63. 5038

53Be2SE8005 63.5*38 WAPAMISK CREEK 010

REPORT

ON

A DIAMOND DRILL PROGRAM

HORSESHOE LAKE PROJECT

FOR

GREENSTRIKE GOLD CORP,

June, 1986

Toronto, Ontario

N.O. Willoughby, B.Se.

MPH CONSULTING LIMITED

makriaJL Contained ir\ V^/5 fi fa /s -Me o-f waits taj -fiUd in Toronto office -fer Crutik.7^/5 cU) fll'OitL. mafoizl has not bctn called out as -h prt&tvt -tic continuity of

/s d^

d) dri li lop -for holes (fib -i to V * -/bond on* 63b{)2.Me-oot7 4 /

assay rt&lk for drill tto/es ; -found on * 53* J oz ve- oo te

SUMMARY

A 4 hole, 1,728 ft drill program has been completed on the Horseshoe Lake

gold property of Greenstrlke Gold Corp.

The drilling was designed to test a number of ground EM/magnetlc anoma

lies for their gold potential.

No gold values of any economic significance were encountered although the

drilling was generally successful in explaining the geophysical fea

tures.

It Is recommended that the entire property area be geologically mapped as

a prelude to any further work.

Two holes that could not be drilled In the course of the current program

due to break-up conditions should be completed at some point.

S3B02SE0ea5 63.5838 WAPAMISK CREEK 010C

TABLE OF CONTENTSPage

1.0 INTRODUCTION l

2.0 LOCATION, ACCESS AND INFRASTRUCTURE 2

3.0 PROPERTY 4

4.0 PREVIOUS WORK 6

5.0 GEOLOGY AND MINERALIZATION 75.1 Regional Geology 75.2 Property Geology 105.3 Mineralization 11

6.0 DIAMOND DRILL PROGRAM 13

7.0 DIAMOND DRILL RESULTS 157.1 Presentation of Results 157.2 Lithological Units 157.3 Drill Hole Synopses and Interpretation 15

7.3.1 Hole GS-86-1; Grid E 157.3.2 Hole GS-86-2; Grid B 187.3.3 Hole GS-86-3; Grid B 197.3.4 Hole GS-86-4; Grid A 19

7.4 General Observations 207.5 Analytical Results

8.0 CONCLUSIONS

9.0 RECOMMENDATIONS

REFERENCES

CERTIFICATES

APPENDIX l Diamond Drill Logs APPENDIX 2 Certificates of Analyses

LIST OF FIGURES

Figure l Location Map 3

Figure 2 Property Map 5

Figure 3 Location and Regional Geology Map 8

LIST OF TABLESPage

Table of Formations 16

LIST OF MAPS

Map l Location Map Hole GS-86-1 1:2,500

Map 2 Location Map Holes GS-86-2, 3 1:2,500

Map 3 Location Map Hole GS-86-4 1:2,500

Map 4 Diamond Drill Section Hole GS-86-1 1:1,000

Map 5 Diamond Drill Section Hole GS-86-2 1:1,000

Map 6 Diamond Drill Section Hole GS-86-3 1:1,000

Map 7 Diamond Drill Section Hoole GS-86-4 1:1,000

1.0 INTRODUCTION

This report discusses the results of a diamond drill program completed

during the period April 9 to 30, 1986 carried out under the direction of

MPH Consulting Limited on behalf of Greenstrlke Gold Corp. of Calgary,

Alberta on the letter's Horseshoe Lake property In northwestern Ontario.

The objective of the diamond drill program was to test several EM con

ductors with coincident high magnetics Interpreted to be caused by oxide

and/or sulphide-facles Iron formation.

Gold mineralization hosted by or associated with Iron formation is well

documented In this general area, particularly to the north at Opapimiskan

Lake and south in the Pickle Lake Gold Camp.

M O M

2.0 LOCATION, ACCESS AND INFRASTRUCTURE

The property Is situated immediately east of Horseshoe Lake which is

located 144 km north of Pickle Lake in northwestern Ontario (Figure 1).

Highway 808, good quality gravel road, connects Pickle Lake to Windigo

Lake to the north and crosses the northeastern portion of the claim

block. The Wiebenville gravel air strip is situated in the east-central

portion of the property. The Horseshoe Lake area is situated within

1:50,000 NTS topographic sheets 53B/7 and 53B/2.

Red Lake is located 270 km to the southwest.

A winter road extending westerly from Highway 808 and located approxi

mately 3 km northwest of Wiebenville served as surface access to the

drill camp and drill sites. The winter road traverses the entire prop

erty west to Horseshoe Lake a distance of some 20 km. The first 3 km of

the road is negotiable by truck in summer.

The road conveniently connects all of the grids on which the drilling

program was completed, hence only minimal road building/clearing to each

drill site was necessary.

Numerous old drill roads covering the eastern portion of the property

connect with the main winter road.

The western part of the property may be accessed by boat via the Pipe

stone River which flows west into Horseshoe Lake. Highway 808 crosses

the Pipestone several kilometers north of the property. At certain times

of the year it is possible to canoe from Horseshoe Lake east into Wap I

Lake.

^ so

.^PROPERTY * LOCATION

U.S.A.

REGIONAL LOCATION MAP

100 O 100 ZOO SOO 400- l II IIIKILOMETRES

GRIDE

GRIDD

GRID A C

DETAILED LOCATION MAP

SCALEBOO O BOO IOOO IBOO

METRES

6REENSTRIKE GOLD CORP

HORSESHOE LAKE PROPERTY

LOCATION MAPPropel No. C- 777teal*'

By R. NicktonDrawn MPH

No; Flgur* l Doit' Oclotxr 1 985

MPH Consulting Limited

- 4 ~

3.0 PROPERTY

The 229 unpatented claims of Greenstrlke Gold Corporation are located In

the Wapamisk Creek and Bugbee Lake areas In the Patricia Mining Division,

Ontario, and are more properly described as follows:

PA 542265 to 542275

PA 542277 to 542279

PA 542411 to 542415

PA 542472 to 542479

PA 542417 to 542439

PA 542485 to 542495

PA 562503 to 562506

PA 562257 to 562550

PA 562556 to 562558

PA 562560 to 562596

PA 562603 to 562605

PA 562611 to 562616

PA 562619 to 562633

PA 562635 to 562658

PA 562666

PA 562710 to 562734

PA 562785 to 562810

The property encompasses approximately 9,200 acres. All the claims were

recorded on June 4, 1981.

Figure 2 shows the relative disposition of the claims.

90' 30'

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Z 7 l *! 5628 043 J | J 6 2 7 !^S j 3 * Z 7Z6 | 36Z7Z 7( ^7261362729 JSS2797I56Z79S . S 6 Z 7 l *! 5628 00 |362647 j 3 6 Z 648 36 2 S 4 9 I 3 6Z 6 50* 3 62375 | 3 6Z37*| J 6 ? J r , 5 6 , sjjl/jsjy^JssZSZ?, 3623 2S l *2529|

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^-

562503 .562304 562505 .562506 562BO9

HORSESHOE LAKE PROPERTY

Z7|36232S l *2529|56Z530 362331

"T ' 1 C T^ T) *' 53 '' t *25SB 562534 562540 36Z34I S6Z54,Z

l

l ' " ' 36Z3., .36Z34,!562-4 ' "949.96*90 , 362547 ' 36234, 56234,

1/2

MILE

6REENSTRIKE GOLD CORP

HORSESHOE LAKE PROJECT

PROPERTYHo. C-777

FTgur* 2

By N. WilloughbyMPH

Dot*- Novambof, I96S

MPH Consulting Limited

6

A.O PREVIOUS WORK

Summaries of mining and exploration work carried out in the vicinity of

the property are presented in MPH reports of 1985 and 1986 entitled,

"Report on a Program of Overburden Drilling and VLF-EM Surveying, Pickle

Lake Area, Patricia Mining District, Northwestern Ontario, for Petromet

Resources Limited", and "Report on Magnetometer, Horizontal Loop and

VLF-EM Surveys, Horseshoe Lake Project, Ontario, for Greenstrike Gold

Corp.", respectively.

By way of brief review, the following pertinent previous work history In

the area is listed:

Rio Tinto Canadian Exploration Limited, 1961-1965; Prospecting, ground

magnetic and electromagnetic surveying, soil sampling, diamond drilling.

Great Plains Development Company of Canada Limited, 1971-1973; Airborne

and surface magnetic and electromagnetic surveying, 25 diamond drill

holes totalling 8,410 ft.

Dome Exploration (Canada) Limited) 1974-1976; Prospecting mapping,

detailed airborne geophysical surveying, diamond drilling.

Norcen Energy Resources Limited, 1981; Prospecting, magnetic and VLF-EM

surveying, basal till sampling.

Petromet Resources Limited, 1983-1984; Input surveying, reconnaissance

VLF-EM surveying and sonic (vibra-corer) overburden drilling.

Greenstrike Gold Corp., 1985; Ground magnetometer, VLF-EM and MaxMin II

surveying.

5.0 GEOLOGY AND MINERALIZATION

5.l Regional Geology

The property is situated at the eastern end of the Horseshoe Lake

greenstone belt, a typical Archean volcano-sedimentary segment with

in the Gods Lake Subprovince of the Superior Structural Province

(Figure 3). The Horseshoe Lake segment is located midway between

the North Caribou Lake segment to the north and the Pickle Lake seg

ment to the south.

The predominant lithologies of the Horseshoe Lake Belt are mafic to

intermediate, massive to foliated and pillowed metavolcanics.

Narrow interbeds of intermediate to felsic metavolcanics and pyro

clastics are reported.

Metasedimentary rocks consisting mainly of greywacke, argillite and

lesser arkose, quartzite and conglomerate occur as a narrow sequence

in the central portion of the belt.

Poorly exposed sulphide, oxide and silicate-facies iron formation

has been identified and traced in previous exploration via diamond

drilling and aeromagnetics along the entire length of the belt.

Several distinct iron formations likely occur.

A substantial assemblage of mafic (gabbroic) intrusive sills occurs

along the southern boundary of the greenstone belt. Quartz-feldspar

porphyry dykes and sills occur locally.

In general, most rock units are moderately to stongly foliated and

steeply dipping, reflecting Isoclinal folding and shearing. Region

al metamorphism ranges from upper greenschist to amphibolite facies.

ll l l l

migmatite.

MAFIC AND ULTRAMAFIC IGNEOUS ROCKS

i Diorite, gabbro, norite, pyroxenite, peridotite, dunite, serpentinite.

METASEDIMENTSConglomerate, sandstone, mudstone, marble, chert, iron formation and related migmatites.

METAVOLCANICSFELSIC TO INTERMEDIATE METAVOLCANICS

Rhyolitic, dacitic, and andesitic flows, tuffs, and breccias.

MAFIC METAVOLCANICS

Basaltic antf anrfesrti'c (lows, luffs, and breccias.

QREENSTRIKE GOLD CORPHORSESHOE LAKE PROJECT

LOCATION ond REGIONAL GEOLOGY

Prtfrtt Mo, C-777l'600,000Figure S

•r N.WilloughbyOro** MPH

P*'*' Novtmtxr 1965

MPH Consulting Limited

- 9

The Horseshoe Belt is surrounded by terrain characterized by granit

ic to grandioritic batholiths and migmatites.

To dale no economic gold concentrations are known in the Belt.

The North Caribou Lake greenstone belt, located 40 km northeast of

Horseshoe Lake, is host to the Opapimiskan Lake gold deposit, a

joint venture of Dome Mines Limited, Esso Minerals Canada, Canadian

Nickel Co. Ltd. and Lacana Mining Corp. Drill indicated reserves as

of 1983 were reported at 3.2 million tons averaging 0.17 oz gold per

ton. The deposit is currently under further evaluation.

Other volcano-sedimentary segments of the Gods Lake Subprovince have

produced significant gold and silver. Over 20,000 oz of gold and

5,000,000 oz of silver have been produced to date from two mines,

the Berens River or Zahavy, 180 km to the west-northwest and the

Sachigo River Mine, 250 km to the north of Horseshoe Lake.

Adjoining the Gods Lake Subprovince to the south is the Uchi Sub

province in which are found the past, present and future producing

gold camps of Pickle Lake and Red Lake located 100 km SSE and 270 km

SW, respectively from the Horseshoe Lake Belt.

The Pickle Lake camp produced 2,113,000 oz gold and 227,000 oz

silver in three mines (Pickle Crow, Central Patricia, Central

Patricia No. 2).

The recently discovered Dona Lake deposit (1984) located 10 km

southeast of Pickle Lake (Dome Mines - Campbell Red Lake joint

venture) has preliminary diamond drill - indicated reserves of

1,470,000 T averaging 0.23 oz gold per ton (1985). Shaft sinking

commenced late last year.

- 10 -

Initial drill-indicated reserves at the Muskeg Lake gold deposit

discovered earlier this year by St. Joe Minerals, are in excess of

600,000 tons grading 0.58 oz gold per ton (April 1986). The deposit

is situated 70 km west of Pickle Lake.

5.2 Property Geology

Although the claim block has not been mapped systematically, the few

scattered exposures which have been examined to date plus airborne

geophysical interpretation indicate that the property is underlain

primarily by east-west trending, steeply dipping massive and foli

ated mafic metavolcanic and pyroclastic rocks. Narrow interbeds of

intermediate to felsic metavolcanic and pyroclastic rocks are

reported. Metasedimentary rocks consisting of quartzite, greywacke,

argillite, arkose and iron formation are also mapped. Garnetiferous

metasediments also are known.

Outcrops of magnetite iron formation are present just north of Glove

Lake. Northeast of Glove Lake, strongly foliated mafic metavolcan-

ics with minor interbedded metasediments have been mapped. A large

exposure of carbonatized mafic metavolcanics forms a prominent east-

west trending ridge situated approximately 800 m north of Wap III

Lake. Other scattered exposures of mafic metavolcanics occur north

of Wap II Lake and south of Wap III Lake. Some metasedimentary

rocks and iron formation are exposed on the south shore of Wap I

Lake.

