende phenocrysts and feldspar. Strongly altered to chlorite. No obvious deformation or fabric.

JL08-088 205.2 227.19 MT-CO.pl conglom like before mylonitized at ~118m to about 220m. Ends with an irregular contact with a mafic dyke at 227.15m. Contains a large (12cm) milky quartz vein at 214.27m.

JL08-088 227.2 229.67 MI.dk.pskdark gray/black unit. Contains epidote veining at 228m. No other evident fabric. No obvious phenos.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-088 229.67 239 MT-CO.pl dark gray-green conglom containing rounded to sub-angular clasts. Clasts are 0.2-3.0cm containing

epidote, quartz, hematite. Weak to moderate magnetism. Sharp contact with upper unit making angle of ~25deg with core axis. Messy lower contact. Contains a small syn-kenematic (or post-kenematic) mafic dyke intrusion (with sharp contacts at 30deg angle to core axis) at 233.70 - 233.96m. Minor-moderate calcite veining.

JL08-088 239 247.66 MT-CO.pl.my purple-dark gray strongly deformed conglom unit. Becomes darker (dark gray-black) near bottom of unit. Strongly magnetic throughout with just a few patches of weak-moderate magnetism. Low content of clasts. Clasts are <1cm with just a few larger clasts (~4cm) near top of unit, where it is more purple. Contains, epidote, chlorite, quartz.

JL08-088 247.66 253.6 MI.dk.psk Dark gray unit exhibiting little foliation/fabric. Makes sharp contact ( ~15 deg to core axis) with above mylonitic conglom.

JL08-088 253.6 255.76 MT-CO.pl.my dark gray strongly deformed mylonitic conglom. Very few visible clasts (elongate). Gradational contact with above mafic dyke.

JL08-088 255.77 258.56 MT-CO.pl.my very broken up rubbley. Red/purple unit grading to a greenish colour some patches are weakly magnetic, however, unit is largely non-magnetic. Highly deformed, no visible clasts. Intruded by a dark gray mafic post kinematic dyke (256.35 - 257.30m)

JL08-088 258.56 259.85 MI.dk.pk Dark gray aphanitic dyke exhibiting deformation in alternating beige bands.JL08-088 259.85 262 MI.dk.pk Red unit. Very rubbley trouble. Exhibits a lot of bandingJL08-088 262 263.7 MI.dk.psk Dark gray aphanitic dyke. No visible fabric. Contains calcite veinsJL08-088 263.7 268.88 MT-IV red and dark gray/black aphanitic meta volcanic unit. Calcite, chlorite and epidote veining. Strongly

magnetic.JL08-088 268.88 270 MI.dk.pk Dark gray/green unit cut by several small dykes: @268.66 - 270m (sharp contacts at both ends

making ~50 deg with core axis). Highly deformed with clacite (and other) veins having a brecciated appearance. Contains phenos ~0.2cm in size.

JL08-088 270 324.13 MT-IVAlternating black-red intermediate volcanic unit. Strongly magnetic. Contains some sulphides. Moderately veined with calcite, chlorite and epidote (higher concentration of epidote veins above 287m) (heavy calcite veining at 309.80 - 310.80m) . Intersected by a dark gray pre-kenematic mafic dyke @ 270.66m - 271-49m containing <0.1cm lathes and many deformed calcite, epidote and other veins. A post-kenematic mafic dyke at 287.09 - 287.30 containing ~0.1cm phenos. Another dyke post-kenematic and mafic at 302.10 - 302.70m with sparce <0.1cm phenos. High scint readings of ~400-500 at 300m and further down hole.

JL08-088 324.13 325.1 MI.dk.psk Dark gray unit exhibiting little veining. Phenos are 0.1 - 0.2cm in size. Very little visible fabric. Sharp upper and lower contacts making an angle of 40 deg to core axis.

JL08-088 325.31 333.3 MT-IV Red and black unit containing magnetite, biotite, chlorite. Veined with carbonate veins. Very magnetic. Scint readings averaging 700 cps. Messy lower contact.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-088 333.3 357.04 MT-MI.fgr

dark gray-black silicious unit. Some patchy magnetism but mostly non to weakly magnetic. Exhibiting foliations, deformed flowy tectures epidote and carbonate veins. Contains quartz, biotite, k-feld.

JL08-088 357.04 358.58 MI.dk.psk Dark gray-black fine grained unit containing ~0.1cm phenos. At ~257.56m contains a 13cm wide intrusion of lower coarse porphoritic unit (stay tunned). Lower portion of dyke contains some porphyroclasts from said unit.

JL08-088 358.88 373.96 FI.por.fpDark gray/black feldspar rich unit. Phenos are ~1.0 - 2.0 cm in size and become significantly less dense towards the bottom of the unit. sharp upper contact making a 50deg angle with core axis. Weakly magnetic. Intruded by a fine grained post kinematic mafic dyke containing no phenos at 362.95-363.06m and another small post kinematic mafic dyke 363.50-363.80 m. contacts of both dykes are sharp, angled away from each other and measure 45deg and 30deg to core axis.

JL08-088 373.96 380.55 MT-CO.plDark gray-black mafic dyke. Fine grained with few phenos, although they occur in a deformed patch at around 278.70m and below 280m. Sharp upper contact measuring 50 deg with core axis. The top part of the dyke contains feldspar phenos from the above porphyritic unit. The unit is moderately-heavily veined with epidote and quatz. Also containing small amounts of carbonate.

JL08-088 380.55 385.84 MT-IVdeformed Dark gray/black to reddish black aphanitic unit. Exhibits moderate beige and greenish banding Moderately to strongly magnetic. Contains epidote, calcite, quartz, and biotite. Syn-kinematic mafic dyke containing biotite and very sparce phenos ~0.1cm located at 282.19 - 282.37m.

JL08-088 385.84 387.04 MI.dk.pskDark green/gray-black unit. Contains biotite and very few feldspar phenos. No fabric or veining is visible. Top (sharp)contact makes a 60 deg angle with core axis. Lower contact is rough.

JL08-088 387.04 396.86 MT-IV Dark Green-Black and red metamophosed exhibiting bands. Very micaceous and moderately to strongly magnetic. Contains; biotite, k-feld, epidote, calcite, quartz,. An annomolous dark green band at 395.84m depth with 0.1- 0.2 cm phenos.

JL08-088 396.86 398.05 MI.dk.sk Dark gray/black syn-kinematic mafic dyke. Containing ~0.1 - 0.2 cm relict phenos and clacite and other veins. Contains biotite. Sharp lower contact at ~25deg to core axis.

JL08-088 398.05 402.08 MT-IVDark gray/black and blackish red metamorphosed unit. Moderately to strongly magnetic. Contains quartz, epidote, chlorite, feldspar. As well as very thin calcite, chlorite and quartz veins. A post-kinematic mafic dyke is located at 399.80 - 400.18m and another 401.33 - 401.73m depth. Dykes have sharp contacts with MT-IV unit and exhibit very little veining or other fabric.

JL08-088 402.08 403.21 MI.dk.sk Dark gray/black syn-kinematic mafic dyke. Contains very few phenos. Moderately veined with calcite, epidote and containing some quartz. Non-magnetic. Sharp upper contact making an angle of ~60 deg with core axis. Lower contact grades into lower unit.



Dark gray/black-reddish black micaceous biotite rich unit. Fairly heavy veining. Veins contain pyrite and chalcopyrite. There are black veins of some mineral containing quite a bit of chalco and pyrite.

JL08-088 408.44 409.8 MI.dk.psk Dark gray-black predominant k-feldspar located at upper and lower contacts. Very little veining. Non-magnetic.

JL08-088 409.8 424.86 MT-IV Dark gray/black to greenish and reddish black micaceous unit (huge amount of biotite). Contains many veins with pyrite, chalcopyrite (~0.5-0.7%),quartz and some phenos of ~0.2cm size. Moderately to highly magnetic.

JL08-088 424.86 447 MI.dk.sk Dark gray/black unit containing biotite, quartz, k-feld. Large quartz and k-feld veins at 435.15 and 435.16m depth. Some

JL08-089 0 4.4 OVBD Not recovered.JL08-089 4.4 5 OVBD Granitic boulderJL08-089 5 13.35 MI.dk.pk In-situ breccia texture with dark grey fine grained clast of mafic dyke(?) surrounded by fractures filled

with carbonate or chlorite. Chlorite rims occur on the fragments that are in a matrix of carbonate. Non-magnetic. Unmineralized

JL08-089 13.35 25.39 MT-IVWhere unaltered this rock appears fine grained grey and massive. Weakly to non-magnetic.�Blebby to sinusoidally banded hem alteration.�The top of this unit has blebby chlorite/hem/kspar alteration, however overall the unit is dominated by red hem staining. (very hard to scratch. The unit becomes an earthy red colour with depth as hematite alteration becomes pervasive and contains closely spaced (~2cm) hairline qtz, carb, kspar, hem vnlts. Several intervals look as though they have been silicified. Both the upper and lower contacts of this unit are defined by intervals of broken core where the actual contact is not preserved. There are several intervals of broken rock within this unit. Unmineralized

JL08-089 25.39 29.49 MT-IV this unit appears the same as the one above but is moderately to strongly magnetic. Upper contact is a broken zone. Lower contact is irregular but sharp (over a few cms) Unmineralized

JL08-089 29.49 37.6 MT-IV MT-IV? Grey with abundant fine hematitic vns at the top of the unit grading down into earthy red intensely stained with banded texture. Bands are often seen in 2-3cm segments that have been fractured and offset. Fine hairline carbonate vns occur and can be spaced ,1cm in some zones. Rare Qtz vns occur typically ,5mm thick. Weakly magnetic. Unmineralized

JL08-089 37.6 45.95 MI.dk Speckled light and dark green. Mafic dyke(?) altered to a chlorite/epidote rich assemblage. Up to 3cm epidote vns occur and are noted to contain trace amounts of malachite and molybdenite. Molybenite is also observed disseminated in the rock. Non-magnetic, unmineralized. Sharp upper and lower contacts.

JL08-089 45.95 48 MI.dk.pk mafic dyke with brittle fractures filled by carbonate (calcite, siderite). In-situ breccia texture. Intensely chloritized. Minor hematite staining.Lower contact sharp and irregular.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-089 48 48.65 MI.dk Fault zone breccia. Matrix of altered rock flour with polylithic clasts (mainly chloritized mafic frags).

Abundant carbonate +/-clay cement. Sharp upper and lower contacts.JL08-089 48.65 53.46 MT-IV

Hematite stained, dark grey aphanitic looking rock. Epidote chlorite hematite +/-kspar blebs give the rock a mottled appearance and alteration textures obliterate primary textures. Hairline carb vns cut the core at variable orientations, spaced a few cms apart and sometimes occur in small swarms. Hematite staining appears to increase towards lower contact. Lower contact is sharp.�Unmineralized�Non-magnetic

JL08-089 53.46 63.88 MI.dk.por Feldspar porphyritic mafic dyke. 10% white lathe shaped ~2mm relict fspar phenos in a dark grey chlorite rich matrix. Minor biotite. No obvious fabric, interpreted as post-kinematic. Hairline to mm scale carb vns occur typically spaced >10cm. Rare qtz veins containing fine (mm scale) euhedral qtz crystals. Lower contact is sharp and characterised by a 15 chill zone where the rock is fine grained and aphanitic. Strongly magnetic. Unmineralized

JL08-089 63.88 65.68 MI.dk Syn-kinematic aphanitic mafic dyke is breciatted with very little clast movement. Fracture fill and breccia matrix is carbonate. Unmineralized.

JL08-089 65.68 71.88 MT-IV Intermediate volcanic is fine grained and moderately hematite altered. Alteration is patchy and banded and gives a psuedo clastic texture. Carbonate is common in the matrix of non-hematite altered patches and on fracture surfaces. Unmineralized.

JL08-089 71.88 73.8 MI.dk.pk Pre-kinematic mafic dyke with brittle fractures(appear perpendicular to contact) filled by carbonate). Fine to medium grained and intensely chloritized. Weak blebby hematite staining. Lower contact sharp and planer 25 degrees TCA. Unmineralized.

JL08-089 73.8 75.67 MT-IV strongly hematized intermediate volcanic. Shearing through this unit is visible, weak carbonate stockwork and moderate carbonate fracture fill.

JL08-089 75.67 77.05 MI.dk.por Porphyritic mafic dyke moderately chloritized. Lower contact 70 degrees TCA. Minor carbonate fracture fill.

JL08-089 77.05 79.41 MT-IV stongly hematite and chlorite altered intermediate volcanic, very broken and rubbly, weak carbonate stockworking and fracture fill

JL08-089 79.41 83.32 MI.dk.sk fine grained mafic dyke, minor <2% feldspar phenocrysts, pervasive chlorite and epidote alteration and veining. 81.5 to 81.9 m intensely breciatted with chlorite epidote matrix. Upper and lower contacts sharp and irregular.

JL08-089 83.32 88.64 MT-IV intermediate volcanic with minor late dykes, moderate hematite and chlorite/epidote alteration. Minor carbonate veining with weak carbonate stockwork. MT-IV texture is sheared.

JL08-089 88.64 92.45 MI.dk.pk Fine grained (almost massive) mafic dyke, sharp contacts, minor carbonate fracture fill. Strongly magnetic.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-089 92.45 150.15 MT-CO.pl.my dominantly mylonitized conglomerate where the mylonitic layers (sheared clasts) are often faint to

indistinct and the rock can have a more massive appearance. Alteration also acts to obscure primary textures. Non-magnetic. Hairline carbonate vnlts occur spaced ~ <10cm.�Upper contact is sharp and oriented at 40tca. Characterized by change in colour, texture, and sharp decline in magnetism. This unit is non-magnetic throughout while the upper unit was strongly magnetic.�Alteration is patchy to banded and typically consists of patches of chlorite+epidote+/-carbonate surrounded by dark red hematite staining. Hematite staining also occurs on it's on as blebs or in bands. In some areas the alteration results in a pseudo-clastic texture.�Lower contact is sharp and oriented at 75tca.�Sections with distinctive clastic (non-mylonitized texture)�120.72 - 121.54 Increased hematite staining�122.05 - 122.86 Three (6,13 and 30cm) intervals of strongly chloritized dyke. Non-magnetic. Contacts sharp and oriented at ~85tca.�

JL08-089 150.15 150.91 MI.dk Strongly chloritized mafic dyke. Fine irregular carbonate vnlts. Some small (3mm) patches of pink iron carbonate (ankerite). Lower contact sharp and oriented at 60tca.

JL08-089 150.91 155.05 MT-FV.por10% ~5mm diameter, rounded quartz eyes with a distinct bluish tinge. Some appear to have a radial texture(?)�15% ~5mm diameter subrounded to elongate (possibly flattened from strain) pink fspar phenos.�Chlorite-rich matrix. Moderately magnetic. Unmineralized.

JL08-089 155.05 158.34 MI.dk.psk Chloritized mafic dyke. UC sharp at 85tca. Lower contact sharp at 55tca. Non magnetic. No obvious fabric.

JL08-089 158.34 164.22 MT-CO.pl.myMylonitized conglomerate with Intense red hematite staining from upper contact to 164.22m. Banded appearance with mm scale bands. Moderately magnetic. Lower contact indistinct but characterized by a sharp decline in magnetism. Alteration often gives this rock a mottled/blebby appearance.�Dykes occur at 161.03 (70cm), 162.08 (14cm), and 162.52 (8cm) with sharp contacts. They are strongly chloritized with no obvious fabric.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-089 164.22 229.68 MT-CO.pl Distinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger

clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.)�Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Some of the clasts are magnetic but overall the conglomerate is non-magnetic.�Most of the unit displays a strong fabric in the form of clast alignment, flattening and bands. This fabric is oriented between 45-85tca.�Appears to be at least two generations of carbonate. Fleshy coloured carb that occurs in bands parallel to foliation or as breccia/conglomerate matrix and later hairline white carbonate veins that typically cut foliation and occur at a low angle to core axis (~20tca).

JL08-089 229.68 231.7 MT-CO.pl.my Mylonitized conglomerate within larger package of clastic weakly deformed conglomerate. Sheared out clasts create bands ~2mm thick of vary colour and mineralogy. Some augens occur. Bands oriented at ~60tca

JL08-089 231.7 257.17 MT-CO.pl Distinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.)�Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Some of the clasts are magnetic but overall the conglomerate is non-magnetic.

JL08-089 257.17 259.52 MI.dk.psk Upper contact sharp with aphanitic chill zone for ~20cm. Becomes coarser grained with depth. Relict hbl phenocrysts now altered to biotite+chlorite occur up to 3mm and comprise ~10% of the rock. Matrix is strongly chloritized. Lower contact sharp but irregular. Magnetic at the top but non-magnetic through the rest.

JL08-089 259.52 264.62 MT-CO.pl Magnetic and polylithic with moderate fabric oriented at ~75tca.JL08-089 264.62 266.67 MI.dk.psk chloritized mafic dyke showing no oriented fabric. Fine mm scale white lathes are interpreted as relict

fspar phenos. Hairline carb vnlts cross-cut the core. Non-magnetic. Unmineralized. Sharp upper and lower contacts.

JL08-089 266.67 269.77 MT-CO.pl Conglomerate - description as per previous. Weakly to moderately magnetic.JL08-089 269.77 270.47 MI.dk

Strongly chloritized with no obvious fabric. Sharp upper and lower contacts oriented at ~60tca.JL08-089 270.47 276.29 MT-CO.pl Distinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger

clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.)�Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Some of the clasts are magnetic but overall the conglomerate is non-magnetic.

JL08-089 276.29 277.95 MI.dk Strongly chloritized mafic dyke


Hole ID From (m) To (m) Lithology Code DescriptionJL08-089 277.95 285.83 MT-CO.pl Distinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger

clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.)�Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Moderately magnetic.

JL08-089 285.83 288.04 MI.dk Dark grey aphanitic rock with mottled appearance resulting from patchy light green chlorite alteration and chloritic veins. Moderately magnetic.

JL08-089 288.04 293.11 MT-CO.plDistinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.) Locally there are areas that appear mylonitized.�Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Some of the clasts are magnetic but overall the conglomerate is non-magnetic.�Patchy hematite alteration.

JL08-089 293.11 299.84 MT-CO.pl.my Mylonitized conglomerate with frequent small (<50cm) thick dykes.�Dykes occur at 296.61 (14cm); 297 (12cm); 297.20 (13cm); 297.43 (10cm); 297.79 (31cm); 298.36 (24cm); 298.80 (17cm)�Red green and white ~2mm thick bands interpreted as mylonitized conglomerate clasts.�Lower contact gradational.

JL08-089 299.84 317.55 MT-IV Aphanitic dark grey competent rock. Magnetic and mineralized. Hematite staining increases to end of unit which is defined by the sharp dissapearance of hematite staining. Strongly magnetic throughout. Hematite alteration is dominantly banded.�Uranium mineralization occurs throughout this unit with spot highs of 580 at 311.8m; 600 at 314.55m; 1400 at 316.66m; and 3100 at 317.23m.�This entire interval sampled.�Unmineralized, non-magnetic late mafic dykes occur at 304.65 (14cm); 305.78 (10cm); and 307.17 (20cm). They are all chlorite rich.

JL08-089 317.55 342.57 MT-IVDark grey aphanitic intermediate volcanic rocks. Local areas of hematite staining. Weak banding is visible locally but not pervasive. Qtz-carb-epid-chl veins occur typically 1cm thick spaced every ~10cm. Mainly strongly magnetic with local sections that are weak to moderatlely magnetic. Mineralized with spot highs of 1700 at 318.85m, 1000 at 320.25m, and 600 at 321.50.

JL08-089 342.57 344.52 MI.dk.psk Porphyritic mafic dyke showing no strain fabric. Fine (1-2mm) white lathes are interpreted as relict fspar phenos. Chloritic matrix. Non-magnetic, unmineralized.

JL08-089 344.52 367.95 MT-IV Dark grey aphanitic massive intermediate volcanic rocks. Strongly magnetic. Lower contact sharp and marked by lack of magnetism in lower unit. Hematite is pervasive and gives the rock a banded appearance. Mineralized with spot highs up to 1109cps.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-089 367.95 368.26 MI.dk Fine grained dark grey mafic dyke. Non-magnetic. In sharp contact with overlying MTIV and

underlying qtz fspar porph.JL08-089 368.26 371.07 FI.por.fp Coarse subhedral 1-2cm relict fspar phenos now altered to qtz+fspar. Matrix is dark grey and fine

grained. Moderately magnetic. Lower contact gradational to indistinct.JL08-089 371.07 382.08 FI.por.fp

Mixed zones of fine featureless massive grey rock and coarsely porphyritic felspar porphyry. The two units grade in and out of each other on a 20-30cm scale with no distinct contacts. Weakly to moderately magnetic. Strong felty chlorite texture with mineral alignment defining a foliation.

JL08-089 382.08 382.8 MI.dk.por Fine grained mafic dyke with ~20% 1-2mm white relict fspar lathes. Dark grey fine grained matrix, chloritic. Non-magnetic. Lower contact sharp but irregular.

JL08-089 382.2 385.29 MT-IV fine grained grey massive rock. Strongly magnetic. Dark fine grained veins ~3mm thick cross cut the core and are typically irregular.

JL08-089 385.29 385.89 MI.dk.por Fine grained mafic dyke with ~20% 1-2mm white relict fspar lathes. Dark grey fine grained matrix, chloritic. Non-magnetic. Upper contact sharp but irregular.

JL08-089 385.89 402.9 MT-IV Grey aphanitic massive metamorphosed intermediate volcanic rocks with patchy to banded hematite alteration. Small carbonate+chlorite veins cut the rock. Weakly to moderately magnetic. High of 323cps at 385m then from 388-390m average of 600cps over the interval with spot highs up to 2100cps. Lower contact sharp and oriented at ~45tca.

JL08-089 402.9 405.87 MI.dk Dark grey dominantly aphanitic mafic dyke with local areas of porphyritic texture. Non-magnetic. At 405.27m there is a ~20cm inclusion of hematized intermediate volcanic rock with irregular margins. Abundant fine biotite and chlorite. Lower contact is sharp but irregular and oriented at ~30tca. Hairline carb vns present.

JL08-089 405.87 414.33 MT-IV Upper contact sharp and irregular. Lower contact sharp and oriented at 90tca. Moderate hematite staining gives the core a pink/grey colour. Carbonate+chlorite vns are irregular in shape and orientation, typically <1cm thick and spaced ~3-10cm apart. Areas of high vein density are typically less magnetic than areas lacking veins. Overall this unit is moderately to strongly magnetic. Spot high of 277cps but otherwise unmineralized.

JL08-089 414.33 415.78 MI.dk Dark grey, non-magnetic mafic dyke. Texture ranges from aphanitic to fine grained equigranular texture. Strong chlorite alteration. No obvious fabric present. Sharp upper and lower contacts. Upper contact oriented at 90tca and lower at 85tca.

JL08-089 415.78 436.3 MT-IV Similar to previous MT-IV unit. Overall the rock is a grey pink colour resulting from moderate hematite staining. Chlorite carbonate vns ~1cm thick occur spaced ~5cm. Moderately magnetic. Mineralized from 420m to 429m with an average cps of 250cps and spot highs up to 374cps. From 429 to 435 mineralized with average cps of 200.

JL08-089 436.3 438.28 MI.dkMafic dyke with porphyritic texture. ~ 25% relict fspar(?) phenos now altered. Strongly chloritized. Has a green/white speckled appearance. Non-magnetic. Lower contact sharp at 45tca.



Similar in appearance to units of MT-IV above. Pink-grey appearance resulting from hematite staining. In areas carbonate chlorite veining becomes so intense (+50%) that the rock has a brecciated appearance (445-446m).�From 435 to 445 an average of 250cps. From 445 to 456 the average value is around 600cps with highs up to 3700cps. The rest of this interval the mineralization drops back down to background.

JL08-089 466.14 467.88 MI.dk.pskMafic dyke intruding the MTIV unit. Dyke margins are sharp and cut veins within the MTIV unit showing clearly that they are later. No evidence of strain fabric within the dyke. Dark grey green in colour and chlorite rich. Quartz veins up to 5cm thick occur in this unit and are not common in surrounding units. These quartz veins host trace amounts of pyrite. This unit is non-magnetic

JL08-089 467.88 473.26 MT-IV Dark grey massive rock with a banded texture resulting from alteration/deformation. �470.60 5cm dark green strongly chloritized dyke.

JL08-089 473.26 475.2 MI.dk.por Composed dominantly of chlorite with lesser biotite and ~10% relict fspar phenos. Fine disseminated pyrite occurs but constitutes<1% of the rock. Non-magnetic. Sharp upper and lower contacts oriented at ~90tca.

JL08-089 475.2 477.04 FI.dk.por This unit is dominated by a diffuse mix of qtz and fspar with local qtz and fspar phenocryst shapes present. Fine disseminated magnetite occurs throughout. Lower contact sharp and oriented at approximately 80tca (beta of 350-oriented core)

JL08-089 477.04 477.68 MI.dk.por ~25% blocky to lathe shaped ~2mm white fspar and relict fspar phenos. Matrix is dark green and chlorite rich. One 3cm quartz vein occurs in this unit. Lower contact sharp oriented at 70 tca (beta of 340). Non magnetic

JL08-089 477.68 496.13 MT-IV Mainly dark grey aphanitic looking rock with local areas of banding, patchy or even porphyritc texture. Moderately to strongly magnetic. Veins are less abundant in this interval and consist of chlorite, carbonate +/- leucoxene. Towards the bottom of this interval large (>5cm) diffuse quartz veins increase in abundance. Matrix appears rich in biotite and chlorite. Lower contact is gradational and indistinct. No mineralization encountered.

JL08-089 496.13 502.09 MT-FV chlorite blebs in a diffuse qtz feldspar matrix. Milky pink qtz kspar vnlts occur up to 2cm in thickness typically spaced >20cm apart. Overall light pink-grey in colour. Moderately magnetic. Unmineralized. Upper contact diffuse. Lower contact sharp and oriented at ~85tca.

JL08-089 502.09 504.41 MI.dk.por Mafic dyke with 25% ~1-2mm white relict fspar lathes. Matrix is dark grey and chlorite rich. Non-magnetic

JL08-089 504.41 507.39 MT-FV Diffuse feldspar and quartz chlorite matrix. Dark to light grey colour speckled white pink grey green in many areas. To small (12cm) dykes occur in this interval. Lower contact sharp but irregular. Moderately magnetic.

JL08-089 507.39 508.41 MI.dk.por ~25% white 1-2mm fspar lathes in a dark chlorite rich matrix. Moderately magnetic throughout. High angle (10tca) gypsum vein runs through this unit and into the unit above.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-089 508.41 513.68 MT-FV Non-descript grey rock with abundant diffuse quartz veins. Several quartz veins show multiple centre

lines. Chloritic matrix contains minor leucoxene.JL08-089 513.68 514.19 MI.dk Sharp contacts upper 85tca lower 45tca.JL08-089 514.19 515.74 MT-FV Dark grey with multiple milky pink diffuse quartz kspar veins.JL08-089 515.74 520.47 MI.dk 2 smaller dykes occur within this dike. At 518.22 m there is a 12cm dyke with 5mm pink fspar phenos

and a chlorite rich matrix. At 519.17 there is a 16cm fspar porphyrtic mafic dyke.JL08-089 520.47 534 MT-FV 522.10m 27cm dyke of porphyritic mafic rock.

JL08-090 0 1.59 OVBD Overburden and casingJL08-090 1.59 6.55 MT-CO.pl

Beige to light green metaconglomerate. High levels of mudstone visible at top of interval, though decreases with depth. Texture is bimodal, though increasingly fine grained towards lower contact. Appears to be increasingly metamorphosed as unit approches lower contact. Lower contact is very gradual. Unit is moderately clastic at top of interval, and tapers to clast poor with depth.�Mineralogy is predominantly mudstone (55%) at top, Large white quartz lens visible at 4.77m, which is then followed by rubble. K-feldspar porphyrys scattered throughout. A few chlorite veines towards lower contact. Some rosy quartz seen towards middle of unit. Weakly magnetic.

JL08-090 6.55 17.08 MI.dk.pskMafic dyke. Little to no deformation. Very broken/blocky in areas. Occasional K-feldspar and quartz lenses. Some rare mudstone visible, though probably from previous unit. Biotite levels range from moderate to very high. High levels coincide with brittle regions. Prominent chlorite veining. Biotite and horneblende present throughout. Very red feldspar visible towards lower contact. Unit is moderately magnetic. Smokey quartz veine also visible towards lower contact.

JL08-090 17.08 18.18 MT-CO.plShort metaconglomerate interval. Chlorite, mudstone and feldspar main minerals. moderately mafic. Moderately clastic. Clasts generally ~5cm. Some horneblende and biotite visible.

JL08-090 18.18 48.67 MI.dk.pskInterval begins rich in biotite clasts. Feldspar lenses and phenos visible throughout. Highly chloritized matrix. Biotite ranges from very strong to moderate. Hornebnlende appears to be replaced by biotite. Very brittle areas, once again, characterised by high levels of biotite. Occasional intervals of carbonate veines. Returns to clast rich at ~33m until 34m. Tapers from moderately clastic to poor up to 39m. Weakly magnetic, though increases with depth to moderate.�Towards lower contact, chlorite and feldspar veining increases.

JL08-090 48.67 49.71 MT-CO.pl Small metaconglomerate interval. Highly mafic towards upper contact, followed by high k-spar and chlorite occurances. Quartz also present sporadically throughout the interval. Unit is moderately magnetic.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-090 49.71 55.61 MI.dk.psk

Unit begins as fine grained, biotite rich mafic dyke. Some very thin epidote veinlets are visible. This section has not been deformed. Quartz vein at 50.16m. As the unit continues, biotite appears to be replaced by horneblende, resulting in a breccia like texture of horneblende phenos in a chlorite rich matrix. Continues to 50.34m, where texture returns to finegrained, biotite rich matrix with small amount of horneblende, and occasional epidote veins. 51.11m sees return of afore mentioned breccia like texture, though not as chlorite rich, and lacks epidote veins. 51.27 to 51.81 is fine grained biotite rich with some like quartz veinlets. 51.81 to 55.61 is consistently chlorite rich matrix with hornblend phenocrists with consistent epidote veins. Unit is moderately magnetic. Occasional calcite vein. Occasional k-spar pheno.

JL08-090 55.61 56.48 QZ.vn Large qtz vein, some biotite encased within.JL08-090 56.48 63.91 MI.dk.psk

Medium grained mafic dyke. Hornblende phenos dominate in biotite rich matrix. Occasional K-spar pheno. Periodic epidote veins. Quartz also present within matrix. Moderately magnetic

JL08-090 63.91 71.19 MI.dk.por Typical porphyritic mafic dyke. Fine grained biotite rich matrix hosting quartz and feldspar, angular like phenos (~10%). Some chlorite present. Unit has very fine grained chill zones on both upper and lower contacts. Stongly magnetic. Occasional carbonate vein

JL08-090 71.19 78.45 MI.dk.psk Mafic dyke with many chlorite and epidote veins. Occasional quartz and feldspar phenos, 0.5 to 2 cm in size. MODERATELY MAGNETIC.

JL08-090 78.45 88.26 MT-CO.pl.my Very feldspar rich metaconglomerate. Feldspar is red, combined with usual chlorite, epidote and quartz. Periodic sections of highly metamorphism towards lower contact. Weakly magnetic. Increasingly occuring carbonate veines with depth.

JL08-090 88.26 111.02 MI.dk.pk Mafic dyke dominated by carbonate veins. Brittle fracture fill carbonate veines. Occasional rosy carbonate vein. Vein desity ranges from sporatic to intense. Carbonate Veine density tapers with depth. Towards lower contact, previously mentioned chlorite rich matrix hosting hornblende phenos are visible. Weakly magnetic.

JL08-090 111.02 111.86 MT-CO.pl Short interval o f metaconglomerate. Finer grained that typical MT-CO of Jacques Lake. Also appears to be more mafic than usual. Usual chlorite, quartz and k-spar. Non magnetic.

JL08-090 111.86 122.04 MI.dk.pk Return to mafic dyke dominated by brittle fracture fill carbonate veins. Still occasional rosy carbonate. Chlorite replaces carbonate veines towards lower contact. Usual biotite rich matrix. Weakly magnetic. Occasional k-spar pheno.

JL08-090 122.04 124.4 MI.dk.psk Mafic dyke, high chlorite levels. No carbonate veines, high levels of biotite and horneblende. Non meganetic. Unmineralized.

JL08-090 124.4 133.49 MT-CO.plRed, feldspar rich metaconglomerate. High levels of feldspar visible throughout interval, starting with ~10cm feldspar vein. Texture is bimodal, though increasingly fine grained towards lower contact. Increasingly deformed with depthk. Lower contact is very gradual. Unit is moderately clastic at top of interval, then becomes deformed, allining clasts into parallel sequences. Non magnetic.



Weakly hematitic, unmineralized metamorphosed intermediate volcanics. Moderately altered. Strained roughly 30 degrees to core axis. Some feldspar present. Hematite is spotty throughout. Overall dark red texture. Trace epidote and chlorite. Non magnetic. Primary texture.

JL08-090 135.14 137.31 MT-CO.plRteturn to previously mentioned metaconglomerate. Moderately deformed. Usual clasts o ffeldspar, chlorite, epidote. Some areas contain high levels of mudstone. Overal light green texture. Large felsic section toward lower contact which borders at roughly 15 degrees to core axis. Increase quartz and feldspar occurances with depth. Typical epidote veines. Carbonate veines visible throughout. Section is non magnetic. Overall a moderately clastic section.

JL08-090 140.31 147.25 MT-FV.por Red feldspar volcanics. Section is moderately deformed. Typical phenos of k-feldspar and blue quartz eyes. Trace amounts of biotite. Unit borders sharply perpendicular to core axis at top contact. Usual small veinlets of white quartz and carbonate. Unit is non magnetic. Pheno concentration is consistantly moderate throughout. Colour is darker towards top, tapering to a maroon towards lower contact, which also borders perpindicular to core axis.

JL08-090 147.25 156.42 MI.dk.pkReutrn to carbonate rich mafic dyke. Carbonate veines appear to be fracture fill. Unit's upper contact is oriented perpindicular to core axis, while lower contact is oriented 80 degrees to core axis. Occasional rosy carbonate. Periodic rich sections of epidote along with occasional salmon feldspar. Towards lower contact, colour becomes slightly red in colour, resulting in a dark maroon aura, suggesting dessiminated hematite. Unit is weakly magnetic. Usual biotite rich matrix.

JL08-090 156.42 170.27 MI.dk.psk Fine grained mafic dyke, ocasional carbonate veine, though obviously different from previous interval. Sharp contact perpindicular to core axis. Unit is moderately magnetic. Biotie rich, with persistant horblende phenos throughout, generally in the <1cm sub-angular range. Periodic epidote and chlorite veining, much more common than carbonate. Occasional quartz and feldspar phenos. Overall, section is poorly deforemed.

JL08-090 170.27 177.26 MT-FV.porReutrn to metamorphosed porphyritic felsic volcanics with feldspar and blue quartz eyes. Red to dark red colour. Moderate to highly depormed, roughly 60 degrees to core axis. Phenos decrease in abundance with depth. Periods of intense epidote mineralization. Epidote and feldspar "blobs" occur close to lower contact. Lower contact is very graudual. Yellow quartz veine towards bottom.

JL08-090 177.26 186.62 MT-CO.pl.my modeately mylonitized metaconglomerate. Beige to light green with intervals of red feldspar rich mineralization. Texture is bimodal throughout. Appears to be increasingly mylonitized as unit approches lower contact. upper contact is very gradual while lower contact is sharp, roughly 25 degrees to CA. Unit is moderately clastic throughout interval.�Mineralogy is predominantly feldspar chlorite, quartz, epidote and some patchy sections of mudstone. Some carbonate veines. Non magnetic.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-090 186.62 187.74 MI.dk.pk Small pre-kinematic mafic dyke. Upper contact show strain. Contacts are sharp. Small (<1cm)

phenos of feldspar are consistent throughout, along with quartz. Usual biotite rich matrix with some horneblende and chlorite. Unit is weakly magnetic.

JL08-090 187.74 188.91 MT-CO.pl Return to previously described mylonitized metaconglomerate.JL08-090 188.91 193.46 MI.dk.por Typical porphyritic mafic dyke. Fine grained biotite rich matrix hosting quartz and feldspar, angular

like phenos (~10%). Some chlorite present. Unit has very fine grained chill zones at upper contact. weakly magnetic. Occasional carbonate vein. Sharp upper contact. Lower contact is broken and blocky.

JL08-090 193.46 234.53 MT-CO.pl Usual Jacques metaconglomerate. Short mafic dyke from 222.95 to 223.41. Dyke is highly fractured and infilled with epidote. Metaconglomerate is clast rich, with intervals of red fladspar. Strain increases towards lower contact(?). Clasts size is generally in the 1-2cm range, except from 218.76 to 22.58 where it decreases to the <1cm range. Unit is non magenetic. Chlorite feldspar, quartz epidote dominate the minearalogy. Some small carbonate veines. One large irregular carbonate fracture fill.

JL08-090 234.53 251.72 MI.dk.porPorphyritic mafic dyke. Fine grained biotite rich matrix hosting quartz and feldspar, angular like phenos (~10%). Some chlorite present. Unit has very fine grained chill zones on both upper and lower contacts. weakly magnetic. Occasional carbonate vein. Usual epidote veining.

JL08-090 251.72 260.86 MT-CO.pl Return to previously mentioned metaconglomerate.JL08-090 260.86 274.75 MT-FV.por

Red feldspar volcanics. Section is moderately deformed. Typical phenos of k-feldspar and blue quartz eyes. Trace amounts of biotite. Unit borders sharply perpendicular to core axis at top contact. Usual small veinlets of white quartz and carbonate. Unit is non magnetic. Pheno concentration is consistantly moderate throughout. Colour predominantly red throughout, though flip flops back and forth from dark maroon to bright red. Section is brecciated towards lower contact.

JL08-090 275.75 279.24 MT-CO.pl.my Feldspar rich mylonitic metaconglomerate. Highly starined. Beige to light green between intervals of red feldspar rich mineralization. Texture is bimodal throughout. Decreasingly mylonitized as unit approches lower contact. upper contact and lower contacts are very pronounced. Unit is moderately clastic throughout interval.�Mineralogy is predominantly feldspar chlorite, quartz, epidote and some patchy sections of mudstone. Some carbonate veines. Non magnetic.



Dark red to dark grey & black, fine-grained metamorphosed intermediate volcanics, strong pervasive hematite alteration in upper 7m of interval, decreasing w/ depth. Moderately hematized, tapering to trace with depth. By 301 rock is almost black. Mininor quartz and feldspar veinlets throughout bottom 10 m. Abundant typical veinlets & stockworks but appear to become more chlorite-dominant w/ depth. Scint values <250 cps, save for short interval from 289.00 - 289.40. Sulphides occasionally present within both veinlets & matrix in upper 10 m of interval. Unit is weakly magnetic at higher scint reading, trace magnetism everywhere else.�Hematization returns at 354.50, weakly hematized. Perioic sections of intense clorite and epidote veining. Slightly altered. Count of XXXXcps at lower contact.

JL08-090 357.86 358.32 MI.dk.por Porphyritic mafic dyke. Usual phenos of feldspar and quartz in fine grained biotite rich matrix. Weakly magnetic.

JL08-090 358.32 406.21 MT-IVhighly altered and hematized. Strongly magnetic. Metamorphic intermediate volcanics. Locally mylonitic. Roasy red intermediate componant. Moderate calcite and amphibole veining. Strongly magnetic is areas, overall, moderate to strong. Moderately to highly altered, high in areas of high cps counts. Mafic dyke visible from 386.20 to 386.56. �After dyke, decrease in hematite, though still moderately altered. Calcite veining increases with depth from this point on. Some carbonate veines visible. Lower contact approximately purpendicular to core axis. Increase in white and rosy quartz veines as lower contact is approched. �Average of 600cps over 26 m, with a max of 5048cps.

JL08-090 406.21 418.1 FI.por.fp Coarsely porphyritic felsic intrusive. Moderately hematized. Medium grained matrix. Moderate levels of biotite and horneblende. Low strain. Very felsic at bottom 0.97m of unit. Lower contact very broken and blocky, appears to be at roughly 90 degrees to core axis. Increases epidote veining with feldspar with depth. Non magnetic. Unmineralized

JL08-090 418.1 440.33 MI.dk.porPophyritic mafic dyke. Top contact purpendicular to core axis. Very broken at top contact, almost breccia like texture. Lots of fracture fill epidote and carbonate veines. Feldspar and quartz pheno rich, though tapers with depth. Magnetics increase with depth to moderate level, and grain size decreases. Still occasional red feldspar pheno, probably broken from upper unit. Carbonate vein rich throughout, along with increase in quartz vein abundance with depth. Usual biotite rich matrix.

JL08-090 440.33 446.84 MT-IVLong section of intermediate volcanics. Hematization is very weak for the most part, but increases to moderate in spotty sections. Alteration is low. Some pyrite visible at 450.48. Regular feldspar lenses and quartz veins. Periodic tiny fracture fill carbonate veins. 453.40 to 453.70 see increase in hematization and alteration. Top contact very gradual and difficult to spot due to the low alteration and hematization of the volcanic unit. Chlorite veining coming throughout. Stongly magnetic


Hole ID From (m) To (m) Lithology Code DescriptionJL08-090 446.84 448.32 MI.dk.por Short mafic dyke. Slightly porphyritic. Some gabbro. A few large quartz phenos (1.5cm). Tiny quartz

and feldspar phenos (<.5cm). Usual biottie rich matrix. Weakly magnetic.JL08-090 448.32 481.47 MT-IV

Return to poorly hematitic intermediate volcanics. Sections of high alteration, and hematization. 453.40 to 453.70 see increase in hematization and alteration. Strongly magnetic. Consistant chlorite veins throughout, though expecially between 454 and 462. Usual fraccture fill carbonate. Sparkly magnetite visible in matrix, along with biottie and actinolite. Periodic feldspar lens. Seams moderately strained atin areas. A few small mineralized sections (just over 300cps).

JL08-090 481.47 482.52 MI.dk.por Fine grained porphyritic mafic dyke. Usual tiny phenos of qtz and feldsparJL08-090 482.52 487.39 FI.por.fp Coarsely porphyritic feldspar porphyry. Sharp contacts 65 degrees to core axis. Increasingly

porphyritic towards center with finer grained chill contacts.JL08-090 487.39 488.27 MI.dk.por Return to previously mentioned med grained porphyritic mafic dyke.JL08-090 488.27 490.86 MT-IV See previous description of weakly hematized, moderately altered intermediate volcanics.JL08-090 490.86 499 FI.por.fp Return to coarsely porphyritic felsic intrusive. Small mafic dyke from 494.43 - 496.35.�

Could be granite, fine grained.�EOH

JL08-091 0 5.2 OVBD overburden and collar.JL08-091 5.2 17.86 MI.dk.sk Dark Green/black (weathered and brown near the top) mafic dyke. Highly moderately to heavily

veined with calcite and quartz. No visible phenoscrysts.JL08-091 17.86 22.98 MT-CO.pl Dark red and green unit. Becoming increasingly deforemed and banded downhole. Containing

epdiote, hematite, calcite veins, quartz and feldspar. Small (~03-0.5cm) rounded clasts more evident in the upper portion of the unit. Messy upper and lower contacts.

JL08-091 22.98 38 MI.dk.pk Black/dark green, highly veined and metamorphosed mafic dyke. Contains calcite, hematite staining, chlorite and quartz.

JL08-091 38 90.5 MT-CO.pl Highly deformed/banded black, red-purple and green conglom. Messy upper contact. Rounded to sub-angular clasts ranging from 0.3 - 15cm. Contains calcite veins, chlorite, quartz, k-feld, epidote. Becoming more deformed downhole. Grades into next unit.

JL08-091 90.5 94.44 MI.dk.sk Dark gray-black aphanitic mafic dyke. No phonos. Some plucked clasts from adjacent congom units. Both upper and lower units are gradational.

JL08-091 94.44 98.4 FI.por.fpRed porphritic felsic unit. Containing k-feld phenos ~0.3 - 0.5 cm. Lower 50cm of the unit is much more strongly deformed. Lower contact is sharp and makes angle of 80deg with core axis.

JL08-091 98.4 116.43 MT-CO.pl Dark gray/black-green strongly deformed felsic conglomerate. Clasts are rounded and range from 0.5 - 10cm in diameter. Contains quartz, k-feld, chlorite, epidote. Some carbonate, quartz and feldspar veins. Sharp upper contact making an angle of 85deg with


Hole ID From (m) To (m) Lithology Code DescriptionJL08-091 116.43 117.23 MI.dk.psk Dark gray-green fine grained syn or possibly post-kinematic mafic dyke. Contains some epidote,

minor veining. Busted-up upper contact. Lower contact is sharp and makes an angle ~80deg with core axis. Non-magnetic.

JL08-091 117.23 119.83 MT-FV.por Dark red/purple highly deformed felsic unit. Contains a lot of k-feld, quartz . A band of chlorite at ~119.58 depth, could be a clast. Contains patches where phenos ~0.1-0.3cm are evident. Some magnetic patches, mostly non magnetic. Sharp upper and lower

JL08-091 119.83 120.78 MI.dk.sk Dark gray/black-green unit. Fairly heavily veined containing carbonate and quartz. Contains some phenos, more evident at lower contact. Some xenolith action around the contacts. Sharp upper and lower contacts making angles of ~75 and 45 deg, respectivily.

JL08-091 120.78 154.82 MT-CO.pl Dark gray-purple conglomerate with a fine grained matrix containing rounded to sub-angular clasts ranging from 0.5 - 10cm in diameter. Clasts are composed of k-feld, epidote,chlorite, quartz and mudstone. Exhibits some veins containing carbonate, chlorite

JL08-091 154.82 158.18 MI.dk.psk Dark gray/black porphyritic post kinematic mafic dyke. Only one veinlet 50deg to core axis. Rediculously tiny phenos. Upper contact is sharp and makes angle of 45deg. Lower contact is 87ish deg to core axis.

JL08-091 158.18 171.55 MT-CO.pl Purple-blackish purple/red meta conglomerate. Clast are sub-rounded to sub-angular and range from 0.2 to 15cm in diameter. Contain chlorite, k-feld, epidote Moderately to high desnity of carbonate veinlets . Patchy moderate to high magnetism.

JL08-091 171.55 172.82 MI.dk.skDark Gray/Green-black porphyritic mafic dyke. Very small phenos ~<0.1cm. Containing cholorite, some quartz very little veining. Sharp upper and lower contacts make 45deg angle to core axis.

JL08-091 172.82 185.94 MT-CO.pl Same comglomerate as previously described. Becoming more mylonitic downhole.JL08-091 185.94 195.23 MT-CO.pl.my Dark red to dark gray/green mylonitic conglomerate. Clasts are strongly deformed but those that are

visible range from ~0.5 - 12 cm in diameter and contain chlorite, k-feld, hornblend, quartz, epidote, and carbonate. Exhibits some veining generally at abo

JL08-091 195.23 195.93 MI.dk.skDark gray/black aphanitic mafic dyke. Contains viens of chlorite and/or epidote at 25 deg to core axis.

JL08-091 195.93 204.54 MT-CO.pl Conglomerate as described previously. 25deg upper contact.JL08-091 204.54 206.37 MI.dk.sk

Dark gray-black synkinematic mafic dyke. Contains chlorite veins making 25deg angles with core axisJL08-091 206.37 229.98 MT-CO.pl Same conglomerate as described above contains a small (28cm) mafic dyke at 213.96 m intruding at

an angle of 40 deg.JL08-091 229.98 233.89 MI.dk.sk Dark gray/black mafic dyke moderately viened at 40deg angles to the core axis. Upper and lower

contacts also make a 40deg core axis.JL08-091 233.89 241.86 MT-CO.pl.my Very felsic unit ranging in colour from a high red occurance to a high green occurance. Strongly

deformed with a fabric aligned 45deg to core axis. Containing quartz, feldspar, epidote. Contains some veining including those of carbonate. Upper contact


Hole ID From (m) To (m) Lithology Code DescriptionJL08-091 241.86 305.41 MT-IV Red-black becoming more green-black at about 259.50m depth and down hole. Highly magnetic.

Containing epidote, chlorite,carbonates, k-feld, quartz (occuring with what appears to be jade). Intruded by a post kinematic mafic dyke at 257.24 - 257.44m depth

JL08-091 305.41 306.06 MI.dk.psk Short black interval. No visible fabric, non-magnetic. Sharp 40deg upper and lower contact.JL08-091 306.06 347.64 MT-IV Dark gray/black- dark red meta volcanics. Moderately to strongly magnetic. Exhibiting pyrite and

calcite veining also containg some k-spar, epidote, chlorite. Unit becomes less hematized down hole losing its red tinting for a more dark-gray colour. Intrud

JL08-091 347.64 349.64 MI.dk.sk Dark gray/black unit containing no phenos but having xenoliths at the lower contact and at spots within the unit from the lower unit (coming up next).

JL08-091 349.64 360.43 FI.por.fp Dark gray porphyritic unmit with rounded feldspar phenos ranging from 0.3 0- 1.8 cm in diameter. Matrix is biotite rich and has varying density of phenos throughout. Upper and lower contacts are gradational and obscured by xenoliths in adjacent units. The

JL08-091 360.43 364.1 MI.dk.sk Dark gray/black biotite rich unit with little disernible fabric and no phenos. Contacts with adjacent units are once again obscured by xenos.

JL08-091 364.1 364.84 FI.por.fp Same porphyritic unit as before.JL08-091 364.84 404.21 MT-MI.fgr Dark Gray/green-black biotite rich unit. Contains veins of chlorite, k-feld and quartz. Strongly

magnetic. Contains occational quartz clasts.JL08-091 404.21 410.49 MI.dk.sk

Dark gray unit becoming more red downhole. Contains moderately high percentage of phenos ~0.1 - 0.4 cm in diameter containing k-feld. Veins show evidence of shearing. Non magnetic.

JL08-091 410.49 419 MT-MI.fgr return to fine-grained mafic intrusive. Fairly large veins (1.0 - 2.5 cm wide) containing cholorite at approximately 45deg to core axis. EOH

JL08-092 0 4.89 OVBD Overburnden and casingJL08-092 4.89 10.12 MT-CO.pl Dark green to pink moderately sheared conglomerate unit. Clasts sizes range from 0.2 to 2cm.

Number of clasts decreases downhole. Only rare clasts after Increasingly felsic towards bottom contact. Clasts are polylithic, brown, green, pink with ct +ap +/-ac +/-fps. Med hm alteration throughout unit. Several sets of micro-fractures with approx 1mm bleaching on each side. Rich in carbonate veins. Non to weakly magnetic.

JL08-092 10.12 14.37 MI.dk.por Porphyritic mafic dyke with usual phenos of feldspar and quartz. Consistant epidote veining. Both contacts very gradual. Blocky and broken for majority of interval. Biotite and horneblende dominate matrix. Weakly magnetic.

JL08-092 14.37 20.47 MI.dk.pk Mafic dyke dominated by carbonate veins. Brittle fracture fill carbonate veines. Occasional rosy carbonate vein. Vein desity ranges from sporatic to intense. Carbonate Veine density tapers with depth. Towards lower contact, previously mentioned chlorite rich matrix hosting hornblende phenos are visible. Weakly magnetic.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-092 20.47 24.18 MT-CO.pl Typical Jacques metaconglomerate. Green, red and light brown polylithic conglomerate. Weakly to

mod sheared. Shearing stronger close to lower contact. Blebby ct alterations still present and more intense than in unit above. Core competent. Clasts are subrounded, 1-10mm, made of light brown mudstone, purple jasper chert, kspar. Rare quartz crystals. Groudmass is aphanitic to very fgr, dark red. Hm altn pe and strong. Kpsar altn patchy and irregular. LCT obscured by broken core. Pa mag. Non magnetic.

JL08-092 24.18 26.05 MT-FV.por Red feldspar volcanics. Section is moderately deformed. Typical phenos of k-feldspar and blue quartz eyes. Trace amounts of biotite. Unit borders sharply perpendicular to core axis at top contact. Usual small veinlets of white quartz and carbonate. Unit is non magnetic. Pheno concentration is consistantly moderate throughout. Colour is darker towards top, tapering to a maroon towards lower contact.

JL08-092 26.05 27.83 MT-CO.pl Return to previously described metaconglomerateJL08-092 27.83 33.51 MT-FV.por See previously mentioned felsic volconics.JL08-092 33.51 39.39 MT-CO.pl Dark gray-green clast poor meta conglomerate with rounded-subangular clasts of mudstone ranging

from 0.5 - 10cm in diameter.JL08-092 39.39 48.25 MT-FV.por Red and black highly deformed felsic meta-conglomerate containing quartz, feldspar and carbonate.

Heavily veined. Patchy weak magnetism, otherwise non-magnetic. Sharp upper contact making an angle of ~20deg with core axis. ~80deg contact with lower unit.

JL08-092 48.25 64.1 MI.dk.psk Dark gray/green mafic dyke containing phenocrysts of 0.1 - 0.3cm diameter. Contains some veins of cholorite, some k-feld and carbonate veins. Unit becomes fine grained at the lower contact which is sharp and roughly 75 degrees to c/a. Dark green from chl + act after hbl (px?). Unit is moderately-to strongly magnitic. Hematite staining is after hematite.

JL08-092 64.1 87.3 MT-IV Foliated metamorphosed intermediate volcanic (volcaniclastic) rock: Unit is hard, dark-grey and red due to silica alteration and hematite staining. The irregulat and somewhat chaotic foliation is defined by altertating darker green/grey and hematite stained red bands on a cm scale. Banding is generaly chaotic but tends to average around 45 degrees to c/a. Occational zones of sheared volcaniclastic material is present and defined by lighter coloured 2mm to 1.5 cm stretched/flattened "clasts", again about 45 degrees to c/a. Both contacts are sharp, the and the banding is truncated on both. The lower contact is at about 70 degrees to c/a. Unit is cut by many < 1mm thick white fractures of various orientations.

JL08-092 87.3 88.05 MI.dk.pk Dark Green metamorphosed mafic dyke which post-dates foliation in the surrounding rocks. Same as the mafic unit above Dark green from chl/act/ser alteration of the mafic component of the rocks. Contacts are both sharp and cut foliation in the intermediate volcanic rocks. Unit is composed of 40-50% plagiaclase and the rest altered mafic minerals, primarily hbl. Unit is equigranular and grain size is in the 0.5 to 1mm range. Unit is patchy magnetic. Unit is cut by a few thin (< 1mm) carbonate veins). The lower contact is at about 50 degrees to c/a.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-092 88.05 94.5 MT-IV Foliated metamorphosed intermediate volcanic (volcaniclastic) rock: Exactly the same as that

discribed at 64.1m. Cut by a 15cm thick highly ser/chl/act altered dyke at about 50 degrees to c/a (cuts foliation); it is courser-grained in the middle and is an altered post kinimatic mafic dyke as above. Lower contactr is broken, but looks to be sharp.

JL08-092 94.5 96.3 MI.dk.por Metamorphosed porphyritic mafic dyke: This unit is dark green due to strong act, ser, chl alteration. It contains 40-50% plagioclase taths, mostly porphyritic with respect to the finer grained and altered mafic matrix (hbl, px?). Rare 1 cm and greater laths of plag are present but comprise << 1% of the rock. The unit is finer grained at near both contacts and the lower contact is sharp and about 70 degrees to c/a. This unit is likely the same as the post kinematic dukes discribed above as it also clearly is not foliated. It is moderately to strongly magnetic and is cut bu late thin < 1mm thick white veins (at least some of which are albite.

JL08-092 96.3 99.6 MT-IV Foliated metamorphosed intermediate volcanic (volcaniclastic) rock: Same as that discribed at 64.1m. Contains a zone of prominent sheared/flattened conglomerate with clasts up to about 2 cm long. Lower contact is sharp and at about 60 degrees to c/a.

JL08-092 99.6 129 MI.dk.psk Fine to medium grained metamorphosed mafic dyke. Unit appears to contain multiple pulses of intrusion as indicated by internal seemingly regilar ratty altered zones and apperent changs in grain size. The unit more resembles a series of mafic volcanic flows, however, I'm not sure how they would fit into the tectonic setting especiallyconsidering they seem to be relatively undeformed (though there is some evidense for deformaion). Unt is generally dark green due to strong ser/act/chl alteration. Weak reddness is also comon present due to FexOy staining (the unit is not very magnetic). In the fresher zones between ratty "contacts" one can clearly make out tiny laths of plag and a small dark mafic component. Unit cut by some late white (albite and carbonate) veins. The lower contact is broken core.

JL08-092 129 132.6 MI.dk.pskMafic Dyke, Post kinematic. Undeformed and realatively fresh mafic dyke. The lower contact is at a low angle to the c/a (15 degrees) and clearly the mafic rock post-dates the unit below as indicated by the allignment of minerals parrallel to the contact within the mafic rock.The rock near the upper contact displays the same allignment of minerals and at roughly the same angle suggesting the upper contact is also about 15 degrees to c/a. The unit contains about 40-50% 0.5 - 1 mm laths plag and a small portion of dark minerals about the same size (hbl or px) within a fg matrix (i.e. the unit is porphyritic). Unit contains very few veins and they are < 1mm thich, white and carbonate.

JL08-092 132.6 137.9 MT-CO.plSheared sand to pebble sized sediments, interpreted to be the finer grained equivelant of the sheared conglogerate unit within adjacent holes and described deeper in this hole. Unit contains primarily sandy and some peddle sized material which is sheared to generally about 40 degrees to c/a. Unit is reddish due to FexOy staining and displays patchy magnatism. Inut contains many up tp 2mm thick veins of carbonate and there appears to be a diminant orientation of about 50 degree to c/a.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-092 137.9 138.9 MI.dk.psk Mafic Dyke, Post kinematic: Same as that described at 129m. Upper and lower contacts display

allignment of minerals with in the mafic unit and are at low angles to the c/a. Upper contact is broken, but can tell it is sharp.

JL08-092 138.9 140.1 MT-CO.plSheared sand to pebble sized sediments, interpreted to be the finer grained equivelant of the sheared conglogerate unit within adjacent holes and described deeper in this hole. Same as above.

JL08-092 140.1 151.1 MI.dk.pskMafic Dyke, Post kinematic. Undeformed and realatively fresh mafic dyke (gabbro). Same as that described at 129m. Upper contact at low angle to c/a and displays allignment of minerals to contact. Lower contact sharp, at 45 degrees to c/a and also displays allignment of minerals. Unit contains very few veins, is magnetic and is a bit reddiish due to FexOy staining. Moderate act+chl alteration. Unit here more equigranular and some hbl for sure, but not sure if px + hbl.

JL08-092 151.1 175.9 MT-CO.plMetamorphosed and strained polylithic caorse grained conglomerate unit. Unit is patchy in its appearance, but generally pebble and greater sized, polylithic (multi-coloured) rounded to sub-angular and variably strained clasts withing a finer grained dark reddish grey groundmass. Some places are more sandy than conglomerate (as with the units above). Red staining from FexOy. Patchy weak magnetism. Deformation is variable in intensity, but generally about 25 - 30 degrees to c/a where the most intense. Moderate carbonate veining. Lower contact with mylonite is sharp. The foliation is cut by the mylonite fabric. The contact is 70 to c/a.

JL08-092 175.9 189.1 MT-FV.por Mylonite zone that looks to have been derived from the intense shearing of quartz clasts /phenocrysts. The unit is generally silt and sand sized material which displays a banded to finely "laminated" in texture to it. The unit here is being "called" a mylonitised meta-felsic volcanic unit primarily based on the differents in shrain noted at the contact (suggesting a change in rock rheology) and the presents of resistant quartz grains, not reallt present in the conglomerate. The unit does however seem to be interlayered with the conglomerate in the conglomerate unit above. The unit is quite hard (silica altn ??), and red/grey in colour due to FexOy staining. There Is a clear gradation present in the angle of the foliation within this unit. The lower contact is somewhat picked arbitrarily based on a shift in apparent grain size. Threre are occational (<<1% of rock) green filled (act+/- chl) veins with reddist salvages present, generally // to foliation. At about 186.1 m, there is an area where there appears to be a weak foliation overprinting the mylonite, it is cutting the mylonite at

JL08-092 189.1 189.55 MT-CO.pl Metamorphosed and strained polylithic caorse grained conglomerate unit: Same as unit above but more reddish matrix and material (few quartz clasts).

JL08-092 189.55 190.25 MI.dk.pk Highly strained and altered pre-kinematic mafic dyke: Green deformed, chl, act and ser altered mafic rocks. Unit has an internal foliation of about 40 degrees and two sharp contacts at 60 degrees. The unit is maderately magnitic. Contains the odd foliation parallel veinlette of carbonate. Origianal mineralogy is not possible to identify.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-092 190.25 193.4 MT-CO.pl Metamorphosed and strained polylithic caorse grained conglomerate unit: Same as unit above

samller grain size and much more strained. This zone is also moderately magnetic and consistantly so (interesting is that this zone is bound on both sides by sheared pre-kinematic mafic dykes which are also quite magnetic. The Orientation of the foliation is fairly consistent within this zone at about 45 degrees to c/a. Both contacts are sharp. The unit is quite hard (quartz altn) and red (FexOy staining). Unit is cut by a few late silica filled veins.

JL08-092 193.4 193.9 MI.dk.pk Highly strained and altered pre-kinematic mafic dyke: Green deformed, chl, act and ser altered mafic rocks. Unit has an internal foliation of about 40 degrees and the lower contact is at 50 degrees to c/a. The unit is moderately magnitic. Contains the odd foliation parallel veinlette of carbonate. Origianal mineralogy is not possible to identify.

JL08-092 193.9 197.3 MT-CO.pl.myMetamorphosed and strained polylithic caorse grained conglomerate unit: Same as unit just above though this unit is not reddish and not magnetic. The unit here takes in a streaked white and grey appearance. The white streaks are quartz +/- plag and the dark is undifferentiable but hard (quartz altered). Some small area resemble the mylonitised volcanic rocks described at 175.9 m (interbedded with conglomerate??). The Orientation of the foliation varies from about 75 to 15 degrees to c\a as seen in the structural measurements.

JL08-092 197.3 197.35 MI.dk.pkHighly strained and altered pre-kinematic mafic dyke: Same as above. Both contacts are dammaged do to drilling however both appear to be at low angles to a/c. This zone is not noticable magnetic.

JL08-092 197.35 199.05 MT-CO.pl.my Metamorphosed and strained polylithic caorse grained conglomerate unit: Same as unit just abovestarting at 193.9m. Unit has a gradational contact with the lower unitwhich we are calling a mylonitised prophyritic felsic volcanic rock (see discription below). The foliation in intense and oriented fairly consistantly at 50 degrees to c/a. Some late thin carbonate filled veins present at low angle to c/a (~15 degrees)

JL08-092 199.05 202.9 MT-FV.porMylonitised porphyritic felsic volcanic rock: Same as the unit discribed at 175.2 m. Clearly can make out 15 -20% 0.5-1mm resistant porphyroclasts of quartz and possibly plag. These sit in a f.g. greyish-red matrix. The reddness is from weak FexOy staining. The unit is cut by a few later silica/plag veins and a few late green filled (looks calc-silicate to me) veins with reddish-brown salvages and also the very late calcite filled fractures common in most of the core thus far. The lower contact is sharp as a razor with the underlying conglomerate unit but is irregular and the foliation in the volcanic rocks goes around the irregular contact as a result in the much easier to deform volcanic rock.



Strained meta-conglomerate unit. Same as that discribed above. This zone has the appearance of the more "characteristic" conglomerate that is present throughout the area. It is composed of polylithis and coloured clasts from 1mm to the occational >10 cm lithic fragment. All display some level of deformation however most of the unit displays only minor to moderate deforemation. Oriented core for this hole starts at 211 m. The unit displays patchy FexOy staining and weak to moderate magnetism. There is trace carbonate veinlettes, primarily oriented about 60 degrees to c/a. Oriented core measurements in separate excel sheet.

JL08-092 238.65 247.8 MI.dk.pk Strained and altered pre-kinematic mafic dyke: Same as above. The upper and lower contacts could not be oriented, they are however sharp and at low angles to the c/a (Upper:20 degrees Lower:15 degrees). The best forliation is not within orientable core but is about 45 degrees to c/a. Unit is highly altered (act/ser/chl) and non-magnetic.

JL08-092 247.8 282 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures. Small post kinematic dyke at about 265.2 m (see oriented core spreadsheet) same as that described below.

JL08-092 282 286.7 MI.dk.pskFine grained post kinematic mafic dyke: Hard to make out mineralogy due to small grain size, but there appears to be about 35-40% lath shaped plag phenos within a dark matrix which may or may not do the same grain size (hard to tell due to chl/ser/act? altn). Unit is moderatly magnetic. Upper contact is sharp and the lower contact, which probably sharp, is broken core. Unit is not strained. Unit cut by late minor carbonate veins at low angle to c/a (see oriented core spreadsheet).

JL08-092 286.7 299.8 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures.

JL08-092 299.8 300.2 MI.dk.psk Fine grained post kinematic mafic dyke: Hard to make out mineralogy due to small grain size, but there appears to be about 35-40% lath shaped plag phenos within a dark matrix which may or may not do the same grain size (hard to tell due to chl/ser/act? altn). Unit is moderatly magnetic. Contacts are sharp (see oriented core spreadsheet).

JL08-092 300.2 332.65 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures. Unit cut by late quartz veins and calcite veins (see oriented core spreadsheet); carbonate veins usually < 1mm, some quartz vwins up to 1 cm.

JL08-092 332.65 333.05 MI.dk.psk Strained and altered pre-kinematic mafic dyke: Same as above. Unit has 2 sharp contacts and internal foliation and contacts are parallel to main foliation (see oriented core spreadsheet). A few carbonate veins, < 1mm and // to foliation.

JL08-092 333.05 356.05 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures. Unit cut by late quartz veins and calcite veins (see oriented core spreadsheet); carbonate veins usually < 1mm, some quartz vwins up to 1 cm. @ 345 is a 20 cm thick intermediate dyke (see oriented core spreadsheet).


Hole ID From (m) To (m) Lithology Code DescriptionJL08-092 356.05 356.6 MI.dk.pk Fine grained dark green mafic dyke. Unit has two sharp contacts which look like they are altered and

healed faults. Unit contains some light green veinlettes (serp? Act? Ep?) and is magnetic. Grain size too small to identify.


JL08-092 366.7 368.2 MI.dk.pk Medium grained prophyriritic/mafic dyke. Unit contains 10-20% relitc porphyroclasts of a bluish/grey mineral within a finer (medium grained) groundmass. The groundmass itself is composed of ~40% plag and 60% elongate dark green minerals (looks like chloritized hbl?). The groundmass minerals are NOT foliated indicating post-kinematic metamorphism. Unit, inlike the surrounding, are not magnetic. See oriented core spreadsheet.


JL08-092 377.85 378.2 MI.dk.pkStrained and altered pre-kinematic mafic dyke: Same as above. Unit has 2 sharp contacts and internal foliation and contacts are parallel to main foliation (see oriented core spreadsheet).


JL08-092 393.6 394.25 MI.dk.pkStrained and altered pre-kinematic mafic dyke: Same as above. Unit has 2 sharp contacts and internal foliation and contacts are parallel to main foliation (see oriented core spreadsheet).

JL08-092 394.25 403.7 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures. Oriented core stopped at 394 m (crew change, attempting to fix). Unit clearly more strained that was above. Similar styles and types of alteration as above though. Lower contact is sharp and at ~ 60 degrees to c/a and parallel to foliation. Foliation is between 45 and 60 degrees to c/a. Weak late carbonate filled fractures < 1mm.

JL08-092 403.7 405.5 MI.dk.sk Medium grained, equigranular gabbro. Unit dark green from the chl, serp?, act, ser, ep alteration. Can clearly make out 1 mmphenocrysts of lath-shaped plag (~50%) and some (~5-10%) hbl with the rest of the mafics being too altered to identify, but the 50% mafics are probably a mix of hbl and px. Unit here is sheared with foliation the same as the regional foliation. The lower gabbro unit (starting at 410.3m) is unfoliated in the middle with plag phenos in random orientations. In this zone of gabbro, much of the grains are milled due to shearing. Unit is weakly to moderately magnetic and trace py and cpy are present as disseminated and blebby grains. Both contacts are sharp and parallel to foliation. The unit is cut by similar carbonate veins as other units as well as some thin ser, ep alteration veins.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-092 405.5 410.3 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for

structures. Oriented core stopped at 394 m (crew change, attempting to fix). Unit clearly more strained that was above. Similar styles and types of alteration as above though. Lower contact is sharp and at ~ 50 degrees to c/a and parallel to foliation. Foliation is between 45 and 60 degrees to c/a. Weak late carbonate filled fractures < 1mm.

JL08-092 410.3 428.3 MI.dk.skMedium grained, equigranular gabbro. Unit dark green from the chl, serp?, act, ser, ep alteration. Can clearly make out 1 mmphenocrysts of lath-shaped plag (~50%) and some (~5-10%) hbl with the rest of the mafics being too altered to identify, but the 50% mafics are probably a mix of hbl and px. Unit here is sheared with foliation in areas and unfoliated in others. Where unfoliated plag phenos are in random orientations. Where strained, much of the grains are milled due to shearing. Unit is weakly to moderately magnetic and trace py and cpy are present as disseminated and blebby grains. Both contacts are sharp and parallel to foliation. The unit is cut by similar carbonate veins as other units as well as some thin ser, ep alteration veins and some ep+carb. Carb + ep are occationally up to 1 cm. Unit has a sharp lower contact, and is relatively unstrained at that location.

JL08-092 428.3 428.75 MI.dk Mylonitized mafic rock. Thought this looks like a dyke at first glance, I believe it to be a descrete intensely mylonitized portion of the gabbro. The unit is the same mineralogy and has similar alterations. Evidence for this as a healed fault include that the gabbro above and below are not strained while this unit is intensely sheared, this unit is mafic and both contacts are razor sharp. There is not good rock code for this. Foloiation is the same as both contacts.

JL08-092 428.75 436.6 MI.dk.sk Medium grained, equigranular gabbro. Exact same as above. Undeformed at mylonite contact but gets more deformed to lower contact.

JL08-092 436.6 440.5 MT-CO.pl.my Strained meta-conglomerate unit. Same as that discribed above but more strained.JL08-092 440.5 450.3 FI.por.fp Strongly sheared felsic intrusive unit. Unit is red/pink in colour and spotty due to the presense of 1 to

10 mm porphyroclasts of feldspar and quartz within a fg often mylonitized quartz/feldspar matrix. Matrix fg due to milling?? Both contacts are sharp and // to foliation however the lower contact looks to be a fault as what look to be strongly stretched fragments on this unit and intercalated with the lower mylonitized mafic rock. Foliation is 55 to 60 degrees to c/a as are the contacts. FAULT AT LOWER CONTACT.

JL08-092 450.3 459.4 MI.dk.sk Medium grained, strongly sheared, equigranular gabbro. Exact same as above. Intensely deformed, but mineralogy, alteration and magnetism the same at the gabbro. Also, sulfides are the same. Weak carbonate and ep veins as before. Lower contact hard to pin-point, but is // to foliation at about 50 degreea to c/a.

JL08-092 459.4 466.5 MT-CO.pl.my Strained meta-conglomerate unit. Same as that discribed above but yet even more strained to the point where clasts are strained over 20:1. Unit is weakly magnitic and is patchy. Lower contact fairly sharp and at about 45 degrees to c/a. Unit contains a couple 5 to 25 cm thick green dykes (intensely altered and sheared beyond recognition). Alteration style changed a bit to more silica and FexOy staining.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-092 466.5 502 MT-IV Intermediate volcanic rocks - Red-Orange coloured unit composed of altered/metamorphosed

intermediate in composition fine grained rocks. This unit does not display the intense mylnitisation of the above units. This could be due to the unit annealing duting alteration/metamorphism. The unit is somewhat foliated though indicating it was subject to the same strain as the above rocks. The unit is radioactive with cint values on hand specimen between 150 and 800 cps. Unit has been sampled. Occational greenish sheared rock (less radioactive) is present and may represent thin mafic units which are more easily deformed. Oriented core present here (see oriented core spreadsheet). The upper contact is // to foliation and is about 55 degrees to c/a. Sampling from 463 to 481 m incl. sholders. Best zone from 472.5 to 478m. Unit gets less reddish and more greenish away from the mineralized zone. Much of the red-pink alteration looks like ksf alteration which tends to be texturally destructive and may explain why mush of this unit does not look foliated (which is more prominent away from mineralization in the greener rock). The lower contact is broken, but likely sharp. A couple 5

JL08-092 502 510.1 MI.dk.skMedium grained meta-gabbro. Unit is green due to alteration to chl, act, ser, ep minerals and in places weakly yo moderately foliated. I believe this to be the same at the gabbro units above though less magnetic (and patchy at that) and the plag grains are not elongate like the above units. But the unit is still composed of about 40-50% plag and the rest altered mafic minerals, some of which is hbl. There is also trace py. Lower contact is sharp with the coarse-grained felsic intrusive and the gabbro clearly post dates it as there are actually a few 5 to 15 cm xenoliths of the cg intrusive present withint the gabbro and the gabbro is less foliated. The unit is cut be minor thin veinlettes of calcite.

JL08-092 510.1 511.8 FI.por.fpCoarse-grained feldspar prophyritic felsic intrusive: Weak to moderately deformed felsci intrusive with a phrphyritic texture of ~50% large subrounded to rounded phenocrysts of k-feldspar + plag (perhaps kfs>plag) and 5% rounded and somewhat smaller quartzphenocrysts. These are within a finer-grained and altered and sheared groundmass now mostly altered to hbl, bio, ep, magnetite, qtz and plag. Foliations weave around the large feldspar and qtz phenos and average ~ 35 - 40 degrees to c/a. Unit contains some py and also some purple flourite has been seen. Lower contact sharp and at about 65 degrees to c/a.

JL08-092 511.8 512.3 MI.dk.pskSmall slightly more porphyritic (spotty) mafic to intermediate intrusive cuts the cg felsic unit. The unit is not deformes, is fairly unaltered and slightly porphyritic (spotty). It is composed of 60% plag, of which 2/3 of that is prophyritic (0.5 to 1.5 mm) and the rest finetr graned dark mafic minerals including hbl and px (px>hbl) with the remainder of the plag to make up the groundmass. The unit is not magnetic. It is clearly younger than the felsic intrusive and both contacts are sharp.

JL08-092 512.3 513.5 FI.por.fp Coarse-grained feldspar prophyritic felsic intrusive: same as above. Lower contact sharp and at about 70 degrees to c/a


Hole ID From (m) To (m) Lithology Code DescriptionJL08-092 513.5 529.8 MI.dk.pk Fine grained dark meta-basite. Dark-grey green unit that is fine grained, foliated and promarily

composed of plagioclase (30-40%) and dark minerals which are mostly altered to chl, hbl. The unit contains both py and cpy up to 2% combined near the upper contact but generally combined < 0.5%. Near the lower contactr are a 1-5% 0.5mm to 7mm phenos of sub-hedral plag within the fg unit confirming it as an intrusive. The lower contact is sharp and the unit below is intensely deformed for a few cm past the contact (

JL08-092 529.8 572.19 FI.por.fpA dark grey-black coarse-grained feldspar prophyritic felsic intrusive. Weak to moderatly strained Phenocrysts ranging is size up to ~15mm. Composed of rounded to sub-rounded plag, k-feld, and a lesser amount of rounded quartz. Matrix is comprised mainly of biotite +/- hornblende. Small amounts of epidote and flourite (>0.5%). Foliation is week to moderate and appears to weave in and out between the larger phenocrysts, at an angle of ~50deg to c.a.Unit is moderatly magntic. Lower contact is noted by a cross cutting relationship where the felsic intursive unit cuts into the unit below it, indicating that this unit is older than the one beneath it. Contact is irregular, and @ ~45deg to c.a.

JL08-092 572.19 583 MT-MI.fgrA dark green-black, moderatly to highly strained fine grained mafic intrusive unit. Silicious. Matrix supported, composed of biotite +/- hornblende +/- k-feldspar +/-plag. Chlorite infilled in some foliation (~2%) as well as epidote (0.5-1%). Small amts of Calcite present as fracture fills (>0.5%). Quatrz vein ~8-9cm present at 572.69m. K-spar alteration present at 582.90. Beginning at 580.95m, grain size alternates between fine graind and courser grained matrix. Foliation @ 45deg to c.a. U.C described above, L.C not present. Unit is patchy and moderatly magnetic. End of Hole.

JL08-093 0 0.77 OVBD Overburden and casingJL08-093 0.77 7.61 MT-CO.pl Metaconglomerate, dominated by mudstone at top of unit, becoming increasingly mafic with depth.

Top sees occasional quartz and feldspar, high levels of chlorite and epidote. Very blocky and broken from 4.69 to 5m. Small mafic dyke from 4m to 4.22m. Borders upper at 20 degrees to core axis, same at lower contact. As unti becomes increasing mafic, it also decreases in clasts. Very clast poor from 6m to 7.61. Mostly black with occasional "blob" of cooked mudstone. Lower contact borsers at rought 90 degrees to core axis. Trace to weak magnetics. Unmineralized. Occasional carbonaite veinlet.

JL08-093 7.61 19.79 MI.dk.pk Small section of metaconglomerate. Dominated by mudstone chlorite and epidote. Very gradual contacts.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-093 19.79 57.99 MI.dk.pk

Unit begins as fine grained, biotite rich mafic dyke. Some very thin epidote veinlets are visible. This section has not been deformed. As the unit continues, biotite appears to be replaced by horneblende, resulting in a breccia like texture of horneblende phenos in a chlorite rich matrix. Continues to 53.01m. occasional epidote veins. Occasional calcite vein. Occasional quartz and k-spar phenos. Periodic fracture fill carbonate. Large chlorite "blobs" from 55.50 to 56.00m. Becomes finer grained and absent of phenos as it approaches lower contact. Chill zone. Weakly magnetic.

JL08-093 57.99 66.23 MI.dk.por Porphyritic mafic dyke. Porphyrys are rather large (1cm) when compared to usual porphyritic mafic dykes. Biotite rich matrix, with an aura of epidote. Large quartz lens from 59.11 to 59.36. weakly magnetic. Prominent carbonate. Some dissiminated feldspar. Hornblende phenos appear throughout. Contacts are gradual. Unmineralized.

JL08-093 66.23 72.8 MI.dk.pskPost kinematic mafic dyke. Prominent chill zones on both borders, top oriented 85 degrees to core axis, same as bottom comtact. Epidote and feldspar hosting horneblende visible at areas. Biotte rich, prevasive horneblende. Occasional quartz. Some carbonate veins. Sections does not appear to be highly metamorphosed, as there is no alteration. Weaklymagnetic. Unmineralized.

JL08-093 72.8 83.71 MI.dk.por Return to previously describe porphyrytic mafic dyke.JL08-093 83.71 104.54 MT-CO.pl

Highly hematized, and feldspar rich metaconglomerate. Unit is dominated by hematite up to 91 meters, followed by feldspar rich, clast poor section until end of interval. Magnetism is moderate throughout. At 101m, magnetics increase to very intense for a section of 5 cm. Chlorite, epidote and lots of quartz. Carbonate fracture fill common throughout, though increasing with depth. Becomes very quartz rich as approching lower contact, which is oriented 50 degreees to core axis. Upper contact is very blocky. Mylonitic texture, expecially at hematite rich top of interval. Unmineralized.

JL08-093 104.54 107.75 MI.dk Fine grained mafic dyke dominated by carbonate veines. Biotite and horneblande matrix. Veryfine grained. Carbonate veining account for roughly 25% of unit. Very gradual contacts on both end as carbonate veines invade neighbouring units. Non magnetic. Unmineralized.

JL08-093 107.7 133 MT-CO.pl Return to metaconglomerate dominated by feldspar. Small sections of clast poor mineral activity. Rich in carbonate veines near top contact, which is very gradual. Non-magnetic. Appears mylonitic from 110.22 to 110.68, oriented 45 degrees to core axis. Chlorite activity increases with depth, a few fracture fill carbonates towards bottom. Unit becomes less and less hematized with. Becomes very feldspar rich at 125.64 to 128.10.�After this unit looks like usual moderately clastic metaconglomerate. Appears somewhat mafic, moderate levels of biotite. Weakly magnetic.

JL08-093 133 133.45 MI.dk.por Small mafic dyke, borders at 60 degrees to core axis on both contacts. Regular epidote veining, usual tiny (<0.5) feldspar and quartz phenos. Matrix rich in biotite and horneblende. Trace magnetism, unmineralized.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-093 133.45 142.67 MT-CO.pl Feldspar rich metaconglomerate. Feldspar tapers with depth. Usual fracture fill carbonate. Small

amounts of mudstone. Becomes very clast poor with depth. Moderate levels of chlorite and epidote throughout, increases to strong as lower contact is approached. Section from 138 to 140 is highly altered and strained. Consistent quartz clasts.�A few tiny faults located at 137.75 oriented 130 degrees to core axis and 138.90 40 degrees to core axis. Trace magnetism througout. Period section of weak hematization.

JL08-093 142.67 143.23 FI.dk.por Shor felsic dyke. Entirely feldspar save for ~5-7% quartz. Apears moderately strained, small fault at 143.10, oriented roughly parallel to core axis.

JL08-093 143.23 143.5 MI.dk.porSmall porphyritic mafic dyke. Probably shouln't make it it's own form entry, but hey, I'm nuts. You know it, I know it, friggin' the core knows it. I leave tomorrow, and I think I'm going a little nuts. �Appears moderately metamorphosed, Strained to roughly 80 degrees to core axis, as are the contacts. Porpheries dominated by epidote (30%) and feldspar (10%) and quartz (10%). Biotite rich matrix. Some hornblende visible as well

JL08-093 143.5 145 MT-CO.pl Very clast por metaconglomerate. Mineralogy is rich in quartz (smokey). Occasional small feldspar lens. Weakly hematized. Some epidote and chlorite. Moderately strained to 80 degrees to core axis. Some fracture fill carbonate. Somewhat mafic. Moderate biottie.

JL08-093 187 201.6 MT-CO.pl Red-Green highly busted up unit. Containing a lot of chlorite, k-feld. Moderate carbonate veining. Becoming increasingly red and mylonitized downhole. Busted up lower contact.

JL08-093 201.6 227 MI.dk.sk Dark graygreen somewhat porous unit. Contains phenos of ~0.1cm diameter. Rough upper and lower contacts.

JL08-093 227 254.07 MT-CO.pl Dark gray, green red conglomerate. Highly deformed sub-rounded to sub-angular clasts ranging from ~0.2 - 15cm in diameter and containing a lot of k-feld, quartz, epidote, chlorite. Patchy strong magnetism and some large carbonate veins as well as small veinlets generally forming angles of ~40deg and 90deg with core axis.

JL08-093 254.07 256.22 MI.dk.sk Dark gray/black aphanitic syn-kinematic mafic dyke. Contains xenoliths at perifery. A 25cm long section of the unit contains a dense population of ~0.1 - 0.2 cm diameter phenos. Moderat veining-veinlets containing epidote. Upper and lower contacts are sharp making angles of ~35deg to core axis.

JL08-093 256.22 280.18 MT-CO.pl return to previously described conglomerate.JL08-093 280.18 287.07 MI.dk.sk Dark Gray/green to brown felsic intrusion containing a high percentage of phenos with notable k-feld.

Intruding at sharp 70 deg angles to core axis.JL08-093 287.07 307.5 MT-CO.pl Return to previously described conglomerate. Becomes more mylonitic down hole.JL08-093 307.5 308.7 MI.dk.psk Highly strained and altered metamorphosed mafic dyke. Unit is highly foliated and dark green.

Foliation // to contacts. Original mineralogy impossible to identify.JL08-093 308.7 310.1 MT-CO.pl.my Mylonitized conglomerate unit: same above. Rock here is very blocky andof poor quality.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-093 310.1 311.2 FI.por.fp Very rusty and red unit of what appears to be the coarse grained felsic porphyry unit. Unit is weakly to

moderately magnetic. Unit looks like it contains 25-35% white phenocrysts which are stretched and unidemtifiable here within a redish highly altered matrix (and this is seen in < 50% of the unit as alteration has been texturally desrtuctive). Lower contact is broken core.

JL08-093 311.2 318.2 MT-CO.pl.my Mylonitized conglomerate unit: same above. Rock here is very blocky andof poor quality.JL08-093 318.2 320.7 FI.por.fp Very rusty and red unit of what appears to be the coarse grained felsic porphyry unit.: Same as

above. Very messed up rock. Lower contact broken core.JL08-093 320.7 324.4 MT-CO.pl.my Mylonitized conglomerate unit: same above. Rock here is very blocky and of poor quality.JL08-093 324.4 355.4 FI.por.fp Very rusty and red unit of what appears to be the coarse grained felsic porphyry unit.: Same as

above. A few small intensely chl/ep/ser altered mafic units present with sharp contacts and one that cuts // to the c/a. Lower contact at 15 degrees to c/a. This section is far less deformed and one can clearly make out 3 - 5 mm white phenos. The unit is cutby many small green (act? Chl) veins and quartz veins all generally < 1mm thick.

JL08-093 355.4 365.1 MI.dk.pkIntrensely alterd and sheared mafic unit: Dark green unit of intense green alteration (chl/ser/ep/act?). Unit is strongly foliated and the original textures have been completely destroyed due to the alteration and tectonism. Foliation is at ~ 30 degrees to c/a and the lower contact is sharp with and at roughly 35 degrees to c/a. Hematite is seem in the upper portion of this unit and is interpreted to me derived from the above felsic porphyry. Unit cut be minor this veinlettes of carbonate.

JL08-093 365.1 369.2 MT-CO.pl.myBanded mylonite of more felsic rock. Alternating mm scale salmon pink, grey, green, white bands at roughly 40 degrees to c/a. The original texture of the rock has been completely destroyed, however, it is interpreted to be mylonitized conglonerate as this rock type is the only in the area and it makes the most sense. Also, there is rock that looks just like this at the JL camp that clearly is deformed conglomerate. The lower contact is sharp and the same as foliation.

JL08-093 369.2 380.9 MT-IVFine grained metamorphosed and tectonized intermediate in composition rock. Green to green with cloudy reddish overprint of hematite and possibly kfs. Unit is weakly to intensely deformed (though intense is less often) and occationally a few 1 to 2 mm white crystals can be made out giving it a bit of a porphyritic texture in places (where present, the larger crystals only make up about 5% of the rock. The lower contact is sharp and appears to be an old healed fault indicated by a 3 to 7 mm thich brecciated zone between the the two units, also a 3 cm thick green altered rock on the hanging wall of the fault which is likely a small mafic dyke that exploited the weakness in the rocks. The contact and fault and dyke are at 25 degrees to c/a.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-093 380.9 389.9 MT-FV.por Spotty foliated intermediate volcanic porphyritic unit. Pinky unit composed of 20 - 25% fuzzy white

spots, 4 - 8mm within a pink/white groundmass. Much of the original texture has been whiped out due to the intense silica and or kfs alteration and straining of the rock. Lower contact (25 degrees to c/a) is sharp and truncates the foliation. Unit is moderately magnetic with magnetite concentrated in veinlettes.

JL08-093 389.9 390.55 MI.dk.psk Fine grained, undeformed equigranular diabase dyke. Unit is composed of 50% plag and 50% mafic minerals (px>hbl). Unit is weakly magnetic, and contains trace blebby pyrite. Lower contact cuts foliation of the lower unit and is about 25 degrees to c/a. Mafic minerals are chl/ep altered giving the rock a green colour.

JL08-093 390.55 408.1 MT-FV.por Spotty foliated intermediate volcanic porphyritic unit. Same as above the dyke. Lower contact is sharp and cuts foliation at a low angle.

JL08-093 408.1 408.85 MI.dk.pkFine grained foliated and altered mafic rock. The dyke cut the foliatin of the above unit, but it itself is foliated at the same angle as the upper and lower unit. The unit has been altered to chl and ser and ep and act? Giving it a green colour. Plag and the occasional hbl can be made out..

JL08-093 408.85 420.8 MT-FV.por Spotty foliated intermediate volcanic porphyritic unit. Same as above the dyke. The lower contact is sharp and at 55 degrees to c/a

JL08-093 420.8 446.9 MT-IVFine grained foliated intermediate in composition sandstone rock: Fine grained green to green w cloudy red alteration rock. Unit is moderately foliated and cut by numerous magnetite/cartlice veins (calcite in the middle). Also pervasive magnetism away from the veinlettes. Reddish colour due to FexOy staining and poss kfs alteration. Also present are a few course grained mag/hbl/act/py veins and occational cpy is present. The unit gets less reddish with depth. The foliation is roughly 45 degrees to c/a and the lower contact is sharp with a mafic intrusive and folliation is cut by the mafic. In places the unit is somewhat porphyritic with up to 5% 3-8mm plag crystals present. Unit is mineralized and the best zones are 421.25 to 412..6 with avg of ~500 and high of 941 cps; 435.2 to 435.7 acg. 400 and high of 573 cps; 440.2 to 441.2 m with avg of 390 and high of 495 cps. Sampled from 418m in the unit above to 445 m.

JL08-093 446.9 449.3 MI.dk.pk Dark green foliated mafic intrusive unit. This rock of composed of 40% plag, and 60% mafics (px>hbl). The unit is mostly equigranular and green altered (chl/ser/ep). It is moderately magnetic and contains 1-2% disseminated py. The lower contact is sharp and contains fragments of thelower described unit (and thus is younger).

JL08-093 449.3 466 FI.por.fp Coarse grained felsic porphyry intrusive rock. Sheared and metamorphosed coarse grained prophyrytic rock. The porphyries (70% of the rock) are 5 to 15 mm in size and composed of sub-angular to rounded feldspars (plag and kfs with kfs>plag complising 90% of phenos) and rounded and slightly smaller quartz eyes (10% of phenos). The matrix is foliated with foliation weaving around phenos and is composed of feldspar, magnetite, biotite, chl and pink garnet.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-093 466 467.25 MI.dk.pk

Fine grained foliated dark green-grey mafic dyke with xenoliths of the above instiusion and crystals from the above intrusion as well. Unit is fine grained plag (45-50%) and deformed and altered mafics (50-55%). Xenoliths complise 5 to 20% of the unit and large chunks of the granodioriter above are present. The unit is non-magnitic. The lower contact is sharp and cuts the fabric of the below unit.

JL08-093 467.25 471.2 MT-IVFine grained foliated intermediate in composition sandstone rock. Same as above. Unit green to greey-red with the red being clould and from hematite and/or poss kfs altn. Lower contact is sharp and cuts foliation. I'm pretty sure this is that same unit as the mineralized unit above. Radiation levels are slightly elevated with spot highs between 200 and 300 cps. Small slightly deformed equigranular mafic dyke at ~469.5 and 20 cm thick at 15 degrees to c/a.

JL08-093 471.2 471.9 MI.dk.por Dark spotty undeformed mafic porphyritic rock: Phenocrysts complise ~15% of the rock are are lath shaped plagioclase crystals up to 3 mm in length and randomly oriented except near the sharp contacts where they are alligned with the contacts. The matrix is about 45% plag and 55% hbl and px.Trace dis py present. Contacts cut the foliation of the volcanics.

JL08-093 471.9 483.45 MT-IV Fine grained foliated intermediate in composition sandstone rock. Same as above. Unit green to greey-red with the red being clould and from hematite and/or poss kfs altn. Lower contact is sharp and cuts foliation. I'm pretty sure this is that same unit as the mineralized unit above. Radiation levels are slightly elevated with spot highs between 200 and 300 cps. The lower contact is sharp and cuts foliation.

JL08-093 483.45 485 MI.dk.psk Undeformed mafic dyke: Unit is dark grey-green, equigranular and composed of 40% plag, 10% hbl and 50% px. Trace py present andunit is greeninst due to weak chl altn. Lower contact // to upper, is sharp and cuts foliation. Grain size slightly smaller at contacts.

JL08-093 485 495.5 MI.dk.porMix of equigranular mafic dyke, porphyritic mafic dyke and coarse grained felsic intrusive (granodiorite). The unit is mostly the two mafics and contan fragments and crystals from the granodiorite. See descriptions of each above. The lower contact is sharp, but irregular with granodiotire. Foliation primarily in the granodiorite, but faint is present occationally in the mafics.

JL08-093 495.5 517 FI.por.fp Coarse grained felsic porphyry intrusive rock. Sheared and metamorphosed coarse grained prophyrytic rock: Same as above. EOH

JL08-094 0 1.9 OVBD OverburdenJL08-094 1.9 7.88 MT-CO.pl.my Dark grey-black unit, fine grained matrix. Strongly foliated and highly sheared clasts (10-15%) with

selvages of yellowish-brown Ankerite, chlotire +/- biotite. Looks like the conglomerate with sheared clasts, altered rims and metamorphosed. Few clasts of dark silicious material as well as very few localized jasper clasts and low amounts of carbonate clasts, possibly Ankerite. Unit is non-magnetic. UC is not present, LC is at 7.88m @ 65 deg.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-094 7.88 13.58 MT-IV Dark grey intermediate volcanic with a fine grained matrix. Locally moderate foliation present.

Composed of large amounts of biotite, as well as chlorite +/- hematite +/- carbonate. Chlorite and hematite is found mainly in foliations and along fractures and calcite is present in fractures. Unit is cut by a possible chlorite-rich magnetic shear zone or dikelet 8-10cm wide @ 65deg to CA with strong potassic (chl-epid-pot) alteration present in host rock. Unit exhibits patch, weak magnetism overall. UC and Lc are @ ~65 deg and are both gradational.

JL08-094 13.58 15.35 MT-CO.pl.my Dark grey-black unit, fine grained matrix. Moderately foliated and highly sheared clasts (10-15%). Contains Ankerite, chlotire +/- biotite +/- epidote. Looks like the Jacques Lake conglomerate consisting of sheared clasts with altered rims and metamorphosed. Few clasts of dark silicious material as well as low amounts of carbonate clasts and possible clasts of Jasper, Ankerite and/or Calcite.Strong potassium alteration (chl-epid-pot) is present from 14.29m to 15.35m. Unit is non-magnetic. LC @ 45deg.

JL08-094 15.35 21.02 MI.dk Medium-dark grey fine grained homogeneous mafic dike with 5-10% chlorite in matrix. Unfoliated and Non-magnetic. Calcite present in fractures. Epidote present. LC @ 50deg.

JL08-094 21.02 24.6 MT-CO.plDark grey to fruit cake coloured locally clast poor metamorphosed polylithic conglomerate. Typical clast assembalage of moderately sorted, subround to subangular multicoloured mudstone, int. volcanics, felsic volcanics and blebby actinolite, sericite throughout. Veining comprised of pistachio epidote and buff, vuggy qtz-carb. Pervasive silica alteration, patchy very weak hematite alteration, fsp + ser alt as blebs + coating/rimming. Locally very blocky and broken. Occasionally intensely veined/altered by ep/chl/act/ser. Bottom contact is roughly perpendicular t.c.a, but vague due to broken core. Patchy moderate magnetism in clast rich sections. Weak local fabric oriented approx 55 degrees t.c.a. Occasional presure shadow around rounded ser alt fp pheno.

JL08-094 24.6 31.9 MT-IV.por.fp Dark grey aphanitic to very finely porphyritic moderately strained metamorphosed intermediate volcanic. Intensely altered by dull green act, lesser fleshy pink blebby kspar alt. Buff white qtz-carb veinlets throughout the unit. Non magnetic, no sulphides. Fabric oriented 60-65 degrees t.c.a. Occasional thin <20cm dark green fine grained mafic dyke cuts the unit, also one <10cm fleshy pink fien grained felsic dyke.

JL08-094 31.91 41.47 MT-CO.plTypical polylithic metamorphosed polylithic conglomerate, usual brown-green fruit cake apperance. Typical clast assembalage of moderately sorted, subround to subangular multicoloured mudstone, int. volcanics, felsic volcanics and blebby actinolite, sericite throughout. Veining comprised of pistachio epidote and buff, vuggy qtz-carb. Pervasive silica alteration, patchy very weak hematite alteration, fsp + ser alt as blebs + coating/rimming. Locally very blocky and broken. Occasionally intensely veined/altered by ep/chl/act/ser. Fabric oriented approximately 50 degrees t.c.a.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-094 41.47 81.03 MT-CO.pl Dark grey, Felsic meta-volcaniclstic. Typical Jacques lake conglomerate consisting of a fine grained

matrix with abundant clasts of various sizes and compositions. Clasts are sheared and metamorphosed. Contains Ankerite, chlotire +/- biotite +/- epidote. Chlorite and Epidote present in veins and veinlets respectively.. Few clasts of dark silicious material as well as low amounts of carbonate clasts and possible clasts of Jasper, and Calcite. Calcite also present in fractures and veins. Deformation increases with depth. Foliation lies ~60deg t.c.a. Unit has patchy magnetism which is moderate to strong. �Unit is cut by various dikelets which vary in length from 8cm to 12cm. At 47.85m, there is a 60cm dike. It contains two sharp contatcs, ~60deg t.c.a. and contains chlorite and epidote veining. At 62.98m, there is a 97cm long dike. It contains two sharp contacts ~58deg t.c.a and also contains chlorite and epidote veins.��The units LC is sharp, at ~60deg t.c.a and at 81.03m

JL08-094 81.03 87.84 MI.dk.pk Dark green-grey, mafic dike. Moderatly foliated. Foliation ~55deg t.c.a. Contains chlorite and epidote veins and fractures, (ep>ct) as well as hemitate in fractures towards the end of the unit. Contains a low amount of k-feld phenos. (>0.05%) and is moderatly magnetic. UC and LC is sharp, at ~60deg t.c.a

JL08-094 87.84 98.47 MT-CO.pl.myFelsic meta-volcaniclstic. Typical Jacques lake conglomerate. See Above. Foliation is strong. Strong Hemitate alteration present from 88.40m to 89.71. Unit is cut by 8cm dikelet at 91.18m, and a 92cm long syn-kinematic mafic dike at 91.22m, both with a folication ~45 deg t.c.a.�Unit Foliation ~45deg t.c.a. U.C ~ 60deg t.c.a, L.C at 98.47m ~45deg.

JL08-094 98.47 117.16 FI.dk.por Dark grey, medium to fine grained felsic intrusive. Abundant biotite +/- hornblende pervasive throughout the matrix. Unit is weakly foliated @~45deg t.c.a. Calcite present on fractures throughout. Possible k-feld. alteration at 111.70m. Unit becomes more porphyritic with depth, containing larger amounts of feldspar phenocrysts (possibley palg.) comprising 10-12% of the unit. LC is sharp, at 117.16m and ~30deg t.c.a. Unit is non-magnetic.

JL08-094 117.16 121.36 MT-CO.pl.myHighly strained, lesser course grained conglomerate. Highly sheared clasts (10-15%) with selvages of yellowish-brown Ankerite, chlorite +/- biotite. Looks like the conglomerate with sheared clasts, altered rims and metamorphosed. Few clasts of dark silicious material as well as very few localized jasper clasts and low amounts of carbonate clasts, possibly Ankerite. Moderate calcite veining throughout as well as low amounts of blebby pyrite (>0.5%) and low amounts of epidote present in veinsn (>0.5%). L.c is sharp, ~15% t.c.a. Patchy, strong magnetism throughout.

JL08-094 121.36 136.13 FI.dk.por Dark grey, medium to fine grained felsic intrusive. See above. Low amount of undeformed quartz phenos. (>0.5%). Becomes more fine grained with depth.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-094 136.13 137.9 MT-CO.pl.my Highly metrmorphosed and highly strained. Possibly conglomerate with high level of deformation and

various quartz veining (ranging in size from 8-12cm) throughout. Chlorite and epidote veining present. (5-10%). With depth, unit become more fuggey with small amounts of calcite dust on fractures. L.c is irregular. Unit exhibits patchy, moderate magnetism.

JL08-094 137.92 139.72 FI.dk Dark grey, fine grained felsic intrusive..Low amount of phenos.Large amount of epidote veining throughout (stockwork). Unit is patchy, weakly magnetic. No clear foliation present.

JL08-094 139.72 239.67 MT-IV.my Dark green, Highly metrmorphosed and highly strained intermediate volcanic. Banded sand size material (80%) with conglomerate bands (20%) of gravel size clasts with high level of deformation and shearing. Various chlorite and epidote veining throughout (ct>ep). Unit has small amounts of calcite in fractures. Very small amount of a blood red mineral, possibly jasper (>>0.5%). Bandes of magnetite present. Patchy, slight hematite alteration present beginning at 150.03m until 175.48. Chlorite alteration begining at 151.77m and is patchy throughout. At 207.05 hematite alteration begins again.��Unit is cut by a mafic pre-kinematic 40cm dike with sharp contacts and strong foliation (~55deg t.c.a) at 149.32m. Also cut by 40cm a mafic post-kinematic dike at 155.49m. At 176.86 unit is cut by a 22cm spotty pre-kin. mafic dike with strong foliation ~55deg t.c.a. At 206.90 there is a 16cm post kinematic dike. At 221.47 there is a 40cm post-kin. Mafic dike. At 226.78 unit is cut by a 54cm porphyritic felsic dike with irregular contacts�

JL08-094 239.67 241.51 MI.dk.pk Dark green-grey, mafic dike. Moderatly foliated. Foliation ~50deg t.c.a. Contains chlorite and epidote in veins and fractures, (ep>ct). Trace amounts of pyrite present. Calcite in fractures. Unit has patchy, weak magnetism.

JL08-094 241.51 252.52 MT-IV.my Dark green, Highly metrmorphosed and highly strained intermediate volcanic. Various chlorite and epidote veining throughout (ct>ep). Unit has small amounts of calcite in fractures as well as a larger amount of calcite and magnetite banding. Small amount of plag. phenos present throughout (>0.5%). Slight hematite alteration beginning at 242.15m untill 243.72m.��Unit is cut by a 33cm porphyritic felsic dyke at 245.43 with plag phenos (~20%). Also cut by an 83cm porphyritic dyke at 246.15m with 20% plag phenos. Both dykes are moderatly foliated, @~50deg t.c.a.��Unit exhibits patchy, moderate magnetism throughout. ��Unit is mineralized from 242.13 to 242.87 with a high of 280cps and an average of 270cps.

JL08-094 252.52 254.44 FI.dk Dark grey, fine grained felsic intrusive. Moderatly foliated. Abundant biotite +/- horneblend. Low amount of plag phenos, ranging up to 8mm (~5-7%). Calcite present in fractures. Trace amount of diseminated pyrite. L.c is irregular. Unit is non-magnetic.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-094 254.44 280.16 MT-IV.my Dark green-grey, Highly metrmorphosed and highly strained intermediate volcanic. Various chlorite

and epidote veining throughout (ct>ep). Unit has small amounts of calcite in fractures as well as a very small amount of calcite and magnetite banding. Small amount of plag. phenos present throughout (>0.5%). Small amount of possible Barite present. Hematite present in fractures. A 2cm quartz vein present at 256.12 along with a small amount of gypsum and chlorite. Minor chlorite alteration present at 258.14. Slight hematite alteration from 273.46 untill 274.16m.��Unit is cut by a 40cm prophyritic felsic dyke at 263.96m with ~15% plag. phenos.��Beginning at 264.75m, bands of calcite, horneblend +/-actinolite begin to increase with depth unitll 276.05m.��Unit is mineralized from 266.07m untill 267.06 with a high of 500 cps and an average of 300 cps. Unit is mineralized from 266.38 untill 272.52 with a high of 230 cps and an average of 215 cps. Unit is mineralized from 273.44 untill 276.00 with a high of 1320cps and an average of 478cps.��

JL08-094 280.16 283.35 FI.dk Dark grey, fine grained felsic intrusive. Moderatly foliated. Abundant biotite +/- horneblend. Low amount of plag phenos, ranging up to 8mm (~5-7%). Calcite present in fractures. Trace amount of blebby pyrite. L.c is sharp and irregular. Unit is non-magnetic.

