52G15NWei79 52G15NWM79 SIXMILE LAKE 01052QISNWt179 S2G1SNWM7S S IXMILE LAKE 010C

II.

III.

IV.

V.

VI.

VII.

VIII.

IX.

x.XI.

No,

TABLE OF CONTENTS

I. INTRODUCTION,

PROPERTY, DESCRIPTION andLOCATION. ...........2*3

ACCESSIBILITY, CLIMATE,LOCAL RESOURCES . . . . . . . . 3 - 5

HISTORY ............5-7

REGIONAL GEOLOGY. . . . . . . . 7 - 9

LOCAL GEOLOGY . . . . . . . . . 9 - 11

EXPLORATION PROGRAM . . . . . .11-24

GEOLOGY . . . . . . . . . . . .24 - 29

COSTS . . . . . . . . . . . . . 29

SUMMARY and CONCLUSIONS . . . .30-33

RECOMMENDATION: 33 - 34

REFERENCE MATERIAL. . . . . . . 35

EXHIBITS

No. No. NO. NO. No. 6 No. 7

2345

General Location of Sturgeon Lake AreaClaim Group.Sturgeon Lake Area Claim Group SL-3.Supplementary Geophysical Information.Preliminary Regional Geological Base Map,Assay Certificates.Geological and Surficial Information.Staking Activity and Group Holdings.

* * * *

52G15NW8179 S2G15NWM79 SIXMILE LAKE 01052G15NW4179 52G15NWM79 SIXMILE LAKE

010C

No.

No. No. No. No. No.

TABLE OF CONTENTS

I. INTRODUCTION. . . . . . . . . . l

II. PROPERTY, DESCRIPTION andLOCATION. ...........2*3

III. ACCESSIBILITY, CLIMATE,LOCAL RESOURCES . . . . . . . . 3 - 5

IV. HISTORY ............5-7

V. REGIONAL GEOLOGY. . . . . . . . 7 - 9

VI. LOCAL GEOLOGY . . . . . . . . . 9 - 11

VII. EXPLORATION PROGRAM . . . . . .11-24

VIII. GEOLOGY . . . . . . . . . . . .24 - 29

IX. COSTS . . . . . . . . . . . . . 29

X. SUMMARY and CONCLUSIONS . . . .30-33

XI. RECOMMENDATIONS . . . . . . . .33 - 34

REFERENCE MATERIAL. . . . . . . 35

EXHIBITS

23456

No. 7

General Location of Sturgeon Lake AreaClaim Group.Sturgeon Lake Area Claim Group SL-3.Supplementary Geophysical Information.Preliminary Regional Geological Base Map,Assay Certificates.Geological and Surficial Information.Staking Activity and Group Holdings.

* * * *

"— —— ————"—————~~~——— JbnnMHim Jfouf&ti fc

1^__INTRODUCTION

This report considers the exploration

program conducted on the 48 claim SL-3 g :pup of

BJ ~on Petroleum S Minerals Limited near Sturgeon Lake in northwestern Ontario in late 1969 and early 1970..

Visits to the general area were made by the author during mid-November 1969 upon completion

of the aerial geophysical work carried out under contract by McPhar Geophysics Limited. During early-February, however, the author conducted sufficient personal inspection to satisfy himself

that the staking was completed in accordance with the regulations of The Mining Act and he inspected the line cutting program in anticipation of further ground work requirements.

Upon the completion of the line cutting and ground geophysical surveys/ a contract was

awarded to St. Lambert Drilling Company Limited

of Thetford Mines, Quebec, for diamond drilling to test and evaluate the anomalous zones indicated

by ground and airborne geophysical surveys. The drilling program commenced in mid-March and

terminated in early-June 1970, drilling however, was suspended for "break-up" from mid-April to

mid-May.

- rf

r-* SECTION r.jnj.-To

F ^ B- l ^ 5

NOV 3 01970r M7i8iO)l(Wil2,l,?,3,4,5,0

EXPLORATION REPORT - BISON PETROLEUM l MINERALS LIMITED

SL-3 CLAIM GROUP,

STURGEON LAKE, ONTARIO.

November 2 5th, 1 970.

W. B. Bleikeman, M. Se. ,Geologist,

CANADIAN JAVELIN LIMITED

- 2 -

II. PROPERTY, DESCRIPTION and LOCATION

The JSL-3 group consists of a contiguous

block of 48 unpatented mining claims located

in the jixmile Lake.- Area, District of Kenora-

Thundar Bay, Patricia Mining Division. A general

location map of the region, (Exhibit 1) and a

specific detailed claims location :.iap, (Exhibit 2)

are appended hereto.

The 48 claircs were purchased by Bison^

Petroleum 6 Minerals Limited from Messrs. L. K.

Smith and I. O. Dearden on October 24th, 1969.

All of the claims were properly recorded with

the Ontario Department of Mines Recorder at

Sioux Lookout, Ontario, on October 16th, 1969.

The original transcripts of the transfers to

Mr. G. N. Milner, "In Trust", a lawyer with the

firm of Day, Wilson, Campbell, Solicitors for

Bison Petroleum s Minerals Limited, are held in

the Engineering Offices of Bison Petroleum fc

Minerals Limited at 100 Bronson Avenue, Ottawa

4, Ontario. The claims are registered as Numbers

PA 211,830 to PA 211,832 inclusive, PA 211,834 to

PA 211,861 inclusive, PA 213.,870 to PA 211,875

inclusive, PA 211,878 to PA 211,888 inclusive;

all appearing on the Ontario Department of Mines,

Claim Map Number M 2877, the Sixmile Lake Sheet

and the Claim Map entitled "Area South of Sturgeon

Lake, District of Thunder Bay." Personal examina

tion of major portions of the property by the

- 3 -

writer indicates that to the best of his knowledge, the claims and the group boundaries are properly

staked, tagged and marked in accordance with The

Mining Act, but thrt the physical location of the south boundary is about one claim width to the

north of its position as indicated on Claim Map Number M 2877.

Canadian Javelin Limited holds a interest in all of the above mining claims, and

under a management agreement with Bison Petroleum S. Minerals Limited, all exploration, engineering

and management services are provided by Canadian Javelin Limited.

III. ACCESSIBILITY, CLIMATE, LOCAL RESOURCES

During the winter months it is possible

to drive within ten miles of the property by the

Ontario Highway #599 and a series of winter roads from the end of the Mattagami Lake Mines road

in Block 7. The last ten miles must be covered

by ski-doo type vehicles. During the summer it

is most easily reached by charter aircraft from Ignace, Savant Lake or Sioux Lookout. The C.N.R. Northern Transcontinental mainline route passes about 15 miles north of the property; and a C.N.R. branchline from Sioux Lookout to the

Lakehead passes about 15 miles southwest of the property.

- 4 -

The SL-3 claim group is situated between Post, Willet and Hump Lakes, below the

western end of the Sturgeon Lake Narrows. The

center of the group is approximately eight miles in an east-northeasterly direction from the

Mattagami Lake Mines Limited property on the "Block

7" timber lea^e held by Abitibi Paper Company Limited.

The climate in the area is described as Cool Temperate East Coast {with short summers). Mean annual precipitation is in the order of 20 inches, and mean annual snowfall is about 80 inches.

The mean January temperature is -5OF with over night lows approaching -60OF, and mean July tem perature is 620F with daily highs approaching 95OF. The winter period extends from mid-October to late

April; the average frost-free period is about 75 days.

The group is roughly longitudinally bisected by an east-xvest trending ridge 200 to 300

feet above Post Lake and is covered with second- growth species of woods, particularly spruce, jackpine, birch, poplar and cedar. An extensive muskeg area is situated in the eastern part of

the group near Willet Lake. The general area is prime logging country that is extensively traversed

by winter logging trails and roads.

- 5 -

The area is in the Brown-Podzoli c, soil

zone which is typical in the northern forests of

mixed hardwoods and conifers. It is in glaciated

country that is underlain with glacial detritus

and scoured bedrock. Accordingly, the agricultural

potential of the soil is low.

The population in the region is sparse

and located in small centre? along the railway

lines at Ignace, Sioux Lookout and Dryden. A

transient logging and forestry population moves

throughout the area during the winter season.

Several Indian Reserves containing small scattered

bands- are also located nearby.

IV. HISTORY

The general region has been investigated

over the past century by the Geological Survey of

Canada, the Ontario Department of Mines, and to

varying degress by several mining companies.

Numerous reports have been written about the

region during this period. The most recent

reports are: the Ontario Department of Mines,

Geological Report Number 24, Metionga Lake Area by

David P. Rogers, 1964; and, the Geological Survey

of Canada, Paper 68-45, Geology of the Sioux

Lookout Map-Area, Ontario, a Part of the Superior

Province of the Precambrian Shield, by R. Skinner,

1968. In addition, the area is extensively covered

on the Ontario Department of Mines Preliminary

•trjove&r*-Ztn

'it;:: i

~ 6 -

Geological Map P-353, the Minnitaki-Sturgeon

Lakes Sheet, Districts of Kenora and Thunder Bay, compiled by J. C. Davies and A. P. Pryslak, issued in 1966, which has been superceded by Map Number 2169, the Sioux Lookout-Armstrong

Sheet. During the summer of 1970, an Ontario Department of Mines field party was mapping the Glitter Lake Area.

Previous mining activity in theSturgeon Lake Area centered around the Darkwater

and St. Anthony gold mines, prior to the Second

World War. Since that time many mining claims have been staked on gold, copper and magnetite iron formation showings, but most of these claims have been allowed to lapse. There is no evidence

of previous staking or mineral exploration in the claims currently described as the Bison SL-3 Group.

The recent claim staking activity in the Sturgeon Lake Area was stimulated by an

announcement of a mineral deposit discovery by

Mattagami Lake Mines Limited in October 1969.

Mattagami Lake Mines Limited drilled an electro

magnetic conductive zone on Block 7, southeast of

Beidelman Bay on Sturgeon Lake. The company reported ore grade intersections of zinc, copper,

silver, lead and gold over 70 to 190 foot true

widths along approximately 1,000 feet of strike

length along what appears to be the contact between acid and basic volcanic rocks. Mattagami

- 7 -

Lake Mines is presently preparing to put the property into production. The intensity of

staking activity ew.d group holdings in the

region is illustrated in Exhibit l , reproduced

from a survey published in the Northern Miner.