Numerous exposures of gabbro are present on the south shore and

south of Wap I Lake, north of Wap II Lake and southeast of Wap III

Lake.

Several airborne and ground magnetic and EM anomalies, attributed to

iron formation horizons, are located (1) north of Wap III Lake, (2)

north of Glove Lake, (3) at the southwest corner of Wap I Lake and,

(4) 6 km west-northwest of Glove Lake.

- 11 -

5.3 Mlneral iza t i on

At the Opapimiskan Lake and Dona Lake gold deposits, auriferous

sulphide-bearing (pyrite and pyrrhotite) quartz stringers occur in

structural zones (folds, shears) within oxide and sulphide facies

iron formations. The past-producing mines at Pickle Lake had a

similar style of mineralization.

Other gold showings in the Gods Lake Subprovince are for the most

part of the auriferous quartz vein variety. These tend to be of

limited lateral and vertical extent and may be hosted by several

different lithologles within the volcano-sedimentary belts.

The quartz vein zones may be associated with contact aureoles

surrounding mafic intrusions as at the Sachigo River Mine. Auri

ferous vein zones and lenses are commonly mineralized with pyrite,

pyrrhotite, chalcopyrite, sphalerite and galena.

Gold mineralization at St. Joe's Muskeg Lake deposit is hosted by a

quartz vein which has been traced over a strike length of at least

1,200 m to a depth of 250 m. A mining width of l.5 m Is reported.

The Berens River (Zahavy) Mine is possibly a volcanogenic Pb-Zn-Au-

Ag deposit hosted by folded mafic to felsic metavolcanics and

clastic to chemical metasediments. Reserves to 1983 were 1,029,000

T grading 0.31 oz Au/T, 5.19 oz Ag/T and 2.37% combined Pb and Zn.

Although economic gold concentrations have yet to be uncovered in

the Horseshoe Lake Belt, several gold occurrences are known In the

area of the southern shoreline of Horseshoe Lake immediately west of

the property.

Gold and silver mineralization was reported by Rio Tinto in a sulph

ide-bearing shear zone in massive gabbro and quartz-feldspar

- 12 -

porphyry dykes (the Rust Seep Group, 1961-1965). Channel samples

returned up to 0.20 oz gold per ton and 0.18 oz silver per ton over

l foot.

At the nearby Sulphide Zone Group, Rio Tinto reported a 23 foot zone

of massive sulphides hosted by mafic volcanics and dacitic lapilli

tuff. Channel samples returned up to 0.50 oz gold per ton over 3

feet. Low copper and silver values are associated. Low gold values

were reported by diamond drilling.

Sampling in the same area by Dome Exploration (1974-1976) uncovered

pyrite and pyrrhotite-bearing quartz veins hosted by andesite and

gabbro. Gold values varying from trace to 0.780 oz gold per ton

over vein widths ranging from 0.2 to 0.6 feet were reported.

Dome also found low gold values in quartz veins hosted by quartz-

feldspar porphyry which is intrusive into greywacke and mafic meta-

volcanlcs.

- 13 -

6.0 DIAMOND DRILL PROGRAM

A total of 6 bedrock EM conductors (VLF-EM and/or MaxMin II) with assoc

iated high magnetics interpreted to be due to oxide and/or silicate

facies iron formation was delineated on 4 of 5 grids during the fall 1985

geophysical program (MPH Consulting Limited, 1985: "Report on Magneto

meter, Horizontal Loop and VLF-EM Surveys, Horseshoe Project, Ontario,

for Greenstrike Gold Corp.").

A number of anomalies were subsequently targeted for diamond drill test

ing in the course of this program.

Locations, lengths, azimuths, dip angles and priority ordering of the

proposed drill holes is summarized below:

Grid Co-ordinate Azimuth Dip Length

B L4+OOE, H25N 150 0 -50 0B L7+OOE, 0+62.5N Grid S -50 0D Ll+OOW, 0+25S Grid S -50 6D L5+OOW, 2+25S Grid S -50"E L6+OOW, 2400N Grid S -50 0A L3+OOW, 2+50N Grid S -50 0

2,268 ft

Owing to early spring break-up conditions, the two holes on Grid D were

already inaccessible by the middle of April and consequently were not

drilled.

The remaining holes were drilled in the locations and at the azimuths as

indicated at dip angles of -52 0 .

A summary list of the completed drill holes documenting total length,

overburden thickness and duration of drilling is given following:

- 14 -

Overburden Thickness/

Hole No.

GS-86-1GS-86-2GS-86-3GS-86-4

Grid/Location

E:B:B:A:

L6+OOW ,L4+OOE ,L7+OOE,L34-OOW,

2+OON1+25N0+6 2. 5N2+50N

Length

437497387407

ftftftft

Casing

18427384

ftftftft

Duration

10423

daysdaysdaysdays

A total of 1,728 ft of drilling was completed of which 253 ft was casing and 1,475 ft was BQ-sized drill core.

The drilling was carried out by Morisette Diamond Drilling Ltd. bury, Ontario.

Hailey-

Drill program supervision, core logging and sampling was carried out by N.O. Willoughby, B.Se. of MPH Consulting Limited.

A total of 263 split core samples representing core lengths varying from 0.5 to 2.5 but averaging 1.0 ft was sent to Thunder Bay Analytical Laboratories Inc., Thunder Bay, Ontario for geochemical analyses for gold, silver, arsenic, copper and zinc.

1 C M

7.0 DIAMOND DRILL RESULTS

7.1 Presentation of Results

Diamond drill logs are presented in Appendix 1. Drill hole loca

tions are shown on Maps l (Hole GS-86-1), 2 (GS-86-2, 3) and 3

(GS-86-4) at a scale of 1:2,500. Some magnetic contours plus the

surface trace of all VLF-EM and/or MaxMin II conductors are also

indicated.

Diamond drill sections at a scale of 1:1,000 are also provided (Map

4: Hole GS-86-1, Map 5: GS-86-2, Map 6: GS-86-3, and Map 7:

GS-86-4). Sample intervals are indicated on each section.

Certificates of analyses are attached as Appendix 2.

7.2 Lithological Units

The various lithologies as logged in the drill core are incorporated

into a single table of formations (Table 1). The numbered units are

consistent with the diamond drill sections (Maps 4,5,6 and 7).

For detailed lithological descriptions the reader is referred to

Table l, the appended drill logs and accompanying diamond drill sec

tions.

? *3 Drill Hole Synopses and Interpretation

7.3.1 Hole GS-86-1; Grid E

The hole was spotted to intersect MaxMin II conductor B on

Grid E (Map 1). The conductor, which is coincident with a

magnetic high, is indicated to be a narrow vertical conductor

at a depth of approximately 180 ft with a conductivity-

thickness greater than 100 mhos. The anomaly is Interpreted

to be due to Interbedded sulphide and oxide facies iron

formation.

- 16 -

TABLE OF FORMATIONS

7 MAFIC INTRUSIVE ROCKS

Diabase (Basalt?)

6 FELSIC INTRUSIVE ROCKS

Diorite, Granodiorite

5 CHEMICAL SEDIMENTARY ROCKS

(a) Magnetite Iron Formation(b) Magnetite-Pyrrhotite Iron Formation(c) Banded Iron Formation

4 METASEDIMENTARY/VOLCANICLASTIC ROCKS

(a) Argillite(b) Chloritic Argillite(c) Tuffaceous Argillite(d) Magnetite-Bearing Argillite, Siltstone (Iron

Formation?)(e) Volcaniclastic Sediment/Sandstone

3 INTERMEDIATE PYROCLASTIC ROCKS

(a) Fine Grained Tuff(b) Crystal Tuff(c) Lithic (j^ Crystal) Tuff(d) Lapilli Tuff(e) Agglomerate

2 INTERMEDIATE METAVOLCANIC ROCKS

I MAFIC METAVOLCANIC, PYROCLASTIC ROCKS

(a) Metavolcanics(b) Tuff

- 17 -

The drill hole In fact Intersected a sequence of Interbedded

sulphide-bearing argillite, tuffaceous argillite plus a sec

tion of sulphide-rich magnetite Iron formation at 297-337 ft

or 220 ft vertical and In the vicinity of the interpreted

conductor (Map 4).

Argillite and tuffaceous argillite are characterized by S-8%

disseminations and stringers of mainly pyrrhotite. Scattered

semi-massive pyrrhotite -f pyrite occur as bands, laminae and

as stringer zones, the latter usually associated with carbon

ate 4 quartz veinlets and masses. These sections measure up

to 1.5 ft in places but are generally less than 0.5 ft thick.

Minor chalcopyrite Is noted.

A 2 ft wide vuggy zone in argillite containing 30% pyrlte-

pyrrhotite occurs at 305.5-307.5 ft.

Some argillite sections contain up to 10% disseminated

magnetite.

Finely laminated and banded iron formation occurs at 324.3-

357 ft or at the base of the interbedded argillite, tuffa

ceous argillite sequence. Black, almost massive magnetite

bands alternate with lighter coloured siliceous and occasion

ally carbonaceous laminae. The best sulphides occur at

324.3-332 ft with up to 102 disseminated pyrrhotite plus 2%

bands and masses of pyrrhotite 4- pyrite. There is some

brecciation (330-331 ft, for example) and sulphide seams/

stringers here and there.

Other predominantly oxide-facies iron formation sections

occur at 364-398.8 ft and 395.7-414.6 ft. Of these two the

former is brecciated frequently showing disruption of laminae

in the form of slumping and mlcrofaulting. Strongly brecci-

18 -

ated sections are noted at 369.6-375 ft, 382-386 ft and con

tain up to 35% pyrrhotite masses.

Thin units of finely laminated magnetite iron formation

conspicuously lacking in sulphides are interbedded with fine

grained intermediate tuff at 414.6-425.4 ft.

Intermediate lithic (crystal) tuff at 184-225.1 ft contains

finely disseminated pyrrhotite, pyrite and magnetite through

out the unit. Several thin portions with S-5% pyrrhotite are

noted.

7.3.2 Hole GS-86-2; Grid B

The hole was drilled to test a strong magnetic high through

which passes a strong VLF-EM conductive trend (conductor A)

(Map 2).

It was drilled beneath a pit near which a grab sample of

quartz-pyrite rubble returned some 1000 ppb Au.

The azimuth of this hole, 1500 , was selected to best inter

sect mineralized cross-fractures which can be seen in the

immediae area of the pit.

Three sections of interbedded volcaniclastic rocks, lithic

tuff and magnetite-rich argillite or iron formation were

intersected at 305.5-320.2 ft, 326-328.5 ft and 362-366.3

ft.

All three are weakly mineralized with occassional l ft sec

tions of up to 5% pyrrhotite ;f pyrite blebs, disseminations

and rarely stringers.

The observed magnetic signature is probably enhanced by the

19 -

disseminated magnetite distributed throughout the 75 ft

of the various mafic to Intermediate pyroclastic rocks at

123.7-198.7 ft.

7.3.3 Hole GS-86-3; Grid B

This hole was drilled to Investigate VLF-EM conductor A' and

associated high magnetics which was Interpreted to be a

faulted continuation of conductor A (Map 2).

The hole Intersected a somewhat monotonous sequence of mafic

to Intermediate volcanic and pyroclastic rocks.

Magnetite-rich (ID-20%) volcanic and pyroclastic rocks occur

at 52.4-127.9 ft, 196.2-217.6 ft and 264.3-346 ft, which

probably account for the high magnetic response In this

vicinity.

Numerous scattered, narrow and weak sulphide sections are

noted throughout the hole In zones generally measuring less

than 2 ft wide. Occasslonal J" to 2" massive pyrltlc bands

are noted for example at 206.6 ft, 261.8 ft.

Iron formation was not encountered.

7.3.4 Hole GS-86-4; Grid A

MaxMln li conductor B on Grid A Is Indicated to be subvert!-

cal and at a depth of from 30-40 meters. It Is coincident

with a strong magnetic high (Map 3).

Sulphide Iron formation was attributed to be the source of

this conductor and magnetic feature.

The drill hole encountered only 407 ft of fine-grained to

aphanitic mafic metavolcanlc which Is strongly carbonatlzed

- 20 -

in places and contains 10X carbonate -f quartz veinlets, veins

and masses.

Numerous (up to 1(^) less than 2 ft thick sections containing

l to 15% pyrrhotite Hh pyrite both associated with the carbon

ate 4 quartz veins, veinlets and masses and pyrrhotite-rich

laminae may account for the conductivity and magnetics in

this area.

7 .4 General Observations

It is immediately apparent that the geology of the property is much

more complex lithologically than initially presumed. For example,

holes GS-86-2 and 3, Grid B are comprised primarily of Intermediate

pyroclastic rocks (tuff to agglomerate) with thicknesses measuring

in excess of 200 ft. Metavolcanic and metasedimentary rocks are

generally subordinate.

Similar lithologies are consciously lacking in Hole GS-86-4, Grid A

3 miles to the east-northeast, which intersected only 27 ft of

intermediate lithic tuff from 374 to 401 ft. The remainder of the

hole consists only of mafic metavolcanic rocks.

Hole GS-86-1, Grid E, 4 miles west-northwest of Grid B, shows a wide

variety of interbedded metavolcanic pyroclastic and both clastic and

chemical metasedimentary units.

Several sections of mafic to intermediate pyroclastic and volanic

rocks in holes GS-86-2 (at 123.7-198.7 ft) and GS-86-3 (at 52.4-

127.9 ft; 196.2-217.6 ft; 264.3-346.0 ft) contain upward of 20%

disseminated magnetite.

