32E12SWee24 2. 1641 HOBLITZELL 010

RECEIVED

NOV261974

PROJECTS UNIT

REPORT ON

GEOPHYSICAL WORK

PERFORMED ON

HOBLITZELL 1-73

HOBLITZELL TOWNSHIP

LARDER LAKE MINING DIVISION

ABITIBI LAKE AREA, ONTARIO

NOVEMBER 14, 1974 W.F. GRAHAMTIMMINS, ONTARIO NORANDA EXPLORATION CO., LTD.

i

This report on the electromagnetic and magnetic surveys is submitted under the Special Provision dated October 16, 1967* for credit of 60 assessment work days per claim. The person in charge of the jlinecutting and geophysical work was Mr. W.F. Graham.

HOBLITZELL 1-73

LOCATION

The property, which consists of 10 contiguous unpatjented rain* ing claims numbered L-372036-45 inclusive, is situated in central Hoblitzell Township, approximately 60 miles east of Cochrane, Ontario. Hoblitzell Township is not surveyed into Lots and Con cessions.

ACCESS

The ground is reached by helicopter or by snowmachine trail which has been cut from West Porphyry Lake 2 miles to the southwest where a fixed wing aircraft can land.

TOPOGRAPHY

The ground is characterized by very flat swamp underlain by clay and vegetated with sparse black spruce and alders.

LINECUTTING

One Base Line was cut 5600' due East from a point 100' south of the #3 post of claim #L-372036. Traverse lines were cut at right angles to the Base Line at 400' intervals. The Base Linje and tra verse lines were all chained and picketed at 100' intervals. In all, about 11.1 miles of line were cut, chained and picketed.

MAGNETIC SURVEY

The magnetic survey (field and office) was performed from February 10 - September 3, 1974. The instrument used was a McPhar Fluxgate M-700. Base readings were taken along the Base Line and all readings were calculated relative to the base readings. Readings were taken at the base control stations at periodic intervals to discern day-to-day and diurnal drift. Any changes noted}in the mag netic intensity were then applied as factors and progressive adjust ments were made to each reading taken during that specific period of time.

The results of the magnetic survey are shown on the accompany ing prints. Background magnetics vary between 700 and BOO gammas. The highest magnetic intensity recorded is 14&5 gammas located at

-2- - :

on Line 4+OOE. The magnetics generally trend East-West which the regional strike of the rocks. There is a buildup along the

southern edge of the property which is consistent with a known but unexplained zone of high magnetics on the government airborne mag netic map. The linear zone of higher magnetics extending from 9+OON on Line 56+OOE to approximately 7+00S on Line 0+OOE may be the mag netic expression of a narrow zone of ferromagnesian enrichment with in the underlying volcanics and sediments.

ELECTROMAGNETIC SURVEY ' . ^

The electromagnetic survey (field and office) was pier formed from February 10 to September 3, 1974. j

The instrument used was a McPhar VLEM dual frequency unit cap able of operation at 1000 cycles per second, 5000 cycles per second, or both frequencies simultaneously. .1

:l

The equipment consists of a transmitter and a receiver. The transmitter is composed of a transmitter coil, transmitter console and motor generator. The receiver is composed of a search coil, amplifier, clinometer and headphones.

The transmitter coil is energized by an alternating4 current produced by the motor generator and resulting in the production of a primary magnetic field. This primary magnetic field links with any conductor in its vicinity, producing an induced current which gives rise to a secondary magnetic field. At a given receiving station, the direction and magnitude of the primary field is altered by the secondary field. The direction of the resultant field is determined by means of the search coil with its attached clinometer;. Measure ments are made in terms of dip angles and are recorded in degrees. The plotting of the dip angles at both frequencies gives| profiles which are useful in estimating the depth of the conductor axis, the dip of the conductor and its relative conductivity.

