39 dona lake 010 - ontario · 39 dona lake 010 diamond drilling area: ... 1 r 4mi toronto, canada....

39 DONA LAKE 010

DIAMOND DRILLING

AREA: DONA LAKE REPORT NO: 39

WORK PERFORMED FOR: Power explorations Inc.

RECORDED HOLDER: Same as above [ xx ] : Other [ ]

Cla

Pa Pa

Pa

Pa

Pa

Pa

Pa

Pa

Pa

am No .

7868567 786855

786856

850854

850855

850846

786864

786869

786868

Hole No.

EL-87-1

EL-87-2

EL-87-3 EL-87-4

EL-87-5

EL-87-6

EL-87-7

EL-87-8

EL-87-9

Footage

297'

317 1

397' 477'

307'

317'

257 '

327 '

397'

Date

Nov/87

Nov/87

Nov/87 Dec/87

Dec/87

Dec/87

Dec/87

Dec/87

Dec/87

Note

(1)

(1)

(1) (1)

(1)

(1)

(1)

(1)

(1)

NOTES: (1) #W8803.111, filed in August/88

iEOCflNEH"

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REPORT ON

GEOLOGICAL MAPPING, PROSPECTING

AND

LITHOGEOCHEMICAL SAMPLING

AND

DIAMOND DRILLING

EYE LAKE PROPERTY

DISTRICT OF KENORA, PATRICIA MINING DIVISION

NORTHWESTERN ONTARIO

FOR

POWER EXPLORATIONS INC.

NTS 52-0/8E

ONTARIO GEOLOGICAL SURVEY ASSESSMENT FILES

APR 2 2 1988

RECEIVED

February 1988 R.I. Fogal, B.Se. R.A.V. Higginson, B.Se,

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TABLE OF52088NE8888 39 DONA LAKE

VV \010C

MAR 2 81988*- HOI.O SUMMARY

2.0 INTRODUCTION

3.0 PROPERTY DESCRIPTION

4.0 LOCATION, ACCESS AND SERVICES

5.0 PHYSIOGRAPHY AND VEGETATION

6.0 PREVIOUS WORK

7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION

8.0 PROPERTY GEOLOGY

8.1 General Geology

8.2 Volcanics

8.3 Intrusives

8.4 Metamorphism

8.5 Structure

9.0 GEOPHYSICAL SUMMARY

10.0 DESCRIPTION OF PROGRAMS

10.1 Geological Mapping, Prospecting, and Lithogeochemical Sampling Programs

10.2 Diamond Drilling Program

II.0 DISCUSSION OF RESULTS

12.0 CONCLUSIONS

13.0 RECOMMENDATIONS

13.1 Phase I

13.2 Phase II

14.0 ESTIMATED COST OF RECOMMENDED EXPLORATION PROGRAM

15.0 REFERENCES

Page

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LIST OF APPENDICES

AA CERTIFICATES OF QUALIFICATION

B TECHNICAL DATA STATEMENT AND REPORT OF WORK

C ROCK SAMPLE DESCRIPTIONS AND ANALYSES

D ROCK SAMPLE ASSAY CERTIFICATES

E DIAMOND DRILL LOGS

F LEGEND AND DIAMOND DRILL SECTIONS

G CORE SAMPLE ASSAY CERTIFICATES

LIST OF TABLES

TABLE NO. 1 - SUMMARY OF DRILL HOLE DATA

LIST OF FIGURES

FIGURE NO. 1 - LOCATION MAP

FIGURE NO. 2 - CLAIM SKETCH

FIGURE NO. 3 - PROPERTY LOCATION ANDREGIONAL GEOLOGY

FIGURE NO. 4 - PLAN OF DRILLING

FIGURE NO. 5 - LEGEND

FIGURE NO. 6 - DIAMOND DRILL SECTION: EL-87-1,2



FIGURE NO. 9 - DIAMOND DRILL SECTION: EL-87-7



LIST OF DRAWINGS

DRAWING NO. 1 - PROPERTY GEOLOGY-EYE LAKE SECTION

DRAWING NO, 2 - PROPERTY GEOLOGY - KOMAR SECTION

Back of report

II M II

II II II

II II II

II H II

II M II

II II II

Page 20

Page 3

Page 5

Page 10

Page 17

Appendix F

F

F

F

F

F

F

In map pocket

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l. O SUMMARY

The Eye Lake property, held under a joint venture agreement

between Van Horne Gold Exploration Inc. and Power

Explorations Inc., is located in the Pickle Lake greenstone

belt, one mile east of the Placer Dome - Dona Lake Mine, and

6.5 miles southeast of the town of Pickle Lake.

The stratigraphy has been subdivided into two distinct

lithologic assemblages; a thick sequence of largely mafic

volcanics which grades into intermediate pyroclastic and

andesitic flows, and a broad package of banded gneiss to the east.

Anomalous gold mineralization of subeconomic grade was

encountered during both the surface geological exploration

program and the nine hole, 3,093 foot diamond drilling

program. The mineralization is hosted in quartz-carbonate

veining and sulphide-bearing horizons spatially associated,

or coincident with a geophysically interpreted regional

fault-shear system, which transects the property in a north-south direction.

A two-phase exploration program is warranted and recommended

for the property. Phase I of the proposed program would involve ground-magnetics and induced polarization surveys

along the interpreted regional break, followed by power

stripping, mapping and sampling of specific areas with

potential to host gold mineralization. Phase II would

involve a minimum of 2,000 feet of diamond drilling as a

follow-up to both Phase I and current progam results.

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- 2 -

2.0 INTRODUCTION

The following report describes the results of a comprehen

sive exploration program consisting of geological mapping,

prospecting, lithogeochemical sampling, and diamond drilling

on the Eye Lake property in the Dona Lake area. The property

is located 6.5 miles southeast of the town of Pickle Lake

(Fig. No. 1) in the Patricia Mining Division, District of

Kenora, northwestern Ontario.

The present program and concurrent geophysical surveys,

including VLF-EM, ground magnetics and induced polarization,

were carried out by Geocanex Ltd.

The property consists of 69 contiguous mining claims. All

work was done on a cut picket line grid. The grid has a

north-south baseline with perpendicular lines at 400 foot

intervals across the strike of the local stratigraphy.

Several tie lines were cut to ensure control on long picket

lines. Geological mapping and geophysical plotting were done

at a scale of l inch ^ 200 feet.

The personnel involved in the geological surface exploration

program were:

R. Higginson Project Geologist Oro Station, Ontario

J. Drew Geologist North Bay, Ontario

B. Howes Field Assistant Kingston, Ontario

Geophysical anomalies were prospected and quartz veins and

mineralized volcanics were sampled. All sample descriptions

and assays are included in this report.

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^,V^v,/^-O-I^-X-v

t

C." N 'V \\OWVPIMISKANLAKE

EYE LAKE'PROPERTYPICKLE5"?*

ONTARIO

KENORA-

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li* 1 —c-L-i:-^^"" s-'""\i

UNITED

STATES

HEM LO,--'-v-;::7 X WAWA

TIMMINS*

KIRKLAND

SAULT STE MARIE

SUDBURY

^1'-" Greenstone Belts

ot

lOOmilo


EYE LAKE PROPERTY Patricia M.D., Ontario

LOCATION MAP

SCALE: It lOOmiDATE: FEB. 1988 I B Y; H.H./H.T.M

FIQ.NOi. l

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- 4 -

The geological work was performed between July 22, 1987 and

August 5, 1987. The time breakdown for the work performed is

as follows:

Man-Days

Mapping and Prospecting: 33 1/4 Man-Days

The personnel involved in the diamond drilling program were:

R. Fogal Geologist Windsor, Ontario

R. Higginson Geologist Oro Station, Ontario

J, Pierce Field Assistant Wasaga Beach, Ontario

A total of nine holes were drilled to investigate geophysical

and geological targets proposed subsequent to the geological

surface exploration program. All diamond drill logs and

assays are included in this report.

The drilling program was carried out between November 23,

1987 and December 18, 1987. The time breakdown for the

diamond drill program is as follows:

Man-Days

Logging and Splitting Core: 52 Man-Days

3.0 PROPERTY DESCRIPTION

The Eye Lake property consists of 69 contiguous unpatented

mining claims in the Dona Lake area, Patricia Mining

Division, northwestern Ontario (Fig. No. 2). The claim

numbers and recording dates are as follows:

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R l l

l90 0 05' CONNELL TWP

l l ,l s

f -T f lI'll9B49I5 j 964914) 964913 964912 964911

9B4920 964919 964918 B649I7

964932 964931 964928 964*27

MCCULLAGHTWR

' l l l l f- — — 4- — — 4- -i—-| 964925.964924 964925 964922 j 964921' '

964933) 964930 964929:

9S4926 \— — 4- —— -f- —— -4~ ' ——J ' 850845 j 8508461,

90S528 l 850849

850850850857 850856

J ': l l 903525 1 403526 . 9035zV 850852 '850851l

-"J-^——— i--, ——— IX-

786857 j 786856 ' 786855 j 78685

786850 786851 786852 78OT53

769379 j 786848 | 786847 l 788846

S

l786642 l 786844 l 786849

l l—— I— r——786840 i 786839 786838

51 0 25' ——

778970 778972 l 786837

- — --j- — —-f- — — -

786863(786864 ' 786865 ' 786866

— _ i _ _ L | _ — .

766869 . 786868 l 786867

7868,72 , 788B73

l mile



CLAIM SKETCH

OEOCANEX LTD TORONTO. CANADA

BYTR.tM.DATE JAN 1988 SC ALE: l"* 2640' FlG. No' 2

MINES, PAST PRODUCER

r"1--'

GEOLOGY LEGEND

'Gc'C C' t1 Ou'1 dO'y

LOCATION MAP

GOLD PRODUCTION -OZ? '."--1 .- 52.806

MAP AREA

Onto rio

On* or-o Geo'ogico' SurveyVise pope" 199, '984S'o" G V 9 Wo"ace HVap 2 2'9 , Co' Lake - D ' eh le Lone,Sage e' a' , '9/2

RED LAKE MD PATRICIA '

Pickte-L^.

Golden Patricia DiscoveryB60,000fo fl s ct 0-58oz7toi Au

Wright Lake

Obaskaka Lake

Hasaga200,000 tons o* 0-19 oz/ton Au

LAKE ST JOSEPH

Carpenter L.

90MINES, PAST PRODUCER

A Central Patricia No lB Cenfroi PatriCic MeC Pickle Crow No lD Pickle Crow No 2

E Albanyf tfowshoreG UMEX Thierry Vine

Collishaw Lake

GOLD PRODUCTION , ,PROPERTY TONS OZS GUL'D OZ/TON

t'-it o Parr.oo l, . . .f.cue Crov. 3,r37, 57? 1,446,214

Total 4,966,820 ?,068,020

MCCULLAGH . TWP

LAKE PROPERTYKOMAR SECTION

Dona Lake Discovery1,400,000 tons at 0-24oz7ton Au

Kawinogans Lake


EYE LAKE PROPERTY

Patricia M. D., Ontario/OsnaburghHasago

'? ?00,000 tons ot 0-19 oz/fon Au PROPERTY LOCATION AND REGIONAL GEOLOGY

l.AKE ST. JOSEPH

DATE: Jan.1988SCALE: 1 r 4miGEOCANEX LTD

TORONTO, CANADA


- 6 -

Claim Numbers

Pa 786837-

Pa 786842

Pa 786844-

Pa 786850-

Pa 786863-

Pa 786871-

Pa 778970,

Pa 769379

Pa 850845,

Pa 850849-

Pa 903525-

Pa 964911-

786840 inclusive

786848 inclusive

786857 inclusive

786869 inclusive

786873 inclusive

778972

850846

850857 inclusive

903528 inclusive

964933 inclusive

Recording Dates

April 30, 1984

April 30, 1984

April 30, 1984

April 30, 1984

April 30, 1984

April 30, 1984

April 30, 1984

April 30, 1984

February 13, 1986

February 13, 1986

June 24, 1986

January 29, 1987

Total Claims 69

The claims are held under a joint venture agreement between

Van Horne Gold Exploration Inc. and Power Explorations Inc.,

both of 1003-34 King Street East, Toronto, Ontario, M5C 1E5.

4.0 LOCATION, ACCESS AND SERVICES

The property can be reached by float/ski plane or helicopter

from Pickle Lake 6.5 miles to the northwest. An all weather

gravel road from Highway 599 ends one mile west of the

property at the Placer Dome Inc. gold deposit near Dona Lake.

A winter drilling road extends from the mine to the

property.

Pickle Lake is a mining and transportation centre with a

population of approximately 350. The Dona Lake mine, slated

for production, has sparked new developments in Pickle Lake,

including housing and related service facilities. UMEX


7

Inc. (Union Miniere) operates a 4,000 TPD copper-nickel mine

and concentrator seven miles northwest of Pickle Lake. The

mine is presently closed due to depressed base metal prices.

Pickle Lake is connected by paved Highway 599 to Savant Lake

and the Canadian National transcontinental railway line, 90

miles to the south, and to Ignace and Trans Canada Highway

17, 180 miles to the south. Electricity is supplied by a

hydro line connecting Pickle Lake to the Ear Falls generating

station. Air, ground and water transportation for local use

are readily available in town. Pickle Lake is also serviced

by regular NorOntair flights from Thunder Bay.

5.0 PHYSIOGRAPHY AND VEGETATION

Most of the property is covered by flat-lying spruce and

spruce-tamarack over muskeg. Cedar-alder swamps and grassy

bogs surround several small lakes and creeks. Several

northeast-southwest trending glacial ridges occur in the

central portion of the property, with hummocky glacial mounds

prevailing to the south. Many of the ridges are bedrock

controlled with outcrop exposures flanking individual ridges.

Vegetation on the ridges consists of birch-poplar and spruce

forests.

Outcrop exposures constitute S-10% of the property, and are

generally confined to the west and central portions of the

property.


- 8 -

6.0 PREVIOUS WORK

In 1967, M. Firth had two holes drilled 1/2 mile southwest of

the property. The drilling encountered andesite, dacite and

rhyolite with minor mineralized tuff horizons. The minerali

zation consisted of pyrite, pyrrhotite and trace chalcopy

rite. Assay values up to 0.01 ounces of gold per ton and

Q.13% copper were reported.

In 1984, Van Horne Gold Exploration Inc. staked the original

block of 31 claims. Geocanex Ltd. was contracted to

undertake geological mapping and geophysical surveys,

including ground magnetics and VLF-EM (Gillick, R.E., 1984, and North, J.W., 1984). Assays of 0.093 and 0.206 ounces of

gold per ton were obtained from grab samples of sulphide and

sulphide-quartz filled shears in andesite. This showing is

located east of BLO between L79N and L78N. Several geo

physical anomalies interpreted as potential gold-bearing

sulphide mineralization zones associated with faulting were

detected in the southwestern part of the property.

In 1985, Geoterrex Ltd. flew airborne regional electro

magnetic and total intensity magnetics surveys over the

Pickle Lake area for the Ontario Geological Survey. The

surveys covered the entire Eye Lake property.

In 1986, Van Horne Gold Exploration Inc. obtained an

additional 28 claims adjoining the original property to the

north. Van Horne Gold Exploration Inc. subsequently signed a

joint venture agreement with Power Explorations Inc.

Geocanex Ltd. was then contracted to complete the current

geophysical, geological and diamond drill programs.

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7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION

The Pickle Lake area is located within the Uchi Subprovince,

a part of the Superior Province of the Canadian Shield. The

area is characterized be several arcuate, highly deformed and

coalescing greenstone belts, consisting of predominantly

mafic to intermediate volcanic flows, which have been

intruded by numerous granitic to ultramafic intrusive bodies.

The metamorphic grade ranges from greenschist to amphibolite

facies. The volcanics host subordinate amounts of felsic to

mafic pyroclastics, sediments and iron formation. Felsic

quartz-feldspar porphyry dykes are commonly found in all

lithologies (Fig. No. 3).

Ultramafic rocks host copper-nickel mineralization at the

Union Miniere Thierry Mine, seven miles northwest of Pickle

Lake, with mined ore and mineral reserves totalling

14,000,000 tons grading 1.6% copper and Q.2% nickel.

Historically, gold production in the Pickle Lake area has

occurred in structurally controlled vein type deposits or

sulphide replacement bodies spatially associated with, or

contained within, bands of Algoman (chert-magnetite) iron

formation.

The former producing Pickle Crow and Central Patricia mines

operated from 1935 to 1966 and 1934 to 1951, respectively,

collectively producing 2,068,020 ounces of gold from

4,966,820 tons of ore for an average grade of 0.416 ounces of

gold per ton. Gold was recovered from quartz veins, vein

networks and sulphide replacement bodies which occupied

shears, faults, fissures and fold axial plane fractures in

highly deformed mafic volcanics and iron formation. Gold-

bearing quartz veins were also mined within quartz-albite


- 11 -

porphyry sills near the contact of mafic volcanics and iron

formation.

Placer Dome Inc. and St. Joe Canada Inc. both recently

announced plans to open new mines in the Pickle Lake area.

Placer Dome's Dona Lake property, located approximately one

mile west of the Eye Lake property, has reported reserves of

1,500,000 tons grading 0.3 ounces of gold per ton. Gold

mineralization occurs as sulphide replacement bodies within a

band of highly deformed oxide facies iron formation (Northern

Miner, September 1986). The mine is expected to produce

approximately 40,000 ounces of gold per year over a ten year

period.

St. Joe Canada's Golden Patricia property is reported to have

an estimated 500,000 ounces of gold reserves with a grade of

0.58 ounces of gold per ton. The property is located

approximately 40 miles west of Pickle Lake. Gold minerali

zation occurs in a quartz vein at a contact between a

mylonitized unit and sheared mafic volcanics in close

proximity to banded iron formation (Northern Miner Magazine,

September 1986). The initial mining project has drill

indicated reserves of 283,000 tons grading 0.88 ounces per

ton, and is expected to produce 40,000 ounces of gold

annually (Northern Miner, March 23, 1987).

8.0 PROPERTY GEOLOGY

8.l General Geology

The Eye Lake property is underlain by a north-south trending

limb of the Pickle Lake greenstone belt. The local strati

graphy, as noted by North (1984) can be subdivided into two


- 12 -

broad sequences: a thick package of mafic volcanics,

including basalt, andesite and amphibolite in the western

portion of the property grading into dacitic pyroclastics and

andesitic flows in the north-east and north central portions

of the property; and a thick sequence of banded gneiss

forming the second area in the eastern part of the property.

The volcanic-gneiss contact has been interpreted as a fault

contact which trends north-northeast across the property.

Gillick (1984) and Medd (1987) indicate that this fault is a

continuous regional feature.

8.2 Volcanics

Mafic volcanics exposed west of BLO+00 are fine-grained,

green, chloritic pillowed to massive flows of basaltic to

andesitic composition. The pillows are generally deformed,

however an exposure on L28+OON at L17+OOW provided a west

facing top direction.

East of the baseline, the mafic volcanics grade into dacitic

tuffs and andesitic flows.

The tuffs are light green to buff in colour, fine-grained,

and laminated to banded.

Banded gneiss exposed in the southwestern portion of the

property is described by North (1984) as varying composi-

tonally from biotite-quartz gneiss to hornblende-quartz-

gneiss.


- 13 -

8.3 Intrusives

A felsic quartz-feldspar porphyry intrusive sill is exposed

at LSO+OONjlO+OOE. The intrusive has an orange-buff fine

grained groundmass of quartz and feldspar with euhedral

porphyritic feldspar laths.

8.4 Metamorphism

The volcanics exposed in the west and central portion of the

property are highly chloritic and indicate a metamorphic

grade of greenschist facies. The banded gneisses in the

southwest corner of the property exhibit lower amphibolite

facies metamorphism. It is suggested that the volcanics and

gneisses are separate units that are fault bounded, and do

not represent gradual changes in metamorphic grade across the

property.

8.5 Structure

Minor isoclinal and kink folding was noted in several

locations on the property and may represent parasitic

features associated with large scale folds and faults

interpeted from geophysical data.

Observed shearing and foliation directions are roughly

concordant with bedding directions obtained from pillows in

the western part of the property and trend due north to

north-northeast.


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9.0 GEOPHYSICAL SUMMARY

Several ground magnetic, VLF-EM and regional airborne magne

tic surveys have been completed over the Eye Lake property.

Based on these surveys, two lithologic packages have been

delineated, separated by an interpreted fault contact

trending approximately north-south through to the middle of

the property. The west side is generally characterized by

relatively higher amplitude magnetics than the eastern

portion. Both units exhibit discontinuous, irregular lenti

cular magnetic expressions roughly trending in a north-south

direction, which corresponds to the regional magnetic

expression.

A large fold/fault structure has been detected in the north-

central area of the property, along the previously mentioned

contact. Several inferred faults transect both lithologic

units, manifested as magnetic discontinuities and/or abrupt

interruptions in the magnetic expression.

Several discontinuous VLF-EM conductors trending subparallel

to the property stratigraphy have been delineated. These

have been interpreted to represent weak to moderate zones of

disseminated mineralization. Of particular interest is a

north-northeast trending conductor in the southwest corner of

the property coinciding with a small creek/lake system. A

fault or shear related source is suggested for this anomalous

conductor.

Combined, these surveys proved valuable in delineating

favourable diamond drill targets.


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10.0 DESCRIPTION OF PROGRAMS

10.1 Geological Mapping, Prospecting and Lithogeochemical

Sampling Programs

The geological mapping, prospecting and lithogeochemical

program was carried out between July 22, 1987 and August 5,

1987, by Geocanex Ltd. Maps were prepared at a scale of l

inch to 200 feet and may be found at the back of the report.

A total of 37 grab samples were collected from favourable

geologic environments. The main focus of sampling included

quartz and quartz carbonate veins and vein networks, sheared and altered volcanics, and sulphide-mineralized horizons.

Bondar-Clegg and Company Ltd., of Ottawa, Ontario analyzed

all submitted surface samples for gold using fire assay

techniques. All results and sample descriptions are included

in Appendix C. Analytical certificates are shown in Appendix D.

10.2 Diamond Drilling Program

The diamond drilling progam was contracted to Midwest

Drilling of Winnipeg, Manitoba. A total of nine B.Q. size

(1-7/16") diamond drill holes totalling 3,093 feet were

completed between November 23, 1987 and December 18, 1987,

under the supervision of Geocanex Ltd. Diamond drill hole

targets were chosen subsequent to the geological mapping/

sampling program. Favourable geophysical targets were also

considered for diamond drill hole testing.

Midwest Drilling provided room and board on site for both

geological and drill crews. The camp was supplied by heli

copter and ski-plane from Pickle Lake.


- 16 -

Detailed core logging was followed by sampling of favourable

horizons. A total of 507 samples were submitted, each

consisting of halved core, over intervals from .5 to 5.0 feet

in length. Core samples were analyzed by two separate

laboratories over the course of the program. The labora

tories involved were Bell-White Analytical Laboratories Ltd.

of Haileybury, Ontario, and Assayers (Ontario) Limited of

Toronto, Ontario.

All samples were analyzed for gold using standard fire assay

techniques; results were reported in ounces of gold per ton.

Hole locations are shown in Figure No. 4. Drill sections are

shown in Appendix F. Diamond drill logs and assay certifi

cates are enclosed in Appendices E and G respectively.

11.0 DISCUSSION OF RESULTS

Several anomalous gold values were obtained during the

mapping and prospecting phases of the program. Significant

gold values up to 1,220 parts per billion were encountered in

various lithologies. A common feature to all of the anoma

lous values was the presence of quartz carbonate veining and

limonitic staining indicating a probable sulphide-gold

association.

On the basis of compiled geological, geochemical and geophy

sical data, several favourable fault-fold structures and

potentially gold-bearing sulphide horizons were defined. A

preliminary set of nine holes were thus chosen to test these

features.

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The primary drilling target of this program was a moderate to

strong VLF-EM conductor interpreted as a regional, north-

south trending fault-shear zone. Several trenches occurring

on the flank of the main conductor were grab sampled by North

(1984), and reportedly returned gold values of .206 and .093

ounces per ton.

