-..-.....1.1111111*1142AI0SW0293 2.3552 CODY

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TEXASGULF CANADA LTD.

REPORT ON MAGNETIC SURVEY

ON

CODY 44

N.T.S. 42-A-11/6 PROJECT: 950

RECEIVEDI10V141980

WINING UNDS SECTION

Timmins, Ontario Don E. Tremblay

TEXASGULF CANADA LTD.

REPORT ON MAGNETIC SURVEY

ON

CODY 44

INTRODUCTION:

In September of 1979, a group of 42 claims were

staked to cover an area of Night Hawk Lake/ in the north half of Cody Township, and west of the main peninsula. A

further five claims were added in January of 1980 to cover the remaining open shoreline area on the west boundary of the group.

The claims are numbered as follows:

P-540038 - P-540049 inclusive

P-540261 - P-540276 inclusive

P-539979 - P-539986 inclusiveP-536831 - P-536836 inclusive

P-528670 - P-528674 inclusive

Total - 47 claims

LOCATION AND ACCESS:

Cody Township is located approximately 12 miles

east of Timmins along Highway 101.

- 2 -

Highway 101 East passes approximately one mile north of Cody Township with Highway 575 branching southward, down onto the Northern Peninsula of Night Hawk Lake. The Cody 44 group lies only 1000 feet to the west of this road access, with only five percent of the claims covering land and the remainder are all water claims.

Highway 575 however, is not open in the winter, and access is generally limited to travel by s'nowmachine.

GENERAL GEOLOGY:

The Night Hawk Lake area consists of Cody, Macklem, Carman and Thomas townships and it has played an important role in the development of the Porcupine Gold Camp, since early 1900.

The rocks underlying it are of Precambrian origin with the oldest rocks being mafic volcanics with some minor felsic flows in south-western Carman Township. These are overlain by a predominantly felsic volcanic sequence which grades into a tuffaceous and sedimentary rock sequence which is most prominent in Cody Township.

Another mafic sequence overlies this and in fact makes up the largest portion of the volcanic rocks in the area.

There is considerable faulting throughout the four townships and it appears that up to five main systems may exist.

- 3 -

The larger regional Destor-Porcupine fault, crosses

the northern part of Cody and Macklem townships and lies just

north of the Cody 44 group.

PREVIOUS WORK:

Relatively little work has been done on this part

icular area covered by Cody 44.

In 1965, Broulan Reef Mines conducted a mag survey

which essentially duplicated the lower three quarters of our

existing property. However, no follow up work or drilling

was conducted at that time.

It appears to be the only recorded geophysical survey

in this area.

SURVEY METHODS:

Line Cutting - North-south lines were established at 100 metre

intervals with 20 metre station spacings.

The lines were numbered from 9 E on the east boundary

of the group to 25 W on the west boundary.

Magnetics - A model G-816 Geometrics Total Field Magnetometer

was used in this survey.

- 4 -

This instrument provides a - l gamma resolution

over a complete range to a maximum of 100,000 gammas.

Readings are given as a digital readout and are

independent of temperature, humidity and battery conditions

Magnetic base stations were established at 100 m

intervals coinciding with baseline and picket line inter

sections. Readings were corrected for duirnal drift using

the closed loop method.

SURVEY RESULTS:

There are only two dominant anomalous linear features,

which were outlined in the magnetic survey of Cody 44.

A north north-west striking mag high and parallel mag

low cuts through the east half of the group. This anomaly is

attributed to a fault structure extending from approximately

940 S on Line O to Line 1000 W at 12 N.

At the northern extremity of this fault, it inter

sects a weak mag high striking west south-west to Line 180 W

at 200 metres north. At this point, there is an abrupt break

in the continuity of the anomaly. While no distinct off

setting continuation of this feature is apparent, it is

probably caused by diabase.

While a number of other local magnetic features

- 5 -

occur within the survey area, no reliable assumptions can

be made as to their causitive nature without further

supportive work.