JL08-094 283.35 300.61 FI.por.fp A grey-black coarse-grained feldspar prophyritic felsic intrusive. Weak to moderatly strained Phenocrysts ranging is size up to ~19mm. Composed of rounded to sub-rounded plag, k-feld, and a lesser amount of rounded quartz. Matrix is comprised mainly of biotite +/- hornblende. Foliation is week to moderate, at an angle of ~50deg to c.a.Unit is moderatly magntic. Upper contact is irregular, and @ ~65deg to c.a. L.c is sharp, @~60deg t.c.a.��Unit is cut by a 57cm felsic dyke with ~5% plag phenos. And >1% blebby pyrite.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-094 300.61 343.53 MT-IV.my A black-brown, Highly metrmorphosed and highly strained intermediate volcanic. Various chlorite and

epidote veining and blebbs throughout (ct>>ep). Unit has small amounts of calcite in fractures as well as a moderate amount of calcite,magnetite, horneblend +/-actinolite banding, which increase in depth. Hematite present in fractures. Slight hematite alteration begins at 301.05m untill 309.70. ��At 305.26m, unit is cut by a 46cm post kinematic porphyritic mafic dyke with ~15% white plag. phenos, >1mm in size and disseminated, with small amounts of calcite in fractures. U.c is @~58deg t.c.a At 330.55m unit is cut by a 30cm post kinematic porphyritic mafic dyke with ~5-7% white plag. Phenos, >1mm in size and disseminated. U.c @~65deg t.c.a ��Unit has patchy, weak magnetism throughout. ��L.c is @~62deg t.c.a.��Unit is mineralized from 300.80 to 303.90, with a high of 170cps and an average of 140cps. Unit is mineralized from 308.15 to 308.78 with a high of 245cps and an average of 177cps. Unit is mineralized from 320m to 321.80m with a high of 170cps and an average of 134cps. Unit is mineralized from 333m to 335m with a high of 139cps and an average of 116cps. Unit is mineralized fr

JL08-094 343.53 345.28 MI.dk.psk Dark grey-black, post-kinematic mafic dyke, 170cm in length. Contains bands of calcite, horneblende +/- biotite. Calcite also present in fractures. No dominant foliation present. Also contains small amt of chlorite veins and blebbs of chlorite. L.c is irregular.

JL08-094 345.28 367.42 MT-IV.my

A black-brown, Highly metrmorphosed and highly strained intermediate volcanic. Various chlorite and epidote veining and blebbs throughout (ct>>ep). Unit has calcite in fractures as well as a moderate amount of actinolitc veining +/- calcite,magnetite, horneblend untill 348.62m. Trace disseminated pyrite. K-feldspare alteration present at 348.14m. Slight hematite alteration begins at 356.69 untill 361.66mm. Unit has patchy, moderate magnetism throughout. ��At 361.74m unit is cut by a 97cm post kinematic porphyritic mafic dyke with ~20% white plag. phenos, >1mm in size and disseminated. Small amounts of epidote and calcite in fractures. U.c is @~62deg t.c.a, l.c is irregular. Unit is cut at 366.21m by a 41cm post kinematic porphyritic mafic dyke with ~10% white plag. phenos, >1mm in size and disseminated. ��Unit is mineralized from 356.77m to 359.70m with a high of 640 cps and an average of 260 cps.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-094 367.42 368.87 MI.dk.psk

A dark grey, 136cm long mafic dyke with a medium to fine grained matrix of plag., biotite +/- horneblend. Unit is non-porphryitic and non-foliated. Contains calcite in fractures. Is non-magnetic. ��Dyke is cut by a 15cm foliated intermediate volcanic lense at 368.43m as well as a 1cm quartz vein at 368.68m.��L.c is @~62deg t.c.a.

JL08-094 368.87 370.05 MT-IV Reddish-brown, metamorphosed and moderatly foliated intermediate volcanics. Medium to fine grained matrix of mainly biotite +/- horneblend +/- amphibole.No alteration present. Caclite in fractures.�Unit is non-magnetic�Upper contact @~62deg t.c.a. Lower contact is slightly irregular, @~60deg t.c.a.

JL08-094 370.05 371.34 MI.dk.psk Dark grey-black, post-kinematic mafic dyke, 129cm in length. Calcite present in fractures. No dominant foliation present. Also contains small amt of epidote in fractures. �Unit is non-magnetic. �L.c is @~50deg t.c.a

JL08-094 371.34 395 MT-IV.my Dark brown, Highly metrmorphosed and highly strained intermediate volcanic. Banded sand size material (70%) with conglomerate bands (30%) of gravel size clasts with high level of deformation and shearing untill 379.30. Various chlorite and epidote veining throughout as well as epidote in fractures (ep>ct). Unit has small amounts of calcite in fractures. Very small amount of a blood red mineral, possibly jasper (>>0.5%). Pervasive, slight hematite alteration present beginning at 1376.95m until 378.60. Unit is locally vuggy untill 379.30. Unit has patchy, strong magnetism. ��Unit is cut at 382.85 by a 92cm pre-kinematic, foliated mafic dyke comprised of plag, biotite +/- horneblend. Foliation ~57deg t.c.a. Lc @~60deg t.c.a. Unit is cut at 384.34 by a 83cm long pre-kinematic, foliated mafic dyke comprised of plag, biotite +/- horneblend. Foliation ~57deg t.c.a. Lc @~60deg t.c.a. At 386.61 unit is cut by a 57cm pre-kinematic, foliated mafic dyke comprised of plag, biotite +/- horneblend. Foliation ~58deg t.c.a. Lc @~60deg t.c.a.��

JL08-095 0 8.2 OVBD OverburdenJL08-095 8.2 28.29 MI.dk.psk

Moderate-strongly chloritized, poorly foliated, fine-grained to locally med-grained, syn-late-kinematic mafic dike. Unit is vuggy throughout. Chlorite present as a replacement mineral for bt. Plagioclase present as phenocrysts w/n unit which increase in size locally downhole. Minor hematitic replacement of pg phenos local to contact to next unit. Unit has a vuggy-bleached look due to proximaty to surface. Non-magnetic. Upper contact is lost. Lower contact is irregular and poorly defined.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-095 28.29 37.02 MT-IV Strongly hematized, fine-grained, intermediate to mafic volcanics. Due to pervasive hematization

foliation is hard to discern. Hematization is less pervasive downhole. Hematic replacement of pg phenocrysts present throughout. Weak-patchy magnetism. Enclaves of more hematized portion of upper unit found at depth. Upper contact is irregular. Lower contact is at an angle of 56 degrees to C.A.

JL08-095 37.02 41.54 MI.dkMafic dike with strong, pervasive carbonate flooding throughout. Relict texture extremely hard to discern due to pervasivity of carbonate flooding in unit, but with abundant ct present throughout unit it appears to be a mafic dike.Phenos are hard to discern but there is some pg present as phenos in areas. Moderate patchy hematite present with patchy magnetite throughout. Upper and lower contacts are irregular with strongly hematized bands alternating with ct defining them. Lower contact is so irregular that it is hard to get an angle measurement to the C.A.

JL08-095 41.54 46.9 MI.dk.pk Fine-grained to locally coarse-grained, chloritic, weak to moderately foliated, pre-kinematic mafic dike. Unit contains larger phenos of pg ~1cm in size (~1%) as well as fine-grained pg phenos giving the unit a bimodal nature. Foliation is present is not well defined. Minor carbonate present along small micro fractures. Weak patchy magnetism. Upper contact is irregular. Lower contact is at an angle of 60 degrees to C.A.

JL08-095 46.9 58.11 MT-IV Strongly hematized, fine-grained, moderate-strongly foliated, intermediate to mafic volcanics. Hematization is less pervasive downhole. Hematic replacement of pg phenocrysts present throughout. Weak-patchy magnetism. Enclaves of more hematized portion of upper unit found at depth. Upper contact is at an angle of 60 degrees to C.A. Lower contact is at an angle of 65 degrees to C.A.

JL08-095 58.11 86.82 MT-IV Dark-grey, grey-black, moderately foliated, fine-grained, chlorite-rich, flow-banded intermediate to mafic volcanics. Flow texture is strong throughout and is dominated by chlorite-rich (+/- ep) nodules surrounded by hematitic replacement haloes. Matrix is fine-grained making mineralogy hard to discern, possible pg+pyroxene matrix w/ minor micacious mineralogy. Minor vuggy carbonate present locally w/n ct nodules. Upper contact is @ an angle of 65 degrees to C.A. Lower contact is @ an angle of 75 degrees.

JL08-095 86.82 97.06 MT-MI.fgr Dark-grey to black, fine-grained, weakly foliated, flow-textured mafic intrusive.Unit conatins minor randomly oriented px/hb patches throughout. The unit is relatively carbonate-rich along fractures and small mafic cross-cutting diklets. Unit contains 2 small (<10cm) highly chloritized mafic dikes. Minor kspar-alteration between 93.00m-94.00m. Some minor ct along fractures. Matrix is dominantly pg+px+/-hb+/-ct+/-bt. Upper contact is @ an angle of 75 degrees to C.A. lower contact is irregular (gradational) and poorly defined. Weak magnetism.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-095 97.06 106.05 MT-IV Green-grey to grey-red, fine-grained to locally clastic, metamorphosed intemediate volcanics. The

matrix is locally ct-rich surrounding large angular to breciatted clasts of jasperoidal material which are riddled throughout the unit making the protolith hard to discern. Sodic alteration present along faintly foliated areas. Small mafic dikes present (<20cm) b/w 91.05m-101.25m. Minor ep present in broken bands of what was previously intermediate volcanics. Minor carbonate present along small cross-cutting fractures. No definitive foliation present. Iron oxide alteration present throughout. Unit is weakly magnetic in areas where the unit is unoxidized.Upper contact and lower contacts are gradational and hard to discern.

JL08-095 106.05 113.8 MT-IVPink to red, Intensley hematitized and albitized, highly strained, fine-grained intermediate volcanics. Unit pervasively hematized and albitized making mineralogy hard to discern. Lobes of ct bearing rock visable intermittent throughout unit indicating an intermediate nature. Abundant sheared porphyroblasts of mt present that are eliptical indicating strain. Unit is cut locally by a small (<1.00m) highly sheared and chloritized pre-kinematic mafic dike from112.70m-113.28m. Upper contact is gradational. Lower contact is at an angle of 65 degrees to C.A.

JL08-095 113.8 129.42 MT-IV.por.fp Dark grey, grey-purple, strongly foliated and sheared, fine-grained, feldspar porphyritc, intemediate volcanics. Porphyroclasts of fp (k-spar+pg) display hm-replacement throughout unit gradually becoming more prominant downhole. Matrix appears to be pg + mafic mineralogy to fine-grained to distinguish. Foliation defined by banding of micacious mineralogy. Unit also contains abundant porphyroclasts of blue quartz eyes throughout. Unit is moderately magnetic. Abundant mafic dikelets present, some crosscutting foliation some along foliation, containing ct and bt +/- ep. Mafic dikelets are locally albitized in areas. Upper contact is @ an angle of 65 to C.A. Lower contact is broken and lost.

JL08-095 129.42 130.69 MI.dk.sk Chloritic, bt-rich, intensley foliated, fine-grained, pre-syn-kinematic, mafic dike. Foliation is strong and defined by banding of ct+bt. Carbonate present alongfoliation as well as in cross cutting minor fractures which are also locally breciatted. Some minor pg present w/n breciatted regions +/- qz. Minor bands of hematite altered enclaves of the unit above (MT-IV.por.fp) b/w 129.90m and 130.05m. Unit is non-magnetic. Upper contact is broken and lost. Lower contact is at an angle of 58 degrees to C.A.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-095 130.69 150.1 MT-IV.por.fp

Dark grey, grey-purple, strongly foliated and sheared, medium-grained to locally fine-grained, feldspar porphyritc, intemediate volcanics. Porphyroclasts of fp (k-spar+pg) display hm-replacement throughout unit. Matrix appears to be pg + mafic mineralogy to fine-grained to distinguish. Foliation defined by banding of micacious mineralogy. Unit also contains abundant porphyroclasts of blue quartz eyes throughout. Unit is strongly hematized and albitized b/w 130.69m-142.60m. Cut locally by 2 small (<1m) highly chloritized, pre-kinematic mafic dike from 142.60m-143.10m and b/w 149.5m-150.10m. Unit is moderately magnetic. Abundant mafic dikelets present, some crosscutting foliation some along foliation, containing ct and bt +/- ep. Mafic dikelets are locally albitized in areas. Upper contact is at an angle of 58 degrees to C.A. Lower contact is broken and lost.

JL08-095 150.1 171.86 MT-CO.pl Pink-brown to green grey, highly strained, meta-conglomerate. Unit is quite rich in enclaves of felsic meta-vocanics and intermediate meta-volcanics (< 2cm wide). Pervasively chloritized and epidotized in areas. Clasts of japeroid and mudstone are present and are angular to subrounded in shape and vary in size and occurrence downhole. Foliation is defined by thick ep+ct bands as well as banding of micacious mineralogy. Non-magnetic. Upper contact is broken and lost. Lower contact is at an angle of 60 degrees to C.A.

JL08-095 171.86 173.86 MT-IV Dark-grey to grey-black, intensely foliated, fine-grained, intermediate meta-volcanics. Porphyroclasts are of pg+qz and are very fine-grained. Chloritization is present in pervasive patches throughout unit. Foliation is strong and is defined by the banding of micacious mineralogy. Unit is moderate to strongly magnetic. Upper contact is at an angle of 60 degrees to C.A. Lower contact is at an angle of 60 degrees to C.A.

JL08-095 173.86 206.68 MT-CO.plContinuation of the previous MT-CO.pl above but more clast-rich. Pink-brown to green grey, highly strained, meta-conglomerate. Unit contains enclaves of felsic meta-vocanics and intermediate meta-volcanics (< 2cm wide). Pervasively chloritized and epidotized in areas. Clasts are of japeroid and mudstone and are angular to subrounded in shape and comprize 40-50% of the unit locally. Vuggy carbonate present in areas. Foliation is defined by angular clasts and by thick ep+ct bands as well as banding of micacious mineralogy. Non-magnetic. Upper contact is at an angle of 60 degrees to C.A.



Grey-green, ep-rich, ct-rich, moderately foliated, med-grained to locally fine-grained, flow-textured, Hb-porphyritic intemediate to mafic meta-volcanics with enclaves of more intemediate meta-volcanics. Flow texture is comprised of ep+ct+/-bt-altered bands of mafic material which are patchy throughout unit. Some minor Na-alteration + hematite alteration haloes around some of the mafic bands. Porphyroclasts are hb and pg. Hb porphyroclasts are euhedral to subhedral, lathe-shaped to sub-rounded and are roughly 0.5cm-0.75cm in size. Pg porphyroclasts are more fine-grained and anhedral. Foliation is defined by micacious mineralogy. The unit is moderately ct-rich throughout. Unit contains multiple late b/d faults that show a moderate offset of ~2cm. Brittle fault containing gyp+hal with minor carbonate located b/w 239.00m-239.72m. Upper contact is at an angle of 40 degrees to C.A. Lower contact is at an angle of 50 degrees to C.A.

JL08-095 273.5 311.53 MT-CO.pl.my Orange-brown to green-grey, ep-rich, highly-strained to mylonitic, polylithic meta-conglomerate. K-spar alteration is the dominate form of alteration which gives the unit its orange-tan colour. Foliation is intense and is defined by strained clasts of sedimentary and igneous rocks. Strain increases down hole displayed by the obliteration of relict clasts of the conglomerate which follow dominant foliation. Ep+ct define much of the foliaiton w/n the unit +/- bt and other micacious mineralogy. Clasts where present vary greatly in size from 0.5cm to 2.5cm. Minor ~5cm enclaves of intermediate volcanics present intermittent. Unit has patchy magnetism in areas of minor brittle faulting which contain abundant carbonate+massive magnetite. Unit is cut locally by an early, brittle, relithified faults b/w 297.00m-297.48m. Upper contact is at an angle of 50 degrees to C.A. Lower contact is at an angle of 45 degrees to C.A.

JL08-095 311.53 318.81 MI.dk.skChloritic, strongly foliated, fine-grained, syn-kinematic mafic dike. Foliation is intense and is defined by ct + banding of micacious mineralogy. Unit is gauge textured in areas of minor brittle faulting. Upper contact is at an angle of 45 degrees to C.A. Lower contact is at an angle of 48 degrees to C.A.

JL08-095 318.81 326.04 MT-IV Red-pink to grey, well-foliated, strongly albitized and hematized to locally unaltered, fined grained to aphanitic, intermediate meta-volcanics. Unit is intensely potassically altered and hematized giving it an deep red-pink colour. Foliation is prominent and defined by the elongation of relict phenocrysts of pg+/- hb+ct replaced px as well as by the banding if micacious mineralogy. Unit contains abundant, patchy ct intermittent throughout. Unit is cut by a large 1.75m re-lithified brittle fault from 324.27m-326.04m. Upper contact of main unit is at an angle of 48 degrees to C.A. Lower contact is 52 degrees to C.A.

JL08-095 326.04 329.62 MI.dk.pskGreen-grey to black, weakly foliated, fine-grained, late-post-kinematic mafic dike. Matrix is fine-grained and undiscernable but more or less mafic. Foliation where present is defined by micacious mineralogy (bt+ct). Minor hematitic alteration present patchy throughout. Unit contains small anastamosing, cross-cutting, chlorite-rich, mafic, micro-vienlets riddled throughout. Weak patchy magnetism present. Upper contact is at an angle of 52 degrees to C.A. Lower contact is indistinct.



Grey-pink to grey-green, moderately foliated, fine-grained, flow-textured intermediate meta-volcanics. Porphyroclasts are fine-grained pg+ chlorite altered mafic mineralogy which is quite fine-grained. Unit contains small anastamosing, cross-cutting, chlorite-rich, mafic, micro-vienlets riddled throughout giving the unit a webby, almost breciatted texture. Foliation is moderate and is defined by the banding of micacious mineralogy such as bt and ct. Hematitic atleration is present in massive patches throughout giving the unit a more reddish-pink colour. Potassic alteration also present patchy throughout giving a fleshy-tan colour to the unit. Upper contact is hard to distinguish. Lower contact is at an angle of 45 degrees to C.A. Patchy magnetism.

JL08-095 332.9 334.86 MI.dk.skChloritic, moderately foliated, fine-grained, syn-late-kinematic mafic dike. Phenocrysts are of pg+altered mafic mineralogy and are fine-grained. Foliation is defined by banding of micacious mineralogy. Unit contains abundant ct as phenocrystic replacement of mafic mineralogy as well as along foliation, in swathy bands and w/n small webby x-cutting minor mafic dikelets throughout unit is weakly magnetic. Contains abundant pyrite disseminated throughout as well as in massive blebs locally which are around 0.5cm in size. Upper contact at an angle of 45 degrees to C.A. and is well-defined. Lower contact is also well deined and at an angle of 40 degrees to C.A.

JL08-095 334.86 338.86 MT-IV Continuation of previous intermediate meta-volcanic unit. Unit display brittle ducitle nature with small local micro-faulting with ~ 1.5cm offset. More pevasive postassic alteration present w/n flow-textured portions of the unit. Carbonate present w/n small micro fractures ~0.3cm wide. Unit is weakly magentic.

JL08-095 338.86 341.16 MI.dk.skChloritic, bt-rich, moderately foliated, fine-grained, pre-kinematic mafic dike. Unit contains abundant phenocrysts of hb around 0.2cm in size as well as finer-grained plag. Webby chlorite throughout. Ct is also present with bt along dominant foliation in unit. Unit is weakly magnetic. Upper contact is at an angle of 57 degrees to C.A. Lower contact is at an angle of 50 degrees to C.A.

JL08-095 341.16 383.23 MT-IV Pink-green to grey, well foliated, fine-grained, intermediate meta-volcanics. Matrix and pheno mineralogy hard to discern due to the units fine-grained nature. Unit is locally ct-rich in areas as well as potassically altered throughout which gives a green to fleshy pink colour to the unit. Foliation is dominated by the banding of micacious mineralogy such as bt+ct. Unit is relatively carbonate rich. The carbonates occurrence is blebby to disseminated local fracture-filled intervals throughout unit. Small <15cm carbonate-rich, strongly foliated, fine-grained, syn-kinematic mafic dikes present throughout unit. Moderately magnetic. Unit has moderate u-mineralization b/w 367.38m-368.52m with a max: 510cps, avg: 232cps, and also b/w 372.69m-375.00m with a max: 397cps, avg: 261cps. Oriented core, Alpha angle for carbonate vein at 380.37m is at an angle of 45 degrees to C.A. Beta angle for carbonate vein is degrees to C.A. Upper contact is at an angle of 50 degrees to C.A. Lower c


Hole ID From (m) To (m) Lithology Code DescriptionJL08-095 383.23 385.74 MI.dk.psk Fine-grained, post-kinematic leuco-gabbro. Unit is moderately fresh and unaltered with no prominent

foliation. Pg phenocrysts create a leopard texture with the mafic matrix. Pg phenos are cloudy-white and around 0.1cm in size. Unit is weakly magnetic. Upper contact is at an angle of 40 degrees to C.A. Lower contact is at an angle of 65 degrees to C.A.

JL08-095 385.74 401.21 MT-IVContinuation of the previous MT-IV unit (341.16m-383.23m). Foliation is weak to locally moderate and is defined by the banding of micacious mineralogy. U-mineralization has ceased w/n this particular unit. Unit contains two enclaves of fine-grained felsic igneous rock b/w 394.90m-395.21m and b/w 395.86m-396.02m. Unit contains local coarser lathe-shaped pg phenos that are roughly 0.5cm-0.8cm. Ct-content is increasing as contact to next unit is approached. Ct occurrence is small blebs to flowing migmatitc swaths. Magnetism is strong in this unit.

JL08-095 401.21 402.89 MI.dk.porModerately Chloritic, unfoliated, coarse-grained to locally fine-grained, post-kinematic mafic dike. Phenocrysts are dominantly lathes of pg that vary from 0.1cm in size locally to 1.5cm. The phenos of pg are cloudy-white and transluscent. Some of the grains display nucleation around a central pheno possible slower grow intervals throughout the intrusives history. There are also finer-grained phenos of ct-altered pyroxene. The px pheno occurrence is in small 0.2cm rounded to subrounded grains with little to no visable cleavage. Matix is comprised of fine grained pg and px+ct as well as fe-rich bt. Weak patchy magnetism. Minor disseminated pyrite present. Upper contact is at an angle of 55 degrees to C.A. Lower contact is broken and lost.

JL08-095 402.89 426.4 MT-IVDeep purple-green to grey-black,moderately foliated, fine-grained, intermediate to mafic meta-volcanics. Matrix and pheno mineralogy hard to discern due to the units fine-grained nature. Unit is locally ct-rich in areas giving a green to colour to the unit. Foliation is dominated by the banding of micacious mineralogy such as bt+ct. Unit contains small enclaves of fine-grained felsic intrusive b/w 411.18m-411.44m and b/w 411.84m-412.62m. Felsic intrusive is pg+qz rich with hb phenos. Hb phenos are black and bladed and ~0.2cm in size. The occurrence of MT-FI is syn-late-kinematic with some of the material following the dominant foliation within the MT-IV unit. Matrix of MT-FI is fine Ct-rich swathes of more mafic material occur proximal to contact of next unit rock Unit is relatively carbonate rich. The carbonate occurrence is blebby to disseminated local fracture-filled intervals throughout unit which contain blebby pyrite +/-cpy. Moderately magnetic. Upper contact is broken and lost lower contact is gradational and unmeasurable b/w the next unit.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-095 426.4 429.2 MI.dk.por

Moderately Chloritic, unfoliated, coarse-grained to locally fine-grained, post-kinematic mafic dike (mela-gabbro). Phenocrysts are dominantly lathes of pg that vary from 0.1cm in size locally to 1.5cm. The unit overall has a dominantly bimodal nature with variant sized phenocrysts of pg. The phenos of pg are cloudy-white and transluscent. Some of the grains display nucleation around a central pheno possible slower grow intervals throughout the intrusive history. Possible two generations of of post-kinematic mafic dikes within this unit based upon the variant texture and size of the phenos of pg. Finer-grained phenos of ct-altered pyroxene present. The px pheno occurrence is in small 0.2cm rounded to subrounded grains with little to no visable cleavage. Matix is comprised of fine grained pg and px+ct as well as fe-rich bt. Weak patchy magnetism. Minor disseminated pyrite present. Upper contact is gradational and irregular lower contact is broken.

JL08-095 429.2 433.71 MT-IVPink-white to grey, moderately foliated, fine-grained, intermediate meta-volcanics. Phenocrysts are of cloudy white pg aroubdwhich comprizes ~2% of the unit. The matrix is more chloritic to bt-rich. Unit appears to have been cooked by the mafic dike above and below it which is reflected in the locally massive (concentration) occurrence of the pg in areas. Upper contact is broken lower contact is sharp but irregular and unmeasurable. Moderate patchy hematization and magnetite.

JL08-095 433.71 438.85 MI.dk.por Moderately Chloritic, unfoliated, coarse-grained to locally fine-grained, post-kinematic mafic dike (mela-gabbro). Phenocrysts are dominantly lathes of pg that vary from 0.1cm in size locally to 1.5cm. Same as mafic dike unit b/w 426.4m-429.2m. Upper contact is irregular but roughly at an angle of 40 degrees to C.A. Lower contact is at 40 degrees to C.A.

JL08-095 438.85 456.95 MT-IV Deep purple-green to grey-black,moderately foliated, fine-grained to locally medium-grained, intermediate to mafic meta-volcanics. Matrix and pheno mineralogy hard to discern due to the units fine-grained nature. Local cludy white 0.3cm mgr of pg present. Unit is locally ct-rich in areas giving a green to colour to the unit. Foliation is dominated by the banding of micacious mineralogy such as bt+ct. Unit contains a small enclaves of fine-grained felsic intrusive b/w 444.78m-444.97m that is well deformed and sheared. Matrix of MT-FI is fine Ct-rich swathes of more mafic material occur proximal to contact of next unit rock Unit is relatively carbonate rich. The carbonate occurrence is blebby to disseminated local fracture-filled intervals throughout unit. Moderately magnetic. Unit contains minor U-mineralization b/w 452m-452.40m with a max of 609cps and a avg: 404cps. The mineralized zone is well breciatted and Na-altered with mt veinlets riddled throughout. The breciation and mineralization appears to be caused by a small 30cm long by 3cm wide felsic intrusive vein. Upper contact isat an angle of 40 degrees to C.A. lower contact is at an angle of 75 degrees to C.A.

JL08-095 456.95 458.1 MI.dk.por Un-foliated, fine-grained, post-kinematic melagabbro. Phenocrysts are ~0.2cm cloudy-white, lathe-shaped grains of pg which have a peppered-like random occurrence throughout. Matix mineralogy is fine-grained and likely px+pg. Patchy strong magnetism. Upper contact is 75 degrees to C.A. Lower contact is broken and lost.



Deep purple-green to grey-black,moderately foliated, fine-grained to locally medium-grained, intermediate to mafic meta-volcanics. Matrix and pheno mineralogy hard to discern due to the units fine-grained nature. Local cloudy white 0.3cm mgr of pg present. Unit is locally ct-rich in areas giving a green to colour to the unit. Foliation is dominated by the banding of micacious mineralogy such as bt+ct. Unit contains a small x-cutting portion of the mafic dike unit below this one from 459.26m-459.45m. Upper and lower contacts are broken and unmeasurable.

JL08-095 460.52 463.29 MI.dk.pskUn-foliated, fine-grained to locally mgr, post-kinematic melagabbro. Mgr and fgr phenocrysts are ~0.2cm to locally 0.4cm cloudy-white, lathe-shaped grains of pg which have a peppered-like random occurrence throughout. Matix mineralogy is fine-grained and likely px+pg. Patchy strong magnetism. Upper contact is broken and lost. Lower contact isat an angle of 58 degrees to C.A.

JL08-095 463.29 492 MT-IVDark grey-green, pink-purple, weakly foliated, fine-grained to locally med-grained, intermediate to mafic volcanics. Unit is locally ct-rich in the more mafic portions.The dominantly mafic and is locally cut by small (<15cm) pre-kinematic mafic dikes throughout. Sparse 0.3cm subhedral, cloudy-white pg phenocrysts are local throughout. Pg is mostly concentrated along swathing bands throughout which also contain small (0.1cm) lathe-shaped phenos of what appears to be actinolite. These bands are anastamosing and random in their orientation sometimes mirroring the weak foliation. Minor hb present in mafic regions of the unit. It appears to be a replacement mineral for px. The unit contains moderate patchy to locally massive amounts of ep. Ep occurrence is as an alteration mineral w/n the mafic dikes. The unit has strong pervasive magnetism. Trace carbonate locally throughout. Upper contact is at an angle 58 degrees to C.A. no lower contact (EOH: 492.00m).

JL08-096 0 0.7 OVBDJL08-096 0.7 4.8 MT-CO.pl Strained and metamorphosed polylithic gravel/conglomerate. Gravel sized (occationally larger) sub-

angular to sub-rounded clasts of various lithologies which is clast supported and with a matrix of finer grained material. Unit is moderately straine stretching all clasts. Unit is mottled white and non-magnetic. Unit is cutmy minor late veinlettes of quartz and calcite. The lower contact is broken but likely sharp.

JL08-096 4.8 49.5 MI.dk.pkPorphyritic and strained mafic intrusion: Dark green with stretched 3 to 12 mm mostly biotite/chl altered hbl phenocrysts within a fine grained matrix. The matrix is conposed of plag and dark mafic mineral(s) which are too altered and deformed to make out. Unit is patchy moderate magnetism and contains trace dsm py. The hbl phenos are in places fresh enough to tell for sure that they are hbl.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-096 49.5 53.3 MI.dk.psk Dark grey aphanitic diabase dyke: Featureless fine-grained dark-grey green mafic dyke. Has two

sharp contacts though the upper is broken core, The lower contact is sharp and has 2 cm altered of alteration. The units greenifh colour is due to fine grained chl alteration. Unit is moderately hard and has a weak pervasive magnetism. Unit cut by minor calcite veins.

JL08-096 53.3 56 MI.dk.pskUndeformed dark greenish hbl porphyritic mafic dyke. Similar mineralogy to the previously described hbl porphyry, but undeformed and relatively unaltered anf smaller phenocrysts. The lower contact is hard to pinpoint with an aphanitic unit and suggests that they are the same. The sharp upper contact may represent multiple pulses of dyking at this time. The unit alsodisplays the same alteration minerals and weak pervasive magnetism as the aphanitic unit.

JL08-096 56 64.9 MI.dk.psk Aphanitic diabase dyke (undeformed): same as above.JL08-096 64.9 74.4 MI.dk.pk Porphyritic and strained mafic intrusion: Dark green with stretched 3 to 12 mm mostly biotite/chl

altered hbl phenocrysts within a fine grained matrix. Same as aboveJL08-096 74.4 79.55 MI.dk.psk

Undeformed meduin grained dark grey with white spots plagioclase porphyrytic mafic dyke: Unit composed of 20% phenocrysts of white 1 to 5 mm plagioclase within a finer grained matrix of interlocking plag and dark mafics now altered to chl, ser and act. Magnetism is strong and the unit is grades from aphanitic on near the contacts to coarser grained and porphyritic in the middle.

JL08-096 79.55 86.3 MI.dk.pk Porphyritic and strained mafic intrusion: Dark green with stretched 3 to 12 mm mostly biotite/chl altered hbl phenocrysts within a fine grained matrix. Same as above. Lower contact is broken, but likely sharp.

JL08-096 86.3 90.6 MI.dk.psk Undeformed meduin grained dark grey with white spots plagioclase porphyrytic mafic dyke: Similar to the above feldspar porphyritic mafic rock. Unit here is composed of 1-2% large (3 to 15mm) long plagioclase withing a finer grained, yet still medium grained, equigranular matrix of interlocking plag (40%) and dark mafics (60%) now altered to chl, ser and act. Hornblende is clearly a magor constituent of the matrix. Magnetism is strong and the unit is grades from aphanitic on near the contacts to coarser grained and porphyritic in the middle.

JL08-096 90.6 94.8 MT-CO.plStrained and metamorphosed conglomerate unit: Unit of poorly sorted polylithic deformed clasts from sand sized to 7 cm long (after straining). The unit takes on a mottled appearance with make colours due to various altertion styles (both pre- and after deformation. Unit is generally hard and usually has some pink/red-brown colour to it from FexOy staining and/or kfs altetration.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-096 94.8 126 MT-IV

Fine-grained deformed and altered intermediate sandstone/volcaniclastic rock: Unit is banded greeny and red-brownish in colour and deformed. It is hard due to kfs alteration +/- silica alteration. The unit is weakly magnetic and some of the redish colour is from FexOy staining. The red-brown/green alteration is texturally destructive, as kfs alteration tends to be. The lower contact is not a lithological contact, it is the same rock, just a shift in alteration style and the contact is gradational over a few metres. 40 cm altered and deformed mafic dyke at 123 m (70 degrees to c/a).

JL08-096 126 146.59 MT-IV Fine-grained deformed and altered intermediate sandstone/volcaniclastic rock: Same as above, but kfs and act alteration minor. Unit looks like a banded sandstone (which is probably what it is rather than a volcanic rock). Some intense folding is present. Unit here is more of a pale grey-green colour. Unit is not magnetic here. Though the unit is banded, orientation with respect to c/a is variable over short distances.

JL08-096 146.59 152.74 MT-CO.pl Unit borders on top at 135 to core axis. Begins as feldspar rich, tapers quickly (by 147.60m) to clast poor metaconglomerate. Occasional chlorite clasts surrounded by mudstone. Periodic feldspar and quartz phenos. Biotite rich matrix. Fracture fill carbonates consistant throughout unit. At 150.78m see a porphyritic type texture rich in feldspar phenos, Slightly strained to 130 degrees to core axis. 152.25 sees return to feldspar rich matrix with quartz phenos. Borders at bottom at 125 degrees to core axis. Non magnetic.

JL08-096 152.47 152.95 MI.dk.psk Fine grained post kinematic mafic dyke. High levels of epidote and biotite within matrix. Moderate levels of angular, crystal like quartz and feldspar. Very short. Non magnetic. No straining. Borders at bottom at 45 degrees to core axis.

JL08-096 152.95 155.51 MT-FV.por Coarse grained felsic vocanics with usual feldspar and quartz phenos. Only one or two blue quartz eyes, the rest of quartz is white. Occasional "blob" of epidote and chlorite. Non magnetic. Strained to roughly 130 degrees to core axis. No foliations.

JL08-096 155.51 188.64 MT-CO.pl Unit begins as moderately clast poor, from 168 to roughly 170 sees very clast poor with intense carbonate fracture filling. Returns to previously describe clast poor conditions afterwards, with no carbonate fracture filling. At 176.35m become very clast rich inapredominately epidote matrix. Clast sizes range from <0.5cm to 2 cm. Mineralogy is predominatley epidote, feldspar, chlorite quartz and some mudstone.�Starting at 188m begins to be highly strained to 50 degrees to core axis. Core is blocky and broken over lower contact. Non magnetic.

JL08-096 188.64 193.06 MT-FV.por Reutrn to previously described unit of metamorphosed felsic volcanics. A few small sections of very pale pink, almost grey. Material is strained to 50 degrees to core axis, though many factures seen at roughly 100 degrees to core axis. Usual phenos of quartz and feldspar. Increased chlorite and epidote occurances with depth. Appear to be fracture fill occurances. Colour flip flops back and foth from a light pink to a dark grey, biotite rich texture. At ~190, texture changes to porphyritic, with small (<0.5cm) phenos of quartz and feldspar.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-096 193.06 195.59 MT-CO.pl Metamorphosed conglomerate. Mineralogy consists of epidote, chlorite, quartz, feldspar, biotite, and

a few fracture fill carbonates. Section is strained moderately to 45 degrees to core axis from 194.28 to 194.66. Outside of this interval, little to no straining, and no common orientation. Becomes quite clast poor, poorly consolidated towards lower contact which borders sharply at 60 degrees to core axis. Non magnetic

JL08-096 195.59 208.59 MT-FV.por Medium pink k feldspar matrix with abundant blue quartz eyes, white quartz and feldspar phenos. Phenos are oriented 120 degrees to core axis, suggesting some straining. This straining tapers by 201m. From top contact to ~202m, there is an almost sandy colour to the matrix, and apears to be some disseminated mud +/- sandstone. Lower contact is sharp and oriented 120 degrees to core axis. Non magnetic.

JL08-096 208.59 209.33 MI.dkSmall medium grained mafic dyke. Section is blocky and broken. High levels of epidote, and biotite. Some fracture fill carbonate. Doesn't appear to be strained. Moderately magnetic.

JL08-096 209.33 231.71 MT-CO.pl.mymylonitized metamorphosed conglomerate. Mineralogy is dominated by fledspar, epidote and biotite. Other minerals include quartz, chlorite, and some fracture fill carbonate. Fabric strained to 70 degrees to core axis. Blocky and broken over several intervals within unit. Large feldspar lense on lower contact, 9cm, 70 deg to CA. Starting at 230, unit becomes quite clast poor. Majority consists of epidote with feldspar halos within what appears to be a highly mafic matrix.

JL08-096 231.71 232.39 MI.dk Light grey/green mafic dyke. High levels of dsm epidote. Biotite is actively being replaced by horneblende. Some secondary migmatite visible from 231.92 to end of unit. Moderately metamorphosed. Weakly magnetic.

JL08-096 232.39 283.16 MT-CO.plVery large section of metamorphosed conglomerate. Section attop contact, which borders sharply at 110 degrees to core axis, has a few short (<0.5m) of metamorphosed volcanics with phenos of quartz and feldspar. Material is oriented 75 degrees to core axis. Volcanics are absent from 234.72 and on, but shows up again at 238.54 to 238.73. Mineralogy throughout is the usual mish-mash of minerals, including feldspar, quartz, epidote, chlorite, mudstone, sandstone. Small amounts of andesite in a few spots, towards lower contact with a "leopard skin" like texture. Clast size is generally large (1-2cm), though reduced to 0.5cm in small sections. 247.66 to 247.87 is a feldspar lens. Occasional rosy carbonate, along with some fracture fill white carbonate. Lower contact is very gradual, at ~ 120 degrees to core axis. Non magnetic, unmineralized.

JL08-096 283.16 357.98 MT-CO.pl.my Continuation of previously described metamorphosed conglomerate, however unit is now mylonitized. Strained to a 30 degrees throughout. Same mineralogy as previous unit.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-096 357.98 359.61 MI.dk.por Porphyritic mafic dyke. Fine grained chill margins, increased grain size towards middle of unit. High

levels of chlorite. Slicken slides visible in breaks. Moderately strained to 60 degrees to core axis. Some small carbonate veines. Small porhyrys (<0.5cm), of chlorite and epidote. Matrix is predominantly biotite and chlorite. Top and bottom contact borders sharply at 75 degrees to core axis.

JL08-096 359.61 401.36 MT-CO.pl.my Reutrn to mylonitized metaconglomerate. Unit has usual assortment of quartz, feldspar, chlorite, epidote, chert (grey and red) some hematite, and carbonate. Material is strongly to moderately strained to 35 degrees to core axis. Some pink carbonate, though mostly white. At 370.23m some army green calcite and pink carbonate with a "bubbly" texture. Some shphalerite scattered thoughout interval. Small levels of magnetic hematite. Unmineralized.

JL08-096 401.36 401.72 MI.dk.pkMedgrained pre-kinematic mafic dyke. Section is very broken and blocky. Sharp contact on top at 70 degrees to core axis. Highly chlorotized. Some epidote oriented 70 degrees to CA as well. Some horneblende, weak. Some "chunks" of feldspar. Lower contact borders at 70 degrees as well

JL08-096 401.72 423.61 MT-FV.por Metamorphosed porphyritic volcanics. Quartz and feldspar phenos are coarse. Few blue eyes quartz phenos, but show up consistantly. Unit is cut by a small felsic dyke at 404.20 to 404.56. Dyke contains epidote. Unit immediately on either side also contains this epidote and chlorite. White quartz crystals are large and sub angular. Some fracture fill chlorite and epidote is visible throughout unit. Over all red colour. Little to no straining. Upper contact is sharp at 70 degrees to core axis. Unit is non magnetic.

JL08-096 423.61 436.18 MI.dk.pk Pre-kinematic mafic dyke, foliations oriented 40 degrees to the core axis. Upper contact is located in a very blocky and broken section. Lower contact is gradual, oriented at roughly 40 degrees to core axis. Mineralogy consists of strong epidote, moderate horneblend which is replacing biotite. Biotite levels are weak. Slightly chloritic. Tiny amounts of feldspar and quartz. Some small fracture fill carbonates. Some disseminated magnetite. Unit is moderately, to strongly magnetic. Unmineralized.

JL08-096 436.18 450.7 MT-CO.pl Reutrn to metamorphosed conglomerate. Unit is strained to 40 degrees to core axis, but clast are still visible. Not quite mylonitic. Mineralogy assemblages of quartz, feldspar, epidote, chlorite, some biotite, serpentine. And carbonate. Clast intensity is generally rich, though section from 447 to 448m is clast poor, dominated by epidote veining. Occasional mudstone is visible. Some patchy magnetism, though overall, unit is non mineralized. Some slicken slides visible on breaks. Unmineralized.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-096 450.7 457.76 MT-CO.pl.my Highly strained and metamorphosed conglomerat with clasts of various sizes and various lithologies.

Many clasts are gravel sized with a few larger..Clast supported and with a matrix of finer grained material. Most clasts have been highly sheared and altered. Foliation @~42deg t.c.a. Chlorite, epidote and minor calcite in fractures (Ct>Ep)�Strong potassic alteration beginning at 450.98m until 454.48m. �Unit has patchy, weak magnetizm. L.c is irregular, @~37deg t.c.a.�At 453.56m, unit is cut by a small, re-lithofied fault containing host rock materal(post-kin to the host rock fabric)�At 456.40m unit is cut by a 37cm mafic intrusive with hematite and cholrite in fractures as well as localized potassic alteration (possibly due to remobilization of elements due to fluid flow). Does not have strong foliation.

JL08-096 457.76 468.04 FI.dkDark gray to red unit. Strong chlorite alteration at 460.25m. Hematization at 461.70m. Weak to moderate patchy magnetism. Irregular upper and lower contacts. Localized potassium alteration. Contains trace calcite fractures, some hematization on fractures, chlorite, epidote, hornblende.

JL08-096 468.04 471.96 MT-CO.pl.myreturn to previous moderately mylonitized sheered and altered conglomerate. Upper contact is irregular, lower contact is broken and irregular . Containing some calcite veining.��Contains Post-kinematic mafic dyke intruding at 469.74 - 470m with phenos ~0.05cm in size with minor hematite veinlet and more plag-rich down hole. Sharp upper and lower contacts ~46deg t.c.a.

JL08-096 471.96 480.22 MI.dk.psk Green unit strongly deformed and veined with chlorite and epidote. Non foliated. Broken upper contact and sharp lower contact ~50 deg t.c.a. weakly magnetic.

JL08-096 480.22 484.29 MT-CO.pl.myMulti-colored, highly metamorphosed conglomerate. Clasts are varoius lithologies and have been highly deformed and altered. Hard to determine the clast lithologies. Dominant foliation @~52deg t.c.a. Minor fracturing and shear zones throughout. Unit contains various chlorite and epidote veining, as well as calcite and epidote in fractures. Unit is non-magnetic. L.c is sharp, @~53deg t.c.a.

JL08-096 484.29 486 MI.dk.sk Black to dark gray-green unit. With sharp upper contact ~54 deg t.c.a. and moderately graded lower contact. Non-magnetic. Contains some xenolith (k-feld + others) action from the adjacent conglomerate unit.

JL08-096 486 487.66 MT-CO.pl Return to previous conglomerate. Weak patchy magnetism. Contains feldspars, epidote, chlorite all highly metamorphosed. Broken messy upper and lower contacts.

JL08-096 487.66 488.57 MI.dk.psk Dark gray-black mafic dyke exhibiting some small veinlets containing epidote. Some hematization in fractures. Lower contact is gradational. Some bands of next unit alternating with dyke. Non-magnetic.

JL08-096 488.57 490.8 FI.por.fp Red aphanitic highly potassic unit. Exhibits veins containing epidote, calcite, quartz, sericite with a general orientation of ~40 deg t.c.a. Contains phenos ~0.2 - 0.4 cm in diameter.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-096 490.8 491.68 MI.dk.sk Dark gray-black mafic dyke with sharp slightly irregular upper and lower contacts making angles of

~65 deg and ~35deg t.c.a. respectively. Some inclusions of neighboring unit. Approx. 5% phenos plag ~0.1 - 0.3 cm.

JL08-096 491.68 492.38 FI.por.fpReturn to felsic unit. Upper and lower contacts are roughly gradational over 4 and 6 cm, respectively. Upper contacti is heavily veined with adjacent dyke. Contains some vienlets with epidote.

JL08-096 492.38 513.85 FI.por.fp return to red felsic/potassic unit. Unit fades near the center to a lighter pink and switches back to a deeper red downhole. Contains phenos( 0.1- 0.3 cm) in patches. Becomes very porphyritic (20% phenos) at end of unit. Highly stockwork veined, viens contain chlorite, epidote, +/- sericite, +/- quartz. Some fractures containing calcite.

JL08-096 513.85 515.08 MI.dk.skDark gray/green to black. Moderate to heavily viened. Veins contain chlorite, epidote, some fracture-fill from adjacent felsic unit. Contains a lens (27cm wide) of said felsic unit with irregular contacts.

JL08-096 515.08 541.75 MT-CO.plReturn to metamorphosed conglomerate. Moderatly foliated. Unit is fractured (shear zone) and contains a minor fault with a 4cm offset at 524.39m depth. Contains a mafic post-kinematic dyke at 527.55 - 528.10 m depth. Moderate veining containing chlorite, calcite. Contains a few roundedclasts in places. Unit becomes increasingly mylonitic with depth. Unit is vuggy in places. Calcite in fractures.��Lower contact of the conglomerate is in contact with a 23cm foliated pre-kin. Mafic dyke.L.c of the conglomerate is irregular and sharp, @~40deg t.c.a. L.c of the dyke is sharp, @~44deg t.c.a.��Unis is non-magnetic.

JL08-096 541.75 543.53 FI.por.fp Dark red, highly altered (hematitie alteration) Feldspar Porphyry. Contains ~5-7% phenos of plag with hematite rims, and ~5% phenos of k-feld. Contains epidote and calcite in fractures. Unit is moderatly magnetic and weakly foliated @~30deg.�L.c of unit is sharp, @~40deg t.c.a.

JL08-096 543.53 544.87 MI.dk.porDark grey-black, very porphyritic mafic dyke containing weak to moderate foliation @~40deg t.c.a. ~20-25% phenos of plag ranging from >1mm-3mm in size. Contains calcite and epidote in fractures.�Unit is non-magnetic.�L.c is sharp, @~27deg t.c.a.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-096 544.87 550.7 FI.por.fp Dark red, highly altered (hematitie alteration) Feldspar Porphyry. Contains ~15% phenos of plag with

hematite rims, and ~5-10% sheared phenos of k-feld. Contains epidote in fractures, as well as magnetite and quartz veinlets. Unit is moderatly magnetic and weakly to moderatly foliated @~34deg t.c.a. �At 545.27m there is a 2cm smoky quartz vein. �At 546.05cm there is a 42cm porphyritic mafic dyke containing weak to moderate foliation @~40ged t.c.a. 10-15% phenos of plag ranging from >1mm-2mm in size. U.c and L.c are sharp, @~45deg t.c.a.�L.c is sharp, @~30deg t.c.a.

JL08-096 550.7 551.48 MI.dk.pk Dark grey-black, mafic dyke containing weak to moderate foliation @~38deg t.c.a. . Contains calcite and epidote in fractures. Contains localized bands of hematite alteration at 550.85m�Unit is moderatly magnetic.�L.c is sharp, @~30deg t.c.a.

JL08-096 551.48 621.8 MT-IV Black-brown, highly altered intermediate volcanics. Chlorite veining present throughout, as well as epidote and calcite in fractures. Unit has patches of chlorite alteration throughout, as well as a more mafic composition locally. Veins of epidote and chlorite increas with depth. Trace amounts of pink carbonate in fractures (>1%, possibly ankerite) Unit has pervasive, moderate to strong magnetism. Unit is locally vuggy. Unit increases in magnetite bands and calcite with an increase in depth. �Foliation @~40deg t.c.a.�At 565.77m, unit is cut by a highly altered mafic dyke with ~10% calcite in fractures and ~10% epidote. U.c @~45deg t.c.a. L.c @~32deg t.c.a. Nonmagnetic.�At 569.85m there is a 5cm mafic dyke. U.c is broken, L.c @~45deg tc.a. Nonmagnetic�At 547.75, unit is cut by a 87cm post-kin. mafic dyke with irregular U.c and L.c. Nonmagnetic�At 585.10, unit is cut by a 50cm, post-kin felsic dike with disseminated pyrite (~1-2%). Contacts are sharp, with U.C broken and L.c @~45deg t.c.a. �At 588.77m, unit is cut by 3cm felsic dyke. Uc and L.c are sharp, at ~45deg t.c.a.�At 599.68 unit is cut by a 40cm post-kin mafic dyke with sharp contacts. U.c is irregular, @~45deg, L.c

JL08-096 621.8 623.37 MI.dk.por Dark grey-black, porphyritic mafic dyke, ~10-12% plag phenos up to 6mm in diameter. Weakly foliated, @~36deg t.c.a. Unit contains calcite and epidote in fractures, which often cut across the foliation. Unit contains disseminated pyrite.�Unit is nonmagnetic. L.c is sharp and slightly irregular, @~42deg t.c.a.

JL08-096 623.37 629.49 FI.por.fpReddish-brown, highly altered feldspar porphyry with ~5-7% phenos. Possibly potassic alteration, with hematite in fractures. Unit is weakly foliated, @~40deg t.c.a. A 1cm quartz vein at 625.92.��Unit is cut by a 55cm post-kin mafic dyke with sharp, long irregular contacts @~80deg t.c.a.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-096 629.49 632.37 MI.dk.por Dark grey-black, porphyritic mafic dyke, ~10-12% plag phenos up to 6mm in diameter. Weakly

foliated, @~36deg t.c.a. Unit contains calcite and epidote in fractures, which often cut across the foliation. Unit contains disseminated pyrite.�Unit is nonmagnetic. L.c is sharp and slightly irregular, @~42deg t.c.a. Unit contains ~3-5% dissaminated pyrrhotite.�At 630.45m, unit is cut by a 55cm lense of intermediate volcanics. Slight potassic alteration and minor calcite in fractures. U.c and L.c are sharp, @~45deg t.c.a.

JL08-096 632.37 634 MT-IV ntermediate volcanics. Slight potassic alteration and minor calcite in fractures. U.c is sharp, @~45deg t.c.a. Unit has minor chlorite and epidote in veins. Moderatly magnetic and weakly foliated. Small, local ptches of a more felsic composition. L.c is not present. End of Hole.

JL08-097 0 0.3 OVBD overburdenJL08-097 0.3 17.34 MT-IV Dark grey-black, porphyritic metamorphosed intermediate volcanic. Fine grained sandy matrix.

Sheared brown-tan phenos of possible arenite or biotite or horneblende alteration. Weak to moderate foliation @~ 54deg t.c.a.�Hematite present in fractures as well as low amounts of calcite and epidote. Unit becomes less porphyritic with an increase in depth. Minor patchy hematite halos present througout. Unit is non-magnetic throughout.��At 8.3m unit is highly altered, possibly potassic alteration until 8.52m and again from 11.24m to 11.40m. Unit has chlorite veining and alteration from 11.71m to 12.40m. ��Unit is cut by a mafic dyke with strong calcite veining and chlorite alteration from 14.35m to 14.66m. L.c is sharp and slightly irregular, @~55deg t.c.a. Also, unit has a low amount of interfingering diklets. Unit is cut from 17m to 17.28m by another highly altered mafic dyke with calcite veining and chlorite alteration. L.c is @~ 63deg t.c.a.��L.c and U.c of unit are not present.

JL08-097 17.34 20.87 MT-CO.pl Dark grey-brown matrix with multi-colored, highly strained clasts of varrying composition. Highly metamorphosed conglomerate with strong foliation @~60deg t.c.a. Contains sub-angluar to sub-rounded clasts of ankerite, jasper, arkose sandstone, chlotire +/- biotite +/- epidote +/- mudstone. Unit contains chlorite veining. Calcite and epidote present in fractures. Minor patchy hematite halos present througout. ��Unit has patchy, moderate magnetism.��L.c is ~60deg t.c.a.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-097 20.87 23.02 MI.dk.pk Light grey, moderat to highly foliated per-kinematic mafic dyke with small bands of intermediate

volcanic throughout and low amounts of highly sheared plag clasts. Highly altered feldspars(possibly plag) with 25cm of talc from 21.40m to 21.65m. Foliation @~55deg t.c.a. Slight calcite present in fractures. �Unit has patchy, weak magnetism.

JL08-097 23.02 31.88 MT-IV Dark grey-black, metamorphosed intermediate volcanic. Fine grained sandy matrix. Moderate foliation @~ 60deg t.c.a.�Hematite present in fractures as well as low amounts of calcite and epidote. Minor patchy hematite halos present througout. Unit is non-magnetic.��Unit is cut by a 9cm mafic dyke at 20.70m.��U.c is sharp, @~60deg t.c.a. L.c is sharp, @~67deg t.c.a.

JL08-097 31.88 55.05 MT-CO.pl.myPolylithic meta-conglomerate, mostly mylonitic. The fragments are a lot various ; Jasperite cherts, cherts, Quartz, Felspars (Kfp and Pg), disseminated carbonate mineralisations. There are two majors alteration minerals, Epidote is found in replacement into the fragments and also into the rhyolitic matrix of the conglomerate, Hematite is just present in replacement in the fragments and never found in the matrix. Local brownish alteration mineral in the rhyolitic matrix (maybe altered epidote). Carbonates, such as calcite are mostly into late small fractures. The unit is locally cut by small mafic intervals (<30cm thick). The magnetism is mostly inexistant but is sometimes strong on several disseminated spots where there are magnetite mineralisations. Mylonitisation is pretty intense almost all over the unit and the foliation is regular and around 60° to the CA.

JL08-097 55.05 56.8 MI.dk.sk Aphanitic to fine grained syn kinematic mafic dike, weakly foliated, the foliation is expressed by Ep±Ct rich bands at the margins, there are also some jasperite rich bands. Both of the contacts are chilled margins. The unit is nonmagnetic, foliation is still 60° to the CA.

JL08-097 56.8 65.58 MT-CO.pl.myPolylithic meta-conglomerate, mostly mylonitic. The fragments are a lot various ; Jasperite cherts, cherts, Quartz, Felspars (Kfp and Pg), disseminated carbonate mineralisations. There are two majors alteration minerals, Epidote is found in replacement into the fragments and also into the rhyolitic matrix of the conglomerate, Hematite is just present in replacement in the fragments and never found in the matrix. Local brownish alteration mineral in the rhyolitic matrix (maybe altered epidote). Carbonates, such as calcite are mostly into late small fractures. The unit is locally cut by small mafic intervals (<30cm thick). The magnetism is mostly inexistant but is sometimes strong on several disseminated spots where there are magnetite mineralisations. Mylonitisation is pretty intense almost all over the unit and the foliation is regular and around 60° to the CA.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-097 65.58 68.25 MI.dk.sk

Dark grey-black fine grained syn-kinematic mafic dike. Foliation is weak. Epidote and chlorite bands (ep>ct) follow the foliation @~45deg t.c.a. Bands of hematite present which cut the foliation @~63deg t.c.a. Hematite also present in fractures. Last 17cm of dyke is more chlorite rich.�U.c is sharp @~56deg t.c.a and L.c is irregular, @~56deg t.c.a.�Unit has pervasive, moderate magnetism.

JL08-097 68.25 84 MT-CO.pl.my Fine to coarse grained dark grey-brown matrix with multi-colored, highly strained clasts of varrying composition. Highly metamorphosed conglomerate with strong foliation @~58deg t.c.a. Contains sub-angluar to sub-rounded clasts of ankerite, jasper, arkose sandstone, qtz, chlotire +/- biotite +/- epidote +/- mudstone. Unit contains chlorite veining. Calcite(1%)and epidote(7%) present in fractures.�Unit has patchy, moderate magnetism.��Unit becomes very strongly foliated beginning at 77.03m�Unit has high potassic alteration beginning at 77.07m until 77.77m.��Unit is cut by various small mafic dikes ranging from 1cm to 5cm throughout the unit. At 68.52m unit is cut by a 23cm syn-kin mafic dyke with chlorite alteration and epidote veining. Unit is cut at 75.55m by a 26cm epidote and chlorite rich post-kin mafic dike. �At 79.88m unit is cut by a 73cm pre-kin mafic dyke with blebbs of chlorite as well as epidote and chlorite veining. Dyke has strong foliation @~58deg t.c.a. L.c @~ 58deg t.c.a. At 80.83m unit is cut by a 46cm per-kin mafic dyke with strong foliation and epidote veining. L.c @~58deg t.c.a. �


Hole ID From (m) To (m) Lithology Code DescriptionJL08-097 84 111.7 MT-IV.my Grey-black, medium to fine grained matrix containig biotite +/- horneblende. Quatrz +/- plag also

present. Calcite in fractures. Intermediate Volcanic. Highly strained with foliation @~56deg t.c.a. Hematite banding and fracture fills beginning at 85.06m. �Slight hematite alteration beginning at 85.06m until 85.73 with potassic alteration beginning at 85.73 until 87.89m.�Unit increases in epidote veiningwith depth, starting at ~101.64m�At 105.92m unit beings to become more altered (sodic alteration maybe?). 8cm quartz vein present at 109.34m�Unit is moderatly magnetic.��Unit is cut at 93.70m by a 24cm felsic dyke containint biotite, caclite, plag +/- hornblende with trace amountsof blebby epidote. L.c@~68deg t.c.a.�Unit is cut at 94.35m by a 37cm feslic dyke containint biotite, calcite, plag +/- hornblende. L.c is @~66deg t.c.a.�Unit is cut at 96.48 by an 11cm felsic dyke. L.c @~68deg t.c.a.�At 97.10 unit is cut by an 87cm feslic dyke containint biotite, calcite, plag +/- hornblende. U.c and L.c is sharp and irregular. �

JL08-097 111.7 113.6 MI.dk Fine grained syn to late kinematic melagabbro dike, weakly foliated, nonmagnetic. Locally cut by thin carbonate filled fractures and by one 1cm thick felsic volcanics vein. Presence of one small (~5cm thick) enclave of felsic materials. Chilled margins.

JL08-097 113.6 194 MT-IVAphanitic to medium grained intermediate volcanics, high strained to mylonitic, strongly to moderately foliated. Strongly magnetic as there are some eyed style magnetite minerals and also disseminated magnetite. Some local carbonate occurences into the foliation as calcite bands. Very weak patchy hematization, local epidote mineralisations, mainly in the more felsics parts of the unit. Some pretty wide (~4cm) bands shows hornblende replacement of pyroxenes. The magnetite is often associated with sulfides mineralisations. The sulfides are mostly really fine-grained pyrite. The accessories minerals are Kfp, high strained plagioclases, carbonates (including calcite), chlorite, epidote, local presence of garnets, and Pyroxenes in the more mafic parts of the unit. Between 124.5 and 129.5m, the unit alternates between thick felsics volcanics intervals (~60cm) and thinner mafic intervals (~15cm). Between 157.50 and ~188m, the unit is almost 75% mafic materials, always with eyed style magnetite associated with sulfides (Py ± Po).


Hole ID From (m) To (m) Lithology Code DescriptionJL08-097 194 233.26 MT-IV Same unit as previous but with several differences ; This part of the unit is U-mineralised as follows ;

�194 - 202m => max 639cps on a small spot, the average value is around 220cps. �202 - 212m => max 3000cps with 9 spots > 1000cps, the average value is around 850cps.�Compared to the upper part of the unit, the major difference in the mineralised interval is that the carbonates mineralisations are important and found as powdered disseminated mineralisations and in fracture filling. The disseminated carbonates are here associated with hornblende. The hematization is patchy and very weak. The magnetite are still present in eyed style mineralisations but also in fractures filling parallel toi the foliation. The most mineralised part of the zone shows a purple cherty-like alteration.

JL08-097 233.26 234.28 MI.dk.skMafic syn-kinematic dike, moderately foliated, sharp contacts, pseudo perpendiculars to the CA, the foliation is around 70° to the CA. Unit is nonmagnetic, locally cut by small carbonate filled fractures.

JL08-097 234.28 264.9 MT-IV Same MT-IV as before the previous dike, mineralised as follows ;�234.28 – 243.33 => avg 478cps ; max 2295cps�243.33 – 259.56 => Background with 2 spots mineralized at 428 and 569cps.�66m thick mineralized zone so far, more mineralization expected tomorrow.

JL08-097 264.9 280.82 FI.por.fpCoarsely porphyritic felsic intrusive, felspar-quartz porphyry, both margins are felspar porphyritic mafic dikes with contacts pseudoperpendicular to the CA, those mafic dike are progressively porphyritic approaching the felsic intrusive, and more aphanitic mafic approching the host MT-IV. Dominant plagioclases cristals, most of those plagioclases are rounded and zoned, sometimes with a Pg core circled by Bt, sometimes the Pg cristalizes around a biotitic core. Most of the cristals are oriented but some of them crosses the foliation, as it was cristalized after deformation. The micaceous foliation (Bt ± Ct) hosts a lot of fine grained sulfides (Pyrite). In the bottom part of the unit, there are some K-spars, sometimes cristalized around plagioclases, and sometimes with a perthitic facies. The unit is nonmagnetic. There are also some disseminated calcite mineralisations into the matrix. The mafic margins are nonmagnetic, hosts green Hb, disseminated carbonates and felspars porphyritics.

JL08-097 280.82 300.15 MT-IVContinuation of the previous mineralised MT-IV, with small differences ; moderate pervasive hematization, locally cut by a syn kinematic mafic dike between 284.46 and 285m, both contacts of that dike are pseudoperpendiculars to the CA, and parallel to the foliation in the dike. �The unit is mineralised as follows ; �280.82 - 286.50m => avg 503cps ; max 1653cps, with 5 spots > 1000cps.�286.50 - 300.15m => avg 324cps ; max 900cps, with 11 spots > 500cps.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-097 300.15 301.62 MI.dk.sk Very fine grained, weakly foliated syn-kinematic mafic dike, with rare disseminated felspar

porphyroclasts, traces of carbonates and fine grained pyrite. The contacts are parallel to the foliation in the host MT-IV. Unit is nonmagnetic. The dike is barren.

JL08-097 301.62 347.05 MT-IVContinuation of the previous mineralised MT-IV, with small differences ; weak patchy hematization, becoming less important to the bottom of the unit, the unit is becoming less carbonate rich too. Locally cut by 3 mafic intrusives, (307.86 - 308.18m => pseudoperpendiculars sharp contacts ; 316.55 - 317.13m => sharp contacts around 65° to the CA ; 319.66 - 320.50m => 45° bottom contact). U-mineralisation stops at 304m with a spot 467cps high.

JL08-097 347.04 348.37 MI.dk.psk Fine grained unfoliated post-kinematic mafic dike, with a sharp top contact perpendicular to the core angle. Fine grained disseminated pyrite mineralisation and rare felspar porphyritics.

JL08-097 348.37 353 MT-IV Continuity of the previous MT-IV.

JL08-098 0 8.27 OVBD Overburden.JL08-098 8.27 20.13 MI.dk.por Pale blue-grey to grey-green-black, Fine-grained to locally coarse-grained. Ct-altered, hb-porphyritic

mafic intrusive. Hb phenos are dark green-black 0.2cm-2cm anhedral, bulbous grains that have been altered by ct. Unit is moderately foliated and ct-rich. The ct occurrence is in swath-like bands throughout the unit also occuring in web-textures giving the unit a pseudo-breciation texture. Local coarse-grained hb phenos display a elliptical, elongated shape which is coherent with foliation. Minor clay (possibly sericite) alteration b/w 15.37m-16.10m. Hb-phenos in this altered region appear larger and show a more stretched, elliptical shape. Lower contact sharp and shallow at an angle of 20 degrees to C.A.

JL08-098 20.13 31.59 FI.dk.porPink-purple, green-grey-pink, weakly foliated, fine-grained to locally aphanitic, porphyritic felsic intrusive. Unit has areas of more mafic material patchy throughout. Weak foliation is discontinuous and unmeasurableThese areas contain swath-like bands of more mafic material containing mineralogy such as ct+bt. Unit is non-magnetic. Unit is representative of the felsic intrusive containing blue qz eyes but the unit itself has no visable qz w/n in it. Upper contact is sharp and at an angle of 20 degrees to C.A. Lower contact is gradational and indistinct.

JL08-098 31.59 50.35 MI.dkWhite-black, fine-grained to locally coarse-grained, unfoliated, late to post-kinematic mafic dike (possible mafic sill?). Unit is carbonate-rich. Carbonate occurrence is in small anastamosing veinlets flooding the unit throughout. These carbonate-rich veinlets give the unit a pseudo-brecciation/web-texture. In carbonate-poor areas of the unit the phenocrysts are more abundant and lie w/n a biege coloured, leucoxene-rich matrix. The phenocrysts are coarse-grained, black, bulbous, anhedral grains, possibly bt-replacement of pre-existing px phenocrysts. The leucoxene-bt-rich portions of the unit give a leopard texture to the unit. Unit has moderate-patchy magnetism. Upper contact is gradational and unmeasureable. Lower contact is at an angle of 60 degrees to the C.A.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-098 50.35 52.05 MT-IV Pink-red-purple to green-red, fine-grained, ct-rich, metamorphosed intermediate volcanics. Unit has

pervasive to patchy ct replacement throughout. The mineralogy is too fine-grained to discern. Upper contact is sharp and at an angle of 60 degrees to C.A. Lower contact is sharp and hematized with an angle of 60 degrees with C.A.

JL08-098 52.05 62.17 MI.dkContinuation of previous mafic dike (31.59m-50.35m). Unfoliated, black and white coloured, bimodal grain-size. Unit is quite the same as the previous mafic interval. Carbonate is intensely pervasive throughout with small patchs of leopard texturedareas containing bt-rich phenos w/n a lecoxene matrix. Moderately magnetics patchy throughout. Upper contact is sharp at an angle of 60 degrees to C.A. Lower contact is sharp and hematized at an angle of 40 degrees to C.A.

JL08-098 62.17 64.4 MT-IV Same as previous intermediate meta-volcanics (50.35m-52.45m). Pink-purple, ct-rich, fine-grained intermediate meta-volcanics. Unit is quite fine-grained making mineralogy hard to discern. Foliation is weak and discontinuous making measurementsdificult. Weak pathcy magnetism. Upper contact is sharp at an angle of 40 degrees to C.A. Lower contact is strongly chloritized and sharp at an angle of 75 degrees to C.A.

JL08-098 64.4 79.7 MT-IV Continuation of previous mafic unit (52.05m-62.17m). Unfoliated, black and white coloured, bimodal grain-size. Unit is quite the same as the previous mafic interval. Carbonate is not as intensley pervasive in this particualr unit. Leopard textured areas containing bt-rich phenos w/n a lecoxene matrix are more prominent in this unit. Moderately magnetics patchy throughout. Unit contains more intermediate portions that are less than 20 cm in length. Upper contact is sharp at an angle of 75 degrees. Lower contact is gradational and hard to discern.�U-mineralization present from 77.00m-78.73 with a max: 603cps avg: 295cps��Unit is possibly intermediate to mafic meta-volcanics.

JL08-098 79.7 97.9 MT-IV Pink-purple, grey-purple, fine-grained, moderately foliated, intermediate meta-volcanics. Unit is rich in felsic material that is relatively hematitic and potassically altered. There are patchy intervals of ct richs swaths throughout. The unit is phenocryst poor. Dominant mineralogy is mostly alteration mineralogy such as ct+bt+hm. Hematite occurs in patchy bands throughout which follow dominant foliation which is defined by the banding of micacious mineralogy. Hm also occurs around the swaths of ct-rich intervals. Unit is dominantly non-magnetic with small locally weak magnetism. Cb is present throughout along fractures as well as peppered finer grains within the matrix material. Upper contact is sharp and hematized with an angle of 50 degrees to C.A. Lower contact is sharp and chilled at an angle of 70 degrees to C.A.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-098 97.9 98.13 MI.dk.sk

Green-black, chloritic, fine-grained, syn-kinematic mafic dike. Unit is ct-rich. Ct occurs along folaition as well as w/n web textured micro-veinlets. Unit is fine-grained thus making discerning mineralogy difficult possibly hb replacing px within the matrix of the unit. Foliation is weak but dominantly defined by fine bands of micacious mineralogy such as bt+ct. Upper contact is sharp and at an angle of 70 degrees. Unit is non-magnetic. Lower contact is also sharp but broken and unmeasurable.

JL08-098 98.13 116.73 MT-IVContinuation of the previous MT-IV (79.7m-97.9m). Pink-purple, grey-purple, fine-grained, moderately foliated, intermediate meta-volcanics. Unit is rich in felsic material that is relatively hematitic and potassically altered. There are patchy intervals of ct richs swaths throughout. The unit is phenocryst poor. Dominant mineralogy is mostly alteration mineralogy such as ct+bt+hm. Hematite occurs in patchy bands throughout which follow dominant foliation which is defined by the banding of micacious mineralogy. Hm also occurs around the swaths of ct-rich intervals. Unit is dominantly non-magnetic with small locally weak magnetism. Cb is present throughout along fractures as well as peppered finer grains within the matrix material. Upper contact is broken and unmeasurable. Lower contact is sharp and hematized at an angle of 70 degrees to C.A.

JL08-098 116.73 141.07 MT-FV.porPink-grey to purple, moderately hematized, well foliated, fine-grained to coarse-grained, metamorphosed feldspar porphyritic volcanics. Porphyroclasts are dominantly sub-rounded, pink-red, 0.2cm-1.5cm regrown, k-spar grains.There are also earlier, elliptical to linearly strained blue qz eyes and pg porphyroclasts of the same occurrence that follow the dominant fabric w/n the unit. Strain is varied throughout the unit. This strain variation is reflected in the shape and size of the porphyroclasts of pg and k-spar. The unit decreases in grain-size along with the diminishing of foliation downhole and ressembles an aggregate of grains similar to a rock of sedimentary origin. Patchy magnetism. Upper contact is sharp at an angle of 70 degrees to C.A. Lower contact with the following intermediate volcanic unit is gradational and unmeasurable.�Very poor core recovery due to brittle faulting b/w 121.00m-134.10m

JL08-098 141.07 150.21 MT-IVGrey-purple to pink green, chlorite-rich, intermediate to felsic meta-volcanics. Slightly ressembles the previous felsic porphyritic unit with finer grains of elliptical pg and more chlorite present in the matrix. Some of the fgr pg suffers from hematitic replacement. Ct also occurs in swathing bands that are surrounded by haloes of hematitic alteration which are patchy throughout the unit. The dominant composition is intermediate with more felsic intervals intermittent throughout the unit. Magnetism is weak and patchy. Upper contact is gradational with the previous felsic unit. Lower contact is truncated by a small <15cm mafic dike an is approx. at an angle of 50 degrees to C.A.



Same as previous porphyritic felsic meta-volcanic unit (116.07m-141.07m). Unit has more pervasive hematitic alteration giving it a more reddish pink bleached colour. Well foliated, med-grained to coarse-grained, metamorphosed feldspar porphyritic volcanics. Porphyroclasts are dominantly sub-rounded, pink-red, 0.4cm-1.5cm regrown, k-spar grains. There are also earlier, elliptical to linearly strained blue qz eyes and pg porphyroclasts of the same occurrence that follow the dominant fabric w/n the unit. Strain is varied throughout the unit. This strain variation is reflected in the shape and size of the porphyroclasts of pg and k-spar. Patchy magnetism. Upper contact isat an angle of 50 degrees to C.A. Lower contact is brittle fault gauge that has been lithified with the mafic dike below and makes an angle of 60 degrees with C.A.�Very poor core recovery due to brittle faulting b/w 151.00m-153.81m

JL08-098 153.81 155.2 MI.dk.sk Chloritic, non-magnetic, well foliated, pre-syn-kinematic mafic dike. Unit has a ct-rich matrix with fgr phenos of highly sericitized and strained anhedral pg. Moderate ct w/n fractures throughout the unit. Upper contact is at 60 degrees to C.A. Lower contact is broken and lost.

JL08-098 155.2 157.18 MT-IV.por.fpSame as previous porphyritic felsic meta-volcanic unit (150.21m-153.21m). Pervasive hematitic alteration gives the unit a reddish pink bleached colour. Well foliated, med-grained to coarse-grained, metamorphosed feldspar porphyritic volcanics. Porphyroclasts are dominantly sub-rounded, pink-red, 0.4cm-1.5cm regrown, k-spar grains. There are also earlier, elliptical to linearly strained blue qz eyes and pg porphyroclasts of the same occurrence that follow the dominant fabric w/n the unit. Strain is varied throughout the unit. This strain variation is reflected in the shape and size of the porphyroclasts of pg and k-spar. Patchy magnetism. Upper and lower contacts are both broken and un recognizable. 30 cm of core missing fr

JL08-098 157.18 158.75 MI.dk.sk Fine grained, syn-kin mafic dyke.Chilled contact. L.c @~ 50deg t.c.a. U.c is not visable. Foliation at 518.2m @70deg.

JL08-098 158.75 162.04 MT-IV.por.fp continuation of previous prorphitic felsic metavolcanic.. First 60cm are intercepted by 3 mafic intervals. Respectivly 17, 5 and 10cm thick. Foliation@70deg t.c.a. L.c @74deg t.c.a. strained blue quatrz eyes.

JL08-098 162.05 163.35 MI.dk.skcontinuation of previous syn-kin mafic dyke. L.c @40deg t.c.a. Moderately patchy hematization.

JL08-098 163.35 169.9 MT-IV.por.fp continuation of previous prophyritic felsic metavolcanic. Strong pervasive hemitaziation, decreases downhole.

JL08-098 169.9 175.37 MI.dk.por Pre to syn-kin mafic dyke. Strongly foliated.Highly porphyritic in the first meter, less in the last meter. Minor Carbonate veins. Horneblende. L.c is pseudo perpendicularl t.c.a and gradationa @86deg. From 174.3 to L.c we have 3 syn-Mt.IV intrusions. Strain is variable throughout the unit. More chloritic near the MT.IV intervals.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-098 175.37 179.7 MT-IV MT.IV, intersected by syn-mafic intervals. A lot of fractured filled epidote and horneblends phenos.

Epidote appears to be highly altered enclaves of the dyke. Chlorite and epidote occurance is in swath-like ribbons throughout. Traces of fracture filled and patchy hemitaziation. Hemitaziation is stronger near the epidote veins.

JL08-098 179.7 181.6 MI.dk.por Porphyritic mafic dyke. Moderatly to strongly foliated. Horneblende prohpyritic. Carbonate veins. Sharp lower and upper contacts. Locally chloritic, mostly in the prophyritic intervals. L.c @~74deg t.c.a.

JL08-098 181.6 184.6 MT-IV continuation of previous MT.IV. L.c is not visable, around 184.6m.JL08-098 184.6 188.27 MI.dk.por

continuation of the previous horneblende porphyritic mafic intrustive. No more carbonates. Weak local magnetism. Foliation @65deg t.c.a. Contacts are really diffused and hard to define precisely.

JL08-098 188.27 191 MT-IV continuation of the previous MT.IV. More mafic materials. A few epidote and chlorite veins in the first 85cm of the unit. No more veins after this point. Traces of fracture filled and dissaminated hematite. Highly strained feldspar porphyritics. High magnetism.

JL08-098 191 199.83 MI.dk.por continuation of the previous horneblende porphyritic mafic intrustive. Moderatly to strongly foliated. pre-kin. Intercepted by 2 syn-kin felsic intervals. Traces of weak patchy magnetism.

JL08-098 199.83 201.76 MI.dk.psk ~fine grained, post-kin mafic dyke. Unfoliated. Plag phenos peppered throughout,~8%. Minor dissimenated pyrite. Small chlorite and carbonate in fractures. Sharp contacts. U.c @~60deg t.c.a. L.c is a chilled zone.

JL08-098 201.76 203.76 MI.dk.por continuation of the previous horneblende porphyritic mafic intrusive.JL08-098 203.76 210.52 MT-CO.pl

Pink-red to grey-yellow-brown-green, cb-rich, fine grained to locally clastic, weakly foliated, moderately hematized, polylithic meta-conglomerate. Unit has a weak foliation that is discontinuous. On a whole the unit is clast-poor. Carbonate occurs within the unit along small brittle micro-fractures throughout. Ct-occurs local to the majority of the areas where the carbonate-filled micro fractures occur. Clasts that are visible appear to be ep-rich. Relict lithology of clasts hard to discern due to intense alteration overprinting w/n the unit. Unit is highly fractured and brecciated locally. Upper contact is relatively sharp and hematitic at an angle of 50 degreesC.A.. Lower contact is sharp and hematized at an angle of 75 degrees to C.A.

JL08-098 210.52 214.55 MI.dk Dark green-black, locally hematized and brecciated, mafic dike. Unit is highly altered making deformation textures difficult to see. Unit is strongly magnetic. Moderate carbonate-fill microfractures locally throughout. Serpentine occurs along a small fracture (2cm wide) b/w 214.05m-214.07m. Upper contact is sharp and at an angle of 75 degrees to C.A. Lower contact is at an angle of 60 degrees to C.A.



Beige-brown to green grey, moderately strained, meta-conglomerate. Unit is quite clast-rich which vary from 1cm-7cm angular to sub rounded clasts. Pervasively chloritized and epidotized in areas. Clasts of red japeroid and mudstone are present and are angular to subrounded in shape and vary in size and occurrence downhole. Unit is relatively cb-rich which occurs along small micro-fractures and w/n small 2cm wide vugs.Minor fine-grained subhedral garnet present. Foliation is defined by thick ep+ct bands as well as banding of micacious mineralogy. Non-magnetic. At an angle of 60 degrees to C.A. Lower contact is gradational with nest unit and unmeasurable.

JL08-098 240.34 243.63 MT-CO.pl.my Red-brown, highly strained and metamorphosed mylonitic conglomerate.Moderate to strong hematite (or potassic?) alteration pervasive throughout the unit. Last 20cm of unit is a pre-kin mafic dyke with foliation @~60deg t.c.a and Uc and L.c at@60deg t.c.a.

JL08-098 243.63 249.97 MT-IV.myDark brown-red, intermediat volcanics. Unit is locally cut by 3 pre-kin mafic dykes between 244.28 and 246.42m, each with a foliation @~60deg t.c.a. Contacts of dkyes are sharp, each @~60deg t.c.a. At 248.42m, unit is cut by a 35cm pre-kin mafic dyke. Foliation @~60get t.c.a. L.c is broken, U.c is sharp, @~60deg t.c.a.�At 248.77m there is some re-lithified breciated clasts of the host rock, indicating a minor fault (5cm wide) wich is also present at 249.42m. Unit is moderatly magnetic, with a few bands of strongly magnetic magnetite. Unit contains trace amounts of purple carbonate (?)in fractures. �L.c of unit is gradational.�Unit is mineralized at 244.80 with spot high of 417cps.

JL08-098 249.97 282 MI.dk.skDark grey-black, syn to late-kin. Mafic dyke. Moderatly foliated @~60deg t.c.a. Unit has caclite in fractures. Approx 5-7% plag phenos and 3-5%quartz phenos. Unit has veins of plag throughout. Unit has chlorite and epidote in fractures (ep>ct) as well as trace amounts of disseminated hornblend throughout. Unit has moderate magnetism. Unit has intervals of more and less prophyritic compositons thoroughout. Unis contains a 3cm quartz vein at 275.87�L.c in not visable, located somewhere around 280.50m. Reason for placing contact here is b/c of the magnetic contrast(moderate v.s strongly magnetic).


Hole ID From (m) To (m) Lithology Code DescriptionJL08-098 282 335.45 MT-IV Pink-green to grey-black, Chlorite rich, felsic poor, Intermediate to mafic volcanics. Weakly foliated

with cross-cutting mafic dikelets. Strongly magnetic. Sparse plag phenos local throughout. Increasingly felsic downhole. Foliation becomes stronger downhole. Hematization becomes more prominent downhole. Ct+minor epidote w/n mafic dikelets. Dikelets appear to be later due to cross-cutting of dominant foliations. Abundant carbonate is found w/n bt+ct-rich swathing veinlets b/w 307.00m-311.00m.�Patchy U mineralization as follows:�299.70m-303.33m: max: 826cps; avg: 332cps�309.35m-310.00m: max 296cps; avg: 200cps�310.65m-312..00m: max: 398cps;avg: 228cps

JL08-098 335.45 336.79 FI.grPink-white, black speckled, Coarse-grained, weakly altered, qtz-monzonite to qtz syenite. Unit contains abundant coarse-grained pink-white, anhedral phenocrysts of k-spar that are roughly 1-1.5cm in size. There are also abundant finer-grained (0.5cm) irregular lathes of bt+hb throughout giving the unit a peppered look. The dike appears unfoliated. Upper contact is irregular and roughly at an angle of 40 degrees to C.A. Lower contact is at an angle of 60 degrees to C.A.

JL08-098 336.79 357.72 MT-IV Continuation of previous MT-IV unit (282.00m-335.45m) Pink-green to grey-black, Chlorite rich, felsic poor, Intermediate to mafic volcanics. Weakly foliated with cross-cutting mafic dikelets. Strongly magnetic. Sparse plag phenos local throughout. Increasingly felsic downhole. Foliation becomes stronger downhole. Unit contains 3 (<50cm) enclaves of the previous FI unit b/w 338.62m-338.97m, 341.72-342.21m and 349.62m-350.32m. Contacts b/w FI and the MT-IV are moderatley fluid altered (hm+K). Hematization becomes more prominent downhole. Ct+minor epidote w/n mafic dikelets. Dikelets appear to be later due to cross-cutting of dominant foliations. Abundant carbonate is found w/n bt+ct-rich swathing veinlets throughout unit. Moderately magnetic. Upper contact is sharp with the previous unit.�Patchy U mineralization as follows:�342.00m-343.00: max: 1242cps ; avg: 721cps�345.00m-346.00m: max:432cps ; avg: 195cps�349.00m-350.00m: max:467cps; avg:279cps�350.00m-351.00m: max:293cps; avg:180cps

JL08-098 357.72 359.55 Intermediate Meta-volcanicsJL08-098 359.55 361.43 Unfoliated Post-kinematic Mela-gabbroJL08-098 361.43 363 Intermediate Meta-volcanicsJL08-098 363 367.3 Fine-grained Felsic IntrusiveJL08-098 367.3 374.89 Intermediate Meta-volcanicsJL08-098 374.89 376 Pg-Porphyritic Mafic DikeJL08-098 376 380.38 Intermediate Meta-volcanicsJL08-098 380.38 382.2 Post-kinematic Mela-gabbro


Hole ID From (m) To (m) Lithology Code DescriptionJL08-098 382.2 388.35 Felsic Meta-volcanicJL08-098 388.35 397.06 Intermediate Meta-volcanicsJL08-098 397.06 389.3 Syn-kinematic Mafic DikeJL08-098 389.3 398.15 Pg-Porphyritic Mafic DikeJL08-098 398.15 410.66 U-mineralized Intermediate Meta-volcanics

Mineralized as follows:399.33 - 398.68: max: 728 cps avg: 398cps

JL08-098 410.66 412.13 Syn-kinematic Mafic Dike

JL08-099 0 1 OVBD Overburden and casingJL08-099 1 26 MT-CO.pl

Polylithic metamorphosed conglomerate. First 12.5m are clast poor. Although this part of the unit looks like MT.IV it seems to be part of the conglomerate b/c there is no magnetism contrast btw this part of the unit and the bottom part of the unit, which is an obvious conglomerate. Also the MT.IV like part of the unit has some poorly disseminated clasts. Also, there are some thin, obvious conglomerat intervals present in the first 12.5m. After 12.5m, the unit is clearly conglomerate, locally cut by a hornblend prophyritic syn-kin mafic dyke btw 23.77m-24.41m. �The clasts in the conglomerate are from various natures such as sandstone, chert, & volcanics. The unit has moderate patchy hemitizatiion in the most clast rich part. Traces of disseminated carbonate mineralization, usually oriented parallel to the dominant foliation. �Locally the unit is epidote ± chlorite rich. L.c is very diffused.

JL08-099 26 28.74 MT-IV.por.fp Porphyritic metamorphic felsic volcanic with quartz and feldspar. Feldspars are strained or rounded. Moderate replacement hematization. Local fracture filled carbonates. Unit is non-magnetic. Foliation @~50deg t.c.a.

JL08-099 28.74 65.24 MT-CO.pl Return to metamorphosed conglomerate.First 81cm of the unit is a syn-kin. Mafic dyke with sharp bottom and top contacts, @~65deg t.c.a and 60deg t.c.a respectively. Conglomerate is weakly strained to mylonitic with a lot of fragments fine to coarse grained and from various natures such as siliceous (chert, quartz), sedimentary (sandstone, mudstone), and volcanics (basaltic to andesitic). Moderate patchy hematization. Very weak to no magnetism.�Unit cut by a50cm syn-kin mafic dyke at 49.79. Lower and upper contacts are sharp, @~5deg and ~50deg respectively.

JL08-099 65.24 66.6 MI.dk.sk Fine grained moderately foliated syn-kinematic melagabbro dike, strongly chloritic. Both sharp contacts, oriented around 50° to the CA.



Continuation of the previous metamorphosed conglomerate. Carbonate alteration starts at 76m to the bottom and is mineralised into small fractures (calcite) and in replacement of clasts (anchorite). Hematisation is, as always, situated in the clasts but never into the rhyolitic matrix of the formation. There is also an Epidote ± chlorite alteration in veins. As always in this unit, the clasts are from really various nature ; Sedimentary (mud/Sandstone), Volcanics (basaltic to andesitic clasts), and siliceous (jasperite, cherts, Quartz, Felsics). The unit is strongly foliated, the clasts are weakly strained, as there is a beginning of mylonitisation. The unit is moderately magnetic.

JL08-099 85.86 94.32 MT-IV.por.fpFine grained plagioclase porphyritic felsic intermediate meta-volcanics, moderately magnetic, cut by fractures filled with epidote ± chlorite. Porphyroclasts of altered plagioclases and amphiboles, fine to medium grained, nevertheless, the unit is locally aphanitic. Both contacts are sharp but they are weakly diffused over 10 cm at the margins. Both contacts are oriented at 40 ° to the CA, the foliation is moderate and irregular, between 40 and 50° to the CA. Disseminated hematised plagioclases. Rare chalcopyrite mineralisations.

JL08-099 94.32 100.4 MT-CO.pl.myIntensely mylonitic meta-conglomerate, strongly foliated, strong patchy hematization, intensely pervasive over the first 2 metres, the nature of the clasts is hard to define as they are all strongly strained, but seem to be the same as in the previous conglomeratic units ; Sedimentary (mud/Sandstone), Volcanics (basaltic to andesitic clasts), and siliceous (jasperite, cherts, Quartz, Felsics), with replacement anchorite, disseminated epidote and chlorite alteration. The foliation is irregular, in a range between 30 and 40° to the CA. The bottom contact is emphasized by a 32cm thick mafic syn-kinematic dike. The unit has patchy weak to moderate magnetism.

JL08-099 100.4 103.81 MT-IV.my Transition zone between the mylonitic conglomerate and the felsic meta-volcanics ; intermediate meta-volcanics, mylonitic, strongly foliated, intersected by a syn-kinematic hornblende (and sulphide) porphyritic mafic intrusive, 20cm thick. The unit has patchy moderate hematization. The foliation is oriented at 40° to the CA. Weak magnetism. The bottom contact is very diffused over 30 cm, alternating between MT-IV and MT-FV.

JL08-099 103.81 117.8 MT-FV.porFine to medium grained plagioclase ± Quartz porphyritic felsic meta-volcanic, strong patchy and plag replacement hematization, locally fracture filled hematization. The unit is cut by 2 mafic intrusives, one syn kinematic hornblende porphyritic mafic dike with chalcopyrite between 104.6 and 105.55m, and one small syn kinematic mafic intrusive 25cm thick. Local chlorite replacement. Unit is barely foliated on top but is moderately to strongly foliated to the bottom. Irregular magnetism, magnetite appears to be mineralised in small veins parallel to the foliation (~40° to the CA). Very weak presence of calcite into fractures. The bottom contact is sharp.



Fine-grained, moderately foliated, intermediate meta-volcanics, locally plagioclase-albite porphyritic. Unit is also locally rich in felsic material that is relatively hematized and with K-spars. The unit is moderately intersected with pale-green veinlets believed to be filled with green Pyroxenes ± Amphiboles (maybe green Hb) . Hematite occurs in patchy bands throughout which follow dominant foliation, and also in replacement of Albite. Albite porphyritics are mostly highky strained. Unit is strongly magnetic. Locally cut by 3 small post kinematic unfoliated mafic dikes, <25cm. Occurences of leucoxenes, hornblende, Biotite locally replaced by chlorite. No eye scale sulphides are visible. Upper contact is sharp but on the first 30cm, there are some small MT-FV intervals. The contact with the dike underneath is also very sharp, 25 degrees to the CA.

JL08-099 143.01 149.95 MI.dk.por Plagioclase porphyritic post-kinematic mafic dike, seems to have a small foliation, but the plagioclases porphyroclasts are not oriented at all so the dike is more likely post-kinematic. Weak hematization replacing plagioclases. Nonmagnetic unit. Both contacts are sharp and chilled, oriented at 40° to the CA for the bottom contact

JL08-099 149.95 162.59 MT-IV.myFine-grained to aphanitic, moderately foliated, intermediate meta-volcanics, mylonitic, intensely foliated, and with occurrences of some isoclinal folds. Black, green and red. Presence of hematized Qz veinlets, and of Amphibole ± Pyroxene pale green veinlets. The hematization is weak and patchy, situated into bands. Presence of leucoxene, rare plagioclases porphyroclasts, and Biotite locally replaced by chlorite. Presence of minor faults, with millimetric to centimetric offset. Some carbonates are sited into fractures and also finely disseminated. Very strong magnetism

JL08-099 162.59 170.35 MI.dk.porPlagioclase porphyritic post-kinematic mafic dike, seems to have a small foliation, but the plagioclases porphyroclasts are not oriented at all so the dike is more likely post-kinematic. Weak hematization replacing plagioclases. Nonmagnetic unit. Both contacts are sharp and chilled, oriented at 26° to the CA for the bottom contact. Weak disseminated calcite mineralisation.

JL08-099 170.35 225.41 MT-IVFine-grained to aphanitic, moderately foliated, intermediate meta-volcanics. Black, green and red. Presence of hematized Qz veinlets, and of Amphibole ± Pyroxene pale green veinlets. The hematization is weak and patchy, situated into bands, and in felspar replacement. Presence of leucoxene, rare plagioclases porphyroclasts, and Biotite locally replaced by chlorite. Presence of minor faults, with millimetric to centimetric offset. Some carbonates are sited into fractures and also finely disseminated. Very strong magnetism. The unit is very locally plagioclase and/or leucoxene porphyritic, and also locally mylonitic, but is globally aphanitic and not mylonitic. Locally cut by a finely porphyritic mafic intrusive, weakly foliated so lately syn-kinematic, at 218.23m, to 219.03. Hematization and carbonates occurences become more important from 204m, carbonates in veinlets are usually associated with biotite, and locally with chalcopyrite.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-099 225.41 226.55 MI.dk.psk Aphanitic post-kinematic mafic intrusive, locally intersected by very thin carbonate filled veinlets.

Occurences of disseminated very fine grained sulfides (chalcopyrite) mineralisations. Moderate magnetism. Both contacts are sharp, top contact oriented 60° to the CA, and bottom contact is at 45° to the CA.

JL08-099 226.55 250.6 MT-IV Continuation of the previous MT-IV unit, entering the mineralised zone around 228m, the mineralisation is as follows ; �Barely mineralised between 228-230�Very good mineralisations between 230-237m ; avg 1600cps ; 33 spots > 1000 cps.�Barely mineralised between 237-250.6m with 3 spots > 500 cps.��Locally cut by a porphyritic syn kinematic mafic intrusives at 246.62m, 26cm thick.�Around 237m, a highly chloritic replacemnt zone is cut by an important small fractures network, filled with carbonates, underneath that 25cm interval, the foliation has turned.

JL08-099 250.6 251.86 MI.dk.por Plagioclase porphyritic fine to medium grained, syn kinematic mafic dike, fine grained disseminated chalcopyrite mineralisations. Nonmagnetic.

JL08-099 251.86 290.1 MT-IV Continuation of the MT-IV unit ; �The unit is locally cut by 5 small (< 1m) mafic intrusives ; 254.41 - 254.54m ; 256.05 - 256.26m ; 267.18 - 267.98m ; 277.08 - 277.53m ; 289.42 - 290.07m. �The bottom contact of the unit is emphasized by a mafic dike between the 2 units. U-mineralised as follows ; �268 - 276m : avg => 800 cps ; 19 spots > 1000 cps ; max 7044 cps.

JL08-099 290.1 305.6 FI.por.fp Coarse grained porphyritic felspar porphyry, weakly foliated, the foliation is expressed by micaceous bands, locally associated with minor very fine grained chalcopyrite mineralisation. Most of the plagioclases are zoned, sometimes nucleated around a biotitic core. Some minor disseminated carbonates are also present. Sometimes, and mostly close to the bottom margin, the very last zonation around plagioclase is K-felspatic. The unit is weakly magnetic. This unit seems to be U-mineralisation destructive, so it is thought to be post mineralisation. Hematisation is disseminated and very weak.

JL08-099 305.6 316.2 MI.dk.sk Very fine grained syn-kinematic mafic dike, barely to moderately foliated. Nonmagnetic, interfingered with the felspar porphyry on the first 3.50m. The dike is strongly biotitic, locally replaced by chloritic bands.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-099 316.2 367 MT-IV

Fine-grained to aphanitic, moderately foliated, intermediate meta-volcanics. Black, green and red. Presence of Amphibole ± Pyroxene pale green veinlets. The hematization is strong and patchy. Presence of Biotite locally replaced by chlorite. Lots of carbonates, sited into fractures and also finely disseminated. Very strong magnetism. Carbonates in veinlets are usually associated with biotite and green hornblende ± Pyroxenes, and locally with chalcopyrite. New lens of U-mineralisation starts at 321m. Association between U-mineralisation and carbonates veinlets ?�Unit is mineralised as follows ; �322-324m => avg 450 cps ; max 1453 cps.�324-332m => Barely mineralised, avg 120 cps ; max 493 cps.�332-334m => avg 350 cps ; max 890 cps.�334-341m => Barely mineralised, avg 120 cps ; max 440 cps.�341-343m => avg 450 cps ; max 1091 cps.

JL08-100 0 9.6 OVBD No core recovery to 8.4m, then overburden to 9.6m.JL08-100 9.6 35.9 MT-IV

Fine grained, medium grey, massive, unfoliated to moderately foliated, weak to strong patchy magnetic intermediate volcanic with locallized chlorite shears along foliation plane. Minor areas (mostly from 11.7-13.0m) with 5-15% green 1-3mm disseminated chlorite phenocrysts replacing probably amphibole (hbl?). From 17.7-23.6m: pachy to pervasive potassic alteration with strong alteration from the top to 18.3m with moderately broken core followed by patchy potassic alteration in the matrix and 10-20% dark chlorite defining foliation. This area has 2% calcite-chlorite filled fractures with a stockwork of calcite-chlorite fractures (30%) from 22.05-22.30m. From 33.0-35.9m: 3-10% fine grained fresh biotite disseminated in foliation plane.

JL08-100 35.9 38.9 MI.dk.sk Fine to medium grained, dark grey-green, post-kinematic, unfoliated to weakly foliated, weak to moderate patchy magnetic. Disseminated plagioclase phenos increaing downhole, white to cream in colour, 5-10%, 0.5-2mm in size. Several larger phenos, probably of amphibole, throughout unit, average 0.5-0.8cm in size, black, <1%, patchy. Upper contact is sharp and concordant, lower contact is broken.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-100 38.9 77.03 MT-IV Fine grained, medium grey to greyish red-brown, weakly foliated to moderately foliated, moderate to

strongly magnetic (mostly assoiated with chlorite) intermediate volcanic with weak to strong hematitic alteration from 44.1-62.2m. Uranium is associated with moderate-strong hematite alteration. Multiple mafic dykes cross the interval from 50.52-51.05m with uct@80 deg tca; 52.65-52.9m with uct@ 65 deg to CA; 54.7-54.9m with uct @ 58 deg to ca; 55.8-55.9m with uct @ 60 deg to CA; 65.65-65.78m with two chlorites and calcite (possibly vein) with uct @ 55 deg to CA; and last mafic dyke at 67.77-67.86m with uct @ 50 deg to CA. �Mineralized intervals occur from 46.35-8.0m with an avg of 340 cps and a max of 401 cps; 48.9-49.9m with an avg of 410 cps and max of 952 cps; from 52.15-52.65m with an avg of 510 cps and a max of 631 cps; from 53.65-54.7m with an avg of 900 cps and a max of 1865 cps; from 55.09-57.35m with an avg of 325 cps and a max of 616 cps; from 58.0-58.67m with an avg of 640 cps and a max of 1161 cps; from 60.9-61.4m with an avg of 825 cps and a max of 2028 cps; from 61.85-62.12m with

JL08-100 77.03 96.87 FI.por.fp Coarsely porphyritic felsic intrusive. Unit is black to salmon coloured. Consists of large phenos of quartz and felspar. Pheno intensity ranges from intense to locally trace. Feldspar phenos periodically contain biotitic nuclei. Magnetism is moderate to strong. White quartz vein at 92.75 - 92.81m. Sharp lower contact oriented 85 degrees to core axis. Unit is genrally undeformed, with little evidence of straining. Some very weak foliations visible in biotite.

JL08-100 96.87 101.34 MT-IV Black to dark grey metamorphosed intermediate volcanics. Moderately to highly foliated, oriented 65 degrees to core axis. Alteration is moderate, locally weak. Hemitization overall is weak, though locally prominent. Disseminated chlorite visible throughout. Occasional vein of neighbouring felsdaprs visible at top of unit. Some chlorite veines visible as well. Patchy black bands of magnetite. �Post kinematic mafic dyke from 98.38 to 98.92, consisting of biotite, dissiminated chlorite, with small (<0.5cm) pophyrys of quartz +/- fp.�Mineralization Highlights:�Weakly mineralized, all readings register background counts when scinted in hand.

JL08-100 101.34 103.53 MI.dk.psk Post kinematic mafic dyke with small (0.5cm) phenos of plag +/- fp. Moderate disseminated chlorite. Biotite rich. Fine grained chill zones towards both top and bottom contacts. Lower contact is broken, top contact oriented 50 degrees to core axis. Non magnetic.

JL08-100 103.53 121.15 MT-IVDark grey fine grained metamorphosed intermediate volcanics. Moderately to highly foliated. Patchy moderately to strongly magnetic. Veins of calcite associated with chlorite veins. Disseminated chlorite and biotite throughout. Patches of feldspars from 117.37-117.75m. Moderate to strong hematization from 118m to end of unit. Lower contact is sharp and concordant with an angle of 50 tca. �Mineralization ranges from background to a high of 3159 cps throughout the unit, with areas of high strain associated with mineralization. Mineralized intervals occur from:�105-106: max of 3159 cps and avg of 810 cps. �114-121m, ave: 257cps, max: 749cps


Hole ID From (m) To (m) Lithology Code DescriptionJL08-100 121.15 122.92 MI.dk.sk Fine to medium grained mafic dyke, syn- to late-kinematic, weakly foliated, moderately to strongly

magnetic, locally porphyritic with phenos of avg size 5-8mm, occupying approximately 5% of the matrix, phenos have been replaced with epidote but were likely feldspar initially. Veinlets and vuggy areas of epidote. Moderate amounts of disseminated biotite throughout and weak amounts of dsm ct throughout. Lower contact is concordant and makes an angle of 55 degrees tca. From 122.86-123.16m, there is a granitoid intrusion that is light pink in colour, moderately magnetic, with irregular contacts.

JL08-100 122.92 133.45 MT-IVMedium to dark grey metamorphosed intermediate volcanics, moderately foliated, patchy moderately to strongly magnetic, patchy areas of moderate to intense hematization. Disseminated chlorite and epidote visible in patches. Some veins of calcite, vuggy, appear to be fracture fill. Foliations oriented 70 degrees to core axis. Lower contact blocky and broken. Unmineralized.�Last 95cm of unit is porphyritic mafic dyke with usual phenos, and veines of chlorite. Little deformation.

JL08-100 133.45 138 MT-FV.por Metamorphosed felsic volcanics, fine grained. Stongly hematized throughout. Usual phenos of quartz and feldspar, though not nearly as abundant as usual from this lithology. Weak to moderately magnetic. Some dsm magnetite. Fracture fill epidote visible locally. Mineralogy is predominately feldspar and hematite. Some tiny FFL calcite. Some smokey quartz veinlets. Bottom contact blocky and broken.

JL08-100 138 144.57 MI.dk.porPorphyritic mafic dyke, highly chloritized, unit is block and broken for majority of interval. Many tiny angular feldspar pophyrys visible throughout unit. Overall colour is dark green, signifying chloritized matrix. Moderately biotitic. Phenos of ct +/- also visible. Some fracture fill carbonate veinlets. �139.25 to 139.97m sees return to previously described metamorphosed felsic volcanics. �Afterwards, unit is increasingly chloritic, with patches of hematite, more than likely from adjacent unit. Increased in carbonates towards lower contact. Weakly magnetic.

JL08-100 144.57 166.68 MT-IVReturn to intermediate volcanics. Unit is very lowly hematized. Overall colour is grey, increasing in hematization to sub-moderate, locally pervasive. Some phenos of chlorite, Some dsm feldspar. Some fracture fill cacite. Dsm epidote also visible in patches. Unit is weakly to moderately foliated. Older, more mafic veins have been altered to chlorite and chlorite-actinolite and have also been folded. Younger generation veins of feldspar and quartz are not folded and are aligned parallel to the foliations. K-spar alteration of the younger generation veins. At 163m, one of the k-spar altered veins shows en echelon fracturing. Minor carbonate associated with the mafic and feldspar veins. Unit is blocky and broken over 153-155m with no evidence of gouge material. Upper contact oriented 80 degrees to core axis, while lower contact is oriented at 70 degrees tca. Both upper and lower contacts are sharp and concordant.


Hole ID From (m) To (m) Lithology Code DescriptionJL08-100 166.68 183.21 FI.por.fp

Dark red-pruple, coarsely porphyritic feldspar felsic rock. Unfoliated to very weakly foliated. Non-magnetic. 20-40% rounded feldspar phenos, 2-20mm in size, most of which have a biotite-rich +/- very fine grained feldspar (?) nucleus, twinning or radial zoning visible on coarser phenos, phenos are partially k-spar altered, minor broken phenos, few 2-4mm ct phenos near lower contact. Fine grained, moderately hematized groundmass, looking mostly felsic but with small patches of ct + bt with trace vfgr pyrite. Phenos less concentrated for about 30cm at each contact, hematization is stronger at both contacts, and foliation intensifies closer to the lower contact. Ct+actinolite+/- carbonate coating, very minor. Sharp lower contact at 60 degrees tca.

JL08-100 183.21 193.05 MT-IVDark green to dark red, vfgr, moderately foliated, intermediate meta-volcanics. Top 6m similar to previous MT-IV unit, is moderately magnetic with minor PE ct alteration, locally 1mm wide feldspar phenos (lamellar). Rest of unit has patchy hematitic alteration, is non-magnetic, and is mineralized with folded 1-4mm carbonate-rich + ct veins. Unit seems brecciated over the last metre with elongated/strongly foliated clasts defining the foliation, some clasts very augen-looking. Rare qz+k-spar clasts are elongated, mostly aligned with the foliation, and are found in the lower part of the unit. Last 20cm of unit is feldspar porphyritic. Unit is locally blocky. Lower contact is irregular.�Mineralization (is cut bu lower porphyritic intrusion):�Between 189-190m, avg 1200 cps and max 2681 cps; �between 190-191m, avg of 553 cps and max of 1508 cps; �from 191-192m, avg of 423 cps and max of 1882; �from 192-193m, avg of 411 cps and max of 748 cps.

JL08-100 193.05 204.25 FI.por.fpDark orangey-red, feldspar porphyritic felsic meta-volcanic, coarse grained, similar to previous porphyritc unit, only minor k-spar alteration of the phenos, very fgr groundmass with PE hematite + k-spar alt, biotite nuclei are less prominent, possibly qz phenos (?), weak foliation defined by aligned phenos and discontinous biotite bands, twinning and/or zoning evident in the coarser phenos, minor discordant carbonate veinlets, moderate to strong PE magnetism, concordant bands of vfgr material that is strongly magnetic and found mostly up-hole. Last 1.5m is broken. Minor ct + actinolite coating on fractures. Foliation increases down-hole. Lower contact is wavy at approx. 55 degrees tca.

