52C15SE0014 Olive Mine

117
r i r r r r r r r r r r r r r n n 52C15SE8ei4 63.5103 LITTLE TURTLE LAKE 010 i - NORONT RESOURCES LTD. ECONOMIC AND GEOLOGICAL EVALUATION OF OLIVE GOLD MINE: DEWATERING AND SAMPLING PROGRAM : JAN. - March 1987 Eduard Ludwig H.BSc. Tech. Consulting Geologist n r

Transcript of 52C15SE0014 Olive Mine

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52C15SE8ei4 63.5103 LITTLE TURTLE LAKE 010

i -

NORONT RESOURCES LTD.

ECONOMIC AND GEOLOGICAL EVALUATION OF

OLIVE GOLD MINE: DEWATERING AND

SAMPLING PROGRAM : JAN. - March 1987

Eduard Ludwig H.BSc. Tech. Consulting Geologist

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rSUMMARY

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The Olive-Preston gold property is comprised of seven leased mining*.

claims located in the Mine Center - Bad Vermillion area, District of

Rainy River.

l. Mine Center, Ontario, has a history of gold production from the early

p 1900's, in which gold was mined from narrow quartz-carbonate veins

hosted by quartz porphry intrusions. The area has seen repeated

P attention through the years but never leading to production on any

sizable or economic scale.

^ Gold on the Olive-Preston property is associated with a narrow,

P quartz-carbonate vein system conformable to a hosting band of

intermediate tuffs. The vein pinches to 0.5" and swells to a width

[ of 5.0' (quartz blow outs) but averages 7.5" throughout the mine

workings. On surface the vein system has been traced for a strike

length of 2,200 feet and down dip only the extent of the underground

T workings (250 feet).

Dewatering was completed to determine the dimensions and grade ofri any ore shoots, through channel sampling, surveying and geological

p mapping. Many low grade ore shoots were discovered on all three

levels along with two economic sections, described as follows:

T (i) First Level: 4040 East to 3900 East, 125 feet long, 3 feet

wide grading 0.30 ounce of gold per ton.

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rr rP (ii) Third Level: 3940 East to 3890 East, 50 feet long, 3 feet widel V

grading 1.46 ounces of gold per ton.

rA program of deep drilling beneath the Olive Mine workings and

l- - along strike of the main strucure is recommended, totalling 8,000

p feet at an estimated cost of $200,000.00i

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TABLE'OF'i 52C15SE0814 63.5183 LITTLE TURTLE LAKE 010Cr '-

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Summary

Section

1.0 Introduction

2.0 Property Description, Location, Accessibility

3.0 Topography

4.0 Exploration and Development History

5.0 Geology

5.1 Regional Geology5.2 Property Geology

6.0 Sampling of the Olive Mine Workings

6.1 Sampling Methods6.2 Sampling Results

7.0 Economic Significance

8.0 Recommendations and Conclusions

References

Certificate of Qualifications

Appendix A: Assays

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Page

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6

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811

12

1212

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cLIST OF FIGURES

Figure

1 Location Map

2 Claim Sketch

3 Regional Geology

LIST OF TABLES

Table 1 Table of Formations

LIST OF MAPS

Map

1 First Level Plan

2 Second Level Plan

3 Third Level Plan

4 Longitudinal Projection

Page

3

10

In Map Pocket

In Map Pocket

In Map Pocket

In Map Pocket

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1.0 INTRODUCTION ):

Noront Resources Ltd. commissioned E. Ludwig and Associates to

manage the 1987 dewatering program of the Olive Mine workings.

This included channel sampling, geological mapping and compilation

of results along with recommendations pertaining to further exploration

work.r1 Material used in this report was obtained from government reports

P and documents stored in the assessment files in the office of the

resident geologist in Kenora and reports supplied by Homestake

[ Explorations Ltd. Data presented on maps is based on observations

P made underground while geological mapping and channel sampling.

' The author is familiar with the property through examinations made

P in 1983 while completing an under graduate thesis on the surface

geology of the property. In 1986 the author performed a

[ metallurgical test on the vein material, where 30 tons of material

P were removed grading 2.75 ounces per ton

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2.0 PROPERTY DESCRIPTION, LOCATION AND ACCESSIBILITY

Location of the property is 35 miles east of Fort Francis, Ontario, in

the Mine Center area, (NTS Reference: 52C/10, 48045'N, 92 040'W), with

highway 11 providing good access to the southern portion of the property

(Fig. 1). The main Olive shaft is located towards the northwest

boundary and is accessible by gravel road, 2.5 miles north of highway

11.

Two electrical power lines, and the main CP railway line traverse the

property in an east-west direction.

The seven claim group, which was the focal point of the 1987 work, are

all currently under 21-year lease arrangements with the Province Of

Ontario, and are recorded in the name of HSK Minerals Limited (Fig. 2).

Claim List: Claim

K-475146

K-475190

K-475191

K-475192

K-475193

K-475269

Status

Leased August 1986

Leased August 1986

Leased August 1986

Leased August 1986

Leased August 1986

Leased August 1986

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Kenora Dryden

Ignace

PRESTON OLIVEMINE

U.S.A.

E. LUOWIG GEOLOGICAL CONSULTING

CLIENT: NORONT RESOURCES LTD.PROPERTY: PRESTON-OLIVE PROPERTYTITLE:

LOCATION MAPFig. l

Date: May 1987

Drawn:

Scale: 1"r25milesInferp:

NTS:

Job No: 0-133

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LITTLE TURTLE LAKEi \ -K475437 : K475436 , K475435 K47S434

'K47545I H475450 K475449 ! K s .! 475.^48

NIVEN'S BASE LINE

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E. LUDWIG GEOLOGICAL CONSULTING

CLIENT: NORONT RESOURCES LTD.PROPERTY: PRESTON-OLIVE PROPERTYTITLE:

KEY PLANFig. 2

1987Drawn: Interp:

NTS:

Job No. 0-133

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r r r3.0 TOPOGRAPHY

j The area around the property consists mainly of low ground and rolling

hills covered by a thin vanier of sand and till. Outcrop exposure is

l plentiful, forming patches across the property.

p Vegetation is comprised of second growth Jackpine, Poplar and White

Birch in areas of high relief and Alders in the low lying regions.

P Little Turtle Lake forms the northern boundary of the property.

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s~* r 4.0 EXPLORATION AND DEVELOPMENT HISTORY

p The property was discovered by "Doc" Gardener in 1885 (O.B.M. Vol. 8,

1 Pt. 2, 1897) and has a detailed history since. A summary of exploration -

P and development work of the Olive-Preston Mine, is as follows:t

1896: Sold to W. A. Preston of the Preston Gold Mining Company

t- - . of Ontario Ltd. Property transferred to a subsidiary company,

r Olive Gold Company of Seine River Limited (O.B.M. Vol. 8, Pt. 2,

1897). . .

l 1RQ7l 1900 - O l ive Gold Company put down a 700 inclined shaft to 251 feet.

p Levels at 60, 135 and 250 feet, with 867 of drifting on the

first level, 290 feet drifted on the second level and 177 feet

P on the third level. A two-stamp mill was increased to 10 theni

25. Operations ceased on June 1900. Production from 1897 tor~

l 1900 was 2,699 ounces of gold from 6,925 tons (0.39 ounce of

r- gold per ton) (O.B.M. Vol. 9, 1900).l

1935: Olive Gold Mines Limited dewatered old workings and sampledr—

[ (O.B.M. Vol. 45, Pt.1, 1936).

p 1937: 20-ton Straub Amalgam Mill installed, 1,000 feet of drifting [

carried out on the second level. Production of 50 ounces ofr-I gold from 330 tons (0.15 ounce of gold per ton) (O.B.M. Vol. 52,V

Pt. 1, 1937).r1942: Leased to Goldorel Mining Company Limited. Workings dewatered

P to 135 foot level, 20-ton Hardings Mill installed. Hoist house t

and mill destroyed by fire in August 1942, stopping operations.r~

L Production was 823 ounces of gold from 2,169 tons (0.38 ounces

r^ of gold per ton) ( O.B.M. Vol. 52, Pt. 1, 1943).

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ri v 1958-59: Property acquired by Olympus Mines Limited. Workings dewatered

to approximately 145 feet below surface where a skip which was

L derailed in the 1942 fire, was encountered in the shaft. Work i;

p stopped early in 1959( Canadian Mines Handbook 1959).

1964-65: Olympus Mines Limited optioned the property to Proteus Minerals

[ ' Limited. Eleven drill holes totalling 3,000 feet, was carried

out along the structure (O.D.M. Circular #13, 1971).

1979: Claims staked by R. Pitkanen and optioned to Sherrit Gordon Mines

l Limited, who completed one drill hole totalling 922 feet.

p the Port Arthur Copper Company mined 26,509 l bs. of copper from a small

1 massive sulfide lense near the southeast corner of the property.

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rrl v 5.0 GEOLOGY

r 5.1 REGIONAL GEOLOGY

The property occurs within the southwestern portion of the Superior

[ . Province, on the boundary between the Wabigoon Subprovince and the

p Quetico Subprovince, seperated by the Quetico Fault (Fig. 3) (Fumerton

^ - 1980).

T In the Mine Center region, the Olive-Preston Gold Mine, occurs in a

wedge shaped fault block of greenstone, boundaries of this block being

[ the Quetico Fault to the north and the Seine River Fault to the south.

P Major Lithologies of this region include, steeply dipping mafic to

^ intermediate metavolcanic rocks intercalated with gabbroic sills

P (possible extrusive origin), turbidite metasedimentary rocks, felsic t

metavolcanic rocks and iron formation. These rocks are cut by grano-

[ diorite, monzonite and trondhjemite intrusives. Metamorphisim is

varible, regionally grading from lower greenschist to upper amphibolite

facis, which is characterized by two periods, first a prograde event,

P secondly retrograde metamorphisim (Pirie et al. 1978). Poulsen et al.w -

(1980), interpeted the rocks in the Mine Center-Atikokan region to be

[ inverted by nappe-like folds. Later work by Poulsen (1983) indicated

axial planes of these folds are southeastwards and create antiforms

i. and synforms which do not reflect the stratigraphic order. Regional

r formations are summarized in table 1.

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UiW/fx,

PRESTON-OLIVE PROPERTY

j i -V' IjUff.n f '-rv a ^ -- 7b - ,* y , nil ' w/,- rt^^^^r^v^^AJV''30 /'' 5'^'^•/•fl^feiPi I 'l.-P -/Al^'1 ^'*— 'l" '-7 S—^f Jf ^

-x . l

E. LUDWIG GEOLOGICAL CONSULTING

CLIENT: NORONT RESOURCES LTD.PROPERTY: PRESTON-OLIVE PROPERTY

REGIONAL GEOLOGY MAPpate: May 1967 Scale: 1:253.440

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PRECAMBRIAN CENOZOIC

QUATERNARY RECENT

Lake, stream and swamp deposits

PLEISTOCENE

Sand, gravel, clay, varved clay

Unconformity

PHANEROZOICEARLY PRECAMBRIAN (ARCHEAN)

MAFIC INTRUSIVE ROCKS

Diabase dikes, lamprophyre dikes, and andesite dikes

Intrusive Contact

FELSIC INTRUSIVE ROCKS DASHWA LAKE BATHOLITH

Biotite and hornblende granite, quartz monzonite. granite gneiss quart/ monzonite gneiss, porphyritic trondhjemite, feldspar quartz por phyry, mylonite, migmatite, aplite pegmatite

Contact Relations Uncertain

MARMION LAKE BATHOLITH

Biotite and hornblende trondhjemite; qiiarlz-scricitc schist; complex of quartz porphyry dikes, mafic dikes, and mafic volcanic rocks

Intrusive Contact

METASEDIMENTSMETASEDIMENTS

r Conglomerate, greywacke, arkosic grit, quartzite, graphitic argillite, phyllite, slate, schist, intercalated sedimentary rocks and volcanic rocks, iron formation

, , , rocks, iron formation

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METAVOLCANICS AND MRTASKIMMENTSFELSIC TO INTERMEDIATE MKTA VOLCANICS

Massive and laminated lavas, qiiailz-sciicite schist, tnfl, agglomerate, pillow lava, feldspar porphyry, foliated volcanic, rocks of inter mediate composition intercalated with mafic luff and lava, iron formation

MAFIC TO INTERMEDIATE MF.TAVOLCAMCS

Massive lava, chlorite schist, chloritc-carbonale schist, pillow lava, tuff, agglomerate, amphibolite and amphibolite schist, coarse-grained lava or niafic intrusive rocks, amphibolite and intercalated sedi mentary rocks, iron formation

T TABLE 1 Table Of Formations (Fenwick 1976)

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r ^.-5.2 PROPERTY GEOLOGY

l The property is underlain by rocks of Archean age, trending east, dipping^

p steeply north. The top of the stratigraphy is north, determined from

1 pillowed basalt flows. Bedrock consists of alternating mafic, intermediate

f and felsic metavolcanic rocks with interbedded tuffaceous units.L

Directly north, the Quetico Faulttrends in an easterly direction, with

[ rocks south of the fault developing a parallel bedding plane foliation.

p To the south, the property is bounded by a 1 mile thick unit of

1 meatmorphosed granitic intrusive rocks, monzonitic to trondhjemite in

P composition. In the summer of 1983 geologists of Homestake Explorations;v

Limited mapped the property using grid lines cut at 300-foot centers.

! The 1983 program defined the lithologies in the vicinity of the Olive

p- Gold Mine, as being comprised of a mafic volcanic-clastic sedimentary

1 package, up to 4,500 feet thick.

