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kL.TIi JDALE A ASSOCIATES IN907- 10 Erskin* Avenu*

Toronto, Onto lo, Canada M4P 1Y4

o 010

SUMMARY REPORT

THE 1990 EXPLORATION PROGRAM

ON THE

ASQUITH TOWNSHIP PROPERTY

SHINING TREE AREA, ONTARIO

FOR

ASQUITH RESOURCES INC.

ASARCO EXPLOATION CO. OF CANADA INC.

EGO RESOURCES LIMITED

(416)481-5781

OFFICE

October 990 Toronto, Ontario

J. L. Tindale Geologist

NTS 41 P 11

11111111111111I1iii

*SUMMA .Y

PREAM ,LE

INTRO lUCTIC

PROPE .TY H(

GENES L GEC

THE 1 90 E)

GEO OGIC^

P ke L;

(1)

(2)

(3)

G bson

(l)

(2)

C aim

C swel

M seel

(i)

(ii)

(iii

GEO HYSK

STR PPINt

( ) Bi

( ) Tl

( ) S

CONCL SION

RE COM ENDA

COST STIMi

APPEN: ix A

APPEN: ix B APPEN: ix cAPPEN: i x D

TABLE OF 41 P 11SE0143 63.6156 ASQUlTH 010C

.TY HOLDINGS, LOCATION AND ACCESS

L GEOLOGY

90 EXPLORATION PROGRAM

OGICAL MAPPING PROGRAM

ke Lake - MacDonald Lake Sheets

(1) Geology

(2) Structure

(3) Mineralization/Areas of Interest

bson Claim - 1146633

(1) Geology and Structure

(2) Mineralization/Area of Interest

aim 1092142

swell Lake Area

scellaneous Prospecting and Sampling

Clarke Area

(ii) Kubiak Area

(iii) Road-Fill Showing

HYSICAL AND GEOCHEMICAL PROGRAM

PPING, WASHING AND SAMPLING PROGRAM

Buckingham Mine Area - Past Exploration

The 1990 Program

Structure and Mineralization

NS

ATIONS

STIMATE 1991 PROGRAM

APPENDICES

Samples by Rob Cinits During Geological Mapping

Surface Samples by J.L. Tindale

Channel Sample Record

Whole Rock Analysis Buckingham Shear

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FIGUF

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FIGURES

Hologden Shaft Area

Claim 1146633

Claim 1092142

Sketch Roadfill Showing

Magnetometer Survey Claim 1092142

MAPS

Geology Grids C-West 6 A-South

Geology Grid B

Geology Caswell - Stewart Lake

Buckingham Mine Area - Stripping Plan

Detailed Geology - Buckingham N. Zone

Sampling Overlay - Buckingham N. Zone

Detailed Geology - Buckingham Mine Area

Sampling Overlay - Buckingham Mine Area

Property Location

Geochemical Orientation Survey

Magnetometer Survey B Grid (West)

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* In ack Pocket

SUMMARY

The Asquith Township property subject of this report consists of 77 contiguous claims located near the village of Shining Tree, Ontario. The property is owned 7C^ by Asquith Resources Inc., "Asquith", and 3C^ by Ego Resources Limited. Asarco Exploration Co. of Canada Inc., "Asarco", have the option to earn a 60/5 interest in the claims by expending S400,000 thereon prior to June 30, 1994.

During the summer of 1990 Asarco funded a program of geological mapping, geophysical surveying, prospecting, stripping, washing and sampling on the property at a cost of approximately $115,000.

Geological mapping of the southern and western portions of the claim block disclosed the presence of an amphibolite predominant terrain hosting brittle fracture occurrences of quartz veining with low, erratic gold values.

The Gibson claim in the northwest corner of the property was found to contain a series of pits, trenches and open cuts within a strong carbonate-rich shear zone traceable along strike for over 800 feet. Assay values up to 0.647 ounces per ton gold were obtained.

Significant gold values were located within strongly sheared carbonate- rich zones from the Kubiak area and east of'MacDonald Lake.

Bulldozer stripping, washing and sampling in the Buckingham Mine area exposed a gold enriched ductile shear zone (named the Buckingham Shear) along which blue quartz veining has been injected. This break has been traced for over 1600 feet and is open to the east and west. Two sections of this occurrence carry gold values across mineable widths along strike lengths of 50 and 150 feet.

Gold values of economic interest on the property are associated with blue quartz veining within intense ductile shear zones hosted by mafic volcanics rocks which have been severely altered by carbonate flood ing accompanied by sericite, chlorite and sulphide accessory mineralizat ion.

Further exploration to evaluate occurrences found during the 1990 program and to advance the potential of the Buckingham Shear structure is recommended at an estimated cost of $115,000 which cost includes further property acquisitions.

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PREAMBLE

The Shining Tree gold area was first identified in the early years of tlv century when rich pockets of gold were located in predominately north strik ng, massive quartz veins. Government geologists of the day favourably compa ed the geology and structures to those at the developing mines at Timmi s and Kirkland Lake, Unfortunately the early promise never materialized into ay significant producing situations and because of the numerous ill- conce (/ed and in some cases fraudulent exploration programs attempted, the area has o er the years gained a reputation best described by the catch words "pock ty", "shallow", "erratic" and "lacking structure". And yet there are over 50 recorded gold showings in the area in such diverse structural settings as qu rtz veins in prophyry, carbonate shears, iron formations and amphibolite- rich racture zones. It is, therefore, our opinion that a determined explora tion ffort focused on a known area of gold occurrence may yet yield the neces ary qualities of structural and geological setting to host a mineable gold eposit at Shining Tree.

INTRODUCTION

Asquith Resources Inc., an Ontario Corporation with offices at 907 - 110 E skine Ave., Toronto, Ontario M4P 1Y4, has since the fall of 1986 been acqui ing mining claims in the east central portion of Asquith Township near the v llage of Shining Tree, in the Larder Lake Mining Division of Ontario. At th s writing the Corporation has assembled a contiguous group of 77 claims upon hich exploration for gold mineralization has been carried out.

The present property holdings are held 70/S by Asquith and 30% by Ego R sources Limited. Asarco entered into an agreement with the owners on June , 1990 whereby Asarco could earn a 60/5 interest in the Asquith Township prope ty by expending $400,000 thereupon on or before June 30, 1994.

The exploration program funded by Asarco and managed by Asquithdurin the summer of 1990 consisted of detailed geological mapping, prospecting and s mpling over areas of the property previously untested, and a program of strip ing, washing and sampling near the Buckingham Mine site as a follow-up to dr Hing carried out in early 1989. Results of this program which was des igned to complete the basic data base over the entire property is described in th following.

PROPERTY HOLDINGS, LOCATION AND ACCESS

The property is located south of Highway 560 near the village of Shini g Tree, Ontario. Trails suitable for ATV travel provide access to the claim . Forestry operations scheduled for the winter of 1990-91 will provide furth r access over the eastern areas.

The terrain is typical of the Canadian Shield and though outcrop is reaso ably abundant in some areas most of the land surface is covered by glaci l deposits, boreal forest, bog and lakes.

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The details of our claim holdings are itemized in the following. 'Asses ment work available for filing is indicated where applicable.

UNPAT NTED CLAIMS

Claim No.

91897 -9799189891898 -98291898

93531 -315*919019190291902 -0249190291902919029190291902

97955 -559**97956 -561**

97334 -354**

98003 **98003 -40,042**

97335 -356**

798897988979890 -912

98004 -049***10461 4***

10486 5-646

10921 111466 3**10921 2**10921 3-144**10921 5-146

* eology survey** eology and mag5'oVjV pnlnov- mao fin

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( 4)( D( 1)( 3)( 1)( 1)( 1)( 1)( D

( 6)( 2)

( 7)

( 1)( 5)

( 2)

( 1)( D(13)

( 4)( D

( 2)

( 1){ l)( D( 2)(J.)

(73)

to be filsurvey t

H VI. F emr

Asses Credits Filed

140 days 120 " 140 "

135 "

Status

100

100140

100

200200200

100100

60

60

60 days due Oct. 2, 1991 on extn. to June 28, 1991 60 days due Oct. 2, 1991 on extn. to June 28, 1991

( 4)( 1)( 1)( 3)( 1)( 1)( 1)( 1)( 1)

( 6)( 2)

120 "165 "160 "170 "157 "180 "140 "120 "110 "

120 "110 "

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2030

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daysdays

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AprilApril

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199119921992199219921992199219911991

, 1991, 1991

30 days due May 25, 1991

40 days due June 5, 1991 60 days due June 5, 1992

40 days due Aug. 11, 1991

extn. to survey Aug. 16, 1991extn. to survey Sept. 4, 1991extn. to survey Aug. 16, 1991

40 days due Feb. 11, 1992 40 days due Sept. 12, 1992

40 days due Nov. 8, 1991

40 days due Apr. 3, 1993 20 days due June 22, 1991 20 days due July 6, 1991 20 days due Aug. l, 1991 20 days due Nov. 1991

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CLAIM UNDER OPTION

TRS 2 07, 2461, 2406, 3664 (O - the Buckingham option has a $200,000 work commi ment outstanding until December 31, 1990 to earn a 100% working interest in th property, subject to a 2^ N.S.R.

GENERAL GEOLOGY

The area is underlain by Precambrian rocks which trend northwesterly and c nsist of a suite of mafic to felsic intrusives interlayered rarely with metas dimentary deriviatives of the volcanic activity. By far, the most domin nt rock type is the mafic volcanics which is predominantly black to dark green colour, fine grained and often pillowed. Interlayered with these mafic units are light green intermediate matavolcanics which are often porphyritic conta ning phenocrysts of blue to white quartz. Thin bands of metasediments occur in the area interbedded with the metavolcanics and these consist prim arily of interflow chert, arkose and greywacke. Ultramafic intrusives grading from ale-rich serpentine bodies to dioritic and gabbroic composition also make p a portion of the interlayered volcanic sequences. Plutonic rocks of grani e intrude the volcanic pile and appear as large masses bordering the area o the north," south and west. Dykes and small stocks of porphyritic grani e occur within the interlayered sequence probably derived from the pluto ic episode. Diabase dykes and sills with northerly trends cut all of the p eceeding units noted above.

In general geological terms there are numerous direct comparisons which can be drawn between the Timmins and Shining Tree gold camps in terms of si s, shape and overall distribution of Archean volcanic-sedimentary formations, At Tii nins the gold-bearing upper Archean succession lies between the Shaw Dome D the north and stratigraphically equivalent sediments of the Porcupine Scarp to the south. At Shining Tree we have the reverse relationship with the g Id-bearing volcanic complex lying south of the Halliday Dome and fringed yet f rther north by remnants of the Porcupine Scarp equivalents.

In both cases the uppermost parts of the main Archean succession is occup sd by a distinctive and important volcanic cycle. This varies from ultrai afic basalts at the base upward through tholeiitic basalts to calc- alkal ne intermediates and acid volcanics at the top. At Timmins these volcanics are k awn as the Tisdale Group; at Shining Tree the corresponding formations are k- Dwn as the Sinclair, Shining Tree and Cabot-Kelvin Groups. Identical relat Dnships occur within the Kirkland-Larder gold camp. Most importantly rocks Df this cycle provide the host for the major gold deposits at these deveL ped camps.

The latest Archean events in all cases are recorded by the development of a 2stricted, funnel shaped dilation zone along the main "break". Felsic porph; ritic intrusives along with enormous volumes of hydrothermal mineralizing fluid migrated upward along this conduit. This last important event very likel; was responsible for the emplacement of much of the gold mineralization as we l as the intense hydrothermal alteration which accompanies it.

Though a main "break" has not as yet been named at Shining Tree we belie' 2 it exists and its presence is established by the intense, widespread carboi ate alteration, porphyritic intrusions and proliferation of gold occur snces apparent in the area.

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THE 1990 EXPLORATION PROGRAM

A program of geological mapping, sampling and minor geophysical and g' Dchemical surveying was initiated over the operators' claim holdings in AS' aith Township during July and August. During the latter part of August a str pping, washing and channel sampling program near the Buckingham Mine was c npleted. Details of the program are provided in the following under corre ponding headings. Sampling results are appended to this report.

GEOLO' ICAL MAPPING PROGRAM

Geological mapping on a scale of l" s 2QO' was carried out over a pre-e isting grid system established in 1987 covering the area south of Seage Creek in the vicinity of Pike Lake and west of MacDonald Lake, effect ively completing the mapping of the southern and western portions of the prope ty. The Caswell Lake area in the northeastern area was also mapped along with recent claim acquisitions along the north side of the property.

Rob Cinits, a contract geologist, and the writer carried out themapp as th

g of the various areas results of which are presented with this report ee large maps and three smaller page size detailed maps at scales of

l'^20 ', 1'^SO' and l'^20' covering portions of the north Clarke area (1092142), Gibso claims (1146633) and the Hologden shaft area at the south end of Pike Lake espectively.

Pike ake - MacDonald Lake Sheets

l

This area (Maps No. l 6 2) is predominent ly underlain with mafic volca ics which range from fine grained and pillowed flows in the north to fine o coarse grained amphibolites in the south. Interbedded with these units are several irregular and discontinuous horizons of mafic, intermediate and f Isic tuffs. A series of late NNW trending diabase dykes crosscut all of th stratigraphies.