Some magnetic features previously thought to be iron formations are

probably these volcanic lithologies. For Instance, Hole GS-86-3,

designed to test a VLF-EM conductive zone with coincident high

- 21 -

magnetics failed to intersect iron formation.

Similarly, Hole GS-86-4, Grid A, did not intersect iron formation.

The drill core, almost all mafic metavolcanics, is comprised of

numerous (up to 15%) thin bands (less than l foot) of massive to

semi-massive strongly magnetic pyrrhotite generally associated with

carbonate 4 quartz.

7.5 Analytical Results

No gold values of any economic significance were indicated from the

extension analytical work. The best gold value was 74 ppb in Hole

GS-86-1 at 190-191.5 ft (sample 18805). The sample was of pyritic

intermediate lithic (crystal) tuff. The sections of iron formation

sampled in this hole, the geophysical target, contain no gold con

centrations of even geochemical interest.

Four copper values of greater than 900 ppm were detected and are

summarized below:

Hole No. Sample No. Footage Cu (ppm)

GS-86-1

GS-86-2

GS-86-4

Sample 18837 contains a l foot section of semi-massive sulphides

(Po * Py) within vuggy argillite.

Sample 18845 occurs within a l foot section of ID-20% bands and

disseminations of pyrrhotite with associated chlorite and epidote.

18837

18845

18970

18988

306.0-307.0

323.3-324.3

362.5-363.5

45.0- 46.0

2,390

1,767

964

1,044

22

Sample 18970 is a l foot section of S-10% pyrrhotite in magnetite-

rich argillite or iron formation.

Sample 18988 occurs within carbonatized mafic volcanic and contains

S-8% pyrrhotite blebs and disseminations.

Six zinc values in excess of 500 ppm were detected and are summar

ized as follows:

Hole No. Sample No. Footage Zn (ppm)

GS-86-1

GS-86-1

GS-86-1

GS-86-1

GS-86-1

18830

18831

18832

18837

18838

299.0-300.0

300.0-301.0

301.0-302.0

306.0-307.0

307.0-308.0

967

1,342

806

580

1,090

Five of the samples occur In pyritic-pyrrhotltlc magnetite-rich

argillite (iron formation?) in hole GS-86-1. Sample 18837 also

contains 2,390 ppm Cu. Sample 18837 also contains 2,390 ppm Cu.

These values suggest slightly elevated base metal backgrounds In

this rock type.

Arsenic and silver values are low. Some elevated arsenic values are

associated with the anomalous zinc values In hole GS-86-1.

** 9 ̂ r

8.0 CONCLUSIONS AND RECOMMENDATIONS

The k hole diamond drilling program totalling 1,728 ft seems to have been

generally successful in explaining the EM/magnetic features being tested.

The EM responses are due mainly to sulphides (pyrite 4 pyrrhotite) in

argillaceous and tuffaceous rocks and sulphide ~ oxide iron formation.

Magnetic responses are due to banded magnetite iron formation and mafic

volcanic/tuffaceous units containing disseminated magnetite.

The geology of the area is indicated to be considerably more complex,

both structurally and lithologically, then indicated by the sparse sur

face exposure.

It is further evident that 4 holes into a property this size do not

represent a comprehensive test of overall gold potential.

By way of recommendation, the remaining 2 holes that could not be

completed should be drilled at some point. The existing airborne geo

physics should also be reviewed to determine if there are any further

areas that warrant detailed ground geophysics and further diamond

drilling.

The property area should also be geologically mapped with particular

attention to small scale structural features. These might be reflective

of larger, potential ore control structures.

Respectfully submitted,

N.O. Willoughby, B.Se.

REFERENCES

Andrews, A.J., Sharpe, D.R. and Janes, D.A., 1981; No. 32, A Preliminary

Reconnaissance of the Weagamow-North Caribou Lake Metavolcanlc-

Metasediroentary belt, Including the Opapimiskan Lake (Musselwhlte)

Gold Occurrence: Ont. Geol. Surv. MP 100, p. 203-213.

M?H Consulting Limited, 1985: Report on a Program of Overburden Drilling

and VLF-EM Surveying, Pickle Lake Area, Patricia Mining District,

Northwestern Ontario, for Petrotnet Resources Limited, Calgary,

Alberta, 51 pages, 4 maps.

MPH Consulting Limited, 1986; Report on Magnetometer, Horizontal Loop and

VLF-EM Surveys, Horseshoe Lake Project, Ontario, for Greenstrlke

Gold Corp., 26 pages, 5 maps.

The Northern Miner, March 24, 1986; "St. Joe has High Grade Find", pages 1-2.

The Northern Miner, April 14, 1986; "Activity Heating Up Around Pickle

Lake", pages l, 19.

Ontario Geological Survey, Mineral Deposit Inventory Records, 1982;

Berens River Mine, Sachigo River Mine, Opapimiskan Lake deposit.

Petromet Resources Limited, 1983; Report on the Horseshoe Lake Project,

Northwestern Ontario, 25 pages.

Sage, R.P. and Breaks, F.W., 1982; Geology of the Cat Lake-Pickle Lake

Area, Districts of Kenora and Thunder Bay, OGS report 207, 238

pages.

CERTIFICATE OF QUALIFICATIONS AND LETTER OF CONSENT

I, N.O. Willoughby of 651 Cosburn Avenue, Toronto, Ontario, certify

that:

1. I hold a Bachelor of Science Degree (Honours) In Applied Geology from

Carleton University, Ottawa, Ontario.

2. I have practiced my profession continuously since graduation In

1974.

3. l have based my conclusions and recommendations contained In this

report on my experience and knowledge of the geology of the area and

on results of the field work carried out on the property during the

month of April, 1986.

4. I hold no Interest, directly or Indirectly, In this property other

than professional fees, nor do l expect to receive any Interest In

the property or In Greenstrlke Gold Corp. or any of Its subsidiary

companies.

5. I consent to the use of this report In any regulatory or government

submlttal or any prospectus or similar document to be filed by the

company.

Toronto, Ontario N.O. Willoughby, B.Se. (Hons.)

June, 1986 ________________________

APPENDIX l

Diamond Drill Logs

MPH CONSULTING LIHITKD DIAMOND DRILL RECORD HOLE NO.

property

Township

location

Horseshoe

Grid E

L6+OOW, 2+OON

logged by

"ore Location

N.O. Willoughby

Glove Lake

Length 437 ft

Bearing 180"

Dip -52"

Objective

Commenced

Completed

Drilling Co

Core Size

Casing Left

April 11, 1986

April 20, 1986

Morissette

BQ

In Hole None

Dip: Collar -52"

Etch Test Depth Degrees

437 ft -58"

Remarks Eight days to get through overburden; from 167-176 ft, aquifer in silty sand filled and cemented the casing; a heavier mud was eventually used .

FROM

0

184

TO

184 ft

225.1

DESCRIPTION

CASING; overburden of sand, boulder and till

INTERMEDIATE LITHIC (CRYSTAL) TUFF:- Dark grey to grey-green; brownish in places- Fine to medium grained- Strongly foliated at 15-20" to c. a.- Well laminated manifest by variation of lithic

clast content and argillaceous sections- Argillaceous laminae consists mainly of sericite,

chlorite; scattered throughout section, notably at185, 194.4, 199.3, 209.5-210, 218.1 ft

- Tuff Is comprised of 2-20X white to grey carbon-atized and silicified elliptical to rounded lithicclasts less than 1" diameter

- 3% blue quartz eyes- Over first 0.8 ft lapilli tuff with S^ subparallel

to c. a.- Scattered finely disseminated po, py and magnetite

throughout- Best mineralized sections as follows:

- At 197-200; 57. py blebs, masses- At 203-205.5 ft; 5-8Z py blebs; somewhat argill

aceous- At 211.5-213 ft; 37. py blebs; somewhat argilla

ceous- At 221.5-225.1 ft; S-5% finely disseminated po +

SAMPLE NO.

18801188021880318804188051880618807188081880918810188111881218813188141881518816188171881818819188201882118822188231882418825

FROM

184.0185.5187.0188.5190.0191.5193.0195.5197.0198.5200.0201.5203.0205.5207.0208.5210.0211.5213.0214.5216.0217.5220.0221.5223.6

TO

185.5187.0188.5190.0191.5193.0195.5197.0198.5200.0201.5203.0205.5207.0208.5210.0211.5213.0214.5216.0217.5220.0221.5223.6225.1

LENGTH

1.51.51.51.51.51.52.51.51.51.51.52.51.51.51.51.51.51.51.51.51.52.51.52.11.5

PPM Cu

PPM Zn

PPB Au

PPM Ag

CONSULTING LIMITED DIAMOND DRILL RKCORD HOLE NO. SHEET NO."

GS-86-1

FROM

225.1

235.7

297.0

TO

235.7

297.0

299.0

DESCRIPTION

ARGILLITH;, TUFFACEOUS ARGILLITE:- Grey green and dark green - Very fine grained - Finely laminated; alternating chloritic and seri

citic laminae- Extremely fissile - Minor scattered chloritic elliptical blebs (frag

ments?) - Minor sulphides - At 227 ft; B! at 25" to c. a. - At 235 ft; S i a t 10" to c. a.

INTERBEDDED TUFF (MAFIC VOLCANIC?), TUFFACEOUS ARGILLITE AND ARGILLITE:- Light grey green and green - Fine to very fine grained - Upwards of 15S! lithic clasts (less than }" dia)

with scattered elliptical carbonate blebs (altered fragments?) at 251.5-253, 258-259, 261-262.2, 284- 286 ft

- The whole section more or less carbonatized andwith approximately 2 7. variably oriented carbonate dykelets-veinlets; generally at 30" to c. a.

- Argillaceous component comprises 15X of section, usually as 3/4" wide laminae; some up to 4" wide

- Three thin carbonate-po bands at 257.5-257.7, 258.7-258.9 ft containing 5 7. p o disseminations, blebs

- At 296-296.3 ft, a po-rich carbonate band - Cp Identified at 258-259 ft (a stringer) - Si generally at 20-25" to c. a.

INTERBEDDED TUFF (MAFIC VOLCANIC?), TUFFACEOUS ARGILLITE:- Fine grained - Light green to grey green - Moderately well carbonatized - Similar to preceding unit but with 5% po blebs,

disseminations- Strongly foliated at 20" to c. a. - Moderate fissility

SAMPLE NO.

18826 18827

18828

18829

FROM

257.0 258.0

296.0

297.0

TO

258.0 259.0

297.0

299.0

LENGTH

1.0 1.0

1.0

2.0

PPM Cu

PPMZn

PPB Au

PPM Ag

U AATUJiXlJ L* IV A L, L.

SHEET NO.

FROM

299.0

30810

317.5

TO

308.0

317.5

324.3

DESCRIPTION

MINERALIZED ARGILLITE:- Black to grey green- Finely laminated- Extremely sericitic, In part weakly graphitic- With some carbonate bands- Strongly magnetic with on average S-8% dissemina

tions, stringers of po, S-5% disseminated mag netite hence showing some affinity fqr ironformation

- S L at 20" to c. a.- At 299-302.6 ft; mainly black argillite '(or mag

netite iron formation?) with good fissility- S-8% py blebs, stringers plus lesser cp (?) as

discontinuous laminae and In carbonate bands,veinlets

- 10% po, py blebs, masses at 299, 301.3-301.6,302 ft

- At 302.6-305.5 ft; black to greyish green andpale green argillite with 3% po bands and dissem inations- moderately magnetic with 1-23! scattered mag

netite- appreciably sericitic- Si at 10" to c. a.

- At 305.5-307.5 ft; serai-massive sulphides Inblack to grey vuggy argillite- 30X po, py, especially over last 1.5 ft- py: po " 50:50

- At 307.5-308 ft; grey green laminated argillite/tuff with 10X po disseminations, blebs and masseswith 3% py associated with po masses

TUFFACEOUS ARGILLITE, INTERMEDIATE VOLCANIC:- Light grey green- Fine to very fine grained- Strongly foliated; in part fissile- Carbonatized , serlcltlzed; with 2!? discontinuous

thin white carbonate laminae- Scattered lQ-15% carbonattzed lithic clasts

(less than V dia)- Si at 20" to c. a.

MINERALIZED TUFFACEOUS ARGILLITE OR INTERMEDIATEVOLCANIC:- Similar to preceding unit but variably mineralized

and with quartz-carbonate veinlng

SAMPLE NO.

18830188311883218833

1883418835

1883618837

18838

FROM

299.0300.0301.0302.0

303.0304.0

305.0306.0

307.0

TO

300.0301.0302.0303.0

304.0305.0

306.0307.0

308.0

LENGTH

1.01.01.01.0

1.01.0

1.01.0

1.0

PPM Cu

PPMZn

PPB Au

PPM Ag

W

HOLE NO. GS-86-1MPH CONSULTING LIMITED DIAMOND DRILL RECORD

FROM

317.5 (cor

TO

324.3 t' d)

324.3

337.0

337.0

364.0

DESCRIPTION

- Some pale green iron silicates? - Extremely indurated section; possibly gradational

with following unit- Some micro-faulting of laminae - At 317.5-317-8 ft; quartz-carbonate vein with 1 7.

po masses; somewhat brecciated - At 319.5-320 ft; contains three quartz-carbonate

veins (one - 2" wide) with minor disseminated py,po

- At 321.3-321.6 ft; quartz-carbonate vein with l O%po blebs

- At 322.7-324.3 ft; mineralized argillite with ID-20% bands, disseminations of po usually associatedwith chlorite, epidote

- Quartz-carbonate vein with po , py masses over lastfoot

MAGNETITE-BEARING BANDED IRON FORMATION: - Dark green to black finely banded/laminated - With pale green and pale grey green silicate-rich

laminae plus white carbonate laminae- Generally fine to very fine grained, very hard - Si at 25 to 30" to c. a.- Considerable sulphides from 324.3-332 ft with 10*

disseminated po plus 2 7. bands and masses of po jh p- At 324.3-325.5 ft; 23! po-py seams/stringers- At 325.5-326.5 ft; 57. po-py seams- At 330-331 ft; breccia and quartz vein containing

S-8% bands, masses of po

INTERMEDIATE VOLCANIC/TUFF:- Green to grey green- Fine grained- Considerable carbonatization, sericitization- Carbonate bands, blebs and masses abundant- Minor finely disseminated py throughout- Quartz-carbonate veining at:

- 337.8-338.5 ft; with 20% po, 5? py as masses,bands plus azurite (?) staining in host

- 341.8-342.8 ft; barren; azurite staining- At 359-361.5 ft; brecciated with fracture planes

at 5Z to c. a.- At 347 ft; S i - 30' to c. a.- At 357 ft; S i - 2 0" to c. a.