T Underground, two units of the above package were observed a) intermediate (.

tuff, which displays a bedding plane foliation, striking N700 E and

[ dipping on average 70 0 north, and b) chlorite schist which appears to

be the derivative of andesite flows, striking N 70 0 E.

Gold is found in a narrow quartz-carbonate vein system conformable

f" to the hosting band of intermediate tuffs. The vein pinches to 0.5"k .

and swells to a width of 5.0' (quartz blow outs) but averages 7.5"

i through out the mine workings.

West of the shaft, located on all three levels is a cross fault which

' ' trends N 40 0 W and displaces the stratigraphy by an average of one foot.

H (IDr

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rf ^~ 6.0 SAMPLING OF THE OLIVE MINE WORKINGS

P 6.1 SAMPLING METHODS

A program of sampling was undertaken to locate ore-grade shoots over

i mining widths and lengths.

Three types of sampling were undertaken, these were:

*- i) Grab Samples - These were taken where chip and channel samples were

p impossible. Locations of these samples include,i

second level-west stope (muck samples) and down the

i shaft, testing for gold content in the vein (Map 4).

p ii) Chip Samples - These were taken along the strike of the vein, to

determine the gold content of the vein only. Chip

T sample results were related to channel sample results

to verify gold anomalies.

l iii) Channel Samples - These were taken across the back of each drift

p where attainable. Each sample was 2" wide and

0.5" deep, taken acroos a width of 3 feet and

T 5 feet where possible. Samples were taken at

5-foot intervals.

6.2 SAMPLING RESULTS

l The following are the weighted averages for the channel samples from

p each level:

i) First Level (Map-1) Shoot 1a: Grade - 0.346 oz/TonWidth - 3 feet

M Length - 56 feeth i

Shoot 1b: Grade - 0.254 oz/Tonfi Width - 3 feeti l Length - 62 feet

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r1 ii) Second Level (Map 2) Shoot 2a: Grade - 0.071 oz/Ton

Width - 3 feet P Length - 10 feet

Shoot 2b: Grade - 0.032 oz/Tonr Width - 3 feet[ Length - 25 feet

Shoot 2c: Grade - 0.036 oz/Ton Width - 3 feet Length - 25 feetr

P Shoot 2d: Grade - 0.057 oz/Ton l Width - 3 feet

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Length - 10 feet

Shoot 2e: Grade - 0.018 oz/Ton Width - 3 feet Length - 30 feet

i- Shoot 2f: Grade - 0.016 oz/TonWidth - 3 feet

p Length - 25 feeti

Shoot 2g: Grade - 0.030 oz/Tonp Width - 3 feet

Length - 25 feet

Shoot 2h: Grade -0.04 oz/Ton Width - 3 feet Length - 40 feet

[ iii) Third Level-(Map 3) Shoot 3a: Grade - 1.466 oz/TonWidth - 3 feet Length - 46 feet

Shoot 3b: Grade - 0.026 oz/Ton Width - 3 feet Length - 15 feet

Shoot 3c: Grade -0.03 oz/Ton Width - 3 feet Length - 30 feet

r Shoot 3d: Grade - 0.019 oz/TonWidth - 3 feet

1 Length - 30 feet

f Shoot 3e: Grade - 0.037 oz/Ton i. Width - 3 feet

Length - 10 feet

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rp ^ 7.0 ECONOMIC SIGNIFICANCE

One main ore shoot exists, which can be traced between all three levels

l in the west drifts. Between the first and second levels, mining has 5

removed all viable ore, leaving behind an estimated 1,100 tons of broken i l ore in the west stope. Sampling of this broken ore indicated an

r average grade of 0.317 ounce of gold per ton, from 12 muck samples.

An ore calculation can be made for the material between the second

[ and third level: Average length: 120 feetWidth: 3 feet

r- Grade: 0.5 oz/Ton [ Height: 112 feet

120x3x112r r

^ 3,360 tons x 0.50 oz/Ton x 902 = 1,512 oz/Au

Between First level and surface: Average length: 120 feetWidth: 3 feet

r Grade: 0.30 oz/Ton l Height: 30 feet

120x3x30 s 900 tons x Oi30 oz7Ton x 90ft z 243 oz/Au 12

r r

An estimated 4,000 tons of material remains, halfway between the first

[ and second level and the surface, located east of the shaft. Grade

r of this material is estimated at 0.25 ounce of gold per ton, yieldingf

1,000 ounces of gold.

[ Therefore a total mineral inventory in all three catagories, proven,

possible and probalble, would be 9,360 tons at a recoverable grade

' i of 0.327 ounce of gold per ton

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r r8.0 RECOMMENDATIONS AND CONCLUSIONS

rThe Olive Mine workings were established through out the years, to

P produce gold from a narrow quartz-carbonate vein, which in sections,t

was extremely high grade. Mining methods used were applicable for

[ such a task, maintaining a mining width of 2-3 feet in the shrinkage

P stopes.

Today, the past mining methods, are extremely costly, therefore not

[ justifying a mining operation, unless grades are consistently high

grade.

L Recommended is a program of diamond core drilling to explore at depth

P and along strike for ore which may be wider and in greater quantity,

to substantiate a mining operation.

^ 8.1 ESIMATED COSTS

[ Phase I ; Diamond Drilling

P - Diamond Drilling, Supervision, Accommodation, Travel. [ Assaying, Management and Report, Contingency:

P All inclusive: 8,000 feet at S25Xft. .................. 1200,000.00

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r r REFERENCES

Fumerton, S.L. - 1981 Redefinition of the Quetico Fault near Atikokan, P Ontario. Canadian Journal Of Earth Sciences Volume 19, No.3 l pp. 222-24.

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Ludwig, E.H. - 1984 Petrographic and Immobile Trace Element Studies of the Olive-Preston Gold Deposit, Mine Center, Ontario. H.BSc. Thesis, Laurentian University.

Page, C.E. - 1983 Geology of the Olive-Preston Gold Occurrence Corporate Report: Harbinson Mining Oil and Gas Group, Toronto, Ontario

Pirie, J. and MacKassey, M. - 1978 Preliminary examination of regional metamorphism in parts of the Quetico Metasedimentary Belt, Superior Province, Ontario, G.S.C. Paper 78-10 pp.37-48.

Poulsen, K.H. and Borradaile, H. - 1980 An inverted Archean Succession at Rainy Lake, Ontario, Canadian Journal of Earth Sciences, Volume 17, pp. 1358-1369

Poulsen, K.H. - 1983 Strucrural Setting of Vein-Type Gold Mineralization in the Mine Center-Fort Frances Areas: Implications for tt Wabigoon Subprovince, O.G.S. Misc. Paper 110. pp. 174-181

p in the Mine Center-Fort Frances Areas: Implications for the

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r rCERTIFICATE

I, Eduard Ludwig, residing at Porcupine, Ontario, hereby certify:

[ i) That I am a graduate of Sir Sandford Fleming College (1980) and

Laurentian University (1984), and that I Have both a technician's

1 diploma and an H.BSc. in Economic Geology.

T ii) That I have been practising my profession as a technician since

1980 and as a consulting geologist since 1984.

( iii) That I have no direct or indirect interest in the mining claimst

referred to in this report nor in the securities of the

l company concerned and that I do not expect to receive any

r such interest.

iv) That I consent to the use in full, or in part, of my report

l dated June 25,1987 for the purposes in accordance with thet,requirements of any Canadian Securities Commission.

[ June 25, 1987 Eduard Ludwj

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r r r r r r r[~ APPENDIX: A

ASSAYS

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r r*SWASTIKA LABORATORIES LIMITED

P.O. BOX 10. SWASTIKA, ONTARIO POK 1TOTELEPHONE: (705)642-3244

ANALYTICAL CHEMISTS * ASSAYERS* CONSULTANTS

nf Analysisr—

Certificate No. 66223

48 Samples off Received March 31. 1987t -

Submitted by Noront Resources Ltd.. Toronto. Ontario.

Date: April 3. 1987

Ore___________

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SAMPLE NO.

5163 'd5164 .'.X 1.-'"'

5165 .0-}-5166 O.'Ji5167 0.I0--

5168 O.MO--

5169 aoig5170 '.^

Second Pulp u~r5171 O.\45172 L?.?'?5173 O.o'i5174 0,S2L^5175 9 - 0 ^

5176 0-015177 0.0^

5178 0/21

5179 o.*l-5180 0.&15181 O.ctf

5182 0.M4"

Samples oer E

GOLDPPB370

140

70

2470

3630

15770

2880

50740/5397037440/330504870

93902540

17970

17802400

1710

7340

26190

28590/29210

3150

15290

. Ludwiq

SAMPLE NO.

-. 5183 o.qq .,,5184 0.2*re

5185 I.DB-Second Pulp'^01

5186 D.CM;-

5187. C?.LV

-5188 Oftb-5189 O.Q^5190 O.D't'.f

5191 0.^.3

5192 O.\LP •5193 o.\ 65194 O .c? l

5195 .00 S51965197 ''-r' yV

5198

51995200 .co'-l5201 ..- ft 1 '-

Second Pulp

GOLDPPB

150201022037370/3970044430/38610

550

2190

11180

3090

3020

2880

5590/3020

5420

350

10

190

110

30

10

160

98060/7502098610/86610

SAMPLE NO.

-5202 O.-l-

5203 o.'.:-v

5204 r-^V

5205 O.iVr

5206 (?. O^H'

5207 ,: x5208 - -. v5209 : ' rt -

5210 O --70 -

GOLDPPB

14330

2950

1170

5620

1170

1920

690

2060

7200/7610

n PerG. Lebel - Manager

ESTABLISHED 1928

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SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS ASSAYERS * CONSULTANTS

(Zfcrtifirat* rf Analysis

Certificate No. ^6207 Date: April 6. 1987

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Received March 30. 1987

Submitted by

SAMPLE NO.

5101Second Pulp

51025103 5104 5105

5106 5107

5108

5109

5110 5111 5112 5113 5114 5115

51165117

5118

5119

512051215122

62 Samples of Ore

Noront Resources Limited. Toronto. Ontario.

Samoles Der E.GOLDPPB

143040/148120124460/124120

666502540 2190 7890

62880/60620 19060

33390 23250/16940

7950

30 7750 100

2130 6580

20780/29490320

1650

3980

123015102060

, LudwiaSAMPLE NO.

512351245125

Second Pulp Third Pulp

5126 5127 5128

5129 5130

5131

5132 5133 5134 5135 5136 5137

5138

51395140

514151425143

GOLDPPB

17900

6720

105810/10560031540/33460 42510/36340

5280 170

4050 2810

2060

1440

3630 6990 1780 4870/4180 3020 12305350

5690

9530

9870/124102401230

SAMPLE NO.

5144514551465147 5148

5149

5150 5151

5152 5153

5154

5155 5156 5157 5158

5159 Second Pulp

516051615162

GOLDPPB

4730160660200

2400 1170

3570/2400

1580

550

2330

3910

3360 21260 3020 117012960/15770 13580/13370

17105620

2260

r Per

ESTABLISHED 1928G. Lebel - Manager

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^ftW SWASTIKA LABORATORIES LIMITEDT^C^^^^^ P.O. BOX 10, SWASTIKA, ONTARIO POK 1TO f ^^^^ TELEPHONE: (705)642-3244

ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

(Errtifiralp of Analysts

Certificate No.

Received April

Submitted by

SAMPLE NO.

5033

5034

5035

5036

5037

5211

5212

5213

5214

5215

5216

5217

5218

5219

5220

5221

5222

5223

5224

.5225

5226

66247

1, 1987 85

Noront Resources Ltd.,

Samples per E.

GOLD PPB

50

240

130

10

Nil

410

1260

1300

3090/2330

700

430

40

1070

440

90

70

420

470

130

50

340

Ludwig

SAMPLE

5227

5228

5229

5230

5231

5232

5233

5234

5235

5236

5237

5238

5239

5240

5241

5242

5243

5244

5245

5246

5247

Date

Samples of Ore

Toronto, Ontario.

NO. GOLD PPB

160

3910/3840

420

1990

570

310

540

210

2880/3150

850

2470/1990

200

160

990

960

40

1510

360

380

550

30

Per.

: April

SAMPLE

5248

5249

5250

5251

5252

5253

5254

5255

5256

5257

5258

5259

5260

5261

5262

5263

5264

5265

5266

5267

Con't.

9, 1987

Page 1 of 2.

NO. GOLD PPB

120

60

1040

620

190

410

960/1510

410

280

370

270

230

1120

440

750

730

810

1990/1920

1370

Nil

n ESTABLISHED 1928G. Lebel - Manager

Page 27: 52C15SE0014 Olive Mine

n r

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Cartlficata No.(ttwttfteat* nf

rt ,rrrrrrrrrrrrrr

SAMPLE NO.

52685269 5270

5271 5272527352745275527652775278 5279

5280 52815282

52835284

5285528652875288

52895290

GOLD PPB

1801710 100

2330 160

2470/28102701340

3700/347080

560 68040 170260

10Nil

370890/960NilNil

Nil

Nil

Page -2-

G. Lebel - Manager

r ESTABLISHED 1928

Page 28: 52C15SE0014 Olive Mine

rr

L

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

(E?rttftratf of Attalyfiia

Certificate No. 66354 Date: April 21, 1987

55 Samples of Split CoreT Received April 13. 1987

Submitted by Noront Resources Ltd., Toronto, Ontario.

L Samples per E. Ludwig

r-i

rrrrrr

rrrrri

SAMPLE NO.