A team of prospectors headed by

Messrs. E. O. Dearden and L. K. Smith staked a substantial block of 132 unpatented mining claims

which they offered for sale to interested parties, including Bison Petroleum fi Minerals Limited/ and

others. Upon the recommendations of its engineering staff, Bison Petroleum s Minerals

Limited acquired the 48 claim SL-3 group from the above block.

V. REGIONAL GEOLOGY

The general relationship between the

regional geology in the area of the Mattagami Lake Mines discovery and the Bison SL-3 claim

group is indicated in the examination of the

Sturgeon Lake Area by the Ontario Department of Mines whose findings are illustrated in Map 2169. Additional data is shov/n on Map 2044, the Metionga Lake Area, {which accompanies

O.D.M. Report Number 24, by D. P. Rogers), and on the Geological Survey of Canada Aeromagnetic

Maps 1117 and 1127.

- 8 -

On the basis of the above data, the

author is of the opinion that the southern

limit of the Archean greenstone belt extends

from Beidelman Bay on Sturgeon Lake, eastward

across Darkwater Lake, north of Bell Lake,

across the southern tip of Glitter Lake and on

to the area southwest of Sassafras Lake, an

approximate distance of 22 miles. The eastern

limit roughly parallels the west shore of

Quest Lake, and then swings south-easterly to

apparently join the southern limit in a "pinched"

situation southwest of Sassafras Lake. The

three major rock types within this triangular

area south and east of Sturgeon Lake are acid

and basic metavolcanics and a band of metasedimentary

and metavolcanic rocks, including magnetite iron

formation, which approximately coincides with

the southeasterly trending axis of the Barge,

Post and Willet Lake series.

The assumed acid-basic metavolcanic

contact extends from just north of Darkwater

Lake, eastward through Claw Lake to Hump Lake

whereupon it swings northwestward approximately

paralleling the south shore of the Barge, Post,

Willet Lake series, to the area at the southwest

end of the Narrows on Sturgeon Lake. The

mineralized zone drilled by Mattagami Lake

Mines is reported to follow the acid-basic meta

volcanic contact (Northern Miner, November 6th,

1969) , along an east-west strike, and dipping

1*1

- 9 -

steeply at 70O to the north. The Ontario Department of Mines Map 2044, the Metionga

Lake Sheet, indicates outcrops of basic volcanics dipping vertically or steeply to the northeast, along the shore line of

Sturgeon Lake south of the southwest end of

the Narrows. This observation, plus the

suggested fold nose structure containing acid

and basic metavolcanics east of the Sturgeon

Lake shore line and at a point west of the north end of Lyon Lake indicates that a major

fold structure may be present, possibly a

syncline overturned to the south and plunging

to the west-northwest. There is little evidence of the fold structure to the west of Sturgeon

Lake; consequently, the author suspects a major

fault zone within the Lake itself. The general regional geology, as derived from all of the foregoing data is illustrated in Exhibit 4.

VI. LOCAL GEOLOGY

In the case of the Mattagami discovery, the acid-basic metavolcanic contact zone appears

to be the geologically favourable area for the

emplacement of sulphide mineralization. Published

data indicates that ore grade intersections of zinc, silver, copper and lead sulphides have been encountered in the rhyolite and acidic flows

and tuffs which are to the north, e.g., hanging wall side of the basic volcanics indicated on Map

- 10 -

Number 2169. The age differences between the

sulphide mineralization and the host rock as

well as the relationship between the mineralization

and the overall inferred synclinal structure are not known to the writer at this time. If the mineralization is controlled by structural features and the presence of fractured and

brecciated rhyolites and tuffs, in close proximity to more competent and inhospitable andesites,

then any area along the contact zone and within the inferred synclinal fold structure would be a geologically encouraging area in which to search for additional zones of ore grade sulphide

mineralization. Under this hypothesis the entire 15 mile length of this contact zone would thus be worthy of detailed examination.

Map 2169 and Exhibit 4 indicate that the SL~ 3 claim group is underlain by 1.) basic

igneous rocks, 2.) metasediments and volcanics,

and 3.) acid and basic metavolcanic rocks, all striking northwest-southeast. Mapped outcrops (Map 2044) on the south shore of Sturgeon Lake,

just west of the claim group suggest that the rock units within the group can be expected to dip vertically or steeply to the northeast, probably representing the northeast limb of the

inferred overturned fold structure. The presence of the favourable acid-basic metavolcanic contact

zone is indicated by mapped outcrops of schists

and gneisses associated with the basic meta-

- l i -

volcanics along the south shore of Post Lake and

by mapped outcrops of acid agglomerate, tuff, or flow breccia along the south shore of Sturgeon Lake, just north of Lyon Lake. The indicated contact crosses the claim group in a northwest- southeast direction over a probable length of about one mile as shown on Exhibit 4, before

swinging west through Hump Lake v;here the nose of a fold appears to be located.

The inferred favourable geologic

setting on and around this property clasp it as one worthy of extensive examination. Due

to a relative scarcity of outcrops within the

group, however, it was necessary to rely heavily on ground geophysical information and exploratory drilling in the attempt to delineate the contact

zone and to verify the presence of mineralized areas along this contact.

VII. EXPLORATION PROGRAM

In view of the potentially favourable

geological conditions on the SL-3 claim group,

Bison Petroleum s, Minerals Limited undertook an

exploration program in which most of the claim

block Wcis examined by airborne and ground

geophysical surveys followed by exploratory

diamond drilling during the winter and spring

of 1970.

- 12 -

Geophysical Surveys

In order to start the exploration

program immediately after "freeze up" the company

initiated the airborne geophysical phase in late-

October 1969. The airborne survey was carried

out in conjunction with two affiliated companies,

Canadian Javelin Limited and Norlex Mines

Limited, who hold the adjacent blocks of claims

to the west and northwest.

McPhar Geophysics Limited of Toronto

conducted the airborne magnetometer and electro-

magnetometer survey ove.. three adjacent groups

of claims the SL-1 (Norlex Mines Limited),

the SL-2 (Canadian Javelin Limited) and SL-3

^Bison Petroleum s. Minerals Limited^, from

November 4th to November 6th f 1969. An F-400

EM instrument which is a single phase, dual

frequency unit and a proton magnetometer were

used, both being mounted in a D.H.C. Beaver

aircraft flying at an altitude of 450 feet and

along lines spaced at 1/8 mile intervals. The

final report was issued by McPhar Geophysics on

January 5th, 1970. The writer has examined this

data and discussed the results with McPhar's

technical personnel who indicated the presence

of three conductive zones within the Bison claim

group (as shown in Exhibit 3). The strikes of

these anomalous zones probably parallel those of

the major rock units indicated on Map 2169.

- 1 3 -

McPhar's report received in early- January 1970, states the following about these conductive zones:

Zone No. 3

A distinct zone of multiple parallel conductors with associated strong magnetic

response correlates with the band of meta- sediments trending through the survey area.

The largest amplitude responses occur in the southern portion of the area, southeast of Post

Lake. Based upon the geologic information, these responses would appear to be due to iron forma

tion's and/or graphitic bands. However, some ground follow-up would be warranted to confirm the accuracy of the geology.

The "A" category EM response on Line 9, fiducial 3026, lies near the contact between the

metasediments and metavolcanics and would

warrant investigation on the ground. Depending upon the results of this ground investigation, further work may be warranted on the "B" category

anomalies within this conductive zone.

Zone No. 4

The geologic map suggests a nose to

the acidic metavolcanics in the area of Line 8 and Line 9, north and east of Claw Lake. If

this is the case Zone No. 4 and Zone No. 5 may

be related. However, if the acidic metavolcanics

- 14 -

instead pinch out to the southeast then Zone

No. l and Zone No. 2 may also be related to Zone No. 4 and Zone No. 5. The "A" category EM

response on Line 9, fiducial 3026 is located at the contact between the acidic and basic meta-

volcanics near the nose of the flexure and should

be investigated en the ground to confirm the geologic information, and to determine the

significance of this conductive zone as a source of sulphide mineralization.

Zone No. 7

This zone lies within the Bison claim group along the southwest shore of Post Lake

near to or at the contact between the metavolcanics

and metasediments. "A" category EM responses are indicated on Line 29, fiducial 1498; Line 20,

fiducial 1219; and Line 31, fiducial 972, with

correlating "B" category responses on Line 18, Line 22, Line 23, Line 24 and Line 25. Although possibly due to graphite zones within the meta

sediments and lacking correlating magnetic response, this zone would warrant further investiga

tion on the ground.

The ground geophysical survey wascontracted to Dearex Limited of Etobicoke, Ontario,

with the line cutting being sub-contracted to

George Potter of Kirkland Lake, Ontario.

- 15 -

The Dearex crew consisting of G. Flaherty

and A. Lindner worked on the property from

January 22nd to February 10th, 1970. The Crone

Shootback EM method and equipment with a 200

foot coil spacing and a basic frequency reading

of 1,800 Hz were used for the EM survey, whereas

a Sharpe Fluxgate Magnetometer was utilized for

the magnetic survey.

The combined survey covered 28.1 miles

of line at 400 foot line spacing, and is covered

in a report entitled, "Report for Canadian

Javelin Limited and Bison Petroleum E, Minerals

Limi-ted covering Magnetic and Electromagnetic

Surveys over a Portion of their Sturgeon Lake

Area Claim Groups, Patricia Mining Division,

Ontario," by J. D. Crone, which was submitted to

the Company in March 1970.

The Dearex survey detected a narrow

(50 foot) conductive zone trending southeast-

northwest adjacent to the south shores of Post

and Willet Lakes, and extending almost continuously

from line 36+OOE to line 60+OOW, a total distance

of 9,600 feet. This zone is generally coincident:

with magnetic highs ranging from 200 to 10,000

gammas and is quite probably closely related

to the mapped metasedimentary-metavolcanic rock

contact which in this area has essentially the

same strike direction.

- 16 -

Even wit^ a 300 foot coil separation,

the Dearex survey did not, however, pick up the

conductive zone detec'-.ed by the McPhar survey

in the Hump Lake area and which trends north

west approximately one mile from the tip of the

northwest arm of Hump Lake. This conductive

zone could be due to mineralization in the area

of the inferred acid-basic metavolcanic rock

contact in the fold structure as indicated on

O.D.M. Map 2169. By intention, the Dearer,

survey did not cover the anomalous zone outlined

in the northeastern portion of the property by

the McPhar survey. Due to the extremely high

magnetic responses associated with the con

ductivity, it was considered that the anomalies

are due to the presence of iron formation,

indicated on O.D.". Map 2169 as being present

in that area.

