42A*5SEW74 2.7368 THORNELOE010

ESSO MINERALS CANADA

Project #676

Report on a Geology Survey

Thornloe Township

September 11, 1984

J. Macpherson

Geologist

f? r r* r * -. f r- ^ '. v, i; i y L D

nr'T05 1984

42A05SEM74 2.7268 THORNELOE 010C

TABLE OF CONTENTS

Page

Summary ................................................ l

Introduction ........................................... 2

Location and Access .................................... 2

Topography and Resources ............................... 4

Method of Survey and Coverage .......................... 4

General Geology ........................................ 6

Property Geology ....................................... 8

Conclusions and Recommendations ........................ 10

LIST OF FIGURES

Location Map, Thornloe Project ......................... 3

Claim Map, Thornloe Project ............................ 5

Compilation of Previous Work ........................... 7

Geology, Grid "A" .......................... in back pocket

Geology, Grid "B" .......................... in back pocket

- l -

Sunmary

This report describes the results of a geological

survey done by J. Macpherson, S. Hurst and D. Piroshco during

the period June 20-28, 1984, on a group of forty-six claims

located in northwest Thornloe Township. The claims are currently

held in the name of Esso Minerals Canada.

Outcrop exposure is limited to the banks of the

Tatachikapika River, where highly deformed and locally altered

arenaceous sediments, argillites and minor mafic metavolcanics

were observed. Minor sulphides in concentrations usually less

than 3 Ji were noted in the most deformed and altered sediments.

A northwesterly shallow-plunging fold is interpreted

to be present in the vicinity of the Tatachikapika River. A set

of ESE shears are believed to trend across the property; late

remobilization of one of these has caused the offset or

interruption of N-S trending diabase dykes.

Further work in the form of overburden drilling and

IP surveys is recommended.

- 2 -

Introduction

In May, 1984, a block of claims located in northwest

Thornloe township was acquired by Esso Minerals through staking

and by option. These claims were acquired for the purpose of

determining the gold potential of an area (interpreted to be

north of the Destor-Porcupine Fault) which has received little

exploration attention in the past.

The property consists of a total of 46 claims, of

which 22 are optioned and 24 are held by Esso directly.

The geological survey described herein is part of a

larger exploration program which includes ground geophysical

surveys (magnetics, horizontal loop, IP), overburden drilling

and future diamond drilling.

The property was mapped during the period June 20-28,

1984, by the Author, with assistance from D. Piroshco and S. Hurst.

Location and Access

The property is located ten miles west-southwest of

the city of Timmins in the District of Cochrane, Ontario. The

NTS reference map number is 42A/5.

Road access from Timmins is excellent, with paved

Highway 144 located just west of the grid area. There are

numerous good gravel and bush roads on the property as well as

the Tatachikapika River near the east boundary, which is

navigable by canoe.

LOCATION MAP..THORNLOE PROJECT SCALE-- l INCH r.

-- Coloured area is covered ty survey.

- 4 -

Topography and Resources

The relief on the property is generally quite low,

with the exception of the steep sand banks of the Tatachikapika

River, where the relief is in the order of 50-75 feet.

The overburden consists of varying thicknesses of

reworked aeolian sands with some boulders and cobbles. Glacial

till is fairly common at or near the overburden-bedrock interface

and also varies in thickness. Results of the overburden drilling

program indicate that the bedrock topography is fairly rugged in

places.

There is an abundant supply of water in the area,

from the Tatachikapika River in the east and several small lakes

in the southeast, as well as several swamps and small streams

in the western part of the property.

The eastern half of the property has been cut and

replanted with white spruce. The remainder of the property is

vegetated with spruce, poplar and birch in the higher sandy

areas and black spruce, moss and alders in the lower areas.

Method of Survey and Coverage

The author spent a total of nine (9) days on the

property carrying out the geological survey assisted at times by

D. Piroshco and S. Hurst. A grid cut originally for geophysical

surveys was used as control for the geological survey. Lines

were cut at 120 m intervals and stations were located every

25 meters.

BRISTOL TWP.

THORNELOE TWP

796732 796733

796739R9674C 796729 75735C 757355757384757351

79847(796478

798489798480.

Claim sketch, Thornloe Project, SCALE; l inch-^2 mile

- 6 -

A total of 38 claims were covered by the geological

survey. The claim numbers are as follows: P-515909, P-515911,

P-515913-914, P-796729-736, P7967AO-745, P-757349-358,

P-798478-479, P798481-482, P-805191-196.