JL08-100 204.25 208.18 MI.dk.sk Dark grey, syn- to late kinematic mafic dyke. Upper 1.5m is finely feldspar porphyritic with phenos % decreasing downhole (30-10%), weakly fol, non-mag, wk to mod ct altn. Localized coarser (0.5cm) fp phenos. Lower part is vfgr with minor concordant qz veins. The lower part could be a short MT-IV interval. Lower 0.5m had qz + fp blebs. LCT is sharp at 80tca. ��205.73-206.26m: mgr granitic intrusion, wk foliated, wk pa mag with minor mafic dyklets. Qz blebs + cb vts trgt. Both contacts are concordant with fol. Minor ep altn (fp replacement?)


Hole ID From (m) To (m) Lithology Code DescriptionJL08-100 208.18 219 FI.gr

Med greyish pink, mgr fps porphyritic granitoid. Wk fol defined by thin discontinuous bt bands. Pa wk mag. 4-5% 2-7mm fp phenos. Local minor saussurization of phenos. Minor kspar altn on phenos (localized downhole). Higher concentration of large phenos at UPC (20%) over approx. 12cm. 2mm concordant qz vein at 214.82m. Ct +ac +/-cb coating on fractures. Odd large (1-7cm) vfgr mafic blebs (xenos?). Series of short fgr mafic dykes between 209.90-215.42m (all similar, syn- to late kinematic but one that is ct-rich syn-kinemtic), all contacts are sharp and discordant to fol. �� EOH (July 12, 2008)

JLM08-002 0 3.26 OVBD overburdenJLM08-002 3.26 8.2 MI.dk.sk unit is very broken and rubbely. Appears to be a mafic dyke with a small granite intrusion? Maybe a

boulder intercepted by the drill as it is close to the top of the hole. Dyke contains phenos ~0.1-0.2cm in diamerter and some minor veining . Contact is undeterminable.

JLM08-002 8.2 12 MT-IV Red to dark gray metamorphosed intermediate volcanics. Unit is moderately to highly magnetic indicating magnetite content and also containing k-feldspar. This unit also conains small veinlets of calcite that cut the core in places at 10deg t.c.a. Again, the unit is extremely broken so orientation measurements are difficult and contacts are undistinguishable.

JLM08-002 12 19.2 MI.dk.sk Dark gray-black syn-kinematic mafic dyke. Unit contains phenos of plag and evidently k-feldspar near the top indicated by pink colour. Dyke also exhibits some veining of calcite, cholorite and epidote with some blebby quartz near some veins. Again the unit is very rubbly and broken with very gradational and busted contacts. Unit is non-magnetic.

JLM08-002 19.2 58.1 MT-IVReturn to dark red and gray/black unit of metamorphosed intermediate volcanics. Unit contains k-feld, and is moderately to strongly magnetic, again indicating magnetite content. Unit is occationally viened by a dark mineral, likely magnetite. Calcite appears in veins throughout the unit and have a general orientation of ~15 deg t.c.a. Hematization occurs in viens throughout the unit as well. Small viens and bands throughout the unit also contain chlorite.��Unit is cut by a minor mafic dyke at a depth of 54.65 - 55.03m with upper and lower contacts of 50 and 45 deg respectively t.c.a.��Mineralization begins at ~27m through to 56m with an average of: 654.78 cps and a max of: 6383 cps, including values of: 4079, 3064, 2646, 1181, 2163 4183 and 1129.


Hole ID From (m) To (m) Lithology Code DescriptionJLM08-002 58.1 60 MI.dk.sk

Dark gray/black syn-kinematic chloritized mafic dyke with a diabase texture. Sparce blebbs of quartz and/or feldspar exist throughout with a max diameter of 1 cm . Unit contains couple of tiny calcite veinlets and is non magnetic. Also contains biotite. Lower contact was determined via magnetism and is not easily visible. Upper contact is sharp and make an angle of 30deg t.c.a.

JLM08-002 60 75.61 MT-IV Return to moderately/strongly magnetic red/dark gray-black metamorphosed intermediate volcanics. As usual this unit contains a large amount of k-feldspar and exhibits hematization at some veins that are generally composed of calcite. Locally well veined areas of chlorite, calcite and possibly biotite or some other vitrious fine grains of dark mineral exhibit vuggy texture. The units lower contact is sharp and makes an angle of 55 deg t.c.a. ��Unit is cut by a small mafic dyke at a depth of 68.92 - 69.44 that has a shape upper contact of ~45deg t.c.a. and a lower contact that is broken and undeterminable. This dyke contains biotite and trace pyrite and chalcopyrite.��Mineralization begins at ~72m

JLM08-002 75.61 77.3 MI.dk.skanother good old non-magnetic syn-kinematic mafic dyke. Our dyke is dark-gray to black containing a lot of biotite throughout and some calcite blebbs and veinlets as well as phenos of felspar/quartz (~0.1 - 02cm in diameter) which appear more elongate at the contacts. The upper and lower contacts are sharp and make angles of 55deg t.c.a. the cross section of a minor quartz vein reveals small lathes (0.4cm x 0.1cm) of some black vitrious mineral possibly biotite.��Mineralized core begins at ~72m…

JLM08-002 77.3 94.94 MT-IVReturn to previously described metamorphosed intermediate volcanic. Contains a large amounts of k-feld veined and foliated with chlorite, calcite, biotite. Frequent banding of veins and flowy texture generally oriented ~40deg t.c.a.��Mineralization was intercepted at 72.00m with an average of , a max of , including high values of

JLM08-002 94.94 96 MI.dk.sk Dark gray/black chloritized syn-kinematic mafic dyke containing veinlets of calcite and also containing biotite. Upper contact is sharp and makes an angle of 40 deg t.c.a. Lower contact is broken but seems to have been sharp also. Unit is non-magnetic.


Hole ID From (m) To (m) Lithology Code DescriptionJLM08-002 96 130.45 MT-IV Return to strongly magnetic metamorphosed intermediate volcanics. This red to dark gray/black unit

contains K-feldspar, magnetite, Chlorite, +/- epidote. It is well foliated with flowy texture at an angle of ~40deg t.c.a. that exhibits some veinlets that roughly follow the orentation of foliation containing calcite, +/- chlorite that are occationally hematized. Unit contains a minor non-magnetic syn-kinematic mafic dyke at 118.22 - 118.59m depth with sharp upper and lower contacts making angles of 50 and 35 deg t.c.a. respectively.

JLM08-002 130.45 132 MI.dk.sk fine-grained Medium grey mafic dyke containing small lathy feldspar phenos up to 2mm in size. Unit is non magnetci and moderately foliated with occational veinlets of a dark green mafic mineral (chlorite?).


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Drill Hole Log JL08-085 Page 1 of 106

345 357.04 MT-CO.pl.my Mylonitized Metamorphic Conglomerate; Unmineralized; Non-magnetic

357.04 387.68 MT-IV Metamorphic Intermediate Volcanic; Mineralization: Spot high of 315 cps occurs approximately 20cm below the upper contact of the MtIV unit; 25cm zone of elevated values with a high of 696 cps centered on 362m; Moderately to strongly magnetic

387.68 401.8 MT-IV Metamorphic Intermediate Volcanic; Unmineralized. Weakly magnetic

401.8 403.7 FI.por.fp Coarsely porphyritic felsic intrusive (feldspar porphyry); Unmineralized. Non-magnetic

403.7 409.83 MI.dk.psk Post kinematic mafic dyke; Unmineralized. Non-magnetic

409.83 412.03 FI.por.fp Coarsely porphyritic felsic intrusive (feldspar porphyry); Unmineralized. Moderately-magnetic

412.03 413.86 MI.dk Undifferentiated mafic dyke with inclusions of feldspar porphyry; Unmineralized. Non-magnetic

413.86 487.41 MT-IV Metamorphosed Intermediate Volcanics; Unmineralized. Moderately to strongly magnetic

487.41 488.79 FI.por.fp Coarsely porphyritic felsic intrusive (feldspar porphyry); Unmineralized. Very weakly to non-magnetic

488.79 502.57 FI.dk Felsic dyke, unmineralized, non-magnetic

502.57 504.01 MI.dk.por Mafic dyke, porphyritic, unmineralized, non-magnetic

504.01 517 MT-IV Metamorphosed Intermediate Volcanics; Moderately to strongly magnetic, unmineralized

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197.15 199.22 MI.dk Dk gy, fgr mafic dyke with very small spotting trgt (possibly phenocrystic) & a slightly felty texture. Occasional blebs of qtz-carbonate material. Late hairline carb vts trgt. Non-mtc.

199.22 216.35 MT-IV Gy, extremely fgr to aphanitic, massive intermediate volcanic; Moderate to abndt carb-chl vnng & stockworking w biotite selvages; Moderate, mico-scale extensional fractures filled w carb & occ clasts of surrounding MT-IV. Bleaching alteration from 200.45-201.4m. Non-mtc. Intruded by multiple small, sublte, very fgr mafic dykes. Mnr epidote & hemative selvages on vnng downhole toward LCT (same alteration found in the conglomerate unit below). LCT irregular.

216.35 222.07 MT-CO.pl Typical multi-coloured, moderately sheared, 'fruit cake' conglomerate; Abndt hem & epidote alteration of matrix w aprx 30% sub-angular to subrndd clasts of MT-IV & qtz generally less than 2cm but ranging up to 5cm in size. Patchy, weak magnetics.

222.07 227 MT-CO.pl Gy, ambiguous unit - probably low to no clast conglomerate sheared out with mnr remenant clasts; Epidote altered nodules with hematite selvages - probably crosscut veins. Thin white bands trgt appearing to be squeezed out clasts. Non-mtc. Late carbonate fracture fill w occasional stockwork of carbonate.

227 233.15 MT-CO.pl Multi-coloured 'fruit cake' conglomerate with intense hem & epidote alteration; also a tan-coloured alteration trgt - poss albite? Abndt sub-angular to subrndd clasts of qtz, jasper, & volcanics ranging up to 7cm in size. Shearing is variable from weak to moderate trgt. Small micro-fracturing causing mnr displacement w/I clasts. Late hairline carbonate fracture fill & occasional section of intense carb altn (<10cm). LCT @ 45 deg tca.

233.15 243.82 MT-CO.pl.my Pinky-maroon, silicified, hem-dusted unit containing small qtz pieces up to a few mm in size; qtz have small foliation tails. Possibly the mylonitized conglomerate with remnant qtz clasts, or foliated qtz porphyritic unit. Occasional bands of bright orange-pink, hem-dusted albite alteration. Non-mtc. Micro-faulting trgt & hairline carbonate fracture fill.


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243.82 247.4 MT-CO.pl Multi-coloured 'fruit cake' conglomerate with predominant epidote & tan-coloured (possibly albite?) alteration trgt the matrix. Clasts are subrndd to sub-angular jasper, volcanics and occasional felsic. Clasts generally less than 3cm but ranging up to 7cm. Foliation genreally weak w a few sections of strongly sheared conglomerate squeezing out the clasts. Patches of weak magnetics. Spidering hairline carb fracture fill & occasional 10cm section of intense carb alteration. LCT wavy @ 70 deg tca. Alteration encrouches aprx 1ft into the lower unit.

247.4 255.65 MT-FV.por Pinky to maroon, hem-dusted, aphanitic qtz-fsp porphyritic felsic metavolanic; Moderately foliated trgt with increased, strong foliation near the UCT. Qtz & fsp tend to be slightly elongate in the plane of foliation & some have tails indicating mnr dextral rotation. Aprx 2% phenos genrally 1-2 mm but up to 5 mm in size. Hematite alteration as phenocryst selvages & along filled, hairline fractures. Occasional chl replacement vns. Contains 2 small chlzd & foliated mafic dykes less than 50 cm in size w one at LCT; LCT fairly gradual.

255.65 266.95 MT-FV.por Typical qtz-fsp porphyritic felsic volcanic w aprx 20% fsp & blue qtz phenos. Pervasive disseminated hematite trgt. Fsp phenos tend to take up mnr hematite alteration. Qtz phenos tend to be smaller ranging up to 5mm in size & fsp phenos range up to 1cm. Mnr qtz vnng & chl vts trgt. Spidering, hairline carb fracture fill trgt. Weakly to moderately mtc trgt. Two small moderiatly foliated & chltzd mafic dykes less than 30 cm in size. LCT gradual & marked by change in alteration. Last meter or so by LCT non-mtc.

266.95 279.4 MT-FV.por Qtz-feldspar porphyritic felsic volcanic w strong foliation squeezing out the phenos & leaving only a few small qtz phenos. Weak to moderate epidote, hematite, & tan-coloured albite (?) alteration along foliation. Nodules of epidote-chl slightly stretched along foliation & ranging up to 4 cm in size - possibly crosscut veins (?). Carb filled hairline fractures & healed fractures trgt. Unit becomes very stongly foliated, almost mylonitized, downhole - phenos are almost completely squeezed out; Epidotized vnng still present & slightly more elongate. Mnr dyking trgt - fg chtzd mafic dykes crosscutting foliation - aprx perpendicular tca. Non-mtc. LCT sharp & irregular.


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279.4 309.7 MT-CO.pl Multi-coloured, weakly foliated, heterolithic conglomerate with variable patchy & occasional clast epidote alteration uphole & sections of pervasive epidote alteration of the matrix trgt. Variable sub-angular to subrndd clasts of japser, qtz, felsic & intermediate volcanics, & mgr intermediate intrusive, ranging from a few mm up to 10 cm in size. Size & distribution of clasts varies trgt possibly representing a fining upward sequence. Aprx 30-40% clasts. Abdnt carb & epidote hairline fracture fill & alteration on jts & fractures. Calcite, siderite (oh my god! The tan-coloured mineral is siderite!), epidote & chl vts trgt. Occasional very small, heavily chloritized, fgr, porphytitic mafic dyke. Becomes weakly magnetic downhole. Pervasive hematite alteration of matrix & clasts w spot high mineralization @ LCT. Spot high of 473 cps @ LCT. Mineralized & hematized fluids probably exploiting the conglomerate-dyke contact.

309.7 311.12 MI.dk Fgr intermediate dyke with amphibole & lathy fsp. Relatively unfoliated. Weak patchy mtc. Trace cpy. UCT has a spot high of 302 cps.

311.12 315.73 MI.dk Pervasively chltzd fgr mafic dyke. Non-mtc. Calcite along jts & fractures. LCT @ 65 deg tca.

315.73 317 MT-IV Med gy, very fgr intermediate volcanic. Unfoliated. Moderately mtc trgt. Hairline carbonate fracture fill. Trace pyrite. E.O.H. @ 317 m.


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Drilling Company: Springdale


0 3.52 OVBD Overburden. Hole started on May 20th.

3.52 5.77 MI.dk Dark green/grey, heavily chloritized porphyritic mafic intrusion. No fabric visible. 0.2 to 1.0 cm euhedral feldpsar phenocrysts (1%) and fine (<2mm) relicts of fps phenos (2%). Minor ct vts stockwork. Contacts are broken up.

5.77 13.87 MT-IV Dark purple/grey, very fine to fine grained metamorphosed intermediate volcanics. Core is extremely broken up (sitting right below ovbd). Non-magnetic, unmineralized. Very weak foliation defined by thin bands of dark material and by set of aligned carbonate veinlets (minor). A few chloritized undifferentiated mafic dykes intrude the units (all in pieces and less than 15 cm). Ct +/-hm alteration throughout. LCT (w/ MT-CO) is irregular but sharp (over 1cm).

13.87 23.44 MT-CO.pl Dark green to pink moderately sheared conglomerate unit. Clasts sizes range from 0.2 to 2cm. Number of clasts decreases downhole. About 10% elongated clast at top of unit. Only rare clasts after 19.50m. Groundmass is similar to MT-IV unit above: dark purple/grey, very fine to fine grained material (could the MT-IV be a clastless MT-CO?). Clasts are polylithic, brown, green, pink… but most clasts are light to dark green with ct +ap +/-ac +/-fps. Med hm alteration throughout unit. Several sets of micro-fractures with approx 1mm bleaching on each side. Non to weakly magnetic wk folation defined by elongated clasts. LCT sharp at 45tca.

23.44 37.96 MT-IV Dark green very fine to fine grained metamorphosed intermediate volcanics. Mod to stgrongly magnetic. Soft with weak ct alteration. About 15% cb veinlets (stockwork). Weak foliation defined by alignment of fine grained light colored minerals (clays, fps, mt, leucoxene). Sporadic 5-20cm soft, chloritized post kinematic mafic dykes. LCT is gradational, over approx 20 cm: stockwork veining goes down to <1%, mt drop to close to nil, ct alteration goes down and hm alteration goes up (about 2-3%).

37.96 52.05 MT-CO.pl.my pink/red to dark red, aphanitic, strongly altered, mod sheared, metamorphosed conglomerate. Low content of clasts. Non magnetic, hm alteration increases downhole. Mod silicified. Minor elongated chloritized clasts (1-2%). Some rounded fine grained ep+ct-rich ppb (ppb relicts?). Minor cb vts (<1%). Minor veins (<1%) filled with bt, mt +/- ct. Some bleaching occurs around vts. 1 undiff ct altered undiffirentiated MI.dk at 41.37m. Broken up with some gouge (FLT ZONE). Ct obscured by broken core. 2 short, mod ct altered syn to post-kinematic II.dk at 49.83 (37cm) and 50.07m (80cm).


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52.05 55.39 MI.dk Light green, pink and cream colored, very fine grained syn- to post kinematic II.dk (INTERMEDIATE DYKE). Weak fol defined by colored bands with blurry con in between. UPC lost in broken core. LCT with MT-CO sharp at 65tca.

55.39 61.26 MT-CO.pl Similar to unit above II.dk. Strong hm alteration with minor ct altn. Mod sheared. Fol defined by colored bands and minor aligned elongated clasts. LCT obscured by broken core. Minor cb vts (<1%). Groundmass is non-mag. Some mag vts (mt +bt +/-ct).

61.26 65.5 MI.dk.pk Dark green, post-kinematic mafic intrusion. Most of the minerals have been replaced by ct. Remnants of possible fps phorphyroclast replaced by light green clays +ct. No visible fabric. Some <10cm sections are highly broken up with some gouge (FLT zones). Non-mag.

65.5 73.91 MT-CO.pl Dark red, mod sheared, metamorphosed conglomerate with mod to strong hm alteration. Similar as unit above dykes. Very low clast content but some bands with diff mineralogy (fgr clays?) suggest sheared clasts. Strong to mod hm alteration, varies trgt. Clast-like elongated ct altered zone (w/ fgr ct, bt, +/-ep +/-cb +/-mt, and some have thin kspar selvage). Core trgt the whole unit is partially to highly broken up. LCT obscured by broken core. Groundmass is very similar to the altered MT-IV. This unit was defined as MT-CO because of the rare clasts, bcs it's non-mag and no cb stockwork.

73.91 79.69 MI.dk.sk Dark green/gray, weakly foliated, strongly ct altered syn-kinematic mafic intrusion. Soft. Similar to MI.dk.sk above previous unit. Mod mag. Presence of relict porphyroclasts filled with clays and vfgr ct. Weak fol define by alignmed ppc. Minor cb veining (<1%). LCT sharp at 80tca.

79.69 90.87 MT-IV MT-IV. Some short sections look definitively clastic (2x <20cm) but overall unit is dark red, vfgr to aphanitic, with some ct +ep altered tube-like veins (As seen in MT-IV in hole JL08-086). Ct +ep also seen as 0.2 to 1cm bands (<1%). Hm alteration is less than in MT-CO uphole but still strong. Mod silicified. Cb as irregular blebs (w/ ct +ep +"kspar selvage") and as rare vts (<1%). LCT with conglomerate is gradual over 10cm. The ct alteration increases close to LCT but blebs get smaller. The alteration overprints the primary fabric and the presence of a foliation is hard to assess. Non-mag. 8cm fault zone at 88.65 with gouge and breciated MT-IV and cb vns.


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90.87 93.02 MT-CO.pl Green, red and light brown polylithic conglomerate. Weakly to mod sheared. Shearing stronger close to UPC. Blebby ct alterations still present and more intense than in unit above. Core competent. Clasts are subrounded, 1-10mm, made of light brown mudstone, purple jasper chert, kspar. Rare quartz crystals. Groudmass is aphanitic to very fgr, dark red. Hm altn pe and strong. Kpsar altn patchy and irregular. LCT obscured by broken core. Pa mag. Wk fol defined by aligned clasts (approx. 45tca).

93.02 98.06 MI.dk.psk Dark green, heavily chloritized, mafic intrusion. No fabric is visible (prob post-kinematic). Fine lathes of fps relicts (replaced by vfgr ct and clays). The "phenocryst" could also be caused by ct alteration. Unit is soft and broken up in place. Sericite coats some fracture walls (<1%). Patchy malachite on fractures as well with rusty dark brown mineral (?) (<1%). Wk to mod mag. Minor cb veining close to LCT. LCT irregular at approx. 40tca.

98.06 103.47 MT-FV.por red to pink, mod sheared, felsic volcanics with elongated blue quartz (10%) and fps (10%) phenocrysts. 50cm flt zone at 90.5 with brown gouge coating. Minor qtz veins (0.1-0.5cm). Mod pe hm altn. Pa kspar altn. Bleaching occurs around microfracture stockwork (1-2%). Small flecks of mt trgt (2-3%). Fol defined by elongated phenocrysts and varies trgt. LCT sharp at about 80tca with increased silicification over last 15cm.

103.47 107.28 MI.dk.psk Dark green, strongly chloritized post-kinematic mafic intrusion. Differs from MI.dk directly above previous unit. This one has specks of bt dessiminated trgt (approx 4%). Non-mag. No cb stockwork but some cb in flt zone (105.30 over 20cm, with dark green gouge). Very soft. Some slickenlines visible on fractures surfaces (ct mineral lineations). LCT sharp at 75tca.

107.28 116.16 MT-CO.pl Dark red, mod to strongly sheared conglomerate. Similar to MT-CO unit above. Clast content varies trgt: from high elongated (mylonitized) clast content close to UPC to low clast content in middle of unit to mod clast content neat LCT. Middle of unit is fgr dark red (strongly hm altered) with only minor large clast. Can see however fgr elongated grains forming foliation. Blebby ct alteration trgt (prob tubular veins w/ ep +/-mt +/-kspar (selvage)). Minor cb stockworking (1-2%)(mostly aligned 45tca). Cb +ep coating on fractures. LCT irregular. Pa mag.

116.16 120.3 MI.dk.sk Dark green, strongly choloritized, syn-kinamtic dykes. Pa ac speckles. Ct stockwork trgt. Some cb vts are aligned and define the only visible foliation (approx. 45tca). LCT sharp at 75tca. Pa mag. Minor cb ppb (<1%). Some fgr red material coating on some fractures.


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120.3 128.37 MT-CO.pl Distinctive dark purple ( aphanitic groundmass) sheared conglomerate. Nature of clasts is similar to one from comglomerate units above. Clast content is higher in this one. Clast are subrounded, sub- to elongated (some even look mylonitized but only over small zones). Mod to strong ct alteration between clasts (more in zones of high clast content). First 5 meters have a low to mod clast content. LCT sharp at 30tca.

128.37 132.28 MI.dk.por Dark green, strongly chloritized, syn-kinematic fps porphyritic mafic intrusion. Wk fol defined by aligned of fp phenos (lathe-like, 1-2mm) but could also be due to flow direction and not to stress. Minor cb stockwork +/-cb (1%). Approx. 10cm chilled margins at both contacts with strong ct alteration (aligned with contacts). UPC at 30tca and LCT at 45tca.

132.28 155.64 MT-CO.pl Green, red, purple clast-rich, mod sheared, metamorphosed conglomerate unit. Distinctive "fruit cake" texture seen in previous holes. Less hm altered than MT-CO uphole. Hm alteration varies trgt from weak to mod, same with ct altn. Clast sizes range from 1mm to approx 10cm. Clasts material includes mudstone, jasperite, IV, quartzite, and kspar altered material. Clasts are sub-rounded to angular. Minor cb stockwork starting at approx 141m until LCT. Cb also in 5-10mm veins (<1%). Pa mag (wk to strong) due to mag clasts or to fine dsm mt. Groundmass is aphanitic, red to green to purple depending on the alteration. Top of unit has about 20% clasts, up tp 35% downhole. Fol defined by aligned clasts (elongated). LCT sharp at 45 tca 87cm syn-kinmetic chloritized mafic dyke at 144.74m

155.64 161.13 MI.dk.sk Dark grey, fgr, syn-kinematic mafic intrusion. <1% dsm specks of pyrite. No other visible sulphides. About 10% fgr angular hb, 15-20% pe fgr ct and about 5% dsm fgr mt. Ac +ct coat fracture walls (ac fibers might show directoin of movement). One angular 2mm wide MT-CO xenolith. Mod ct alteration. Wk fol defined by alignment of white minerals (fps, clays). UCT sharp at 45tca with 1cm aphanitic ct-rich chilled margin. LCT sharp at 45tca with 1mm dark grey aph chilled margin.

161.13 180.16 MT-CO.pl Conglomerate. Typical "fruit cake" texture. Similar to unit above pyritic dyke. Large range of clast sizes and material (see desc fom units above). Groundmass is approx 5% of unit (aphanitic, dark purple, red or green, depending on alteration). Shearing intensity increases downhole, fom wk to mod. Altns vary trgt (wk to strong hm, wk to strong ct, wk kpsar. Fol defined by elongated clasts. LCT sharp at 40 tca


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180.16 181.95 II.dk Dark green, fine to mgr syn-kinematic, chloritized, intermediate intrusion. <1% cb stockwork (postdating intrusion bcs cross-cut LCT). Non mag. Primary fabric partially obscured by ct altn. Wk fol defined by aligned fgr fps. 1% dsm ac . 15-20% fps, Minor bt, rest is fgr ct and/or clays. LCT sharp at 35tca.

191.6 203.9 MT-CO.pl Unit is Dark grey/green to lighter grey/green. Grain size changes from a coarse grained (~1.0-5.0cm and <) conglomerate to a finer grained (~0.5-1.0cm) at ~197.90m and back to the coarser grained conglom at ~201.60m. Contains angular-subrounded clasts containing epidote, quartz, chlorite, and hematite . Mild to medium deformation towards ends of unit with very little deformation in center at finer grained section.

203.9 205.23 MI.dk.psk contains relict hornblende phenocrysts and feldspar. Strongly altered to chlorite. No obvious deformation or fabric.

205.23 227.19 MT-CO.pl conglom like before mylonitized at ~118m to about 220m. Ends with an irregular contact with a mafic dyke at 227.15m. Contains a large (12cm) milky quartz vein at 214.27m.

227.19 229.67 MI.dk.psk dark gray/black unit. Contains epidote veining at 228m. No other evident fabric. No obvious phenos.

229.67 239 MT-CO.pl dark gray-green conglom containing rounded to sub-angular clasts. Clasts are 0.2-3.0cm containing epidote, quartz, hematite. Weak to moderate magnetism. Sharp contact with upper unit making angle of ~25deg with core axis. Messy lower contact. Contains a small syn-kenematic (or post-kenematic) mafic dyke intrusion (with sharp contacts at 30deg angle to core axis) at 233.70 - 233.96m. Minor-moderate calcite veining.

239 247.66 MT-CO.pl.my purple-dark gray strongly deformed conglom unit. Becomes darker (dark gray-black) near bottom of unit. Strongly magnetic throughout with just a few patches of weak-moderate magnetism. Low content of clasts. Clasts are <1cm with just a few larger clasts (~4cm) near top of unit, where it is more purple. Contains, epidote, chlorite, quartz.

247.66 253.6 MI.dk.psk Dark gray unit exhibiting little foliation/fabric. Makes sharp contact ( ~15 deg to core axis) with above mylonitic conglom.

253.6 255.76 MT-CO.pl.my dark gray strongly deformed mylonitic conglom. Very few visible clasts (elongate). Gradational contact with above mafic dyke.


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255.77 258.56 MT-CO.pl.my very broken up rubbley. Red/purple unit grading to a greenish colour some patches are weakly magnetic, however, unit is largely non-magnetic. Highly deformed, no visible clasts. Intruded by a dark gray mafic post kinematic dyke (256.35 - 257.30m)

258.56 259.85 MI.dk.pk Dark gray aphanitic dyke exhibiting deformation in alternating beige bands.

259.85 262 MI.dk.pk Red unit. Very rubbley trouble. Exhibits a lot of banding

262 263.7 MI.dk.psk Dark gray aphanitic dyke. No visible fabric. Contains calcite veins

263.7 268.88 MT-IV red and dark gray/black aphanitic meta volcanic unit. Calcite, chlorite and epidote veining. Strongly magnetic.

268.88 270 MI.dk.pk Dark gray/green unit cut by several small dykes: @268.66 - 270m (sharp contacts at both ends making ~50 deg with core axis). Highly deformed with clacite (and other) veins having a brecciated appearance. Contains phenos ~0.2cm in size.

270 324.13 MT-IV Alternating black-red intermediate volcanic unit. Strongly magnetic. Contains some sulphides. Moderately veined with calcite, chlorite and epidote (higher concentration of epidote veins above 287m) (heavy calcite veining at 309.80 - 310.80m) . Intersected by a dark gray pre-kenematic mafic dyke @ 270.66m - 271-49m containing <0.1cm lathes and many deformed calcite, epidote and other veins. A post-kenematic mafic dyke at 287.09 - 287.30 containing ~0.1cm phenos. Another dyke post-kenematic and mafic at 302.10 - 302.70m with sparce <0.1cm phenos. High scint readings of ~400-500 at 300m and further down hole.

324.13 325.31 MI.dk.psk Dark gray unit exhibiting little veining. Phenos are 0.1 - 0.2cm in size. Very little visible fabric. Sharp upper and lower contacts making an angle of 40 deg to core axis.

325.31 333.3 MT-IV Red and black unit containing magnetite, biotite, chlorite. Veined with carbonate veins. Very magnetic. Scint readings averaging 700 cps. Messy lower contact.

333.3 357.04 MT-MI.fgr dark gray-black silicious unit. Some patchy magnetism but mostly non to weakly magnetic. Exhibiting foliations, deformed flowy tectures epidote and carbonate veins. Contains quartz, biotite, k-feld.


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357.04 358.58 MI.dk.psk Dark gray-black fine grained unit containing ~0.1cm phenos. At ~257.56m contains a 13cm wide intrusion of lower coarse porphoritic unit (stay tunned). Lower portion of dyke contains some porphyroclasts from said unit.

358.58 373.96 FI.por.fp Dark gray/black feldspar rich unit. Phenos are ~1.0 - 2.0 cm in size and become significantly less dense towards the bottom of the unit. sharp upper contact making a 50deg angle with core axis. Weakly magnetic. Intruded by a fine grained post kinematic mafic dyke containing no phenos at 362.95-363.06m and another small post kinematic mafic dyke 363.50-363.80 m. contacts of both dykes are sharp, angled away from each other and measure 45deg and 30deg to core axis.

373.96 380.55 MT-CO.pl Dark gray-black mafic dyke. Fine grained with few phenos, although they occur in a deformed patch at around 278.70m and below 280m. Sharp upper contact measuring 50 deg with core axis. The top part of the dyke contains feldspar phenos from the above porphyritic unit. The unit is moderately-heavily veined with epidote and quatz. Also containing small amounts of carbonate.

380.55 385.84 MT-IV deformed Dark gray/black to reddish black aphanitic unit. Exhibits moderate beige and greenish banding Moderately to strongly magnetic. Contains epidote, calcite, quartz, and biotite. Syn-kinematic mafic dyke containing biotite and very sparce phenos ~0.1cm located at 282.19 - 282.37m.

385.84 387.04 MI.dk.psk Dark green/gray-black unit. Contains biotite and very few feldspar phenos. No fabric or veining is visible. Top (sharp)contact makes a 60 deg angle with core axis. Lower contact is rough.

387.04 396.86 MT-IV Dark Green-Black and red metamophosed exhibiting bands. Very micaceous and moderately to strongly magnetic. Contains; biotite, k-feld, epidote, calcite, quartz,. An annomolous dark green band at 395.84m depth with 0.1- 0.2 cm phenos.

396.86 398.05 MI.dk.sk Dark gray/black syn-kinematic mafic dyke. Containing ~0.1 - 0.2 cm relict phenos and clacite and other veins. Contains biotite. Sharp lower contact at ~25deg to core axis.

398.05 402.08 MT-IV Dark gray/black and blackish red metamorphosed unit. Moderately to strongly magnetic. Contains quartz, epidote, chlorite, feldspar. As well as very thin calcite, chlorite and quartz veins. A post-kinematic mafic dyke is located at 399.80 - 400.18m and another 401.33 - 401.73m depth. Dykes have sharp contacts with MT-IV unit and exhibit very little veining or other fabric.


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402.08 403.21 MI.dk.sk Dark gray/black syn-kinematic mafic dyke. Contains very few phenos. Moderately veined with calcite, epidote and containing some quartz. Non-magnetic. Sharp upper contact making an angle of ~60 deg with core axis. Lower contact grades into lower unit.

403.21 408.44 MT-IV Dark gray/black-reddish black micaceous biotite rich unit. Fairly heavy veining. Veins contain pyrite and chalcopyrite. There are black veins of some mineral containing quite a bit of chalco and pyrite.

408.44 409.8 MI.dk.psk Dark gray-black predominant k-feldspar located at upper and lower contacts. Very little veining. Non-magnetic.

409.8 424.86 MT-IV Dark gray/black to greenish and reddish black micaceous unit (huge amount of biotite). Contains many veins with pyrite, chalcopyrite (~0.5-0.7%),quartz and some phenos of ~0.2cm size. Moderately to highly magnetic.

424.86 447 MI.dk.sk Dark gray/black unit containing biotite, quartz, k-feld. Large quartz and k-feld veins at 435.15 and 435.16m depth. Some


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0 4.4 OVBD Not recovered.

4.4 5 OVBD Granitic boulder

5 13.35 MI.dk.pk In-situ breccia texture with dark grey fine grained clast of mafic dyke(?) surrounded by fractures filled with carbonate or chlorite. Chlorite rims occur on the fragments that are in a matrix of carbonate. Non-magnetic. Unmineralized

13.35 25.39 MT-IV Where unaltered this rock appears fine grained grey and massive. Weakly to non-magnetic. Blebby to sinusoidally banded hem alteration. The top of this unit has blebby chlorite/hem/kspar alteration, however overall the unit is dominated by red hem staining. (very hard to scratch. The unit becomes an earthy red colour with depth as hematite alteration becomes pervasive and contains closely spaced (~2cm) hairline qtz, carb, kspar, hem vnlts. Several intervals look as though they have been silicified. Both the upper and lower contacts of this unit are defined by intervals of broken core where the actual contact is not preserved. There are several intervals of broken rock within this unit. Unmineralized

25.39 29.49 MT-IV this unit appears the same as the one above but is moderately to strongly magnetic. Upper contact is a broken zone. Lower contact is irregular but sharp (over a few cms) Unmineralized

29.49 37.6 MT-IV MT-IV? Grey with abundant fine hematitic vns at the top of the unit grading down into earthy red intensely stained with banded texture. Bands are often seen in 2-3cm segments that have been fractured and offset. Fine hairline carbonate vns occur and can be spaced ,1cm in some zones. Rare Qtz vns occur typically ,5mm thick. Weakly magnetic. Unmineralized

37.6 45.95 MI.dk Speckled light and dark green. Mafic dyke(?) altered to a chlorite/epidote rich assemblage. Up to 3cm epidote vns occur and are noted to contain trace amounts of malachite and molybdenite. Molybenite is also observed disseminated in the rock. Non-magnetic, unmineralized. Sharp upper and lower contacts.

45.95 48 MI.dk.pk mafic dyke with brittle fractures filled by carbonate (calcite, siderite). In-situ breccia texture. Intensely chloritized. Minor hematite staining.Lower contact sharp and irregular.

48 48.65 MI.dk Fault zone breccia. Matrix of altered rock flour with polylithic clasts (mainly chloritized mafic frags). Abundant carbonate +/-clay cement. Sharp upper and lower contacts.


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48.65 53.46 MT-IV Hematite stained, dark grey aphanitic looking rock. Epidote chlorite hematite +/-kspar blebs give the rock a mottled appearance and alteration textures obliterate primary textures. Hairline carb vns cut the core at variable orientations, spaced a few cms apart and sometimes occur in small swarms. Hematite staining appears to increase towards lower contact. Lower contact is sharp. Unmineralized Non-magnetic

53.46 63.88 MI.dk.por Feldspar porphyritic mafic dyke. 10% white lathe shaped ~2mm relict fspar phenos in a dark grey chlorite rich matrix. Minor biotite. No obvious fabric, interpreted as post-kinematic. Hairline to mm scale carb vns occur typically spaced >10cm. Rare qtz veins containing fine (mm scale) euhedral qtz crystals. Lower contact is sharp and characterised by a 15 chill zone where the rock is fine grained and aphanitic. Strongly magnetic. Unmineralized

63.88 65.68 MI.dk Syn-kinematic aphanitic mafic dyke is breciatted with very little clast movement. Fracture fill and breccia matrix is carbonate. Unmineralized.

65.68 71.88 MT-IV Intermediate volcanic is fine grained and moderately hematite altered. Alteration is patchy and banded and gives a psuedo clastic texture. Carbonate is common in the matrix of non-hematite altered patches and on fracture surfaces. Unmineralized.

71.88 73.8 MI.dk.pk Pre-kinematic mafic dyke with brittle fractures(appear perpendicular to contact) filled by carbonate). Fine to medium grained and intensely chloritized. Weak blebby hematite staining. Lower contact sharp and planer 25 degrees TCA. Unmineralized.

73.8 75.67 MT-IV strongly hematized intermediate volcanic. Shearing through this unit is visible, weak carbonate stockwork and moderate carbonate fracture fill.

75.67 77.05 MI.dk.por Porphyritic mafic dyke moderately chloritized. Lower contact 70 degrees TCA. Minor carbonate fracture fill.

77.05 79.41 MT-IV stongly hematite and chlorite altered intermediate volcanic, very broken and rubbly, weak carbonate stockworking and fracture fill

79.41 83.32 MI.dk.sk fine grained mafic dyke, minor <2% feldspar phenocrysts, pervasive chlorite and epidote alteration and veining. 81.5 to 81.9 m intensely breciatted with chlorite epidote matrix. Upper and lower contacts sharp and irregular.


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83.32 88.64 MT-IV intermediate volcanic with minor late dykes, moderate hematite and chlorite/epidote alteration. Minor carbonate veining with weak carbonate stockwork. MT-IV texture is sheared.

88.64 92.45 MI.dk.pk Fine grained (almost massive) mafic dyke, sharp contacts, minor carbonate fracture fill. Strongly magnetic.

92.45 150.15 MT-CO.pl.my dominantly mylonitized conglomerate where the mylonitic layers (sheared clasts) are often faint to indistinct and the rock can have a more massive appearance. Alteration also acts to obscure primary textures. Non-magnetic. Hairline carbonate vnlts occur spaced ~ <10cm. Upper contact is sharp and oriented at 40tca. Characterized by change in colour, texture, and sharp decline in magnetism. This unit is non-magnetic throughout while the upper unit was strongly magnetic. Alteration is patchy to banded and typically consists of patches of chlorite+epidote+/-carbonate surrounded by dark red hematite staining. Hematite staining also occurs on it's on as blebs or in bands. In some areas the alteration results in a pseudo-clastic texture. Lower contact is sharp and oriented at 75tca. Sections with distinctive clastic (non-mylonitized texture) 120.72 - 121.54 Increased hematite staining 122.05 - 122.86 Three (6,13 and 30cm) intervals of strongly chloritized dyke. Non-magnetic. Contacts sharp and oriented at ~85tca. Overall this rock is very hard, knife streaks on it. There is fine disseminated carbonate and chlorite in the matrix. Possible silicification. 141.76- 143.30m Intense chlorite epidote hematite alteration occurs as blebs and bands. No mineralization observed

150.15 150.91 MI.dk Strongly chloritized mafic dyke. Fine irregular carbonate vnlts. Some small (3mm) patches of pink iron carbonate (ankerite). Lower contact sharp and oriented at 60tca.

150.91 155.05 MT-FV.por 10% ~5mm diameter, rounded quartz eyes with a distinct bluish tinge. Some appear to have a radial texture(?) 15% ~5mm diameter subrounded to elongate (possibly flattened from strain) pink fspar phenos. Chlorite-rich matrix. Moderately magnetic. Unmineralized.

155.05 158.34 MI.dk.psk Chloritized mafic dyke. UC sharp at 85tca. Lower contact sharp at 55tca. Non magnetic. No obvious fabric.


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158.34 164.22 MT-CO.pl.my Mylonitized conglomerate with Intense red hematite staining from upper contact to 164.22m. Banded appearance with mm scale bands. Moderately magnetic. Lower contact indistinct but characterized by a sharp decline in magnetism. Alteration often gives this rock a mottled/blebby appearance. Dykes occur at 161.03 (70cm), 162.08 (14cm), and 162.52 (8cm) with sharp contacts. They are strongly chloritized with no obvious fabric.

164.22 229.68 MT-CO.pl Distinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.) Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Some of the clasts are magnetic but overall the conglomerate is non-magnetic. Most of the unit displays a strong fabric in the form of clast alignment, flattening and bands. This fabric is oriented between 45-85tca. Appears to be at least two generations of carbonate. Fleshy coloured carb that occurs in bands parallel to foliation or as breccia/conglomerate matrix and later hairline white carbonate veins that typically cut foliation and occur at a low angle to core axis (~20tca).

229.68 231.7 MT-CO.pl.my Mylonitized conglomerate within larger package of clastic weakly deformed conglomerate. Sheared out clasts create bands ~2mm thick of vary colour and mineralogy. Some augens occur. Bands oriented at ~60tca

231.7 257.17 MT-CO.pl Distinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.) Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Some of the clasts are magnetic but overall the conglomerate is non-magnetic.

257.17 259.52 MI.dk.psk Upper contact sharp with aphanitic chill zone for ~20cm. Becomes coarser grained with depth. Relict hbl phenocrysts now altered to biotite+chlorite occur up to 3mm and comprise ~10% of the rock. Matrix is strongly chloritized. Lower contact sharp but irregular. Magnetic at the top but non-magnetic through the rest.

259.52 264.62 MT-CO.pl Magnetic and polylithic with moderate fabric oriented at ~75tca.


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264.62 266.67 MI.dk.psk chloritized mafic dyke showing no oriented fabric. Fine mm scale white lathes are interpreted as relict fspar phenos. Hairline carb vnlts cross-cut the core. Non-magnetic. Unmineralized. Sharp upper and lower contacts.

266.67 269.77 MT-CO.pl Conglomerate - description as per previous. Weakly to moderately magnetic.

269.77 270.47 MI.dk Strongly chloritized with no obvious fabric. Sharp upper and lower contacts oriented at ~60tca.

270.47 276.29 MT-CO.pl Distinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.) Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Some of the clasts are magnetic but overall the conglomerate is non-magnetic.

276.29 277.95 MI.dk Strongly chloritized mafic dyke

277.95 285.83 MT-CO.pl Distinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.) Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Moderately magnetic.

285.83 288.04 MI.dk Dark grey aphanitic rock with mottled appearance resulting from patchy light green chlorite alteration and chloritic veins. Moderately magnetic.

288.04 293.11 MT-CO.pl Distinctly clastic metamorphic porphyry. Polylithic. Clasts are typically <5cm in size however larger clasts up to 10's of cm's also occur. Clasts are subangular to subrounded and commonly show evidence of deformation (flattening, tails etc.) Locally there are areas that appear mylonitized. Clast types include black aphanitic clasts, quartz clasts, red hematitic aphanitic clasts, and green intensely chloritzed clasts. The matrix is typically chlorite rich. Some of the clasts are magnetic but overall the conglomerate is non-magnetic. Patchy hematite alteration.


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293.11 299.84 MT-CO.pl.my Mylonitized conglomerate with frequent small (<50cm) thick dykes. Dykes occur at 296.61 (14cm); 297 (12cm); 297.20 (13cm); 297.43 (10cm); 297.79 (31cm); 298.36 (24cm); 298.80 (17cm) Red green and white ~2mm thick bands interpreted as mylonitized conglomerate clasts. Lower contact gradational.

299.84 317.55 MT-IV Aphanitic dark grey competent rock. Magnetic and mineralized. Hematite staining increases to end of unit which is defined by the sharp dissapearance of hematite staining. Strongly magnetic throughout. Hematite alteration is dominantly banded. Uranium mineralization occurs throughout this unit with spot highs of 580 at 311.8m; 600 at 314.55m; 1400 at 316.66m; and 3100 at 317.23m. This entire interval sampled. Unmineralized, non-magnetic late mafic dykes occur at 304.65 (14cm); 305.78 (10cm); and 307.17 (20cm). They are all chlorite rich.

317.55 342.57 MT-IV Dark grey aphanitic intermediate volcanic rocks. Local areas of hematite staining. Weak banding is visible locally but not pervasive. Qtz-carb-epid-chl veins occur typically 1cm thick spaced every ~10cm. Mainly strongly magnetic with local sections that are weak to moderatlely magnetic. Mineralized with spot highs of 1700 at 318.85m, 1000 at 320.25m, and 600 at 321.50.

342.57 344.52 MI.dk.psk Porphyritic mafic dyke showing no strain fabric. Fine (1-2mm) white lathes are interpreted as relict fspar phenos. Chloritic matrix. Non-magnetic, unmineralized.

344.52 367.95 MT-IV Dark grey aphanitic massive intermediate volcanic rocks. Strongly magnetic. Lower contact sharp and marked by lack of magnetism in lower unit. Hematite is pervasive and gives the rock a banded appearance. Mineralized with spot highs up to 1109cps.

367.95 368.26 MI.dk Fine grained dark grey mafic dyke. Non-magnetic. In sharp contact with overlying MTIV and underlying qtz fspar porph.

368.26 371.07 FI.por.fp Coarse subhedral 1-2cm relict fspar phenos now altered to qtz+fspar. Matrix is dark grey and fine grained. Moderately magnetic. Lower contact gradational to indistinct.

371.07 382.08 FI.por.fp Mixed zones of fine featureless massive grey rock and coarsely porphyritic felspar porphyry. The two units grade in and out of each other on a 20-30cm scale with no distinct contacts. Weakly to moderately magnetic. Strong felty chlorite texture with mineral alignment defining a foliation.


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382.08 382.8 MI.dk.por Fine grained mafic dyke with ~20% 1-2mm white relict fspar lathes. Dark grey fine grained matrix, chloritic. Non-magnetic. Lower contact sharp but irregular.

382.8 385.29 MT-IV fine grained grey massive rock. Strongly magnetic. Dark fine grained veins ~3mm thick cross cut the core and are typically irregular.

385.29 385.89 MI.dk.por Fine grained mafic dyke with ~20% 1-2mm white relict fspar lathes. Dark grey fine grained matrix, chloritic. Non-magnetic. Upper contact sharp but irregular.

385.89 402.9 MT-IV Grey aphanitic massive metamorphosed intermediate volcanic rocks with patchy to banded hematite alteration. Small carbonate+chlorite veins cut the rock. Weakly to moderately magnetic. High of 323cps at 385m then from 388-390m average of 600cps over the interval with spot highs up to 2100cps. Lower contact sharp and oriented at ~45tca.

402.9 405.87 MI.dk Dark grey dominantly aphanitic mafic dyke with local areas of porphyritic texture. Non-magnetic. At 405.27m there is a ~20cm inclusion of hematized intermediate volcanic rock with irregular margins. Abundant fine biotite and chlorite. Lower contact is sharp but irregular and oriented at ~30tca. Hairline carb vns present.

405.87 414.33 MT-IV Upper contact sharp and irregular. Lower contact sharp and oriented at 90tca. Moderate hematite staining gives the core a pink/grey colour. Carbonate+chlorite vns are irregular in shape and orientation, typically <1cm thick and spaced ~3-10cm apart. Areas of high vein density are typically less magnetic than areas lacking veins. Overall this unit is moderately to strongly magnetic. Spot high of 277cps but otherwise unmineralized.

414.33 415.78 MI.dk Dark grey, non-magnetic mafic dyke. Texture ranges from aphanitic to fine grained equigranular texture. Strong chlorite alteration. No obvious fabric present. Sharp upper and lower contacts. Upper contact oriented at 90tca and lower at 85tca.

415.78 436.3 MT-IV Similar to previous MT-IV unit. Overall the rock is a grey pink colour resulting from moderate hematite staining. Chlorite carbonate vns ~1cm thick occur spaced ~5cm. Moderately magnetic. Mineralized from 420m to 429m with an average cps of 250cps and spot highs up to 374cps. From 429 to 435 mineralized with average cps of 200.


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436.3 438.28 MI.dk Mafic dyke with porphyritic texture. ~ 25% relict fspar(?) phenos now altered. Strongly chloritized. Has a green/white speckled appearance. Non-magnetic. Lower contact sharp at 45tca.

438.28 466.14 MT-IV Similar in appearance to units of MT-IV above. Pink-grey appearance resulting from hematite staining. In areas carbonate chlorite veining becomes so intense (+50%) that the rock has a brecciated appearance (445-446m). From 435 to 445 an average of 250cps. From 445 to 456 the average value is around 600cps with highs up to 3700cps. The rest of this interval the mineralization drops back down to background.

466.14 467.88 MI.dk.psk Mafic dyke intruding the MTIV unit. Dyke margins are sharp and cut veins within the MTIV unit showing clearly that they are later. No evidence of strain fabric within the dyke. Dark grey green in colour and chlorite rich. Quartz veins up to 5cm thick occur in this unit and are not common in surrounding units. These quartz veins host trace amounts of pyrite. This unit is non-magnetic

467.88 473.26 MT-IV Dark grey massive rock with a banded texture resulting from alteration/deformation. 470.60 5cm dark green strongly chloritized dyke.

473.26 475.2 MI.dk.por Composed dominantly of chlorite with lesser biotite and ~10% relict fspar phenos. Fine disseminated pyrite occurs but constitutes<1% of the rock. Non-magnetic. Sharp upper and lower contacts oriented at ~90tca.

475.2 477.04 FI.dk.por This unit is dominated by a diffuse mix of qtz and fspar with local qtz and fspar phenocryst shapes present. Fine disseminated magnetite occurs throughout. Lower contact sharp and oriented at approximately 80tca (beta of 350-oriented core)

477.04 477.68 MI.dk.por ~25% blocky to lathe shaped ~2mm white fspar and relict fspar phenos. Matrix is dark green and chlorite rich. One 3cm quartz vein occurs in this unit. Lower contact sharp oriented at 70 tca (beta of 340). Non magnetic

477.68 496.13 MT-IV Mainly dark grey aphanitic looking rock with local areas of banding, patchy or even porphyritc texture. Moderately to strongly magnetic. Veins are less abundant in this interval and consist of chlorite, carbonate +/- leucoxene. Towards the bottom of this interval large (>5cm) diffuse quartz veins increase in abundance. Matrix appears rich in biotite and chlorite. Lower contact is gradational and indistinct. No mineralization encountered.


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496.13 502.09 MT-FV chlorite blebs in a diffuse qtz feldspar matrix. Milky pink qtz kspar vnlts occur up to 2cm in thickness typically spaced >20cm apart. Overall light pink-grey in colour. Moderately magnetic. Unmineralized. Upper contact diffuse. Lower contact sharp and oriented at ~85tca.

502.09 504.41 MI.dk.por Mafic dyke with 25% ~1-2mm white relict fspar lathes. Matrix is dark grey and chlorite rich. Non-magnetic

504.41 507.39 MT-FV Diffuse feldspar and quartz chlorite matrix. Dark to light grey colour speckled white pink grey green in many areas. To small (12cm) dykes occur in this interval. Lower contact sharp but irregular. Moderately magnetic.

507.39 508.41 MI.dk.por ~25% white 1-2mm fspar lathes in a dark chlorite rich matrix. Moderately magnetic throughout. High angle (10tca) gypsum vein runs through this unit and into the unit above.

508.41 513.68 MT-FV Non-descript grey rock with abundant diffuse quartz veins. Several quartz veins show multiple centre lines. Chloritic matrix contains minor leucoxene.

513.68 514.19 MI.dk Sharp contacts upper 85tca lower 45tca.

514.19 515.74 MT-FV Dark grey with multiple milky pink diffuse quartz kspar veins.

515.74 520.47 MI.dk 2 smaller dykes occur within this dike. At 518.22 m there is a 12cm dyke with 5mm pink fspar phenos and a chlorite rich matrix. At 519.17 there is a 16cm fspar porphyrtic mafic dyke.

520.47 534 MT-FV 522.10m 27cm dyke of porphyritic mafic rock.


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0 1.59 OVBD Overburden and casing

1.59 6.55 MT-CO.pl Beige to light green metaconglomerate. High levels of mudstone visible at top of interval, though decreases with depth. Texture is bimodal, though increasingly fine grained towards lower contact. Appears to be increasingly metamorphosed as unit approches lower contact. Lower contact is very gradual. Unit is moderately clastic at top of interval, and tapers to clast poor with depth. Mineralogy is predominantly mudstone (55%) at top, Large white quartz lens visible at 4.77m, which is then followed by rubble. K-feldspar porphyrys scattered throughout. A few chlorite veines towards lower contact. Some rosy quartz seen towards middle of unit. Weakly magnetic.

6.55 17.08 MI.dk.psk Mafic dyke. Little to no deformation. Very broken/blocky in areas. Occasional K-feldspar and quartz lenses. Some rare mudstone visible, though probably from previous unit. Biotite levels range from moderate to very high. High levels coincide with brittle regions. Prominent chlorite veining. Biotite and horneblende present throughout. Very red feldspar visible towards lower contact. Unit is moderately magnetic. Smokey quartz veine also visible towards lower contact.

17.08 18.18 MT-CO.pl Short metaconglomerate interval. Chlorite, mudstone and feldspar main minerals. moderately mafic. Moderately clastic. Clasts generally ~5cm. Some horneblende and biotite visible.

18.18 48.67 MI.dk.psk Interval begins rich in biotite clasts. Feldspar lenses and phenos visible throughout. Highly chloritized matrix. Biotite ranges from very strong to moderate. Hornebnlende appears to be replaced by biotite. Very brittle areas, once again, characterised by high levels of biotite. Occasional intervals of carbonate veines. Returns to clast rich at ~33m until 34m. Tapers from moderately clastic to poor up to 39m. Weakly magnetic, though increases with depth to moderate. Towards lower contact, chlorite and feldspar veining increases.

48.67 49.71 MT-CO.pl Small metaconglomerate interval. Highly mafic towards upper contact, followed by high k-spar and chlorite occurances. Quartz also present sporadically throughout the interval. Unit is moderately magnetic.


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49.71 55.61 MI.dk.psk Unit begins as fine grained, biotite rich mafic dyke. Some very thin epidote veinlets are visible. This section has not been deformed. Quartz vein at 50.16m. As the unit continues, biotite appears to be replaced by horneblende, resulting in a breccia like texture of horneblende phenos in a chlorite rich matrix. Continues to 50.34m, where texture returns to finegrained, biotite rich matrix with small amount of horneblende, and occasional epidote veins. 51.11m sees return of afore mentioned breccia like texture, though not as chlorite rich, and lacks epidote veins. 51.27 to 51.81 is fine grained biotite rich with some like quartz veinlets. 51.81 to 55.61 is consistently chlorite rich matrix with hornblend phenocrists with consistent epidote veins. Unit is moderately magnetic. Occasional calcite vein. Occasional k-spar pheno.

55.61 56.48 QZ.vn Large qtz vein, some biotite encased within.

56.48 63.91 MI.dk.psk Medium grained mafic dyke. Hornblende phenos dominate in biotite rich matrix. Occasional K-spar pheno. Periodic epidote veins. Quartz also present within matrix. Moderately magnetic

63.91 71.19 MI.dk.por Typical porphyritic mafic dyke. Fine grained biotite rich matrix hosting quartz and feldspar, angular like phenos (~10%). Some chlorite present. Unit has very fine grained chill zones on both upper and lower contacts. Stongly magnetic. Occasional carbonate vein

71.19 78.45 MI.dk.psk Mafic dyke with many chlorite and epidote veins. Occasional quartz and feldspar phenos, 0.5 to 2 cm in size. MODERATELY MAGNETIC.

78.45 88.26 MT-CO.pl.my Very feldspar rich metaconglomerate. Feldspar is red, combined with usual chlorite, epidote and quartz. Periodic sections of highly metamorphism towards lower contact. Weakly magnetic. Increasingly occuring carbonate veines with depth.

88.26 111.02 MI.dk.pk Mafic dyke dominated by carbonate veins. Brittle fracture fill carbonate veines. Occasional rosy carbonate vein. Vein desity ranges from sporatic to intense. Carbonate Veine density tapers with depth. Towards lower contact, previously mentioned chlorite rich matrix hosting hornblende phenos are visible. Weakly magnetic.

111.02 111.86 MT-CO.pl Short interval o f metaconglomerate. Finer grained that typical MT-CO of Jacques Lake. Also appears to be more mafic than usual. Usual chlorite, quartz and k-spar. Non magnetic.


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111.86 122.04 MI.dk.pk Return to mafic dyke dominated by brittle fracture fill carbonate veins. Still occasional rosy carbonate. Chlorite replaces carbonate veines towards lower contact. Usual biotite rich matrix. Weakly magnetic. Occasional k-spar pheno.

122.04 124.4 MI.dk.psk Mafic dyke, high chlorite levels. No carbonate veines, high levels of biotite and horneblende. Non meganetic. Unmineralized.

124.4 133.49 MT-CO.pl Red, feldspar rich metaconglomerate. High levels of feldspar visible throughout interval, starting with ~10cm feldspar vein. Texture is bimodal, though increasingly fine grained towards lower contact. Increasingly deformed with depthk. Lower contact is very gradual. Unit is moderately clastic at top of interval, then becomes deformed, allining clasts into parallel sequences. Non magnetic.

133.49 135.14 MT-IV Weakly hematitic, unmineralized metamorphosed intermediate volcanics. Moderately altered. Strained roughly 30 degrees to core axis. Some feldspar present. Hematite is spotty throughout. Overall dark red texture. Trace epidote and chlorite. Non magnetic. Primary texture.

135.14 140.31 MT-CO.pl Rteturn to previously mentioned metaconglomerate. Moderately deformed. Usual clasts o ffeldspar, chlorite, epidote. Some areas contain high levels of mudstone. Overal light green texture. Large felsic section toward lower contact which borders at roughly 15 degrees to core axis. Increase quartz and feldspar occurances with depth. Typical epidote veines. Carbonate veines visible throughout. Section is non magnetic. Overall a moderately clastic section.

140.31 147.25 MT-FV.por Red feldspar volcanics. Section is moderately deformed. Typical phenos of k-feldspar and blue quartz eyes. Trace amounts of biotite. Unit borders sharply perpendicular to core axis at top contact. Usual small veinlets of white quartz and carbonate. Unit is non magnetic. Pheno concentration is consistantly moderate throughout. Colour is darker towards top, tapering to a maroon towards lower contact, which also borders perpindicular to core axis.

147.25 156.42 MI.dk.pk Reutrn to carbonate rich mafic dyke. Carbonate veines appear to be fracture fill. Unit's upper contact is oriented perpindicular to core axis, while lower contact is oriented 80 degrees to core axis. Occasional rosy carbonate. Periodic rich sections of epidote along with occasional salmon feldspar. Towards lower contact, colour becomes slightly red in colour, resulting in a dark maroon aura, suggesting dessiminated hematite. Unit is weakly magnetic. Usual biotite rich matrix.


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156.42 170.27 MI.dk.psk Fine grained mafic dyke, ocasional carbonate veine, though obviously different from previous interval. Sharp contact perpindicular to core axis. Unit is moderately magnetic. Biotie rich, with persistant horblende phenos throughout, generally in the <1cm sub-angular range. Periodic epidote and chlorite veining, much more common than carbonate. Occasional quartz and feldspar phenos. Overall, section is poorly deforemed.

170.27 177.26 MT-FV.por Reutrn to metamorphosed porphyritic felsic volcanics with feldspar and blue quartz eyes. Red to dark red colour. Moderate to highly depormed, roughly 60 degrees to core axis. Phenos decrease in abundance with depth. Periods of intense epidote mineralization. Epidote and feldspar "blobs" occur close to lower contact. Lower contact is very graudual. Yellow quartz veine towards bottom.

177.26 186.62 MT-CO.pl.my modeately mylonitized metaconglomerate. Beige to light green with intervals of red feldspar rich mineralization. Texture is bimodal throughout. Appears to be increasingly mylonitized as unit approches lower contact. upper contact is very gradual while lower contact is sharp, roughly 25 degrees to CA. Unit is moderately clastic throughout interval. Mineralogy is predominantly feldspar chlorite, quartz, epidote and some patchy sections of mudstone. Some carbonate veines. Non magnetic.

186.62 187.74 MI.dk.pk Small pre-kinematic mafic dyke. Upper contact show strain. Contacts are sharp. Small (<1cm) phenos of feldspar are consistent throughout, along with quartz. Usual biotite rich matrix with some horneblende and chlorite. Unit is weakly magnetic.

187.74 188.91 MT-CO.pl Return to previously described mylonitized metaconglomerate.

188.91 193.46 MI.dk.por Typical porphyritic mafic dyke. Fine grained biotite rich matrix hosting quartz and feldspar, angular like phenos (~10%). Some chlorite present. Unit has very fine grained chill zones at upper contact. weakly magnetic. Occasional carbonate vein. Sharp upper contact. Lower contact is broken and blocky.


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193.46 234.53 MT-CO.pl Usual Jacques metaconglomerate. Short mafic dyke from 222.95 to 223.41. Dyke is highly fractured and infilled with epidote. Metaconglomerate is clast rich, with intervals of red fladspar. Strain increases towards lower contact(?). Clasts size is generally in the 1-2cm range, except from 218.76 to 22.58 where it decreases to the <1cm range. Unit is non magenetic. Chlorite feldspar, quartz epidote dominate the minearalogy. Some small carbonate veines. One large irregular carbonate fracture fill.

234.53 251.72 MI.dk.por Porphyritic mafic dyke. Fine grained biotite rich matrix hosting quartz and feldspar, angular like phenos (~10%). Some chlorite present. Unit has very fine grained chill zones on both upper and lower contacts. weakly magnetic. Occasional carbonate vein. Usual epidote veining.

251.72 260.86 MT-CO.pl Return to previously mentioned metaconglomerate.

260.86 274.75 MT-FV.por Red feldspar volcanics. Section is moderately deformed. Typical phenos of k-feldspar and blue quartz eyes. Trace amounts of biotite. Unit borders sharply perpendicular to core axis at top contact. Usual small veinlets of white quartz and carbonate. Unit is non magnetic. Pheno concentration is consistantly moderate throughout. Colour predominantly red throughout, though flip flops back and forth from dark maroon to bright red. Section is brecciated towards lower contact.

274.75 279.24 MT-CO.pl.my Feldspar rich mylonitic metaconglomerate. Highly starined. Beige to light green between intervals of red feldspar rich mineralization. Texture is bimodal throughout. Decreasingly mylonitized as unit approches lower contact. upper contact and lower contacts are very pronounced. Unit is moderately clastic throughout interval. Mineralogy is predominantly feldspar chlorite, quartz, epidote and some patchy sections of mudstone. Some carbonate veines. Non magnetic.


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279.24 357.86 MT-IV Dark red to dark grey & black, fine-grained metamorphosed intermediate volcanics, strong pervasive hematite alteration in upper 7m of interval, decreasing w/ depth. Moderately hematized, tapering to trace with depth. By 301 rock is almost black. Mininor quartz and feldspar veinlets throughout bottom 10 m. Abundant typical veinlets & stockworks but appear to become more chlorite-dominant w/ depth. Scint values <250 cps, save for short interval from 289.00 - 289.40. Sulphides occasionally present within both veinlets & matrix in upper 10 m of interval. Unit is weakly magnetic at higher scint reading, trace magnetism everywhere else. Hematization returns at 354.50, weakly hematized. Perioic sections of intense clorite and epidote veining. Slightly altered. Count of XXXXcps at lower contact.

357.86 358.32 MI.dk.por Porphyritic mafic dyke. Usual phenos of feldspar and quartz in fine grained biotite rich matrix. Weakly magnetic.

358.32 406.21 MT-IV highly altered and hematized. Strongly magnetic. Metamorphic intermediate volcanics. Locally mylonitic. Roasy red intermediate componant. Moderate calcite and amphibole veining. Strongly magnetic is areas, overall, moderate to strong. Moderately to highly altered, high in areas of high cps counts. Mafic dyke visible from 386.20 to 386.56. After dyke, decrease in hematite, though still moderately altered. Calcite veining increases with depth from this point on. Some carbonate veines visible. Lower contact approximately purpendicular to core axis. Increase in white and rosy quartz veines as lower contact is approched. Average of 600cps over 26 m, with a max of 5048cps.

406.21 418.1 FI.por.fp Coarsely porphyritic felsic intrusive. Moderately hematized. Medium grained matrix. Moderate levels of biotite and horneblende. Low strain. Very felsic at bottom 0.97m of unit. Lower contact very broken and blocky, appears to be at roughly 90 degrees to core axis. Increases epidote veining with feldspar with depth. Non magnetic. Unmineralized

418.1 440.33 MI.dk.por Pophyritic mafic dyke. Top contact purpendicular to core axis. Very broken at top contact, almost breccia like texture. Lots of fracture fill epidote and carbonate veines. Feldspar and quartz pheno rich, though tapers with depth. Magnetics increase with depth to moderate level, and grain size decreases. Still occasional red feldspar pheno, probably broken from upper unit. Carbonate vein rich throughout, along with increase in quartz vein abundance with depth. Usual biotite rich matrix.


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440.33 446.84 MT-IV Long section of intermediate volcanics. Hematization is very weak for the most part, but increases to moderate in spotty sections. Alteration is low. Some pyrite visible at 450.48. Regular feldspar lenses and quartz veins. Periodic tiny fracture fill carbonate veins. 453.40 to 453.70 see increase in hematization and alteration. Top contact very gradual and difficult to spot due to the low alteration and hematization of the volcanic unit. Chlorite veining coming throughout. Stongly magnetic

446.84 448.32 MI.dk.por Short mafic dyke. Slightly porphyritic. Some gabbro. A few large quartz phenos (1.5cm). Tiny quartz and feldspar phenos (<.5cm). Usual biottie rich matrix. Weakly magnetic.

448.32 481.47 MT-IV Return to poorly hematitic intermediate volcanics. Sections of high alteration, and hematization. 453.40 to 453.70 see increase in hematization and alteration. Strongly magnetic. Consistant chlorite veins throughout, though expecially between 454 and 462. Usual fraccture fill carbonate. Sparkly magnetite visible in matrix, along with biottie and actinolite. Periodic feldspar lens. Seams moderately strained atin areas. A few small mineralized sections (just over 300cps).

481.47 482.52 MI.dk.por Fine grained porphyritic mafic dyke. Usual tiny phenos of qtz and feldspar

482.52 487.39 FI.por.fp Coarsely porphyritic feldspar porphyry. Sharp contacts 65 degrees to core axis. Increasingly porphyritic towards center with finer grained chill contacts.

487.39 488.27 MI.dk.por Return to previously mentioned med grained porphyritic mafic dyke.

488.27 490.86 MT-IV See previous description of weakly hematized, moderately altered intermediate volcanics.

490.86 499 FI.por.fp Return to coarsely porphyritic felsic intrusive. Small mafic dyke from 494.43 - 496.35. Could be granite, fine grained. EOH


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0 5.2 OVBD overburden and colar.

5.2 17.86 MI.dk.sk Dark Green/black (weathered and brown near the top) mafic dyke. Highly moderately to heavily veined with calcite and quartz. No visible phenoscrysts.

17.86 22.98 MT-CO.pl Dark red and green unit. Becoming increasingly deforemed and banded downhole. Containing epdiote, hematite, calcite veins, quartz and feldspar. Small (~03-0.5cm) rounded clasts more evident in the upper portion of the unit. Messy upper and lower contacts. Non-magnetic.

22.98 38 MI.dk.pk Black/dark green, highly veined and metamorphosed mafic dyke. Contains calcite, hematite staining, chlorite and quartz.

38 90.5 MT-CO.pl Highly deformed/banded black, red-purple and green conglom. Messy upper contact. Rounded to sub-angular clasts ranging from 0.3 - 15cm. Contains calcite veins, chlorite, quartz, k-feld, epidote. Becoming more deformed downhole. Grades into next unit.

90.5 94.44 MI.dk.sk Dark gray-black aphanitic mafic dyke. No phonos. Some plucked clasts from adjacent congom units. Both upper and lower units are gradational.

94.44 98.4 FI.por.fp Red porphritic felsic unit. Containing k-feld phenos ~0.3 - 0.5 cm. Lower 50cm of the unit is much more strongly deformed. Lower contact is sharp and makes angle of 80deg with core axis.

98.4 116.43 MT-CO.pl Dark gray/black-green strongly deformed felsic conglomerate. Clasts are rounded and range from 0.5 - 10cm in diameter. Contains quartz, k-feld, chlorite, epidote. Some carbonate, quartz and feldspar veins. Sharp upper contact making an angle of 85deg with core axis.

116.43 117.23 MI.dk.psk Dark gray-green fine grained syn or possibly post-kinematic mafic dyke. Contains some epidote, minor veining. Busted-up upper contact. Lower contact is sharp and makes an angle ~80deg with core axis. Non-magnetic.

117.23 119.83 MT-FV.por Dark red/purple highly deformed felsic unit. Contains a lot of k-feld, quartz . A band of chlorite at ~119.58 depth, could be a clast. Contains patches where phenos ~0.1-0.3cm are evident. Some magnetic patches, mostly non magnetic. Sharp upper and lower contacts, both making angles of ~85deg with core axis.


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119.83 120.78 MI.dk.sk Dark gray/black-green unit. Fairly heavily veined containing carbonate and quartz. Contains some phenos, more evident at lower contact. Some xenolith action around the contacts. Sharp upper and lower contacts making angles of ~75 and 45 deg, respectivily.

120.78 154.82 MT-CO.pl Dark gray-purple conglomerate with a fine grained matrix containing rounded to sub-angular clasts ranging from 0.5 - 10cm in diameter. Clasts are composed of k-feld, epidote,chlorite, quartz and mudstone. Exhibits some veins containing carbonate, chlorite, quartz and epidote. moderately to strongly magnetic.

154.82 158.18 MI.dk.psk Dark gray/black porphyritic post kinematic mafic dyke. Only one veinlet 50deg to core axis. Rediculously tiny phenos. Upper contact is sharp and makes angle of 45deg. Lower contact is 87ish deg to core axis.

158.18 171.55 MT-CO.pl Purple-blackish purple/red meta conglomerate. Clast are sub-rounded to sub-angular and range from 0.2 to 15cm in diameter. Contain chlorite, k-feld, epidote Moderately to high desnity of carbonate veinlets . Patchy moderate to high magnetism.

171.55 172.82 MI.dk.sk Dark Gray/Green-black porphyritic mafic dyke. Very small phenos ~<0.1cm. Containing cholorite, some quartz very little veining. Sharp upper and lower contacts make 45deg angle to core axis.

172.82 185.94 MT-CO.pl Same comglomerate as previously described. Becoming more mylonitic downhole.

185.94 195.23 MT-CO.pl.my Dark red to dark gray/green mylonitic conglomerate. Clasts are strongly deformed but those that are visible range from ~0.5 - 12 cm in diameter and contain chlorite, k-feld, hornblend, quartz, epidote, and carbonate. Exhibits some veining generally at about 20deg to core axis. Upper contact is a gradual grade into the above conglomerate. Sharp lower 40 deg contact. Only patchy weak to moderate magnetism.

195.23 195.93 MI.dk.sk Dark gray/black aphanitic mafic dyke. Contains viens of chlorite and/or epidote at 25 deg to core axis.

195.93 204.54 MT-CO.pl Conglomerate as described previously. 25deg upper contact.

204.54 206.37 MI.dk.sk Dark gray-black synkinematic mafic dyke. Contains chlorite veins making 25deg angles with core axis


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206.37 229.98 MT-CO.pl Same conglomerate as described above contains a small (28cm) mafic dyke at 213.96 m intruding at an angle of 40 deg.

229.98 233.89 MI.dk.sk Dark gray/black mafic dyke moderately viened at 40deg angles to the core axis. Upper and lower contacts also make a 40deg core axis.

233.89 241.86 MT-CO.pl.my Very felsic unit ranging in colour from a high red occurance to a high green occurance. Strongly deformed with a fabric aligned 45deg to core axis. Containing quartz, feldspar, epidote. Contains some veining including those of carbonate. Upper contact is sharp with an angle of ~40 deg to core axis, lower contact is rough/gradational. Post-kinematic mafic dyke located at 238.71 - 239.23 m depth having intruded at about 45 deg to core.

241.86 305.41 MT-IV Red-black becoming more green-black at about 259.50m depth and down hole. Highly magnetic. Containing epidote, chlorite,carbonates, k-feld, quartz (occuring with what appears to be jade). Intruded by a post kinematic mafic dyke at 257.24 - 257.44m depth. Achieving scint readings of ~300cps around 280m depth.

305.41 306.06 MI.dk.psk Short black interval. No visible fabric, non-magnetic. Sharp 40deg upper and lower contact.

306.06 347.64 MT-IV Dark gray/black- dark red meta volcanics. Moderately to strongly magnetic. Exhibiting pyrite and calcite veining also containg some k-spar, epidote, chlorite. Unit becomes less hematized down hole losing its red tinting for a more dark-gray colour. Intruded by a small syn or post-kinematic mafic dyke with a dense population of phenocrysts at a depth of 310.56 - 310.90 m and an angle of ~80deg to core axis. Scint readings running to just over 2000cps.

347.64 349.64 MI.dk.sk Dark gray/black unit containing no phenos but having xenoliths at the lower contact and at spots within the unit from the lower unit (coming up next).

349.64 360.43 FI.por.fp Dark gray porphyritic unmit with rounded feldspar phenos ranging from 0.3 0- 1.8 cm in diameter. Matrix is biotite rich and has varying density of phenos throughout. Upper and lower contacts are gradational and obscured by xenoliths in adjacent units. The unit is weak to non-mangnetic and possibly contains several very small mafic dykes. Xenoliths make them difficult to distinguish.

360.43 364.1 MI.dk.sk Dark gray/black biotite rich unit with little disernible fabric and no phenos. Contacts with adjacent units are once again obscured by xenos.


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364.1 364.84 FI.por.fp Same porphyritic unit as before.

364.84 404.21 MT-MI.fgr Dark Gray/green-black biotite rich unit. Contains veins of chlorite, k-feld and quartz. Strongly magnetic. Contains occational quartz clasts.

404.21 410.49 MI.dk.sk Dark gray unit becoming more red downhole. Contains moderately high percentage of phenos ~0.1 - 0.4 cm in diameter containing k-feld. Veins show evidence of shearing. Non magnetic.

410.49 419 MT-MI.fgr return to fine-grained mafic intrusive. Fairly large veins (1.0 - 2.5 cm wide) containing cholorite at approximately 45deg to core axis. EOH


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0 4.89 OVBD Overburnden and casing

4.89 10.12 MT-CO.pl Dark green to pink moderately sheared conglomerate unit. Clasts sizes range from 0.2 to 2cm. Number of clasts decreases downhole. Only rare clasts after Increasingly felsic towards bottom contact. Clasts are polylithic, brown, green, pink with ct +ap +/-ac +/-fps. Med hm alteration throughout unit. Several sets of micro-fractures with approx 1mm bleaching on each side. Rich in carbonate veins. Non to weakly magnetic.

10.12 14.37 MI.dk.por Porphyritic mafic dyke with usual phenos of feldspar and quartz. Consistant epidote veining. Both contacts very gradual. Blocky and broken for majority of interval. Biotite and horneblende dominate matrix. Weakly magnetic.

14.37 20.47 MI.dk.pk Mafic dyke dominated by carbonate veins. Brittle fracture fill carbonate veines. Occasional rosy carbonate vein. Vein desity ranges from sporatic to intense. Carbonate Veine density tapers with depth. Towards lower contact, previously mentioned chlorite rich matrix hosting hornblende phenos are visible. Weakly magnetic.

20.47 24.18 MT-CO.pl Typical Jacques metaconglomerate. Green, red and light brown polylithic conglomerate. Weakly to mod sheared. Shearing stronger close to lower contact. Blebby ct alterations still present and more intense than in unit above. Core competent. Clasts are subrounded, 1-10mm, made of light brown mudstone, purple jasper chert, kspar. Rare quartz crystals. Groudmass is aphanitic to very fgr, dark red. Hm altn pe and strong. Kpsar altn patchy and irregular. LCT obscured by broken core. Pa mag. Non magnetic.

24.18 26.05 MT-FV.por Red feldspar volcanics. Section is moderately deformed. Typical phenos of k-feldspar and blue quartz eyes. Trace amounts of biotite. Unit borders sharply perpendicular to core axis at top contact. Usual small veinlets of white quartz and carbonate. Unit is non magnetic. Pheno concentration is consistantly moderate throughout. Colour is darker towards top, tapering to a maroon towards lower contact.

26.05 27.83 MT-CO.pl Return to previously described metaconglomerate

27.83 33.51 MT-FV.por See previously mentioned felsic volconics.


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33.51 39.39 MT-CO.pl Dark gray-green clast poor meta conglomerate with rounded-subangular clasts of mudstone ranging from 0.5 - 10cm in diameter.

39.39 48.25 MT-FV.por Red and black highly deformed felsic meta-conglomerate containing quartz, feldspar and carbonate. Heavily veined. Patchy weak magnetism, otherwise non-magnetic. Sharp upper contact making an angle of ~20deg with core axis. ~80deg contact with lower unit.

48.25 64.1 MI.dk.psk Dark gray/green mafic dyke containing phenocrysts of 0.1 - 0.3cm diameter. Contains some veins of cholorite, some k-feld and carbonate veins. Unit becomes fine grained at the lower contact which is sharp and roughly 75 degrees to c/a. Dark green from chl + act after hbl (px?). Unit is moderately-to strongly magnitic. Hematite staining is after hematite.

64.1 87.3 MT-IV Foliated metamorphosed intermediate volcanic (volcaniclastic) rock: Unit is hard, dark-grey and red due to silica alteration and hematite staining. The irregulat and somewhat chaotic foliation is defined by altertating darker green/grey and hematite stained red bands on a cm scale. Banding is generaly chaotic but tends to average around 45 degrees to c/a. Occational zones of sheared volcaniclastic material is present and defined by lighter coloured 2mm to 1.5 cm stretched/flattened "clasts", again about 45 degrees to c/a. Both contacts are sharp, the and the banding is truncated on both. The lower contact is at about 70 degrees to c/a. Unit is cut by many < 1mm thick white fractures of various orientations.

87.3 88.05 MI.dk.pk Dark Green metamorphosed mafic dyke which post-dates foliation in the surrounding rocks. Same as the mafic unit above Dark green from chl/act/ser alteration of the mafic component of the rocks. Contacts are both sharp and cut foliation in the intermediate volcanic rocks. Unit is composed of 40-50% plagiaclase and the rest altered mafic minerals, primarily hbl. Unit is equigranular and grain size is in the 0.5 to 1mm range. Unit is patchy magnetic. Unit is cut by a few thin (< 1mm) carbonate veins). The lower contact is at about 50 degrees to c/a.

88.05 94.5 MT-IV Foliated metamorphosed intermediate volcanic (volcaniclastic) rock: Exactly the same as that discribed at 64.1m. Cut by a 15cm thick highly ser/chl/act altered dyke at about 50 degrees to c/a (cuts foliation); it is courser-grained in the middle and is an altered post kinimatic mafic dyke as above. Lower contactr is broken, but looks to be sharp.


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94.5 96.3 MI.dk.por Metamorphosed porphyritic mafic dyke: This unit is dark green due to strong act, ser, chl alteration. It contains 40-50% plagioclase taths, mostly porphyritic with respect to the finer grained and altered mafic matrix (hbl, px?). Rare 1 cm and greater laths of plag are present but comprise << 1% of the rock. The unit is finer grained at near both contacts and the lower contact is sharp and about 70 degrees to c/a. This unit is likely the same as the post kinematic dukes discribed above as it also clearly is not foliated. It is moderately to strongly magnetic and is cut bu late thin < 1mm thick white veins (at least some of which are albite.

96.3 99.6 MT-IV Foliated metamorphosed intermediate volcanic (volcaniclastic) rock: Same as that discribed at 64.1m. Contains a zone of prominent sheared/flattened conglomerate with clasts up to about 2 cm long. Lower contact is sharp and at about 60 degrees to c/a.

99.6 129 MI.dk.psk Fine to medium grained metamorphosed mafic dyke. Unit appears to contain multiple pulses of intrusion as indicated by internal seemingly regilar ratty altered zones and apperent changs in grain size. The unit more resembles a series of mafic volcanic flows, however, I'm not sure how they would fit into the tectonic setting especiallyconsidering they seem to be relatively undeformed (though there is some evidense for deformaion). Unt is generally dark green due to strong ser/act/chl alteration. Weak reddness is also comon present due to FexOy staining (the unit is not very magnetic). In the fresher zones between ratty "contacts" one can clearly make out tiny laths of plag and a small dark mafic component. Unit cut by some late white (albite and carbonate) veins. The lower contact is broken core.

129 132.6 MI.dk.psk Mafic Dyke, Post kinematic. Undeformed and realatively fresh mafic dyke. The lower contact is at a low angle to the c/a (15 degrees) and clearly the mafic rock post-dates the unit below as indicated by the allignment of minerals parrallel to the contact within the mafic rock.The rock near the upper contact displays the same allignment of minerals and at roughly the same angle suggesting the upper contact is also about 15 degrees to c/a. The unit contains about 40-50% 0.5 - 1 mm laths plag and a small portion of dark minerals about the same size (hbl or px) within a fg matrix (i.e. the unit is porphyritic). Unit contains very few veins and they are < 1mm thich, white and carbonate.


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132.6 137.9 MT-CO.pl Sheared sand to pebble sized sediments, interpreted to be the finer grained equivelant of the sheared conglogerate unit within adjacent holes and described deeper in this hole. Unit contains primarily sandy and some peddle sized material which is sheared to generally about 40 degrees to c/a. Unit is reddish due to FexOy staining and displays patchy magnatism. Inut contains many up tp 2mm thick veins of carbonate and there appears to be a diminant orientation of about 50 degree to c/a.

137.9 138.9 MI.dk.psk Mafic Dyke, Post kinematic: Same as that described at 129m. Upper and lower contacts display allignment of minerals with in the mafic unit and are at low angles to the c/a. Upper contact is broken, but can tell it is sharp.

138.9 140.1 MT-CO.pl Sheared sand to pebble sized sediments, interpreted to be the finer grained equivelant of the sheared conglogerate unit within adjacent holes and described deeper in this hole. Same as above.

140.1 151.1 MI.dk.psk Mafic Dyke, Post kinematic. Undeformed and realatively fresh mafic dyke (gabbro). Same as that described at 129m. Upper contact at low angle to c/a and displays allignment of minerals to contact. Lower contact sharp, at 45 degrees to c/a and also displays allignment of minerals. Unit contains very few veins, is magnetic and is a bit reddiish due to FexOy staining. Moderate act+chl alteration. Unit here more equigranular and some hbl for sure, but not sure if px + hbl.

151.1 175.9 MT-CO.pl Metamorphosed and strained polylithic caorse grained conglomerate unit. Unit is patchy in its appearance, but generally pebble and greater sized, polylithic (multi-coloured) rounded to sub-angular and variably strained clasts withing a finer grained dark reddish grey groundmass. Some places are more sandy than conglomerate (as with the units above). Red staining from FexOy. Patchy weak magnetism. Deformation is variable in intensity, but generally about 25 - 30 degrees to c/a where the most intense. Moderate carbonate veining. Lower contact with mylonite is sharp. The foliation is cut by the mylonite fabric. The contact is 70 to c/a.


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175.9 189.1 MT-FV.por Mylonite zone that looks to have been derived from the intense shearing of quartz clasts /phenocrysts. The unit is generally silt and sand sized material which displays a banded to finely "laminated" in texture to it. The unit here is being "called" a mylonitised meta-felsic volcanic unit primarily based on the differents in shrain noted at the contact (suggesting a change in rock rheology) and the presents of resistant quartz grains, not reallt present in the conglomerate. The unit does however seem to be interlayered with the conglomerate in the conglomerate unit above. The unit is quite hard (silica altn ??), and red/grey in colour due to FexOy staining. There Is a clear gradation present in the angle of the foliation within this unit. The lower contact is somewhat picked arbitrarily based on a shift in apparent grain size. Threre are occational (<<1% of rock) green filled (act+/- chl) veins with reddist salvages present, generally // to foliation. At about 186.1 m, there is an area where there appears to be a weak foliation overprinting the mylonite, it is cutting the mylonite at approximatly 75 degrees (both cut cut at about 40 degrees to c/a, but opposite.

189.1 189.55 MT-CO.pl Metamorphosed and strained polylithic caorse grained conglomerate unit: Same as unit above but more reddish matrix and material (few quartz clasts).

189.55 190.25 MI.dk.pk Highly strained and altered pre-kinematic mafic dyke: Green deformed, chl, act and ser altered mafic rocks. Unit has an internal foliation of about 40 degrees and two sharp contacts at 60 degrees. The unit is maderately magnitic. Contains the odd foliation parallel veinlette of carbonate. Origianal mineralogy is not possible to identify.

190.25 193.4 MT-CO.pl Metamorphosed and strained polylithic caorse grained conglomerate unit: Same as unit above samller grain size and much more strained. This zone is also moderately magnetic and consistantly so (interesting is that this zone is bound on both sides by sheared pre-kinematic mafic dykes which are also quite magnetic. The Orientation of the foliation is fairly consistent within this zone at about 45 degrees to c/a. Both contacts are sharp. The unit is quite hard (quartz altn) and red (FexOy staining). Unit is cut by a few late silica filled veins.

193.4 193.9 MI.dk.pk Highly strained and altered pre-kinematic mafic dyke: Green deformed, chl, act and ser altered mafic rocks. Unit has an internal foliation of about 40 degrees and the lower contact is at 50 degrees to c/a. The unit is moderately magnitic. Contains the odd foliation parallel veinlette of carbonate. Origianal mineralogy is not possible to identify.


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193.9 197.3 MT-CO.pl.my Metamorphosed and strained polylithic caorse grained conglomerate unit: Same as unit just above though this unit is not reddish and not magnetic. The unit here takes in a streaked white and grey appearance. The white streaks are quartz +/- plag and the dark is undifferentiable but hard (quartz altered). Some small area resemble the mylonitised volcanic rocks described at 175.9 m (interbedded with conglomerate??). The Orientation of the foliation varies from about 75 to 15 degrees to c\a as seen in the structural measurements.

197.3 197.35 MI.dk.pk Highly strained and altered pre-kinematic mafic dyke: Same as above. Both contacts are dammaged do to drilling however both appear to be at low angles to a/c. This zone is not noticable magnetic.

197.35 199.05 MT-CO.pl.my Metamorphosed and strained polylithic caorse grained conglomerate unit: Same as unit just abovestarting at 193.9m. Unit has a gradational contact with the lower unitwhich we are calling a mylonitised prophyritic felsic volcanic rock (see discription below). The foliation in intense and oriented fairly consistantly at 50 degrees to c/a. Some late thin carbonate filled veins present at low angle to c/a (~15 degrees)

199.05 202.9 MT-FV.por Mylonitised porphyritic felsic volcanic rock: Same as the unit discribed at 175.2 m. Clearly can make out 15 -20% 0.5-1mm resistant porphyroclasts of quartz and possibly plag. These sit in a f.g. greyish-red matrix. The reddness is from weak FexOy staining. The unit is cut by a few later silica/plag veins and a few late green filled (looks calc-silicate to me) veins with reddish-brown salvages and also the very late calcite filled fractures common in most of the core thus far. The lower contact is sharp as a razor with the underlying conglomerate unit but is irregular and the foliation in the volcanic rocks goes around the irregular contact as a result in the much easier to deform volcanic rock.

202.9 238.65 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. This zone has the appearance of the more "characteristic" conglomerate that is present throughout the area. It is composed of polylithis and coloured clasts from 1mm to the occational >10 cm lithic fragment. All display some level of deformation however most of the unit displays only minor to moderate deforemation. Oriented core for this hole starts at 211 m. The unit displays patchy FexOy staining and weak to moderate magnetism. There is trace carbonate veinlettes, primarily oriented about 60 degrees to c/a. Oriented core measurements in separate excel sheet.


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238.65 247.8 MI.dk.pk Strained and altered pre-kinematic mafic dyke: Same as above. The upper and lower contacts could not be oriented, they are however sharp and at low angles to the c/a (Upper:20 degrees Lower:15 degrees). The best forliation is not within orientable core but is about 45 degrees to c/a. Unit is highly altered (act/ser/chl) and non-magnetic.

247.8 282 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures. Small post kinematic dyke at about 265.2 m (see oriented core spreadsheet) same as that described below.

282 286.7 MI.dk.psk Fine grained post kinematic mafic dyke: Hard to make out mineralogy due to small grain size, but there appears to be about 35-40% lath shaped plag phenos within a dark matrix which may or may not do the same grain size (hard to tell due to chl/ser/act? altn). Unit is moderatly magnetic. Upper contact is sharp and the lower contact, which probably sharp, is broken core. Unit is not strained. Unit cut by late minor carbonate veins at low angle to c/a (see oriented core spreadsheet).

286.7 299.8 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures.

299.8 300.2 MI.dk.psk Fine grained post kinematic mafic dyke: Hard to make out mineralogy due to small grain size, but there appears to be about 35-40% lath shaped plag phenos within a dark matrix which may or may not do the same grain size (hard to tell due to chl/ser/act? altn). Unit is moderatly magnetic. Contacts are sharp (see oriented core spreadsheet).

300.2 332.65 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures. Unit cut by late quartz veins and calcite veins (see oriented core spreadsheet); carbonate veins usually < 1mm, some quartz vwins up to 1 cm.

332.65 333.05 MI.dk.psk Strained and altered pre-kinematic mafic dyke: Same as above. Unit has 2 sharp contacts and internal foliation and contacts are parallel to main foliation (see oriented core spreadsheet). A few carbonate veins, < 1mm and // to foliation.

333.05 356.05 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures. Unit cut by late quartz veins and calcite veins (see oriented core spreadsheet); carbonate veins usually < 1mm, some quartz vwins up to 1 cm. @ 345 is a 20 cm thick intermediate dyke (see oriented core spreadsheet).


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356.05 356.6 MI.dk.pk Fine grained dark green mafic dyke. Unit has two sharp contacts which look like they are altered and healed faults. Unit contains some light green veinlettes (serp? Act? Ep?) and is magnetic. Grain size too small to identify.


366.7 368.2 MI.dk.pk Medium grained prophyriritic/mafic dyke. Unit contains 10-20% relitc porphyroclasts of a bluish/grey mineral within a finer (medium grained) groundmass. The groundmass itself is composed of ~40% plag and 60% elongate dark green minerals (looks like chloritized hbl?). The groundmass minerals are NOT foliated indicating post-kinematic metamorphism. Unit, inlike the surrounding, are not magnetic. See oriented core spreadsheet.


377.85 378.2 MI.dk.pk Strained and altered pre-kinematic mafic dyke: Same as above. Unit has 2 sharp contacts and internal foliation and contacts are parallel to main foliation (see oriented core spreadsheet).


393.6 394.25 MI.dk.pk Strained and altered pre-kinematic mafic dyke: Same as above. Unit has 2 sharp contacts and internal foliation and contacts are parallel to main foliation (see oriented core spreadsheet).

394.25 403.7 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures. Oriented core stopped at 394 m (crew change, attempting to fix). Unit clearly more strained that was above. Similar styles and types of alteration as above though. Lower contact is sharp and at ~ 60 degrees to c/a and parallel to foliation. Foliation is between 45 and 60 degrees to c/a. Weak late carbonate filled fractures < 1mm.


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403.7 405.5 MI.dk.sk Medium grained, equigranular gabbro. Unit dark green from the chl, serp?, act, ser, ep alteration. Can clearly make out 1 mmphenocrysts of lath-shaped plag (~50%) and some (~5-10%) hbl with the rest of the mafics being too altered to identify, but the 50% mafics are probably a mix of hbl and px. Unit here is sheared with foliation the same as the regional foliation. The lower gabbro unit (starting at 410.3m) is unfoliated in the middle with plag phenos in random orientations. In this zone of gabbro, much of the grains are milled due to shearing. Unit is weakly to moderately magnetic and trace py and cpy are present as disseminated and blebby grains. Both contacts are sharp and parallel to foliation. The unit is cut by similar carbonate veins as other units as well as some thin ser, ep alteration veins.

405.5 410.3 MT-CO.pl Strained meta-conglomerate unit. Same as that discribed above. See oriented core spreadsheet for structures. Oriented core stopped at 394 m (crew change, attempting to fix). Unit clearly more strained that was above. Similar styles and types of alteration as above though. Lower contact is sharp and at ~ 50 degrees to c/a and parallel to foliation. Foliation is between 45 and 60 degrees to c/a. Weak late carbonate filled fractures < 1mm.

410.3 428.3 MI.dk.sk Medium grained, equigranular gabbro. Unit dark green from the chl, serp?, act, ser, ep alteration. Can clearly make out 1 mmphenocrysts of lath-shaped plag (~50%) and some (~5-10%) hbl with the rest of the mafics being too altered to identify, but the 50% mafics are probably a mix of hbl and px. Unit here is sheared with foliation in areas and unfoliated in others. Where unfoliated plag phenos are in random orientations. Where strained, much of the grains are milled due to shearing. Unit is weakly to moderately magnetic and trace py and cpy are present as disseminated and blebby grains. Both contacts are sharp and parallel to foliation. The unit is cut by similar carbonate veins as other units as well as some thin ser, ep alteration veins and some ep+carb. Carb + ep are occationally up to 1 cm. Unit has a sharp lower contact, and is relatively unstrained at that location.

428.3 428.75 MI.dk Mylonitized mafic rock. Thought this looks like a dyke at first glance, I believe it to be a descrete intensely mylonitized portion of the gabbro. The unit is the same mineralogy and has similar alterations. Evidence for this as a healed fault include that the gabbro above and below are not strained while this unit is intensely sheared, this unit is mafic and both contacts are razor sharp. There is not good rock code for this. Foloiation is the same as both contacts.


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428.75 436.6 MI.dk.sk Medium grained, equigranular gabbro. Exact same as above. Undeformed at mylonite contact but gets more deformed to lower contact.

436.6 440.5 MT-CO.pl.my Strained meta-conglomerate unit. Same as that discribed above but more strained.

440.5 450.3 FI.por.fp Strongly sheared felsic intrusive unit. Unit is red/pink in colour and spotty due to the presense of 1 to 10 mm porphyroclasts of feldspar and quartz within a fg often mylonitized quartz/feldspar matrix. Matrix fg due to milling?? Both contacts are sharp and // to foliation however the lower contact looks to be a fault as what look to be strongly stretched fragments on this unit and intercalated with the lower mylonitized mafic rock. Foliation is 55 to 60 degrees to c/a as are the contacts. FAULT AT LOWER CONTACT.

450.3 459.4 MI.dk.sk Medium grained, strongly sheared, equigranular gabbro. Exact same as above. Intensely deformed, but mineralogy, alteration and magnetism the same at the gabbro. Also, sulfides are the same. Weak carbonate and ep veins as before. Lower contact hard to pin-point, but is // to foliation at about 50 degreea to c/a.

459.4 466.5 MT-CO.pl.my Strained meta-conglomerate unit. Same as that discribed above but yet even more strained to the point where clasts are strained over 20:1. Unit is weakly magnitic and is patchy. Lower contact fairly sharp and at about 45 degrees to c/a. Unit contains a couple 5 to 25 cm thick green dykes (intensely altered and sheared beyond recognition). Alteration style changed a bit to more silica and FexOy staining.


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466.5 502 MT-IV Intermediate volcanic rocks - Red-Orange coloured unit composed of altered/metamorphosed intermediate in composition fine grained rocks. This unit does not display the intense mylnitisation of the above units. This could be due to the unit annealing duting alteration/metamorphism. The unit is somewhat foliated though indicating it was subject to the same strain as the above rocks. The unit is radioactive with cint values on hand specimen between 150 and 800 cps. Unit has been sampled. Occational greenish sheared rock (less radioactive) is present and may represent thin mafic units which are more easily deformed. Oriented core present here (see oriented core spreadsheet). The upper contact is // to foliation and is about 55 degrees to c/a. Sampling from 463 to 481 m incl. sholders. Best zone from 472.5 to 478m. Unit gets less reddish and more greenish away from the mineralized zone. Much of the red-pink alteration looks like ksf alteration which tends to be texturally destructive and may explain why mush of this unit does not look foliated (which is more prominent away from mineralization in the greener rock). The lower contact is broken, but likely sharp. A couple 5 to 20 cm thick alteration zones which post date the red alteration are sheared and pale-green in colour and composed of calc-silicate minerals including calcite, epidote, a pale-green mineral (which I can not remember what it is but know it is a calc-silicate), and act. These minerals are restricted to these zones and small veins. The unit below 484 is not oriented. There also appears to be a fault at about 501.7 m, just above the lower contact where about 15 cm of core is bleached and clearly altered somewhat to clay minerals (rock is broken).

502 510.1 MI.dk.sk Medium grained meta-gabbro. Unit is green due to alteration to chl, act, ser, ep minerals and in places weakly yo moderately foliated. I believe this to be the same at the gabbro units above though less magnetic (and patchy at that) and the plag grains are not elongate like the above units. But the unit is still composed of about 40-50% plag and the rest altered mafic minerals, some of which is hbl. There is also trace py. Lower contact is sharp with the coarse-grained felsic intrusive and the gabbro clearly post dates it as there are actually a few 5 to 15 cm xenoliths of the cg intrusive present withint the gabbro and the gabbro is less foliated. The unit is cut be minor thin veinlettes of calcite.


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510.1 511.8 FI.por.fp Coarse-grained feldspar prophyritic felsic intrusive: Weak to moderately deformed felsci intrusive with a phrphyritic texture of ~50% large subrounded to rounded phenocrysts of k-feldspar + plag (perhaps kfs>plag) and 5% rounded and somewhat smaller quartzphenocrysts. These are within a finer-grained and altered and sheared groundmass now mostly altered to hbl, bio, ep, magnetite, qtz and plag. Foliations weave around the large feldspar and qtz phenos and average ~ 35 - 40 degrees to c/a. Unit contains some py and also some purple flourite has been seen. Lower contact sharp and at about 65 degrees to c/a.

511.8 512.3 MI.dk.psk Small slightly more porphyritic (spotty) mafic to intermediate intrusive cuts the cg felsic unit. The unit is not deformes, is fairly unaltered and slightly porphyritic (spotty). It is composed of 60% plag, of which 2/3 of that is prophyritic (0.5 to 1.5 mm) and the rest finetr graned dark mafic minerals including hbl and px (px>hbl) with the remainder of the plag to make up the groundmass. The unit is not magnetic. It is clearly younger than the felsic intrusive and both contacts are sharp.

512.3 513.5 FI.por.fp Coarse-grained feldspar prophyritic felsic intrusive: same as above. Lower contact sharp and at about 70 degrees to c/a

513.5 529.8 MI.dk.pk Fine grained dark meta-basite. Dark-grey green unit that is fine grained, foliated and promarily composed of plagioclase (30-40%) and dark minerals which are mostly altered to chl, hbl. The unit contains both py and cpy up to 2% combined near the upper contact but generally combined < 0.5%. Near the lower contactr are a 1-5% 0.5mm to 7mm phenos of sub-hedral plag within the fg unit confirming it as an intrusive. The lower contact is sharp and the unit below is intensely deformed for a few cm past the contact (

529.8 572.19 FI.por.fp Coarse-grained feldspar prophyritic felsic intrusive: Same as above.

572.19 583 MT-MI.fgr NULL


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0 0.77 OVBD Overburden and casing

0.77 7.61 MT-CO.pl Metaconglomerate, dominated by mudstone at top of unit, becoming increasingly mafic with depth. Top sees occasional quartz and feldspar, high levels of chlorite and epidote. Very blocky and broken from 4.69 to 5m. Small mafic dyke from 4m to 4.22m. Borders upper at 20 degrees to core axis, same at lower contact. As unti becomes increasing mafic, it also decreases in clasts. Very clast poor from 6m to 7.61. Mostly black with occasional "blob" of cooked mudstone. Lower contact borsers at rought 90 degrees to core axis. Trace to weak magnetics. Unmineralized. Occasional carbonaite veinlet.

7.61 19.79 MI.dk.pk Small section of metaconglomerate. Dominated by mudstone chlorite and epidote. Very gradual contacts.

19.79 57.99 MI.dk.pk Unit begins as fine grained, biotite rich mafic dyke. Some very thin epidote veinlets are visible. This section has not been deformed. As the unit continues, biotite appears to be replaced by horneblende, resulting in a breccia like texture of horneblende phenos in a chlorite rich matrix. Continues to 53.01m. occasional epidote veins. Occasional calcite vein. Occasional quartz and k-spar phenos. Periodic fracture fill carbonate. Large chlorite "blobs" from 55.50 to 56.00m. Becomes finer grained and absent of phenos as it approaches lower contact. Chill zone. Weakly magnetic.

57.99 66.23 MI.dk.por Porphyritic mafic dyke. Porphyrys are rather large (1cm) when compared to usual porphyritic mafic dykes. Biotite rich matrix, with an aura of epidote. Large quartz lens from 59.11 to 59.36. weakly magnetic. Prominent carbonate. Some dissiminated feldspar. Hornblende phenos appear throughout. Contacts are gradual. Unmineralized.

66.23 72.8 MI.dk.psk Post kinematic mafic dyke. Prominent chill zones on both borders, top oriented 85 degrees to core axis, same as bottom comtact. Epidote and feldspar hosting horneblende visible at areas. Biotte rich, prevasive horneblende. Occasional quartz. Some carbonate veins. Sections does not appear to be highly metamorphosed, as there is no alteration. Weaklymagnetic. Unmineralized.

72.8 83.71 MI.dk.por Return to previously describe porphyrytic mafic dyke.


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83.71 104.54 MT-CO.pl Highly hematized, and feldspar rich metaconglomerate. Unit is dominated by hematite up to 91 meters, followed by feldspar rich, clast poor section until end of interval. Magnetism is moderate throughout. At 101m, magnetics increase to very intense for a section of 5 cm. Chlorite, epidote and lots of quartz. Carbonate fracture fill common throughout, though increasing with depth. Becomes very quartz rich as approching lower contact, which is oriented 50 degreees to core axis. Upper contact is very blocky. Mylonitic texture, expecially at hematite rich top of interval. Unmineralized.

104.54 107.75 MI.dk Fine grained mafic dyke dominated by carbonate veines. Biotite and horneblande matrix. Veryfine grained. Carbonate veining account for roughly 25% of unit. Very gradual contacts on both end as carbonate veines invade neighbouring units. Non magnetic. Unmineralized.

107.75 133 MT-CO.pl Return to metaconglomerate dominated by feldspar. Small sections of clast poor mineral activity. Rich in carbonate veines near top contact, which is very gradual. Non-magnetic. Appears mylonitic from 110.22 to 110.68, oriented 45 degrees to core axis. Chlorite activity increases with depth, a few fracture fill carbonates towards bottom. Unit becomes less and less hematized with. Becomes very feldspar rich at 125.64 to 128.10. After this unit looks like usual moderately clastic metaconglomerate. Appears somewhat mafic, moderate levels of biotite. Weakly magnetic.

133 133.45 MI.dk.por Small mafic dyke, borders at 60 degrees to core axis on both contacts. Regular epidote veining, usual tiny (<0.5) feldspar and quartz phenos. Matrix rich in biotite and horneblende. Trace magnetism, unmineralized.

133.45 142.67 MT-CO.pl Feldspar rich metaconglomerate. Feldspar tapers with depth. Usual fracture fill carbonate. Small amounts of mudstone. Becomes very clast poor with depth. Moderate levels of chlorite and epidote throughout, increases to strong as lower contact is approached. Section from 138 to 140 is highly altered and strained. Consistent quartz clasts. A few tiny faults located at 137.75 oriented 130 degrees to core axis and 138.90 40 degrees to core axis. Trace magnetism througout. Period section of weak hematization.

142.67 143.23 FI.dk.por Shor felsic dyke. Entirely feldspar save for ~5-7% quartz. Apears moderately strained, small fault at 143.10, oriented roughly parallel to core axis.