Subsequent to the Dearex survey,

members of the Bison engineering staff, utilizing

a Ronka EM-16 and a Jalander magnetometer,

delineated the northeastern anomalous area (iron

formation) and re-ran lines in the Hump Lake area.

The results of this work are presented in the map

entitled, "Supplementary Geophysical Information,"

Exhibit 3, which is hereto attached.

The ground work in the northeast

portion of the group outlined a conductive zone,

coincident with a 5,000 to 15,000 gamma magnetic

high, extending from line 8+OOW to 28+OOW,

——————— jba dl'a

l- 17 -

approximately 1,600 feet north of Baseline 0+00.

This zone was subsequently drilled (Hole BI-3)

and the results are covered below under Diamond

Drilling.

The EM work in the Hump Lake area

detected a conductor extending from line 32+OOW

to 48-fOOW, whereupon it crossed into the

Canadian Javelin ground to continue to line

56+OOW. This conductor was tested by two drill

holes, BI-5 and BI-6 due to its location in

respect to the inferred acid-basic metavolcanic

rock contact and the results of the drilling

are-discussed below.

Diamond Drilling

A contract for AXQ wireline diamond

drilling was awarded to St. Lambert Drilling

Company of Thetford Mines, Quebec.

Drilling commenced in mid-March and

continued until April 15th, when it was suspended

for break-up. Drilling was resumed in late-May

and the last hole was completed in early-June.

During the winter, the camp on Barge

Lake was serviced by tractor and a ski-doo type

vehicle, and excellent aircraft service was

provided by Ignace Airways.

- 18 -

The first, second and fourth holes, located on the shore line of Post and Willet Lakes were drilled to test the conductive

zones detected by the Dearex survey, whereas holes BI*-3, BI-5 and Bl-6 were drilled to

investigate two separate EM anomalies indicated by the EM-16 survey. The locations, dips and

depths of the individual holes ara presented below:

Hole No. Coordinates Claim No. prilling Dip Depth

BI-1

HI -2B 1-3BI-4BI-5BI-6

24+OOW/31+25N48+OOW/32+OON12+OOW/48+50N28+OOE/30+OON32+OOW/12+50S48+OOW/12+50S

211859211885211857211844211871211875

Grid SGrid SGrid SGrid SGrid SGrid S

45045045O55O55 550

529'511'600'350'547'452'

Total Footage 2,989'

The logs and cross sections of the

individual holes are included herein, with a

brief description of the rock types encountered

in each hole being presented below. The assay certificates of Bondar-Clegg Limited are appended hereto as Exhibit 5.

Hole BI-1 located at 24+OOW/31+25N,

was drilled grid south at 45O to test the

conductive zone detected by the Dearex survey.

The hole was drilled from the ice, immediately

adjacent to the shore line and went through

four feet of overburden. From 4 to 111 feet,

the rock consists of banded and amygdaloidal

"l

- 3.9 -

chloritized andesitic tuffs, with l" to 2"

pyrite-pyrrhotite seams at 14.5, 58.0, 61.0,

75.0 and 82.5 feet. From 111 to 280 feet

the rock becomes more massive andesite with l" to 3" seams of pyrite and pyrrhotite at

117, 118.5, 120.5 and 122.5 feet. In addition, there is a zone of moderate disseminated,

banded and massive pyrite and pyrrhotite from

171 to 176 feet. From 280 feet to 392 feet

the rock consists of interlayered graphitic seams, rhyolitic tuffs and quartzose zones.

Weak to moderate disseminated to massive sulphide mineralization is associated with both the graphitic and quartzose horizons. From

392 feet to the end of the hole at 529 feet, the rock is essentially interlayered, very

fine grained, very finely banded light green chloritized andesitic tuffs and more massive

andesite, with a 1/2" seam of pyrite occurring at 455 feet. Assays of split core from 171

to 176 feet, 279 to 285 feet, 285 to 290 feet,

306 to 309 feet, 320 to 325 feet, 342.5 to 343.75 feet, 362 to 365 feet and 365 to 371 feet did not indicate the presence of commercial

quantities of copper, zinc, nickel, gold and

silver.

Hole BI-2, spotted at 32+OON on line

48+OOW, was drilled from the ice on Post Lake to further test the anomaly detected by the Dearex survey. Bedrock was encountered at 90

- 20 -

feet, and from 90 to 122 feet the rock is essentially

very fine grained, light to dark gray silicified

and chloritized tuffs with occasional very minor

disseminated pyrite and occasional rhyolitic

zones. A zone of interbedded tuffs and slaty

graphitic material is present from 122 to 147 feet,

followed by 14? feet of silicified and chloritized

tulfi; containing prominent slaty-graphitic pyrite

bearing horizons from 147 to 290 feet. Tuffaceous

rock containing minor l" to 2" seams of massive

pyrite and pyrrhotite continues from 290 to 425

feet, whereupon the core becomes more andesitic

from 425 to 477 feet. From 477 to 499 feet the

rock is interbedded andesitic and rhyolitic tuffs.

The hole ended in diorite from 499 to 511 feet.

Two .small samples, e.g., from 103 to 107 feet and

from 107 to 111.5 feet were assayed, but were not

found to contain commercial quantities of copper,

zinc, nickel, gold or silver.

Hole BI-3, at 48450N on line 12+OOW

was drilled grid south at 45O to test the combined

magnetic EK anomalous zone indicated by the

supplementary geophysical work. The hole

penetrated 6 feet of overburden followed by 239

feet of interlayered very fine grained, finely

banded chloritized tuffs and siltstones from 6

to 245 feet. A slaty graphitic zone was encountered

from 245 to 277 feet, followed by five feet of

tuffs to 282 feet. From 282 to 294 feet the rock

consists of tuffs intercalated with 2" to 6" layers

- 21 -

of banded iron formation. The material responsible

for the magnetic anomaly is undoubtedly the

cherty-slaty very fine grained, thinly laminated

highly magnetic iron formation which was encountered

from 294 to 366 feet. The banded iron formation

continues in l" to 6" beds interlayered with tuffs

from 366 to 404 feet, whereupon the rock becomes

essentially silL^tones and chloritized tuffs with

1/36" to 1/8" solitary bands of iron formation

each 5 to 10 feet of core, from 404 feet to the

end of the hole at 600 feet.

Sulphide mineralization in this hole

was extremely weak, therefore, no samples were

taken for assaying.

Hole BI-4 located at 30+OON on line

28+OOE was drilled grid south at 55O to test the

anomaly detected by the Dearex survey as being

adjacent to the shore line of Willet Lake. The

hole was drilled from the ice in April, and as

the ice was starting to soften, the hole was

drilled to only 350 feet. It was sufficiently

deep, however, to intersect the graphitic material

which is probably responsible for the conductivity

detected by the EM survey. Bedrock, encountered

at 25 feet, consists of gray to black very fine

grained, very finely banded carbonaceous siltstones

commonly exhibiting graphitic Flip faces parallel

to the banding, from 25 to 98 feet. From 98 to

14S feet, the rock ic interbedded chloritized

tuffs and quartz-chlorite schist, followed by 39

- 22 -

feet (148 to 187 feet) of slaty graphitic silt-

stones with minor associated pyrite and pyrrhotite.

Interbedded chloritized tuffs, rhyolite and

gneiss are present from 187 to 199 feet, followed

by 50 feet of indurated slaty carbonaceous

material containing minor associated pyrite and

pyrrhotite to 249 feet. From 249 to 350 feet, the rock is essentially interbedded rhyolitic and chJcritized tuffs with minor graphitic horizons carrying weak pyrite-pyrrhotjte mineralization.

Sulphide mineralization was generally

weak, therefore, none of the core was assayed.

Hole BI-5. spotted at 12+50S on line

32+OOW, was drilled grid south at 55O to test the conductive zone indicated by the Ronka (supplemental) survey as being in the vicinity of the assumed acid-basic {felsic-mafic) metavolcanic rock contact. The hole encountered 10 feet of over

burden followed by 219 feet (10 feet to 229 feet) of interbedded light gray-green, very fine grained,

very finely bedded chloritized and rhyolitic tuffs with minor slaty-carbonaceous graphitic zones,

minor disseminated pyrite and pyrrhotite (61 to 71 feet and 75 to 76 feet) and minor zones of quartz-feldspar schist. Very fine grained, light gray-green, very finely banded rhyolitic tuff and massive rhyolite containing weakly disseminated

pyrite and pyrrhotite was encountered from 229 to

360 feet. From 360 to 381 feet the rock consists of rhyolitic tuffs interbedded with slaty graphitic

- 23 -

material, and from 381 to 417 feet, it is inter

bedded chloritized and rhyolitic tuffs. Dark green, very fine grained, dense massive and banded

silicified tuffs are present from 417 to 439 feet, and from 439 to 471 feet light green-gray very

fine grained chloritized and rhyolitic tuffs are

present. The hole ended (471 to 547 feet) in medium to dark gray-green chloritizcd andesitic tuffs containing minor disseminated pyrite.

Split core was assayed, however, the

analysis did not indicate the presence of com mercial quantities of copper, zinc, nickel, gold

or silver. The sampled intervals are as follows:

75 to 80 feet, 90 to 94 feet, 168 to 170.25 feet,

177.5 to 180.0 feet, 182.5 to 185.0 feet, 252.5

to 255.0 feet, 260 to 265 feet, and 372 to 375

feet.

The last hole, BI-6 located at 12+50S

on line 48+OOW, drilling grid south at 55O , was drilled to test the westward extension of the

conductive zone outlined by the Ronka survey in

the Hump Lake area. After passing through 12 feet of overburden, the hole encountered inter

bedded fine grained andesite and very fine grained,

very finely banded strongly chloritized tuffs,

carrying weak pyrite mineralization from 12 to

176 feet. However, a minor lens of light gray, fine grained massive diorite was also encountered

from 80 to 90 feet. From 176 to 373 feet the

rock consists of medium gray to white, very fine

- 24 -

grained massive and very finely banded rhyolite

and rhyolitic tuffs carrying weak to moderate

disseminated and lightly banded pyrite and pyrrhotite

over the entire section. At 373 feet,the hole encountered light to medium green, very fine

grained, very finely banded chloritized tuffs with minor pyrite associated with the chloritized slip

faces. This rock type continued to the end of

the hole at 452 feet, except for a 10 foot zone

of very fine ^-_,.ed massive rhyolite from 424

to 434 feet.