5038

5039

50405041

5042

5043

5044

5045

5046

5047

5048

50495050

Second Pulp

505150525053

5054

50555056

5057

5058

GOLDPPB

1580/1370

6070

140

70

70

80

70

190240

34770

309033260/2901034560/32570

4180

398013370/14190

510

410

Nil70

170

SAMPLE NO.

5059

5060

5061

5062

50635064

5065

5066

5067

5068

5069

50705071

' 5072

50735074

5075

5076

5077

5078

50795080

GOLDPPB

1510

30

20

30110

240

210210

1720

280

610

18501850510

2001370

1300

690

3430/3500

960

1440

1300

Per

SAMPLE NO.

50815082

50835084

5085

5086

5087

5088

50895090

5091

5092

y?//^

x/ .~s \J

GOLDPPB

13701580

3801650

8070

370

100

70

2330

2470

30

^7 JII Jl MM

G. Lebel - ManagerESTABLISHED 1928

Page 29: 52C15SE0014 Olive Mine

rrr r

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705)642-3244 ANALYTICAL CHEMISTS * ASSAYERS* CONSULTANTS

drrtifirat? of Analysts

Certificate No. 66355 Date: April 22. 1987

42 Samples of Split CoreP Received April 13, 1987

Submitted by Noront Resources Ltd.. Toronto. Ontario.

r Samples per E. Ludwig

rrrrr.r.rr .rrrri

SAMPLE NO.

5093

5094

5095

5096

5097

5098

5099

5100

5291

5292

5293

5294

5295

5296

5297

5298

5299

'5301

5302

5303

5304

5305

5306

5307

GOLDPPB

2060/1710

110

1100

10

1230

170

620

Nil

340/610

110

320

Nil

30

Nil

20

Nil

60

420

50

4050/3840

750

210

40

60

SAMPLE NO.

5308

5309

5310

5311

5312

5313

5314

5315

5316

5317

5318

5319

5320

5321

5322

5323

5324

5325

Per

GOLDPPB

190

58420/59250

80370/74260

32020

270

28660

6380

97440/95040

390860/424670

9670

4730

79680/72690

110

1300

90

30

20

Nil

,i , J9 j lA 7//y^j uAf^i

G. Lebel - Manager

ESTABLISHED 1928

Page 30: 52C15SE0014 Olive Mine

rr rr.

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705)642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

of Analysis

Certificate No. _______66354-A______

Received April 13. 1987 14

Submitted by Noront Resources Ltd.. Toronto. Ontario.

Date: Mav 1. 1987

Samples of Split Core

Samples per E. Ludwig

r

rr r rr~

r r rrr

SAMPLE NO. GOLD (Second Pulp) PPB

5046 200

5047 180

5048 26740/26400

5049 3360

5051 3120

5052 6040/6520

5053 12480/13230

5054 570

5055 290

5056 110/100

5057 * 4705058 3605059 1170/1710

5060 30

NOTE: Since preliminary results for Sample # 5057 were very erratic, we reported the average of replicate analysis.

PerG. Lebel - Manager

ESTABLISHED 1928

Page 31: 52C15SE0014 Olive Mine

r

•rVolume l

52C15SE0814 63.5183 LITTLE TURTLE LAKE

N.T.S. 52 C/10

020

rr

r\

rwrr i

r*.

r

REPORT ON THE 1987 DIAMOND DRILL PROGRAM

ON THE

PRESTON - OLIVE GOLD PROPERTY

MINE CENTRE AREA, ONTARIO

NORONT RESOURCES LIMITED 1116-111 Richmond Street W. Toronto, Ontario M5H 2G4

CHARLES E. PAGE, M.Sc. April 15, 1988

Page 32: 52C15SE0014 Olive Mine

52C15SE08M 63.5103 LITTLE TURTLE LAKE 020C

r TABLE OF CONTENTS

r

Volume l

1.0 INTRODUCTION

2.0 LOCATION AND ACCESS

3.0 PROPERTY DESCRIPTION

4.0 EXPLORATION HISTORY

5.0 GENERAL GEOLOGY OF THE AREA

6.0 PROPERTY GEOLOGY

7.0 MINERALIZATION

8.0 1987 DRILL PROGRAM

9.0 CONCLUSIONS AND RECOMMENDATIONS

CERTIFICATE OF QUALIFICATION

REFERENCES

APPENDICES

APPENDIX: A (DIAMOND DRILL LOGS)

APPENDIX: B (ASSAYS)

Volume 2

l

l

3

5

6

9

11

13

14

15

16

17

APPENDIX: C (DIAMOND DRILL SECTIONS)

Page 33: 52C15SE0014 Olive Mine

LIST OF FIGURES

rFigure l :

Figure 2 :

Figure 3 :

Map l

Map 2

Map 3

Location and Access

Claim Map

Distribution of Gold Deopsits and Fault Zones in the Wabigoon Province

Figure 4 : Gold Properties in the Mine Centre Area

Figure 5 : Geology of Preston - Olive Property

2

4

8

10

Surface Plan of 1987 Drilling

Longitudinal Projection

Surface Plan of 1984 Drilling

in pocket

in pocket

in pocket

r

Page 34: 52C15SE0014 Olive Mine

1.0 INTRODUCTION

Noront Resources Ltd. carried out an eleven (11) hole, 6,153 foot diamond drill program on the Preston - Olive gold property held by HSK Minerals Limited. This program was completed in June 1988 as a follow up to an underground evaluation of the Olive workings.

This report presents the results of recent data with previous drilling.

the program and compiles the

2.0 LOCATION AND ACCESS

The Preston - Olive gold property is located 35 miles east of Fort Francis and 5 miles west of Mine Center, Ontario in the Kenora Mining District (fig. 1).

The property is accessible by a gravel road which extends one mile north of Highway 11.

- l -

Page 35: 52C15SE0014 Olive Mine

- 2 -

Kenora

Ignace

PRESTON OLIVE MINE

U.S.A.

Figure 1: Location and Access

Page 36: 52C15SE0014 Olive Mine

- 3 -

3.0 PROPERTY DESCRIPTION

The property consists of 55 mineral claims comprising 4 patents, 6 leased claims and 45 unpatented mineral claims all located in the Little Turtle Lake (Map G2682) and Porter Inlet (Map G2693) areas in the Kenora Mining Division (fig. 2). All of the unpatented mineral claims have 200 day credits.

CLAIM NUMBERS

Patented Claims

HP 438FF 3711-3712FF 3658

Leased Claims

K475146K475190-193K475269

Unpatented Claims

K475433-452K475455K558996-000K589465K589638-640K590515-517K629001-009K629023K629164-169

NO. OF CLAIMS

12l

l 4 l

20l 5 l 3 3 9 l 6

EXPIRY DATE

89/03/10 88/03/10 88/12/08 89/04/28 88/11/12 88/12/13 88/12/08 88/12/08 88/05/10

55

Page 37: 52C15SE0014 Olive Mine

r

r

r

r

rr

r

Page 38: 52C15SE0014 Olive Mine

- 5 -

4.0 EXPLORATION HISTORY

The following is a brief history of the Olive - Preston property.

1885 : Discovered by "Doc" Gardener.

1897-1900 : Olive Gold Co. sunk shaft to 251 feet, levels at 60, 135, 245 feet with 867, 290 and 177 feet of drifting. A two stamp mill was increased to 10 then 25.Production: 2699 oz. of gold from 6925 tons (0.39 oz/ton).

1935 : Olive Gold Mines dewatered old workings.

1937 : 20 ton amalgam mill installed, 1000 ft. of drifting on second level.Production: 50 oz of gold from 330 tons (0.15 oz/ton).

1942 : Property leased to Golderel Mining Co. Ltd.Workings dewatered to 135 ft. level and 20 ton millinstalled.Hoist and mill destroyed by fire.Production: 823 oz. gold from 2169 tons (0.38oz/ton).

1958-1959 : Olympus Mines Limited dewatered to 145 feet.

1963-1964 : Proteus Minerals Ltd. completed an 11 hole, 3,000 ft. drill program.

1979 . Sherritt Gordon Limited completed an 11 hole, 3,000 ft. drill program

1983 : Homestake Explorations Limited completed a program of airborne geophysics, linecutting, ground geophysics, mapping, trenching and 44 diamond drill holes totalling 8,286 feet.

1985 . Homestake completed a soil geochemical survey over known geophysical and geological trends.

1986 : Metallurgical test carried out by private contractor on surface vein material.

Page 39: 52C15SE0014 Olive Mine

j r*-- 6 -

r1987 : Noront Resources completed shaft rehabilitation,

j dewatering and sampling of underground: workings.

5.0 GENERAL GEOLOGY OF THE AREAr- f1 The property is located in the southwestern portion of the Superior ^ Province in the Wabigoon Subprovince. The Preston - Olive property is*~ located in the Mine Center area which lies within a wedge shaped

greenstone fault block along the southwestern margin of the Wabigoon subprovince. The northern boundary of this block is the Quetico Fault

^~ and the southern boundary is the Seine River - Rainy River Fault. This east-west trending fault network is associated with a 3 to 6 mile thick sequence of volcanic rocks which extend for 300 miles,

^ from Rainy Lake in the west through Atikokan to the Beardmore and Geraldton areas in the east.

r~ The Mine Center area is underlain by steeply north dipping, east-- west trending mafic and intermediate metavolcanic rocks with

intercalated gabbroic sills, turbiditic metasediments, felsic volcanics and iron formation cut by granodioritic, monzonitic and

trondhjomitic intrusions. The rocks are metamorphosed to assemblages characteristic of the lower to upper amphibolite facies and are

^ folded into antiforms and synforms which do not reflect the stratigraphic order (Poulsen, 1983).

p The majority of the gold deposits in the Mine Center area occur asf discontinuous tabular quartz-carbonate veins in ductile shear zones.

These veins have been exploited intermittently in the area since 1893^ and range from a few inches to a few feet in width. Approximately 90**

of these gold occurrences most commonly occur in acidic intrusiverocks ranging from trondhjemite to quartz monzonite. A second type ofgold occurrences are shear zone related vein systems hosted in

"~ metavolcanic rocks.

Page 40: 52C15SE0014 Olive Mine

- 7 -

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(L UJ O

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Page 41: 52C15SE0014 Olive Mine

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- 8 -

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Page 42: 52C15SE0014 Olive Mine

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- - 9 -

r! 6.0 PROPERTY GEOLOGYl, ~~f~—**a^—i——^^^mi^—m^^^^^^^^^^^^m^^lm^^

\ The property is underlain by an east-west trending, northerly L dipping assemblage of mafic-felsic metavolcanic rocks containing

volcanoclastic and metasedimentary units.

Felsic metavolcanic rocks predominate in the southern portion of the property characterized by massive and foliated quartz eye rhyolite

i with intercalated units of felsic and lapilli tuff.

The felsic assemblage grades northward into a sequence of mafic ^ metavolcanic rocks with intercalated units of felsic to intermediate

tuffaceous units. The mafic rocks consist of generally fine grained to coarse grained basalt which is metamorphosed to display gabbroic or amphibolitic textures. It is uncertain whether these mafic rocks

represent flows as many of the textures suggest mafic intrusive similarities. Locally the mafic rocks are severely foliated and sheared developing talc-chlorite schists.

The intercalated tuffaceous rocks within the mafic assemblage form generally narrow continuous units. The intermediate variety are described as feldspar " ash, quartz-feldspar ash, and quartz-

"~ carbonate ash tuff. The felsic varieties are described as rhyolitic and lapillis. Often the intermediate and felsic tuffs grade into one another along strike. A 2,800 foot long gold bearing cherty-carbonate

foliated tuff within the center of the mafic assemblage hosts the Preston-Olive gold mineralization. Similar cherty tuff units occur elsewhere on the property and have potential for hosting gold

^ mineralization.

The Quetico Fault Zone runs through - Little Turtle Lake on the northern portion of the property boundary. This east-west trending

— fault is a major structure which can be traced for 180 miles. Many of the rocks on the property have developed a foliation parallel to the Quetico Fault. Within the more competent felsic tuff units this has

^. developed into intense shearing.

Page 43: 52C15SE0014 Olive Mine

r r r r r r rr

r r r r r r r r rr

- 10 -

Page 44: 52C15SE0014 Olive Mine

r r. rr

7.O MINERALIZATIONr

The majority of gold exploration and production to date has occurred on the Olive Vein Zone. Here gold occurs closely associated with quartz veins and veinlets conformable to a sheared felsic tuff horizon.

The Olive vein is the most extensive displaying pinching and swelling along strike varying in width from l to 8 inches. This vein dips steeply north at approximately 75 degrees. Several parallel veinlets occur associated to the Olive vein which combine to form an overall mineralized zone varying from 1.5 to 3.5 feet thick.

The gold is fine grained and generally occurs along foliation planes associated with approximately l* to 3\ sulphides. Pyrite is dominant with minor amounts of pyrrhotite, chalcopyrite and sphalerite.

Gold values from sampling along the 2,200 foot long Olive vein range from trace to 5.4 oz./ton. The better values are associated to the thicker portions of vein. On surface the most significant area of enrichment is located east of the Olive Main shaft where a 250 foot length of the Olive vein averaged 0.52 oz. gold/ton, over an average width of 3.5 feet. It is from this area that a 30 ton metallurgical sample was extracted grading 2.75 oz. gold/ton in 1986.

Recorded gold production from the property amounts to 3,572 ounces intermittently recovered from underground operations between 1897 to 1942. This production was recovered from 9,424 tons of Olive vein material representing an average grade of 0.38 oz./ton.