The range of penetration is normally considered to be approxi mately one-half the separation distance between the transmitter and receiver, although other factors such as the conductivity of the overburden must also be taken into consideration.

, .j.

The results of the electromagnetic survey are shown on the prints accompanying this report. Two conductive zones were located.

-3-

onductor "A" extends from 4+OON on Line 20+OOE to 7+OON on LineE. The conductor is weak on the western end and strong on the

eastern end where it is open for extension. The conductivity is excellent. Conductor "B" extends from 1 2+00 S on Line 52*001! to 11+OOS on Line 56+OOE. The conductor is open for extension both east and west and the angles at the ends of Lines 3 6E, 40S, 44E and

all indicate a conductor to the south.

CONCLUSIONS AND RECOMMENDATIONS

Two conductive zones were located. Conductor "B" appears to have flanking mag to the south. Conductor "A" should be' evaluated further east and Conductor "B" should be detailed to determine its length and its relation to the zone of high magnetics to the south. The property should be geologically mapped with special emphasis on the geophysical anomalies located.

W.F. GRAHAMNORANDA EXPLORATION CO., LTD.

32E12SW8024 2.1641 HOBLITZELL

•i \(M\

020

NOV261974

PROJECTS UNIT,

RECEIVED

NOV261974

PROJECTS UNIT

REPORT ON

GEOPHYSICAL WORK

PERFORMED ON

HOBLITZELL 2-73

HOBLITZELL TOWNSHIP

LARDER LAKE MINING DIVISION

ABITIBI LAKE AREA, ONTARIO

NOVEMBER 15, 1974 TIMMINS, ONTARIO

W.F. GRAHAM |NORANDA EXPLORATION CO., LTD.

This report on the electromagnetic and magnetic surveys !is submitted under the Special Provision dated October l6, 1967* for credijt of 60 assessment work days per claim. The person in charge of the iinecutting and geophysical work was Mr. W.F. Graham. j

HOBLITZELL 2-73 ,

' v .i '.-"'---

LOCATION—————— ..^ . . ^ ,j

The property, which consists of 12 contiguous unpatented min ing claims numbered L-374337-4& inclusive* is situated c^n the center of the eastern boundary of Hoblitzell Township with Noseworthy Township. Hoblitzell Township lies approximately 60 miles east of Cochrane, Ontario.

ACCESS v

The ground is reached by helicopter or by snowraachine trail from a small lake l mile to the : southeast which can be Reached by fixed wing aircraft during the wet seasons or in the winter on theice. The lake is very shallow. i

TOPOGRAPHY

The property is characterized by low hills of glacial drift and intervening swamp. Vegetation is black spruce and pioplar. The Burntbush River flows through the property from north to' south.

LINECUTTING.

Two Base Lines were cut. Base Line #1 was cut 2400' at and 3200' at NS00W from the #1 post of claim #L-374343* ! Base Line #2 was cut parallel to Base Line #1 between Line 0+00 arid Line 53+OOE at 12+OOS. Traverse lines were cut at right angles to the Base Lines at 400' intervals. The Base Lines and traverse lines were chained and picketed at 100' intervals.- In all, atjiout 11.5 miles of line were cut, chained and picketed.

MAGNETIC SURVEY :,:: ; '! "

The magnetic survey (field and office) was performed from June 13 - September 3, 1974. The instrument used was a McPhiir Fluxgate M- 700. Base readings were taken along the Base Lines and 1 all read ings were calculated relative to the base readings; Readings were taken at the base control stations at periodic interval^ to discern day-to-day and diurnal driift. Any changes noted in the; i magnet! c in tensity were then applied as factors and progressive adjustments were made to each reading taken during that specific period of time.

The results of the magnetic survey are shown on .fh prints

-2- . . . :' '' ".

this report. Background magnetics vary between 700 900 gammas. The highest magnetic intensity recorded^ is'.1780

gammas located at 13+50S on Line 20+OOE which is an a linear zonei ' of high magnetics extending from 24+OOS on Line 36+QOE to l7+00Son Line 0+00 which is open for extension at both ends. This linear zone flanks the north side of a strongly conductive zoni| which dips to the north. The source of the magnetics may be pyrrhotite.