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143.23 143.5 MI.dk.por Small porphyritic mafic dyke. Probably shouln't make it it's own form entry, but hey, I'm nuts. You know it, I know it, friggin' the core knows it. I leave tomorrow, and I think I'm going a little nuts. Appears moderately metamorphosed, Strained to roughly 80 degrees to core axis, as are the contacts. Porpheries dominated by epidote (30%) and feldspar (10%) and quartz (10%). Biotite rich matrix. Some hornblende visible as well

143.5 145 MT-CO.pl Very clast por metaconglomerate. Mineralogy is rich in quartz (smokey). Occasional small feldspar lens. Weakly hematized. Some epidote and chlorite. Moderately strained to 80 degrees to core axis. Some fracture fill carbonate. Somewhat mafic. Moderate biottie.

164.03 169.42 MT-FV.por NULL

169.42 170.42 MI.dk.pk NULL

187.76 201.6 MT-CO.pl Red-Green highly busted up unit. Containing a lot of chlorite, k-feld. Moderate carbonate veining. Becoming increasingly red and mylonitized downhole. Busted up lower contact.

201.6 227 MI.dk.sk Dark graygreen somewhat porous unit. Contains phenos of ~0.1cm diameter. Rough upper and lower contacts.

227 254.07 MT-CO.pl Dark gray, green red conglomerate. Highly deformed sub-rounded to sub-angular clasts ranging from ~0.2 - 15cm in diameter and containing a lot of k-feld, quartz, epidote, chlorite. Patchy strong magnetism and some large carbonate veins as well as small veinlets generally forming angles of ~40deg and 90deg with core axis.

254.07 256.22 MI.dk.sk Dark gray/black aphanitic syn-kinematic mafic dyke. Contains xenoliths at perifery. A 25cm long section of the unit contains a dense population of ~0.1 - 0.2 cm diameter phenos. Moderat veining-veinlets containing epidote. Upper and lower contacts are sharp making angles of ~35deg to core axis.

256.22 280.18 MT-CO.pl return to previously described conglomerate.

280.18 287.07 MI.dk.sk Dark Gray/green to brown felsic intrusion containing a high percentage of phenos with notable k-feld. Intruding at sharp 70 deg angles to core axis.


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287.07 307.5 MT-CO.pl Return to previously described conglomerate. Becomes more mylonitic down hole.

307.5 308.7 MI.dk.psk Highly strained and altered metamorphosed mafic dyke. Unit is highly foliated and dark green. Foliation // to contacts. Original mineralogy impossible to identify.

308.7 310.1 MT-CO.pl.my Mylonitized conglomerate unit: same above. Rock here is very blocky andof poor quality.

310.1 311.2 FI.por.fp Very rusty and red unit of what appears to be the coarse grained felsic porphyry unit. Unit is weakly to moderately magnetic. Unit looks like it contains 25-35% white phenocrysts which are stretched and unidemtifiable here within a redish highly altered matrix (and this is seen in < 50% of the unit as alteration has been texturally desrtuctive). Lower contact is broken core.

311.2 318.2 MT-CO.pl.my Mylonitized conglomerate unit: same above. Rock here is very blocky andof poor quality.

318.2 320.7 FI.por.fp Very rusty and red unit of what appears to be the coarse grained felsic porphyry unit.: Same as above. Very messed up rock. Lower contact broken core.

320.7 324.4 MT-CO.pl.my Mylonitized conglomerate unit: same above. Rock here is very blocky and of poor quality.

324.4 355.4 FI.por.fp Very rusty and red unit of what appears to be the coarse grained felsic porphyry unit.: Same as above. A few small intensely chl/ep/ser altered mafic units present with sharp contacts and one that cuts // to the c/a. Lower contact at 15 degrees to c/a. This section is far less deformed and one can clearly make out 3 - 5 mm white phenos. The unit is cutby many small green (act? Chl) veins and quartz veins all generally < 1mm thick.

355.4 365.1 MI.dk.pk Intrensely alterd and sheared mafic unit: Dark green unit of intense green alteration (chl/ser/ep/act?). Unit is strongly foliated and the original textures have been completely destroyed due to the alteration and tectonism. Foliation is at ~ 30 degrees to c/a and the lower contact is sharp with and at roughly 35 degrees to c/a. Hematite is seem in the upper portion of this unit and is interpreted to me derived from the above felsic porphyry. Unit cut be minor this veinlettes of carbonate.


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365.1 369.2 MT-CO.pl.my Banded mylonite of more felsic rock. Alternating mm scale salmon pink, grey, green, white bands at roughly 40 degrees to c/a. The original texture of the rock has been completely destroyed, however, it is interpreted to be mylonitized conglonerate as this rock type is the only in the area and it makes the most sense. Also, there is rock that looks just like this at the JL camp that clearly is deformed conglomerate. The lower contact is sharp and the same as foliation.

369.2 380.9 MT-IV Fine grained metamorphosed and tectonized intermediate in composition rock. Green to green with cloudy reddish overprint of hematite and possibly kfs. Unit is weakly to intensely deformed (though intense is less often) and occationally a few 1 to 2 mm white crystals can be made out giving it a bit of a porphyritic texture in places (where present, the larger crystals only make up about 5% of the rock. The lower contact is sharp and appears to be an old healed fault indicated by a 3 to 7 mm thich brecciated zone between the the two units, also a 3 cm thick green altered rock on the hanging wall of the fault which is likely a small mafic dyke that exploited the weakness in the rocks. The contact and fault and dyke are at 25 degrees to c/a.

380.9 389.9 MT-FV.por Spotty foliated intermediate volcanic porphyritic unit. Pinky unit composed of 20 - 25% fuzzy white spots, 4 - 8mm within a pink/white groundmass. Much of the original texture has been whiped out due to the intense silica and or kfs alteration and straining of the rock. Lower contact (25 degrees to c/a) is sharp and truncates the foliation. Unit is moderately magnetic with magnetite concentrated in veinlettes.

389.9 390.55 MI.dk.psk Fine grained, undeformed equigranular diabase dyke. Unit is composed of 50% plag and 50% mafic minerals (px>hbl). Unit is weakly magnetic, and contains trace blebby pyrite. Lower contact cuts foliation of the lower unit and is about 25 degrees to c/a. Mafic minerals are chl/ep altered giving the rock a green colour.

390.55 408.1 MT-FV.por Spotty foliated intermediate volcanic porphyritic unit. Same as above the dyke. Lower contact is sharp and cuts foliation at a low angle.

408.1 408.85 MI.dk.pk Fine grained foliated and altered mafic rock. The dyke cut the foliatin of the above unit, but it itself is foliated at the same angle as the upper and lower unit. The unit has been altered to chl and ser and ep and act? Giving it a green colour. Plag and the occasional hbl can be made out..


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408.85 420.8 MT-FV.por Spotty foliated intermediate volcanic porphyritic unit. Same as above the dyke. The lower contact is sharp and at 55 degrees to c/a

420.8 446.9 MT-IV Fine grained foliated intermediate in composition sandstone rock: Fine grained green to green w cloudy red alteration rock. Unit is moderately foliated and cut by numerous magnetite/cartlice veins (calcite in the middle). Also pervasive magnetism away from the veinlettes. Reddish colour due to FexOy staining and poss kfs alteration. Also present are a few course grained mag/hbl/act/py veins and occational cpy is present. The unit gets less reddish with depth. The foliation is roughly 45 degrees to c/a and the lower contact is sharp with a mafic intrusive and folliation is cut by the mafic. In places the unit is somewhat porphyritic with up to 5% 3-8mm plag crystals present. Unit is mineralized and the best zones are 421.25 to 412..6 with avg of ~500 and high of 941 cps; 435.2 to 435.7 acg. 400 and high of 573 cps; 440.2 to 441.2 m with avg of 390 and high of 495 cps. Sampled from 418m in the unit above to 445 m.

446.9 449.3 MI.dk.pk Dark green foliated mafic intrusive unit. This rock of composed of 40% plag, and 60% mafics (px>hbl). The unit is mostly equigranular and green altered (chl/ser/ep). It is moderately magnetic and contains 1-2% disseminated py. The lower contact is sharp and contains fragments of thelower described unit (and thus is younger).

449.3 466 FI.por.fp Coarse grained felsic porphyry intrusive rock. Sheared and metamorphosed coarse grained prophyrytic rock. The porphyries (70% of the rock) are 5 to 15 mm in size and composed of sub-angular to rounded feldspars (plag and kfs with kfs>plag complising 90% of phenos) and rounded and slightly smaller quartz eyes (10% of phenos). The matrix is foliated with foliation weaving around phenos and is composed of feldspar, magnetite, biotite, chl and pink garnet.

466 467.25 MI.dk.pk Fine grained foliated dark green-grey mafic dyke with xenoliths of the above instiusion and crystals from the above intrusion as well. Unit is fine grained plag (45-50%) and deformed and altered mafics (50-55%). Xenoliths complise 5 to 20% of the unit and large chunks of the granodioriter above are present. The unit is non-magnitic. The lower contact is sharp and cuts the fabric of the below unit.


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467.25 471.2 MT-IV Fine grained foliated intermediate in composition sandstone rock. Same as above. Unit green to greey-red with the red being clould and from hematite and/or poss kfs altn. Lower contact is sharp and cuts foliation. I'm pretty sure this is that same unit as the mineralized unit above. Radiation levels are slightly elevated with spot highs between 200 and 300 cps. Small slightly deformed equigranular mafic dyke at ~469.5 and 20 cm thick at 15 degrees to c/a.

471.2 471.9 MI.dk.por Dark spotty undeformed mafic porphyritic rock: Phenocrysts complise ~15% of the rock are are lath shaped plagioclase crystals up to 3 mm in length and randomly oriented except near the sharp contacts where they are alligned with the contacts. The matrix is about 45% plag and 55% hbl and px.Trace dis py present. Contacts cut the foliation of the volcanics.

471.9 483.45 MT-IV Fine grained foliated intermediate in composition sandstone rock. Same as above. Unit green to greey-red with the red being clould and from hematite and/or poss kfs altn. Lower contact is sharp and cuts foliation. I'm pretty sure this is that same unit as the mineralized unit above. Radiation levels are slightly elevated with spot highs between 200 and 300 cps. The lower contact is sharp and cuts foliation.

483.45 485 MI.dk.psk Undeformed mafic dyke: Unit is dark grey-green, equigranular and composed of 40% plag, 10% hbl and 50% px. Trace py present andunit is greeninst due to weak chl altn. Lower contact // to upper, is sharp and cuts foliation. Grain size slightly smaller at contacts.

485 495.5 MI.dk.por Mix of equigranular mafic dyke, porphyritic mafic dyke and coarse grained felsic intrusive (granodiorite). The unit is mostly the two mafics and contan fragments and crystals from the granodiorite. See descriptions of each above. The lower contact is sharp, but irregular with granodiotire. Foliation primarily in the granodiorite, but faint is present occationally in the mafics.

495.5 517 FI.por.fp Coarse grained felsic porphyry intrusive rock. Sheared and metamorphosed coarse grained prophyrytic rock: Same as above. EOH


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0 1.9 OVBD Overburden

1.9 7.88 MT-CO.pl.my Dark grey-black unit, fine grained matrix. Strongly foliated and highly sheared clasts (10-15%) with selvages of yellowish-brown Ankerite, chlotire +/- biotite. Looks like the conglomerate with sheared clasts, altered rims and metamorphosed. Few clasts of dark silicious material as well as very few localized jasper clasts and low amounts of carbonate clasts, possibly Ankerite. Unit is non-magnetic. UC is not present, LC is at 7.88m @ 65 deg.

7.88 13.58 MT-IV Dark grey intermediate volcanic with a fine grained matrix. Locally moderate foliation present. Composed of large amounts of biotite, as well as chlorite +/- hematite +/- carbonate. Chlorite and hematite is found mainly in foliations and along fractures and calcite is present in fractures. Unit is cut by a possible chlorite-rich magnetic shear zone or dikelet 8-10cm wide @ 65deg to CA with strong potassic (chl-epid-pot) alteration present in host rock. Unit exhibits patch, weak magnetism overall. UC and Lc are @ ~65 deg and are both gradational.

13.58 15.35 MT-CO.pl.my Dark grey-black unit, fine grained matrix. Moderately foliated and highly sheared clasts (10-15%). Contains Ankerite, chlotire +/- biotite +/- epidote. Looks like the Jacques Lake conglomerate consisting of sheared clasts with altered rims and metamorphosed. Few clasts of dark silicious material as well as low amounts of carbonate clasts and possible clasts of Jasper, Ankerite and/or Calcite.Strong potassium alteration (chl-epid-pot) is present from 14.29m to 15.35m. Unit is non-magnetic. LC @ 45deg.

15.35 21.02 MI.dk Medium-dark grey fine grained homogeneous mafic dike with 5-10% chlorite in matrix. Unfoliated and Non-magnetic. Calcite present in fractures. Epidote present. LC @ 50deg.

21.02 24.6 MT-CO.pl Dark grey to fruit cake coloured locally clast poor metamorphosed polylithic conglomerate. Typical clast assembalage of moderately sorted, subround to subangular multicoloured mudstone, int. volcanics, felsic volcanics and blebby actinolite, sericite throughout. Veining comprised of pistachio epidote and buff, vuggy qtz-carb. Pervasive silica alteration, patchy very weak hematite alteration, fsp + ser alt as blebs + coating/rimming. Locally very blocky and broken. Occasionally intensely veined/altered by ep/chl/act/ser. Bottom contact is roughly perpendicular t.c.a, but vague due to broken core. Patchy moderate magnetism in clast rich sections. Weak local fabric oriented approx 55 degrees t.c.a. Occasional presure shadow around rounded ser alt fp pheno.


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24.6 31.9 MT-IV.por.fp Dark grey aphanitic to very finely porphyritic moderately strained metamorphosed intermediate volcanic. Intensely altered by dull green act, lesser fleshy pink blebby kspar alt. Buff white qtz-carb veinlets throughout the unit. Non magnetic, no sulphides. Fabric oriented 60-65 degrees t.c.a. Occasional thin <20cm dark green fine grained mafic dyke cuts the unit, also one <10cm fleshy pink fien grained felsic dyke.

31.91 41.47 MT-CO.pl Typical polylithic metamorphosed polylithic conglomerate, usual brown-green fruit cake apperance. Typical clast assembalage of moderately sorted, subround to subangular multicoloured mudstone, int. volcanics, felsic volcanics and blebby actinolite, sericite throughout. Veining comprised of pistachio epidote and buff, vuggy qtz-carb. Pervasive silica alteration, patchy very weak hematite alteration, fsp + ser alt as blebs + coating/rimming. Locally very blocky and broken. Occasionally intensely veined/altered by ep/chl/act/ser. Fabric oriented approximately 50 degrees t.c.a.

41.47 81.03 MT-CO.pl Dark grey, Felsic meta-volcaniclstic. Typical Jacques lake conglomerate consisting of a fine grained matrix with abundant clasts of various sizes and compositions. Clasts are sheared and metamorphosed. Contains Ankerite, chlotire +/- biotite +/- epidote. Chlorite and Epidote present in veins and veinlets respectively.. Few clasts of dark silicious material as well as low amounts of carbonate clasts and possible clasts of Jasper, and Calcite. Calcite also present in fractures and veins. Deformation increases with depth. Foliation lies ~60deg t.c.a. Unit has patchy magnetism which is moderate to strong. Unit is cut by various dikelets which vary in length from 8cm to 12cm. At 47.85m, there is a 60cm dike. It contains two sharp contatcs, ~60deg t.c.a. and contains chlorite and epidote veining. At 62.98m, there is a 97cm long dike. It contains two sharp contacts ~58deg t.c.a and also contains chlorite and epidote veins. The units LC is sharp, at ~60deg t.c.a and at 81.03m

81.03 87.84 MI.dk.pk Dark green-grey, mafic dike. Moderatly foliated. Foliation ~55deg t.c.a. Contains chlorite and epidote veins and fractures, (ep>ct) as well as hemitate in fractures towards the end of the unit. Contains a low amount of k-feld phenos. (>0.05%) and is moderatly magnetic. UC and LC is sharp, at ~60deg t.c.a


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87.84 98.47 MT-CO.pl.my Felsic meta-volcaniclstic. Typical Jacques lake conglomerate. See Above. Foliation is strong. Strong Hemitate alteration present from 88.40m to 89.71. Unit is cut by 8cm dikelet at 91.18m, and a 92cm long syn-kinematic mafic dike at 91.22m, both with a folication ~45 deg t.c.a. Unit Foliation ~45deg t.c.a. U.C ~ 60deg t.c.a, L.C at 98.47m ~45deg.

98.47 117.16 FI.dk.por Dark grey, medium to fine grained felsic intrusive. Abundant biotite +/- hornblende pervasive throughout the matrix. Unit is weakly foliated @~45deg t.c.a. Calcite present on fractures throughout. Possible k-feld. alteration at 111.70m. Unit becomes more porphyritic with depth, containing larger amounts of feldspar phenocrysts (possibley palg.) comprising 10-12% of the unit. LC is sharp, at 117.16m and ~30deg t.c.a. Unit is non-magnetic.

117.16 121.36 MT-CO.pl.my Highly strained, lesser course grained conglomerate. Highly sheared clasts (10-15%) with selvages of yellowish-brown Ankerite, chlorite +/- biotite. Looks like the conglomerate with sheared clasts, altered rims and metamorphosed. Few clasts of dark silicious material as well as very few localized jasper clasts and low amounts of carbonate clasts, possibly Ankerite. Moderate calcite veining throughout as well as low amounts of blebby pyrite (>0.5%) and low amounts of epidote present in veinsn (>0.5%). L.c is sharp, ~15% t.c.a. Patchy, strong magnetism throughout.

121.36 136.13 FI.dk.por Dark grey, medium to fine grained felsic intrusive. See above. Low amount of undeformed quartz phenos. (>0.5%). Becomes more fine grained with depth.

136.13 137.9 MT-CO.pl.my Highly metrmorphosed and highly strained. Possibly conglomerate with high level of deformation and various quartz veining (ranging in size from 8-12cm) throughout. Chlorite and epidote veining present. (5-10%). With depth, unit become more fuggey with small amounts of calcite dust on fractures. L.c is irregular. Unit exhibits patchy, moderate magnetism.

137.92 139.72 FI.dk Dark grey, fine grained felsic intrusive..Low amount of phenos.Large amount of epidote veining throughout (stockwork). Unit is patchy, weakly magnetic. No clear foliation present.


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139.72 239.67 MT-IV.my Dark green, Highly metrmorphosed and highly strained intermediate volcanic. Banded sand size material (80%) with conglomerate bands (20%) of gravel size clasts with high level of deformation and shearing. Various chlorite and epidote veining throughout (ct>ep). Unit has small amounts of calcite in fractures. Very small amount of a blood red mineral, possibly jasper (>>0.5%). Bandes of magnetite present. Patchy, slight hematite alteration present beginning at 150.03m until 175.48. Chlorite alteration begining at 151.77m and is patchy throughout. At 207.05 hematite alteration begins again. Unit is cut by a mafic pre-kinematic 40cm dike with sharp contacts and strong foliation (~55deg t.c.a) at 149.32m. Also cut by 40cm a mafic post-kinematic dike at 155.49m. At 176.86 unit is cut by a 22cm spotty pre-kin. mafic dike with strong foliation ~55deg t.c.a. At 206.90 there is a 16cm post kinematic dike. At 221.47 there is a 40cm post-kin. Mafic dike. At 226.78 unit is cut by a 54cm porphyritic felsic dike with irregular contacts Unit exhibits patchy, moderate magnetism untill 209.06 and is locally fuggy, which increases with depth. Possible fault at 151.86m as well as a minor fault peresnt at 175.65m. At 209.06 Magnetite alteration begins, and increase with depth. Unit becomes strongly magnetic to very strongly magnetic. Beginning at 215.34 unit increase in fuggy calcite bands with depth. At 222.10 unit becomes mineralized unitl 226.15 with a high of 4000cps and an average of 1825cps. Unit is mineralized from 234.50 untill 238.25m with a high of 3250cs and an average of 1118cps. L.c is sharp, at ~55deg t.c.a at 239.67m

239.67 241.51 MI.dk.pk Dark green-grey, mafic dike. Moderatly foliated. Foliation ~50deg t.c.a. Contains chlorite and epidote in veins and fractures, (ep>ct). Trace amounts of pyrite present. Calcite in fractures. Unit has patchy, weak magnetism.

241.51 252.52 MT-IV.my Dark green, Highly metrmorphosed and highly strained intermediate volcanic. Various chlorite and epidote veining throughout (ct>ep). Unit has small amounts of calcite in fractures as well as a larger amount of calcite and magnetite banding. Small amount of plag. phenos present throughout (>0.5%). Slight hematite alteration beginning at 242.15m untill 243.72m. Unit is cut by a 33cm porphyritic felsic dyke at 245.43 with plag phenos (~20%). Also cut by an 83cm porphyritic dyke at 246.15m with 20% plag phenos. Both dykes are moderatly foliated, @~50deg t.c.a. Unit exhibits patchy, moderate magnetism throughout. Unit is mineralized from 242.13 to 242.87 with a high of 280cps and an average of 270cps.


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252.52 254.44 FI.dk Dark grey, fine grained felsic intrusive. Moderatly foliated. Abundant biotite +/- horneblend. Low amount of plag phenos, ranging up to 8mm (~5-7%). Calcite present in fractures. Trace amount of diseminated pyrite. L.c is irregular. Unit is non-magnetic.

254.44 280.16 MT-IV.my Dark green-grey, Highly metrmorphosed and highly strained intermediate volcanic. Various chlorite and epidote veining throughout (ct>ep). Unit has small amounts of calcite in fractures as well as a very small amount of calcite and magnetite banding. Small amount of plag. phenos present throughout (>0.5%). Small amount of possible Barite present. Hematite present in fractures. A 2cm quartz vein present at 256.12 along with a small amount of gypsum and chlorite. Minor chlorite alteration present at 258.14. Slight hematite alteration from 273.46 untill 274.16m. Unit is cut by a 40cm prophyritic felsic dyke at 263.96m with ~15% plag. phenos. Beginning at 264.75m, bands of calcite, horneblend +/-actinolite begin to increase with depth unitll 276.05m. Unit is mineralized from 266.07m untill 267.06 with a high of 500 cps and an average of 300 cps. Unit is mineralized from 266.38 untill 272.52 with a high of 230 cps and an average of 215 cps. Unit is mineralized from 273.44 untill 276.00 with a high of 1320cps and an average of 478cps. L.c is at 280.15m and is @ ~45deg t.c.a

280.16 283.35 FI.dk Dark grey, fine grained felsic intrusive. Moderatly foliated. Abundant biotite +/- horneblend. Low amount of plag phenos, ranging up to 8mm (~5-7%). Calcite present in fractures. Trace amount of blebby pyrite. L.c is sharp and irregular. Unit is non-magnetic.

283.35 300.61 FI.por.fp A grey-black coarse-grained feldspar prophyritic felsic intrusive. Weak to moderatly strained Phenocrysts ranging is size up to ~19mm. Composed of rounded to sub-rounded plag, k-feld, and a lesser amount of rounded quartz. Matrix is comprised mainly of biotite +/- hornblende. Foliation is week to moderate, at an angle of ~50deg to c.a.Unit is moderatly magntic. Upper contact is irregular, and @ ~65deg to c.a. L.c is sharp, @~60deg t.c.a. Unit is cut by a 57cm felsic dyke with ~5% plag phenos. And >1% blebby pyrite.


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300.61 343.53 MT-IV.my A black-brown, Highly metrmorphosed and highly strained intermediate volcanic. Various chlorite and epidote veining and blebbs throughout (ct>>ep). Unit has small amounts of calcite in fractures as well as a moderate amount of calcite,magnetite, horneblend +/-actinolite banding, which increase in depth. Hematite present in fractures. Slight hematite alteration begins at 301.05m untill 309.70. At 305.26m, unit is cut by a 46cm post kinematic porphyritic mafic dyke with ~15% white plag. phenos, >1mm in size and disseminated, with small amounts of calcite in fractures. U.c is @~58deg t.c.a At 330.55m unit is cut by a 30cm post kinematic porphyritic mafic dyke with ~5-7% white plag. Phenos, >1mm in size and disseminated. U.c @~65deg t.c.a Unit has patchy, weak magnetism throughout. L.c is @~62deg t.c.a. Unit is mineralized from 300.80 to 303.90, with a high of 170cps and an average of 140cps. Unit is mineralized from 308.15 to 308.78 with a high of 245cps and an average of 177cps. Unit is mineralized from 320m to 321.80m with a high of 170cps and an average of 134cps. Unit is mineralized from 333m to 335m with a high of 139cps and an average of 116cps. Unit is mineralized from 336m to 340.10m with a high of 810cps and an average of 183cps.

343.53 345.28 MI.dk.psk Dark grey-black, post-kinematic mafic dyke, 170cm in length. Contains bands of calcite, horneblende +/- biotite. Calcite also present in fractures. No dominant foliation present. Also contains small amt of chlorite veins and blebbs of chlorite. L.c is irregular.

345.28 367.42 MT-IV.my A black-brown, Highly metrmorphosed and highly strained intermediate volcanic. Various chlorite and epidote veining and blebbs throughout (ct>>ep). Unit has calcite in fractures as well as a moderate amount of actinolitc veining +/- calcite,magnetite, horneblend untill 348.62m. Trace disseminated pyrite. K-feldspare alteration present at 348.14m. Slight hematite alteration begins at 356.69 untill 361.66mm. Unit has patchy, moderate magnetism throughout. At 361.74m unit is cut by a 97cm post kinematic porphyritic mafic dyke with ~20% white plag. phenos, >1mm in size and disseminated. Small amounts of epidote and calcite in fractures. U.c is @~62deg t.c.a, l.c is irregular. Unit is cut at 366.21m by a 41cm post kinematic porphyritic mafic dyke with ~10% white plag. phenos, >1mm in size and disseminated. Unit is mineralized from 356.77m to 359.70m with a high of 640 cps and an average of 260 cps.


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367.42 368.87 MI.dk.psk A dark grey, 136cm long mafic dyke with a medium to fine grained matrix of plag., biotite +/- horneblend. Unit is non-porphryitic and non-foliated. Contains calcite in fractures. Is non-magnetic. Dyke is cut by a 15cm foliated intermediate volcanic lense at 368.43m as well as a 1cm quartz vein at 368.68m. L.c is @~62deg t.c.a.

368.87 370.05 MT-IV Reddish-brown, metamorphosed and moderatly foliated intermediate volcanics. Medium to fine grained matrix of mainly biotite +/- horneblend +/- amphibole.No alteration present. Caclite in fractures. Unit is non-magnetic Upper contact @~62deg t.c.a. Lower contact is slightly irregular, @~60deg t.c.a.

370.05 371.34 MI.dk.psk Dark grey-black, post-kinematic mafic dyke, 129cm in length. Calcite present in fractures. No dominant foliation present. Also contains small amt of epidote in fractures. Unit is non-magnetic. L.c is @~50deg t.c.a

371.34 395 MT-IV.my Dark brown, Highly metrmorphosed and highly strained intermediate volcanic. Banded sand size material (70%) with conglomerate bands (30%) of gravel size clasts with high level of deformation and shearing untill 379.30. Various chlorite and epidote veining throughout as well as epidote in fractures (ep>ct). Unit has small amounts of calcite in fractures. Very small amount of a blood red mineral, possibly jasper (>>0.5%). Pervasive, slight hematite alteration present beginning at 1376.95m until 378.60. Unit is locally vuggy untill 379.30. Unit has patchy, strong magnetism. Unit is cut at 382.85 by a 92cm pre-kinematic, foliated mafic dyke comprised of plag, biotite +/- horneblend. Foliation ~57deg t.c.a. Lc @~60deg t.c.a. Unit is cut at 384.34 by a 83cm long pre-kinematic, foliated mafic dyke comprised of plag, biotite +/- horneblend. Foliation ~57deg t.c.a. Lc @~60deg t.c.a. At 386.61 unit is cut by a 57cm pre-kinematic, foliated mafic dyke comprised of plag, biotite +/- horneblend. Foliation ~58deg t.c.a. Lc @~60deg t.c.a. Chlorite alteration present at 390.47m. At 393.34m unit becomes porphyritic with horneblend phenos. (possible replacement) End of Drill hole.


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0 8.2 OVBD Overburden

8.2 28.29 MI.dk.psk Moderate-strongly chloritized, poorly foliated, fine-grained to locally med-grained, syn-late-kinematic mafic dike. Unit is vuggy throughout. Chlorite present as a replacement mineral for bt. Plagioclase present as phenocrysts w/n unit which increase in size locally downhole. Minor hematitic replacement of pg phenos local to contact to next unit. Unit has a vuggy-bleached look due to proximaty to surface. Non-magnetic. Upper contact is lost. Lower contact is irregular and poorly defined.

28.29 37.02 MT-IV Strongly hematized, fine-grained, intermediate to mafic volcanics. Due to pervasive hematization foliation is hard to discern. Hematization is less pervasive downhole. Hematic replacement of pg phenocrysts present throughout. Weak-patchy magnetism. Enclaves of more hematized portion of upper unit found at depth. Upper contact is irregular. Lower contact is at an angle of 56 degrees to C.A.

37.02 41.54 MI.dk Mafic dike with strong, pervasive carbonate flooding throughout. Relict texture extremely hard to discern due to pervasivity of carbonate flooding in unit, but with abundant ct present throughout unit it appears to be a mafic dike.Phenos are hard to discern but there is some pg present as phenos in areas. Moderate patchy hematite present with patchy magnetite throughout. Upper and lower contacts are irregular with strongly hematized bands alternating with ct defining them. Lower contact is so irregular that it is hard to get an angle measurement to the C.A.

41.54 46.9 MI.dk.pk Fine-grained to locally coarse-grained, chloritic, weak to moderately foliated, pre-kinematic mafic dike. Unit contains larger phenos of pg ~1cm in size (~1%) as well as fine-grained pg phenos giving the unit a bimodal nature. Foliation is present is not well defined. Minor carbonate present along small micro fractures. Weak patchy magnetism. Upper contact is irregular. Lower contact is at an angle of 60 degrees to C.A.

46.9 58.11 MT-IV Strongly hematized, fine-grained, moderate-strongly foliated, intermediate to mafic volcanics. Hematization is less pervasive downhole. Hematic replacement of pg phenocrysts present throughout. Weak-patchy magnetism. Enclaves of more hematized portion of upper unit found at depth. Upper contact is at an angle of 60 degrees to C.A. Lower contact is at an angle of 65 degrees to C.A.


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58.11 86.82 MT-IV Dark-grey, grey-black, moderately foliated, fine-grained, chlorite-rich, flow-banded intermediate to mafic volcanics. Flow texture is strong throughout and is dominated by chlorite-rich (+/- ep) nodules surrounded by hematitic replacement haloes. Matrix is fine-grained making mineralogy hard to discern, possible pg+pyroxene matrix w/ minor micacious mineralogy. Minor vuggy carbonate present locally w/n ct nodules. Upper contact is @ an angle of 65 degrees to C.A. Lower contact is @ an angle of 75 degrees.

86.82 97.06 MT-MI.fgr Dark-grey to black, fine-grained, weakly foliated, flow-textured mafic intrusive.Unit conatins minor randomly oriented px/hb patches throughout. The unit is relatively carbonate-rich along fractures and small mafic cross-cutting diklets. Unit contains 2 small (<10cm) highly chloritized mafic dikes. Minor kspar-alteration between 93.00m-94.00m. Some minor ct along fractures. Matrix is dominantly pg+px+/-hb+/-ct+/-bt. Upper contact is @ an angle of 75 degrees to C.A. lower contact is irregular (gradational) and poorly defined. Weak magnetism.

97.06 106.05 MT-IV Green-grey to grey-red, fine-grained to locally clastic, metamorphosed intemediate volcanics. The matrix is locally ct-rich surrounding large angular to breciatted clasts of jasperoidal material which are riddled throughout the unit making the protolith hard to discern. Sodic alteration present along faintly foliated areas. Small mafic dikes present (<20cm) b/w 91.05m-101.25m. Minor ep present in broken bands of what was previously intermediate volcanics. Minor carbonate present along small cross-cutting fractures. No definitive foliation present. Iron oxide alteration present throughout. Unit is weakly magnetic in areas where the unit is unoxidized.Upper contact and lower contacts are gradational and hard to discern.

106.05 113.8 MT-IV Pink to red, Intensley hematitized and albitized, highly strained, fine-grained intermediate volcanics. Unit pervasively hematized and albitized making mineralogy hard to discern. Lobes of ct bearing rock visable intermittent throughout unit indicating an intermediate nature. Abundant sheared porphyroblasts of mt present that are eliptical indicating strain. Unit is cut locally by a small (<1.00m) highly sheared and chloritized pre-kinematic mafic dike from112.70m-113.28m. Upper contact is gradational. Lower contact is at an angle of 65 degrees to C.A.


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113.8 129.42 MT-IV.por.fp Dark grey, grey-purple, strongly foliated and sheared, fine-grained, feldspar porphyritc, intemediate volcanics. Porphyroclasts of fp (k-spar+pg) display hm-replacement throughout unit gradually becoming more prominant downhole. Matrix appears to be pg + mafic mineralogy to fine-grained to distinguish. Foliation defined by banding of micacious mineralogy. Unit also contains abundant porphyroclasts of blue quartz eyes throughout. Unit is moderately magnetic. Abundant mafic dikelets present, some crosscutting foliation some along foliation, containing ct and bt +/- ep. Mafic dikelets are locally albitized in areas. Upper contact is @ an angle of 65 to C.A. Lower contact is broken and lost.

129.42 130.69 MI.dk.sk Chloritic, bt-rich, intensley foliated, fine-grained, pre-syn-kinematic, mafic dike. Foliation is strong and defined by banding of ct+bt. Carbonate present alongfoliation as well as in cross cutting minor fractures which are also locally breciatted. Some minor pg present w/n breciatted regions +/- qz. Minor bands of hematite altered enclaves of the unit above (MT-IV.por.fp) b/w 129.90m and 130.05m. Unit is non-magnetic. Upper contact is broken and lost. Lower contact is at an angle of 58 degrees to C.A.

130.69 150.1 MT-IV.por.fp Dark grey, grey-purple, strongly foliated and sheared, medium-grained to locally fine-grained, feldspar porphyritc, intemediate volcanics. Porphyroclasts of fp (k-spar+pg) display hm-replacement throughout unit. Matrix appears to be pg + mafic mineralogy to fine-grained to distinguish. Foliation defined by banding of micacious mineralogy. Unit also contains abundant porphyroclasts of blue quartz eyes throughout. Unit is strongly hematized and albitized b/w 130.69m-142.60m. Cut locally by 2 small (<1m) highly chloritized, pre-kinematic mafic dike from 142.60m-143.10m and b/w 149.5m-150.10m. Unit is moderately magnetic. Abundant mafic dikelets present, some crosscutting foliation some along foliation, containing ct and bt +/- ep. Mafic dikelets are locally albitized in areas. Upper contact is at an angle of 58 degrees to C.A. Lower contact is broken and lost.

150.1 171.86 MT-CO.pl Pink-brown to green grey, highly strained, meta-conglomerate. Unit is quite rich in enclaves of felsic meta-vocanics and intermediate meta-volcanics (< 2cm wide). Pervasively chloritized and epidotized in areas. Clasts of japeroid and mudstone are present and are angular to subrounded in shape and vary in size and occurrence downhole. Foliation is defined by thick ep+ct bands as well as banding of micacious mineralogy. Non-magnetic. Upper contact is broken and lost. Lower contact is at an angle of 60 degrees to C.A.


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171.86 173.86 MT-IV Dark-grey to grey-black, intensely foliated, fine-grained, intermediate meta-volcanics. Porphyroclasts are of pg+qz and are very fine-grained. Chloritization is present in pervasive patches throughout unit. Foliation is strong and is defined by the banding of micacious mineralogy. Unit is moderate to strongly magnetic. Upper contact is at an angle of 60 degrees to C.A. Lower contact is at an angle of 60 degrees to C.A.

173.86 206.68 MT-CO.pl Continuation of the previous MT-CO.pl above but more clast-rich. Pink-brown to green grey, highly strained, meta-conglomerate. Unit contains enclaves of felsic meta-vocanics and intermediate meta-volcanics (< 2cm wide). Pervasively chloritized and epidotized in areas. Clasts are of japeroid and mudstone and are angular to subrounded in shape and comprize 40-50% of the unit locally. Vuggy carbonate present in areas. Foliation is defined by angular clasts and by thick ep+ct bands as well as banding of micacious mineralogy. Non-magnetic. Upper contact is at an angle of 60 degrees to C.A.

206.68 273.5 MT-IV Grey-green, ep-rich, ct-rich, moderately foliated, med-grained to locally fine-grained, flow-textured, Hb-porphyritic intemediate to mafic meta-volcanics with enclaves of more intemediate meta-volcanics. Flow texture is comprised of ep+ct+/-bt-altered bands of mafic material which are patchy throughout unit. Some minor Na-alteration + hematite alteration haloes around some of the mafic bands. Porphyroclasts are hb and pg. Hb porphyroclasts are euhedral to subhedral, lathe-shaped to sub-rounded and are roughly 0.5cm-0.75cm in size. Pg porphyroclasts are more fine-grained and anhedral. Foliation is defined by micacious mineralogy. The unit is moderately ct-rich throughout. Unit contains multiple late b/d faults that show a moderate offset of ~2cm. Brittle fault containing gyp+hal with minor carbonate located b/w 239.00m-239.72m. Upper contact is at an angle of 40 degrees to C.A. Lower contact is at an angle of 50 degrees to C.A.


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273.5 311.53 MT-CO.pl.my Orange-brown to green-grey, ep-rich, highly-strained to mylonitic, polylithic meta-conglomerate. K-spar alteration is the dominate form of alteration which gives the unit its orange-tan colour. Foliation is intense and is defined by strained clasts of sedimentary and igneous rocks. Strain increases down hole displayed by the obliteration of relict clasts of the conglomerate which follow dominant foliation. Ep+ct define much of the foliaiton w/n the unit +/- bt and other micacious mineralogy. Clasts where present vary greatly in size from 0.5cm to 2.5cm. Minor ~5cm enclaves of intermediate volcanics present intermittent. Unit has patchy magnetism in areas of minor brittle faulting which contain abundant carbonate+massive magnetite. Unit is cut locally by an early, brittle, relithified faults b/w 297.00m-297.48m. Upper contact is at an angle of 50 degrees to C.A. Lower contact is at an angle of 45 degrees to C.A.

311.53 318.81 MI.dk.sk Chloritic, strongly foliated, fine-grained, syn-kinematic mafic dike. Foliation is intense and is defined by ct + banding of micacious mineralogy. Unit is gauge textured in areas of minor brittle faulting. Upper contact is at an angle of 45 degrees to C.A. Lower contact is at an angle of 48 degrees to C.A.

318.81 326.04 MT-IV Red-pink to grey, well-foliated, strongly albitized and hematized to locally unaltered, fined grained to aphanitic, intermediate meta-volcanics. Unit is intensely potassically altered and hematized giving it an deep red-pink colour. Foliation is prominent and defined by the elongation of relict phenocrysts of pg+/- hb+ct replaced px as well as by the banding if micacious mineralogy. Unit contains abundant, patchy ct intermittent throughout. Unit is cut by a large 1.75m re-lithified brittle fault from 324.27m-326.04m. Upper contact of main unit is at an angle of 48 degrees to C.A. Lower contact is 52 degrees to C.A.

326.04 329.62 MI.dk.psk Green-grey to black, weakly foliated, fine-grained, late-post-kinematic mafic dike. Matrix is fine-grained and undiscernable but more or less mafic. Foliation where present is defined by micacious mineralogy (bt+ct). Minor hematitic alteration present patchy throughout. Unit contains small anastamosing, cross-cutting, chlorite-rich, mafic, micro-vienlets riddled throughout. Weak patchy magnetism present. Upper contact is at an angle of 52 degrees to C.A. Lower contact is indistinct.


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329.62 332.9 MT-IV Grey-pink to grey-green, moderately foliated, fine-grained, flow-textured intermediate meta-volcanics. Porphyroclasts are fine-grained pg+ chlorite altered mafic mineralogy which is quite fine-grained. Unit contains small anastamosing, cross-cutting, chlorite-rich, mafic, micro-vienlets riddled throughout giving the unit a webby, almost breciatted texture. Foliation is moderate and is defined by the banding of micacious mineralogy such as bt and ct. Hematitic atleration is present in massive patches throughout giving the unit a more reddish-pink colour. Potassic alteration also present patchy throughout giving a fleshy-tan colour to the unit. Upper contact is hard to distinguish. Lower contact is at an angle of 45 degrees to C.A. Patchy magnetism.

332.9 334.86 MI.dk.sk Chloritic, moderately foliated, fine-grained, syn-late-kinematic mafic dike. Phenocrysts are of pg+altered mafic mineralogy and are fine-grained. Foliation is defined by banding of micacious mineralogy. Unit contains abundant ct as phenocrystic replacement of mafic mineralogy as well as along foliation, in swathy bands and w/n small webby x-cutting minor mafic dikelets throughout unit is weakly magnetic. Contains abundant pyrite disseminated throughout as well as in massive blebs locally which are around 0.5cm in size. Upper contact at an angle of 45 degrees to C.A. and is well-defined. Lower contact is also well deined and at an angle of 40 degrees to C.A.

334.86 338.86 MT-IV Continuation of previous intermediate meta-volcanic unit. Unit display brittle ducitle nature with small local micro-faulting with ~ 1.5cm offset. More pevasive postassic alteration present w/n flow-textured portions of the unit. Carbonate present w/n small micro fractures ~0.3cm wide. Unit is weakly magentic.

338.86 341.16 MI.dk.sk Chloritic, bt-rich, moderately foliated, fine-grained, pre-kinematic mafic dike. Unit contains abundant phenocrysts of hb around 0.2cm in size as well as finer-grained plag. Webby chlorite throughout. Ct is also present with bt along dominant foliation in unit. Unit is weakly magnetic. Upper contact is at an angle of 57 degrees to C.A. Lower contact is at an angle of 50 degrees to C.A.


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341.16 383.23 MT-IV Pink-green to grey, well foliated, fine-grained, intermediate meta-volcanics. Matrix and pheno mineralogy hard to discern due to the units fine-grained nature. Unit is locally ct-rich in areas as well as potassically altered throughout which gives a green to fleshy pink colour to the unit. Foliation is dominated by the banding of micacious mineralogy such as bt+ct. Unit is relatively carbonate rich. The carbonates occurrence is blebby to disseminated local fracture-filled intervals throughout unit. Small <15cm carbonate-rich, strongly foliated, fine-grained, syn-kinematic mafic dikes present throughout unit. Moderately magnetic. Unit has moderate u-mineralization b/w 367.38m-368.52m with a max: 510cps, avg: 232cps, and also b/w 372.69m-375.00m with a max: 397cps, avg: 261cps. Oriented core, Alpha angle for carbonate vein at 380.37m is at an angle of 45 degrees to C.A. Beta angle for carbonate vein is degrees to C.A. Upper contact is at an angle of 50 degrees to C.A. Lower contact isat an angle of 40 degrees to C.A.

383.23 385.74 MI.dk.psk Fine-grained, post-kinematic leuco-gabbro. Unit is moderately fresh and unaltered with no prominent foliation. Pg phenocrysts create a leopard texture with the mafic matrix. Pg phenos are cloudy-white and around 0.1cm in size. Unit is weakly magnetic. Upper contact is at an angle of 40 degrees to C.A. Lower contact is at an angle of 65 degrees to C.A.

385.74 401.21 MT-IV Continuation of the previous MT-IV unit (341.16m-383.23m). Foliation is weak to locally moderate and is defined by the banding of micacious mineralogy. U-mineralization has ceased w/n this particular unit. Unit contains two enclaves of fine-grained felsic igneous rock b/w 394.90m-395.21m and b/w 395.86m-396.02m. Unit contains local coarser lathe-shaped pg phenos that are roughly 0.5cm-0.8cm. Ct-content is increasing as contact to next unit is approached. Ct occurrence is small blebs to flowing migmatitc swaths. Magnetism is strong in this unit.


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401.21 402.89 MI.dk.por Moderately Chloritic, unfoliated, coarse-grained to locally fine-grained, post-kinematic mafic dike. Phenocrysts are dominantly lathes of pg that vary from 0.1cm in size locally to 1.5cm. The phenos of pg are cloudy-white and transluscent. Some of the grains display nucleation around a central pheno possible slower grow intervals throughout the intrusives history. There are also finer-grained phenos of ct-altered pyroxene. The px pheno occurrence is in small 0.2cm rounded to subrounded grains with little to no visable cleavage. Matix is comprised of fine grained pg and px+ct as well as fe-rich bt. Weak patchy magnetism. Minor disseminated pyrite present. Upper contact is at an angle of 55 degrees to C.A. Lower contact is broken and lost.

402.89 426.4 MT-IV Deep purple-green to grey-black,moderately foliated, fine-grained, intermediate to mafic meta-volcanics. Matrix and pheno mineralogy hard to discern due to the units fine-grained nature. Unit is locally ct-rich in areas giving a green to colour to the unit. Foliation is dominated by the banding of micacious mineralogy such as bt+ct. Unit contains small enclaves of fine-grained felsic intrusive b/w 411.18m-411.44m and b/w 411.84m-412.62m. Felsic intrusive is pg+qz rich with hb phenos. Hb phenos are black and bladed and ~0.2cm in size. The occurrence of MT-FI is syn-late-kinematic with some of the material following the dominant foliation within the MT-IV unit. Matrix of MT-FI is fine Ct-rich swathes of more mafic material occur proximal to contact of next unit rock Unit is relatively carbonate rich. The carbonate occurrence is blebby to disseminated local fracture-filled intervals throughout unit which contain blebby pyrite +/-cpy. Moderately magnetic. Upper contact is broken and lost lower contact is gradational and unmeasurable b/w the next unit.

426.4 429.2 MI.dk.por Moderately Chloritic, unfoliated, coarse-grained to locally fine-grained, post-kinematic mafic dike (mela-gabbro). Phenocrysts are dominantly lathes of pg that vary from 0.1cm in size locally to 1.5cm. The unit overall has a dominantly bimodal nature with variant sized phenocrysts of pg. The phenos of pg are cloudy-white and transluscent. Some of the grains display nucleation around a central pheno possible slower grow intervals throughout the intrusive history. Possible two generations of of post-kinematic mafic dikes within this unit based upon the variant texture and size of the phenos of pg. Finer-grained phenos of ct-altered pyroxene present. The px pheno occurrence is in small 0.2cm rounded to subrounded grains with little to no visable cleavage. Matix is comprised of fine grained pg and px+ct as well as fe-rich bt. Weak patchy magnetism. Minor disseminated pyrite present. Upper contact is gradational and irregular lower contact is broken.


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429.2 433.71 MT-IV Pink-white to grey, moderately foliated, fine-grained, intermediate meta-volcanics. Phenocrysts are of cloudy white pg aroubdwhich comprizes ~2% of the unit. The matrix is more chloritic to bt-rich. Unit appears to have been cooked by the mafic dike above and below it which is reflected in the locally massive (concentration) occurrence of the pg in areas. Upper contact is broken lower contact is sharp but irregular and unmeasurable. Moderate patchy hematization and magnetite.

433.71 438.85 MI.dk.por Moderately Chloritic, unfoliated, coarse-grained to locally fine-grained, post-kinematic mafic dike (mela-gabbro). Phenocrysts are dominantly lathes of pg that vary from 0.1cm in size locally to 1.5cm. Same as mafic dike unit b/w 426.4m-429.2m. Upper contact is irregular but roughly at an angle of 40 degrees to C.A. Lower contact is at 40 degrees to C.A.

438.85 456.95 MT-IV Deep purple-green to grey-black,moderately foliated, fine-grained to locally medium-grained, intermediate to mafic meta-volcanics. Matrix and pheno mineralogy hard to discern due to the units fine-grained nature. Local cludy white 0.3cm mgr of pg present. Unit is locally ct-rich in areas giving a green to colour to the unit. Foliation is dominated by the banding of micacious mineralogy such as bt+ct. Unit contains a small enclaves of fine-grained felsic intrusive b/w 444.78m-444.97m that is well deformed and sheared. Matrix of MT-FI is fine Ct-rich swathes of more mafic material occur proximal to contact of next unit rock Unit is relatively carbonate rich. The carbonate occurrence is blebby to disseminated local fracture-filled intervals throughout unit. Moderately magnetic. Unit contains minor U-mineralization b/w 452m-452.40m with a max of 609cps and a avg: 404cps. The mineralized zone is well breciatted and Na-altered with mt veinlets riddled throughout. The breciation and mineralization appears to be caused by a small 30cm long by 3cm wide felsic intrusive vein. Upper contact isat an angle of 40 degrees to C.A. lower contact is at an angle of 75 degrees to C.A.

456.95 458.1 MI.dk.por Un-foliated, fine-grained, post-kinematic melagabbro. Phenocrysts are ~0.2cm cloudy-white, lathe-shaped grains of pg which have a peppered-like random occurrence throughout. Matix mineralogy is fine-grained and likely px+pg. Patchy strong magnetism. Upper contact is 75 degrees to C.A. Lower contact is broken and lost.


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458.1 460.52 MT-IV Deep purple-green to grey-black,moderately foliated, fine-grained to locally medium-grained, intermediate to mafic meta-volcanics. Matrix and pheno mineralogy hard to discern due to the units fine-grained nature. Local cloudy white 0.3cm mgr of pg present. Unit is locally ct-rich in areas giving a green to colour to the unit. Foliation is dominated by the banding of micacious mineralogy such as bt+ct. Unit contains a small x-cutting portion of the mafic dike unit below this one from 459.26m-459.45m. Upper and lower contacts are broken and unmeasurable.

460.52 463.29 MI.dk.psk Un-foliated, fine-grained to locally mgr, post-kinematic melagabbro. Mgr and fgr phenocrysts are ~0.2cm to locally 0.4cm cloudy-white, lathe-shaped grains of pg which have a peppered-like random occurrence throughout. Matix mineralogy is fine-grained and likely px+pg. Patchy strong magnetism. Upper contact is broken and lost. Lower contact isat an angle of 58 degrees to C.A.

463.29 492 MT-IV Dark grey-green, pink-purple, weakly foliated, fine-grained to locally med-grained, intermediate to mafic volcanics. Unit is locally ct-rich in the more mafic portions.The dominantly mafic and is locally cut by small (<15cm) pre-kinematic mafic dikes throughout. Sparse 0.3cm subhedral, cloudy-white pg phenocrysts are local throughout. Pg is mostly concentrated along swathing bands throughout which also contain small (0.1cm) lathe-shaped phenos of what appears to be actinolite. These bands are anastamosing and random in their orientation sometimes mirroring the weak foliation. Minor hb present in mafic regions of the unit. It appears to be a replacement mineral for px. The unit contains moderate patchy to locally massive amounts of ep. Ep occurrence is as an alteration mineral w/n the mafic dikes. The unit has strong pervasive magnetism. Trace carbonate locally throughout. Upper contact is at an angle 58 degrees to C.A. no lower contact (EOH: 492.00m).


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0 0.7 OVBD NULL

0.7 4.8 MT-CO.pl Strained and metamorphosed polylithic gravel/conglomerate. Gravel sized (occationally larger) sub-angular to sub-rounded clasts of various lithologies which is clast supported and with a matrix of finer grained material. Unit is moderately straine stretching all clasts. Unit is mottled white and non-magnetic. Unit is cutmy minor late veinlettes of quartz and calcite. The lower contact is broken but likely sharp.

4.8 49.5 MI.dk.pk Porphyritic and strained mafic intrusion: Dark green with stretched 3 to 12 mm mostly biotite/chl altered hbl phenocrysts within a fine grained matrix. The matrix is conposed of plag and dark mafic mineral(s) which are too altered and deformed to make out. Unit is patchy moderate magnetism and contains trace dsm py. The hbl phenos are in places fresh enough to tell for sure that they are hbl.

49.5 53.3 MI.dk.psk Dark grey aphanitic diabase dyke: Featureless fine-grained dark-grey green mafic dyke. Has two sharp contacts though the upper is broken core, The lower contact is sharp and has 2 cm altered of alteration. The units greenifh colour is due to fine grained chl alteration. Unit is moderately hard and has a weak pervasive magnetism. Unit cut by minor calcite veins.

53.3 56 MI.dk.psk Undeformed dark greenish hbl porphyritic mafic dyke. Similar mineralogy to the previously described hbl porphyry, but undeformed and relatively unaltered anf smaller phenocrysts. The lower contact is hard to pinpoint with an aphanitic unit and suggests that they are the same. The sharp upper contact may represent multiple pulses of dyking at this time. The unit alsodisplays the same alteration minerals and weak pervasive magnetism as the aphanitic unit.

56 64.9 MI.dk.psk Aphanitic diabase dyke (undeformed): same as above.

64.9 74.4 MI.dk.pk Porphyritic and strained mafic intrusion: Dark green with stretched 3 to 12 mm mostly biotite/chl altered hbl phenocrysts within a fine grained matrix. Same as above

74.4 79.55 MI.dk.psk Undeformed meduin grained dark grey with white spots plagioclase porphyrytic mafic dyke: Unit composed of 20% phenocrysts of white 1 to 5 mm plagioclase within a finer grained matrix of interlocking plag and dark mafics now altered to chl, ser and act. Magnetism is strong and the unit is grades from aphanitic on near the contacts to coarser grained and porphyritic in the middle.


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79.55 86.3 MI.dk.pk Porphyritic and strained mafic intrusion: Dark green with stretched 3 to 12 mm mostly biotite/chl altered hbl phenocrysts within a fine grained matrix. Same as above. Lower contact is broken, but likely sharp.

86.3 90.6 MI.dk.psk Undeformed meduin grained dark grey with white spots plagioclase porphyrytic mafic dyke: Similar to the above feldspar porphyritic mafic rock. Unit here is composed of 1-2% large (3 to 15mm) long plagioclase withing a finer grained, yet still medium grained, equigranular matrix of interlocking plag (40%) and dark mafics (60%) now altered to chl, ser and act. Hornblende is clearly a magor constituent of the matrix. Magnetism is strong and the unit is grades from aphanitic on near the contacts to coarser grained and porphyritic in the middle.

90.6 94.8 MT-CO.pl Strained and metamorphosed conglomerate unit: Unit of poorly sorted polylithic deformed clasts from sand sized to 7 cm long (after straining). The unit takes on a mottled appearance with make colours due to various altertion styles (both pre- and after deformation. Unit is generally hard and usually has some pink/red-brown colour to it from FexOy staining and/or kfs altetration.

94.8 126 MT-IV Fine-grained deformed and altered intermediate sandstone/volcaniclastic rock: Unit is banded greeny and red-brownish in colour and deformed. It is hard due to kfs alteration +/- silica alteration. The unit is weakly magnetic and some of the redish colour is from FexOy staining. The red-brown/green alteration is texturally destructive, as kfs alteration tends to be. The lower contact is not a lithological contact, it is the same rock, just a shift in alteration style and the contact is gradational over a few metres. 40 cm altered and deformed mafic dyke at 123 m (70 degrees to c/a).

126 146.59 MT-IV Fine-grained deformed and altered intermediate sandstone/volcaniclastic rock: Same as above, but kfs and act alteration minor. Unit looks like a banded sandstone (which is probably what it is rather than a volcanic rock). Some intense folding is present. Unit here is more of a pale grey-green colour. Unit is not magnetic here. Though the unit is banded, orientation with respect to c/a is variable over short distances.


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146.59 152.74 MT-CO.pl Unit borders on top at 135 to core axis. Begins as feldspar rich, tapers quickly (by 147.60m) to clast poor metaconglomerate. Occasional chlorite clasts surrounded by mudstone. Periodic feldspar and quartz phenos. Biotite rich matrix. Fracture fill carbonates consistant throughout unit. At 150.78m see a porphyritic type texture rich in feldspar phenos, Slightly strained to 130 degrees to core axis. 152.25 sees return to feldspar rich matrix with quartz phenos. Borders at bottom at 125 degrees to core axis. Non magnetic.

152.74 152.95 MI.dk.psk Fine grained post kinematic mafic dyke. High levels of epidote and biotite within matrix. Moderate levels of angular, crystal like quartz and feldspar. Very short. Non magnetic. No straining. Borders at bottom at 45 degrees to core axis.

152.95 155.51 MT-FV.por Coarse grained felsic vocanics with usual feldspar and quartz phenos. Only one or two blue quartz eyes, the rest of quartz is white. Occasional "blob" of epidote and chlorite. Non magnetic. Strained to roughly 130 degrees to core axis. No foliations.

155.51 188.64 MT-CO.pl Unit begins as moderately clast poor, from 168 to roughly 170 sees very clast poor with intense carbonate fracture filling. Returns to previously describe clast poor conditions afterwards, with no carbonate fracture filling. At 176.35m become very clast rich inapredominately epidote matrix. Clast sizes range from <0.5cm to 2 cm. Mineralogy is predominatley epidote, feldspar, chlorite quartz and some mudstone. Starting at 188m begins to be highly strained to 50 degrees to core axis. Core is blocky and broken over lower contact. Non magnetic.

188.64 193.06 MT-FV.por Reutrn to previously described unit of metamorphosed felsic volcanics. A few small sections of very pale pink, almost grey. Material is strained to 50 degrees to core axis, though many factures seen at roughly 100 degrees to core axis. Usual phenos of quartz and feldspar. Increased chlorite and epidote occurances with depth. Appear to be fracture fill occurances. Colour flip flops back and foth from a light pink to a dark grey, biotite rich texture. At ~190, texture changes to porphyritic, with small (<0.5cm) phenos of quartz and feldspar.

193.06 195.59 MT-CO.pl Metamorphosed conglomerate. Mineralogy consists of epidote, chlorite, quartz, feldspar, biotite, and a few fracture fill carbonates. Section is strained moderately to 45 degrees to core axis from 194.28 to 194.66. Outside of this interval, little to no straining, and no common orientation. Becomes quite clast poor, poorly consolidated towards lower contact which borders sharply at 60 degrees to core axis. Non magnetic


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195.59 208.59 MT-FV.por Medium pink k feldspar matrix with abundant blue quartz eyes, white quartz and feldspar phenos. Phenos are oriented 120 degrees to core axis, suggesting some straining. This straining tapers by 201m. From top contact to ~202m, there is an almost sandy colour to the matrix, and apears to be some disseminated mud +/- sandstone. Lower contact is sharp and oriented 120 degrees to core axis. Non magnetic.

208.59 209.33 MI.dk Small medium grained mafic dyke. Section is blocky and broken. High levels of epidote, and biotite. Some fracture fill carbonate. Doesn't appear to be strained. Moderately magnetic.

209.33 231.71 MT-CO.pl.my mylonitized metamorphosed conglomerate. Mineralogy is dominated by fledspar, epidote and biotite. Other minerals include quartz, chlorite, and some fracture fill carbonate. Fabric strained to 70 degrees to core axis. Blocky and broken over several intervals within unit. Large feldspar lense on lower contact, 9cm, 70 deg to CA. Starting at 230, unit becomes quite clast poor. Majority consists of epidote with feldspar halos within what appears to be a highly mafic matrix.

231.71 232.39 MI.dk Light grey/green mafic dyke. High levels of dsm epidote. Biotite is actively being replaced by horneblende. Some secondary migmatite visible from 231.92 to end of unit. Moderately metamorphosed. Weakly magnetic.

232.39 283.16 MT-CO.pl Very large section of metamorphosed conglomerate. Section attop contact, which borders sharply at 110 degrees to core axis, has a few short (<0.5m) of metamorphosed volcanics with phenos of quartz and feldspar. Material is oriented 75 degrees to core axis. Volcanics are absent from 234.72 and on, but shows up again at 238.54 to 238.73. Mineralogy throughout is the usual mish-mash of minerals, including feldspar, quartz, epidote, chlorite, mudstone, sandstone. Small amounts of andesite in a few spots, towards lower contact with a "leopard skin" like texture. Clast size is generally large (1-2cm), though reduced to 0.5cm in small sections. 247.66 to 247.87 is a feldspar lens. Occasional rosy carbonate, along with some fracture fill white carbonate. Lower contact is very gradual, at ~ 120 degrees to core axis. Non magnetic, unmineralized.

283.16 357.98 MT-CO.pl.my Continuation of previously described metamorphosed conglomerate, however unit is now mylonitized. Strained to a 30 degrees throughout. Same mineralogy as previous unit.


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357.98 359.61 MI.dk.por Porphyritic mafic dyke. Fine grained chill margins, increased grain size towards middle of unit. High levels of chlorite. Slicken slides visible in breaks. Moderately strained to 60 degrees to core axis. Some small carbonate veines. Small porhyrys (<0.5cm), of chlorite and epidote. Matrix is predominantly biotite and chlorite. Top and bottom contact borders sharply at 75 degrees to core axis.

359.61 401.36 MT-CO.pl.my Reutrn to mylonitized metaconglomerate. Unit has usual assortment of quartz, feldspar, chlorite, epidote, chert (grey and red) some hematite, and carbonate. Material is strongly to moderately strained to 35 degrees to core axis. Some pink carbonate, though mostly white. At 370.23m some army green calcite and pink carbonate with a "bubbly" texture. Some shphalerite scattered thoughout interval. Small levels of magnetic hematite. Unmineralized.

401.36 401.72 MI.dk.pk Medgrained pre-kinematic mafic dyke. Section is very broken and blocky. Sharp contact on top at 70 degrees to core axis. Highly chlorotized. Some epidote oriented 70 degrees to CA as well. Some horneblende, weak. Some "chunks" of feldspar. Lower contact borders at 70 degrees as well

401.72 423.61 MT-FV.por Metamorphosed porphyritic volcanics. Quartz and feldspar phenos are coarse. Few blue eyes quartz phenos, but show up consistantly. Unit is cut by a small felsic dyke at 404.20 to 404.56. Dyke contains epidote. Unit immediately on either side also contains this epidote and chlorite. White quartz crystals are large and sub angular. Some fracture fill chlorite and epidote is visible throughout unit. Over all red colour. Little to no straining. Upper contact is sharp at 70 degrees to core axis. Unit is non magnetic.

423.61 436.18 MI.dk.pk Pre-kinematic mafic dyke, foliations oriented 40 degrees to the core axis. Upper contact is located in a very blocky and broken section. Lower contact is gradual, oriented at roughly 40 degrees to core axis. Mineralogy consists of strong epidote, moderate horneblend which is replacing biotite. Biotite levels are weak. Slightly chloritic. Tiny amounts of feldspar and quartz. Some small fracture fill carbonates. Some disseminated magnetite. Unit is moderately, to strongly magnetic. Unmineralized.


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436.18 450.7 MT-CO.pl Reutrn to metamorphosed conglomerate. Unit is strained to 40 degrees to core axis, but clast are still visible. Not quite mylonitic. Mineralogy assemblages of quartz, feldspar, epidote, chlorite, some biotite, serpentine. And carbonate. Clast intensity is generally rich, though section from 447 to 448m is clast poor, dominated by epidote veining. Occasional mudstone is visible. Some patchy magnetism, though overall, unit is non mineralized. Some slicken slides visible on breaks. Unmineralized.

450.7 457.76 MT-CO.pl.my Highly strained and metamorphosed conglomerat with clasts of various sizes and various lithologies. Many clasts are gravel sized with a few larger..Clast supported and with a matrix of finer grained material. Most clasts have been highly sheared and altered. Foliation @~42deg t.c.a. Chlorite, epidote and minor calcite in fractures (Ct>Ep) Strong potassic alteration beginning at 450.98m until 454.48m. Unit has patchy, weak magnetizm. L.c is irregular, @~37deg t.c.a. At 453.56m, unit is cut by a small, re-lithofied fault containing host rock materal(post-kin to the host rock fabric) At 456.40m unit is cut by a 37cm mafic intrusive with hematite and cholrite in fractures as well as localized potassic alteration (possibly due to remobilization of elements due to fluid flow). Does not have strong foliation.

457.76 468.04 FI.dk Dark gray to red unit. Strong chlorite alteration at 460.25m. Hematization at 461.70m. Weak to moderate patchy magnetism. Irregular upper and lower contacts. Localized potassium alteration. Contains trace calcite fractures, some hematization on fractures, chlorite, epidote, hornblende.

468.04 471.96 MT-CO.pl.my return to previous moderately mylonitized sheered and altered conglomerate. Upper contact is irregular, lower contact is broken and irregular . Containing some calcite veining. Contains Post-kinematic mafic dyke intruding at 469.74 - 470m with phenos ~0.05cm in size with minor hematite veinlet and more plag-rich down hole. Sharp upper and lower contacts ~46deg t.c.a.

471.96 480.22 MI.dk.psk Green unit strongly deformed and veined with chlorite and epidote. Non foliated. Broken upper contact and sharp lower contact ~50 deg t.c.a. weakly magnetic.

480.22 484.29 MT-CO.pl.my Multi-colored, highly metamorphosed conglomerate. Clasts are varoius lithologies and have been highly deformed and altered. Hard to determine the clast lithologies. Dominant foliation @~52deg t.c.a. Minor fracturing and shear zones throughout. Unit contains various chlorite and epidote veining, as well as calcite and epidote in fractures. Unit is non-magnetic. L.c is sharp, @~53deg t.c.a.


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484.29 486 MI.dk.sk Black to dark gray-green unit. With sharp upper contact ~54 deg t.c.a. and moderately graded lower contact. Non-magnetic. Contains some xenolith (k-feld + others) action from the adjacent conglomerate unit.

486 487.66 MT-CO.pl Return to previous conglomerate. Weak patchy magnetism. Contains feldspars, epidote, chlorite all highly metamorphosed. Broken messy upper and lower contacts.

487.66 488.57 MI.dk.psk Dark gray-black mafic dyke exhibiting some small veinlets containing epidote. Some hematization in fractures. Lower contact is gradational. Some bands of next unit alternating with dyke. Non-magnetic.

488.57 490.8 FI.por.fp Red aphanitic highly potassic unit. Exhibits veins containing epidote, calcite, quartz, sericite with a general orientation of ~40 deg t.c.a. Contains phenos ~0.2 - 0.4 cm in diameter.

490.8 491.68 MI.dk.sk Dark gray-black mafic dyke with sharp slightly irregular upper and lower contacts making angles of ~65 deg and ~35deg t.c.a. respectively. Some inclusions of neighboring unit. Approx. 5% phenos plag ~0.1 - 0.3 cm.

491.68 492.38 FI.por.fp Return to felsic unit. Upper and lower contacts are roughly gradational over 4 and 6 cm, respectively. Upper contacti is heavily veined with adjacent dyke. Contains some vienlets with epidote.

492.38 513.85 FI.por.fp return to red felsic/potassic unit. Unit fades near the center to a lighter pink and switches back to a deeper red downhole. Contains phenos( 0.1- 0.3 cm) in patches. Becomes very porphyritic (20% phenos) at end of unit. Highly stockwork veined, viens contain chlorite, epidote, +/- sericite, +/- quartz. Some fractures containing calcite.

513.85 515.08 MI.dk.sk Dark gray/green to black. Moderate to heavily viened. Veins contain chlorite, epidote, some fracture-fill from adjacent felsic unit. Contains a lens (27cm wide) of said felsic unit with irregular contacts.


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515.08 541.75 MT-CO.pl Return to metamorphosed conglomerate. Moderatly foliated. Unit is fractured (shear zone) and contains a minor fault with a 4cm offset at 524.39m depth. Contains a mafic post-kinematic dyke at 527.55 - 528.10 m depth. Moderate veining containing chlorite, calcite. Contains a few roundedclasts in places. Unit becomes increasingly mylonitic with depth. Unit is vuggy in places. Calcite in fractures. Lower contact of the conglomerate is in contact with a 23cm foliated pre-kin. Mafic dyke.L.c of the conglomerate is irregular and sharp, @~40deg t.c.a. L.c of the dyke is sharp, @~44deg t.c.a. Unis is non-magnetic.

541.75 543.53 FI.por.fp Dark red, highly altered (hematitie alteration) Feldspar Porphyry. Contains ~5-7% phenos of plag with hematite rims, and ~5% phenos of k-feld. Contains epidote and calcite in fractures. Unit is moderatly magnetic and weakly foliated @~30deg. L.c of unit is sharp, @~40deg t.c.a.

543.53 544.87 MI.dk.por Dark grey-black, very porphyritic mafic dyke containing weak to moderate foliation @~40deg t.c.a. ~20-25% phenos of plag ranging from >1mm-3mm in size. Contains calcite and epidote in fractures. Unit is non-magnetic. L.c is sharp, @~27deg t.c.a.

544.87 550.7 FI.por.fp Dark red, highly altered (hematitie alteration) Feldspar Porphyry. Contains ~15% phenos of plag with hematite rims, and ~5-10% sheared phenos of k-feld. Contains epidote in fractures, as well as magnetite and quartz veinlets. Unit is moderatly magnetic and weakly to moderatly foliated @~34deg t.c.a. At 545.27m there is a 2cm smoky quartz vein. At 546.05cm there is a 42cm porphyritic mafic dyke containing weak to moderate foliation @~40ged t.c.a. 10-15% phenos of plag ranging from >1mm-2mm in size. U.c and L.c are sharp, @~45deg t.c.a. L.c is sharp, @~30deg t.c.a.

550.7 551.48 MI.dk.pk Dark grey-black, mafic dyke containing weak to moderate foliation @~38deg t.c.a. . Contains calcite and epidote in fractures. Contains localized bands of hematite alteration at 550.85m Unit is moderatly magnetic. L.c is sharp, @~30deg t.c.a.


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551.48 621.8 MT-IV Black-brown, highly altered intermediate volcanics. Chlorite veining present throughout, as well as epidote and calcite in fractures. Unit has patches of chlorite alteration throughout, as well as a more mafic composition locally. Veins of epidote and chlorite increas with depth. Trace amounts of pink carbonate in fractures (>1%, possibly ankerite) Unit has pervasive, moderate to strong magnetism. Unit is locally vuggy. Unit increases in magnetite bands and calcite with an increase in depth. Foliation @~40deg t.c.a. At 565.77m, unit is cut by a highly altered mafic dyke with ~10% calcite in fractures and ~10% epidote. U.c @~45deg t.c.a. L.c @~32deg t.c.a. Nonmagnetic. At 569.85m there is a 5cm mafic dyke. U.c is broken, L.c @~45deg tc.a. Nonmagnetic At 547.75, unit is cut by a 87cm post-kin. mafic dyke with irregular U.c and L.c. Nonmagnetic At 585.10, unit is cut by a 50cm, post-kin felsic dike with disseminated pyrite (~1-2%). Contacts are sharp, with U.C broken and L.c @~45deg t.c.a. At 588.77m, unit is cut by 3cm felsic dyke. Uc and L.c are sharp, at ~45deg t.c.a. At 599.68 unit is cut by a 40cm post-kin mafic dyke with sharp contacts. U.c is irregular, @~45deg, L.c @~45deg t.c.a. At 568.61m, unit has a 133cm interval with a mafic dyke like composition, but is strongly magnetic and lacks a sharp U.c or L.c. Unit is mineralized from 571.94m to 573.20m with a high of 1110cps and an avergae of 390cps. Unit is mineralized from 578.78m to 579.12m with a high of 860cps and an average of 374cps. Unit is mineralized from 593.58m to 494.06m with a high of 410cps and an average of 280cps. Unit is mineralized from 595.92m to 601m with a high of 710cps and an average of 258cps. Unit is mineralizef from 602.10 to 603.25m with a high of 620cps and an average of 248cps. Unit is mineralized from 605.50 to 606.02 with a high of 430cps and an average of 310cps. Lower contact of unit is sharp, @~40deg t.c.a.

621.8 623.37 MI.dk.por Dark grey-black, porphyritic mafic dyke, ~10-12% plag phenos up to 6mm in diameter. Weakly foliated, @~36deg t.c.a. Unit contains calcite and epidote in fractures, which often cut across the foliation. Unit contains disseminated pyrite. Unit is nonmagnetic. L.c is sharp and slightly irregular, @~42deg t.c.a.

623.37 629.49 FI.por.fp Reddish-brown, highly altered feldspar porphyry with ~5-7% phenos. Possibly potassic alteration, with hematite in fractures. Unit is weakly foliated, @~40deg t.c.a. A 1cm quartz vein at 625.92. Unit is cut by a 55cm post-kin mafic dyke with sharp, long irregular contacts @~80deg t.c.a.


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629.49 632.37 MI.dk.por Dark grey-black, porphyritic mafic dyke, ~10-12% plag phenos up to 6mm in diameter. Weakly foliated, @~36deg t.c.a. Unit contains calcite and epidote in fractures, which often cut across the foliation. Unit contains disseminated pyrite. Unit is nonmagnetic. L.c is sharp and slightly irregular, @~42deg t.c.a. Unit contains ~3-5% dissaminated pyrrhotite. At 630.45m, unit is cut by a 55cm lense of intermediate volcanics. Slight potassic alteration and minor calcite in fractures. U.c and L.c are sharp, @~45deg t.c.a.

632.37 634 MT-IV ntermediate volcanics. Slight potassic alteration and minor calcite in fractures. U.c is sharp, @~45deg t.c.a. Unit has minor chlorite and epidote in veins. Moderatly magnetic and weakly foliated. Small, local ptches of a more felsic composition. L.c is not present. End of Hole.


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0 0.3 OVBD overburden

0.3 17.34 MT-IV Dark grey-black, porphyritic metamorphosed intermediate volcanic. Fine grained sandy matrix. Sheared brown-tan phenos of possible arenite or biotite or horneblende alteration. Weak to moderate foliation @~ 54deg t.c.a. Hematite present in fractures as well as low amounts of calcite and epidote. Unit becomes less porphyritic with an increase in depth. Minor patchy hematite halos present througout. Unit is non-magnetic throughout. At 8.3m unit is highly altered, possibly potassic alteration until 8.52m and again from 11.24m to 11.40m. Unit has chlorite veining and alteration from 11.71m to 12.40m. Unit is cut by a mafic dyke with strong calcite veining and chlorite alteration from 14.35m to 14.66m. L.c is sharp and slightly irregular, @~55deg t.c.a. Also, unit has a low amount of interfingering diklets. Unit is cut from 17m to 17.28m by another highly altered mafic dyke with calcite veining and chlorite alteration. L.c is @~ 63deg t.c.a. L.c and U.c of unit are not present.

17.34 20.87 MT-CO.pl Dark grey-brown matrix with multi-colored, highly strained clasts of varrying composition. Highly metamorphosed conglomerate with strong foliation @~60deg t.c.a. Contains sub-angluar to sub-rounded clasts of ankerite, jasper, arkose sandstone, chlotire +/- biotite +/- epidote +/- mudstone. Unit contains chlorite veining. Calcite and epidote present in fractures. Minor patchy hematite halos present througout. Unit has patchy, moderate magnetism. L.c is ~60deg t.c.a.

20.87 23.02 MI.dk.pk Light grey, moderat to highly foliated per-kinematic mafic dyke with small bands of intermediate volcanic throughout and low amounts of highly sheared plag clasts. Highly altered feldspars(possibly plag) with 25cm of talc from 21.40m to 21.65m. Foliation @~55deg t.c.a. Slight calcite present in fractures. Unit has patchy, weak magnetism.

23.02 31.88 MT-IV Dark grey-black, metamorphosed intermediate volcanic. Fine grained sandy matrix. Moderate foliation @~ 60deg t.c.a. Hematite present in fractures as well as low amounts of calcite and epidote. Minor patchy hematite halos present througout. Unit is non-magnetic. Unit is cut by a 9cm mafic dyke at 20.70m. U.c is sharp, @~60deg t.c.a. L.c is sharp, @~67deg t.c.a.


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31.88 55.05 MT-CO.pl.my Polylithic meta-conglomerate, mostly mylonitic. The fragments are a lot various ; Jasperite cherts, cherts, Quartz, Felspars (Kfp and Pg), disseminated carbonate mineralisations. There are two majors alteration minerals, Epidote is found in replacement into the fragments and also into the rhyolitic matrix of the conglomerate, Hematite is just present in replacement in the fragments and never found in the matrix. Local brownish alteration mineral in the rhyolitic matrix (maybe altered epidote). Carbonates, such as calcite are mostly into late small fractures. The unit is locally cut by small mafic intervals (<30cm thick). The magnetism is mostly inexistant but is sometimes strong on several disseminated spots where there are magnetite mineralisations. Mylonitisation is pretty intense almost all over the unit and the foliation is regular and around 60° to the CA.

55.05 56.8 MI.dk.sk Aphanitic to fine grained syn kinematic mafic dike, weakly foliated, the foliation is expressed by Ep±Ct rich bands at the margins, there are also some jasperite rich bands. Both of the contacts are chilled margins. The unit is nonmagnetic, foliation is still 60° to the CA.

56.8 65.58 MT-CO.pl.my Polylithic meta-conglomerate, mostly mylonitic. The fragments are a lot various ; Jasperite cherts, cherts, Quartz, Felspars (Kfp and Pg), disseminated carbonate mineralisations. There are two majors alteration minerals, Epidote is found in replacement into the fragments and also into the rhyolitic matrix of the conglomerate, Hematite is just present in replacement in the fragments and never found in the matrix. Local brownish alteration mineral in the rhyolitic matrix (maybe altered epidote). Carbonates, such as calcite are mostly into late small fractures. The unit is locally cut by small mafic intervals (<30cm thick). The magnetism is mostly inexistant but is sometimes strong on several disseminated spots where there are magnetite mineralisations. Mylonitisation is pretty intense almost all over the unit and the foliation is regular and around 60° to the CA.

65.58 68.25 MI.dk.sk Dark grey-black fine grained syn-kinematic mafic dike. Foliation is weak. Epidote and chlorite bands (ep>ct) follow the foliation @~45deg t.c.a. Bands of hematite present which cut the foliation @~63deg t.c.a. Hematite also present in fractures. Last 17cm of dyke is more chlorite rich. U.c is sharp @~56deg t.c.a and L.c is irregular, @~56deg t.c.a. Unit has pervasive, moderate magnetism.


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68.25 84 MT-CO.pl.my Fine to coarse grained dark grey-brown matrix with multi-colored, highly strained clasts of varrying composition. Highly metamorphosed conglomerate with strong foliation @~58deg t.c.a. Contains sub-angluar to sub-rounded clasts of ankerite, jasper, arkose sandstone, qtz, chlotire +/- biotite +/- epidote +/- mudstone. Unit contains chlorite veining. Calcite(1%)and epidote(7%) present in fractures. Unit has patchy, moderate magnetism. Unit becomes very strongly foliated beginning at 77.03m Unit has high potassic alteration beginning at 77.07m until 77.77m. Unit is cut by various small mafic dikes ranging from 1cm to 5cm throughout the unit. At 68.52m unit is cut by a 23cm syn-kin mafic dyke with chlorite alteration and epidote veining. Unit is cut at 75.55m by a 26cm epidote and chlorite rich post-kin mafic dike. At 79.88m unit is cut by a 73cm pre-kin mafic dyke with blebbs of chlorite as well as epidote and chlorite veining. Dyke has strong foliation @~58deg t.c.a. L.c @~ 58deg t.c.a. At 80.83m unit is cut by a 46cm per-kin mafic dyke with strong foliation and epidote veining. L.c @~58deg t.c.a. L.c of the unit is broke and thus not present

84 111.7 MT-IV.my Grey-black, medium to fine grained matrix containig biotite +/- horneblende. Quatrz +/- plag also present. Calcite in fractures. Intermediate Volcanic. Highly strained with foliation @~56deg t.c.a. Hematite banding and fracture fills beginning at 85.06m. Slight hematite alteration beginning at 85.06m until 85.73 with potassic alteration beginning at 85.73 until 87.89m. Unit increases in epidote veiningwith depth, starting at ~101.64m At 105.92m unit beings to become more altered (sodic alteration maybe?). 8cm quartz vein present at 109.34m Unit is moderatly magnetic. Unit is cut at 93.70m by a 24cm felsic dyke containint biotite, caclite, plag +/- hornblende with trace amountsof blebby epidote. L.c@~68deg t.c.a. Unit is cut at 94.35m by a 37cm feslic dyke containint biotite, calcite, plag +/- hornblende. L.c is @~66deg t.c.a. Unit is cut at 96.48 by an 11cm felsic dyke. L.c @~68deg t.c.a. At 97.10 unit is cut by an 87cm feslic dyke containint biotite, calcite, plag +/- hornblende. U.c and L.c is sharp and irregular. At 98.39m unit is cut by a 23cm long feslic dyke containint biotite, calcite, plag +/- hornblende with sharp and irregular contacts. Unit is cut at 110.90m by a50cm feslic dyke containint biotite, calcite, plag +/- hornblende. Contacts are sharp and irregular. Unit is cut again at 111.18m by a ___cm long feslic dyke containint biotite, calcite, plag +/- hornblende. Uc is irregular.

111.7 113.6 MI.dk Fine grained syn to late kinematic melagabbro dike, weakly foliated, nonmagnetic. Locally cut by thin carbonate filled fractures and by one 1cm thick felsic volcanics vein. Presence of one small (~5cm thick) enclave of felsic materials. Chilled margins.


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113.6 194 MT-IV Aphanitic to medium grained intermediate volcanics, high strained to mylonitic, strongly to moderately foliated. Strongly magnetic as there are some eyed style magnetite minerals and also disseminated magnetite. Some local carbonate occurences into the foliation as calcite bands. Very weak patchy hematization, local epidote mineralisations, mainly in the more felsics parts of the unit. Some pretty wide (~4cm) bands shows hornblende replacement of pyroxenes. The magnetite is often associated with sulfides mineralisations. The sulfides are mostly really fine-grained pyrite. The accessories minerals are Kfp, high strained plagioclases, carbonates (including calcite), chlorite, epidote, local presence of garnets, and Pyroxenes in the more mafic parts of the unit. Between 124.5 and 129.5m, the unit alternates between thick felsics volcanics intervals (~60cm) and thinner mafic intervals (~15cm). Between 157.50 and ~188m, the unit is almost 75% mafic materials, always with eyed style magnetite associated with sulfides (Py ± Po).

194 233.26 MT-IV Same unit as previous but with several differences ; This part of the unit is U-mineralised as follows ; 194 - 202m => max 639cps on a small spot, the average value is around 220cps. 202 - 212m => max 3000cps with 9 spots > 1000cps, the average value is around 850cps. Compared to the upper part of the unit, the major difference in the mineralised interval is that the carbonates mineralisations are important and found as powdered disseminated mineralisations and in fracture filling. The disseminated carbonates are here associated with hornblende. The hematization is patchy and very weak. The magnetite are still present in eyed style mineralisations but also in fractures filling parallel toi the foliation. The most mineralised part of the zone shows a purple cherty-like alteration.

233.26 234.28 MI.dk.sk Mafic syn-kinematic dike, moderately foliated, sharp contacts, pseudo perpendiculars to the CA, the foliation is around 70° to the CA. Unit is nonmagnetic, locally cut by small carbonate filled fractures.

234.28 264.9 MT-IV Same MT-IV as before the previous dike, mineralised as follows ; 234.28 – 243.33 => avg 478cps ; max 2295cps 243.33 – 259.56 => Background with 2 spots mineralized at 428 and 569cps. 66m thick mineralized zone so far, more mineralization expected tomorrow.


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264.9 280.82 FI.por.fp Coarsely porphyritic felsic intrusive, felspar-quartz porphyry, both margins are felspar porphyritic mafic dikes with contacts pseudoperpendicular to the CA, those mafic dike are progressively porphyritic approaching the felsic intrusive, and more aphanitic mafic approching the host MT-IV. Dominant plagioclases cristals, most of those plagioclases are rounded and zoned, sometimes with a Pg core circled by Bt, sometimes the Pg cristalizes around a biotitic core. Most of the cristals are oriented but some of them crosses the foliation, as it was cristalized after deformation. The micaceous foliation (Bt ± Ct) hosts a lot of fine grained sulfides (Pyrite). In the bottom part of the unit, there are some K-spars, sometimes cristalized around plagioclases, and sometimes with a perthitic facies. The unit is nonmagnetic. There are also some disseminated calcite mineralisations into the matrix. The mafic margins are nonmagnetic, hosts green Hb, disseminated carbonates and felspars porphyritics.

280.82 300.15 MT-IV Continuation of the previous mineralised MT-IV, with small differences ; moderate pervasive hematization, locally cut by a syn kinematic mafic dike between 284.46 and 285m, both contacts of that dike are pseudoperpendiculars to the CA, and parallel to the foliation in the dike. The unit is mineralised as follows ; 280.82 - 286.50m => avg 503cps ; max 1653cps, with 5 spots > 1000cps. 286.50 - 300.15m => avg 324cps ; max 900cps, with 11 spots > 500cps.

300.15 301.62 MI.dk.sk Very fine grained, weakly foliated syn-kinematic mafic dike, with rare disseminated felspar porphyroclasts, traces of carbonates and fine grained pyrite. The contacts are parallel to the foliation in the host MT-IV. Unit is nonmagnetic. The dike is barren.

301.62 347.05 MT-IV Continuation of the previous mineralised MT-IV, with small differences ; weak patchy hematization, becoming less important to the bottom of the unit, the unit is becoming less carbonate rich too. Locally cut by 3 mafic intrusives, (307.86 - 308.18m => pseudoperpendiculars sharp contacts ; 316.55 - 317.13m => sharp contacts around 65° to the CA ; 319.66 - 320.50m => 45° bottom contact). U-mineralisation stops at 304m with a spot 467cps high.

347.05 348.37 MI.dk.psk Fine grained unfoliated post-kinematic mafic dike, with a sharp top contact perpendicular to the core angle. Fine grained disseminated pyrite mineralisation and rare felspar porphyritics.

348.37 353 MT-IV Continuity of the previous MT-IV.


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0 8.27 OVBD Overburden.

8.27 20.13 MI.dk.por Pale blue-grey to grey-green-black, Fine-grained to locally coarse-grained. Ct-altered, hb-porphyritic mafic intrusive. Hb phenos are dark green-black 0.2cm-2cm anhedral, bulbous grains that have been altered by ct. Unit is moderately foliated and ct-rich. The ct occurrence is in swath-like bands throughout the unit also occuring in web-textures giving the unit a pseudo-breciation texture. Local coarse-grained hb phenos display a elliptical, elongated shape which is coherent with foliation. Minor clay (possibly sericite) alteration b/w 15.37m-16.10m. Hb-phenos in this altered region appear larger and show a more stretched, elliptical shape. Lower contact sharp and shallow at an angle of 20 degrees to C.A.

20.13 31.59 FI.dk.por Pink-purple, green-grey-pink, weakly foliated, fine-grained to locally aphanitic, porphyritic felsic intrusive. Unit has areas of more mafic material patchy throughout. Weak foliation is discontinuous and unmeasurableThese areas contain swath-like bands of more mafic material containing mineralogy such as ct+bt. Unit is non-magnetic. Unit is representative of the felsic intrusive containing blue qz eyes but the unit itself has no visable qz w/n in it. Upper contact is sharp and at an angle of 20 degrees to C.A. Lower contact is gradational and indistinct.

31.59 50.35 MI.dk White-black, fine-grained to locally coarse-grained, unfoliated, late to post-kinematic mafic dike (possible mafic sill?). Unit is carbonate-rich. Carbonate occurrence is in small anastamosing veinlets flooding the unit throughout. These carbonate-rich veinlets give the unit a pseudo-brecciation/web-texture. In carbonate-poor areas of the unit the phenocrysts are more abundant and lie w/n a biege coloured, leucoxene-rich matrix. The phenocrysts are coarse-grained, black, bulbous, anhedral grains, possibly bt-replacement of pre-existing px phenocrysts. The leucoxene-bt-rich portions of the unit give a leopard texture to the unit. Unit has moderate-patchy magnetism. Upper contact is gradational and unmeasureable. Lower contact is at an angle of 60 degrees to the C.A.

50.35 52.05 MT-IV Pink-red-purple to green-red, fine-grained, ct-rich, metamorphosed intermediate volcanics. Unit has pervasive to patchy ct replacement throughout. The mineralogy is too fine-grained to discern. Upper contact is sharp and at an angle of 60 degrees to C.A. Lower contact is sharp and hematized with an angle of 60 degrees with C.A.


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52.05 62.17 MI.dk Continuation of previous mafic dike (31.59m-50.35m). Unfoliated, black and white coloured, bimodal grain-size. Unit is quite the same as the previous mafic interval. Carbonate is intensely pervasive throughout with small patchs of leopard texturedareas containing bt-rich phenos w/n a lecoxene matrix. Moderately magnetics patchy throughout. Upper contact is sharp at an angle of 60 degrees to C.A. Lower contact is sharp and hematized at an angle of 40 degrees to C.A.

62.17 64.4 MT-IV Same as previous intermediate meta-volcanics (50.35m-52.45m). Pink-purple, ct-rich, fine-grained intermediate meta-volcanics. Unit is quite fine-grained making mineralogy hard to discern. Foliation is weak and discontinuous making measurementsdificult. Weak pathcy magnetism. Upper contact is sharp at an angle of 40 degrees to C.A. Lower contact is strongly chloritized and sharp at an angle of 75 degrees to C.A.

64.4 79.7 MT-IV Continuation of previous mafic unit (52.05m-62.17m). Unfoliated, black and white coloured, bimodal grain-size. Unit is quite the same as the previous mafic interval. Carbonate is not as intensley pervasive in this particualr unit. Leopard textured areas containing bt-rich phenos w/n a lecoxene matrix are more prominent in this unit. Moderately magnetics patchy throughout. Unit contains more intermediate portions that are less than 20 cm in length. Upper contact is sharp at an angle of 75 degrees. Lower contact is gradational and hard to discern. U-mineralization present from 77.00m-78.73 with a max: 603cps avg: 295cps Unit is possibly intermediate to mafic meta-volcanics.

79.7 97.9 MT-IV Pink-purple, grey-purple, fine-grained, moderately foliated, intermediate meta-volcanics. Unit is rich in felsic material that is relatively hematitic and potassically altered. There are patchy intervals of ct richs swaths throughout. The unit is phenocryst poor. Dominant mineralogy is mostly alteration mineralogy such as ct+bt+hm. Hematite occurs in patchy bands throughout which follow dominant foliation which is defined by the banding of micacious mineralogy. Hm also occurs around the swaths of ct-rich intervals. Unit is dominantly non-magnetic with small locally weak magnetism. Cb is present throughout along fractures as well as peppered finer grains within the matrix material. Upper contact is sharp and hematized with an angle of 50 degrees to C.A. Lower contact is sharp and chilled at an angle of 70 degrees to C.A.


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97.9 98.13 MI.dk.sk Green-black, chloritic, fine-grained, syn-kinematic mafic dike. Unit is ct-rich. Ct occurs along folaition as well as w/n web textured micro-veinlets. Unit is fine-grained thus making discerning mineralogy difficult possibly hb replacing px within the matrix of the unit. Foliation is weak but dominantly defined by fine bands of micacious mineralogy such as bt+ct. Upper contact is sharp and at an angle of 70 degrees. Unit is non-magnetic. Lower contact is also sharp but broken and unmeasurable.

98.13 116.73 MT-IV Continuation of the previous MT-IV (79.7m-97.9m). Pink-purple, grey-purple, fine-grained, moderately foliated, intermediate meta-volcanics. Unit is rich in felsic material that is relatively hematitic and potassically altered. There are patchy intervals of ct richs swaths throughout. The unit is phenocryst poor. Dominant mineralogy is mostly alteration mineralogy such as ct+bt+hm. Hematite occurs in patchy bands throughout which follow dominant foliation which is defined by the banding of micacious mineralogy. Hm also occurs around the swaths of ct-rich intervals. Unit is dominantly non-magnetic with small locally weak magnetism. Cb is present throughout along fractures as well as peppered finer grains within the matrix material. Upper contact is broken and unmeasurable. Lower contact is sharp and hematized at an angle of 70 degrees to C.A.

116.73 141.07 MT-FV.por Pink-grey to purple, moderately hematized, well foliated, fine-grained to coarse-grained, metamorphosed feldspar porphyritic volcanics. Porphyroclasts are dominantly sub-rounded, pink-red, 0.2cm-1.5cm regrown, k-spar grains.There are also earlier, elliptical to linearly strained blue qz eyes and pg porphyroclasts of the same occurrence that follow the dominant fabric w/n the unit. Strain is varied throughout the unit. This strain variation is reflected in the shape and size of the porphyroclasts of pg and k-spar. The unit decreases in grain-size along with the diminishing of foliation downhole and ressembles an aggregate of grains similar to a rock of sedimentary origin. Patchy magnetism. Upper contact is sharp at an angle of 70 degrees to C.A. Lower contact with the following intermediate volcanic unit is gradational and unmeasurable. Very poor core recovery due to brittle faulting b/w 121.00m-134.10m


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141.07 150.21 MT-IV Grey-purple to pink green, chlorite-rich, intermediate to felsic meta-volcanics. Slightly ressembles the previous felsic porphyritic unit with finer grains of elliptical pg and more chlorite present in the matrix. Some of the fgr pg suffers from hematitic replacement. Ct also occurs in swathing bands that are surrounded by haloes of hematitic alteration which are patchy throughout the unit. The dominant composition is intermediate with more felsic intervals intermittent throughout the unit. Magnetism is weak and patchy. Upper contact is gradational with the previous felsic unit. Lower contact is truncated by a small <15cm mafic dike an is approx. at an angle of 50 degrees to C.A.

150.21 153.81 MT-IV.por.fp Same as previous porphyritic felsic meta-volcanic unit (116.07m-141.07m). Unit has more pervasive hematitic alteration giving it a more reddish pink bleached colour. Well foliated, med-grained to coarse-grained, metamorphosed feldspar porphyritic volcanics. Porphyroclasts are dominantly sub-rounded, pink-red, 0.4cm-1.5cm regrown, k-spar grains. There are also earlier, elliptical to linearly strained blue qz eyes and pg porphyroclasts of the same occurrence that follow the dominant fabric w/n the unit. Strain is varied throughout the unit. This strain variation is reflected in the shape and size of the porphyroclasts of pg and k-spar. Patchy magnetism. Upper contact isat an angle of 50 degrees to C.A. Lower contact is brittle fault gauge that has been lithified with the mafic dike below and makes an angle of 60 degrees with C.A. Very poor core recovery due to brittle faulting b/w 151.00m-153.81m

153.81 155.2 MI.dk.sk Chloritic, non-magnetic, well foliated, pre-syn-kinematic mafic dike. Unit has a ct-rich matrix with fgr phenos of highly sericitized and strained anhedral pg. Moderate ct w/n fractures throughout the unit. Upper contact is at 60 degrees to C.A. Lower contact is broken and lost.

155.2 157.18 MT-IV.por.fp Same as previous porphyritic felsic meta-volcanic unit (150.21m-153.21m). Pervasive hematitic alteration gives the unit a reddish pink bleached colour. Well foliated, med-grained to coarse-grained, metamorphosed feldspar porphyritic volcanics. Porphyroclasts are dominantly sub-rounded, pink-red, 0.4cm-1.5cm regrown, k-spar grains. There are also earlier, elliptical to linearly strained blue qz eyes and pg porphyroclasts of the same occurrence that follow the dominant fabric w/n the unit. Strain is varied throughout the unit. This strain variation is reflected in the shape and size of the porphyroclasts of pg and k-spar. Patchy magnetism. Upper and lower contacts are both broken and un recognizable. 30 cm of core missing fr


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157.18 158.75 MI.dk.sk Fine grained, syn-kin mafic dyke.Chilled contact. L.c @~ 50deg t.c.a. U.c is not visable. Foliation at 518.2m @70deg.

158.75 162.04 MT-IV.por.fp continuation of previous prorphitic felsic metavolcanic.. First 60cm are intercepted by 3 mafic intervals. Respectivly 17, 5 and 10cm thick. Foliation@70deg t.c.a. L.c @74deg t.c.a. strained blue quatrz eyes.

162.05 163.35 MI.dk.sk continuation of previous syn-kin mafic dyke. L.c @40deg t.c.a. Moderately patchy hematization.

163.35 169.9 MT-IV.por.fp continuation of previous prophyritic felsic metavolcanic. Strong pervasive hemitaziation, decreases downhole.

169.9 175.37 MI.dk.por Pre to syn-kin mafic dyke. Strongly foliated.Highly porphyritic in the first meter, less in the last meter. Minor Carbonate veins. Horneblende. L.c is pseudo perpendicularl t.c.a and gradationa @86deg. From 174.3 to L.c we have 3 syn-Mt.IV intrusions. Strain is variable throughout the unit. More chloritic near the MT.IV intervals.

175.37 179.7 MT-IV MT.IV, intersected by syn-mafic intervals. A lot of fractured filled epidote and horneblends phenos. Epidote appears to be highly altered enclaves of the dyke. Chlorite and epidote occurance is in swath-like ribbons throughout. Traces of fracture filled and patchy hemitaziation. Hemitaziation is stronger near the epidote veins.

179.7 181.6 MI.dk.por Porphyritic mafic dyke. Moderatly to strongly foliated. Horneblende prohpyritic. Carbonate veins. Sharp lower and upper contacts. Locally chloritic, mostly in the prophyritic intervals. L.c @~74deg t.c.a.

181.6 184.6 MT-IV continuation of previous MT.IV. L.c is not visable, around 184.6m.

184.6 188.27 MI.dk.por continuation of the previous horneblende porphyritic mafic intrustive. No more carbonates. Weak local magnetism. Foliation @65deg t.c.a. Contacts are really diffused and hard to define precisely.

188.27 191 MT-IV continuation of the previous MT.IV. More mafic materials. A few epidote and chlorite veins in the first 85cm of the unit. No more veins after this point. Traces of fracture filled and dissaminated hematite. Highly strained feldspar porphyritics. High magnetism.


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191 199.83 MI.dk.por continuation of the previous horneblende porphyritic mafic intrustive. Moderatly to strongly foliated. pre-kin. Intercepted by 2 syn-kin felsic intervals. Traces of weak patchy magnetism.

199.83 201.76 MI.dk.psk ~fine grained, post-kin mafic dyke. Unfoliated. Plag phenos peppered throughout,~8%. Minor dissimenated pyrite. Small chlorite and carbonate in fractures. Sharp contacts. U.c @~60deg t.c.a. L.c is a chilled zone.

201.76 203.76 MI.dk.por continuation of the previous horneblende porphyritic mafic intrusive.

203.76 210.52 MT-CO.pl Pink-red to grey-yellow-brown-green, cb-rich, fine grained to locally clastic, weakly foliated, moderately hematized, polylithic meta-conglomerate. Unit has a weak foliation that is discontinuous. On a whole the unit is clast-poor. Carbonate occurs within the unit along small brittle micro-fractures throughout. Ct-occurs local to the majority of the areas where the carbonate-filled micro fractures occur. Clasts that are visible appear to be ep-rich. Relict lithology of clasts hard to discern due to intense alteration overprinting w/n the unit. Unit is highly fractured and brecciated locally. Upper contact is relatively sharp and hematitic at an angle of 50 degreesC.A.. Lower contact is sharp and hematized at an angle of 75 degrees to C.A.

210.52 214.55 MI.dk Dark green-black, locally hematized and brecciated, mafic dike. Unit is highly altered making deformation textures difficult to see. Unit is strongly magnetic. Moderate carbonate-fill microfractures locally throughout. Serpentine occurs along a small fracture (2cm wide) b/w 214.05m-214.07m. Upper contact is sharp and at an angle of 75 degrees to C.A. Lower contact is at an angle of 60 degrees to C.A.

214.55 240.34 MT-CO.pl Beige-brown to green grey, moderately strained, meta-conglomerate. Unit is quite clast-rich which vary from 1cm-7cm angular to sub rounded clasts. Pervasively chloritized and epidotized in areas. Clasts of red japeroid and mudstone are present and are angular to subrounded in shape and vary in size and occurrence downhole. Unit is relatively cb-rich which occurs along small micro-fractures and w/n small 2cm wide vugs.Minor fine-grained subhedral garnet present. Foliation is defined by thick ep+ct bands as well as banding of micacious mineralogy. Non-magnetic. At an angle of 60 degrees to C.A. Lower contact is gradational with nest unit and unmeasurable.


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240.34 243.63 MT-CO.pl.my Red-brown, highly strained and metamorphosed mylonitic conglomerate.Moderate to strong hematite (or potassic?) alteration pervasive throughout the unit. Last 20cm of unit is a pre-kin mafic dyke with foliation @~60deg t.c.a and Uc and L.c at@60deg t.c.a.

243.63 249.97 MT-IV.my Dark brown-red, intermediat volcanics. Unit is locally cut by 3 pre-kin mafic dykes between 244.28 and 246.42m, each with a foliation @~60deg t.c.a. Contacts of dkyes are sharp, each @~60deg t.c.a. At 248.42m, unit is cut by a 35cm pre-kin mafic dyke. Foliation @~60get t.c.a. L.c is broken, U.c is sharp, @~60deg t.c.a. At 248.77m there is some re-lithified breciated clasts of the host rock, indicating a minor fault (5cm wide) wich is also present at 249.42m. Unit is moderatly magnetic, with a few bands of strongly magnetic magnetite. Unit contains trace amounts of purple carbonate (?)in fractures. L.c of unit is gradational. Unit is mineralized at 244.80 with spot high of 417cps.

249.97 282 MI.dk.sk Dark grey-black, syn to late-kin. Mafic dyke. Moderatly foliated @~60deg t.c.a. Unit has caclite in fractures. Approx 5-7% plag phenos and 3-5%quartz phenos. Unit has veins of plag throughout. Unit has chlorite and epidote in fractures (ep>ct) as well as trace amounts of disseminated hornblend throughout. Unit has moderate magnetism. Unit has intervals of more and less prophyritic compositons thoroughout. Unis contains a 3cm quartz vein at 275.87 L.c in not visable, located somewhere around 280.50m. Reason for placing contact here is b/c of the magnetic contrast(moderate v.s strongly magnetic).

282 335.45 MT-IV Pink-green to grey-black, Chlorite rich, felsic poor, Intermediate to mafic volcanics. Weakly foliated with cross-cutting mafic dikelets. Strongly magnetic. Sparse plag phenos local throughout. Increasingly felsic downhole. Foliation becomes stronger downhole. Hematization becomes more prominent downhole. Ct+minor epidote w/n mafic dikelets. Dikelets appear to be later due to cross-cutting of dominant foliations. Abundant carbonate is found w/n bt+ct-rich swathing veinlets b/w 307.00m-311.00m. Patchy U mineralization as follows: 299.70m-303.33m: max: 826cps; avg: 332cps 309.35m-310.00m: max 296cps; avg: 200cps 310.65m-312..00m: max: 398cps;avg: 228cps


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335.45 336.79 FI.gr Pink-white, black speckled, Coarse-grained, weakly altered, qtz-monzonite to qtz syenite. Unit contains abundant coarse-grained pink-white, anhedral phenocrysts of k-spar that are roughly 1-1.5cm in size. There are also abundant finer-grained (0.5cm) irregular lathes of bt+hb throughout giving the unit a peppered look. The dike appears unfoliated. Upper contact is irregular and roughly at an angle of 40 degrees to C.A. Lower contact is at an angle of 60 degrees to C.A.