In 1984 an 8,286 foot diamond drill program tested the near surface potential of the Olive vein zone with a view to develope sufficient material to open cut mine and transport to a custom mill in the area. This program consisted of a series of short holes drilled at 50 foot intervals along the eastern extent of the Olive vein for approximately 1,100 feet. This drilling continued to encounter the Olive vein eastward over narrow widths in the order of l foot. Also as a part of this drilling program 18 drill holes tested areas between and in the vicinity of the old mine workings to a depth of 300 feet. As a result of this drilling program and with the aid of old assay plans of the mine a mineral inventory of 23,225 tons grading 0.22 oz. gold/ton was calculated.

Page 45: 52C15SE0014 Olive Mine

r r- 12 -

Hole #43 of the 1984 drilling program tested a cherty-tuff sulphide zone some 1,500 ft. southwest of the Olive vein zone on claim K 475269. Here 1983 sampling of muck from a small exploration pit returned anomalous gold values. The hole intersected a 12 foot thick sulphide zone in tuff averaging Q.02% Cu, Q.32% Zn, 0.005 oz. Au/ton and 0.23 oz. Ag/ton.

The Olive workings consist of a main 6x8 foot inclined shaft to sunk to 247 feet. A total of 2,344 feet of drifting is reported on three levels at 60 feet, 138 feet and 210 feet. In 1987 Noront Resources Ltd. dewatered the old Olive workings to determine the dimensions and grade of any remaining ore shoots. Underground the Olive vein pinches to 0.5 inches and swells to 5 feet. The average width through out the mine workings is approximately 7.5 inches.

As a result of this program two gold shoots have been identified within the mine workings. The west shoot occurs on all three levels and has partially been mined between the first and second. Sampling results from this shoot returned 130 feet averaging 0.319 oz. gold/ton across 3 feet on the first level, and 46 feet averaging 1.466 oz. gold/ton across 3 feet on the third level. Between the first and second levels there remains approximately 1,100 tons of broken material averaging 0.317 oz. gold/ton. Ludwig (1987) calculates a total of 5,360 tons of material remaining in this shoot grading 0.38 oz. gold/ton. The east shoot located 150 feet east of the shaft extends from surface to midway between the first and second levels. Here Ludwig (1987) calculates a reserve of 4,000 tons grading 0.25 oz. gold/ton. Combined the total reserve within the mine workings is 9,360 tons grading 0.327 oz. gold/ton.

Page 46: 52C15SE0014 Olive Mine

- 13 -

8.0 1987 DIAMOND DRILL PROGRAM

Following the underground evaluation an 11 hole, 6,167 foot diamond drill program commenced in May 1987 to test: a) the down dip extension of the Olive vein at 500 feet below surface, b) stratigraphy north of the Olive vein zone, and c) a quartz-fracture zone located in the northeastern portion of the property.

At the back of this report a location plan of the 1987 drill holes are plotted in reference to the 1984 holes (Map 1). In addition a longitudinal section of the drilling and underground workings is enclosed (Map 2). As Appendix l to this report drill logs of the 1987 program are attached with cross sections.

Seven holes (87-2,3,4,5,6,7 and 8) tested the Olive vein zone over a length 1,500 feet beneath the old workings at approximately 500 feet below surface. Of these holes only 87-3, encountered an enriched gold value of 0.107 oz./ton across 5.0 feet in the Olive vein. The remaining holes returned only anomalous values over narrow widths. In holes 87-4 and 87-5 a quartz-carbonate vein system was encountered 100 and 200 feet respectively north of the Olive vein in the hanging wall intermediate volcanics. Hole 87-4 returned 0.178 oz. gold/ton across 5.5 feet with 1,020 ppm Cu and 55 ppm Zn. Hole 87-5 returned 0.096 oz. gold/ton with 1,230 ppm Cu and 4.55% Zn across 5.5 feet. The relationship between these two intersections is unknown as they occur in different stratigraphic positions away from the Olive vein zone.

Three holes (87-1,9 and 10) tested the stratigraphy north of the Olive vein zone. These holes encountered metasedimentary and metavolcanic rocks intercalated with oxide iron formation and grey feldspar porphyry. Hole 87-1 intersected a zone of quartz-carbonate veining with pyrite and chalcopyrite approximately 500 feet north of the Olive vein. This zone returned 0.077 oz. Au/ton across 5.0 feet hosted in a chlorite schist.

Hole 87-11 was drilled in the northeastern portion of the property to test a quartz-carbonate fracture zone identified during mapping in 1983. This hole was drilled on claim K 629006 encountering a 14 foot section of the fracture zone returning anomalous gold values of 306 ppb, with copper values up to 1,900 ppb.

Page 47: 52C15SE0014 Olive Mine

r

- 14 -

rl

j- 9.0 CONCLUSIONS AMD RECOMMENDATIONS

Diamond drilling of the Olive vein zone below the old workings at P approximately 500 feet below surface encountered poor results. l Although the narrow vein was encountered in each drill hole only one

returned an encouraging intersection. At this time no further r- drilling is warranted below the Olive mine workings.

While drilling the fence of 7 holes below the mine and 3 stratigraphic holes to the north three new parallel vein systems

P were encountered returning economic gold and zinc values. Further exploration is required in this area to delineate the extent and significance of these new zones.

Drill testing of a surface quartz-carbonate fracture zone in the northeastern portion of the property returned anomalous gold values

r over 14 feet. Further work is warranted to define the extent of this! zone.fr -

To define the significance of the parallel vein systems north of theP Olive vein zone a minimum 5 hole, 3,000 foot diamond drill program is

recommended. At the same time consideration should be given to drilltest the eastern extent of the Olive vein system at a minimum of 500

( feet below surface.

To further define the extent and significance of the quartz- ^ carbonate fracture zone in the northeastern portion of the property a

program of stripping and trenching is recommended. If this is successful in identifying a significant structure additional drilling is required.

Respectful

April 15, 1987 Charles E. Q*4e]ttKsBd.SFGAC

r

Page 48: 52C15SE0014 Olive Mine

r

- 15 -

CERTIFICATE OF QUALIFICATION

I, Charles E. Page, of 1454 Westbury Avenue, in the City of Burlington, in the Province of Ontario,

DO HEREBY CERTIFY:

1. THAT I am a graduate of Brock University (1975) with a degree of Bachelor of Science (B.Se) with Honours in Geological Sciences, and the University of Waterloo (1983) with the degree of Master of Science (M.Se) in Earth Sciences.

2. THAT I am a Fellow of the Geological Association of Canada.

3. THAT I have been practicing my profession as a geologist and engaged in exploration since 1975.

4. THAT I have worked in the Mine Center area since 1983 carrying out exploration. I have worked intermittently in northern Ontario since 1975.

5. THAT I have supervised the exploration carried out on the property disclosed in this report.

April 15, 1988 Charles

Page 49: 52C15SE0014 Olive Mine

- 16 -

rV

r- REFERENCES

i

P Goettler, G. W., 1986: An Evaluation of the Gold Claims of i- Homestake Explorations Limited, Mine Centre Area of Ontario for

Noront Resources Limited of Toronto, Ontario. Private Company r~ Report.l

r- Ludwig, E. H., 1987: Economic and Geological Evaluation of Olive Gold Mine : Dewatering and Sampling Program : Jan. - March 1987. Private Company Report.

Page, C. E., 1983: Geological, Geophysical, Geochemical Report on the Mine Centre Area Claims, Ft. Frances Area, Kenora Mining

f- Division, Ontario. Private Company Report.

Poulsen, K.H., 1983: Structural Setting of Vein-type Gold P Mineralization in the Mine Centre - Ft. Frances Area:

Implications for the Wabigoon Subprovince. Ontario Geological Survey, Misc. paper 110; A. C. Colvine, Editor.

r

ri

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Page 50: 52C15SE0014 Olive Mine

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Page 51: 52C15SE0014 Olive Mine

r

APPENDIX : A

DIAMOND DRILL LOGS

r i

r

Page 52: 52C15SE0014 Olive Mine

r

i i DIAMOND DRILL RECORDi! ft. !dio iazim!i i PROPERTY.... OLIVE HINE i -60 i i TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE I.... 87-1i! CJ-WJ1 NUMBER.... K-475146 i i i COLLAR CO-ORDINATES.... 5980N. 4200E N TOTAL LENGTH.... 599'i i L. STATION ....DUE SOUTH i i i COMPANY.... NORONT RESOURSES LTD. " ' " ' SHEET I.... 1i! LOGGED BY.... E. LUDUIG CORE SIZE.... BD CORE LOCATION.... ON SITE DATE START... FIN...II V i J* - " " v ' l 1 , - \1 l ; l

1 t

1 11 1

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1 |1 1

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to

34

286.5

293

DESCRIPTION

CHLORITE SCHIST

-contorted appears waveyy, extreme contortions contain 21 py-possible quartz fragments or boudins, carbonated along boundries-no measurable core axis-25' - 34* uncontoured chlorite schist, C.A. 40 degrees at 33'-minor quartz stringers-1" seam of 25Z pyrite cubes at 29.6'

INTERCALATED BIOTITE AND CHLORITE SCHISTS

-up to 15Z quartz carbonate stringers, 0.2'-0.5" thick at randomorientations

-C.A. 35 degrees at 38'-biotitic sections contain up to 10Z disseminated pyrite on average21 pyrite and minor chalcopyrite-feldspars are eaten away, with granules remaining appearing pitted-both chlorite and biotite are fine grained and flakey-biotite rich layers contain mor pyrite than chlorite layers-carbonate isolated to quartz stringers-deformation of foliation from 65-73, 21 pyrite trace cpy, carbonate infractures

-stretched quartz-carbonate stringers - boudins associated withenveloping band of pyrite-deformation of foliation from 68.0' -73.0' up to 5Z desseminated py-C.A. 45 degrees at 199'-C. A. 52 degrees at 285'-extremely deformed from 228-237.5 up to 8Z diss. pyrite foliationcompletely destroyed - silicified grey green MSS-199-209 almost pure chlorite dark green 1-2Z pyrite

GRAY FELDSPAR PORPHRY

-ground mass comprised of biotite, chlorite and quartz in equalproportions-phenocrysts starting to break down, edges eaten away and comprised ofplagioclase-phenocrysts up to 0.25" in size-extremely broken up from 289-293 up to 5Z pyrite weakly carbonated,vith chloritic slips

C

i

ll

SAMPLE i ASSAY1l

no*

12O

45

6 t

8q

1011121314151617IB192021

no 122232425262728293031323334353637M

3940414243

from

192829.53338

434853586368737883889398103108113118

133138143148153158163168173178183188193198203208213218223228233

to

232934.73843

4853586368737883889398103108113118123

138143148153158163168173178183188193198203208213218223228233238

length! AUippb'sf

1

4' i 101' i nil5.2' i nil5' i nil5' i nil

1

11

5' i nil5' i 105' i nil5' i 705' i 2405' i nil5' i nil5' l 205' i nil5' i nil5' i 26405* inil5' !205' inil5' inil5' inil

i5' i 205' i 1005' !705' 1205' inil5' inil5' inil5' inil5' inil5' inil5' inilS' inil5' inilS' inil5' inil5' inil5' inil5' i 105' i 305' !20

0.077 jz/ton

iii

5' 1755 i i

Page 53: 52C15SE0014 Olive Mine

rr*0rfflffffoifrcc"KCffRff 1 1il PROPERTY...

Ift. dip iaziii.OLIVE HINE 1 ! l TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE t.... 87-1

1 1 0^*1 NUHBER. . . . V; - ' . ; itl t- i 1 i COLLAR CO-ORDINATES. . f. -vv.- V j TOTAL LENGTH....1! BUiflTATION ....DUE SOUTH i i ! COMPANY.... NORONT RESOURSES LTD. SHEET I.... 2i! LOGGED BY..1 1 1 i

.. E. LUDHIG CORE SIZE.... BO CORE LOCATION.... ON SITE DATE START... FIN...

1 1

II i

II FOOTAGE1 11 1

llfroi i to1 t1 1.

1 1 i i

i l 1 l

1 i t i

!!1 1 1 11 1 1 11 1 1 11 1 1 11 1 1 1II 2931!1 1 1 1

! I1 1 1 1: :i:1 1 1 1:: 3161 1 1 11 1 1 11 1 1 11 1

1 1 t 11 1

I!11321.2!!1 1 1 11 1 1 11 11 1

!!1 1 1 1i 1334.81 1 1 11 11 1 1 11!lili 3521 11 1

IIt 1 l 1

1 1 1 1

1 1

II

316

321.2

334.B

352

599

DESCRIPTION

SILICIOUS CHLORITE SCHIST

-C.A. 85 degrees at 309, highly deforied belov 309'-weakly carbonated, non-iagnetic, soptty pyrite-up to 51 pyrite enveloping 0.5* quartz-carbonate veins-quartz knots along foliation- ediui green colour, extremely soft

GRAY FELDSPAR PDRPHRY

-upper contact fine grained between 316-317'- i nor quartz carbonate veinlets-chloritic slips along fractures-plagioclase pbenocrysts up to 0.25*-groundmass of biotite, chlorite and quartz

FAULT AND DEFORMATION ZONE

-up to 1Z pyrite cubes-ground core froi 331 to 334' - strongly carbonated-brick red heutite staining-chlorite is crennulated with quartz knots froi 321.2-330-no wasureable core axis

GRAY FELDSPAR PORPHRY

-grades into feldspar porphry froi quartz-biotite-chlorite schist-light greenish gray in colour - odd phenocrysts-up to 21 pyrite, linor carbonate - no quartz carbonate stringers

INTERCOLLATED ANDESITE FLOWS AND TUFFS

-Mdiui green, foliated, chloritic - weak to loderately carbonated-no sulfides, non-iagnetic - linor quartz carbonate stringers-tuffs C.A. 52 degrees well foliated, chloritic - flows ussive, nopillows

599 1 END OF HOLE Acid test 300' - 54 deg Acid test 599'- 49 deg

SAHPLE

no.

