this report on the^electromagnetic and magnetic surveys

N.T.S. #32-0-13x

320i3NEeeee 2.1374 HEPBURN010

REPORT ON

GEOPHYSICAL WORK

PERFORMED ON HEPBURN 1-72

HEPBURN TOWNSHIP

LARDER LAKE MINING DIVISION

NOVEMBER 30, 1973 W.F. GRAHAM

TIMMINS, ONTARIO NORANDA EXPLORATION CD., LTD.

This report on the^electromagnetic and magnetic surveys^ is submitted

under the Special Provision dated October 16, 1967, for credit of J50^

assessment work days per claim. The person in charge of the linecutting

and geophysical work was Mr. E.A Galio.

LOCATION

ie property, which consists of 12 contiguous unpatented mining claims

numbered L-363385 to L-363396, inclusive, is situated in south-central

Hepburn Township and north-central Sargeant Township, It is approximately

75 miles east of Iroquois Falls, Ontario. Hepburn Township is not surveyed

into Lots and Concessions.

ACCESS

The property is reached by traveling north from the Abitibi.Paper

Company Mill in Iroquois Falls along a private road. At mile 74, a bush

road leads north about l mile to the property.

TOPOGRAPHY

The ground is generally low, f l at... lying, and cut by numerous small

creeks. The area has been cut over and the present vegetation ̂ consists of

small spruce, balsam, and alders.

LINECUTTING

One Base Line was cut at an azimuth of 90 (Grid East) for 2400 feet

and in the opposite direction (Grid West) for 2400 feet, from Post #1 of

Claim L-363395. Traverse lines were then cut at right angles to the Base

Line at .400 foot intervals^ The Base Line and traverse lines were all

chained and picketed at 100 foot intervals^ In all, approximately 11,2

miles of line were cut, chained and picketed.

INSTRUMENTS AND SENSITIVITY

ELECTROMAGNETIC

The electromagnetic survey was conducted using a Vertical LOOPli i i M lin M.i in..... i,.. l' linn i i ' -~~~- l IP P P "

Electromagnetic Unit (V.L.E.M.) Model SSI5 manufactured by McPhar Geo

physics Limited.

The instrument consists of a transmitting unit and Receiving unit.

The transmitter is composed of a transmitting coil, signal generating con

sole and motor generator. The receiver is composed of a search coil,

signal amplifier, clinometer and headphones.

-2-*

The transmitting coil produces a primary magnetic field when it is

subj^Red to an alternating current. If the alternating primary magnetic

field comes in contact with a conductive body,a current within the con

ductor will result. It in turn will produce a magnetic field of its own

which is termed the s,econdaryJL

The direction of the resultant field (ie. primary plus secondary) is

measured at given receiving stations by using the search coil and its

attached clinometer. The deviation of the resultant magnetic field from

the direction of the horizontal magnetic field is measured in degrees of

dip. Readings are taken using transmitting frequencies of 5QQO ,Hertz and.

1000 HertzA The correlation of the results between the two frequencies

gives an indication of the relative conductivity of the anomalous body.

The range of penetration of the primary field is normally considered

to be approximately one-half the separation distance between the trans

mitter and receiver, however, other factors such as conductive overburden

must also be taken into consideration.

The results of the V.L.E.M. survey are shown on the prints accompany

ing this report.

MAGNETIC

The instrument used was a Fluxgate Magnetometer Model M-700manufac-

tured by MePhar Geophysics Limited.

The Fluxgate Magnetometer measures the strength of the vertical com

ponent of the total magnetic field in units of gammas. The magnetic field

at any particular station will consist of the vectoral sum of the earth's

magnetic field and the magnetic field of any anomalous body. The latter of

these fields is caused by material that is either naturally magnetic or is

capable of possessing a secondary field which is induced by the earth's

primary field.

To conduct the survey, a base station was established with all sub

sequent readings being taken relative to this value. By reading the Base

Line in this manner, it can be used as a series of base stations from which

the rest of the grid lines are read at 100 foot station intervals. In the

event of a zone of anomalous magnetics (ie. greater than 200 gamma change

between stations) the station interval is reduced to 50 feet.

r -3-

the earth's magnetic field fluctuates with them, it is periodically

neces*s"ary to take readings at a base station to discern possible instrument

or magnetic drift. Any apparent change in the magnetic intensity which

occurs during the time interval between Base Line checks is th|fn applied as

a progressive adjustment to the readings taken during that period of time.

When contoured^ the results of the magnetic survey aid in the determin

ation of the strike/ dip and depth of an anomalous body.

The results of the magnetic survey are shown on the prints accompany

ing this report.