Sulphide mineralization was generally

weak, however, core from the following intervals was assayed: 226 to 232 feet, 232 to 237 feet,

240.5 to 247 feet, 256 to 262 feet, 274 to 276.5 feet, 281 to 284 feet. As usual, assays did not

indicate the presence of commercial quantities

of ore grade material.

VIII. GEOLOGY

The major outcrop area on the SL-3 claim

group is located south of Post and Willet Lakes and north of Hump Lake, in the vicinity of, and gonerally parallel to Baseline 0+00. This section

is characterized by a ridge rising 150 to 200 feet above Post Lake and providing good exposures

of medium grained andesite and andesitic tuffs

striking on azimuths of 34Oo to 350O and dipping

Jfa fKttt

- 25 -

generally northeast at 75O to 85 , but occasionally

steeply to the southwest. None of the outcrops

examined exhibited sulphide mineralization.

The ground east of Post Lake, in the

vicinity of claim numbers 211845, 846 and 211852

rises about 20 to 30 feet above the lake, and is

quite probably underlain by near surface bedrock.

Except for the land adjacent to the

south shore of Willet Lake, which is generally flat

and fairly wet, the claim group is covered by

relatively well drained soil, which supports a

moderately extensive cover of mature second growth

spruce and jackpine. Small cedar swamps, however,

are common in the poorly drained depressions

within the ridge area in the longitudinal central

portion of the property.

Most of the geological information

presented on the map entitled, "Geological and

Surficial Information," Exhibit 6, is interpreted

from the diamond drilling because four of the

six holes were located in areas without outcrops.

Based upon the core recovered from

holes BI-1 and BI-2, the ground containing the

conductive zone parallel to the south shore of

Post Lake is underlain by interlayered andesite,

chloritized andesitic tuffs and minor zones of

rhyolitic tuffs. The drilling has indicated that

- 2 6 -

the conductivity is due to the presence of numerous 2 f to 10' graphitic horizons/ containing

massive and disseminated pyrite and pyrrhotite, interbedded with the tuffaceous rock. Hole BI-1

intersected graphitic horizons from 280 to 392 feet, whereas this material was encountered over

a wider interval, i.e., 170 to 400 feet in hole BI-2.

The rock types encountered in these two holes indicate that they were drilled into the

predominantly meta (mafic) volcanic side of an inferred metasedimentary-metavolcanic contact zone

indicated as being present parallel to the south shore of Post Lake.

Hole BI-4, however, drilled to test the eastern extension of essentially the same con

ductive zone, intersected interbedded carbonaceous siltst nes, graphitic horizons, chlorite schist, chloritized tuffs and rhyolitic tuffs, more typical of the metasedimentary rock series. In other

words, these rocks are representative of the sedimentary side of the metasedimentary-metavolcanic

contact zone.

The rocks encountered in holes BI-1,

BI-2 and BI-4, appear to be a mixture of meta- sediments and metavolcanics, thus it is difficult

to establish a clearly defined contact as indicated on the Provincial Geologic Map 2169.

For the purpose of this report, therefore, it is

- 27 -

considered that the above holes were drilled within a transitional contact zone between the

major metasedimentary and mafic metavolcanic horizons.

The sulphide mineralization encountered in the drilling was generally associated with graphitic horizons, and was definitely not of a

commercial nature. Furthermore, this long con ductive zone tested by the above drill holes, is due primarily to the presence of fairly extensive

graphitic horizons, thus additional drilling on this anomaly would quite probably produce the

same'results.

Hole BI-3 intersected interlayered

chloritized tuffs and siltstones, a 12 foot graphitic horizon and 110 feet of cherty banded

sedimentary magnetic iron formation, followed by 196 feet of interlayered tuffs, siltstones and

solitary bands of iron formation. The rock types indicate that this hole was drilled well within

the metasedimentary horizon presented in O.D.M. Map 2169, and the presence of iron formation in the core accounts for the strong magnetic response

by both the airborne and ground surveys, as well as substantiating the north-westward extension of

iron formation beneath Post Lake. The graphitic

zone on the other hand, accounts for the con

ductivity associated with the magnetic high.

- 28 -

Additional drilling of this particular anomaly

would, in all likelihood, produce the same results.

The rock types encountered in hole BI-5 and BI-6, near the south boundary are more indica

tive of the inferred northwest trending mafic-

felsic metavolcanic icck contact zone indicated as being present in the Hump Lake area on O.D.M. Map 2169. Both holes encountered steeply north eastward dipping interbedded chloritized tuffs and andesitic tuffs followed by extensive (200 feet ) intersections of rhyolitic tuffs and massive rhyolite. The rhyolitic horizons in both holes carry weak to moderate banded and dis

seminated pyrite and pyrrhotite mineralization.

However, a narrow {20 foot) zone of intercalated

rhyolitic tuffs and slaty graphitic material at 360 feet in hole BI-5 probably is the stronger cause of the conductivity detected by the Ronka

survey. The north-westward extension of the anomaly

tested by hole BI-6, can probably be attributed

to stronger sulphide mineralization in the rhyolitic horizon of this hole than in the same

horizon in hole BI-5.

The anomaly tested by these two holes, extends off the property both to the southeast

on to Mattagami Lake Mines ground, and to the northwest, into claim group SL-2 held by Canadian

Javelin Limited, and it is probably coincident

with or closely parallel to the inferred mafic-

- 29 -

felsic metavolcanic rock contact. Based upon

the drilling results, it is believed that the

mafic-felsic contact in this area is not sharply defined, but that it too is of a transitional

nature, similar to that between the metasedimentary and mafic metavolcanic rocks as observed in the

core from holec EI-l, 81-2 and BI-4.

IX. COSTS

A brief breakdown of the total November

1969 to September 1970 expenditures other than

the acquisition costs on the SL-3 claim group is presented below:

Assays

Diamond Drilling

Geophysics S Line Cutting

Cenerel Field Expenses SuppliesTravel and Aircraft*

Services

Wages

Total

$ 410.50

28,917.00

9,700.50

925.00

60.00

5,694.50

4,418.00

$50,125.50

*Includes partial de-mobilization/ mobilization due to spring breakup.

- 30 -

X. SUMMARY and CONCLUSIONS

The SL-3 groug^ of 48 unpatented mining

claims^ in the Sturgeon Lake area, Patricia Mining

Division, Ontario, was purchased from L. K. Smith^

and E. O. Dearden in October 1969.______ ^ __________ ______—^—^.^***~****

An airborne EM and magnetic survey was

conducted over the property by McPhar Geophysics

in early-November 1969, and the line cutting,

ground EM and magnetic survey totalling 28.1

line miles were completed in Janauary and February

1970 by Dearex Limited.

The McPhar airborne survey detected

three major conductive zones striking conformably

with the map indicated rock units within the

claim group. Two of the anomalies are parallel

to the north-westward trending axis of Post Lake,

and the northernmost of these exhibits strong

magnetic responses coincident with the conductivity,

suggestive of the presence of iron formation as

indicated on O.D.M. Map 2169.

The second anomaly was indicated as

occurring near and parallel to the south shores

of Post and Willet Lakes, for an overall length

of approximately l 3/4 miles.

The third anomaly was outlined as being

conformable with the nose of a map indicated fold

'- 4.'- "t

- 31 -

structure and mafic-felsic metavolcanic rock

contact in the vicinity of Hump Lake and its northwest arm.

The Dearex survey concentrated on the

portion of the group situated generally south of the longitudinal axis of Post Lake, as it was

considered that the northernmost anomaly,

(associated with the magnetic high) picked up by

the airborne survey, was due to iron formation. Within the area examined, the Dearex survey

delineated the conductive zone parallel to the

south shore of Post and Willet Lakes, but even

with a 300 foot coil separation for greater

depth penetration, it did not pick up a conductor

north of Hump Lake in the region of the inferred

favourable contact zone.

A supplemental EM survey using a Ronka

EM-16, was carried out by Bison Petroleum S Minerals Limited. This program did outline a conductor in the so-called favourable contact

area north of Hump Lake, as well as precisely locating the (iron formation) anomaly north of

the center line of Post Lake. The eventual decision to tie down the "iron formation"

anomaly was based upon the desire to arill it, thereby verifying the cause of the conductivity.

The diamond drilling program commenced

in mid-March 1969 and was suspended in mid-April

- 32 -

for spring breakup. Drilling was resumed in

late-May and terminated in June 1970 with a

total of 2/989 feet being completed on the pro

perty. The drilling program resulted in six

holes, three of which tested the long conductive

zone adjacent to the south shore of Post and

Willet Lakes, one tested the iron formation

anomaly, while two tested the conductive zone

determined by .he supplemental survey in the

area of the inferred mafic-felsic metavolcanic

rock contact northwest of Hump Lake.

Holes BI-1, BI-2 and BI-4 were drilled

in a transitional contact zone between meta-

sedimentary and mafic metavolcanic rocks, and

encountered graphitic horizons with moderate

associated pyrite and phrrhotite mineralization

as being the cause of the conductivity detected

by the EM surveys. Hole BI-3 was drilled in the

more typical metasedimentary rock sequence and

encountered banded magnetite iron formation as well as a graphitic horizon, which account for

the anomalous magnetic and EM responses in that

area.

Holes BI-5 and BI-6 were drilled in a

transitional contact zone between mafic and felsic

metavolcanic rocks, and determined that the con

ductivity was due to weak to moderate disseminated

pyrite and pyrrhotite mineralization associated

with rhyolitic horizons.

- 33 -

Although sulphide mineralization was moderately strong in the sampled sections of

all holes except BI-3, assays did not reveal

the presence of commercial quantities of copper, zinc, nickel, gold or silver.

It is believed that the mafic-felsic metavolcanic contact, although transitional and

not sharply marked, has been reasonably well

located by geophysical methods. Drilling in this contact area within the SL-3 group has

indicated the presence of disseminated sulphide mineralization, although none of a commercial

nature,. If stronger sulphide mineralization is

associated with the contact zone, it is probably

too deeply buried to have been detected by the

geophysical equipment utilised in the ground surveys.

Based upon the geophysical surveys

completed to date, there are no untested

anomalous areas on the SL-3 claim group.