44454647484950515253545556575859606162636465666768697071727374757677787980818283B4

froi

238243248253258263268273278283288293298303308313318323328333338343346348352355359368388401423465480483494509527534548560578

to llength

243248253258263268273278283288293298303308313318323328333338343346348352355359363371394408426468483486500511530538550563579

5'5'5'5'5'5'5'5'5'5'5'5'5'5'5'5'yyyyy3'2'4'3'4'4'3'6'7'3f3'3'3'6'2'3'4'2'3'1'

j

ASSAY

AU.ppb'sJSS?Xrnilnilnilnil10nilnil10nilnilnil25nilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnil20nil30nilnilnilnilnilnil

•^so

to

1 11 1i;

Page 54: 52C15SE0014 Olive Mine

i l DIAHOND DRILL RECORD

:: PROPERTY...!ft. Idin lazii!

.OLIVE HINE i 1-651 l TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE t.... 87-2l! tr*H NUMBER.... K-475146 i l l i COLLAR CO-ORDINATES.... 5:: k. STATIONII LOGGED BY..1 1 1 1

....DUE SOUTH i i ! i COMPANY.... NORONT RESOUR.. E. LUDUIG CORE SIZE.... BQ CORE LOCATION.... ON SITE

770N, 4370E TOTAL LENGTH.... 589' SES LTD. - """" ' SHEET I....1

DATE START... FIN...t- . , . . ; ". ' ' -

1 l1 l

li FOOTAGE 1

i i froi i toli:: oi! II 37i!1 1 t 1

1 l 1 1

1 1

1 1 t l

l!1 1 1 1

1 tt 1

1 1 1 1

1 11 1

l! 79!!1 1 1 11 1 1 11 1 1 11 1M

j ji!1 1 1 11 11 1:: 1021 11 11 1 1 11 11 11 1 1 1

!!1 11 1 1 11 11 1 1 11 1 1 11!i!i!1 1 1 11 1 1 1:: 2031 1 1 11 1 1 1i!i!li1 1 1 1

~37 "

79

102

203

251

DESCRIPTION

"OVERBURDEN "" ~" " ~" "~

INTERCOLLATED BIOTITE AND CHLORITE SCHISTS

-unit highly variable froi fine to wdiui grained sections with coarsechlorite clots-quartz stringers throughoutsulfides sparsely dispersed in bands-sul fides associated with silicified sections of core pyrite,pyrrhotite, and trace chalcopyrite-weakly carbonated-C. A. 45 degrees at 65'

FAULT AND DEFORMATION ZONE

-fault gouge froi 96-98'-highly contorted core on either side of fault-pyrite froi 1-21-unit highly carbonated along irregular fractures-luit i pi e highly distorted quartz stringers-quartz vein froi 79 to 79.5-quartz vein froi 80.5 to 81.5, 51 pyrite, trace cpy, po.-quartz vein froi 101-102 trace pyrite

INTERCOLLATED ANDESITE FLOHS AND TUFFS

-flows ussive fine grained, udiui green-abundant quartz stringters containing up to 51 pyrite-tuffs have distorted foliation with quartz knots and traces of pyriteand pyrrhotite, appears as silicified chlorite schist

-lover contact gradational-quartz stringers at no preferred orientation-weakly carbonated throughout-froi 121 to 126 unit becot-es grey and silicious hard and fractured,1Z pyrite, altered porphry?

OUARTZ FELDSPAR PORPHRY

-brownish - grey utrix, lediui to fine grained-non-carbonated, up to li pyrite-phenocrysts up to 0.25* and are well forwd, becoie larger towardscenter of unit-phenocrysts plagioclase in composition-quartz vein froi 246-246.5

SAMPLE

no....m

BS868788B9909192

93

94959697

VU)TD

99100101102103104105106107108109110111112113114115

froi......

3742455257646871

77

82869197

109116130136139144159164169174179184189194199203209214

116 1 224117 l 229

-quartz vein froi 247.5-248 ! 118 ! 234i 119 i 239i 120 1 244

to......

4245525762667077

82

869197101

114121135139144150164169174179184189194199203209214224229234239244

length......

y3'TyyV2'6'

5'

4'5'6'4'

5'5'5'3'5'5'5'5'5'5'5'5'5'5'5'6'5'10'5'5'5'5'

249 i 5'

ASSAY

AU.ppb's

nilnil10nilnil145nilnil

20

10nilnil10

30101010nilnilnilnil30nil1010nilnil10nilnil10

___

k

nilnilnilnilnil

__

i! 121 249 251 2' nil1 1 1 1 __________ ____ ____ ___

Page 55: 52C15SE0014 Olive Mine

DIAMOND DRILL RECORD1 t

!! PROPERTY... l ! (1 NUHBE i! ORIENTATION i! LOGGED BY..1 l

If t. idio iaziii.OLIVE HINE i l i 1 TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE I.... 87-2R.... i ! i i COLLAR CO-ORDINATES.... : - -i^.i- i TOTAL LENGTH........DUE SOUTH III! COHPANY....NORONT RESOURSES LTD. SHEET I.... 2

.. E. LUDUIG CORE SIZE.... BD CORE LOCATION.... ON SITE DATE START... FIN...

1 1

1 11 l

li FOOTAGE

lifroe1 1:: 2511 1 1 11 1 1 1

It1 1 1 11 1 1 11 1 1 11 11 1

i;1 1 1 11 1 1 11 1 1 11 1 1 11 1 1 11 1 1 11 1 1 1

:: 4851 11 11 1 1 11 1

1 1 1 11 11 1

:: 5291 1 1 11 1 1 11 1 1 1

!!1 1 1 11 11 1

li1 11 1

1 11 11 11 1

1 11 1l!1 11 11 11 1

1 11 1

1 11 |

.'11 11 1

1 1

i!

to

485

529

589

589

DESCRIPTION

INTERCOLLATED ANDESITE FLDUS AND TUFFS

-flovs ussive fine grained, lediiu green-up to 31 quartz stringers-tuffs chloritic and silicified with distorted foliation-quartz knots or boudins found along distorted foliation-weakly carbonatedquartz stringers at no preferred orientation-trace pyrite

TALC CHLORITE SCHIST

-highly deforced crennulated schist - tediui green-quartz carbonate stringers and quartz boudins throughout - toderately

carbonated - trace pyrite

INTERMEDIATE TUFF - OLIVE TUFF

-well foliated C. A. 43 degrees-grey-black in colour moderately carbonated-silicious, fine grained, with up to 2Z pyrite-Olive quartz vein at 567 - 2Z po, cpy, py

END OF HOLE: Acid test: 300' - 65 degrees589' - 61 degrees

1

1

SAMPLE

no.

122123124125126127128129130131132133134135136137138139140141

142143144145146

froi

251254265291316325337355379398402410435459462476483505519524

529556576581586

i j

to

252256271296320329339359382402406411439462476482488510524529

534557581586589

length

1'2'6'5'4'4'V4'3'4'4'1'4'3'12'6'5'5'5'5'

5'1'5'5'3'

}

ASSAY

AU ippb's!nil 1nil1010nil26530nilnilnilnilnil1010nil10nilnil1020

nilnilnilnilnil

Page 56: 52C15SE0014 Olive Mine

r!! DIAMOND DRILL RECORDi! If t. dio iaziil! PROPERTY.... OLIVE MINE 10 -65 i TOWNSHIP.. ..LITTLE TURTLE LAKE AREA HOLE I.... 87-3i! f^fl NUMBER.... K-475146 1300 -65! COLLAR CO-ORDINATES..,. 5770N. 41B5E TOTAL LENGTH.... 597'l! ORIENTATION ....DUE SOUTH !597 -59 i COHPAN Y.... NORONT RESOURSES LTD. SHEET I.... 11! LOGGED BY.... E. LUDUIG CORE SIZE.... BO CORE LOCATION.... ON SITE DATE START... FIN...

i!

!! FOOTAGE1 11 1

iifroil ;i i T"1 11 1

II 19i!1 l

!!1 1 1 11 1;i1 1 1 1:: 77.51 1

i i1 11 1i i i rt l

! il l i f

11105.5i f l 1

t!1 1 1 11 1 1 11 1 1 1! i i11132.5!!1 1 1 11 1 1 11 11 1 1 11 11 1l!jj1 11 i 1 1i! 1951 1 1 1

i!"i!1 1

i!i!1!

1 1

to"li"

77.5

105.5

132.5

195

223

DESCRIPTION SAMPLE

.

no.

OVERBURDEN

INTERCOLLATED BIOTITE AND CHLORITE SCHISTS 147148

-C.A. 39 degrees at 46 149-biotitic sections contain up to 51 pyrite 150-weakly carbonated 151-31 quartz stringers throughout !152-foliation distorted towards lower contact i 153

i 154FAULT AND DEFORMATION ZONE i 156

!157a-77.5-79 fault gouge brown oxidized !157b-2-5Z pyrite within unit i 158-unit highly carbonated along irregular fractures 1159Multiple distorted quartz stringers i 160- ainly chlorite present !161

1162INTERCOLLATED ANDESITE FLOWS AND TUFFS i 163

i 164-flows ussive, ndiui green '165-21 quartz stringers, weakly carbonated 1166-tuffs have distorted foliation with quartz boudins and 1Z pyrite, i 167traces of cpy i 168

i 169INTERCOLLATED BIOTITE AND CHLORITE SCHISTS i 170

1171-C.A. 41 degrees at 184 . i 172-5Z quartz stringers, oderatily carbonated i 173-up to 31 pyrite i 174-porphry dykes at 183.7-186, 189.8-192.3 .'ITS

i 176i 177117811791180

BUARTZ FELDSPAR PORPHRY i 181i 182

-brownish grey latrix, Mdiui to fine grained i 183-weakly carbonated, up to 1Z pyrite 1184-phenocrysts up to 1/4" and are well foried i 185-phenocrysts plagioclase in composition !I86-li nor quartz stringers containing biotite flakes i 187

5. .

.

fro*

19242934394449545964697480869196101107112117122126130134138143148156161166171177182187192197202207212217222

to i lengthjj

242934394449545964697480869196101107112117122126130134138143148153161166171177182187192197202207212217222227

5'5 r5'5'5'5'5'5'5'5'5'6'6'5'5'5'5'5'5'5'4'4'4'4'5'5'5'5'5'5'6'5'5'5'5'5'5'5'5'5'5'

ASSAY

AU.ppb's

6030nilnil10nilnilnilnilnilnilnilnilnilnilnilnilnil3010nilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnil

i!

Page 57: 52C15SE0014 Olive Mine

DIAMOND DRILL RECORDft. idio Eazii!

PROPERTY.... OLIVE HINE ! ! l TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE I.... 87-3/^^ H NUMBER.... ;-'i.-'iv.- ! ! | COLLAR CO-ORDINATES.;./ v - ~ -- TOTAL LENGTH....UnENTATI ON ....DUE SOUTH i i ! COMPANY.... NORONT RESOURSES LTD. SHEET I.... 2LOGGED BY.... E. LUDUIG CORE SIZE.... BD CORE LOCATION.... ON SITE DATE START... FIN...

t" H. . -. : ,-. '. .

FOOTAGE

froi""223"

484

to

484

597

597

DESCRIPTION

INTERCALATED ANDESITE FLOWS AND TUFFS

-flows lassive, lediui green, weakly carbonated-41 quartz stringers, with 51 pyrite-tuffs are distorted with quartz boudins-C. A. 20 degrees at 384-froi 474-484 tuffs becoie talc-chlorite schists with highlycrennulated foliation

INTERMEDIATE TUFF - OLIVE TUFF

-well foliated, C. A. 32 degrees at 525-grey-black, uderately hard,-well carbonated, extreee along fractures-silicious, fine grained with up to 21 pyrite-Olive Vein froi 561.8-563 with 151 po. cpy and py-550.5 fracture and silicified zone illustrated tay quartz-carbonatestringers at irregular angles

END OF HOLE Acid test: 300, 65 degrees597, 59 degrees

-

1

SAMPLE

no."iii~18919019119219319419519619719B

froi~227~~

257262324335422467472485558567

to~232"

262267327338424472477487563571

l

length...

5'5'3'3'2'E,

5'91

5'4'

ASSAY

AU.ppb'snilnil10nilnilnil30nil300.107nil

1

.

oz/ton

i!

Page 58: 52C15SE0014 Olive Mine

r

r

r

r

r

DIAMOND DRILL RECORD .........,............................ ____ !ft. IdiD lazii!

PROPERTY.... OLIVE NINE i 1-65*1 i TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE I.... 87-4(~*9 NUHBER....K-475146 i l l i COLLAR CO-ORDINATES.... see 'blan ' ' u' '^ TOTAL LENGTH.... 599'DkitNTATION ....DUE SOUTH ! ! ! ! COMPANY.... NORONT RESOURSES LTD. SHEET I.... 1LOG6ED BY.... E. LUDUI6 CORE SIZE.... BO CORE LOCATION.... ON SITE DATE START... FIN...

t , . - ;. .