GEOPHYSICAL RESULTS

ELECTROMAGNETIC

The elec^omagnjgj^c^sji^vej^ utilizing a fixed transmitter, was under

taken from ̂ November 22 to November 26, 1973.. Several poorly conductive

zones were detected on the ground. One^, extends from 0+50 south on Line

24+00 west to 4+00 south on Line 4+00 west. Another extends from 5+50 south

on Line 16+00 east to 6+00 south on Line 24+00 east where it is open for

extension to the east. A third conductive zone extends from 19+50 north

Line 20+00 east to 21+00 north on Line 24+00 east where it is open for ex

tension to the east. There is a flanking magnetic high associated with

this conductor but it gives a response characteristic of diabase. A fourth

zone extends from 15+50 north on Line 20 west to 15+00 north on Line 24+00

west where it is open for extension to the west.

MAGNETIC

The magnetic survey was conducted from November 16 to November 18.

inclusive. Background magnetics vary between 1750 to 1900 gammas. A linear

magnetically high area extends from the northwest corner of claim L-363393

to the southeast corner of claim L-363388. It has an east-northeast trend

and values as high as 3900 gammas were detected. It shows a characteristic

response of diabase. A smaller zone of high magnetics is located on the

north boundary of claim L-363392. It is also linear and may be an off

shoot of the larger diabase dyke. An isolated magnetic high is centered on

the Base Line at 6+00 east.

r

' CONCLUSIONS

ie conductive zones located by the electromagnetic survey display

only weak conductivity and in general no magnetic correlation. The magne

tic high extending across the entire property can be attributed to dia

base. The northern and southern portions of the property are magnetically

flat. The conductors are probably due to conductive overburden rather

than massive sulphides or graphite in bedrock. The property should be

geologically mapped, placing special emphasis on the zones of conductivity.

6 ~W.F. GRAHAM

NORANDA EXPLORATION CO., LTD,

H.T.B. #32-D-13

DEC 1 2 1973PROJECTS SECTION

f

i 32Di3NEeaee 2.1374 HEPBURN

REPORT ON

GEOPHYSICAL WORK

PERFORMED ON

SARGEANT 1-72

SARGEANT TOWNSHIP


NOVEMBER 29, 1973 W.F. GRAHAM

TIMMINGS, ONTARIO NORANDA EXPLORATION CO., LTD.

This report on the electromagnetic and magnetic surveys is submitted

under the Special Provision^ dated October 16, 1967, for credit of 60


and geophysical work was Mr. E.A. GAllo.

-1-

LOCATION

ie property which,consists of two contiguous unpatented mining claims.

numbered L-363397 and L-363398, is situated in North-central Sargeant Town

ship at mile 74 on the Abitibi Paper Company road leading north from

Iroquois Falls. Sargeant Township is not surveyed into Lots and Concessions,

ACCESS

The property is reached by traveling north from the Abitibi Paper Com

pany Mill in Iroquois Falls along a private road. The road passes through

the centre of the claim group at approximately Mile 74.

TOPOGRAPHY

The ground is generally low and flat lying. Vegetation consists pre

dominantly of small spruce and second growth balsam..

LINECUTTING

One Base Line was cut 2500 feet afr an azimuth of 9QO from a point 700

feet south and 100 feet east of the #3 post of claim #L-363398. Traverse

lines were cut at right angles to the Base Line at 400 foot intervals. The

Base Line and traverse lines were all chained and picketed at 100 foot in

ter yals. in all, approximately^2,2 miles of line were cut, chained and

picketed.


ELECTROMAGNETIC

The jelectromagneti^survev^was conducted using a Vertical Loop

Electromagnetic Unit (V.L.E.M.) Model SSi5 manufactured by McPhar Geo-

physics Limited.

The instrument consists of a transmitting unit and receiving unit.

The transmitter is composed of a transmitting coil, signal generating con

sole and motor generator. The receiver is composed of a search coil,



subjected to an alternating current. If the alternating primary magnetic

field comes in contact with a conductive body a current within the

-2-* fi *

conductor will result. It in turn will produce a magnetic field of its own

whicnHs termed the secondary.


measured at given receiving stations by using the search'coil and its

attached clinometer. The deviation of the resultant magnetic field from

the direction of the horizontal magnetic field is measured in degrees jpf

dip. Readings are taken using transmitting frequencies of 5000 Hertz and,

1000 Hertz. The correlation of the results between the two frequencies

gives an indication of the relative conductivity of the anomalous body.

The range of penetration of the primary field is normally considered

to be approximately one-half the separation distance between the trans

mitter and receiver, however/ other factors such as conductive overburden

must also be taken into consideration.

The results of the V.L.E.M. survey are shown on the prints accom

panying this report.