Elevated gold values were obtained from Holes EL-87-1, 2, 3

and 4 (see Table No. 1). Hole EL-87-1 returned a 5.0 foot

intersection grading .010 ounces per ton gold in intermediate

to felsic tuff containing quartz ^ carbonate stringers with

minor sulphides. Hole EL-87-2 y-ielded a 5.0 foot interval of

.02 ounces per ton gold in quartz j^ carbonate veinlets hosted

in intermediate flows. Hole EL-87-3 returned .026 ounces per

ton gold over 3.0 feet in well-banded intermediate tuff

containing up to 31 pyrrhotite, pyrite and trace chalco

pyrite. A 21.0 foot interval in Hole EL-87-4 returned gold

values ranging from trace to .024 ounces per ton in inter

bedded felsic and intermediate tuffs containing S-5% pyrite

and pyrrhotite. Hole EL-87-5 returned a gold value of .024

ounces per ton over 1.9 feet in calcite j^ quartz veinlets

containing up to 3ti pyrite and pyrrhotite hosted in mafic to

intermediate volcanics.

The gold mineralization in these holes was intersected in

various lithologies, however, it was consistently associated

with quartz jj^ carbonate stringers and/or pyrite-pyrrhotite

mineralization.

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12.0 CONCLUSIONS

Gold mineralization of sub-economic grade was encountered on all phases of the current program. Compilation of geological, geochemical, geophysical and diamond drilling results indicate that the gold mineralization encountered occurs in association with quartz-carbonate veining and sulphide-bearing horizons, spatially related to a geophysically indicated regional fault-shear system, which transects the property in a north-south direction.

Additional work is warranted and indicated to delineate the nature and extent of potentially economic gold minerali zation.

13.0 RECOMMENDATIONS

A two-phase exploration program is recommended and warranted for the property and would involve:

13.1 Phase I

Geophysical surveys, including detailed ground magnetics with readings at 10 to 25 foot intervals, as well as induced polarization on a 100 foot spaced picket line grid over selected portions of the regional fault-shear system. This would be followed by power stripping of selected sites to delineate potential structurally or stratigraphically controlled gold mineralization.

13.2 Phase II

A minimum of 2,000 feet of diamond drilling is estimated to test potentially gold-bearing structures and horizons defined in Phase I and as a follow-up to the current program.

TABLE I SUMMARY TABLE OF DRILL HOLE DATA

Drillhole Number

Grid Location (metric)

Length

(feet)

ASSAY RESULTSSUMMARY DESCRIPTION Intersection

(feet)Width (feet)

oz./Au/ ton

Description

EL-87-1 0+50S, 297 Mafic flows intercalated with felsic to inter- 2+15E mediate well banded tuffs, exhibiting two

distinct sulphide-bearing silicified zones, typically containing minor sericite j^ garnet.

195.5-200.5 5.0 .010 Felsic to inter mediate tuffs, well developed banding, sul phides to 5% l containing quartz HK carbo nate stringers.

EL-87-2

EL-87-3

0+50S, BL 0

11+OON, 6+35E

317 Thick intermediate flows with minor felsic 105.0-110.0 constituent as well as a banded tuff horizon, typically containing abundant barren quartz + carbonate veinlets, randomly distributed.

397 Felsic to intermediate flows, with minor 370.5-373.7 poorly banded siltstone as thin horizons, and

5.0 .020 Intermediate flows containing irregular quartz * carbonate stringers, minor chlorite, sul phides to 2% as fracture coatings .

3.2 .026 Well banded intermediate

ro o

intermediate tuffs dominating further down hole. Trace disseminated sulphides and garnet.

tuffs, abundant quartz -*- calcite stringers. Trace sulphides.

EL-87-4 11-K30N 477 Dominantly mafic to intermediate flows and 3+20E tuffs, minor narrow siltstone horizons and

quartz - feldspar porphyry.

Abundant quartz j^ carbonate, sericite, epidote.

with lesser

89.2-91.0 1.8 .016 Well banded maficto intermediate tuff, minor silt stone, quartz- carbonate stringers.

240.6-242.6 2.0 .012 Mafic to inter- 252.0-255.6 3.6 .014 mediate tuffs,

containing pyrite * pyrrhotite


Drillhole Grid Length Number Location

(metric) (feet)

ASSAY RESULTSSUMMARY DESCRIPTION Intersection Width oz./Au/ Description

(feet) (feet) ton

fracture infill ing to 5?;. Minor associated garnet .

426.0-430.0 4.0 .012 Interbedded 433.5-437.0 3.5 .016 felsic and inter- 442.0-447.0 5.0 .024 mediate tuffs,

abundant carbonate veinlets, minor pyrrhotite blebs; garnets to 5*.

EL-87-5 44+50N, 307 3+30W

EL-87-6 44+50N, 317 9+OOW

EL-87-7 0+00, 257 12+55W

Mafic to intermediate flows and tuffs contain- 186.8-188.7 1.9 .024 Massive mafic to ing several highly altered, silicified zones, intermediate minor sericite, tourmaline. flows, finely

disseminated sulphides to 3%.

Dominantly mafic to intermediate volcanics as flow and tuffs, moderately carbonate zed. Abundant quartz * calcite typically barren.

Mafic to intermediate tuffs, containing minor mafic flows. Highly silicified section,

l

K)

containing up to 5% sulphides, occurs with minor associated sericite + muscovite.


Drillhole Number

Grid Location (metric)

Length

(feet)

ASSAY RESULTSSUMMARY DESCRIPTION Intersection

(feet)Width (feet)

oz./Au/ ton

Description

EL-87-8 2OOOS, 327 Mafic to intermediate volcanic flows, massive, 7-fOOW grading into well banded tuffs of similar

composition. Sporadic quartz * calcite veinlets, typically barren. ~~

24+OOS,397Mafic to intermediate tuffs, overlain by flows 1+60E of similar composition. Trace sulphides as

fine disseminations throughout.

EL-87-9

l - 23 -

l 14.0 COST OF RECOMMENDATION

14.1 Phase I

l Line cutting 25.5 miles at ?350Xlinemile, all inclusive————————————————————————5 8,925,00

l Ground magnetics at 10 to 25 footintervals, over 36 miles at ?3007linemile, all inclusive————————————————————————5 10,800.00

— Induced Polarization survey overselected VLF-EM axes 5 line miles

M at 31,2007line mile———————————————————————5 6,000.00

Power stripping/trenching, bacXhoe

I plus operator for 10 days at a rate of ^SOO/day, all inclusive———————————————————5 5,000.00

g Trenching, mapping and sampling, onel geologist plus assistant for 10 days at— a rate of SSOO/day, all inclusive—————————5 5,000.00

l Contingencies 201——-————————————-——-——-——3 7,145.00

Total Cost of Phase I ——————————————————————— S 42,870.00

l 14.2 Phase II

I Diamond Drilling: 2,000 feet at a rate of 535/foot——————————————————————————5 70,000.00

— Contingencies 20*———————————————————————S 14,000.00

" Total Cost of Phase II———————————————————? 84,000.00

l Total Cost of Phases I and II —————————————— 3126,670.00

fl Respectfully Submitted,

l R.A.V. Higgihson, B.Se.

I s/YsT^ tf "7c s f*' f f* t—*- '''f fi

R.I. Fogal, B.Se. Geocanex Ltd.

l


- 24 -

:5.0 REFERENCES

Gillick, R.E., 1984. Report on Ground Magnetic and VLF-EM Surveys on the Eye Lake property of Van Horne Gold Exploration Inc. for 591343 Ontario Ltd., Pickle Lake area, Northwestern Ontario; unpublished report of Geocanex Ltd.

Map 2218. Cat Lake - Pickle Lake area, O.G.S. Geological Compilation Series.

Medd, S.B., 1987. Report on Magnetic and VLF-EM Surveys on the Komar Property, District of Kenora, Patricia Mining Division, Northwestern Ontario for Van Horne Gold Exploration Inc.; unpublished report of Geocanex Ltd.

North, J.W., 1984. Report on Geological Mapping and Geochemical Sampling, Eye Lake property, Dona Lake area, Patricia Mining Division, Northwestern Ontario for Van Horne Gold Exploration Inc.; unpublished report of Geocanex Ltd.

O.G.S., 1980. Dona Lake area, District of Kenora (Patricia Portion); Ontario Geological Survey Preliminary Map P.2319, Sioux Lookout Data Series, Scale 1:15,840. Data compiled 1979.

O.G.S., 1986. Airborne Electromagnetic and Total Intensity Magnetic Survey, Pickle Lake area, District of Kenora (Patricia Portion), Ontario; by Geoterrex Limited for Ontario Geological Survey, Geophysical/ Geochemical Series, Map 80932, 80934. Scale 1:20,000. Survey and compilation from February to July, 1986.

O.G.S., Resident Geologist Files - Toronto and Sioux Lookout, Various unpublished assessment reports.


APPENDIX A

CERTIFICATES OF QUALIFICATION

CERTIFICATE OF QUALIFICATIONl l l l l l l l l l l1

V"i /^A, j J /tf&f B DATED THIS 7 DAY OF /'//U^ //^*

l

l

l

l

l

THIS IS TO CERTIFY THAT:

I am a resident of Oro Township, Ontario.

I am a graduate of the University of Waterloo, Waterloo, Ontario, with a degree in Bachelor of Science, Earth Science; major (Geology).

I have worked continuously as an exploration geologist since 1984, in gold exploration in northwestern Ontario.

I supervised geological mapping and geochemical sampling programs on the Eye Lake property, from July 22, 1987 to August 5, 1987.

The statements contained in this report, and conclusions reached, are based upon the study of all relevant assessment work records of the Ontario Geological Survey, and geological reports and maps published by the Ontario Ministry of Natural Resources.

In this report, I have disclosed all relevant descriptive and interpretative material, which is, to the best of my knowledge, necessary to gain a complete understanding of the viability of the project and the recommendations.

Robert A.V. Higginson, B.Se Geologist

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

APPENDIX B

TECHNICAL DATA STATEMENT AND REPORT OF WORK

l l l l l l l l l l l l l l lal

EYE LAKEMinistry of Geophysical-Geologlcal-Geochemical Northern Development Technical Data Statementand Mines

Ontario

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s). Township or Area. Claim Holder(s)—

Geological Sampling S Mapping

Dona Lake—.^—,,—,—.,.-———.——,—— Power Explorations Inc.

Survey Company —. Author of Report — Address of Author R ' R -

Geocanex Ltd.R. Higginson

Oro Station, Ontario, LOG

Covering Dates of Survey July 22, 1987 ~ August 5.(linecutting to office)

Total Miles of Line Cut—————————.————.——————.

1987

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

Geophysical

—Electromagnetic.

—Magnetometer_—Radiometric——

—Other-™—-

DAYS per claim

40

Geochemical.AIRBORNE CREDITS (Special provision credit* do not apply to airborne jurveyi)

Magnetometer. .Electromagnetic

DATE:.

(enter dayi per claim)

SIGNATURE:t or Agent

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

See Attached Sheet(prefix) (number)

i

TOTAL CLAIMS. 38

837 (857(2)

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

[

INDUCED POLARIZATION

PFmSTTVTTV GRAVITY ELECTROMAGNETIC MAGNETIC

Miimher of Stations Niimher of Readings

Station interval Line spar.ina

Profile srale

Hontour interval

Instrument

Arrurary — Srale ronstant

Diurnal rorrertion method

Rase Station rherk-in interval (hours)

Rase Station loration and value

Instrument

Toil ronfipuration

Toil separation

Arrurary

Method: CD Fixed transmitter O Shoot back O In lineFrequenry

(specify V.L.F. station)

Parameters measured

Instrument

Srale ronstant

Torrertions made

Base station value and loration

Elevation accuracy

Instrument .. ..

Method d Time Domain D Frequency DomainParameters - On time Frequency

Off time Range1

' — J Via y timet | — Tnt^gratinn time

i i-

Electrode array- ————————————————————————————————————————————————

Electrode spacing — ———————————————————————————————————— - — —— — ——Type of electrode . ——————————————————————————————————————————————————

1111111

D Parallel line

1

1

1

1

1

1

1

1

1

1

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken 964922, 964917, 850857, 850856, 903525, 903527, 786856, 786868, 850854

Total Number of Samples Type of Sample.

37

(Nature of Material)

Average Sample Weight——————— Method of Collection Grab Samples

2 kg

Soil Horizon Sampled. Horizon Development. Sample Depth————. Terrain.————————

Drainage Development——————————— Estimated Range of Overburden Thickness.

ANALYTICALValues expressed in: per cent

p. p. m. p. p. b.

D d S

Cu, Pb, Zn, Ni, Co, Ag, Mo, As.-(circle)

___Gold

Field Analysis (. .tests)Extraction Method.AnalyticalReagents

Field Laboratory AnalysisNo. (.——-.-^——

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

Mesh size of fraction used for analysis -150

Extraction Analytical Method. Reagents Used __

Commercial Laboratory 37 -tests)Name of Laboratory, Bondar-Clegg s Co. Extraction Mrthnrl Aqua Regia ______ Analytical Reagents Used

F. A. - A. A. S.

GeneraL General.

1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1

t

SELF POTENTIALInstrument

Survey Method

Corrections made

RADIOMETRIC

Instrument

Values measured

Energy windows (levels)

Heipht of instrument

Size of detector

Overburden

Range

Background Count ,

(type, depth - include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)

Type of survey

Instrument

Accuracy,

Parameters measured

Additional information (for understanding results),,. ,

AIRBORNE SURVEYSType of snrvey(s) .. .

Instrument(s) — ————————————————————————————————(specify for each type of survey)

Accuracy(specify for each type of lurvey)

Aircraft used,

Sensor altitude . . ,

Navigation and flight path recovery method ,C* O l J

Aircraft altitude

Miles flown over total area

Line Snarino

Over claims only

—————————————————————— ^^^^^^m^mf


- LIST OF CLAIMS

P,-i H 5 O H 4 5 R r)OH46

Pa H50H49 M 5 OH 5 O M50H5 l H 5OB 5 2 H 5 O H 5 3 H50H54 M50H55 H50H56

Pn 90 3 r) 2 5

903527 90 3 r) 2 M

J'a 96491.1 9649 l 296491396491496491596491696491 7964910964919964920964921964922964923964924964925964926964927 96492H964929964930964931964932964933

Totnl : 38 Claims

lll

l l ll

APPENDIX C

ROCK SAMPLE DESCRIPTIONS AND ANALYSIS

11 '11I11111w1

1111111

^ EYE

SAMPLE # ASSAY #

KE-1 1201

KE-2 1202

KE-3 1203

KE-4 1204

JD-01 1205

JD-02 1206

JD-03 12-7

JD-04 1208

JD-05 1209

JD-06 1210

JD-07 1211

JD-08 1212

JD-09 1213

JD-10 1214

JD-11 1215

LAKE GRAB

LOCATION

63+OON,42+OOE

60+OON,20+30E

50+OON,09+30E

48+20N,06+60E

48+OON,16+50E

48+OON,16+50E

45+25N,09+50E

45+25N,09+50E

44+30N,08+40E

44+30N,08+40E

44+40N,08+35E

36+70N,07+80W

31+80N,17+OOW

31+80N,17+OOW

31+80N,17+OOW

SAMPLE DESCRIPTIONS

DESCRIPTION

grab, highly folded dacite tuff withquartz vein, quartz-carbonate-hematitestringers, i-2% arsenopyrite.

12" quartz vein in dacite tuff.

24" quartz-feldspar porphyry in ande-sitic-dacitic volcanics.

8" X 24" quartz pod in folded inter mediate volcanics.

intermediate-volcanic (dacite tuff?) withlimonite staining along fractures.

quartz vein, 6", in intermediate vol canics, limonite staining near wallrock.

silicified intermediate volcanics withheavy limonite staining.

quartz pod (2" X 6") in intermediatevolcanics.

dacitic tuff(?) with trace-0.5% pyrite,minor limonite staining.

6" quartz vein, folded, minor limonitestaining, trace-0.5% pyrite.

folded, intermediate volcanics{possibly dacitic tuff with trace-0.5%pyrite), heavy limonite staining.

3" quartz vein, cross-cutting maficvolcanics, minor limonite staining.

4' wide quartz vein network, chertnear center of veins, limonite stain ing near contact with mafic volcanic.

mafic volcanic with carbonate and minorlimonite staining.

3" wide felsic dyke, boudinages andsinistrally offset.

Au ppb

^

^

10

5

10

^

10

105

10

925

1220

90

95

10

5

11 ' 1111111111I111111

tSAMPLE #

JD-12

JD-13

JD-14

JD-15

EY-BH-1

EY-BH-2

EY-BH-3

EY-BH-4

EY-BH-5

EY-BH-8

EY-BH-6

EY-BH-7

JD-16

JD-17

EY-BH-9

ASSAY

1216

1217

1218

1219

1220

1221

1222

1223

1224

1225

1226

1227

1228

1229

1230

EYE LAKE GRAB

# LOCATION

26+OON,22+40W

26+OON,22+40W

27+70N,17+OOW

27+70N, 17+OOW

03+48E,16+OON

13+OON,03+50E

12+OON,03+85E

11+OON,03+50E

11+OON,03+50E

11+OON,03+50E

10+25N,03+40E

10+25N,03+40E

00+80S, 00+80W

00+80S,00+80W

03+80E,08+OON

SAMPLE DESCRIPTIONS

DESCRIPTION

10" wide shear in mafic volcanic(pillowed) with quartz stringers throughout.

2" X 6" quartz pod, minor limonitestaining.

12" X 18" quartz pod in pillowedmafic volcanic, minor limonite stain ing.

12" quartz cross-cutting pillows, minor limonite staining.

dacite, minor limonite staining.

mafic, fine pillowed flow minor ironweathering.

andesite, limonite staining.

quartz vein, 2" wide, traces of pyrrho-tite/pyrite and arsenopyrite.

andesite, minor limonite staining,traces of pyrite.

andesite, disseminated sulphides,S-5% pyrite, T-2% arsenopyrite.

andesite, 1-23, pyrite.

quartz pod, 3" X 12", clear.

12" wide felsic dyke in intermediate volcanics.

mafic volcanics with limonite stain ing, trace pyrrhotite.

quartz vein, 3" wide, minor ironstaining.

Au ppb

70

^

5

tf

^

^

25

630

15

100

10

G

^

5

5

11 1111111g1111iiiiii

^ EYE LAKE GRAB

SAMPLE # ASSAY # LOCATION

JD-18 1231 mOON,04+OOE

JD-19 1232 11+OON,04+OOE

JD-20 1233 09+OON,03+80E

JD-21 1234 08+OON,04+OOE

KE-5 1235 31+90N,14+50W

EY-BH-10 1236 18+50N,30+OON

KE-6 1237 20+80S,05+OOW

SAMPLE DESCRIPTIONS

DESCRIPTION Au

6" wide sheared dacite (?), 2-33Spryite, quartz-carbonate stringers.

3" wide quartz-carbonate vein with2-3# pyrite, limonite staining.

1" quartz carbonate vein, trace-0.5%pyrite, limonite staining.

medium grained mafic volcanic withtrace-0.5% pyrite, quartz-carbonatestringers present, limonite staining.

1" quartz-carbonate vein in pillowedmafic flows, limonite staining.

2" quartz vein in pillowed mafic flowswith trace of sulphides.

1" - 6" quartz-carbonate vein, irregular,minor limonite staining in bandedgneissic mafic-intermediate flows.

ppb

5

10

10

^

5

rt

G

ll l l l l l l l l l l I l l l l l l

APPENDIX D

ROCK SAMPLE ASSAY CERTIFICATES

I //'" yyfocek lid..

/A, Oninrin. /Ait,*one'

f Mnp*n) l.ld.

W ll i i i i i i i i i i i i i i i

KIJ 8xsI6QI 744.2J2n

Geochemical Lab Report

REPORT: 017-3930 ( COflPLETE

CLIENT: GEOCftNEX L1HUED PROJECT: KOftAR

REFERENCE INFO:

SUBMITTED ir. J.D, WU PRINTED: 3-SEP-87

ORDER ELEHENTmm OF LOVERANALYSES DETECTION LlfllT EXTRACTION IIETHOD

1 ftij Silver 2 Au Gold

SARPLE TYPES NURBER

ROCK 18 '

1 0.1 18 5

SIZE FRACTIONS•268

m m

' ' : ' -'* '

HC1-HN03, (1 AQUA RE6IA

NURBERST^^Wft^

IB

:3) Atoiit Absorption FA-AA 1 10 ji Height

SARPLE PREPARATIONS NURIER

*BiiiP8F*^REHARKS: (: HEANS LESS THAN

REPORT COPIES TO: H. HODGER. HI66INSON

INVOICE TOt H, HODGE

1l/

111111I111111i111

S -bf tt 4 (unpin) Lid. ' **'' '0*

/Awl M., ifflmffl/

f Art* toT's'x'i Bmnir. ,fanc: UMtW 2220 WffiBI

REPORT! 017-3930

SAHPLE EIEHENTmm UNIIS

12201221 122212231224

12251226122712261229

123012311232 1233 1234

1235 12361237

. . , ...,..,, ...

.•ftjuM m .. ^PAV.... . . . ,''^^toifciifAih^^ neochemicfll/^//^M^jjMiiaiayfciiaiiiii^^ j Lab RCPOHIB^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^HNJ^^^^^^^^^^^^^^^^^^^^^^^^H

j | PROJECT: wm PAGE iAg Au

PPft PPB :

<5 ' - -(5 25

63015

" ioo "•- ---------- - •••-•---•- - . -...-.- — - -.....--..... . . . .10 .

. ^ '^\:^M^W^.^^l^---

l

50.4 5 .

10 '' '-;' -'^iti^J ' .' .- ' . to i-^f -^:iy^ ' , ; , ..-i.;. . ; ^ '--. .

5 ; , . . "' ----— — - --- - - <5 : . . ,,,-.:- . ,(5

V

.,.-..-...-^-, __ -r - -v-, r , r TT^

' -' ' ' -

li liGeochemical

Lab Report

" REPORT: o!7-3?G9('COMPLETE")""" """""""l r, V; ^fEFERENCi INFO:. . ...—.—,...... ,-.™..——.____...J i':':";.v', :.:.'-.;::_____..._.

( "CLIhNiV'^CCANEniMiiED"* ~~~~"———~—~-——;--:————, ;! ...;, ; . ,;v;?:; SUBfllTIEU DH U HllkST- PROJECT: KOMAR ' -^ ''^v'-vi^^y.,;:f JAiE'PJiiHiEP:.24-AUG-87

. ... _......,.....-..,-..-,.___.. m.........™..™,.__.____' :'..^:;. i :::. •.'.••: ^WM'.'^:'f** '^:*j,..'^ '.'.L'-'v ' •,.... - -.,-,-. ........,, .....,.......,™... ......--,......,,.. ^.^^^ LOWER •.,:;i,.,v,v:: v ^7" ~~

l ORDER ELEHENT ftNltt.YSES'-;'':.reiECII(|l|.4i||3f;^•i ' ; - : ' '' , -'- ^''' : ..''^|v|^^' -'' -' '••••^'''• : ^':-?'; i,' ' ' '

l ftu Gold ' 19 ' ' 5 PPB^'^'A'QUA Jii8!frr s : :v " ' FA-AA B 10 gm weight

I...... . .......-Sfihi'Lt TYPES"~ """""""}|UJiiiK~~". ™"SI2E'fRfiCIII)HS—^"Tl,,

l, . ....ROCK ': ^.l.itfK;:- W^?^^ -

M... ... ..pc^,i^c;!..^asi.p.42^ i^C,.J^.fiTurD HAIIIP6. tie t tin ' . : -'r .v ,.iJ ,*. :',;.v ^ r . . ,. . , ,i

™ """ SAMPLE 12i i "HAS""IW '' MEANS LESS THAN,

lREPORT COPIES TO! K. HODGE , V ' r'' WVOICE10: HvfjODGB

D iiTppTiipnii ^ " Jl: -"'"".' H r:"' r /"r r "T""~"™~"~r.'r~."r.

l

l

t^m^^^mt^^&^y^"''

l S/f li lixnptii) Ud.

Kil , (, Onlano,

l KIJ 8X5

lelev 033 J2J

Geochemical Lab Report

l l l l l l l

. jtm. ~

l l

l

l

l

l l

l l

———'PftQE lIZ1

SAWIEXLnfcEIi

1203

1205

1206 12:7 120B

1210

12111212121312141215

"ELEKEiil"

UNITS PPP

105

10

!0i 105

10925

1220" 9095

,: 10;: ; '3

259

70•;s5x'5

' ;: : ^:i^TfTTTT'l\*Xjfff\F'{':3!-"\':

^^^.V^wy^*v;,.'--v,;

l.Adv-Ora A Comprnj Li*.