The mafic pillowed flows are moderately deformed with thin chlori- tized selvages and often display amygdaloidal phases. Pillows indicate flow tops o be ENE to the east of Pike Lake and NNE to the west of MacDonald Lake .

The transition into the higher metamorphic grade is abrupt and follows the r gional stratigraphy. Often the transition is marked by a horizon of very oarse grained gabbroic rock which may be a coarse grained phase of the mafic flows. The amphibolites are variable in texture and composition ranging from ine to medium grained equigranular to very coarse grained porphyritic phase with euhedral hornblende crystals up to \ " i n diameter within a felds- par-r eh matrix. Translucent quartz-eyes up to 1/8" across are present in some utcrop areas. The finer grained amphibolites tend to have a stronger folia ion than the coarser porphyritic types which tend to display more idiom rphic textures. Several narrow, discontinuous bands of fine grained volca ics and tuffs were noted within the amphibolite sequence.

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Felsic flows and quartz-eye tuffs are present throughout the mapped area. They range in thickness from less than 10 feet to 200 feet and are most commc ly hosted within and interbedded with the amphibolite schists. The quart -eye tuffs are moderately sheared with l-5% translucent to smokey or blue quart -eyes ranging from 1/16" to 1/8" in diameter is a fine grained felsic groun mass. In a few localities lapilli and fine grained ash tuff units were mappe , neither of which are very extensive and are minor features of the felsi sequence.

Small and insignificant quartz-feldspar porphyry and granite dykes were lapped along the southern boundary of the map sheets and may be related to a lat phase of the Miramichi Batholith which lies a few kilometers to the south

Diabase dykes strike NNW, dip subvertically, and cross the area bisec ing all the above stratigraphies. These dykes range in thickness from a few feet to over 200 feet with rapid variation along strike. Commonly they are f ne to medium grained equigranular units though in some cases are porphr- itic ith light green to yellow phenocrysts of olivene, characteristic of the Match wan phase diabase. The dykes tend to weather recessively and therefore occur as long continuous prominent ridges. The units represent a large percentage of th rock types mapped, consistently repeating every 200 to 800 feet.

(2) tructure

The majority of the rocks, aside from the diabase, display a moderate folia ion which parallels the stratigraphy striking 320 0 -350 0 east of Pike Lake and 2 0 0 -300 0 west of MacDonald Lake. Dips are moderate to steep to the south.

Two prominent shears, parallel and approximately 500 feet apart,strik at 250 0 across the lower portion of MacDonald Lake and through the central porti n of the property. Associated with these shears are zones of moderate carbo ate alteration, silicification and quartz veining, chloritization and trace to 2% fine disseminated pyrite. Sericite and fuchsite occur locally. These zones appear to define and are roughly coincident with VLF trends apparent from earli r geophysical surveys. There does not appear to be any significant off- setti g of the stratigraphy by these shears.

There are other shear directions mapped within the area with east-west and n rthwesterly strikes along which quartz veining has been uncovered by prosp cting. There are less well defined but nevertheless may be more econom- icall interesting than those described above. There appears to be no elect omagnetic expression for these structures.

(3) ineralization/Areas of Interest

The mapped area is dotted with a multitude of old pits, trenches, shaft and stripped areas many of which are overgrown or caved in. Wherever possi le these showings were sampled in an attempt to identify the gold content. Unfor unately most of the areas sampled, particularly in the amphibolite dominated terra n, returned low values (tr. to 20 ppb). A few localities did return higher value and because of this warrent further consideration or, had promising geological struc ures deserving of a second look. Some of the more interesting areas exami ed are discussed in point form below.

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(i) ^o^ojjder^Slia^f^Ai^eji ~ (see l" ~ 20' detail Map) - located along 'the se ith shore of Pike Lake. A series of trenches, pits and an 18' shaft expose i a 2" - 6" wide smokey translucent quartz vein for about 40' in a south- westei ,y direction away from the lakeshore. The vein is hosted by lightly carbor itized, chlorite rich amphibolite schist with traces of finely disseminated pyrite and chalcopyrite evident in the vein and wall rock. Seven grab and/or chip s imples from the vein area failed to return significant values. Further work i i this area is not planned.

(ii) Unnamecl .Sl\aft^ - B Grid 4+80E, 4+OON - located approximately 150 f( ;t north and east of the NW corner of the Holding Mine leases this shaft appeal s to be 20' to 30' deep and measures 10'xl2' at the collar. The rather extent Lve dump is moss covered leaving the impression of having seen few visitors for mi iy years. Exposed along the walls of the shaft is a 1.5' to 2' wide trans] irent to white, coarse grained quartz vein striking at 90 0 and dipping to the south at 75 0 with dark green chlorite inclusions and bands of chlorite- rich \ a ll rock. The vein contains mere traces of pyrite along its edges. The amphil jlite host rocks are moderately to well sheared, altered with carbonate and ci Lorite and contain up to 2 7, pyrite as streaks and dissemination. Narrow blue-j rey quartz stringers are noted within the sheared wall rock. Chalcopyrite traces were seen in the sheared wall rocks. Grab samples taken by Rob Cinits and l; :er by the writer from the shaft dump returned the following values:

38,941 ppb (1.133 opt) grab of vein material, dump.222 ppb (0.006 opt) qtz. rubble 80' west shaft, tr. cpy.24 ppb ( -- ) qtz. from shaft dump, transparent.

10,485 ppb (0.305 opt) sheared wall rock, l-27o py, 1 07, q tz.517 ppb (0.015 opt) sheared wall rock, Z-3% py, 5 07* I b. qtz. strs,

8 ppb ( ~ transparent qtz., main vein, nvm.

Further work in the form of grubhoe prospecting, detailed mapping and possi le bulldozer or backhoe stripping is recommended to trace this structure along strike and to provide exposure for further sampling.

(iii) jStockjrfork. Area - B Grid L24W, 7+OOS - a series of white quartz veins varying in width from l' to 1.5' and striking at 90 G , 120 0 and horizontal are c ntained within an exposed area of 60'xlOO' hosted by a brecciated felsic tuff nd amphibolite. The veined area is rusted and moderately carbonatized and c ntains up to 2% pyrite and traces of chalcopyrite. Grab samples (4) faile to return any values of note. However, the zone is intensely altered and may b indicating, a stronger nearby structure. A VLF conductor, striking NW, cross s line 24W at 6+OOS.

It is recommended that a program of grubhoe prospecting, detailed mappi g and further sampling be carried out over this area to determine if any signi icant values exist.

Gibso Claim - 1146633

(l) G ology and Structure

This single claim, named for its original staker in the early part of the c ntury, contains a portion of the village of Shining Tree and Highway 560 cross s the northwest quarter. Approximately two miles of grid were cut over the c aim by D. LaForest personnel from Timmins during the summer. Line 40W from Grid ) was extended north crossing the claim from which an east west base

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lline E d north south lines at 200' intervals were turned off. Mafic volcanics, dark j reen, fine to coarse grained, massive to pillowed in part, underlay the claim Two narrow diabase dykes strike northerly across the property.

A strong shear zone striking 230 0 and dipping 50 C to the south crosses the c' aim commencing near the No. l post. The zone is heavily carbonatized, rusty up to 40' wide and has been traced for approximately 700' in a south- weste; Ly direction where it appears to weaken though exposure is poor. The zone contii aes strongly to the northeast where it passes off the claim into low groum ,

(2) t Lneralization/Area of Interest

Pits, trenches and shallow open cuts trace a gold mineralized serie: of quartz veins within the above described shear zone. The veins are l" - ( ' wide within the heavily sheared portion of the alteration zone which attaii i widths varying from 5' to 10". A l'^50' detail map of the sheared area c 'picts the assay results obtained by Cinits' sampling. Visible gold was ne :ed by the writer in quartz from the open cut near line 34W. The trenches are bc lly overgrown and often in low ground. A program of stripping is required to bet :er understand the significance of the zone.

Claims 979946 and 573098 are Onitap Resources' property adjoining the ec it boundary of the Gibson claim. Along the southshore of Moorecamp Lake on the ie claims stripping has exposed a 10' to 20' wide zone of intense sheari ig in carbonate-rich pillowed mafic volcanics. Within the intense shear are b] ie, grey quartz veins up to 12" wide along with stringers and boudins of simile ' material. Pyrite is a common accessory mineral. A pale grey, 3' wide, very f .ne grained felsic dyke forms the footwall of the zone. The zone passes into t .e lake to the west striking for the Gibson claim open cut which is appro* mately 700' to the west. Whether the Onitap showing is actually the extens on of our mineralized shear cannot be positively determined. Regardless, the Or tap occurrence is one of the better showings the writer has seen in the camp a d should be acquired for future evaluation. The intensity of shearing, streng h of veining and high degree of alteration practically guarantees the presen e of gold in this setting.

Claim Q92142

Staked during the summer to add to our holdings in the Clarke porphyry area a ong the north boundary of the property, a program of line cutting, geolog cal mapping and magnetometer surveying was carried out over the claim. Approx mately one mile of line was cut by D. LaForest personnel of Timmins, accomp ished by extending the existing lines 8W and 4W to the north from the D Grid

Mapping revealed the claim to be completely underlain with soft green talcos peridotite and gabbroic phases thereof. These massive rocks form steep ided irregular hills across the claim. From our previous mapping on claims to the east of Stewart Lake it appears that this mafic-ultramafic sequen e may form an accuate band striking southeasterly and passing through the no eh in Stewart Lake and then passingnorth of the Buckingham shaft area where he Corporation intersected a similar unit in drilling.

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Aside from adding Co the geological knowledge of the property the clain appears to have little economic value.

Caswe l Lake Area

This area lying in the northeastern sector of the property was mappe . at I"s 200' (Map #3) for preliminary evaluation and assessment work purpc es. A grid was established over the area during the winter of 1988 and magne ometer and partial coverage with VLF had been accomplished.

As previously indicated by magnetometer results diabase dykes are the p eminent rock type lying between Stewart and Caswell Lakes. These are NNW s riking, dark green, medium grained ridge forming features which split and c alese giving rise to a braided appearance.

Mafic volcanic flow rocks, massive dark green units underly the south and w st of Caswell Lake. Occasional poorly developed pillows were noted along the e stern shore of Stewart Lake.

Northeast of Caswell Lake the stratigraphy changes- abruptly to a pale green fine grained massive tuffacious unit. The unit appears to contain trace of pyrite and is poorly foliated in a northwesterly direction parallel to th stratigraphy.

Near the north end of Stewart Lake a narrow east-west striking quartz- felds ar porphyry dyke was noted which cut across both the mafic volcanics and diaba e dyke rocks and must therefore be a very late stage epoch of volcanic activ ty in the area.

Structurally, aside from the diabase, the rock units appear to trend north esterly with foliation moderate to weak paralleling this regional trend.

An area of intense shearing and carbonatization was noted crossing the n rthend of Stewart Lake in an east-west direction. Pyrite gossan is preva ent across approximately 100' of exposure over the shear trace. Quartz veini g was lacking within the structure. This may be the easterly extension of th Clarke carbonate zone.

A few random quartz veins were sampled during the course of mapping all o which returned low values in gold.

M i s c e ! Laneous Prospecting and Sampling

During the course of the summer the writer assisted by Roy Annett, a pro pector from Shining Tree, examined and sampled a number of areas where old w rkings suggested the possibility of mineralization. In many cases trenches and p ts were cleared of debris with grubhoes allowing fresh rock to be sampl d. Some of these areas are discussed in the following.

(i) Clark^Area^ - A broad area of intense carbonate alteration, quart veining, shearing and pyrite mineralization somehow associated with a quart -feldspar porphyry adjacent to the Clarke patented claim WD 1166. Numer as pits, trenches and opencuts were found on claims 918977 and 918978 appar- ntly to test quartz veining with pyrite and fuchsite mineralization in highl altered carbonate-rich prophyry. Veins are mostly white quartz striking

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10

est to northwesterly with dips varying from flat to vertical. The entire hich is over 200' wide is an intriguing exploration target given theof alteration, the persistent pyrite content, the bright green fuchsite

ation and multitude of quartz veins. We took twenty-three grab and chip s across pits and trenches which appeared to expose the more intensely lized zones. These on analysis returned values ranging from trace to a f 181 ppb with the majority falling within the 25 to 50 ppb range. These esults discouraged further work on this area during the summer program.

(ii) Kubiak^reti ~ Located at approximately 2+50E, 8+OON on Grid eries of blue grey quartz veins are contained within a 10' wide intensely d, carbonate-rich, east-west structure mineralized with disseminatedthroughout. The main "leader" is a 12" - 15" wide blue grey quartz vein

eh a series of pits, and a shallow shaft have been sunk along a strikeof 50 feet. The easterly extension is swamp covered whereas the westerly

ion appears to pass into heavy overburden. Aside from the -surface work appears to be at least 50 years old there is no evidence of drilling or exploration activity.

Sampling of the best exposure, a shallow open cut at the edge of the swamp assayed 584 ppb across 3.5'; 901 ppb across 4.0'; and 1137 ppb across 2.0'; all in chip samples.