SAMPLENO.

18839 18840 18841 18842 1884318844

18845

18846 18847 18848 1884918850 1885118852

18853

18854

FROM

317.0 318.0 318.7 319.7 320.3321.3

323.3

324.3 325.5 326.5 327.5328.5 329.5330.5

337.5

341.8

TO

318.0 318.7 319.7 320.3 321.3323.3

324.3

325.5 326.5 327.5 328.5329.5 330.5331.5

338.5

342.8

LENGTH

1.0 0.7 1.0 0.6 1.02.0

1.0

1.2 1.0 1.0 1.01.0 1.01.0

1.0

1.0

PPMCu

PPMZn

PPBAu

SHEET

PPMAg

NO. It:*JW~ ' -

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO

FROM

364.0

387.8

395.7

TO

387.8

395.7

414.6

DESCRIPTION

BANDED IRON FORMATION:- At 364-369.6 ft; interbedded grey green to green

finely laminated magnetite and silicate ironformation

- Finely granular- At 367 ft; S i - 20" to c. a.- Considerable carbonatization In places a,s narrow

bands and elliptical blebs- Up to IX disseminated po At 366-367 ft; 2'OJt po as discontinuous laminae- At 369.6-375 ft; grey green brecciated iron forma

tion- Similar to preceding section but brecciated,

faulted and slumping of bedding

SAMPLE NO.

188551885618857188581885918860

18861188621886318864

- With up to 35X po bands, masses and dissemina- 18865tions; larger masses contain angular iron forma tion fragments measuring 3/4" dia

- At 374 ft; B! - 5 0 to c. a.- At 375 ft; S t - 20" to c. a.- At 375-382 ft; grey to grey green and black mag

netite iron formation- Well banded and laminated- Similar to preceding section, especially numerous

micro-faults- W/, f inely disseminated po , py

- At 382-386 ft; brecciated Iron formation, similarto 369.6-375 ft- At 384.5-385.7 ft, an indurated chlorite-f Illed

breccia zone- At 386-387.8 ft; magnetite Iron formation, similar

to 375-382 ft

INTERMEDIATE TUFF/VOLCANIC:- Light grey to grey green- Fine grained, well foliated- Carbonatized with lS-20% white masses, blebs and

discontinuous laminae- Somewhat sericitic

MAGNETITE IRON FORMATION:- Finely banded and granular Black to grey and grey green- In places, carbonaceous

18866188671886818869188701887118872188731887418875188761887718878

18879188801888118882

FROM

364.0365.0366.0367.0368.0369.0

370.0371.0372.0373.0374.0

375.0376.0377.0378.0379.0380.0381.0382.0383.0384.0385.0386.0387.0

397.0398.5400.0401.5

TO

365.0366.0367.0368.0369.0370.0

371.0372.0373.0374.0375.0

376.0377.0378.0379.0380.0381.0382.0383.0384.0385.0386.0387.0388.0

398.5400.0401.5403.0

LENGTH

1.01.01.01.01.01.0

1.01.01.01.01.0

1.01.01.01.01.01.01.01.01.01.01.01.01.0

1.51.51.51.5

PPMCu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL KKCUK.USHEET NO.

FROM

395.7(co

414. 6

125. A

TO

414.6nt'd)

425.4

437.0

EOH

DESCRIPTION

- Massive magnetite sections at 395.7-397, 400.4-401.2, 408.4-408.9 ft

- At 397-407 ft; 10% po laminae, disseminations- Silicate component approximately 60% of section

(lighter coloured bands)

INTERBEDDED INTERMEDIATE TUFF, MAGNETITE IRON

FORMATION:- Similar to previous tuff and iron formation bands

but not appreciably mineralized414.6-415.2 = t uff415.2-417.5 " iron formation417.5-420.4 - t uff420.4-421.0 ^ iron formation421.0-422.7 - tuff422.7-423.7 - iron formation423.7-424.7 - tuff424.7-425.4 * i ron formation

INTERMEDIATE TUFF/VOLCANIC:- Similar to 387.8-395.7

CORE BOX SUMMARY

Core Box Footage

Box 1 184.0-201.5Box 2 201.5-221.0Box 3 221.0-240.7Box 4 240.7-260.7Box 5 260.7-279.4Box 6 279.4-298.3Box 7 298.3-316.4Box 8 316.4-334.6Box 9 334.6-352.8Box 10 352.8-372.0Box 11 372.0-390.6Box 12 390.6-409.4Box 13 409.4-428.8Box 14 428.8-437.0

SAMPLE NO.

188831888418885

FROM

403.0404.5406.0

TO

404.5406.0407.5

LENGTH

1.51.51.5

PPM Cu

PPMZn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. GS-86-2

Property

Township

Location

Logged by

Core Location

Horseshoe

Grid B

L4+OOE, 14-2 5N

N.O. Willoughby

Glove Lake

Length 497 ft

Bearing ISO 0

Dip ~52 0

Objective

Commenced

Completed

Drilling Co.

Core Size

Casing Left in

April 23, 1986

April 26, 1986

Morissette

BQ

Hole None

Dip: Collar -52"

Etch Test Depth Degrees

497 ft -49 0

Remarks

FROM

0

27

38.6

TO

27 ft

38.6

65.0

DESCRIPTION

CASING

INTERMEDIATE CRYSTAL TUFF:- Grey and grey green- Fine-medium grained- With up to 2031 white subangular to subrounded

feldspar crystals- Some crytals are carbonatized- Very hard rock; may in part be porphyritic subvol

canic Weakly magnetic- Minor scattered py- Moderate to strong foliation at 15-20" to c. a.

INTERMEDIATE LITHIC TUFF, LAPILLI TUFF:- Grey to grey green Medium grained- Up to 552; rounded to subangular white lithic

clasts; some may be feldspar- A chloritized groundmass- Clasts measure on average 1/8" in diameter, a few

up to 1/4"- Both cnrbonat Lzcci and chloritic clasts- Occassional sericite, pyrite- In general S^ is at 20" to c. a.; at 65 ft, Sj "

less than 5" to c. a.- At 57 ft; garnet porphyroblasts associated with

SAMPLE NO. FROM TO LENGTH

PPM Cu

PPMZn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO.

FROM

38.6(CO

65.0

83.0

114.3

123.7

TO

65.0nt'd)

83.0

114.3

123.7

194.0

DESCRIPTION

clasts " a lteration of clasts?; also carbonatlzed- A few scattered carbonate veinlets

MAFIC TO INTERMEDIATE TUFF:- Green and grey to grey green- Fine grained; may In part be volcanic- Some carbonatization, chloritization- More or less massive with good foliation at

parallel to c. a. from 67 ft- Scattered chlorite-carbonate zones/veins especially

at 68.6-68.9 (with epidote), 72.6-72,7 ft- At 80.7-81.3 ft; quartz vein at 20" to c. a.- At 82.9 ft; quartz vein with large muscovite

crystals (pegmatite?)

INTERBEDDED LITHIC TUFF, LAPILLI TUFF:- Similar to 38.6-65 ft- With scattered carbonate veinlets at 50" to c. a.- Strongly foliated with S| parallel to c. a. at

83-85 ft; from 85-114.3 ft at 15" to c. a.- At 96.1 ft; 3/4" quartz vein at 40 0 to c. a.

MAFIC TO INTERMEIDATE TUFF, VOLCANIC:- Similar to 65-83 ft but with somewhat finer

chloritic sections- Scattered epidotization- Minor carbonate veinlets and bands at 20" to c. a.- Strongly foliated and streaky from 121 ft; alter

nating chloritic and discontinuous white carbonatelaminae or drawn out alteration patches/llthlcfragments

- Sj at less than 5 0 to c. a.- Slightly silicified

INTERMEDIATE LITHIC TUFF, LAPILLI TUFF:- Similar to 38.6-65 ft

SAMPLENO.

- With scattered disseminated py especially at 153-157 ft (1-23! py)

- At 129-137 ft, S i parallel to c. a.; throughoutremainder of section, at 5" to c-a.

- Moderately to strongly magnetic- Scattered sausseritization; biotitlc in places- At 133.4-135 ft; fine grained mafic to intermediate

volcanic with 10% feldspar phenocrysts- At 135.5-136 ft; J" quartz vein at 10" to c. a. 18917

FROM

135.5

TO

136.8

LENGTH

1.3

PPM Cu

PPMZn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO.

FROM

123.7

TO

194.0(cont'd)

194.0

198.7

214.0

217.5

198.7

214.0

217.5

223.0

DESCRIPTION

with associated chlorite, epidote, pyrite- At 169 ft; quartz 4- carbonate - pyrite tension

gash or veinlet measuring 1/8" wide by 2" long; at40" to c. a.

- At 170.5-171.2 ft; quartz 4- carbonate-pyrite vein let and containing large biotite/amphibolecrystals (tourmaline?)

1

MAIFC TO INTERMEDIATE LAPILLI TUFF, AGGLOMERATE:- Dark grey green- Medium grained- Clast supported consisting of greyish green rounded

and elliptical lithic fragments which measure up3/4" in places

- Chloritic groundmass constitutes lS-20% of the rock- Generally with \ 7. d isseminations and blebs of py;

in places up to 5% finely disseminated py 4- po- Also with 155! disseminated magnetite- Scattered carbonatized , chloritized patches- Considerably carbonatized to base

INTERMEDIATE LITHIC, TUFF LAPILLI TUFF:- Similar to 123.7-194 ft- Somewhat feldspathized to base

INTERMEDIATE LITHIC TUFF:- Bleached pale green and light green; fine-medium

grained- Carbonatized, chloritized and in places epidotized- Numerous carbonate veinlets- Up to 32 disseminated py over first half of section

INTERMEDIATE LAPILLI TUFF:- Fine to medium grained- With 252 white elliptical lapilli-sized clasts

within a finer lithic tuff matrix- Some clasts up to J" long- Clasts are frequently carbonatized- Well foliated with Si at 20" to c. a.- Scattered disseminated py plus scattered carbonate

veinlets- Somewhat sericitized, chloritized

SAMPLE NO.

18918189191892018921

18922189231892418925

1892618927189281892918930

18931189321893318934

FROM

153.0154.0155.0156.0

168.7169.3170.3171.3

194.5195.5196.5197.5198.5

214.0215.0216.0217.0

TO

154.0155.0156.0157.0

169.3170.3171.3172.0

195.5196.5197.5198.5199.5

215.0216.0217.0218.0

LENGTH

1.01.01.01.0

0.61.01.00.7

1.01.01.01.01.0

1.01.01.01.0

PPM Cu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO.

FROM

223.0

226.5

254.3

262.3

TO

226.5

254.3

262.3

267.0

DESCRIPTION

INTERMEDIATE LITHIC TUFF:- Green to light green and grey green- Fine grained- Strongly carbonatized and silicified; possibly

altered lithic tuff- Numerous carbonate veinlets at 40 0 to c. a.- Some irregular chlorite-carbonate veins and masses

at 225.2-226.5 ft- Scattered biotite and amphibole

INTERMEDIATE LITHIC TUFF, LAPILLI TUFF:- Similar to 123.7-194 ft- Minor disseminated py- Well foliated at 5 0 to c. a.- A chlorite-carbonate banded section at 230.3-231 ft

INTERBEDDED MAFIC TO INTERMEDIATE TUFF, LITHIC TUFF:- Mainly fine grained green to dark grey and dark

grey green tuff with scattered thin interbeds oflithic tuff (2 OS! of section)

- Lithic tuff comprised of 2 07. extremely stretched-out carbonatized and silicified rounded clasts orfragments

- A few rounded chloritic fragments measuring up to1J" x 3/4"

- Some sericite- S i a t 10" to 5 0 to c. a.- Scattered carbonate-chlorite and carbonnte-quartz-

chlorite + e pidote + pyrite veins, bands/massesparticulaTly at 258.5-260.2, 260.7-261.9 ft

- IX cp in a carbonate vein at 257.5 ft

MINERALIZED MAFIC TO INTERMEDIATE AGGLOMERATE:- Grey to grey green- With 20X bluish-grey cherty elliptical and rounded

to angular clasts or "eyes"- Also elongate Irregular and angular white and grey

lithic fragments usually with carbonate boundaries- Some half moon shapes measuring up to 2" x 1"- On average they measure from less than 1/8" to 1/4"

along long axis- Carbonate and pyrite Inclusions are common in

larger fragments- Also contains 10-155! irregular to elliptical white

SAMPLE NO.

1893518936189371893818939

1894018941189421894318944

FROM

257.5258.5259.5260.5261.5

262.5263.5264.5265.5266.5

1

TO

258.5259.5260.5261.5262.5

263.5264.5265.5266.5267.5

LENGTH

1.01.01.01.01.0

1.01.01.01.01.0

PPM Cu

PPM Zn

PPB Au

PPM Ag

1

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO."