5420 Cu

CiniilaPhone: (61 J) 149-1220Telci: 053-3233

Certincate of Analysis

\m

j j •i'l 1

l

l

REPORT: 417-3769 ( COHPIETE )

M

REFERENCE INFO: .

CLIENT: 6EOCANEX L1HITED PROJECT: KOHftR

SUBMITTED BY: R. HIGG1SON DATE PRINTED: U-KEP-87

ORDFR ELFHEN!

l ftu Gold -Assay

HUHBER OF LOUERWftLVSCS OEtECIION Llflll EXTRACTION

l 0.001 OPT

rirtfir-II IVCff;

OIK

NUHOER

1

SI7F f RUCTIONS

'1'ilV l Ml

^, . . . . ,... . .., , ; . . ; ; ,.

NUH9CR fiftHllf PRIffiRAHON^

1 I'lj; V|iv!,! i*Ji

V™*r.r^-*.

trrmt tR. IllGGINSON

i

l

-OrttACompuiyLld.J420 Cinottk M.,

Onllii KU

(413)149)110

Certificate of Analysis

l l l l

i l

RFPOK1: 417-3/69

NUDl.ll K

i;'i!i

FSoJECTi KOMAR PAGE l

AuUN! ir; od

i'adi^a^MlaMl^siia^aliiiiM:^^:,::,

,; viI|'; -i^llillSS*; 5:^-0::/- •'•.."^V.'O'V ^•Y^M^S^j^^W.v.-y ; .-.-- - ^•^-.••y: : --' ".


APPENDIX E

DIAMOND DRILL LOGS

DIAMOND DRILL RECORDHOLE NO. EL-87- l SHEET NO. ' " '_

NAME OF PROPERTY EYE LAKE

HOLE NC

LOG ATIO

LATITUD

ELE VATI

STARTED

i. EL-R7-1 LENGTH 297N 00+505, 02+15E

FOOTAGE DIP AZIMUTH

.0' ———— ——0.0 45 0

29/.0 10"

3N A7IMUTH 090" DIP -45" ———————— —————— —— —————

Nov. 27/87 F.NisnFn Nov. 28/87 ———— ——— ———— -

FOOTAGE DIP AZIMUTH

REMARK S PA786856

f.

LOGGE

PA786855

UMMARY LOG

R HigginsonD BY

FOOTAGE

FROM

0.0

10.0

57.8

98.0

171.7

194.3

195.5

224.8

266.2

271.0

TO

10.0

57.8

98.0

171.7

194.3

195.5

224.8

266.2

271.0

297.0

297.0

DESCRIPTION

SUMMARY LOG

CASING

MAFIC FLOWS

SILICIFIED - SHEARED INTERMEDIATE TUFF

MAFIC FLOWS AND TUFFS, 80:20

SILICIFIED - SHEARED INTERMEDIATE TUFF

MAFIC FLOWS

FELSIC TO INTERMEDIATE TUFF

- 195.5' to 200.5' - well-banded tuff containing quartz-car bonate stringers, pyrrhotite ft pyrite as fracture infillings.

MAFIC TO INTERMEDIATE VOLCANICS, tuffs - flows, 40:60.

FELSIC TO INTERMEDIATE TUFF

MAFIC TO INTERMEDIATE VOLCANICS, as above.

E.O.H.

ONTARIO GEOLOGICAL SURVEY ' ASSESSMENT FILES

OFFICE

APR 2 2 1988

RECEIVED

SAM

NO.

12041

SI^PSH

3-5

P L E

FOOTAGEFROM

195.5

TO

200. 5

TOTAL

5.0

ASSAYS

OZ/TON

.010

OZ/TON

DIAMOND DRILL RECORDNAM E OF

HOLE NO.

LOC AT ION

LATITUDE

ELEVATION

STARTED

PROPERTYEL-87-1

JQ15QS.

Nov.

OP+15F

27/87

EYE LAKEL E N G T H

DEPARTURE

AZIMUTH

FINISH Fn

297

090 0

Nov.

.0'

-45 0

28/87

FOOTAGE

0.0

297.0

DIP

45 040 0

AZIMUTH FOOTAGE DIP A7IMUTHHOLE NO. EL -87- 1 SHEET NO.

REMARK s PA786856^^Pa786855

LOGGED BYR. Higginson

FOOTAGE

FROM

0.0

10.0

57.8

TO

10.0

57.8

98.0

DESCRIPTION

Casing.

Mafic Flows - dark green to black, medium grained, massive.Modal percent: Amphibole 45-5036

Plagioclase 40-4536Chlorite 3-5*Quartz 1-256Carbonate 1-256Pyrite tr-0.5*

Amphibolitic to oohit.ic texture, disseminated pyrite as fracturecoatings, 1-256 quartz-carbonate stringers, foliation at 36 0 tocore axis at 21.0', 50" at 37.0', 38" at 50.0'. Fracturing at 27 0to core axis at 12.0', 35 0 at 47.0'.

Silicified - Sheared Intermediate Tuff - light to dark grey, finegrained, banded.

Modal percent: Quartz 35-4056 Plagioclase -, 2Q -^ Sericite J ^ "*Chlorite 10-15*Amphibole 5-10*Pyrrhotite -i , r*Pyrite J J ~ S*Carbonate 2-3* Garnet tr-2*

Common sericite pseudomorphs after plagioclase, disseminated,allotriomorphic, pink, garnet porphyroblasts in some sections,2-3X carbonate as bands, pyrrhotite and pyrite as bands, stringersand blebs, minor parasitic-kink folds.

- 57.8' to 58. l 1 - quartz-carbonate, clean banded vein.

SAMPLE

NO.

12001

1 200?

Ol

1 2003

SULPH IDES

tr

tr

JTARK ASS

J

RE

tr

FOOTAGEFROM

10.0

52.8

) G6OLO ESSME

OFFI

iPR2l

CE!

TO

15.0

57.8

SIGAL S NT FIL CF.

i miVE

57.8 62.8

TOTAL

5.0

5.0

URVEY EfS

D

5.0

ASSAYS

/4IXfi?(S/j

\X

^^?v~(TjTT

n-f/yjLy^"-,vs^^^

ozAUON

.002

tr

PJpDGi^ —

oF o^ vnfffc^Hfit^

tr

07/TON

X' \j]'J

y

DIAMOND DRILL RECORD NAME OF

HOLE NO

. EYE LAKE

".MM T NO

FOO T AC- F

f ROM

57.8

98.0

TO

98.0

171.2

DESCRIPTION

Cont'd.- 58. T to 59.1' - friable with garnets.- 59.1' to 61.0' - irregular coarse grained quartz vein, 2-3*

coarse grained pyrite blebs.- 61.0' to 62.8' - 2-3* disseminated garnets, 3-5* pyrite

bands.- 62.8' to 74.3' - well banded, 1-2* pyrite as fine grained

wispy blebs, 2-3* quartz-carbonate veiningwith 2-3* coarse grained pyrite blebs,1-2* muscovite-biotite coronas aroundfeldspar (microcline?) grains.

- 74.3' to 80.7' - dark grey, finely banded, 2-3* pyrrhotite,pyrite blebs, bands and stringers, crenu-lated, kink folded.

- 80.7' to 98.0' - finely banded, 5-7* carbonate parasiticfolds with 2-3* quartz-carbonate veins upto 0.4 feet wide (possibly axial planar),2-3* pyrite as fracture coatings, zones of1-2* wispy pyrite blebs, 1-2* dissemin ated garnets.

Fracturing at 40 0 to core axis at 68.0', foliation at 64 0 -67 0 tocore axis.

Mafic Flows and Tuffs - 80:20. Flows typical, tuffs banded with2-3* quartz-carbonate-epidote stringers and 3-10* biotite as bandsand disseminated grains foliation at 61 0 to core axis at 116.0,58 0 at 126.5', banding at 64" to core axis at 154.5', 67" at141.0', fracturing at 50 0 to core axis at 155.0'.

- 98.0' to 121.8' - flows, 2-3* quartz-carbonate veins up to0.3 feet wide, trace pyrite in veins.

- 121.8' to 124.1' - crudely banded tuff, biotite - 1-2*tourmaline blebs, 2-3* quartz-carbonatestringers.

- 124.1' to 132.1' - tuff, 1-2* quartz-carbonate stringerswith trace pyrite.

- 132. T to 142.3' - flows, 2-3* quartz-carbonate stringers.

SAMPLE

' IO

120041200512006

1200712008

1200912010120111201212013

120141201512016120171201812019

1202012021120221202312024

•'.1)1 CM

lur 5

1-21-21-2

2-32-3

3-53-53-53-53-5

trtrtrtrtrtr

trtr

FOOT AGt

FROM

62.867.872.8

74.377.3

80.782.787.092.095.3

98.0102.0107.0112.0117.0121.8

124.1129.1132.1137 .1140.1

ro

67.872.874.3

77.380.7

82.787.092.095.398.0

102.0107.0112.0117.0121.8124.1

129.1132.1137.1140.1142.3

*0 Ml

5.05.01.5

3.03.4

2.04.35.03.32.7

4.05.05.05.04.82.3

5.03.05.03.02.2

A'.r.AY'j

- "l.

tr.002.002

.006tr

trtrtrtrtr

trtr.008tr

.006

.006

trtrtrtr

.008

DIAMOND DRILL RECORD NAMl Df

HOLE: NO

EYE EAKEEL-87-1 3 of 4

FOOT AGf

F ROM

98.0

171.?

194.3

195.5

TO

171.2

194.3

195.5

224.8

DE- SCRIPT ION

Cont'd.- 142.3' - 146.3' - tuff, 1-2* quartz-carbonate stringers.- 146.3' - 171.2' - flows with 2-3* quartz-carbonate-epidote

interflow and stringers, massive, traceto 1* disseminated pyrite blebs, limonitestaining.

Silicified - Sheared Intermediate Tuff - typical, foliation at 60"to core axis at 177.0', 61" at 192.0'.

- 171.2' - 177.2' - laminated to finely banded, 2-3* wispypyrrhotite, pyrite blebs, 2-3* dissemin ated fine to medium grained garnets, 1-2*quartz-carbonate stringers.

- 177.2' - 185.5' - 3-5* quartz-carbonate stringers and bandstrace-3* wispy pyrite blebs, finely lami nated with 3-5* pyrrhotite near bottom ofsection.

- 185.5' - 187.0' - coarsely banded, trace-0.5* pyrrhotiteand pyrite, 1-2* quartz-carbonate strin gers.

- 187.0' - 189.2' - crudely banded, folded, crenulated, 2-3*pyrite, 1-2* pyrrhotite.

- 189.2' - 194.3' - crudely banded, trace-0.5* pyrrhotite andpyrite.

Mafic Flows - atypical, 15-20* chlorite, fracturing at 52 0 to coreaxis at 195.0'.

Felsic to Intermediate Tuff - dark grey, fine grained, banded.Modal percent: Quartz 40-45*

Plagioclase 15-20*Chlorite 10-15*Sericite -i g ^QVMuscoviteCarbonate 3-5*Pyrrhotite i T rvPyrite J *

SAMPLF

•K,

1202512026T2027I202S120291203012031

1203212033

1203412035

12036

12037

1203812039

12040

12041120421204312044

IPFS

tr-1tr-1tr-1tr-1tr-1tr-1

2-32-3

tr-3tr-3

tr

3-5

trtr

tr

3-53-53-53-5

F O O T A G F

fBQM

142.3146.3149.5152.0157.0162.0167.0

171.2174.2

177.2182.0

185.5

187.0

189.2191.8

194.3

195.5200.5204.0207.0

rn

146.3149.5152.0157.0162.0167.0171.2

174.2177.2

182.0185.5

187.0

189.2

191.8194.3

195.5

200.5204.0207.0210.9

T'lFAI

4.03.22.55.05.05.04.2

3.03.0

4.83.5

1.5

2.2

2.62.5

1.2

5.03.53.03.9

A ', fl, A Y S

AM,,.

.002trtrtrtrtrtr

trtr

trtr

tr

tr

trtr

tr

.010trtrtr

DIAMOND DRILL RECORD NAMI: or pKOPF.fi'i'v E lE LAKE

HOLb NO ...E L -87-1 mi i no 4 Of 4

FOOT AC.F-

I ROM

195.5

224.8

266.2

271.0

TO

224.8

266.2

271.0

297.0

297.0

ntSCRIPTION

Cont 'd.Minor parasitic folding, S-5% quartz-carbonate stringers, pyrrho tite and pyrite as very fine grained blebs and stringers, bandingat 47" to core axis at 211.0'.

- 210.9' - 215.3' - 3-5X carbonate and quartz-carbonatestringers and veins up to 0.5 feet wide.

Mafic to Intermediate Volcanics - 60:40 - flows: tuff, light greyto green, fine to medium grained, banded to massive.

Modal percent: Amohibole -i Ar. Ac- vs* i i . , HVJ — *T 0 rt)Chlorite JPlagioclase 35-37%Quartz 3-5JSBiotite 2-55SCarbonate 1-355Pyrite tr-0.5%

T-3% carbonate and quartz-carbonate stringers, wispy biotite bandsminor kink folding, banding at 48" to core axis at 237.0', 78 0at 262.0'.

- 257.3' - 258.3' - light grey, sericite (5-10X), poorlydeveloped schistosity.

Felsic to Intermediate Tuff - typical mottled to coarsely banded,light grey.

Mafic to Intermediate Volcanic - as above, banding at 48 0 to coreaxis at 277.0', 68" at 297.0', fracturing at 55 0 to core axis at275.0'.

- 287.3' - 290.6' - kink folded, 2-3X quartz-carbonatestringers at fold hinge, with coarsegrained amphibole prisms as inclusions.

E.O.H.

SAMPLE

•M,

120451204612047

12048

12049

12050

12051

12052

!l*f 5

3-53-53-5

tr

FOOT AGfc

f ROM

210.9215.3220.3

224.8

257.3

266.2

287.3

294.0

TO

215.3220.3224.8

227,8

258.3

271.0

290.6

297.0

r.ctM

4.45.04.5

3.0

1.0

4.8

3.3

3.0

A V, AY S

.A v,,.

trtrtr

tr

tr

tr

tr

tr

j : T 14

DIAMOND DRILL RECORDNAME OF PROPERTY

HOLE NO. EL-87-2

EYE LAKELENGTH 317.0'

LOCATION 00+50S. BLO__.—^—--——LATITUDE ___________________ DEPARTURE

ELEVAT ION

STARTED — Nov. 28/87AZIMUTH

FINISHED ,

090 0 -46"

Nov. 30/87

FOOTAGE

0.0

307.0

DIP

-46"-43 0

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-2 SHEET N0.

REMARKSPA786856______

SUMMARY LOG

LOGGED BY R. Hjgginson

r o o T A G E

FROM

0.0

14.0

228.5

250.0

TO

14.0

228.5

250.0

317.0

317.0

D E S C R 1 P T 1 ON

SUMMARY LOG

CASING

INTERMEDIATE FLOWS- 105.0' - 110.0' - randomly distributed quartz-carbonate

stringers; chloritic fractures. Tracesulphides as fracture infillings.

FELSIC TUFFMAFIC TO INTERMEDIATE FLOWSE.O.H.

ONTARIO GEOLOGICAL SURVEY' ASSESSMENT FILES

OFFICE

APR 2 2 1988

RECEIVED

SAMPLE

NO.

12073

sAfeg" FOOTAGEFROM

105.0

TO

110.0

TOTAL

5.0

ASSAYS

-,; OZ^VON

.020

OZ/TON

DIAMOND DRILL RECORDNAME OF PROPERTY EYE LAKE

LOCATION

LATITUDE

ELEVATION

STARTED

EL-87-200+50S, BLO

Nov. 28/87

1- ENGTH

AZIMUTH

FINI^HFn

317.0'

090 0 DIP -46 0Nov. 30/87

FOOTAGE

0.0

307.0

DIP

-46 0-43 0

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-? SHEET NO. ' Of 3

REMARKS PA786856


FOOTAGE

FROM

0.0

14.0

TO

14.0

228.5

DESCRIPTION

Casino,.

Intermediate Flows - light grey to green, fine to medium grained,massive to poorly banded.

Modal percent: Plagioclase 35-405! Amphibole 30-355! Quartz 10-155!Biotite 5-105!Carbonate 1-25!Pyrite trace

1-25! quartz-carbonate stringers, wispy biotite bands in some sec tions few widely spaced fractures with carbonate-limonite coatingsfoliation at 41" to core axis at 32.0', 50" at 63.0', 50" at 137.057 0 at 166.0', 66 0 at 205.8', 50 0 at 228.5'.

- 14.0' - 27.6' - fine to medium grained, medium grainedamphibole prisms in fine grained groundmass.

- 26.2' - 27.6' - medium grained, felted bio-tite-amphibole, carbonate stringers with1-25! vuggy pyrite.

- 27.6' - 43.1' - fine grained, massive.- 43.1' - 55.0' - 2-35! quartz-carbonate stringers, medium

grained biotite rich bands.

- 55.0' - 121.8' - fine grained, 2-35!, irregular quartz-car bonate stringers, chloritic fractures,1-25! pyrite as fracture coatings, trace-15!pyrrhotite as fine disseminated grains.

SAMPLE

NO.

i

120531205412055

120561205712058120591206012061I20621 2063120641206512066

SJ&SM-

*NTAFAS

trtr

1-2

1-3

FOOTAGEFROM

iOOEOLSESSM

OFf

APR 2

ECE

14.019.024.0

27.632.637.640.643.147.052.055.060.065.070.0

TO

XJICALENT FI ICE

2 198

1 VE

19.024.027.6

32.637.640.643.147.052.055.060.065.070.075.0

TOTAL

ASSAYS

/#

SURVEY!^*/pq l 'J \\ r; i/ l" tL (siB IWj V0r^ l ^D 1——— 1

5.05.03.6

5.05.03.02.53.95.03.05.05.05.05.0

•;.

^"

lm' r

s.'/f, ^^•'ctic

07/TON

^x^0J/ '

IGI.,*

^/' f"-'o^/'' -s-^'

trtrtr

trtrtrtrtrtrtrtrtrtrtr

OZ/TON

S'o\

ri 1

f

73

DIAMOND DRILL RECORD NAMf OF PI.-OPF. HI ' EYE LAKE

of 3

F GO f AGT

FROM

14.0

T fi

228.5 Cont'd.

DESCRIPTION

?1.8' - 126.2' - medium grained amphibole, fine grainedbiotite bands.

?6.2' - 151.5' - fine to medium grained, 2-35S irregularquartz-carbonate stringers, minor kinkfolding.

31.5' - 164.8' - crudely banded to mottled, medium grainedamphibol itic. T-2% pyrite as fracturecoatings. Z-5% carbonate.

54.8' - 180.2' - fine grained, massive, 2-33S fine quartz-carbonate stringers, minor discontinuitieswith changes in orientation of stringersand foliation, T-2% disseminated-roundedpyrite blebs.

- 166.0' - 167.0' - *\-21l, tourmaline asaggregates of grains with pyrite matrix.

- 176.0'- 180.2' - 2-3SS pyrite as stringersblebs and disseminated grains.

30.2' - 186.9' - altered tuff?, 10-15* fine grained seri cite and biotite, 2-3* quartz-carbonatestringers with 1-3* pyrite grains.

36.9' - 205.8' - fine grained, 2-3* quartz-carbonatestringers.

- 200.0'- 205.8' - 1-2* disseminated pyriteblebs along fractures or contacts ofquartz-carbonate stringers.

35. 8' - 210.5' - massive, fine grained, dark grey, 1-2*pyrite along fractures.

10.5' - 228.5' - crudely banded to mottled, 2-55! quartz-carbonate stringers, 1-2* disseminatedpyrite blebs.

SAMPL F

;.,

I2067I20681 2069I207012071I2072I2073I20741 207 5I2076I2077I2078I20791 2030120811 20821 20831 20841 20851 2086I20871 20881 20891 2090120911 20921 20931 20941 20951 2096I2097

1 2098209921002101

•••H PH

IDFS

1-21-21-21-21-21-22-31-31-3

1-21-21-2

1-21-21-21-2

FOOTAGt

FROM

75.080.085.090.095.0100.0.105.0110.0115.0119.0121.8126.2130.0135.0140.0145.0149.0151.5156.0161.0164.8167.8172.8176.0180.2183.2186.9191.9196.9201.9205.8

210.5215.5220.5224.5

TO

80.085.090.095.0100.0105.0110.0115.0119.0121.8126.2130.0135.0140.0145.0149.0151.5156.0161.0164.8167.8172.8176.0180.2183.2186.9191.9196.9201.9205.8210.5

215.5220.5224.5228.5

T 'j7Al

5.05.05.05.05.05.05.05.04.02.84.43.85.05.05.04.02.54.55.03.83.05.03.24.23.03.95.05.05.03.94.7

5.05.04.04.0

A S A Y *o

.AU

trtrtr

.002trtr.020trtr.trtrtrtr

.002trtrtr.002trtrtrtrtrtrtrtrtrtrtrtrtr

trtrtrt r

, , ,,

DIAMOND DRILL RECORD N AMI OF P*' O F-' F- f? T V .

nni r MO t L -o f -t

EYE LAKE

r,MI i T MO 3 Of J

F DOT Ac;r

228.5

250.0

250.0

317.0

317.0

DFSCRIPT ION

Felsic Tuff - light grey, fine to medium grained, foliated tobanded.

Modal percent: Quartz -i re enyr* , . -j J D 3 ~" DU/bPlagioclase Sericite 10-15*Microcline S-10%Muscovite 5-7*Carbonate 2-5*Pyrite 1-3*

Highly fractured, minor brecciation, 2-5* quartz-carbonate frac ture fillings and stringers with disseminated pyrite blebs and grains, abundant plagioclase lapilli, waxy sericitic coatings on fractures and foliation planes, foliation at 50 0 to core axis at 239.0'; 47 0 at 248.0'.

Mafic to Intermediate Flows - dark green to grey, fine to mediumgrain"'!, massive to foliated.

Modal percent: Amphibole 40-45* Plagioclase 35-40* Sericite 3-5*Chlorite 3-5*Quartz 2-3* Carbonate 2-3*Pyrite 1-2*

Amphibolitic to schistose(sericite-chlorite sections), 2-3* quartz- carbonate stringers, few widely spaced fractures, disseminated pyrite blebs, foliation at 55 C to core axis at 276.0' and 291.0'; 50" at 316.0'.

- 250.0' - 255.6' - 2-3* quartz-carbonate stringers.

- 279.3' - 283.0' - tuff, 3-5* biotite bands, 2-3* quartz- carbonate bands.

E.O.H.

SAMPL.E

•10

12102 1210;12104 1210P 1210E

121071210f

121091211C12111

-•-ut CH

mf s

1-3 1-31-3 1-3 1-3

f OOTAGtf ROM

228.5 233.5238.5 243.5 247.0

250.0.252.8

255.6279.3312.0

m

233.5 238.5243.5 247.0 250.0

252.8255.6

260.6283.0317.0

Tlj TAl

5.0 5.05.0 3.5 3.0

2.82.8

5.03.75.0

— ---A *, 3 A Y ',

7^

.002 trtrtr tr

t rtr

trtrtr

, r.

DIAMOND DRILL RECORDHOLE NO. EL-87-3 SHEET NO. ' 0 ^ \


HOLE NC

L OCA T 10

L ATITUD

EL E VAT 1

STARTED

) EL-87-3 LENGTH 397N 11+OON, 06+35E

0'

3 N A7 ,MUTH 090 0 n .o -44. 5 0Nov. 30/87 FINISHED Dec

FOOTAGE

FROM

0.0

44.0

60.2

60.7

70.2

98.8

101.5

129.2

230.1

236.5

273.9

324.5

TO

44.0

60.2

60.7

70.2

98.8

101.5

129.2

230.1

236.5

273.9

324.5

397.0

397.0

D E

2/87

S C R 1 P T 1 O N

SUMMARY LOG

FOOTAGE

0.0200.0397.0

DIP

-44.5-43.0-41.0

CASING

FELSIC TO INTERMEDIATE VOLCANICS

MAFIC INTRUSIVE DYKE


SILTSTONE


MAFIC TO INTERMEDIATE FLOUS

MAFIC TO INTERMEDIATE VOLCANICS AND SILTSTONE, 45:55

INTERMEDIATE FLOWS

INTERMEDIATE TUFF

INTERMEDIATE FLOWS- 370.5' - 373.7' - well banded tuff, abundant quartz-carbon

ate eyes.