FOOTA6E

froiT"

27

127

142

to~27~~

127

142

239

DESCRIPTION

OVERBURDEN

INTERCOLLATED BIOTITE AND CHLORITE SCHIST

-defoned froi 27-59' - distorted foliation, trace pyrite cubes, linorr-2* quartz carbonate stringers

-up to 1Z pyrite through remainder of unit-appears lore sericitic (rot 81.2-86 and silicified-grey siliceous rock froi 86-89.5 - 31 diss. pyrite

ANDESITE FLOW AND TUFFS

- i nor quartz stringers parallel to foliated sections-trace pyrite, soft lediui green-foliate sections C.A. 43* !-siiilar to other descriptions

QUARTZ FELDSPAR PORPHRY

-chlorite and biotite groundmass, lore Kspar in unit rather thanplagioclase alone as in other descriptions-sow granitic fragments-highly carbonated, iinor chlorite slips up to 1'-fracture zone: 173.5-179 with quartz veins

SAMPLE

no. ! froiii iii

199 l 27200 i 31.9201 i 36.3202 l 41.5203 l 46204 i 50.8205 1 55.5206 i 81.1207 i 87.4208 i 103209 i 110210 i 115211 i 119.5212 i 124.4213 i 129.2214 l 134.4

l 1

1 t 1 1

!1

215 i 139.5216 i 144217 i 149218 i 154219 i 156220 i 162221 i 167222 i 171.7223 i 176224 i 181225 ! IBS226 l 190.2227 i 194.8228 i 200229 i 204230 i 209.1231 i 214232 i 219233 i 224

l 234 i 228i 235 i 233.5

J i1 '

to llengthHHH

31.936.341.54650.855.558.287.492.1105115119124.4129.2134.4139.9

i

144149154158162167171.7176181185190.2194.8200204209.1214219224228233.5239

___

4.94.45.24.54.84.72.70*34.7254.54.94.85.25.5

11

4.5S54454.74.3545.24.65.245.14.9D545.55.5

ASSAY

AU.ppb's

nilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnil

1

nilnilnilnilnilnilnilnilnil20nilnilnilnilnilnilnilnilnilnilnil

'

1

1

' " ~*"*

11

j

Page 59: 52C15SE0014 Olive Mine

1 1 DIAMOND DRILL RECORD:: ift. IdiD iazii!i! PROPERTY.... OLIVE NINE i i l l TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE I.... 87-41 1 ^^^f^|1 1 r r NUMBER.... * i i i i COLLAR CO-ORDINATES.... ' - TOTAL LENGTH....l! foiiENTATION ....DUE SOUTH i i l l COMPANY.... NORONT RESOURSES LTD. SHEET I.... 2II LOGGED BY.... E. LUDUIG CORE SIZE.... BB CORE LOCATION.... ON SITE

1 l l li!~"

ii! FOOTAGE ! DESCRIPTION1 1 1

II froi; j11 2391 l

1 1l i

1 1 1 t

1 1 1 1

1 1 1 1

II 2631 1 1 1

iiII1 1 l 1

1 1 l 1

:: 283i i i i1 1 1 1i i i i1 1 i ii i i i

II 4991 1 1 1

i!1 1 1 1

l l

1 1516.2i!!!i!1 11 11 1 1 11 1 1 1

1 1 1 11 11 1ii1 1 1 11 1 1 11 1 1 11 1 1 11 1 1 11 1 1 11 1 1 1

ii;;1 11 1M

to 11

263 1 ANDESITE TUFFS AND FLOWSji -siiilar to other descriptionsi -lassive flows, tediui green, soft chloritic, 1-2Z pyrite tuffsi C. A. 37* at 242*!

283 i FAULT AND DEFORHATION ZONEi it Saie as descriptions in holes 213! -quartz veins froi 276.2-2781 282.5-283.11 1

499 1 ANDESITE FLOWS AND TUFFSji -quartz vein froa 460 to 464 with up to 30Z diss. po. py and cpy! well carbonatedi -trace to 31 diss pyrite cubes with in uniti i

516.2! TALC CHLORITE SCHISTii -highly deforced and contorted! -becomes crennulated towards lower contact1

599 1 INTERMEDIATE TUFF11

! -Olive vein at 569.0-569.5l -C. A. 44* at 535'i -Siiilar to previous descriptionsi

599 l END OF HOLE

1 Tests: 300' : 61*l 599' : 58*ii iiiii '

iiii

i

j1 1

DATE START... FIN...

SAMPLE -..--.-....-.-ll ,......

no. i froi i to1 1

236

237238239240241242243244245246

247248249250251252253254255256257

248.2

263268272.9278294.3369.1414418.6455.6460.5

466479484489494535560565571576580

253.5

268272.9278283295.8375418.6423.4460.5466

469.4484489494499540565571576580584

i

length

5.3

54.95.151.55.94.64.84.95.5

3.45555556544

.

ASSAY

Au.ppb's nil

nilnilnilnilnilnilnilnil100.178

oz/ton80nilnilnil30nilnilnilnil20nil

CuJP*'s

1020

Zn

50

!~- l!

Page 60: 52C15SE0014 Olive Mine

! DIAMOND DRILL RECORD ........^ .^...^..^...!ft. Idip lazii!

PROPERTY.... OLIVE HINE i -65" i ! TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE I....B7-5fit! NUMBER.... K-475146 l ! ! COLLAR CO-ORDINATES.... 5770N. 3B85E TOTAL LENGTH. . . .-609' i -ORIENTATION . . . . DUE SOUTH i ! l COMPANY. . . . NORONT RESOURCES LTD. ' ' ~ SHEET t. . . . lLOGGED BY.... E. LUDUIG CORE SIZE.... BD CORE LOCATION.... ON SITE DATE START... FIN...

FOOTAGE

froi

0

14

109

122

203

256

5B4

Sii!1 1l 1

||1 | 1 1

to

14

109

122

203

256

584

688

688

DESCRIPTION

OVERBURDEN

INTERCOLLATED BIOTITE AND CHLORITE SCHISTS

-C. A. 43* at 87-21 quartz stringers-up to 21 pyrite-weakly carbonated

OUARTZ FELDSPAR PORPHRY

-2-5Z pyrite-sericite developed along fractures-grey in colour, stall unifori phenocryst 5 of quartz and plagioclase-carbonated along fractures and with quartz stringers

INTERCOLLATED BIOTITE AND CHLORITE SCHISTS

-sue as above unit-C.A. 45* at 155

QUARTZ FELDSPAR PORPHRY

-siiilar to unit above only larger phenocrysts- ore quartz stringers, weakly carbonated

INTERCOLLATED ANDESITE FLOWS AND TUFFS

-flows lassive, wdiui green-weakly carbonated-21 quartz stringers with trace pyrite-froi 566-584 unit is talc chlorite schist-C. A. 31* at 525

INTERMEDIATE TUFF - OLIVE TUFF

-unifori unit as logged previously.-21 pyrite-C. A. 68* at 590 and 70* at 680-Olive vein at 667 - 11 po and py

END OF HOLE

SAMPLE

no. i f roti ii i

386 i 14387 l 18388 i 22389 i 82390 i 87391 ! 109392 i 114393 i 118394 i 137395 i 142396 i 146397 l 151398 i 156399 i 158400 l 164401 1418.8402 1455.5403 S460.2

1 1

404 i 560405 i 566406 i 572407 i 576408 i 581409 l 603410 i 651411 i 656412 i 660413 i 665414 i 671415 i 675416 l 678

t 1

11

j1

!ii

iAcid Test: 325 : 63* i i

688 i 55* ! i! i

j j

to

1822278796114118121142146151156158164171422460465.7

564572576581584606656660665669675678684

length

4t5B

9543e

4552473.24.55.5

4645335454436

HHVMH

Au.ppb's

nilnilnil10nilnilnilnilnilnilnilnilnilnilnilnilnil

ASSAY

Cu i Zn.ppb'sippb's

0.096 11230oz/toni135 inilnilnilnilnilnilnilnilnilnil10nil

t - .

45500

4.5Z

.

Page 61: 52C15SE0014 Olive Mine

rDIAMOND DRILL RECORD

PROPERTY...ft. idio lazii!

.OLIVE MINE !-65*: i TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE t.... 87-6r^H NUMBER.... K-475146 l ! l COLLAR CO-ORD I NATES...,' , - . ~. TOTAL LENGTH.... 609'k.cNTATION ....DUE SOUTH i ! ! COMPANY....NORONT RESOURSES LTD. SHEET i.... 1LOGGED BY.. .. E. LUDU16 CORE SIZE.... BQ CORE LOCATION.... ON SITE DATE START... FIN...

"'' -- V - - ' - -'

FOOTAGE

froi

0

8

22

147

223

259

560

577

to"i

22

.

147

223

259

260

577

609

DESCRIPTION

"oVERiuRDEN

ANDESITE FLOW

- assive, aediua green, einor pyrite-extremely carbonated-fine grained, occasional quartz stringer

INTERCOLLATED BIOTITE AND CHLORITE SCHISTS

-siailar to previously logged unit-lack of sulfides, trace pyrite-C.A. 46* at 140

INTERCOLLATED ANDESITE TUFFS AND FLOWS

-foliation of tuffs less distorted C.A. 39* at 210'-no observed sulfides in unit-siiilar to unit in other holes-very few quartz stringers

QUARTZ FELDSPAR PORPHRY

-brownish grey eatrix, strongly carbonated-trace pyrite, ainor quartz carbonate stringers-becoKS fine grained towards bottoa of hole

INTERCOLLATED ANDESITE TUFFS AND FLOYS

-85Z flows, Kdiui green aassive - weakly carbonated - siiilar to unithole - 21 pyrite associated with quartz stringers - foliationdistorted in tuffs - silicified zone froi 494 to 502, light greenepidote alteration, 10Z quartz stringers-fracture zone with fault gouge froa 509-535 no pyrite or carbonate-fault at 529

TALC CHLORITE SCHIST

-crennulated laiinations of chlorite with talc

INTERMEDIATE TUFF - OLIVE TUFF

! -up to 31 diss. pyrite cubes between 580 and 5941 -uny quartz stringers throuth the above section C.A. 47* at 580i -Olive vein 601-602 1-2X pyritej

609 S END OF HOLE Acid test i 63* at 300' 54* at 609'

SAMPLE

no.___

417418419420421422423424425426

froa i to i length___

11172228489493498525570600

l

___

14222834493498503530575605

q

566j

6J

5J

5

ASSAY

Au.ppb's

nil10nilnilnilnil130nilnilnil

1

___

::

Page 62: 52C15SE0014 Olive Mine

rDIAMOND DRILL RECORD

r

r

rr

1 1

!! f^ERTY...ift. diQjazii

.OLIVE NINE i -65" l TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE i.... 87-7!! tUJM NUMBER.... K-475146 i l COLLAR CO-ORDINATES. .".. ' TOTAL LEN6TH....600l! ORIENTATION ....DUE SOUTH i ! COMPANY.... NORONT RESOURSES LTD. SHEET i.... 1i! LOGGED BY..1 t

.. E. LUDUIG CORE SIZE.... BB CORE LOCATION.... ON SITE DATE START... FIN...

1 1 1 1

i! FOOT1 t1 t -- - ,

"fro! 1 1:: o:: :: 41 1 1 11 1 1 11 1 1 11 1 1 1

:: 12

1 1

1 1 1 1

:: B31 11 11 1 1 11 1 1 11 1 1 11 1 1 1

i: IB?1 1 1 11 11 11 1 1 1i:1 1 1 1

:: 551

i:1 1 1 1

l!1 11 1

1 1 1 1

,'i

1 1 1 l

1 1 1 1

1 1 1 l

!!

1 1 1 1

1 1 1 1

i!

AGE

to

4

12

83

f

167

551

600

600

DESCRIPTION

OVERBURDEN

ANDESITE FLOU

- assive, carbonated, linor quartz stringers -fine grained, tediui green

INTERCOLLATED BIOTITE AND CHLORITE SCHISTS

-siiilar to unit logged in other hole -non-carbonated, very few quartz stringers C.A. 42*at 45- nil sulfides

OUARTZ FELDSPAR PORPHRY

-quartz vein breccia froa 98-104 -41 pyrite extremely carbonated -porphry siiilar to unit logged in other holes -reiains coarse grained (phenocrysts)

'INTERCOLLATED ANDESITE TUFFS AND FLOPS

-tultiple quartz stringers through out - assive green, fine grained flows -tuff beds alMst totally chlorite, 1-2* beds -wiakly carbonated

INTERMEDIATE TUFF - OLIVE TUFF

-C.A. 42* at 575-Olive vein: wltiple stringers between 564-567 3-5Z diss. pyrite in vein -upper contact gradational with talc-chlorite schist

END OF HOLE Acid Test: 300' - 62-600' - 57-

SAMPLE

no.

427428429430

froi

9298280562

to

98104285568

length

6654

ASSAY

Au jipb's

nil90nilnil

Page 63: 52C15SE0014 Olive Mine

!! DIAMOND DRILL RECORD

P^ERTY... L.iN NUHBE

!ft. idio iazii!.OLIVE HINE l i-65"! ! TOWNSHIP.... LITTLE TURTLE LAKEIR....K-475146 i l l i COLLAR CO-ORDINATE5....L7+30U/

AREA HOLE I.... 87-8 5+45N TOTAL LENGTH.... 787'

ORIENTATION ....DUE SOUTH III! COMPANY.... NORONT RESOURSES LTD. SHEET i.... 1L066ED BY..

FOOTAGE

froi

0

37

242

275

509

545

578

to

37

242

275

509

545

578

787

787

.. E. LUDUI6 CORE SIZE.... BO CORE LOCATION.... ON SITE DATE START... FIN...

! l l

DESCRIPTION i ii no.

__ ____ ___ . _____ I.. ..OVERBURDEN i

i

INTERCOLLATED BIOTITE AND CHLORITE SCHISTS i1 1

QUARTZ FELDSPAR PORPHRY i

INTERCOLLATED MAFIC TUFFS AND FLOUS i1 1

INTERMEDIATE TUFF - OLIVE TUFF li

-no quartz veins !