MAGNETIC

The instrument used was a Fluxgate Magnetometer Model M-700 manufac-

tured by McPhar Geophysics Limited.






capable of possessing a secondary field which is induced by the earth's

primary field.i i

To conduct the survey, a base station was established with all sub

sequent readings being taken relative to this value. By reading the Base


the 1 rest of the grid lines are read at 100 foot station intervals. In the


between stations) the station interval is reduced to 50 feet,*

As the earth's magnetic field fluctuates with time, it is periodically

necessary to take readings at a base station to discern possible instrument

-3-


occuflPduring the time interval between Base Line checks is then applied

as a progressive adjustment to the readings taken during that period of

time.

When contoured^the results of the magnetic survey aid in the deter

mination of the strike, dip and depth of an anomalous body.


ing Ithis report.

GEOPHYSICAL RESULTS

ELECTROMAGNETIC

The electromagnetic survey, utilizing a fixed transmitter/ was under

taken from November 27-28, 1973. Two zones of conductivity were detected.

One zone extends from 0+50 N on Line 4+00 E to 4+00 S on Line 12+00 E.

This displays a northwesterly trend and is of moderate conductivity. The

second zone consists of an isolated dual frequency crossover located on

Line 4+00 W at 3+50 N. AS this isolated conductor is on strike with the

previous one and/ the area in between is characterized by extremely flat

values it is believed that the two separate zones are caused by a single

conductor.

MAGNETIC

The magnetic survey^ which was undertaken on November 10/ 1973/ failed

to reveal any significant anomalous areas. Values vary between 1800 and

2025 gammas. There is a slight increase in values towards the south but

this is probably due to a change in the bulk composition of "the underlying

rocks, chiefly granite.

There is a linear zone of low magnetics associated with the conductor.

A depression in the bedrock topography is the probable explanation.

CONCLUSIONS

One conductor of low to moderate conductivity was located. It shows

some correlation with a magnetic low. The cause of this anomalous area may

not have a bedrock source. It is probably due to a depression in the bed

rock which has been filled with conductive overburden. The property should

be ge^fcjgically mapped placing special emphasis on the zone of conductivity.

W.F. GRAHAM

NORANDA EXPLORATION 00., LTD.

N.T.S. #42-A-15

RECEIVED

DEC l 2 1973PROJECTS SECTION

32D13NE0838 3.1374 HEPBURN 030

REPORT ON

GEOPHYSICAL WORK

PERFORMED ON

MORTIMER 1-72


DECEMBER 3, 1973 W.F. GRAHAM

TIMMINS, ONTARIO NORANDA EXPLORATION CO., LTD.

This report on the ̂ electromagnetic and magnetic surveys is submitted

under the Special^ Provision dated October 16, 1967, for credit of 60


and geophysical work was Mr. E.A. Gallo.

-1-

LOCAq

The property, which consists of 4 contiguous unpatented mining claims

numbered L-366679 and L-366682, inclusive, are located in south-central

Mortimer Township approximately 10 miles north of Iroquois Falls, Ontario.

Mortimer Township is not surveyed into Lots and Concessions.

ACCESS

The property is reached by driving to the 10 mile post on the Abitibi

Paper Company road leading north from Iroquois Falls. The claim group is

situated approximately l mile east of the road.

TOPOGRAPHY

The qrouridis qeneral^ly low and swampy ywith spruce forest covering,

most of the ciainL.gjEojaBJ. In the south portion of claim L-366681 there is

a large outcrop ridge standing 100-125 feet above the mean level.

LINECUTTING

One Base Line was cut which extends 3200 feet at an azimuth of 140

from a point 350' east and 125' south of Post #3 of Claim #L-366680. Tra

verse lines were cut at 400 foot intervals along the Base Line. The Base

Line and traverse lines were chained and picketed at 100 foot fntervals t

In all, approximately 3,7 miles of line were cut, chained and picketed.


ELECTROMAGNETIC ", \

The electromagnetic survey was conducted using a,Vertical Loop

Electromagnetic Unit (V.L.E.M.) Model 5515 manufactured by McPhar Geo

physics Limited. '

The instrument consists of a transmitting unit and receiving unit.

The transmitter is composed of a transmitting coil, signal generating

console and motor generator. The receiver is composed of a search coil,



subjected to an alternating current. If the alternating primary magnetic

field comes in contact with a conductive body a current within the

-2-

conductor will result. It in turn will produce a magentic field of its own

whiolr is termed the secondary.


measured at given receiving stations by using the search coil and its

attached,clinometer. The deviation of the resultant magnetic field from the

direction of the horizontal magnetic field is jmeasured in degrees of dip.

Readings are taken using transmitting frequencies of 5000 Hertz and 1000

Hertz. The correlation of the results between the two frequencies gives an

indication of the relative conductivity of the anomalous body.

The range of penetration of the primary field is normally considered to

be approximately one-half the separation distance between the transmitter

and receiver, however, other factors such as conductive overburden must also

be taken into consideration.

The results of the V.L.E.M. survey are shown on the prints accompany

ing this report.