The zone is very strong and we had planned backhoe cleanup during the s mmer program. This should be done in a future program.

(iii) Road-Fill Showing - This showing was uncovered by the bull- while filling in a low swampy section of the Buckingham Road while g in to carry out the stripping program at the Buckingham Mine area. The g is located at 3+50W, 12+OOS on Grid D (see attached sketch) and consists t-west striking blue grey and white quartz veins hosted by sheared, pale carbonate-rich, pillowed mafic volcanics. The alteration zone is approxi- 150' wide and it is suspected that the best part of the showing may be 50' central interval below swampy ground. On either side are strongveins witti .pyrite ^Rfbi " •---—~- •—' —---- --

sheared rqck with thin blue

l l l l l l l l l l l l l l l l l l l

10

east- est to northwesterly with dips varying from flat to vertical. The entire zone hich is over 200' wide is an intriguing exploration target given the amoun of alteration, the persistent pyrite content, the bright green fuchsite assoc at ion and multitude of quartz veins. We took twenty-three grab and chip sampl s across pits and trenches which appeared to expose the more intensely miner lized zones. These on analysis returned values ranging from trace to a high i 1 81 ppb with the majority falling within the 25 to 50 ppb range. These poor esults discouraged further work on this area during the summer program.

(ii) KuHaJ^Ajrea. ~ Located at approximately 2+50E, 8+OON on Grid C, a eries of blue grey quartz veins are contained within a 10' wide intensely shear d, carbonate-rich, east-west structure mineralized with disseminated pyrit throughout. The main "leader" is a 12" - 15" wide blue grey quartz vein on wh eh a series of pits, and a shallow shaft have been sunk along a strike lengt of 50 feet. The easterly extension is swamp covered whereas the westerly exten ion appears to pass into heavy overburden. Aside from the -surface work which appears to be at least 50 years old there is no evidence of drilling or other exploration activity.

Sampling of the best exposure, a shallow open cut at the edge of the swamp assayed 584 ppb across 3.5'; 901 ppb across 4.0'; and 1137 ppb across 2.0'; all in chip samples.

The zone is very strong and we had planned backhoe cleanup during the S' miner program. This should be done in a future program.

(iii) Road-Fill Showing - This showing was uncovered by the bull dozer rfhile filling in a low swampy section of the Buckingham Road while walki' g in to carry out the stripping program at the Buckingham Mine area. The showii j is located at 3+50W, 12+OOS on Grid D (see attached sketch) and consists of ea, t-west striking blue grey and white quartz veins hosted by sheared, pale green :arbonate-rich, pillowed mafic volcanics. The alteration zone is approxi mate!; 150' wide and it is suspected that the best part of the showing may be in thi 50' central interval below swampy ground. On either side are strong quart: veins with pyrite in the well sheared carbonate altered rocks. Sampling of thi sheared rock with thin blue grey quartz veinlets on the north side of the fill : 'turned an assay of 1411 ppb gold.

Because of the wet nature of the central portion of this structure it woi Id best be tested with a drill hole from a road setup during a future progr; n.

GEOPH1 SIGAL AND GEOCHEMICAL PROGRAMS

Magnetometer surveys utilizing a Scintrex model MP-2 proton precision instn nent on loan from Asarco Exploration were carried out over claims 1092143 and K 32144 at the western side of the property, over claim 1146633, the Gibson, and ci ;r 1092142 on the north side of the property.

The western claims covered lines 32W to 44W, at 400 foot line spacing, over i previously cut grid. The Gibson claim was controlled by a new grid cut di ring the summer by D. LaForest personnel as well as claim 1092142.

ir1

i i i i i i

i i i i i i i i

/.aw

772

"/9V

i 293

-583

, W/

i 240

-1

32 .Vi

- /033

t 9V.9

^ V32

^ fl,v

. -V3V

, 383voo

St*/*. "*

8l3

F;,. s

{.4*01*1*4.**.*:'

l l l l l l l l l l l l l l l l l l l

11Details of the survey are presented on three maps included in this

repoi :. Suffice to say the results were reasonably useful in locating the trace of diabase dykes but these in turn appear to mask any subtle structural relat .onships which might be interpreted otherwise.

A geochemical orientation survey was run over lines 20E, 22E and 24E on tr i A Grid from the baseline to 16S in the Buckingham Mine area. It was hopec that the known veins in this area would exhibit a geochemical signature in tt : overlying soils and give confidence to carrying out geochemical surveys over ither overburden covered areas of the property. Such did not prove to be the c ise as both the A and B horizons returned exceptionally low values with no cc 'relation with the known structures. It was subsequently decided to abanc m any further geochemical soil tests on the property.

In total, approximately 100 samples from the A and B horizon were anal} ;ed for gold. The A horizon was a brown sandy unit varying in width from l" tc 6" whereas the B was a rusty brown clay-rich material. Results of the orier ation survey are enclosed with this report in map form at a scale of 1"-5C .

STRII 'ING, WASHING AND SAMPLING PROGRAM

(l) E .ckingham Mine Area - Past Explorations

The Buckingham Mine area is situated on four leased claims in eastern centr .1 Asquith Township. These claims were staked early in the century and broug .t to lease in 1916. Work on the claims culminated in 1928 when a 182', 65 0 i .dined shaft was sunk on a wide gold bearing quartz vein. Drifting to the e .st and west totalling approximately 500 feet was carried out at the 100 foot evel. Various reports of high grade gold in the shaft and drifts are noted in the literature of the time but the Buckingham Mine Limited company faile . in 1929 and the equipment and claims were sold at auction in 1935 to one of tb directors, a Mr. P. A. Vale of Toronto, the heirs of whom are the present owner . Apparently the property was optioned to a prospector, Ed. James of Cobal , during the early 1950's who carried out shallow drilling adjacent to the s aft, and in 1959 was optioned to Central Porcupine Mines who likewise drill :d two shallow holes at 40 foot centres immediately west of the shaft.

Asquith Resources Inc. optioned the property from the Vale Estate on J a .uary 14, 1987 and carried out geological and geophysical surveys over the p operty. During November of 1988 Ego Resources Limited negotiated an optic . with Asquith to earn an interest in Asquith's properties by carrying out a diamond drilling program which culminated in the drilling of 21 holes, 7560 :eet in early 1989, mainly over a five hundred foot strike section centt :d around the Buckingham Mine, thereby earning a 30% interest in Asquith's holdi tgs in the township. The drilling resulted in numerous intersections, many showi ig fine visible gold, over widths approaching 9 feet, confined to intensely shear ;d carbonate-rich shear zones with blue grey, quartz veining accompanied by pi ite and tourmaline. Difficulty was experienced in correlating the inter sect! ms with any certainty and a program of stripping and washing was proposed to e n 'ose the veins on surface to better understand the distribution of these occur ences. This program was implemented in the summer of 1990.

l l l l l l l l l l l l l l l l l l l

12

(2) T e 1990 Program

(i) ItjLiEPA.n.S 5.n^ XalLh!nil ~ Utilizing a D-8 Caterpillar bulldozer contr cted from Wilfred Paiement and Sons of Earlton an area roughly 1000" long n an east-west direction by 150' wide was stripped at a location appro imately 700 feet west of the Buckingham Shaft. This was followed by a strip ing program covering an area 400' north-south by 100' wide immediately east f the shaft .

Bedrock topography was found to be extremely uneven with deep overb rden filling weathered shear structures and soft zones of carbonate- rich Itered rocks. Cleanup of these incised zones necessitated the contract ing o a Caterpillar backhoe from Gunter Contracting of Shining Tree which clear d the zones of interest to permit washing, sampling and mapping to proce d.

(ii) Gec)lc^gju:jal J^pjung - Mapping at a scale of I"s 20' was carried out a ross the stripped area utilizing a grid tied to the previously cut 200' grid. Pickets were erected at 50' intervals along the original grid and the inter ening areas.

The predominant rock-type underlying the stripped areas is a mafic pillo ed volcanic, dark to pale green, which has been intensely carbonatized adjac nt to areas of shearing, and lessening in intensity proceeding away from these active zones. Pillow textures are obliterated in the intense carbonate alteri d zones but are recognized where this activity lessens. Tops face north asterly over most of the exposures but appear to swing more northerly in th most westerly outcrops. Pillow selvages are epidote-rich .

Thin north striking diabase dykes cut across the flow rocks and the s earing at rare intervals. In the stripped area these dykes are l to 2 feet ' ide, chilled, very fine grained, black intrusions which have no apparent offse ting characteristics to the surrounding rocks or structures.

A north striking highly altered felsic intrusion, prophyritic in part, was m pped at 12+25E, 6+75S. The rock is very fine grained, creamy white in colou , with quartz phenocysts and has been sericitized, sheared and injected with andom bluish quartz veining. Approximately 150' further east a rubble zone f quartz-feldspar prophyry was found which may be genetically related to th s more highly altered phase.

( 3 ) ^ ructure and Mineralization

The prime structural feature, and the locus of the alteration and the gi Id mineralization across the area of interest is the Buckingham Shear. Strip ing has exposed this prominent break, intermittent ly for a distance of 1600 2et in a roughly east-west direction. Previous drilling to the east may h, ve added a further 400" to this length.

The Buckingham Shear is a zone varying in width from l foot up to 10 fei t of intensely schistose, crenulated, carbonate-rich, pale green mafic volcai ic along which bluish-grey quartz stringers and veins have been injec 2d which carry free gold. Finely disseminated pyrite is distributed throu; lout the shear with rare sightings of chalcopyrite. Chorite and sericite

l l l l l l l l l l l l l l l l l l l

13

alter tion products are present within the shear and along fractures in the veini g. The quartz may form wide sections such as at the Buckingham Shaft where the vein is over 3.5' wide or as narrow, boudinage-like fillings, as along the shear planes. Wide sections of quartz are also evident at AS on line E where the shear has been tightly isoclinally folded. Tourmaline is a com on constituent of the quartz..

The Buckingham Shear is anything but a straight-line break. Rather it is a sinuous, ductile-appearing zone given to rapid changes in strike though carry ng a general east-west trend. Secondary splays branch from the main break but these appear limited in strike extent and tend to be less well miner lized and often carry white quartz veining. The main break where it is folde plunges westerly at approximately 75 0 as do the crenulations within the s ear. Possibly this plunge may be a guide to tracing the depth extension of th gold bearing shoots.

The entire shear is enriched in gold mineralization. A total of 301 chann l samples were cut along the shear and its branches utilizing a Stihl diaino d saw during late August. Two areas of significant gold values were confi Tied, these being located at 4S on line 8E and immediately west of the Bucki gham Shaft. The former has gold values distributed along a strike lengt' of 150 feet coincident with folding of the shear which has proliferated a mar 2d increase in blue quartz. Assay values up to 1.94 ounces per ton gold acros 2.0 feet were returned from this area. A fifty foot trench west of the si aft returned values up to 0.69 ounces per ton across 6.0 feet from this stron, ly veined area.

All values greater than 1000 ppb were reassayed with the variable resul 3 strongly indicating the expected influence of free gold in the system. From total of 74 samples with results over 1000 ppb, 30 samples reassayed highe on average by 35.7% and 44 samples reassayed lower by 23%. This so cal le' "nugget effect" must be addressed in future programs.

The sampling program while verifying that the Buckingham Shear is enricl ed in gold also indicated that concentrations of quartz veining appears neces ary for the shear to approach economic interest. The quartz need not be in :he form of a massive vein to carry significant values. Thin, boudii aged veinlets, also carry across significant widths provided they are concei :rated to at least 20i? of the shear zone. Possibly the stronger portii i o f the shear occurs at 12E near the Buckingham Road but quartz is notici ably a minor constituent and values were correspondingly lacking. The naturi of the shear is such, however, that an increase in quartz content could jccur within a short distance laterally or vertically.

There appears to be little doubt that the Buckingham Shear is a signi icant gold bearing structure. The zone appears to continue to the west past ne stripped area and to the east as verified by stripping and drilling. It is possible to visualize the structure having a lateral strike of at least doubli the present 1600 feet.

Future evaluation of this structure should include tracing the zone irough the gaps in stripping particularly between the Buckingham Shaft area . id the more westerly stripped area. This may best be accomplished by a ser 3s of shallow closely spaced holes to trace the break laterally with folio* jp deeper holes to verify the vertical extent. A similar program to the e, st and west is warrented.

l l l l l l l l l l l l l l l l l l l

H

CONCLUSIONS

There are several prime, structurally controlled, gold bearing occur Bnces present on the Asquith Township property. Some of these have emergi d from the 1990 summer program, others have been further verified and s rengthened in their potential from this work.

There are many marked similarities to these occurrences. All have a gen ral east-west strike, are hosted by mafic, often pillowed, volcanics, are c aracterized by intensely sheared wall rocks into which have been injec ed blue to smokey grey quartz veining accompanied by a contemparaneous influ of carbonate, chlorite and sericite alteration products, sulphide miner lization and free gold. These zones have remarkable lateral extent, varia le widths and are highly crenulated and folded both locally and on a broad r scale. These are ductile shear zones although later brittle fracture- type eatures are seen crossing and displacing them.