General Geology

The general geology of the Timmins region consists

of two volcanic sequences - the Tisdale and Deloro Groups. A

thick wedge of metasediments forming a turbidite sequence is

considered to be time equivalent to the Upper Deloro Group and

the entire Tisdale Group. The Destor-Porcupine Fault dips north

and is considered to at least in part mark the boundary between

the Deloro and Tisdale Groups.

There is strong evidence for a major offset of the

Destor Porcupine Fault just east of the Ogden-Bristol township

boundary. The offset appears to be in the order of 6 km and

this places the main break just north of the east-west portion

of the Tatachikapika River in central Thornloe Township.

North of the fault the rocks appear to be folded

around a series of E-W trending axes which dip north and may

plunge to the east. South of the fault there is little evidence

for folding, aside from some minor slumping or possible drag

folds in the iron formation.

The volcanic sequence thins rapidly westward and

pinches down to a few hundred metres in thickness in western

Denton Township. Intrusives in the area consist of the large

BRISTOL TWP.

THORNELOE

HOLLINGER, 1958-60-a . ̂ B. K t mi **4^4fcl * rmag, EM, DO (5800');

PRBUS8AG CANAO/ M, VLF, 00(397 Thorn

Projei Area

ACME OIL ft GAS, 1968 AEM aurvty

HOLLINGER, I960 mo g, EM. DO

DOMINION GULF, 1951 mdg.EM, DD(2007')

COMPILATION OF PREVIOUS WORK IN NORTHWEST THORNELOE TOWNS

SCALE;

8 ~

granitic batholiths, quartz-feldspar porphyries, gabbro sills and

late diabase dykes. Some of the diabase dykes fill late north-

south faults which have varying degrees of offset.

Property Geology

The only outcrop exposures found on the property are

located along the banks of the Tatachikapika River.

Highly deformed arenacous sediments are exposed

along the riverbank for a distance of about 400 meters. There

are also minor amounts of interbedded argillite and mafic

metavolcanics.

The arenacous sediments vary from medium to coarse-

grained and contain clasts which are usually feldspar and/or

quartz. In a couple of localities, the rock appears to be more

like a porphyritic intrusive. The beds vary in thickness from

a few centimeters up to 2 meters. Contacts are usually sharp

and are represented either by a narrow argillaceous unit (*C 5 cm)

or by a distinct change in grain size. Aside from quartz, the

mineralogy consists of feldspar, sericite, carbonate and iron

sulphides. The concentration of the latter three minerals vary

greatly from outcrop to outcrop but are predominant in the more

deformed sediments. In these areas, the rock is a quartz-sericite-

carbonate schist, with up to 3% disseminated sulphides, usually

pyrite.

The structure of the exposed areas is very complex

and interpretation is difficult due to the lack of good exposure.

- 9 -

There are at least two main foliations visible in the rocks,

along with one major lineation. The first foliation (Sp trends

about N45 0W and dips anywhere from 65 0 SW to vertical. The 82

crenulation strikes N40 eE on the average and dips are shallow

(35 0-45 C ) to the northwest. The lineation caused by the inter

section of S^ and S2 strikes N400W and plunges 15 0-20e .

Bedding contacts, where visible, appear to strike

subparallel to S^. There appears to be a set of weak shears which

strike approximately HO0 . It is in these shear zones that the

greatest alteration and concentration of sulphides occur.

Interpretation is difficult with the limited amount

of information available; however, one possible picture is that

there is a shallow-plunging syncline oriented at about 1300 and

plunging to the northwest. Late N-S faulting and possibly further

folding have complicated the picture. It is pointed out that the

above is a possibility only and is based on very limited data.

Elsewhere on the property, the geology must be

inferred from geophysics and the bedrock chips from the overburden

drill program. There are three diabase dykes: on L2080E, L1320E

and L600E. All three are interrupted around the baseline and two

show appreciable offsets of about 150 meters. This suggests a

major break trending at about 105 0 , which was remobilized

subsequent to the intrusion of the diabase dykes. The iron

formation indicated on L-240E-720E, south of TL900S is abruptly

terminated between L240E and L120E by a N-S trending fault which

can be traced at least as far north as the Bristol Thornloe

township boundary.

.../10

- 10 -

Conclusions and Recommendations

The property is underlain mainly by sediments, trending

roughly 110 0 and dipping to the north. There may also be lesser

amounts of metavolcanics present. These units are cut by one or

more shears which are approximately parallel to bedding and also

dip north. These may be splays of the Destor-Porcupine Fault

System.