MAGNETIC

The instrument used was a Fluxgate Magnetometer Model M-700 manufac-

tured by McPhar Geophysics Limited.






capable of possessing a secondary field which is iriduced by the earth's

primary field.

To conduct the survey, a base station w^s ost-ahi-i ab^ with all sub

sequent readings being -taken relative to this value^ By reading the Base


the rest of the grid lines are read at 100 foot station intervals,. In the


between stations) the station interval is reduced to 50 feet.

As the earth's magnetic field fluctuates with time, it is periodically

necessary to take readings at a base station to discern possible instrument

, -i -3- i . * .


occur^ during the time interval between Base Line checks is then applied

as a progressive adjustment to the readings taken during that period of

time.

When contoured -, the results of the magnetic survey aid in the determin

ation of the strike, dip and depth of anomalous body.


ing this report.

GEOPHYSICAL RESULTS

ELECTROMAGNETIC

The electromagnetic survey, utilizing a fixed transmitter, was con

ducted from November 29 to December 2, 1973.

One significant zone of conductivity was detected. It extends from

5+50 west on Line 12+00 north to 3+50 west on Line 0+00. It is only weakly

conductive and there appears to be no magnetic correlation. An isolated

dual freguency gros sover occurs at 4+00 west on Line 12+00 south and a low

frequency crossover occurs on Line 8+00 south at 1+00 east. It is asso

ciated with a 100 gamma magnetic high.

MAGNETIC ,

The magnetic survey was conducted on November 10 , 1973,

Background magnetics vary between 1800 and 1900 gammas. The highest

magnetic intensity recorded is 3800 gammas located at 12+00 west on Line

0+00. Two zones of anomalously high magnetics trend north-south through

the centre of claim L-366681. They are separated by an anomalous low

area with a minimum intensity of 275 gammas. The two magnetic highs are

probably due to diabase dykes which apparently dip to the east.

CONCLUSIONS

One zone of weak conductivity with no magnetic correlation was

detected. It is probably caused by conductive overburden rather than

massive sulphides or graphite in bedrock. The zone of anomalous magnetics

can be attributed to diabase as shown on O.D.M. Preliminary Map No. P-101.

-4-

The M^perty should be gologically mapped with special emphasis on the

geophysical anomalies located.

r "7 6

W.F. GRAHAM

- NORANDA EXPLORATION 00., LTD.

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL .RECEIVE

f

H

flp'Br.* 1 -' ZIftSi,;.*. '. .

L' - ' '" '' m̂

"i.,^";,;,,

Illllllllllllllllllllllllllllilllllllllllllllllll

FECHNICAL R ssoiSNEeaea 2.1374 HEPBURN

Sir Tvnp nf Snrvpv Geophysical (Electromacmetic)

OFFICE USE ONLY

Township or Area hepburn Townshipniaim hniHpr(s) Noranda Exploration Co., (No Personal

Box 45, Commerrft Court West, TORONTO, Ontaric

Author nf Report W. F . Graham

Address Box 1205. TIMMINS. Ontario

Covering Dates of S

Total Miles of Line

iirvpy October 19-November 29 , 1973(linccutting to office)

rut. 11.2

SPECIAL PROVISIONS DAYS CREDITS REQUESTED r,^,.-,^ v?***

ENTER 40 days line cutting) for i survey.

ENTER 20 days additional survey same grid.

i ^0 \-Electromagnetic, l ' l[includes l Jr irsl -Magnetometer. ,,A ̂ x-v4

MaHintni-lrir 1

for each -Other.,.., .... y

USHlfi' /"^ I ' 1

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

Mag'ietornPler

DATF-N.OV * 29,

PROJECTS SECTK

RPS tfrol. L

Previous Surveys

Checked by

GEOLOGICAL BR

Approved by

GEOLOGICAL BR,

Approved by

K]prtrnmafrnr.tir Radinmetrir{enter days per claim)

y *H A 71 Q "7 O t J -i i*' Sis A s-L i/ 7 ,3 Qlf^1 N ATT f R I*1 * * ^ -x^*^Vi^ ^-v-

Aitfioprf RQfK^H/^f nt

N CVx

date

ANCH

date

ANflH

....... ... .... ..ria t p.

DEC 1 2 1973PROJECTS SECTION

3007

LiaMClIiS^LAIMS TRAVERSED List numerically

L 363385(prefix) (number)

L 363387

L 363388

L 363389

l 36339Q

I L 363391

L 363392

L 363393

,,,,,,,L........................3.6.3.3.?..4.........

L 363395

...,.........l........,....,..........3.63.39.6..........

TOT AT .CLAIMS 12

If space insufficient, attach list

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

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS

Number of Stations_____576_____________________Number of Readings. 1Q8Q Station interval. 100 feet_____———————————————————————————————————

Line spacing 40Q feet_________________________________________

Profile scale or Contour intervals l" = 20______________________________.——(specify for each type of survey)

MAGNETIC

Instrument.