The overall magnetic background is uniform through

out the property, which tends to re-affirm most geological

speculation that the property is underlain mainly by mafic

volcanics.

Previous overburden drilling however, indicates at

least two areas on the group indicate bedrock of a sedimentary

nature.

Very generally, these would be claims P-540264,

P-536833 and P-536834 in the northwest. The second area would

be in the south end of the property, bounded by the assumed

fault to the east on claim P-540047 and on the north by a

possible contact extending from the fault westward along the

700 metre south stations of the picket lines to claim P-540271,

The area below this appears to be underlain by sediments.

CONCLUSIONS AND RECOMMENDATIONS:\

The magnetic survey in itself yielded little useful

information in the way of providing information on the under

lying geological nature of the property.

Due to the short erratic winter season and typical

thin ice conditions on the Night Hawk Lake, overburden drill

ing had to be carried out prior to the availability of the

magnetic survey results.

- 6 -

Consequently a number of magnetic features which could have been determined by drilling, were in fact, missed by the original pattern of the holes.

Therefore, if there is sufficient interest and importance attached to this group as a potential area of gold exploration, then I would recommend a partial reinstatement of the grid in a future winter season, in order to conduct follow up overburden drilling to determine the nature of other unconfirmed magnetic features.

October 31, 1980 Don E. Tremblay

W. E. Fisher

3807323807SI, 38079

536833 536832 '536831

Night How*——— 4--—— 4 ——

536834(5368351536836 '539979'5399801539981 '5399 1.1 l l i

540264 640263 1 540262

540265540266"540267 5400381 5400395400 RIO ALGOM

— -- - — f —540270 540269l540268

—— f

"" 1540272 J540273 1540049 |5 -1 —— '

540274 540275 A l p -.. " * r* i

*i i* S- ' t~- - — - -

O 3744

Vi?*--

GECOntario 42A18SW0293 2.3552 CODY

TO BE ATTACHED AS AN APPENDIXFACTS SHOWN HERE NEED NOT BE l

TECHNICAL REPORT MUST CONTAIN INTERP;

Type of Survey(s) - Magnet"Township or Area Cody_____________. Claim HniH^M Texasgulf Canada Ltd*

Ave.P.O. BOX nan, s?iSurveynnmpny Texasgulf Inc. (Explor^l^lj Author of Report Don E. Tremblay

nf A,.tw p-0- Box 1140, 571 Jan/80 - SeiCovering Dates of Survey.

Tptal Miles of Line Cut—(linecuttlng to office) 65.26 Km '

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

AIRBORNE CREDITS (Special provision crediu do not apply to airborne j

Magnetometer————Electromagnetic.(enter days per claim)

. Oct. 31/80 SIGNATURE:.

Res. Geo!..Previous Surveys

File No. Type Date

Geophysical

—Radiometric-Other

Radiometric

Author of Report or-" *::yfl ;*-:.s.i* swS

.Qualifications.

MINING CLAIMS TRAVERSED

P-528670 ^

P-528671 '/^

P-528672 ""

P-528673 ^

P-528674 ^'

P-536831 X

P-536832^

P-536833 XP-536834 ^

P-536835-'

P-536836

P-539979"

P-539980^P-539981 1^

P-539982^

P-539983^

P-539984 7P-539985^

P-539986

P-540038P-540039'x

P-540040 ^

P-540041^

P- 540042^

P-540043 XP-540044'x

P-540045 ^P-540046'X

P-540046

P-540047 P-540048"X

P-540049^

P-540261 1^

P-540262^

P-540263^

P-540264 ix

P-540265^"

P-540266 ^

P-540267^P-540268-^

P-540269^P- 540270^

P-540271 '/'

P-540272 ^

P-540273 x

P-540274^

P- 540275^

P-540276 *

TOTAL CLAIMS -47

BILL OF LADING NOT NEGOTIABLE CONNAISSEMENT NON NEGOCIABLE

TYPE OF 8ERV1ICE/TYPE? DE SERVICE

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