ELECTROMAGNETIC SURVEYM^M^^MW^MMMMMM^MBH^MHMHMMMMMM^B . | j

The electromagnetic survey (field and office) was performed from June 13 - September 3, 1974. j

The instrument used was a McPhar VLEM dual frequency unit capable of operation at 1000 cycles per second, 5000 cycles per second, or both frequencies simultaneously.

The equipment consists of a transmitter and a receiver. The transmitter is composed of a transmitter coil, transmitter console and motor generator. The receiver is composed of a search coil, amplifier, clinometer, and headphones.

The transmitter coil is energized by an alternating current produced by the motor generator and resulting in the production of a primary magnetic field. This primary magnetic field links with any conductor in its vicinity, producing an induced current which gives rise to a secondary magnetic field. At a given receiving station, the direction and magnitude of the primary field is altered by the secondary field. The direction of the resultant - field is determined by means of the search coil with its attached clinometer. Measurements are made in terms of dip angleSs and are recorded in degrees. The plotting of the dip angles at both fre quencies gives profiles which are useful in estimating -the depth of the conductor axis, the dip of the conductor and its relative conductivity.

The range of penetration is normally considered to ;jbe approxi-: \\

mately one-half the separation distance between the transmitter andreceiver, although other factors such as the conductivity of the overburden must also be taken into consideration. ;

The results of the electromagnetic survey are shown on the prints accompanying this report. Two strongly conductivje zones

li N#00W extend completely across the property. Conductor rt

tends from 1+OON on Line 4+OOW to 9+OOS on Line 52+OOljjt It is a very strong conductor with very good conductivity and probably has its source in massive pyrite and possibly graphite, l Conductor "B11 extends from 17+OOS on Line 0+00 to 24+OOS on Line 3^+OOE. Its characteristics are very similar to those of conductor "A" and it probably has a similar source with the addition of pyrrhotite as evidenced by the flanking mag high to the north. |

CONCLUSIONS AND RECOMMENDATIONS* A V [

Conductors/is probably caused by massive pyrite and possibly graphite. Conductor "B" probably has its source in massive pyrite and pyrrhotite with graphite possibly contributing to the conduc tivity. The property should be mapped geologically with special emphasis on the geophysical anomalies located. *

W.F. GRAHAMNORANDA EXPLORATION CO., LTD.

gtd

Sb O

GEOPHYSICAL - GEOLOGI TECHNICAL DATA

32EiaSW0e24 2.1641 HOBLITZELL 900

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETCJ.

Type of Survey Magnetic and ElectromagneticTownship or ArPa Hoblitzell Twp.

ClaimhniHpr(s)Noranda Exploration Co.,

Author of Report W*F* GrahamBox 1205Timmins T Ontario

Covering Dates of

Total Miles of Line(linecutting to office)

3.1. S

SPECIAL PROVISIONS CREDITS REQUESTED

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

ENTER 20 days for each additional survey using same grid.

Geophysical

--Electromagnetic.

Magnetometer.

Radiometric.

-Other

Geological.

Geochemical.

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer. .Electromagnetic.(enter days per claim)

HATF.. NOV. 15/74 Sir.MATTTRF. ^7 . JAuther irf Report•^r.:

PROJECTS SECTION

Res. Geol.. . -

Previous Surveys f-

Qualifications^

Checked by. .date.

GEOLOGICAL BRANCH.

Approved by- .date.

GEOLOGICAL BRANCH.

Approved by. -date.

Ltd.oronto, Ont.

er 3, 3Q7L.