GS-86-2

FROM

262.3

TO

267.0(cont'd)

267.0

297.0

297.0

DESCRIPTION

carbonaceous clasts measuring 1/8" in diameter- A few short chloritic streaks (fragments)- Bluish grey to grey coloration to matrix- Strongly foliated and lineated with S} ~ 5-10" to

c -a.- Numerous closely spaced chloritic and carbonaceous

streaks impart a laminated appearance to some por tions of the section; some of these may -be largeaggloraeratic fragments

- Strongly carbonatized 4- chloritized- 10Z disseminations, blebs and masses of py 4- po

throughout; also as streaks and discontinuouslaminae

VOLCANICLASTIC SEDIMENT:- Grey to brownish grey and greenish grey Fine to very fine grained- Strongly carbonatized, some chloritization- A few dark grey siliceous zones- Generally massive- Scattered carbonate veinlets at 20", 40" and per

pendicular to c. a.- At 285-287 ft; a coarser clastic sediment or mafic

lithic tuff section with scattered disseminated pyin carbonatized zones and carbonate veinlets

- At 289.5-290, 293.5-294 ft; laminated chloritic-argillaceous sections

- A few scattered lapilli tuff sections which arestrongly carbonatized and with carbonate veins upto 1/8" wide parallel to c. a. over first 2 ft ofsection- Some compositional bands or carbonate/chlorite

305.5

alteration

INTERBEDDED VOLCANICLASTIC SEDIMENT, LITHIC TUFF:- Volcaniclastic sediment similar to previous section- Mafic lithic tuff generally fine grained, green to

grey green and brownish green- With up to 102! elliptical and rounded carbonatized

sections; may represent strongly lineated coarselithic fragments

- Lithic tuff sections at 297.2-297.8, 298.8-299.8,300.8-301.3, 301. 4-302. A, 302.8-305.5 ft

SAMPLE NO.

1894518946189471894818949

FROM

301.0302.0303.0304.0305.0

TO

302.0303.0304.0305.0306.0

LENGTH

1.01.01.01.01.0

PPM Cu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO."

-t*- --mi

GS-86-.X

FROM

305.5

320.2

326.0

328.5

TO

320.2

326.0

DESCRIPTION

- Agglomerate section at 302.5-302.8 ft- Several narrow chloritic tuff or argillite bands

containing 2-3X carbonntlzed garnet porphyro-blasts occassionally with py inclusions

- Strongly foliated with S^ at 20" to c. a.

INTERBEDDED VOLCANICLASTIC SEDIMENT, LITHIC TUFF,MAGNETITE-BEARING ARGILLITE (IRON FORMATION?):- Mainly dark grey to dark grey green fine grained

magnetite-bearing massive argillite; in par.t maybe iron formation

- Consists of up to 50X magnetite in chloritized,carbonattzed "groundmass" (amphlbolitic?)

- With 5-15/S garnet porphyroblasts, frequentlyaltered to carbonate

- Some carbonate pseudoraorphs (apparently after gar net) are included by py cubes

- Porphyroblasts measure up to J" in diameter- Contains finely disseminated py 4- po throughout- Chloritized lithic tuff contains~20S: carbonatlzed

lithic fragments- Magnetite-rich lithic tuff or volcaniclastic at

305.5-306.5, 310.7-312.9 ft; in part argillaceous- Finely disseminated py * po- Volcaniclastic sediment at 307.6-310.5 ft, 319. 4-

320.2 ft and similar to previous sections- At 317.9-319.4 ft, 4Z disseminated py with a py-

rich band at 318.9 ft

INTERMEDIATE LITHIC TUFF:- Similar to 38.6-65 ft- Foliation varies from parallel to 20" to c. a.

328.5

354.0

- Quartz veins with minor py at 324.2-324.5, 325-325.2 ft; at perpendicular to c. a.

MAGNETITE-BEARING ARGILLITE AND LESSER TUFF:- Similar to 305.5-320.2 ft but mainly argillite and

with up to l-25i finely disseminated py 4- po

INTERBEDDED MAFIC TO INTERMEDIATE TUFF, LITHIC TUFFAND LESSER VOLCANICLASTIC SEDIMENT, CHLORITICARGILLITE:- Similar to 297-305.5 ft but with more tuff, lithic

tuff- Strongly foliated at 30" to c. a.- Moderately carbonatlzed

SAMPLE NO.

1895018951189521895318954189551895618957189581895918960189611896218963

1896418965

189661896718968

FROM

306.0307.0308.0309.0310.0311.0312.0313.0314.0315.0316.0317.0318.0319.0

323.9325.4

326.4327.4328.4

TO

307.0308.0309.0310.0311.0312.0313.0314.0315.0316.0317.0318.0319.0320.0

325.4326.4

327.4328.4329.4

LENGTH

1.01.01.01.01.01.01.01.01.01.01.01.01.01.0

1.51.0

1.01.01.0

PPM Cu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEKT NO

FROM

354.0

362.0

366.3

TO

362.0

366.3

383.4

DESCRIPTION

MAFIC TO INTERMEDIATE TUFF, LITHIC TUFF:- Grey green to green and dark green- Fine to medium grained- Mainly a l ithic tuff with 2 07, c arbonatlzed ellipt

ical subrounded fragments- Subordinate finer grained sections may be tuff

aceous argillite or volcanic

INTERBEDDED INTERMEDIATE LITHIC TUFF, TUFFACEOUSARGILLITE .AND MAGNETITE-BEARING ARGILLITE -f IRONFORMATION:- Mainly grey green to light grey green fine grained

lithic tuff- Numerous quartz-carbonate veinlets at 40" to 50"

to c. a.- At 363.8-364.1 ft; 402! rounded and elliptical

lithic clasts measuring up to 1/8" in diameter- At 362-363.4 ft; fine grained magnetite-rich

argillite or iron formation with lS-20% dissemina ted magnetite, S-10% disseminations, blebs py + p o

- Foliation (bedding?) at 20" to c. a.- At 364.8-365.5 ft; finely banded magnetite iron

formation and tuffaceous argillite with scatteredpy blebs

- At 365.5-366.3 ft; lithic tuff with 3-531 dissemin ated py

INTERBEDDED MAFIC TO INTERMEDIATE LITHIC TUFF, TUFFAND VOLCANIC (?):- Similar to previous sections with a very fine

grained section at 374.6-380.3 ft; possibly vol canic

- Strongly foliated at 20 0 to c. a.- Numerous carbonate veinlets at 40-50" to c. a.- At 372.7-375.2 ft; mineralized carbonate-filled

fault/breccia zone; 13! disseminated py associatedwith carbonate 4- chlorite veinlets cutting the zone

- Pervasive chloritization of host rock- At 378.2-380.9 ft; barren fault/breccia zone, sim-

lar to above

SAMPLE NO.

1896918970189711897218973

18974189751897618977

FROM

361.5362.5363.5364.5365.6

372.5373.5374.5375.5

TO

362.5363.5364.5365.5367.0

373.5374.5375.5376.5

LENGTH

1.01.01.01.01.5

1.01.01.01.0

PPM Cu

PPM Zn

PPB Au

PPMAg

HPH CONSULTIKG LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO."

GS-86-2

FROM

382.4

TO

497.0

EOH

DESCRIPTION

INTERMEDIATE LITKIC TUFF, LAPILLI TUFF:- Similar to 38.6-65 ft- Perhaps a few thin mafic sections- In places the section looks subvolcanic- Well foliated at 5" to 25" to c. a.- Up to 1Z disseminated py 4- po throughout; also 5-

10% disseminated magnetite- At 428-447 ft; strongly carbonatized and-chlortt-

ized with 5% blebs, disseminations py 4- po at 428-431J!

CORE BOX SUMMARY

Box No. Footage

Box 1 27.0-45.5Box 2 45.5-65.5Box 3 65.5-83.5Box 4 83.5-102.5Box 5 102.5-121.3Box 6 121.3-140.4Box 7 140.4-157.7Box 8 157.7-176.4Box 9 176.4-194.5Box 10 194.5-213.5Box 11 213.5-232.0Box 12 232.0-250.5Box 13 250.5-269.5Box 14 269.5-287.5Box 15 287.5-306.0Box 16 306.0-326.0Box 17 326.0-344.0Box 18 344.0-362.5Box 19 362.5-380.4Box 20 380.4-398.2Box 21 398.2-417.0Box 22 417.0-435.4Box 23 435.4-453.6Box 24 453.6-472.0Box 25 472.0-489.0Box 26 489.0-497.0

SAMPLENO.

189781897918980189811898218983

FROM

428.0429.5431.0432.5434.0435.5

TO

429.5431.0432.5434.0435.5437.0

LENGTH

1.51.51.51.51.51.5

PPM Cu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. GS-86-3

Property Horseshoe

Township

Location Grid B

L7+OOE, 0+62. 5N

Logged by N.O. Willoughby

Core Location Glove Lake

Length 387 ft

Bearing 180"

Dip -52"

Objective

Commenced

Completed

Drilling Co.

Core Size

Casing Left in

April 21, 1986

April 22, 1986

Morissette

BQ

Hole None

Dip: Collar -52"

Etch Test Depth Degrees

387 ft -57"

Remarks

FROM

0

38.0

47.0

52.4

TO

38 ft

47.0

52.4

102.7

DESCRIPTION

CASING

MAFIC VOLCANIC:- Very fine grained - Green to dark green - Strongly chloritized - Moderate foliation with S^ at 5" to parallel to

c. a.

MAFIC TO INTERMEDIATE VOLCANIC:- Fine grained - Green to dark green - Similar to preceding unit but generally coarser - 15Z chloritic elliptical laths may be altered

pyroxene/araphibole phenocrysts - Some pyrite cubes associated with carbonate vein-

lets

INTERMEDIATE VOLCANIC/LITHIC TUFF:- Grey to grey green - Fine to medium grained; strongly foliated - 20% chloritized ampliibole laths/phenocrys ts - Up to 6 Q7, I rregular sausseritized white lithic

clasts and/or feldspar phenocrysts, the unit may ir fact be subvolcanic

- A very hard rock-105! disseminated iMPnpMtP. hnnr-p cl-rnmil v maane-Hf

SAMPLE NO. FROM TO LENGTH

PPMCu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO.

FROM

52.4

TO

102.7(cont'd)

102.7

104.4

109.8

127.9

133.9

104.4

109.8

127.9

133.9

138.8

DESCRIPTION

perhaps alteration product of ferro-magnesium min erals (amphibole - magnetite + chlorite 4 pyrite)

- Minor chloritization, epidotization- Scattered py streaks, disseminations, blebs- Feldspathic alteration at 75-87 ft as individual

reddish-orange feldspar grains and as riras ofseveral quartz-carbonate veinlets

- Scattered streaks and veinlets of carbonate 4-chlorite-epidote

- At 97 ft S 1 " 20" to c. a.

BRECCIATED VOLCANIC/TUKK (CONTACT ZONE):- Fine to raedlum grained- Strongly feldspathized

BASALT/DIABASE:- Fine to very fine grained- Dark green- 152 disseminated magnetite- Although upper contact brecciated (see above unit),

lower contact apparently conformable- Considerable quartz-carbonate veinlets at 60" to

c. a. at base

MAFIC TO INTERMEDIATE VOLCANIC:- Dark grey to dark grey green- Fine grained; in part aphanitic- Very hard- Somewhat Inequigranular in places- S-20% altered feldspar (?) phenocrysts, raicro-

phenocrysts and occassionally has the appearanceof a porphyry

- Moderately to strongly magnetic containing upwardsof 10X magnetite

- Some carbonatization, silicification with a fewscattered carbonate veinlets

- A feldspathized section at 118.3-121.8 ft- Minor disseminated po, py

SULPHIDE-BEARING MAFIC TO INTERMEDIATE VOLCANIC:- Similar to preceding unit with 22 po blebs, dissem

inations; py, po laminae at 128.6 and 130.8 ft- Scattered magnetite

MAFIC TO INTERMEDIATE VOLCANIC:- Similar to 109.8 - 127.9 ft but not magnetic and

SAMPLE NO.

18886188871888818889

FROM

127.9129.4130.9132.4

TO

129.4130.9132.4133.9

LENGTH

1.51.51.51.5

PPM Cu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO.

GS-86-3

FROM

133.9(c

138.8

139.6

148.0

153. A

155.2

TO

138.8ont'd)

139.6

148.0

153.4

155.2

192.2

DESCRIPTION

with 15-207, scattered sericite flecks

BRECCIA-QUARTZ VEIN ZONE r- Pale green sericite filled and sericltlzed mafic

volcanic encasing a coarse milky-white quartz vein- Barren of sulphides

BASALT/DIABASE:- Green to dark grey green- Fine to very fine grained- Some sericitization, chloritization- Numerous carbonate veinlets at 60" to core axis- B! ~ 20-30 0 to c. a.

MAFIC TO INTERMEDIATE VOLCANIC:- Similar to 109.8 - 127.9 ft- A feldspathized zone over first 6"- Scattered po streaks- Foliation at 10 0 to c. a.- At the base an irregular quartz vein with attendant

feldspathization

MICRO-DIORITE, GRANODIORITE DIKE:- Light green, fine grained- 23! pink feldspar phenocrysts (anhedral)- lS-20% amphibole phenocrysts- Some carbonatization, chloritization- Moderately well developed foliation at 20" to c. a.- Numerous carbonate veinlets parallel to foliation- Minor disseminated pyrite- Irregular contact with following unit

MAFIC TO INTERMEDIATE VOLCANIC:- Similar to 109.8 - 127.9 ft- Generally finer grained- At 166.5 - 168.2 ft; l-2% disseminated po and some

po bands within chloritic laminae- At 163.2 - 163.7 ft; quartz breccia zone; no

sulphides- At 174.2 - 174.9 ft; qunrtz-carbonate-chlorlte vein

with minor disseminated py; oriented 20" to c. a.- At 185 - 187 ft; 13! streaks, disseminations of py;

this section is amphibole/chlorlte-rich- Poorly magnetic

SAMPLE NO.