INTERMEDIATE TUFF

E.G. H.


OFFICE

APR 2 2 1988

RECEIVED

AZIMUTH "DOTAGE

SAM

NO.

12195

S,^PSH

DIP

RLE

AZIMUTH

REMARKS PA850854

SUW

LOGGE

FOOTAGEFROM

370.5

TO

373 7

TOTAL

3.2

1ARY LOG

R. Higginson3 BY

ASSAYS

X

Ven ^

,***— " ,**L:

'/P

^^'*CE ci""•-^

oz/HoN

:;0-^"yp,yo**/***^

.026

O 7 /T ON

1X

.J^

DIAMOND DRILL RECORDNAME OF PROPERTY EYE

HOL E NO. -

LOCATION

LATITUDE

ELEVATION

STARTED

EL-87-31HOON, 06+35E

Nov. 30/87

LAKELENGTH

DEPARTUR E

AZ IMUTH

FIN ISHFn

397.0'

090 0 DIP -44. 5 0Dec. 2/87

FOOTAGE

0.0

200.0

397.0

DIP

-44.5-43.0-41.0

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO.

EL-87-3SHEET NO. L-.-,.l Of 5

R EM ARKS PA850854

LOGGED BY.R. Higginson

FOOTAGE

FROM

0.0

44.0

60.2

TO

44.0

60.2

60.7

DESCRIPTION

Casing,

Felsic to Intermediate Volcanic - light to dark grey, fine grainedmassive to banded.

Modal percent: Quartz j 70-75* PlagioclaseAmphibole 10-15*Biotite 3-5*Chlorite 2-3*Pyrite tr-3*Carbonate tr-1

Variable textures from fine grained massive to weakly banded,foliation at 60" to core axis at 45,5' and 60.0' fracturing at48 0 to core axis at 60.0' .

- 44.0' - 52.0' - 2-3* disseminated pyrite.- 51.2' - 52.0' - quartz vein with felsic

inclusions, 1-2* pyrite along contacts.- 52.0' - 56.8' - cherty, massive trace pyrite, epidote in

filling of minor fractures.- 56.8' - 60.2' - light greenish-grey, massive 20-25* quartz

veining, trace disseminated pink garnets.0.5-1* chalcopyrite blebs, trace-0.5*pyrite, 10-15* potash feldspar in maficinclusions, angular mafic inclusions - xeno-liths in host - possibly agglomeratic.

Mafic Intrusive Dyke - light green, fine to medium grained, por-pyritic.

Modal percent: Amphibole 65-70*Biotite 15-20*Plagioclase 5-10*

SAMPLE

NO. SULPH IDES

ONT/A

j1i F———

1211212113

12114

12115

121 1 6

2-32-3

tr

0.5-1

FOOTAGEFROM

RIO QECSSESS

O

APR

EC

44.048.0

52.0

56.8

60.2

TO TOTAL

cumupLOOICAr ^-...^ /ENT FILES TICF.

2 2 N88

E i V|E D

48.052.0

56.8

60.2

60.7

.

4.04.0

4.8

3.4

0.5

ASSAYS

OZ/TON

trtr

tr

tr

t r

OZ/TON

DIAMOND DRILL RECORD MAM! OF PCOCF-fM V

EL-87-3

EYE LAKE

HOt-E NO NO 2 Of 5

FOOT AGF

F ROM

60.2

60.7

70.2

98.8

101.5

1 O

60.7

70.2

98.8

101.5

129.2

DESCRIPTION

Cont'd.Medium grained biotite flakes in fine grained amphibole-plagio-clase groundmass, contacts at 80" to core axis.

Felsic to Intermediate Volcanic - as above gradational lower con tact with sediments.

Siltstone - dark green to brownish grey, fine grained, massive tobanded.

Modal percent: Quartz ] 4CM5XPlagioclaseBiotite 20-25*Chlorite ID-15%Carbonate 5-10*Amphibole 3-5*Pyrite tr-0.5*

Massive on top and bottom of section, increasingly well bandedtoward middle, minor kink folding, 1-2* quartz-carbonate stringers,banding at 49 0 to core axis at 92.0', 70 0 at 97.4', conjugatefractures at 40/500 to core axis.

- 87.3' - 87.8' - quartz vein, clean.- 97.4' - 98.3' - quartz veining, 2 generations, trace tour-

maline on contacts of second set of veinscross-cutting first set, clean.

Felsic to Intermediate Volcanic - as above 1-2* quartz-carbonatestringers near lower contact with 1-25! pyrite and 1-2* epidotebands, foliation at 55 0 to core axis at 101.0'.

Mafic to Intermediate Flows - dark green, fine grained, massive.Modal percent: Amphibole 45-50*

Plagioclase 40-45*Chlorite 3-5*Quartz 0.5-1*Carbonate tr-1*Pyrite trace

Massive, few widely spaced chloritic fractures, minor disseminated

SAMPLE

•m

121171211f

1211?121 2(12121

121251212-12124

1212E

1212612125121261212?1213C12131

Mil fit

.Df S

tr-3tr-3

tr-.5tr-.5tr-.5

tr-.5tr-.5tr-.5

1-2

trtrtrtrtrtr

FOCTAGt

FROM

60.765.7

70.275.280.2

85.290.295.2

98.8

101.5106.5111.5116.5121.5126.5

TO

65.770.2

75.280.285.2

90.295.298.8

101.5

106.5111.5116.5121.5126.5129.2

T' ( TAI

5.04.5

5.05.05.0

5.05.03.6

2.7

5.05.05.05.05.02.7

———— lA r, j AYS~~Au

•UN

trtr

trtrtr

trtrtr

tr

trtrtrtrtrtr

DIAMOND DRILL RICORD ,of.rmv. EYE LAKE

EL-87-3 3 of 5

F QQT Ae-f

FROM

101.5

129.2

TO

129.2

230.1

DF SCRIPT ION

Coni 'd.quartz blebs and pyrite grains, irregular fractures at 21" to coreaxis.

Mafic to Intermediate Volcanics and Siltstone - 45:55.- 129.2' - 134.8' - siltstone, atypical, 25-30* carbonate,

35-40* biotite, fractures at 30 0 and 60 0to core axis.

- 134.8' - 136.3' - intermixed tuff and siltstone gradationalzone.

- 136.3' - 139.3' - silicified tuff, massive light grey toto banded grey-green, amphibolitic tocherty, 1-2* carbonate stringers, folatiorat 61 C to core axis at 137.0'.

- 139.3' - 152.8' - tuff and flows, 20:80, 3-5* quartz-carbon ate veining, trace-1* disseminated tour maline, trace pyrite, banding at 50-56 0to core axis.

- 152.8' - 168.4' - siltsone and tuff, 90:10, amphibole bandswith carbonate stringers as cores, bandimat 52 0 to core axis, at 154.0'.

- 168.4' - 179.6' - tuff, 5-10* carbonate stringers, minorkink folding, dislocations at 25" to coreaxis, 0.8 feet apart, 1/4 inch displace ment, fracturing at 47" to core axis at169.0', foliation at 60 0 to core axis at172.0'.

- 179.6' - 189.6' - flows, typical, foliated at 52" to coreaxis.

- 181.5'-184.5' - 3-5* quartz-carbonatestringers with trace tourmaline blebs.

- 189.6' - 200.1' - siltstone, finely banded, 5-10* carbonate,crenulated kink folded.

SAMPLE

-,o

121321213:

1213'

1213!

1213f121371213?1213?1214C12141121421214:1214'1214J1214(

1214/1214?

121491215012151

mf S

trtrtrtr

FOOT AGEFROM

129.2132.2

134.8

136.3

139.3144.3147.3150.3152.8153.8158.8163.8168.4172.4177.4

179.6184.6

189.6194.6197.6

TO

132.2134.8

136.3

139.3

144.3147.3150.3152.8153.8158.8163.8168.4172.4177.4179.6

184.6189.6

194.6197.6200.1

P'.TAI

3.02.6

1.5

3.0

5.03.03.02.51.05.05.04.64.05.02.2

5.05.0

5.03.02.5

ASSAY *j

.-w.

trtr

tr

tr

trtrtrtrtrtrtrtrtrtrtr

tr.002

tr.002tr

IP.' T; (i

DIAMOND DRILL RECORD NAMI: or PROPERTY ..

not.E NO -J-L-87-3

EYC LAKF.4 of 5

TOO T A Li E

F ROM

129.2

230.1

236.5

273.9

T o

230.1

236.5

273.9

324.5

DESCRIPTION

Cont'd.- 200.1' - 205.5' - tuff, medium grained, amphibolitic, crude-

banded, sericitic alteration of plagio clase.

- 205.5' - 220.2' - mixed sediments and tuff, banding at 45 0to core axis at 206.0' .

- 220.2' - 224.2' - tuff, minor dislocation or disconformi ties2-3% quartz-carbonate stringers.

- 224.2' - 226.0' - intermixed sediments and tuff.- 226.0' - 230.1' - siltstone, folded, 10-2056 carbonate,

3-556 quartz-carbonate stringers, tracelimonite staining.

Intermediate Flows - 2-356 quartz-carbonate stringers, banding at57 0 to core axis at 235.5'.

Intermediate Tuff - atypical, sericitic with potassic alterationalong contacts of quartz-carbonate stringers (3-556), 20-2556 car bonate, banding at 45" to core axis at 245.0', 30 0 at 269.0',fractures at 40 0 to core axis at 282.0'.

- 251.9' - 253.3' - massive, no stringers.- 253.3' - 273.9' - 1-356 rounded pyrite blebs, minor discon

tinuities from faulting or erosion?

Intermediate Flows - foliation at 53" to core axis at 274.5'.

- 273.9' - 284.6' - massive, foliated, tr-256 pyrite as wispyblebs in 1-356 fine quartz-carbonatestringers.

- 284.6' - 285.8' - chloritic, schistose, 2-356 pyrite blebs.- 285.8' - 290.4' - massive, as above- 290.4' - 301.2' - massive, light grey, ampibole and chlorite

wisps, foliated at 70 0 to core axis,trace-356 pyrite blebs.

SAMPLE

' IO

12152

12153121541215512156

1215712158

1215912160

121611216212163

1216412165121661216712168

12169121701217112172

1217321741217E1217612177

sill fn

KiFS

1-31-31-31-3

1-3tr-2tr-2tr-2

2-3

tr-3tr-3tr-3

FOOTAGEFROM

200.1

205.5210.5215.5220.2

224.2226.0

230.1233.1

236.5241.5246.5

251.9253.3258.3263.3268.3

271.3273.9278.9281.9

284.6285.8290.4294.3297.8

10

205.5

210.5215.5220.2224.2

226.0230.1

233.1236.5

241.5246.5251.9

253.3258.3263.3268.3271.3

273.9278.9281.9284.6

285.8290.4294.3297.8301.2

TOTAL

5.4

5.05.04.74.0

1.84.1

3.03.4

5.05.05.4

2.45.05.05.03.0

2.65.03.02.7

1.24.63.93.53.4

ASSAYS

"1\1T

tr

trtrtrtr

trtr

trtr

trtrtr

trtrtrtrtr

trtrtrtr

trtrtrtrtr

DIAMOND DRILL RECORD NAMt or PPOPERT Y..,. EYE LAKE noi.t NO . EL-87-3 H, l r NO 5 Of

FOOT A Li F.

F ROM

273.9

324.5

T l)

324.5

397.0

397.0

Ot OCRIPTION

Coni' d.- 301.2' - 324.5' - foliated - schistose, S-7% quartz-carbon-

ate-epidote stringers, crenulation andkink folding, S-5% biotite bands, 0. 5-156pyrite grains.

Intermediate Tuff - typical, banded, abundant quartz-carbonate eyesand s'tringers banding at 40-68" to core axis (average 58").

- 353.8' - 355.2' - flow, massive, typical.- 358.8' - 359.7' - as above.- 361.7' - 362.7' - as above.- 363.5' - 364.2' - as above.- 367.0' - 373.7' - greyish-green, foliated, Z-3% quartz-car

bonate stringers.

E.O.H.

SAMPLE

.10

1217812179J2180121811218212183

121841218512166121871218812189121901219112192121931219412195121961219712198121991 2200

IDFS

.5-1

.5-1

.5-1

.5-1

.5-1

.5-1

FOOTAGLF BOM

301.2304 . 2307.5312.5317.5322.5

324.5327.0332.0337.0342.0347.0352.0355.5360.5363.5367.0370.5373.7377.0382.0387.0392.0

JO

304.230 7 .531?. 5317.5322.5324.5

327.0332.0337.0342.0347.0352.0355.5360.5363.5367.0370.5373.7377.0382.0387.0392.0397.0

F uT At

3.03.35.05.05.02.0

2.55.05.05.05.05.03.55.03.03.53.53.23.35.05.05.05.0

A 'j 'j A Y 'j

AU

trtrtrtrtrtr

trtrtrtrtrtrtrtrtrtrtr.026trtr.002trtr

,: T..V

DIAMOND DRILL RECORDEL-87-4 SHEE1 N0 . of ?


HOLE NC

LOC AT IO

LATITUD

ELEVATI

STARTED

v EL-87-4 LENGTH 477.0'N 11+OON. 03+20E

3N AZIMUTH 090 0 n,P 47 0Dec. 2/87 F.N.SHFO Dec . 5/87

FOOTAGE

FROM

0.0

14.0

60.0

91.0

151.6

155.0

156.1

177.9

183.0

255.6

263.2

277.3

281.5

293.7

311.2

326.0

346.4

TO

14.0

60.0

91.0

151.6

155.0

156.1

177.9

183.0

255.6

263.2

277.3

281.5

293.7

311.2

326.0

346.4

421.0

FOOTAGE

0.0

200.0477.0

DIP

47"

46"

44.5"

DESCRIPTION

SUMMARY LOG

CASING

MAFIC TO INTERMEDIATE FLOWS

MAFIC TO INTERMEDIATE TUFF AND SILTSTONE - 80:20.

- 89.2' - 91.0' - quartz-carbonate stringers; sulphides to 23,

INTERMEDIATE FLOWS AND TUFF

QUARTZ-FELDSPAR PORPHYRY

INTERMEDIATE VOLCANICS


INTERMEDIATE TUFF

MAFIC TO INTERMEDIATE FLOWS AND TUFF- 240.6' - 242.6' - quartz-carbonate stringers to 3!

tite to 355. - 252.0' - 255.6' - as above.

MAFIC TO INTERMEDIATE TUFF

FELSIC VOLCANICS



INTERMEDIATE FLOWS


INTERMEDIATE FLOWS


i; pyrrho-

ONTARIO GEOLOGICAL SUHVl-Y ' ASSESSMENT FILtS

OFFICE

APR 2 2 1988

RECEIVED

AZIMUTH FOOTAGE

SAM

NO.

12211

12246

12249

SULPH IDES

2-3

DIP

P L E

AZIMUTH

RFMARKSPA850854

SUMMARY LOG

R. HigginsonLOGGED BY 3J

FOOTAGEFROM

89.2

240.6

252.0

TO

91.

242.

255.

0

6

6

TOTAL

1.8

2.0

3.6

(i

y

ASSAYS

f. "*v'Oi

— — *,FESS/0,

m™-~--

OZ^TON

.016

.012

.014

OZ/TON

. -t -,-i

•MAmVNU VKILL KEVVKV ., , t ,, ,, ; , ,.- L , L ^HOI. E NO ..EL-87-4 SKI i ^ NO 2 of 2

F OO T AC.E

F ROM

421.0

456.2

T fi

456.2

477.0

477.0

DESCRIPTION

SUMMARY LOG CONI 'D

INTERBEDDED FELSIC AND INTERMEDIATE TUFFS -- 426.0' - 430.0' - quartz-carbonate stringers; fine-grained

wispy pyrrhotite, pyrite, S-5% garnetpoiki loblasts.

INTERMEDIATE VOLCANICS

E.O.H.

SAMPLE

NO

I22781 2280I2282

••ill Pu

l DF S

1-51-51-5

FOOT A G t

CROM

426.0433.5442.0

TO

430.0437.0447.0

T 0 T A i

4.03.55.0

A ^ ". A Y 'J.

,. AAi

.012

.016

.024


EL-87-4EYE LAKF

HOLE NO. LENGTH 477.0'L oc A T ION ,11+OON. 03+20E ________LATITUDE —————-———.—.^———— DEPARTURE

ELEVATION _____________________ AZIMUTH ———

STARTED O eC - 2/87______ FINISHED -—

090 0 47 C

Dec. 5/87

FOOTAGE

0.0

200.0477.0

DIP

470

46 044.5'

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-4 SHEET NO. ] Of 5

PFMARKC.PA850854___________________


FOOTAGE

FROM

0.0

14.0

60.0

TO

14.0

60.0

91.0

DESCRIPTION

Casing.

Mafic to Intermediate Flows - dark green, fine grained massive.Modal percent: Amphibole 45-50*

Plagioclase 40-45* Sericite 3-5*Quartz 1-2*Calcite 1-2*

Amphibolitic to phaneritic, minor zones of medium grained amphi bole in fine grained sericitized plagioclase groundmass, foliationat 55 0 to core axis at 19.0', 44 0 at 42.0', 60 0 at 33.0', 50" at60.0'.

- 29.5' - 30.5' - 0.3-foot clean quartz vein, crosscutting. - 39.5' - 40.5' - 0.2' carbonate vein, medium grained.

Mafic to Intermediate Tuff and Siltstone - 80:20, dark green, tobrown to white fine grained, banded.

Modal percent: Amphibole 55-60*Biotite 15-20*Quartz 15-20*Carbonate 2-3*

Well to crudely banded, 2-3* carbonate veins and stringers, 3-5 *quartz-carbonate bands and stringers, banding at 48 0 to core axisto 66.0', 55 0 at 74.2', 62 0 at 88.0'.

- 74.2' - 75.6' - biotite rich siltstone, brown, fine grainedbanded.

- 77.6' - 80.4' - as above.- 87.0' - 89.2' - as above.- 90.0' - 91.0' - carbonate vein, 1-2* finely disseminated

pyrrhotite, 0.2-foot quartz vein at lowercontact.

SAMPLE

NO.

12201

1220:

1220412205

I220612208122091221012211

SULPH IDES

~~.

3NTAI At

R

1-2

FOOTAGEFROM

14.0

;io GfioiSESSW

OF

APR l

ECE39.5

55.060.0

70.275.677.687.089.2

TO

19.0

OQICAL ENT F:)CE:

i m(VE40.5

60.065.0

75.677.680.489.291.0

TOTAL

5.0

ASSAYS

i

LERV it f'

I li1 \*

B \

D l l .1.0

5.05.0

5.42.02.82.21.8

^v.'^wj\sJ-Z f

^VV0'-/ "^^*Sfe f*"''

'"

OZ/TON

-tn"--L/r^PAs*

-^ .;w--r fiv c '

tr.008

trtr

.002tr

.004tr

.016

OZ/TON

'CySs ,o f•;''''y"7' . -s*

V,l.;

DIAMOND DRILL RECORD N AM t. OF PRO P E R T N ^ t IL LAKL

HOLE NO .EL-87-4.. .. NO 2 Of 5

F OOT AGT

TROM

91.0

151.6

TO

151.6

155.0

DESCRIPTION

Intermediate Flows and Tuffs - dark greenish-grey, fine to mediumgrained, massive to schistose (flows), banded (tuffs).

Modal percent: Plagioclase 45-5055Amphibole 40-453!Quartz 3-5*Carbonate 3-5*Pyrite tr-1%

- 91.0' - 101.8' - flows, few quartz-carbonate stringers,trace pyrite.

- 101.8' - 125.0' - flows, carbonatized, S-5% carbonatestringers, abundant irregular fractures,trace - 0.5* disseminated pyrite, minorzones of sericitized plagioclase.

- 101.8'-103.7'- highly fractured, highlycarbonatized.

- 103.7'- 125.0' - moderately to weaklycarbonatized.

- 125.0' - 147.9' - tuff and flows, 70:30, 2-3* quzrtz-car-bonate stringers.

- 146.6'-147.9'- schistose, 2-3* dissemin ated garnets.

- 147.9' - 151.6' - carbonatized, schistose, 10-20* carbonatestringers, minor breccia, minor disloca tions, trace-0.5* finely disseminatedpyrite.

Foliation averages 60 0 to core axis.

Quartz-Feldspar Porphyry - white medium grained phenocrysts in afine grained grey groundmass.

Modal percent: Quartz 45-50*Plagioclase 45-50*Carbonate 2-3*Pyrite tr-1%

SAMPLE

'1O

1221212213122141221512216122171221E1221912220

12221122221222312224122251222612227

12228

tor*;

trtrtr

tr-.5tr-.5tr-.5tr-.5tr-.5tr-.5

tr-.5

tr-1

FOOT AOLf ROM

91.094.097.0101.8103.7107.0112.0117.0122.0

125.0128.0132.0137.0142.0146.6147.9

151.6

TO

94.097.0101.8103.7107.0112.0117.0122.0125.0

128.0132.0137.0142.0146.6147.9151.6

155.0

'l)TAl

3.03.04.81.93.35.05.05.03.0

3.04.05.05.04.61.33.7

3.4

•\G"j AY cj

.ML

trtrtrtrtrt rtrtrtr

.008tr

.002

.002trtrtr

tr

DIAMOND DRILL RECORD EYC LAKE

E; NO EL-87-4 3 of 5

FOOT AOL

F- ROM

151.6

155.0

156.1

177.9

183.0

255.6

TO

155.0

156.1

177.9

183.0

255.6

263.2

OE- SCRIPT ION

Cont'd.Highly fractured, foliated at 50 C to core axis, quartz-carbonatefracture fillings, minor brecciation, plagioclase phenocrysts inqiiartz-plagioclase groundmass.

Intermediate Volcanics - carbonatized, as per 147.9' - 151.6', witt'{-2'?* disseminated and banded tourmaline, amphibole bands withquartz-carbonate cores, foliation at 51" to core axis at 155.5'.

Mafic to Intermediate Flows - typical foliation at 48 C to core axisat 160.5' , 54" at 170.0'.

- 156.1' - 168.0' - irregular quartz-carbonate-epidote strin gers, Q.5-1% disseminated pyrite, coarsegrained bleb of pyrrhotite at tip ofsection.

Intermediate Tuff - 3-536 wispy biotite bands, T-2% disseminatedpyrite foliation at 50 0 to core axis at 183.0'.

Mafic to Intermediate Flows and Tuff - 80:20, 1-3/& quartz-carbonatestringers.

- 247.6' - 255.6' - 2-336 carbonate and quartz-carbonate vein-ing and 2-356 pyrrhotite blebs.

Foliation averages 58 0 to core axis fracturing at 400 to core axisat 221.0'.

Mafic to Intermediate Tuff - atypical, 3-5X garnet, S-10% chlorite,3-536 irregualr pyrite stringers, trace-1% pyrrhotite, slightlymagnetic, foliation at 62 0 to core axis at 262.0'.

- 255.6' - 257.0' - quartz veining, clean, 1-236 pyrite, tracesubhedral garnets.

SAMPLF

MO

12229

1223012231122321225012207

12233

122341223512236122371223S12239 1224C1224112242

122431224412245122461224712248122491225112252

'-.lit PH

i or s

tr-.5

.5-1

.5-1

.5-1

1-2

2-32-32-33-53-5

r DOT A G t

FROM

155.0

156.1161.1166.1170.2174.9

177.9

183.0188.0193.0198.0203.0207.0 212.0217.0222.0

227.0232.0237.0240.6242.6247.0252.0255.6259.4

T 0

156.1

161.1166.1168.0171.6177.9

183.0

188.0193.0198.0203.0207.0212.0 217.0222.0227.0

232.0237.0240.6242.6247.0252.0255.6259.4263.2

r '.T*l

1.1

5.05.01.91.43.0

5.1

5.05.05.05.04.05.0 5.05.05.0

5.05.03.62.04.45.03.63.83.8

A 'j 'j A Y 'j

".-Ay,

ir

trtrtrtrtr

tr

trtrtrtrtrtr trtr

.002

trtrtr

.012

.002tr

.014trt r

j - r 'W

DIAMOND DRILL RECORD

263.2

277.3

281.5

293.7

311.2

277.3

281.5

293.7

311.2

326.0

HOLE NO

F c) f-'OPF:m V-

EL-87-4

EYE LAKE

Sill l T NO 4 Of 5

DESCRIPTION

Felsic Volcanics - dark grey to white, fine grained, finely toto crudely banded.