ANDESITE FLOH i

INTERMEDIATE TUFF - OLIVE TUFF i 431i 432

-Olive vein at 708-710 !-C.A. at 42* at 710 ' !

l. i

END OF HOLE Acid Test: 400' : 60* !787' i 55- !

1

1 1

1

1

l

l 1

!l

l

1

!f tt

t 9

\t

t t

t

t

l

11

l

SAMPLE

"froi to""ilengfh

600707

615712

155

'

"AU"".ppb's

90nil

i i

ASSAY

!

Page 64: 52C15SE0014 Olive Mine

rDIAMOND DRILL RECORD

PROPERTY....'ft. IdiD lazii!

.OLIVE NINE i 1-45"! i TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE I.... 87-9/*"MH NUHBER.... K-475146 i i l i COLLAR CO-ORDINATES....!V .cNTATION ....DUE SOUTH l i i l COUP ANY.... NORONT RESOUfiLOGGED BY.. ,. E. LUDHIG CORE SIZE.... BQ CORE LOCATION.... ON SITE

ee'ipian '' - TOTAL LENGTH.... 400' SES LTD. SHEET I.... 1

DATE START... FIN...

FOOTA6E

froi

0

82

108

203

i 3051

t

:

311

8l!i!i!1 1 1 1

to

82

108

203

305

311

399

399

DESCRIPTION

OVERBURDEN

BANDED OXIDE IRON FORMATION

-intercollated with pink-red schists (altered arkose)-pyrite in distinct bands parallel to lagnetite bands- agnetite in up to 1* bands-sulfide content: 20Z- i nor carbonate in arkosic uterial, lainly in fractures-traces of pyrite in arkosic bands

ANDESITE FLOUS AND TUFFS

-invaded by narrow (6") porphry dyklets, svaris-di BS. py. and cpy froi 136-137.5 up to 15Z-variable foliation-porphry dyke contacts variavle - grade into volcanics

INTERCOLLATED BIOTITE AND CHLORITE SCHISTS

DIORITE

-fine to lediui grained-trace pyrite, equigranular, irregular contact

6REY IIACKE

-very siliceous, trace to 21 pyrite-C. A. 50* at 330'-deforKd for 379-399 41 po, cpy froi 395-399

END OF HOLE Acid test 42- at 399'

!!:ii

i!li"

no."MO29129229329429S29629729B29930030130230330430530630730B30931031131231331431531631731B319320321322323324325326327328329330331332333334335336337338

SAMPLE

frw"if"879297102107124133136143162178.5184189195199205210215221225237243247265270277282287292297302307312317322327332337342347352357362367372377382390

to"I?""

9297102107110129136141145166184189190199205210215219225230243247253270273282287292297302307312317322327332337342347352357362367372377382390399

iBngth~5

555525*

5245.5514655445646535555555555555555555538jo

ASSAY

Aujpb's1030202030nilnil1107010nil20201020nilnilnilnil10nilnil101010nil30nilnil1010nilnilnil10nil1025nilnil10nilnilnilnilnilnilnilnil !

HH*

*

1

Page 65: 52C15SE0014 Olive Mine

DIAHOND DRILL RECORD

r

:: PROPERTY...!ft. din lazii

.OLIVE NINE i -45*! TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE I.... 87-10l ! PHWI NUMBER. . .'.' : " " * ! ! COLLAR CO-ORDINATES. . ,. v.. .---..--v - TOTAL LENGTH.... 299'

i! L STATION ....DUE SOUTH i i CONPANY....NORONT RESOURSES LTD. SHEET I....1i! LOGGED BY.. .. E. LUDUIG CORE SIZE.... BO CORE LOCATION.... ON SITE DATE START... FIN...

1 1

1 I1 I

:: FOOTAGE1 11 1

llfroi1 1 1 1

:: o:: 54::1 1 1 11 1 1 1:: 1201 1

\\1 11 11 1 1 11 11 1 i i

1 11 1 1 1

:: 1691 1 1 11 11 11 1 1 11 1 1 11 1 1 1

11186.5li1 11 1 1 11 11 1 1 1M1 |

1 1

:: 23i1 11 1

i!

1 1

1 1 1 1

1 1 1 1

1 t

| J

! l1 1 1 111262.41 1 1 1

!!1 1 1 11 11 1 1 11 11 1

to

54120

169

186.5

231

262.4

299

299

:: :

DESCRIPTION

OVERBURDENINTERCOLLATED FINE GRAINED TUFFS AND FLOUS-foliated, ei nor carb. OZ -) trace py cubes- inor silicified sections

1

FINE GRAINED SILICIFIED SCHIST (ALTERED PORPHRY) (QUARTZ-EYE TUFF)-intercollated with chlorite schists (tuffs ?) silicified- near top 10'-each porphritic section has a 1' wide carbonated Diorite leader-Diorite Schist -120-121 121-123 light brown silicified intercollatedwith tuffs-Diorite schist-125-126, porphry 126-130(siiilar to other qtz-eye tuff)- inor fractures - carb, with chlorite-sericite parting planes-this appears as a qtz.-eye tuff

HAFIC-MNTERHEDIATE TUFF-porphry at 174.8-176-qtz-eye selicite schist - qtz eyes and knots in utm of sericite-OZ - trace sulfides-C.A. tuffs 54*

DIORITE - GRANODIORITE INTRUSIONS-weak to loderated carb. - trace - OZ sulfides-pyroxenes - altered to chlorite-centre of unit is granodiorite - grades into diorite again-epidote, Kspar, Nag., Cbl., Quartz- oderate foliation 5,82 - developed-bottoi of unit becoies lore intercollated with sil-chl. schists

BANDED OXIDE (NAG.) IRON FORMATION INTERCOLLATED-with aetagreywacke's and ieta Arkose icibers (ser. schist)- SIM ashole 19 - bands of Fe average between 1/I6M/2* with pyrite developedalong foliation between Fe and Arkose (Gwke)

-C. A. at 60*-dip becoHS flatter towards little Turtle lake- inor py in Arkose and Gwke - lightly Carb.-Arkose - Pink - light pink - beige-quartz blebs in Fe For aa t i on

INTERCOLLATED PORPHRY DYKES AND MAFIC TUFFS AND ANDESITE FLOUS-tuffs could be interflow sediments-sau as hole 19

END OF HOLE Acid Test s 300' - 42*

SAMPLE

no.

339340341342343344345346347348349350351352353354355356357358359360361362363364365366367368369370371372373374375

fro*

545963. B68.874.878.673.488.09397.7102.3106.9112117122126.3131.8136141146151155160165170175179183189194198203.6208213218222.5227.5

376 l 231.8377 i 236.7378 l 241.5379 l 246380 ! 251381 l 255.5382 l 260.1383 ! 384384 l 389

to l length

5963.868. B74.878.673.48B.O93.097.7102.3106.9112117122126.3131.2136141146151155159165170175179183189194198203.6208213218222.5227.5231.8236.7241.5246251255.5260.1262.8389393

ill! i 385 : 393 i 399

ASSAY

Auppb's"nil

nilnilnilnilnilnilnil10nilnil1010nilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnilnil10nilnilnilnil

i:

Page 66: 52C15SE0014 Olive Mine

DIAMOND DRILL RECORD ..^^ .

PROPERTY...ft. idio iazii!

.OLIVE NINE :-45-!180-: TOWNSHIP.... LITTLE TURTLE LAKE AREA HOLE t.... 87-11P-MH NUMBER.... 629006 i l ! COLLAR CO-ORDINATES.... Li JNTATION LOGGED BY..

....DUE SOUTH : : : : COMPANY... . NORONT RESOUR.. E. LUDUIG CORE SIZE.... BQ CORE LOCATION.... ON SITE

. V

FOOTAGE

froi

0

7

170.8

186.5

195

307

328

i

;;::

to

7

170.8

186.5

195.0

307

328

401

i 401

-9tOOU,15*75U TOTAL LENGTH.... 401' SES LTD. SHEET I.... 1

DATE START... FIN...

——————————— .

DESCRIPTION yKK SAMPLE

Q-' jrtOVERBURDEN O^ O^TT V^

\/ ry .v Jq QLT' ' MAFIC (ANDESITIC) FLOHS \Jf \J* //k -fine-ied. grained S t^^ *? -•inor qtz stringers, CO, in stringers p ffi ! ;-no sul f ides {^-foliation t 22.0' it 27* to C.A.-linor foliation alteration-47-93.1 FRACTURE ZONE-qtz fracture zone-top of unit larked by stringers and py.-bottoi of unit lore deforied, foliated with quartz stringers-quartz veins vith up to 351 po, cpy ,py-SiO, veins 1 74.5'-6'

fcpy 77.0' to 80.0'82.5' to 85.2'

-irregular contacts - no C.A.-quartz fracture zone linor sulphides C 113.0 to 118.5 trace py-Si Da stringers-Pillows i Flow top Breccias C 113' to 133'

FINE GRAINED SILICEOUS UNIT FELSIC TUFF-pink siliceous nodules C 176.5 to 177'-fine grained, grades froi green chlorite rich to black biotite rich-no sulphides, weak carbonate along foliation 1 50* to C.A.

HIGHLY DEFORMED IRON FORMATION - 01 IDE-thin 1/2* bands Fe, blebs of Py-qtz stringers norial to C.A.-pyrite bands parallel to foliation with assoc. SiO, stringers-fractured

MAFIC INTERMEDIATE FLOWS-intercalated with sow tuffs

MAFIC TUFF-chl-ttiotite schists-315 to 320.8 - 10Z diss. py, po t cpy along foliation planes-•i nor SiOa, stringers t C0t

MAFIC VOLCANICS t TUFF-saie as 195 to 307 1 365 feet increase of sulphides, po, cpy, py-•i nor Si Da, CO* stringers-possible shaft vein

END DF HOLE

.—. ,•i ' -'

! '

;

.

,. ~ 1

^ v-;.^ --.. "~f

J'..- ;

1-*

J-.'-•:: \

' '-'

1 - - ."

.

-.

. '

-

" r ?

'".^•':' 'i -- ' ' L

.T "

to

1 ' v -!

• ' ' -

,

1

1 -

' - '

- """J./f-V ,

:'A ;: , ~

" ' •...^ .

'"'"~ '

' '-•'"' ~-

length

...—ASSAY

-

l" N"

i

'- . -

11 . ;

i

\

'" ! '"

v, -

V

, -

.

-

ii

Page 67: 52C15SE0014 Olive Mine

L

r

APPENDIX : B

ASSAYS

r

Page 68: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705)642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

(Zfcrttftrat? nf Atmlgtfa

Certificate No. 66788 Date: June 12. 1987

Received June 7, 1987 58 Samples of

Submitted by Noront Resources Ltd., Toronto,

Samples per E.

SAMPLE NO.

R-053432^ 05344

Second Pulp^*** 05345

i 05346z 05347^ 053484 05349^ 05350fe 05351

- 1 053525 05353

- ^ 05354tc 05355i' 0535613. 05357if 05358

~ i-s- 05359

ffc 05360- n 05361

1 8 05362^

GOLDPPB70

6860/59705490/54903290 -1-0-

10NilNilNilNilNil10

Nil70

240Nil20

NilNil2330/2950Nil20

Ludwig

SAMPLE NO.

R-05363053640536505366

22- 05367^ 05368"^ 05369^ c 05370z** 0537 1~~i 05372-z** 05373

?*( 05374^ 05375^i 05376^i 05377^ 05378•^ 05379^ 05380^^ 0538137 05382

Ontario.

GOLDPPBNilNilNilNil2020HO/1407020

NilNilNil10/Nil

NilNilNilNilNilNilNil

Split Core

SAMPLE NO.

^ R-05383^ 05384^- 05385^. i 05386**\*- 05387^^ 05388"H 05389^B 05390

^ 0539 l^^ 05392^*i 05393^ 05394^~ 05395^i 0539652 0539753 05398

^ 05399S^ 05400

A^lPPT ^ W /r

GOLDPPB

Nil

Nil103020750/7503080

NilNilNilNil10

NilNil10

NilNil

•77vW

G. Lebel - ManagerESTABLISHED 1928

Page 69: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Ckrttftrate of Analgata

Certificate No. 66849

Received June 11, 1987 34

Submitted bv Noront Resources Ltd.,

Samples per E.

SAMPLE NO.

^ R-5401-37 5402

54035404540554065407540854095410541154125413541454155416

T2- 5417

Ludwig

GOLD PPBNil30/20

NilNilNilNilNilNilNilNilNilNilNilNilNilNilNil

Date:

Samples of Split

Toronto, Ontario.

SAMPLE NO

7^ R-54187" 5419

"i ^ 5420

~l± 5421

7-7 5422-7*5 5423

54245425542654275428

GA 5429fc^ 5430

"^ 5431^'' 5432

^ 5433'^ 5434

June 17, 1987

Core

GOLD PPBNilNilNil30/10

Nil30

NilNilNilNilNilNilNil10

NilNilNil

ESTABLISHED 1928G. Lebel - Manager

Page 70: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Cfcrtiftratp of AttalgaiB

Certificate No.

Received June

Submitted by

SAMPLE NO.

C\C- R-5435543654375438543954405441544254435444544554465447544854495450545154525453

l~c\ 5454

66868

14, 1987 55

Date:

Samples of Core

June 17, 1987

Noront Resources Ltd., Toronto, Ontario.

Samples per E.

GOLD PPB140/150NilNil2010

NilNil1030101010

NilNilNilNil30

Nil1010

Ludwig

SAMPLE

H? R-54555456545754585459546054615462546354645465546654675468

uM 54695470547154725473

W 5474

NO. GOLD PPB

Nil iNil10

NilNil10/Nil

NilNil (Nil iNil 'Nil 'Nil fNilNil1010

Nil260/27030

Nil

SAMPLE NO.