At this writing the two main occurrences with the above similarities are t e Buckingham and the Gibson. Potentially the Kubiak and Road-Fill Show ings ay be as important but have had comparatively little exploration aside from onfirmatiori that they carry gold and are in a geologically similar envir nment to the aforementioned. I am of the opinion that there are probably a num er of other as yet uncovered similar showings on the property.

Those showings in the amphibolite terrain along the southern and weste n portion of the property all appear to be related to brittle fracture- type hears with late stage quartz emplorements. Though some carry gold (ie. olding) they appear limited in strike and hence tonnage potential.

Concern must be expressed when discussing the carbonate-rich shear struc ures explored to date that widths for the most part are narrow and sampl ng results due to the free gold aspect have given erratic values. Grant d, where the shear is less than 2 feet wide it will not be mineable, howe\ r, these narrow zones usually carry low values anyways. Where the shear widens it is accompanied by an increase in quartz and a corresponding incre .se in gold content. If a number of these wider higher grade zones can t located within reasonably compact areas then a mineable deposit is possi ile.

RECOMMENDATIONS

The following recommendations are listed as the next stage in the explc 'ation and evaluation of the Asquith Township property.

1. Acquisition of Onitap and Downey claim groups in the Gibson area.

2. Consolidate geology, magnetometer and electromagnetic data on 200 scale overlays.

3. Prospect and trace extensions of the Holding area shaft showing, the quartz stockwork on claim 1092145, the Buckingham Road-Fill Showing and the westerly Buckingham Shear. Detailed mapping and sampling of these areas at l'^50'.

l l I l l lll l l ll l l l l l l l

15

1.

2.

3.

4.

5.

6.

7.

8.

Extend existing grid over the Downey and Onitap acquisitions and geologically map, sample and run geophysical surveys.

Backhoe trench and clean (wash) the Kubiak showing on line 2E, 8N Grid C, and the Downey showings if acquired.

Diamond drill at 50 foot centres the Buckingham shear between lines 12E and 17E and along overburden covered areas in the western stripped area. These holes will be shallow and are primarily to test the widths and mineral content of the overburden covered shear.

An east grid over the Buckingham Mine area to be established to better isolate the diabase occurrences as an aid to future drill locations in this area.

Dependent on the results of surface explorations above a drill program can be designed for further evaluation of specific targets.

COST ESTIMATE 1991 PROGRAM

Property Acquisition (including Buckingham extn.) $ 25,000.00

Linecutting 5 miles @ ?4007mile 2,000.00

Prospecting, Mapping, Sampling(i) Geologist 30 days @ $350/day $10,500.00(ii) Prospector 30 days @ $150/day 4,500.00 15,000.00

Backhoe, Washing, Sampling (Kubiak, Downey, Gibson) 25,000.00

Diamond Drilling 15 holes @ 100' @ $15/ft. 22,500.00

Assaying 500 samples @ $ll/sample 5,500.00

Fuel, Transport, Accomodation 10,000.00

Supervision and Reports 10,000.00

TOTAL RECOMMENDED 1991 BUDGET $l15,OOP.00

Respectfully submitted,

J. L. TINDALE S ASSOCIATES INC.

Toron D, Ontario Octobi r 1990

J. L. Tindale President

Al

APPENDIX A SURFACE SAMPLES BY ROB CINITS

DURING GEOLOGICAL MAPPING JULY-AUGUST 1990FOR ASQUITH RESOURCES INC.

ON THE ASQUITH TOWNSHIP PROPERTY

Sample Descriptions

Local ion^ ^-^ Description Gold ppb. Oz./T.

15640

15640:

15640:

156404

156405

156406

156407

156408

156409

156410

11-t-lOW, 0+05N grid C West

17+OOW.10+40N grid C West

16+05W, 4 + OON grid C West

17+60N.21+OOW grid C West

as above

17+60N.21+30W grid C West

19+80W, 1+80N grid C West

24*40W,22*OON grid C

26*30W,24-f50N grid C

grid C

lf-mafic tuff intensely silici- 5 ^.001 fied S carbonatized; 3% smokey- blue qzt. eyes 2mm across; l-5% subhedral-euhedral py; moderate ly sericitized-strong sheared

quartz vein; rubble in old < 5 -CO.001 trench; moderately carbonatized 6 sericitized; minor tourmaline? trace sulphides

float boulder-well rounded < 5 ^ .001 pyritized mafic volcanic;heavily carbonatized; S-10% medium to coarse euhedral pyrite

quartz veinlets a"-6" in int. < 5 *C0.001tuff (sheared d carb)-veinscarb along fractures nil sulphides

wall rock of above (int. tuff) 15 ^.001 -trace malachite staining

sheared zone-carbonatized 4 seri- 33 0.001 citized mafic volcanics J.% fine py as irreg. stringers S blebs parallel to shearing-areas of brecciation with intense silicification

mafic volcanics lightly sheared 6 ^ ^.001 chlori tized-1V qtz. vein nil sulphides-white vein

sheared St chloritized mafic vol- 6 canics, l-5% fine dissem py; minor qtz. fractures

quartz vein 9" wide nil sulphides ^

quartz vein 6" wide nil sulphides

A2

Sample lo.

156411

15641 l

156413

Location

156414

156415

156416

156417

1564H

15641?

156421

15642

15642

15642

24+80W.23+40N grid C

34*OOW,29*OON grid C

34*OOW,29*OON grid C

L36W.24+50S grid C

L36W,29*07S grid C

L32W, 6+90S grid C

Description Gold ppb.

<5

Oz./T.

quartz vein-rubble 7" wide nil sulphides

quartz veinlets O"-lV in sheared zone; trace suplphides

sheared mafic volcanics-silici- fied-light carb-moderate sericite J.% fine dissem py. (host rock of above veinlets)

silicified i sericitized zone 2' 5 exposed on edge of la outcrop; qtz. stringer ^"-2" wide; trace sulphides minor carb.

white qtz. vein rubble < l7<, sulphides^ -py. -minor staining along fractures; moderate carb.

quartz vein 1-1^' wide in sheared 61 bx mafic volcanics; l-5% py . ; heavily chl i carb. -vein traced 40'

14

41+20W, 0+60S quartz vein 2-8" wide in amphi- grid C on shore belite; white; trace sulphides of Pike Lake

19+80W.23+80S grid A-South

23*20W,33-f50S grid A-South

28*40W,1(H80S grid A-South

31-t-OOW,16*40S grid A-South east shore Mac- Donald Lake

56+05W.23+805 grid C-West south shore Pike? Lake

55+40W.H + 30S grid C-West west shore Pike Lake

white quartz vein rubble in la < 5 vein up to 10" wide?-chl-carb.

heavily sheared rubble-ser-chl- O carb-blue qtz. eyes; probably 3c-felsic tuff; IX pyrite

sheared S. carb mafic tuff < 17o py- < 5 very fine-carb.

white qtz vein 5" wide at 50/40W O in amphibolite-no sulphides

white qtz vein 10" wide at 80/45N in felsic tuff (qtz-eye); chl-minor Fe staining-no carb.

quartz-carb vein 10" wide in an < 5 intense sheared zone @ 330/60W; heavy carb in vein, < 17, f ine py.

<0.001

<0.001

<0.001

<0.001

<0.001

<0.001

ll l l l l l l l l ll l l l l l l l

A3

jJampJ. No.

15642

15642

15642

15642

15642

15642

15643

15643

15643

15643

15643

15643

15643

Locat ion Description

grid C-West Hologden Mine

57*52W,24*34S grid C-West Hologden Mine

sheared zone in amphibolite; minor qtz veinlets "CI" wide; moderate carb.

Gold ppb. Oz./T.

CO.001

57-f40W,24*26S grid C-West Hologden Mine

57*34W,24*24S grid C-West Hologden Mine

57+26W.24+16S grid C-West Hologden Mine

57+34W.24+25S grid C-West Hologden Mine

56+40W.24+78S grid C-West Hologden Mine-E.

as above

28+50W.28+30S grid A-South

quartz vein 2' wide (Main Hologden vein)-vein composed of grey-white qtz stringers l"-8" wide in carb, f* sheared amphibolite (entire zone about 2' wide;trending 48/90 trace py, cpy; composite chip across 2'

quartz vein as above; 20' further NE along vein-grab sample

sheared amphibolite-wall rock 13 to vein; light carbonatization; <I7a f ine dissem py.

quartz vein as 156425; 30' further 6 to NE-grab sample

grab sample of qtz vein material 8 from dump; description similar to 156425

white qtz vein 1.5' wide in qtz-eye 5 felsic tuff; lightly rusted S carb.

as above

28W.21+80S grid A-South

27*80W,20*40S grid A-South

as 156435

qtz rubble from pit < 5

quartz vein 2' wide inopen cut pit; 11 white qtz; heavily chloritized carbonatized along fractures; trace cpy, py.

as above 7

white qtz vein up to 2' wide in < S qtz-eye felsic tuff; no sulphide; very minor carb.

sheared zone; 8' exposed; sheared 5 felsic tuff?; heavily carb. 6 sericitized; many qtz stringers up to 3" wide; l-2% fine dissem. py; cor relates with major SW conductor

as 156435 <5

-(0.001

CO.OOl

CO.001

CO.001

^.001

^.001

-co.ooi

^.001

CO.001

^.001

^.001

co.001

l l l l l l lll l l l ll l l l l l

Sampl No.

15643

15643

15643

15644'

15644

15644:

15644!

15644'

15644.'

15644*

15644^

Location Description

28+001^,20+008 grid A-South

33+40W.23+80S grid A-South

33+20W.24+OOS grid A-South

33+2014,24 + 208 grid A-South

63+508,25' E. of Line 0+00 extension fr. D grid

64+408,140' east of line 0+00 extension from D grid -trench

17+30E.10+30N grid B-west sh. of MacDonald Lk in narrows about 100' n. of old bridge

16+OOE, 3+50N grid B-trench

white qtz vein 4"-lV; heavily chloritized 6 carbonatized; <l%, py, cpy; minor malachite staining

white to smokey qtz vein up to 2' wide in sheared mafic vol canics (40 1 wide); in old trench, well filling in; trace py; moderate chl-carb-composite chip across 2'

as above-grab

44

as above-dump grab

sheared ft Fe-stained qtz-eye felsic tuff-rubble; S-5% dissem py; outcrop not located by likely nearby

smokey grey qtz vein-hosted in amphibolite to gabbro?-heavily carbonatized minor sericite and Fe staining along fractures; trace sulphides

sheared S fuchsite;

carbonatized <17<> f ine py;

zone-minor silic ified

16+OOE, 3+OON grid B-trench

16+OOE, 2+80N grid B-trench

16+50E, 3+70N grid B-Lrench

16

17

11

intensely altered mafic volcanics? 15 -silicified-very minor carbonate; very rusted weathered surface;-C12! very fine py; several irreg qtz fractures

intensely altered volcanics; very 10 silicified 6 sheared; white boudinaged qtz. veinlets; 5/5 finely dissem and subhedral py.

8" qtz vein in above alteration < 5 zone; white qtz; highly fractured with Fe-carb; 'Cl-2% py and cpy.

intensely altered mafic? volcanics; 7 heavily silicified; <l% fine dissem py; moderate fuchsite; minor carbona tization; wall rock to white qtz vein (156448)

A4

Gold ppb. Oz./T.

CO.001

CO.001

^.001

^.001

^.001

CO.001

CO.001

CO.001

CO.001

CO.001

l l l l l l ll l l l l l l l l l l l

Slampl

15644

15644

15645

15645

15645

15645

15645

15645

15645

15645

15645

15645

15646

Locat ion Description Gold ppb.

16+50E, 3+70N grid B-trench

16+OOE, 8+90S grid B

16+60E, 9440S grid B

8+10E, 1+70N grid B

8+10E, 1+70N grid B

12430E, 3+40N grid B

10+60E, 5-t-OOS grid B

pit; qv rubble; heavily rusted qtz; 8 l-3% py along fractures; 37a f ine dissem specks mt; minor chl-carb. alt. along fracs.

C5from same pit as above white qtz. with dark green-black chl alt. along fractures; trace py.

white qtz vein; l' wide; hosted in -C5 f.g. mafic volcanics; minor chl-carb alt.; vein in pit

pit; qtz vein 2" wide; smokey- 121 white; moderate chl-carb alt. along fractures; < 17a f ine-medium py; vein @ 90/90

11+lOE, 1+10S pit SW of shaft-main vein? 2' wide- < 5 grid B interbedded white to smokey qtz vein Holding Prop. and chloritized 6 carb, amphibolite; -composite chip light to moderate shearing; < l7° f ine over 2' dissem py; vein 60/75 S.

11+40E, 0+40S dump grab of above vein material 11 grid B Holding Prop.

12+60E, 0+60S grid B Holding Prop.

as above

7+20S, 5+20E grid B

3+30E, 7+30N grid B

A5

Oz./T.