XI. RKCOMMENDATION S

The 1970 geophysical work on the SL-3

claim group outlined three major areas of interest

and all of the targets have been drilled, resulting in the determination that graphitic horizons, iron formation and pyrite-pyrrhotite mineralization

were responsible for the anomalous magnetic and

- 34 -

EM responses determined by the surveys. The

exploration program has provided sufficient

assessment work credit to maintain a major

portion of the claims in good standing for

over two years. It is recommended that the

company defer additional expenditures on the

claim group until sufficient additional work is

performed on the adjacent groups held by Canadian

Javelin Limited and Norlex Mines Limited. If,

in the near future, either of the above companies

conduct on I.P. Survey across the favourable

mafic-felsic metavolcanic rock contact, it would

be advisable to run an I.P. check on the cross

lines in the contact area on the SL-3 group.

Respectfully submitted,

November 25th, 1970. W. B. Blakeman, M. Se., Geologist.

V

- 35 -

REFERENCE MATERIAL

1. Ontario Department of Mines, Report Number 24 - Metionga Lake Area (includes Map 2044) by David P. Rogers - 1964.

2. Geological Survey of Canada, Paper 68-45 - Geology of the Sioux Lookout Map-Area, A Part of the Superior Province of the Pre cambrian Shield by R. Skinner - 1968.

3. Ontario Department of Mines - PreliminaryGeological Map P-353 - The Minnitaki-Sturgeon Lake Sheet, Districts of Kenora and Thunder Bay, compiled by J. C. Davies and A. P. Pryzlak 1966.

4. Ontario Department of Mines Map 2169 - The Sioux Lookout-Armstrong Sheet - 1970.

5. Geological Survey of Canada Aero-magnetic Series

Sheets 1117G - Bell Lake 1127G - Watcomb

6. Northern MinerIssue dated November 6th , 3 969.

7. Bateman, A. M. - Econom.i o Mineral Deposits, J. Wiley s Sons, New York - 1952.

8. Putnam, D. F. and K'^rr, D. P., A RegionalGeography of Canada, j. M. Dent S Sons, Toronto 1966.

9. Report on the Jombined Airborne Magnetic and Electromagnetic Survey, Post Lake Area, Patricia Mining Division, Ontario by McPhar Geophysics -- 1970, Report Number 580.

10. Report for Canadian Javelin Limited and Bison Petroleum s Minerals Limited covering Magnetic and Electromagnetic surveys' over a portion of their Sturgeon Lake Area claim groups, Patricia Mining Division, Ontario by Crone Geophysics - 1970, Report Number 613.

V

Assaying Norlex SL-1

and Bison SL-3

Total Assay charges - Bondar-Clegg f, Co. Ltd. (See Attached invoices.)

- $931.50

Assay man days @ l man day per $15.00931.50 divided by 15.00 equals 62 man days.

Determinateons:

Norlex Bison

98104

or or

491

Man Day Distribution based on Above:

Norlex

Bison

30 divided by 49 equals approx imately .6 :.ian days per claim.32 divided Ly 38 equals approx imately .b man days per claim.

iam B. Blakeman

EXHIBITS

DRILL CORD

COXPAKYBISON PETROLEUM S MINERALS LTD? R0J2CT

RSXARKS :A2.

220 0 Mag

INCL.

JLS:COORDINATES

L 24W/31+25N

ELEVATION Tost

Hole No. 1

.. h .ch. 282/S29

D r i 1 1 b y :

F o o L aiize!

R 'j c o v e i1 y

' ? 3SJ5LrL.? 0 .. - IJ4^i T " TO l 4 l 4 l

j D a t e j F r o r.i

atteiair ~-T ToLog&ed by: Dace

From ToAssay R 2 s . i,

nmort r K. 9 ;;

DESCRIPTION

•21SL .l - 4 .:... i li LI 0,1, loo

i! 111|117 6 100

-C.asJLncL.

,-l^ed-dark..gr,.oQ,n. f ,]^andod,g-nd Amygdaloidal nhioritiiy.&d r?Ri hi r;tuffs w/chloritized shear faces and minor x-cutting quartz veins. Very minor diss py and pyrr w/very minor bleb of chalco in quartz"Vel.T~a"t 14.5' . l"^zones~"or banded and" diss py and* pvrrr "@ 58.0 1 , 61.0 1 , 75.0', 82.5', banded 45O TGA @ 24', 50O TGA @ 77.0'

Med gray^, medium to v-fg, very finely banded to massive quartzdiorite w/chloritized shear faces which carry strong pyrite mineralization.

.117 279.5 162 5 100

'279.5 282 2.5 100

Same as 4-111, but, slightly..m.QTg-jRiaS-^iA'.e;-,less v.'el]_handed ..-ind..^ non-amygdaloidal. Weak to moderate l"-3" zones banded and diss py and pyrr @ 117', 118.5', 120.5', 122.5', 140.2', 147.5'.lTd~dTs~s~p7~alTa~p ./T^lTo w/l L/2 1 missive py @ 173.75. Sampled 171-176. Banded 50O TCA @ ISO'.

Veined and massive quartzose zone greater than .60^ quartz w/moderate di3 S and banded py and pyrr.

COMPANYBISON

D R I L

PROJECT

E C O R D

SL-3

REMARKSAZ. INCL . COORDINATES ELEVATION

Hole No. l

Sheet ^C. 2

Depth: 325/529

Drill by: Dater' 7" O . TO

Logged by: DateFrom To

Recovery i A s s r. y Res.

l FrnrJ To ! Feed DESCRIPTION

l l i i l j 2S2 : 283.5 1.5- 100 l

i

Banded, contorted and brecciated carbonaceous (black) graphiticmaterial w/moderate to strong diss and banded py and pyrr.

i

283.5! 289.5 6 ! 100 i Same as 279.5-282, but w/strong massive sulfides 287.5-288.5.

285.5! 297.5 8 ! 100 Banded/ contorted and brecc.i,fte^ black carbonaceous graphiticzone w/weak to moderate banded and diss py and pyrr.

1 ii il1

]

' i 297.5 309 ! 11.5 100

i

i

31 u,. 'i 7. S

i ti 316.5 325

l il

i1 1

.S. 5

;: Coarse to med arained cru'i texture w/minor weak to

ji

^nn ; ; M e d gray, m- f g diorite -ii , '

! "' '

100 ' Coarse to 'mcd orained au i graphitic seams carrying |! 322.75' , 323' , and 323.5

artz diorite , aranitic-norohvroblasticmoderate banded py and pyrr.

*

no mineralization.

art?, dioritepy and pyrr

i*

but w/rflvhr^arprm*-@ 317' , 322.25' , 322.5' ,

|;

DRILL 'E C O R D

COMPANY BISON PROJECT SL- 3

RSV ?..^KS: AZj INCL. COORDINATES EL EVA

Drill by: JDate Logged by: Da- . - .- .-..TT. I ...^...... ,, , , , J 1-ron i ii . ii i iMiii| To r , I M m m iii| n i I IIIM 1 IB ^ ,,, ,, ,, ,, Fr

Footage | Iscjcovery Assay X s . !Si - c i ^ m p . ! : DESCRIPTION i Fro- To Feet: *i ; u !

Hole No. 1

TION s^ ecc ^^3

Depth: 529

t Qoro To

pa- ^

325 345 20 i 100 '' v-fcj banded rhvolitic tuff w/quartz oorphvroblasts 1X16"-1X8"j max dim and w/weak to moderate diss py and pyrr 342.5-343.5'.

i i, i ii i

345 360 15 i 100 ' Massive mq diorite - no ir.ineralization.i i ' i i *i ' i i

i i ' 360 1371.5 1 11.5 100 : Banded v-fg rhyolitic tuffs w/quartz porphyroblasts and moderate

,,. ' banded and diss py and pyrr and minor massive i ! occasional blebs very minor - probable chalco' - - '' ^ "S T f" " j . . . . . .. .. . -. . -.. J/ivL'.-

ii o? 1 1 392 20. 5: 100 - ; V-fg very finely banded rhyoliti,p tVlffp.

py and pyrr and - sampled 360-

\ i

392 529 137 100 i Lt-ned qreen, v-fq,, very finely banded chloritized andesitic! i tuffs w/occasional x-cutting quartz veins and

' zones. Occasional quartz amygdules up to ^ "quartzose breccia

diam. V seam offi . , ^ .i : -" i py @' 455. 25. Massive zone 460-48y. banded 5u--;uw TCA in

137 feet of sec'tion.l i'

:; * , i

i i I.. ' 529 ! End of hole - -No Test.

1 j!i

'

.r

COMPANY: B/SOMPETROLEUM* M/MERALS L/M/TED .D.H.NO.: &I ~

220" MAG. SIZE: AXQLINE: 24- + OO W.

23o-269.sr'- f

CCX.PAXY

DRILL

BISON PETROLEUM i .MINERALS LTD PROJECT

CORD

SL-3

REMARKS : AZ.

22O0 MagINC L,450

COORDINATES

L 4CW/32+0ON Ice

Hole No.

Sheet N

Depth; 189/511

Drill by: D .1 u eFrom Mar 23 To Mar 26

Logged by: Date

Recovery jAssay Res.,:i ise!

l ?rosi' To l Feet| t lp^B. .j^., , . ——^.. , —— ^ -^.- -.——-*-,.- ——l. -^. .1 M ...-^ l*——-^——

DESCRIPTION

"i Sri? EX. s50 i 90

AXQ ! 90 ;122.5 32.6 10C:

Casing

Lt-dark gray v-fq f inely^ banded silicified aad chlorJL.tji.gec'l.tuffs w/minor carbonate (calcite) banding and prominent quartz porphyroblasts up to V max dim. scattered weak py mineralize ti on

~Wedk""tcnnoderate ' barrdefi'~an'ct~iSl"S"S'~py~cnfra pyrir 103-111". 5

1122.5' 147 l 24.5: 100; V-fg very finely banded slaty carbonaceous graphitic....r.\ate^.icLLinterbedded w/light gray v-fg, very finely banded silicified tuffs. Fracturing parallels banding. Fracture faces are

hltlC TCA~py

.11? a7?.. s! ?.s.fc Lt-rcftd', ,gr.ay, .-medium, t o v-fg, finoJ.y...,banded-sillcXXd. w/minor diss py banded 45O TGA @ 157'.

a?2.5! 176 i 3.5 i 100: Dark gray v-fg silicified tuffs interbedded w/slaty, black.carbonaceous graphitic material. Fracture faces are graphitic.