336.79 357.72 MT-IV Continuation of previous MT-IV unit (282.00m-335.45m) Pink-green to grey-black, Chlorite rich, felsic poor, Intermediate to mafic volcanics. Weakly foliated with cross-cutting mafic dikelets. Strongly magnetic. Sparse plag phenos local throughout. Increasingly felsic downhole. Foliation becomes stronger downhole. Unit contains 3 (<50cm) enclaves of the previous FI unit b/w 338.62m-338.97m, 341.72-342.21m and 349.62m-350.32m. Contacts b/w FI and the MT-IV are moderatley fluid altered (hm+K). Hematization becomes more prominent downhole. Ct+minor epidote w/n mafic dikelets. Dikelets appear to be later due to cross-cutting of dominant foliations. Abundant carbonate is found w/n bt+ct-rich swathing veinlets throughout unit. Moderately magnetic. Upper contact is sharp with the previous unit. Patchy U mineralization as follows: 342.00m-343.00: max: 1242cps ; avg: 721cps 345.00m-346.00m: max:432cps ; avg: 195cps 349.00m-350.00m: max:467cps; avg:279cps 350.00m-351.00m: max:293cps; avg:180cps

357.72 361.43 MI.dk.psk 357.72 - 359.55 Intermediate Meta-volcanics; 359.55 - 361.43 Unfoliated Post-kinematic Mela-gabbro

361.43 363 MT-IV Intermediate Meta-volcanics

363 367.3 FI.dk Fine-grained Felsic Intrusive

367.3 374.89 MT-IV Intermediate Meta-volcanics

374.89 376 MI.dk.por Pg-Porphyritic Mafic Dike

376 380.38 MT-IV Intermediate Meta-volcanics

380.38 382.2 MI.dk.psk Post-kinematic Mela-gabbro

382.2 388.35 MT-FV Felsic Meta-volcanic


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388.35 397.06 MT-IV Intermediate Meta-volcanics

397.06 398.15 MI.dk.por Syn-kinematic Mafic Dike

398.15 410.66 MT-IV U-mineralized Intermediate Meta-volcanics; Mineralized as follows: 399.33 - 398.68: max: 728 cps avg: 398cps

410.66 412.13 MI.dk.sk Syn-kinematic Mafic Dike


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0 1 OVBD Overburden and casing

1 26 MT-CO.pl Polylithic metamorphosed conglomerate. First 12.5m are clast poor. Although this part of the unit looks like MT.IV it seems to be part of the conglomerate b/c there is no magnetism contrast btw this part of the unit and the bottom part of the unit, which is an obvious conglomerate. Also the MT.IV like part of the unit has some poorly disseminated clasts. Also, there are some thin, obvious conglomerat intervals present in the first 12.5m. After 12.5m, the unit is clearly conglomerate, locally cut by a hornblend prophyritic syn-kin mafic dyke btw 23.77m-24.41m. The clasts in the conglomerate are from various natures such as sandstone, chert, & volcanics. The unit has moderate patchy hemitizatiion in the most clast rich part. Traces of disseminated carbonate mineralization, usually oriented parallel to the dominant foliation. Locally the unit is epidote ± chlorite rich. L.c is very diffused.

26 28.74 MT-IV.por.fp Porphyritic metamorphic felsic volcanic with quartz and feldspar. Feldspars are strained or rounded. Moderate replacement hematization. Local fracture filled carbonates. Unit is non-magnetic. Foliation @~50deg t.c.a.

28.74 65.24 MT-CO.pl Return to metamorphosed conglomerate.First 81cm of the unit is a syn-kin. Mafic dyke with sharp bottom and top contacts, @~65deg t.c.a and 60deg t.c.a respectively. Conglomerate is weakly strained to mylonitic with a lot of fragments fine to coarse grained and from various natures such as siliceous (chert, quartz), sedimentary (sandstone, mudstone), and volcanics (basaltic to andesitic). Moderate patchy hematization. Very weak to no magnetism. Unit cut by a50cm syn-kin mafic dyke at 49.79. Lower and upper contacts are sharp, @~5deg and ~50deg respectively.

65.24 66.6 MI.dk.sk Fine grained moderately foliated syn-kinematic melagabbro dike, strongly chloritic. Both sharp contacts, oriented around 50° to the CA.

66.6 85.86 MT-CO.pl Continuation of the previous metamorphosed conglomerate. Carbonate alteration starts at 76m to the bottom and is mineralised into small fractures (calcite) and in replacement of clasts (anchorite). Hematisation is, as always, situated in the clasts but never into the rhyolitic matrix of the formation. There is also an Epidote ± chlorite alteration in veins. As always in this unit, the clasts are from really various nature ; Sedimentary (mud/Sandstone), Volcanics (basaltic to andesitic clasts), and siliceous (jasperite, cherts, Quartz, Felsics). The unit is strongly foliated, the clasts are weakly strained, as there is a beginning of mylonitisation. The unit is moderately magnetic.


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85.86 94.32 MT-IV.por.fp Fine grained plagioclase porphyritic felsic intermediate meta-volcanics, moderately magnetic, cut by fractures filled with epidote ± chlorite. Porphyroclasts of altered plagioclases and amphiboles, fine to medium grained, nevertheless, the unit is locally aphanitic. Both contacts are sharp but they are weakly diffused over 10 cm at the margins. Both contacts are oriented at 40 ° to the CA, the foliation is moderate and irregular, between 40 and 50° to the CA. Disseminated hematised plagioclases. Rare chalcopyrite mineralisations.

94.32 100.4 MT-CO.pl.my Intensely mylonitic meta-conglomerate, strongly foliated, strong patchy hematization, intensely pervasive over the first 2 metres, the nature of the clasts is hard to define as they are all strongly strained, but seem to be the same as in the previous conglomeratic units ; Sedimentary (mud/Sandstone), Volcanics (basaltic to andesitic clasts), and siliceous (jasperite, cherts, Quartz, Felsics), with replacement anchorite, disseminated epidote and chlorite alteration. The foliation is irregular, in a range between 30 and 40° to the CA. The bottom contact is emphasized by a 32cm thick mafic syn-kinematic dike. The unit has patchy weak to moderate magnetism.

100.4 103.81 MT-IV.my Transition zone between the mylonitic conglomerate and the felsic meta-volcanics ; intermediate meta-volcanics, mylonitic, strongly foliated, intersected by a syn-kinematic hornblende (and sulphide) porphyritic mafic intrusive, 20cm thick. The unit has patchy moderate hematization. The foliation is oriented at 40° to the CA. Weak magnetism. The bottom contact is very diffused over 30 cm, alternating between MT-IV and MT-FV.

103.81 117.8 MT-FV.por Fine to medium grained plagioclase ± Quartz porphyritic felsic meta-volcanic, strong patchy and plag replacement hematization, locally fracture filled hematization. The unit is cut by 2 mafic intrusives, one syn kinematic hornblende porphyritic mafic dike with chalcopyrite between 104.6 and 105.55m, and one small syn kinematic mafic intrusive 25cm thick. Local chlorite replacement. Unit is barely foliated on top but is moderately to strongly foliated to the bottom. Irregular magnetism, magnetite appears to be mineralised in small veins parallel to the foliation (~40° to the CA). Very weak presence of calcite into fractures. The bottom contact is sharp.


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117.8 143.01 MT-IV.por.fp Fine-grained, moderately foliated, intermediate meta-volcanics, locally plagioclase-albite porphyritic. Unit is also locally rich in felsic material that is relatively hematized and with K-spars. The unit is moderately intersected with pale-green veinlets believed to be filled with green Pyroxenes ± Amphiboles (maybe green Hb) . Hematite occurs in patchy bands throughout which follow dominant foliation, and also in replacement of Albite. Albite porphyritics are mostly highky strained. Unit is strongly magnetic. Locally cut by 3 small post kinematic unfoliated mafic dikes, <25cm. Occurences of leucoxenes, hornblende, Biotite locally replaced by chlorite. No eye scale sulphides are visible. Upper contact is sharp but on the first 30cm, there are some small MT-FV intervals. The contact with the dike underneath is also very sharp, 25 degrees to the CA.

143.01 149.95 MI.dk.por Plagioclase porphyritic post-kinematic mafic dike, seems to have a small foliation, but the plagioclases porphyroclasts are not oriented at all so the dike is more likely post-kinematic. Weak hematization replacing plagioclases. Nonmagnetic unit. Both contacts are sharp and chilled, oriented at 40° to the CA for the bottom contact

149.95 162.59 MT-IV.my Fine-grained to aphanitic, moderately foliated, intermediate meta-volcanics, mylonitic, intensely foliated, and with occurrences of some isoclinal folds. Black, green and red. Presence of hematized Qz veinlets, and of Amphibole ± Pyroxene pale green veinlets. The hematization is weak and patchy, situated into bands. Presence of leucoxene, rare plagioclases porphyroclasts, and Biotite locally replaced by chlorite. Presence of minor faults, with millimetric to centimetric offset. Some carbonates are sited into fractures and also finely disseminated. Very strong magnetism

162.59 170.35 MI.dk.por Plagioclase porphyritic post-kinematic mafic dike, seems to have a small foliation, but the plagioclases porphyroclasts are not oriented at all so the dike is more likely post-kinematic. Weak hematization replacing plagioclases. Nonmagnetic unit. Both contacts are sharp and chilled, oriented at 26° to the CA for the bottom contact. Weak disseminated calcite mineralisation.


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170.35 225.41 MT-IV Fine-grained to aphanitic, moderately foliated, intermediate meta-volcanics. Black, green and red. Presence of hematized Qz veinlets, and of Amphibole ± Pyroxene pale green veinlets. The hematization is weak and patchy, situated into bands, and in felspar replacement. Presence of leucoxene, rare plagioclases porphyroclasts, and Biotite locally replaced by chlorite. Presence of minor faults, with millimetric to centimetric offset. Some carbonates are sited into fractures and also finely disseminated. Very strong magnetism. The unit is very locally plagioclase and/or leucoxene porphyritic, and also locally mylonitic, but is globally aphanitic and not mylonitic. Locally cut by a finely porphyritic mafic intrusive, weakly foliated so lately syn-kinematic, at 218.23m, to 219.03. Hematization and carbonates occurences become more important from 204m, carbonates in veinlets are usually associated with biotite, and locally with chalcopyrite.

225.41 226.55 MI.dk.psk Aphanitic post-kinematic mafic intrusive, locally intersected by very thin carbonate filled veinlets. Occurences of disseminated very fine grained sulfides (chalcopyrite) mineralisations. Moderate magnetism. Both contacts are sharp, top contact oriented 60° to the CA, and bottom contact is at 45° to the CA.

226.55 250.6 MT-IV Continuation of the previous MT-IV unit, entering the mineralised zone around 228m, the mineralisation is as follows ; Barely mineralised between 228-230 Very good mineralisations between 230-237m ; avg 1600cps ; 33 spots > 1000 cps. Barely mineralised between 237-250.6m with 3 spots > 500 cps. Locally cut by a porphyritic syn kinematic mafic intrusives at 246.62m, 26cm thick. Around 237m, a highly chloritic replacemnt zone is cut by an important small fractures network, filled with carbonates, underneath that 25cm interval, the foliation has turned.

250.6 251.86 MI.dk.por Plagioclase porphyritic fine to medium grained, syn kinematic mafic dike, fine grained disseminated chalcopyrite mineralisations. Nonmagnetic.

251.86 290.1 MT-IV Continuation of the MT-IV unit ; The unit is locally cut by 5 small (< 1m) mafic intrusives ; 254.41 - 254.54m ; 256.05 - 256.26m ; 267.18 - 267.98m ; 277.08 - 277.53m ; 289.42 - 290.07m. The bottom contact of the unit is emphasized by a mafic dike between the 2 units. U-mineralised as follows ; 268 - 276m : avg => 800 cps ; 19 spots > 1000 cps ; max 7044 cps.


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290.1 305.6 FI.por.fp Coarse grained porphyritic felspar porphyry, weakly foliated, the foliation is expressed by micaceous bands, locally associated with minor very fine grained chalcopyrite mineralisation. Most of the plagioclases are zoned, sometimes nucleated around a biotitic core. Some minor disseminated carbonates are also present. Sometimes, and mostly close to the bottom margin, the very last zonation around plagioclase is K-felspatic. The unit is weakly magnetic. This unit seems to be U-mineralisation destructive, so it is thought to be post mineralisation. Hematisation is disseminated and very weak.

305.6 316.2 MI.dk.sk Very fine grained syn-kinematic mafic dike, barely to moderately foliated. Nonmagnetic, interfingered with the felspar porphyry on the first 3.50m. The dike is strongly biotitic, locally replaced by chloritic bands.

316.2 367 MT-IV Fine-grained to aphanitic, moderately foliated, intermediate meta-volcanics. Black, green and red. Presence of Amphibole ± Pyroxene pale green veinlets. The hematization is strong and patchy. Presence of Biotite locally replaced by chlorite. Lots of carbonates, sited into fractures and also finely disseminated. Very strong magnetism. Carbonates in veinlets are usually associated with biotite and green hornblende ± Pyroxenes, and locally with chalcopyrite. New lens of U-mineralisation starts at 321m. Association between U-mineralisation and carbonates veinlets ? Unit is mineralised as follows ; 322-324m => avg 450 cps ; max 1453 cps. 324-332m => Barely mineralised, avg 120 cps ; max 493 cps. 332-334m => avg 350 cps ; max 890 cps. 334-341m => Barely mineralised, avg 120 cps ; max 440 cps. 341-343m => avg 450 cps ; max 1091 cps.


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0 9.6 OVBD No core recovery to 8.4m, then overburden to 9.6m.

9.6 35.9 MT-IV Fine grained, medium grey, massive, unfoliated to moderately foliated, weak to strong patchy magnetic intermediate volcanic with locallized chlorite shears along foliation plane. Minor areas (mostly from 11.7-13.0m) with 5-15% green 1-3mm disseminated chlorite phenocrysts replacing probably amphibole (hbl?). From 17.7-23.6m: pachy to pervasive potassic alteration with strong alteration from the top to 18.3m with moderately broken core followed by patchy potassic alteration in the matrix and 10-20% dark chlorite defining foliation. This area has 2% calcite-chlorite filled fractures with a stockwork of calcite-chlorite fractures (30%) from 22.05-22.30m. From 33.0-35.9m: 3-10% fine grained fresh biotite disseminated in foliation plane.

35.9 38.9 MI.dk.sk Fine to medium grained, dark grey-green, post-kinematic, unfoliated to weakly foliated, weak to moderate patchy magnetic. Disseminated plagioclase phenos increaing downhole, white to cream in colour, 5-10%, 0.5-2mm in size. Several larger phenos, probably of amphibole, throughout unit, average 0.5-0.8cm in size, black, <1%, patchy. Upper contact is sharp and concordant, lower contact is broken.

38.9 77.03 MT-IV Fine grained, medium grey to greyish red-brown, weakly foliated to moderately foliated, moderate to strongly magnetic (mostly assoiated with chlorite) intermediate volcanic with weak to strong hematitic alteration from 44.1-62.2m. Uranium is associated with moderate-strong hematite alteration. Multiple mafic dykes cross the interval from 50.52-51.05m with uct@80 deg tca; 52.65-52.9m with uct@ 65 deg to CA; 54.7-54.9m with uct @ 58 deg to ca; 55.8-55.9m with uct @ 60 deg to CA; 65.65-65.78m with two chlorites and calcite (possibly vein) with uct @ 55 deg to CA; and last mafic dyke at 67.77-67.86m with uct @ 50 deg to CA. Mineralized intervals occur from 46.35-8.0m with an avg of 340 cps and a max of 401 cps; 48.9-49.9m with an avg of 410 cps and max of 952 cps; from 52.15-52.65m with an avg of 510 cps and a max of 631 cps; from 53.65-54.7m with an avg of 900 cps and a max of 1865 cps; from 55.09-57.35m with an avg of 325 cps and a max of 616 cps; from 58.0-58.67m with an avg of 640 cps and a max of 1161 cps; from 60.9-61.4m with an avg of 825 cps and a max of 2028 cps; from 61.85-62.12m with an avg of 330 cps and a max of 347 cps. Mineralization tapers with depth, to backgroud readings by 62m. Lower contact broken. Short intervals of adjacent porphyritic intrusive towards lower contact.


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77.03 96.87 FI.por.fp Coarsely porphyritic felsic intrusive. Unit is black to salmon coloured. Consists of large phenos of quartz and felspar. Pheno intensity ranges from intense to locally trace. Feldspar phenos periodically contain biotitic nuclei. Magnetism is moderate to strong. White quartz vein at 92.75 - 92.81m. Sharp lower contact oriented 85 degrees to core axis. Unit is genrally undeformed, with little evidence of straining. Some very weak foliations visible in biotite.

96.87 101.34 MT-IV Black to dark grey metamorphosed intermediate volcanics. Moderately to highly foliated, oriented 65 degrees to core axis. Alteration is moderate, locally weak. Hemitization overall is weak, though locally prominent. Disseminated chlorite visible throughout. Occasional vein of neighbouring felsdaprs visible at top of unit. Some chlorite veines visible as well. Patchy black bands of magnetite. Post kinematic mafic dyke from 98.38 to 98.92, consisting of biotite, dissiminated chlorite, with small (<0.5cm) pophyrys of quartz +/- fp. Mineralization Highlights: Weakly mineralized, all readings register background counts when scinted in hand.

101.34 103.53 MI.dk.psk Post kinematic mafic dyke with small (0.5cm) phenos of plag +/- fp. Moderate disseminated chlorite. Biotite rich. Fine grained chill zones towards both top and bottom contacts. Lower contact is broken, top contact oriented 50 degrees to core axis. Non magnetic.

103.53 121.15 MT-IV Dark grey fine grained metamorphosed intermediate volcanics. Moderately to highly foliated. Patchy moderately to strongly magnetic. Veins of calcite associated with chlorite veins. Disseminated chlorite and biotite throughout. Patches of feldspars from 117.37-117.75m. Moderate to strong hematization from 118m to end of unit. Lower contact is sharp and concordant with an angle of 50 tca. Mineralization ranges from background to a high of 3159 cps throughout the unit, with areas of high strain associated with mineralization. Mineralized intervals occur from: 105-106: max of 3159 cps and avg of 810 cps. 114-121m, ave: 257cps, max: 749cps

121.15 122.92 MI.dk.sk Fine to medium grained mafic dyke, syn- to late-kinematic, weakly foliated, moderately to strongly magnetic, locally porphyritic with phenos of avg size 5-8mm, occupying approximately 5% of the matrix, phenos have been replaced with epidote but were likely feldspar initially. Veinlets and vuggy areas of epidote. Moderate amounts of disseminated biotite throughout and weak amounts of dsm ct throughout. Lower contact is concordant and makes an angle of 55 degrees tca. From 122.86-123.16m, there is a granitoid intrusion that is light pink in colour, moderately magnetic, with irregular contacts.


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122.92 133.45 MT-IV Medium to dark grey metamorphosed intermediate volcanics, moderately foliated, patchy moderately to strongly magnetic, patchy areas of moderate to intense hematization. Disseminated chlorite and epidote visible in patches. Some veins of calcite, vuggy, appear to be fracture fill. Foliations oriented 70 degrees to core axis. Lower contact blocky and broken. Unmineralized. Last 95cm of unit is porphyritic mafic dyke with usual phenos, and veines of chlorite. Little deformation.

133.45 138 MT-FV.por Metamorphosed felsic volcanics, fine grained. Stongly hematized throughout. Usual phenos of quartz and feldspar, though not nearly as abundant as usual from this lithology. Weak to moderately magnetic. Some dsm magnetite. Fracture fill epidote visible locally. Mineralogy is predominately feldspar and hematite. Some tiny FFL calcite. Some smokey quartz veinlets. Bottom contact blocky and broken.

138 144.57 MI.dk.por Porphyritic mafic dyke, highly chloritized, unit is block and broken for majority of interval. Many tiny angular feldspar pophyrys visible throughout unit. Overall colour is dark green, signifying chloritized matrix. Moderately biotitic. Phenos of ct +/- also visible. Some fracture fill carbonate veinlets. 139.25 to 139.97m sees return to previously described metamorphosed felsic volcanics. Afterwards, unit is increasingly chloritic, with patches of hematite, more than likely from adjacent unit. Increased in carbonates towards lower contact. Weakly magnetic.

144.57 166.68 MT-IV Return to intermediate volcanics. Unit is very lowly hematized. Overall colour is grey, increasing in hematization to sub-moderate, locally pervasive. Some phenos of chlorite, Some dsm feldspar. Some fracture fill cacite. Dsm epidote also visible in patches. Unit is weakly to moderately foliated. Older, more mafic veins have been altered to chlorite and chlorite-actinolite and have also been folded. Younger generation veins of feldspar and quartz are not folded and are aligned parallel to the foliations. K-spar alteration of the younger generation veins. At 163m, one of the k-spar altered veins shows en echelon fracturing. Minor carbonate associated with the mafic and feldspar veins. Unit is blocky and broken over 153-155m with no evidence of gouge material. Upper contact oriented 80 degrees to core axis, while lower contact is oriented at 70 degrees tca. Both upper and lower contacts are sharp and concordant.


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166.68 183.21 FI.por.fp Dark red-pruple, coarsely porphyritic feldspar felsic rock. Unfoliated to very weakly foliated. Non-magnetic. 20-40% rounded feldspar phenos, 2-20mm in size, most of which have a biotite-rich +/- very fine grained feldspar (?) nucleus, twinning or radial zoning visible on coarser phenos, phenos are partially k-spar altered, minor broken phenos, few 2-4mm ct phenos near lower contact. Fine grained, moderately hematized groundmass, looking mostly felsic but with small patches of ct + bt with trace vfgr pyrite. Phenos less concentrated for about 30cm at each contact, hematization is stronger at both contacts, and foliation intensifies closer to the lower contact. Ct+actinolite+/- carbonate coating, very minor. Sharp lower contact at 60 degrees tca.

183.21 193.05 MT-IV Dark green to dark red, vfgr, moderately foliated, intermediate meta-volcanics. Top 6m similar to previous MT-IV unit, is moderately magnetic with minor PE ct alteration, locally 1mm wide feldspar phenos (lamellar). Rest of unit has patchy hematitic alteration, is non-magnetic, and is mineralized with folded 1-4mm carbonate-rich + ct veins. Unit seems brecciated over the last metre with elongated/strongly foliated clasts defining the foliation, some clasts very augen-looking. Rare qz+k-spar clasts are elongated, mostly aligned with the foliation, and are found in the lower part of the unit. Last 20cm of unit is feldspar porphyritic. Unit is locally blocky. Lower contact is irregular. Mineralization (is cut bu lower porphyritic intrusion): Between 189-190m, avg 1200 cps and max 2681 cps; between 190-191m, avg of 553 cps and max of 1508 cps; from 191-192m, avg of 423 cps and max of 1882; from 192-193m, avg of 411 cps and max of 748 cps.

193.05 204.25 FI.por.fp Dark orangey-red, feldspar porphyritic felsic meta-volcanic, coarse grained, similar to previous porphyritc unit, only minor k-spar alteration of the phenos, very fgr groundmass with PE hematite + k-spar alt, biotite nuclei are less prominent, possibly qz phenos (?), weak foliation defined by aligned phenos and discontinous biotite bands, twinning and/or zoning evident in the coarser phenos, minor discordant carbonate veinlets, moderate to strong PE magnetism, concordant bands of vfgr material that is strongly magnetic and found mostly up-hole. Last 1.5m is broken. Minor ct + actinolite coating on fractures. Foliation increases down-hole. Lower contact is wavy at approx. 55 degrees tca.


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204.25 208.18 MI.dk.sk Dark grey, syn- to late kinematic mafic dyke. Upper 1.5m is finely feldspar porphyritic with phenos % decreasing downhole (30-10%), weakly fol, non-mag, wk to mod ct altn. Localized coarser (0.5cm) fp phenos. Lower part is vfgr with minor concordant qz veins. The lower part could be a short MT-IV interval. Lower 0.5m had qz + fp blebs. LCT is sharp at 80tca. 205.73-206.26m: mgr granitic intrusion, wk foliated, wk pa mag with minor mafic dyklets. Qz blebs + cb vts trgt. Both contacts are concordant with fol. Minor ep altn (fp replacement?)

208.18 219 FI.gr Med greyish pink, mgr fps porphyritic granitoid. Wk fol defined by thin discontinuous bt bands. Pa wk mag. 4-5% 2-7mm fp phenos. Local minor saussurization of phenos. Minor kspar altn on phenos (localized downhole). Higher concentration of large phenos at UPC (20%) over approx. 12cm. 2mm concordant qz vein at 214.82m. Ct +ac +/-cb coating on fractures. Odd large (1-7cm) vfgr mafic blebs (xenos?). Series of short fgr mafic dykes between 209.90-215.42m (all similar, syn- to late kinematic but one that is ct-rich syn-kinemtic), all contacts are sharp and discordant to fol. EOH (July 12, 2008)


333030.2156066396.456

NAD83_21

190.571336-90 142.0

7/21/20087/23/2008

NREastingNorthing



Logged By


Drilling Company: Durado

Drill Hole Log JLM08-001 Page 103 of 106

0 4.05 OVBD NULL

4.05 8.15 MT-IV Metamorphosed Intermediate Volcanics

8.15 10.11 MI.dk.sk Post-kinematic mafic dyke

10.11 42.42 MT-IV Metamorphosed Intermediate Volcanics

42.42 47.88 MI.dk.sk Syn-kinematic mafic dyke

47.88 92.96 MT-IV Metamorphosed intermediate volcanics; Mineralization occurring at: 47.93 – 73.01m with an average of 587.65 cps (including highs of 3414, 2017, 2034, and 2338) with a max of 3373 cps.

92.96 94.76 MI.dk.sk Syn-kinematic mafic dyke

94.76 140.14 MT-IV Metamorphosed intermediate volcanics; Mineralization occurring at: 83.15 – 89.50m with an average of 403 cps and a max of 1500 cps. 110.50 – 131.50m with an average of 724 cps and a max of 4992 cps.

140.14 142.01 MI.dk.sk Post-kinematic mafic dyke


333030.0436066396.756

NAD83_21

190.571336-80 132.5

7/28/20088/3/2008

NREastingNorthing



Logged By




0 3.26 OVBD overburden

3.26 8.2 MI.dk.sk unit is very broken and rubbely. Appears to be a mafic dyke with a small granite intrusion? Maybe a boulder intercepted by the drill as it is close to the top of the hole. Dyke contains phenos ~0.1-0.2cm in diamerter and some minor veining . Contact is undeterminable.

8.2 12 MT-IV Red to dark gray metamorphosed intermediate volcanics. Unit is moderately to highly magnetic indicating magnetite content and also containing k-feldspar. This unit also conains small veinlets of calcite that cut the core in places at 10deg t.c.a. Again, the unit is extremely broken so orientation measurements are difficult and contacts are undistinguishable.

12 19.2 MI.dk.sk Dark gray-black syn-kinematic mafic dyke. Unit contains phenos of plag and evidently k-feldspar near the top indicated by pink colour. Dyke also exhibits some veining of calcite, cholorite and epidote with some blebby quartz near some veins. Again the unit is very rubbly and broken with very gradational and busted contacts. Unit is non-magnetic.

19.2 58.1 MT-IV Return to dark red and gray/black unit of metamorphosed intermediate volcanics. Unit contains k-feld, and is moderately to strongly magnetic, again indicating magnetite content. Unit is occationally viened by a dark mineral, likely magnetite. Calcite appears in veins throughout the unit and have a general orientation of ~15 deg t.c.a. Hematization occurs in viens throughout the unit as well. Small viens and bands throughout the unit also contain chlorite. Unit is cut by a minor mafic dyke at a depth of 54.65 - 55.03m with upper and lower contacts of 50 and 45 deg respectively t.c.a. Mineralization begins at ~27m through to 56m with an average of: 654.78 cps and a max of: 6383 cps, including values of: 4079, 3064, 2646, 1181, 2163 4183 and 1129.

58.1 60 MI.dk.sk Dark gray/black syn-kinematic chloritized mafic dyke with a diabase texture. Sparce blebbs of quartz and/or feldspar exist throughout with a max diameter of 1 cm . Unit contains couple of tiny calcite veinlets and is non magnetic. Also contains biotite. Lower contact was determined via magnetism and is not easily visible. Upper contact is sharp and make an angle of 30deg t.c.a.


333030.0436066396.756

NAD83_21

190.571336-80 132.5

7/28/20088/3/2008

NREastingNorthing



Logged By




60 75.61 MT-IV Return to moderately/strongly magnetic red/dark gray-black metamorphosed intermediate volcanics. As usual this unit contains a large amount of k-feldspar and exhibits hematization at some veins that are generally composed of calcite. Locally well veined areas of chlorite, calcite and possibly biotite or some other vitrious fine grains of dark mineral exhibit vuggy texture. The units lower contact is sharp and makes an angle of 55 deg t.c.a. Unit is cut by a small mafic dyke at a depth of 68.92 - 69.44 that has a shape upper contact of ~45deg t.c.a. and a lower contact that is broken and undeterminable. This dyke contains biotite and trace pyrite and chalcopyrite. Mineralization begins at ~72m

75.61 77.3 MI.dk.sk another good old non-magnetic syn-kinematic mafic dyke. Our dyke is dark-gray to black containing a lot of biotite throughout and some calcite blebbs and veinlets as well as phenos of felspar/quartz (~0.1 - 02cm in diameter) which appear more elongate at the contacts. The upper and lower contacts are sharp and make angles of 55deg t.c.a. the cross section of a minor quartz vein reveals small lathes (0.4cm x 0.1cm) of some black vitrious mineral possibly biotite. Mineralized core begins at ~72m…

77.3 94.94 MT-IV Return to previously described metamorphosed intermediate volcanic. Contains a large amounts of k-feld veined and foliated with chlorite, calcite, biotite. Frequent banding of veins and flowy texture generally oriented ~40deg t.c.a. Mineralization was intercepted at 72.00m with an average of , a max of , including high values of

94.94 96 MI.dk.sk Dark gray/black chloritized syn-kinematic mafic dyke containing veinlets of calcite and also containing biotite. Upper contact is sharp and makes an angle of 40 deg t.c.a. Lower contact is broken but seems to have been sharp also. Unit is non-magnetic.

96 130.45 MT-IV Return to strongly magnetic metamorphosed intermediate volcanics. This red to dark gray/black unit contains K-feldspar, magnetite, Chlorite, +/- epidote. It is well foliated with flowy texture at an angle of ~40deg t.c.a. that exhibits some veinlets that roughly follow the orentation of foliation containing calcite, +/- chlorite that are occationally hematized. Unit contains a minor non-magnetic syn-kinematic mafic dyke at 118.22 - 118.59m depth with sharp upper and lower contacts making angles of 50 and 35 deg t.c.a. respectively.


333030.0436066396.756

NAD83_21

190.571336-80 132.5

7/28/20088/3/2008

NREastingNorthing



Logged By




130.45 132 MI.dk.sk fine-grained Medium grey mafic dyke containing small lathy feldspar phenos up to 2mm in size. Unit is non magnetci and moderately foliated with occational veinlets of a dark green mafic mineral (chlorite?).


128



APPENDIX VI

ASSAY CERTIFICATES

Aurora Energy Resources Inc. Suite 303, 10 Fort William Place, St. John's, NL A1C 1

Document Page 128

CERTIFICATE OF ANALYSIS

Innovative Technologies Quality Analysis ...

Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

23-Jun-08

28-May-08

A08-2699

Aurora Energy Resources Inc.

Suite 1650, 1055 West HastingsVancouver BC V6E 2E9Canada

Cam McLeanATTN:

This report may be reproduced without our consent. If only selected portions of the report are reproduced, permission must be obtained. If no instructions were given at time of sample submittal regarding excess material, it will be discarded within 90 days of this report. Our liability is limited solely to the analytical cost of these analyses. Test results are representative only of material submitted for analysis.

ACTIVATION LABORATORIES LTD.

1336 Sandhill Drive, Ancaster, Ontario Canada L9G 4V5 TELEPHONE +1.905.648.9611 or +1.888.228.5227 FAX +1.905.648.9613

E-MAIL [email protected] ACTLABS GROUP WEBSITE http://www.actlabsint.com

Elitsa Hrischeva, Ph.D.

CERTIFIED BY :

REPORT A08-2699

Notes:

1 Pulp sample and 12 Rock samples were submitted for analysis.

Code 1E3 - Aurora Pkg. Aqua Regia ICP(AQUAGEO)Code 5D-U-Total DNCCode Specific Gravity Pulp

Values which exceed the upper limit should be assayed for accurate numbers.

Quality Control

The following analytical packages were requested:

Document Page 129

Activation Laboratories Ltd. Report: A08-2699Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P PbAnalyte Symbol

ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % ppm % ppm ppm % ppm % ppmUnit Symbol0.2 0.01 2 10 10 0.5 2 0.01 0.5 1 1 1 0.01 10 1 0.01 10 0.01 5 1 0.001 1 0.001 2Detection Limit

AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICPAnalysis Method

0.3 1.64 < 10 63CMB19051 < 0.5 < 2 1.62 0.6 13 32 162 2.86 < 10 < 1 0.06 59 0.95 399 < 1 0.084 16 0.026 2627

< 0.2 1.00 < 10 32CMB19052 < 0.5 < 2 1.58 < 0.5 7 24 38 1.66 < 10 < 1 0.11 76 0.29 202 < 1 0.075 6 0.020 584

< 0.2 0.61 < 10 19CMB19053 0.7 < 2 1.56 1.2 33 42 55 5.60 < 10 < 1 0.02 37 0.34 207 1 0.126 11 0.092 208

< 0.2 0.22 < 10 24CMB19054 < 0.5 < 2 1.28 0.9 11 8 8 4.94 < 10 < 1 0.02 53 0.08 117 1 0.131 5 0.095 45

< 0.2 0.34 < 10 33CMB19055 < 0.5 < 2 1.73 0.9 9 13 44 4.57 < 10 < 1 0.03 53 0.08 163 1 0.135 4 0.094 84

< 0.2 0.32 < 10 19CMB19056 < 0.5 < 2 1.67 1.2 4 9 45 4.75 < 10 < 1 0.02 54 0.09 167 2 0.144 5 0.097 117

< 0.2 0.32 < 10 17CMB19057 < 0.5 < 2 1.91 0.8 9 8 45 4.33 < 10 < 1 0.01 52 0.07 157 1 0.120 3 0.091 117

0.3 0.44 < 10 369CMB19058 < 0.5 < 2 1.96 0.9 19 16 86 4.80 < 10 < 1 0.16 39 0.34 348 1 0.184 16 0.096 209

0.2 0.53 < 10 626CMB19059 Received as pulp

< 0.5 < 2 1.20 0.5 11 29 32 2.19 < 10 < 1 0.12 74 0.37 326 4 0.179 45 0.042 1423

< 0.2 2.75 < 10 63CMB19060 < 0.5 < 2 3.23 0.7 26 82 16 4.13 10 < 1 0.21 11 1.62 814 < 1 0.117 27 0.048 105

0.3 0.59 < 10 22CMB19061 0.6 < 2 2.52 0.8 11 20 116 4.88 < 10 < 1 0.01 53 0.14 278 2 0.130 6 0.123 5014

< 0.2 0.43 < 10 23CMB19062 < 0.5 < 2 3.91 1.2 4 26 7 4.87 < 10 < 1 0.03 37 0.09 656 1 0.128 4 0.078 58

< 0.2 0.58 < 10 28CMB19063 < 0.5 < 2 1.82 0.8 11 41 38 3.49 < 10 < 1 0.09 27 0.20 240 < 1 0.129 5 0.058 55

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Activation Laboratories Ltd. Report: A08-2699S Sb Sc Sr Ti Tl U V W Zn U Mass Spec GravAnalyte Symbol% ppm ppm ppm % ppm ppm ppm ppm ppm ppm g -Unit Symbol

0.01 2 1 1 0.01 10 10 1 10 2 0.1 0.01Detection LimitAR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP DNC DNC GRAVAnalysis Method

0.01 < 2 113 0.18CMB19051 < 10 < 10 77 < 10 49 5.3 1.025 2.706

0.02 < 2 96 0.15CMB19052 < 10 < 10 46 < 10 19 5.1 1.0684

0.11 3 75 0.38CMB19053 < 10 126 107 < 10 20 113 1.097 2.664

0.02 < 2 30 0.34CMB19054 < 10 14 43 < 10 10 15.9 1.0162

0.02 < 2 61 0.34CMB19055 < 10 35 49 < 10 13 35.0 1.067 2.722

0.02 3 48 0.33CMB19056 < 10 58 44 < 10 15 64.4 1.0752

0.02 2 52 0.31CMB19057 < 10 69 39 < 10 11 69.5 1.050 2.712

0.04 4 56 0.43CMB19058 < 10 < 10 71 < 10 66 11.8 1.0961

0.09 < 2 65 0.18CMB19059 Received as pulp

< 10 421 54 < 10 100 405 1.069 2.703

0.05 3 246 0.30CMB19060 < 10 < 10 128 < 10 96 4.9 1.05511

0.04 2 108 0.36CMB19061 < 10 449 85 < 10 13 396 1.044 2.734

0.02 3 58 0.36CMB19062 < 10 < 10 72 < 10 12 12.0 1.0695

0.02 < 2 60 0.35CMB19063 < 10 < 10 65 < 10 22 8.0 1.048 2.733

Page 3 of 5

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Activation Laboratories Ltd. Report: A08-2699

Quality Control

Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P PbAnalyte Symbolppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % ppm % ppm ppm % ppm % ppmUnit Symbol

0.2 0.01 2 10 10 0.5 2 0.01 0.5 1 1 1 0.01 10 1 0.01 10 0.01 5 1 0.001 1 0.001 2Detection LimitAR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICP AR-ICPAnalysis Method

24.4 0.35 11 425GXR-1 Meas 0.8 1360 0.75 3.2 6 7 1100 22.8 < 10 3 0.02 < 10 0.13 776 14 0.084 29 0.037 558325

31.0 3.52 15 750GXR-1 Cert 1.2 1380 0.96 3.3 8 12 1110 23.6 14 4 0.05 8 0.22 852 18 0.052 41 0.065 730 427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.1 2.72 < 10 42GXR-4 Meas 1.4 18 0.92 0.7 15 52 5920 3.14 10 < 1 1.29 47 1.58 133 307 0.115 38 0.111 3993

4.0 7.20 5 1640GXR-4 Cert 1.9 19 1.01 0.9 15 64 6520 3.09 20 0 4.01 65 1.66 155 310 0.564 42 0.120 52 98

18.1 3.62 20 1040GXR-2 Meas 1.0 < 2 0.80 4.8 10 25 80 2.04 10 3 0.54 20 0.53 1050 1 0.259 17 0.055 73714

17.0 16.50 42 2240GXR-2 Cert 1.7 1 0.93 4.1 9 36 76 1.86 37 3 1.37 26 0.85 1007 2 0.556 21 0.105 690 25

0.3 7.06 < 10 905GXR-6 Meas 0.9 < 2 0.17 1.2 15 78 64 5.64 20 < 1 0.88 10 0.40 990 1 0.151 21 0.030 85222

1.3 17.70 10 1300GXR-6 Cert 1.4 0 0.18 1.0 14 96 66 5.58 35 0 1.87 14 0.61 1007 2 0.104 27 0.035 101 330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2640 5.46 2220

OREAS 13P Cert 2500 7.58 2261

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

< 0.2 0.43 < 10 23CMB19062 Orig < 0.5 < 2 3.91 1.2 4 26 7 4.87 < 10 < 1 0.03 37 0.09 656 1 0.128 4 0.078 58

< 0.2 0.43 < 10 22CMB19062 Split < 0.5 < 2 3.70 1.3 10 26 7 4.65 < 10 < 1 0.03 36 0.08 641 < 1 0.095 4 0.077 58

< 0.2 0.58 < 10 28CMB19063 Orig < 0.5 < 2 1.82 0.8 11 41 38 3.49 < 10 < 1 0.09 27 0.20 240 < 1 0.129 5 0.058 55

< 0.2 0.58 < 10 29CMB19063 Split < 0.5 < 2 1.82 0.7 11 41 40 3.51 < 10 < 1 0.09 28 0.20 242 < 1 0.130 5 0.059 56

< 0.2 0.58 < 10 28CMB19063 Orig < 0.5 < 2 1.85 0.8 11 42 39 3.56 < 10 < 1 0.09 28 0.20 245 1 0.131 5 0.060 56

< 0.2 0.57 < 10 27CMB19063 Dup < 0.5 < 2 1.78 0.8 11 40 37 3.42 < 10 < 1 0.09 27 0.20 236 < 1 0.128 6 0.055 55

< 0.2 < 0.01 < 10 < 10Method Blank Method Blank

< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.011 < 1 < 0.001 < 2< 2

Method Blank Method Blank


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Quality Control

S Sb Sc Sr Ti Tl U V W Zn U Mass Spec GravAnalyte Symbol% ppm ppm ppm % ppm ppm ppm ppm ppm ppm g -Unit Symbol


0.19 76 175GXR-1 Meas < 10 36 73 142 6001

0.26 122 275GXR-1 Cert 0 35 80 164 760 2

DH-1a Meas 2760 2650

DH-1a Cert 2629 2629

DH-1a Meas 2600

DH-1a Cert 2629

1.72 5 68GXR-4 Meas < 10 < 10 80 13 647

1.77 5 221GXR-4 Cert 3 6 87 31 73 8

0.04 33 86GXR-2 Meas < 10 < 10 49 < 10 5505

0.03 49 160GXR-2 Cert 1 3 52 2 530 7

0.01 4 32GXR-6 Meas < 10 < 10 169 < 10 11522

0.02 4 35GXR-6 Cert 2 2 186 2 118 28

SY-2 Meas 286

SY-2 Cert 284

SY-2 Meas 286

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10200

BL-3 Cert 10200

BL-4a Meas 1260

BL-4a Cert 1248

0.02 3 58 0.36CMB19062 Orig < 10 < 10 72 < 10 12 12.0 1.0695

0.03 3 58 0.35CMB19062 Split < 10 12 71 < 10 11 12.5 1.0254

0.02 < 2 60 0.35CMB19063 Orig < 10 < 10 65 < 10 22 8.0 1.0483

0.02 2 61 0.35CMB19063 Split < 10 < 10 67 < 10 22 7.7 1.0613

0.02 < 2 61 0.35CMB19063 Orig < 10 < 10 67 < 10 233

0.02 2 60 0.34CMB19063 Dup < 10 < 10 64 < 10 223

< 0.01 < 2 < 1 < 0.01Method Blank Method Blank

< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

Page 5 of 5

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

26-Jun-08

28-May-08

A08-2700



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-2700

Notes:




Quality Control


Document Page 134




0.7 2.64 < 10 800CMB15401 < 0.5 < 2 2.17 0.7 34 764 176 4.01 < 10 < 1 1.13 12 4.04 617 < 1 0.251 297 0.101 73

4.0 1.90 < 10 254CMB15402 < 0.5 < 2 1.62 1.5 42 62 1240 9.17 10 < 1 0.48 < 10 2.01 523 < 1 0.153 42 0.135 1927

1.6 2.10 < 10 134CMB15403 0.7 < 2 2.80 1.4 36 79 446 8.43 10 < 1 0.35 < 10 1.78 676 < 1 0.240 49 0.131 185

< 0.2 0.63 < 10 45CMB15404 < 0.5 < 2 2.69 0.8 10 106 27 4.00 < 10 < 1 0.08 11 0.12 440 < 1 0.128 17 0.025 513

0.3 1.08 < 10 34CMB15405 < 0.5 < 2 2.98 0.6 10 82 21 3.03 < 10 < 1 0.11 11 0.25 457 < 1 0.086 15 0.030 712

0.3 0.65 < 10 107CMB15406 < 0.5 < 2 1.56 0.8 11 113 36 3.81 < 10 < 1 0.06 12 0.17 203 < 1 0.171 21 0.024 3610

0.2 2.65 < 10 303CMB15407 < 0.5 < 2 1.34 1.0 26 308 57 2.91 < 10 < 1 0.92 12 2.79 357 < 1 0.147 198 0.063 13< 2

< 0.2 0.52 < 10 547CMB15408 Received as pulp

< 0.5 < 2 1.17 0.5 10 29 29 2.13 < 10 < 1 0.11 69 0.36 313 4 0.160 43 0.039 1432

0.4 2.71 < 10 297CMB15409 < 0.5 < 2 1.53 0.5 24 290 97 2.73 < 10 < 1 0.79 13 2.54 345 < 1 0.166 177 0.065 473

< 0.2 2.86 < 10 224CMB15410 < 0.5 < 2 1.86 0.6 25 231 186 2.89 < 10 < 1 0.54 13 2.69 406 < 1 0.190 175 0.075 113

< 0.2 3.33 < 10 267CMB15411 < 0.5 < 2 0.90 0.7 36 480 66 3.40 < 10 < 1 1.22 < 10 4.62 376 < 1 0.109 367 0.050 17< 2

< 0.2 0.20 < 10 203CMB15412 < 0.5 < 2 0.75 < 0.5 8 58 1 1.84 < 10 < 1 0.02 21 0.13 72 1 0.181 15 0.016 83

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0.03 4 49 0.22CMB15401 < 10 < 10 143 < 10 120 1.6 1.0547

0.05 4 136 0.41CMB15402 < 10 146 369 < 10 139 129 1.089 2.7811

0.03 4 194 0.36CMB15403 < 10 < 10 183 < 10 120 2.4 1.07116

0.02 3 69 0.30CMB15404 < 10 < 10 120 < 10 11 3.4 1.048 2.714

0.02 4 96 0.30CMB15405 < 10 < 10 115 < 10 20 1.8 1.0416

0.02 2 98 0.33CMB15406 < 10 197 193 < 10 12 190 1.027 2.735

0.02 < 2 152 0.17CMB15407 < 10 49 81 < 10 33 46.9 1.081 2.784


< 10 388 53 < 10 98 407 1.0472

0.02 3 176 0.18CMB15409 < 10 256 96 < 10 31 237 1.0305

0.03 < 2 243 0.15CMB15410 < 10 < 10 80 < 10 27 1.7 1.064 2.796

0.01 3 33 0.12CMB15411 < 10 < 10 66 < 10 30 1.2 1.074 2.734

0.07 < 2 41 0.21CMB15412 < 10 46 41 < 10 9 49.0 1.095< 1

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Quality Control



24.4 0.35 11 425GXR-1 Meas 0.8 1360 0.75 3.2 6 7 1100 22.8 < 10 3 0.02 < 10 0.13 776 14 0.084 29 0.037 558325

31.0 3.52 15 750GXR-1 Cert 1.2 1380 0.96 3.3 8 12 1110 23.6 14 4 0.05 8 0.22 852 18 0.052 41 0.065 730 427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.1 2.72 < 10 42GXR-4 Meas 1.4 18 0.92 0.7 15 52 5920 3.14 10 < 1 1.29 47 1.58 133 307 0.115 38 0.111 3993

4.0 7.20 5 1640GXR-4 Cert 1.9 19 1.01 0.9 15 64 6520 3.09 20 0 4.01 65 1.66 155 310 0.564 42 0.120 52 98

18.1 3.62 20 1040GXR-2 Meas 1.0 < 2 0.80 4.8 10 25 80 2.04 10 3 0.54 20 0.53 1050 1 0.259 17 0.055 73714

17.0 16.50 42 2240GXR-2 Cert 1.7 1 0.93 4.1 9 36 76 1.86 37 3 1.37 26 0.85 1007 2 0.556 21 0.105 690 25

0.3 7.06 < 10 905GXR-6 Meas 0.9 < 2 0.17 1.2 15 78 64 5.64 20 < 1 0.88 10 0.40 990 1 0.151 21 0.030 85222

1.3 17.70 10 1300GXR-6 Cert 1.4 0 0.18 1.0 14 96 66 5.58 35 0 1.87 14 0.61 1007 2 0.104 27 0.035 101 330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2640 5.46 2220

OREAS 13P Cert 2500 7.58 2261

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

CMB15406 Orig

CMB15406 Dup

< 0.2 2.86 < 10 224CMB15410 Orig < 0.5 < 2 1.86 0.6 25 231 186 2.89 < 10 < 1 0.54 13 2.69 406 < 1 0.190 175 0.075 113

< 0.2 2.65 < 10 211CMB15410 Split < 0.5 < 2 1.75 < 0.5 24 216 178 2.72 < 10 < 1 0.51 12 2.54 384 < 1 0.174 165 0.073 93

< 0.2 3.33 < 10 267CMB15411 Orig < 0.5 < 2 0.90 0.7 36 480 66 3.40 < 10 < 1 1.22 < 10 4.62 376 < 1 0.109 367 0.050 17< 2

< 0.2 3.29 < 10 292CMB15411 Split < 0.5 < 2 0.99 0.7 39 517 65 3.71 < 10 < 1 1.33 < 10 5.07 408 < 1 0.106 406 0.055 183

< 0.2 0.21 < 10 200CMB15412 Orig < 0.5 < 2 0.75 < 0.5 8 59 1 1.83 < 10 < 1 0.02 21 0.13 72 1 0.180 16 0.016 83

0.3 0.20 < 10 206CMB15412 Dup < 0.5 < 2 0.75 < 0.5 8 56 1 1.85 < 10 < 1 0.02 21 0.13 72 1 0.183 15 0.016 73


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.011 < 1 < 0.001 < 2< 2



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Quality Control



0.19 76 175GXR-1 Meas < 10 36 73 142 6001

0.26 122 275GXR-1 Cert 0 35 80 164 760 2

DH-1a Meas 2760 2650

DH-1a Cert 2629 2629

DH-1a Meas 2600

DH-1a Cert 2629

1.72 5 68GXR-4 Meas < 10 < 10 80 13 647

1.77 5 221GXR-4 Cert 3 6 87 31 73 8

0.04 33 86GXR-2 Meas < 10 < 10 49 < 10 5505

0.03 49 160GXR-2 Cert 1 3 52 2 530 7

0.01 4 32GXR-6 Meas < 10 < 10 169 < 10 11522

0.02 4 35GXR-6 Cert 2 2 186 2 118 28

SY-2 Meas 286

SY-2 Cert 284

SY-2 Meas 286

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10200

BL-3 Cert 10200

BL-4a Meas 1260

BL-4a Cert 1248

CMB15406 Orig 2.74

CMB15406 Dup 2.71

0.03 < 2 243 0.15CMB15410 Orig < 10 < 10 80 < 10 27 1.7 1.0646

0.03 < 2 231 0.15CMB15410 Split < 10 < 10 77 < 10 26 1.9 1.0225

0.01 3 33 0.12CMB15411 Orig < 10 < 10 66 < 10 30 1.2 1.0744

0.02 3 37 0.13CMB15411 Split < 10 < 10 72 < 10 33 1.2 1.0824

0.07 < 2 41 0.21CMB15412 Orig < 10 47 40 < 10 9< 1

0.07 < 2 41 0.21CMB15412 Dup < 10 46 41 < 10 9< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

26-Jun-08

09-Jun-08

A08-3023



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-3023

Notes:




Quality Control


Document Page 139




< 0.2 1.03 < 10 78CMB15701 < 0.5 < 2 1.65 1.2 13 16 20 5.43 < 10 < 1 0.35 44 0.52 499 1 0.158 15 0.138 910

< 0.2 0.66 < 10 60CMB15702 < 0.5 < 2 1.63 1.1 9 22 6 5.88 < 10 < 1 0.13 41 0.27 360 1 0.207 11 0.143 59

< 0.2 0.96 < 10 627CMB15703 0.7 < 2 2.90 1.2 13 12 < 1 6.04 < 10 < 1 0.27 39 0.79 895 < 1 0.277 13 0.122 129

< 0.2 0.82 < 10 1040CMB15704 1.0 < 2 2.40 1.3 13 13 4 6.51 < 10 < 1 0.23 40 0.75 834 < 1 0.343 13 0.123 349

0.2 0.52 < 10 538CMB15705 < 0.5 < 2 1.79 1.6 12 14 73 5.01 < 10 < 1 0.11 37 0.33 380 2 0.244 9 0.127 907

< 0.2 2.60 < 10 536CMB15706 < 0.5 < 2 2.25 1.4 30 37 21 6.13 10 < 1 0.88 20 1.85 727 < 1 0.337 47 0.099 95

< 0.2 0.59 < 10 106CMB15707 < 0.5 < 2 1.56 1.3 13 13 29 4.79 < 10 < 1 0.17 39 0.31 347 2 0.215 10 0.126 124

< 0.2 0.53 < 10 542CMB15708 0.9 < 2 2.06 2.6 13 10 43 5.05 < 10 < 1 0.08 44 0.37 394 13 0.295 9 0.104 977

< 0.2 0.73 < 10 869CMB15709 1.6 < 2 2.69 1.4 12 14 15 5.78 < 10 < 1 0.17 34 0.71 683 4 0.303 15 0.114 495

< 0.2 1.28 < 10 782CMB15710 1.3 < 2 2.81 0.9 20 26 29 5.55 < 10 < 1 0.34 27 1.28 830 2 0.350 26 0.117 378

< 0.2 0.80 < 10 220CMB15711 2.6 < 2 2.53 1.0 15 16 120 5.96 < 10 < 1 0.26 34 1.01 699 < 1 0.275 22 0.115 119

< 0.2 0.72 < 10 92CMB15712 2.1 < 2 2.22 1.2 13 17 14 6.18 < 10 < 1 0.24 32 0.91 593 < 1 0.229 20 0.113 89

0.6 1.04 < 10 77CMB15713 1.7 < 2 3.05 1.1 23 23 58 5.54 < 10 < 1 0.03 28 0.83 725 < 1 0.186 20 0.116 14710

2.0 1.03 < 10 49CMB15714 1.9 < 2 3.12 0.9 23 19 70 5.34 < 10 < 1 0.03 33 0.81 719 < 1 0.200 19 0.115 20012

< 0.2 0.59 < 10 23CMB15715 0.8 < 2 2.70 1.2 32 15 29 6.03 < 10 < 1 0.03 43 0.31 395 2 0.193 11 0.114 3389

< 0.2 0.78 < 10 272CMB15716 0.8 < 2 3.28 1.7 15 12 149 5.55 < 10 < 1 0.06 39 0.69 671 2 0.192 14 0.108 1136

< 0.2 0.71 < 10 26CMB15717 1.0 < 2 2.90 1.1 13 16 39 6.37 < 10 < 1 0.03 28 0.65 608 < 1 0.159 19 0.113 316

< 0.2 0.80 < 10 23CMB15718 1.3 < 2 3.04 1.1 13 16 37 6.59 < 10 < 1 0.03 32 0.79 693 1 0.214 20 0.116 367

< 0.2 0.72 < 10 56CMB15719 1.6 < 2 2.60 1.1 15 17 8 5.96 < 10 < 1 0.09 29 0.81 637 < 1 0.167 19 0.115 175

0.4 0.92 < 10 109CMB15720 1.8 < 2 2.81 1.1 15 20 51 5.51 10 < 1 0.04 31 0.78 640 < 1 0.206 18 0.104 2656

0.8 0.57 < 10 62CMB15721 3.4 < 2 3.00 1.3 13 18 13 5.47 < 10 < 1 0.03 26 0.62 641 < 1 0.218 18 0.129 2478

< 0.2 0.65 < 10 862CMB15722 2.3 < 2 3.07 1.0 15 16 11 5.66 < 10 < 1 0.05 27 0.72 677 < 1 0.374 18 0.113 308

< 0.2 0.74 < 10 666CMB15723 2.6 < 2 3.38 1.2 14 20 19 5.15 < 10 < 1 0.04 28 0.87 725 < 1 0.342 18 0.109 325

0.3 0.91 < 10 612CMB15724 1.8 < 2 3.46 1.0 15 16 37 5.65 < 10 < 1 0.04 30 0.89 766 1 0.386 19 0.114 1046

< 0.2 1.00 < 10 469CMB15725 1.0 < 2 2.51 1.2 20 24 37 6.33 < 10 < 1 0.08 38 1.09 644 3 0.250 26 0.125 617

0.3 0.96 < 10 565CMB15726 3.0 < 2 3.27 1.2 18 18 65 6.29 < 10 < 1 0.09 33 1.03 655 < 1 0.362 24 0.128 367

< 0.2 1.50 < 10 452CMB15727 2.5 < 2 6.27 1.1 22 44 9 5.98 < 10 < 1 0.22 15 1.63 1010 < 1 0.418 31 0.114 4012

< 0.2 0.81 15 886CMB15728 1.7 < 2 3.91 1.0 16 14 22 5.72 < 10 < 1 0.03 33 0.82 791 < 1 0.428 20 0.122 3610

0.3 0.65 < 10 590CMB15729 1.9 < 2 4.47 0.9 13 7 63 4.99 < 10 < 1 0.02 37 0.68 840 3 0.315 14 0.119 738

< 0.2 2.85 < 10 285CMB15730 < 0.5 < 2 3.38 1.2 30 74 42 4.56 < 10 < 1 0.17 11 2.48 656 2 0.762 65 0.069 3011

0.2 0.87 < 10 812CMB15731 1.9 < 2 4.45 1.3 13 14 61 5.30 < 10 < 1 0.03 27 0.89 821 < 1 0.428 15 0.114 1288

0.5 0.65 < 10 680CMB15732 1.6 < 2 4.71 1.0 11 10 35 4.49 < 10 < 1 0.02 23 0.74 820 < 1 0.345 11 0.119 22710

1.3 0.82 < 10 445CMB15733 1.5 < 2 4.93 0.7 10 11 49 4.12 10 < 1 0.02 22 0.85 752 < 1 0.395 11 0.132 42213


0.5 < 2 1.21 0.6 16 33 37 2.40 < 10 < 1 0.09 92 0.23 340 9 0.147 97 0.033 3382

0.3 0.78 < 10 399CMB15735 1.2 < 2 4.29 0.9 9 13 24 4.38 < 10 < 1 0.02 20 0.76 718 < 1 0.329 12 0.128 11211

0.3 0.81 < 10 424CMB15736 PREP DUPLICATE FOR CMB15735

1.3 < 2 4.40 0.9 9 14 24 4.44 < 10 < 1 0.02 21 0.80 749 < 1 0.347 12 0.129 11512

0.4 0.87 < 10 122CMB15737 1.7 < 2 4.16 0.9 11 15 6 4.91 < 10 < 1 0.02 20 0.84 660 < 1 0.289 17 0.113 1849

< 0.2 1.28 < 10 308CMB15738 1.9 < 2 3.90 0.8 11 10 40 4.54 10 < 1 0.01 26 0.50 519 4 0.204 10 0.108 988

0.8 0.64 < 10 434CMB15739 3.5 < 2 3.43 1.1 16 10 37 5.21 < 10 < 1 0.06 31 0.70 618 3 0.275 15 0.117 3468

0.8 0.61 < 10 468CMB15740 PULP DUPLICATE FOR CMB15739

3.4 < 2 3.32 1.0 14 10 35 5.06 < 10 < 1 0.06 29 0.66 593 3 0.276 13 0.113 3369

< 0.2 0.95 < 10 531CMB15741 1.3 < 2 2.20 1.5 20 14 34 5.39 < 10 < 1 0.29 28 0.97 613 5 0.257 22 0.118 718

< 0.2 1.12 < 10 687CMB15742 0.6 < 2 1.48 0.8 15 14 18 4.54 < 10 < 1 0.49 32 0.95 538 2 0.283 19 0.118 64

< 0.2 1.08 < 10 544CMB15743 0.7 < 2 1.34 0.8 13 13 20 4.19 < 10 < 1 0.50 35 0.91 476 < 1 0.250 17 0.113 102

1.8 0.43 < 10 45CMB15752 < 0.5 < 2 1.34 1.0 10 19 745 4.78 < 10 < 1 0.09 34 0.28 351 1 0.142 11 0.127 73

1.1 0.59 < 10 73CMB15753 < 0.5 < 2 1.49 1.1 11 20 446 4.81 < 10 < 1 0.15 34 0.43 328 < 1 0.156 11 0.130 83

0.2 2.44 < 10 308CMB15754 < 0.5 < 2 2.74 1.0 29 63 188 4.72 < 10 < 1 0.90 35 2.48 718 < 1 0.293 22 0.168 139

< 0.2 0.44 < 10 54CMB15755 < 0.5 < 2 1.50 1.4 12 16 122 4.94 < 10 < 1 0.09 35 0.23 272 2 0.144 13 0.135 187

< 0.2 0.65 < 10 111CMB15756 < 0.5 < 2 1.90 1.1 14 18 94 4.46 < 10 < 1 0.15 42 0.38 319 1 0.146 14 0.134 2310

< 0.2 2.74 < 10 370CMB15757 < 0.5 < 2 2.63 0.9 33 67 79 4.64 < 10 < 1 0.77 < 10 2.52 648 < 1 0.355 67 0.076 74

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< 0.2 0.50 < 10 49CMB15758 < 0.5 < 2 1.54 0.9 10 19 257 4.58 < 10 < 1 0.07 38 0.24 256 2 0.169 10 0.126 84

< 0.2 0.36 < 10 37CMB15759 < 0.5 < 2 1.37 0.8 8 15 247 4.33 < 10 < 1 0.05 37 0.14 214 2 0.129 8 0.121 64

< 0.2 2.06 < 10 268CMB15760 < 0.5 < 2 2.48 0.8 23 53 194 4.15 < 10 < 1 0.64 37 2.08 632 < 1 0.247 20 0.171 66

< 0.2 1.01 34 83CMB15761 < 0.5 < 2 1.70 1.2 16 20 129 5.11 < 10 < 1 0.19 37 0.69 508 2 0.214 19 0.119 175

< 0.2 2.87 < 10 204CMB15762 < 0.5 < 2 2.79 1.0 30 66 57 4.71 < 10 < 1 0.44 < 10 2.36 597 < 1 0.343 65 0.079 183

< 0.2 1.25 79 97CMB15763 < 0.5 < 2 1.80 0.8 14 21 205 4.62 < 10 < 1 0.30 40 0.91 520 1 0.173 16 0.127 45

0.5 1.21 < 10 179CMB15764 < 0.5 < 2 1.17 1.1 14 15 560 5.40 < 10 < 1 0.63 41 0.95 577 1 0.149 16 0.124 53

0.4 0.90 < 10 114CMB15765 < 0.5 < 2 1.31 1.1 15 18 360 5.31 < 10 < 1 0.38 39 0.68 530 1 0.149 15 0.131 64

< 0.2 0.38 < 10 74CMB15766 < 0.5 < 2 1.19 < 0.5 6 48 29 1.66 < 10 < 1 0.08 23 0.38 165 2 0.157 13 0.024 212

1.3 0.92 < 10 79CMB15767 < 0.5 < 2 1.60 1.3 14 19 907 5.19 < 10 < 1 0.27 40 0.71 578 2 0.165 15 0.128 122

< 0.2 1.15 < 10 97CMB15768 < 0.5 < 2 1.90 1.1 15 22 60 4.69 < 10 < 1 0.33 39 0.83 599 2 0.164 15 0.132 234

< 0.2 2.28 < 10 286CMB15769 < 0.5 < 2 2.44 0.9 28 61 77 4.86 < 10 < 1 0.89 36 2.31 662 < 1 0.248 25 0.173 167

< 0.2 1.35 < 10 144CMB15770 < 0.5 < 2 1.29 1.6 14 13 66 5.00 10 < 1 0.55 42 1.05 603 < 1 0.155 17 0.130 52

< 0.2 0.58 < 10 38CMB15771 < 0.5 < 2 1.49 1.1 11 16 53 4.64 < 10 < 1 0.14 37 0.40 424 1 0.136 13 0.126 283

0.2 1.45 < 10 180CMB15772 < 0.5 < 2 1.69 1.1 15 13 140 5.38 < 10 < 1 0.65 40 1.07 676 2 0.186 16 0.119 157

0.6 1.09 < 10 99CMB15773 < 0.5 < 2 1.57 0.9 14 14 251 4.90 < 10 < 1 0.50 39 0.77 446 1 0.142 14 0.125 257

< 0.2 0.84 < 10 81CMB15774 < 0.5 < 2 1.76 0.9 9 14 24 4.45 < 10 < 1 0.36 40 0.49 481 < 1 0.112 9 0.130 284

< 0.2 1.70 < 10 327CMB15775 < 0.5 < 2 1.58 1.2 28 40 63 5.71 < 10 < 1 0.62 22 1.47 510 1 0.221 28 0.113 104

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0.05 2 53 0.26CMB15701 < 10 < 10 49 < 10 71 8.20 1.0617

0.02 3 61 0.26CMB15702 < 10 < 10 52 < 10 37 5.10 1.018 2.775

0.03 3 83 0.28CMB15703 < 10 32 80 < 10 102 36.2 1.0607

0.04 4 76 0.28CMB15704 < 10 109 130 < 10 143 114 1.0418

0.08 3 61 0.24CMB15705 < 10 70 95 < 10 160 74.4 1.0194

0.07 < 2 109 0.30CMB15706 < 10 < 10 100 < 10 202 5.50 1.034 2.8211

0.10 2 53 0.23CMB15707 < 10 < 10 50 < 10 92 10.3 1.0114

0.11 2 94 0.28CMB15708 < 10 121 118 < 10 317 130 1.0565

0.05 2 128 0.26CMB15709 < 10 139 132 < 10 117 145 1.0768

0.08 3 152 0.27CMB15710 < 10 < 10 94 < 10 156 8.50 1.0608

0.03 3 84 0.32CMB15711 < 10 < 10 235 < 10 87 12.7 1.0719

0.02 3 66 0.29CMB15712 < 10 27 194 < 10 63 29.9 1.0517

0.08 < 2 167 0.28CMB15713 < 10 108 159 < 10 52 114 1.0347

0.08 < 2 163 0.31CMB15714 < 10 210 160 < 10 53 216 1.0707

0.20 < 2 99 0.32CMB15715 < 10 42 118 < 10 86 45.6 1.0225

0.11 2 100 0.27CMB15716 < 10 53 135 < 10 192 55.7 1.0906

0.03 3 106 0.23CMB15717 < 10 65 124 < 10 51 68.2 1.0956

0.02 2 88 0.26CMB15718 < 10 54 138 < 10 60 54.6 1.0447

0.02 2 79 0.24CMB15719 < 10 47 219 < 10 70 50.7 1.0907

0.03 2 151 0.27CMB15720 < 10 612 256 < 10 72 628 1.067 2.817

0.02 2 98 0.26CMB15721 < 10 1080 347 < 10 87 1060 1.0736

0.04 3 111 0.25CMB15722 < 10 110 168 < 10 70 115 1.0297

0.04 2 102 0.24CMB15723 < 10 133 201 < 10 75 140 1.0817

0.04 2 126 0.26CMB15724 < 10 425 261 < 10 77 432 1.0068

0.03 < 2 81 0.25CMB15725 < 10 134 186 < 10 102 137 1.0579

0.04 < 2 104 0.25CMB15726 < 10 113 189 < 10 107 117 1.0089

0.05 < 2 271 0.22CMB15727 < 10 138 265 < 10 147 149 1.00911

0.05 3 150 0.24CMB15728 < 10 127 146 < 10 103 132 1.043 2.808

0.09 2 159 0.18CMB15729 < 10 216 155 < 10 96 222 1.0887

0.10 < 2 53 0.21CMB15730 < 10 37 109 < 10 77 37.5 1.08313

0.06 2 175 0.21CMB15731 < 10 227 152 < 10 168 242 1.0498

0.05 < 2 184 0.18CMB15732 < 10 644 73 < 10 87 689 1.0836

0.04 < 2 214 0.19CMB15733 < 10 1380 63 < 10 81 1390 1.0727

0.08 3 77 0.17CMB15734 Received as pulp

< 10 1010 77 < 10 92 995 1.0852

0.04 < 2 155 0.19CMB15735 < 10 361 59 < 10 69 389 1.0277

0.04 < 2 160 0.19CMB15736 PREP DUPLICATE FOR CMB15735

< 10 362 61 < 10 72 383 1.0598

0.04 3 149 0.21CMB15737 < 10 685 76 < 10 77 735 1.0498

0.07 < 2 500 0.21CMB15738 < 10 305 83 < 10 55 339 1.0296

0.13 < 2 170 0.23CMB15739 < 10 1020 100 < 10 158 1020 1.0396

0.13 < 2 165 0.22CMB15740 PULP DUPLICATE FOR CMB15739

< 10 980 97 < 10 154 1020 1.0136

0.13 3 85 0.21CMB15741 < 10 18 63 < 10 218 21.0 1.0827

0.05 2 38 0.23CMB15742 < 10 < 10 59 < 10 90 4.20 1.065 2.786

0.04 < 2 36 0.23CMB15743 < 10 < 10 56 < 10 115 4.00 1.050 2.826

0.09 3 19 0.20CMB15752 < 10 < 10 65 < 10 77 3.70 1.0125

0.06 2 39 0.21CMB15753 < 10 < 10 72 < 10 70 4.20 1.0495

0.06 2 131 0.21CMB15754 < 10 < 10 134 < 10 144 3.60 1.04315

0.06 < 2 59 0.25CMB15755 < 10 < 10 68 < 10 106 11.8 1.0142

0.08 3 60 0.36CMB15756 < 10 21 68 < 10 79 28.8 1.0953

0.13 2 26 0.25CMB15757 < 10 < 10 108 < 10 66 0.30 1.04412

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0.06 < 2 46 0.24CMB15758 < 10 < 10 64 < 10 41 5.20 1.0604

0.04 2 40 0.23CMB15759 < 10 < 10 59 < 10 36 4.30 1.0763

0.05 < 2 78 0.20CMB15760 < 10 < 10 118 < 10 94 3.50 1.03513

0.07 2 39 0.25CMB15761 < 10 < 10 69 < 10 106 3.20 1.0548

0.12 < 2 45 0.22CMB15762 < 10 < 10 106 < 10 81 0.40 1.04112

0.04 3 65 0.24CMB15763 < 10 < 10 66 < 10 75 3.60 1.0538

0.07 2 34 0.26CMB15764 < 10 < 10 64 < 10 115 4.00 1.0539

0.05 < 2 24 0.25CMB15765 < 10 < 10 71 < 10 96 3.90 1.0148

0.09 < 2 48 0.22CMB15766 < 10 < 10 39 < 10 59 8.10 1.0872

0.12 < 2 18 0.22CMB15767 < 10 < 10 62 < 10 95 3.70 1.0888

0.04 < 2 44 0.21CMB15768 < 10 < 10 63 < 10 98 3.40 1.0488

0.17 < 2 56 0.23CMB15769 < 10 < 10 134 < 10 147 3.20 1.08615

0.02 < 2 20 0.23CMB15770 < 10 < 10 59 < 10 334 3.20 1.0739

0.02 < 2 12 0.20CMB15771 < 10 < 10 62 < 10 139 3.50 1.0657

0.03 3 21 0.28CMB15772 < 10 < 10 61 < 10 390 3.90 1.0639

0.05 2 25 0.25CMB15773 < 10 < 10 81 < 10 212 4.00 1.0807

0.02 < 2 28 0.24CMB15774 < 10 < 10 55 < 10 106 4.70 1.0765

0.21 < 2 23 0.27CMB15775 < 10 < 10 98 < 10 90 1.70 1.0329

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Quality Control



26.5 0.32 14 157GXR-1 Meas 0.8 1490 0.79 3.3 8 6 1130 24.2 < 10 3 0.02 < 10 0.13 785 15 0.052 37 0.036 575351

31.0 3.52 15 750GXR-1 Cert 1.2 1380 0.96 3.3 8 12 1110 23.6 14 4 0.05 8 0.22 852 18 0.052 41 0.065 730 427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.5 2.89 < 10 24GXR-4 Meas 1.5 25 0.99 0.8 16 57 6450 3.46 10 < 1 1.40 40 1.75 144 336 0.115 42 0.119 4399

4.0 7.20 5 1640GXR-4 Cert 1.9 19 1.01 0.9 15 64 6520 3.09 20 0 4.01 65 1.66 155 310 0.564 42 0.120 52 98

17.0 3.33 18 1210GXR-2 Meas 1.0 < 2 0.79 4.5 9 23 74 1.96 < 10 3 0.50 19 0.51 980 < 1 0.261 16 0.052 69115

17.0 16.50 42 2240GXR-2 Cert 1.7 1 0.93 4.1 9 36 76 1.86 37 3 1.37 26 0.85 1007 2 0.556 21 0.105 690 25

0.3 7.53 < 10 875GXR-6 Meas 0.9 < 2 0.16 0.9 15 81 71 6.31 20 < 1 0.87 < 10 0.41 1040 1 0.158 25 0.031 90218

1.3 17.70 10 1300GXR-6 Cert 1.4 0 0.18 1.0 14 96 66 5.58 35 0 1.87 14 0.61 1007 2 0.104 27 0.035 101 330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2730 5.60 2280

OREAS 13P Cert 2500 7.58 2261

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

0.6 1.06 < 10 78CMB15713 Orig 1.7 < 2 3.05 1.1 22 23 59 5.54 < 10 < 1 0.03 28 0.83 726 < 1 0.192 20 0.116 14910

0.5 1.01 < 10 76CMB15713 Dup 1.7 < 2 3.06 1.1 23 23 57 5.54 < 10 < 1 0.03 28 0.83 724 < 1 0.180 20 0.115 14610

< 0.2 1.46 < 10 452CMB15727 Orig 2.5 < 2 6.28 0.9 22 44 9 6.01 < 10 < 1 0.23 15 1.62 1010 < 1 0.407 31 0.114 3912

< 0.2 1.53 < 10 452CMB15727 Dup 2.5 < 2 6.26 1.2 22 44 8 5.95 < 10 < 1 0.22 15 1.63 1010 < 1 0.430 30 0.114 4012

< 0.2 2.85 < 10 285CMB15730 Orig < 0.5 < 2 3.38 1.2 30 74 42 4.56 < 10 < 1 0.17 11 2.48 656 2 0.762 65 0.069 3011

< 0.2 2.84 < 10 283CMB15730 Split < 0.5 < 2 3.35 0.8 32 74 43 4.56 < 10 < 1 0.17 12 2.43 649 1 0.764 65 0.069 2911

< 0.2 2.06 < 10 268CMB15760 Orig < 0.5 < 2 2.48 0.8 23 53 194 4.15 < 10 < 1 0.64 37 2.08 632 < 1 0.247 20 0.171 66

< 0.2 2.24 < 10 299CMB15760 Split < 0.5 < 2 2.73 0.9 26 58 192 4.58 < 10 < 1 0.68 37 2.29 697 < 1 0.293 21 0.175 75

< 0.2 2.93 < 10 209CMB15762 Orig < 0.5 < 2 2.81 1.1 29 67 59 4.85 < 10 < 1 0.45 < 10 2.38 605 < 1 0.349 66 0.080 173

< 0.2 2.82 < 10 199CMB15762 Dup < 0.5 < 2 2.77 0.8 32 66 56 4.58 < 10 < 1 0.43 < 10 2.35 589 < 1 0.336 64 0.079 183

< 0.2 1.35 < 10 144CMB15770 Orig < 0.5 < 2 1.29 1.6 14 13 66 5.00 10 < 1 0.55 42 1.05 603 < 1 0.155 17 0.130 52

< 0.2 1.49 < 10 155CMB15770 Split < 0.5 < 2 1.36 1.1 15 15 73 5.33 < 10 < 1 0.59 44 1.12 640 < 1 0.170 17 0.137 62

< 0.2 1.70 < 10 327CMB15775 Orig < 0.5 < 2 1.58 1.2 28 40 63 5.71 < 10 < 1 0.62 22 1.47 510 1 0.221 28 0.113 104

< 0.2 1.78 < 10 333CMB15775 Split < 0.5 < 2 1.65 1.3 30 40 67 5.98 < 10 < 1 0.64 23 1.52 525 1 0.236 27 0.116 105

0.8 0.60 < 10 470CMB15740 PULP DUPLICATE FOR CMB15739 Orig

3.4 < 2 3.32 1.0 14 10 36 5.05 < 10 < 1 0.06 30 0.67 593 3 0.277 14 0.113 3388

0.8 0.61 < 10 465CMB15740 PULP DUPLICATE FOR CMB15739 Dup

3.4 < 2 3.32 1.0 13 10 35 5.06 < 10 < 1 0.06 29 0.66 594 3 0.276 13 0.113 3349


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.010 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.009 < 1 < 0.001 < 2< 2



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Quality Control



0.20 80 145GXR-1 Meas < 10 32 78 139 6431

0.26 122 275GXR-1 Cert 0 35 80 164 760 2

DH-1a Meas 2620

DH-1a Cert 2629

DH-1a Meas 2640

DH-1a Cert 2629

1.88 3 66GXR-4 Meas < 10 < 10 87 13 677

1.77 5 221GXR-4 Cert 3 6 87 31 73 8

0.03 32 89GXR-2 Meas < 10 < 10 46 < 10 5095

0.03 49 160GXR-2 Cert 1 3 52 2 530 7

0.02 3 30GXR-6 Meas < 10 < 10 175 < 10 11622

0.02 4 35GXR-6 Cert 2 2 186 2 118 28

SY-2 Meas 283

SY-2 Cert 284

SY-2 Meas 281

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-4a Meas 1270

BL-4a Cert 1248

BL-4a Meas 1250

BL-4a Cert 1248

0.08 2 168 0.28CMB15713 Orig < 10 109 159 < 10 527

0.08 < 2 165 0.28CMB15713 Dup < 10 108 158 < 10 527

0.05 2 272 0.22CMB15727 Orig < 10 138 264 < 10 14811

0.05 < 2 270 0.22CMB15727 Dup < 10 138 265 < 10 14511

0.10 < 2 53 0.21CMB15730 Orig < 10 37 109 < 10 77 37.5 1.08313

0.11 < 2 53 0.22CMB15730 Split < 10 36 108 < 10 77 37.8 1.07713

0.05 < 2 78 0.20CMB15760 Orig < 10 < 10 118 < 10 94 3.50 1.03513

0.05 2 94 0.22CMB15760 Split < 10 < 10 130 < 10 101 2.9 1.04415

0.12 3 45 0.23CMB15762 Orig < 10 < 10 107 < 10 8112

0.12 < 2 45 0.22CMB15762 Dup < 10 < 10 105 < 10 8012

0.02 < 2 20 0.23CMB15770 Orig < 10 < 10 59 < 10 334 3.20 1.0739

0.02 < 2 22 0.25CMB15770 Split < 10 < 10 62 < 10 371 3.4 1.0499

0.21 < 2 23 0.27CMB15775 Orig < 10 < 10 98 < 10 90 1.70 1.0329

0.22 2 24 0.29CMB15775 Split < 10 < 10 101 < 10 93 1.7 1.06310

0.13 2 164 0.22CMB15740 PULP DUPLICATE FOR CMB15739 Orig

< 10 983 97 < 10 1556

0.12 < 2 166 0.21CMB15740 PULP DUPLICATE FOR CMB15739 Dup

< 10 977 96 < 10 1536


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

26-Jun-08

09-Jun-08

A08-3026



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-3026

Notes:

3 Pulp samples and 107 Rock samples were submitted for analysis.



Quality Control


Document Page 146




< 0.2 2.16 < 10 177CMB15119 0.5 < 2 1.96 < 0.5 24 32 220 4.34 10 < 1 0.19 20 2.00 851 < 1 0.082 20 0.155 1117

< 0.2 2.05 < 10 90CMB15120 < 0.5 < 2 1.93 < 0.5 29 46 458 4.58 10 < 1 0.04 16 2.16 913 < 1 0.068 24 0.148 246

< 0.2 0.19 < 10 24CMB15121 < 0.5 < 2 0.86 < 0.5 5 71 3 2.43 < 10 < 1 0.02 26 0.07 71 < 1 0.156 16 0.029 < 23

< 0.2 2.14 < 10 95CMB15122 < 0.5 < 2 2.61 0.5 25 43 407 4.71 < 10 < 1 0.07 16 2.07 857 < 1 0.084 22 0.150 196

0.3 2.45 < 10 88CMB15123 0.5 < 2 1.95 0.7 31 54 317 5.14 10 < 1 0.10 18 2.77 1060 < 1 0.085 32 0.158 134

< 0.2 2.47 < 10 112CMB15124 0.7 < 2 2.03 0.6 32 90 204 5.06 10 < 1 0.11 19 2.80 1120 < 1 0.072 45 0.127 123


< 0.5 < 2 1.19 < 0.5 9 31 34 2.40 < 10 < 1 0.13 79 0.37 333 4 0.107 53 0.050 168< 2

< 0.2 2.51 < 10 109CMB15126 PULP DUPLICATE FOR CMB15124

0.6 < 2 1.95 0.5 31 87 205 4.86 < 10 < 1 0.09 18 2.85 1090 < 1 0.062 45 0.125 124

< 0.2 2.49 < 10 107CMB15127 PREP DUPLICATE FOR CMB15124

0.7 < 2 1.96 < 0.5 31 84 204 4.84 < 10 < 1 0.09 18 2.75 1110 < 1 0.060 45 0.126 104

0.2 0.44 < 10 76CMB15128 < 0.5 < 2 1.45 0.8 10 19 101 4.62 < 10 < 1 0.10 34 0.27 245 2 0.168 13 0.130 95

< 0.2 2.60 < 10 227CMB15129 < 0.5 < 2 2.90 0.6 31 77 102 4.58 < 10 < 1 0.37 < 10 2.39 571 13 0.510 69 0.074 74

< 0.2 0.86 < 10 311CMB15130 0.7 < 2 1.94 1.0 20 25 83 5.89 < 10 < 1 0.35 29 0.67 423 < 1 0.239 25 0.127 156

0.2 1.52 < 10 522CMB15131 0.9 < 2 2.66 0.9 29 59 73 5.67 < 10 < 1 0.29 16 1.42 603 < 1 0.388 45 0.098 3210

0.8 1.29 < 10 147CMB15132 1.5 < 2 3.88 2.2 31 74 189 5.04 < 10 < 1 0.14 < 10 1.12 584 1 0.380 37 0.082 1689

1.0 1.51 < 10 429CMB15133 1.6 < 2 4.84 0.8 24 37 74 5.38 10 < 1 0.27 11 1.37 734 2 0.409 23 0.111 2989

< 0.2 1.46 < 10 312CMB15134 1.0 < 2 5.74 0.6 13 8 15 4.10 10 < 1 0.22 23 1.43 721 < 1 0.383 12 0.130 5214

< 0.2 0.65 < 10 866CMB15135 1.5 < 2 2.37 0.7 14 16 49 5.34 < 10 < 1 0.23 24 0.65 590 < 1 0.240 21 0.122 316

< 0.2 0.70 < 10 937CMB15136 2.0 < 2 2.45 1.0 16 16 72 5.65 < 10 < 1 0.13 24 0.88 683 < 1 0.358 20 0.122 305

< 0.2 0.71 < 10 776CMB15137 1.4 < 2 3.19 1.0 15 16 66 5.39 < 10 < 1 0.14 24 0.76 709 < 1 0.312 20 0.117 423

< 0.2 0.62 < 10 946CMB15138 2.4 < 2 2.58 1.0 15 16 53 5.53 < 10 < 1 0.14 24 0.73 617 < 1 0.306 21 0.128 317

< 0.2 0.60 < 10 830CMB15139 1.6 < 2 2.74 0.7 15 16 36 5.17 < 10 < 1 0.12 24 0.69 573 8 0.302 19 0.119 326

< 0.2 0.65 < 10 719CMB15140 1.5 < 2 2.97 0.9 19 18 39 5.46 < 10 < 1 0.14 27 0.64 598 4 0.278 23 0.131 527

< 0.2 0.60 < 10 423CMB15141 1.2 < 2 2.29 0.7 18 20 28 6.00 < 10 < 1 0.19 28 0.48 493 1 0.224 24 0.127 106

< 0.2 2.43 < 10 1210CMB15142 0.6 < 2 3.05 0.7 27 52 47 4.80 < 10 < 1 1.04 33 2.51 635 1 0.458 20 0.179 77

< 0.2 1.10 < 10 282CMB15143 0.9 < 2 4.28 0.7 11 13 22 3.47 < 10 < 1 0.05 27 0.98 476 < 1 0.428 15 0.121 4410

0.3 1.36 < 10 217CMB15144 1.0 < 2 3.81 0.6 11 22 94 3.26 < 10 < 1 0.06 26 1.17 443 < 1 0.510 16 0.129 2613

< 0.2 1.23 < 10 294CMB15145 1.2 < 2 4.05 0.9 10 15 61 3.23 < 10 < 1 0.05 28 1.06 453 < 1 0.492 14 0.138 8212

< 0.2 2.87 12 260CMB15146 < 0.5 < 2 4.04 0.7 26 65 59 5.02 < 10 < 1 0.11 < 10 2.47 630 < 1 0.848 51 0.087 4412

< 0.2 1.64 < 10 598CMB15147 1.3 < 2 5.23 0.8 11 10 13 3.76 10 < 1 0.05 28 1.38 618 < 1 0.604 13 0.130 2220

0.4 1.45 < 10 284CMB15148 1.2 < 2 4.99 0.7 10 11 121 3.66 10 < 1 0.05 26 1.24 657 < 1 0.556 12 0.122 2516

1.9 1.37 < 10 242CMB15149 1.1 < 2 5.51 1.2 10 9 560 3.64 < 10 < 1 0.04 26 1.18 801 1 0.516 11 0.119 4916

0.2 1.28 < 10 538CMB15150 1.0 < 2 7.10 0.9 10 8 57 4.00 < 10 < 1 0.08 21 1.35 963 < 1 0.528 12 0.104 2520

< 0.2 1.01 < 10 156CMB15161 0.6 < 2 2.61 0.5 20 24 12 5.65 < 10 < 1 0.19 25 0.78 532 < 1 0.142 22 0.117 45

< 0.2 0.36 < 10 94CMB15162 < 0.5 < 2 3.25 0.6 18 16 17 4.95 < 10 < 1 0.02 29 0.16 354 5 0.097 7 0.120 36

< 0.2 0.32 < 10 16CMB15163 < 0.5 < 2 2.75 0.6 15 18 20 5.53 < 10 < 1 0.02 29 0.18 318 2 0.111 11 0.126 76

< 0.2 0.69 < 10 121CMB15164 0.5 < 2 2.72 0.6 27 16 63 5.83 < 10 < 1 0.26 26 0.76 563 < 1 0.084 19 0.120 88

< 0.2 0.61 < 10 50CMB15165 0.8 < 2 2.36 0.8 14 19 15 6.26 < 10 < 1 0.10 32 0.58 488 4 0.168 20 0.129 48

0.4 0.59 < 10 97CMB15166 1.1 < 2 3.19 0.7 22 16 30 5.87 < 10 < 1 0.05 29 0.54 541 3 0.140 16 0.126 267

< 0.2 0.86 < 10 89CMB15167 1.0 < 2 3.42 0.7 14 18 44 5.91 10 < 1 0.02 35 0.89 631 1 0.139 21 0.117 784

< 0.2 0.89 < 10 122CMB15168 1.3 < 2 3.54 0.6 12 17 72 5.95 10 < 1 0.02 36 0.91 652 < 1 0.133 19 0.117 895

< 0.2 0.84 < 10 519CMB15169 1.1 < 2 2.97 0.9 17 16 29 6.06 < 10 < 1 0.05 40 0.94 651 2 0.182 21 0.113 525

0.3 0.69 < 10 736CMB15170 1.4 < 2 3.84 0.9 18 16 51 5.92 < 10 < 1 0.03 32 0.83 655 2 0.186 21 0.115 1996

1.4 0.62 < 10 438CMB15171 1.9 < 2 3.76 0.7 18 16 45 5.85 10 < 1 0.02 28 0.72 586 2 0.188 19 0.118 373< 2

< 0.2 0.45 < 10 30CMB15172 1.4 < 2 1.36 < 0.5 8 42 14 3.05 < 10 < 1 0.25 31 0.63 267 < 1 0.157 12 0.072 204

0.7 1.86 < 10 309CMB15173 2.2 < 2 4.10 0.8 28 55 42 6.02 10 < 1 0.29 16 1.72 754 1 0.403 36 0.114 2706

< 0.2 2.45 < 10 309CMB15174 < 0.5 < 2 3.20 0.8 30 63 28 5.58 < 10 < 1 0.33 < 10 2.31 782 < 1 0.510 41 0.102 93

< 0.2 2.46 < 10 428CMB15175 < 0.5 < 2 3.17 0.7 39 60 202 5.70 < 10 < 1 0.32 < 10 2.28 833 < 1 0.539 38 0.102 126

< 0.2 1.07 < 10 357CMB15176 1.0 < 2 2.70 0.7 22 29 39 5.67 < 10 < 1 0.22 24 1.01 567 2 0.255 22 0.118 166

0.2 0.75 < 10 319CMB15177 1.5 < 2 2.69 1.8 22 15 34 5.99 < 10 < 1 0.29 30 0.87 540 1 0.165 19 0.129 229

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< 0.2 0.83 < 10 570CMB15178 0.9 < 2 2.14 0.7 17 17 22 5.76 < 10 < 1 0.35 30 0.88 588 1 0.188 20 0.129 138

< 0.2 0.77 < 10 138CMB15179 0.8 < 2 2.24 0.7 14 17 33 5.25 < 10 < 1 0.21 33 0.61 529 1 0.176 17 0.133 116

< 0.2 0.62 < 10 114CMB15180 0.7 < 2 1.89 0.7 13 19 38 5.41 < 10 < 1 0.19 31 0.51 411 < 1 0.145 15 0.133 114

< 0.2 0.81 < 10 169CMB15181 1.0 < 2 2.07 0.7 15 18 26 5.46 < 10 < 1 0.28 32 0.80 559 1 0.167 17 0.129 365

0.2 0.73 < 10 158CMB15182 1.2 < 2 2.68 0.7 15 17 48 5.62 < 10 < 1 0.21 33 0.69 551 8 0.153 15 0.126 497

< 0.2 0.66 < 10 65CMB15183 0.8 < 2 2.29 0.7 13 17 71 4.56 < 10 1 0.11 34 0.50 444 2 0.151 11 0.121 96

< 0.2 1.22 < 10 160CMB15184 0.6 < 2 1.76 < 0.5 15 17 53 4.65 < 10 < 1 0.50 41 0.88 541 2 0.174 17 0.136 43

< 0.2 0.53 < 10 59CMB15185 < 0.5 < 2 1.33 0.7 12 18 39 4.35 < 10 < 1 0.09 34 0.38 292 1 0.114 11 0.127 66


< 0.5 < 2 1.18 < 0.5 9 30 31 2.41 < 10 < 1 0.13 79 0.35 328 5 0.104 52 0.051 172< 2

< 0.2 1.14 < 10 391CMB15187 < 0.5 < 2 0.91 0.8 20 20 64 6.04 < 10 < 1 0.65 36 0.85 371 1 0.087 18 0.131 734

< 0.2 1.10 < 10 381CMB15188 < 0.5 < 2 0.90 0.9 19 20 51 5.68 < 10 < 1 0.63 35 0.84 366 1 0.084 17 0.129 184

< 0.2 1.84 < 10 182CMB15189 < 0.5 < 2 1.35 0.8 18 17 30 5.73 10 < 1 1.05 43 1.14 632 < 1 0.121 21 0.132 204

< 0.2 2.54 < 10 639CMB15190 < 0.5 < 2 1.10 0.7 18 14 30 5.91 10 < 1 1.54 40 1.65 652 < 1 0.129 20 0.118 15< 2

< 0.2 1.28 < 10 352CMB15191 0.5 < 2 1.70 0.6 18 22 46 4.47 < 10 < 1 0.56 35 0.78 487 1 0.149 18 0.133 175

< 0.2 0.95 < 10 109CMB15192 < 0.5 < 2 1.76 1.1 16 16 44 4.98 < 10 < 1 0.43 38 0.69 499 1 0.162 16 0.131 1813

0.2 0.69 < 10 157CMB15193 < 0.5 < 2 2.04 1.4 15 17 51 5.09 < 10 < 1 0.35 29 0.49 489 < 1 0.122 17 0.124 3215

0.6 0.88 < 10 897CMB15194 1.8 < 2 3.68 1.3 10 13 61 4.80 < 10 < 1 0.19 37 0.72 682 < 1 0.275 10 0.106 1868

1.1 0.53 < 10 847CMB15195 1.5 < 2 2.44 0.7 8 7 55 5.59 < 10 < 1 0.06 38 0.49 576 < 1 0.254 6 0.124 2917

0.9 1.11 < 10 425CMB15196 1.2 < 2 4.47 0.7 16 34 65 4.92 < 10 < 1 0.04 17 1.04 566 1 0.408 20 0.104 26412

0.7 0.97 < 10 1020CMB15197 1.6 < 2 3.33 0.9 13 15 75 5.48 < 10 < 1 0.24 27 0.96 642 < 1 0.319 17 0.121 2837

< 0.2 1.27 < 10 792CMB15198 0.9 < 2 1.91 0.7 19 18 53 6.00 < 10 < 1 0.77 32 1.12 589 < 1 0.197 25 0.125 164

< 0.2 0.84 < 10 170CMB15199 0.7 < 2 1.62 0.7 15 17 39 5.09 < 10 < 1 0.35 34 0.57 462 < 1 0.180 20 0.128 134

< 0.2 1.11 < 10 211CMB15200 0.8 < 2 1.78 0.7 15 17 23 4.61 < 10 < 1 0.44 36 0.82 481 < 1 0.215 18 0.129 144

< 0.2 1.16 < 10 681CMB15413 1.2 < 2 4.38 0.7 12 18 13 3.74 < 10 < 1 0.07 21 1.06 557 1 0.466 17 0.115 429

< 0.2 0.11 < 10 101CMB15414 < 0.5 < 2 0.87 < 0.5 5 62 < 1 2.41 < 10 < 1 < 0.01 23 0.05 58 2 0.103 15 0.027 3< 2

< 0.2 0.93 < 10 697CMB15415 1.4 < 2 4.08 0.7 12 14 15 4.44 < 10 < 1 0.05 24 0.89 536 < 1 0.467 15 0.105 377

< 0.2 1.12 < 10 572CMB15416 1.4 < 2 4.51 0.9 10 12 4 4.03 < 10 < 1 0.04 25 1.03 603 1 0.524 12 0.120 2210

< 0.2 0.89 < 10 532CMB15417 1.8 < 2 4.25 0.7 11 14 12 4.90 < 10 < 1 0.04 24 0.86 580 < 1 0.447 14 0.129 298

< 0.2 0.85 < 10 780CMB15418 1.6 < 2 4.25 0.8 12 13 7 4.85 < 10 < 1 0.08 23 0.89 648 1 0.408 14 0.121 308

< 0.2 1.27 < 10 913CMB15419 1.9 < 2 4.61 1.0 14 17 42 4.68 < 10 < 1 0.16 27 1.28 731 2 0.501 17 0.118 467

0.3 1.43 < 10 914CMB15420 1.5 < 2 4.94 0.7 14 25 68 3.94 < 10 < 1 0.16 26 1.39 696 2 0.553 15 0.132 3210

0.3 1.35 < 10 543CMB15421 1.6 < 2 4.64 2.8 13 22 48 4.11 < 10 < 1 0.15 26 1.29 728 2 0.475 12 0.135 779

0.2 0.97 < 10 312CMB15422 3.6 < 2 3.53 2.1 21 10 140 5.05 < 10 < 1 0.10 36 0.86 674 8 0.373 15 0.121 3110

< 0.2 1.02 < 10 337CMB15423 1.7 < 2 3.04 0.8 15 14 33 3.85 < 10 < 1 0.07 33 0.72 537 2 0.311 10 0.111 689

< 0.2 2.36 < 10 362CMB15424 < 0.5 < 2 1.38 0.5 34 351 94 4.24 < 10 < 1 1.37 20 2.85 484 17 0.259 106 0.066 274

< 0.2 2.38 < 10 503CMB15425 < 0.5 < 2 0.99 0.5 27 295 39 4.31 < 10 < 1 1.46 27 2.28 399 3 0.188 70 0.078 12< 2

< 0.2 1.02 < 10 143CMB15426 1.5 < 2 2.04 0.8 17 18 89 4.77 < 10 < 1 0.13 35 0.72 499 3 0.299 18 0.120 596

0.2 1.02 < 10 816CMB15427 1.5 < 2 2.33 0.9 15 51 33 4.99 < 10 < 1 0.15 27 0.99 570 2 0.379 23 0.110 727

0.3 0.85 < 10 1210CMB15428 1.4 < 2 3.40 0.8 13 47 50 5.24 < 10 < 1 0.10 23 0.99 646 < 1 0.430 22 0.105 627

< 0.2 0.65 < 10 1000CMB15429 1.1 < 2 4.70 0.9 11 13 12 4.78 < 10 < 1 0.04 22 0.79 664 < 1 0.376 15 0.101 466

< 0.2 0.56 < 10 1150CMB15430 1.4 < 2 3.56 0.7 13 14 13 4.56 < 10 < 1 0.03 23 0.63 557 < 1 0.336 17 0.109 528

< 0.2 0.73 < 10 1200CMB15431 Prep Duplicate for CMB 15432

1.8 < 2 3.80 0.7 11 11 38 4.64 < 10 < 1 0.03 30 0.75 540 2 0.406 13 0.101 488

0.2 0.69 < 10 1190CMB15432 1.7 < 2 3.78 0.7 11 11 36 4.55 < 10 < 1 0.03 28 0.74 533 2 0.383 12 0.099 486

< 0.2 0.74 < 10 811CMB15433 1.7 < 2 3.73 0.7 9 12 25 3.99 < 10 < 1 0.02 28 0.74 516 2 0.380 12 0.109 4010

< 0.2 1.10 < 10 813CMB15434 1.3 < 2 5.24 1.0 10 8 7 4.29 < 10 < 1 0.03 28 0.98 707 2 0.492 13 0.109 4413

< 0.2 0.89 < 10 645CMB15435 1.2 < 2 4.79 1.3 10 8 8 3.46 < 10 < 1 0.02 24 0.80 551 2 0.391 11 0.116 8212

0.8 0.98 < 10 416CMB15436 1.8 < 2 3.90 1.6 10 12 8 3.42 10 < 1 0.02 24 0.89 528 2 0.470 9 0.129 29416

0.7 0.76 < 10 730CMB15437 1.9 < 2 3.41 1.2 11 12 26 4.30 10 < 1 0.02 30 0.70 634 1 0.418 10 0.121 3106

0.2 0.58 < 10 1100CMB15438 1.4 < 2 2.79 0.8 7 8 32 5.03 < 10 < 1 0.01 34 0.52 702 1 0.340 7 0.105 1416

0.9 0.76 < 10 952CMB15439 1.9 < 2 3.83 1.6 9 7 37 5.21 10 < 1 0.02 29 0.73 849 20 0.394 8 0.095 3926

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0.4 0.47 < 10 1000CMB15440 2.2 < 2 2.59 1.0 13 17 23 6.03 < 10 < 1 0.03 23 0.47 799 4 0.291 14 0.114 1866

0.3 0.44 < 10 519CMB15441 3.2 < 2 2.60 1.2 14 14 27 5.95 < 10 < 1 0.05 29 0.48 679 33 0.244 15 0.113 1576

< 0.2 0.44 < 10 682CMB15442 2.3 < 2 2.05 0.9 9 8 40 5.83 < 10 < 1 0.06 37 0.46 669 1 0.252 9 0.122 638

0.4 0.19 < 10 752CMB15443 1.1 < 2 1.58 0.7 7 8 10 5.57 < 10 < 1 0.03 34 0.19 553 1 0.107 7 0.123 18810


1.1 < 2 1.57 0.8 7 8 10 5.45 < 10 < 1 0.03 35 0.18 545 2 0.104 6 0.121 17910


1.1 < 2 1.54 0.8 7 8 10 5.37 < 10 < 1 0.03 33 0.18 534 5 0.109 7 0.121 17810

< 0.2 0.73 < 10 611CMB15446 2.5 < 2 2.37 0.7 9 9 12 5.60 < 10 < 1 0.13 45 0.69 838 1 0.285 9 0.114 4116

< 0.2 0.82 < 10 863CMB15447 0.8 < 2 1.79 1.6 10 18 23 4.95 < 10 < 1 0.38 36 0.65 649 2 0.219 9 0.110 3510

< 0.2 1.19 < 10 96CMB15448 < 0.5 < 2 1.28 < 0.5 11 50 11 3.37 < 10 < 1 0.71 29 0.99 383 < 1 0.150 15 0.063 202


0.5 < 2 1.19 < 0.5 10 32 28 2.37 < 10 < 1 0.11 84 0.30 328 5 0.108 49 0.044 2964

< 0.2 0.10 < 10 136CMB15450 < 0.5 < 2 0.65 < 0.5 5 69 < 1 2.35 < 10 < 1 < 0.01 23 0.05 52 1 0.114 11 0.022 32

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0.02 3 275 0.19CMB15119 < 10 < 10 115 < 10 142 1.8 1.0915

0.01 < 2 224 0.17CMB15120 < 10 < 10 111 < 10 159 1.7 1.082 2.825

0.03 < 2 27 0.24CMB15121 < 10 < 10 73 < 10 12 10.1 1.080< 1

0.02 < 2 228 0.19CMB15122 < 10 < 10 106 < 10 134 1.8 1.0256

0.01 < 2 258 0.20CMB15123 < 10 < 10 117 < 10 191 1.1 1.0586

0.01 3 271 0.20CMB15124 < 10 < 10 109 < 10 215 1.2 1.0466


< 10 416 56 < 10 110 410 1.0562


< 10 < 10 104 < 10 212 1.3 1.0306


< 10 < 10 104 < 10 210 1.5 1.0826

0.04 3 30 0.21CMB15128 < 10 < 10 67 < 10 107 4.7 1.0614

0.14 < 2 23 0.25CMB15129 < 10 < 10 105 < 10 52 0.6 1.06213

0.09 2 42 0.25CMB15130 < 10 10 84 < 10 221 11.0 1.0426

0.10 < 2 47 0.24CMB15131 < 10 25 113 < 10 190 23.7 1.03510

0.18 < 2 106 0.26CMB15132 < 10 346 120 < 10 547 345 1.06911

0.14 < 2 164 0.25CMB15133 < 10 855 81 < 10 125 859 1.087 2.839

0.06 < 2 161 0.21CMB15134 < 10 34 40 < 10 95 31.1 1.0865

0.04 2 101 0.23CMB15135 < 10 < 10 78 < 10 78 6.3 1.0684

0.09 < 2 184 0.23CMB15136 < 10 < 10 75 < 10 81 8.2 1.0808

0.11 2 191 0.22CMB15137 < 10 27 78 < 10 105 29.1 1.0768

0.08 2 168 0.21CMB15138 < 10 < 10 79 < 10 79 7.4 1.0688

0.10 < 2 149 0.22CMB15139 < 10 71 70 < 10 69 71.8 1.0457

0.12 < 2 102 0.26CMB15140 < 10 93 79 < 10 105 95.0 1.0658

0.07 < 2 64 0.26CMB15141 < 10 17 79 < 10 58 17.0 1.0606

0.11 < 2 134 0.22CMB15142 < 10 < 10 125 < 10 79 3.0 1.05812

0.04 < 2 115 0.22CMB15143 < 10 84 44 < 10 66 86.4 1.0677

0.03 3 75 0.25CMB15144 < 10 42 54 < 10 46 44.2 1.0528

0.04 < 2 92 0.27CMB15145 < 10 154 46 < 10 51 149 1.0467

0.05 4 74 0.25CMB15146 < 10 35 111 < 10 52 31.3 1.08813

0.05 < 2 142 0.25CMB15147 < 10 73 42 < 10 68 71.2 1.0918

0.04 < 2 122 0.24CMB15148 < 10 56 43 < 10 96 53.6 1.0567

0.06 2 118 0.24CMB15149 < 10 55 38 < 10 95 57.0 1.0517

0.06 < 2 244 0.21CMB15150 < 10 51 37 < 10 70 49.6 1.0526

0.08 < 2 108 0.27CMB15161 < 10 12 68 < 10 53 13.2 1.0665

0.09 < 2 152 0.23CMB15162 < 10 10 49 < 10 15 13.3 1.0613

0.06 < 2 109 0.24CMB15163 < 10 < 10 57 < 10 16 11.9 1.0833

0.20 < 2 112 0.20CMB15164 < 10 < 10 59 < 10 59 10.1 1.069 2.764

0.05 2 97 0.25CMB15165 < 10 < 10 64 < 10 44 4.5 1.0825

0.09 2 143 0.23CMB15166 < 10 71 74 < 10 40 66.0 1.0255

0.03 2 144 0.28CMB15167 < 10 335 93 < 10 57 320 1.0707

0.03 < 2 164 0.29CMB15168 < 10 374 92 < 10 58 366 1.0797

0.05 3 134 0.28CMB15169 < 10 200 120 < 10 109 194 1.0797

0.07 2 134 0.24CMB15170 < 10 420 168 < 10 118 411 1.0536

0.08 < 2 154 0.25CMB15171 < 10 1220 202 < 10 102 1140 1.0535

0.03 < 2 19 0.29CMB15172 < 10 12 68 < 10 77 7.7 1.0505

0.12 < 2 172 0.25CMB15173 < 10 865 277 < 10 132 840 1.04413

0.03 < 2 114 0.22CMB15174 < 10 < 10 123 < 10 97 6.1 1.06015

0.10 3 99 0.21CMB15175 < 10 < 10 121 < 10 96 0.6 1.05015

0.09 < 2 80 0.22CMB15176 < 10 < 10 88 < 10 94 10.2 1.0288

0.12 3 107 0.24CMB15177 < 10 56 95 < 10 283 60.6 1.0536

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0.04 2 82 0.23CMB15178 < 10 29 69 < 10 71 28.8 1.0465