Modal percent: Quartz 40-45*Plagioclase BO-35%Sericite 30-35*Carbonate ID-15%Chlorite 5-10*Pyrite Q.5-1%

Q.5-1% finely disseminated pyrite, foliation - banding at 72 0 tocore axis at 276.0', 67 0 at 266.5'.

- ?76.3' - 277.3' - quartz veining, trace garnet, 1-2* pyrite.

Mafic to Intermediate Tuff - as per 255.6' - 263.2', finely banded,foliation at 59" to core axis at 280.5'.

Felsic to Intermediate Volcanic - dark grey to black, fine grained,banded to massive.

Modal percent: Quartz 60-65*Plagioclase eO-65%Amphibole IB-20%Chlorite ID-15%Pyrite 1-2*

Finely disseminated pyrite, foliation at 62 0 to core axis at 284.0'- 286.2' - 287.2' - quartz-carbonate veining, carbonate on

contacts, T-2% pyrite on fracture planesnear contacts.

Intermediate Flows - typical, foliation at 62 0 to core axis at304.0', 52 0 at 310.0', 1-2* quartz-carbonate stringers .

- 308.2' - 308.9' - banded quartz-carbonate veining, 1-2*disseminated pyrite and pyrrhotite.

Mafic to Intermediate Flows - foliation at 53 C to core axis at312.0'.

SAMPLE

- 10

122531225412255

12256

12257

1225812259

12260122611226212263

122641226512266

H)F*i

3-5

1-2

1-21-2

1-2

^COT AGt

f R'JM

263.2268.2273.2

277.3

281.5

286.5291.5

293.7297.0302.0307.0

311.2316.2321.2

TO

268.2273.2277.3

281.5

286.5

281.5293.7

297.0302.0307.0311.2

316.2321,2326.0

TOTM

5.05.04.1

4.2

5.0

5.02.2

3.35.05.04.2

5.05.04.8

f, 'j'. A Y 'j

•ty*

tr.002tr

tr

tr

trtr

trtrtrtr

trtrtr

DIAMOND DRILL RECORD EYE LAKE

E MO ,EL-87-4 o 5 of 5

FOOT AGt

FHOM

326.0

346.4

421.0

456.2

T O

346.4

421.0

456.2

477.0

477.0

lit SCRIPTION

Intermediate Flows - foliation at 37" to core axis.

Mafic to Intermediate Flows - atypical, medium grained, 2-35I5quartz-carbonate stringers with minor potash feldspar, amphibo-litic texture, foliation at 37-40 0 to core axis, banding at 48 0 tocore axis at 373.0', fractures at 35 0 and 50 0 to 58 0 to core axis.

- 377.0' - 392.0' - T-2% disseminated pyrite and pyrrhotiteblebs.

- 419.0' - 419. 5 1 - 0.3-foot clean quartz vein.

Interbedded Felsic and Intermediate Tuffs - 2-3X quartz-carbonatestringers with horizons of S-10% carbonate stringers, 3-5X garnetin intermediate tuff. T-3% fine grained wispy pyrrhotite blebs,spotty horizons of S-5% pyrite blebs, well to poorly banded, foli ation and banding at 45 0 to core axis.

Intermediate Volcanics - typical, fractures with quartz-carbonateor pyrite infillings (1-2X).

- 457.7' - 467.0' - fault gouge, soft, friable, foliated,highly fractured with minor compet ntclasts hosted in schistose matrix.

Foliation at 50 0 to core axis at 477.0', fracturing at 55 0 to coreaxis at 477.0' .

E.O.H.

SAMPLE

,,0

122671226812269

122701227112272

12273122741227512276

1227712278122791228012281122821228312284

12285

12286122871228812289

S'U PM

H' F S

1-21-21-2

1-51-51-51-51-51-51-51-5

1-2

1-21-2

FOOT A Gf

r B:} M

326.0331.0336.0

341.0344.0346.4

377.0382.0387.0417.0

421.0426.0430.0433.5437.0442.0447.0452.0

456.2

457.7462.0467.0472.0

TO

331.0336.0341.0

344.0346.4351.4

382.0387.0392.0421.0

426.0430.0433.5437.0442.0447.0452.0456.2

457.7

462.0467.0472.0477.0

IfilAI

5.05.05.0

3.02.45.n

5.05.05.04.0

5.04.03.53.55.05.05.04.2

1.5

4.35.05.05.0

A 'j i, A Y r, .,. .^ — .

. .' r r j M

trtrt r

trtr.002

trtrtrtr

tr.012tr

.016

.002

.024trtr

tr

.002trtrtr

1 i ,' r . K

DIAMOND DRILL RECORDEL-87-5 SHEET NO. Of l

NAME OF PROPERTY EYE LAKE FOOTAGE DIP

HOLE NC

LOG AT IO

LATITUD

ELE VAT 1

STARTED

, EL-87-5 IF NC,TH 307.0' —— —^—^N 44+50N. 03+30W —— iL-dL.

307.0 -43 0

DM AZIMUTH Grid East DIP -45" ———— — — —Dec. 5/87 FINI^HFH Dec . 10/87 ———— — —

FOOTAGE

FROM

0.0

117.0

121.9 144.8 152.6 178.2

201.6 245.7 263.3

TO

117.0

121.9

144.8

152.6

178.2

201.6

245.7

263.3

307.0

307.0

DESCRIPTION

SUMMARY LOG

CASING.


MAFIC TO INTERMEDIATE VOLCANICS (FLOWS)

SILICIFIED MAFIC VOLCANICS (FLOWS)

SILICIFIED MAFIC TO INTERMEDIATE TUFF

MAFIC TO INTERMEDIATE VOLCANICS (FLOWS)- 186.8' - 188.7' - abundant calcite veinlets to 3mm wide;

sulphides to 31i as fins disseminations.MAFIC TO INTERMEDIATE TUFF AND FLOWS - 70:30

FELSIC TUFF

SILICIFIED MAFIC TO INTERMEDIATE TUFF

E.O.H.

i ONTARIO GEOLOGICAL SURVEY ' ASSESSMENT FILES

OFFICE

APR 2 2 1988

RECEIVED

AZIMUTH "OOTAGE

SAM

NO.

12316

S^PSH.

1-3

DIP

P L E

AZIMUTH

RFMARKSPA850855

SUMM

LOGGE

FOOTAGEFROM

186.8

TO

188 7

TOTAL

1.9

ARY LOG

R. I. FogalD BY

ASSAYS

•; OZ/^ON

.024

OZ/TON


EL-87-5EYE LAKE

HOLE NO. 307.0'LOCATION 44+50N. 03+30WLATITUDE

ELEVATION

STARTED —

DEPARTURE

Dec. 5/87AZIMUTH Grid East DIP

Dec. 10/87

FOOTAGE

0.0

307.0

DIP

-45"-43 0

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. L l -O7 - 3 SHEET NO. ' U '

REMARKS PA850855

LOGGED 8YR.I. Fogal

FOOTAGE

FROM

0.0

117.0

121.9

TO

117.0

121.9

144.8

DESCRIPTI ON

Casing.

Mafic to Intermediate Tuff - medium grained, grey to medium green.massive to poorly foliated. Plagioclase-quartz lapilli to 2mmlong appear locally, showing poorly developed foliation. No evi dence of quartz and/or calcite veining. Dominantly massive, med ium green. Red feldspar as minor fracture infilling. Little/no evidence of sulphides. Minor limonitic staining.

Modal percent: Plagioclase 35-40* Quartz 35-40*Amphibole 35-40*Chlorite 5-10*Mica 3-5*

B"C

Feldspar 1-3* LLimonite 1-3*Sulphide trace

- 117.0' - 121.9' - as above

Mafic to Intermediate Volcanics (Flows) - light grey to green,massive. Fine to medium grained, dominated by 1-2mm amphiboles.Trace evidence of sulphides as fine disseminations of pyrite.Minor limonitic staining, restricted to fractures, commonly infill ed with quartz-calcite.

Modal percent: Amphibole 45-55*Plagioclase 25-35*Quartz 3-5*Calcite 3-5*Limonite 1-3*Sulphides trace

- 121.9' - 131.9' - typical, as above

SAMPLE

NO,

•~..~..

NTARAS:

R

12301

1230212303

S,^1H -

0 Gi(ifcSS

oAPR

EC

tr

trtr

FOOTAGEFROM

LOGlCAiWENT fFFICE

22 19

TO

SURVEILES

88

E IV

117.0

121.9126.9

ED

121.9

126.9131.9

TOTAL

{ rl *

1 ^

x"\

4.9

5.05.0

ASSAYS

jQ

fv*^vlf

"— ***.1 —— -v

m.,**r..-I*^

^ra****

AUOZ/TON

•y^\/s y\V'\k s•o

\0 f-5'' jT

*r

tr

trt r

O7-/TOM

\

DIAMOND DRILL RECORD N AMf OF" PPOF J F (^ I ' EYE LAKE2 of 4

FOOT AOf

f ROM

121.9

144.8

152.6

178.2

Td

144.8

152.6

178.2

201.6

DESCRIPTION

Cont'd.- 137.1' - 144.8' - as above, containing up to WU quartz-

calcite veins, typically barren ofmineralization, containing minor sericiteand epidote, both as wisps and discontinu ous lenses within quartz veins.

Silicified Mafic Volcanics (Flows) - interval similar compositionally to 121.9' - 144.8', containing up to 40* as quartz veins(with lesser carbonate). Volcanics appear dominated by dark greenamphiboles, locally as crystals to 8mm across. Overall massiveappearance. Quartz veins containing sericite withlesser amounts of tourmaline and blebs of pyrite, pyrrhotite asfracture coatings. Veins appear highly deformed, often inter mixed with wisps, lenses of mafic country rock.

- 147.5' - 149.1' - interval dominated by quartz vein, con taining up to 3* pyrite as secondaryfracture coating within vein.

- 149.1' - 152.6' - as above.

Silicified Mafic to Intermediate Tuff - well developed banding,light to medium grey, fine to medium grained. Typical foliations;45 0 at 157.0', 3D 0 at 169.5', 38 0 at 172.0'. Abundant quartz andcalcite veins, parallel to banding, containing trace amounts ofpyrite and pyrrhotite as fine disseminations. Veins averaging1-2mm wide, hosted in an assemblage dominated by amphibole andplagioclase. Few carbonate-rich veins contain blood-red blebs oflimonite along with trace chalcopyrite. Irregularly distributed -discontinuous streaks of mica (potassic alteration?).

Modal percent: Plagioclase 40-55*Quartz 40-55*Amphibole 35-45*Carbonate 8-10*Mica 3-5*Limonite 1-3*Sulphides trace

Mafic to Intermediate Volcanics (Flows) - light to medium green,

SAMPLE

...,

I2304I2305

1 2306

I2307

1 2038

1 23091231012311123121231312314

12315

•or s

trtr

tr

1-3

tr

trtrtrtrtrtr

tr

FOOTAGtfflOM

137.1140.1

144.8

147.5

M9.1

152.6157.6162.6167.6172.6175.6

178.2

TO

140.1144.8

147.5

149.1

152.6

157.6162.6167.6172.6175.6178.2

183.2

TOTAL

3.04.7

2.7

1.6

3.5

5.05.05.05.03.02.6

5.0

iVjSAY 1,

..AM,,.

trtr

tr

tr

tr

trtrtrtrtrtr

tr

,,.- t,*

DIAMOND DRILL RECORD N AMI Of PHOf* FH1 Y.

t-1 n i r" M f i t L - o l - D

EYE LAKE

..H, l r NO 3 Of 1

Foo 1 A c, r

178.2

201.6

201.6

245.7

DESCRIPTION

Cont'ri.

massive, fine-grained. Simi lar compositionally, texturally to121.9' - 144.8' containing very few quartz veins, typically 1-2mmwide, discontinuous, randomly distributed, and barren of minerali zation. Trace evidence of finely disseminated pyrite.

- 186.8' - 188.7' - typical, containing abundant calcite(-quartz) veins averaging 2-3mm wide,sulphides as fine disseminations of py rite, pyrrhotite, with lesser chalcopy rite, overall up to 3?S. Veins trendingat 35 0 to C. A.

- 195.3' - 198.9' - similar to 186.8' - 188.7', containinglesser amounts of sulphides, commonlytr.-U. Veining at 48 0 to C, A.

Mafic to Intermediate Tuffs and Flows - 70:30. Well banded, finegrained, medium green tuffs, containing abundant quartz and cal cite veins, intercalated with lesser amounts of massive, fine grained mafic flows, light to medium green colour. The tuffs con tain abundant (up to 403S) quartz and calcite veins, averaging2-3mm in width, typically barren of mineralization, similar com positionally, texturally to 117.0' - 121.9', trending at 42" toC. A. The flows show little/no quartz or calcite veining, containingtrace pyrite as fine disseminations; less commonly as fracturecoatings. Similar to 121.9' - 144.8' .

- 201.6' - 204.4' - typical mafic-intermediate tuff. Traceevidence of finely disseminated sulphides.

- 207.3' - 211.3' - as per 201.6' - 204.4'.- 212.7' - 217.0' - as above, containing trace arsenopyrite a:

fracture infillings, typically Ornrn wide.- 218.9' - 245.7' - typical mafic to intermediate tuff, con

taining numerous streaks (averaging 8-10mm wide) of mica-rich zones. Also evi dence of orange-red limonite staining.Well developed banding at 40 0 to C. A.

SAMPLE

-H,

1231J

12316

12317

1231E

1231S1232C

1232 1123221232j123241232512326

icirs

tr

1-3

tr-1

tr

trtr

trtrtrtrtrtr

FOOT AGtCBOM

178.2

186.8

195.3

201.6

207.3212.7

218.9223.9228.9233.9238.9241.9

TO

183.2

188.7

198.9

204.4

211.3217.0

223.9228.9233.9238.9241.9245.7

TOTAl

5.0

1.9

3.6

2.8

4.04.3

5.05.05.05.03.03.8

A ', :. A Y '?

Mu,

tr

.024

tr

tr

trtr

trtrtr

.002

.002tr

DIAMOND DRILL RECORD N AMT OF PKOPF.f* I r

HOt-E NO EL-87-5

EYE LAKL

.H|-f ' NO 4 Of 4

FOOT A C. F

263.3 307.0

307.0

DESCRIPTION

Silicified Mafic to Intermediate Tuff - similar compositional ly,texturally to 152.6' - 178.2'. Well developed banding at 40 0 toC. A. Abundant quartz and calcite stringers, typically 2-3mm wide,parallel to banding; trace pyrite, as fine disseminations, re stricted to mafic-intermediate tuff. Micaceous zones as discon tinuous streaks, lenses, barren of mineralization.

- 267.0' - 282.6' - banding becomes highly irregular, contortod.

- 282.6' - 291.9' - banding is quite distinct, at 45 0 to C. A.Barren quartz vein at 282.7' - 283.3'.

- 291.9' - 293.4' - highly carbonatized section showing cavitywith well developed calcite crystals(about 1mm across) growing inwards fromcavity wall. Dusting of pyrite crystalsis also evident, up to 31t.

- 293.4' - 307.0' - typical, showing well developed banding a40 0 to C. A. Quartz vein with minor pyrr hotite and sericite-tourmaline at 305.8' -306.3'.

E . 0 . H .

SAMPLE

r IO

12331

12332I2333I2334I233512336I2337

I2338I2339I2340

'.in PHl [ ' F r.

tr

trtrtrtrtr1-3

trtrtr

FOOT AGEFROM

263.3

267.0272.0277.0282.6287.6291.9

293.4298.4303.4

TO

267.0

272.0277.0282.6287.6291.9293.4

298.4303.4307.0

' ri i A i

3.7

5.05.05.65.04.31.5

5.05.03.6

A rj r, A Y r.Au,,,

tr

trtrtrtrtrt r

trtrtr


EL-87-6[YE LAKE

HOLE NO.

LOCAT.ONLATITUDE

ELEVATION

STARTED

44+50N, 09+OOW

DeC. 10/87

LENGTH 317.0'

DEPARTURE ————

AZIMUTH GridFINISHED —

-45 C

Dec. 12/87

FOOTAGE

0.0307.0

DIP

45"42"

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. t- L ~\" " SHEET NO.

REMARKS PA850R46___________

Of

SUMMARY LOG

LOGGED BY R - ?- F0 9 a1

FOOTAGE

FROM

0.0

81.8

200.3

225.0

244.5

TO

81.8

200.3

225.0

244.5

317.0

317.0

DESCRIPTION

SUMMARY LOG

CASING.





E.O.H.

i ONTARIO GEOLOGICAL SURVEY ' ASSESSMENT FILES

OFFICE

APR 2 2 1988

RECEIVED

SAMPLE

NO. ',UDLEHSH -FOOTAGE

FROM TO TOTAL

ASSAYS

07^4 ON O7/TON

DIAMOND DRILL RECORDNAME OF PROPERTY ____EYE! LAKE

HOLE NO. EL-87-6_________ LENG

LOCAT.ON 44+50N. 09-^OOW

LATITUDE

ELEVATION

STARTED

317.Q'

Dec. 10/87

DEPARTURE ^———^^^—

AZIMUTH Grid East

FINISHED .

-45 C

Oec. 12/87

FOOTAGE

0.0307.0

DIP

45"42"

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-6 SHEET NO. ' Of 5

REMARK s PM50846————.———-

LOGGED BY.R.I. Fogal

FOOTAGE

FROM

0.0

81.8

TO

81.8

200.3

DESCRIPTION

Casing.

Mafic to Intermediate Volcanics (Flows) - moderately carbonatized,fine-grained, dark to medium green, massive to poorly foliated.Abundant calci te-quartz stringers, averaging 2-5mm in width, typically barren of mineralization; stringers appear discontinuousoften as lensoidal pods at 50" to C. A. Blood-red limonitic stain ing occurs as fracture infillings associated with calcite string ers. Country rock containing little/no sulphides, rarely as finedisseminations of pyrite.

Modal percent: Amphibole 55-65*Plagioclase 15-20*Calcite 10-15*Quartz 3-5*Limonite tr-1%Sulphide tr-1*

- 81.8' - 91.8' - typical

- 97.0' - 102.0' - typical, containing abundant calcite stringers, few containing light-green carbonateankerite?

- 113.3' - 123.3' - typical.

- 128.8' - 133.8' - typical, containing irregular pods, lens es of calcite veins/lenses, commonly withlittle/no quartz content.

- 133.8' - 137.3' - as per 128.8' - 133.8', containing minorwisps, streaks of mica, commonly Ommwide.

- 138.9' - 142.2' - typical, containing up to 3* sulphides as

SAMPLE

NO.

f~i

123411234212343

123441234512346

12347

12348

S^PSH-

3NTA

R

trtrtr

trtrtr

tr

1-3

FOOTAGEFROM TO

HO GEOLOGICALibtSSMENT F

APR

ECf

81.886.897.0

113.3118.3128.8

133.8

138.9

5219

; i v i

86.891.8102.0

118.3123.3133.8

137.5

142.2

TOTAL

SUF1VEVILES

8 (1

". D

5.05.05.0

5.05.05.0

3.7

3.3

ASSAYS

X*"*^•o^fyi'• i -N/%^v.

-,

^,'r '-''

"T

fm,;,•C; OV--- -.i •,.

OZ/TON

ix^'•j ^""\X;

.- ..' !.'

..''•''"''S..•'^-

.002

.002

.002

.002

.003

.002

.003

.002

OZ/TON

)

\ ' \

j

DIAMOND DRILL RECORD NAME. OF Ph'OF J E.liT V

HOI.t NO JL-87-6

EYE LAKE

rocn

r ROM

81.8

r AGE.

T f)

200.3 Cont'd.

- 142.2'

- 147.0' - 152.0'

- 162.7'

- 167.0'

- 170.6' - 177.0'

- 182.8'

- 191.2'

l ) E: SC R 1 P T 1 0 N

fracture fillings associated with calciteinjection, typically in stringers Ommwide; parallel to calcite veinlets, dis continuous; sulphides as pyrite, withlesser pyrrhotite.

.2' - 147.0' - as per 138.9' - 142.2', however pyrrhotitecontent increases, as discontinuous blebs,typically Omm wide; also associated withcalcite (with lesser quartz) stringers,particularly at 144.5' .

.0' - 152.0' - typical.

.0' - 156.1' - typical, with highly carbonatized, brec ciated zone at 154.6' - 155.0', containingup to 3X sulphides, commonly pyrite asfine fracture infillings, and a light-green carbonate-ankerite.

.7' - 167.0' - typical, containing highly contorted cal cite stringers, typically barren ofmineralization.

.0' - 170.6' - as per 162.7' - 167.0'. containing 1-3*pyrrhotite as vein infilling at 168.2',approximately 8-10mm wide, associated withcalci te-quartz veining.

.6' - 175.6' - typical.

.0' - 180.0' - typical, containing pyrrhotite lens asso ciated with calcite stringers at 177.1'.

.8' - 186.6' - typical, showing well developed brecciateczone at 183.0' - 183.6', infilled withcalcite-quartz, along with T-3% sulphides,commonly pyrrhotite with lesser pyrite;associated with calcite infilling.

.2' - 195.9' - typical, containing numerous hair linefractures infilled with calcite randomlydistributed throughout interval, typicallybarren of mineralization.

SAMPLE

..o

12349

1235012351

12352

12353

1235412355

12356

12357

j U f . S

1-3

tr1-3

tr

1-3

tr1-3

1-3

tr

F O Ci T AGt

FflOM

142.2

147.0152.0

162.7

167.0

170.6177.0

182.8

191.2

TO

147.0

152.0156.1

167.0

170.6

175.6180.0

186.6

195.9

rrjlAI

4.8

5.04.1

4.3

3.6

5.03.0

3.8

4.7

,\',:,,\Y ',

mi

.003

.003

.004

.003

.003

.003

.002

.003

.002

,- ,.,

DIAMOND DRILL RECORD NAMl OF PROPERTY..

HOLE NO ..EL -87 -6

EYE EAKE

NO 3 of 5

FOOT AGE

F HOW

81.8

200.3

225.0

TO

?00.3

??5.0

?44.5

DESCRIP7 ION

Coni 'd.- 195.9' - 200.3' - typical. An increased feldspar content

is noted.

Mafic to Intermediate Tuff - medium grey to light green, fine tomedium grained. A well developed compositional banding is observerindividual discrete bands varying from 2mm to 3cm in width; cross cutting at 45-50 0 to C. A. Composition ranging from amphibole-richdark green bands to amphibole-poor, feldspar(plagioclase)-rich bands,light to medium grey in colour. Secondary carbonization is evi dent as calcite stringers, subparallel to banding, and as irregularcalci te-inf i 1 led hairline fractures, sporadically distributed,typically barren of mineralization; minor associated brecciationzones, also calcite infilled. Trace evidence of sulphides, com monly as fine disseminations of pyrite; to a lesser extent as py rite and pyrrhotite fracture infillings/coatings. Individualfeldspar lapilli rarely observed. Few intercalated bands of mas sive, dark to medium green volcanic flows.

Modal percent: Amphibole 40-555SFeldspar 20-30*Quartz TO-15%Calcite 8-10tChlorite 1-3JSSulphide trace

- 200.3' - 204.6' - typical, containing amphibole needles to8mm.

- 204.6' - 207.0' - typical with up to 30X calcite in irregu lar pods, veins to 10cm wide.

- 207.0' - 217.0' - typical.

- 218.4' - 225.0' - typical, containing trace arsenopyrite asfine disseminations.

Mafic to Intermediate Volcanics (Flows) - similar compositional ly,texttirally to 81.8' - 200.3'. Massive, light to dark green incolour, fine-grained, moderate degree of carbonization as numerouscalcite stringers, averaging 2-3mm wide, typically barren ofmineralization. Few 2-3cm wide tuffaceous horizons are evident,

SAMPLE

NO

1235S

12359

1?360

12361123621236312364

1236512366

SIM PH

l[tf ^

tr

tr

tr

trtrtrtr

trtr

12367 tr

FOOT AGtFROM

195.9

200.3

204.6

207.0212.0218.4222.0

225.0230.0239.5

Tt

200.3

204.6

207.0

212.0217.0222.0225.0

230.0235.0244.5

if)TAi

4.4

4.3

2.4

5.05.03.63.0

5.05.05.0

A:.:, A Y;.'In*

.003

.004

.003

.001

.00?

.002

.004

.00?