Accuracy - Scale constant —

Diurnal correction method.

Base station location-———

ELECTROMAGNETIC

Instrument McPhar 1/5 V,L.E,Mt

Coil configuration Ver-hiral T.nnpCoil separation 400 feet

er scale division

Method: 63 Fixed transmitter d Shoot back EH Inline D Parallel lineFrequency 100Q CPS and 500Q CPS *___________________________________________

(specify V.L.F. station)Parameters mr^im-H Dip Angles_______________________________^______.GRAVITY

Instrument.

Scale constant.

Corrections made.

Base station value and location.

Elevation accuracy.INDUCED POLARIZATION RESISTIVITY

Instrument.

Time domain___________________________ Frequency domain.

Frequency_____________________________ Range——^————Power™————^————————..^———.^—————^——————.——..^^^—Electrode array-—.

Electrode spacing_

Type of electrode.

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

OFFICE USE ONLY

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORT DEC 1 t'i J9/ *- FACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC. PROJECT;,

Type of Survey Geophysical (Magnetometer)Township or Arp* Hepburn TownshipClaim r,r,]der( s)Noranda Exploration Co. , Ltd.

Box 45, Commerce Court West, TORONTO, OntarJAuthor of Rr-pm-t W. F. GrahamAddress Box 1205, TIMMINS, OntarioCnveringDatPsnfSurypy October 19-November 29, 1973

(linccutting to office)

TWalMiWnf l.inprnt 1:L * 2

SPECIAL PROVISIONS DAYS CREDITS REQUESTED ^^...5,,,

ENTER 40 days (includes ' f \ line cutting) for first -Magnetometer 7 20 1 ———survey — Hadinmetrir. \^-S

ENTER 20 days for each -Oilier ^V|additional survey using G^lngi™! " Jfsame grid. fi

Geochemical y


Magnetometer KJertrnmupmetu: Rndiomptrir(enter days per claim)

HATR-NOV. 29 f 1973 SIGNATURE- '^ ' ' ^ ̂ -L^Author of Report or Agent

PROJECTS SECTION on "^4O kl^-

Res. Geol. Oualifirations tX'^Wcy

Previous Surveys

r.riprked hv rbtp

GEOLOGICAL HRANPJI

Approved hy date

GF.OI.OGinAI. RKAMP.H

Approved hy datp

MINING CLAIMS TRAVERSEDList numerically

0

L 363385(prefix) (number)

,,,,,,..!i'........................36.33.86...........L 363387

L 363388

......,,....L........................3.63.389........... L 363390

L 363391 ...

L 363392

L 363393

L 363394

L 363395

L 363.3.96

TOTAL CLAIMS 12

If space insufficient, attach list



GROUND SURVEYS

Number of Stations _______ 576 _____________________ Number of ReadingsStation interval 100 feet L-———-———-.^—^.^^^.^—^^-.—^—^^—^^

Line spacing _____ 400 feetProfile scale or Contour intervals 1800. 2000. 2200, 2400. 2600, 2800 f 3000 gammas

(specify for each type of survey)

MAGNETIC

Instrument McPhar Fluxgate ___ M-.7QQ -——-—-—-—-———————————-————^—Accuracy - Scale mnstant 20 gammas per scale divisionDiurnal correction method closed loops of less than l hour duration, progressive factor-——— — ing o f readings 7Base station inrat inn Every 400* along the base line. ——^^—^^————————-————

ELECTROMAGNETIC

Instrument _________________________________________________________________

Coil configuration ̂ ^^_______^_______^^^__^_________________^____________^_^^^________Coil separation -^^^^^——-————,.—^^--^^—^-^.—.———^.—..——.———....—..—.——.—^^^—^^^^.—.

Accuracy --------—-^--^--——----——^—-^--^-^^^-—^—--——--^^—^^^^^^^^-^^^^—---———-—-—.—^^—^—^—^.Method: CD Fixed transmitter D Shoot back CD In line d Parallel line

Frequency ̂ ———^—^——.........—.—.———...^—^—.—..——^^^^—^——————.—......—.........—^-—.—.-(specify V.L.F. station)

Parameters measured -—————————-———-————————————————-————-————-————-———.—GRAVITY

Instrument Scale constant ,

Corrections made.


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

Instrument—-——.—-——.-——.—^^—^——————

Time domain——————————————————————————— Frequency domain.Frequency————————^————————-——^——--.^^— Range,——————.Power—^^^^^—^———————-—.---——--—-—————-—^—.——^—^^—.