0.03 < 2 102 0.22CMB15179 < 10 < 10 55 < 10 75 5.4 1.0516

0.04 < 2 100 0.24CMB15180 < 10 11 64 < 10 66 11.7 1.0835

0.05 < 2 80 0.28CMB15181 < 10 < 10 69 < 10 86 6.3 1.0506

0.07 < 2 112 0.29CMB15182 < 10 99 82 < 10 101 94.2 1.0896

0.05 < 2 100 0.25CMB15183 < 10 < 10 55 < 10 54 10.5 1.0665

0.03 < 2 59 0.23CMB15184 < 10 < 10 62 < 10 59 3.1 1.0458

0.02 < 2 44 0.20CMB15185 < 10 < 10 61 < 10 134 3.7 1.0824


< 10 403 55 < 10 111 394 1.0952

0.04 2 34 0.20CMB15187 < 10 < 10 77 < 10 231 3.5 1.0476

0.02 < 2 33 0.20CMB15188 < 10 < 10 76 < 10 233 3.5 1.0946

0.02 < 2 43 0.27CMB15189 < 10 < 10 69 < 10 284 3.5 1.0488

0.03 < 2 34 0.30CMB15190 < 10 < 10 62 < 10 216 3.5 1.0967

0.08 < 2 61 0.23CMB15191 < 10 < 10 62 < 10 141 2.8 1.0356

0.08 < 2 49 0.23CMB15192 < 10 < 10 58 < 10 309 3.2 1.0325

0.06 < 2 55 0.21CMB15193 < 10 < 10 60 < 10 449 3.3 1.0313

0.05 3 106 0.23CMB15194 < 10 414 50 < 10 172 417 1.0666

0.04 < 2 80 0.19CMB15195 < 10 1020 55 < 10 59 995 1.0456

0.04 3 159 0.25CMB15196 < 10 952 60 < 10 131 937 1.0108

0.06 2 133 0.26CMB15197 < 10 495 84 < 10 151 485 1.0707

0.03 2 65 0.24CMB15198 < 10 14 74 < 10 150 13.1 1.0725

0.02 < 2 42 0.21CMB15199 < 10 < 10 67 < 10 99 4.9 1.0415

0.02 < 2 48 0.24CMB15200 < 10 13 63 < 10 118 14.5 1.0167

0.05 < 2 171 0.22CMB15413 < 10 143 51 < 10 78 146 1.0567

0.07 < 2 56 0.23CMB15414 < 10 10 63 < 10 14 11.3 1.076< 1

0.04 < 2 162 0.24CMB15415 < 10 110 54 < 10 99 110 1.0407

0.04 < 2 136 0.24CMB15416 < 10 60 43 < 10 92 59.3 1.0687

0.04 < 2 139 0.20CMB15417 < 10 98 61 < 10 93 97.0 1.0718

0.04 < 2 158 0.20CMB15418 < 10 59 58 < 10 96 59.0 1.0398

0.06 < 2 254 0.24CMB15419 < 10 51 69 < 10 104 50.2 1.0489

0.06 < 2 289 0.22CMB15420 < 10 89 69 < 10 99 87.4 1.09310

0.07 < 2 225 0.18CMB15421 < 10 51 65 < 10 199 50.9 1.00310

0.20 < 2 115 0.25CMB15422 < 10 23 56 < 10 181 20.7 1.0149

0.17 < 2 157 0.28CMB15423 < 10 104 52 < 10 89 105 1.0578

0.23 2 30 0.20CMB15424 < 10 < 10 88 < 10 65 3.3 1.0566

0.07 < 2 46 0.26CMB15425 < 10 < 10 105 < 10 51 7.8 1.0313

0.36 < 2 39 0.34CMB15426 < 10 74 70 < 10 102 81.0 1.0387

0.09 < 2 70 0.27CMB15427 < 10 48 79 < 10 111 47.4 1.0777

0.06 < 2 145 0.21CMB15428 < 10 105 75 < 10 101 104 1.0678

0.06 < 2 213 0.18CMB15429 < 10 36 63 < 10 96 36.2 1.0606

0.06 2 160 0.22CMB15430 < 10 124 60 < 10 135 124 1.0607

0.06 < 2 190 0.20CMB15431 Prep Duplicate for CMB 15432

< 10 92 67 < 10 200 89.8 1.0877

0.06 < 2 184 0.19CMB15432 < 10 90 66 < 10 200 87.6 1.0037

0.04 < 2 157 0.22CMB15433 < 10 68 54 < 10 152 67.1 1.0877

0.07 < 2 237 0.22CMB15434 < 10 90 46 < 10 145 88.0 1.0247

0.07 4 212 0.21CMB15435 < 10 234 41 < 10 142 235 1.0386

0.04 < 2 179 0.26CMB15436 < 10 1040 46 < 10 108 1040 1.0587

0.05 < 2 174 0.26CMB15437 < 10 985 59 < 10 135 947 1.0567

0.06 < 2 159 0.19CMB15438 < 10 333 50 < 10 98 323 1.0435

0.09 < 2 197 0.17CMB15439 < 10 973 58 < 10 125 961 1.083 2.776

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0.08 < 2 150 0.22CMB15440 < 10 450 92 < 10 121 438 1.0547

0.13 < 2 115 0.24CMB15441 < 10 294 95 15 114 278 1.0607

0.09 < 2 80 0.21CMB15442 < 10 155 80 < 10 90 156 1.0307

0.09 < 2 76 0.19CMB15443 < 10 596 79 < 10 86 575 1.0693


< 10 571 78 < 10 83 599 1.056 2.823


< 10 565 76 < 10 82 572 1.0333

0.15 < 2 65 0.27CMB15446 < 10 93 70 < 10 92 93.1 1.0317

0.08 < 2 39 0.34CMB15447 < 10 22 60 < 10 89 22.1 1.0367

0.08 < 2 21 0.30CMB15448 < 10 10 68 < 10 76 11.6 1.084 2.765


< 10 873 59 < 10 113 842 1.0922

0.05 < 2 40 0.24CMB15450 < 10 15 46 < 10 11 10.7 1.057< 1

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26.3 0.32 14 272GXR-1 Meas 0.8 1460 0.77 3.3 8 7 1180 24.3 < 10 4 0.02 < 10 0.13 762 15 0.050 35 0.034 583347

31.0 3.52 15 750GXR-1 Cert 1.2 1380 0.96 3.3 8 12 1110 23.6 14 4 0.05 8 0.22 852 18 0.052 41 0.065 730 427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.6 2.73 < 10 54GXR-4 Meas 1.4 23 0.92 0.8 16 56 6510 3.59 10 < 1 1.39 42 1.71 138 342 0.118 41 0.119 48102

4.0 7.20 5 1640GXR-4 Cert 1.9 19 1.01 0.9 15 64 6520 3.09 20 0 4.01 65 1.66 155 310 0.564 42 0.120 52 98

18.8 3.43 19 1310GXR-2 Meas 1.1 < 2 0.82 4.7 10 26 82 2.14 10 4 0.54 20 0.54 1020 < 1 0.214 18 0.056 76517

17.0 16.50 42 2240GXR-2 Cert 1.7 1 0.93 4.1 9 36 76 1.86 37 3 1.37 26 0.85 1007 2 0.556 21 0.105 690 25

0.3 6.76 < 10 775GXR-6 Meas 0.9 < 2 0.14 0.7 14 81 75 6.11 20 < 1 0.81 < 10 0.39 1010 2 0.098 24 0.030 90233

1.3 17.70 10 1300GXR-6 Cert 1.4 0 0.18 1.0 14 96 66 5.58 35 0 1.87 14 0.61 1007 2 0.104 27 0.035 101 330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2850 5.99 2350

OREAS 13P Cert 2500 7.58 2261

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

DL-1a Meas

DL-1a Cert

0.2 1.51 < 10 521CMB15131 Orig 0.9 < 2 2.65 0.9 28 59 72 5.65 < 10 < 1 0.29 16 1.42 603 < 1 0.385 44 0.097 3110

0.2 1.53 < 10 522CMB15131 Dup 0.9 < 2 2.67 0.9 29 59 74 5.69 < 10 < 1 0.29 16 1.42 603 < 1 0.390 46 0.099 3311

< 0.2 1.25 < 10 298CMB15145 Orig 1.2 < 2 4.10 0.9 10 15 61 3.26 < 10 < 1 0.05 28 1.07 458 < 1 0.498 14 0.142 8212

< 0.2 1.22 < 10 291CMB15145 Dup 1.1 < 2 4.01 0.9 10 15 61 3.20 < 10 < 1 0.05 28 1.05 448 < 1 0.486 15 0.134 8211

0.4 1.45 < 10 284CMB15148 Orig 1.2 < 2 4.99 0.7 10 11 121 3.66 10 < 1 0.05 26 1.24 657 < 1 0.556 12 0.122 2516

0.5 1.35 < 10 272CMB15148 Split 1.2 < 2 4.97 0.8 9 11 104 3.51 10 < 1 0.04 24 1.22 649 < 1 0.517 12 0.119 2614

< 0.2 0.92 < 10 125CMB15168 Orig 1.4 < 2 3.58 0.7 13 17 73 6.02 10 < 1 0.02 37 0.93 658 < 1 0.137 19 0.118 897

< 0.2 0.87 < 10 120CMB15168 Dup 1.1 < 2 3.50 0.6 12 17 71 5.87 10 < 1 0.02 36 0.90 646 < 1 0.130 19 0.116 893

< 0.2 0.83 < 10 570CMB15178 Orig 0.9 < 2 2.14 0.7 17 17 22 5.76 < 10 < 1 0.35 30 0.88 588 1 0.188 20 0.129 138

< 0.2 0.83 < 10 560CMB15178 Split 0.9 < 2 2.15 0.6 16 16 21 5.66 < 10 < 1 0.34 29 0.89 590 1 0.194 19 0.125 135

0.2 0.74 < 10 157CMB15182 Orig 1.2 < 2 2.70 0.7 15 17 47 5.62 < 10 < 1 0.21 34 0.69 554 9 0.155 15 0.126 497

0.2 0.72 < 10 158CMB15182 Dup 1.2 < 2 2.67 0.7 14 17 48 5.62 < 10 < 1 0.20 33 0.68 547 8 0.152 16 0.125 488

< 0.2 1.10 < 10 381CMB15188 Orig < 0.5 < 2 0.90 0.9 19 20 51 5.68 < 10 < 1 0.63 35 0.84 366 1 0.084 17 0.129 184

< 0.2 1.10 < 10 379CMB15188 Split < 0.5 < 2 0.89 0.8 20 19 54 5.80 < 10 < 1 0.63 34 0.83 363 2 0.085 17 0.127 184

< 0.2 0.89 < 10 534CMB15417 Orig 1.8 < 2 4.25 0.7 11 14 12 4.93 < 10 < 1 0.04 23 0.87 582 < 1 0.448 13 0.130 309

< 0.2 0.88 < 10 530CMB15417 Dup 1.7 < 2 4.24 0.7 11 13 12 4.88 < 10 < 1 0.04 24 0.86 578 < 1 0.445 15 0.128 298

< 0.2 0.56 < 10 1150CMB15430 Orig 1.4 < 2 3.56 0.7 13 14 13 4.56 < 10 < 1 0.03 23 0.63 557 < 1 0.336 17 0.109 528

< 0.2 0.58 < 10 1130CMB15430 Split 1.4 < 2 3.50 0.7 13 14 14 4.42 < 10 < 1 0.03 24 0.62 550 < 1 0.346 15 0.107 516

< 0.2 0.73 < 10 1190CMB15431 Prep Duplicate for CMB 15432 Orig

1.8 < 2 3.81 0.7 11 11 39 4.66 < 10 < 1 0.03 31 0.75 542 2 0.404 14 0.101 488

0.2 0.73 < 10 1210CMB15431 Prep Duplicate for CMB 15432 Dup

1.8 < 2 3.79 0.7 11 10 37 4.63 < 10 < 1 0.03 30 0.75 538 2 0.407 13 0.101 488

CMB15439 Orig

CMB15439 Dup

< 0.2 0.10 < 10 136CMB15450 Orig < 0.5 < 2 0.65 < 0.5 5 69 < 1 2.35 < 10 < 1 < 0.01 23 0.05 52 1 0.114 11 0.022 32

< 0.2 0.09 < 10 122CMB15450 Split < 0.5 < 2 0.56 < 0.5 4 59 < 1 2.09 < 10 < 1 < 0.01 18 0.05 47 < 1 0.101 8 0.020 < 2< 2

0.7 0.19 < 10 724CMB15444 PULP DUPLICATE FOR CMB15443 Orig

1.1 < 2 1.57 0.7 7 8 10 5.43 < 10 < 1 0.03 36 0.18 543 2 0.103 6 0.119 18110

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Quality Control



0.4 0.19 < 10 783CMB15444 PULP DUPLICATE FOR CMB15443 Dup

1.1 < 2 1.57 0.8 7 8 10 5.46 < 10 < 1 0.03 34 0.18 546 1 0.105 6 0.122 1789


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.008 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.008 < 1 < 0.001 < 2< 2



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Quality Control



0.20 76 142GXR-1 Meas < 10 32 77 124 6221

0.26 122 275GXR-1 Cert 0 35 80 164 760 2

DH-1a Meas 2620

DH-1a Cert 2629

DH-1a Meas 2650

DH-1a Cert 2629

1.87 4 70GXR-4 Meas < 10 < 10 86 14 737

1.77 5 221GXR-4 Cert 3 6 87 31 73 8

0.04 36 92GXR-2 Meas < 10 < 10 50 < 10 5445

0.03 49 160GXR-2 Cert 1 3 52 2 530 7

0.02 4 27GXR-6 Meas < 10 < 10 167 < 10 11821

0.02 4 35GXR-6 Cert 2 2 186 2 118 28

SY-2 Meas 281

SY-2 Cert 284

SY-2 Meas 284

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 9840

BL-3 Cert 10200

BL-4a Meas 1250

BL-4a Cert 1248

BL-4a Meas 1270

BL-4a Cert 1248

DL-1a Meas 2590

DL-1a Cert 116

0.10 < 2 47 0.24CMB15131 Orig < 10 24 113 < 10 19010

0.11 < 2 47 0.24CMB15131 Dup < 10 26 114 < 10 19111

0.04 < 2 92 0.27CMB15145 Orig < 10 155 47 < 10 527

0.04 < 2 91 0.27CMB15145 Dup < 10 153 46 < 10 507

0.04 < 2 122 0.24CMB15148 Orig < 10 56 43 < 10 96 53.6 1.0567

0.04 < 2 118 0.23CMB15148 Split < 10 53 42 < 10 97 53.6 1.0707

0.03 < 2 165 0.29CMB15168 Orig < 10 376 93 < 10 587

0.03 < 2 164 0.28CMB15168 Dup < 10 372 91 < 10 577

0.04 2 82 0.23CMB15178 Orig < 10 29 69 < 10 71 28.8 1.0465

0.04 < 2 84 0.24CMB15178 Split < 10 28 68 < 10 68 28.1 1.0465

0.07 < 2 113 0.30CMB15182 Orig < 10 98 83 < 10 1006

0.07 2 111 0.29CMB15182 Dup < 10 99 82 < 10 1016

0.02 < 2 33 0.20CMB15188 Orig < 10 < 10 76 < 10 233 3.5 1.0946

0.02 2 33 0.20CMB15188 Split < 10 < 10 74 < 10 223 3.7 1.0336

0.04 < 2 140 0.20CMB15417 Orig < 10 98 62 < 10 948

0.04 < 2 138 0.20CMB15417 Dup < 10 97 61 < 10 938

0.06 2 160 0.22CMB15430 Orig < 10 124 60 < 10 135 124 1.0607

0.05 < 2 157 0.23CMB15430 Split < 10 120 59 < 10 131 122 1.0797

0.06 2 190 0.20CMB15431 Prep Duplicate for CMB 15432 Orig

< 10 93 68 < 10 2007

0.06 < 2 190 0.20CMB15431 Prep Duplicate for CMB 15432 Dup

< 10 92 67 < 10 2007

CMB15439 Orig 2.78

CMB15439 Dup 2.76

0.05 < 2 40 0.24CMB15450 Orig < 10 15 46 < 10 11 10.7 1.057< 1

0.04 < 2 35 0.20CMB15450 Split < 10 < 10 39 < 10 10 10.9 1.014< 1

0.08 < 2 76 0.19CMB15444 PULP DUPLICATE FOR CMB15443 Orig

< 10 581 78 < 10 833

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Quality Control



0.09 < 2 77 0.18CMB15444 PULP DUPLICATE FOR CMB15443 Dup

< 10 562 78 < 10 823


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

01-Jul-08

11-Jun-08

A08-3139



Cam McLeanATTN:





Eric Hoffman, Ph.D.

CERTIFIED BY :

REPORT A08-3139

Notes:




President/General Manager


Document Page 157




< 0.2 0.49 < 10 30CMB15801 0.5 < 2 1.06 < 0.5 8 21 37 1.72 < 10 < 1 0.10 56 0.18 148 2 0.114 5 0.013 303

0.3 0.31 < 10 19CMB15802 0.6 < 2 0.82 < 0.5 7 21 55 0.98 < 10 < 1 0.04 60 0.08 110 < 1 0.104 2 0.007 38< 2

< 0.2 0.54 < 10 54CMB15803 < 0.5 < 2 0.47 < 0.5 6 21 16 0.88 < 10 < 1 0.20 59 0.30 145 5 0.104 5 0.003 13< 2

< 0.2 1.14 < 10 44CMB15804 0.6 < 2 1.88 < 0.5 18 56 44 4.09 < 10 < 1 0.30 37 0.62 326 1 0.088 25 0.097 65


0.6 < 2 1.37 < 0.5 12 34 28 2.59 < 10 < 1 0.13 85 0.42 356 5 0.119 51 0.045 163< 2

< 0.2 1.12 < 10 42CMB15806 0.6 < 2 1.84 < 0.5 16 48 38 4.06 < 10 < 1 0.28 40 0.58 315 1 0.089 22 0.095 64

< 0.2 0.11 < 10 143CMB15807 < 0.5 < 2 0.70 < 0.5 8 65 < 1 2.17 < 10 < 1 < 0.01 23 0.05 55 < 1 0.121 14 0.017 < 22

< 0.2 1.11 < 10 324CMB15808 1.3 < 2 2.97 0.5 20 37 126 5.89 < 10 < 1 0.20 45 0.99 875 2 0.275 16 0.121 2510

< 0.2 1.12 < 10 861CMB15809 0.8 < 2 2.95 0.6 20 22 16 6.01 < 10 < 1 0.14 40 1.19 928 < 1 0.347 17 0.124 2310

0.8 0.42 < 10 1390CMB15810 1.0 < 2 1.88 0.7 16 12 143 6.12 < 10 < 1 0.08 57 0.44 517 < 1 0.244 10 0.105 1654

2.0 0.22 < 10 900CMB15811 1.1 < 2 1.53 < 0.5 15 14 303 6.07 < 10 < 1 0.01 44 0.16 287 < 1 0.203 9 0.122 24212

0.7 2.46 < 10 467CMB15812 1.9 < 2 3.09 0.6 38 47 184 6.95 10 < 1 0.32 14 2.28 954 2 0.544 53 0.083 527

0.8 0.42 < 10 1370CMB15813 1.8 < 2 2.60 0.6 17 13 144 6.27 < 10 < 1 0.03 41 0.55 645 < 1 0.282 14 0.123 746

< 0.2 0.29 < 10 950CMB15814 1.7 < 2 2.01 0.5 13 8 5 5.72 < 10 < 1 0.04 55 0.37 695 < 1 0.224 8 0.096 518

< 0.2 0.47 < 10 1070CMB15815 2.1 < 2 2.83 0.6 14 7 4 6.12 < 10 < 1 0.04 53 0.69 895 < 1 0.305 9 0.098 259

1.3 0.48 < 10 516CMB15816 2.7 < 2 2.90 0.6 15 10 278 5.61 < 10 < 1 0.02 47 0.67 757 < 1 0.283 11 0.100 22111

< 0.2 0.68 < 10 598CMB15817 3.4 < 2 3.81 0.7 16 9 10 5.65 < 10 < 1 0.02 46 0.96 811 < 1 0.311 12 0.106 13412

0.6 0.45 < 10 779CMB15818 4.8 < 2 3.30 0.6 20 16 10 5.90 < 10 < 1 0.03 36 0.71 678 < 1 0.291 18 0.102 2918

0.5 0.73 < 10 874CMB15819 2.0 < 2 4.01 0.5 21 17 35 6.29 10 < 1 0.05 41 0.98 825 < 1 0.316 20 0.113 2258

0.3 0.75 < 10 696CMB15820 1.7 < 2 3.80 0.6 20 17 14 5.95 < 10 < 1 0.05 37 1.01 781 < 1 0.317 18 0.108 1237

< 0.2 0.71 < 10 1380CMB15821 1.4 < 2 3.02 0.6 17 15 6 5.92 < 10 < 1 0.05 34 0.87 702 < 1 0.345 15 0.090 575

0.4 1.28 < 10 1070CMB15822 1.6 < 2 3.91 0.5 21 137 86 5.25 < 10 < 1 0.25 32 1.93 904 < 1 0.441 67 0.108 566

< 0.2 0.43 < 10 901CMB15823 1.4 < 2 3.40 < 0.5 18 17 21 5.61 < 10 < 1 0.02 33 0.65 635 < 1 0.286 18 0.112 218

< 0.2 0.50 < 10 498CMB15824 1.6 < 2 3.74 0.7 18 17 45 5.00 < 10 < 1 0.03 36 0.71 609 2 0.264 18 0.110 637


0.5 < 2 1.29 < 0.5 12 37 38 3.08 < 10 < 1 0.12 78 0.40 343 8 0.121 55 0.043 161< 2

< 0.2 0.54 < 10 619CMB15826 1.8 < 2 3.68 0.7 19 16 61 5.09 < 10 < 1 0.03 35 0.74 583 2 0.289 18 0.108 778

< 0.2 0.12 < 10 53CMB15827 < 0.5 < 2 0.82 < 0.5 9 71 < 1 2.45 < 10 < 1 0.01 25 0.07 59 2 0.130 14 0.023 < 2< 2

< 0.2 2.81 12 207CMB15828 0.8 < 2 3.96 < 0.5 70 84 79 5.46 < 10 < 1 0.12 < 10 2.60 766 2 0.871 60 0.068 4514

0.3 0.91 < 10 257CMB15829 2.2 < 2 4.21 0.7 20 16 97 4.93 < 10 < 1 0.06 30 1.08 764 1 0.373 20 0.107 827

< 0.2 0.79 < 10 622CMB15830 4.6 < 2 3.80 0.6 19 16 19 5.66 < 10 < 1 0.05 33 1.00 693 < 1 0.352 19 0.107 726

< 0.2 0.75 < 10 565CMB15831 2.7 < 2 3.55 0.6 19 16 15 5.28 < 10 < 1 0.06 33 0.96 704 < 1 0.346 20 0.109 686

0.2 0.75 < 10 549CMB15832 1.7 < 2 3.92 0.6 17 17 22 4.83 < 10 < 1 0.04 29 0.90 780 < 1 0.361 17 0.111 1206

< 0.2 0.66 < 10 1130CMB15833 1.6 < 2 3.82 0.6 14 16 25 4.31 < 10 < 1 0.04 29 0.80 639 < 1 0.365 12 0.111 1346

0.4 1.96 < 10 679CMB15834 2.3 < 2 4.86 1.0 33 68 49 6.16 10 < 1 0.28 13 1.82 779 4 0.552 40 0.132 10514


2.5 < 2 4.99 1.1 34 70 50 6.28 10 < 1 0.29 13 1.89 805 4 0.579 40 0.137 10813

1.8 1.26 < 10 576CMB15836 4.3 < 2 4.88 0.8 26 39 18 5.75 20 < 1 0.13 21 1.45 811 2 0.471 25 0.116 7118

0.4 0.67 < 10 530CMB15837 1.7 < 2 3.54 0.9 18 16 35 5.30 < 10 < 1 0.11 32 0.94 627 1 0.289 17 0.107 1517


1.6 < 2 3.42 0.9 17 16 31 5.09 < 10 < 1 0.11 31 0.89 606 < 1 0.266 17 0.102 1376

< 0.2 0.76 < 10 891CMB15839 1.9 < 2 2.12 0.6 24 18 28 6.17 < 10 < 1 0.29 35 1.17 503 1 0.313 23 0.109 986

< 0.2 0.68 < 10 705CMB15840 2.5 < 2 3.00 0.6 25 16 21 5.77 < 10 < 1 0.20 35 0.83 618 4 0.290 21 0.109 727

< 0.2 0.77 < 10 814CMB15841 0.8 < 2 2.11 0.5 22 20 20 5.18 < 10 < 1 0.36 33 0.98 602 1 0.249 23 0.107 57

< 0.2 2.93 < 10 1230CMB15842 < 0.5 < 2 3.95 0.6 38 87 19 6.34 10 < 1 0.80 12 2.83 881 2 0.735 66 0.081 109

< 0.2 0.73 < 10 1180CMB15843 0.7 < 2 1.60 0.5 24 16 17 5.73 < 10 < 1 0.53 38 0.94 628 < 1 0.243 22 0.109 3019

< 0.2 0.80 < 10 735CMB15844 < 0.5 < 2 1.40 0.7 25 17 43 5.84 < 10 < 1 0.65 38 0.98 628 1 0.193 26 0.107 2217

< 0.2 0.89 < 10 670CMB15845 0.6 < 2 1.33 0.8 25 18 61 6.13 < 10 < 1 0.63 39 1.02 649 2 0.205 22 0.108 418

< 0.2 0.83 < 10 200CMB15846 < 0.5 < 2 1.11 0.5 23 18 23 5.82 < 10 < 1 0.56 36 0.83 541 2 0.150 21 0.112 135

< 0.2 0.70 < 10 85CMB15847 < 0.5 < 2 1.63 0.5 20 19 15 5.33 < 10 < 1 0.40 39 0.70 444 2 0.131 20 0.106 274

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0.5 < 2 1.37 < 0.5 12 35 28 2.57 < 10 < 1 0.13 81 0.43 355 4 0.120 46 0.044 1623

< 0.2 0.15 < 10 65CMB15849 < 0.5 < 2 0.66 < 0.5 8 51 < 1 1.67 < 10 < 1 0.01 23 0.08 57 < 1 0.152 12 0.016 2< 2

< 0.2 0.58 < 10 398CMB15850 < 0.5 < 2 1.96 1.2 20 17 23 5.14 < 10 < 1 0.36 36 0.61 466 2 0.098 19 0.112 1316

< 0.2 0.64 < 10 349CMB15851 < 0.5 < 2 1.95 1.3 21 17 23 5.15 < 10 < 1 0.38 36 0.67 485 2 0.137 21 0.106 1014

< 0.2 0.76 < 10 717CMB15852 0.9 < 2 2.69 0.7 20 16 24 5.65 < 10 < 1 0.33 36 0.85 604 < 1 0.163 20 0.110 1057

< 0.2 0.83 < 10 202CMB15853 0.5 < 2 1.61 0.6 21 16 22 5.53 < 10 < 1 0.47 38 0.90 478 1 0.155 20 0.110 173

< 0.2 0.96 < 10 163CMB15855 < 0.5 < 2 1.35 0.6 22 16 28 5.33 < 10 < 1 0.65 43 0.93 476 2 0.138 21 0.115 164

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0.04 < 2 72 0.11CMB15801 < 10 118 24 < 10 17 128 1.0962

0.04 < 2 47 0.05CMB15802 < 10 119 10 < 10 10 129 1.060 2.67< 1

0.04 < 2 45 0.05CMB15803 < 10 < 10 6 < 10 27 12.8 1.066< 1

0.04 2 130 0.32CMB15804 < 10 < 10 54 < 10 44 5.4 1.0896


< 10 394 63 < 10 109 410 1.0783

0.03 2 127 0.32CMB15806 < 10 < 10 52 < 10 46 6.3 1.0806

0.03 < 2 33 0.24CMB15807 < 10 < 10 65 < 10 16 9.9 1.018< 1

0.10 3 113 0.37CMB15808 < 10 75 111 < 10 98 79.5 1.08411

0.05 4 89 0.32CMB15809 < 10 54 139 < 10 78 59.0 1.079 2.7310

0.07 < 2 97 0.34CMB15810 < 10 441 137 < 10 83 459 1.0036

0.05 2 68 0.40CMB15811 < 10 986 317 < 10 22 999 1.0443

0.04 2 88 0.40CMB15812 < 10 98 189 < 10 115 101 1.07215

0.06 3 117 0.32CMB15813 < 10 221 107 < 10 48 233 1.0466

0.04 2 88 0.30CMB15814 < 10 160 98 < 10 52 168 1.0375

0.05 3 114 0.30CMB15815 < 10 42 87 < 10 59 41.9 1.0778

0.04 3 114 0.33CMB15816 < 10 761 214 < 10 62 794 1.0798

0.04 3 148 0.31CMB15817 < 10 430 263 < 10 79 451 1.0158

0.04 < 2 137 0.35CMB15818 < 10 1150 355 < 10 79 1180 1.0497

0.05 < 2 168 0.34CMB15819 < 10 761 172 < 10 140 758 1.077 2.809

0.04 2 140 0.32CMB15820 < 10 470 172 < 10 125 493 1.0558

0.06 3 164 0.33CMB15821 < 10 218 167 < 10 87 237 1.0618

0.06 < 2 170 0.30CMB15822 < 10 190 122 < 10 130 208 1.0719

0.05 6 150 0.30CMB15823 < 10 51 180 < 10 69 53.7 1.0187

0.10 < 2 150 0.32CMB15824 < 10 140 228 < 10 63 148 1.0288


< 10 374 60 < 10 111 409 1.0533

0.13 < 2 141 0.32CMB15826 < 10 180 234 < 10 67 194 1.0188

0.03 < 2 30 0.28CMB15827 < 10 < 10 67 < 10 9 9.1 1.047< 1

0.29 3 118 0.28CMB15828 < 10 10 136 < 10 81 9.6 1.06215

0.08 < 2 169 0.32CMB15829 < 10 227 171 < 10 91 242 1.0369

0.04 2 187 0.32CMB15830 < 10 137 222 < 10 116 143 1.0889

0.04 2 148 0.32CMB15831 < 10 182 176 < 10 120 205 1.02410

0.04 < 2 175 0.28CMB15832 < 10 393 168 < 10 91 429 1.0259

0.06 < 2 197 0.30CMB15833 < 10 386 127 < 10 83 418 1.0468

0.04 < 2 213 0.29CMB15834 < 10 243 176 < 10 187 275 1.07317


< 10 248 181 < 10 194 271 1.07517

0.05 < 2 284 0.31CMB15836 < 10 2420 226 < 10 157 2800 1.067 2.7912

0.05 3 164 0.27CMB15837 < 10 221 82 < 10 184 233 1.0288

0.05 2 159 0.26CMB15838 PULP DUPLICATE FOR CMB15837

< 10 205 78 < 10 175 231 1.0758

0.10 3 133 0.36CMB15839 < 10 52 92 < 10 231 53.4 1.0819

0.13 < 2 130 0.37CMB15840 < 10 53 97 < 10 118 56.2 1.0328

0.07 < 2 113 0.37CMB15841 < 10 < 10 71 < 10 80 6.0 1.0166

0.11 2 98 0.36CMB15842 < 10 < 10 129 < 10 90 3.5 1.08916

0.07 < 2 179 0.45CMB15843 < 10 19 74 < 10 89 21.3 1.0694

0.07 < 2 121 0.43CMB15844 < 10 < 10 73 < 10 131 7.1 1.0743

0.07 2 75 0.45CMB15845 < 10 79 96 < 10 147 91.8 1.0464

0.02 2 45 0.36CMB15846 < 10 < 10 78 < 10 102 4.0 1.083 2.744

0.03 < 2 53 0.37CMB15847 < 10 < 10 70 < 10 170 7.2 1.0504

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< 10 391 62 < 10 131 409 1.0563

0.02 < 2 28 0.23CMB15849 < 10 < 10 45 < 10 13 9.1 1.082< 1

0.07 < 2 75 0.37CMB15850 < 10 14 69 14 212 17.2 1.0582

0.07 < 2 72 0.39CMB15851 < 10 13 68 < 10 215 16.7 1.0603

0.07 3 97 0.35CMB15852 < 10 139 67 < 10 168 150 1.014 2.795

0.05 < 2 56 0.40CMB15853 < 10 < 10 69 < 10 208 12.5 1.0434

0.07 < 2 52 0.41CMB15855 < 10 < 10 70 < 10 168 9.0 1.0683

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Quality Control



DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

< 0.2 1.11 < 10 41CMB15806 Orig 0.6 < 2 1.81 < 0.5 16 48 38 4.01 < 10 < 1 0.27 40 0.57 312 1 0.087 21 0.095 75

< 0.2 1.13 < 10 42CMB15806 Dup 0.6 < 2 1.86 < 0.5 16 49 39 4.11 < 10 < 1 0.28 40 0.59 319 1 0.091 22 0.096 64

0.5 0.74 < 10 866CMB15819 Orig 2.0 < 2 4.03 0.5 21 17 35 6.31 10 < 1 0.05 40 0.99 826 < 1 0.316 20 0.112 2257

0.5 0.73 < 10 883CMB15819 Dup 2.0 < 2 4.00 0.6 20 17 35 6.26 10 < 1 0.05 41 0.98 825 < 1 0.316 20 0.114 2268

< 0.2 0.79 < 10 622CMB15830 Orig 4.6 < 2 3.80 0.6 19 16 19 5.66 < 10 < 1 0.05 33 1.00 693 < 1 0.352 19 0.107 726

< 0.2 0.84 < 10 631CMB15830 Split 4.8 < 2 3.86 0.6 20 16 21 5.86 < 10 < 1 0.05 33 1.04 710 < 1 0.373 20 0.107 756

< 0.2 0.64 < 10 1110CMB15833 Orig 1.5 < 2 3.74 0.6 13 16 23 4.21 < 10 < 1 0.04 29 0.77 622 < 1 0.356 12 0.109 1316

0.2 0.67 < 10 1140CMB15833 Dup 1.6 < 2 3.91 0.6 14 16 28 4.41 < 10 < 1 0.04 30 0.82 657 < 1 0.374 12 0.113 1376

< 0.2 0.58 < 10 398CMB15850 Orig < 0.5 < 2 1.96 1.2 20 17 23 5.14 < 10 < 1 0.36 36 0.61 466 2 0.098 19 0.112 1316

< 0.2 0.57 < 10 391CMB15850 Split < 0.5 < 2 1.94 1.3 21 18 22 5.14 < 10 < 1 0.36 36 0.61 465 2 0.097 20 0.107 1354

< 0.2 0.57 < 10 391CMB15850 Split < 0.5 < 2 1.94 1.3 21 18 22 5.14 < 10 < 1 0.36 36 0.61 465 2 0.097 20 0.107 1354

< 0.2 0.96 < 10 163CMB15855 Orig < 0.5 < 2 1.35 0.6 22 16 28 5.33 < 10 < 1 0.65 43 0.93 476 2 0.138 21 0.115 164

< 0.2 0.91 < 10 161CMB15855 Split < 0.5 < 2 1.32 0.5 22 16 26 5.25 < 10 < 1 0.64 40 0.92 476 2 0.130 22 0.112 162


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.009 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.011 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.009 < 1 < 0.001 < 2< 2



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Quality Control



DH-1a Meas 2610

DH-1a Cert 2630

DH-1a Meas 2570

DH-1a Cert 2630

SY-2 Meas 285

SY-2 Cert 284

SY-2 Meas 288

SY-2 Cert 284

BL-4a Meas 1270

BL-4a Cert 1250

BL-4a Meas 1250

BL-4a Cert 1250

0.03 2 125 0.32CMB15806 Orig < 10 < 10 52 < 10 456

0.04 3 130 0.32CMB15806 Dup < 10 < 10 53 < 10 466

0.05 3 168 0.33CMB15819 Orig < 10 763 173 < 10 1409

0.05 < 2 167 0.35CMB15819 Dup < 10 758 171 < 10 1419

0.04 2 187 0.32CMB15830 Orig < 10 137 222 < 10 116 143 1.0889

0.04 < 2 195 0.32CMB15830 Split < 10 134 227 < 10 121 144 1.0759

0.06 < 2 193 0.29CMB15833 Orig < 10 380 124 < 10 808

0.06 < 2 200 0.30CMB15833 Dup < 10 393 131 < 10 879

0.07 < 2 75 0.37CMB15850 Orig < 10 14 69 14 212 17.2 1.0582

0.08 < 2 74 0.36CMB15850 Split < 10 15 69 12 216 17.0 1.0472

0.08 < 2 74 0.36CMB15850 Split < 10 15 69 12 2162

0.07 < 2 52 0.41CMB15855 Orig < 10 < 10 70 < 10 168 9.0 1.0683

0.07 < 2 50 0.37CMB15855 Split < 10 < 10 69 < 10 172 9.4 1.0423


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

11-Jul-08

27-Jun-08

A08-3573



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-3573

Notes:

22 Core samples and 1 Pulp sample were submitted for analysis.



Quality Control


Document Page 164




< 0.2 0.95 < 10 59CMB15901 < 0.5 < 2 0.89 < 0.5 11 23 26 2.11 < 10 < 1 0.04 66 0.55 221 < 1 0.074 16 0.020 2010

< 0.2 1.03 < 10 40CMB15902 < 0.5 < 2 0.99 0.5 11 24 60 2.35 < 10 < 1 0.05 64 0.69 254 < 1 0.069 17 0.024 233

0.2 0.62 < 10 21CMB15903 < 0.5 < 2 1.01 < 0.5 8 28 37 1.70 < 10 < 1 0.05 55 0.38 159 < 1 0.060 11 0.031 533

< 0.2 0.59 < 10 14CMB15904 < 0.5 < 2 2.11 1.1 25 18 3 5.67 < 10 < 1 0.03 22 0.37 220 2 0.044 14 0.135 238

< 0.2 0.50 < 10 13CMB15905 < 0.5 < 2 2.43 1.3 34 20 < 1 5.73 < 10 < 1 0.02 21 0.30 210 1 0.084 12 0.123 318

< 0.2 0.83 < 10 12CMB15906 < 0.5 < 2 1.96 1.0 19 17 1 4.81 < 10 < 1 < 0.01 22 0.26 189 < 1 0.068 10 0.121 327

< 0.2 1.57 < 10 12CMB15907 < 0.5 < 2 2.61 0.7 37 23 2 3.59 10 < 1 0.02 16 0.71 325 1 0.054 19 0.115 207

< 0.2 1.37 < 10 12CMB15908 < 0.5 < 2 2.58 1.2 37 27 3 6.06 10 < 1 0.02 24 1.19 446 2 0.056 32 0.130 258

< 0.2 0.91 < 10 12CMB15909 < 0.5 < 2 3.53 1.3 19 15 3 6.08 < 10 < 1 0.02 25 0.69 390 2 0.068 18 0.122 305

< 0.2 0.90 < 10 13CMB15910 < 0.5 < 2 2.66 1.1 8 14 4 5.53 < 10 < 1 0.03 24 0.76 365 < 1 0.059 18 0.123 415

0.2 0.88 < 10 11CMB15911 < 0.5 < 2 3.38 0.9 7 16 41 4.70 < 10 < 1 0.02 23 0.46 328 < 1 0.057 12 0.121 697

< 0.2 1.18 < 10 13CMB15912 < 0.5 < 2 3.24 1.1 14 30 9 5.43 < 10 < 1 0.03 26 0.93 430 1 0.058 19 0.121 517

< 0.2 1.27 < 10 22CMB15913 < 0.5 < 2 2.29 1.0 21 76 4 4.84 < 10 < 1 0.07 27 1.20 429 1 0.058 24 0.100 295

0.3 0.55 < 10 16CMB15914 < 0.5 < 2 2.57 1.3 10 8 11 5.80 < 10 < 1 0.01 50 0.43 305 < 1 0.084 8 0.108 6023

0.4 0.97 < 10 86CMB15915 0.6 < 2 3.19 1.1 10 24 24 5.92 < 10 < 1 0.23 31 0.75 452 < 1 0.063 15 0.112 1189

< 0.2 1.22 < 10 248CMB15916 0.5 < 2 2.55 1.1 17 25 8 5.52 < 10 < 1 0.71 37 1.09 505 1 0.095 15 0.094 93

< 0.2 0.88 < 10 72CMB15917 < 0.5 < 2 1.74 0.7 8 30 5 2.99 < 10 < 1 0.46 28 0.63 280 < 1 0.060 11 0.065 3< 2

< 0.2 1.04 < 10 77CMB15918 < 0.5 < 2 1.05 0.6 10 28 9 2.48 < 10 < 1 0.48 32 0.72 292 < 1 0.049 12 0.068 < 2< 2

< 0.2 1.02 < 10 59CMB15919 < 0.5 < 2 1.14 0.6 9 28 7 2.48 < 10 < 1 0.47 30 0.72 292 < 1 0.051 12 0.067 2< 2

< 0.2 0.10 < 10 89CMB15920 < 0.5 < 2 0.57 < 0.5 5 46 < 1 1.82 < 10 < 1 0.01 20 0.04 42 < 1 0.103 12 0.022 < 22


< 0.5 < 2 0.94 < 0.5 8 21 29 1.85 < 10 < 1 0.12 75 0.27 271 3 0.097 41 0.051 159< 2

< 0.2 0.81 < 10 12CMB15886 PREP DUP FROM CMB15906

< 0.5 < 2 1.93 1.0 20 17 < 1 4.68 < 10 < 1 < 0.01 22 0.26 186 < 1 0.070 10 0.118 346

< 0.2 1.21 < 10 13CMB15887 PULP DUP FROM CMB15912

< 0.5 < 2 3.33 1.0 15 31 9 5.50 < 10 < 1 0.03 26 0.94 442 1 0.058 19 0.123 536

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< 0.01 < 2 88 0.07CMB15901 < 10 < 10 18 < 10 33 2.3 1.0051

< 0.01 < 2 67 0.07CMB15902 < 10 < 10 23 < 10 35 2.6 1.060 2.681

< 0.01 < 2 63 0.08CMB15903 < 10 < 10 22 < 10 21 4.5 1.0931

0.12 2 104 0.11CMB15904 < 10 94 80 < 10 21 96.7 1.064 2.805

0.18 < 2 83 0.14CMB15905 < 10 143 77 < 10 21 144 1.0354

0.10 2 190 0.11CMB15906 < 10 150 93 < 10 15 154 1.0076

0.22 < 2 296 0.10CMB15907 < 10 65 92 < 10 29 88.5 1.0526

0.20 < 2 122 0.11CMB15908 < 10 75 100 < 10 56 83.8 1.0895

0.10 < 2 122 0.13CMB15909 < 10 87 124 < 10 29 91.6 1.0795

0.02 < 2 95 0.13CMB15910 < 10 150 161 < 10 33 158 1.052 2.725

0.03 < 2 167 0.13CMB15911 < 10 326 170 < 10 19 352 1.0596

0.05 2 123 0.15CMB15912 < 10 239 220 < 10 37 250 1.0536

0.08 < 2 87 0.12CMB15913 < 10 87 111 < 10 44 92.1 1.0684

0.02 2 63 0.15CMB15914 < 10 385 170 < 10 22 379 1.0765

0.03 3 118 0.13CMB15915 < 10 590 228 < 10 36 586 1.080 2.708

0.08 < 2 38 0.15CMB15916 < 10 < 10 47 < 10 39 6.8 1.0769

0.02 < 2 35 0.13CMB15917 < 10 < 10 39 < 10 37 5.5 1.077 2.744

0.02 < 2 35 0.13CMB15918 < 10 < 10 30 < 10 55 5.5 1.085 2.773

0.02 < 2 39 0.13CMB15919 < 10 < 10 31 < 10 50 5.0 1.0733

0.04 < 2 39 0.10CMB15920 < 10 < 10 43 < 10 11 7.8 1.079< 1


< 10 408 42 < 10 108 404 1.0541

0.10 3 183 0.12CMB15886 PREP DUP FROM CMB15906

< 10 152 91 < 10 15 155 1.0516

0.05 < 2 125 0.14CMB15887 PULP DUP FROM CMB15912

< 10 238 224 < 10 38 248 1.0606

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Quality Control



31.0 0.31 15 266GXR-1 Meas 0.8 1470 0.77 3.3 8 6 1180 24.9 < 10 4 0.02 < 10 0.13 750 15 0.059 37 0.035 551347

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

4.0 2.85 < 10 35GXR-4 Meas 1.4 22 0.97 0.9 16 57 6580 3.59 10 < 1 1.40 45 1.73 141 346 0.117 40 0.124 45102

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

21.2 3.51 22 1320GXR-2 Meas 1.1 < 2 0.84 4.8 10 24 83 2.16 < 10 3 0.54 22 0.54 1030 < 1 0.270 18 0.057 74815

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.4 7.23 < 10 867GXR-6 Meas 0.9 < 2 0.15 1.5 15 83 77 6.76 20 < 1 0.89 10 0.42 1040 2 0.141 26 0.033 96239

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2740 5.58 2200

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

< 0.2 1.25 < 10 22CMB15913 Orig < 0.5 < 2 2.30 1.0 21 75 4 4.85 < 10 < 1 0.07 27 1.19 430 1 0.057 25 0.101 294

< 0.2 1.28 < 10 21CMB15913 Dup < 0.5 < 2 2.29 1.0 21 76 4 4.84 < 10 < 1 0.07 28 1.20 428 1 0.058 24 0.100 285


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.006 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.006 < 1 < 0.001 < 2< 2



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Quality Control



0.20 77 150GXR-1 Meas < 10 32 78 127 640< 1

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2730 2650

DH-1a Cert 2630 2630

DH-1a Meas 2640

DH-1a Cert 2630

1.93 5 73GXR-4 Meas < 10 < 10 90 15 717

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 33 98GXR-2 Meas < 10 < 10 50 < 10 5535

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 5 31GXR-6 Meas < 10 < 10 186 < 10 12320

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 281

SY-2 Cert 284

SY-2 Meas 284

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10200

BL-3 Cert 10200

BL-4a Meas 1270

BL-4a Cert 1250

BL-4a Meas 1280

BL-4a Cert 1250

0.08 < 2 85 0.12CMB15913 Orig < 10 87 111 < 10 444

0.08 < 2 88 0.12CMB15913 Dup < 10 87 112 < 10 444


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

Page 5 of 5

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

11-Jul-08

27-Jun-08

A08-3574



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-3574

Notes:




Quality Control


Document Page 169




0.3 0.69 < 10 57CMB15776 < 0.5 < 2 1.55 1.2 14 13 53 5.18 < 10 < 1 0.40 44 0.72 565 1 0.070 13 0.133 248

0.2 0.67 < 10 388CMB15777 < 0.5 < 2 2.34 1.1 13 10 14 5.14 < 10 < 1 0.32 35 0.73 724 < 1 0.134 12 0.152 278

< 0.2 0.36 < 10 368CMB15778 < 0.5 < 2 2.35 0.8 12 9 3 4.41 < 10 < 1 0.07 30 0.41 618 < 1 0.114 12 0.132 247

< 0.2 0.51 < 10 655CMB15779 < 0.5 < 2 2.26 1.5 14 10 2 5.41 < 10 < 1 0.24 26 0.59 686 < 1 0.159 15 0.144 118

< 0.2 0.43 < 10 224CMB15780 < 0.5 < 2 1.49 1.2 14 13 20 5.80 < 10 < 1 0.23 29 0.46 449 1 0.117 13 0.145 89

< 0.2 0.19 < 10 382CMB15781 < 0.5 < 2 0.83 1.0 8 11 29 4.73 < 10 < 1 0.08 31 0.16 210 < 1 0.131 6 0.111 56

0.5 0.24 < 10 582CMB15782 < 0.5 < 2 1.61 1.0 9 11 41 4.74 < 10 < 1 0.06 27 0.23 346 1 0.149 8 0.123 357

0.3 0.24 < 10 606CMB15783 < 0.5 < 2 1.47 1.0 9 8 37 4.64 < 10 < 1 0.05 29 0.21 323 1 0.163 7 0.123 377


< 0.5 < 2 0.93 0.5 9 21 31 1.81 < 10 < 1 0.12 73 0.26 268 4 0.089 43 0.050 1546

0.4 0.32 < 10 774CMB15785 < 0.5 < 2 1.97 1.6 12 10 38 4.86 < 10 < 1 0.13 23 0.33 401 1 0.161 11 0.133 696

< 0.2 1.12 < 10 356CMB15786 < 0.5 < 2 1.95 1.0 27 22 24 4.66 < 10 < 1 0.26 16 1.01 634 2 0.252 26 0.111 326

0.7 0.37 < 10 566CMB15787 0.8 < 2 2.82 1.6 15 10 42 5.23 < 10 < 1 0.04 22 0.42 426 2 0.171 12 0.117 1445

0.4 0.33 < 10 966CMB15788 1.0 < 2 2.47 1.3 12 10 67 5.08 < 10 < 1 0.03 27 0.36 444 6 0.212 11 0.118 594

< 0.2 0.49 < 10 688CMB15789 0.9 < 2 1.90 1.8 15 19 20 5.53 < 10 < 1 0.08 19 0.58 470 2 0.198 16 0.128 316

0.4 0.55 < 10 1070CMB15790 1.2 < 2 2.51 1.1 16 15 9 5.48 < 10 < 1 0.25 20 0.82 651 < 1 0.246 20 0.114 155

0.2 0.59 < 10 946CMB15791 1.2 < 2 4.08 1.0 14 14 6 5.22 < 10 < 1 0.15 25 0.82 774 < 1 0.241 14 0.113 755

0.6 0.46 < 10 520CMB15792 1.1 < 2 2.40 1.1 14 14 6 4.92 < 10 < 1 0.10 22 0.57 527 < 1 0.181 14 0.126 1236

< 0.2 0.38 < 10 972CMB15793 0.7 < 2 2.96 0.9 12 12 6 4.53 < 10 < 1 0.06 20 0.46 501 < 1 0.173 13 0.124 546

< 0.2 1.17 < 10 1380CMB15794 0.8 < 2 3.03 1.3 19 27 55 4.88 < 10 < 1 0.17 16 1.36 813 2 0.247 22 0.129 1507

< 0.2 0.56 < 10 613CMB15795 1.4 < 2 1.95 0.9 13 13 75 4.82 < 10 < 1 0.14 20 0.69 510 < 1 0.181 15 0.115 328

1.0 0.50 < 10 49CMB15796 1.5 < 2 2.52 1.2 14 14 1 5.26 < 10 < 1 0.11 22 0.58 511 < 1 0.113 15 0.122 939

1.0 0.47 < 10 244CMB15797 1.5 < 2 3.03 1.0 11 14 < 1 4.88 < 10 < 1 0.07 22 0.35 466 < 1 0.106 13 0.131 23610

0.3 0.57 < 10 103CMB15798 1.0 < 2 3.41 1.0 12 13 16 5.13 < 10 < 1 0.15 24 0.50 543 < 1 0.090 13 0.125 1197

1.4 0.87 < 10 112CMB15799 1.2 < 2 3.12 0.9 17 12 19 4.80 10 < 1 0.24 23 0.66 579 2 0.106 14 0.115 2386

0.6 0.49 < 10 541CMB15800 1.6 < 2 3.52 0.9 11 12 28 4.47 < 10 < 1 0.07 19 0.57 638 < 1 0.190 13 0.124 517

0.3 1.05 < 10 444CMB15744 1.0 < 2 3.05 1.1 21 37 47 4.93 < 10 < 1 0.36 12 1.20 605 3 0.220 25 0.112 578

0.2 0.45 < 10 358CMB15745 < 0.5 < 2 1.25 0.9 11 14 52 4.20 < 10 < 1 0.13 27 0.48 321 1 0.167 11 0.123 65

0.2 0.38 < 10 213CMB15746 < 0.5 < 2 0.98 0.7 8 15 71 3.34 < 10 < 1 0.11 40 0.33 171 1 0.128 8 0.125 < 23

< 0.2 1.27 < 10 335CMB15747 < 0.5 < 2 1.40 0.6 19 31 86 2.66 < 10 < 1 0.33 < 10 1.07 308 < 1 0.212 20 0.100 45

0.4 0.46 < 10 344CMB15748 < 0.5 < 2 1.08 0.6 8 14 222 2.71 < 10 < 1 0.15 40 0.31 220 1 0.129 8 0.128 34

< 0.2 0.77 < 10 584CMB15749 < 0.5 < 2 1.04 0.7 11 13 52 3.25 < 10 < 1 0.37 40 0.54 333 2 0.148 10 0.123 5< 2

< 0.2 0.78 < 10 401CMB15750 < 0.5 < 2 0.76 0.8 11 12 26 3.07 < 10 < 1 0.49 41 0.58 330 3 0.081 10 0.124 64

< 0.2 0.72 < 10 194CMB15751 < 0.5 < 2 1.17 0.8 12 13 18 3.74 < 10 < 1 0.37 39 0.56 377 2 0.116 11 0.120 74

< 0.2 0.85 < 10 237CMB15752 < 0.5 < 2 1.45 0.8 16 28 28 3.90 < 10 < 1 0.29 19 0.78 353 < 1 0.140 23 0.116 106

0.3 0.41 < 10 304CMB15753 1.0 < 2 2.04 1.1 15 15 61 4.74 < 10 < 1 0.10 23 0.35 411 < 1 0.131 14 0.133 199

< 0.2 0.45 < 10 466CMB15754 0.8 < 2 2.03 1.3 16 16 36 4.98 < 10 < 1 0.15 23 0.42 484 2 0.140 18 0.135 307

< 0.2 0.48 < 10 691CMB15755 0.8 < 2 2.33 1.1 14 14 45 5.05 < 10 < 1 0.18 21 0.48 494 < 1 0.153 16 0.131 296

< 0.2 0.51 < 10 355CMB15756 < 0.5 < 2 1.65 1.0 13 15 19 4.62 < 10 < 1 0.31 20 0.51 424 < 1 0.084 15 0.123 127

0.8 0.38 < 10 328CMB15957 < 0.5 < 2 1.48 1.0 13 17 83 4.56 < 10 < 1 0.22 27 0.41 308 < 1 0.125 18 0.108 358

0.2 0.36 < 10 918CMB15958 PREP DUP FROM CMB15793

0.7 < 2 2.91 0.8 12 12 6 4.45 < 10 < 1 0.06 19 0.45 491 < 1 0.163 13 0.123 537

1.3 0.84 < 10 111CMB15959 PULP DUP FROM CMB15799

1.2 < 2 3.04 0.9 16 12 17 4.79 < 10 < 1 0.23 23 0.65 564 2 0.103 14 0.113 22912

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0.02 < 2 23 0.13CMB15776 < 10 < 10 49 < 10 90 6.8 1.0784

0.02 < 2 40 0.15CMB15777 < 10 72 48 < 10 80 80.0 1.039 2.775

0.02 < 2 40 0.11CMB15778 < 10 70 43 < 10 68 76.0 1.0894

0.03 < 2 46 0.12CMB15779 < 10 18 44 < 10 65 20.7 1.073 2.785

0.02 2 32 0.14CMB15780 < 10 13 52 < 10 50 15.9 1.0324

0.02 < 2 34 0.12CMB15781 < 10 15 37 < 10 23 18.0 1.0712

0.03 < 2 47 0.12CMB15782 < 10 21 37 < 10 52 26.5 1.0642

0.03 < 2 48 0.13CMB15783 < 10 15 34 < 10 44 18.5 1.0762


< 10 398 42 < 10 100 403 1.0871

0.08 < 2 68 0.12CMB15785 < 10 48 46 < 10 182 50.5 1.0382

0.15 < 2 62 0.17CMB15786 < 10 16 63 < 10 112 20.6 1.0706

0.09 2 95 0.12CMB15787 < 10 270 86 < 10 286 268 1.0443

0.05 < 2 109 0.10CMB15788 < 10 113 81 < 10 197 113 1.0783

0.03 < 2 88 0.12CMB15789 < 10 < 10 79 < 10 111 9.5 1.0553

0.04 < 2 136 0.13CMB15790 < 10 44 133 < 10 76 47.8 1.0594

0.05 < 2 187 0.14CMB15791 < 10 260 139 < 10 70 267 1.0504

0.03 < 2 115 0.13CMB15792 < 10 538 105 < 10 61 530 1.060 2.794

0.05 < 2 136 0.10CMB15793 < 10 239 111 < 10 60 239 1.0652

0.07 2 189 0.13CMB15794 < 10 160 139 < 10 192 169 1.0874

0.03 2 85 0.13CMB15795 < 10 19 122 < 10 80 22.0 1.0324

0.02 < 2 77 0.13CMB15796 < 10 424 162 < 10 57 440 1.0613

0.02 < 2 188 0.16CMB15797 < 10 1010 350 < 10 47 1010 1.056 2.773

0.02 < 2 144 0.15CMB15798 < 10 433 192 < 10 62 449 1.0834

0.04 < 2 221 0.16CMB15799 < 10 1250 174 < 10 68 1240 1.0425

0.04 < 2 126 0.11CMB15800 < 10 220 179 < 10 69 225 1.0823

0.05 < 2 89 0.12CMB15744 < 10 120 185 < 10 77 126 1.0736

0.03 < 2 27 0.11CMB15745 < 10 < 10 58 < 10 39 6.0 1.0864

0.01 < 2 14 0.09CMB15746 < 10 < 10 57 < 10 27 3.2 1.0493

0.02 < 2 13 0.11CMB15747 < 10 < 10 62 < 10 41 0.2 1.0937

0.03 < 2 18 0.09CMB15748 < 10 < 10 50 < 10 26 3.1 1.0403

0.02 < 2 16 0.14CMB15749 < 10 < 10 50 < 10 45 2.9 1.0734

0.01 < 2 10 0.13CMB15750 < 10 < 10 45 < 10 46 3.4 1.095 2.812

0.02 < 2 21 0.14CMB15751 < 10 < 10 55 < 10 47 3.5 1.0594

0.06 < 2 30 0.12CMB15752 < 10 16 68 < 10 53 18.7 1.0334

0.11 < 2 46 0.12CMB15753 < 10 41 89 < 10 95 44.0 1.0663

0.14 < 2 53 0.12CMB15754 < 10 35 88 < 10 93 37.8 1.069 2.784

0.09 < 2 74 0.12CMB15755 < 10 45 77 < 10 155 49.5 1.0234

0.03 < 2 48 0.10CMB15756 < 10 < 10 59 < 10 124 7.1 1.0522

0.04 2 37 0.14CMB15957 < 10 < 10 66 < 10 59 10.0 1.0482

0.05 < 2 133 0.10CMB15958 PREP DUP FROM CMB15793

< 10 236 109 < 10 59 248 1.0082


< 10 1240 168 < 10 66 1230 1.0555

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Quality Control



31.0 0.31 15 266GXR-1 Meas 0.8 1470 0.77 3.3 8 6 1180 24.9 < 10 4 0.02 < 10 0.13 750 15 0.059 37 0.035 551347

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

4.0 2.85 < 10 35GXR-4 Meas 1.4 22 0.97 0.9 16 57 6580 3.59 10 < 1 1.40 45 1.73 141 346 0.117 40 0.124 45102

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

21.2 3.51 22 1320GXR-2 Meas 1.1 < 2 0.84 4.8 10 24 83 2.16 < 10 3 0.54 22 0.54 1030 < 1 0.270 18 0.057 74815

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.4 7.23 < 10 867GXR-6 Meas 0.9 < 2 0.15 1.5 15 83 77 6.76 20 < 1 0.89 10 0.42 1040 2 0.141 26 0.033 96239

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2740 5.58 2200

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

< 0.2 0.52 < 10 653CMB15779 Orig < 0.5 < 2 2.26 1.4 14 10 2 5.46 < 10 < 1 0.24 27 0.59 687 < 1 0.159 15 0.144 118

< 0.2 0.51 < 10 656CMB15779 Dup < 0.5 < 2 2.26 1.6 15 10 2 5.36 < 10 < 1 0.24 26 0.59 685 < 1 0.158 14 0.145 119

0.5 0.45 < 10 518CMB15792 Orig 1.1 < 2 2.41 1.2 14 15 6 4.88 < 10 < 1 0.10 22 0.57 529 < 1 0.186 15 0.125 1237

0.6 0.46 < 10 522CMB15792 Dup 1.1 < 2 2.39 1.0 14 14 6 4.96 < 10 < 1 0.10 22 0.58 524 < 1 0.175 13 0.126 1235

CMB15797 Orig

CMB15797 Dup

0.4 0.46 < 10 344CMB15748 Orig < 0.5 < 2 1.08 0.6 8 14 222 2.71 < 10 < 1 0.15 40 0.31 220 1 0.129 8 0.128 34

0.4 0.46 < 10 350CMB15748 Split < 0.5 < 2 1.09 0.6 8 14 223 2.72 < 10 < 1 0.15 41 0.31 221 1 0.129 7 0.130 37

< 0.2 0.78 < 10 583CMB15749 Orig < 0.5 < 2 1.02 0.7 11 13 52 3.23 < 10 < 1 0.38 40 0.54 329 2 0.151 10 0.123 4< 2

< 0.2 0.76 < 10 584CMB15749 Dup < 0.5 < 2 1.05 0.7 11 13 51 3.27 < 10 < 1 0.37 41 0.54 336 2 0.146 10 0.123 52


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.006 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.006 < 1 < 0.001 < 2< 2



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Quality Control



0.20 77 150GXR-1 Meas < 10 32 78 127 640< 1

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2730 2650

DH-1a Cert 2630 2630

DH-1a Meas 2640

DH-1a Cert 2630

1.93 5 73GXR-4 Meas < 10 < 10 90 15 717

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 33 98GXR-2 Meas < 10 < 10 50 < 10 5535

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 5 31GXR-6 Meas < 10 < 10 186 < 10 12320

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 281

SY-2 Cert 284

SY-2 Meas 284

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10200

BL-3 Cert 10200

BL-4a Meas 1270

BL-4a Cert 1250

BL-4a Meas 1280

BL-4a Cert 1250

0.03 < 2 46 0.12CMB15779 Orig < 10 19 45 < 10 655

0.03 < 2 46 0.12CMB15779 Dup < 10 18 44 < 10 665

0.03 < 2 115 0.13CMB15792 Orig < 10 532 106 < 10 614

0.03 < 2 115 0.13CMB15792 Dup < 10 544 105 < 10 614

CMB15797 Orig 2.75

CMB15797 Dup 2.79

0.03 < 2 18 0.09CMB15748 Orig < 10 < 10 50 < 10 26 3.1 1.0403

0.03 < 2 18 0.09CMB15748 Split < 10 < 10 50 < 10 26 3.3 1.0563

0.01 < 2 16 0.13CMB15749 Orig < 10 < 10 50 < 10 454

0.02 < 2 16 0.14CMB15749 Dup < 10 < 10 51 < 10 464


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

17-Jul-08

27-Jun-08

A08-3577 (i)



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-3577 (i)

Notes:




Quality Control


Document Page 174

Activation Laboratories Ltd. Report: A08-3577 (i)Ag Al As B Ba Be Bi Ca Cd Co Cr Cu Fe Ga Hg K La Mg Mn Mo Na Ni P PbAnalyte Symbol



< 0.2 0.32 < 10 13CMB15854 < 0.5 < 2 0.51 0.5 < 1 8 18 1.13 < 10 < 1 0.16 61 0.07 176 < 1 0.105 < 1 0.002 18< 2

< 0.2 0.31 < 10 17CMB15856 0.9 < 2 0.42 < 0.5 1 9 17 1.36 < 10 < 1 0.13 67 0.08 130 < 1 0.118 < 1 0.003 19< 2

< 0.2 0.14 < 10 13CMB15857 0.5 < 2 0.67 < 0.5 < 1 10 34 1.01 < 10 < 1 0.04 46 0.02 74 < 1 0.090 < 1 0.007 17< 2

0.4 0.47 < 10 42CMB15858 1.1 < 2 3.68 0.8 12 51 11 3.25 < 10 < 1 0.05 13 0.54 369 2 0.133 19 0.058 4415

< 0.2 0.40 < 10 14CMB15859 < 0.5 < 2 2.75 0.6 6 48 < 1 2.20 < 10 < 1 0.03 22 0.43 374 < 1 0.091 11 0.059 511

< 0.2 0.81 < 10 252CMB15860 0.5 < 2 2.11 0.8 10 45 < 1 3.58 < 10 < 1 0.33 27 0.94 410 < 1 0.136 14 0.076 1010

< 0.2 0.79 < 10 240CMB15861 0.9 < 2 2.91 0.7 10 42 33 2.85 < 10 < 1 0.47 27 1.02 492 < 1 0.104 15 0.075 118

< 0.2 0.32 < 10 34CMB15862 0.8 < 2 1.26 < 0.5 9 33 53 1.46 < 10 < 1 0.13 27 0.39 241 < 1 0.120 9 0.063 104

< 0.2 0.32 < 10 32CMB15863 0.8 < 2 1.77 0.5 8 39 41 2.06 < 10 < 1 0.12 29 0.39 285 2 0.131 7 0.060 134

< 0.2 0.58 < 10 58CMB15864 1.0 < 2 2.35 0.7 8 37 1 2.57 < 10 < 1 0.07 28 0.64 463 < 1 0.173 10 0.068 178

< 0.2 0.31 < 10 165CMB15865 0.7 < 2 2.54 1.0 9 22 < 1 4.01 < 10 < 1 < 0.01 20 0.36 505 < 1 0.095 12 0.116 1413

< 0.2 0.55 < 10 362CMB15866 < 0.5 < 2 2.31 0.9 12 21 48 3.72 < 10 < 1 0.05 14 0.58 472 2 0.135 17 0.115 496

0.3 0.48 < 10 612CMB15867 < 0.5 < 2 2.73 0.9 13 16 42 3.97 < 10 < 1 0.03 17 0.50 513 1 0.158 13 0.114 956

0.4 0.30 < 10 343CMB15868 < 0.5 < 2 2.96 1.3 12 14 62 4.40 < 10 < 1 0.05 19 0.37 547 < 1 0.081 14 0.124 625

0.6 0.52 < 10 208CMB15869 < 0.5 < 2 2.46 1.2 21 13 61 4.58 < 10 < 1 0.09 21 0.59 538 2 0.075 16 0.128 307

< 0.2 0.30 < 10 368CMB15870 < 0.5 < 2 1.39 0.8 11 11 39 3.44 < 10 < 1 0.10 32 0.29 259 < 1 0.098 10 0.122 34

0.5 0.43 < 10 151CMB15871 < 0.5 < 2 1.97 1.0 16 14 52 4.56 < 10 < 1 0.11 21 0.50 415 < 1 0.078 16 0.128 136

< 0.2 0.39 < 10 63CMB15872 0.6 < 2 2.71 1.3 12 15 73 4.87 < 10 < 1 0.04 21 0.41 444 < 1 0.130 14 0.124 127

0.3 0.58 < 10 77CMB15873 1.1 < 2 2.33 1.0 13 14 91 4.70 < 10 < 1 0.04 20 0.55 447 < 1 0.145 13 0.127 1007

0.8 0.65 < 10 308CMB15874 1.1 < 2 2.19 2.0 15 14 142 4.76 < 10 < 1 0.15 24 0.66 464 9 0.174 16 0.125 746

< 0.2 0.53 < 10 383CMB15875 < 0.5 < 2 0.75 1.9 14 12 117 3.97 < 10 < 1 0.16 32 0.63 326 1 0.077 12 0.118 104

< 0.2 0.50 < 10 285CMB15876 < 0.5 < 2 0.70 1.3 13 12 87 3.68 < 10 < 1 0.15 32 0.57 302 2 0.072 13 0.121 84


< 0.5 < 2 0.97 < 0.5 9 23 30 1.91 < 10 < 1 0.10 77 0.23 278 5 0.100 42 0.046 289< 2

< 0.2 0.10 < 10 255CMB15878 < 0.5 < 2 0.49 < 0.5 5 57 10 2.02 < 10 < 1 < 0.01 17 0.03 42 < 1 0.122 11 0.027 2< 2

< 0.2 0.42 < 10 173CMB15879 < 0.5 < 2 1.05 1.0 10 13 103 3.79 < 10 < 1 0.19 31 0.43 281 < 1 0.071 11 0.132 124

0.8 0.54 < 10 381CMB15880 0.7 < 2 1.31 1.3 15 14 185 4.73 < 10 < 1 0.07 24 0.44 363 < 1 0.169 12 0.124 337

0.5 0.63 < 10 459CMB15881 < 0.5 < 2 2.15 0.9 12 14 67 4.26 < 10 < 1 0.04 23 0.52 585 < 1 0.169 10 0.127 1218

< 0.2 0.59 < 10 259CMB15882 0.5 < 2 2.04 0.9 13 14 137 4.29 < 10 < 1 0.08 25 0.41 402 < 1 0.122 12 0.140 229

< 0.2 0.87 < 10 292CMB15883 0.5 < 2 1.07 0.7 12 12 27 3.50 < 10 < 1 0.43 36 0.67 380 1 0.164 11 0.124 354

< 0.2 1.15 < 10 543CMB15884 0.5 < 2 1.02 0.7 12 11 38 3.21 < 10 < 1 0.60 37 0.78 458 1 0.163 12 0.115 163

< 0.2 0.68 < 10 187CMB15885 < 0.5 < 2 0.78 0.8 11 13 26 3.46 < 10 < 1 0.38 37 0.47 307 2 0.080 11 0.126 118


1.5 < 2 3.66 0.8 14 55 10 3.57 < 10 < 1 0.05 14 0.64 397 2 0.175 21 0.060 5614


1.1 < 2 2.31 1.0 13 15 89 4.63 < 10 < 1 0.04 20 0.54 442 < 1 0.142 14 0.128 1008

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Activation Laboratories Ltd. Report: A08-3577 (i)S Sb Sc Sr Ti Tl U V W Zn U Mass Spec GravAnalyte Symbol% ppm ppm ppm % ppm ppm ppm ppm ppm ppm g -Unit Symbol


0.01 < 2 8 0.03CMB15854 < 10 11 5 < 10 84 14.8 1.086< 1

0.01 < 2 8 0.03CMB15856 < 10 36 10 < 10 29 37.9 1.066 2.65< 1

0.01 < 2 15 0.02CMB15857 < 10 14 9 < 10 12 16.9 1.062< 1

0.02 < 2 90 0.07CMB15858 < 10 166 107 < 10 49 172 1.0853

0.02 < 2 77 0.07CMB15859 < 10 < 10 61 < 10 38 6.8 1.083 2.782

0.01 2 46 0.13CMB15860 < 10 21 133 < 10 74 21.8 1.0265

0.02 < 2 54 0.11CMB15861 < 10 23 95 < 10 86 24.2 1.0654

0.21 < 2 24 0.10CMB15862 < 10 < 10 25 < 10 29 4.6 1.0802

0.16 < 2 33 0.12CMB15863 < 10 < 10 53 < 10 34 9.7 1.0482

0.02 < 2 52 0.10CMB15864 < 10 < 10 80 < 10 56 9.5 1.0442

0.02 < 2 62 0.10CMB15865 < 10 47 90 < 10 48 51.9 1.0482

0.03 < 2 58 0.08CMB15866 < 10 99 91 < 10 64 98.8 1.0963

0.08 < 2 78 0.09CMB15867 < 10 239 85 < 10 56 243 1.049 2.853

0.07 < 2 76 0.07CMB15868 < 10 97 85 < 10 189 101 1.0592

0.13 < 2 64 0.08CMB15869 < 10 75 73 < 10 203 82.2 1.0803

0.07 < 2 35 0.08CMB15870 < 10 < 10 36 < 10 65 3.3 1.0512

0.10 < 2 45 0.09CMB15871 < 10 < 10 75 < 10 117 9.6 1.0563

0.05 < 2 64 0.11CMB15872 < 10 < 10 73 < 10 163 12.6 1.0574

0.04 < 2 81 0.12CMB15873 < 10 286 138 < 10 153 294 1.0264

0.10 < 2 68 0.15CMB15874 < 10 133 184 < 10 447 138 1.070 2.855

0.08 < 2 36 0.10CMB15875 < 10 < 10 47 12 598 11.9 1.0862

0.05 < 2 33 0.09CMB15876 < 10 < 10 41 < 10 318 12.3 1.0672


< 10 886 46 < 10 114 853 1.0581

0.02 < 2 35 0.10CMB15878 < 10 11 48 < 10 10 14.4 1.046< 1

0.03 < 2 31 0.09CMB15879 < 10 26 48 < 10 206 26.4 1.0862

0.08 < 2 65 0.12CMB15880 < 10 106 89 < 10 289 111 1.0864

0.04 < 2 88 0.13CMB15881 < 10 409 65 < 10 201 411 1.0364

0.08 < 2 85 0.10CMB15882 < 10 42 62 < 10 149 49.8 1.0583

0.04 < 2 35 0.14CMB15883 < 10 86 51 < 10 76 85.8 1.053 2.754

0.02 < 2 28 0.15CMB15884 < 10 < 10 45 < 10 87 4.9 1.0344

0.04 < 2 17 0.10CMB15885 < 10 < 10 46 < 10 68 5.0 1.062 2.793


< 10 217 129 < 10 58 163 1.0704


< 10 282 137 < 10 155 295 1.0294

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Activation Laboratories Ltd. Report: A08-3577 (i)

Quality Control



31.0 0.31 15 266GXR-1 Meas 0.8 1470 0.77 3.3 8 6 1180 24.9 < 10 4 0.02 < 10 0.13 750 15 0.059 37 0.035 551347

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

4.0 2.85 < 10 35GXR-4 Meas 1.4 22 0.97 0.9 16 57 6580 3.59 10 < 1 1.40 45 1.73 141 346 0.117 40 0.124 45102

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

21.2 3.51 22 1320GXR-2 Meas 1.1 < 2 0.84 4.8 10 24 83 2.16 < 10 3 0.54 22 0.54 1030 < 1 0.270 18 0.057 74815

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.4 7.23 < 10 867GXR-6 Meas 0.9 < 2 0.15 1.5 15 83 77 6.76 20 < 1 0.89 10 0.42 1040 2 0.141 26 0.033 96239

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2740 5.58 2200

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

< 0.2 0.55 < 10 364CMB15866 Orig < 0.5 < 2 2.34 0.9 12 21 49 3.73 < 10 < 1 0.05 14 0.58 474 2 0.136 17 0.116 506

0.3 0.54 < 10 360CMB15866 Dup < 0.5 < 2 2.29 0.9 12 21 47 3.71 < 10 < 1 0.05 14 0.57 470 1 0.134 17 0.115 487

0.9 0.53 < 10 385CMB15880 Orig 0.7 < 2 1.31 1.5 15 14 184 4.76 < 10 < 1 0.07 24 0.43 360 < 1 0.168 11 0.124 338

0.7 0.54 < 10 376CMB15880 Dup 0.7 < 2 1.32 1.1 15 15 186 4.69 < 10 < 1 0.08 23 0.44 366 < 1 0.170 13 0.124 337

< 0.2 1.15 < 10 543CMB15884 Orig 0.5 < 2 1.02 0.7 12 11 38 3.21 < 10 < 1 0.60 37 0.78 458 1 0.163 12 0.115 163

< 0.2 1.22 < 10 562CMB15884 Split 0.5 < 2 1.06 0.7 13 11 41 3.35 < 10 < 1 0.62 38 0.80 473 1 0.168 13 0.119 17< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.006 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.006 < 1 < 0.001 < 2< 2



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Activation Laboratories Ltd. Report: A08-3577 (i)

Quality Control



0.20 77 150GXR-1 Meas < 10 32 78 127 640< 1

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2730 2650

DH-1a Cert 2630 2630

DH-1a Meas 2640

DH-1a Cert 2630

1.93 5 73GXR-4 Meas < 10 < 10 90 15 717

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 33 98GXR-2 Meas < 10 < 10 50 < 10 5535

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 5 31GXR-6 Meas < 10 < 10 186 < 10 12320

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 281

SY-2 Cert 284

SY-2 Meas 284

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10200

BL-3 Cert 10200

BL-4a Meas 1270

BL-4a Cert 1250

BL-4a Meas 1280

BL-4a Cert 1250

0.03 < 2 58 0.08CMB15866 Orig < 10 101 91 < 10 643

0.03 < 2 58 0.08CMB15866 Dup < 10 98 90 < 10 633

0.08 < 2 65 0.13CMB15880 Orig < 10 105 89 < 10 2884

0.08 < 2 65 0.12CMB15880 Dup < 10 106 89 < 10 2914

0.02 < 2 28 0.15CMB15884 Orig < 10 < 10 45 < 10 87 4.9 1.0344

0.02 < 2 29 0.16CMB15884 Split < 10 < 10 47 < 10 90 4.4 1.0444


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

14-Aug-08

08-Jul-08

A08-3868



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-3868

Notes:

26 Core samples and 2 Pulp samples were submitted for analysis.

Code 1E3 - Aurora Pkg. Aqua Regia ICP(AQUAGEO)Code Specific Gravity PulpCode 5D-U-Total DNC


Quality Control


Document Page 179




< 0.2 0.15 < 10 54CMB19151 < 0.5 < 2 1.39 < 0.5 7 11 40 4.93 < 10 < 1 0.01 52 0.04 134 5 0.078 5 0.098 473

< 0.2 0.28 < 10 54CMB19152 < 0.5 < 2 2.25 0.6 8 9 88 5.02 < 10 < 1 0.03 52 0.13 200 2 0.128 6 0.117 384

< 0.2 0.58 < 10 80CMB19153 1.0 < 2 3.11 < 0.5 10 9 93 4.31 < 10 < 1 0.04 55 0.37 364 < 1 0.188 7 0.130 7610

< 0.2 1.22 < 10 380CMB19154 1.4 < 2 5.02 0.6 12 19 16 3.72 < 10 < 1 0.09 43 1.05 638 < 1 0.336 12 0.122 3510

< 0.2 0.58 < 10 57CMB19155 < 0.5 < 2 1.68 < 0.5 12 49 43 3.90 < 10 < 1 0.06 24 0.55 223 < 1 0.135 18 0.068 64

< 0.2 1.54 < 10 132CMB19156 < 0.5 < 2 2.29 < 0.5 21 56 45 5.10 < 10 < 1 0.13 27 1.51 410 2 0.343 40 0.087 102

< 0.2 0.53 < 10 1080CMB19157 0.8 < 2 1.92 0.6 11 9 47 4.74 < 10 < 1 0.05 58 0.28 271 < 1 0.262 6 0.103 994

< 0.2 0.57 < 10 1210CMB19158 0.7 < 2 2.43 < 0.5 10 9 45 4.39 < 10 < 1 0.06 55 0.34 365 1 0.263 6 0.101 915


< 0.5 < 2 1.26 < 0.5 10 31 32 2.48 < 10 < 1 0.12 83 0.38 315 4 0.142 48 0.044 1483

< 0.2 0.08 < 10 137CMB19160 < 0.5 < 2 0.78 < 0.5 8 54 < 1 2.26 < 10 < 1 < 0.01 24 0.03 45 1 0.082 17 0.028 33

< 0.2 0.12 < 10 63CMB19161 < 0.5 < 2 1.44 < 0.5 9 9 14 4.45 < 10 < 1 < 0.01 55 0.03 133 < 1 0.056 5 0.102 655

< 0.2 0.35 < 10 307CMB19162 0.7 < 2 2.05 0.5 10 8 62 4.58 < 10 < 1 0.04 61 0.17 244 15 0.114 4 0.110 648

< 0.2 0.23 < 10 368CMB19163 0.5 < 2 1.82 0.6 12 15 74 5.30 < 10 < 1 0.04 43 0.14 242 2 0.109 10 0.118 176

< 0.2 0.44 < 10 69CMB19164 0.9 < 2 2.89 0.5 13 17 47 5.28 < 10 < 1 0.05 35 0.36 386 < 1 0.108 13 0.128 1415

< 0.2 0.73 < 10 277CMB19165 0.7 < 2 2.80 < 0.5 18 19 66 6.28 < 10 < 1 0.25 42 0.54 439 1 0.160 21 0.136 167

< 0.2 0.92 < 10 363CMB19166 0.7 < 2 2.79 0.5 19 17 28 5.80 < 10 < 1 0.55 41 0.66 415 2 0.148 20 0.128 98

< 0.2 0.42 < 10 63CMB19167 < 0.5 < 2 1.07 0.6 14 19 7 5.40 < 10 < 1 0.23 34 0.44 319 < 1 0.072 13 0.124 84

< 0.2 0.25 < 10 82CMB19168 < 0.5 < 2 1.12 0.5 12 20 25 5.21 < 10 < 1 0.09 37 0.20 247 2 0.066 11 0.100 143

< 0.2 0.68 < 10 192CMB19169 1.0 < 2 1.82 0.6 15 17 16 5.48 < 10 < 1 0.13 50 0.38 405 < 1 0.156 13 0.126 628

< 0.2 0.64 < 10 197CMB19170 0.8 < 2 1.76 0.6 14 16 20 5.23 < 10 < 1 0.13 46 0.37 392 1 0.168 13 0.120 338


< 0.5 < 2 1.28 < 0.5 10 32 31 2.51 < 10 < 1 0.12 84 0.38 322 3 0.153 48 0.046 1503

< 0.2 0.05 < 10 37CMB19172 < 0.5 < 2 0.68 < 0.5 7 60 < 1 2.20 < 10 < 1 < 0.01 26 0.02 35 1 0.058 14 0.027 < 23

0.2 0.40 < 10 76CMB19173 < 0.5 < 2 1.12 0.5 16 20 18 5.67 < 10 < 1 0.21 34 0.44 367 < 1 0.085 15 0.120 83

< 0.2 0.48 < 10 71CMB19174 < 0.5 < 2 1.25 < 0.5 15 19 13 5.42 < 10 < 1 0.26 38 0.49 402 < 1 0.092 15 0.126 74

CMB19175 Missing Sample

< 0.2 2.61 < 10 230CMB19176 < 0.5 < 2 3.05 0.5 39 58 59 6.72 < 10 < 1 0.46 < 10 2.56 668 < 1 0.393 63 0.090 32


< 0.5 < 2 3.14 0.6 40 59 62 6.85 10 < 1 0.47 < 10 2.62 687 < 1 0.402 64 0.092 46


< 0.5 < 2 1.21 < 0.5 15 20 12 5.27 < 10 < 1 0.25 35 0.50 397 < 1 0.089 15 0.123 64

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0.02 < 2 98 0.30CMB19151 < 10 43 37 < 10 18 49.6 1.045 2.63< 1

0.03 < 2 110 0.36CMB19152 < 10 44 43 < 10 33 49.1 1.030 2.852

0.03 2 134 0.39CMB19153 < 10 192 44 < 10 42 197 1.0484

0.06 < 2 151 0.33CMB19154 < 10 40 43 < 10 117 41.3 1.0757

0.04 < 2 44 0.29CMB19155 < 10 14 57 < 10 19 13.9 1.0663

0.06 < 2 84 0.35CMB19156 < 10 17 77 < 10 41 17.8 1.0286

0.06 < 2 141 0.37CMB19157 < 10 298 42 < 10 45 312 1.0723

0.09 < 2 163 0.34CMB19158 < 10 261 38 < 10 46 275 1.0183


< 10 372 56 < 10 103 416 1.0432

0.04 < 2 50 0.26CMB19160 < 10 < 10 65 < 10 10 12.6 1.031< 1

0.01 < 2 131 0.37CMB19161 < 10 227 38 < 10 16 249 1.089 2.86< 1

0.03 3 132 0.38CMB19162 < 10 102 31 < 10 49 107 1.006 2.842

0.03 < 2 105 0.37CMB19163 < 10 11 50 < 10 85 13.1 1.080 2.822

0.04 3 79 0.35CMB19164 < 10 16 56 < 10 67 16.8 1.016 2.783

0.06 3 90 0.44CMB19165 < 10 < 10 71 < 10 63 8.2 1.0604

0.07 < 2 88 0.41CMB19166 < 10 < 10 62 < 10 48 4.9 1.0255

0.02 < 2 48 0.27CMB19167 < 10 < 10 67 < 10 59 3.4 1.045 2.793

0.02 4 62 0.29CMB19168 < 10 < 10 64 < 10 92 9.4 1.079 2.842

0.02 2 140 0.45CMB19169 < 10 152 77 < 10 48 147 1.0103

0.02 2 129 0.41CMB19170 < 10 39 71 < 10 45 39.5 1.0033


< 10 383 57 < 10 102 403 1.0822

0.02 < 2 26 0.28CMB19172 < 10 < 10 58 < 10 6 8.4 1.055< 1

0.05 2 55 0.30CMB19173 < 10 < 10 68 < 10 41 2.6 1.078 2.783

0.04 2 66 0.33CMB19174 < 10 < 10 69 < 10 46 3.2 1.009 2.874


0.17 2 49 0.34CMB19176 < 10 < 10 139 < 10 69 0.4 1.01714


< 10 < 10 146 < 10 70 0.4 1.09414


< 10 < 10 67 < 10 47 2.8 1.0284

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Quality Control



24.7 0.33 14 363GXR-1 Meas 0.8 1460 0.78 3.5 8 6 1200 25.2 10 4 0.02 < 10 0.13 743 15 0.071 35 0.041 609361

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.3 2.70 < 10 23GXR-4 Meas 1.4 20 0.96 0.7 15 56 6400 3.56 10 < 1 1.38 48 1.65 132 327 0.124 39 0.125 45103

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

17.4 3.31 22 1290GXR-2 Meas 1.0 < 2 0.85 4.6 10 27 80 2.17 < 10 4 0.54 21 0.53 967 < 1 0.269 18 0.056 73215

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.2 6.61 < 10 864GXR-6 Meas 1.0 < 2 0.18 0.8 14 85 70 6.44 20 < 1 0.92 11 0.42 967 1 0.131 24 0.033 96233

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2860 5.87 2300

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

< 0.2 0.28 < 10 55CMB19152 Orig < 0.5 < 2 2.26 0.6 8 8 88 5.02 < 10 < 1 0.03 52 0.13 201 2 0.130 7 0.118 384

< 0.2 0.28 < 10 53CMB19152 Dup < 0.5 < 2 2.25 0.6 9 9 89 5.03 < 10 < 1 0.03 52 0.13 199 2 0.127 5 0.117 374

CMB19162 Orig

CMB19162 Dup

< 0.2 2.70 < 10 238CMB19177 PREP DUP FROM CMB19176 Orig

< 0.5 < 2 3.15 0.6 40 60 62 6.87 10 < 1 0.47 < 10 2.63 690 < 1 0.404 64 0.093 55

< 0.2 2.67 < 10 238CMB19177 PREP DUP FROM CMB19176 Dup

< 0.5 < 2 3.12 0.6 40 59 62 6.82 10 < 1 0.47 < 10 2.60 684 < 1 0.400 64 0.091 38


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.014 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.009 < 1 < 0.001 < 2< 2



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Quality Control



0.22 74 181GXR-1 Meas < 10 33 75 141 6291

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2590 2610

DH-1a Cert 2630 2630

DH-1a Meas 2640

DH-1a Cert 2630

1.95 2 73GXR-4 Meas < 10 < 10 82 12 696

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 26 92GXR-2 Meas < 10 < 10 48 < 10 5465

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 4 30GXR-6 Meas < 10 < 10 171 < 10 12221

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 280

SY-2 Cert 284

SY-2 Meas 280

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10100

BL-3 Cert 10200

BL-4a Meas 1280

BL-4a Cert 1250

BL-4a Meas 1270

BL-4a Cert 1250

0.03 < 2 109 0.36CMB19152 Orig < 10 44 43 < 10 332

0.03 2 110 0.36CMB19152 Dup < 10 43 43 < 10 332

CMB19162 Orig 2.84

CMB19162 Dup 2.84

0.17 3 51 0.35CMB19177 PREP DUP FROM CMB19176 Orig

< 10 < 10 146 < 10 7014

0.17 3 50 0.35CMB19177 PREP DUP FROM CMB19176 Dup

< 10 < 10 145 < 10 7114


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


1.000


< 0.01

Page 5 of 5

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

12-Nov-08

08-Jul-08

A08-3877



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-3877

Notes:


Code Specific Gravity PulpCode 1E3 - Aurora Pkg. Aqua Regia ICP(AQUAGEO)Code 5D-U-Total DNC


Note: Revised-Corrected Sample ID's that were entered wrong in the system.

Quality Control


Document Page 184




< 0.2 0.58 < 10 139CMB19201 < 0.5 < 2 1.59 0.6 16 12 15 5.65 < 10 < 1 0.26 44 0.49 402 1 0.146 13 0.139 1415

< 0.2 0.72 < 10 145CMB19202 < 0.5 < 2 1.33 0.5 17 13 21 5.72 < 10 < 1 0.49 47 0.63 390 3 0.115 17 0.128 357

< 0.2 0.83 < 10 220CMB19203 < 0.5 < 2 1.18 0.5 18 11 18 6.11 < 10 < 1 0.53 49 0.67 481 2 0.161 18 0.130 305

< 0.2 1.10 < 10 377CMB19204 < 0.5 < 2 2.03 0.6 22 11 33 6.51 < 10 < 1 0.65 46 1.03 777 9 0.201 19 0.130 418

0.3 0.44 < 10 823CMB19205 0.8 < 2 2.33 < 0.5 15 14 34 4.93 < 10 < 1 0.17 40 0.58 494 17 0.242 12 0.106 104

0.2 0.71 < 10 485CMB19206 1.7 < 2 3.36 0.6 15 12 27 5.91 < 10 < 1 0.23 43 0.97 791 24 0.315 14 0.105 715

< 0.2 0.63 < 10 483CMB19207 1.2 < 2 2.83 0.6 17 12 36 5.46 < 10 < 1 0.20 41 0.87 634 10 0.321 13 0.119 95

0.2 0.65 < 10 340CMB19208 1.0 < 2 2.32 0.6 19 12 55 6.22 < 10 < 1 0.32 39 0.87 699 1 0.225 15 0.115 158

< 0.2 0.74 < 10 283CMB19209 1.7 < 2 3.59 0.6 17 10 3 6.17 < 10 < 1 0.11 40 0.94 932 < 1 0.400 14 0.120 1411

< 0.2 0.60 < 10 1250CMB19210 1.7 < 2 2.62 0.5 17 10 2 5.78 < 10 < 1 0.17 40 0.75 743 < 1 0.376 16 0.125 4210

0.7 0.63 < 10 434CMB19211 1.6 < 2 2.82 0.5 17 12 < 1 5.99 < 10 < 1 0.10 35 0.68 782 6 0.249 15 0.131 28811


1.6 < 2 2.83 < 0.5 17 12 48 6.04 < 10 < 1 0.10 35 0.68 787 6 0.252 16 0.128 30312

< 0.2 0.60 < 10 1520CMB19213 1.8 < 2 3.07 0.6 16 8 3 5.54 < 10 < 1 0.11 42 0.78 809 < 1 0.438 13 0.118 319

< 0.2 0.57 < 10 1050CMB19214 1.5 < 2 2.51 0.5 16 18 2 6.25 < 10 < 1 0.06 35 0.58 583 5 0.308 16 0.140 809

< 0.2 0.56 < 10 803CMB19215 2.5 < 2 2.76 0.6 15 10 3 6.05 < 10 < 1 0.15 48 0.73 701 < 1 0.338 12 0.130 659

< 0.2 0.64 < 10 439CMB19216 1.6 < 2 2.47 < 0.5 18 10 7 6.24 < 10 < 1 0.31 38 0.86 782 < 1 0.225 15 0.133 2211

1.5 0.20 < 10 1260CMB19217 3.5 < 2 2.30 < 0.5 14 9 < 1 5.32 < 10 < 1 0.04 41 0.28 576 < 1 0.213 11 0.139 57612


3.6 < 2 2.30 0.5 14 8 < 1 5.21 10 < 1 0.05 42 0.29 580 < 1 0.212 11 0.135 62111

0.2 0.53 < 10 1120CMB19219 4.5 < 2 3.30 0.8 17 16 13 6.34 < 10 < 1 0.09 43 0.76 755 < 1 0.397 16 0.098 20813

0.3 0.55 < 10 184CMB19220 1.9 < 2 2.97 0.6 16 9 10 6.00 < 10 < 1 0.05 51 0.70 685 < 1 0.330 13 0.118 23710

0.7 0.51 < 10 145CMB19221 2.6 < 2 2.92 < 0.5 17 10 7 5.85 < 10 < 1 0.04 48 0.67 594 < 1 0.330 13 0.132 3848

1.6 0.37 < 10 566CMB19222 2.4 < 2 2.72 0.7 15 9 44 5.39 < 10 < 1 0.04 44 0.52 551 5 0.246 10 0.120 5926

0.4 2.57 < 10 386CMB19251 1.2 < 2 4.02 0.6 36 41 65 7.18 10 < 1 0.29 17 2.34 855 9 0.919 48 0.093 1816

1.0 0.65 < 10 360CMB19252 3.5 < 2 3.56 0.8 14 10 25 5.26 10 < 1 0.05 46 0.91 688 6 0.420 12 0.113 4605

1.1 0.73 < 10 630CMB19253 4.1 < 2 3.81 0.9 15 10 26 5.60 10 < 1 0.06 44 1.06 736 3 0.519 13 0.107 4835

< 0.2 1.45 < 10 240CMB19254 < 0.5 < 2 1.44 < 0.5 16 4 9 5.48 < 10 < 1 0.72 31 1.15 793 < 1 0.192 1 0.167 2< 2


0.6 < 2 1.20 < 0.5 18 34 34 2.53 < 10 < 1 0.09 96 0.26 329 9 0.148 92 0.028 3033

0.4 0.51 < 10 856CMB19256 2.7 < 2 2.60 0.6 13 9 19 5.57 < 10 < 1 0.03 58 0.66 586 2 0.410 11 0.090 2703

0.4 0.66 < 10 627CMB19257 2.5 < 2 3.88 0.6 16 15 17 5.61 < 10 < 1 0.03 44 0.94 741 < 1 0.451 16 0.107 1795

1.6 0.64 < 10 670CMB19258 3.2 < 2 3.82 0.6 15 15 47 4.77 10 < 1 0.03 47 0.88 765 < 1 0.451 13 0.109 5546

0.4 0.60 < 10 489CMB19259 3.0 < 2 4.00 0.7 15 15 45 5.47 < 10 < 1 0.04 38 0.85 827 < 1 0.403 13 0.119 2158

< 0.2 0.59 < 10 290CMB19260 2.5 < 2 3.21 0.6 17 15 9 5.71 < 10 < 1 0.04 38 0.81 726 1 0.378 17 0.117 838

0.7 0.60 < 10 249CMB19261 3.4 < 2 3.75 0.6 16 13 21 5.24 < 10 < 1 0.05 34 0.86 778 2 0.384 16 0.115 32213

0.5 1.63 < 10 706CMB19262 1.8 < 2 5.57 1.0 26 44 115 6.16 < 10 < 1 0.36 18 1.61 849 5 0.574 33 0.086 538

1.2 2.09 < 10 447CMB19263 0.6 < 2 4.22 2.1 31 49 297 5.75 < 10 < 1 0.27 14 1.97 829 6 0.766 38 0.077 3519

0.4 0.57 < 10 774CMB19264 1.1 < 2 2.86 2.6 20 15 74 5.75 < 10 < 1 0.20 37 0.95 725 3 0.363 20 0.109 2537

< 0.2 0.60 < 10 1160CMB19265 1.0 < 2 1.60 1.0 22 16 22 6.23 < 10 < 1 0.37 35 1.13 740 7 0.328 21 0.112 417

0.7 0.70 < 10 993CMB19266 2.7 < 2 3.11 1.0 20 16 18 6.11 < 10 < 1 0.29 35 1.11 799 < 1 0.345 19 0.107 2825

0.2 0.72 < 10 1140CMB19267 2.2 < 2 2.94 1.0 20 16 33 6.03 < 10 < 1 0.28 34 1.14 701 16 0.343 19 0.109 1825

0.3 0.60 < 10 837CMB19268 2.6 < 2 3.72 0.8 17 15 16 5.73 < 10 < 1 0.08 32 0.90 793 < 1 0.381 18 0.111 2086

< 0.2 0.58 < 10 823CMB19269 1.8 < 2 3.51 1.0 18 15 25 5.95 < 10 < 1 0.14 32 0.91 748 3 0.325 18 0.114 885

0.4 0.64 < 10 895CMB19270 2.5 < 2 3.14 1.5 18 15 58 5.80 < 10 < 1 0.18 33 0.96 821 < 1 0.343 19 0.107 1054

0.3 0.52 < 10 964CMB19271 1.2 < 2 2.28 1.1 21 16 50 6.07 < 10 < 1 0.22 36 0.70 602 2 0.258 21 0.115 856

0.2 0.63 < 10 997CMB19272 1.1 < 2 2.29 0.8 21 15 50 5.63 < 10 < 1 0.34 39 0.76 586 2 0.239 19 0.110 556

< 0.2 0.87 < 10 655CMB19273 0.6 < 2 2.17 0.6 21 23 28 5.45 < 10 < 1 0.45 35 0.95 562 1 0.234 25 0.108 134

< 0.2 0.87 < 10 371CMB19274 0.7 < 2 1.97 1.3 21 22 52 5.38 < 10 < 1 0.35 37 0.97 533 1 0.233 23 0.112 154

< 0.2 2.96 < 10 392CMB19275 < 0.5 < 2 3.64 0.6 36 91 41 5.60 < 10 < 1 0.46 < 10 3.06 787 1 0.716 73 0.069 133

0.4 0.62 < 10 801CMB19276 1.8 < 2 2.97 0.7 20 16 30 5.18 < 10 < 1 0.09 38 0.66 636 < 1 0.275 15 0.106 2155

1.2 0.63 < 10 978CMB19277 3.0 < 2 2.97 1.1 19 16 39 6.08 < 10 < 1 0.18 38 0.83 768 10 0.287 19 0.107 4486

1.0 0.80 < 10 598CMB19278 2.9 < 2 3.77 1.4 19 15 172 6.10 < 10 < 1 0.25 39 1.00 862 5 0.258 17 0.088 4035

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0.6 0.71 < 10 571CMB19279 3.0 < 2 3.32 1.3 20 15 126 6.13 < 10 < 1 0.21 39 0.88 766 3 0.255 17 0.097 2456

< 0.2 1.53 < 10 247CMB19280 < 0.5 < 2 1.51 0.5 18 3 11 5.71 10 < 1 0.76 32 1.21 820 3 0.186 2 0.174 < 2< 2


0.6 < 2 1.20 < 0.5 19 34 33 2.49 < 10 < 1 0.09 98 0.26 328 10 0.147 93 0.028 305< 2

< 0.2 0.70 < 10 1140CMB19282 1.0 < 2 2.16 1.7 20 15 18 5.69 < 10 < 1 0.36 40 0.92 657 1 0.280 19 0.112 456

< 0.2 0.71 < 10 464CMB19283 0.9 < 2 1.66 1.2 20 16 20 5.50 < 10 < 1 0.35 40 0.80 561 1 0.215 19 0.112 314

< 0.2 0.64 < 10 691CMB19284 0.8 < 2 1.78 1.1 19 16 42 5.73 < 10 < 1 0.29 38 0.78 551 2 0.247 18 0.113 286

< 0.2 0.59 < 10 853CMB19285 1.7 < 2 2.95 0.8 18 15 86 5.30 < 10 < 1 0.10 38 0.73 667 < 1 0.295 17 0.110 907

< 0.2 0.78 < 10 1060CMB19286 1.9 < 2 3.21 1.0 20 20 24 6.13 < 10 < 1 0.17 34 0.99 771 < 1 0.349 22 0.115 707

0.5 0.71 < 10 799CMB19287 1.8 < 2 3.50 1.2 18 15 108 5.81 < 10 < 1 0.12 34 0.91 837 1 0.335 18 0.111 1628

0.4 0.69 < 10 835CMB19288 2.2 < 2 2.66 1.2 19 16 122 6.32 < 10 < 1 0.12 38 0.85 722 3 0.348 17 0.117 3210

0.2 0.72 < 10 602CMB19289 1.3 < 2 2.70 0.7 21 16 72 6.05 < 10 < 1 0.29 40 0.85 666 3 0.256 19 0.118 128

< 0.2 0.81 < 10 268CMB19290 0.7 < 2 1.86 0.8 19 16 16 5.46 < 10 < 1 0.41 41 0.84 535 2 0.221 18 0.116 72

< 0.2 1.12 < 10 230CMB19291 0.7 < 2 1.89 < 0.5 19 15 15 5.02 < 10 < 1 0.59 43 0.94 636 2 0.216 17 0.122 75

< 0.2 1.37 < 10 242CMB19292 0.6 < 2 1.91 < 0.5 20 15 13 5.35 < 10 < 1 0.75 43 1.05 713 1 0.219 20 0.119 64

< 0.2 0.74 < 10 149CMB19293 0.7 < 2 1.83 < 0.5 18 15 25 5.22 < 10 < 1 0.33 40 0.72 529 1 0.189 15 0.119 97

< 0.2 0.63 < 10 272CMB19294 0.9 < 2 1.88 0.5 20 16 28 5.91 < 10 < 1 0.25 40 0.78 573 1 0.240 17 0.119 914

< 0.2 0.75 < 10 672CMB19295 1.1 < 2 2.11 < 0.5 21 17 42 5.99 < 10 < 1 0.30 41 0.92 628 1 0.305 19 0.116 815

< 0.2 0.58 < 10 1160CMB19296 2.1 < 2 2.92 0.5 19 15 37 5.66 < 10 < 1 0.17 40 0.79 652 1 0.314 18 0.114 309

< 0.2 0.74 < 10 749CMB19297 2.6 < 2 2.96 0.5 20 15 30 5.51 < 10 < 1 0.23 38 0.97 714 3 0.329 19 0.109 618

< 0.2 0.78 < 10 770CMB19298 1.7 < 2 2.91 0.6 19 14 24 5.52 < 10 < 1 0.35 36 1.00 666 8 0.283 21 0.099 127

< 0.2 0.59 < 10 525CMB19299 1.3 < 2 2.79 < 0.5 19 15 28 5.13 < 10 < 1 0.16 38 0.66 517 6 0.251 18 0.109 507

< 0.2 0.57 < 10 626CMB19300 < 0.5 < 2 1.60 0.6 19 15 21 5.53 < 10 < 1 0.35 34 0.66 360 2 0.184 19 0.102 84

< 0.2 0.65 < 10 455CMB19301 0.6 < 2 1.76 0.6 21 14 50 5.58 < 10 < 1 0.30 34 0.77 446 < 1 0.241 18 0.105 104

< 0.2 0.59 < 10 684CMB19302 2.2 < 2 2.26 0.8 20 16 70 5.61 < 10 < 1 0.14 40 0.68 556 1 0.292 21 0.098 367

< 0.2 1.71 < 10 742CMB19303 1.4 < 2 4.21 0.5 26 39 67 5.99 < 10 < 1 0.62 27 1.96 862 1 0.463 36 0.086 556

< 0.2 0.69 < 10 424CMB19304 1.2 < 2 1.78 0.6 22 16 22 6.12 < 10 < 1 0.28 40 0.70 421 5 0.251 21 0.108 157

< 0.2 0.54 < 10 888CMB19305 0.6 < 2 1.37 0.6 19 15 27 5.50 < 10 < 1 0.31 34 0.79 437 2 0.214 18 0.106 156

< 0.2 0.89 < 10 116CMB19306 1.6 < 2 1.04 < 0.5 9 6 8 3.02 < 10 < 1 0.54 67 0.40 503 3 0.157 2 0.084 174

< 0.2 1.26 < 10 275CMB19307 1.1 < 2 1.31 < 0.5 18 36 14 3.72 < 10 < 1 0.75 54 1.03 472 6 0.210 25 0.082 134

< 0.2 1.09 < 10 505CMB19308 2.1 < 2 2.37 0.6 24 27 46 5.31 < 10 < 1 0.41 39 1.16 664 7 0.348 29 0.097 537

< 0.2 0.74 < 10 1350CMB19309 2.3 < 2 2.99 0.7 19 17 15 5.66 < 10 < 1 0.15 35 0.97 755 < 1 0.429 17 0.104 8613

0.5 1.25 < 10 1020CMB19310 1.7 < 2 3.83 < 0.5 20 31 14 5.09 10 < 1 0.11 31 1.38 781 26 0.575 26 0.094 27316

0.6 0.60 < 10 817CMB19311 1.1 < 2 3.60 < 0.5 14 15 23 4.22 < 10 < 1 0.05 31 0.73 581 67 0.326 14 0.093 32013

< 0.2 2.23 < 10 678CMB19312 0.5 < 2 1.68 < 0.5 26 21 91 5.81 10 < 1 0.75 38 1.27 353 2 0.297 18 0.244 4< 2


0.5 < 2 1.18 < 0.5 10 29 26 2.39 < 10 < 1 0.10 89 0.31 307 5 0.140 40 0.038 254< 2