.003

.001

1 1 .' l in

DIAMOND DRILL RECORD NAMF of PROFJ EF; T Y... EYE LAKE HOI.c NO .EL-87-6.. . NO 4 of 5

225.0

244.5

244.5

317.0

DESCRIPTION

Cont'd.exhibiting well preserved lapilli to 1mm. Sulphides restricted tofine disseminations of pyrite; pyrrhotite to a lesser extent.

Mafic to Intermediate Tuff - similar compositionally, texturallyto 200.3' - 225.0'. Well developed compositional banding is alsoobserved, trending at 50 0 to C. A. Sulphides as finely dissemin ated pyrite, trace amount.

- 244.5' - 254.5' - typical, containing abundant barren cal cite stringers, veinlets, averaging 3-5mmwide, parallel to subparallel to banding.

- 257.9' - 266.8' - typical, appearing well brecciated withcalcite infilling. Individual lapillialso observed. Trace evidence of sul phides, as fine disseminations of pyritethroughout.

- 271.3' - 285.6' - typical.

- 285.6' - 292.3' - typical, containing an increase in feld spar content to WZ, brown-red in colour,forming discrete beds, averaging 8mm widebarren of mineralization. Sub td anhedraquartz grains to 2mm wide occur in a dis tinct band at 291.6' - 292.3'. Ground mass appears fine grained, light grey,well banded, dominantly feldspar. Traceevidence of pyrite and pyrrhotite as dis continuous pods/lenses within this unit.Probably of sedimentary origin. Barrenquartz vein at 287.1' - 287.4'.

- 292.3' - 309.8' - typical, exhibiting an increased silicacontent, along with decrease in feldsparcontent. Well developed banding at 50"to C. A.

SAMPLE

,,,.

1236?1236?

1237C1237112372

1237;123741237E1237C12377

123781237?1238C12381

f,\n PH :nrs

trtr

trtrtr

trtrtrtrtr

trtrtrtr

POOT AGt

* ROM

244.5249.5

257.9261.2264.1

271.3276.3281.3285.6288.5

292.3297.3302.3305.3

'O

249.5254.5

261.2264.1266.8

276.3281.3285.6288.5292.3

297.3302.3305.3309.8

"i 1 Al

5.05.0

3.32.92.7

5.05.04.32.93.8

5.05.03.04.5

A 'S, AY',

,-AH.

.002

.004

.004

.003

.003

.002

.002

.001

.002

.002

.002

.002

.002

.002

i.; [MN

DIAMOND DRILL RECORDFOOT A C. C

244.5 317.0

317.0

Cont'd.

E.O.H.

NAMt. Of PRO!J tF-iTV

HOLE NO EL-87-6

EYE LAKE

NO 5 of 5

HF. SCRIPT ION

09.8' - 311.2' - well laminated, light grey, fine to med ium grained. Anhedral quartz grains to2mm enveloped by feldspar and quartz-richmatrix. Probably of sedimentary origin,as at 291.6' - 292.3'. Mica laminations(Omm wide) define the bedding, which islocally contorted, but typically at 50 0to C. A. Pyrrhotite and pyrite as discon tinuous pods, to 35S,

!11.2' - 317.0' - as per 292.3' - 309.8'.

SAMPLE

M,.

12382

1238:1238^

MM Pu

lUf S

1-3

trtr

FOOT AGtFROM

309.8

311.2314.2

ro

311.2

314.2317.0

Tl 1AI

1.4

3.02.8

'••j'.. A y o

,'^

.001

.002

.002

DIAMOND DRILL RECORD

00+00, I2+55W

NAME OF PROPERTY

HOLE NO. FI -87- 7

LOCATION

LATITUDE

ELEVATION

STARTED

EYE LAKE

Dec. 13/87

DEPARTURE —————^———

AZIMUTH Grid EastFINISHED Dec. 14/87

-45 0

FOOTAGE

0.0

247.0

DIP

45"44.5

AZIMUTH FOOTAGE DIP AZIMUTHSHEET NO. Of

REMARKS PA786864

SUMMARY LOG

P.I. FogalLOGGED BY

FOOTAGE

FROM

0.0

21.4

111.4

203.8

238.5

TO

21.4

111.4

203.8

238.5

257.0

257.0

DESCRIPTION

SUMMARY LOG

CASING.

MAFIC VOLCANICS.

MAFIC TO INTERMEDIATE TUFF.

FELSIC TO INTERMEDIATE TUFF.

MAFIC TO INTERMEDIATE TUFF - silicified.E.O.H.

^.mm^ t i ii H i" 1 "' —— *

ONTARIO OEOtOOICAt SURVEY. ASSESSMENT FILtS

OFFICE

APR 2 2 1988

SAMPLE

NO. S ut PH - ICES

FOOTAGEFROM TO TOTAL

f

\\

A S S A V S

s '

fi''" /'

f^t'

\^',-

-- -.

,ui i- ; - ;

^

" \ .

AUOZ/TON

: .^r;f: -'-.iy*-

OZ/TON

1

; \


EL-87-7EYE LAKE

HOLE NO.

LOCATION

LATITUDE

ELEVATION

STARTED —

257.0'00+00. 12+55U —

Dec. 13/87

DEPARTURE

AZIMUTH

FINISHED .

Grid East Dec. 14/87

-45 C

FOOTAGE

0.0

247.0

DIP

45"44.5

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-7 SHEET MO.

R.MARKS PA786864

Of 3

LOGGED BY.R.I. Fogal

FOOTAGE

FROM

0.0

21.4

- ^.- ARICi ASSss

l

R l^D

D

|

/)

S iJ!

j

TO

21.4

111.4

GEOLOISSMEOFFI

.PR2

C tr c

DESCRIPTION

Casing.

Mafic Volcanics - dark qreen, massive, fine grained. Few sporadiccalcite-quartz veinlets, 2-5mm in width, typically barren ofmineralization. Sulphides limited to fracture coatings and infillings of pyrite, in trace amounts.

Modal percent: Amphibole 55-7055Feldspar 15-20*Calcite 3-55!Quartz 1-355Sulphide trace

- 33.1' - 36.6' - typical, containing lenses/clots of pyrite,with lesser pyrrhotite, 1-2mm across.

iiCAL suRv^'P' - 46.2' - typical with numerous calcite stringers, !IT tin 0 averaging 1-3mm in width, associated pyrite VL '~ ILUO and pyrrhotite to 35! as fracture infilling*2f. coatings.

- 54. ' - 59.3' - typical.J 1988' 69 - ; ' " 72 - 8 ' - typical, containing numerous quartz and cal

cite stringers, barren of mineralization.- 76. '' - 78.9' - as per 69.8' - 72.8', containing orange-red

w C n feldspars as accessory minerals associated1 v u with quart7-ralritP vpirx:

- 87.0' - 90.4' - typical, containing light to medium bluemineral as fracture infilling, associatedwith quartz-calcite. Possibly sodalite (?)

- 90.4' - 92.3' - typical, containing quartz vein, continuousfrom 90.8' - 91.8'. Minor orange-red feld spar and chlorite; small flecks (Ornmacross) of pyrite.

SAMPLE

NO.

123851238^

12385

1238J 1238S

1239C12391

12392

12393

12394

sti^-

trtr

tr

1-31-3

trtr

tr

tr

tr

FOOTAGEFROM

21.426.4

33.1

39.0 42.2

54.369.8

76.0

87.0

90.4

TO

26.431.4

36.6

42.2 46.2

53.372.8

78.9

90.4

92.3

TOTAL

5.05.0

3.5

3.2 4.0

5.03.0

2.9

3.4

1.9

ASSAYS

AU OZ/TOH

.001

.001

.003

.003

.001

.002

.002

.002

.002

.001

OZ/TON

DIAMOND DRILL RECORD OF PROPF-KlY ..EYE LAKE

HOLE. NO

FOOTAGF

21.4

111.4

111.4

203.8

DESCRIPTION

Cont'd.106.4' - 111.4' - typical.

Mafic to Intermediate Tuff - moderate to well developed banding,at 48" to C. A. Fine to medium grained, light grey to medium greenIndividual lapilli observed to 2mm. Quartz grains, sub to anhedraalso locally observed, enveloped by feldspar and amphibole matrix.Trace sulphides as fine disseminations of pyrite. Few sporadiccalcite stringers, barren.

Modal percent: Amphibole 40-55XPlagioclase 15-25*Quartz S-10%Chlorite 1-351!Calcite 1-3*Sulphide trace

- 118.4' - 120.2' - typical, with quartz-feldspar vein at118.8' - 119.5'. Feldspar appears purplein colour, crystals to 1cm across. Minorassociated chlorite. Barren of minerali zation.

- 126.2' - 137.0' - typical, containing an increase in feld spar content, to 40*. Trace evidence ofdisseminated pyrite. Well Banded at 40 0to C. A. Barren quartz veins at 126.5' -126.7' and 136.1' - 136.4'.

- 146.2' - 153.4' - typical, well banded at 380 to C. A.

- 153.4' - 166.0' - typical, highly deformed and contorted inappearance. Numerous quartz-calciteveins; barren.

- 166.0" - 176.0 - typical, displaying well developed bandintat 400 to C. A.

- 179.1' - 194.8' - typical, containing numerous quartzstringers, averaging 5.8mm wide, withtrace amounts of pyrite and pyrrhotite asclots/pods, ^mm wide.

- 197.0' - 203. 8 1 - typical.

SAMPLC

no

1239E

12396

12397

1239E1239912400

124011240212403124041240S12406124071240f124091241C12411124121241:

IDE 5

tr

tr

tr

trtrtr

trtrtrtrtrtrtrtrtrtrtrtrtr

F O O T A G tF RUM

106.4

111.4

118.4

126.2129.2132.5

146.2150.4153.4157.0161.8166.0171.0179.1182.1187.0191.6197.0199.8

TO

111.4

116.4

120.2

129.2132.5137.0

150.4153.4157.0161.8166.0171.0176.0182.1187.0191.6194.8199.8203.8

"i 1 *1

5.0

5.0

1.8

3.03.34.5

4.23.03.64.84.25.05.03.04.94.63.22.84.0

A V. A Y S

.,/to,

.002

.003

.001

.002

.001

.001

.002

.002

.002

.003

.001

.002

.002

.001

.001

.001

.002

.001

.001

...' T'.,

DIAMOND DRILL RECORD NAMf OF PKOPEFi I V. .

HOLE NO EL-87-7

EYE LAKE

HI i i MO 3 of 3

FOOT AUf

203.8

238.5

238.5

257.0

257.0

DESCRIPTION

Felsic to Intermediate Tuff - medium to light grey, well banded,fine to medium grained. No mafic component is observed. Micaceousstreaks (sericite L muscovite) define the banding, often contortedand intercalated with quartz and calcite stringers, commonly Ownwide, subparallel to banding at 45" to C. A. Trace to 35! associatecpyrite and pyrrhotite, also occuring in blebs/clots.

Modal percent: Plagioclase -, rr 7m;Quartz J 3D-/U*Mica 20-25*Calcite 8-103!Sulphide tr-3%

- 203.8' - 209.3' - typical with pyrite and pyrrhotite bearincquartz-calcite veins at 204.3' - 205.7'and 207.7' - 209.0'.

- 209.3' - 214.3' - typical, containing contorted beds. Foldclosure at 209.9' .

- 214.3' - 238.5' - typical, containing 1-33! pyrrhotite (withlesser pyrite) as fracture infillings,commonly Omm wide. Well banded at 480to C. A.

Mafic to Intermediate Tuff - highly silicified. Similar compo-sitionally to 111.4' - 203.8', however abundant quartz veins occur,making up to 405! of interval. Quartz veins contain pyrrhotite andpyrite, locally to 53!, as fracture infillings. Minor carbonatiza tion. Little evidence of chloritization. Sericite-muscovite alsoassociated with quartz veining, infilling fractures.

- 238.5' - 240.1' - typical, containing pyrrhotite as fractureinfillings. Few quartz veins.

- 240.1' - 245.6' - continuous quartz vein, containing 1-32!pyrrhotite, with minor amphibole andchlorite and sericite as fracture infill ing.

- 245.6' - 248.2' - as per 238.5' - 240.1'.- 248.2' - 251.3' - as per 240.1' - 245.6'.- 251.3' - 257.0' - typical.

E.O.H.

SAMPLF

l IO

1241412415

12416

1241712418124191242012421

12422

1242312424

1242512426124271242E

•".in PH

I0f S

1-31-3

1-3

1-31-31-31-31-3

1-3

1-31-3

tr1-31-31-3

FOOT AGEFROM

.

203.8207.0

209.3

214.3219.3224.3229.3234.3

238.5

240.1243.1

245.6248.2251.3254.1

10

207.0209.3

214.3

219.3224.3229.3234.3238.5

240.1

243.1245.6

248.2251.3254.1257.0

T 0 I A 1

3.22.3

5.0

5.05.05.05.04.2

1.6

3.02.5

2.63.12.82.9

A'jGAVS

.001

.003

.004

.001

.004

.001

.007

.002

.001

.001

.001

.001

.001

.001

.002

DIAMOND DRILL RECORDHOLE NO. El-87-8 SHEE1 N0. l Of


HOU E NC

LOG AT IO

L ATITUD

EL E VAT 1

STARTED

, EL-87-8 , .r*,,-.™ 3?7.n'N 20-H)OS. 07+OOW

ON A7IMLITH Gfld EdSt46"

Dec. 15/87 F , N ,SHF D Dec. 16/87

FOOTAGE

FROM

0.0

14.1

49.4

231.2

TO

14.1

49.4

231.2

327.0

327.0

D E S C R 1

SUMMARY

CASING.

P T 1 O N

LOG

FOOTAGE

0.31/.

00

DIP

46 043 0

MAFIC TO INTERMEDIATE VOLCANICS (FLOWS).

INTERMEDIATE TUrF.


E.O.H.


OFFICE

APR 2 2 1988

RECEIVED

AZIMUTH FOOTAGE

SAM

NO. siS^

DIP

P L E

AZIMUTH

RFMARKS PA786869

SUMM

LOGGE

FOOTAGEFROM TO TOTAL

ARY LOG

D BY K.I- Fogal

ASSAYS

OZ/TON OZ/TON


HOLE NO. EL-87-8LOCAT ION

LATITUDE

EL EVATION

STARTED

EYE LAKE

20+OOS, 07+OOW

Dec. 15/87

327.0'

DEPARTURE

AZIMUTH .

FINISHED

Grid East Dec. 16/87

46 C

FOOTAGE

0.0

317.0

DIP

46 043"

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. EL-87-8 SHEET NO.

REMARKS PA786869_____

LOGGED BYR.I. Fogal

FOOTAGE

FROM

0.014.1

49.4

TO

14.149.4

231.2

DESCRIPTION

Casing.Mafic to Intermediate Volcanics (Flows) - medium green to lightgrey, massive, fine to medium grained. A poorly developed bandingis locally observed; overall massive appearance. Sporadic quartz-calcite stringers, averaging 2-5mm wide, typically barrenof mineralization. Sulphides restricted to finely disseminated pyrite, less commonly as fracture infillings. Isolated brecciated zones appear secondarily infilled with quartz-calcite.

Modal percent: Amphibole 45-5556Plagioclase -, ,n , n5(.Quartz ^Calcite 3-5XChlorite 1-356Sulphide trace

- 29.9' - 39.9' - typical.

Intermediate Tuff - well developed banding at 70 0 to C. A. Lightto medium grey with isolated amphibole-rich dark green bands.Sulphides as fine disseminations of pyrite. Micaceous laminations,averaging Omm wide, define the banding. Minor calcite and quartzveinlets, discontinuous, typically barren of mineraliation.

Modal percent: Plagioclase -, ,,. 7t.~.Quartz J bt) -' b *Sericite , , Muscovite J '"-'^Amphibole S-5%Calcite 3-556Sulphide trace

- 49.4' - 54.4' - typical, isolated brecciated zone, barren,

SAMPLE

NO.

1242912430

194111 C *T -J \

12432

12433

S^PSH-

trtr

tr tr

tr

FOOTAGEFROM

14.119.1

TO

19.124.1

| ~*N i AF H f\L

29.9*34.9

49.4

R39.9

54.4

TOTAL

5.0

5.0

(0 GEOl SESSN

OF

APR J

ECE5.0

5.0

A S S A V S

5GICAI ENT FICE

2 19

IV l

r

l\

-,;

SUFiVEILES

38

: D

.^^^f fi j

s h*J M/,^4C -r-S/^o,^v'''"^'

OZ/TON

.001

C001

y

001 001

ofr-^ff*^0-"1 -

"t T" ' '

7?^. .

'Ci OV (

^jla^-rfS

.002

07/TON

"l-s,

'''f

'.S^

"f . 4/

i f/

Jr. - o

**** jj^\ v jf^

7

i

\

DIAMOND DRILL RECORD NAMI" Of PKOPKRTY

HOLE NO --- EL-87-8.

EYC LAKC

2 of 3

FOOT A O f

f ROM

49.4

T O

231.2 Cont'd.

54.4'

67.0'

81.3'

98.2'

104.4' 112.5'

123.8' 131.0'

183.2'

194.5'

198.1 208.0'

- 143.8' -

DESCRIPTION

at 50.6' - 50.9' infilled with calcite (withlesser quartz ).

1 - 63.0' - typical.

1 - 77.0' - typical, appearing poorly banded to locallymassive.

1 - 91 .3' -as per 67.0' - 77.0' .

' - 102.5' - typical, containing finely disseminatedpyrite and pyrrhotite to 3/6, as fractureinfilling in poorly banded intermediatetuff.

4' - 109.2' - as per 98.2' - 102.5'.5' - 122.5' - poorly banded to massive, possibly an

intermediate flow.8' - 125.1' - as per 98.2' - 102.5' .0' - 141.0' - massive intermediate, containing streaks/

clots of pyrite and pyrrhotite to 35S asfracture infillings. Quartz vein, barrencontaining orange feldspar, at 131.3' -131.5'.

8' - 183.2' - highly altered sulphidized zone containincdiscontinuous streaks of pyrite, withlesser pyrrhotite up to 1cm wide, sporadi cally distributed throughout poorly tomoderately banded intermediate volcanic(flow or tuff).

2' - 188.2' - typical, well banded intermediate tuff,crosscutting at 65" to C. A. Trace evid ence of finely disseminated pyrite.

5' - 196.4' - typical, containing distorted bands with1-3^ pyrite, with lesser pyrrhotite asfracture infillings to 1mm wide.

1' - 202.0' - as per 194.5' - 196.4'.D' - 219.8' - as per 183.2' - 188.2', containing pyrite-

SAMPLF

MO

I2434I2435I2436I2437I243824392440

12441124421244;1244'1244512446

124471244812449124501245112452124531245412455

12456

1245712458

'.III PH

HIT'.

trtrtrtrtrtr1-3

1-3trtr1-31-31-3

8-108-108-108-108-108-108-108-10tr

1-3

1-33-5

FOOT AGt

FROM

54.458.567.072.081.386.398.2

104.4112.5117.5123.0131.0136.0

143.8148.8153.8158.8163.8168.8173.8178.8183.2

194.5

198.1208.0

TO

58.553.072.077.086.391.3102.5

109.2117.5122.5125.1136.0141.0

148.8153.8158.8163.8168.8173.8178.8183.2188.2

196.4

202.0212.5

*') Mi

4.14.55.05.05.05.04.3

4.85.05.01.35.05.0

5.05.05.05.05.05.05.04.45.0

1.9

3.94.5

A S 0 A V 'j

Ay-. ; H DN

.001

.001

.001

.001

.002

.002

.002

.003

.003

.003

.001

.001

.001

.001^001.002.001.001

^001.001.001

<.001

.002

.002

.002

i j ; r . K

DIAMOND DRILL RECORD NAMF. OF" PHOPEH1 r ..

HOLE: NO ...EL-87-8

EYE LAKE

'.MI I ^ NO 3 of 3

FOOT A L; r

FROM

49.4

231.2

7 O

231.2

327.0

327.0

INSCRIPTION

Cont'd.pyrrhotite to 5X as fracture infilling* tc1mm wide, scattered randomly, parallel tosubparallel to banding.

Mafic to Intermediate Tuff - well developed compositional banding,crosscutting at 55 0 to C. A. Alternating 2-5mm bands of dark greenamphibole-rich mafics and medium to light grey feldspar-rich assem blage. Sulphides typically as fine disseminations of pyrite, andpyrrhotite to a lesser extent.

Modal percent: Amphibole 45-5536Plagioclase -, , g , Q^Quartz ^Chlorite 1-336Calcite 1-336Sulphide trace

- 244.5' - 254.5' - highly contorted bands, exhibiting foldclosures. Sulphides as trace pyrite -finely disseminated.

- 262.0' - 279.6' - well banded, containing light green feld spar, possibly as an alteration product.No associated sulphides.

- 287.3' - 295.8' - poorly banded, containing light-greenfeldspar, as per 262.0' - 279.6'. Tracepyrite.

- 302.0' - 327.0' - poorly banded to massive, containing tractevidence of finely disseminated pyrite.Light green feldspar as secondary infill ing making up to 205! of interval. Minorcarbonatization as calcite stringers. Veinmaterial consisting of feldspar and quartzcalcite; typically barren of minerali zation.

E.O.H.

SAMPLE

'40

1245912460

1246112462

1246312464

124651246612467124681246912470

1247112472124731247412475

Mil (Ml

Htf r*

3-53-5

trtr

trtr

trtrtrtrtrtr

trtrtrtrtr

FOOTAGE:FROM

212.5215.6

231.2236.2

244.5249.5

262.0267.0272.0275.0287.3291.3

302.0307.0312.0317.0322.0

TO

215.6219.8

236.2241.2

249.5254.5

267.0272.0275.0279.6291.3295.8

307.0312.0317.0322.0327.0

TOTAL

3.14.2

5.05.0

5.05.0

5.05.03.04.64.04.5

5.05.05.05.05.0

ftV.AY'j

.,'w.

.001

.001

.002

.001

.001

.001

.002

.002

.001

.001

.001

.002

.002

.001

.001

.001^001


EL-87-9EYE LAKE

24+OOS, 01+60EHOU E NO.

LOCATION

LATITUDE ———————————

ELEVATION ——————————

STARTED Dec. 16/87

397.0'

DEPARTURE

7IMUTH Grid East DIP Dec. 17/87

-45. 5 C

FOOTAGE

0.0

200.0

397.0

DIP

45. 5 043. 0 040. 0 0

AZIMUTH FOOTAGE DIP AZIMUTHHOLE NO. FL-87-9 SHEET NO.

REMARKS PA786868 ————————

SUMMARY LOG

P.I. FogalLOGGED BY

FOOTAGE

FROM

0.0

36.6

150.5

TO

36.6

150.5

397.0

397.0

D E S C R 1 P T 1 ON

SUMMARY LOG

CASING.

MAFIC TO INTERMEDIATE VOLCANICS (FLOWS).


E.G. H.

SAMPLE

NO. bMH ' FOOTAGEFROM TO TOTAL

ASSAYS

ON TARIO C ASSE5

AF

..,

O//HON

EOLOG iSMEN OFF1C

R22..,

OZ/TON

CAL B H T i-ll^

1988

V E t

" : !'.'tV

0

)

DIAMOND DRILL RECORDNAME OF PROPERTY FYF

HOLE NO. .

LOCATION

LATITUDE

EL E VAT ION

STARTED

EL-87-924+OOS, 01+60E

Dec. 16/R7

l AKFLENGTH 397.0'

DEPARTIIB F

AZIMUTH Grid East OIP -45. 5 0F.NISHFH Dec. 17/87

FOOTAGE

0.0200.0397.0

DIP

45.543.040.0

AZIMUTH

'

1

FOOTAGE DIP AZIMUTHHOLE NO. EL-87-9 SHEET NO. ] Of 3

.PA786868REMARKS.

LOGGED BYR.I. Fogal

y- u*ST- jVi

z

vB*7"7

* i•••ZO a O

1•J)UJ

1<

FOOTAGE

FROM

0.0

36.6

p j C- C"- C* oh ci 5 i*, *ir

-•-•^,-r.

TO

36.6

150.5

* .'.'-i'-'^

D f3 L3O "m

* Lf C^ U

Q

DESCRIPT ION

Casing.

Mafic to Intermediate Volcanics - dark grey to dark green, massive,medium grained. Very few quartz veins, typically barren of minera lization. Sulphides limited to fine disseminations of pyrite, intrace amounts.