DAYSperdaim

etic l^s- l)- J

FT f*ty':,:f{]:,'^~^

f to airborne surveys)

inmptrir

V , Ir sm/Mifa*.J'.^QilAHftK"rr/ *7 ^ i^,vu) *~^ ^ *r\

D

MINING CLAIMS TRAVERSED. ^ ̂ List numerically fha^J

K* ft/I . . , A

L \/ 374337 ^(prefix) l y (number) y

L P 37W9 ixL v^ 37434Q vIf *^ Jj //i X M- "j

J t J? y *4*J? wiv ' y

i y L *^ 3743A3 ^

^ yL r 3743A4 v

JU f ! **i^ j X /L 3/1-5 i j

L '/r/ 3TO46 /Y

L './r . 374347 7*y T

L *^ 37434S ^ yt*3^ '

f

''

'Tr*T A I r*T A IMC 12

Show instrument technical data in each space for type of survey submitted or indicate "not applicable"

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS

Number of Stations 6Q2 i nn'Station interval J-VA^ t

It

.Number of (EM) 6l9 (Mag )50* for Mag detailing

Profile scale or

MAGNETIC

Instrument,

Contour

McPhar

intervals 1" * 20 0 (EM)(specify for each

Fluxgate M- 700

200 gammastype of survey)

(Mag)

, .

2 ammas er scale divisionAccuracy - ScaleDiurnal correction mpthoH closed loops of less than l hour dujafrion jjand prpgrespive Base station inratinnEvery 400* along Base Line_______ factoring of readings.

ELECTROMAGNETIC instrument McPhar VLEM SS15Coil ronfignratinn Vertical Loop

Coil separation LOO - 1500 '

Amirary 2 d per scale divisionMethod: SJ Fixed transmitter Frequenry- 1000 Ops and 6000 Ops

D Shoot back D Inline D Parallel line

(specify V.L.F. station)Parameters GRAVITY

Instrument.

tilt, anles

Scale constant.Corrections made.

Base station value and location.

Elevation accuracy________________ INDUCED POLARIZATION - RESISTIVITY

Instrument ——————.——.^.^-—..————.Time domain. Frequency— Power.

Frequency domain.

Drfp array.

nHp sparing

if elertrode

File. . li v/-

lw S9Mu,IK O

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey Magnetic and Electromagnetic Township or Area Hoblitzell Twp.________

hoider(s) Noranda Exploration Co.. Ltd.——- Box 451 Commerce Court West, Torontoi Ont.

Author of Report W* F t Graham———————————.Address Box 1205, Timmins, Ontario

Feb. 10 - Set. 3. 197/1-

Total Miles of Line mt 11.1(linecutting to office)

SPECIAL PROVISIONS CREDITS REQUESTED

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

Geophysical—Electromagnetic—Magnetometer,—Radiometric—Other———

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer. .Electromagnetic. . Radiometric

nATR-Nov. 14/74

(enter days per claim)

SI^NATHRF.-

PROJECTS SECTION Res. Geol. ——..———

* 5 1 OJ

Previous Surveys i-

Qualifications.

Checked by. .date.

BRANCH.

Approved by. .date.

GEOLOGICAL BRANCH.

Approved hy Haf"

MINING CLAIMS TRAVERSED

t H

...k......i..J.7SP3.fe(prefix). (numb

^ ,.mQ3.9,,3

3.7,20/K?,

TOTAL CLAIMS, 10

Show instrument technical data in each space for type of survey submitted or indicate "not applicable"

GEOPHYSICAL TECHNICAL DATA

SURVES

Number of Stations.station interval 100' (50* for Mag detailing)Line snacintr___A.OO*

.Number of

spacing.Profile scale or Contour intervals l" = 20 0 (EM) 200 gammas (Mag)

(specify for each type of lurvey)

MAGNETIC

Instrument McPhar Fluxgate M-700————^———^.———————.