Electrode array——

Electrode spacing. Type of electrode,

File.


l

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey Geophysical (Electromagnetic? Township or AT-P* Sargeant Township —————.Claim h"1dpr( sôranda Exploration Co., Ltd. (No Pers

Box 45 t Commerce Court West, TORONTO, OntariAuthor of Report W. F. Graham ——————————————————

Box 1205, TIMMINSy Ontario ___________ ̂

November 1-November 29. 1973Covering Dates of

Total Miles of Line cut(linccutting to office)

212 ——————

SPECIAL PROVISIONS CREDITS REQUESTED

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

GeophysicalDAYS

perxlîm

—Magnetometer

—Radiometric—OtherGeological.

Geochemical.

TRAVERSED List numerically

(prefix) (number)

gl


Magnetometer_____Electromagnetic.(enter days per claim)

DATE:Nov * 29 f 1973 SIGNATURE:.

. Radiometric

t 1 Âuthor of Report or Agent

PROJECTS SECTIO g flffinl.

Previous Surveys

Checked by. .date.

GEOLOGICAL BRANCH .

Approved by. .date.

GEOLOGICAL BRANCH.

Approved by. -date.TOTAL CLAIMS.



GROUND SURVEYS

Number of Stations_________110_________________Number of Readings. 182—————— Station interval__ 100 feet—————————————————————————————————————————————— Line spacing____400 feet_____________________________________________Profile scale or Contour intervals l" = 20_________________________^__^________^______


MAGNETIC

Instrument _______________________________________:-^——————————^————Accuracy - Scale constant———-——-————-—-—-—-—-—————-———-——^—^^^—^^——-————-————————Diurnal correction method——————————————————————————————.—————————————————— Base station location.^—^^^—^——————^^^^—^—-.—.-.—....—-———-———^—^^—^^-—.———.—.—

ELECTROMAGNETICInstrument McPhar 1/5 V.L.E.M,^_______________________________________

Coil rnnfigiiratmn Vertical loop_______________________________________________________

Coil separation 400 feet^^^^^^^^^^^^^^^^^^^—-^^^^^^^^—,^—---^——^^^—,^.,.

Arnirary 2 per scale division-———-^.—.^———..-—^.^-^^—^^—-—..^.^-—.— Method: B Fixed transmitter EH Shoot back Q Inline d Parallel lineFreqiienry 10 QO CPS Snd 500Q CPS___________________________________________________

(specify V.L.F. station)

Parameters measured. Dip angles-—.—..—.——..—.^..,...^...-.-..——^-..,—.^—....——.GRAVITY

Instrument__________________________________________________________Scale constant.Corrections made.


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

Instrument—.^^———^^——————————Time domain___________________________ Frequency domain. Frequency_____________________________ Range^^————^ Power____________________________________________Electrode array— Electrode spacing. Type of electrode .

File-j2.lL:i.

lWS


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 Geophysical (Magnetomer) Township or Area. SargeantClaim Hr.iHpr(s)Noranda Exploration Co*, Ltd. (No Pers

Box 45, Commerce Court West, TORONTO , OntaricAuthor of Report W. F. GrahamAHdress pox 1205, TIMMINS^ Ontario

Covering Dates of Survey

Total Miles of Line cut

.November 1-November 29, 1973(linccutting lo office)

2.2——————


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

Geophysical- -Electromagnetic.

DAYS per claim

-Other

Geological.

Geochemical.


Magnetometer. .Electromagnetic, .Radiometric(enter days per claim)

November 29, t'.y.tAuthor of Report or Agent

PROJECTS SECTION Res. Geol. —————.

o f) L r'}cX ' ^^^

Previous Surveys

Checked by. .date.

GEOLOGICAL BRANCH.

Approved by. .date.

GEOLOGICAL BRANCH.

Approved by. -date.


.L........................3 6.3.39.7..(prefix) (number)L 363398

2-u"

g •ol

TOTAL- CLAIMS-



GROUND SURVEYS

Number of Stations ___ ______________________ Number of Readings Station interval ______ 100 feet

Line spacing ________ 400 feetProfile scale or Contour intervals 1900. 2000 gammas -


MAGNETIC

Instrument McPhar Fluxgate M- 700 ,—...—————Accuracy - Scale constant 20 gammas per scale divisionDiurnal correction mpthori closed loops of less than l hour duration; progressi ve factor- Base station location every 400* along the base line. ____________ l ________ L

ELECTROMAGNETIC

Instrument —^---^——.-—-—.^^.^^-^^—--.——..-—-----..^.—.-..-...^^--^^————..—.-----..——-—-.—.-—-—.-—Coil configuration ̂ _______________________^^^_^____^_____________________.^^___Coil separation ._____^___________^__^__.^_____._______________^^__^_^__^_______

Accuracy ——^^^——^—————-^-———————————————^^—^^^^^——^^-—————————-———..——Method: CH Fixed transmitter CD Shoot back O Inline CD Parallel line

Frequency .——————-—^^—-—.^-—.-.——————^———.—^^^^^———..—.———..——.—..—.———....^——.(specify V.L.F. station)

Parameters measured .—.^..——.—-—.^-..——^^--——..-——-———-—...—-..-.—————.^.^—^-—-—-..—...—.-.———— GRAVITY

Instrument.