Modal percent: Amphibole 50-65*Plagioclase -i ?(; ^vQuartz J "- 1"*Mica 3-5*Calcite 1-3*Sulphide trace

11"

1)1

- 50.0' - 52.5' - typical, containing barren quartz vein at51.4' - 51. 7'.

- 57.5' - 59.5' - typical, containing small quartz vein at58.5' - 58.7', barren of mineralization.

- 64.9' - 68.3' - typical, containing irregular zones with alight green feldspar associated with lesserquartz, no apparent sulphides, discontinu ous.

- 69.9' - 73.7' - as per 64.9' - 68.3'.- 77.0' - 87.0' - typical.

- 93.7' - 96.0' - typical, containing barren quartz and feld spar vein at 94.4' - 94.8'.

- 107.3' - 112.2' - typical, with quartz and feldspar (lightgreen) vein, barren of mineralization at109.7' -110.0'.

- 114.7' - 117.7' - typical intermediate volcanic containinga quartz-feldspar vein at 115.1' - 116.2';minor chlorite, barren of mineralization.

SAMPLE

NO.

1247612477

1247?

1247?

1248C

12481124821248:12484

12185

12486

SULPH IDES

trtr

tr

tr

tr

trtrtrtr

tr

tr

FOOTAGEFROM

36.641.6

50.0

57.5

64.9

69.977.082.093.7

107.3

114.7

TO

41.646.6

52.5

59.5

68.3

73.782.087.096.0

112.2

117.7

TOTAL

5.05.0

2.5

2.0

3.4

3.85.05.02.3

4.9

3.0

ASSAYS

r* 1

f, A

f 3

l"

l 5 L1 W k l 06 "

',

V^Y'"'/^~i*y^

OzVVoN

.001

.002

:.001

.001

.001

:.001c. 001.001.001

,., f , i

.66X

^'/24k..f^..~~

OZ/TON

VX/fX7 \- jjl.

DIAMOND DRILL RECORD CYC LAKL

Fi P7 QL L - u f - 7 of 3

FOOT A GT

F ROM

36.6

150.5

TO

150.5

397.0

DESCRIPTION

Cont'd.- 117.7' - 128.3' - interval contains few intercalated tuf

faceous beds up to 5cm wide, typicallybarren, individual lath-like crystals upto 2mm long.

- 133.4' - 148.9' - typical, containing abundant tuffaceoushorizons. This marks a transition zonebetween intermediate to mafic volcanicflows and tuffs. A broad gradational con tact is observed, over a width of approxi mately 30 feet. Trace sulphides as finedisseminations of pyrite.

Mafic to Intermediate Tuff - similar compositionally to 36.6' -150.5', however crystals (laths) of feldspar are visible. Noapparent banding, rather massive. Few quartz veins, up to 5cmwide, discontinuous in nature, containing no visible sulphides.Trace pyrite overall.

- 157.0' - 159.8' - typical, containing barren quartz vein at157.9' - 158.2'.

- 168.7' - 170.9' - typical, increasing feldspar content, to50X, imparting a light grey colour.Quartz S, feldspar vein at 169.1' - 169.4'

- 184.4' - 188.9' - typical, containing quartz and feldsparvein at 187.8' - 188.1', barren of mine ral ization.

- 191.8' - 195.5' - numerous quartz and feldspar-calciteveins, averaging 1cm wide, typically bar ren of mineralization.

- 200.0' - 205.0' - typical.- 210.2' - 220.2' - typical, with numerous quartz and feldspar

veins, averaging 2-5cm in width, barrenof mineral ization.

- 227.8' - 237.8' - typical, lapilli to 2mm long evident.

- 245.0' - 247.6' - typical, quartz and feldspar vein, barrenof mineralization of 245.4' - 245.7'.

- 259.6' - 269.6' - typical, containing irregular blebs/clots

SAMPLE

•10

1248/1248f1248?

1249C1249'1249;

1249;

1249'

12495

1249e

12497

1249E1249?1250C

125011250212502

12504

-.III PH

tot S

irtrtr

trtrtr

tr

tr

tr

tr

tr

trtrtr

trtrtr

tr

FOOTAGt

FROM

117.7121.9124.9

133.9138.9143.9

150.5

157.0

168.7

184.4

191.8

200.0210.2215.2

227.8232.8245.0

259.6

ro

121.9124.9128.3

138.9143.9148.9

155.5

159.8

170.9

188.9

195.5

205.0215.2220.2

232.8237.8247.6

264.6

'i.lAl

4.23.03.4

5.05.05.0

5.0

2.8

2.2

4.5

3.7

5.05.05.0

5.05.02.6

5.0

ASS A Y 'o

,4w,

.001

.001

.001

^ 001.001.001

.001

^001

.002

.001

.002

.001

.001

.002

.001

.001

.001

^001

i ; T .*

DIAMOND DRILL RECORD NAME OF PROPERTY.

HOLE: NO ...E,L-.87-9

EYE LAKt

NO 3 of 3

rooi

F ROM

150.5

ACT

TO

397.0

397.0

Cont'd.

- 272.0'

- 283.2'

- 290.2'

- 301.8'- 310.5'- 329.1'

- 344.8'

- 363.0'

- 377.0'

- 388.9'

E.O.H.

O C SC R 1 P 7 1 0 N

of orange-red feldspar, sporadically dis tributed, averaging 1-3cm across; barrenof mineralization. Slight increase inamphibole content.

272.0' - 277.0' - containing numerous light green feldspar-quartz veins, 2-5cm wide, typicallybarren of mineralization.

283.2' - 286.0' - typical with abundant quartz veins at283.4' - 283.5' and at 284.0' - 285.1'.Minor chlorite, no evidence of sulphides.

290.2' - 295.2' - typical, containing hairline fracturesinfilled with feldspar and lesser quartz.Epidote vein, 2mm wide, at 294.8'.

301.8' - 304.5' - as per 290.2' - 295.2'.310.5' - 313.9' - as per 290.2' - 295.2'.329.1' - 339.1' - typical.

344.8' - 349.2' - typical, containing barren quartz vein at348.1' - 349.0'.

363.0' - 366.4' - containing quartz veins, weakly chlori-tized, barren of mineralization at 363.2'to 364.3' and 365.4' - 365.7'.

377.0' - 387.0' - typical, containing trace sulphides asfine disseminations of pyrite.

388.9' - 397.0' - containing abundant quartz veins, typically Ocm wide, barren of mineralization.

SAMPLE

'!O

12505

12506

12507

12508

1250912510125111251212513

12514

12515125161251712518

f,\n PH iurs

tr

tr

tr

tr

trtrtrtrtr

tr

trtrtrtr

FOOTAGE.

f ROM

264.6

272.0

283.2

290.2

301.8310.5329.1334.1344.8

363.0

377.0382.0388.8393.7

ro

269.6

277.0

286.0

295.2

304.5313.9334.1339.1349.2

366.4

382.0387.0393.7397.0

IN TAi

5.0

5.0

2.8

5.0

2.73.45.05.04.4

3.4

5.05.04.93.3

M. G AYS

W,.

.002

'.001

.001

.001

.002

.001

.001•c. 001.002

.001

•c. 001.001

^001.001


APPENDIX F

LEGEND AND DIAMOND DRILL SECTIONS


LEGEND FOR THE DIAMOND DRILL HOLE SECTIONS

FOR THEEYE LAKE (INC. KOMAR) PROPERTY

Patricia M.D., Ontario

q.v.,c.v. Quartz/carbonate veins

8 Intermediate and felsic intrusives 8a Granite 8b Diorite 8c Granite gneiss 8d Porphyry, quartz/feldspar

Mafic to ultramafic intrusives 7a Gabbro, diabase 7b Peridotite

Iron formation6a Oxide facies6b Carbonate faciesGc Silicate facies6d Sulphide facies

Clastic sediments5a Wacke5b Mudstone, argillite5c Siltstone

Felsic volcanics4a Flows4b Tuff, lapilli tuff4c Breccia, agglomerate

Intermediate volcanics3a Flows3b Tuff, lapilli tuff3c Breccia, agglomerate

Mafic volcanics2a Flows2b Tuff, lapilli tuff2c Breccia, agglomerate2d Amphibolite

Ultramafic volcanics

SYMBOLS Overburden...................^JGeological contact........77—

Bedding............................"^

Foliation...........................r-

Fault, shear zone........

Sample interval (feet) with gold assay in ounces per ton .............wt

Lost core...........................

o/b

(5 — 4

LG

Alterationsi - silicification

se - sericitization eh - chloritization ea - carbonatization

Mineralizations - sulphides

po - pyrrhotite py - pyrite cp - chalcopyrite As - arsenopyrite sp - sphalerite

Ga - galena Mo - Molybdenite

gf - Graphite tour - tourmaline

Fig. 5

VLF EM Fraser Filtered Inphase Profile (%)Vertical Field Magnetic Profile

(x 1000 gammas)

EL-87-lEL-87-2&L. 00

' E.O.H. 297-0'

E.O.H. 3I7-0


EYE LAKE PROPERTY Pickle Lake Area Patricia MD., Ontario

D.D.H. SECTION 0+50 SLOOKING NORTH

Scale r - 40 feet

For legend see Figure No. 5DDJH.Nos.EL-87-142

GEOCANEX LTDTORONTO CANADA

Vertical Fold Magnetic ProfB* (x 1000 gammas)

- 1.5

- 10

EL-87-4—— — — — Surface — -

VLF EM Fraser Filtered Inprtase Profile (S)

75 -

- 0.5- MAG

50 -*

25 -EL-87-3

4E L--0——-I- 5E 6Ei

~-!00

--20O

SEi

9E -J——O -J

•-100'-

-200-


EYE LAKE PROPERTY Pickle Lake Area, Patricia M.D., Ontario

D.D.H. SECTION 11+00 NLOOKING NORTH

KOMAR GRID SECTION

DD.H. No*. EL-87-3 ft 4

m^x GEOCANEX LTD TORONTO. CANADA

BY: RF. /R.TJI.DATE: Nov. 1987SCALE: 1:480

SO1 TOO-

Scale r - 40 feet

For legend see Rgure No. 5

E.O.H. 397-0'

•-300-

3o E.O.H. 477-0'

Vertical Field Magnetic Profile (x 1000 gammas)

- 1.5

- 1.0

- 0.5

- - O

EL-87-68W

l

20O-

7W i

EL-87-56W 5W

i

E.O.H. 317-0'

MAG

VLF EM Fraser Filtered Inphase Profile (y0)

75 -i

50 -

25 -EL-87-5

4W l o -

E.O.H. 307-0

50' 100'

Scale 1" - 40 feet

For legend see Figure No. 5

-~-—————-IOO -


--200

EYE LAKE PROPERTYPickle Lake Area Patricia M.D., Ontario

D.D.H. SECTION 44+50 NLOOKING NORTH

KOMAR GRID SECTION

D.D.H. Nos. EL-87-5 X 6

GEOCANEX LTD.TORONTO. CANADA

BY: R.F. l R.T.M.DATE: Nov. 1987SCALE: 1: 480FIGURE No. 8

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

Venice! Field Magnetic Profile (x 1000 gammas)

l- 1.5

VLF EM Fr*ser Filtered InphtM Profit* f.%)

75 -

MAG50 -


--30O——


EYE LAKE PROPERTY Pickle Lake Area, Patricia M .D., Ontario

D.D.H. SECTION 0+00LOOKING NORTH

KOMAR GRID SECTION

D.D.H. No. EL-87-7

QEOCANEX LTDTORONTO CANADA

BY: RF. /R.T.M.Nov. 19*7SCALE: 1:480FIQURE No. t

• rVertlceJ Field Magnetic Profile (x 1000 gammas) VLF EM Fraser Filtered

Inphuft Profile

i i i i i i i i i i i i i i i i l i

1.5

-•300-


EYE LAKE PROPERTY Pickle Lake Area, Patricia M.D., Ontario

D.D.H. SECTION 20400 SLOOKING NORTH

D.D.H. No. EL-87-8

GEOCANEX LTDTOnONTO. CANADA

BY:R.F.DATE: Nov. W8TSCALE: 1:480FIOURE No. W

O 50' l i , i . l

E.O.H. 327-0

100'

Scale r - 40 feet


Vertical Field Magnetic Profito (x 1000 gammas)1-15

VLF EM Fraser Filtered Inphase Profto (%)

5E

--iOO -

-300-

--IOO -

50* 100-

Scato r - 40 feet


-200-

E.O.H. 397-0


EYE LAKE PROPERTY Pickle Lake Area. Patricia MD., Ontario

D.D.H. SECTION 24+00 SLOOKING NORTH

DDK No. EL-87-9

BDBC&MIEJL GEOCANEX LTD.TORONTO. CANADA

BY: RF. t R.T.M.DATE: Nov. 1987SCALE: 1:460FIGURE No. H

ijgi\5i

NO.

•SAMPLE

•SAMPLE

^^ BELL- WHITE ANALYTICAL LABORATORIES LTD.\^r^ P.O.

4061

BOX 187,

/TT .\t*4-f -

(S) OF: Core (136)

(S) FROM: Mr

l Sample No. 0

1

1

1

1

1

1

1

1

1

1

1

H BfccORDANCt

121123456789

12120123456 789

12130123d56 789

1214012345

* Estimated

WITH LONO. ESTABLISHED

. R. Higgi

z. Gold

TraceTraceTraceTraceTraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTrace TraceTrace1 raceTrace1 raceTraceTrace TraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTrace

NORTH

HAILEYBURY. ONTARIO TEL

firat? of AnnlptfiPage 1 of 2

DATE:

RECEIVED:

nson, Geocanex Ltd.

PROJECT:

Sample No

12146789

12150123456789

12160 1234567 S9

12170 123456789

672-3107

December 17, 1987

December 1987

Lye Lake

Oz. Gold

TraceTrace0.002*Trace0.002*TraceTraceTrace TraceTraceTraceTraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTrace TraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTrace

BELL-WHITE ANALYTICAL LABORATORIES LTD.

.MCRICAN CUSTOM. UNLtOG IT IS i P C C II It ALL * STATED ^^J*~\ ^^^F

HEU| SHEETS HAVE NOT BEfN ADJUSTED TOKAT^VOR LOSSES AND CAINS INHERENT IN 1 H ASSAY PROCESS

COMHEN.THE FIRE f J4g^^

DELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-31O7

lf

LNO. 4061

SAMPLE (S) OF:

Qlerttfirat? of AnalplaPage 2 of 2

DATE:

Core (136)

JAMPLE(S) FROM: Mr. R. Higginson, Geocanex Ltd

December 17, 1987

RECEIVED: December 1987

PROJECT: Eye Lake

1Sample Mo. Oz. Gold

1

1

1

1

1

1

1

1

1

1

1

1 ^CORDINCCMEHICAN CUSTOMTHERWISE COLD(ES^SHEETS HAV

JAltMoR LOSSES

12180123456 789

12190123456 789

12200 123 456 789

12210 123

* Estimated

WITH LONG-ESTABLISHEDUNLESS IT IS SPECiriCAlL

TraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTraceTrace Trace0.026Trace Trace0.002*TraceTraceT r s c eTrace0.008 TraceTrace0.002* TraceTrace0.004Trace 0.016TraceTrace

NORTHY STATED

Sample No.

12214567 89

122201234567 89

12230 1234567 89

12240 1234 567

BELL-WHITE ANALYTICAL

^ __ ^^

Oz. Gold

TraceTraceTraceTrace TraceTraceTrace 0.008Trace0.002*0.002*TraceTraceTrace TraceTraceTrace TraceTraceTraceTrace T r d c eTraceTrace TraceTraceTrace Trace0.002*TraceTrace Trace0.0120.002*

LABORATORIES LTD.

AND SILVER VALUES RI PORTED ON .^^ J^^^i NOT BEEN ADJUSTED TOAND CAINS INHlHlNt IN ASSAY PHOCCSS

COMPEN.THE r IRE /J^^r


APPENDIX G

CORE SAMPLE ASSAY CERTIFICATES

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187. HAILEYBURY. ONTARIO TEL: 672-3IO7

111

"

1111111111111

Qkrttf irafe of AuaUjBtaNO. 0140

SAMPLE(S) OF:

SAMPLE(S) FROM:

S amp le No .

12301231 56789

123101 234 56189

12320

* Estimated

IN ACCORDANCF WITH l ONG -f STAHL ID

Core (40)

Mr . Rob Fogal ,

Oz. Gold

TraceTraceTraceTrace Trace1 raceTraceTraceTraceTraceTrace TraceTraceT r ace Trace0.024TraceT raceTraceTrace

HfO NORTH

DATE:

RECEIVED:

Geocanex Ltd.

PROJECT: E

Sample No.

1232123

b6789

123301 234 56789

12340

BELL-WHITE ANALYTICAL. __ ---7

January 6, T988

December 1987

ye Lake

Oz . Gold

TraceTraceT r o c en . o o 2 *0.002*TraceTraceTraceTraceTraceTrace TraceTraceT r o c e TraceTrace1 r a c eTraceTraceTrace

LABORATORIES LTD.

OTHrPWI'.f GOLD AND 5.ILVIM VAillf;; Mff'OMTrD ON s^SJS ^^~***^ IHIsr MltlTS IIAV1 NOT litIN AOnlMI.D lo COMPIN. /S^^ .^P^*^^ SA1E rOH LOSSES AND GAINS INIILHINT IN THE FIHt S-jK——^l'^^^

AbbAV PKOCrsi. ^-^^S^C*^^

1 JB1 Vi

^ BEU.VVHITE ANALYTICAL LABORATORIES LTD.••^ ——————— .1. .11.1 K l' ————————————————————————————————————————————————————————————————————————————

^^^ P.O. BOX 187. HAILEYBURY. ONTARIO TEL

(Crrtiffrat? of AnalgaiBNO. 4008

| SAMPLE (S) OF: Core (67)

. SAMPLEBB

1

1

11

1

1

11

1

1

1

1III ACCORDANCIAffTHICAN CUtTOMOTHtftWKI GOLD

(S) FROM: Mr. James

Sample No .

120456789

12050123456789

12060123456789

120701234567e

* Estimated

WITH LONO'tfTA*LliH(D NORTH. UNLII* IT II irtCiriCALLY (TATCOAND *H.VIN VAlUtt KtrOXItO OH

Pierce,; ,, '

Pt Cold

TraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTraceTrace0.002*TraceTrace0.020TraceTraceTraceTraceTrace

i 672-3107

DATE: December 11, 1987

RECEIVED:

Geocanex Ltd.PROJECT:

Sample No.

1207912080

123456789

12090123 A56789

12100123 456789

121102

'

,

•CLL-WHITt ANALYTIC^-**o yy.^^r JS^

December 1987

Eye Lake

Oz Gold

Trace0.002*TraceTraceTrace0.002*TraceTraceTraceTraceTraceTraceTraceTraceTrace TraceTraceTraceTraceTraceTraceTraceTrace0.002*Trace TraceTraceTraceTraceTraceTraceTraceTrace

AL LABORATORIES LTD.

THIK (NlfTI HAV1 NOT IICN ADJUIUD TO COMFIN- ^'^5f ^.^^'•flk f on koittt

1

AMP OAINf INMININT IN TMt r mlAIIAT PNOCtll. ffj^^^&rfi*"*^^

1 4^^

i JgPE

•m BELL -WHITE ANALYTICAL LABORATORIES LTD.V^y P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-3IO7

Qfcriifiratr of AnalpteNO. 4007

1 SAMPLE(S) OF: Core (44)

I SAMPLE(S) FROM: R. nigginson, Geocanex

1

1

1

1

1

1

1

,

1

1

1 re^

IN HcCORDANCrAM^CAN CUSTOMbrnEBWISE COLD

Sample No.

120012345 6789

12010123456789

1202012

* Estimated

oSt/ecd ' .

WITH LONrt ESTABLISHED NORTHUNLESS 11 IS S.PECIMCAI.LY STATtD

AND SILVEf* VALUES REPORTED ON

Oz Gold

0.002TraceTraceTrace0.002* 0.002*0.006TraceTraceTraceTraceTraceTraceTraceTraceO.OORTrace0.0060.006TraceTraceTrace

DATE: December 11,1987

RECEIVED:

Ltd.

PROJECT: Eye

-

Sample No.

120234567 89

12030123456789

120401234

December 1987

Lake

Oz Gold

Trace0.0080.002*TraceTrace TraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTraceTrace0.010TraceTraceTrace

BELL-WHITE ANALYTICAL LABORATORIES LTD.

^-tSlIHISf SHEETS HAVC NOT BEEN ADJU&TCO TO COMPCM. ^^^ ^^^^^^BATE.tOB LOSSES

1

AND CAINS INHERENT IN THE TIREASSAY PROCESS /^r^j^L^U&^E^^

Pv* ^^^^^^^^^^^fisr . . . , . . . .

I^SJHL BELL- WHITE ANALYTICAL LABORATORIES LTD.iiSSSr P.O. BOX 187. HAILEYBURY. ONTARIO TEL: 672-31O7

QJrritfiratr of AttalgataNO. 0114

JsAMPLE(S) OF:

— SAMPLE(S) FROM:

1

1

1

1

1

1

1

1

1

1

1

1

l,/

Core (28)

Mr. James

Sample No.

122489

122501234567 B9

1226012

1227789

122801 2345678 9

* E st i m a t

DATE: January 5, 1988

RECEIVED: December 1987

Pierce, Geocanex Ltd.

PROJECT: Eye Lake'

Oz. Gold

Trace -0.014-TraceTrace -Trace-Trace *0.002*Trace*Trace -Trace- Trace-Trace-Trace-Trace-Trace-Trace .0.012-Trace-0.016v0.002* 0.024'Trace-Trace*Trace'0.002*Trace'Trace ' Trace *

ed

IN ^•tCCOnDAMCf WITH I.ONG-tSTARLISHrD NORTH*M||ICAN CUSTOM. UNLES? (T IS iPfCIMCALLY STATEDOTHtfiVVISE GOLD AND btLVfft VAL Utb REMOftftD ONT Mf SE t M f C T S HA^L' NOT li LIN APJUSH.D TO COMf't N-

ATE f OR LOSSES AND OAiNb INMtNtNT IN T H t FINE•j AS&Ar PNOCC&S.

BELL-WHITE ANALY LABORATORIES LTD.

1 111l11111111111111

t

OU.h;,;..

Receive-:

Submituv i. 1,

Pro j ect :

Sample No.

12450

12451

12452

12453

12454

12455

12456

12457

12458

12459

12460

12461

12462

12463

12464

12465

12466

12467

12468

12469

l/

GEO-77/

Geocane

EYE LAKE

Auoz/ton

.001-

.001'

^001.

.001 .

.001 -<.001 .

.002 '

.002 '

.002 '

.001 '

.001-

.002,

.001'

.001'

.001-

.002-

.002-

.001-

.001-

.oor

7262

x Ltd.

Sample No.

12470

12471

12472

12473

12474

12475

12476

12477

12478

12479

12480

12481

12482

12483

12484

12485

12486

12487

12488

12489

69

Auoz/ton

.002 -

.002'

.001'

.001'

.001 ,

^001 t

.001 '

.002'

^001 .

.001,

.001 .

^001-<.001 .

.001 '

.001'

.001'

.001'

.001'

.oor

.001'

Sample No.

12490

12491

12492

12493

12494

12495

12496

12497

12498

12499

12500

12501

12502

12503

12504

12505

12506

12507

12508

12509

j

J . va,n

,,,,,,3^,

December 31, 1987

Drill Core

Att'n: Mr. H. J. Hoclgec. c. Mr. J. Adams

Au Auoz/ton Sample No. oz/ton

^001, 12510 .001-

.001' 12511 .001-

.001' 12512 ^001-

.001' 12513 .002'

^001' 12514 .001-

.002' 12515 ^OOr

.001- 12516 .oor

.002' 12517 *:.001-

.001- 12518 .001'

.001-

.002-

.001',

.001-

.001.<.001''

.002'

<.001 '

..001")

\QQ1'.002-•1

I^-Jt t <^f^.^f^'^J} L- JKii 1 f. l i

s'

' ' l !

Engelen Mgr.

•^ ^EHRfcSENFATION

f1i:

S*

ItiflCiili: i .

O(;K- :.

M GubmiMu-i i ,

Pro i e c t :

Sa

1

1

1

1

1

1

1

1

1

1

1

11

mp le No

12401

12402

12403

12404

124051240612407

1240812409

1241012411

12412

12413

12414

12415

1241612417

12418

1241912420

ASS; ; ,:nc;n/.