188901889118892188931889418895

IRRQ^

FROM

162.8163.8165.3166.0167.0168.0

1 01 .9

TO

163.8165.3166.0167.0168.0169.0

1 09 .9

LENGTH

1.01.50.71.01.01.0

i n

PPM Cu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO.

GS-

FROM

155.2(c

192.2

196.2

217.6

TO

192.2ont'd)

196.2

217.6

231.9

DESCRIPTION

- To 190 ft; Si ~ subparallel to c. a.- Over remainder S| s 15-20" to c. a.

QUARTZ VEIN - VOLCANIC BRECCIA ZONE:- Predominantly coarse white bull quartz plus strong

ly chloritlzed and silicified green brecciatedintermediate volcanic (?)

- No obvious sulphide mineralization- More or less sharp contact of quartz vein with

preceding unit- Brecciated contact with following unit

MAFIC TO INTERMEDIATE VOLCANIC:- Similar to 109.8 - 127.9 ft- With up to 2 7. c arbonate-chlorlte veinlets at 15",

40" to c. a.- A few quartz-carbonate veinlets- Pervasive carbonatization as streaks, stringers and

blebs oriented parallel to foliation- From 196.2 - 205.5 ft; S i is parallel to c. a.;

elsewhere Sj^ at 20" to c. a.- The section is strongly magnetic from 205.5 ft;

with up to l5% magnetite- At 206.5 ft; a thin carbonate-pyrite stringer- A lV side magnetite-rich zone with 10? py at

206.6 ft- At 211.8 - 212.5 for a quartz-feldspar-chlorite

vein zone- Quartz-chlorite veins at 216.5-216.7, 217-217.2 ft;

the latter with 102 py blebs- At 215 - 216.2 ft a band of strongly foliated and

chloritized mafic-intermediate lapilli tuff

INTERMEDIATE TUFF, VOLCANIC:- Grey to grey green- Fine to very fine grained- With up to 25% carbonatized feldspar phenocrysts

and/or lithic clasts/fragments- Well foliated with S| - 15-20" to c. a.- Weakly magnetic- At 225 - 227 ft; a feldspathized section containing

S-5% disseminated py- At 227 - 227.5 ft; a chloritic section containing

3% py streaks, disseminations

SAMPLE NO.

18897188981889918900

18901

189021890318904

FROM

192.2193.2194.2195.2

216.3

225.0226.0227.0

TO

193.2194.2195.2196.4

217.8

226.0227.0228.0

LENGTH

1.01.01.01.2

1.5

1.01.01.0

PPM Cu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO."

CS-86-3

FROM

231.9

261.8

264.3

TO

261.8

264.3

346.0

DESCRIPTION

INTERMEDIATE LITHIC TUFF, VOLCANIC:- Similar to preceding unit but generally with

coarser lithic sections- Sj at 15-20" to c. a.- 1-3Z finely disseminated py in a few scattered tliir

bands/laminae- 1 7, quartz-carbonate + chlorite veinlets measuring

1", oriented parallef to S^- At 256 - 258.5 ft; agglomerate- At 258.5 - 259.5 ft; 153: thin carbonate bands/vein-

lets with 2 7, a ssociated py

INTERBEDDED CHLORITIC ARGILLITE, TUFF,' LITHIC TUFF:- Green, fine grained- Over first half, 3Z finely disseminated py and

containing a 2" chloritic band with 10Z py blebs Argillaceous to base with S]^ at 25 0 to c. a. Some quartz-carbonate veinlets

INTERMEDIATE LITHIC TUFF, VOLCANIC:- Grey to grey-green- Fine to medium grained- Similar to 231.9 - 261.8 ft; with 55* carbonatized

4- silicified angular to rounded lithic clasts; Inpart may be altered feldspars

- A few fragments of lapilli s ize- Well foliated with S ± at 1 5-20" to c. a.- Some chloritization of matrix Scattered thin carbonate + q uartz veinlets- A few finer grained sections from 307 ft- Minor disseminated py plus scattered blebs- Strongly magnetic; 10% disseminated magnetite- At 277 - 277.7 ft; chloritic arglllite/maf ic

volcanic similar to 261.8 - 264.3 ft- At 308.5 - 311.5 ft; 3 7. d isseminations, stringers

and laminae of pyrite- At 312.1 ft; a }" pyrite band- At 313.1 - 313.4 ft; a quartz + chlorite vein with

205J pyrite masses- At 313.5 - 313.8 ft; quartz vein with associated

feldspathization- a 2" quartz vein perpendicular to c. a. at 322.5 ft

SAMPLE NO.

18905189061890718908

18909189101891118912

FROM

261.5262.5263.5264.5

310.5312.0313.0313.5

TO

262.5263.5264.5265.5

312.0313.0313.5315.0

LENGTH

1.01.01.0 ,1.0

1.51.00.51.5

PPM Cu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEET NO."

CS-86-3

FROM

346.0

358.0

1

379.7

TO

358.0

379.7

387.0

EOH

DESCRIPTION

MAFIC TO INTERMEDIATE VOLCANIC:- Similar to 109.8 - 127.9 ft- Strongly carbonat t zed with numerous carbonate

streaks and bands containing up to 3 7, d isseminatedpy

- Scattered sericite flecks

INTERMEDIATE LITHIC TUFF, VOLCANIC:- Similar to 264.3 - 346 ft- Strongly magnetic- Sy at 15-20 0 to c. a.- Scattered disseminated py- At 359.7 - 360.7 ft; quartz-carbonate-muscovlte

vein over first 7" then brecciated, carbonatized ,chloritized volcanic with up to 42! disseminated py

- At 369.5 - 370.5 ft; somewhat fractured with 8 7.disseminated py

INTERBEDDED MAFIC VOLCANIC AND INTERMEDIATE TUFF,VOLCANIC:

- mainly dark green, fine grained mafic volcanicwhich is magnetic

- chloritized patches and blebs plus carbonatestreaks and blebs

- Intermediate tuff/volcanic similar to previousunit and generally occurs only as 4" wide bands

- quartz-muscovite veining at 380 (2"), 380.6 (i"),381.2 - 381.4 ft; all perpendicular to c. a.

- S} at 15" to c. a.

SAMPLE NO.

189131891418915

18916

FROM

359.0360.0361.0

369.5

TO

360.0361.0362.0

370.5

LENGTH

1.01.01.0

1.0

PPM Cu

PPM Zn

PPB Au

PPM Ag

^w

Ml'U CONSULTING LIMITED DIAMOND DRILL RKCORD HOLE NO. SHRET NO."

GS-86-3

FROM TO DESCRIPTION

CORE BOX SUMMARYBOX NO. FOOTAGE

Box 1 38.0-56.8Box 2 56.8 - 74.7Box 3 74.7-93.9Box 4 93.9 - 112. 7Box 5 112.7 - 13K7Box 6 131.7 - 149.8Box 7 149.8 - 167.6 .Box 8 167.6 - 136.2Box 9 186.2-205.3Box 10 205.3 -'223.5Box 11 223.5 - 242.1Box 12 242.1 - 260.0Box 13 260.0 - 278.6Box 14 278.6 - 298'.7Box 15 298.7 - 317.6Box 16 317.6 - 336.4Box 17 336.4 - 355.4Box 18 355.4 - 374.2Box 19 374.2 - 387.0

SAMPLE NO. FROM TO LENGTH

PPM Cu

PPM Zn

PPB Au

PPM Ag

-*~-^ ——— , ————— ,

MPH CONSULTING LIMITED DIAMOND DRILL RKCORD HOLE NO. GS-86-4

Property

Township

Location

Logged by

Core Location

Horseshoe

Grid A

L3+OOW, 2+50N

N.O. Willoughby

Glove Lake

Length 407 ft

Bearing 180"

Dip -52"

Objective

Commenced

Completed

Drilling Co.

Core Size

Casing Left in

April 27 , 1986

April 29, 1986

Morlssette

BQ

Hole None

Dip: Collar -52"

Etch Test Depth Degrees

407 ft -60"

Remarks

FROM

0

4.0

1

TO

4 ft

279.7

DESCRIPTION

CASING

MAFIC METAVOLCANIC :— Green, generally fine to very fine-grained- Variably carbonatized , silicified- Moderately to strongly chloritized at 15" to 20"

to c.a.- 1(K scattered irregular and regular patches and

veinlets of carbonate and quartz-carbonate ^• epi dote + chlorite at various orientations to c.a.

- Scattered disseminated py, po throughout- Occassional coarser amphibole-rich sections or

bands with associated quartz and carbonate contain ing po 4 py; also some garnet porphyroblasts inplaces

- Also banded appearance in places with thin chlor itic laminae; suggestive of interflow sediment

- Considerable sericitization at 167-190 ft- Scattered disseminated magnetite from 210 ft- Sulphide-bearing sections and vein zones tabulated

following:- At 34-34.6 ft; quartz-carbonate veinlng with 205;

po masses, blebs - all hosted by coarse amphi bole-rich rock

- Amphibole zone commences at 33 ft and containsi'/i p o blebs, [Jiitciieri, perhaps an annealedbreccia zone?

SAMPLE NO.

189841898518986

FROM

33.534.035.5

TO

34.035.536.5

LENGTH

0.51.51.0

PPM Cu

PPM Zn

PPB Au

PPMAS

MPH CONSULTING LIMITED DIAMOND DRILL RKOORD HOI,R NO. GS-86-4SHEET NO. 7—— i^-

FROM

A .0 - (CO

TO

279.7 nt'd)

DESCRIPTION

- At 44.3-45.3 ft; similar to above but lessquartz-carbonate and with S-5% disseminations, blebs po + p y

- At 45.7-46.7 ft; S-8% blebs, disseminations poassociated with carbonate veinlets and masses

- At 53.1-53.5 ft; as above but somewhat banded at20" to c. a.

- At 72.7-74.5 ft; annealed breccia zone withquartz-carbonate veinlets; minor po? or py?

- At 88.3-88.5 ft; carbonate vein or band withincoarse amphibole rock (sediment?); with 13! garnet porphyroblasts - 1-251 po , py masses, disseminations

- At 95.3 ft; a 2" wide barren white quartz veinat 35" to c. a.

- At 96-98 ft; quartz-carbonate band with someamphibole, scattered garnet - 105! masses, disseminations of po , py with

massive sulphides over last foot - At 101-103 ft; to 102 ft, carbonate and quartz

carbonate veinlets and bands containing 5X po masses - To 103 ft, garnet-bearing (10%) amphibole rock

with a few carbonate veinlets; barren - At 105-107 ft; carbonate-quartz bands, veinlets

and patches containing 22 po within amphibolide rock ( tuff?)

- At 110.5-110.7 ft; as above with 103! po masses,disseminations

- At 119-119.6 ft; garnet-bearing amphibole rockwith less than 13! po masses

- At 121.5-122.1 ft; a 3" quartz-carbonate veinat 10" to c. a. with some associated amphibole

- At 123.1-123.5 ft; amphibole rock (sediment?)with 103! py masses, blebs

- At 124.9-126.4 ft; section commences and endswith 2" quartz-carbonate bands containing 83! po masses, disseminations; minor po in host tneta- volcanic

- At 130-137 ft; strongly carbonatized zone withseveral bands of garnetiferous amphibole rock plus carbonate t quartz bands, veining; with 7- 105! po 4- py disseminations, masses - Best "sulphides at 130.5-131.5, 132.8-133.3 ft - N.B.: Other carbonatized zones above this sec

tion and containing finely disseminated sulph-

S AMPLENO.

18987 18988 18989

18990

18991 18992

18993

18994 18995 18996

18997 18998

18999 19000

19001

19002 19003 19004 19005 19006 19007

19008 19009 19010 19011 19012 19013 19014

FROM

44.0 45.0 46.0

52.5

72.5 73.5

88.0

96.0 97.0 98.0

101.0 102.0

105.0 106.0

110.5

121.0 122.0 123.0 124.0 125.0 126.0

130.0 131.0 132.0 133.0 134.0 135.0 136.0

TO

45.0 46.0 47.0

53.5

73.5 74.5

89.0

97.0 98.0 99.0

102.0 103.0

106.0 107.0

111.5

122.0 123.0 124.0 125.0 126.0 127.0

131.0 132.0 133.0 134.0 135.0 136.0 137.0

LENGTH

1.0 1.0 1.0

1.0

1.0 1.0

1.0

1.0 1.0 1.0

1.0 1.0

1.0 1.0

1.0

1.01.0 1.0 1.0 1.0 1.0

1.0 1.0 1.0 1.0 1.0 1.0 1 .0

PPM Cu

PPM Zn

PPB Au

PPM Ag

- ^^

MPH CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEHT NO.

GS-

FROM

4.0

TO

279.7(cont'd)

DESCRIPTION

- At 144-149 ft; numerous carbonate bands withinamphibole rock with a narrow py stringer at 144-144.5 ft, U po blebs at 145.5-147 ft, 15% poblebs, masses, stringers plus IX py blebs at147.7-148.3 ft

- Barren 2" wide quartz veins at 163, 167, 171.5 ft- At 164-165 ft; carbonatized zone with.20% car

bonate veinlets and masses. - At 176.8-177 ft; quartz-carbonate-sericite band

or vein (?); host rock sericitized- A small po-py bleb (less than 1/4") at 182.3 ft- At 184.5-184.9 ft; quartz-epidote 4- carbonate

vein or band at 25" to c. a.- At 190.5-191.5 ft; carbonate zone or band with

considerable carbonate + q uartz veining withlS-20% po masses, disserainations

- At 193-195.5 ft; as above with narrow sulphidesections consisting of 10% finely disseminatedpo and minor po, py blebs at 193.1-193.4, 193.7,194, 195, 195.5 ft

- Looks like interflow sediment- At 197-199 ft; 1 07. po, py + c p as disserainations,

laminae 4- blebs both within carbonate bands andmetavolcanics

- At 210-210.5 ft; 2X disseminated py, po In car bonatized raetavolcanic and within carbonateveinlets and masses- Some disseminated magnetite

- At 221-221.8 ft; barren quartz-carbonate-sericitevein or band at 5 0 to c. a.