Scale constant.

Corrections made.


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

Instrument.

Time domain___________________________ Frequency domain. Frequency_______________________________ Range.^——-——Power.—-—^——^——^——————-.———————-..—.^-.^^.—..—..^—^—

Electrode array—— Electrode spacing. Type of electrode.

File

Sll




Perse lal

Type of Survey Geophysical (Electromagnetic) Township or Are. Mortimer Township__________Claim holder(s)Noranda Exploration Co., Ltd. (No

Box 45, Commerce Court West, TORONTO, Ontario Author of Report W,F, Graham___________________ Address Box 1205, TIMMINS, Ontario——————^———Covering Dates of Survey November 10-December 3, 1973

(linccutting to office)

Total Miles of Line cut______~-?——.-—.^^^^...—--.—-.—^^-——


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

ENTER 20 days for each additional survey using same grid.

DAYSGeophysical

--Electromagnetic.

-Magnetometer—

-Radiometric——

-Other^————

Geological.

neorhemiral


Magnetometer_____Electromagnetic .(enter days per claim)

nATF.-Dec. 3, 1973 SIONATITRF-

. Radiometric

4 ^

PROJECTS SECTION Res Jgeol. LOPrevious Surveys ^ ^ ' ^ \ \

tUil^j-

;ations? -

^ "t^VO A*" . 5^ V

Checked by. .date.

GEOLOniCAI.HRANCH

Approved by. .date.

Approved hv.


(number)

366681

TOTAL CLAIMS.



164GROUND SURVEYSNumber of Stations—— Station interval 100 feet Line spacing.

.Number of Readings. 328

400 feet

Profile scale or Contour intervals.

MAGNETIC

Instrument-^^-^—-——————

l" = 20(specify for each type of survey)

Accuracy - Scale constant — Diurnal correction method. Base station location..—^

ELECTROMAGNETIC

Instrument MCPhar 1/5 V.L.E.M.

Coil configuration vertical loopCoil separation 400 feet

2 er scale divisionMethod:

Frequency.

E Fixed transmitter 1000 H* and 5000 H*

O Shoot back D Inline D Parallel line

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

Instrument

dip angles

Scale constant.Corrections made.


Elevation accuracy————— INDUCED POLARIZATION

Instrument———^^-^————.

RESISTIVITY

Time domain.

Frequency_ Power,———

Frequency domain.

. Range—^——^^—

Electrode array——

Electrode spacing.

Type of electrode,

File.


ifa-b O



Type of Survey Geophysical (Magnetometer) Township or Area Mortimer Township -—^Claim hnidpr(^orancla Exploration Co* , Ltd, (No Person al

Box 45, Commerce Court West/ TORONTO, OntarioAuthor of Rppnrt W.F. Graham Address BOX 1205^.Covering Dates of Snrw^y November IP-December 3 f 1973

(linccutting to office)3.7Total Miles of Line cut.


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

ENTER 20 days for each additional survey using same grid.

Geophysical

-Electromagnetic.

DAYS V per claim "^

tomdt-r ,' 20'

-Other.

Geological.

Geochemical.

/


(enter days per claim)Magnetometer_____Electromagnetic

DATE: Dec. 3^3973 SIGNATURE:

. Radiometric

^ , y . /vwt

PROJECTS SECTION Res. Geol._______

Previous Surveys —.

Checked by. .date.

GEOLOGICAL BRANCH .

Approved by. .date.

GEOLOGICAL BRANCH.

Approved by. .date.

TRAVERSED isf numerically /L

C6"UC7t*Q3666=79

(prefix) (number)

.366681.

.3.6.66.82.

TOTAL CLAIMS.



GROUND SURVEYS

Number of Stations 164______________________Number of Readings——212 Station interval 1QO feet———-.--—-—--—---—--——-—--———-^--——---—-. Line sparing 400 feet_________^^_^_________^^__^_____^_^_Profile scale or Contour interval, 1QOO - 3000 gammas @ 200 gamma intervals


MAGNETIC

Instrument McPhar Fluxgate M-700^______________^__________

Accuracy - Scale mnstant 20 gammas per srale division^_^_______^____

Diurnal correction meihndclosed loops of less than 1 hour duration.Base station lotion every 400' along the base line.___________ing of readings.