: 17C , 189 i 13 l 100 Same as 14-7-172.5.

DRILL E C O R D

CO.XPAXY BISON PROJECT SL-3

REMARKS: Az IXCL. COORDINATES ELEVA

Drill by: lDa:e Logged by: Da1 F r or, To F r

roocas^ Recovery ;Assay Res.Si*C' i ' r " ; 1 DESCRIPTION ; ? r o r. 1 T o F e e c ^ .[ir

Hole No. 2

* 0i iU-X

Depth: 2 57 /511

ceom To

139 ;196.5' 7.5 100 | '. V-fg, slaty-black-carbonaceous graphitic materials/minori | j -i py and pyrr assoc w/graphitic fracture faces.1 ' i! 1 li

- - 1 1 't h '!i !

J196.5 1 207.5 111 100 ;! San^ as 347-172.5, hiif w/Kr^^i^ Zon^ 2^0'-?^II j ^

4 ' . ,, - ,,..-. .......-

! i i ^ 207.5! 223.5 16 100 ' V-fg-slaty-black , carbonaceous graphitic material w/araohitic

|j fracture faces banding 450 TGA @ 219'.

i i i ;l ! i

'223. 5 1 227 3.5 T 00 '- S ame as 347-372.5.'ii i

i ' i

L - l227 J235.2 8. '2 100 |! V-fg-slatv-black, carbonaceous graphitic material w/araohitic1 'l fracture- faces.li! i:————— ——————————— . ———————————

^35.2*233.5 18. b 100 ' Same as 147-172.5, but -w/minor It. cray rhyol:i i ji '

J. \

| ! fracture faces. Strong py mineralization 256

Ltiq .zone*?..

-257' .

i j

DRILL E C O R D

COMPANY BISON PROJECT ' SL-3 H OlC N O 2 -

RSXARKS : AZ. INCL. COORDINATES ELEVATION S heet N o 'Depth: 492.5/51

Drill by: Date Logged by: Date ?rotr, To From To

SizeXCMBBC

rootage Recovery Assay Res.!^ __ - - ,. . 1 i! DESCRIPTION r ?o:r. ; o ;* ee L v [ :i

i i

257 272 15 1001 i

272 2 11,1 5 .5 100i

1

277.5 423 iiiO.5 100

i|

li 1 Same as 147-172.5.

•' Slaty-black, carbnnar.Arnic; grsphiti^- 'mat^ri^] JJ/ora^hdrti'C— fc-r-tVC^U-E^i faces, minor py assoc w/py.

1i Essentially the same as 1^7-175.5. hnf- mp-d crrainprt na^cs-i v/r,

' ! (less well banded) more siliceous and w/minor rhyolitic zones, ! and occasional zones w/prom. quartz porphyroblasts. 2" seam: massive py g 3b2', l'1 seams massive py @ 377', 378.5' and 379.5',

; 3" seam massive py @ 391.5', 2V seam @ 425.5'. Banding well——— j ———————————————— | ————————————— d^v^Uop^d 450 TGA e-4 2-4-r^-. ————————————————————————————————

j 1 '

423 '465.5 37.5 100

,i

465. 5 470. S 5 100

470.5 477.5 7 100

! 1 77*^ *92.. 5 15 10 0

jLt-med cjr"een, v-fo^ very finely banded chloriti?,e{i anflftsiti f.

j tuffs - banded 65W TGA @ 448'.i

li - * Rhyolitir1 t^iff*?

l!' ^ 9

i Andesitic tuffs - chloritized.li

i

11

11

DRILL E CORD

COMPANY

REMARKS

Drill by

iizft

Hole No, 2BISON PROJECT SL- 3 ^5 AZ. INCL. COORDINATES ELEVATION S heec N3^

Depth: 511

: Dace Loggedby; Dace From To From To

?ooca S e

?ror

49?- 5

499.5i i

--

i1

Recovery

To reel 5

! 499,

511

? 7

11.5'

51 1

100

Assay Res .;!j j ! DESCRIPTION

ii| Chloritized andesitie tuffs.i

ji 100 ; Medium arained quartz diori to .

i i

t

1

l

i;

i.

\

li 1

1l

l ' 9 .

\\

i '

L * * t

i 1

j!

i

eCOMPANY: B /SOA/ PETROLEUM*MMZ3ALS LTD.

2O C

ttll

2 O Oo

*

c(O

z8

DRILL i C O R D

COM?ANY BISON PETROLEUM E, MINERALS LTD.PROJECT S L-3REMARKS: AZ.

22 O0 Mag

INCL. COORDINATES

L 12W/48+50N

ELEVATION10'

Irakis'

Hole No. 3

Sheet NcVl

Depth: 294/600

Drill by:Lambert..

Dale ?ro-.Mar 28 ToMar 31

Logged by:B

Date From M Tp Apr 1/70,

Foocas a i Recovery (Assay Res.i'DESCRIPTION

AX i O i 61 6 i Casing.^i j i

AXQ l 6 1 245.5 239.5 100 ..L t,-med,.gre,en-gray,,, y- f g- yje.ry, f ing .ly... Xnterband ed.. chlnr.i tl?.p.ri...jr.uf f.

245.5 277 ! 31.a 100

and calcitic siltstones, scattered l"-2" zones in which light min, is quartz rather than calcite. Dark min. is generally chlorite. "ClTTartrl1 z 1e1 (S' 1 '- 1"S'llp""- 1 "s~h~elir" races" carry1 minor" py minor v-i 11 x-cutting quartz veins. Gneissic texture {quartz-bio-chlorite-

s) ...l 82' - 3 8 c-' . Mi nor- --* S-'---l-.-5-L-225'. Banded: 400-50O TCA 6'-50', 40O TCA @ 70', 50O TCA @ 94', 550 TCA @ 123', 550 TCA @ 174', 55O TCA @ 216'. Quartz breccia

V-f(?-black~slatv, contorv.ed, fractured and sheared carbonaceousgraphitic material w/very minor diss, py on strong graphitic slip-shear faces.

1279 ! 2 l 100 |

!27Q '-i- q inn

1282.5 294 11. 5' 100 i

...Chlor i-tJ

.Sa.me as ^6 ' -245,. 5 ' f j,,bu.t V//6 , 2 "r 4", ZOAQS ...y-f g j very finely cherty sedimentary iron formation, very magnetic.

DRILL 'E C O R D

COMPANY BISON PROJECT SL-3

R2XARXS: AZ INCL . COORDINATES ELEVATION

Hole No.

Sheet NW

Depth: 600

3

2

Drill by:To

Logged by: Dace From To

.ize? c o c s s ! Recovery !Assay Res

Prod To ! Feet DESCRIPTION

AXQ. 294 366 72 100 V-fg-yery finely banded, alternating black and gray bands 1/16"-1/8" cherty-slaty sedimentary iron formation, very magnetic.l' Quartz-chlorite schist 334-335 and 6" zone 347-347.5'. BandedGO TGA Q 348' .—————————————————————————————————————————————

366 l 404 38 100 Same as 282.5-294.0, w/solitary V8"-174" bands of iron formationand l"-6" zones banded iron formation in chloritized tuffs and siltstones banded 65O TGA @ 394'.

i4041 600 i 196 100 Lt. green-gray v-fg, very finely banded chloritized tuffs and

siltstones" w/bccasional 1/16 "-1/8*"" s earns bif iron formation, i.e., one seam each 5'-10' of core and occasional l'-2' gneissic

o 500-550', banded 70O TGA Q 4.25'-474' r-300 TGA 6 540'-600'.

600 i End pf hole - test taken, but suspect that hole flattened

c

PETRQLEUMeMINERALS LTD. - 5'Z. - 3 O.O.H.NO.: &I -3

ENDED: AMcj/31, i?7O

D.D.H*3

Grahitic, stone tecraa'srf

formation

6 J ~

f /"-G'' .Zone* o?' gafjaffd' /.-on fbr.r.af.

^ G Z "-c" 'toffs - C/irrfy Vffy f 'in f Grai/i

for/tialiofi , Very . Wa

-t i -vvsj' " ' PC , T1'

'-fr^ of c*re.

W D R I L L 1rnvp; vv

' "'BISON PETROLEUM l MINERALS LTD. PROJECT-^yj^.^,,, .

Dri

^ V ."•A

AXQ

H -

Hole stopped at 350' due to A2 .unsafe ice conditions. ^-s^n ,, 2 2 C 0 Mag

1 1 b y ; Date St. Lambert F r or, Aor 5 To Aor 8

7 o o t a g e Recovery iA f- say Res.!:i ' l ' l | ! F r or:.1 To i Feet ro j ^ "

i i !! 0 ; 25 25 !: Casinq.

^E CORD V

Hole No. 4 SL~ 3 *A

IXCL. COORDINATES ELEVATION S hcet N" LWillet La. ;e f...

550 L 28E/30+OON ice drepcn. 1 37 y 350Logged by: Date

W. B. Blakeman From Any 9 To

DESCRIPTION

' ! 25 i 98 73 100 i! Ked dark crray-black-v-fa , very finely banded car bon arsons ?,ilt-

\ s tones w/graphitic slip faces and minor py assoc. w/graphite. j Minor slaty-shaley zones. 1' quartz rich zone w/minor chlorite and

i ; ' l 1 leached banflefl and "fil'SS py 'and pytif - /^'-/j 1 ; c^uartz-chiorite 'j j; breccia zones w/very minor assoc. py and pyrr @ 75.75-76.5',

i ! j banded 35O-40O TCA 25 '-98'.