^0.001

white qtz vein-rubble; vein < 5 l'-2' wide?; heavily fract ured with Fe-carb; trace py.

brecciated mafic? volcanics; < 5 intense silicification;moderate carbonatization; l-3% very fine dissem py.

altered felsic intrusive? intense < 5 •CO.001 silicification 6 fuchsite alteration; <l7o f ine dissem py-rubble but outcrop likely nearby

iO.OOl

.ooi

^.001

0.004

CO.001

CO.001

pit-white qtz vein; 110' east of 11 shafts-east extension of main vein; similar description as above

dump grab of above vein 8

sheared fi c arbonatized mafic tuff? < ^ "CO.001<l% fine dissem py-near VLFconductor

white qtz vein l"-4" @ 30/80N; 5 <0.001hosted in amphibolite; trace py;intense carbonatization in wall rockfi a long fractures in vein along with chl.

l l l l l l ll l l l l l l l l l l l

A6

Sampl No.

15646

15646

15646

15646

15646

15646

15646

15646

15646

15647

15647

15647

Locat ion

4+80E, 4+OON grid B

as above

4+OOE, 4+OON grid B

3430E, 2+OON grid B

4+OOE, 6+OOS grid B

grid B

15+30E.15+60N grid B

as above

14+20E.10+90N grid B

grid B

9+90E.12+80N grid B stripped area

10+OOE.13+40N grid B stripped area

4+OOE.12+40N grid Bstripped area east pit

De ser ipt ion Gold ppb. Oz./T.

pit or shaft-9 1 to top of water 17 ^.001lots of dump material-20-30'deep? qtz. vein 1.5'-2" wide75^0S;ribboned in amphibolite;moderate to intense carb-chl.alt. <l-2% fine dissem py-dumpgrub

as above 38941 1.133

quartz vein rubble 80' west of 222 0.006 above shaft; trace cpy

carbonate sheared zone 8' wide? < 5 •(O.OOl ribboned with qtz-carb stringers sheared @ 60/65S; trace py.

smokey qtz vein l'-3' wide; < 5 "CO.001 ribboned in mafic tuff (silici fied); minor rusting along fractures

sheared zone-mafic flow silici- < 5 •iO.OOl fied-carb-py.d/O

boudinaged qtz vein (smokey) < 5 *C0.001 1"-2V; hosted in sheared mafic pillows; trace py-carb -2.5' composite chip

grab of above vein O 'CO.OOl

sheared zone; 67/55S silicified, < 5 ^ .001 carb (minor)-trace fuchsite; vp to 1 7o cubic py; sericite alt in places

same zone as 156469-trench 20' < 5 -CO.001 west of previous sample-grab

smokey to white qtz vein at 20/90; < 5 -(0.001 perpendicular to shearing; l'-2' wide trace py; light carb f* c hl alt.

smokey qtz vein 6"-2' wide in O ^.001 sheared zone at 100/803-trace py; light carb-chl alt; vein boudin aged- very similar

pinch 6 swell smokey qtz vein 137 0.004 ^"-1.5'; hosted in sheared amphi bolite 60/90; vein heavily rusted; l-2% fine dissem py; intense carb, along fractures; moderate chl alt.

l l l l l ll l l l l l ll l l l l l

A7

Samp li No.

15647-

15647!

156471

Location

as abovemain pit

as abovewest pit

4+25E,18+80N grid B

Description

as above

as above

sheared 6 silicified zone near edge of lake; rusted weathered

Gold ppb .

119

415

5

Oz./T.

0.003

0.012

^.001

15647'

15647!

15647!

15648(

156481

15648;

15648:

1564 8-!

15648?

15648(

grid B

2+20E, 1+90N grid B

2+OOE, 0+35N grid B

2+35E, 3+50S grid B

as above

2+OOE, 0+OOBL grid B

O+IOW^O+SON grid B

grid B

12+OOW.18+OON grid B 20' W. of M-798903

20+OOW, 9 + 70N grid B

surface; light grey aphanitic; intense silicification minor carb; trace py .

qv-white; 6"-!'; hosted in same 23 0.001 sheared zone as 156476; heavily rusted along fractures-Fe-carb? trace py.

white qv; l'-2.5'; 70/90; minor chl-carb alt; no sulphides; hosted in amphibolite

white qv; 5' at 60/90? light Fe 8 ^.001 staining along fracture heavily - carbonat ized; no sulphides

trench-several white to smokey qtz 6 ^.001 veins < l" t o 5" @ 120/80S; hosted in sheared amphibolite; intense chl- carb alt; < 17<, f ine py-grab sample

as above

qv rubble just south of 5' qv 6 ^.001 (156479); 1-107, coarse subhedral py ; heavy chl-carb alt; no outcrop located

qv; white; l'-2' wide; minor rust- 10 ^.001 ing; hosted in amphibolite-near felsic tuff contact

trench; 2?qv's 2'2.5 ! wide @ 140 0 ; 5 -CO. 001 hosted amphibolite near felsic tuff contact light chl-carb alt; no sulphides

irreg. smokey-white pinch 6 swell 9 CO. 001 qtz vein ^"-8" @ 20/90; light rust ing; trace py ; minor chl-alt.

smokey-white qtz vein rubble- 5 -CO.001 likely near outcrop?; hosted in intermed. tuff; silicified trace py.

1 111111111111111111

^Sampl No

15648

15648

15648

15649

15649

15649

15649

15649.

15649

15649.

15649

15649.

15649'

Location

23+50W, 7+40S grid Bflat veingrab

as above

7+508,23+OOW

as above

32+OOW, 4+OOS grid B

44+OOW, 2+OOSgrid B

44+80W.29+60Ngrid BNorth

44-i-30W,30*40Ngrid BNorth

as above

42+OOW,34+60N grid BNorth

40*OOW,32*60Ngrid BNorth

40-)-OOW,32*80Ngrid BNorth

404-OOW,34*OONgrid BNorth

Description Gold ppb .

qtz vein stockwork? area 60x 7 100' exposed; 2 main sets 120/90S sub-horizontal; white; *C1"-1.5';rusted S carbonatized; <l%-2% py 6cpy in places; hosted in brecciatedfelsic tuff St amphibolite (nearbyVLF conductor)

as above 7

as above-vertical vein grab 7

as above 7

quartz vein rubble possibly 23 located nearby?; smokey transl ucent qtz; 5% streaky chl; < l7<,py, cpy

intensely sheared qtz-eye felsic Otuff (105/90); carb-sericite alt.-pervasive; nil sulphides

irreg. pinch d swell smokey qtz 31vein *a"-10" @ 92/80S lightlyrusted along fractures hosted insheared pillows

pit 8'x8'x4' deep silicified 31breccia zone 3' wide @ 110/90;angular qtz 6. silicified basalt?frags in a fine grained silicous matrix; intense carb-sericite alt;l-5/^ fine dissem 6 cubic py 3' comp osite chip along west wall of pit

dump grab of above 63

white qtz vein 1' @ 70/50S (on < 5 edge of highway) footwall-shearedle

sheared i carbonatized zone; sev- 61eral boudinaged smokey qtz veinlets cV-l" subparallel to shearing (40/45S); < 17<, very fine dissem py thruout

many smokey boudinaged qtz veinlets512^" in sheared mafic volcanics;heavily carbonatized; <l% finedissem py .

pit 10'xl5'x8' deep; sheared mafic 513volcanics at 50/50S; heavily carb.;qtz vein 1-6" wide parallel toshearing; carb-chl alt-grab

A.

Oz./T.

CO. 001

^.001

^.001

^.001

0.001

-co. ooi

0.001

0.001

0.002

^.001

0.002

0.015

0.015

1111111111111111111

Sampl

15650

end o

19450

19450

19450

19450

19450

19450

19450

19450

19450

19451

19451

19451

19451

No. Location

as above

number sequence

se+oow^s+songrid BNorth

34+25W.36+25Ngrid BNorth

34+95W.36+25N

34+60W.37+85Ngrid BNorth

as above

as above

36+10W.37+35N grid BNorth

as above

80' east alongsouth claim1 ine from#3-1146633

as 194509

64+30W, 9+50Sgrid DWest

as above

16E,27-t-OONgrid B

Description Gold ppb .

as above 492

quartz vein l"-6"; smokey 9 pinch b swell; hosted insheared mafic volcanics(80790)

pit; qtz veins in fine grained ^ 5felsic volcanics; veins < l"-3"; smokey to white; no carb;wall rock sheared 58/60S; tracesulphides

as above 8

pit (open cut) 25'xlO'xlO' deep 1516sheared mafic volcanics; heavilycarbonat ized ; several smokey qtzveinlets a"-6" @ 58/55S sub-parallel to shearing; veinletsboudinaged; <l% fine dissem py thruout-dump grab qv material

as above 4665

as above-wall rock 15

trench 30'x5'xl'-2' deep shearing 2155 (t c arbonatized mafic volcanics asat 194504; likely the same shear zone150" further along strike compositechip across 4 '

as above-grab 18661

pit-filled in; sheared amphibo- < 5lite @ 120/70S; several white-smokey qtz veins 1"-!' parallelto shear; < 17o f ine dissem py; lightchl-carb. alt. -grab of qtz vein

as 194509 5

white qtz vein rubble on hillside 7along Wild Dog Lake-area 120'x60'large angular qtz light carb-chlalt along fracs; trace py-grab

as above 10

carbonate altered zone @ 50/80S < 5sheared; light green to creamy; moderate carb-sil alt; rustedweathered surface; minor whiteqtz veins O"; trace py-grab

A!

Oz./T.

0.014

-CO. 001

*C0.001

CO.OOl

0.044

0.136

CO. 001

0.063

0.543

^.001

CO. 001

l l l l l l l l l l l l l l l l l l l

Aid

jJampJ^ No.

19451

19451

19451

19451

19451

1945]

Location

as above

44E, 0+40N grid D

36E.14+OON grid D

29*50W,BLO grid A

35+40W, 6+OOS grid A

20+30W, 6+50S grid A

Description Gold ppb. Oz./T.

as above

intense shear zone 85/80S; chl-carb altered; buckled S contorted beds; trace? sulphides

trench-qtz vein l'-2' ribboned; heavy chl-amph alt; vein white; trace py.

pit 6'x5'x2' deep sheared mafic volcanics-chl-carb alt.; white qv rubble 6" wide @ 90/65S?

sheared zone 15' exposed; @ 90/60S; coarse grained volcanics lightly rusted; trace sulphides

boulders-mafic volcanics; carb.; several white qtz fractures 6. veinlets <k"; t race pyrite

1 1 1 1111111111111111

4fc APPENDIX B SURFACE SAMPLES TAKEN BY J. L. TINDALE

JUNE-AUGUST 1990 FOR ASQUITH RESOURCES INC.

ON THE ASQUITH TOWNSHIP PROPERTY

Samp] .No. Date/Location

17104 June 27, Gibson CI.300'S,60'W,#1 post1146633

17104 June 27, Gibson CI.as above

17104- June 27, Gibson CI .as above

17104' June 27, Gibson CI .150 'S of in show ing above

171051 June 27,Gibson CI.Tower hill pits

17105 June 27, Silica Veinoff dump road west;S. T.

17105: June 27, Silica Vein

17105: June 28, Natal Twp.

17105' July 6, D GridL12W, 13420N

17105.' July 7, on MacDonaldLake, Onitap CI.//573098

17105i July 7, same as above

17105' July 7, near //l postof CI . //1146633

tr .

Descr ipt ion

blue grey qtz carb, 1" veins alongschisosity, to py.From pit.Grab

blue grey qtz from east end pit.Minor V.G. Grab

shistose wall rock from pit withxls py, med. e.g. gn. gy. carb.rock. Grab

blue gy . qtz veins in poorlysheared wall rock, tr. v.f. g. py .Grab

shear zone with conglomeratephases, blue qtz veins with 2 7o± pyrite, <3% wide shear. Grab

quartz, wh, e.g., with sulphidealong edge, possible Mo, pyrite

quartz, white, pure

dark green mottled with gy. wh .qtz, cherty matrix, dissem. cpy

carbonate porphyry, laced withi/8-V q-c veins, tr green fuch site, eg. pyrite cubes

sheared carb-rich mafic vole.,with blue qtz veins as "boudins"along shear planes, py . cubes dissin wall

bl . to dark grey qtz grab, tr. pyr i t e

pit with dark grey qtz, shearedcarb-rich cerp. like boundary,

pyrite

Bl

Values

557 ppb0.016 opt

980 ppb0.029 opt

120 ppb

17 ppb

25 ppb

221 ppb, 0060 optCu 17 ppm, Pb 39 ppmZn42 ppm, Fe 3.39%Mo 390 ppm

S:0z 94.77,Au 17 ppb

Ag < l, Cu 1.847oPb 15 ppm, Zn 47Au 23 ppb

32 ppb

5 ppb

.

10 ppb

6099 ppb, 0.177 optCK. 22238 ppm, 0.647 opt

1111111111111111111

SampLNo.

17105,

17105'

171061

17106:

17106!

17106!

17106^

17106.'