- At 231 ft; thin carbonate vein containing 255? po- At 234-234.3 ft; carbonate vein with 1-2Z dis

seminated po- At 2.36.8-237.5 ft; quartz-carbonate vein at 15"

to c. a. with minor disseminated po , py at startplus some garnet

- At 238.7-239.6 ft; 5Z disserainations, streaksand blebs py 4- po in carbonatized metavolcanicand carbonate veinlets

- At 243.5-244.5, 246-249.5 ft; po-rich carbonatezones; mainly irregular carbonate masses

SAMPLE NO.

1901519016190171901819019

190201902119022190231902419025190261902719028

19029

19030

1903119032

FROM

144.0145.0146.0147.0148.0

190.0191.0192.0193.0194.0195.0196.0197.0198.0

236.5

238.7

243.5244.5

TO

145.0146.0147.0148.0149.0

191.0192.0193.0194.0195.0196.0197.0198.0199.0

238.0

240.7

244.5245.5

LENGTH

1.01.01.01.01.0

1.01.01.01.01.01.01.01.01.0

1.5

2.0

1.01.0

PPM Cu

PPM Zn

PPB Au

PPM Ag

MPH CONSULTING LIMITED DIAMOND DRILL RECORD MOIR NO. SHEKT NO.

GS-

FROM

4.0(co

279.7

283.0

TO

279.7nt'd)

283.0

374.8

DESCRIPTION

- At 250.5-253.3 ft; quartz-carbonate zone (vein-lets, masses) with 5-10X po 4- py-rich bands

- At 261-261.8 ft; 2-33! bands and disseminationsof po

- At 262-264 ft; annealed breccia zone; sausseriticand with quartz-carbonate veining; minor dissem inated po , py; some angular sericitic fragments - Main fracturing at 20" to c. a.

- At 266.5-267.5 ft; S-4% laminae, disseminationsof po

- At 269-271.5 ft; carbonate-filled fracture/breccia zone containing S-4% po 4 py masses, blebs and stringers

- At 271.6-272 ft; carbonate zone with 5Z dissem inated po

- At 275-276 ft; scattered po , py- At 277.6-277.8; two thin sulphide stringer zones

QUARTZ VEIN: - Barren, massive, milky white quartz vein

MAFIC METAVOLCANICS: - Similar to 4-279.7 ft - At 284.1-287.1 ft; numerous carbonate veins and

stringers containing ID-15% po + py disseminations, stringers; some blebs at 285.4 ft

- At 293.7-294.5 ft; carbonate band/vein at 10-15"to c. a. containing minor po

- At 295.5-296.5 ft; quartz-carbonate-sausseritezone/breccia with minor disseminated py

- At 301-304.5, 306.5-318 ft; carbonatlzed zones wit)numerous carbonate 4 quartz veinlets and masses with 5% blebs, masses, disseminations of po + p y; a few sulphide laminae; a sulphide band over last foot; could be fault/breccia zone

- At 335-335.3 ft; minor disseminated py in bandedquartz-carbonate-chlorite; at 20" to c. a. - Possibly interflow sediment

- At 337.3-338, 339.5-341.1, 342-245.5 ft; quartz-carbouat.^ bn n J ^ ririi in :m

SAMPLE NO.

1903319034 19035 19036 19037 19038 19039 19040

19041 19042

1904319044

1904519046 19047

19048

1904919050 19051 19052 19053 19054

19055

1 Q n e; A

FROM

245.5246.5 247.5 248.5 249.5 250.5 251.5 252.5

261.0 262.0

269.0270.5

284.1285.1 286.7

293.7

306.5308.5 310.5 312.5 314.5 316.5

334.5

•3 ~n r\

TO

246.5247.5 248.5 249.5 250.5 251.5 252.5 254.5

262.0 264.0

270.5272.0

285.1286.7 288.3

294.7

308.5310.5 312.5 314.5 316.5 318.5

335.5

TOO A

LENGTH

1.01.0 1.0 1.0 1.0 1.0 1.0 2.0

1.02.0

1.51.5

1.01.0 1.5

1.0

2.02.0 2.0 2.0 2.0 2.0

1.0

l r*

PPM

CuPPM Zn

PPB Au

PPM Ag

MP1I CONSULTING LIMITED DIAMOND DRILL RECORD HOLE NO. SHEKT NO,

FROM

283.0

TO

374.8(cont'd)

374.8

401.0

401.0

407.0

EOH

DESCRIPTION

- At 361-365 ft; considerable carbonatization withsome po + magnetite

- At 366.5-367.2 ft; barren quartz-carbonate veinat 30' to c. a.

- At 368.6-368.8 ft; po and magnetite-rich carbonateband

INTERMEDIATE LITHIC TUP K:- Medium grained~ Green to grey green- With up to 30X subangular carbonatized lithic

clasts- Some carbonatization, chloritization- At 384-387 ft; 5X po + p y streaks, blebs

MAFIC MRTAVOLCANIC:- Similar to 4-279 ft- Not as altered or fractured- With minor disseminated po , py

CORE BOX SUMMARY

Box No. Footage

Box 1 4.0-23.0Box 2 23.0-41.7Box 3 41.7-60.3Box 4 60.3-79.0Box 5 79.0-97.5Box 6 97.5-116.8Box 7 116.8-135.0Box 8 135.0-154.5Box 9 154.5-172.8Box 10 172.8-191.7Box 11 191.7-210.5Box 12 210.5-229.6Box 13 229.6-248.2Box 14 248.2-266.8Box 15 266.8-285.0Box 16 285.0-303.7Box 17 303.7-322.0Box IS 322.0-341.6Box 19 341.6-360.8Box 20 360.8-380.0Box 21 380.0-398.7Knv IT 1QH 7-',n? fi

SAMPLENO.

19057

1905819059

1906019061

19062

1906319064

FROM

339.0

342.0344.0

361.0363.0

368.0

384.0385.5

TO

341.0

344.0346.0

363.0365.0

369.0

385.5387.0

LENGTH

1.0

2.02.0

2.02.0

1.0

1.51.5

PPM 'Cu

PPMZn

PPBAu

PPMAg

APPENDIX 2

Analytical Results and Certificates of Analysis

1 ^^A fPm i nuixucn DMI MIMMUT i IOML. M H LABORATORIES INC.^^ . ^ ^ ̂ ^B BALMORAL COMPLEX, 1081 BARTON STREET, THUNDER BAY, ONTARIO P7B 5N3 * TEL. (807) 623-6463

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

I^^BIl\9E/ ASSAY LABORATORY - CHEMISTS - GEOCHEMISTS

(Eevttftcate 0f jXnaitmg*

SAMPLE FROM:

REPORT TO:

DATE RECEIVED:

LAB. REF. NO.:

SAMPLE(S)OF:

MPH Consulting Limited2406 - 120 Adelaide Street W.TORONTO, Ontario M5H 1T1

L. J. Smith, P. Geologist Greenstrike Gold CorporationSuite 200, 701 - 14th Street N.W.CALGARY, Alberta T2N 2A4May 5, 198686A380

Drill Core. Geochemical analysis

v- r?

for - Au, Ag, Cu, Zn S As.

SUBMITTED TO US SHOW RESULTS AS FOLLOWS:

CLIENT'S

188011880218803 .188041880518806188071880818809188101881118812 18813188141881518816188171881818819188201882118822 1882318824

No. GOLD SILVER(ppb)- (ppm)

ND 0.14ND 0.0915 0.11ND 0.0674 0.30ND 0.12ND 0.09ND 0.03ND 0.12ND 0.12ND 0.11ND 0.11 ND 0.06ND 0.05ND 0.11

' ND 0.08ND 0.08ND 0.11

' ND 0.08ND 0.11ND 0.08ND 0.08 ND 0.11IT 0.08

COPPER(ppm)

86106

677066

102806870807664 72757774636983797272 7395

ZINC(ppm)

5727365834338339'60376154 56627181413865756847 6591

ARSENIC(ppm)

195822

' 2742502913501248 6220

22

2419

9531155 6921

. .continued

MEMBER OF THE CANADIAN TESTING ASSOCIATION

1

,

111111111111111111

Or-iU Core

C^ffPSJlo

18825188261882718828 18829188301883118832188331883418835188361883718838 18839188401884118842188431884418845188461884718848 18849188501885118852188531885418855 188561885718858 18859188601886118862188631886418865 188661886718868 188691887018871188721887318874

- Geochem analysis

GOLD (ppb) '

NDND10ND ND1024232412ND101821 2040624120414120NDND 55ND42ND70ND13 NDNDND NDNDNDNDND15ND ND50ND NDNDNDNDNDND

2 -

. . .cont'd

SILVER (ppm)

0.090.090.090.03 0.060.290.740.370.320.14 .0.140.431.420.83 0.140.110.400.060.080.720.520.180.170.17 0.230.140.290.170.200.140.17 0.110.280.07 0.100.250.470.170.270.250.15 0.100.020.07 0.030.040.030.030.090.13

COPPER

8068

11139 49

139203137978780358

2390263 12810776701425

1767634827no25 -

2561172126182 295825 727266

. 306322

- 81 302117 121619114144

ZINC (ppm)

7412711760 84

9671342806384178138159580

1090 8985669690

252147534638 253457206038

. 5 1933 4345456 379 556

3145

. . . . . . cont

ARSENIC (ppm)

25834851 70576059496842194360 2

191221744560546246 78519091663827 231812 1415139

107

16 1298 8763

1010

'd 3

- 3 -

Drill Core - Geochem analysis ...cont'd

CULT'S No

1887518876188771887818879188801888118882188831888418885188861888718888188891889018891188921889318894188951889618897188981889918900189011890218903189041890518906189071890818909189101891118912189131891418915189161891718918189191892018921189221892318924

GOLD(ppb)

NDNDNDNDNDND11NDNDNDNDNDNDNDNDNDNDNDNDND10NDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDND11NDNDNDND

SILVER(ppm)

0.040.270.130.090.030.120.040.030.040.020.030.090.090.030.090.030 D20.220.130.030.300.040.020.020.020.040.100.030.030.230.160.100.260.030.320.17

. 0.260.090.030.100.090.210.030.050.100.050.050.020.010.01

COPPER(ppm)

2980461721502423302612282114211514395548628131281025172022597041171315192317171421253637.3842283938

ZINC(ppm)

70212

29466

. 4487

1167470954870

142956992915

.85133575856961041211285292766471664749606990938794929398

ARSENIC{ppm)

912556

11745546576538898632325467

10667

11657934566867

1097

. cont'd

- 4 -

Drill Core - Geochem analysis

cm

1892518926199271892818929189301893118932189331893418935189361893718938189391894018941189421894318944189451894618947189481894918950189511895218953189541895518956189571895818959189601896118962189631896418965189661896718968189691897018971180721897318974

T'S'NO. GOLD (ppb)

ND ND ND ND ND ND ND 10 ND ND ND ND ND ND ND 12 ND10 .NDNDNDNDNDNDNDNDNDNDNDNDND1112 12 10 1.0 ND ND ND ND ND ND ND ND 201819 23 ND ND

...cont'd

SILVER(ppm)

0.070.050.170.070.010.050.080.070.010.010.010.010.020.010.100.170.270.260.070.030.240.020.020.010.300.01NDNDNDNDND

0.020.030.050.050.08ND

0.100.020.080.080.030.02ND

0.110.21NDNDNDND

COPPER(ppm)

4025482721242773732220 .102319275928385430559832276140265752775238

14915715914461

13164 .24

146765020

10096441

112no33

ZINC(PPm)

908890817337685152527846607360739372516845777858907910495779259.6811912713613092666555

1151281383868

11936596072

ARSENIC(ppm)

1167659

12101151487

1146565

10171188676

. 9101389

1518171715117

181613148

18771618,266

.continued

t1111111111111111AH

Drill core -

CLIENT'S NO.91897518976 189771897818979189801898118982189831898418985189861898718988-1898918990189911899218993189941899518996 18997189981899919000190011900219003190041900519006 190071900819009190101901119012190131901419015190161901719018190191902019021190221902319024

Geoch.em analysis

GOLDiBEklNDND NDNDNDNDNDMDNDNDNDND103117ND1112NDNDNDND NDNDND101010NDNDNDND NDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDMD

- 5 -

. . . .cont'd

SILVER(ppm)

NDND NDND

0.020.02NDNDNDNDNDNDND

0.130.180.20NDNDND

0.01NDND NDND

0.020.100.10ND

0.02NDND

0.02 NDNDNDND

0.010.01NDNDNDNDNDNDNDNDNDNDNDND

COPPER(ppm)

3321 21404541414434

135379121236

104433538394

125130199323115 38

104187130395122144112121114 2189912269

170185172136184387108185 -14531618349

199179

ZINC(ppm)

5654 648582959284' 86

1331147

3011149

1125182511 47341820141915161612171923162311188

191813168

117

121114

ARSENIC(ppm)

34 87813188

128

102912374119202816361918 157

281229378

301827 22148

10341915132128162738403183020

continued 6

Dr-m Core -

GENT'S No.