ELECTROMAGNETIC

Instrument.^.-—-———----—-—.---^—-—^—.-.^—^..^-^^—,-..———^^^,—...-——-—-—-.-.—^^—-——.Coil configuration-————^-^—---——————.^—.————.—-.^^^——————^-—^—---—.—..—.——...—^^-—

Coil separation ^^^^-^^^^.^^^^^^^^^.^^^^^^^^^^^^.^^^^^^^^^^^^^^^^^^^.^^^^^^.^^.^^^^^^^^^^^^^ Accuracy——^^^——-—.^^^.^-.——..^^.^^--—-————-—.——.—^^.—..—....—.^—.^^.^—..————.—^-^-^—^—.—Method: CD Fixed transmitter CU Shoot back d Inline CD Parallel line Frequency^^^^^^^^^^^^^.^^^^^^-^^^.^,^^^^^,^^^^^^^^^.^^^^^^^^^^^^-.^^^.^^^^^^^.^^^^-^^,

(specify V.L.F. station)

Parameters measured-————.——-—-———-^——.-——-—-^——.—-—^—^^.——.————.———...—^^—.^^—. GRAVITY

Instrument_________________________________________________________________

Scale constant.Corrections made.


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

Instrument—-..—————^^———.—.^^—

Time domain___________________________ Frequency domain. Frequency_______________________________ Range________Power™.—.——.——^-^-—....——^-^——..^—-——————..—.—^^—...——

Electrode array-—

Electrode spacing^

Type of electrode.

Edwards Twp32DI3NE0008 2.1374 HEPBURN

VI

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IV

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THE TOWNSHIP OF

MORTIMEDISTRICT OF COCHRANE

"LARDER LAKE MINING DIVISION

SCALE'I-INCH*40 CHAINS

LEGENDPATENTED LAND

CROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONROADSIMPROVED ROADSKING'S HIGHWAY

RAILWAYSPOWER LINESMARSH OR MUSKEG

MINES

GEODETIC STATION A

NOTESLO 2553 to Abitibi Electric Development Co. Ltd. 5 Feb. 1932 , covers Power Lin* .

L05958 to Abitibi Pomr 8 Paper Co. Ltc 6Moy. 1942, covers Boil w ay 6 Grovel Pit.

" '

* j"

l

Surfoc* Right*7all Lakes and Riven.

DATEOFISSUI

DEC

PLAN NO.-MON" HO

MINISTRY O' NATURAL RfSOURCjSURVEYS AND MAPflNG ftRANCH

ABBOTSFORD TWP. ADAIR TWP

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- THE TOWNSHIP OF •'tsi

HEPBURNDISTRICT OF COCHRANE

LARDER MINING DIVISION

SCALE:! INCh^4O CHAINS

LEGENDPATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCdjFWTIONMINING RIGHTS ONLYSURFACE -RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINES*CANCELLED

*

NOTES400

"

reservation nro , ,' o'! takes

OF ISSUE

oec tain

F^LAN NO M.500

MINISTRY OF NATURAL RESOURCESSURVfcYS AND MAPt'ING BkANCH

NOTES

400* surface rights reservation along the shores of all lakes and rivers.

The subdivision of the south part of Sargeant TP by A.Bell(O.LS.) as shown on plan dated Oct.3,1912 signed by N.J. Slater(O.L.S.) has been wholly annulled under sec'nH subsec'nl of the Public Lands Act. Jan.4,1963

HEPBURN TR M.500

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48048'49" (appro*.)

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3634*85 i 363484 '-— Oi-L - . -.

2

UNDS iDATEOFISSUi

DEC 12 1973

OPNATUfULMSOUMCIt

LEGEND

HIGHWAY AND ROUTE No.

OTHER ROADS

TRAILS

SURVEYED LINES:TOWNSHIPS, BASE LINES, ETC. LOTS, MINING CLAIMS, PARCELS. ETC.

UNSURVEYED LINES: LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY

UTILITY LINES

NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION

ORIGINAL SHORELINE

MARSH OR MUSKEG

MINES

DISPOSITION' OF CROWN LANDS

TYPE OF DOCUMENT

PATENT, SURFACE S, MINING RIGHTS

SURFACE RIGHTS ONLY

MINING RIGHTS ONLY

LEASE, SURFACE ft MINING RIGHTS

SURFACE RIGHTS ONLY

MINING RIGHTS ONLY

LICENCE OF OCCUPATION

CROWN LAND SALE

ORDER-tN-COUNClL

RESERVATION

CANCELLED

SAND 4 GRAVEL

SYMBOL

QB B BT

.c.s. oc

© (T)

SCALE : 1 INCH 40 CHAINSO 900 lOOO ?OOO

FEETMETRES

O 100 4OO 6OO BOO l KM

ACRES HECTARES

TOWNSHIP

SARGEANTDISTRICT

COCHRANE

MINING DIVISION

LARDER LAKE

Ministry of Natural ResourcesSurveys and Mapping BranchOntario

DateMAY , 1973

WHITNEY BLOCK QUEEN'S PARK, TORONTO

Plan No.

M.582

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MORTIMER 1-72

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this report on the^electromagnetic and magnetic surveys

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