17106*

17106/

171066

17106S

17107C

Date/Location

July 10,6+508,12415grid A

July 11 ,6*65N,84-20Wgrid D

July 11,64-65N,8*20W grid D-Clarke

July 11,6*65N,8*20Ngrid D-Clarke

July 11.6+85N.7+90Wgrid D-Clarke

July 11,7400N,8*OOWgrid D-Clarke

July 11,12N,7*90W grid D-Clarke

July 11,20'N of 064grid D-Clarke

July 11,15'N of 065grid D-Clarke

July 11 ,150'NE of12N on Line 8E ,50'SE of //3 post918977

July 11, as 067grid D-Clarke

July 11,1008 of //3 post 918977grid D-Clarke

July 11, Vein 5'Sparallel ci to069

B2

Description Values

white qtz vein in granophy . db?, 50 ppbminor pyrite

pit, sample 1' on F. W. chip in 38 ppbporphyry

9" quartz vein with pyrite in 181 ppb porphyry

pit, 2' chip in HW of main vein, 8 ppbgn. porphyry

1' chip across vein, carbrich with 62 ppbfuchsite, pyrite

N.W. striking sheared tt with 1"- 46 ppb6" white qtz mainly flat lying, chip3' of rusty bn, beige sheared i with py.

10' tr., NS, altered qtz porphyry, 14 ppb network white qtz, f. g. py , gnmariposite, very rusty, 2V chip

5' pit, n. end of trench, porphyry, < 5 ppbf. diss. py with bright greenmariposite, % -k" wh. qtz strs. Chipacross 4'

4' pit with wh qtz strs N-S, vert 14 ppbdip, across pit. Chip 4' across face pit

10' deep pit with water, 5' wide 63 ppbqtz, fractured, with gn. chl. strs.,streets of f. g. py, FW:lt withrusty shear, st. NW, 65" dip SW.Chip SE face 4'

chip sample rusty gn. porphyry 50 ppbwith blobs e.g. py, qtz stringers,bright gn with f. w. qtz, fuchsite.Chip 3'

pale gn carb, rusty, NW str. qtz 26 ppb vein, IV wide, dip 60 0 SW. Chip1.5'

6" wh qtz in gn carb, mariposite, 24 ppbhoy cubic pyrite. Chip 2'

1111111111111111111

0Samp LNo.

17107

17107

17107

17107

17107

17107

17107

17107

17107

17108

17108

17108

Date/Locat ion

July 11,5'SE of070, grid D

July 11, FW 071grid D-Clarke

July 16,12N L12Wgrid D-Clarke

July 16,13+SON L12Wgrid D

July 16,15N 11+75Wgrid D

July 16, as abovegrid D

July 16, as abovegrid D

July 16, 16N, 12W grid D

July 16, as abovegrid D

July 16, 5W 12 Nstrip areagrid D

July 15, L8E 4+50S grid A-Kuckingham

July 16, L8E 4+50Sgrid A-Buckingham

Description

rusty gn carb, porphyry, lacedwith V'-V qtz veins, py dissthruout , 3" chip of pit vein

Wellsheared, heavy qtz veiningrandom orientation, NW shearing,parallel veins, dip SW, 3'chip in FW of 071

porphyry with E-W qtz-carb veinsl"-5", py , rusty, 6' chip alongoutcrop

50' long tr. with pit, NS tr, strs white qtz, fuchsite, pyrite heavy.Chip 3' along trench face

pit with bright green carb.py,ribbony qtz-carb veins, maripositeheavy chip 3' N end of Tr .

trench up oc . to north from pit,rusty carb, green mariposite, py,random network qtz-carb veins,4 ' chip across trench

grab of west side Tr, wavy shear ing, green mariposite-like mica,carb rich

pit trenches, EW greeny white qtz- carb veins in green white alt.carb, py , chip 3', mostly qtz.

veins and rusty porphyry wallrock, dk. green in places, 1-2/5 pywell sheared, 3' chip mostly wallrock

stripped area, old trench, 3.5'chip across face of old pit, carbporphyry with mariposite, flatlying qtz veins, NW strike

pit, grab of blue qtz vein in FW of tr.

4' chip sample incl. 1' blue greyqtz, pyrite, common and in heavystreaks, well sheared 61 carbonatedsir. of vein 260 0 . Dip S @ 70 0

B3

Values

16 ppb

13 ppb

179 ppb

.77 ppb

9 ppb

7 ppb

9 ppb

32 ppb

36 ppb,

O ppb

666 ppb .019 opt

989 ppb, .029 optCK1450 ppb, .042 opt

1111111111111111111

Sampl'No.

17108

17108.

17108

17108'

17108

17108

11710 3-1711" D

14880-1488- 9

1488]'

14882

14882

Date/Location

July 16, as abovegrid A-Buckingham

July 16grid A-Buckingham

July 16, as abovegrid A-Buckingham

July 16, as abovegrid A-Buckingham

July 16,20'E ofL10E @ 4+50S appr. grid A-Buckingham

July 16, Ed Jamesshowing on Bucking ham rd. Appr 5+50W 3+OOSgrid A-Buckingham

resample of DDHB89-5

resample of DDHB89-5

July 27, resampleB89-6

July 28,L44W 2+OOSgrid B

July 29,L8W 4+20Sgrid A

Description Values

grab of veining on southend of 2693 ppb , 0Tr. blue qtz with diss. streaks CK 3970pyrite 0.116 opt

approx 30' E of above, 12' NS 817 ppbtrench, 3' deep, vein swells to 0.024 opt6' wide, wall rock well sheared,heavy pyrite in vein 6 dark gn.,carb-rich wall rock. 2' chip Nend vein

IV chip of central veined section 2861 ppb, .CK 46200.135 opt

3' chip over south portion of 6218 ppb, 0veined section, mixture of rusty CK 5850wall rock i blue qtz veining 0.171 opt

close to hole //6, stripped out- 145 ppbcrop, well sheared, pale gn. carb- .004 opt rich, blue qtz veins ^-2" wide,diss pyrite, 5' chip along edge ofoutcrop in NS direction

clean trenches, could not find 11 ppbvein in place, grab of grey qtzwith pyrite

ree 'dplot on DDH

ree 'dplot on DDH

rec'dplot on DDH

silicified shear, beige to brown, 5 ppbdk green with blue qtz eyes infresh oc , trace py, non carb,white qtz along shear planes EWstrike

Ed James showing, line of trenches 8 ppbfollowing white grey qtz vein 6.strs. in dark gn . foliated wall rock,Str 290 0 , dip SE @ 40 0 tr py , carbrich, tr. tourmaline, lV chip grab

B4

.078 opt

083 opt

.181 opt

log

log

log

1111111111111111111

^^ Sampl

No.

14882

14882

14883

14883

14883

H883

14883

14883

Date/Location

July 29, L9+40W5+25Sgrid A

July 29, LO, 2+OOSgrid A

July 31 , S ext . ,Line 0, 495or445 grid A

July 31, as above

Aug. 4,4*50E,16Ngrid C

Aug.4,4450E,16Ngrid C

Aug. 4,3*50E,16Ngrid C

Aug. 4,2*50E,8N Kubiakgrid C

Description

located by R. A. , series of EWblue grey qtz veins in carb-richshear zone, dark gn. tuff wallrock, trace pyrite, str. 90 0 , dip 90 0 . Chip Sample 6' taken inseries of V to 6" blue qtz veins

at E edge of outcrop, blastedrock, grab of green f. g. tuff,moderate foliated with whitesugary qtz, trace carb, tr f.g.,py

pit (3 MacDonaldLake/Seager cr.junction, with blue gy qtz, heavy streaks pyrite, sheared silicifieddk. grey host, vein 12" wide ond'ump, grab best vein

quartz veining as above, largefrom dump-grab

shallow pit with 1/8"--^" blue-.white qtz veins in sheared pale gncarb rich rock, 4' chip, f. g. pydiss .

4' chip next to above, note EWstrike, dip vertical

EW white qtz vein, 2' wide, inlong EW trench in sheared palegreen carbonate-rich W. R. sample2 }-i' chip mostly vein

pit with blue qtz vein in black sheared, carb-rich host rock, py .rich W. R., serp, grab of wall rock

B5

Values

8 ppb

5 ppb

-

5 ppb

8 ppb

300 ppb.009 opt

46 ppb

<5 ppb

707 ppb .021 opt

sheared with blue qtz injected along

14883

14883

14883

Aug. 4.2+80E.8Ngrid C

Aug. 4,2*80E,8Ngrid C

Aug. 4,2-(-80E,8Ngrid C

shear planes

sample pit @ edge of swamp 20'Eof 15' shaft/pit, sheared pale gncarb rich tuff with 1/8-1" blueqtz veins, 2% py, chip across 2 k'

next to above west, 4' chip ofcarb-rich pale green tuff, shearedminor blue qtz strs., pyrite 1 -27,along shearing

grab of best of 837 with k " b lueqtz stringers S 2% py.

584 ppb.017 opt

901 ppb. .026 opt

89 ppb.003 opt

1 11111111

tSamplNo.

14883

14884

14884

14884

14884

14884

Date/Locat ion

Aug. 4.2+80E, 8Ngrid C

Aug. 4.2+80E, 8Ngrid C

Aug. 13,68E H60Ngrid D

Aug. 14,L8E 4+50S200' westgrid A

Aug. 14, as above

Aug. 16.L4E 12+40Ngrid B

Description

mainly 12" blue grey qtz, coarsegrd, str 280 0 , dip S @ 70 0 , withminor pale green carb wall rock6 pyrite. 2 ! chip

grab of vein material from above

grab of white qtz in si. shearedrusty, pale green aphanitic tuff

grab of weathered blue grey qtzfrom stripping, rusty, tourmalinerich, pyrite leached

fresh grab, stripping area, 2-5%py, trace argentite?, heavytourmaline, blue grey qtz, chloritearound pyrite cubes

stripped area-grab of blue greyqtz strs. and 3" vein, l-2% py .

B6

Values

1137 ppb0.033 opt

2733 ppb0.08 opt

13 ppb

138 ppb.004 opt

781 ppb.023 opt

140 ppb.004 opt

in wall rock, east end of stripping

1

1

1

1

1

1

1

1

1

1

14884

14884

14884

14884 l

14884 i

1488! )

1488!

Aug. 16.L4E 12+40Ngrid B

Aug. 16, L4E 4Ngrid B

Aug. 16, L4E 4Ngrid B

Aug. 16, as above

Aug. 16, as above

Aug. 19, 230 'W L8E4 Sgrid A

Aug. 19, as above

grab of blue, white, grey qtz from 83 ppbmain pit in centre of stripped area,tr. py.

transparent to white qtz, with dk.green inclusives, chlorite rich,pyrite, fine qtz strs. in wall rock (amphibolite). Grab fromshaft dump

grab from shaft dump, shearedwall rock, l-2% py, carb-rich107o qtz.

white to transparent qtz, rarepy, rare green chl, all vein,v.c.g. qtz, grab shaft dump

intensely sheared wall rock,malacite stained, 50% blue qtz,injected along shear planes, py . 2-3%, grab shaft dump

grab of blue qtz from strippedarea, e.g., rusty leached py ,chlorite replacements

rusty heavy sheared wall rock with 2-3% py along shear, 1 07ablue qtz boudins along shear

24 ppb

10485 ppb.305 opt

8 ppb

517 ppb.015 opt

8 ppb

9723 - 0.283 opt

B7

Sampl

14885

14885

14885

14885

148851

14885',

14885*

14885G

14886C

Date/Location

Aug. 19, L.02+65N grid A

Aug. 19,as above grid A

Aug. 19,as above grid A

Description Values

trench with blue qtz, str. 60-80, 13 ppb vertical 2' wide with strs in wall rock, tr. py, cpy, 6' W of line grab

grab vein on line, blue qtz with yellowish carb inclusions, ag, tr py 2" wide vein

ppb

grab wall rock, sheared pale gn. 6 ppb carb, soft, minor blue qtz boudins, tr-Upy.

Aug. 19,25'N, 0+80WBLgrid A

stripped oc . with rough knobbly < 5 ppbsurface, blue-grey qtz veins @70 0 , south dip steep, rusty leachedpy, zone 12' wide, 6" vien grabsampled

Aug. 19,cat fillroadgrid D

Aug. 19,N side fill grid D

Aug. 19,Grab E. side Stewart Lk grid A

Aug. 21,stripping Oni tap

Aug. 21,stripping Onitap

148861 Aug. 23,I,6E 15N

148862 Aug. 23.1.6E 15N

148863 Aug. 23.5+50E 15N

148864 Aug. 23,5+SOE 15N

blue grey qtz, pyrite tr, 6", 90" 8 ppb strike, 5' strong shear in pale green carb

grab of wall rock, intense shear 1411 ppb with boudins of ^-1" blue qtz, 4' .041 opt wide shear, 2-4/^ py, pyrite cubic and f.g. along shear

felsic shear zone, qtz strs, tr 6 ppb pyrite

E. of Gibson, S. shore Moore Lake, 207 ppb grab of blue qtz from vein dump

grab of sheared wall rock with 65 ppb 1055 blue qtz, py.

east of Stewart Lake, sheared 9 ppb peridotite?, with white qtz, grab of qtz.

sheared yellowish wall rock with 5 ppb trace pyrite cubes

at south shore of bay on Stewart 82 ppb Lake, 12' wide white qtz in pale green vole, not well carb, tr py, grab white qtz.

pale green wall rock, sheared, 7 ppb f.g. py along shear planes, 103? qtz strs.

l l l l l l l l l l l l l l l l l l l

B8

Samp] ; No.