GEO-76/02

Geoc ane x

EYE LAKE

Au oz 1 1 on

.002-

.002-

.002.

.003.

.001 *

.002-

.002-

.001-

.001'

.001 '

.002 '

.001 ,

.001-

.001 '

.003 -

.004 '

.001 -

.004 '

.001 '

.007'

X7262

109

Ltd.

Sample No.

12421

12422

12423

12424

124251242612427

12428

12429

12430

12431

12432

12433

12434

12435

1243612437

12438 12439

12440

;. , u;j:M9-35?/

December 31, 1987

Drill Core . ... . ...... _ ..., _ ....

Att 'n: Mr. H....J. Hodgec . c . Mr . J . Adams

Au oz/ton Sample No. Au oz/ton

.002 - 12441 .003 -

.001- 12442 .003-

.001- 12443 .003'

.001- 12444 .001'

.001- 12445 .001*

.001 - 12446 .001 -

.001 - 12447 .001 "

.002 ' 12448 <.001 '

.001 ' 12449 .002 '<.001 /

•C. 001 '

.001'.

.002-

.001'

.001'

.001-

.001-

.002- ^^

.002- --^ f

.002 .

1 7 S yi^.M^y^lTED S

t'— 1 i

J . va'n Erfge len Mgr .: v HfPMtSENTATION

1 1 11111111111111111

Certificate No

Received

Submition ir,-

Project :

Sample No

12341

12342

12343

12344

12345

1234612347

12348

12349

12350

12351

12352

12353

12354

12355

1235612357

12358

12359

12360

x/

GEO-76/01 77262

Geocanex Ltd.

EYE LAKE

Au oz/ton

.002.

.002 -

.002-

. .002-

.003 -

.002-

.003 '

.002'

.003-

.003-

.004 -

.003-

.003-

.003-

.002-

.003-

.002 .

.003-

.004 .

.003'

109

Sample No .

12361

12362

12363

12364

12365

123661236712368

12369

12370

12371

12372

12373

12374

12375

1237612377

12378

12379

12380

- '!

Au oz/ton

.001 v

.002,

.002'

.004-

.002-

.003.

.001 -

.002 .

.004-

.004 '

.003-

.003.

.002- ;

.002-

.001-

.002'

.002.

.002-

.002-

.002'

J . van

•it (116)239-3527

Decembe

Drill Core

Att 'n: Mr. c .c . Mr.

Sample No

12381

12382

12383

12384

12385

123861238712388

123891239012391

12392

12393

1239412395

1239612397jU*98"~~

^'"""' 1239?

12400x-;/' s'•^7*

s

Enge l en Mgr

r 31, 1987

H. J. HodgeJ . Adams

Au oz/ton

.002-

.001 '

.002 *

.002*

.001.

.001-

.003-

.003'

.001'

.002'

.002 '

.002 .

.002'

iOOL

^002-

.003'

.001 -~) .002'

.001'

.001-

s

m

i Hi ^HfSFNIATION

EYE LAKE - LIST OF CLAIMS

Pa 769379 778970 778972786837786838786839786840786842786844786845786846786847786848786850786851786852786853786854786855786856786857786863786864786865786866786867786868786869786871786872786873

Credi

MP

^

ts Requested

60 Pa606060606060606090906060606060

100120606060606060606060606060

115

,^^^5/yX^\^- ^-V0\ f*As*. \^^*\ N j\flSfkî1 fiV- 1 ' '~N ^* Mi Vk' o;-' vK f- A \"n^7 tf/vx ^-Vvv Vv-, ^" v -7

964911964912964913964914964915964916964917964918964919964920964921964922964923964924964925964926964927964928964929964930964931964932964933

(l*

Totalw

Credits Requested

202020 ,2020202020202020202020202020202020202020

xÊB*\f g? x^/^N/ \î i j^ ^' \|^^.E 5/vv^— v/x^r^x

Total: 54 Claims

,--.KTp- Credits: 2,^35 :i:Jj^X -••"" -

/. ,'71:' .

i -

P ol 726BC8 l

Pol 7?C - 067ll - i ;-'"'-'.

•n/'.. lykarr. j^, l ^ O j ^0 7;,,r, l

P"

S

l""V""tpT-

J\

l \ i l

. Pa ,: Pa '76'9435 769446 ' Po ' j p 0 l i' 1*18/6707 '48C

] l/ l

v (466709 1486710 PO ? , i

(Pa 406719

©i-i .-" |Po -^~J...™- - T-Vt.i,O9?,OiCbO9a-* i Pa'•••lt: 'iO(.Mtt loogire e:.09J?

e -f] [ ,^,rt j**};**' j /".l*. l;

4---v---1..-^. j.;__i--.-..J'-^ .j /' ^ i\*W '83059? '^ ^30590 , 7 :61 43G | 7a69445 'lP?^f^;.f6 |pr--

I 'j . l l' l V769/447! t. I 1 486720

M ei l

|Po Po9" .'80? BO ?96I 1802960 l','

962

•T,::-.~-

Pq-

.'802959,

•X ',830529 1771440 1-771/1,0 'Po\ l pa l Po \)pa l Pa - ' Pa\1 'j 1771439 1 77\437 j 769437 l 769444 ) | 7 g9 ,,,, 8 . 769^455 J 76945 7; v^xj- - -\ ~ — — - . l i i i /i ; i

c l Po Xri l Po? 1830534^(1^77144

Po

.p.—t—-'—i--J1 830576] f

M N B;L4. L- (J ^\\(P rO v[4 r-)C

*Vi G } f" fy w

--l; ..J--." J77I44I \77l438lpa |(7aX l pa

\ j l 769438/1" 7 ''f'69443 ]7C9449 176 9454 1769458

L|77I443 77 |444 \ 77i^ Po ,| p a ,pa | ./pa |

. , l 7694 -1769442 7694501 769453 iPol \ l -3V l ' j |t69

.p~o ~lfa""""~-rP7n—Li----I---u-—.j/^1830587 ,830r,86 l 7 7i4|Pa ' l Po P Q l P" '' l Po l ^ ^^]769440| 7G944I | 769451 769,'452

^ S /'

•-recttfo '

iPo830^- 589

'-H^"^-!-- •r1

— l—Pa

ftSOete l 86O6+0 l 6&O6+4 l 8-5661-3 | 86

~~l Pa

-:'.' Po \

l2l 8650'64 ^

Lf'ff 0 'i —^-"iL jj^0^ —— —— —— — —— --—— —c —— —— —— —, - . ., .

__V-— V-^l"' 4,3.1 i L,.^ l^^l^ee^^-^we-l^ l , .^ l—— H-— -- — —l— — —l— —— — —-i.—j-—|Po

" ; ft 4,so) f( Mzy ^(^^^^^11^1^1.1 l±-L*4 If -J J

8508 .-49 l ' '

* 4650...-: l l.

r^jjrt70 IT^JI.' ^^j r^^iwy | 850857 l

850853 1/850850 |

---^1 __ ____ l Po \ (Po j 850852 '^ j B5085I *~'903^ X 19.-T53526|90352 ;.7

y"525 j \ * \

786857^1786856 . j 766655;

--X----^--J-^-----t---'""V0 7 '^4V47I

pa .7/86852 l 786

i CB rio;; \ ^—— :-K——T^."" "" TP"? ~~.S~ — ~ 769379 786848 |786847 | 78684'6

787357/78734.^B Jc

U--J—-____^'Po |Po i pa if '776219 , 785840 J 786839 X

f7G?\7!\ (765069 I78f,860

i ^.. ~. ^., ~.. .., ^., ^.j . \ ,, _ ^, -L- ^ , t i, ,: . [ . ... ....,. ... .,. ...^' ..-rk""" |Pf' IPO " " i \"F; O~" "" TP'C "' "" ]po"y i pa IPO j

r ..--V.|y-\ y ly-,4 -5V j 7874.10 | 78YiV-8 l \7Ht87l l 78611/2 /j/tiStt/Ti 769?0-l | W.iSf'l. j

: i'-". ; .i (N {K'-'"^ r'" ' i"-- .....! ! N ! /'""''^./' l ! .'i

Onlatio

Minist.yol RcportS'BoCUMENT No.Natural f iMn JLnesources T V'v'880^' III

Name and Postal Address of Recorded Holder

Explorations Inc.BsoasNEeeae 39 DONA LAKE

.__________S l1003-34 King Street East, Toronto, Ontario, M5C 1E5

Summary of Work Performance and Distribution of CreditsTotal Work Days Cr. claimed

3,093nlng Claim

Number

for Performance of the following work. (Chock one only)

Q) Manual Work

[]^]shalt Sinking Drifting or other Lateral Work.

| | Compressed Air, other Powor driven or mechanical equip.

Q Power Stripping

r~) Diamond or other Core drilling

| |Land Survey

ttached She(

HIO OEOtOGlCAl SSE5SMENT--T

E-G-E-4-V

Work Days Cr.

SURVEY IttS

P D

Mining ClaimPrefix Number Days Cr.

Mining ClelmPrefix Number

Work Days Cr.

All the work was performed on Mining Clai U 786856, 786855, 8508.4, 8508"55, 850846, 786864, 786869, M -786868_____:___________________'___'

Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)^ "* \ t '~ - ~~"

Drilling Contractor: Midwest Drilling, Winnipeg, Manitoba -"'-.'O- -' 7

Core Size: BQ 1-7/16" ^ , 7Ci -jp*^ 't*~- V l ^Zrr

Number of Holes: Nine (9)

Footage: 3,093 *ttf*~ \tf/

Geologist in Chfarge: Robert I. Fogal, 1543 Marentette AvenueXFlrtdspr;, On

Dates: November 23, 1987 tj/êtîêr/^fi,, 1987

Certification Verifying Report of Work \j\'.

89o*-t" ~ 263^

4E4

^Sx.Date of Report Recorded Holder or/\gent (Signeture)

4——————————————x: 1 i ' -ii \uy^————————————————1|-;——vi——l hereby certify that l have a personal and IntlmateicoQy'*^'8 Ojf^H'^'acti let forth In the Report of Work annexed hereto, having performed-*he work or witnessed same during and/or after It* completion and the annexed report l* true.

Nnrne and Postal Addiesf o( Person Certifying

II.J. Hodge, 1003-3A King Street East, Toronto, Ontario, M5C 1E5Date Certified

Table of Information/Attachments Required by the Mining Recorder

Typo of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other powor driven or mechanical equip.

Power Stripping

Diamond or other coredrilling

Lnrirl Survey

Specific Information per type

Nil

Type of equipment

Type of equipment and amount expended. Note: Proof of actual cost must be submitted within 30 days of recording.

Siflned core log showing; foolngo, diameter of core, number and angles of holes.

Namo and address of Ontario land surveyor.

Other Information (Common to 2 or more types)

Names and addresses of men who performed manual work/operated equipment, together with dates and houri of employment.

Names and addresses of owner or operator together with dates when drilling/strippingdone.

Nil

—— — VjAttachments

Work Sketch: those ere required to show the location and extent of work In relation to the nearest claim post.

Work Sketch (as above) in duplicate

Nil

7GH (HI '31

LLI

o

l , ....^—^

L 60N

L40N

L20IM

KOMAR GRID SECTION

LOO

L20N

LEGEND

Surface projection of d lomond drill ho'e ..

Go'd in OZ/ ton —...

In *ervo ! in feet ——O 053-0

8, f- ig No. o' Section dr

DRILL HOLES ! TO 9 PRE^'XED EL-87-

O IOOO li ill-

20OO 3000

LOO

L 20S

L32S

UJ

-iUJCO

OD

LU t\J CM



PLAN OF DRILLING 1987

GEOCANEX LTD TORONTO. CANADA

DATE: JAN. 88 SCALE: I/I2000FIG. No: 4

AFRI PROJECT

HOLD QAFO#:

AFRI #:

ITEM:

uufc {PT

///r/

Y L o( l- (f c /C(2 c

Date: JrT. c Indexer: { ),., ( Supervisor: /'

RESOLVE

Date: Authorized by:

90 0 lb 40' OO

r w

Mccullagh Twp i

_ _ — J

Komar Property

Dona Lake Discovery

PROPERTY LOCATION

LU UJ UJ

Alders,

cedars ,

* T

Black spruce,

muskeg\\\

Open spruce, muskeg

- X

96491 5

Black spruce,

muskeg

\

X"

V

muskeg t ' X l boulders on )

y | sand S\ Spruce on Y. -l ysand boulder'

7

^X ^

) ^^^

Spruce, muskeg,

f boulders on

sand

7

x

"JMU UVAJIUCI i

Xridge l 1

}X 96 49l9x-

xx

l:\ J ^*

Spruce, muskeg

\

l

/ Open spruce, ,

l muskeg

jfc-

7l Spruce i birch '

, on sand \

Spruce,

muskegs

X/

X l A

x/

Open spruce,

muskeg

l

l \964932\

/ Spruce,muskeg r7 on sand and j" S

7 hnnlHpi-c ' \/

Spruce - cedarf' j a|ders,swamP

Spruce,muskeg on sand and boulders

96 4927

/\ Cedars* spruce

Open spruce, - muskeg -

64925

Spruce,! cedar, t alder swamp

•it

\

Spruce, poplar,

l-f

Open spruce

muskeg

\ cedarsl/

X\- 7

\ Spruce, muskeg and boulders

\ on sand

\ }

\ 4^r t ~ ^r \ *9 64924 c^ \ Spruce, muskeg,

X

Spruce, muskeg

\ Spruce, muskeg

Open spruce, ;

muskeg ; 9 6 4 9 l 2

-7-Spruce, muskeg

Mature spruce, poplar

on sand-gravel

77

y ^j Boulder - L 'sanj '"—' X

v sand ridge'

X"" W/ l ^ ~ Spruce - alder

Open spruce, muskeg

964918

7Xedar-alderX

tamarack \swamp \

X ja Spruce, \ .it \ muskeg. f. ^x

\- X* -~^ \ ^\ .,,

9649IIy Open spruce,tamarack,

/' swamp

Spruce,

muskeg

4917

l Cedar

/-tfe-

.SMomp \_i^, •~^^*\

\

Spruce, muskeg

Cedar-alder-spruce ^ swamp

\Boulder , \ sand \

\ \ hl"

X. x^

\

\ *A

. 964916 J^ :vh /\. Ooen grassy boaV. J ^V?*- "'.Q\

-^*-.^-^7l\*fX \

^ fe /: —-—"—-^ j i jt ,y~b ^

Spruce, muskeg

\

V *. x

7

l xcedars l

———f

//

96 4^933 Vi

muskeg 7-9-6 4930 /

s *- Open spruce,tamarack, /muskeg *

/

y Itf-

Spruce and birchover sand a boulders

/9 6 4 9 2 6

//

Spruce, muskeg on sand

//

850846

Spruce,muskeg on sand

Open spruce, lmuskeg

A

z.

Sandhill

~-Cedar-alder- -^

.32 spruce swamp i-

1203-

y

/

96492/2l /Cedar-spruce, j s tamarack

9649211 Sand-boulder

^ ridge

3d,4c

Spruce, muskeg

-———^^-^^--^-I204-5 /,-.â ^

•J Sand hill

/3a^l207-IO

V * "-^ jt 7 Kx Spruce-tamarack, ^-^/^ X

, ^\ swamp _^^Û1 ^x Y ~^-u—^ -^ .. v - - -v * -

Cedar-alder \ X^ \ X

jfct

Spruce, muskeg

/

\

1209-10 s X

\ - spruce^ \ ^ î\ swamp )

\

JU- X

y it \

Spruce, muskeg

LEGEND

QUATERNARY

Stream, lake , bog deposits Glacial, glaciofluvial lacustrine sediments

LATE PRECAMBRIAN (Keeweenawan?)

Ma Diabase

EARLY PRECAMBRIAN

Intermediate and Felsic IntrusivesI0a Granite pegmatitelOb AplitelOc Granite

kgMMM

10* Ouorti monmite(Of GranodioritelOg TrondjemitelOh Quartz dioriteIOJ Diorite10k Unsubdivided gneiss10 l Granite gneiss

Mafic Intrusives9a Unsubdivided9b Gabbro9c Leucogabbro9d Plagioclase-phyric gabbro9e Peridotite9f Pyroxenite

Iron Formation8a Oxide facies8b Carbonate facies8c Silicate facies8d Sulphide facies


KOMAR PROPERTY Dona Lake Area

Patricia M.D., Ontario

GEOLOGY

GEOCANEX LTD

BY- RTMDATE: July 1987SCALE-

WG. No: 2

Chemical Metosediments7a Chert7b Calcitic marble7c Dolomitic marble

Clastic Metasediments6a Clast supported conglomerate6 b Matrix supported conglomerate6c Oligomictic conglomerate6d Polymictic conglomerate6e Sandstone, unsubdivided6f Wacke6g Arenite6h Mudstone, argillite6] P*W***t*ic wacke6k Feldspathic arenite61 Quartz arenite6m Schistose rock ± amphibole,! biotite,

± garnet, ± chlorite of probablesedimentary origin

Felsic and Intermediate Subvolcanic Rocks5a Unsubdivided5 b Quartz-feldspar porphyry5c Quartz porphyry5d Feldspar porphyry

Felsic Metavolcanics '

4a Massive f me-medium grained flow4b Pyroclastic breccia, tuff breccia4c Tuff, lapilli tuff

Intermediate Metavolcanics3a Massive f me-medium grained flow3b Flow breccia3c Pyroclastic breccia, tuff breccia3d Tuff , lapilli tuff

Mafic Metavolcanics2a Massive fine-medium grained flow2b Amygdaloidal flow2c Variolitic flow2d Pillowed f low, pillow breccia2e Flow breccia2f Medium-coarse groined flow centres2g Plagioclase- phyric flow2h Amphibolite2i Co-magmatic sills, dikes2j Pyroclastic breccia, tuff breccia2k Tuff, lapilli tuff21 Chorite ± amphibole schist

Ultramafic Metavolcanicsla Massive fine-medium grained flowIb Spinifex textured flowle Talc-carbonate

± magnetite ± amphibole ± serpentine i chlorite schist

SYMBOLS

ShorelineCreek, showing flow

Swamp

Beaver Dam

Break in slope

Claim post, line,witness post

Township line

Trench, pit

Diamond drill hole

Highway, bush road

Power transmission line

Outcrop, outcrop area .Geological boundary , observed,

y 2a..... \.--2a' ^r'""r'^ r...

x x x

IT ^50857Open spruce,

tamarack

\ x y '" 2ax

Jqv -.2d' -1212-90 "' :(l

x field y850856

\ ^\ Spruce,

2d y tamarack,- O

2a,

y

yyy X ^

\ Cedar - spruce j ^ \ tamarack ' Spruce, \ s*amp j muskeg \ ^ ^ ;

\/- - . \ ^±

'3a-

\

xX

X

Mature spruce foresti ^

.y y

x :y

y Spruce, muskeg

Spruce forest

\ XX"

50855\

Sand hill7 y

X xa

Open spruce, muskeg

-/-^^ X^ ^ Cedar, alder, ^

* s P ruce . s^mP 903528J&L JL M.

X x— . . . . n. , . . . i . . .Vjt \ X

K — T"

Spruce, muskeg n~ — - -^ ' hill )

X X

xX

-r-4L

1213-95.1214-IO-1215- 5'

V..2a

I236-5-2d^-^2d \ Boulders

xô1*,*,.*- z'qv

y -f-' 2d

Inferred, inferred from geophysics.^- ———G—G

Surficial feature boundary..... ..--———----'

Rock sample location S number . . •I750IAssay for Au(ppb), Ag(ppm) -I3-0-6

Pillow;tops known, unknown ... -du -Q- Bedding ; inclined, vertical Hj— .4-.Foliation, cleavage;

60 vX .x XInclined, vertical, unknown r r r

Gneissosity, incl , vert, unknown. f ( t

Lineation , plunge ———^ 7060^ ^

Fracture, inclined , vertical . . ..

Shear zone , dip .. ~^

Shear fracture; inclined,vertical. c

Fault zone, dextral, sinistral ^ Anticline , syncline, plunge . -i- — -L.

Drag folds with plunge /7 6

Dyke ; width , dip 2

Vein, width,dip, quartz, carbonate Glacial striae

ABBREVIATIONS

t^-1216-TD" -I2l7-t5

2dWf*

2d

XX

x

-J—^

x^

x

x x x Spruce,poplar on boulders

X

50 4CaX

x

^

7

-/.

X

\Sand ^, h,ll f \

jskL

850849

Cedar,alder swamp ^ /

Spruce , muskeg, /

Open spruce,tamarack J*--Jfc. 4.

x tamarack7. I di. A

bpruce l ,forest '

muskeg/\ Spruce, t

i muskeg

^y

^

t

77

XX N

xmuskeg

, ^ jt/Open spruce/j S Cedar 7 muskeg \/* *' * i

X*x' Open spruce, '*~ swamp y | -j

^

60

i9a qv.cv

Spruce, poplar, i birch X

Silicification SIL, silSericitization..... SER.serCarbonatization CAR,carChloritization . CHL, chl

X l strong weak

Pyrite pyPyrrhotite poChalcopyrite cpArsenopyrite aspSphalerite. sphGalena gaBornite brMalachite malGraphite grChrysocolla chry

MagnetiteLimoniteHematiteMolybdeniteGruneriteSideriteDolomiteAnkeriteGarnetEpidoteTourmalineXenolithMyloniteShearingCarbonatized

\ \

,4\Alder \ swamp'

l ' l ^ /'

903526± S

/

MX S yy

. 7

.felder y7V *i '

S tr* Zy /

xy7

x x

x x x x

Cedar * ^

jTTAAOpen spruce,

muskeg |7

' 2a,ia

^2a .-it 2d

l228-<5s .1229-5:

2d /.- \2a.v ^. 3Qy.::: M

muskeg on 0 - ^sandhill t SprUC6 ' \

^50 8 5 4)- tamarack. ^/t muskeg ,

. . r . . !

7 Open spruce, i ^^ -^ . , ra.-A"^ tamarack, y

.muskeg X

xx 8 508|53X Spruce,muskeg L

X on sandhill

^

Xx x

Ôpen spruce,

tamarack

/"

-A

\

l

Spruce, muskeg Marsh

X J

850850

1220^5

Open spruce, tamarack y

7d*- /Spruce,

y muskeg

\Spruce, tamarack,

\\

1231-5-0 41232-10

\

Spruce , muskeg

— ' —— r -——

\

\

Open spruce, tamarack,muskeg

^^î

7j _ A.

/

/' 4fc— -A- — —— ~x

———————————— —— . —— ——

—— y ~^^k7 '^^^Ceddr

/

Spruce, 3a muskeg

1222-25'——'1223-6301224-15

2 1225-100

1230-5 I234-K5

i/ , . 7. i

y 77 Spruce,

muskeg

77 75

XX ^

Â S

x 7

X7 muskeg \ /Mature f

f y spruce 7

850851 yX

7

7

Spruce, muskeg

x -^jL.X

A- / Xy

/./

~^ ^. y

cc :'-;. 2a,po

Grassy tamarack, ^~ marsh ^

00

2d,

1000

FEET

Floating l bog l

39 DONA LAKE 20(3

80 N

76 N

72 N

68 N

64 N

60 N

56 N

52 N

48 N

44 N

40 N

36 N

32 N

28 N

24 N

20 N

16 N

12 N

8N

4N

Ul

L. 8 S

L 12 S

L 16 S

L 20S

——— i--. — Tl

L 79 N

L 76 N

L 72 N

L 68 N

L64N ] r ~~-~J

L 60 N

L 56 N

L 52 N

L 48 N

L 44 N

— —-l — — -— —.f _ _ _ ***M , \ _ _ _ _ -ami*

. . ^ __ __ Tina l ~/ 7

——— ——— ——— ——. ___. 7M*U /

i__ t ^ i \~ '— —— — —— ivwn ——a— J—— —— —— —— ;__ __ __ __ nun J

LEGEND

O O

O O

Lafct thor* iff— — -*- _.Cruk — — —

Swamp t' ,

Claim lint -———"~ ——"

Claim post B

B* (ascumtd)

UJ Oo

39 DONA LAKE 210

VAN HOfWE QOLO EXPLORATION MG.

EYE LAKE GRID

GEOLOGY

OiOCAJCX LTD

39 dona lake 010 - ontario · 39 dona lake 010 diamond drilling area: ... 1 r 4mi toronto, canada....

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