^ R- 5475,-,, 5476^- 54771 "^ 5478r~v 5479'^ 54801V(- 5481

^ 5482** 5483

5484^ 5485rt. 5486^ 5487i 1-'-} 5488

I^H 5489

GOLD PPBNilNilNilNil1010

Nil10

NilNil1020

NilNilNil

ESTABLISHED 1928G. Lebel - Manager

Page 71: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

(Eertfftrat? nf

Certificate No. 66954 Date: June 25, 1987

t -

r

r-

r-

*

rit —[

rt —r—ir.

r ~~

-~

,—

Received June

Submitted by

SAMPLE NO.

M1^ R-5490

H c, 5491\^1 54921^ 5493W* 5494i^'0 5495

i^\ 54961^-0- 5497i^ 5498\54 5499i'35' 5500

S-50015002500350045005500650075008

itfe 5009

19, 1987 78

Noront Resources Limited,samples per: E. Ludwig

GOLD PPBNilNil50/7030NilNil10-.

NilNilNilNilNil-

NilNilNilNilNilNilNil30/1,0

Samoles of solit core

Toronto. Ontario

SAMPLE NO.

i^ S-5010501150125013501450155016501750185019502050215022502350245025502650275028

lsEs 5029

con 't...

P.r Xl/

GOLD PPB10NilNilNilNilNilNilNilNilNilNilNilNilNilNil/30NilNilNilNilNil

' '^JUESTABLISHED 1928

G. Lebel, Manager

Page 72: 52C15SE0014 Olive Mine

CartUlnata No. 66 954

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Gfcrtifirat* of AnaluBtHt^f Q M

SAMPLE NO.

S-50305031503250335034503550365037

'M- 5038

'^ 5039Kit- 5040

fen 5041 second pulp

ire 5042

50435044504550465047

.^.-A 5048

GOLD PPB

NilNilNil10NilNilNilNil30Nil303440/3220 4390NilNilNilNilNilNilNil

SAMPLE NO.

~-* S-5049

50505051505250535054

505550565057505850595060506150625063506450655066

^ 5067

GOLD PPBNilNilNilNilNilNilNilNilNilNil/NilNilNilNilNilNilNilNilNilNil

Per.G. Lebel, Manager

ESTABLISHED 1928

Page 73: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS* CONSULTANTS

(ftrctiftrat? nf Analysts

Certificate No. 66988 Date: June 25, 1987

Received June 22, 1987 44

Submitted by Noront

samples per:SAMPLE NO.

•z?^ S-5068

50695070507150725073507450755076507750785079508050815082508350845085508650875088

^ s* 5089

2^-j 5090

Resources Limited,

E. LudwigGOLD PPB 10/30NilNilNilNilNilNilNilNilNilNilNil/NilNilNilNilNilNilNilNilNilNil1080

Samoles of split core

Toronto, Ontario

SAMPLE NO.

^* S-5091

50925093

•^ 50945095509650975098

Zc^ 5099^7 5100

2-^ 5101

51025103

**\ 5104•2.&Z. 5105z*s 5106*^t 5107zfi.'S 51087Z*~ 51092'tsn 5110

Zl 5111

..x!

GOLD PPB NilNilNil30NilNilNilNil20NilNilNilNil30370110350/260140NilNilNil

s;rf Pi f1 ^f 41 ' If^/k/l

G. Lebel, ManagerESTABLISHED 1928

Page 74: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

titertiftrat? of Analysis

Certificate No. 66988 - A Date: July 21. 1987

Received June 22, 1987 J_ Samples of Split Core

Submitted by Noront Resources Ltd.. Toronto, Ontario.

Samples per E. Ludwig

r

r

SAMPLE NO.

S-51045105510651075108

COPPER PPM

13501910309152264

ZINC PPM1071028310555

Per

ESTABLISHED 1928 6. Lebel - Manager

Page 75: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705)642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Qkrtifiratr of

Certificate No. 67118 Date: July 9, 1987

Received July 1, 1987

- Submitted by

SAMPLE NO.

JZt*^ S-51125113511451155116

- Zty 511751185119

ZTi 512051215122

Z^ 512351245125

ZT& 5126^ 5127^ 5128

51295130

Z*e,V 5131

60 Samolesof Split Core

Noront Resources Ltd., Toronto,

samples per

GOLD PPBNilNilNilNilNil80/90

NilNil

10NilNil

20NilNil

702010

NilNilNil

E. Ludwig

SAMPLE NO.

-^ S-5132mc 51332^ 5134z**- 5135**^ 5136?*H 5137

. 51382--*t, 5139•z*"7 5140

^ 5141z ew 5142^ 5143

**-*' 5144^2- 5145•*^ 5146-?^ 5H7"^^ 5148•s^t, 5149"^07 5150^ofc 5151

Ontario.

GOLD PPBNil

1030202030

NilNil110/1107010

Nil20201030/10

NilNilNilNil

Pe

'

SAMPLE NO.

•t^i S-51525153515451555156515751585159

^"- 5160

51615162

"*"i 5163^^ 5164

516551665167

^z^ 5168*2* 5169^- 5170-327 5171

//y. ,Xiv M

GOLD PPB

10NilNil

101010

NilNil30/30

NilNil

1010

NilNilNil

10Nil

1030/20

"If/K

ESTABLISHED 1928G. Lebel - Manager

Page 76: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

(Eertifirat* nf

- Certificate No.

Received July

~~ Submitted by

SAMPLE NO.

X* S-5172-30 5173

5174

517551765177517851795180

2* 518151825183518451855186518751885189

5^-1 5190

W* 5191

67119

1, 1987

Noront

GOLD PPBNil10

NilNilNilNilNilNilNilNilNilNilNilNilNilNilNilNil10

Nil

75

Resources Limited,

page 1 of

SAMPLE

^-^( S-5192^^ 5193-•5^ 5 j 94

5195519651975198519952005201520252035204520552065207520852095210

5A* 5211

Date:

Samoles of split core

Toronto, Ontario

2

NO. GOLD PPBNil ^1010

NilNilNilNilNilNilNilNilNilNil ^NilNilNilNilNilNilNil 3

con 't.

Per

July 14, 1987

SAMPLE NO.

* S-5212

52135214521552165217521852195220522152225223

si 5224522552265227

^ 522852295230

•BS- 5231

XU ' A/G. Lebel,

GOLD PPBNilNilNilNilNilNilNilNilNilNilNilNil10

NilNilNilNilNilNilNil

kAMana jer

ESTABLISHED 1928•l**

Page 77: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS* CONSULTANTS

67H9 Qkrtiftrat* of AttaluBta 2 of 2Certificate No __________ CT Page C UT c_________

-too

SAMPLE NO.

S-523252335234523552365237523852395240524152425243524452455246

GOLD PPB10

NilNilNilNilNilNilNilNilNilNilNilNilNil140/130

ESTABLISHED 1928

Per

6. Lebel, Manager

Page 78: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

Gtatifirat* of Analysts

r Certificate No. 67137 Date: July 22. 19fl7

Received July 3. 1987 29 Samples of Split Core

j Submitted by Noront Resources l imited, Toronho, Dntarin

SAMPLE NO.

-wS 5247

5248

5249

5250

5251

5252

5253

5254

5255

5256 •4^5" 5257-4-1 K* 5258

M-H 5259Mifc 5260

W* 5261

GOLD PPB

Nil -Uc

Nil

Nil

Nil Aft~*±

Nil

Nil

NilNil -4-2-?

Nil

Nil

10 -43*

Nil ^

Nil 4 z

10 H^S

Nil

SAMPLE NO.

1 5262

5263

5264

5265

5266

5267

5268

5269

5270

5271

5272

5273

5274

5275

GOLD PPB

Nil

Nil

Nil

130Nil

Nil

Nil

50

Nil

Nil

Nil90

Nil

Nil

Per

ESTABLISHED 1928G. Lebel-Manager

Page 79: 52C15SE0014 Olive Mine

SWASTIKA LABORATORIES LIMITEDP.O. BOX 10, SWASTIKA, ONTARIO POK 1TO

TELEPHONE: (705) 642-3244 ANALYTICAL CHEMISTS * ASSAYERS * CONSULTANTS

(Eertifirat? of Atralgaw

r Certificate No.

Received

66788 -ADate:

July 21, 1987

7 ' Samples of Split Core

Submitted by Noront Resources Ltd.. Toronto. Ontario.

Samples per E. Ludwig

r

r

r

r

SAMPLE NO.

R-053430534405345

COPPER PPM66710201230

ZINC PPM3855

45500

Per6. Lebel - Manager l

ESTABLISHED 1928

Page 80: 52C15SE0014 Olive Mine

r

r

APPENDIX : C

DIAMOND DRILL SECTIONS

Page 81: 52C15SE0014 Olive Mine

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Page 83: 52C15SE0014 Olive Mine

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Page 110: 52C15SE0014 Olive Mine

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Page 111: 52C15SE0014 Olive Mine

SURFALE I'ROJEtTIUN OF OLIVE

Page 112: 52C15SE0014 Olive Mine

81 -fO t*' .

TABLE OF FORMATIONSLEGEND

ORPHYRITIC

-- (jRANITE

LAIN POST

LAKE UR PUNU CLASTIC VOLCANIC ROCKS

STREAM OR BROOK

SWAMP OR WET AREA

- - FELSIC TUFFA) RHYOLITE TUFFB) LAPILLIS TUFF

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: --POWER l INF

SHAFT OR PITS

AREA OF BEDROCK OUTCROP

FAULT

FOLIATION

BEDDING

DRILL HOLES

QUARTZ VEIN

FeS 2 BANDS

•MAY - AUGUST 1987

/,c

i, - - - - -

2- --

- - - - - FOLIATED CHERTY TUFF (OLIVE TYPE)

INTERMEDIATE TUFFD) FELDS ASH TUFFE) QUARTZ-FELDS ASH TUFFF) CARB-FELDS. TUFFG) INTERMEDIATE TUFFH) aUARTZ-CARB TUFF

FELSIC VOLCANIC ROCKS

- - C) MASSIVE QUAR l/-LYE RHYOLITE fi) FOLIATED QUARTZ-EYE RHYOLITE

INTERMEDIATE VOLCANIC ROCKS

-- A) MASSIVE FINE GRAINED FLOWB) CARBONATED WEAKLY SHEAREDC) FOLIATED/SHEARED

MAFIC INTRUSIVE (FLOW) ROCKS- - A) COARSE GRAINED

B) FINE GRAINEDC) SHEARED

E. LUDWIG GEOLOGICAL CONSULTING

CLIENT: NORONT RESOURCES LTD.

PROPERTY: PRESTON - OLIVE PROPERTY

TITLE:

Map. 1Date: May 1987Drawn:

Scale: I M *40IInterp:

NTS:

Job No: 0-133

Page 113: 52C15SE0014 Olive Mine

S4Q(j N

\\\

Face

OPEN STOPE FROM SECOND LEVEL

STOPED TOSURFACE - BACKFILLED

INTERMEDIATE TUFF

STOPED FROM SECOND LEVEL\

52C15SE08M 63.B1B3 LITTLE TURTLE LAKE 810

o

7(f

SYMBOLS

ASSAY - OZ/TON ACROSS WIDTH IN FEET

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SURVEY PEG WITH IDENTIFICATION NUMBER

STRIKE WITH DIP

QUARTZ VEINING

FAULT

70i69*

J^

BACK SLASH * ?0'

S4QO M ''SHAFT

EVtL BLOCKED

Li Y WASTh

INTERMEDIATE TUFF

NORONT RESOURCES LTD.

OLIVE MINE PROJECT

FIRST LEVEL PLAN -60'

LITTLE TURTLE LAKE AREA

KENORA MINING DIVISION

BY'. E.LUDWIG

MARCH 25,1987l" * 20'

Map l

Page 114: 52C15SE0014 Olive Mine

CHLORITE SCHIST

r324l'oOC6|o.035 G .37 C.CQ4|CGl9 C v-^| 0.069 | C C34 0-C8C| .: . 04 e O 016 0-C67 1C 097 j Cei\ J (0088| c 034 |

INTERMEDIATE TUFF

INTERMEDIATE TUFF

NORONT RESOURCES LTD.

OLIVE MINE PROJECT

SECOND LEVEL PLAN -I38'

LITTLE TURTLE LAKE AREA

KENORA MINING DIVISION

BY: E.LUDWIG

MARCH 25,1987

Page 115: 52C15SE0014 Olive Mine

\

\

INTERMEDIATE TUFF

FACE

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SYMBOLS

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FAULT

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NORONT RESOURCES LTD.

OLIVE MINE PROJECT

THIRD LEVEL PLAN -210'

LITTLE TURTLE LAKE AREA

KENORA MINING DIVISION

BY: E. LUDWIG

MARCH 25, 1987

f* 20'

MOP 3 x-, r\ ri

Page 116: 52C15SE0014 Olive Mine

84-18 trace

©84-16 trace

84-19 no vein

® 84-17.023/1 6

84-21 013/1.0

240

®64~6tr

64-03 0.014/1.5'

064-7tr

E. LUDWIG GEOLOGICAL CONSULTING

CLIENT: NORONT RESOURCES LTD.

PROPERTY: PRESTON - OLIVE PROPERTY

TITLE:LONGITUDINAL PROJECTION

Map. 4

Date: May I987 Scale: r*40' NTS:Drawn: Interp: Job No: 0-I33

Page 117: 52C15SE0014 Olive Mine

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