•:

l i li98 09 1 100 \ Lt.-med qray, v-fq, verv finely banded/ interbedded siliceous

i i i j ;l chloritized and serpentinized tuffs w/very minor diss py.t , j;

i | t

1 '99' 105 6 100 i ; 1 Ouartz-chlorite schist - foliation 40O TCA.lil j!

i i !:105 i 120 15 100 : Lt.-mc-:d crav.

l i f; minor diss py -

120 ; 137 17 100 ii ?q, very fine!

t

v-fq f very- finely banded rhyolitic tuff.3 w/veryon fracture faces.

y banded quartz-chlorite qneiss w/very minor 1/16"| i; seams Of black carbonaceous material and occasional 3"-!' zones ' ;' of rhyoj.itic tuff npc;^ fhsn i^s-^

DRILL E C O R D

COMPANY BISON PROJECT SL-3

REXARXS: A z ^ INCL. COORDINATES

Drill by: Dace Logged by:.mm F r o m To

] Footage i Recovery Assay Res. li

Hole No. 4

ELEVATION S hcct N"^ 2

Depth: 196/350

Dace From To

fiZC Fro, To Fee, 6 | ! DESCRIPTION

i j i AXQ 127jn8.5 1,5 100 \\ Ouartz-chlorite schist.li! i!li( ! 'l

j j . 1

•138.5 146. '5 8 100 i i S^me as 1^0-137, l^vit- gr^at-i^r t-hAn pna. rhy rili^-ii"1 t-iTf^c\ -\

p|ii

J ij146.5 147.75 1.25 100 )| Med-dark rjr^n, y-fg/ v^ry finely banded,

;! quartzose-chloritized tuffs w/very minor i -i! pyrr.

banded and diss py and

| i t .

! : j . li 147.75 187 39.25 100, ' . i Predominantly {greater than, Rfi*) hlap.k,,v ,. , ,-f r.', \rfri-v f i nrO \ r . K,i /-l^/-!

li to massive carbonaceous material (siltstone) with graphitic j! shead-slid faces and minor assoc. py. Minor zones of interbedded

j : i :, v-fcj, vex'y zineiy Danaea rn.yoiitic and chioritized tuffs w/weak j to moderate diss and banded py and pyrr @ 149 . 5 '-152 .0 ' , 154.75'-

i '' , :' , , 156 0' bmndod •lO TCA @ 151'. -.. ,- .^..i ' ' *

ii; ; *i 187 '189.5: 2.5 100 ; Ma, quarts - f elds - bio. nneiss.

t

i '' ' l 1 1189. 51 196 5.5 100 i 1 V-fg, very finely banded - massive rhyolitic tuffs.

i i! -

c DRILL S C O R D

CCXPAXY

REXARXS :

Drill by:

j ?oo:ase-. z e ; j-

! ? r o r.: To1

".XQ l 196 i 197j , i! 11 ; 1

i 197 1198.5i i

i '198.5 2491 i

1

Recovery.

reef S!

1 i ICO

i1. 5 ' 100

l

50.5 100

^ H o 1 e N o . 4ilSON PROJECT SL-3

AZ. l INCL. COORDINATES' ELEVATION S heec N cDe?th:2747350

Dace jLogged by; Dace 7ro- To From To

Assay A s s . 'ii . i .- DESCRIPTIONi i

i|!

: ; Fg, finely banded chlorite - calcite schist.•ji*

i ( ' l v-fcr, rhyolitic tuffs.

V-fg, verv finelv banded massive, indurated black, slaty-carbonacecgraphitic material w/prevalent graphitic slid faces and w/minor oy assoc. w/graphite. Contains cuartz-chlorite zones w/weak zo: : - uy tissue, w/giapr.

, , ' I M "' "•;:.ccc!ra iw'S i~ id iiss a;ju ; i ; - :' 209'-209.5' , 219' : : i -J "-P" rhynl-jMo *1 ; j : ' . ' 2 39.0' . Banded 4

! 249 270.5 20.5 100' :; Med-dark gray, y-

iv.e. v.onzair.s quar*.z-cno.orj. ue ^or.es w/weci^; *.o

-219.5' ," 222.0'-222.5' . Minor (less than 15S)\". f f ^ ~H''"! ^ ?^^— "54^ Q'lArt" 7 — f'n 1 HTI i*A qnAicvt? ? ^-7 c ' -

O6 TGA @ 239' .

rg, verv finelv banded massive rhyolitic tuffsi ; : ; ; 'i w/weak diss and banded py and pyrr 249 .75 ' -250.25 ' , 252 . 5 ' -253. 5 ' ,

i ; ; ' and graphitic zone w/weak to moderate py and pyrr 266 '-267.5'.

i ; l i 1 ; ; * ' '. li 1 .; i i i j : 270.5 274 ! 3.5 : 100 ' - Same as 198.5r249 w/weak diss and banded py and pyrr.

' \ - ': ' \ '~

; . ' , l :

: ; ; - .

c r .cCOMPANY: BISON PETROLEUM s MMZRALS LTD,

S/era/to* ' Wrf/ft Late i l z e.

Ye s y /"//fg J2a*a'ftji' Car&os/a to/fti

CA'iis: i,7z.t\*' Ti/rYbAify f/nor

DRIL.L^ECO•*

COMPLY BISON PROJECT S L- 3 H OlC * *

X&A™*'' \ AZ. INCL.i

. , ,. , .. ,, . M. , J^————

COORDINATES ELEVATION S hect N^4Depth; 350

i) v i 1 1 b y : "^-. u a L o g g o d b y : Date— - — ...- ...-,... .-.....-..r ... n . .. . . ..., , J'.r.o."..... ^.To,,,,, .....- ,, M l , n t* t on T o _ ,

l' o o t c. z z i R t c o v t r y ! A s t, a y R a s . rS 123 i ' ' : 1 ' i " T " T - ". n

? r or/ To i Fceti f- ; . ! - !

1 r i :! AXO 274 i 318 44 100 j Ked.-dark arav, v-fa.

ESCRIPTION

verv finelv banded massive jrhvolitic tuffs ,! . :i w/less than 15^, 2"-6" graohitic zones, very weak banded and i j , diss py and pyrr @ 2g7'-298.5', 307 ( -308', 309-309. 5', 312'-314',l 1 ' i ;' 316 ' -318 ' '.""Banded" 40 "

i ': iTC'A \S J UU ' .

318' 324 ! 6 ;100 Sof t-crumbly-qraphite- no sulfides. . . ... .i i i 1

j | i

i l .

324 : 330 6 100 1 ' !' Interbanded rhyolitic tuffs and limey siltstones w/weak to moderate1 j ' ; i 1 diss py and pyrr 328-330.1 ' l

'- i 1 'ii 1 i'330 : 331, 5 1.5 100^ : Soft crumbly graphite w/rnoderate diss DY and pvrr.

: i i i . i; - "i '. 1

! ' i 1 .' 331.5 350 3.8.5 100: ,i Same as 324-330 - no mineralization, banded 45O TGA @ 343.

! : ' i i i,i . 1 ;- i ^ i 'ii : ! 'i ! 350 i ' End of Hole ~, No Test.

iii''

l i li l

* DRILL E C O R D*"*f} V "^ j^v BISON PETROLEUM fi, MINER/vLS LTD.P^OJECTREMARKS: AZ.

Grid South

SL-3

INCL,55'

COORDINATES

L 32M/12+5QS

ELEVATION

10.

Hole No. 5

Sheec x9l

Depth: 76.5/547

Drill by:St. Latr.bert

u a t eFrom Apr 12 TO Apr 14

Legged by:W. B, Blakeman

Dater1 r o TV. Apr 14;o

Recovery i Assay Res.

l Frorr.! To \ F eed-

r.X O ! 10 i 10 i. 5

DESCRIPTION

Casing.

AXO JLO ': 51.51 41.5; 100 t,., gr.gen~gray,j, y— f g, very finely, silicified and ch.lnri t.i.7.ecltuffs interbedded w/rhyolitic tuffs, very minor py assoc w/ chloritized slip faces. Slip faces parallel banding @ 35 TGA TOT6 bl.b 1 - badly tractured JLO'-iJtt 1 .————————————————————

51.51 54 2.5 i 100 i

l

slaty black v-fg , carbonaceous, gr aph i tic zone w/steong g r aph i t i c slip 'faces, moderate leached banded py'assoc w/graphite faces.

54 ! 61 ' 7__i 100 M-vfq. finely banded It. gray rhyolitic tuff.

61 i 71 10' 1100 M-v-fg, finely banded It. gray rhyolitic tuff w/minor very finely. diss pyrr and py parallel to banding @ 35O TCA

71 i 75.5 - 4 .5 100 Lt. gray-It, green, v-fcr. very finely banded rhyolitic tuffs andmassive rhyolite. Minor biotite diss in tuffs. Very minor py assoc w/fracture faces.

75. 5(76. 51 l.OilOO Same host as above but w/weak to moderate py and pyrr diss , narallel to banding.

DRILL E C O R D

COMPANYBISON PROJECT SL-S

REXARXS AZ. CNCL. COORDINATES ELEVATION'

Hole No. 5

Sheet N

Depth: 360.5/541

Drill by: Dace "' r o r. To

Size!'Footage Recovery .Assay Res.ii

Logged by: Date From To

?ro-' To Fee DESCRIPTION

AXQ ! 76.5; 91 14.5! 10Cii i

Same as 71 to 75.5.

91 ;94.5! 3.5! 100 Same as 75.5 to 76.5 but with me derate py and pyrr diss parallel to banding.

y . 3 ! . l 3 B : O Same as 71 to 75 t 5. no diss sulfides, graphitic zone 112 to 112.75. banded 40O TGA @ 143.

158 ' 218 : 60 ; lOOi Essentially same ,mineralogy as 71 to 75. 5 but w/gneissic-porphyroblastic texture. Prominent angular quartz fragments 1/64" to 1/8", commonly well foliated appearance, moderate •cis's-pyrr "and py '161.75 "tu "l6"3 y 16^9 v 5 tu~ -17O .'S ,' V fc-rdiss pyrr - 176 to 177.75, moderate diss pyrr 177.75 to 178,Waak di sg pyrr '.ft A fn Ift^ h*nrJori A ^ TPR Q '. 7 d .——————————————

iiL.

!218 22S.5 11.5 100! Well foliated m-calcite - no

m~v-fg, chlorite qu art z jC eldspar schist w/very mino- culfides, foliated 2"20^TCA @ 220'.

229.5 : 360.5 100i

Same as 158 tQ,218, but, w/5%. to 101 massive rhyolite and 10V.to 15% banded rhyolite, very weak diss pyrr 232 to 242.5, scattered blebs calco noted @ 236; weak diss^oy.rr. and py 252.5 to j

DRILL RECORD

COMPANY BISON PROJECTREMARKS :

Dri

Size

11 by

Foot

? r or.

417

-

see

To

DateFrom

Recovery

Feet *

i

t

1 439 22

i

il

439 456! 17

459ii

459 4*,1

3

f\

100

100

Assay Res."

____ i .

AZ.