19025190261902719028190291903019031190321903319034190351903619037190381903919040190411904219043190441904519046190471904819049190501905119052190531905419055190561905719058190591906019061190621906319064

Detection

Geochem analy

GOLD (ppb)

NDNDND10ND1112NDNDNDNDNDNDNDNDNDNDND

, NDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDND

Limits 10 pp

6 -

. . . .cont'd

SILVER(ppm)

NDNDND

0.070.110.130.19NDNDNDND .NDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDNDND

0.1 ppm

COPPER(ppm)

1641307651917440225310213132379

3118077

20816110083130158879692

19310696

11811919531812418310217316413216915911387

1 ppm

INC3pm)

111212 .1615135679819198108

168

5719101616213818308

118

.1713'15

161313158

5614

1 ppm

ARSENIC(ppm)

23196

822048341113266

23A1

1211788

10426

14865

1812211314151923121411108

1 ppnND - none detected

DATED: June 13, 1986

THUNDER BAY ANALYTICAL LABORATORIES INC.

ApprovedR. Matthews, B.Se.

L5+OOW L4+OOW L3+OOW L2+OOW L1+OOW LO+00

4-fOON —

3+OON -

2+OON -

1+OON —

BASE LINE

1-1-00 S -

562577

63.5*38 W APAMISK CREEK 200

GRID E

GRIDD

DETAILED LOCATION MAP

SCALEBOO O BOO lOOOIBOO

METRES

U.S.A HNi^TiP

REGIONAL LOCATION MAP

SCALE100 O 100

KILOMETRES

400

LEGENDMAGNETIC SURVEY

Instrument: McPhar MF-100 Fluxgate Magnetometer

Magnetic Contour

GEOPHYSICAL INTERPRETATION

w* MBMM HLEM Conductor Axis

Fault

DIAMOND DRILL HOLE LOCATIONS

Diamond Drill Hole Location, Projected to Surface

Drill Rood

Pit

SCALE50 100

S METRES

6REENSTRIKE GOLD CORPHORSESHOE LAKE GRID

GRID A

DIAMOND DRILL HOLE LOCATIONSProject No: C-777

Scale* 1 :2,500

Drawing No: Map 3

By N.O. Willoughby

Drawn' MPH

Date- May, 1986

MPH Consulting Limited

. 6038

L1+OOW LO+00 L1+OOE L2+OOE L3+OOE L4+OOE L5+OOE L6+OOE L7+OOE L8+OOE

562799

5628072+OOS -

63.5036 WAPAMISK CREEK

GRIDE

GRID D

DETAILED LOCATION MAP

562656

210

GRID A ;

SCALE5OO O 5OO IOOO ISOO

UETKE5

900

\ QUEBEC50"

U.S.A

450

^ TORONTO,^

toJK

REGIONAL LOCATION MAP

SCALE100 O tOO

KILOMETRES

50

LEGENDMAGNETIC SURVEY

Instrument- McPhar MF - 1OOFluxgatB Magnetometer

Magnetic Contour

GEOPHYSICAL INTERPRETATION

••taMB* v-^*w HLEM Conductor Axis

*VA/* *W* Fault

DIAMOND DRILL HOLE LOCATIONS

Diamond Drill Hola Location, Projected to Surface

Drill Road

Pit

SCALE50 IOO ISO 200

METRES

GREENSTRIKE GOLD CORPHORSESHOE LAKE GRID

GRID B

DIAMOND DRILL HOLE LOCATIONSProject No: C-777Scale: 1:2,500

Drawing No: Map

By: N .O. WilloughbyDrawn* MPH

Date: May, 1986

MPH} MPH Consulting Limited

M- 5038

L7+-OOW L6+OOW L5+OOW L4+OOW

l

L3+OOW L2+OOW

l

L1+OOW LO+00

l

6+OON -

542420

5+00 N-

542426

4-t-OON ~

3+OON-

2+.OON-

1+OON -

542432

O+OO -

53B92SE0005 63.5*38 WAPAMISK CREEK 220

GRIDE

DETAILED LOCATION MAP

SCALEBOO O BOO IOOO IgOO

METRES

REGIONAL LOCATION MAP

LEGENDMAGNETIC SURVEY

Instrument: McPhor MF - 100 Fluxgate Magnetometer

Magnetic Contour

GEOPHYSICAL INTERPRETATION

wMft •••••MM HLEM Conductor Axis

*\A/* *\A/* *\AX* Fault

DIAMOND DRILL HOLE LOCATIONS

(ry^-^** Diamond Drill Hole Location, ^ Projected *o Surface~^-z.~~—~-~ Drill Road

X p'*

50SCALE50 100

METRES

ISO 200

GREENSTRIKE GOLD CORPHORSESHOE LAKE GRID

GRID E

DIAMOND DRILL HOLE LOCATIONSProject No: C-777

Scale: 1:2,500

Drawing No: Map1

By N.O. WilloughbyDrawn' MPH

Date: May, 1986

MPfO MPH Consulting Limited\. \ * f * f *^

SOUTHNORTH

LEGEND

7 l" . "l MAFIC INTRUSIVE ROCKS

Diabase (Basalt"

6 l* * *| FELSIC INTRUSIVE ROCKS

Diorite. Granodionle

CHEMICAL SEDIMENTARY ROCKS

la] Magnehte Iron formation

(b) Wagnelite-Pyrrnotite Iron Formation

(ci Banded Iroa Formation

METASEDIMENTARY/VOLCANICLASTIC ROCKS

(a) Argillite

(b) Chloritic Argillite

(c) TuHaceous Argilliie

(d) Magnetite-Bearing Argillite. Siltstone (Iron Formation'')

(el Volcaniclastic Sediment .'Sandstone

INTERMEDIATE PYROCLASTIC ROCKS

(a| Fine Grained Tun

(b) Crystal Tuff

(C) Lithic (^ CryslalfTulf

(di Lapilli Tulf

le) Agglomerate

INTERMEDIATE METAVOLCANIC ROCKS

MAFIC METAVOLCANIC, PYROCLASTIC ROCKS

la) Metavoicanics

(b! Tull

ABBREVIATIONS

bx brecciated

cp chalcopyrite

diss disseminated

rnag rnagnelue

po pyrrhotite

PY pyrite

q-cv quart?-carbonate veiniets

qv quartz vein

GS-86-4 L3+00W, 2+50N

SURFACE TRACE OFHLEI^ CONDUCTOR 'B

OUTCROP

T4.6 : 18991,18992

. 18994-18996 18997,18998

!8?; 18999,19000

19002 - 19007

19008 - 19014

19015 - 19019

19020 - 19028

18984-18986

18987-18989

' 19029,19030

19031-19040

.21- '9041,19042

i 19043, 19044

.. 19045- 19047

GRIDE GRID A !

GRIDD

DETAILED LOCATION MAP

SCALESCO O 8OO __IOOO1BOO

UETKE5

19049-1905410

SCALE 10 20 30

____i FEET

40

19056 - 19059

.19060, 19061

387

19062

.19063-19064

63.5B38 WAPAMISK CREEK 230

6REENSTRIKE GOLD CORPHORSESHOE LAKE GRID

GRID A

DIAMOND DRILL SECTIONHOLE GS -

Project No : C-777Scale: l"s 20'

Drawing No: 7

: N.a Willoughby

Drawn- MPH

^ May, 1986

MPH ) MPH Consulting Limited

SOUTHNORTH

LEGEND

7 l" - "l MAFIC INTRUSIVE ROCKS

Diabase (Basa

6 !* * *1 FELSIC INTRUSIVE ROCKS

Diorile. Granodiorite

CHEMICAL SEDIMENTARY ROCKS

(al Magnelile Iron Formation

[D| Magnetite-Pyrrhotite Iron Formalion

(C| Banded Iron Formation

METASEDIMENTARY/VOLCANICLASTIC POCKS

(a) Afgillite

(b) Chloritic Argillite

(c) Tullaceous Argillite

|d) W agnel He-Beat mg Argillile, Sdlsione (Iron Formation 1 !

|e] Volcaniclastic Sediment i1 Sandstone

INTERMEDIATE PYROCLASTIC ROCKS

la] Fine Grained Tuff

(bt Crystal Tuff

(c) Lithic (^ CryslaljTult

(di Lapilli Tull

(et Agglomerate

INTERMEDIATE METAVOLCANIC ROCKS

MAFIC METAVOLCANIC, PYROCLASTIC ROCKS

(a) Melavolcanics

(D| Tuff

ABBREVIATIONS

bx brecciated

cp chalcopynle

diss disseminatetl

mag magretiie

po oyrrhotile

PV PV" 1e

g.cv quartz-carbonate vemleis

(jw quarl; vein

SURFACE TRACE OF . VLF-EM CONDUCTOR 'A

GS-86-2 L44-OOE 1+25 N

CONDUCTOR TRACE PROJECTED TO DEPTH

I89I7

. I89I8-I892I

IGB.7|72, I8922-I8925

, I8926-I8930

I893I-I8934

18935 - 18944

18945-18963

320

.18964-18968 DETAILED LOCATION MAP

SCALEBOO _ O B(*^— I OQO

UCTHCS

361.5'. 18969 - 18973

•367

'v 18974-1897710

SCALE10 20 - 30

l FEET

40 50

S3B02SE*a*5 63.5038 WAPAMISK CREEK

GREENSTRIKE GOLD CORPHORSESHOE LAKE GRID

GRID B

DIAMOND DRILL SECTION HOLE

Project No: C-777

Scale: i"s 20

Drawing No: 5

By N.O. Willoughby

Drawn' MPH

Date: May, 1986

MPH) MPH Consulting Limited

LEGEND

7 S' - "l MAFIC INTRUSIVE ROCKS

Diabase (Basa ! i?;

6 \ * * *| FELSIC INTRUSIVE ROCKS

Diorite. Gianodionie

CHEMICAL SEDIMENTARY ROCKS

ia. Magnetite Iron Formation.

(b| Magnedle Pyrrholite Iron Fo-malion

(c| Banded Iron ^ormahori

4 I^L:-1 METASEDIMENTARY/VOLCANICLASTIC ROCKS

la] Argillite

(b) Chlorine Argillile

(c) Tullaceous Argillite

(d| Magnetile-Beanng Argiiine. liilislone (iron Fofma!ion''|

(e| VoH:anit:laslic Sedimenl/SanOslone

INTERMEDIATE PYROCLASTIC ROCKS

(a( Fine Grained Tutf

(b] Crystal lull

(c) Lilted Crystal) Tull

(0| Lapilli Tuff

|e| Agglomerate

INTERMEDIATE METAVOLCANIC ROCKS

MAFIC METAVOLCANIC, PYROCLASTIC ROCKS

(a( Meta/olcanics

ID] Tull

ABBREVIATIONS

b* brecciated

co chalcopyrite

diss disseminated

mag magnetite

po pyrrhotite

py pyrite

Q'Cv quart; carbonate vemlets

qv quar!/ vein

SOUTHNORTH

SURFACE TRACE OF VLF - EM CONDUCTOR 'A

CONDUCTOR TRACE PROJECTED TO DEPTH

18886-18889

18890-18895

. 18896-18900

GS-86-3 L7tOOE,0+62.5N

IZ;fft ' 18902-18904

GRIDE GRID A :

GRIDD

DETAILED LOCATION MAP

SCALEBOO O 6OO IOOO IBOO

METRES

18905-18908

10 O

SCALE

10 2O 30l

FEET

40 50

18909-18913

359 18913-18915•36Z

18916

6REENSTRIKE GOLD CORPHORSESHOE LAKE GRID

GRID B

DIAMOND DRILL SECTIONHOLE GS -

Project No: C-777Scale:

Drawing No: 6

By N.O. WilloughbyDrawn: MPH

Date- May, 1986

MPH ) MPH Consulting Limited

53B02SEaa05 63.5038 WAPAMISK CREEK 350

SOUTHNORTH

GS - 86- 1 L6+OOW, 2+OON

LEGEND

7 l" * "[ MAFIC INTRUSIVE ROCKS

Diabase (Basalt]

6 l* * *| FELSIC INTRUSIVE ROCKS

Diorite. Granodiorite

5 \ "a " l CHEMICAL SEDIMENTARY ROCKS

[aj Magnetite Iron Formation

(D) Magnetile-Pyrrholite Iron Formation

(c) Banded Iron Formation

4 l^s-f-l METASEDIMENTARY/VOLCANICLASTIC ROCKS

lai Argillite

(l)) CtllontiC Argillite

(C) Tuffaceous Aigillife

{di Magneliie-Beanng Argillite. Siltstone (iron Formation'*}

(e t Volcaniclastic Sediment/Sandstone

3 l" 'J INTERMEDIATE PYROCLASTIC ROCKS

(a) Fine Grained TuM

(b| Crystal lull

[c| Lurnc (^ Crystal! Tul'

Id] Lapilli Tuff

(e] Agglomerate

2 l y ' :\ I NTERMEDIATE METAVOLCANIC ROCKS

1 \.'-'-':'.] M AFIC METAVOLCANIC, PYROCLASTIC ROCKS

(a) Meiauolcanics

(b) Tuff

ABBREVIATIONS

bx brecciated

cp chalcopv"' 6

diss Oissemmated

mag magnetite

3Q,2

SURFACE TRACE OF HLEM CONDUCTOR 'B

I880I - I8825

•3-S% potpytcptmag

18826,18827

296

18628-18838

DETAILED LOCATION MAP

SCALE500 O BOO IOOO I9OO

317

18839-18852

331.5'

SCALE10 20 30

S-20% potpy 18855-18878

397'

18879-18885

po pyrrnotne

PV Pynfe

q ev quarl;-carbijnate

QV quartz jem

3a,5a

63.5038 WAPAMISK CREEK 260

GREENSTRIKE GOLD CORPHORSESHOE LAKE GRID

GRID E

DIAMOND DRILL SECTIONHOLE GS -

Project No: C-777

Scale:Drawing No: 4

By : NO.Willoughby

Drawn;

Date: May, 1986

M PH) MPH Consulting Limited

63-5038