0.4 0.62 < 10 459CMB19314 2.6 < 2 2.83 0.6 19 13 40 5.84 < 10 < 1 0.05 39 0.75 605 2 0.363 15 0.103 23210


2.6 < 2 2.84 0.7 19 14 41 5.96 < 10 < 1 0.05 40 0.75 613 2 0.373 15 0.108 23310

< 0.2 2.69 < 10 225CMB19316 < 0.5 < 2 3.84 < 0.5 35 84 57 5.21 < 10 < 1 0.14 < 10 2.58 720 6 0.962 60 0.070 628

0.3 0.83 < 10 709CMB19317 1.2 < 2 2.96 0.7 20 27 33 5.27 < 10 < 1 0.06 31 0.88 550 3 0.390 23 0.113 2147

0.2 0.61 < 10 840CMB19318 2.5 < 2 3.59 0.6 15 9 10 5.34 < 10 < 1 0.03 37 0.78 742 < 1 0.383 13 0.119 1378

< 0.2 0.85 < 10 213CMB19319 1.6 < 2 3.92 0.5 14 8 7 5.86 < 10 < 1 0.03 32 0.99 832 3 0.434 11 0.124 9110

< 0.2 0.67 < 10 69CMB19320 1.2 < 2 2.94 0.6 14 9 < 1 6.11 < 10 < 1 0.02 35 0.73 843 1 0.334 10 0.129 437

< 0.2 1.05 < 10 524CMB19321 1.8 < 2 4.02 0.8 16 8 2 5.94 < 10 < 1 0.03 34 1.14 1030 2 0.507 11 0.130 9510

< 0.2 0.65 < 10 358CMB19322 1.5 < 2 2.77 0.6 15 9 6 6.31 < 10 < 1 0.02 35 0.68 796 < 1 0.381 11 0.127 957

< 0.2 0.44 < 10 307CMB19323 1.5 < 2 2.36 0.6 15 9 6 5.84 < 10 < 1 0.02 39 0.45 722 < 1 0.263 10 0.123 1005

< 0.2 0.84 < 10 373CMB19324 1.9 < 2 3.94 0.5 13 5 3 4.96 < 10 < 1 0.03 44 0.94 1090 2 0.494 7 0.110 837

< 0.2 0.82 < 10 444CMB19325 1.7 < 2 2.82 0.6 16 7 1 5.83 < 10 < 1 0.11 43 0.74 793 3 0.395 13 0.105 957

< 0.2 0.59 < 10 296CMB19326 1.5 < 2 2.71 0.5 17 8 4 5.56 < 10 < 1 0.05 38 0.61 771 2 0.337 14 0.095 287

< 0.2 0.58 < 10 209CMB19327 1.4 < 2 2.94 0.7 17 10 1 5.75 < 10 < 1 0.03 40 0.64 768 2 0.313 14 0.089 10112

< 0.2 0.85 < 10 202CMB19328 1.6 < 2 2.71 0.6 22 10 < 1 5.68 < 10 < 1 0.08 39 0.90 631 5 0.392 19 0.102 389

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< 0.2 0.86 < 10 560CMB19329 1.6 < 2 4.53 0.8 14 9 < 1 5.87 < 10 < 1 0.05 34 1.10 1100 < 1 0.501 11 0.108 1289

< 0.2 1.23 < 10 381CMB19330 2.1 < 2 1.20 < 0.5 21 12 < 1 6.10 10 < 1 0.32 37 0.95 311 2 0.335 29 0.140 565

0.3 0.52 < 10 884CMB19331 1.3 < 2 2.07 0.6 14 11 35 6.17 < 10 < 1 0.04 41 0.51 559 < 1 0.308 10 0.145 728

< 0.2 2.43 < 10 385CMB19332 < 0.5 < 2 3.16 < 0.5 31 70 47 4.88 < 10 < 1 0.14 < 10 2.32 638 < 1 0.820 56 0.073 135

< 0.2 0.71 < 10 545CMB19333 2.0 < 2 2.15 0.6 17 13 38 5.34 < 10 < 1 0.13 45 0.79 556 2 0.336 16 0.089 436

< 0.2 0.52 < 10 755CMB19334 1.4 < 2 2.79 0.5 16 27 < 1 4.93 < 10 < 1 0.05 32 0.67 610 < 1 0.325 11 0.076 196

< 0.2 0.44 < 10 313CMB19335 0.9 < 2 2.80 < 0.5 12 26 < 1 3.91 < 10 < 1 0.05 28 0.57 518 < 1 0.213 9 0.033 325


0.9 < 2 2.82 < 0.5 12 26 < 1 3.87 < 10 < 1 0.04 29 0.55 514 < 1 0.206 8 0.032 333

< 0.2 0.27 < 10 347CMB19337 0.5 < 2 1.65 < 0.5 14 38 < 1 4.38 < 10 < 1 0.04 30 0.35 334 < 1 0.128 8 0.043 147

< 0.2 0.58 < 10 474CMB19338 0.7 < 2 2.29 < 0.5 13 35 2 3.65 < 10 < 1 0.20 30 0.69 487 < 1 0.183 8 0.050 176

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0.04 2 34 0.36CMB19201 < 10 < 10 70 < 10 61 6.0 1.044 2.788

0.03 < 2 20 0.32CMB19202 < 10 22 60 < 10 103 21.8 1.096 2.768

0.02 < 2 21 0.33CMB19203 < 10 < 10 61 < 10 82 3.9 1.06610

0.03 2 45 0.38CMB19204 < 10 < 10 60 < 10 122 5.3 1.0989

0.04 2 86 0.35CMB19205 < 10 16 52 < 10 66 13.4 1.0396

0.04 2 98 0.28CMB19206 < 10 219 68 < 10 85 215 1.0419

0.04 2 78 0.31CMB19207 < 10 14 57 < 10 83 10.5 1.0679

0.03 2 44 0.31CMB19208 < 10 11 61 < 10 95 12.2 1.04010

0.04 2 74 0.32CMB19209 < 10 42 52 < 10 73 38.3 1.0309

0.05 2 121 0.33CMB19210 < 10 139 60 < 10 104 135 1.05410

0.04 3 124 0.29CMB19211 < 10 1270 61 < 10 86 1220 1.0468


< 10 1340 61 < 10 87 1250 1.0949

0.06 < 2 158 0.29CMB19213 < 10 73 51 < 10 67 67.4 1.0369

0.05 2 141 0.26CMB19214 < 10 259 73 < 10 67 261 1.0358

0.04 < 2 137 0.31CMB19215 < 10 179 76 < 10 83 173 1.0229

0.03 < 2 100 0.31CMB19216 < 10 43 72 < 10 95 40.6 1.08610

0.05 2 184 0.26CMB19217 < 10 2220 199 < 10 71 2250 1.0534


< 10 2360 203 < 10 72 2200 1.0604

0.06 3 203 0.30CMB19219 < 10 588 213 < 10 220 567 1.0408

0.03 < 2 166 0.28CMB19220 < 10 693 129 < 10 122 670 1.0078

0.03 < 2 170 0.29CMB19221 < 10 1320 197 < 10 83 1240 1.0919

0.04 < 2 178 0.31CMB19222 < 10 2060 194 < 10 98 2060 1.006 2.856

0.15 < 2 104 0.37CMB19251 < 10 677 147 < 10 86 660 1.09817

0.06 < 2 199 0.22CMB19252 < 10 1630 146 < 10 89 1640 1.0309

0.05 < 2 219 0.20CMB19253 < 10 1660 154 < 10 98 1670 1.06910

0.04 < 2 40 0.30CMB19254 < 10 < 10 112 < 10 50 5.1 1.02010


< 10 1020 81 < 10 89 997 1.0972

0.04 < 2 219 0.25CMB19256 < 10 774 191 < 10 82 747 1.0099

0.05 < 2 240 0.27CMB19257 < 10 642 222 < 10 116 629 1.0669

0.05 < 2 377 0.32CMB19258 < 10 2090 192 < 10 103 2120 1.0979

0.05 < 2 361 0.28CMB19259 < 10 707 222 < 10 91 652 1.0728

0.04 < 2 387 0.31CMB19260 < 10 272 281 < 10 87 258 1.008 2.868

0.04 < 2 456 0.31CMB19261 < 10 1140 211 < 10 79 1110 1.0548

0.11 < 2 228 0.28CMB19262 < 10 46 123 < 10 114 38.5 1.03313

0.22 3 123 0.26CMB19263 < 10 < 10 109 < 10 173 2.3 1.08115

0.13 2 258 0.37CMB19264 < 10 < 10 68 < 10 158 6.8 1.0888

0.05 < 2 170 0.37CMB19265 < 10 < 10 85 < 10 106 6.3 1.0657

0.07 < 2 276 0.35CMB19266 < 10 1040 131 < 10 112 981 1.0669

0.07 < 2 196 0.29CMB19267 < 10 569 107 < 10 109 540 1.0989

0.06 < 2 224 0.30CMB19268 < 10 726 139 < 10 86 693 1.0098

0.06 2 197 0.28CMB19269 < 10 227 103 < 10 127 223 1.0938

0.06 < 2 167 0.31CMB19270 < 10 166 111 < 10 184 163 1.0189

0.11 < 2 142 0.36CMB19271 < 10 32 80 < 10 157 29.8 1.0106

0.08 2 124 0.40CMB19272 < 10 32 76 < 10 162 29.6 1.0185

0.07 2 84 0.35CMB19273 < 10 < 10 78 < 10 113 5.6 1.0586

0.09 < 2 54 0.37CMB19274 < 10 < 10 77 < 10 128 6.6 1.0046

0.10 < 2 51 0.33CMB19275 < 10 < 10 126 < 10 80 2.0 1.08517

0.13 2 156 0.37CMB19276 < 10 776 109 < 10 70 758 1.0477

0.07 < 2 161 0.36CMB19277 < 10 1520 163 < 10 103 1400 1.0688

0.10 2 208 0.35CMB19278 < 10 1220 164 < 10 111 1160 1.0818

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0.08 3 182 0.38CMB19279 < 10 746 159 < 10 99 715 1.0208

0.06 2 45 0.29CMB19280 < 10 < 10 113 < 10 52 5.1 1.09511


< 10 1020 79 < 10 90 1000 1.0432

0.07 < 2 109 0.38CMB19282 < 10 16 77 < 10 100 14.3 1.0087

0.03 < 2 74 0.39CMB19283 < 10 < 10 77 < 10 100 9.0 1.0385

0.05 < 2 76 0.37CMB19284 < 10 < 10 72 < 10 95 5.2 1.0656

0.07 < 2 111 0.37CMB19285 < 10 294 103 < 10 87 289 1.0728

0.07 2 127 0.33CMB19286 < 10 141 109 < 10 137 134 1.06210

0.07 3 148 0.34CMB19287 < 10 508 108 < 10 122 477 1.0559

0.07 < 2 120 0.35CMB19288 < 10 19 81 < 10 103 15.4 1.0768

0.09 < 2 110 0.38CMB19289 < 10 15 83 < 10 79 12.2 1.0867

0.04 < 2 63 0.35CMB19290 < 10 < 10 71 < 10 68 3.5 1.0447

0.02 3 36 0.36CMB19291 < 10 < 10 69 < 10 70 3.6 1.0989

0.02 < 2 38 0.35CMB19292 < 10 < 10 69 < 10 74 3.2 1.05910

0.04 < 2 41 0.33CMB19293 < 10 < 10 69 < 10 58 5.1 1.0588

0.04 < 2 55 0.40CMB19294 < 10 < 10 78 < 10 66 7.0 1.0757

0.06 < 2 66 0.41CMB19295 < 10 < 10 73 < 10 77 4.2 1.0808

0.07 < 2 151 0.40CMB19296 < 10 39 88 < 10 72 34.5 1.0827

0.12 2 136 0.38CMB19297 < 10 163 94 < 10 75 154 1.0708

0.10 3 125 0.35CMB19298 < 10 < 10 65 < 10 84 7.6 1.0696

0.10 3 91 0.37CMB19299 < 10 56 76 < 10 94 57.1 1.0865

0.05 < 2 57 0.35CMB19300 < 10 < 10 65 < 10 114 5.2 1.0083

0.14 < 2 42 0.36CMB19301 < 10 < 10 65 < 10 129 3.6 1.0465

0.08 2 74 0.39CMB19302 < 10 73 85 < 10 148 75.9 1.0298

0.13 < 2 136 0.35CMB19303 < 10 187 93 < 10 138 193 1.07911

0.05 < 2 70 0.41CMB19304 < 10 28 75 < 10 96 28.5 1.069 2.886

0.06 2 67 0.34CMB19305 < 10 < 10 66 < 10 84 4.1 1.031 2.855

0.03 < 2 18 0.27CMB19306 < 10 < 10 25 < 10 72 6.7 1.014 2.746

0.06 < 2 29 0.32CMB19307 < 10 < 10 61 < 10 62 10.9 1.074 2.846

0.16 2 82 0.38CMB19308 < 10 130 107 < 10 90 129 1.0789

0.06 < 2 186 0.34CMB19309 < 10 288 109 < 10 128 297 1.0589

0.08 < 2 161 0.32CMB19310 < 10 977 106 < 10 94 960 1.02811

0.09 < 2 158 0.26CMB19311 < 10 1100 84 < 10 66 1100 1.0256

0.07 < 2 31 0.17CMB19312 < 10 < 10 78 < 10 65 5.3 1.08912


< 10 849 59 < 10 106 841 1.0582

0.13 2 148 0.32CMB19314 < 10 765 169 < 10 137 760 1.0759


< 10 780 174 < 10 139 756 1.0169

0.21 < 2 82 0.30CMB19316 < 10 160 117 < 10 90 147 1.08816

0.14 < 2 141 0.31CMB19317 < 10 576 108 < 10 130 564 1.078 2.928

0.05 < 2 152 0.31CMB19318 < 10 605 94 < 10 90 617 1.0408

0.04 2 129 0.26CMB19319 < 10 354 49 < 10 66 373 1.0328

0.03 2 94 0.30CMB19320 < 10 160 45 < 10 56 168 1.0128

0.05 < 2 160 0.30CMB19321 < 10 305 54 < 10 75 312 1.0039

0.03 < 2 132 0.28CMB19322 < 10 324 59 < 10 61 339 1.0738

0.03 < 2 155 0.29CMB19323 < 10 349 72 < 10 62 357 1.0287

0.04 < 2 190 0.25CMB19324 < 10 277 55 < 10 60 272 1.0598

0.03 2 180 0.29CMB19325 < 10 360 59 < 10 64 361 1.0759

0.03 3 123 0.33CMB19326 < 10 68 79 < 10 76 69.5 1.0438

0.03 2 115 0.34CMB19327 < 10 381 76 < 10 78 382 1.0638

0.03 < 2 119 0.34CMB19328 < 10 100 74 < 10 121 94.9 1.05010

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0.05 2 173 0.28CMB19329 < 10 478 69 < 10 81 472 1.049 2.938

0.02 < 2 41 0.23CMB19330 < 10 172 81 < 10 104 171 1.04711

0.09 3 99 0.26CMB19331 < 10 126 72 < 10 48 130 1.0708

0.15 2 44 0.26CMB19332 < 10 < 10 116 < 10 53 7.7 1.07114

0.08 < 2 69 0.31CMB19333 < 10 95 99 < 10 72 96.5 1.06111

0.04 < 2 100 0.37CMB19334 < 10 58 100 < 10 77 54.4 1.0376

0.03 < 2 87 0.31CMB19335 < 10 143 77 < 10 62 144 1.0595


< 10 147 76 < 10 61 142 1.0075

0.02 2 45 0.41CMB19337 < 10 56 86 < 10 68 57.3 1.069 2.783

0.03 < 2 68 0.30CMB19338 < 10 26 66 < 10 74 24.6 1.022 2.834

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Quality Control



30.9 0.32 15 186GXR-1 Meas 0.9 1580 0.88 3.5 10 7 1090 25.3 < 10 4 0.03 < 10 0.14 854 15 0.052 36 0.036 635367

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.7 2.46 < 10 30GXR-4 Meas 1.4 15 0.90 0.5 15 51 5930 3.39 10 < 1 1.30 43 1.60 128 325 0.105 36 0.115 4399

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

21.7 3.07 19 1110GXR-2 Meas 1.1 < 2 0.80 4.8 10 25 83 2.29 < 10 3 0.54 22 0.54 1070 1 0.201 18 0.061 78516

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.3 6.00 < 10 883GXR-6 Meas 0.9 < 2 0.17 0.5 14 73 63 5.95 20 < 1 0.81 11 0.38 925 1 0.120 23 0.030 89234

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2510 5.81 2070

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

< 0.2 0.58 < 10 1520CMB19213 Orig 1.7 < 2 3.06 0.6 16 8 3 5.47 < 10 < 1 0.10 41 0.76 804 1 0.432 12 0.119 328

< 0.2 0.61 < 10 1520CMB19213 Dup 1.8 < 2 3.08 0.6 16 8 3 5.60 < 10 < 1 0.11 42 0.80 814 < 1 0.443 13 0.118 319

0.4 0.53 < 10 875CMB19256 Orig 2.8 < 2 2.66 0.5 13 9 22 5.69 < 10 < 1 0.03 60 0.68 606 2 0.420 10 0.092 2763

0.4 0.50 < 10 838CMB19256 Dup 2.6 < 2 2.54 0.6 12 9 17 5.44 < 10 < 1 0.03 57 0.65 565 2 0.401 12 0.088 2633

1.6 0.64 < 10 670CMB19258 Orig 3.2 < 2 3.82 0.6 15 15 47 4.77 10 < 1 0.03 47 0.88 765 < 1 0.451 13 0.109 5546

1.7 0.67 < 10 707CMB19258 Split 3.3 < 2 3.96 0.6 16 16 53 5.10 10 < 1 0.03 50 0.93 793 < 1 0.474 13 0.111 57510

< 0.2 0.58 < 10 833CMB19269 Orig 1.8 < 2 3.54 1.0 18 15 26 6.01 < 10 < 1 0.14 32 0.92 756 2 0.322 17 0.117 886

< 0.2 0.58 < 10 814CMB19269 Dup 1.8 < 2 3.48 0.9 17 15 25 5.88 < 10 < 1 0.13 31 0.91 740 4 0.328 18 0.111 874

1.0 0.80 < 10 598CMB19278 Orig 2.9 < 2 3.77 1.4 19 15 172 6.10 < 10 < 1 0.25 39 1.00 862 5 0.258 17 0.088 4035

0.9 0.79 < 10 566CMB19278 Split 2.9 < 2 3.56 1.4 19 14 171 5.80 < 10 < 1 0.23 38 0.95 777 4 0.252 15 0.096 3785

< 0.2 0.63 < 10 694CMB19284 Orig 0.8 < 2 1.79 1.1 19 16 42 5.74 < 10 < 1 0.29 38 0.78 545 2 0.246 18 0.114 287

< 0.2 0.64 < 10 687CMB19284 Dup 0.8 < 2 1.77 1.1 19 16 41 5.72 < 10 < 1 0.29 38 0.79 558 2 0.247 17 0.111 276

0.4 0.69 < 10 835CMB19288 Orig 2.2 < 2 2.66 1.2 19 16 122 6.32 < 10 < 1 0.12 38 0.85 722 3 0.348 17 0.117 3210

0.4 0.64 < 10 753CMB19288 Split 2.0 < 2 2.44 1.1 17 14 113 5.69 < 10 < 1 0.11 35 0.78 661 3 0.328 16 0.105 309

< 0.2 1.26 < 10 276CMB19307 Orig 1.1 < 2 1.32 < 0.5 18 36 15 3.73 < 10 < 1 0.76 55 1.03 475 6 0.210 26 0.082 124

< 0.2 1.27 < 10 274CMB19307 Dup 1.1 < 2 1.30 < 0.5 18 36 14 3.71 < 10 < 1 0.74 54 1.02 468 5 0.210 24 0.082 135

0.2 0.61 < 10 840CMB19318 Orig 2.5 < 2 3.59 0.6 15 9 10 5.34 < 10 < 1 0.03 37 0.78 742 < 1 0.383 13 0.119 1378

0.4 0.65 < 10 853CMB19318 Split 2.6 < 2 3.64 < 0.5 15 10 10 5.51 < 10 < 1 0.03 38 0.79 751 < 1 0.405 13 0.114 1398

< 0.2 0.65 < 10 360CMB19322 Orig 1.6 < 2 2.79 0.6 16 9 8 6.38 < 10 < 1 0.03 35 0.69 805 < 1 0.388 12 0.123 958

< 0.2 0.65 < 10 357CMB19322 Dup 1.5 < 2 2.76 0.6 15 8 4 6.25 < 10 < 1 0.02 35 0.67 787 < 1 0.374 10 0.131 946

CMB19329 Orig

CMB19329 Dup

< 0.2 0.44 < 10 317CMB19335 Orig 0.9 < 2 2.80 < 0.5 12 26 < 1 3.95 < 10 < 1 0.05 29 0.57 522 < 1 0.211 8 0.033 335

< 0.2 0.44 < 10 310CMB19335 Dup 0.9 < 2 2.80 0.5 12 26 < 1 3.87 < 10 < 1 0.05 28 0.57 514 < 1 0.214 9 0.032 314

< 0.2 0.58 < 10 474CMB19338 Orig 0.7 < 2 2.29 < 0.5 13 35 2 3.65 < 10 < 1 0.20 30 0.69 487 < 1 0.183 8 0.050 176

< 0.2 0.58 < 10 470CMB19338 Split 0.7 < 2 2.28 < 0.5 13 34 2 3.63 < 10 < 1 0.20 29 0.69 479 < 1 0.185 8 0.049 155


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.011 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.012 < 1 < 0.001 < 2< 2



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Quality Control



0.22 78 160GXR-1 Meas < 10 30 78 196 6491

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2450 2640

DH-1a Cert 2630 2630

DH-1a Meas 2620

DH-1a Cert 2630

1.81 3 71GXR-4 Meas < 10 < 10 82 16 677

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 32 90GXR-2 Meas < 10 < 10 52 < 10 6085

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 5 30GXR-6 Meas < 10 < 10 166 < 10 11522

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 289

SY-2 Cert 284

SY-2 Meas 286

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10000

BL-3 Cert 10200

BL-4a Meas 1280

BL-4a Cert 1250

BL-4a Meas 1250

BL-4a Cert 1250

0.06 < 2 158 0.28CMB19213 Orig < 10 76 50 < 10 659

0.06 3 158 0.29CMB19213 Dup < 10 70 52 < 10 689

0.04 < 2 224 0.26CMB19256 Orig < 10 790 194 < 10 859

0.04 < 2 214 0.24CMB19256 Dup < 10 757 188 < 10 809

0.05 < 2 377 0.32CMB19258 Orig < 10 2090 192 < 10 103 2120 1.0979

0.05 5 400 0.32CMB19258 Split < 10 2220 199 < 10 106 2180 1.0069

0.07 2 199 0.29CMB19269 Orig < 10 230 104 < 10 1288

0.06 2 195 0.27CMB19269 Dup < 10 224 101 < 10 1278

0.10 2 208 0.35CMB19278 Orig < 10 1220 164 < 10 111 1160 1.0818

0.09 < 2 193 0.36CMB19278 Split < 10 1170 154 < 10 104 1170 1.0698

0.05 < 2 77 0.38CMB19284 Orig < 10 < 10 73 < 10 956

0.05 3 76 0.36CMB19284 Dup < 10 < 10 71 < 10 946

0.07 < 2 120 0.35CMB19288 Orig < 10 19 81 < 10 103 15.4 1.0768

0.07 < 2 109 0.32CMB19288 Split < 10 17 73 < 10 95 15.3 1.0368

0.06 < 2 29 0.32CMB19307 Orig < 10 11 61 < 10 626

0.06 < 2 29 0.31CMB19307 Dup < 10 < 10 60 < 10 616

0.05 < 2 152 0.31CMB19318 Orig < 10 605 94 < 10 90 617 1.0408

0.05 < 2 154 0.29CMB19318 Split < 10 612 95 < 10 91 623 1.0358

0.03 < 2 134 0.28CMB19322 Orig < 10 322 60 < 10 628

0.03 < 2 131 0.28CMB19322 Dup < 10 325 59 < 10 608

CMB19329 Orig 2.93

CMB19329 Dup 2.94

0.03 < 2 86 0.31CMB19335 Orig < 10 146 77 < 10 625

0.03 < 2 87 0.32CMB19335 Dup < 10 140 77 < 10 625

0.03 < 2 68 0.30CMB19338 Orig < 10 26 66 < 10 74 24.6 1.022 2.834

0.03 3 65 0.29CMB19338 Split < 10 27 65 < 10 74 24.8 1.043 2.814


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

Page 9 of 9

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

25-Jul-08

10-Jul-08

A08-3945



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-3945

Notes:




Quality Control


Document Page 193




< 0.2 0.37 < 10 12CMB19351 1.4 < 2 2.68 < 0.5 8 56 3 3.23 < 10 < 1 0.03 31 0.32 345 2 0.171 11 0.062 1815

< 0.2 0.25 < 10 < 10CMB19352 1.8 < 2 1.87 < 0.5 6 53 < 1 3.25 < 10 < 1 < 0.01 53 0.14 203 < 1 0.176 8 0.063 117

< 0.2 0.30 < 10 13CMB19353 2.3 < 2 2.88 < 0.5 8 79 < 1 2.98 < 10 < 1 0.02 36 0.23 311 < 1 0.151 11 0.077 1206

< 0.2 0.45 < 10 13CMB19354 2.3 < 2 2.88 < 0.5 9 70 < 1 3.31 < 10 < 1 0.03 27 0.33 341 < 1 0.160 13 0.085 357

< 0.2 0.30 < 10 < 10CMB19355 1.1 < 2 2.68 < 0.5 6 40 < 1 2.14 < 10 < 1 0.01 21 0.22 279 < 1 0.138 10 0.025 124

< 0.2 1.49 < 10 61CMB19356 1.4 < 2 2.15 < 0.5 11 208 < 1 2.47 < 10 < 1 0.30 18 1.15 384 < 1 0.120 45 0.070 83


1.9 < 2 2.56 < 0.5 13 235 < 1 2.97 < 10 < 1 0.32 19 1.45 479 < 1 0.173 53 0.069 8< 2

< 0.2 0.27 < 10 10CMB19358 0.8 < 2 0.82 < 0.5 6 45 < 1 2.16 < 10 < 1 0.01 18 0.19 109 < 1 0.134 10 0.029 < 2< 2


0.8 < 2 0.82 < 0.5 6 46 < 1 2.18 < 10 < 1 0.01 19 0.19 113 < 1 0.138 11 0.029 < 23

< 0.2 0.16 < 10 < 10CMB19360 < 0.5 < 2 2.11 < 0.5 6 58 < 1 2.42 < 10 < 1 < 0.01 20 0.10 183 < 1 0.101 9 0.026 < 22

< 0.2 0.16 < 10 < 10CMB19361 < 0.5 < 2 2.17 < 0.5 6 61 < 1 2.24 < 10 < 1 < 0.01 26 0.05 170 < 1 0.058 8 0.029 2< 2

< 0.2 2.06 < 10 187CMB19362 1.5 < 2 2.21 < 0.5 23 91 69 5.13 10 < 1 0.79 17 1.70 572 1 0.110 38 0.087 207

< 0.2 1.59 < 10 111CMB19363 1.5 < 2 2.13 < 0.5 17 86 111 4.06 < 10 < 1 0.44 18 1.19 454 1 0.121 29 0.086 395

< 0.2 2.78 < 10 366CMB19364 < 0.5 < 2 2.03 < 0.5 25 29 60 4.35 < 10 < 1 0.52 24 1.15 362 < 1 0.391 27 0.161 < 2< 2


< 0.5 < 2 1.14 < 0.5 9 29 30 2.38 < 10 < 1 0.11 89 0.28 306 4 0.124 42 0.043 2762

< 0.2 0.37 < 10 15CMB19366 < 0.5 < 2 2.27 < 0.5 11 6 178 3.85 < 10 < 1 0.01 59 0.06 115 3 0.095 6 0.078 44

< 0.2 0.45 < 10 < 10CMB19367 < 0.5 < 2 1.58 < 0.5 10 13 129 4.74 < 10 < 1 < 0.01 42 0.10 100 < 1 0.097 7 0.098 66

< 0.2 0.36 < 10 < 10CMB19368 0.7 < 2 2.33 0.5 12 17 < 1 6.44 < 10 < 1 < 0.01 23 0.30 254 < 1 0.071 14 0.130 519

0.4 0.62 < 10 14CMB19369 0.9 < 2 2.20 0.6 15 17 < 1 6.61 < 10 < 1 < 0.01 27 0.55 301 < 1 0.086 18 0.124 1322

6.0 0.56 < 10 641CMB19370 1.2 < 2 2.42 < 0.5 14 17 < 1 5.87 < 10 < 1 0.01 26 0.59 320 < 1 0.187 16 0.127 2321

< 0.2 0.80 < 10 11CMB19371 0.6 < 2 3.56 < 0.5 16 15 < 1 5.88 < 10 < 1 < 0.01 25 0.73 389 < 1 0.108 19 0.112 79

< 0.2 0.71 < 10 < 10CMB19372 PREP DUP FROM CMB19371

< 0.5 < 2 3.56 0.5 14 15 < 1 5.91 < 10 < 1 < 0.01 22 0.70 384 < 1 0.065 18 0.116 610

< 0.2 0.46 < 10 11CMB19373 0.7 < 2 3.93 < 0.5 11 14 < 1 5.42 < 10 < 1 < 0.01 25 0.33 338 < 1 0.088 11 0.100 2912


0.7 < 2 4.03 < 0.5 11 15 < 1 5.64 < 10 < 1 < 0.01 25 0.35 352 < 1 0.090 12 0.104 2912

< 0.2 0.92 < 10 19CMB19375 0.6 < 2 3.13 < 0.5 15 17 < 1 6.23 < 10 < 1 < 0.01 29 0.64 394 < 1 0.063 19 0.127 3316

< 0.2 0.99 < 10 31CMB19376 1.3 < 2 4.23 0.5 19 14 < 1 6.41 < 10 < 1 0.01 35 1.06 627 < 1 0.118 20 0.116 11313

< 0.2 2.30 < 10 126CMB19377 < 0.5 < 2 1.57 < 0.5 24 43 26 5.23 < 10 < 1 0.35 20 0.77 205 < 1 0.411 40 0.142 < 2< 2

< 0.2 0.93 < 10 24CMB19378 1.0 < 2 4.19 0.5 17 15 < 1 6.14 < 10 < 1 0.01 32 0.94 591 < 1 0.089 19 0.121 10011


< 0.5 < 2 1.16 < 0.5 9 29 27 2.41 < 10 < 1 0.11 92 0.28 307 4 0.125 42 0.044 2813

< 0.2 1.06 < 10 22CMB19380 0.8 < 2 3.49 0.6 18 16 3 6.27 < 10 < 1 0.01 31 0.90 514 < 1 0.112 20 0.111 7514

< 0.2 1.10 < 10 15CMB19381 1.3 < 2 3.82 0.6 21 20 < 1 6.19 < 10 < 1 0.01 27 1.15 646 < 1 0.103 22 0.104 3211

< 0.2 0.94 < 10 23CMB19382 0.8 < 2 3.42 < 0.5 17 50 2 4.23 < 10 < 1 0.02 21 0.85 499 < 1 0.095 17 0.130 2511

< 0.2 0.55 < 10 77CMB19383 1.5 < 2 3.57 < 0.5 13 15 < 1 5.27 < 10 < 1 0.02 26 0.58 400 < 1 0.168 13 0.128 118

0.3 0.50 < 10 < 10CMB19384 1.1 < 2 3.17 < 0.5 10 14 < 1 5.14 < 10 < 1 < 0.01 21 0.42 321 < 1 0.062 13 0.127 157

< 0.2 0.94 < 10 16CMB19385 2.3 < 2 3.22 < 0.5 16 15 < 1 4.77 < 10 < 1 0.01 27 0.94 524 < 1 0.134 20 0.143 339

< 0.2 0.89 < 10 16CMB19386 2.7 < 2 2.77 < 0.5 14 16 < 1 5.30 < 10 < 1 0.01 29 0.82 433 < 1 0.138 18 0.132 189

0.4 0.82 < 10 18CMB19387 3.0 < 2 2.61 < 0.5 14 21 < 1 6.17 < 10 < 1 0.02 30 0.81 421 < 1 0.161 21 0.121 2810

< 0.2 0.60 < 10 15CMB19388 2.7 < 2 2.95 < 0.5 12 15 22 5.89 < 10 < 1 0.02 27 0.67 404 < 1 0.179 17 0.125 147

< 0.2 0.64 < 10 17CMB19389 1.8 < 2 2.71 < 0.5 14 29 5 4.48 < 10 < 1 0.03 24 0.65 350 < 1 0.139 20 0.113 76

< 0.2 1.81 < 10 31CMB19390 1.2 < 2 2.98 < 0.5 19 175 33 4.87 < 10 < 1 0.09 24 2.02 686 < 1 0.117 81 0.119 34

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0.03 < 2 66 0.22CMB19351 < 10 12 91 < 10 22 11.3 1.070 2.803

0.02 < 2 48 0.21CMB19352 < 10 26 140 < 10 12 28.8 1.017 2.762

0.02 < 2 68 0.26CMB19353 < 10 523 128 < 10 16 531 1.081 2.732

0.02 < 2 89 0.25CMB19354 < 10 157 100 < 10 21 159 1.015 2.814

0.02 < 2 60 0.19CMB19355 < 10 46 46 < 10 12 42.2 1.0862

0.02 < 2 199 0.16CMB19356 < 10 17 67 < 10 40 18.7 1.0616


< 10 19 78 < 10 45 18.8 1.0487

< 0.01 < 2 41 0.19CMB19358 < 10 < 10 40 < 10 10 4.4 1.0642

< 0.01 < 2 41 0.20CMB19359 PULP DUP FROM CMB19358

< 10 < 10 41 < 10 10 4.0 1.0152

0.02 < 2 38 0.22CMB19360 < 10 < 10 43 < 10 5 4.8 1.0691

0.02 < 2 52 0.22CMB19361 < 10 < 10 42 < 10 3 6.3 1.0951

0.03 < 2 239 0.31CMB19362 < 10 91 121 < 10 86 87.5 1.06910

0.03 < 2 223 0.30CMB19363 < 10 184 102 < 10 60 175 1.0068

0.08 < 2 56 0.16CMB19364 < 10 < 10 91 < 10 53 1.2 1.0028


< 10 870 58 < 10 111 847 1.0682

0.06 < 2 105 0.23CMB19366 < 10 13 29 < 10 4 15.2 1.040 2.793

0.04 < 2 105 0.26CMB19367 < 10 18 41 < 10 6 22.9 1.080 2.863

0.02 2 84 0.19CMB19368 < 10 20 46 < 10 24 20.1 1.058 2.893

0.02 < 2 117 0.28CMB19369 < 10 104 71 < 10 36 110 1.078 2.844

0.04 < 2 92 0.28CMB19370 < 10 179 63 < 10 36 181 1.027 2.854

0.03 < 2 132 0.26CMB19371 < 10 28 55 < 10 40 29.6 1.0385


< 10 29 53 < 10 40 27.9 1.0664

0.03 < 2 131 0.27CMB19373 < 10 186 58 < 10 19 189 1.0053


< 10 193 58 < 10 20 190 1.0113

0.03 < 2 203 0.24CMB19375 < 10 192 69 < 10 42 185 1.078 2.845

0.03 < 2 127 0.31CMB19376 < 10 517 71 < 10 76 517 1.0595

0.04 < 2 81 0.13CMB19377 < 10 < 10 159 < 10 48 1.0 1.0213

0.03 2 124 0.25CMB19378 < 10 493 67 < 10 68 484 1.0225


< 10 876 59 < 10 115 851 1.0782

0.05 2 170 0.31CMB19380 < 10 172 69 < 10 54 169 1.0366

0.06 3 137 0.30CMB19381 < 10 201 70 < 10 71 197 1.0475

0.08 < 2 160 0.23CMB19382 < 10 107 63 < 10 49 107 1.0864

0.03 < 2 87 0.27CMB19383 < 10 64 70 < 10 39 62.5 1.0874

0.03 < 2 103 0.21CMB19384 < 10 103 68 < 10 28 104 1.0573

0.03 < 2 124 0.29CMB19385 < 10 197 111 < 10 62 198 1.0285

0.02 2 142 0.28CMB19386 < 10 132 100 < 10 55 134 1.0195

0.02 2 98 0.29CMB19387 < 10 235 97 < 10 56 229 1.0436

0.03 < 2 77 0.27CMB19388 < 10 76 81 < 10 52 73.2 1.0016

0.03 < 2 108 0.27CMB19389 < 10 41 60 < 10 35 41.9 1.035 2.894

0.03 < 2 233 0.28CMB19390 < 10 < 10 62 < 10 85 4.3 1.032 2.946

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Quality Control



30.5 0.38 14 330GXR-1 Meas 0.8 1520 0.82 3.1 9 7 1110 25.6 < 10 4 0.02 < 10 0.14 736 15 0.065 37 0.040 641353

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.6 2.94 < 10 23GXR-4 Meas 1.4 28 0.96 < 0.5 15 53 6010 3.47 10 < 1 1.41 48 1.66 141 323 0.130 38 0.117 4398

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

21.6 3.63 22 1210GXR-2 Meas 1.2 < 2 0.85 4.7 10 27 83 2.28 < 10 4 0.59 24 0.57 1070 < 1 0.242 19 0.061 78115

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.3 7.43 < 10 994GXR-6 Meas 1.0 < 2 0.20 0.8 15 82 67 6.27 20 < 1 0.96 12 0.43 993 1 0.154 26 0.032 95223

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2620 5.78 2170

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

< 0.2 1.58 < 10 112CMB19363 Orig 1.5 < 2 2.13 < 0.5 18 86 109 4.04 < 10 < 1 0.44 18 1.19 454 1 0.122 29 0.086 385

< 0.2 1.60 < 10 111CMB19363 Dup 1.5 < 2 2.12 < 0.5 17 85 112 4.08 < 10 < 1 0.44 18 1.19 454 1 0.121 28 0.086 405

CMB19375 Orig

CMB19375 Dup

< 0.2 2.31 < 10 126CMB19377 Orig < 0.5 < 2 1.57 < 0.5 24 43 26 5.22 < 10 < 1 0.35 20 0.78 207 < 1 0.406 39 0.141 < 2< 2

< 0.2 2.29 < 10 127CMB19377 Dup < 0.5 < 2 1.56 < 0.5 24 43 26 5.23 < 10 < 1 0.35 20 0.77 203 < 1 0.415 40 0.142 < 2< 2

< 0.2 1.06 < 10 22CMB19380 Orig 0.8 < 2 3.49 0.6 18 16 3 6.27 < 10 < 1 0.01 31 0.90 514 < 1 0.112 20 0.111 7514

< 0.2 1.02 < 10 21CMB19380 Split 0.8 < 2 3.36 0.6 18 16 3 6.10 < 10 < 1 0.01 28 0.87 493 < 1 0.107 18 0.109 7111

< 0.2 1.81 < 10 31CMB19390 Orig 1.2 < 2 2.98 < 0.5 19 175 33 4.87 < 10 < 1 0.09 24 2.02 686 < 1 0.117 81 0.119 34

< 0.2 1.87 < 10 30CMB19390 Split 1.3 < 2 3.01 < 0.5 19 175 32 4.89 < 10 < 1 0.09 24 2.02 682 < 1 0.123 79 0.118 34

< 0.2 1.78 < 10 30CMB19390 Orig 1.2 < 2 2.98 < 0.5 19 174 33 4.84 < 10 < 1 0.09 23 2.01 689 < 1 0.115 81 0.119 25

< 0.2 1.83 < 10 31CMB19390 Dup 1.2 < 2 2.98 < 0.5 19 175 33 4.89 < 10 < 1 0.09 24 2.02 683 < 1 0.118 81 0.120 44


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.009 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.008 < 1 < 0.001 < 2< 2



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Quality Control



0.22 82 187GXR-1 Meas < 10 30 77 139 6391

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2640 2640

DH-1a Cert 2630 2630

DH-1a Meas 2600

DH-1a Cert 2630

1.83 3 80GXR-4 Meas < 10 < 10 85 14 687

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 32 96GXR-2 Meas < 10 < 10 54 < 10 5955

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 2 37GXR-6 Meas < 10 < 10 179 < 10 12324

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 287

SY-2 Cert 284

SY-2 Meas 286

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10200

BL-3 Cert 10200

BL-4a Meas 1260

BL-4a Cert 1250

BL-4a Meas 1280

BL-4a Cert 1250

0.03 < 2 223 0.30CMB19363 Orig < 10 180 102 < 10 598

0.03 < 2 223 0.29CMB19363 Dup < 10 187 103 < 10 608

CMB19375 Orig 2.83

CMB19375 Dup 2.85

0.04 < 2 82 0.14CMB19377 Orig < 10 < 10 158 < 10 473

0.04 < 2 81 0.13CMB19377 Dup < 10 < 10 160 < 10 483

0.05 2 170 0.31CMB19380 Orig < 10 172 69 < 10 54 169 1.0366

0.05 2 159 0.30CMB19380 Split < 10 168 67 < 10 52 168 1.0525

0.03 < 2 233 0.28CMB19390 Orig < 10 < 10 62 < 10 85 4.3 1.032 2.946

0.03 < 2 235 0.31CMB19390 Split < 10 < 10 63 < 10 82 3.7 1.058 2.976

0.03 < 2 232 0.28CMB19390 Orig < 10 < 10 61 < 10 846

0.03 < 2 234 0.28CMB19390 Dup < 10 < 10 62 < 10 856


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

Page 5 of 5

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

07-Aug-08

10-Jul-08

A08-3946



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-3946

Notes:


Code Specific Gravity PulpCode 5D-U-Total DNCCode 1E3 - Aurora Pkg. Aqua Regia ICP(AQUAGEO)


Quality Control


Document Page 198




< 0.2 1.08 < 10 306CMB15922 < 0.5 < 2 2.83 0.6 21 14 57 7.25 < 10 < 1 0.62 50 1.12 817 5 0.200 17 0.122 79

< 0.2 0.80 < 10 293CMB15923 < 0.5 < 2 1.16 0.6 18 16 27 6.48 < 10 < 1 0.53 45 0.74 580 8 0.110 19 0.142 217

< 0.2 0.99 < 10 1650CMB15924 < 0.5 < 2 1.73 0.5 20 15 25 6.44 < 10 < 1 0.57 50 0.94 766 3 0.314 18 0.125 1410

< 0.2 0.63 < 10 1070CMB15925 < 0.5 < 2 1.93 0.6 19 12 3 6.57 < 10 < 1 0.28 46 0.69 702 < 1 0.284 15 0.112 68

< 0.2 0.71 < 10 440CMB15926 0.6 < 2 2.61 0.5 17 13 29 6.22 < 10 < 1 0.26 43 0.81 815 < 1 0.262 17 0.130 1110

< 0.2 0.60 < 10 869CMB15927 0.8 < 2 3.41 0.8 15 10 < 1 6.70 < 10 < 1 0.18 39 0.82 886 < 1 0.263 14 0.125 912

< 0.2 0.52 < 10 892CMB15928 1.1 < 2 2.71 0.7 14 9 < 1 5.94 < 10 < 1 0.06 49 0.67 662 < 1 0.351 13 0.133 3511

< 0.2 0.78 < 10 904CMB15929 1.4 < 2 4.19 0.8 16 9 < 1 6.55 < 10 < 1 0.06 46 1.00 1140 1 0.461 13 0.121 2413

< 0.2 0.78 < 10 924CMB15930 1.5 < 2 2.49 0.7 20 11 3 6.20 < 10 < 1 0.22 47 0.86 721 3 0.329 18 0.123 2712

1.7 0.51 < 10 439CMB15931 2.0 < 2 2.64 < 0.5 19 12 9 7.48 10 < 1 0.10 47 0.64 775 3 0.250 7 0.138 8836

3.9 0.85 < 10 148CMB15932 1.0 < 2 2.63 < 0.5 20 20 74 6.71 30 1 0.13 40 0.90 651 5 0.270 15 0.132 1610< 2

2.4 0.86 < 10 150CMB15933 1.7 < 2 2.78 0.7 19 16 25 7.45 20 < 1 0.11 39 0.91 726 2 0.301 15 0.109 8643

0.8 1.35 < 10 297CMB15934 1.7 < 2 3.10 1.6 23 23 78 6.26 < 10 < 1 0.11 31 1.22 734 5 0.479 26 0.107 4145

< 0.2 0.52 < 10 820CMB15935 1.1 < 2 2.68 3.2 12 7 81 5.81 < 10 < 1 0.06 57 0.57 518 < 1 0.219 8 0.099 3645

< 0.2 0.74 < 10 331CMB15936 1.1 < 2 2.29 0.6 14 42 16 5.91 < 10 < 1 0.14 58 0.85 543 < 1 0.328 12 0.113 898

< 0.2 0.98 < 10 830CMB15937 1.3 < 2 2.90 1.3 18 73 33 5.86 < 10 < 1 0.21 45 1.21 630 < 1 0.427 25 0.114 1437

0.3 0.43 < 10 1470CMB15938 1.9 < 2 2.05 0.6 15 13 2 6.93 < 10 < 1 0.05 51 0.47 479 < 1 0.312 12 0.103 2328

< 0.2 0.97 < 10 1230CMB15939 2.0 < 2 3.21 0.7 19 25 50 7.11 < 10 < 1 0.15 32 1.06 729 32 0.487 19 0.106 648

< 0.2 2.55 < 10 709CMB15940 1.2 < 2 4.21 0.6 35 71 60 7.88 10 < 1 0.60 12 2.55 909 4 0.708 43 0.091 4610

< 0.2 0.40 < 10 686CMB15941 2.1 < 2 2.69 0.7 14 8 29 5.59 < 10 < 1 0.04 40 0.52 709 < 1 0.303 11 0.104 489

0.2 0.34 < 10 598CMB15942 1.7 < 2 2.71 0.7 15 9 61 6.01 < 10 < 1 0.03 37 0.52 731 < 1 0.285 14 0.122 388

< 0.2 0.35 < 10 543CMB15943 1.7 < 2 2.73 0.8 16 9 60 6.27 < 10 < 1 0.03 38 0.53 751 1 0.289 14 0.119 367


0.6 < 2 1.11 < 0.5 7 39 5 2.60 10 < 1 0.01 115 0.02 294 2 0.157 6 0.009 9403

< 0.2 0.97 < 10 186CMB15945 0.9 < 2 1.28 0.6 14 25 98 3.14 < 10 < 1 0.52 46 0.78 277 4 0.164 15 0.082 166

0.8 0.64 < 10 743CMB15946 2.0 < 2 3.80 1.2 17 10 161 5.81 < 10 < 1 0.06 47 0.85 716 2 0.381 15 0.112 894

0.6 0.46 < 10 872CMB15947 1.9 < 2 3.14 1.8 17 11 126 6.54 < 10 < 1 0.04 41 0.60 666 2 0.336 15 0.117 815

0.6 0.58 < 10 840CMB15948 2.8 < 2 3.82 1.3 16 10 64 6.38 < 10 < 1 0.05 46 0.75 681 4 0.358 16 0.121 2754

2.2 0.79 < 10 933CMB15949 2.9 < 2 4.07 0.8 17 10 56 5.75 10 < 1 0.06 42 0.97 752 4 0.441 14 0.101 6392

1.4 0.65 < 10 1260CMB15950 2.6 < 2 3.89 1.3 17 14 136 5.63 < 10 < 1 0.07 42 0.84 731 11 0.388 17 0.093 4334

1.2 0.57 < 10 1600CMB19101 3.0 < 2 4.92 0.5 13 10 25 5.67 < 10 < 1 0.05 36 0.86 1180 4 0.325 9 0.108 5154

0.2 0.68 < 10 665CMB19102 1.6 < 2 3.18 0.9 18 15 45 5.76 < 10 < 1 0.12 36 0.83 769 6 0.352 19 0.103 784

< 0.2 0.83 < 10 976CMB19103 1.7 < 2 3.41 1.1 20 15 49 6.21 < 10 < 1 0.31 37 1.01 981 5 0.342 21 0.101 3410

< 0.2 0.82 < 10 363CMB19104 < 0.5 < 2 1.86 < 0.5 21 15 39 5.65 < 10 < 1 0.46 42 0.71 588 3 0.209 21 0.107 117

0.5 0.98 < 10 951CMB19105 1.5 < 2 4.23 0.6 18 13 60 5.04 < 10 < 1 0.25 41 1.07 830 17 0.400 17 0.103 889

< 0.2 0.91 < 10 756CMB19127 1.5 < 2 4.25 0.6 18 15 22 5.84 < 10 < 1 0.20 37 1.08 919 1 0.371 19 0.104 656

0.2 0.65 < 10 1440CMB19128 1.7 < 2 3.61 0.7 17 16 43 5.67 < 10 < 1 0.16 37 0.86 928 10 0.364 17 0.107 585

< 0.2 0.50 < 10 1130CMB19129 1.7 < 2 2.79 0.8 18 16 47 5.99 < 10 < 1 0.11 34 0.69 700 5 0.290 18 0.103 505

< 0.2 1.65 < 10 613CMB19130 0.9 < 2 2.99 0.7 25 45 56 5.77 < 10 < 1 0.23 26 1.61 721 4 0.458 44 0.099 239

< 0.2 0.58 < 10 378CMB19106 1.1 < 2 2.23 0.7 20 21 81 5.98 < 10 < 1 0.13 39 0.55 457 1 0.244 21 0.107 155

< 0.2 2.09 < 10 495CMB19107 0.7 < 2 3.17 0.6 28 54 54 6.04 < 10 < 1 0.37 22 1.92 698 < 1 0.577 44 0.095 94

0.2 0.69 < 10 739CMB19108 1.2 < 2 2.94 1.1 20 41 55 5.68 < 10 < 1 0.18 37 0.88 590 5 0.318 26 0.112 555

0.2 0.74 < 10 1120CMB19109 2.6 < 2 3.88 1.2 18 15 194 5.57 < 10 < 1 0.10 35 0.88 634 1 0.417 18 0.106 1617

0.4 0.65 < 10 908CMB19110 2.8 < 2 2.89 1.5 21 15 165 6.62 < 10 < 1 0.09 35 0.85 618 < 1 0.405 22 0.105 736

0.2 1.14 < 10 915CMB19111 2.1 < 2 5.25 1.1 16 12 67 4.68 < 10 < 1 0.04 33 1.25 730 1 0.570 13 0.105 6616

< 0.2 1.01 < 10 801CMB19112 2.0 < 2 6.05 1.0 14 10 17 4.78 < 10 < 1 0.03 25 1.20 692 1 0.542 12 0.106 7619

0.2 0.31 < 10 798CMB19113 1.4 < 2 3.82 0.6 12 13 31 4.93 < 10 < 1 0.02 26 0.42 599 < 1 0.216 11 0.107 876

< 0.2 0.46 < 10 1120CMB19114 2.2 < 2 3.49 1.0 16 14 17 5.67 < 10 < 1 0.03 33 0.66 665 < 1 0.368 16 0.111 717

1.0 0.69 < 10 1340CMB19115 3.1 < 2 5.61 0.9 15 12 135 5.23 < 10 < 1 0.07 33 0.94 874 < 1 0.457 15 0.097 3186

< 0.2 0.30 < 10 1090CMB19116 1.0 < 2 2.52 1.0 14 14 25 5.17 < 10 < 1 0.05 28 0.47 556 < 1 0.239 13 0.107 987

0.8 0.78 < 10 1010CMB19117 3.0 < 2 5.33 0.8 16 14 50 5.68 < 10 < 1 0.17 28 1.14 927 2 0.330 14 0.112 4307

0.8 0.78 < 10 1030CMB19118 3.1 < 2 4.55 0.9 17 13 36 5.49 < 10 < 1 0.14 34 1.03 826 1 0.413 16 0.097 3615

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0.7 < 2 1.69 < 0.5 6 45 7 2.57 < 10 < 1 0.01 140 0.04 420 1 0.163 7 0.003 510< 2

< 0.2 0.05 < 10 81CMB19120 < 0.5 < 2 0.77 < 0.5 7 52 < 1 1.70 < 10 < 1 < 0.01 25 0.02 41 2 0.058 10 0.026 3< 2

< 0.2 0.67 < 10 864CMB19121 2.3 < 2 2.99 1.0 19 16 20 6.14 < 10 < 1 0.23 32 0.91 719 < 1 0.320 20 0.107 737

0.2 0.99 < 10 846CMB19122 2.0 < 2 4.61 0.8 15 13 45 4.95 < 10 < 1 0.13 37 1.15 841 < 1 0.457 14 0.096 16010

0.2 0.79 < 10 618CMB19123 0.7 < 2 1.77 0.8 20 16 40 5.70 < 10 < 1 0.41 38 0.79 575 1 0.213 21 0.109 4910

< 0.2 0.89 < 10 277CMB19124 < 0.5 < 2 1.54 0.9 21 17 22 6.00 < 10 < 1 0.52 40 0.74 573 < 1 0.176 21 0.107 196

< 0.2 0.94 < 10 194CMB19125 < 0.5 < 2 1.48 0.5 20 16 21 5.74 < 10 < 1 0.56 43 0.75 590 1 0.177 20 0.108 214

< 0.2 1.10 < 10 248CMB19126 0.8 < 2 1.65 0.6 17 14 21 4.75 < 10 < 1 0.56 43 0.94 700 1 0.224 16 0.110 304

< 0.2 0.60 < 10 478CMB19131 1.1 < 2 2.35 0.8 16 9 19 5.94 < 10 < 1 0.24 58 0.67 912 < 1 0.166 12 0.118 347

< 0.2 0.50 < 10 621CMB19132 1.6 < 2 2.17 0.7 14 7 14 5.98 < 10 < 1 0.06 54 0.52 716 < 1 0.276 9 0.110 137

0.2 0.63 < 10 172CMB19133 2.0 < 2 2.48 0.6 17 8 1 5.75 < 10 < 1 0.08 56 0.67 736 < 1 0.279 10 0.105 409

< 0.2 0.86 < 10 413CMB19134 1.8 < 2 2.78 0.7 16 10 < 1 5.68 < 10 < 1 0.17 55 0.89 821 < 1 0.337 11 0.109 3210

< 0.2 0.79 < 10 323CMB19135 0.7 < 2 1.51 0.5 16 11 18 5.28 < 10 < 1 0.46 56 0.79 637 1 0.134 10 0.103 2910

0.9 0.96 < 10 590CMB19136 0.8 < 2 1.70 1.6 22 17 61 6.19 < 10 < 1 0.35 34 0.92 610 2 0.286 23 0.121 5159

0.2 0.90 < 10 509CMB19137 0.5 < 2 1.84 1.1 20 14 38 5.68 < 10 < 1 0.45 29 0.94 572 < 1 0.157 22 0.118 1284

0.4 0.77 < 10 511CMB19138 1.1 < 2 3.34 0.6 15 14 20 5.16 < 10 < 1 0.10 28 0.75 644 3 0.298 15 0.113 1207

0.3 0.57 < 10 1350CMB19139 1.1 < 2 2.47 0.6 14 16 52 5.18 < 10 < 1 0.04 28 0.52 475 < 1 0.320 15 0.116 1039

0.2 0.66 < 10 746CMB19140 0.8 < 2 3.09 0.5 13 14 58 4.46 < 10 < 1 0.05 30 0.63 509 < 1 0.322 11 0.124 759

0.3 0.86 < 10 86CMB19141 0.9 < 2 4.01 0.6 15 12 94 4.79 < 10 < 1 0.07 29 0.94 634 2 0.305 17 0.103 1757

0.4 0.74 < 10 115CMB19142 0.7 < 2 4.15 0.6 16 13 81 4.95 < 10 < 1 0.07 26 0.76 586 2 0.215 17 0.106 2086


< 0.5 < 2 1.08 < 0.5 8 27 28 2.25 < 10 < 1 0.10 86 0.27 288 7 0.120 38 0.039 262< 2

< 0.2 0.08 < 10 47CMB19144 < 0.5 < 2 0.67 < 0.5 7 55 < 1 2.06 < 10 < 1 < 0.01 22 0.03 40 1 0.095 14 0.026 2< 2

< 0.2 0.69 < 10 222CMB19145 < 0.5 < 2 1.26 1.0 20 11 43 6.77 < 10 < 1 0.23 22 0.60 407 2 0.118 14 0.147 436

< 0.2 1.58 < 10 262CMB19146 1.0 < 2 2.43 < 0.5 25 16 54 4.33 < 10 < 1 0.47 46 1.62 550 22 0.230 30 0.075 273


0.9 < 2 3.53 0.5 9 12 27 4.69 < 10 < 1 0.02 20 0.29 536 < 1 0.144 11 0.106 855


2.3 < 2 5.47 0.8 13 12 142 4.98 < 10 < 1 0.06 27 0.73 822 < 1 0.394 13 0.105 3295

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0.04 3 46 0.41CMB15922 < 10 < 10 57 < 10 115 6.5 1.0376

0.02 < 2 26 0.33CMB15923 < 10 < 10 63 < 10 85 3.8 1.020 2.858

0.05 < 2 51 0.43CMB15924 < 10 < 10 67 < 10 85 6.0 1.0497

0.04 3 40 0.41CMB15925 < 10 < 10 55 < 10 66 6.7 1.0106

0.03 < 2 47 0.32CMB15926 < 10 < 10 61 < 10 69 7.5 1.0779

0.05 < 2 96 0.25CMB15927 < 10 13 51 < 10 56 12.4 1.080 2.877

0.04 3 109 0.21CMB15928 < 10 77 49 < 10 49 74.3 1.0799

0.05 3 177 0.24CMB15929 < 10 34 54 < 10 90 33.0 1.0838

0.04 3 89 0.30CMB15930 < 10 46 90 < 10 101 44.6 1.0739

0.03 2 106 0.37CMB15931 < 10 2870 94 < 10 71 2960 1.0458

0.04 3 66 0.27CMB15932 < 10 5400 127 < 10 88 5260 1.083 2.929

0.03 3 77 0.27CMB15933 < 10 2980 137 < 10 155 3020 1.0269

0.11 < 2 76 0.30CMB15934 < 10 1140 146 < 10 181 1150 1.07811

0.07 < 2 111 0.24CMB15935 < 10 272 84 < 10 285 273 1.0519

0.05 < 2 77 0.25CMB15936 < 10 231 78 < 10 59 238 1.0019

0.07 < 2 106 0.26CMB15937 < 10 243 100 < 10 89 246 1.0149

0.06 3 110 0.30CMB15938 < 10 820 108 < 10 70 795 1.0328

0.08 3 138 0.28CMB15939 < 10 147 134 < 10 82 147 1.06110

0.13 < 2 160 0.30CMB15940 < 10 82 170 < 10 123 79.0 1.08016

0.05 < 2 188 0.26CMB15941 < 10 21 79 < 10 166 22.1 1.0736

0.05 < 2 173 0.23CMB15942 < 10 18 89 < 10 203 17.8 1.0405

0.05 < 2 173 0.24CMB15943 < 10 20 90 < 10 199 18.1 1.0745


< 10 3460 70 < 10 90 3410 1.036< 1

0.02 < 2 75 0.38CMB15945 < 10 < 10 69 < 10 108 6.8 1.0526

0.10 < 2 197 0.21CMB15946 < 10 125 128 < 10 255 130 1.0609

0.12 < 2 207 0.24CMB15947 < 10 85 102 < 10 380 86.0 1.0417

0.07 < 2 200 0.23CMB15948 < 10 751 209 < 10 258 744 1.0089

0.07 < 2 256 0.29CMB15949 < 10 2410 348 < 10 187 2380 1.097 2.9310

0.09 3 244 0.31CMB15950 < 10 1330 186 < 10 307 1290 1.0488

0.08 < 2 414 0.25CMB19101 < 10 1730 224 < 10 118 1720 1.0026

0.05 < 2 146 0.29CMB19102 < 10 202 130 < 10 180 198 1.0859

0.12 2 171 0.34CMB19103 < 10 17 80 < 10 194 15.4 1.0709

0.14 < 2 72 0.38CMB19104 < 10 < 10 71 < 10 124 5.6 1.0393

0.12 4 163 0.38CMB19105 < 10 38 64 < 10 125 37.0 1.0248

0.07 < 2 163 0.32CMB19127 < 10 175 109 < 10 104 166 1.0279

0.08 < 2 161 0.34CMB19128 < 10 88 83 < 10 100 79.2 1.0548

0.06 < 2 120 0.32CMB19129 < 10 11 73 < 10 130 8.0 1.0187

0.12 < 2 82 0.32CMB19130 < 10 38 126 < 10 137 34.7 1.07310

0.11 < 2 58 0.35CMB19106 < 10 < 10 80 < 10 170 7.9 1.0006

0.13 < 2 50 0.31CMB19107 < 10 < 10 100 < 10 135 2.3 1.06711

0.14 < 2 121 0.33CMB19108 < 10 < 10 73 < 10 186 6.2 1.0336

0.09 < 2 185 0.33CMB19109 < 10 336 94 < 10 159 318 1.0519

0.06 2 141 0.32CMB19110 < 10 40 81 < 10 211 36.5 1.0698

0.07 < 2 207 0.33CMB19111 < 10 205 56 < 10 90 203 1.0328

0.07 < 2 288 0.24CMB19112 < 10 229 73 < 10 69 225 1.0767

0.05 < 2 237 0.21CMB19113 < 10 191 75 < 10 67 202 1.0444

0.06 < 2 234 0.28CMB19114 < 10 50 72 < 10 105 50.7 1.0157

0.09 < 2 408 0.26CMB19115 < 10 1080 86 < 10 101 1070 1.0947

0.05 < 2 194 0.25CMB19116 < 10 23 60 < 10 160 21.7 1.0704

0.07 < 2 354 0.26CMB19117 < 10 1110 77 < 10 127 1080 1.0367

0.07 < 2 315 0.30CMB19118 < 10 1060 82 < 10 128 1050 1.0528

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< 10 2020 114 < 10 56 2060 1.068< 1

0.04 < 2 46 0.26CMB19120 < 10 15 51 < 10 9 10.5 1.047< 1

0.05 < 2 156 0.32CMB19121 < 10 64 87 < 10 134 61.4 1.0578

0.06 < 2 202 0.34CMB19122 < 10 435 63 < 10 135 422 1.0578

0.06 < 2 79 0.38CMB19123 < 10 56 69 < 10 165 53.7 1.0933

0.03 3 55 0.40CMB19124 < 10 < 10 73 < 10 245 5.6 1.0412

0.04 < 2 60 0.37CMB19125 < 10 < 10 71 < 10 155 4.0 1.0314

0.03 < 2 41 0.34CMB19126 < 10 < 10 60 < 10 136 3.4 1.0858

0.03 < 2 74 0.31CMB19131 < 10 45 60 < 10 129 48.8 1.0728

0.03 2 68 0.35CMB19132 < 10 39 60 < 10 123 39.6 1.0937

0.03 2 70 0.37CMB19133 < 10 165 60 < 10 119 161 1.0749

0.03 3 68 0.35CMB19134 < 10 113 57 < 10 143 110 1.01010

0.02 < 2 36 0.34CMB19135 < 10 11 54 < 10 125 13.0 1.0869

0.11 < 2 29 0.33CMB19136 < 10 15 80 < 10 332 16.1 1.0618

0.17 < 2 39 0.25CMB19137 < 10 12 66 < 10 255 12.8 1.0874

0.17 < 2 88 0.26CMB19138 < 10 331 79 < 10 119 319 1.0608

0.05 < 2 98 0.27CMB19139 < 10 299 82 < 10 102 294 1.0566

0.04 < 2 88 0.27CMB19140 < 10 275 64 < 10 76 259 1.0306

0.05 < 2 99 0.24CMB19141 < 10 481 58 < 10 86 467 1.0787

0.07 < 2 120 0.21CMB19142 < 10 415 58 < 10 78 401 1.0486


< 10 811 55 < 10 107 848 1.0662

0.05 < 2 25 0.22CMB19144 < 10 < 10 52 < 10 7 11.4 1.058< 1

0.09 < 2 25 0.23CMB19145 < 10 22 76 < 10 120 21.3 1.088 2.874

0.12 < 2 38 0.29CMB19146 < 10 23 70 < 10 70 22.6 1.050 3.058


< 10 184 67 < 10 57 199 1.0692


< 10 1120 79 < 10 86 1080 1.0966

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Quality Control



28.5 0.36 15 176GXR-1 Meas 1.0 1540 0.90 3.3 8 6 1190 27.0 < 10 4 0.03 < 10 0.15 895 16 0.040 26 0.042 662404

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

30.9 0.35 15 219GXR-1 Meas 0.9 1580 0.86 3.4 9 6 1170 26.1 < 10 4 0.03 < 10 0.14 803 16 0.057 38 0.035 636375

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.4 2.65 < 10 38GXR-4 Meas 1.0 21 0.95 0.5 15 57 6560 4.00 10 1 1.48 47 1.73 140 337 0.110 40 0.127 44105

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

3.5 2.85 < 10 29GXR-4 Meas 1.4 24 0.93 < 0.5 15 52 6060 3.48 < 10 < 1 1.39 46 1.64 137 325 0.124 39 0.111 4198

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

21.0 3.44 21 1320GXR-2 Meas 1.1 < 2 0.85 4.6 10 25 81 2.23 < 10 4 0.54 23 0.54 1030 < 1 0.251 17 0.056 76314

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.3 7.00 < 10 1030GXR-6 Meas 1.0 < 2 0.19 0.6 15 93 74 6.67 20 1 0.97 12 0.43 1050 2 0.070 24 0.035 97244

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

0.3 6.78 < 10 874GXR-6 Meas 0.9 < 2 0.16 0.7 15 80 65 6.26 20 < 1 0.85 11 0.40 973 1 0.121 25 0.030 93238

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2670 6.13 2260

OREAS 13P Cert 2500 7.58 2260

OREAS 13P Meas 2590 5.57 2160

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

1.7 0.51 < 10 439CMB15931 Orig 2.0 < 2 2.64 < 0.5 19 12 9 7.48 10 < 1 0.10 47 0.64 775 3 0.250 7 0.138 8836

1.6 0.48 < 10 420CMB15931 Split 1.0 < 2 2.53 < 0.5 18 12 9 7.20 10 < 1 0.09 46 0.60 741 3 0.240 8 0.131 8386

3.9 0.85 < 10 148CMB15932 Orig 1.0 < 2 2.63 < 0.5 20 20 74 6.71 30 1 0.13 40 0.90 651 5 0.270 15 0.132 1610< 2

3.7 0.83 < 10 139CMB15932 Split 1.0 < 2 2.59 < 0.5 20 19 70 6.54 20 1 0.13 41 0.89 635 6 0.270 16 0.129 15505

CMB15932 Split

0.7 1.35 < 10 295CMB15934 Orig 1.7 < 2 3.09 1.6 23 23 78 6.29 < 10 < 1 0.11 31 1.22 730 8 0.475 26 0.105 4125

0.8 1.36 < 10 300CMB15934 Dup 1.7 < 2 3.11 1.7 23 23 77 6.23 < 10 < 1 0.11 32 1.23 737 3 0.483 25 0.108 4165

0.6 0.58 < 10 850CMB15948 Orig 2.8 < 2 3.86 1.3 16 10 64 6.40 < 10 < 1 0.05 47 0.76 688 4 0.362 17 0.123 2753

0.6 0.58 < 10 830CMB15948 Dup 2.7 < 2 3.78 1.3 16 10 64 6.37 < 10 < 1 0.05 45 0.75 674 4 0.355 16 0.118 2744

1.2 0.57 < 10 1600CMB19101 Orig 3.0 < 2 4.92 0.5 13 10 25 5.67 < 10 < 1 0.05 36 0.86 1180 4 0.325 9 0.108 5154

1.2 0.57 < 10 1530CMB19101 Split 3.0 < 2 4.87 0.5 13 10 30 5.64 < 10 < 1 0.05 35 0.86 1170 3 0.320 8 0.108 5123

1.1 0.57 < 10 1600CMB19101 Orig 3.0 < 2 4.89 0.5 13 10 23 5.60 < 10 < 1 0.05 36 0.85 1170 4 0.320 8 0.107 5154

1.2 0.58 < 10 1600CMB19101 Dup 3.0 < 2 4.95 0.5 13 10 26 5.74 < 10 < 1 0.05 36 0.87 1180 4 0.330 9 0.108 5154

< 0.2 2.08 < 10 493CMB19107 Orig 0.7 < 2 3.16 0.6 28 54 54 6.04 < 10 < 1 0.36 22 1.92 697 < 1 0.577 42 0.095 94

< 0.2 2.09 < 10 496CMB19107 Dup 0.7 < 2 3.19 0.6 29 54 54 6.04 < 10 < 1 0.37 22 1.93 700 < 1 0.577 45 0.095 95

0.8 0.78 < 10 1010CMB19117 Orig 3.0 < 2 5.33 0.8 16 14 50 5.68 < 10 < 1 0.17 28 1.14 927 2 0.330 14 0.112 4307

0.8 0.78 < 10 1000CMB19117 Split 3.0 < 2 5.29 0.7 16 13 50 5.73 < 10 < 1 0.17 29 1.13 928 1 0.330 13 0.113 4387

< 0.2 0.66 < 10 854CMB19121 Orig 2.3 < 2 2.96 1.0 19 15 20 6.00 < 10 < 1 0.22 31 0.90 709 < 1 0.311 20 0.106 727

< 0.2 0.68 < 10 873CMB19121 Dup 2.4 < 2 3.03 1.1 19 16 21 6.28 < 10 < 1 0.23 33 0.93 729 < 1 0.329 20 0.108 738

< 0.2 0.60 < 10 478CMB19131 Orig 1.1 < 2 2.35 0.8 16 9 19 5.94 < 10 < 1 0.24 58 0.67 912 < 1 0.166 12 0.118 347

< 0.2 0.53 < 10 477CMB19131 Split 0.9 < 2 2.19 0.8 14 9 22 5.79 < 10 < 1 0.24 49 0.58 847 < 1 0.136 12 0.124 339

< 0.2 1.58 < 10 262CMB19146 Orig 1.0 < 2 2.43 < 0.5 25 16 54 4.33 < 10 < 1 0.47 46 1.62 550 22 0.230 30 0.075 273

0.2 1.64 < 10 271CMB19146 Split 1.0 < 2 2.48 < 0.5 26 16 56 4.42 < 10 < 1 0.49 29 1.68 564 19 0.240 32 0.078 274

1.1 0.53 < 10 1540CMB19148 PULP DUP FROM CMB19115 Orig

2.3 < 2 5.44 0.9 13 11 149 4.92 < 10 < 1 0.06 27 0.72 818 < 1 0.398 13 0.105 3275

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Quality Control



1.0 0.53 < 10 1580CMB19148 PULP DUP FROM CMB19115 Dup

2.4 < 2 5.49 0.8 13 12 135 5.03 < 10 < 1 0.07 27 0.73 826 < 1 0.390 13 0.105 3316


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.011 < 1 < 0.001 < 2< 2

< 0.2 < 0.01 < 10 20Method Blank Method Blank

< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 0.02 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.009 < 1 < 0.001 < 2< 2




< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 < 0.001 < 1 < 0.001 < 2< 2

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Quality Control



0.24 84 172GXR-1 Meas < 10 34 79 147 6421

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

0.22 81 162GXR-1 Meas < 10 32 80 158 6491

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2550 2640

DH-1a Cert 2630 2630

DH-1a Meas 2600

DH-1a Cert 2630

1.95 5 72GXR-4 Meas < 10 < 10 81 14 686

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

1.82 4 78GXR-4 Meas < 10 < 10 84 19 666

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 30 95GXR-2 Meas < 10 < 10 51 < 10 5825

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 3 34GXR-6 Meas < 10 < 10 182 < 10 12123

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

0.02 4 30GXR-6 Meas < 10 < 10 172 < 10 12022

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 287

SY-2 Cert 284

SY-2 Meas 286

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10100

BL-3 Cert 10200

BL-4a Meas 1260

BL-4a Cert 1250

BL-4a Meas 1280

BL-4a Cert 1250

0.03 2 106 0.37CMB15931 Orig < 10 2870 94 < 10 71 2960 1.0458

0.03 2 102 0.36CMB15931 Split < 10 2750 91 < 10 67 2920 1.0558

0.04 3 66 0.27CMB15932 Orig < 10 5400 127 < 10 88 5260 1.083 2.929

0.04 2 65 0.30CMB15932 Split < 10 5280 125 < 10 86 5230 1.090 2.949

CMB15932 Split 2.94

0.11 < 2 75 0.30CMB15934 Orig < 10 1130 145 < 10 18211

0.11 < 2 76 0.30CMB15934 Dup < 10 1150 146 < 10 18110

0.07 2 203 0.23CMB15948 Orig < 10 755 212 < 10 2599

0.07 < 2 198 0.22CMB15948 Dup < 10 746 206 < 10 2589

0.08 < 2 414 0.25CMB19101 Orig < 10 1730 224 < 10 118 1720 1.0026

0.08 2 405 0.24CMB19101 Split < 10 1710 222 < 10 118 1710 1.0706

0.08 < 2 411 0.25CMB19101 Orig < 10 1720 221 < 10 1166

0.08 < 2 416 0.24CMB19101 Dup < 10 1740 227 < 10 1196

0.13 < 2 51 0.30CMB19107 Orig < 10 < 10 101 < 10 13512

0.14 < 2 49 0.32CMB19107 Dup < 10 < 10 100 < 10 13611

0.07 < 2 354 0.26CMB19117 Orig < 10 1110 77 < 10 127 1080 1.0367

0.07 < 2 350 0.26CMB19117 Split < 10 1120 77 < 10 121 1090 1.0807

0.05 < 2 154 0.31CMB19121 Orig < 10 64 85 < 10 1338

0.05 < 2 157 0.34CMB19121 Dup < 10 65 89 < 10 1368

0.03 < 2 74 0.31CMB19131 Orig < 10 45 60 < 10 129 48.8 1.0728

0.03 < 2 72 0.22CMB19131 Split < 10 48 56 < 10 120 47.4 1.0797

0.12 < 2 38 0.29CMB19146 Orig < 10 23 70 < 10 70 22.6 1.050 3.058

0.13 < 2 38 0.29CMB19146 Split < 10 22 72 < 10 72 22.6 1.039 3.028

0.10 < 2 414 0.20CMB19148 PULP DUP FROM CMB19115 Orig

< 10 1110 77 < 10 856

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Quality Control



0.10 < 2 417 0.21CMB19148 PULP DUP FROM CMB19115 Dup

< 10 1120 80 < 10 876


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000


< 10 < 10 < 1 < 10 < 2< 1

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

13-Aug-08

15-Jul-08

A08-4085



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-4085

Notes:




Quality Control


Document Page 207




< 0.2 2.21 < 10 241CMB19179 0.6 < 2 2.26 0.5 28 195 110 5.14 < 10 < 1 1.11 13 2.58 614 < 1 0.208 52 0.094 1511

< 0.2 1.82 < 10 289CMB19180 0.5 < 2 2.14 < 0.5 25 197 61 5.12 < 10 < 1 1.01 12 2.09 563 < 1 0.114 52 0.095 177

1.2 2.27 < 10 361CMB19181 0.7 < 2 4.66 0.8 32 201 1060 6.51 < 10 < 1 1.57 13 2.84 900 1 0.091 59 0.092 4417

0.5 2.61 < 10 372CMB19182 1.0 < 2 5.45 0.7 30 212 180 6.69 10 < 1 1.45 15 2.53 973 < 1 0.083 60 0.095 17810

0.4 1.27 < 10 305CMB19183 0.5 < 2 5.35 < 0.5 18 170 21 4.29 < 10 < 1 0.65 17 1.29 736 < 1 0.087 34 0.097 6716

0.5 1.02 < 10 165CMB19184 < 0.5 < 2 4.66 < 0.5 16 153 25 3.64 < 10 < 1 0.47 17 0.98 618 < 1 0.065 26 0.096 9415

< 0.2 2.61 < 10 371CMB19185 < 0.5 < 2 1.99 0.5 31 54 85 5.06 < 10 < 1 0.56 22 1.35 388 < 1 0.372 46 0.142 2< 2


< 0.5 < 2 1.17 < 0.5 10 30 34 2.57 < 10 < 1 0.13 87 0.35 319 4 0.140 53 0.054 1663

< 0.2 1.13 < 10 190CMB19187 < 0.5 < 2 3.76 < 0.5 20 148 3 4.14 < 10 < 1 0.77 19 1.37 662 < 1 0.063 35 0.085 1215


< 0.5 < 2 3.88 < 0.5 21 153 3 4.33 < 10 < 1 0.80 20 1.43 692 < 1 0.069 37 0.090 1317

< 0.2 0.10 < 10 78CMB19189 < 0.5 < 2 1.95 < 0.5 7 15 14 3.32 < 10 < 1 0.01 29 0.02 389 < 1 0.065 2 0.048 421


< 0.5 < 2 1.97 < 0.5 7 14 14 3.28 < 10 < 1 0.01 28 0.02 395 < 1 0.061 3 0.047 520

< 0.2 0.07 < 10 169CMB19191 < 0.5 < 2 1.41 < 0.5 6 13 2 2.79 < 10 < 1 < 0.01 30 0.01 212 < 1 0.072 2 0.064 315

< 0.2 0.13 < 10 309CMB19192 < 0.5 < 2 0.83 < 0.5 4 20 20 2.09 < 10 < 1 0.06 38 0.04 159 < 1 0.106 < 1 0.033 215

< 0.2 0.16 < 10 10CMB19193 < 0.5 < 2 1.38 < 0.5 1 27 < 1 0.84 < 10 < 1 0.01 87 < 0.01 151 < 1 0.050 2 0.006 < 23

0.2 0.52 < 10 18CMB19194 < 0.5 < 2 1.22 < 0.5 5 38 1 1.78 < 10 < 1 0.11 75 0.32 192 < 1 0.055 9 0.022 10< 2

< 0.2 0.30 < 10 15CMB19195 < 0.5 < 2 0.89 < 0.5 2 27 26 1.18 < 10 < 1 0.04 89 0.06 85 < 1 0.036 3 0.005 7< 2

< 0.2 0.98 < 10 52CMB19196 < 0.5 < 2 1.02 < 0.5 12 56 579 3.10 < 10 < 1 0.26 52 0.75 243 < 1 0.056 19 0.038 21< 2

< 0.2 0.98 < 10 48CMB19197 0.5 < 2 1.32 < 0.5 11 57 484 2.89 < 10 < 1 0.23 59 0.63 240 1 0.072 16 0.037 303

< 0.2 1.88 < 10 113CMB19198 < 0.5 < 2 1.26 0.5 26 49 35 5.18 < 10 < 1 0.33 21 0.73 198 < 1 0.351 47 0.154 < 2< 2


< 0.5 < 2 1.20 < 0.5 11 31 36 2.64 < 10 < 1 0.13 90 0.36 329 4 0.159 53 0.055 170< 2

< 0.2 0.87 < 10 79CMB19200 0.6 < 2 0.98 < 0.5 8 47 3 1.79 < 10 < 1 0.29 56 0.65 201 < 1 0.049 16 0.029 < 2< 2

< 0.2 0.31 < 10 22CMB19451 < 0.5 < 2 0.48 < 0.5 2 24 7 0.95 < 10 < 1 0.07 65 0.09 68 < 1 0.030 3 0.007 < 2< 2


< 0.5 < 2 0.49 < 0.5 2 26 8 0.97 < 10 < 1 0.07 67 0.09 67 < 1 0.032 4 0.006 < 2< 2

< 0.2 1.64 < 10 165CMB19453 0.6 < 2 1.17 < 0.5 14 65 32 2.89 < 10 < 1 0.72 39 1.35 366 < 1 0.047 32 0.030 93


0.6 < 2 1.21 < 0.5 14 64 35 2.97 < 10 < 1 0.73 40 1.36 370 < 1 0.048 32 0.031 113

< 0.2 1.19 < 10 54CMB19455 0.6 < 2 1.74 < 0.5 16 57 36 2.67 < 10 < 1 0.23 31 0.82 260 2 0.053 21 0.068 3< 2

< 0.2 2.72 < 10 201CMB19456 0.5 < 2 2.05 < 0.5 33 88 34 4.46 < 10 < 1 0.44 18 2.91 595 2 0.052 107 0.052 47

< 0.2 0.69 < 10 514CMB19401 1.2 < 2 1.61 1.3 11 13 23 6.03 < 10 < 1 0.08 43 0.56 646 < 1 0.255 11 0.165 535

< 0.2 0.88 < 10 728CMB19402 2.0 < 2 2.31 1.1 11 14 10 4.99 < 10 < 1 0.06 42 0.58 837 < 1 0.285 12 0.137 625

0.3 1.90 < 10 202CMB19403 1.5 < 2 2.90 1.3 27 67 47 5.66 < 10 < 1 0.35 < 10 1.67 617 < 1 0.487 36 0.142 556

0.4 1.75 < 10 155CMB19404 1.3 < 2 2.71 1.2 25 63 47 5.16 < 10 < 1 0.31 < 10 1.51 560 < 1 0.440 34 0.144 807

< 0.2 1.52 < 10 257CMB19405 < 0.5 < 2 1.32 0.6 16 8 13 5.86 < 10 < 1 0.78 31 1.15 777 < 1 0.213 2 0.196 < 2< 2


0.5 < 2 1.19 < 0.5 10 32 31 2.56 < 10 < 1 0.11 97 0.30 325 5 0.157 49 0.048 2942

< 0.2 2.11 < 10 139CMB19407 0.9 < 2 3.32 0.8 27 64 49 5.19 < 10 < 1 0.37 < 10 1.68 647 < 1 0.513 37 0.093 136

0.3 2.12 < 10 178CMB19408 1.1 < 2 4.29 0.8 24 55 92 4.61 < 10 < 1 0.37 < 10 1.56 720 < 1 0.435 34 0.128 256

0.5 1.59 < 10 79CMB19409 1.2 < 2 4.17 1.2 19 53 153 3.88 < 10 < 1 0.25 < 10 1.10 741 < 1 0.308 28 0.168 636

< 0.2 1.92 < 10 110CMB19410 1.2 < 2 3.48 1.0 25 55 34 4.40 < 10 < 1 0.36 < 10 1.44 656 < 1 0.398 37 0.075 223

< 0.2 2.42 < 10 238CMB19411 1.6 < 2 3.49 1.0 33 71 38 6.12 < 10 < 1 0.60 < 10 1.89 809 < 1 0.424 44 0.096 264


1.6 < 2 3.49 1.0 34 71 38 6.11 < 10 < 1 0.60 < 10 1.89 815 < 1 0.427 43 0.096 273

< 0.2 1.34 < 10 213CMB19413 0.8 < 2 3.13 0.7 39 97 26 6.97 < 10 < 1 0.54 < 10 1.18 662 < 1 0.188 60 0.109 285

< 0.2 2.39 < 10 304CMB19414 1.4 < 2 4.49 0.8 40 90 41 7.31 < 10 < 1 1.05 < 10 2.16 907 < 1 0.327 58 0.104 318

< 0.2 2.06 < 10 415CMB19415 0.9 < 2 3.37 0.7 30 66 47 6.63 < 10 < 1 0.90 14 1.99 725 < 1 0.328 41 0.091 143

< 0.2 0.76 < 10 655CMB19416 1.1 < 2 1.58 0.5 13 15 58 5.40 < 10 < 1 0.32 36 0.74 411 < 1 0.192 16 0.143 286

< 0.2 0.64 < 10 174CMB19417 1.1 < 2 1.56 < 0.5 12 16 18 4.02 < 10 < 1 0.08 43 0.51 400 < 1 0.190 13 0.098 544

< 0.2 0.70 < 10 44CMB19418 0.9 < 2 1.74 0.6 17 40 28 4.81 < 10 < 1 0.10 23 0.61 448 < 1 0.199 23 0.130 373

< 0.2 1.23 < 10 127CMB19419 1.0 < 2 2.59 < 0.5 20 67 18 5.11 < 10 < 1 0.15 < 10 0.79 427 < 1 0.251 31 0.179 337

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< 0.2 0.80 < 10 243CMB19420 0.9 < 2 1.60 < 0.5 14 41 5 4.68 < 10 < 1 0.18 20 0.66 402 < 1 0.200 13 0.085 126

< 0.2 0.86 < 10 269CMB19421 0.8 < 2 1.17 0.5 15 40 14 4.91 < 10 < 1 0.43 21 0.95 547 < 1 0.174 12 0.077 55

< 0.2 1.45 < 10 127CMB19422 < 0.5 < 2 2.27 < 0.5 21 53 6 4.65 < 10 < 1 0.34 < 10 1.49 494 2 0.359 25 0.079 < 26

< 0.2 0.58 < 10 147CMB19423 0.5 < 2 1.94 0.7 14 14 5 4.43 < 10 < 1 0.17 46 0.61 509 < 1 0.156 12 0.141 1314

< 0.2 0.78 < 10 743CMB19424 0.6 < 2 1.65 1.1 17 13 3 5.72 < 10 < 1 0.36 41 0.87 815 < 1 0.207 17 0.147 1913

< 0.2 0.47 < 10 315CMB19425 < 0.5 < 2 1.07 0.8 15 13 22 4.85 < 10 < 1 0.29 42 0.50 487 < 1 0.099 16 0.118 2510

0.8 0.69 < 10 398CMB19426 0.9 < 2 1.70 < 0.5 16 11 53 4.60 < 10 < 1 0.29 44 0.63 542 3 0.194 13 0.110 2967

0.4 0.54 < 10 376CMB19427 0.6 < 2 1.53 < 0.5 16 11 28 4.77 < 10 < 1 0.28 40 0.57 520 2 0.110 15 0.093 2059

< 0.2 1.59 < 10 118CMB19428 < 0.5 < 2 1.13 < 0.5 24 43 29 4.98 < 10 < 1 0.36 19 0.74 185 < 1 0.274 40 0.165 < 2< 2


0.5 < 2 1.16 < 0.5 10 31 29 2.46 < 10 < 1 0.11 94 0.29 315 4 0.145 48 0.047 306< 2

< 0.2 0.66 < 10 549CMB19430 0.7 < 2 1.16 0.6 19 15 56 5.88 < 10 < 1 0.41 35 0.98 760 < 1 0.171 20 0.134 57

< 0.2 0.45 < 10 665CMB19431 < 0.5 < 2 1.54 0.8 14 12 15 4.68 < 10 < 1 0.22 39 0.62 635 1 0.190 13 0.106 58

< 0.2 0.52 < 10 276CMB19432 1.0 < 2 2.17 0.6 14 12 < 1 5.15 < 10 < 1 0.16 35 0.60 624 2 0.188 13 0.133 2412


1.0 < 2 2.18 0.6 13 13 < 1 5.22 < 10 < 1 0.16 35 0.62 636 2 0.186 13 0.135 2614

< 0.2 0.50 < 10 775CMB19434 1.5 < 2 2.19 < 0.5 16 15 1 4.66 < 10 < 1 0.15 30 0.57 548 1 0.232 16 0.118 1812

< 0.2 0.58 < 10 936CMB19435 1.0 < 2 1.88 0.6 19 16 < 1 5.58 < 10 < 1 0.33 32 0.72 593 < 1 0.167 21 0.181 1618

< 0.2 0.71 < 10 1550CMB19436 0.9 < 2 2.53 0.5 18 16 1 4.56 < 10 < 1 0.29 36 0.82 626 2 0.293 17 0.115 1723

0.5 0.52 < 10 362CMB19437 < 0.5 < 2 1.55 < 0.5 13 12 17 3.01 < 10 < 1 0.28 32 0.52 389 < 1 0.114 11 0.070 6322


< 0.5 < 2 1.54 < 0.5 13 12 16 2.94 < 10 < 1 0.28 32 0.52 383 < 1 0.111 13 0.070 6015

0.3 0.68 < 10 201CMB19439 0.9 < 2 1.97 < 0.5 14 15 57 3.56 < 10 < 1 0.24 34 0.69 479 1 0.171 10 0.095 4311

< 0.2 1.07 < 10 184CMB19440 0.8 < 2 1.24 0.7 22 36 3 7.44 < 10 < 1 0.72 14 1.24 958 < 1 0.120 11 0.093 512

< 0.2 1.10 < 10 144CMB19441 < 0.5 < 2 1.11 0.6 19 35 25 7.12 < 10 < 1 0.81 17 1.18 865 < 1 0.089 10 0.079 68

< 0.2 2.05 < 10 289CMB19442 < 0.5 < 2 2.04 0.6 30 50 71 5.48 < 10 < 1 0.58 < 10 1.91 586 < 1 0.359 49 0.087 154

< 0.2 0.58 < 10 121CMB19443 < 0.5 < 2 0.90 0.6 11 37 48 2.96 < 10 < 1 0.20 48 0.56 210 < 1 0.140 14 0.045 63

< 0.2 0.54 < 10 47CMB19444 0.6 < 2 0.99 < 0.5 11 19 36 1.65 < 10 < 1 0.08 51 0.46 173 14 0.114 13 0.031 823

< 0.2 1.97 19 139CMB19445 < 0.5 < 2 1.82 0.7 31 38 44 4.05 < 10 < 1 0.26 < 10 1.78 425 < 1 0.269 50 0.092 507

0.6 0.49 < 10 52CMB19446 < 0.5 < 2 0.85 < 0.5 9 16 20 1.25 < 10 < 1 0.07 52 0.46 146 1 0.102 12 0.033 193

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0.02 < 2 142 0.28CMB19179 < 10 < 10 116 < 10 99 3.0 1.051 2.9410

0.02 < 2 169 0.24CMB19180 < 10 < 10 113 < 10 119 2.6 1.076 2.956

0.08 < 2 199 0.30CMB19181 < 10 < 10 172 < 10 178 9.4 1.070 2.917

0.04 3 592 0.36CMB19182 < 10 212 267 < 10 178 224 1.035 2.9113

0.05 2 296 0.32CMB19183 < 10 231 180 < 10 130 231 1.0946

0.04 3 272 0.29CMB19184 < 10 466 158 < 10 106 498 1.0725

0.12 < 2 52 0.19CMB19185 < 10 < 10 97 < 10 65 2.2 1.0317


< 10 414 55 < 10 103 397 1.0572

0.03 2 180 0.31CMB19187 < 10 19 141 < 10 157 19.2 1.0946


< 10 20 146 < 10 163 18.4 1.0446

0.02 4 22 0.32CMB19189 < 10 12 93 < 10 7 12.0 1.0402

0.01 4 21 0.31CMB19190 PULP DUP FROM CMB19189

< 10 12 92 < 10 7 11.9 1.0552

0.01 3 33 0.31CMB19191 < 10 < 10 98 < 10 5 10.2 1.069 2.721

0.01 < 2 31 0.26CMB19192 < 10 13 56 < 10 13 16.8 1.068 2.702

< 0.01 < 2 39 0.07CMB19193 < 10 < 10 17 < 10 3 3.8 1.057 2.671

< 0.01 < 2 80 0.14CMB19194 < 10 17 83 < 10 15 19.1 1.086 2.622

< 0.01 < 2 71 0.06CMB19195 < 10 13 64 < 10 5 16.1 1.040 2.652

0.08 3 96 0.16CMB19196 < 10 60 155 < 10 34 60.4 1.0723

0.08 2 111 0.19CMB19197 < 10 89 141 < 10 30 88.1 1.0363

0.03 < 2 57 0.13CMB19198 < 10 < 10 158 < 10 49 1.1 1.0683


< 10 427 57 < 10 111 406 1.0752

0.01 < 2 78 0.17CMB19200 < 10 < 10 48 < 10 24 4.1 1.038 2.703

< 0.01 < 2 41 0.06CMB19451 < 10 < 10 15 < 10 6 4.6 1.0972

< 0.01 < 2 43 0.06CMB19452 PREP DUP FROM CMB19451

< 10 < 10 15 < 10 6 5.2 1.0912

0.02 < 2 88 0.17CMB19453 < 10 < 10 48 < 10 46 4.3 1.0514


< 10 < 10 49 < 10 45 3.3 1.0844

0.05 < 2 136 0.24CMB19455 < 10 < 10 50 < 10 30 5.5 1.079 2.814

0.07 3 151 0.24CMB19456 < 10 < 10 52 < 10 70 2.7 1.036 2.904

0.02 < 2 54 0.24CMB19401 < 10 137 67 < 10 87 143 1.0116

0.03 3 100 0.36CMB19402 < 10 198 91 < 10 74 209 1.072 2.776

0.03 2 137 0.22CMB19403 < 10 218 130 < 10 135 206 1.040 2.9814

0.02 < 2 164 0.20CMB19404 < 10 312 121 < 10 129 308 1.05812

0.04 3 36 0.31CMB19405 < 10 < 10 113 < 10 48 3.5 1.0489


< 10 890 60 < 10 113 861 1.0602

0.03 2 65 0.22CMB19407 < 10 26 116 < 10 105 18.8 1.09014

0.04 < 2 367 0.23CMB19408 < 10 40 95 < 10 108 42.8 1.08812

0.03 < 2 233 0.23CMB19409 < 10 177 93 < 10 90 182 1.038 3.0110

0.04 < 2 84 0.20CMB19410 < 10 10 112 < 10 88 8.5 1.05412

0.03 3 89 0.25CMB19411 < 10 15 127 < 10 120 12.0 1.08614


< 10 10 127 < 10 121 11.9 1.06414

0.03 3 52 0.25CMB19413 < 10 17 150 < 10 152 17.3 1.05311

0.04 3 90 0.28CMB19414 < 10 34 141 < 10 162 36.4 1.04313

0.04 3 70 0.26CMB19415 < 10 < 10 115 < 10 96 7.1 1.07011

0.02 < 2 54 0.23CMB19416 < 10 74 81 < 10 68 78.7 1.0467

0.01 2 61 0.31CMB19417 < 10 174 92 < 10 62 173 1.0454

0.01 < 2 42 0.25CMB19418 < 10 113 95 < 10 68 106 1.0955

0.02 2 127 0.24CMB19419 < 10 89 109 < 10 78 92.4 1.0508

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0.02 < 2 61 0.31CMB19420 < 10 22 89 < 10 70 24.0 1.0585

0.01 2 24 0.34CMB19421 < 10 < 10 84 < 10 90 7.2 1.045 2.834

0.02 < 2 29 0.20CMB19422 < 10 < 10 90 < 10 52 1.0 1.045 2.9410

0.03 3 52 0.45CMB19423 < 10 28 65 < 10 67 35.4 1.080 2.865

0.05 < 2 58 0.37CMB19424 < 10 62 65 < 10 80 64.2 1.047 2.836

0.02 < 2 35 0.35CMB19425 < 10 85 83 < 10 59 87.9 1.0543

0.07 < 2 88 0.39CMB19426 < 10 1030 122 < 10 65 976 1.0263

0.07 < 2 74 0.38CMB19427 < 10 719 135 < 10 68 702 1.0472

0.04 2 48 0.13CMB19428 < 10 < 10 149 < 10 47 3.2 1.0262


< 10 859 58 < 10 114 851 1.0352

0.02 2 52 0.31CMB19430 < 10 10 65 < 10 99 10.8 1.0786

0.03 2 67 0.40CMB19431 < 10 < 10 47 < 10 83 8.5 1.0414

0.02 2 55 0.34CMB19432 < 10 80 59 < 10 66 85.1 1.0725


< 10 84 59 < 10 67 87.9 1.0415

0.04 2 72 0.34CMB19434 < 10 47 87 < 10 75 52.3 1.0644

0.04 2 75 0.33CMB19435 < 10 44 106 < 10 101 46.8 1.0602

0.06 < 2 93 0.37CMB19436 < 10 51 117 < 10 72 51.5 1.0073

0.03 < 2 50 0.28CMB19437 < 10 282 111 < 10 56 252 1.0722


< 10 268 110 < 10 56 263 1.0522

0.02 < 2 52 0.36CMB19439 < 10 132 108 < 10 52 136 1.0844

< 0.01 3 20 0.32CMB19440 < 10 < 10 123 < 10 149 5.6 1.068 2.854

0.02 3 21 0.34CMB19441 < 10 < 10 122 < 10 156 7.9 1.070 2.823

0.05 < 2 26 0.27CMB19442 < 10 < 10 105 < 10 62 1.4 1.06210

0.04 < 2 25 0.22CMB19443 < 10 < 10 67 < 10 34 6.2 1.042 2.773

0.06 < 2 22 0.14CMB19444 < 10 252 60 < 10 36 251 1.0603

0.17 < 2 24 0.21CMB19445 < 10 < 10 81 < 10 92 1.9 1.063 3.008

0.05 < 2 17 0.11CMB19446 < 10 64 34 < 10 24 64.2 1.032 2.782

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Quality Control



24.7 0.31 15 213GXR-1 Meas 1.0 1400 0.83 3.4 7 7 1200 24.0 < 10 3 0.02 < 10 0.13 828 15 0.060 36 0.037 549372

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

25.2 0.31 13 165GXR-1 Meas 0.8 1400 0.77 3.7 9 6 1200 25.0 10 4 0.02 < 10 0.13 748 14 0.054 39 0.037 603359

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.1 2.73 < 10 33GXR-4 Meas 1.0 15 0.94 0.9 14 60 6760 3.31 10 < 1 1.30 47 1.62 133 328 0.120 40 0.121 43100

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

3.3 2.72 < 10 27GXR-4 Meas 1.4 31 0.93 0.6 15 56 6700 3.63 < 10 < 1 1.41 45 1.68 142 333 0.128 37 0.126 46106

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

18.7 3.36 20 1000GXR-2 Meas 1.0 < 2 0.81 5.0 9 27 92 2.29 10 3 0.55 23 0.54 1100 1 0.260 17 0.063 79618

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

17.9 3.03 19 1110GXR-2 Meas 1.1 < 2 0.77 4.4 10 25 83 2.16 < 10 3 0.52 22 0.52 993 < 1 0.249 17 0.060 76012

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.3 6.81 < 10 895GXR-6 Meas 1.0 < 2 0.16 0.7 13 84 73 6.31 20 < 1 0.86 10 0.40 1030 1 0.160 24 0.034 94242

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

0.3 6.69 < 10 955GXR-6 Meas 0.9 < 2 0.18 0.7 14 84 73 6.64 20 < 1 0.89 11 0.41 986 1 0.143 27 0.034 94245

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2990 6.53 2480

OREAS 13P Cert 2500 7.58 2260

OREAS 13P Meas 2820 6.04 2330

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

< 0.2 0.07 < 10 172CMB19191 Orig < 0.5 < 2 1.43 < 0.5 6 13 1 2.83 < 10 < 1 < 0.01 31 0.01 212 < 1 0.072 2 0.065 315

< 0.2 0.07 < 10 166CMB19191 Dup < 0.5 < 2 1.40 < 0.5 6 13 2 2.76 < 10 < 1 < 0.01 30 0.01 211 < 1 0.072 2 0.064 315

CMB19200 Orig

CMB19200 Dup

< 0.2 1.20 < 10 54CMB19455 Orig 0.6 < 2 1.73 < 0.5 16 57 37 2.70 < 10 < 1 0.23 31 0.83 263 2 0.053 21 0.069 35

< 0.2 1.18 < 10 54CMB19455 Dup 0.6 < 2 1.76 < 0.5 16 57 35 2.65 < 10 < 1 0.22 31 0.81 258 3 0.053 21 0.068 3< 2

< 0.2 0.88 < 10 728CMB19402 Orig 2.0 < 2 2.31 1.1 11 14 10 4.99 < 10 < 1 0.06 42 0.58 837 < 1 0.285 12 0.137 625

< 0.2 0.91 < 10 773CMB19402 Split 2.0 < 2 2.38 1.1 12 14 11 5.22 < 10 < 1 0.06 44 0.60 860 < 1 0.290 12 0.148 635

< 0.2 0.84 < 10 704CMB19402 Orig 2.0 < 2 2.25 1.0 10 13 9 4.88 < 10 < 1 0.06 40 0.55 807 < 1 0.270 11 0.134 604

< 0.2 0.92 < 10 752CMB19402 Dup 2.0 < 2 2.37 1.2 11 14 11 5.11 < 10 < 1 0.07 43 0.61 866 < 1 0.300 12 0.140 635

< 0.2 0.91 < 10 773CMB19402 Split 2.0 < 2 2.38 1.1 12 14 11 5.22 < 10 < 1 0.06 44 0.60 860 < 1 0.290 12 0.148 635

< 0.2 0.61 < 10 678CMB19402 Split 1.23 < 2 1.76 0.56 10.8 12.6 10.9 5.12 < 10 < 1 0.05 36.2 0.44 677 < 1 0.21 11.8 0.17 59.13.85

< 0.2 2.37 < 10 237CMB19412 PREP DUP FROM CMB19411 Orig

1.6 < 2 3.49 1.0 33 70 37 6.02 < 10 < 1 0.60 < 10 1.88 812 < 1 0.429 43 0.097 273

< 0.2 2.39 < 10 239CMB19412 PREP DUP FROM CMB19411 Dup

1.6 < 2 3.50 1.1 34 71 39 6.20 < 10 < 1 0.60 < 10 1.89 818 < 1 0.424 43 0.096 273

< 0.2 1.45 < 10 127CMB19422 Orig < 0.5 < 2 2.27 < 0.5 21 53 6 4.65 < 10 < 1 0.34 < 10 1.49 494 2 0.359 25 0.079 < 26

< 0.2 1.43 < 10 123CMB19422 Split < 0.5 < 2 2.21 < 0.5 20.0 51.5 5.36 4.51 < 10 < 1 0.33 < 10 1.46 487 1.81 0.35 27.0 0.08 < 23.16

0.8 0.70 < 10 400CMB19426 Orig 0.9 < 2 1.70 0.5 16 11 54 4.65 < 10 < 1 0.29 44 0.64 545 2 0.195 12 0.110 2977

0.8 0.68 < 10 397CMB19426 Dup 0.9 < 2 1.69 < 0.5 16 11 51 4.55 < 10 < 1 0.28 43 0.63 540 3 0.193 13 0.110 2947

< 0.2 0.45 < 10 665CMB19431 Orig < 0.5 < 2 1.54 0.8 14 12 15 4.68 < 10 < 1 0.22 39 0.62 635 1 0.190 13 0.106 58

< 0.2 0.44 < 10 661CMB19431 Split < 0.5 < 2 1.53 0.9 13 13 14 4.72 < 10 < 1 0.22 40 0.61 628 1 0.175 12 0.112 410

< 0.2 0.44 < 10 661CMB19431 Split < 0.5 < 2 1.53 0.9 13 13 14 4.72 < 10 < 1 0.22 40 0.61 628 1 0.175 12 0.112 410

CMB19440 Orig

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Quality Control



CMB19440 Dup

CMB19446 Orig

CMB19446 Split


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.009 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.010 < 1 < 0.001 < 2< 2




< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 < 0.001 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 < 0.001 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 < 0.001 < 1 < 0.001 < 2< 2

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Quality Control



0.20 79 156GXR-1 Meas < 10 32 75 187 6211

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

0.21 71 151GXR-1 Meas < 10 32 77 137 6341

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2970 2660

DH-1a Cert 2630 2630

DH-1a Meas 2610

DH-1a Cert 2630

1.93 4 67GXR-4 Meas < 10 < 10 82 12 646

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

1.98 3 76GXR-4 Meas < 10 < 10 84 16 676

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 36 85GXR-2 Meas < 10 < 10 51 < 10 5785

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.04 28 84GXR-2 Meas < 10 < 10 48 < 10 5524

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 4 30GXR-6 Meas < 10 < 10 175 < 10 11519

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

0.02 2 34GXR-6 Meas < 10 < 10 173 < 10 11821

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 282

SY-2 Cert 284

SY-2 Meas 286

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 11700

BL-3 Cert 10200

BL-4a Meas 1270

BL-4a Cert 1250

BL-4a Meas 1270

BL-4a Cert 1250

0.01 4 33 0.31CMB19191 Orig < 10 < 10 99 < 10 51

0.01 3 32 0.30CMB19191 Dup < 10 < 10 97 < 10 51

CMB19200 Orig 2.69

CMB19200 Dup 2.70

0.05 < 2 138 0.24CMB19455 Orig < 10 < 10 50 < 10 304

0.06 < 2 134 0.24CMB19455 Dup < 10 < 10 49 < 10 314

0.03 3 100 0.36CMB19402 Orig < 10 198 91 < 10 74 209 1.072 2.776

0.03 2 108 0.38CMB19402 Split < 10 209 95 < 10 76 206 1.024 2.846

0.03 3 95 0.34CMB19402 Orig < 10 190 88 < 10 725

0.03 2 105 0.37CMB19402 Dup < 10 206 93 < 10 766

0.03 2 108 0.38CMB19402 Split < 10 209 95 < 10 766

0.03 2.24 83.0 0.23CMB19402 Split < 10 202 78.7 < 10 61.54.07

0.03 2 87 0.25CMB19412 PREP DUP FROM CMB19411 Orig

< 10 11 126 < 10 12014

0.03 3 88 0.25CMB19412 PREP DUP FROM CMB19411 Dup

< 10 10 127 < 10 12214

0.02 < 2 29 0.20CMB19422 Orig < 10 < 10 90 < 10 52 1.0 1.045 2.9410

0.02 < 2 27.5 0.21CMB19422 Split < 10 < 10 88.3 < 10 47.3 1.1 1.051 2.939.47

0.07 < 2 88 0.39CMB19426 Orig < 10 1030 122 < 10 653

0.07 < 2 88 0.39CMB19426 Dup < 10 1030 121 < 10 653

0.03 2 67 0.40CMB19431 Orig < 10 < 10 47 < 10 83 8.5 1.0414

0.03 3 66 0.41CMB19431 Split < 10 < 10 47 < 10 84 9.7 1.0214

0.03 3 66 0.41CMB19431 Split < 10 < 10 47 < 10 844

CMB19440 Orig 2.86

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Quality Control



CMB19440 Dup 2.85

CMB19446 Orig 64.2 1.032 2.78

CMB19446 Split 66.1 1.030 2.81


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1

Page 9 of 9

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

06-Aug-08

16-Jul-08

A08-4123



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-4123

Notes:




Quality Control


Document Page 216




< 0.2 0.35 < 10 854CMB19391 0.8 < 2 1.61 < 0.5 16 31 25 5.24 < 10 < 1 0.12 33 0.38 602 < 1 0.113 8 0.079 1012

< 0.2 0.23 < 10 707CMB19392 1.0 < 2 1.55 0.6 17 31 4 5.62 < 10 < 1 0.05 25 0.25 559 1 0.140 7 0.080 1612

0.2 0.33 < 10 227CMB19393 1.0 < 2 1.72 0.5 22 33 6 6.82 < 10 < 1 0.05 27 0.34 610 < 1 0.140 7 0.076 6113

< 0.2 0.54 < 10 160CMB19394 1.0 < 2 2.18 0.8 24 38 2 7.96 < 10 < 1 0.26 17 0.67 936 < 1 0.110 12 0.087 109

< 0.2 0.22 < 10 1180CMB19395 1.0 < 2 1.62 0.7 15 17 1 5.85 < 10 < 1 0.07 42 0.26 614 < 1 0.180 7 0.090 479

0.5 0.36 < 10 420CMB19396 1.0 < 2 2.53 0.5 13 6 2 6.11 < 10 < 1 0.05 55 0.42 702 1 0.160 5 0.081 26912

0.2 0.15 < 10 800CMB19397 < 0.5 < 2 1.29 0.5 12 6 46 5.23 < 10 < 1 0.04 53 0.17 341 5 0.120 6 0.074 594

0.2 2.14 < 10 319CMB19398 1.0 < 2 2.37 0.5 29 170 221 5.00 < 10 < 1 1.08 22 2.25 651 10 0.200 44 0.130 367

< 0.2 0.20 < 10 1270CMB19399 < 0.5 < 2 1.46 0.7 11 7 32 5.64 < 10 < 1 0.05 55 0.19 363 8 0.180 6 0.094 176

0.3 1.07 < 10 719CMB19400 1.0 < 2 2.39 0.6 16 31 66 4.91 < 10 < 1 0.09 42 0.93 508 1 0.360 20 0.092 1306

0.4 0.33 < 10 1580CMB19551 1.0 < 2 2.11 0.5 11 7 25 5.05 < 10 < 1 0.02 62 0.30 460 2 0.230 7 0.077 1418

0.8 0.48 < 10 895CMB19552 1.0 < 2 3.00 0.5 11 8 5 5.00 10 < 1 0.05 58 0.45 618 1 0.190 6 0.097 4529

< 0.2 0.70 < 10 861CMB19553 1.0 < 2 2.33 0.5 14 53 22 5.20 < 10 < 1 0.20 52 0.75 550 1 0.200 17 0.122 1167

< 0.2 0.44 < 10 1030CMB19554 1.0 < 2 1.96 0.5 14 23 51 5.53 < 10 < 1 0.12 52 0.45 476 1 0.180 11 0.090 1243

< 0.2 0.29 < 10 1030CMB19555 1.0 < 2 2.04 0.6 14 7 37 6.32 < 10 < 1 0.05 55 0.35 519 4 0.190 10 0.103 1225

0.4 0.36 < 10 1120CMB19556 1.0 < 2 2.38 0.5 12 6 49 5.02 < 10 < 1 0.04 50 0.41 562 1 0.200 8 0.098 1754

< 0.2 0.42 < 10 862CMB19557 1.0 < 2 2.32 0.6 16 13 25 5.96 < 10 < 1 0.09 42 0.56 490 < 1 0.200 15 0.104 386

0.6 0.49 < 10 842CMB19558 1.0 < 2 2.74 0.6 17 16 5 5.83 < 10 < 1 0.07 39 0.55 491 1 0.220 17 0.118 2567

0.6 0.56 13 563CMB19559 1.0 < 2 2.09 0.6 20 18 21 5.88 < 10 < 1 0.25 38 0.63 480 1 0.130 21 0.124 347

< 0.2 0.44 < 10 79CMB19560 < 0.5 < 2 1.34 0.6 15 18 24 5.76 < 10 < 1 0.15 36 0.39 300 2 0.120 14 0.119 175

< 0.2 2.91 < 10 608CMB19581 < 0.5 < 2 2.89 1.0 33 111 54 5.73 < 10 < 1 0.69 10 3.05 942 < 1 0.490 71 0.077 402

< 0.2 1.60 < 10 252CMB19582 < 0.5 < 2 2.25 1.0 28 49 205 5.55 < 10 < 1 0.31 23 1.57 658 1 0.330 42 0.107 637

1.5 0.89 < 10 640CMB19583 2.0 < 2 3.39 0.5 16 10 3 4.83 10 < 1 0.08 36 0.91 708 1 0.360 12 0.133 55816

< 0.2 0.51 < 10 1180CMB19584 2.0 < 2 3.06 0.8 16 10 1 4.80 < 10 < 1 0.07 36 0.66 656 < 1 0.340 11 0.125 13618

< 0.2 0.36 < 10 880CMB19585 2.0 < 2 2.18 0.6 17 12 2 5.76 < 10 < 1 0.07 40 0.46 589 < 1 0.240 18 0.136 2720

< 0.2 0.50 < 10 1290CMB19586 1.0 < 2 1.67 0.6 21 13 11 6.35 < 10 < 1 0.23 41 0.63 614 < 1 0.330 21 0.129 1512

< 0.2 0.45 < 10 1350CMB19561 1.0 < 2 2.51 0.6 17 12 2 5.01 < 10 < 1 0.06 39 0.54 617 < 1 0.310 15 0.127 1414

< 0.2 0.47 < 10 864CMB19562 2.0 < 2 2.61 0.5 14 8 2 3.49 < 10 < 1 0.06 42 0.56 624 3 0.290 11 0.144 2618

< 0.2 0.49 < 10 493CMB19563 1.0 < 2 2.17 0.5 13 9 1 3.62 < 10 < 1 0.05 38 0.56 533 < 1 0.270 9 0.130 6610

< 0.2 0.51 < 10 413CMB19564 1.0 < 2 2.17 < 0.5 13 10 1 3.79 < 10 < 1 0.05 37 0.59 549 < 1 0.280 11 0.140 6713

< 0.2 2.89 < 10 448CMB19565 < 0.5 < 2 2.36 0.5 28 43 29 5.45 10 < 1 0.68 31 1.56 456 < 1 0.430 37 0.170 2< 2


< 0.5 < 2 1.17 < 0.5 9 29 31 2.22 < 10 < 1 0.11 76 0.34 292 4 0.130 46 0.041 1416

< 0.2 0.46 < 10 211CMB19567 1.0 < 2 2.16 0.5 12 10 < 1 3.69 < 10 < 1 0.04 38 0.52 502 < 1 0.235 10 0.149 5614

0.2 0.39 < 10 703CMB19568 1.0 < 2 1.86 < 0.5 11 10 1 3.68 < 10 < 1 0.04 31 0.41 424 < 1 0.220 9 0.136 10811

< 0.2 0.48 < 10 490CMB19569 2.0 < 2 2.00 0.5 12 8 < 1 3.31 < 10 < 1 0.04 40 0.50 485 < 1 0.270 10 0.156 6914

0.2 0.31 < 10 1430CMB19570 1.0 < 2 1.72 0.5 13 10 2 4.14 < 10 < 1 0.02 37 0.33 355 < 1 0.260 9 0.165 19114

< 0.2 0.43 < 10 980CMB19571 3.0 < 2 1.99 0.6 16 11 4 4.70 < 10 < 1 0.05 38 0.48 503 < 1 0.260 12 0.157 6012

< 0.2 0.45 < 10 764CMB19572 2.0 < 2 1.92 0.6 17 15 1 6.14 < 10 < 1 0.04 41 0.39 456 < 1 0.220 13 0.144 7413

< 0.2 1.76 < 10 479CMB19573 1.0 < 2 2.68 < 0.5 26 56 27 5.32 < 10 < 1 0.72 28 2.03 783 < 1 0.340 36 0.107 4611

0.2 1.82 < 10 313CMB19574 1.0 < 2 2.47 < 0.5 25 52 86 4.57 < 10 < 1 0.51 20 1.97 706 < 1 0.300 38 0.113 779

0.3 0.23 < 10 39CMB19575 1.0 < 2 1.34 < 0.5 11 42 1 2.14 < 10 < 1 0.14 23 0.59 209 < 1 0.120 25 0.023 49

< 0.2 0.39 < 10 11CMB19576 1.0 < 2 2.13 < 0.5 8 37 < 1 2.04 < 10 < 1 0.02 24 0.45 252 < 1 0.160 16 0.022 99

< 0.2 0.72 10 23CMB19577 1.0 < 2 3.12 < 0.5 11 34 < 1 1.98 < 10 < 1 0.04 26 0.81 379 < 1 0.260 21 0.025 6210

< 0.2 0.53 < 10 12CMB19578 1.0 < 2 2.80 < 0.5 10 44 < 1 2.28 < 10 < 1 0.03 24 0.62 341 < 1 0.200 20 0.027 197

< 0.2 0.72 10 23CMB19579 PREP DUP FROM CMB19577

1.0 < 2 3.12 < 0.5 11 35 < 1 1.96 < 10 < 1 0.04 25 0.81 378 < 1 0.260 21 0.025 6110


1.0 < 2 2.80 < 0.5 10 45 < 1 2.34 < 10 < 1 0.03 25 0.64 346 < 1 0.210 20 0.027 197

0.4 0.11 40 16CMB19651 < 0.5 < 2 0.70 < 0.5 6 22 32 0.87 < 10 < 1 0.01 24 0.12 72 < 1 0.080 7 0.010 238

< 0.2 0.77 < 10 50CMB19587 < 0.5 < 2 1.25 0.7 16 81 68 4.65 < 10 < 1 0.36 27 0.80 349 4 0.140 23 0.056 135

0.2 0.90 < 10 72CMB19588 3.0 < 2 1.50 0.5 16 166 29 3.47 < 10 < 1 0.34 24 1.00 354 < 1 0.140 37 0.034 336

1.8 2.38 17 82CMB19589 2.0 < 2 3.82 0.9 22 48 114 4.36 20 < 1 0.15 12 1.32 526 < 1 0.330 27 0.076 55311

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0.9 2.60 11 130CMB19590 1.0 < 2 3.85 0.6 31 51 148 5.87 10 < 1 0.24 < 10 2.26 812 < 1 0.540 47 0.079 1569

1.1 1.19 66 32CMB19591 1.0 < 2 2.45 < 0.5 12 55 114 2.48 10 < 1 0.06 21 0.69 300 1 0.180 16 0.049 1559

1.4 2.00 < 10 108CMB19592 2.0 < 2 3.57 0.5 19 69 289 3.87 10 < 1 0.22 17 1.10 455 2 0.260 24 0.064 15215

0.8 1.60 < 10 90CMB19593 2.0 < 2 2.95 0.5 17 67 211 3.53 < 10 < 1 0.20 18 0.97 421 1 0.210 20 0.063 1068

< 0.2 2.60 < 10 482CMB19594 < 0.5 < 2 1.90 < 0.5 25 38 66 4.94 10 < 1 0.65 35 1.27 379 1 0.400 29 0.181 4< 2


< 0.5 < 2 1.14 < 0.5 9 28 33 2.14 < 10 < 1 0.11 75 0.33 284 4 0.140 43 0.041 1372

< 0.2 0.45 < 10 34CMB19596 < 0.5 < 2 1.05 0.6 9 11 16 4.41 < 10 < 1 0.15 106 0.29 318 1 0.130 6 0.036 193

< 0.2 0.30 < 10 30CMB19597 < 0.5 < 2 0.82 0.5 6 6 3 4.05 < 10 < 1 0.14 136 0.11 293 < 1 0.080 < 1 0.055 168

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0.03 3 60 0.43CMB19391 < 10 14 81 < 10 66 17.8 1.084 2.804

0.03 3 49 0.52CMB19392 < 10 51 113 < 10 67 52.7 1.074 2.853

0.02 4 51 0.65CMB19393 < 10 302 131 < 10 97 303 1.0545

0.02 4 51 0.47CMB19394 < 10 13 137 < 10 157 12.2 1.0659

0.04 3 73 0.41CMB19395 < 10 124 147 < 10 108 124 1.0663

0.03 2 219 0.33CMB19396 < 10 942 184 < 10 91 931 1.0405

0.03 3 58 0.31CMB19397 < 10 134 91 < 10 52 141 1.0572

0.06 < 2 118 0.32CMB19398 < 10 13 115 < 10 86 12.8 1.0639

0.05 2 67 0.33CMB19399 < 10 16 90 < 10 110 18.8 1.0812

0.04 2 73 0.32CMB19400 < 10 409 120 < 10 75 403 1.0506

0.06 2 101 0.34CMB19551 < 10 372 130 < 10 71 360 1.0223

0.05 3 138 0.32CMB19552 < 10 1390 121 < 10 71 1380 1.0513

0.04 2 93 0.35CMB19553 < 10 331 109 < 10 63 319 1.0445

0.05 2 84 0.33CMB19554 < 10 311 175 < 10 90 317 1.0784

0.05 3 75 0.35CMB19555 < 10 326 118 < 10 106 326 1.0345

0.05 2 97 0.32CMB19556 < 10 610 72 < 10 120 643 1.0595

0.04 3 72 0.37CMB19557 < 10 50 77 < 10 164 53.6 1.0395

0.04 2 82 0.39CMB19558 < 10 928 108 < 10 132 924 1.011 2.826

0.03 < 2 55 0.38CMB19559 < 10 87 83 < 10 192 89.2 1.0854

0.02 3 35 0.30CMB19560 < 10 < 10 67 < 10 129 5.6 1.0525

0.10 3 72 0.31CMB19581 < 10 14 125 < 10 220 13.9 1.00314

0.12 2 66 0.37CMB19582 < 10 25 112 < 10 188 24.7 1.0458

0.04 3 170 0.36CMB19583 < 10 2130 114 < 10 102 2480 1.0256

0.06 2 142 0.38CMB19584 < 10 355 120 < 10 93 370 1.0755

0.04 3 94 0.41CMB19585 < 10 55 124 < 10 133 60.0 1.0785

0.05 4 95 0.46CMB19586 < 10 13 83 < 10 142 15.0 1.0453

0.06 3 113 0.42CMB19561 < 10 23 62 < 10 61 22.9 1.0904

0.04 3 100 0.35CMB19562 < 10 55 56 < 10 60 56.1 1.0035

0.03 2 76 0.30CMB19563 < 10 241 29 < 10 50 253 1.0906

0.03 2 71 0.31CMB19564 < 10 275 31 < 10 52 278 1.0386

0.04 < 2 63 0.21CMB19565 < 10 < 10 80 < 10 72 1.6 1.0779


< 10 350 51 < 10 97 391 1.0842

0.02 3 61 0.30CMB19567 < 10 200 25 < 10 53 199 1.0496

0.03 < 2 67 0.28CMB19568 < 10 440 29 < 10 48 440 1.0805

0.03 < 2 70 0.30CMB19569 < 10 77 32 < 10 64 79.3 1.0777

0.05 2 84 0.33CMB19570 < 10 504 47 < 10 56 493 1.065 2.844

0.04 2 83 0.34CMB19571 < 10 228 36 < 10 63 227 1.0635

0.03 3 103 0.35CMB19572 < 10 196 43 < 10 45 196 1.0565

0.03 < 2 146 0.28CMB19573 < 10 32 111 < 10 127 34.2 1.0549

0.03 2 119 0.26CMB19574 < 10 16 96 < 10 106 17.4 1.0848

< 0.01 < 2 37 0.26CMB19575 < 10 13 80 < 10 48 14.7 1.0642

0.01 < 2 74 0.21CMB19576 < 10 22 56 < 10 34 22.2 1.0652

0.02 2 88 0.19CMB19577 < 10 197 30 < 10 51 218 1.0744

0.02 < 2 73 0.20CMB19578 < 10 68 49 < 10 43 71.9 1.0593


< 10 198 29 < 10 51 209 1.0294


< 10 68 50 < 10 44 73.9 1.0183

< 0.01 < 2 28 0.22CMB19651 < 10 92 19 < 10 14 101 1.0561

0.02 2 50 0.35CMB19587 < 10 12 109 < 10 126 11.6 1.0783

0.02 2 62 0.24CMB19588 < 10 66 137 < 10 118 72.0 1.0544

0.04 < 2 240 0.33CMB19589 < 10 1840 183 < 10 261 2100 1.062 3.149

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0.04 2 165 0.36CMB19590 < 10 643 169 < 10 161 663 1.03514

0.03 < 2 136 0.27CMB19591 < 10 486 115 < 10 144 534 1.0044

0.07 2 185 0.34CMB19592 < 10 436 117 < 10 158 456 1.0538

0.05 3 142 0.33CMB19593 < 10 293 106 < 10 142 305 1.0837

0.06 < 2 46 0.18CMB19594 < 10 < 10 78 < 10 69 2.1 1.0638


< 10 341 50 < 10 97 395 1.0862

0.02 2 24 0.25CMB19596 < 10 10 39 < 10 90 19.2 1.054 2.736

0.01 2 21 0.22CMB19597 < 10 < 10 23 < 10 44 10.4 1.0126

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Quality Control



25.2 0.33 15 272GXR-1 Meas 1.0 1540 0.82 3.3 8 6 1230 26.0 < 10 3 0.02 < 10 0.14 798 15 0.060 38 0.042 614389

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.1 2.57 < 10 29GXR-4 Meas 1.0 28 0.94 0.7 14 55 6360 3.00 10 < 1 1.34 45 1.58 138 317 0.130 40 0.118 4397

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

18.1 3.40 21 1240GXR-2 Meas 1.0 < 2 0.85 4.7 10 27 86 2.00 10 3 0.55 22 0.54 997 1 0.250 19 0.057 75612

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.3 6.91 < 10 853GXR-6 Meas 1.0 < 2 0.16 0.8 15 88 76 6.55 20 < 1 0.94 12 0.41 998 2 0.130 25 0.034 98243

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 2780 5.80 2260

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

< 0.2 0.22 < 10 1170CMB19395 Orig 1.0 < 2 1.60 0.7 15 17 1 5.77 < 10 < 1 0.07 41 0.26 607 < 1 0.180 7 0.089 479

< 0.2 0.22 < 10 1200CMB19395 Dup 1.0 < 2 1.63 0.7 15 17 1 5.93 < 10 < 1 0.07 42 0.27 621 1 0.180 7 0.092 479

0.5 0.56 13 562CMB19559 Orig 1.0 < 2 2.08 0.6 20 18 21 5.90 < 10 < 1 0.25 38 0.63 479 1 0.130 21 0.124 347

0.6 0.56 13 563CMB19559 Dup 1.0 < 2 2.10 0.6 19 18 20 5.85 < 10 < 1 0.25 37 0.63 480 1 0.130 21 0.123 337

< 0.2 0.51 < 10 413CMB19564 Orig 1.0 < 2 2.17 < 0.5 13 10 1 3.79 < 10 < 1 0.05 37 0.59 549 < 1 0.280 11 0.140 6713

< 0.2 0.55 < 10 423CMB19564 Split 1.00 < 2 2.26 < 0.5 14.0 10.0 1.00 4.04 < 10 < 1 0.05 39.0 0.62 572 < 1 0.30 11.0 0.14 69.011.0

< 0.2 0.46 < 10 211CMB19567 Orig 1.0 < 2 2.16 0.5 12 10 1 3.73 < 10 < 1 0.04 38 0.52 501 < 1 0.240 10 0.153 5514

< 0.2 0.46 < 10 210CMB19567 Dup 1.0 < 2 2.16 0.5 12 9 < 1 3.65 < 10 < 1 0.04 38 0.52 502 < 1 0.230 9 0.146 5613

0.4 0.11 40 16CMB19651 Orig < 0.5 < 2 0.70 < 0.5 5 22 37 0.89 < 10 < 1 0.01 24 0.12 72 < 1 0.080 7 0.010 238

0.5 0.11 40 15CMB19651 Dup < 0.5 < 2 0.70 < 0.5 6 22 27 0.84 < 10 < 1 0.01 23 0.12 72 < 1 0.080 7 0.010 228

1.8 2.38 17 82CMB19589 Orig 2.0 < 2 3.82 0.9 22 48 114 4.36 20 < 1 0.15 12 1.32 526 < 1 0.330 27 0.076 55311

1.80 2.40 17.0 85.0CMB19589 Split 2.00 < 2 3.84 0.90 22.0 48.0 130 4.52 19.0 < 1 0.16 11.0 1.34 536 1.00 0.33 30.0 0.08 5708.00

< 0.2 0.30 < 10 30CMB19597 Orig < 0.5 < 2 0.82 0.5 6 6 3 4.05 < 10 < 1 0.14 136 0.11 293 < 1 0.080 < 1 0.055 168

< 0.2 0.28 < 10 28.0CMB19597 Split < 0.5 < 2 0.79 < 0.5 6.00 5.00 3.00 3.81 < 10 < 1 0.13 124 0.10 277 < 1 0.07 1.00 0.05 17.0< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 < 0.001 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 < 0.001 < 1 < 0.001 < 2< 2



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Quality Control



0.22 81 184GXR-1 Meas < 10 35 78 172 6361

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2610 2590

DH-1a Cert 2630 2630

DH-1a Meas 2670

DH-1a Cert 2630

1.86 3 73GXR-4 Meas < 10 < 10 79 18 696

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 29 91GXR-2 Meas < 10 < 10 48 < 10 5595

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 5 30GXR-6 Meas < 10 < 10 178 < 10 12322

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 285

SY-2 Cert 284

SY-2 Meas 279

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 9460

BL-3 Cert 10200

BL-4a Meas 1280

BL-4a Cert 1250

BL-4a Meas 1280

BL-4a Cert 1250

0.04 2 72 0.41CMB19395 Orig < 10 122 145 < 10 1073

0.05 3 74 0.42CMB19395 Dup < 10 125 149 < 10 1093

0.03 2 54 0.38CMB19559 Orig < 10 87 83 < 10 1944

0.03 < 2 55 0.38CMB19559 Dup < 10 86 82 < 10 1904

0.03 2 71 0.31CMB19564 Orig < 10 275 31 < 10 52 278 1.0386

0.03 2.00 74.0 0.32CMB19564 Split < 10 277 33.0 < 10 54.0 279 1.0876.00

0.02 2 61 0.30CMB19567 Orig < 10 202 25 < 10 536

0.02 3 61 0.29CMB19567 Dup < 10 198 24 < 10 536

< 0.01 < 2 28 0.23CMB19651 Orig < 10 94 19 < 10 131

< 0.01 < 2 27 0.22CMB19651 Dup < 10 90 19 < 10 141

0.04 < 2 240 0.33CMB19589 Orig < 10 1840 183 < 10 261 2100 1.062 3.149

0.04 3.00 235 0.33CMB19589 Split < 10 1870 185 < 10 266 2100 1.053 3.099.00

0.01 2 21 0.22CMB19597 Orig < 10 < 10 23 < 10 44 10.4 1.0126

< 0.01 < 2 20.0 0.20CMB19597 Split < 10 < 10 22.0 < 10 43.0 10.6 1.0725.00


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

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Invoice No.:

Invoice Date:

Date Submitted:

Your Reference:

15-Aug-08

18-Jul-08

A08-4174



Cam McLeanATTN:






CERTIFIED BY :

REPORT A08-4174

Notes:


Code Specific Gravity PulpCode 5D-U-Total DNCCode 1E3 - Aurora Pkg. Aqua Regia ICP(AQUAGEO)


Quality Control


Document Page 223




< 0.2 0.53 < 10 865CMB19601 < 0.5 < 2 2.49 < 0.5 15 12 3 5.67 < 10 < 1 0.26 37 0.70 714 < 1 0.163 14 0.119 2123

< 0.2 0.73 < 10 558CMB19602 0.5 < 2 2.08 0.6 16 11 20 6.39 < 10 < 1 0.53 35 1.03 746 < 1 0.095 18 0.130 137

< 0.2 0.67 < 10 450CMB19603 0.6 < 2 1.81 1.3 14 9 6 5.98 < 10 < 1 0.50 51 0.92 663 < 1 0.099 15 0.095 537

< 0.2 0.47 < 10 456CMB19604 < 0.5 < 2 2.34 < 0.5 11 9 19 4.32 < 10 < 1 0.13 49 0.56 461 < 1 0.174 9 0.102 705

< 0.2 2.27 < 10 376CMB19605 < 0.5 < 2 3.15 0.7 34 48 70 6.15 10 < 1 0.33 < 10 2.06 750 < 1 0.707 57 0.080 85

< 0.2 0.51 < 10 820CMB19606 0.7 < 2 2.36 0.6 14 12 26 5.58 < 10 < 1 0.12 40 0.62 538 1 0.234 15 0.122 327

0.2 0.37 < 10 519CMB19607 0.7 < 2 2.97 0.6 11 11 39 4.64 < 10 < 1 0.07 35 0.48 665 < 1 0.170 9 0.089 455

< 0.2 0.27 < 10 691CMB19608 0.7 < 2 2.93 0.5 13 12 33 5.25 < 10 < 1 0.02 37 0.38 665 < 1 0.159 13 0.132 509

2.2 0.38 < 10 577CMB19609 1.7 < 2 3.25 0.6 14 8 13 4.98 10 < 1 0.02 52 0.49 744 1 0.245 11 0.151 79311

0.5 0.19 < 10 634CMB19610 1.2 < 2 2.56 < 0.5 10 8 7 3.72 < 10 < 1 0.01 43 0.27 492 1 0.142 8 0.126 26910


1.2 < 2 2.62 < 0.5 10 7 5 3.79 < 10 < 1 0.01 48 0.28 506 < 1 0.146 7 0.132 27211

1.9 0.27 < 10 443CMB19612 1.6 < 2 2.74 < 0.5 10 6 5 3.17 10 < 1 0.02 50 0.37 538 1 0.196 6 0.114 7898

3.1 0.28 < 10 38CMB19613 1.5 < 2 2.85 < 0.5 9 6 5 3.07 20 < 1 0.02 57 0.40 561 < 1 0.154 4 0.162 122010

2.0 0.23 < 10 190CMB19614 1.8 < 2 3.10 < 0.5 11 7 2 4.10 10 < 1 0.02 39 0.33 611 < 1 0.149 7 0.137 78012

1.7 0.20 < 10 997CMB19615 1.7 < 2 3.06 0.8 11 8 7 4.84 10 < 1 0.02 34 0.28 570 < 1 0.173 8 0.122 61912

1.0 0.44 < 10 1080CMB19616 1.8 < 2 3.03 1.4 14 24 152 6.04 < 10 < 1 0.07 29 0.55 579 2 0.234 14 0.101 2918

< 0.2 0.98 < 10 514CMB19617 < 0.5 < 2 2.62 0.7 19 37 74 5.52 < 10 < 1 0.24 15 1.11 589 3 0.288 25 0.114 398

< 0.2 0.24 < 10 561CMB19618 1.2 < 2 2.29 0.6 13 9 36 5.69 < 10 < 1 0.11 30 0.38 571 10 0.111 14 0.152 377

< 0.2 0.11 < 10 499CMB19619 < 0.5 < 2 2.37 1.1 13 10 51 5.37 < 10 < 1 0.05 28 0.14 411 2 0.083 13 0.130 536


< 0.5 < 2 2.44 1.2 13 10 49 5.32 < 10 < 1 0.05 29 0.14 419 3 0.080 13 0.132 577

0.3 0.35 < 10 871CMB19621 1.0 < 2 2.26 0.6 14 10 27 5.25 < 10 < 1 0.19 33 0.45 439 3 0.142 13 0.131 1998

0.3 0.23 < 10 1210CMB19622 1.3 < 2 2.35 0.5 13 9 21 5.25 < 10 < 1 0.09 32 0.36 445 < 1 0.170 10 0.128 1278

< 0.2 0.37 < 10 871CMB19623 1.0 < 2 2.65 0.5 14 14 18 4.96 < 10 < 1 0.15 27 0.54 499 < 1 0.169 15 0.115 778

0.3 0.45 < 10 722CMB19624 1.1 < 2 3.31 < 0.5 16 15 5 5.17 < 10 < 1 0.19 29 0.68 557 < 1 0.173 15 0.124 1755

0.4 0.48 < 10 782CMB19625 1.0 < 2 3.36 < 0.5 14 15 9 5.15 < 10 < 1 0.19 28 0.67 574 < 1 0.185 16 0.119 2295

< 0.2 1.39 < 10 110CMB19626 < 0.5 < 2 1.10 < 0.5 23 44 27 4.76 < 10 < 1 0.33 18 0.69 181 < 1 0.233 39 0.149 < 2< 2


0.5 < 2 1.24 < 0.5 10 33 30 2.51 < 10 < 1 0.11 93 0.31 322 4 0.134 49 0.047 289< 2


< 0.2 0.26 < 10 667CMB19628 < 0.5 < 2 1.64 0.8 18 17 51 5.91 < 10 < 1 0.13 36 0.40 293 1 0.127 18 0.122 237

0.5 0.92 < 10 578CMB19629 < 0.5 < 2 1.59 0.7 19 34 41 4.68 < 10 < 1 0.50 26 1.03 412 1 0.151 30 0.113 97

< 0.2 0.53 15 320CMB19630 < 0.5 < 2 1.00 0.6 17 18 43 5.43 < 10 < 1 0.38 36 0.54 371 < 1 0.072 21 0.123 145

< 0.2 0.53 < 10 122CMB19631 < 0.5 < 2 1.11 0.6 16 17 32 5.49 < 10 < 1 0.36 37 0.53 326 1 0.083 17 0.121 1118

0.2 0.26 < 10 648CMB19632 0.5 < 2 2.63 0.7 15 15 42 4.94 < 10 < 1 0.10 29 0.39 414 2 0.127 15 0.119 1299

0.3 1.32 < 10 236CMB19633 0.6 < 2 3.41 0.7 33 44 125 3.68 < 10 < 1 0.12 11 1.12 444 < 1 0.448 39 0.099 4912

0.7 0.40 < 10 500CMB19634 1.5 < 2 3.27 1.8 18 17 66 4.64 < 10 < 1 0.07 25 0.51 465 < 1 0.194 17 0.115 26311

1.1 0.25 < 10 705CMB19635 1.1 < 2 2.32 1.7 14 16 193 4.88 < 10 < 1 0.05 27 0.32 413 < 1 0.149 15 0.120 2189


1.0 < 2 2.29 1.8 14 16 195 4.83 < 10 < 1 0.05 27 0.31 408 < 1 0.144 15 0.117 20411

< 0.2 0.22 < 10 712CMB19637 0.9 < 2 2.43 0.8 13 13 38 4.51 < 10 < 1 0.04 26 0.33 377 < 1 0.158 14 0.118 4911

2.6 0.55 < 10 429CMB19638 3.1 < 2 3.39 0.8 16 26 140 4.65 10 < 1 0.11 24 0.64 565 2 0.230 16 0.114 71312

0.4 0.42 < 10 649CMB19639 1.0 < 2 3.91 0.8 11 15 66 4.03 < 10 < 1 0.02 22 0.50 488 < 1 0.247 11 0.121 11519

1.2 0.25 < 10 937CMB19640 1.2 < 2 2.77 1.0 13 14 95 4.88 < 10 < 1 0.03 27 0.34 541 < 1 0.180 12 0.110 3866

1.7 0.29 < 10 1010CMB19641 1.3 < 2 2.91 1.1 13 14 170 4.75 < 10 < 1 0.03 28 0.38 563 < 1 0.209 17 0.106 4956

< 0.2 2.03 < 10 387CMB19642 < 0.5 < 2 1.66 < 0.5 23 50 28 3.77 < 10 < 1 0.60 19 1.17 299 < 1 0.233 34 0.141 4< 2


0.5 < 2 1.23 < 0.5 17 34 36 2.45 < 10 < 1 0.09 94 0.24 321 8 0.127 101 0.036 3312

3.5 0.28 < 10 857CMB19644 1.3 < 2 2.70 1.1 14 15 142 5.09 10 < 1 0.06 29 0.39 490 24 0.153 15 0.114 10103

1.1 0.33 < 10 710CMB19645 0.9 < 2 2.83 1.2 13 14 185 5.00 < 10 < 1 0.09 25 0.46 544 2 0.151 16 0.111 2614


0.9 < 2 2.89 1.1 14 15 175 5.17 < 10 < 1 0.10 26 0.47 554 2 0.147 17 0.113 2665

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0.3 0.39 < 10 704CMB19647 0.9 < 2 2.34 0.9 16 18 74 5.09 < 10 < 1 0.15 25 0.56 437 < 1 0.151 20 0.119 625

< 0.2 1.06 < 10 713CMB19648 0.6 < 2 1.66 < 0.5 24 159 71 3.99 < 10 < 1 0.62 25 1.89 404 < 1 0.255 113 0.128 147

< 0.2 0.38 < 10 701CMB19649 0.6 < 2 2.07 0.6 17 17 32 5.22 < 10 < 1 0.21 29 0.58 470 < 1 0.141 20 0.117 278

< 0.2 0.46 < 10 785CMB19652 < 0.5 < 2 0.75 0.9 16 15 21 5.29 < 10 < 1 0.39 27 0.63 360 4 0.091 16 0.108 244

0.3 0.46 < 10 1250CMB19653 1.1 < 2 2.08 1.3 15 14 42 4.78 < 10 < 1 0.24 35 0.65 486 < 1 0.170 15 0.110 936

0.3 0.56 < 10 1270CMB19654 1.1 < 2 1.65 0.7 16 15 68 5.05 < 10 < 1 0.25 27 0.84 489 2 0.209 20 0.103 1176

0.8 0.50 < 10 1310CMB19655 1.0 < 2 2.43 0.5 14 14 18 5.03 < 10 < 1 0.19 33 0.65 487 1 0.205 14 0.107 1108

0.6 0.47 < 10 1300CMB19656 1.4 < 2 3.20 < 0.5 12 12 18 4.20 < 10 < 1 0.12 31 0.66 578 5 0.231 11 0.093 2106


1.4 < 2 3.16 0.6 12 12 20 4.09 < 10 < 1 0.12 30 0.65 571 6 0.238 11 0.091 2165

0.3 0.41 < 10 940CMB19658 1.0 < 2 1.89 0.9 16 14 59 4.16 < 10 < 1 0.15 31 0.61 372 26 0.169 14 0.108 1366

0.4 0.42 < 10 915CMB19659 0.9 < 2 1.79 1.0 15 14 49 4.93 < 10 < 1 0.26 32 0.71 439 2 0.156 16 0.105 756

< 0.2 0.62 < 10 782CMB19660 < 0.5 < 2 1.20 0.6 18 15 55 5.38 < 10 < 1 0.53 26 0.89 471 2 0.111 19 0.111 265

0.3 0.59 < 10 735CMB19661 0.8 < 2 2.32 0.9 17 15 69 5.46 < 10 < 1 0.41 33 0.88 526 4 0.143 17 0.114 1108

< 0.2 0.44 < 10 1160CMB19662 1.6 < 2 2.95 < 0.5 12 13 14 4.65 < 10 < 1 0.08 32 0.59 507 < 1 0.222 13 0.112 826

0.3 0.38 < 10 909CMB19663 1.1 < 2 1.86 0.5 15 16 35 5.25 < 10 < 1 0.15 31 0.53 423 4 0.158 15 0.117 815

< 0.2 0.55 < 10 490CMB19664 < 0.5 < 2 1.16 0.5 22 17 47 6.06 < 10 < 1 0.46 26 0.80 490 < 1 0.086 22 0.115 155

< 0.2 0.56 < 10 704CMB19665 0.7 < 2 1.50 0.5 19 16 26 6.03 < 10 < 1 0.38 30 0.83 478 < 1 0.126 21 0.113 1423

< 0.2 0.48 < 10 660CMB19666 1.3 < 2 2.51 1.0 18 18 34 5.96 < 10 < 1 0.15 35 0.58 465 4 0.158 20 0.131 7220


1.3 < 2 2.52 0.7 19 18 31 5.89 < 10 < 1 0.15 35 0.58 467 2 0.152 19 0.131 728

0.2 0.87 < 10 129CMB19668 0.9 < 2 2.37 < 0.5 21 33 49 4.54 < 10 < 1 0.08 25 0.86 403 1 0.264 29 0.120 1148

0.2 1.94 < 10 233CMB19669 < 0.5 < 2 2.78 0.6 30 57 68 4.12 < 10 < 1 0.24 < 10 1.84 486 2 0.448 60 0.088 193

< 0.2 0.42 < 10 562CMB19670 0.9 < 2 2.04 0.6 14 17 59 4.76 < 10 < 1 0.08 32 0.46 422 8 0.167 17 0.119 247

0.2 0.43 < 10 960CMB19671 1.1 < 2 2.54 0.7 12 15 75 4.34 < 10 < 1 0.09 32 0.51 514 10 0.201 12 0.114 348

< 0.2 0.40 < 10 675CMB19672 1.6 < 2 1.96 0.7 16 16 57 5.02 < 10 < 1 0.11 32 0.52 417 16 0.164 16 0.119 496

< 0.2 1.13 < 10 532CMB19673 1.6 < 2 2.50 0.5 22 33 97 4.63 < 10 < 1 0.15 24 1.17 496 15 0.374 30 0.104 367

0.5 0.41 < 10 854CMB19674 1.5 < 2 1.94 0.7 15 16 57 5.62 < 10 < 1 0.13 31 0.54 422 < 1 0.170 18 0.118 875

0.2 0.50 < 10 673CMB19675 0.8 < 2 1.25 0.6 15 15 39 5.09 < 10 < 1 0.16 37 0.69 230 1 0.183 18 0.100 343

0.3 0.36 < 10 795CMB19676 0.8 < 2 2.35 0.6 13 14 35 4.85 < 10 < 1 0.06 28 0.46 421 < 1 0.169 15 0.109 995

0.4 0.38 < 10 1020CMB19677 1.0 < 2 2.55 0.6 13 14 31 5.03 < 10 < 1 0.06 27 0.50 479 < 1 0.203 14 0.111 1193

< 0.2 2.06 < 10 453CMB19678 < 0.5 < 2 1.47 < 0.5 26 78 37 4.14 < 10 < 1 0.70 18 1.33 279 < 1 0.212 44 0.126 < 2< 2


< 0.5 < 2 1.22 < 0.5 10 30 33 2.43 < 10 < 1 0.13 86 0.35 319 5 0.125 49 0.051 168< 2

1.5 0.41 < 10 914CMB19680 0.9 < 2 3.46 0.9 13 15 103 5.31 < 10 < 1 0.07 29 0.47 694 2 0.185 14 0.124 3104

0.8 0.41 < 10 777CMB19681 0.9 < 2 3.57 0.9 11 15 235 5.02 < 10 < 1 0.12 28 0.50 789 < 1 0.170 13 0.121 395

0.7 0.37 < 10 963CMB19682 0.7 < 2 3.25 0.5 9 14 71 4.00 < 10 < 1 0.09 28 0.40 589 < 1 0.168 13 0.125 287

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0.04 2 56 0.25CMB19601 < 10 37 66 < 10 70 43.2 1.000 2.906

0.02 2 33 0.22CMB19602 < 10 22 72 < 10 112 27.6 1.000 2.887

0.03 < 2 26 0.25CMB19603 < 10 166 76 < 10 228 194 1.0009

0.06 < 2 40 0.23CMB19604 < 10 221 107 < 10 50 257 1.0005

0.18 3 37 0.36CMB19605 < 10 < 10 119 < 10 70 2.8 1.00013

0.06 < 2 73 0.24CMB19606 < 10 61 159 < 10 67 70.3 1.0007

0.05 < 2 92 0.21CMB19607 < 10 117 103 < 10 64 132 1.0004

0.04 < 2 115 0.22CMB19608 < 10 78 98 < 10 101 89.5 1.0004

0.04 3 158 0.27CMB19609 < 10 2740 108 < 10 111 2850 1.0005

0.04 < 2 160 0.21CMB19610 < 10 825 90 < 10 77 892 1.0003


< 10 841 92 < 10 78 916 1.0003

0.03 < 2 181 0.24CMB19612 < 10 2590 106 < 10 93 2890 1.0004

0.02 < 2 135 0.23CMB19613 < 10 3820 78 < 10 74 4060 1.0004

0.03 2 157 0.26CMB19614 < 10 2650 169 < 10 98 2820 1.000 2.853

0.05 < 2 208 0.28CMB19615 < 10 2360 248 < 10 102 2650 1.0003

0.08 3 147 0.28CMB19616 < 10 685 220 < 10 182 724 1.0005

0.07 < 2 119 0.20CMB19617 < 10 11 90 < 10 142 10.0 1.000 2.997

0.07 2 138 0.21CMB19618 < 10 65 88 < 10 147 74.6 1.0003

0.12 < 2 167 0.19CMB19619 < 10 < 10 53 < 10 221 7.8 1.0001


< 10 < 10 53 < 10 220 7.8 1.0001

0.13 < 2 127 0.28CMB19621 < 10 528 59 < 10 163 557 1.0003

0.07 < 2 154 0.28CMB19622 < 10 352 93 < 10 126 388 1.0003

0.05 < 2 122 0.23CMB19623 < 10 171 72 < 10 133 198 1.0004

0.05 < 2 135 0.30CMB19624 < 10 477 69 < 10 158 491 1.0004

0.05 2 143 0.27CMB19625 < 10 639 68 < 10 157 650 1.0004

0.03 < 2 44 0.13CMB19626 < 10 < 10 146 < 10 45 1.8 1.0002


< 10 909 60 < 10 115 844 1.0002


0.1 1.000

0.13 3 70 0.36CMB19628 < 10 < 10 73 < 10 313 9.5 1.0002

0.06 < 2 37 0.27CMB19629 < 10 15 69 < 10 247 16.9 1.0004

0.10 3 33 0.29CMB19630 < 10 12 67 < 10 202 15.3 1.000 2.952

0.04 < 2 35 0.29CMB19631 < 10 < 10 68 < 10 219 6.0 1.000 2.913

0.11 < 2 187 0.24CMB19632 < 10 34 58 < 10 144 39.0 1.000 2.942

0.33 2 92 0.23CMB19633 < 10 82 70 < 10 102 90.5 1.000 3.038

0.14 2 194 0.26CMB19634 < 10 835 96 < 10 209 884 1.000 2.934

0.11 < 2 150 0.26CMB19635 < 10 525 85 < 10 178 601 1.0003


< 10 520 84 < 10 178 560 1.0003

0.08 < 2 164 0.22CMB19637 < 10 41 59 < 10 69 45.5 1.0003

0.04 2 225 0.26CMB19638 < 10 2350 221 < 10 120 2530 1.000 2.975

0.05 < 2 176 0.23CMB19639 < 10 377 105 < 10 65 399 1.0004

0.05 < 2 180 0.25CMB19640 < 10 1080 227 < 10 81 1180 1.0004

0.06 < 2 195 0.26CMB19641 < 10 1360 210 < 10 89 1490 1.0004

0.05 < 2 33 0.16CMB19642 < 10 < 10 66 < 10 59 2.6 1.0004


< 10 1020 77 < 10 95 1030 1.0002

0.06 < 2 205 0.24CMB19644 < 10 2990 233 < 10 90 3090 1.0004

0.06 < 2 179 0.23CMB19645 < 10 785 116 < 10 100 847 1.0004


< 10 799 120 < 10 96 860 1.0004

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0.10 < 2 133 0.22CMB19647 < 10 110 78 < 10 126 128 1.0004

0.14 < 2 102 0.20CMB19648 < 10 < 10 54 < 10 61 9.3 1.000 2.984

0.13 < 2 120 0.26CMB19649 < 10 < 10 59 < 10 78 12.7 1.000 2.854

0.05 < 2 43 0.25CMB19652 < 10 < 10 59 < 10 144 5.9 1.000 2.911

0.07 < 2 93 0.30CMB19653 < 10 77 96 < 10 152 89.8 1.000 2.923

0.05 2 83 0.28CMB19654 < 10 73 79 < 10 146 84.0 1.0005

0.05 2 127 0.31CMB19655 < 10 318 168 < 10 115 354 1.0004

0.07 < 2 148 0.27CMB19656 < 10 647 137 < 10 104 690 1.0004


< 10 645 135 < 10 100 690 1.0004

0.12 2 68 0.30CMB19658 < 10 15 59 < 10 132 17.1 1.0003

0.14 < 2 81 0.30CMB19659 < 10 22 68 < 10 170 26.2 1.0003

0.16 < 2 60 0.28CMB19660 < 10 < 10 57 < 10 213 6.9 1.0001

0.12 < 2 92 0.28CMB19661 < 10 11 68 < 10 249 14.2 1.0003

0.06 < 2 126 0.27CMB19662 < 10 275 94 < 10 88 295 1.000 2.914

0.07 < 2 63 0.29CMB19663 < 10 28 69 < 10 86 31.1 1.0004

0.24 3 38 0.28CMB19664 < 10 < 10 63 < 10 116 6.9 1.0002

0.09 2 49 0.28CMB19665 < 10 < 10 67 < 10 105 11.5 1.0004

0.14 < 2 66 0.28CMB19666 < 10 127 90 < 10 107 126 1.0005


< 10 125 91 < 10 106 129 1.0005

0.12 < 2 38 0.29CMB19668 < 10 380 107 < 10 90 388 1.0006

0.18 < 2 21 0.23CMB19669 < 10 < 10 92 < 10 68 3.8 1.00010

0.10 < 2 52 0.28CMB19670 < 10 < 10 60 < 10 90 7.7 1.0004

0.06 < 2 82 0.29CMB19671 < 10 < 10 52 < 10 105 10.3 1.0004

0.12 < 2 63 0.28CMB19672 < 10 11 67 < 10 134 13.5 1.0004

0.21 3 59 0.28CMB19673 < 10 49 87 < 10 102 52.1 1.0007

0.07 < 2 75 0.24CMB19674 < 10 187 93 < 10 167 191 1.0004

0.06 < 2 38 0.23CMB19675 < 10 26 56 < 10 197 33.8 1.0004

0.07 < 2 82 0.22CMB19676 < 10 156 78 < 10 139 176 1.0004

0.09 < 2 102 0.21CMB19677 < 10 250 91 < 10 136 276 1.0005

0.06 < 2 27 0.17CMB19678 < 10 < 10 73 < 10 64 1.0 1.0004


< 10 405 55 < 10 103 409 1.0002

0.08 < 2 136 0.23CMB19680 < 10 694 117 < 10 115 702 1.000 2.874

0.07 < 2 99 0.23CMB19681 < 10 27 70 < 10 91 26.6 1.000 2.885

0.05 < 2 107 0.23CMB19682 < 10 41 57 < 10 63 43.8 1.000 2.874

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Quality Control



26.0 0.35 15 249GXR-1 Meas 0.9 1490 0.85 3.3 8 7 1220 26.0 10 4 0.03 < 10 0.14 805 15 0.059 36 0.044 595400

31.0 3.52 15.0 750GXR-1 Cert 1.22 1380 0.960 3.30 8.20 12.0 1110 23.6 13.8 3.90 0.0500 7.50 0.217 852 18.0 0.0520 41.0 0.0650 730427

DH-1a Meas

DH-1a Cert

DH-1a Meas

DH-1a Cert

3.5 2.58 < 10 23GXR-4 Meas 1.4 27 0.99 0.6 15 58 6640 3.58 10 < 1 1.45 52 1.70 133 340 0.128 41 0.126 43104

4.00 7.20 4.50 1640GXR-4 Cert 1.90 19.0 1.01 0.860 14.6 64.0 6520 3.09 20.0 0.110 4.01 64.5 1.66 155 310 0.564 42.0 0.120 52.098.0

20.8 3.50 24 1100GXR-2 Meas 1.2 < 2 0.85 5.1 11 31 93 2.54 10 4 0.65 25 0.59 1090 < 1 0.223 20 0.066 82013

17.0 16.5 42.0 2240GXR-2 Cert 1.70 0.690 0.930 4.10 8.60 36.0 76.0 1.86 37.0 2.90 1.37 25.6 0.850 1010 2.10 0.556 21.0 0.105 69025.0

0.3 6.64 < 10 886GXR-6 Meas 0.9 < 2 0.17 0.8 14 85 72 6.41 20 < 1 0.96 12 0.41 978 1 0.123 25 0.032 94218

1.30 17.7 9.80 1300GXR-6 Cert 1.40 0.290 0.180 1.00 13.8 96.0 66.0 5.58 35.0 0.0680 1.87 13.9 0.609 1010 2.40 0.104 27.0 0.0350 101330

SY-2 Meas

SY-2 Cert

SY-2 Meas

SY-2 Cert

OREAS 13P Meas 3020 6.18 2420

OREAS 13P Cert 2500 7.58 2260

BL-3 Meas

BL-3 Cert

BL-4a Meas

BL-4a Cert

BL-4a Meas

BL-4a Cert

3.0 0.28 < 10 40CMB19613 Orig 1.5 < 2 2.88 < 0.5 10 5 5 3.06 20 < 1 0.02 58 0.41 566 < 1 0.156 5 0.162 122010

3.3 0.28 < 10 37CMB19613 Dup 1.5 < 2 2.83 < 0.5 9 6 5 3.09 20 < 1 0.02 56 0.40 555 < 1 0.151 4 0.161 12109

0.2 0.37 < 10 741CMB19627 Received as pulp Orig

0.5 < 2 1.22 < 0.5 10 31 29 2.47 < 10 < 1 0.11 92 0.30 316 4 0.129 50 0.046 2842

0.5 0.38 < 10 762CMB19627 Received as pulp Dup

0.5 < 2 1.26 < 0.5 10 34 30 2.54 < 10 < 1 0.11 95 0.31 328 4 0.138 47 0.048 294< 2

0.5 0.92 < 10 578CMB19629 Orig < 0.5 < 2 1.59 0.7 19 34 41 4.68 < 10 < 1 0.50 26 1.03 412 1 0.151 30 0.113 97

0.9 0.92 < 10 598CMB19629 Split < 0.5 < 2 1.61 0.6 19 33 43 4.98 < 10 < 1 0.52 27 1.06 422 < 1 0.148 33 0.117 107

CMB19634 Orig

CMB19634 Dup

0.4 0.41 < 10 659CMB19639 Orig 1.1 < 2 3.96 0.8 11 15 65 4.08 < 10 < 1 0.02 22 0.51 493 < 1 0.243 11 0.122 11719

0.4 0.43 < 10 639CMB19639 Dup 1.0 < 2 3.85 0.7 10 14 68 3.97 < 10 < 1 0.02 22 0.49 483 < 1 0.251 11 0.119 11319

< 0.2 0.38 < 10 701CMB19649 Orig 0.6 < 2 2.07 0.6 17 17 32 5.22 < 10 < 1 0.21 29 0.58 470 < 1 0.141 20 0.117 278

< 0.2 0.40 < 10 735CMB19649 Split 0.6 < 2 2.22 < 0.5 18 17 35 5.43 < 10 < 1 0.22 30 0.61 499 < 1 0.147 21 0.125 269

CMB19649 Split

0.8 0.49 < 10 1340CMB19655 Orig 1.0 < 2 2.39 0.5 14 14 14 4.98 < 10 < 1 0.18 33 0.65 481 1 0.210 14 0.106 1097

0.8 0.51 < 10 1280CMB19655 Dup 1.0 < 2 2.47 0.5 14 14 21 5.07 < 10 < 1 0.19 33 0.66 493 1 0.200 14 0.108 1108

0.3 0.59 < 10 735CMB19661 Orig 0.8 < 2 2.32 0.9 17 15 69 5.46 < 10 < 1 0.41 33 0.88 526 4 0.143 17 0.114 1108

0.3 0.58 < 10 808CMB19661 Split 0.8 < 2 2.30 0.9 17 15 68 5.40 < 10 < 1 0.40 33 0.86 516 2 0.144 19 0.115 1076

< 0.2 2.07 < 10 451CMB19678 Orig < 0.5 < 2 1.47 < 0.5 26 78 37 4.12 < 10 < 1 0.69 17 1.32 279 < 1 0.214 44 0.125 < 2< 2

< 0.2 2.04 < 10 456CMB19678 Dup < 0.5 < 2 1.47 < 0.5 25 79 37 4.16 < 10 < 1 0.71 18 1.34 279 < 1 0.209 43 0.126 < 2< 2

0.7 0.37 < 10 963CMB19682 Orig 0.7 < 2 3.25 0.5 9 14 71 4.00 < 10 < 1 0.09 28 0.40 589 < 1 0.168 13 0.125 287

0.7 0.35 < 10 925CMB19682 Split 0.7 < 2 3.22 0.7 10 14 71 3.82 < 10 < 1 0.08 28 0.39 576 < 1 0.156 11 0.118 255


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.009 < 1 < 0.001 < 2< 2


< 0.5 < 2 < 0.01 < 0.5 < 1 < 1 < 1 < 0.01 < 10 < 1 < 0.01 < 10 < 0.01 < 5 < 1 0.008 < 1 < 0.001 < 2< 2



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Quality Control



0.22 78 191GXR-1 Meas < 10 31 76 194 6331

0.257 122 275GXR-1 Cert 0.390 34.9 80.0 164 7601.58

DH-1a Meas 2640 2600

DH-1a Cert 2630 2630

DH-1a Meas 2640

DH-1a Cert 2630

1.97 3 73GXR-4 Meas < 10 < 10 86 14 707

1.77 4.80 221GXR-4 Cert 3.20 6.20 87.0 30.8 73.07.70

0.04 31 92GXR-2 Meas < 10 < 10 55 < 10 6055

0.0313 49.0 160GXR-2 Cert 1.03 2.90 52.0 1.90 5306.88

0.02 4 33GXR-6 Meas < 10 < 10 175 < 10 12422

0.0160 3.60 35.0GXR-6 Cert 2.20 1.54 186 1.90 11827.6

SY-2 Meas 284

SY-2 Cert 284

SY-2 Meas 283

SY-2 Cert 284

OREAS 13P Meas

OREAS 13P Cert

BL-3 Meas 10100

BL-3 Cert 10200

BL-4a Meas 1250

BL-4a Cert 1250

BL-4a Meas 1280

BL-4a Cert 1250

0.02 < 2 135 0.23CMB19613 Orig < 10 3790 78 < 10 754

0.02 < 2 134 0.24CMB19613 Dup < 10 3840 78 < 10 744

0.09 < 2 77 0.20CMB19627 Received as pulp Orig

< 10 888 59 < 10 1122

0.10 < 2 80 0.20CMB19627 Received as pulp Dup

< 10 930 61 < 10 1182

0.06 < 2 37 0.27CMB19629 Orig < 10 15 69 < 10 247 16.9 1.0004

0.07 < 2 38 0.26CMB19629 Split < 10 16 71 < 10 256 17.2 1.0004

CMB19634 Orig 2.93

CMB19634 Dup 2.92

0.05 < 2 176 0.23CMB19639 Orig < 10 386 105 < 10 664

0.05 < 2 176 0.23CMB19639 Dup < 10 368 104 < 10 644

0.13 < 2 120 0.26CMB19649 Orig < 10 < 10 59 < 10 78 12.7 1.000 2.854

0.14 < 2 128 0.27CMB19649 Split < 10 11 63 < 10 84 12.8 1.000 2.924

CMB19649 Split 2.92

0.05 2 125 0.30CMB19655 Orig < 10 318 164 < 10 1134

0.05 2 129 0.31CMB19655 Dup < 10 318 171 < 10 1174

0.12 < 2 92 0.28CMB19661 Orig < 10 11 68 < 10 249 14.2 1.0003

0.11 < 2 90 0.29CMB19661 Split < 10 12 67 < 10 249 13.5 1.0003

0.06 < 2 26 0.17CMB19678 Orig < 10 < 10 73 < 10 644

0.06 < 2 27 0.17CMB19678 Dup < 10 < 10 74 < 10 644

0.05 < 2 107 0.23CMB19682 Orig < 10 41 57 < 10 63 43.8 1.000 2.874

0.05 2 96 0.24CMB19682 Split < 10 39 55 < 10 64 44.6 1.000 2.854


< 10 < 10 < 1 < 10 < 2< 1


< 10 < 10 < 1 < 10 < 2< 1


< 0.01


< 0.1 1.000

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230



APPENDIX VII

DRILL SECTION LITHOLOGY KEY CODE

Aurora Energy Resources Inc. Suite 600, 140 Water Street TD Place, St. John's, NL A1C 6H6

Litho_Code Litho_DescriptionFI.dk Felsic DykeFI.dk.por Felsic Dyke, PorphyriticFI.gr Granite/GranitoidFI.gr Medium-Grained GraniteFI.por.fp Coarsely Porphyritic Felsic Intrusive (Feldspar Porphyry)II.dk Intermediate DykeMI.dk Mafic Dyke (Undifferentiable)MI.dk.pk Mafic Dyke, Pre-KinematicMI.dk.por Mafic Dyke, PorphyriticMI.dk.psk Mafic Dyke, Post-KinematicMI.dk.sk Mafic Dyke, Syn-KinematicMT-CO.pl Metamorphosed Conglomerate, Polylithic. Former Volcaniclastic Unit (Mt-Fv.Vc)MT-CO.pl.my Metamorphosed Conglomerate, Polylithic, Mylonitic. Former Mt-Fv.Vc.MyMT-FV Felsic MetavolcanicsMT-FV.por Felsic Metavolcanics, PorphyriticMT-FV.por.qz Quartz-Phyric Felsic Meta-VolcanicMT-FV.vc Metamorphosed Felsic VolcaniclasticMT-FV.vc.my Metamorphosed Felsic Volcaniclastic, MyloniticMT-FV.vc.pl Polylithic Felsic Meta-VolcaniclasticMT-IV Metamorphosed Intermediate VolcanicsMT-IV.my Metamorphosed Intermediate Volcanics, MyloniticMT-IV.por.fp Metamorphosed Intermediate Volcanics, Feldspar PorphyriticMT-MI.fgr Metamorphosed Mafic Intrusive, Fine GrainedMT-SA.fgr Arkosic Sandstone, Fine-GrainedOVBD OverburdenQZ.vn Quartz Vein (>0.5 M)

231

232



APPENDIX VIII

DOWNHOLE SAMPLE INFO

Aurora Energy Resources Inc. Suite 600, 140 Water Street TD Place, St. John's, NL A1C 6H6

232

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-085 354.6 355.55 CMB19051 CORE 153.3JL08-085 355.55 357.05 CMB19052 CORE 150.1JL08-085 357.05 358.05 CMB19053 CORE 160.8JL08-085 358.05 359.05 CMB19054 CORE 138.3JL08-085 359.05 360.05 CMB19055 CORE 136.8JL08-085 360.05 360.8 CMB19056 CORE 162.6JL08-085 360.05 360.8 CMB19057 DUP 201.6JL08-085 0 0 CMB19058 blank 186.3JL08-085 0 0 CMB19059 std A 177JL08-085 360.8 361.45 CMB19060 CORE 178.3JL08-085 361.45 362.45 CMB19061 CORE 412.1JL08-085 362.45 363.95 CMB19062 DUPPREP 177.7JL08-085 363.95 365.45 CMB19063 DUPPULP 154JL08-086 123.1 123.8 CMB15401 CORE 127.5JL08-086 123.8 124.5 CMB15402 CORE 186JL08-086 124.5 125 CMB15403 CORE 134.5JL08-086 307.2 308.2 CMB15404 CORE 133.2JL08-086 308.2 309.2 CMB15405 CORE 135.1JL08-086 309.2 309.7 CMB15406 CORE 232.8JL08-086 309.7 310.2 CMB15407 CORE 180.7JL08-086 0 0 CMB15408 std A 146JL08-086 309.7 310.2 CMB15409 DUP 185.4JL08-086 310.2 311.2 CMB15410 DUPPREP 155.1JL08-086 311.2 312.2 CMB15411 DUPPULP 143.8JL08-086 0 0 CMB15412 blank 139.9JL08-088 297 298 CMB15701 CORE NULLJL08-088 298 299 CMB15702 CORE NULLJL08-088 299 300 CMB15703 CORE 350JL08-088 300 301 CMB15704 CORE 350JL08-088 301 302 CMB15705 CORE 400JL08-088 302 303 CMB15706 CORE 168JL08-088 303 304 CMB15707 CORE 500JL08-088 304 305 CMB15708 CORE 250JL08-088 305 306 CMB15709 CORE 300JL08-088 306 307 CMB15710 CORE 200JL08-088 307 308 CMB15711 CORE 200JL08-088 308 309 CMB15712 CORE 200JL08-088 309 310 CMB15713 CORE 430JL08-088 309 310 CMB15714 DUP NULLJL08-088 310 311 CMB15715 CORE 200JL08-088 311 312 CMB15716 CORE 200JL08-088 312 313 CMB15717 CORE 215JL08-088 0 0 CMB15718 blank NULLJL08-088 313 314 CMB15719 CORE 400JL08-088 314 315 CMB15720 CORE 720JL08-088 315 316 CMB15721 CORE 650JL08-088 316 317 CMB15722 CORE 1000JL08-088 317 318 CMB15723 CORE 400JL08-088 318 319 CMB15724 CORE 600JL08-088 319 320 CMB15725 CORE 200JL08-088 320 321 CMB15726 CORE 500JL08-088 321 322 CMB15727 CORE 250JL08-088 322 323 CMB15728 CORE 280JL08-088 323 324 CMB15729 CORE 350JL08-088 324 325 CMB15730 CORE 300JL08-088 326 327 CMB15731 CORE 400

233

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-088 327 328 CMB15732 CORE 1050JL08-088 328 329 CMB15733 CORE 1600JL08-088 0 0 CMB15734 std C NULLJL08-088 329 330 CMB15735 CORE 440JL08-088 329 330 CMB15736 DUPPREP 440JL08-088 330 331 CMB15737 CORE 1000JL08-088 331 332 CMB15738 CORE 500JL08-088 332 333 CMB15739 CORE 1000JL08-088 332 333 CMB15740 DUPPREP 1000JL08-088 333 334 CMB15741 CORE 1000JL08-088 334 335 CMB15742 CORE NULLJL08-088 335 336 CMB15743 CORE NULLJL08-088 395 396 CMB15752 CORE NULLJL08-088 396 397 CMB15753 CORE NULLJL08-088 397 398 CMB15754 CORE NULLJL08-088 398 399 CMB15755 CORE NULLJL08-088 399 399.8 CMB15756 CORE NULLJL08-088 399.8 400.2 CMB15757 CORE NULLJL08-088 400.2 401 CMB15758 CORE NULLJL08-088 401.33 401.76 CMB15760 CORE NULLJL08-088 401.76 402.08 CMB15761 CORE NULLJL08-088 402.08 403.2 CMB15762 CORE NULLJL08-088 403.2 405 CMB15763 CORE NULLJL08-088 405 406 CMB15764 CORE NULLJL08-088 406 407 CMB15765 CORE NULLJL08-088 0 0 CMB15766 blank NULLJL08-088 407 408 CMB15767 CORE NULLJL08-088 408 408.45 CMB15768 CORE NULLJL08-088 408.45 409.85 CMB15769 CORE NULLJL08-088 409.85 411 CMB15770 CORE NULLJL08-088 411 412 CMB15771 CORE NULLJL08-088 412 413 CMB15772 CORE NULLJL08-088 413 414 CMB15773 CORE NULLJL08-088 414 415 CMB15774 CORE NULLJL08-088 415 416 CMB15775 CORE NULLJL08-089 41 42 CMB15119 CORE NULLJL08-089 42 43 CMB15120 CORE NULLJL08-089 0 0 CMB15121 blank NULLJL08-089 43 44 CMB15122 CORE NULLJL08-089 44 45 CMB15123 CORE NULLJL08-089 45 46 CMB15124 CORE NULLJL08-089 0 0 CMB15125 std A NULLJL08-089 45 46 CMB15126 DUPPULP NULLJL08-089 45 46 CMB15127 DUPPREP NULLJL08-089 384 385.3 CMB15128 CORE NULLJL08-089 385.3 385.9 CMB15129 CORE NULLJL08-089 385.9 387 CMB15130 CORE 349JL08-089 387 388 CMB15131 CORE 159JL08-089 388 389 CMB15132 CORE 757JL08-089 389 390 CMB15133 CORE 1646JL08-089 390 391 CMB15134 CORE 144JL08-089 391 392 CMB15135 CORE 110JL08-089 397 398 CMB15136 CORE 172JL08-089 398 399 CMB15137 CORE 205JL08-089 399 400 CMB15138 CORE 326JL08-089 400 401 CMB15139 CORE 335

234

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-089 401 402 CMB15140 CORE 473JL08-089 402 402.92 CMB15141 CORE 146JL08-089 402.92 404 CMB15142 CORE NULLJL08-089 418 419 CMB15143 CORE 230JL08-089 419 420 CMB15144 CORE NULLJL08-089 420 421 CMB15145 CORE 295JL08-089 421 422 CMB15146 CORE 227JL08-089 422 423 CMB15147 CORE 274JL08-089 423 424 CMB15148 CORE 190JL08-089 424 425 CMB15149 CORE 185JL08-089 425 426 CMB15150 CORE 221JL08-089 307 308 CMB15161 CORE NULLJL08-089 308 309 CMB15162 CORE NULLJL08-089 309 310 CMB15163 CORE 234JL08-089 310 311 CMB15164 CORE 294JL08-089 311 312 CMB15165 CORE 580JL08-089 312 313 CMB15166 CORE 600JL08-089 313 314 CMB15167 CORE 400JL08-089 313 314 CMB15168 DUP NULLJL08-089 314 315 CMB15169 CORE 600JL08-089 315 316 CMB15170 CORE 577JL08-089 316 317 CMB15171 CORE 1400JL08-089 0 0 CMB15172 blank NULLJL08-089 317 318 CMB15173 CORE 3100JL08-089 318 319 CMB15174 CORE 1700JL08-089 319 320 CMB15175 CORE 800JL08-089 320 321 CMB15176 CORE 1000JL08-089 321 322 CMB15177 CORE 600JL08-089 322 323 CMB15178 CORE 400JL08-089 323 324 CMB15179 CORE 325JL08-089 324 325 CMB15180 CORE 305JL08-089 325 326 CMB15181 CORE 388JL08-089 326 327 CMB15182 CORE 370JL08-089 327 328 CMB15183 CORE 168JL08-089 328 329 CMB15184 CORE 227JL08-089 329 330 CMB15185 CORE 101JL08-089 0 0 CMB15186 std A NULLJL08-089 330 331 CMB15187 CORE 115JL08-089 330 331 CMB15188 DUPPULP 115JL08-089 348 349 CMB15189 CORE 190JL08-089 349 350 CMB15190 CORE 195JL08-089 350 351 CMB15191 CORE 317JL08-089 351 352 CMB15192 CORE 500JL08-089 352 353 CMB15193 CORE NULLJL08-089 353 354 CMB15194 CORE 647JL08-089 354 355 CMB15195 CORE 888JL08-089 355 356 CMB15196 CORE 1069JL08-089 356 357 CMB15197 CORE 736JL08-089 357 358 CMB15198 CORE 145JL08-089 358 359 CMB15199 CORE 119JL08-089 359 360 CMB15200 CORE NULLJL08-089 426 427 CMB15413 CORE 221JL08-089 427 428 CMB15414 CORE 305JL08-089 0 0 CMB15415 blank NULLJL08-089 428 429 CMB15416 CORE 213JL08-089 429 430 CMB15417 CORE 250

235

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-089 430 431 CMB15418 CORE 212JL08-089 431 432 CMB15419 CORE 157JL08-089 432 433 CMB15420 CORE 156JL08-089 433 434 CMB15421 CORE 300JL08-089 434 435 CMB15422 CORE 180JL08-089 435 436.3 CMB15423 CORE NULLJL08-089 436.3 437 CMB15424 CORE 309JL08-089 437 438.29 CMB15425 CORE 210JL08-089 438.29 439 CMB15426 CORE 220JL08-089 439 440 CMB15427 CORE 319JL08-089 440 441 CMB15428 CORE 294JL08-089 441 442 CMB15429 CORE 308JL08-089 442 443 CMB15430 CORE 290JL08-089 443 444 CMB15431 DUP 369JL08-089 443 444 CMB15432 CORE 369JL08-089 444 445 CMB15433 CORE 386JL08-089 445 446 CMB15434 CORE 260JL08-089 446 447 CMB15435 CORE 945JL08-089 447 448 CMB15436 CORE 600JL08-089 448 449 CMB15437 CORE 2636JL08-089 449 450 CMB15438 CORE 2600JL08-089 450 451 CMB15439 CORE 3000JL08-089 451 452 CMB15440 CORE NULLJL08-089 452 453 CMB15441 CORE 2000JL08-089 453 454 CMB15442 CORE 1000JL08-089 454 455 CMB15443 CORE 330JL08-089 455 456 CMB15444 CORE 160JL08-089 455 456 CMB15445 DUPPULP NULLJL08-089 455 456 CMB15446 DUPPREP NULLJL08-089 456 457 CMB15447 CORE 350JL08-089 457 458 CMB15448 CORE 140JL08-089 0 0 CMB15449 std B NULLJL08-089 0 0 CMB15450 blank NULLJL08-090 285.79 287 CMB15801 CORE 204JL08-090 287 288 CMB15802 CORE 265JL08-090 288 289 CMB15803 CORE 108JL08-090 289 290 CMB15804 CORE 97JL08-090 0 0 CMB15805 std A 126JL08-090 289 290 CMB15806 DUP 97JL08-090 0 0 CMB15807 blank 101JL08-090 358.24 359 CMB15808 CORE 224JL08-090 359 360 CMB15809 CORE 195JL08-090 360 361 CMB15810 CORE 798JL08-090 361 361.87 CMB15811 CORE 1226JL08-090 361.87 362.12 CMB15812 CORE 199JL08-090 362.12 363 CMB15813 CORE 287JL08-090 363 364 CMB15814 CORE 335JL08-090 364 365 CMB15815 CORE 184JL08-090 365 366 CMB15816 CORE 1409JL08-090 366 367 CMB15817 CORE 650JL08-090 367 368 CMB15818 CORE 900JL08-090 368 369 CMB15819 CORE 1054JL08-090 369 370 CMB15820 CORE 945JL08-090 370 371 CMB15821 CORE 371JL08-090 371 372 CMB15822 CORE 389JL08-090 372 373 CMB15823 CORE 199

236

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-090 373 374.1 CMB15824 CORE 337JL08-090 0 0 CMB15825 std A 174JL08-090 373 374.1 CMB15826 DUP 304JL08-090 0 0 CMB15827 blank 146JL08-090 374.1 374.59 CMB15828 CORE 133JL08-090 374.59 376 CMB15829 CORE 482JL08-090 376 377 CMB15830 CORE 80JL08-090 377 378 CMB15831 CORE 361JL08-090 378 379 CMB15832 CORE 651JL08-090 379 380 CMB15833 CORE 519JL08-090 380 381 CMB15834 CORE 418JL08-090 380 381 CMB15835 DUPPREP NULLJL08-090 381 382 CMB15836 CORE 2498JL08-090 382 383 CMB15837 CORE 480JL08-090 382 383 CMB15838 DUPPULP NULLJL08-090 383 384 CMB15839 CORE 270JL08-090 384 385 CMB15840 CORE 258JL08-090 385 386.19 CMB15841 CORE 239JL08-090 386.19 386.55 CMB15842 CORE 220JL08-090 386.55 388 CMB15843 CORE 254JL08-090 388 389 CMB15844 CORE 211JL08-090 389 390 CMB15845 CORE 338JL08-090 390 391 CMB15846 CORE 222JL08-090 460 461 CMB15847 CORE 219JL08-090 0 0 CMB15848 std A 159JL08-090 0 0 CMB15849 blank 173JL08-090 460 461 CMB15850 DUP 202JL08-090 461 462 CMB15851 CORE 216JL08-090 462 463 CMB15852 CORE 284JL08-090 464 465 CMB15853 CORE 220JL08-090 463 464 CMB15855 CORE 213JL08-091 303 304 CMB15744 CORE 166JL08-091 304 305 CMB15745 CORE 135JL08-091 305 305.41 CMB15746 CORE 113JL08-091 305.41 306.06 CMB15747 CORE 124JL08-091 306.06 307 CMB15748 CORE 118JL08-091 307 308 CMB15749 CORE 111JL08-091 308 309 CMB15750 CORE 120JL08-091 280 281 CMB15776 CORE 113JL08-091 281 282 CMB15777 CORE 166JL08-091 282 283 CMB15778 CORE 156JL08-091 283 284 CMB15779 CORE 130JL08-091 284 285 CMB15780 CORE 125JL08-091 285 286 CMB15781 CORE 127JL08-091 286 287 CMB15782 CORE 136JL08-091 286 287 CMB15783 DUP 136JL08-091 0 0 CMB15784 std A 137JL08-091 287 288 CMB15785 CORE 179JL08-091 288 289 CMB15786 CORE 128JL08-091 289 290 CMB15787 CORE 275JL08-091 290 291 CMB15788 CORE 207JL08-091 291 292 CMB15789 CORE 128JL08-091 292 293 CMB15790 CORE 152JL08-091 293 294 CMB15791 CORE 293JL08-091 294 295 CMB15792 CORE 644JL08-091 295 296 CMB15793 CORE 336

237

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-091 296 297 CMB15794 CORE 257JL08-091 297 298 CMB15795 CORE 129JL08-091 298 299 CMB15796 CORE 410JL08-091 299 300 CMB15797 CORE 1020JL08-091 300 301 CMB15798 CORE 661JL08-091 301 302 CMB15799 CORE 1091JL08-091 302 303 CMB15800 CORE 262JL08-091 309 310 CMB15951 CORE 140JL08-091 310 311 CMB15952 CORE 126JL08-091 311 312 CMB15953 CORE 157JL08-091 312 313 CMB15954 CORE 140JL08-091 313 314 CMB15955 CORE 157JL08-091 314 315 CMB15956 CORE 133JL08-091 0 0 CMB15957 blank NULLJL08-091 295 296 CMB15958 DUPPREP 336JL08-091 301 302 CMB15959 DUPPULP 1091JL08-092 468 469 CMB15886 DUPPREP NULLJL08-092 474 475 CMB15887 DUPPULP NULLJL08-092 463 464.5 CMB15901 CORE NULLJL08-092 464.5 465.5 CMB15902 CORE NULLJL08-092 465.5 466.5 CMB15903 CORE NULLJL08-092 466.5 467 CMB15904 CORE NULLJL08-092 467 468 CMB15905 CORE NULLJL08-092 468 469 CMB15906 CORE NULLJL08-092 469 470 CMB15907 CORE NULLJL08-092 470 471 CMB15908 CORE NULLJL08-092 471 472 CMB15909 CORE NULLJL08-092 472 473 CMB15910 CORE NULLJL08-092 473 474 CMB15911 CORE 412JL08-092 474 475 CMB15912 CORE 355JL08-092 475 476 CMB15913 CORE NULLJL08-092 476 477 CMB15914 CORE NULLJL08-092 477 478 CMB15915 CORE NULLJL08-092 478 479 CMB15916 CORE NULLJL08-092 479 480 CMB15917 CORE NULLJL08-092 480 481 CMB15918 CORE NULLJL08-092 480 481 CMB15919 DUP NULLJL08-092 0 0 CMB15920 blank NULLJL08-092 0 0 CMB15921 std A NULLJL08-093 418 419 CMB15854 CORE 156JL08-093 419 420 CMB15856 CORE 165JL08-093 420 420.8 CMB15857 CORE 150JL08-093 420.8 421.55 CMB15858 CORE 231JL08-093 421.55 422.35 CMB15859 CORE 130JL08-093 422.35 423 CMB15860 CORE 137JL08-093 423 424 CMB15861 CORE 151JL08-093 424 425 CMB15862 CORE 147JL08-093 425 426 CMB15863 CORE 131JL08-093 426 427 CMB15864 CORE 144JL08-093 427 428 CMB15865 CORE 184JL08-093 428 429 CMB15866 CORE 214JL08-093 429 430 CMB15867 CORE 243JL08-093 430 431 CMB15868 CORE 188JL08-093 431 432 CMB15869 CORE 181JL08-093 432 433 CMB15870 CORE 137JL08-093 433 434 CMB15871 CORE 135

238

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-093 434 435 CMB15872 CORE 135JL08-093 435 436 CMB15873 CORE 377JL08-093 436 437 CMB15874 CORE 248JL08-093 437 438 CMB15875 CORE 147JL08-093 437 438 CMB15876 DUP 114JL08-093 0 0 CMB15877 std B 164JL08-093 0 0 CMB15878 blank 128JL08-093 438 439 CMB15879 CORE 131JL08-093 439 440.2 CMB15880 CORE 207JL08-093 440.2 441.25 CMB15881 CORE 563JL08-093 441.25 442 CMB15882 CORE 162JL08-093 442 443 CMB15883 CORE 169JL08-093 443 444 CMB15884 CORE 123JL08-093 444 445 CMB15885 CORE 131JL08-093 420.8 421.55 CMB15888 DUPPREP NULLJL08-093 435 436 CMB15889 DUPPULP NULLJL08-094 213 214 CMB15922 CORE NULLJL08-094 214 215 CMB15923 CORE NULLJL08-094 215 216 CMB15924 CORE NULLJL08-094 216 217 CMB15925 CORE NULLJL08-094 217 218 CMB15926 CORE NULLJL08-094 218 219 CMB15927 CORE NULLJL08-094 219 220 CMB15928 CORE NULLJL08-094 220 221 CMB15929 CORE NULLJL08-094 221 222 CMB15930 CORE NULLJL08-094 222 223 CMB15931 DUPPULP NULLJL08-094 223 224 CMB15932 DUPPREP NULLJL08-094 224 225 CMB15933 CORE NULLJL08-094 225 225.5 CMB15934 CORE NULLJL08-094 225.5 226.15 CMB15935 CORE NULLJL08-094 226.15 227 CMB15936 CORE NULLJL08-094 227 228 CMB15937 CORE NULLJL08-094 228 229 CMB15938 CORE NULLJL08-094 229 230 CMB15939 CORE NULLJL08-094 230 231 CMB15940 DUPPULP NULLJL08-094 231 232 CMB15941 CORE NULLJL08-094 232 233 CMB15942 CORE NULLJL08-094 232 233 CMB15943 DUP NULLJL08-094 0 0 CMB15944 std E NULLJL08-094 0 0 CMB15945 blank NULLJL08-094 233 234 CMB15946 CORE NULLJL08-094 234 234.5 CMB15947 CORE NULLJL08-094 234.5 235 CMB15948 CORE NULLJL08-094 235 236 CMB15949 CORE NULLJL08-094 236 237 CMB15950 CORE NULLJL08-094 237 238 CMB19101 CORE NULLJL08-094 238 239 CMB19102 CORE NULLJL08-094 239 239.65 CMB19103 CORE NULLJL08-094 239.65 241.45 CMB19104 CORE NULLJL08-094 241.45 242 CMB19105 CORE NULLJL08-094 263 264 CMB19106 CORE NULLJL08-094 264 265 CMB19107 CORE NULLJL08-094 265 266.1 CMB19108 CORE NULLJL08-094 266.1 267 CMB19109 CORE NULLJL08-094 267 268 CMB19110 CORE NULLJL08-094 268 269 CMB19111 CORE NULL

239

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-094 269 270 CMB19112 CORE NULLJL08-094 270 271 CMB19113 DUPPREP NULLJL08-094 271 271.9 CMB19114 CORE NULLJL08-094 271.9 272.5 CMB19115 DUPPULP NULLJL08-094 272.5 273.4 CMB19116 CORE NULLJL08-094 273.4 274 CMB19117 CORE NULLJL08-094 273.4 274 CMB19118 DUP NULLJL08-094 0 0 CMB19119 std D NULLJL08-094 0 0 CMB19120 blank NULLJL08-094 274 275.2 CMB19121 CORE NULLJL08-094 275.2 275.8 CMB19122 CORE NULLJL08-094 275.8 277 CMB19123 CORE NULLJL08-094 277 278 CMB19124 CORE NULLJL08-094 278 279 CMB19125 CORE NULLJL08-094 279 280 CMB19126 CORE NULLJL08-094 242 243 CMB19127 CORE NULLJL08-094 243 244 CMB19128 CORE NULLJL08-094 244 245 CMB19129 CORE NULLJL08-094 245 246 CMB19130 CORE NULLJL08-094 334.53 336.03 CMB19131 CORE NULLJL08-094 336.03 337.53 CMB19132 CORE NULLJL08-094 337.53 338.53 CMB19133 CORE NULLJL08-094 338.53 339.53 CMB19134 CORE NULLJL08-094 339.53 341.03 CMB19135 CORE NULLJL08-094 353.69 355.19 CMB19136 CORE NULLJL08-094 355.19 356.69 CMB19137 CORE NULLJL08-094 356.69 357.69 CMB19138 CORE NULLJL08-094 357.69 358.69 CMB19139 CORE NULLJL08-094 358.69 359.39 CMB19140 CORE NULLJL08-094 359.39 359.69 CMB19141 CORE NULLJL08-094 359.39 359.69 CMB19142 DUP NULLJL08-094 0 0 CMB19143 std B NULLJL08-094 0 0 CMB19144 blank NULLJL08-094 359.69 361.19 CMB19145 CORE NULLJL08-094 361.19 362.69 CMB19146 CORE NULLJL08-094 270 271 CMB19147 DUPPREP NULLJL08-094 271.9 272.5 CMB19148 DUPPULP NULLJL08-095 364.53 366 CMB19151 CORE 250JL08-095 366 367.5 CMB19152 CORE 221JL08-095 367.5 368.5 CMB19153 CORE 309JL08-095 368.5 369.49 CMB19154 CORE 187JL08-095 369.49 370.97 CMB19155 CORE 245JL08-095 370.97 372.48 CMB19156 CORE 260JL08-095 372.48 373.48 CMB19157 CORE 515JL08-095 372.48 373.48 CMB19158 DUP 493JL08-095 0 0 CMB19159 std A 262JL08-095 0 0 CMB19160 blank 100JL08-095 373.48 374.48 CMB19161 CORE 563JL08-095 374.48 375.47 CMB19162 CORE 344JL08-095 375.47 376.46 CMB19163 CORE 263JL08-095 376.46 378.45 CMB19164 CORE 219JL08-095 378.45 379.45 CMB19165 CORE 230JL08-095 379.45 380.45 CMB19166 CORE 234JL08-095 448.92 450.5 CMB19167 CORE 196JL08-095 450.5 452 CMB19168 CORE 215JL08-095 452 453 CMB19169 CORE 346

240

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-095 452 453 CMB19170 DUP 286JL08-095 0 0 CMB19171 std A 250JL08-095 0 0 CMB19172 blank 100JL08-095 453 454.52 CMB19173 CORE 220JL08-095 454.52 456 CMB19174 CORE 189JL08-095 456 456.99 CMB19175 CORE 180JL08-095 456.99 457.99 CMB19176 CORE 182JL08-095 456.99 457.99 CMB19177 DUPPREP NULLJL08-095 454.52 456 CMB19178 DUPPULP NULLJL08-096 569.94 570.94 CMB19351 CORE NULLJL08-096 570.94 571.94 CMB19352 CORE NULLJL08-096 571.94 572.94 CMB19353 CORE NULLJL08-096 572.94 573.94 CMB19354 CORE NULLJL08-096 573.94 574.86 CMB19355 CORE NULLJL08-096 574.86 575.7 CMB19356 CORE NULLJL08-096 574.86 575.7 CMB19357 DUPPREP NULLJL08-096 575.7 576.7 CMB19358 CORE NULLJL08-096 575.7 576.7 CMB19359 DUPPULP NULLJL08-096 576.7 577.7 CMB19360 CORE NULLJL08-096 577.7 578.7 CMB19361 CORE NULLJL08-096 578.7 579.7 CMB19362 CORE NULLJL08-096 578.7 579.7 CMB19363 DUP NULLJL08-096 0 0 CMB19364 blank NULLJL08-096 0 0 CMB19365 std B NULLJL08-096 579.7 580.7 CMB19366 CORE NULLJL08-096 580.7 581.7 CMB19367 CORE NULLJL08-096 591.51 592.51 CMB19368 CORE NULLJL08-096 592.51 593.51 CMB19369 CORE NULLJL08-096 593.51 594.51 CMB19370 CORE NULLJL08-096 594.51 595.51 CMB19371 CORE NULLJL08-096 594.51 595.51 CMB19372 DUPPREP NULLJL08-096 595.51 596.51 CMB19373 CORE NULLJL08-096 595.51 596.51 CMB19374 DUPPULP NULLJL08-096 596.51 597.51 CMB19375 CORE NULLJL08-096 597.51 598.51 CMB19376 CORE NULLJL08-096 0 0 CMB19377 blank NULLJL08-096 597.51 598.51 CMB19378 DUP NULLJL08-096 0 0 CMB19379 std B NULLJL08-096 598.51 599.51 CMB19380 CORE NULLJL08-096 599.51 600.51 CMB19381 CORE NULLJL08-096 600.51 601.51 CMB19382 CORE NULLJL08-096 601.51 602.51 CMB19383 CORE NULLJL08-096 602.51 603.51 CMB19384 CORE NULLJL08-096 603.51 604.51 CMB19385 CORE NULLJL08-096 604.51 605.51 CMB19386 CORE NULLJL08-096 605.51 606.51 CMB19387 CORE NULLJL08-096 606.51 607.51 CMB19388 CORE NULLJL08-096 607.51 608.51 CMB19389 CORE NULLJL08-096 608.51 609.51 CMB19390 CORE NULLJL08-097 192.01 193.01 CMB19201 CORE 196JL08-097 193.01 193.9 CMB19202 CORE 202JL08-097 193.9 194.9 CMB19203 CORE 193JL08-097 194.9 195.9 CMB19204 CORE 185JL08-097 195.9 196.94 CMB19205 CORE 196JL08-097 196.94 197.94 CMB19206 CORE 477JL08-097 197.94 198.94 CMB19207 CORE 247

241

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-097 198.94 199.95 CMB19208 CORE 193JL08-097 199.95 200.96 CMB19209 CORE 210JL08-097 200.96 201.96 CMB19210 CORE 271JL08-097 201.96 203.07 CMB19211 CORE 1763JL08-097 201.96 203.07 CMB19212 DUPPREP NULLJL08-097 203.07 204.04 CMB19213 CORE 216JL08-097 204.04 205.03 CMB19214 CORE 476JL08-097 205.03 206.05 CMB19215 CORE 360JL08-097 206.05 207.04 CMB19216 CORE 238JL08-097 207.04 208.02 CMB19217 CORE 3345JL08-097 207.04 208.02 CMB19218 DUPPULP NULLJL08-097 208.02 209.09 CMB19219 CORE 775JL08-097 209.09 210.1 CMB19220 CORE 940JL08-097 210.1 211.08 CMB19221 CORE 1657JL08-097 211.08 212.12 CMB19222 CORE 2382JL08-097 212.12 213.12 CMB19251 CORE 1317JL08-097 213.12 214.09 CMB19252 CORE 1442JL08-097 213.12 214.09 CMB19253 DUP 544JL08-097 0 0 CMB19254 blank NULLJL08-097 0 0 CMB19255 std C 1178JL08-097 214.09 215.13 CMB19256 CORE 1156JL08-097 215.13 216.13 CMB19257 CORE 942JL08-097 216.13 217.12 CMB19258 CORE 1886JL08-097 217.12 217.92 CMB19259 CORE 971JL08-097 217.92 218.63 CMB19260 CORE 508JL08-097 218.63 219.6 CMB19261 CORE 1506JL08-097 219.6 221.12 CMB19262 CORE 234JL08-097 221.12 222.12 CMB19263 CORE 188JL08-097 222.12 223.13 CMB19264 CORE 213JL08-097 223.13 224.16 CMB19265 CORE 183JL08-097 224.16 225.16 CMB19266 CORE 1070JL08-097 225.16 226.14 CMB19267 CORE 1062JL08-097 226.14 227.08 CMB19268 CORE 787JL08-097 227.08 228.08 CMB19269 CORE 432JL08-097 228.08 229.09 CMB19270 CORE 330JL08-097 229.09 230.09 CMB19271 CORE 208JL08-097 230.09 231.04 CMB19272 CORE 193JL08-097 231.04 232.03 CMB19273 CORE 191JL08-097 232.03 233.26 CMB19274 CORE 189JL08-097 233.26 234.28 CMB19275 CORE 178JL08-097 234.28 235.29 CMB19276 CORE 1014JL08-097 235.29 236.29 CMB19277 CORE 1357JL08-097 236.29 237.29 CMB19278 CORE 978JL08-097 236.29 237.29 CMB19279 DUP 883JL08-097 0 0 CMB19280 blank 90JL08-097 0 0 CMB19281 std C NULLJL08-097 237.29 238.32 CMB19282 CORE 212JL08-097 238.32 239.33 CMB19283 CORE 213JL08-097 239.33 240.33 CMB19284 CORE 207JL08-097 240.33 241.33 CMB19285 CORE 467JL08-097 241.33 242.33 CMB19286 CORE 320JL08-097 242.33 243.33 CMB19287 CORE 601JL08-097 243.33 244.31 CMB19288 CORE 230JL08-097 244.31 245.45 CMB19289 CORE 186JL08-097 245.45 246.45 CMB19290 CORE 224JL08-097 246.45 247.45 CMB19291 CORE 221

242

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-097 247.45 248.46 CMB19292 CORE 195JL08-097 248.46 249.46 CMB19293 CORE 178JL08-097 249.46 250.47 CMB19294 CORE 193JL08-097 250.47 251.5 CMB19295 CORE 220JL08-097 251.5 252.49 CMB19296 CORE 220JL08-097 252.49 253.52 CMB19297 CORE 268JL08-097 253.52 254.52 CMB19298 CORE 167JL08-097 254.52 255.53 CMB19299 CORE 237JL08-097 255.53 256.54 CMB19300 CORE 180JL08-097 256.54 257.58 CMB19301 CORE 161JL08-097 257.58 258.59 CMB19302 CORE 238JL08-097 258.59 259.56 CMB19303 CORE 364JL08-097 259.56 260.63 CMB19304 CORE 275JL08-097 260.63 261.63 CMB19305 CORE 159JL08-097 278.44 279.44 CMB19306 CORE 225JL08-097 279.44 280.44 CMB19307 CORE 216JL08-097 280.44 281.44 CMB19308 CORE 305JL08-097 281.44 282.44 CMB19309 CORE 466JL08-097 282.44 283.45 CMB19310 CORE 1283JL08-097 282.44 283.45 CMB19311 DUP 1033JL08-097 0 0 CMB19312 blank 90JL08-097 0 0 CMB19313 std B 281JL08-097 283.45 284.45 CMB19314 CORE 1290JL08-097 283.45 284.45 CMB19315 DUPPREP NULLJL08-097 284.45 285 CMB19316 CORE 320JL08-097 285 286 CMB19317 CORE 1457JL08-097 286 287 CMB19318 CORE 1199JL08-097 287 288 CMB19319 CORE 496JL08-097 288 289 CMB19320 CORE 332JL08-097 289 290 CMB19321 CORE 472JL08-097 290 291 CMB19322 CORE 639JL08-097 291 292 CMB19323 CORE 529JL08-097 292 293 CMB19324 CORE 488JL08-097 293 294 CMB19325 CORE 467JL08-097 294 295 CMB19326 CORE 220JL08-097 295 296 CMB19327 CORE 547JL08-097 296 297 CMB19328 CORE 247JL08-097 297 298 CMB19329 CORE 596JL08-097 298 299 CMB19330 CORE 243JL08-097 299 300.15 CMB19331 CORE 307JL08-097 300.15 301.58 CMB19332 CORE 150JL08-097 301.58 302.58 CMB19333 CORE 281JL08-097 302.58 303.58 CMB19334 CORE 222JL08-097 303.58 304.58 CMB19335 CORE 314JL08-097 303.58 304.58 CMB19336 DUPPULP NULLJL08-097 304.58 305.58 CMB19337 CORE 319JL08-097 305.58 306.58 CMB19338 CORE 150JL08-098 74.09 75.06 CMB19179 CORE 130JL08-098 75.06 76 CMB19180 CORE 182JL08-098 76 76.92 CMB19181 CORE 130JL08-098 76.92 77.89 CMB19182 CORE 352JL08-098 77.89 78.89 CMB19183 CORE 415JL08-098 77.89 78.89 CMB19184 DUP 420JL08-098 0 0 CMB19185 blank 133JL08-098 0 0 CMB19186 std A 181JL08-098 78.89 79.89 CMB19187 CORE 184

243

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-098 78.89 79.89 CMB19188 DUPPREP NULLJL08-098 79.89 81.06 CMB19189 CORE 159JL08-098 79.89 81.06 CMB19190 DUPPULP NULLJL08-098 81.06 81.97 CMB19191 CORE 149JL08-098 81.97 82.96 CMB19192 CORE 158JL08-098 241.6 242.63 CMB19193 CORE 113JL08-098 242.63 243.6 CMB19194 CORE 136JL08-098 243.6 244.55 CMB19195 CORE 136JL08-098 244.55 245.51 CMB19196 CORE 185JL08-098 244.55 245.51 CMB19197 DUP 161JL08-098 0 0 CMB19198 blank 106JL08-098 0 0 CMB19199 std A 151JL08-098 245.51 246.57 CMB19200 CORE 123JL08-098 297.63 298.64 CMB19401 CORE 274JL08-098 298.64 299.64 CMB19402 CORE 461JL08-098 299.64 300.67 CMB19403 CORE 287JL08-098 299.64 300.67 CMB19404 DUP 379JL08-098 0 0 CMB19405 blank 161JL08-098 0 0 CMB19406 std B 199JL08-098 300.67 301.68 CMB19407 CORE 154JL08-098 301.68 302.69 CMB19408 CORE 217JL08-098 302.69 303.69 CMB19409 CORE 283JL08-098 303.69 304.66 CMB19410 CORE 146JL08-098 304.66 305.63 CMB19411 CORE 153JL08-098 304.66 305.63 CMB19412 DUPPREP NULLJL08-098 305.63 306.63 CMB19413 CORE 140JL08-098 306.63 307.63 CMB19414 CORE 205JL08-098 307.63 308.63 CMB19415 CORE 144JL08-098 308.63 309.63 CMB19416 CORE 205JL08-098 309.63 310.63 CMB19417 CORE 280JL08-098 310.63 311.63 CMB19418 CORE 201JL08-098 311.63 312.63 CMB19419 CORE 200JL08-098 312.63 313.63 CMB19420 CORE 163JL08-098 313.63 314.63 CMB19421 CORE 186JL08-098 314.63 315.63 CMB19422 CORE 187JL08-098 339 340 CMB19423 CORE 167JL08-098 340 341 CMB19424 CORE 190JL08-098 341 342 CMB19425 CORE 192JL08-098 342 343 CMB19426 CORE 1223JL08-098 342 343 CMB19427 DUP 563JL08-098 0 0 CMB19428 blank 134JL08-098 0 0 CMB19429 std B 188JL08-098 343 344 CMB19430 CORE 130JL08-098 344 345 CMB19431 CORE 134JL08-098 345 346 CMB19432 CORE 184JL08-098 345 346 CMB19433 DUPPREP NULLJL08-098 346 347 CMB19434 CORE 186JL08-098 347 348 CMB19435 CORE 206JL08-098 348 349 CMB19436 CORE 174JL08-098 349 350 CMB19437 CORE 342JL08-098 349 350 CMB19438 DUPPULP NULLJL08-098 350 351 CMB19439 CORE 305JL08-098 351 352 CMB19440 CORE 187JL08-098 352 353 CMB19441 CORE 191JL08-098 397 398 CMB19442 CORE 192JL08-098 398 399 CMB19443 CORE 169

244

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-098 399 400 CMB19444 CORE 318JL08-098 400 401 CMB19445 CORE 179JL08-098 401 402 CMB19446 CORE 221JL08-098 246.57 247.61 CMB19451 CORE 146JL08-098 246.57 247.61 CMB19452 DUPPREP NULLJL08-098 247.61 248.62 CMB19453 CORE 142JL08-098 247.61 248.62 CMB19454 DUPPULP NULLJL08-098 248.62 249.63 CMB19455 CORE 140JL08-098 249.63 250.63 CMB19456 CORE 142JL08-099 221 222 CMB19601 CORE 162JL08-099 222 223.41 CMB19602 CORE 170JL08-099 223.41 224.41 CMB19603 CORE 645JL08-099 224.41 225.41 CMB19604 CORE 355JL08-099 225.41 226.56 CMB19605 CORE 142JL08-099 226.56 228 CMB19606 CORE 222JL08-099 228 229 CMB19607 CORE 284JL08-099 229 230 CMB19608 CORE 227JL08-099 230 231 CMB19609 CORE 4271JL08-099 231 232 CMB19610 CORE 1078JL08-099 231 232 CMB19611 DUPPULP NULLJL08-099 232 233 CMB19612 CORE 2789JL08-099 233 234 CMB19613 CORE 3986JL08-099 234 235 CMB19614 CORE 3232JL08-099 235 236 CMB19615 CORE 2933JL08-099 236 237 CMB19616 CORE 780JL08-099 237 238 CMB19617 CORE 139JL08-099 238 239 CMB19618 CORE 290JL08-099 239 240 CMB19619 CORE 158JL08-099 239 240 CMB19620 DUPPREP NULLJL08-099 241 242 CMB19621 CORE 644JL08-099 242 243 CMB19622 CORE 578JL08-099 243 244 CMB19623 CORE 356JL08-099 244 245 CMB19624 CORE 518JL08-099 244 245 CMB19625 DUP 614JL08-099 0 0 CMB19627 std B 216JL08-099 245 246 CMB19628 CORE 199JL08-099 246 247 CMB19629 CORE 190JL08-099 247 248 CMB19630 CORE 152JL08-099 248 249 CMB19631 CORE 159JL08-099 266 267 CMB19632 CORE 201JL08-099 267 268 CMB19633 CORE 231JL08-099 268 269 CMB19634 CORE 1042JL08-099 269 270 CMB19635 CORE 868JL08-099 269 270 CMB19636 DUPPULP NULLJL08-099 270 271 CMB19637 CORE 184JL08-099 271 272 CMB19638 CORE 5081JL08-099 272 273 CMB19639 CORE 547JL08-099 273 274 CMB19640 CORE 1216JL08-099 273 274 CMB19641 DUP 891JL08-099 0 0 CMB19642 blank 145JL08-099 0 0 CMB19643 std B 188JL08-099 274 275 CMB19644 CORE 4680JL08-099 275 276 CMB19645 CORE 1222JL08-099 275 276 CMB19646 DUPPREP NULLJL08-099 276 277 CMB19647 CORE 267JL08-099 277 278 CMB19648 CORE 144

245

hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-099 278 279 CMB19649 CORE 149JL08-099 240 241 CMB19650 CORE 177JL08-099 319 320 CMB19652 CORE 161JL08-099 320 321 CMB19653 CORE 198JL08-099 321 322 CMB19654 CORE 183JL08-099 322 323 CMB19655 CORE 516JL08-099 323 324 CMB19656 CORE 944JL08-099 323 324 CMB19657 DUPPULP NULLJL08-099 324 325 CMB19658 CORE 150JL08-099 325 326 CMB19659 CORE 164JL08-099 326 327 CMB19660 CORE 140JL08-099 327 328 CMB19661 CORE 159JL08-099 328 329 CMB19662 CORE 379JL08-099 329 330 CMB19663 CORE 175JL08-099 330 331 CMB19664 CORE 140JL08-099 331 332 CMB19665 CORE 159JL08-099 332 333 CMB19666 CORE 259JL08-099 332 333 CMB19667 DUPPREP NULLJL08-099 333 334 CMB19668 CORE 416JL08-099 334 335 CMB19669 CORE 149JL08-099 335 336 CMB19670 CORE 164JL08-099 336 337 CMB19671 CORE 134JL08-099 337 338 CMB19672 CORE 155JL08-099 338 339 CMB19673 CORE 176JL08-099 339 340 CMB19674 CORE 356JL08-099 340 341 CMB19675 CORE 171JL08-099 341 342 CMB19676 CORE 291JL08-099 341 342 CMB19677 DUP 261JL08-099 0 0 CMB19678 blank 134JL08-099 0 0 CMB19679 std A 170JL08-099 342 343 CMB19680 CORE 883JL08-099 343 344 CMB19681 CORE 140JL08-099 344 345 CMB19682 CORE 150JL08-099 345 346 CMB19683 CORE 149JL08-100 44.05 45.15 CMB19391 CORE 149JL08-100 45.15 46.35 CMB19392 CORE 170JL08-100 46.35 46.8 CMB19393 CORE 299JL08-100 46.8 48 CMB19394 CORE 158JL08-100 48 49 CMB19395 CORE 222JL08-100 49 49.75 CMB19396 CORE 637JL08-100 49.75 50.5 CMB19397 CORE 228JL08-100 50.5 51.2 CMB19398 CORE 161JL08-100 51.2 52.15 CMB19399 CORE 143JL08-100 52.15 53 CMB19400 CORE 600JL08-100 53 54 CMB19551 CORE 481JL08-100 54 54.7 CMB19552 CORE 1302JL08-100 54.7 55.7 CMB19553 CORE 347JL08-100 55.7 57 CMB19554 CORE 486JL08-100 57 58 CMB19555 CORE 549JL08-100 58 59 CMB19556 CORE 743JL08-100 59 60.5 CMB19557 CORE 220JL08-100 60.5 61.5 CMB19558 CORE 1120JL08-100 61.5 63 CMB19559 CORE 253JL08-100 63 64 CMB19560 CORE 177JL08-100 112 113 CMB19561 CORE 194JL08-100 113 114 CMB19562 CORE 214

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hole_id mfrom mto sampleid Sample_Type Scint_CpsJL08-100 114 115 CMB19563 CORE 310JL08-100 114 115 CMB19564 DUP 304JL08-100 0 0 CMB19565 blank 167JL08-100 0 0 CMB19566 std A 205JL08-100 115 116 CMB19567 CORE 342JL08-100 116 117 CMB19568 CORE 801JL08-100 117 118 CMB19569 CORE 234JL08-100 118 119 CMB19570 CORE 512JL08-100 119 120 CMB19571 CORE 318JL08-100 120 121.17 CMB19572 CORE 312JL08-100 121.17 122 CMB19573 CORE 204JL08-100 122 123 CMB19574 CORE 184JL08-100 146 147 CMB19575 CORE 164JL08-100 147 148 CMB19576 CORE 140JL08-100 148 149 CMB19577 CORE 278JL08-100 149 150 CMB19578 CORE 183JL08-100 148 149 CMB19579 DUPPREP NULLJL08-100 149 150 CMB19580 DUPPULP NULLJL08-100 102 103 CMB19581 CORE 177JL08-100 103 104 CMB19582 CORE 164JL08-100 104 105 CMB19583 CORE 183JL08-100 105 106 CMB19584 CORE 2442JL08-100 106 107 CMB19585 CORE 621JL08-100 107 108 CMB19586 CORE 196JL08-100 187 188 CMB19587 CORE 161JL08-100 188 189 CMB19588 CORE 234JL08-100 189 190 CMB19589 CORE 1980JL08-100 190 191 CMB19590 CORE 545JL08-100 191 192 CMB19591 CORE 645JL08-100 192 193 CMB19592 CORE 461JL08-100 192 193 CMB19593 DUP 119JL08-100 0 0 CMB19594 blank 146JL08-100 0 0 CMB19595 std A 356JL08-100 193 194 CMB19596 CORE 173JL08-100 194 195 CMB19597 CORE 137JL08-100 150 151 CMB19651 CORE 217

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