To

zones commonly

Hole No 5 SL-3 ^

INCL . COORDINATES ELEVATION S hect X o 'Depth: 471/547

Logged by: Date From To

D1

ESCRIPTION

carry anaular cmartz oorohvroblasts uo to 1/4"j maximum dimension.i|

'' Dark qreen-aray-black . masfiivf* and handed silicified tuffs hadlv; broken and fractured- (fracture faces carry mod. py) 417 to 425.

j; Massive rhyolite commonly carries quartz (angular) porphyroblastsj; up to 1/2" max

i!

. dimension Quar'tz-chlorite zono 4 32 to 433.

Tf-*^ f i HP'1 w han^or! oh 1 o-r i i- -i .^.o/? /.^nr'./a.cj. i t- i r-*? \

l! tuffs, banded 65 TGA'i

@ 444' .

1.1: ' i1 i'100 i: V-fq, verv finely banded It.-med arav rhvolitic tuf^s.

100l

i!i

i:

li V-fg, massive to verv1; 9 ra

finely banded blacX .slaty...c.arbonacfiousphitic material interbedded w/25% It. gray rhyolitic tuffs.

461 471 10 100 Lt. gray vr-fq, very finely banded ,wZvg,yy,. PUi, py assoc w/ and parallel to banding 50O to 55O TGA in 10' section.

DRILL RECORD

cox? AX yREMARKS

Drill by

Size1 1.- - r-jx.

BISON PROJECT SL-3 H olG * * '^t AZ. INCL. COORDINATES ELEVATION S hcet N o ' 5

Depth: 517

: Dace Logged by: Dace Froir. To From To

?oo cage

?ror

471

To

547

Recovery Assay Res i i!Feet fc ! f i "i DESCRIPTION

76

i

i

;l ;i

100 !' Med-dark qreen, v-fcr, very finelv banded chloritized (andesitic?)

l

1

j

1 1 '

l

1

"

ji tuffs w/minor diss py assoc w/ and parallel to banding as well as i cross cutting fractures. Massive andeiitic zones at 484' to 494 ',

———————————— 525' Lo 528'; 532.75 Lu 534.2-5', blebs of py asijoc w/cM^lTtYelS —— ! slip faces at 532 to 533' banded 45O TGA @ 544'.

i!,/

|i

J;

i i!

] 1

1 ____

i i i i

j;

j! '

| j

i' ' . .i j

S ' i

DRILL E C O R D

COV? I*NV' Hole No. SBISON . PROJECT SL-3 ^

REMARKS :-. . . .. . ,..,-,.. — —— — — — - —— i — , , , — —... ...,. -.. . .,. . ^^—

A2. l INCL. COORDINATES ELEVATION S heet N^Depth; 417/547

Drill by: Dace Logged by: Date From To From To

? o o t s g i j Recovery | Assay Res.ls *2ej i : j j | | DESCRIPTION 1 From' To i Feet! S i J l i

J 4

|

360.

t

l -.r-,' 3 67

: 371

!

375t

1

j

1 381

! i j

i : . 254.5. 261.5 -to 2fi4. 765 ^ ? fi q . 5 71 t o ? 7 ^ . v nrv wpalc ^isc; nvrrl

j

^ 367 ' 6.5

ii t

371: 4

i

37: i 4;

381 6

! and py 276 to 277, 278 to 284, 303.5 to 304.5 chloritic zone" i 343.5 to 344.5. Banded 60O TGA @ 299'.i1 i!1 ' i i

ji

100 : Same as above (229.5 to 360.5} but interbedded w/30% to 353, v-fcr.i ;; slaty/ black, carbonaceous graphitic material, minor py assoc

i w/graphite.i -;

i . 'i

100 ' ' Same as 158 to 218 feet.i pj i ; ii

- - i 1 100! ' Same as 360.5 to 367, but w/40% to 501 slaty carbonaceous qraphitic

i- material w/minor py. banded 60" TGA O 374 feet.1 i

100' V-fg, banded rhyolitic tuffs w/30% slaty black carbonaceousi j . : graphitic material.1 !:i i

417! t g

.1 ' "•"' " ' - ' ' - i

inn ; ;: T,t. . rrrAAn-lt-.- rrr^v rh T nr i t i 7.&A s nr? RI T i ri f i Pr3 Anrfps -i t- -i r ^ '?^

i j j j; tuffs interbedded w/10% to 151 v-fg rhyolitic tuffs. Rhyolitic

COMPANY: BISON PETROLEUM * MINERALS LTD. PROPERTY: - 3 O.D.H.HO,: &I ~ So

L.ME: 32+OOW. AZ . 220 OIP . SIZE: LOOKING:

STARTED: ENDED: SCALE:

D.D.H."5\'0

0 g/tretibs: t/t/mp tate -no'j___SvurAcc

i IQO'

////.r^- tfsatffj, Z. iff Si/ Gray - Gff** 1/ss/ .f/ae Gra/fi

r J Tuffs

M,-ticr f'ofifi of

102:a tf/i/o/S/t'c 7irSf AV/yo/tfe

}'o Moo's rvfc Pyr/. o^tr f^tfirc

S.yM /c Mce&urrt Gsft* f"'/ fit f Gtw, Mv CSifartfizet/ Ti/ffc mM M/'aos Py Axsoc.

Afassire

f.DRILL RECORD

COV?ANVBISON' PETROLEUM S, MINERALS LIMIIt?#'""7:CT

REMARKS :

Drill by:

Sizenmmasss.

ACQ

? o o t a z c'mi

Fret:icaa— .'*-3m

0

1 To

12

12 80

St.Date

Lambert From June 1Recovery

Feet

™JL2^.

68

it

80 84.5i

4.5

84.5 176j

i

176 373

91.5

197

fci

Assay Res.!:

1 i M

AZ.

2 2 O0 Mag

ToJune 4

Hole N o^^ 6SL-3 ^

INCL.

550

COORDINATES ELEVATION S heet N o 'dump L3Ke D e pth 5373/4 52 la + SOS/T.inP 4RW 4-1^ T?R^.. u t lj '- 11 --" '

Logged by : Date

D ESCRIPTICN

Z)f?t? ^."x S~ ' i /asincf.1

100 i i' K- f a andesite anri r-.h 1 nr 1! f i v nA \r-fn. \rm-\r f i^olx/ Kanr^Ari i n /-Ir. .n -i J- . .i s~ ?

;| tuffs. Strongly chloritized slip faces parallel to banding j ,! commonly carry weak to moderate py mineralization. Banded 45li iij!

100 i Lt.

100

1 * 3b', 55^

-med gray,

TGA @ '79'.

f-mg. generally massive diorite.1;

' j

|

j

- j Same SK 12 to. RO 1 . hiahTv fihlnr i l-.i ,--r-^ 1 r--! t-. r* hanrlprt ?.nnA.- 1 m ' -Hoj; 103.5' minor porphyroblastic rhyolitic zone 134' to 136'. Banded i 450 TGA @ 147, 156, 175, and 3Cb TGA @ 153.5'.

!100

. ..

, i

: M-v-fq, massive to very finely banded, whito to med qray, hicrhlyj ! siliceous rhyolite and rhyolitic tuffs w/woak to moderate diss !| and lightly banded py and pyrr over entire section, but best

: jiiiutJi. cilization .is cit : j; 256' to 262' , 274' to

/..'b' CO 1 61' , m. tO A 11 , .^U.S 1 tO fi 1 ,276. 5 1 , 281' to 284', 287' to 291', 348.5'

Ij commonly carry nodular and platy pyrite. Occasional (secondary) ;| quartz fracture filling voinlets also carry weak to moderatei di s s py banded

____________ l _ ———————— —T—65W TGA @ 207', 8CO TGA @ 316'.

j^^^v~iDRILL R'E C O R D

COM? ANY BISON PROJECT

REMARKS :

D r i 1 1 b y : Date ••.in Frorp,

iise

tfQ

Footage Recovery

Fro x' To Feet

373 424-

45

Assay R e s . |!

A. ____ L L

100 ; ; Lt

AZ.

SL-3 H 01C N 0 6

INCL. COORDINATES ELEVATION S hcec X o ' 2Depth : 452

Logged by: Date To F r o Tii T o

-med areen*

DESCRIPTION

v-fa, verv finelv banded Chloritized (andesitic?);; tuffs w/ about 10'%'to 154 calcitic bands (white) 1/16" - 1/8" p in width. Chloritized slip faces commonly carry minor nodular

1 •™" - — -f jr jL-a.'^.*sv" l -ucuiucw"UV — uv— y v — '"i U'rv j.n~ a uv,nii?ii L. iiwxv; x o.u. L. v-i-nxjiy .i' 1'

i i •••"•••i ••""•~ r ' -~ . . . - ,, - - . . . . -; l

1 ' i'424 '428.5 4.5 100 ! Lt.-med arav v-fa massive rhvolite w/verv minor diss DV.

428.5 452 23.5i 4

100 l Same as 346 to 424, but more massive w/only about 20?; finelyi. banded Chloritized tuffs.li

i

452

i

t i

1 End of hple, Angle Test equals 5O ! 1-!|

i 1

it *i'

Bay

BISON PROPERTYCLAIM GROUP SL.3

, noyi LOOKOUT

100 VO

126.3 M IUS TO 1HE

r;*

FEB.

BISOK PETROLEUM E MINERALS LTD.GENERAL LOCATION OF

STURGEON LAKE AREA CLAIM GROUPPROVINCE OF ONTARIO, CANADA EXHIBIT l

21

X

UJ

4V52/30'

V! 11 887

2H67I

CLAIM GROUPSL.3

48 CLAIMS

H a so

y. 1 1 &S.O

2 11 B.V)

2IIR5C

r G////er

BISON PETROLEUM r MINERALS LTD.i

CLAIM GROUP SL-3STURGEON LAKE AREA j PATRiC/A MINING DIVIS/ON.ONT.

FEB. 1^70 SCALE \ " -^ M ILE .^ M'L6

\

-V

A* ^y ^*C^.

xx

O

g

It

la 4as

SCD

in

fi i

fa/rt

i l*

-^

/tf.^^

/a;

^

t*

1a

/ft 61a

5\

/a

fa

56

1*

IIINIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIII in52G16NW9I79 62QI6NWM79 SIXMILE LAKE 200

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BISON PETROLEUM?MINERALS IIP,

PRELIMINARY REGIONAL

GEOLOGICAL BASE MAP. STURGEON LAKE AREA, ONTARIO

FEB 1^70 SCALE : 1 INCH ' 2 MILES EXHIBIT