1488( i

Date/Location

Sept. 7.L20E grid A

Description

channel samples reported else where

Values

7 ppb

14886 t Sept. 4,Hassett Lk area

grab rusty shear from pit W. Ag. Ippm of Hassett Lake, qtz injected Cu 29 ppm along shear planes, Z-3% to Zn 13 ppm massive py, assay Cu,Zn,Pb,Au,Ag

11 ' 1 1111111111111111

ft

Samp ; No.

19491 l

9( l

9( !

9( t

9( i

9C .9C '

9C i

9C

91 '

91

91

91

91

9]

9]

91

91

91

92

92

92

92

92'

92.

92i

92

92!

92!

93(

93;

Length

3.0'

3.0'

5.0'

5.0'

5.0'

4.0'

5.0'

4.0'

3.0'

5.0'

1.6'

5.0'

6.0'

5.0'

5.0'

5.0'

3.0'

5.0'

5.0'

4.0'

4.0'

4.0'

3.0'

4.0'

4.0'

4.0'

6.0'

4.0'

3.0'

4.0'

6.0'

APPENDIX C CHANNEL SAMPLE RECORD

AUGUST- SEPTEMBER 1990 FOR ASQUITH RESOURCES INC.

ON THE ASQUITH TOWNSHIP PROPERTY

Description

carb altn, shearedII 1 1 H

II 11 11

It 11 M

II 11 II

veiningM 11 M

It II It

It 11 It

11 li 11

rusty11 II 11

" " " veining

veining

veiningII It M

It II 11

It 11 It

11 II It

veining

weak F. W. shear

heavy foliation, F. W.

F. W. carb, brown, q.v.

F. W. carb, brown, q.v.

vein main, +HW

H. W. zone

F. W. carb, white q.v.

F . W . carb, wh i t e q.v.

main vain with shear

H. W. shear with veins

H. W. shears

CI

Values

6 ppb

32 ppb

27 ppb

231 ppb, .007 opt

7 ppb

9 ppb

91 ppb

13 ppb

43 ppb

44 ppb

8 ppb

9 ppb

294 ppb, '.009 opt

<5 ppb

5 ppb

90 ppb

8 ppb

32 ppb

9 ppb

20 ppb

31 ppb

<5 ppb

5 ppb

5 ppb

23 ppb

14 ppb

12 ppb

21 ppb

119 ppb, .003 opt

30 ppb

19 ppb

l l l l l l l l l l l l l l l l l l l

C2

Sampl No. Length Description Values

19493

93

93

93

93

93

93

93

3.0'

3.0'

3.0'

3.0'

3.0'

4.0'

6.0'

2.0'

94

94

94

94

94

94

94

94

94

94

95

95

95

95

95

95

95

95

95

95

96

96

96

96

96

96

3.0'

5.0'

3.0'

2.0'

3.0'

3.5'

3.5'

3.0'

4.0'

3.0'

3.0'

2.0'

3.0'

2.0'

2.0'

4.0'

3.0'

3.0'

3.0'

3.0'

4.0'

3.0'

3.0'

4.0'

2.0'

2.0'

main vein shear

F.W. shear

H.W. shear, carb

Main vein shear

F.W. carb

F.W. carb stained

F.W. carb stained

main vein shear

H.W. shear

H.W. shear

H.W. shear

main vein shear

main vein shear

H.W. altn.

H.W. altn.

H.W. S main vein shear

H.W. sheared

main vein 6 H.W.

central area F.W.

vein main

H.W.

main vein

main vein

main vein - next to dyke

main vein - shear

main vein - shear

F.W. of main shear, q.v.

m. shear, part H.W. q.v.

sheared F.W.

main vein

main vein

H.W. vein

F.W. of main vein

main vein junct. with F.W. vein

201 ppb, .006 opt

41 ppb

67 ppb

156 ppb, .005 opt

<5 ppb

<5 ppb

16 ppb

2070 reassay1296 ppb, .038 opt

9 ppb

255 ppb, .007 opt

93 ppb, .003 opt

52 ppb

38 ppb

391 ppb, .006 opt

217 ppb, .006 opt

12 ppb

193 ppb, .006 opt

93 ppb, .003 opt

24 ppb

2248 ppb, .065 opt

42 ppb

1905 ppb, .055 opt

3099 ppb, .090 opt

10406 ppb, .303 opt

671 ppb, .020 opt

795 ppb, .023 opt

2307 CK, .067 opt 2267 ppb, .066 opt

5416 ppb, .158 opt

961 ppb, .028 opt

6772 ppb, .197 opt

66535 ppb, 1.936 opt

2248 ppb, .065 opt

348 ppb, .010 opt

478 ppb, .014 opt

l l l l l l l l l l l l l l l l l l l

C3

Sampl

19496

96

96

96

No, Length

3.0'

4.5'

3.0'

2.0 1

Descript ion Values

97 i

97

97

97 ;

97

97 .

97 ,

97

97 i

97 i

9f )

9f

9? !

9* 1

9* .

9J i

9J )

9! '

9i 5

9? )

9? )

9! L

9' l

9' l

9! *

9 ( i

9' S

9' 1

2. 0 12.0'

5. 0 14.0'

2.0'

3.0'

4.0'

3.0'

4.0'

3.0'

2.5'

3.0'

2.0'

2.0'

2.0'

2.0'

3.0'

2.0'

2.0'

2.0'

4.0'

5.0'

3.0'

2.0'

3.0'

2.0'

2.0'

1.0'

5.0'

F.W. fold veins

F.W. sheared

main vein

H.W. vein

H.W. vin swings S.

F.W. vein

F.W. shear/carb.

F.W. vein shear adj. main vein

across vein nose (fold)

E/W across fold nose

E/W across fold nose

H.W. shear

main branch vein, fold arm

vein - N. limb

F.W. carb, veins

F.W. carb

F.W. vein

F.W.

line 8 section; F.W., br. vein

F.W.

qtz 6- carb, F.W.

intense qtz/carb

main vein?

H.W.

main vein qtz/shear

H.W. of S. limb

vein

H.W. of vein - 80% qtz

qtz - carb fold

S. limb - qtz

S. limb - qtz

S. limb - qtz

H.W. poor altn. with qtz

94 ppb

51 ppb

1023 ppb, .030 opt

4089 ppb, .119 opt 3733 ppb, .109 opt

1168 ppb, .034 opt

452 ppb, .013 opt

1657 ppb, .048 opt

753 ppb, .022 opt

3455 ppb, .101 opt

3505 ppb, .102 opt

1839 ppb, .054 opt

92 ppb

4297 ppb, .125 opt

2153 ppb, .063 opt 1827 ppb, .053 opt

421 ppb, .012 opt

532 ppb, .015 opt

1702 ppb, .050 opt

167 ppb, .005 opt

14 ppb

460 ppb, .013 opt

8267 ppb, .240 opt

974 ppb, .028 opt

3297 CK .096 ppb 3119 ppb, .091 opt

689 ppb, .020 opt

614 ppb

869 ppb

018 opt

025 opt

841 ppb, .024 opt

218 ppb, .006 opt

4624 ppb, .135 opt

2703 ppb, .079 opt

2356 ppb, .069 opt

3703 ppb, .108 opt 4056 ppb, .118 opt

7 ppb

1111111111111111111

Samp] ' No.

1949? 1

1948C .

8( !

8( !

8( .

8( t

8( i8C '

8( 1

8( i

8] 1

8]

8] .

83 .

81

81 .

81 .

81

81 ,

81

82 i

82

82

82

82

82

82

82

82

82

83

83

83

83

Length

5.0'

3.0'

2.0'

2.0'

2.0'

2.0'

2.0'

2.0'

3.0'

3.0'

3.0'

3.0'

2.0'

3.0'

3.0'

3.0'

4.0'

2.0'

2.0'

2.0'

2.0'

2.0'

3.0'

2.0'

2.0'

2.0'

3.0'

3.0'

5.0'

5.0'

2.0'

3.0'

2.0'

3.0'

Description

H. W. poor altn. with qtz

H. W. south side

H. W. vein 5"

H. W. south

F . W . ve in

F. W. vein

vein

H. W.

fold 6 veins

fold S veins

fold 6 veins

fold i veins

fold ft veins

shear with veins

shear with veins

H. W.

shear folded

shear ^ vein

shear 6 vein

main vein

main vein

main vein

H. W.

shear Si vein

F. W.

sheared fold

sheared fold

shear vein

centre line of fold

centre line of fold (nose)

F. W. vein shear

F. W.

F. W. shear

F. W. shear

Values

13 ppb

10 ppb

35 ppb

16 ppb

100 ppb,

1137 ppb,

380 ppb,

231 ppb,

580 ppb,

424 ppb,

93 CK122 ppb,

92 ppb

462 ppb,

2036 ppb,

283 ppb,

962 ppb,

78 ppb

5059 ppb,

125 ppb,

508 CK, .568 ppb,

269 ppb,

83 ppb

14 ppb

134 ppb,

57 ppb

504 ppb,

161 ppb,

714 ppb,.

196 CK, .282 ppb,

67 ppb

5871 CK,5851 ppb,

42 ppb

8 ppb

103 ppb,

C4

.003 opt

.034 opt

.011 opt

.007 opt

.017 opt

.012 opt

.004 opt

.013 opt

.059 opt

.008 opt

.028 opt

. 147 opt

.004 opt

015 opt.017 opt

.008 opt

.004 opt

.015 opt

.005 opt

021 opt

006 opt.008 opt

.171 opt.170 opt

.003 opt

1111111111111111111

tSamp] i No. Length

1948: ( 2.0'

8: i 2.0'

8: ) 2.0'

s: ' 3.0'8: i 2.0'

s: ) 3.0'8O 2.0'

8t . 2 .0'

8t l 2 .0'

8M 2.0'

8^ t 2.0'

8" i 2.0'

8^ i 2.0'

8/ ' 4.0'

8M 3.0'

8M 4.0'

8! ) 3.0'

8! . 4.0'

8! l 6 .0'

8! i 4.0'

8! i 3.0'

8! i 2.5'

8! ) 4.5'

81 ' 2.5'

8! 5 4.0'

8! J 3.0'

81 ) 3.0'

8( L 2.5'

81 ' 3.0'

81 3 3.0'

81 t 3.0'

8( i 2.0'

8l i 2.0'

8( 7 4.0'

81 i 4.0'

Description

vein with shear

vein with shear

H. W. shear

fold

vein shear

F. W. shear

vein shear

vein shear

vein shear

vein shear

vein shear

vein shear

vein shear

vein shear

vein shear

vein shear

vein shear

vein shear

fold arm

shear 4 qtz

shear 4 qtz

qtz 4 folded shear

qtz 4 folded shear

qtz

rusty shear, qtz

shear 4 vein

F. W.

shear 4 vein

shear 4 vein

shear with qtz boudins

shear "

shear "

H. W. shear

vein with folded shear

sheared with qtz

Values

6950 ppb,

362 ppb,

71 ppb

478 ppb,

3257 ppb,

931 ppb,

63 ppb

2485 ppb,

232 ppb

3911 ppb,

6634 ppb,

690 ppb,

11881 ppb

2158 ppb,

3970 ppb,

8277 CK,6465 ppb,

3248 ppb,

62 ppb

1570 ppb,

1139 ppb,

3041 ppb,

278 ppb

7079 ppb,

2802 ppb,

6901 CK,3861 ppb,

583 ppb,

3386 ppb,3614 ppb,

1051 ppb,

1390 ppb,

125 ppb,

60 ppb

120 ppb,

268 ppb,

167 ppb,

952 ppb,

C5

.202 opt

.011 opt

.014 opt

.095 opt

.027 opt

.072 opt

.114 opt

.193 opt

.020 opt

, .346 opt

.063 opt

.116 opt

.241 opt.188 opt

.095 opt

.046 opt

.030 opt

.115 opt

.260 opt

.082 opt

.201 opt.112 opt

.017 opt

.099 opt

.105 opt

.031 opt

.046 opt

.005 opt

.004 opt

.008 opt

.005 opt

.028 opt

1111111111111111111

ftSamp] ! No.

1928f 1

s: .s: i8; l

s; ,8', i

8; i8', '

s; is; i8? )

8f .

8* !

8f i

8( .

8{ i

8* i

WQ t )O t 5

8* )

8' )

8? .

8' !

8? 5

8' t

8? i

8' i

8' '

8? 3

8' )

2049C .