Exploration activity must be directed towards further

overburden drilling coupled with IP surveys to help locate

areas of sulphide mineralization in or around the major ESE-

trending shear zones.

STATEMENT OF QUALIFICATIONS

I, Joseph A. Macpherson, do certify the following:

1. I am a graduate of Laurentian University in

Sudbury, Ontario, and hold an Honours Bachelor

of Science degree in Geology.

2. I have been practising my profession

continuously since graduation in 1980.

3. I have no personal monetary or stock interest

in any of the properties which are discussed

in this report.

Date: /. ///W Signed: Q,

42A*5SE8*74 2.7268 THORNELOE 300

Mining Lands Section

Control Sheet

File No

TYPE OF SURVEY

MINING LANDS COMMENTS:

GEOPHYSICAL.——•••W*

/ GEOLOGICAL

GEOCHEMICAL

EXPENDITURE

l IfJ Signature of Assessor

Date

Ministry ofNaturalResources

Ontario

Report of Work(Geophysical, Geological, Geochemical and Expenditures)

Mining Act

Instructions: Please type or print.- If number of mining claims traversed

exceeds space on this form, attach a list.Not*: Only days credits calculated in the

"Expenditures" section may be enteredin the "Expend. Days Cr." columns.

Do not use shaded areas below.Type of SurveyisT

GEOLOGICALTownship or Ar*a

THORNELOE5NEL;Claim Holder(s)

ESSO RESOURCES CANADA respecter's Licence No.

T-872Address

]0 ADELAIDE ST. W, TORONTO, ONTARIO-jarvey Company

ESSO MINERALS CANADA_____ ^ __Name and Address of Author (of Geo-Technical report)

Data of Survey (from 4 to)20 06 84 28 06 84Day j Mo. j Yr. Day | Mo. | Yr.

Total Miles of lin* Cut

35

Joseph Macpherson, 1340 Richard Cresc., P.O. Box 431. Timmins, OntarioCredits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Mining Claims Traversed (List in numerical sequence)

Man Days

Complete reverse sid* j and enter total (s) here

f,-', -.:

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Expenditures (excludes power stripping) E C O R D E D

OCT1 5 1984

Electromag

MagnetometeT

Radiometric

Type of Work Performed

Performed on Claimlt)

Calculation of Expenditure Days Credits

Total Expenditures

S -f-

Total Days Credits

K -1 1Instructions

Total Days Credits may be apportioned at the claim holder's choice. Enter number of aays credits per claim selected in columns at right.

Total number of mining claims covered by this report of work

DateSept. 20, 1984 (

Record/a Holder or Agent (Signature)

Certification Verifying Report of Workndv

/~

\hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work snn At w itnessed same during and/or after its completion and the annexed report is true.

to, havingAsrformed the work

Name and Postal Addrett of Parson Certifying

Joseph Macpherson, 1340 Richard Crescent, P.O. BnTimmins, Ontario P4N 7E3

|- Dat* Certified

September 20/84ifJed (Sig

1362

1984 10 12 Your File:Our File: 2.7268

Mining RecorderMinistry of Natural Resources60 Wilson AvenueTimmins, OntarioP4N 2S7

Dear Sir:

We received reports and maps on October 5, 1984 for a Geological Survey submitted under Special Provisions (credit for Performance and Coverage) on Mining Claims P 757349 et al 1n the Township of Thorneloe.

This material will be examined and assessed and a statement of assessment work credits will be Issued.

We do not have a copy of the report of work which 1s normally filed with you prior to the submission of this technical data. Please forward a copy as soon as possible.

Yours sincerely,

S.E. YundtDI rectorLand Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3 Phone:(416)965-6918

A. Barr:secc: Esso Resources Canada

120 Adelaide Street WestToronto, OntarioM5H 1T1

cc: Joseph M,acPhtrson1310 Richard CrescP.O. Box 431Timmins, OntarioP4N 7E3

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i ———FSSO MINTRALS CANADA(i'v 'N DF F'^n RE S HI R Cf S C AN A [) A LIMBED

PROSPECT THORNELOE- 1, GRID "B"

— — -. — — .,vj E UL-OOY/i /Hyi j^ f

Q.Jj/flfbtfw&p^

ACCOUNT N 0 ML C N? TORONTO

DRAWN BY j .y. DAT E N 1 c-

AUG 7/84 42 A 5

n* - N 0 MAP N'-1 676 - 1 B

'.C A L. t

1 2500

42A05SE0074 2.7268 THORNELOE