*

fEM) S?? (Mag )

Accuracy - Scale mutant 2 gammas per scale division-—----—--.^.—4—-—--—-—--—~ Diurnal correction methr.fi closed loops of less than l hour duration (fend progressive^ i"

Base station inration Every /i-OO' along Base Line_______factoring! pf readings*

ELECTROMAGNETICVLEM SS15

Coil ronfigiiratinn Vertical LOOp

Coil separation 400' tO 1500'*

Method: Frequency

Parameters nGRAVITY

Instrument

S Fixed transmitter D Shoot back v D In line 1000 cps and 5000 ops

(specify V.L.F. station)iratiiiwi tilt angles

D Parallelline

Scale constant.Corrections made.

Base station value and location.

Elevation accuracy————i-————^————— INDUCED POLARIZATION - RESISTIVITY

Instrument.Time domain. Frequency—— Power———-

Frequency domain. . Range———————

Electrode array-— Electrode spacing. Type of electrode.

HOBLJTZELJLLARDER LAKE MlNMGDIVISION

DISTRICT OF COCHRANE

M502ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

K)Chains tind?NOTE

400* Surface Rights Reservation around all Lakes and Rivers

•r/ ri

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Scale -40NOTE

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around all Lakes and Rivers.

i M

V

\ N

\

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61M

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N"431 "H

7203

S--204

V

V

(

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!147?e8 l 347789 l 347790, 347791 | 347792

l Li i3477941347795'347796

— — -— -j—--.~j.- - —L i L l L

1 347798 34T799 ' 347BOO I3478OIf L i L I~ L i L15^7802 '347803 347804 347805

/347808 347809"

347810 ( 347811 '^547812 '347813

^..^^347821 1347822 | 347823J 3 '17' 82 '1 v

L \ l L - r

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rf^K- i i3671 l? 367H3 | 367M4

, L l L It' J j l

367IIB 136711* l 367H7 '36711* t 367119

32E12SW0024 2.1641 HOBLITZELL

L O E L4 E L 8 E L 12 E LI6E L20E L24E L28E L32E 6E L40E L 44 E L 48 E L 52E L 56 E

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JZZ045

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LOCATION.

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SCALE "* 400'REVISED

PROJ.N9.8.6.

DWG.N2

Magnetic SurveyHOBLITZELL 1-73.

HOBUTZELL TWP. ONTARIO.

PROJ ECT : BiiftMTflUSH AREA

SURVEYED BY: .................,... .DRAWN BY'.....R,.BEAULifiU....... SCALE-..

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J H '" ; B . ; . . t . ; vV '- i . . A 1 ( O

PROJECT: ausBTBjsn ,KL^PROJ.N9..jb;..... SUBVFYFDBY: DATE:N.T.S..3.^t.:;..,.^.. DP AWN BY: p rL , Jjfl! SCALE: v- ^r,'

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ilj

33E125*0024 2.1641 HOBLITZELL 240

L O E L4 E L8E LI2E Lt6E L 2 O E L24E L 2 8 E L 3 2 E L 5 6E L 40E L 44 E L 48 E L 52 E L 56 E

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scale |" E 2640

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ft e At INS S: fattiftont E M. F in togf*** ffl/fl

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SCALE 11 * 400'REVISED

PROJ.NS.9.5.

DWG. N?

V. L.E. M. SurveyHOBLITZELL 1-73.

HOBLITZELL TWP. ONTARIO

PROJECT : .

SURVEYED BY: DATE:...,........,...............,.......DRAWN BY: R^BEAULJEU. . SCALE: .i'V.4OO!............

NORANDA EXPLORATION CO. LTD.OFFICE v TI.MW INS, . QRT,.. ............,.... -. -

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32Ef2SW0B24 2.1641 HOBLITZELL H50

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HOBLITZELL 2-73

SURVEYED BY v... .... ......... DATE'-.DRAWN BY SCALE'-,

NOR AN DA EXPLORATION CO. LTD.OFFICE:.

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