9( J

9( 5

9( *

Length

2.0'

5.0'

4.0'

4.0'

2.0'

3.0'

3.5'

3.5'

2.0'

3.0'

3.0'

3.0'

3.0'

4.0'

3.0'

4.0'

2.0'

3.0'

3.0'

3.0'

4.0'

4.0'

2.0'

2.0'

3.0'

2.5'

4.0'

3.5'

3.0'

3.0'

3.0'

4.0'

3.0'

5.0'

2.0'

Description

shear with qtz

carb shear, minor qtz

carb shear, minor qtz

vein * shear

H. W.

vein * main shear

vein

vein

vein

H. W.

vein

vein

vein

vein

F. W.

F. W.

west of 803, wh . qtz veins

dk. gn . shear minor q.v.

dk. gn. shear minor q.v.

dk. gn. shear minor q.v.

dk. gn. shear, q.v.

irregular shear, q.v.

irregular shear, narrov; q.v.

folded shear, narrow q.v.

folded shear, narrow q.v.

edge of oc , shear with narrow q.v.

wavy shear, q.v. V

wavy shear, q.v.

wavy shear, q.v.

wavy shear, q.v.

wavy shear, q.v.

irregular wavy shear, white q.v.

irregular wavy shear, white q.v.

irregular wavy shear, white q.v.

edge shear, carb, qtz

Values

2723 ppb,

341 ppb,271 ppb,

723 ppb,

478 ppb,

682 ppb,

444 ppb,

1800 ppb,

628 ppb,

148 ppb,

765 ppb,

1508 ppb,

766 ppb,

2036 ppb,

277 ppb,

584 ppb,

14 ppb

35 ppb

25 ppb

10 ppb

32 ppb

459 ppb,

95 ppb

481 ppb,

18 ppb

2337 ppb,

42 ppb

231 ppb,

42 ppb

77 ppb

35 ppb

292 ppb,

1018 ppb,

278 ppb,

25 ppb

27 ppb

C6

.079 opt

.010 opt

.008 opt

.021 opt

.014 opt

.020 opt

.018 opt

.052 opt

.018 opt

.004 opt

.022 opt

.044 opt

.022 opt

.059 opt

.008 opt

.016 opt

.018 opt

.014 opt

.068 opt

.007 opt

.008 opt

.030 opt

.008 opt

1

92

92

92

C7

Samp] ! No. Length Description______________________ Values

2049C

l l 2049C i 5.0' shear, carb, minor qtz 152 ppb, .004 opt

l 9C i 5.0' shear, carb, minor qtz 229 ppb, .007 opt

9C ' 3.0' rusty shear, qtz vein 124 ppb, .004 opt

l 9C S 4.0' rusty shear, qtz vein 61 ppb

9C i 2.5" rusty shear, qtz vein 67 ppb

l 91 ) 1.5' intense wavy shear, edge oc. 250 ppb, .007 opt

91 2.5' gn. wavy shear, rusty 141 ppb

191 ' 3.0' gn. wavy shear, rusty 30 ppb

91 i 3.0' gn. wavy shear, rusty 137 ppb

91 1.5' gn. wavy shear, rusty 37 ppb

H 91 ' 3.0' wavy carb rusty dk. gn., waxy q.v. 168 ppb, .005 opt

91 . 2.0' main zone - intense shear 963 ppb, .028 opt

l 91 3.0' main zone - intense shear 3891 ppb, .113 opt

ni 5.0' main zone - blue qtz 918 ppb, .027 opt

m 9 1 2.5' main zone - blue qtz .050 ppb, .031 opt

91 -

91

92 i 3.0' main zone - blue qtz 709 ppb, .021 opt

92 4.5' main zone - blue qtz 1864 ppb, .054 opt

l 92 3.0' main zone - blue qtz 318 ppb, .009 opt

92 4.0' main zone - rusty 103 ppb M 60 ppb

3.0' main zone ~ rusty 1239 ppb, .036 opt

-j L 2 .7' main zone - intense shear 1152 ppb, .034 opt

l 92 2.5' F.W. 101 ppb

2.0' 6" bl. wh. qtz 499 ppb, .015 opt

H 92 5.0' main zone - intense shear 171 ppb

92 5.0' main zone - fold 159 ppb

B 93 ' 3.0' H.W. 34 ppb

93 3.0' main zone - intense shear 64 ppb

193 3.5' main zone - intense shear 86 ppb

93 2.5' main zone - H.W. 1350 ppb, .039 opt

93 3.0' main zone - intense shear 48 ppb

l 93 2.5' H.W. shear 252 ppb

93 3.0' main zone - shear 147 ppb

l 93 4.0' H.W. shear 390 ppb

93 3.7' main zone 257 ppb

1 93 3.5' H.W. shear 89 ppb

94 3.0' horst qtz vein 124 ppb

jJampJ ; No.

20494

94 :

94 .

94

94 .

94 .

94

94 ,

94 '

95 i

95

95

95

95

95

95

95

95

95

96

96

96

96

96

96

96

96

96

96

97

97

97

97

97

97

97

97

Descript ion

3.5'

5.0'

3.O 1

3.5'

4.4'

5.0'

4.3'

2.3'

3.0'

5.0'

2.0'

2.5'

2.0'

2.0'

2.0'

2.0'

3.0'

2.0'

3.5'

3.5'

2.5'

1.7'

2.5'

2.7'

2.0'

4.0'

1.0'

2.5'

2.0'

3.0'

2.0'

4.5'

2.5'

1.5'

2.0'

2.0'

5.0'

main zone

H.W. - main zone - q.v.

horst - sk, sh. q.v.

intense shear

main zone - H.W.

horst with minor q.v.

intense F.W. shear

main zone - H.W. felsic vole, blocks

intense rusty altn.

F.W. main zone - intense shear

intense rusty sh, bl. q.v.

intense rusty sh, bl. q.v.

intense rusty sh, bl. q.v.

intense rusty sh, bl. q.v.

F.W. shear, qtz boudins

F.W. shear, qtz boudins

F.W. shear, qtz boudins

F.W. shear, qtz boudins

F.W. shear, qtz boudins

F.W. shear, qtz boudins

H.W. felsic dyke, shear

blue q.v. in felsic dyke

shearing in H.W. of felsic dyke

sheared felsic dyke @ fold

Buckingham vein tr - vein gy. wh.

H.W. not well sheared

Buckingham vein

H.W. partially sheared

Buckingham vein with minor F.W. shear

H.W.

Buckingham vein

H.W. dk. gn. sheared

sheared F.W.

Buckingham vein

H.W. sheared with q.v.

Buckingham vein blue qtz with shearing

H.W. sheared with q.v.

C8

Values__________

525 ppb, .015 opt

50 ppb

60 ppb

111 ppb

67 ppb

20 ppb

115 ppb

139 ppb

25 ppb

27 ppb

220 ppb

27 ppb

147 ppb

2139 ppb, .062 opt

145 ppb

222 ppb

176 ppb

35 ppb

318 ppb

417 ppb

20 ppb

7941 ppb, .231 opt

42 ppb

24 ppb

7139 ppb, .208 opt

5o ppb

12376 ppb, .36 opt

38 ppb

959 ppb, .028 opt

70 ppb, .002 opt

3040 ppb, .088 opt

408 ppb, .012 opt

648 ppb, .019 opt

6297 ppb, .183 opt

1564 ppb, .046 opt

9030 ppb, .263 opt

23713 ppb, .69 opt

1111111111111111111

tSampl No.

20497

97

98

98

98

98

98

98

98

98

98

98

99

99

99

99

99

99

99

99

99

99

14886

86

86

86

Length

3.0'

3.5'

4.0'

2.02.0'

2.5'

2.0'

4.0'

3.0'

3.5'

1.5'

4.0'

1.5'

1.5'

3.0'

3.0'

2.0'

2.0'

4.5'

3.0'

2.0'

2.0'

3.0'

2.3'

1.5'

3.0'

Description

Buckingham vein, gy wh . qtz, blue minor

H. W. sheared with qtz strs.

F. W. rusty shear with q.v.

Buckingham vein, bl. wh. q.v.

H. W. intense shear

F. W. - shear with blue q.v. 's

Buckingham vein gy. wh. q.v.

H. W. sheared with q.v. 's

Buckingham vein with F. W. d H . W. shear

bl . wh . q.v. 's with carb rock, sheared

bl . grey q.v. 6" in carb rock

carb, rusty shear with gy. wh . q.v.

H. W. shear

Buckingham vein, 12", with sh. H. W. 6 F.

F. W., poorly sh . , minor bl. qtz

H. W., intense sh., bl. q. strs.

Buckingham vein, 12" gy . wh . q.v. with F. W. , H. W.

Buckingham vein

sheared F. W., carb, q.v. 's

strong shear, intense, possible Buckingham vein

as above

as above

F .W. shear , bl . q.v.

poor exposure, irregular bl. wh . q.v.

6" wh . gy. bl. q.v. with shearing

6":2" wh . gy. q.v. in shear, carb

End of Channel Samples

Used 4-^ saw blades

Total Samples cut 301

Total Footage cut 928.7 ft.

Avg. Footage/blade 206.4 ft.

Values

1064 ppb,

2156 ppb,

2446 ppb,

589 ppb,

6950 ppb,

16663 ppb

134 ppb

1753 ppb,

1288 ppb,

883 ppb,

675 ppb,

3069 ppb,

395 ppb,

W. 216 ppb

2762 ppb,

373 ppb.

126 ppb

714 ppb,

305 ppb,

2257 ppb,

817 ppb,

569 ppb,

47 ppb

1021 ppb,

59 ppb, .

265 ppb,

C9

.031 opt

.063 opt

.071 opt

.017 opt

.202 opt

, .485 opt

.051 opt

.037 opt

.026 opt

.020 opt

.089 opt

.011 opt

.08 opt

.011 opt

.021 opt

.009 opt

.066 opt

.024 opt

.017 opt

.03 opt

002 opt

.008 opt

l l l l l l l l l l l l l l l l l l l

DIAPPENDIX D

WHOLE ROCK ANALYSIS FROM BUCKINGHAM SHEAR

SEPTEMBER 1990 FOR ASQUITH RESOURCES INC. ASQUITH TOWNSHIP PROPERTY

Samp]

Si02

A1202

Fe20:

MgO

CaO

Na20

K20

T102

P205

MnO

BaO

LO l

Sampl : No. lNo. 2No. 3No. 4

49.89

18.38

9.39

5.09

4.44

2.56

0.86

0.20

0.05

0.27

0.01

8.32

51.65

16.85

10.72

7.06

2.90

2.22

0.19

0.20

0.03

0.21

0.01

7.15

58.75

15.46

9.21

5.70

2.00

1.77

0.81

0.20

0.03

0.19

0.01

6.15

51.20

16.10

9.61

3.54

6.56

5.16

.13

.92

.02

.17

N.D.

6.91

204942 Main shear, 5' channel, qtz. veining 50 ppb204943 Rusty, poorly sheared, 3' channel, minor qtz 60 ppb204944 Secondary intense shear, 3.5' channel 111 ppb Pillowed intermediate volcanic Kelvin Township

Sampl s l to 3 were cut across the Buckingham Shear at the west stripping area .

973350973348

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- IOS

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L E G E N D

0.8. - Overburden7 - Mafic Intrusive Rocks

7a - Diabase7c - Diabase, porphyritic

6 - Felsic Intrusive Rocks

6b - Quartz-Feldspar Porphyry

6c - Granite

5 - Mafic Intrusive Rocks

5c - Gabbro

l - Felsic Mctavolcanics

3a - Flows, massive3b - Flows, porphyritic. Foliated

3c - Quartz-eye Tuff 3d - Ash Tuff

? - Intermediate Metavolcanics

2c - Tuff

1 - Hafic Mctavolcanics

la - Flows-massive, fine to medium-grained

1b - Flows-massive, coarse grained

1c - Pi l lowed Flows

Id - Flows, porphyritic, amygdaloidal

If - Tuff to lapilli tuff

lg - Amphibolite

Alteration

Silcarbkserbx

silica carbonate potassi Jn serici te brecc i ated

au - goldpy - pyritecpy - chalcopyritemt - magnetite

a

r^ -r' l_i j_;

Area of bedrock outcrop

Small bedrock outcrop

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Jointing - dip indicated

Paul t/sheared zone

Fault sheared zr.ne - inferred

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Creek - flow direction indicated

Quartz vein

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Dump Pi le

Sample location - Auppb

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Claim L i ne

S* amp

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ASQUITH RESOURCES INC.

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ASQUITH RESOURCES INC.

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7a - Diabase7c - Diabase, porphyritic

6 - Felsic Intrusive Rocks

6b - Quartz-Feldspar Porphyry

6e - Granite

S - Mafic Intrusive Rocks

5c - Gabbro

3 - Felsic Metevolcanics

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3c - Quartz-eye Tuff 3d - Ash Tuff

2 - Intermediate Metavolcanfcs

2c - Tuff

1 - Mafic Metavotcanics

1a - Flows-massive, fine to medium-Brained

1b - Flows-massive, coarse grained

le - Pillowed Flows

1d - Flows, porphyritic, amygdaloidal

1f - Tuff to lapilli tuff

1g - Amphibolite

1048645

sil - silicacarb - carbonatek - potassiumser - sericitebx - brecciated

au - goldpy - pyritecpy - chalcopyritemt - magnet i te

1048646 Area of bedrock outcrop

Small bedrock outcrop

Contact - inferred

Contact - known

Foliation - dip indicated, vertical

Pillowed lava flow - top direction indicated

Jointing - dip indicated

Fault/sheared zone

Fault sheared zone - inferred

Trench, Pit

Creek - flow direction indicated

sample location - Auppbr-, r-V?[J |J ' Claim Post, un l oca ted

Claim Line

Swamp

Slope Change

-- - - r ; 't' A .T.V. Trail

Footpath

ASQUITH RESOURCES INC.

ASQUITH TOWNSHIP PROPERTYGEOLOG Y

GRIDS C-WEST a A-SOUTH

DATE: SEPT/90 CHECKED B Y: R. C-

SCALE : l"r 200N.T.S. 41 P/l lDRAWN BY: R.C.

J.L. TINDALE a ASSOCIATES