this report on the^electromagnetic and magnetic surveys
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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
LARDER LAKE MINING DIVISION
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
assessment work days per claim. The person in charge of the linecutting
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.
INSTRUMENTS AND SENSITIVITY
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,
signal amplifier, clinometer and headphones.
The transmitting coil produces a primary magnetic field when it is
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.
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 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.
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.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
Line in this manner, it can be used as a series of base stations from which
the 1 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,*
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-
or magnetic drift. Any apparent change in the magnetic intensity which
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.
The results of the magnetic survey are shown on the prints accompany
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
LARDER LAKE MINING DIVISION
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
assessment work days per claim. The person in charge of the linecutting
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.
INSTRUMENTS AND SENSITIVITY
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,
signal amplifier, clinometer and headphones.
The transmitting coil produces a primary magnetic field when it is
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.
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 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.
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 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
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.
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 . * .
or magnetic drift. Any apparent change in the magnetic intensity which
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.
The results of the magnetic survey are shown on the prints accompany
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
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flp'Br.* 1 -' ZIftSi,;.*. '. .
L' - ' '" '' m̂
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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
AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)
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
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 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.
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,
File.
GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT
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( s^oranda 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
perxl^im
—Magnetometer
—Radiometric—OtherGeological.
Geochemical.
TRAVERSED List numerically
(prefix) (number)
gl
AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)
Magnetometer_____Electromagnetic.(enter days per claim)
DATE:Nov * 29 f 1973 SIGNATURE:.
. Radiometric
t 1 ^Author 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.
Show instrument technical data in each space for type of survey submitted or indicate "not applicable"
GEOPHYSICAL TECHNICAL DATA
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_________________________^__^________^______
(specify for each type of survey)
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.
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 .
File-j2.lL:i.
lWS
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 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——————
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.
DAYS per claim
-Other
Geological.
Geochemical.
AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)
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.
TRAVERSED List numerically
.L........................3 6.3.39.7..(prefix) (number)L 363398
2-u"
g •ol
TOTAL- CLAIMS-
Show instrument technical data in each space for type of survey submitted or indicate "not applicable"
GEOPHYSICAL TECHNICAL DATA
GROUND SURVEYS
Number of Stations ___ ______________________ Number of Readings Station interval ______ 100 feet
Line spacing ________ 400 feetProfile scale or Contour intervals 1900. 2000 gammas -
(specify for each type of survey)
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.
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.
File
Sll
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.
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______~-?——.-—.^^^^...—--.—-.—^^-——
SPECIAL PROVISIONS CREDITS REQUESTED
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
AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)
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.
TRAVERSED List numerically
(number)
366681
TOTAL CLAIMS.
Show instrument technical data in each space for type of survey submitted or indicate "not applicable"
GEOPHYSICAL TECHNICAL DATA
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.
Base station value and location.
Elevation accuracy————— INDUCED POLARIZATION
Instrument———^^-^————.
RESISTIVITY
Time domain.
Frequency_ Power,———
Frequency domain.
. Range—^——^^—
Electrode array——
Electrode spacing.
Type of electrode,
File.
GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT
ifa-b O
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 (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.
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.
DAYS V per claim "^
tomdt-r ,' 20'
-Other.
Geological.
Geochemical.
/
AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)
(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.
Show instrument technical data in each space for type of survey submitted or indicate "not applicable"
GEOPHYSICAL TECHNICAL DATA
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
(specify for each type of survey)
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.
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.
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
IM. 2M.
4M.
•rf ' 9M.
Q.
2NI--
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\
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I8M I9M. 20M,
SARGEANT TWP.32D13NEe00B 2.1374 HEPBURN 210
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97M.
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LU O
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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
CM
-Q]tla<
O)J* o
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LU
(T O
TP OF BONIS TR OF BERRY
32D13NE08B8 2.1374 HEPBURN 220
OKIKODOSIK BAY (Lake Abitibi) M.583
48048'49" (appro*.)
79*~3l'O3n bpproK)
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
/6A I2N
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•V
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LOCATION PLAN
MORTIMER 1-72
125
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PROJ.N9NT. S.DWG.N2
. and E. M. SurveysMORTIMER 1-72
OHTAKIO
PROJECT:SURVEYED DRAWN BY 4.4 w*//
DATE:,.. SCALE'.
NORANDA EXUORAHON m LTD.OFFICE ̂ ......^^..^.
Hepburn Twp. Sargent Twp.
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A/toe 1973
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670
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PROJ.N9NT.S..DWG. N2
Magnetic SurveyHEPBURN 1-72
HEPBUHN TWP ONTA^/O
PROJECT:SURVEYED BY DRAWN L A Wadden SCALE- l"* *9'
NOR AN DA EXPLORATION CO LTD.OFFICE^ .
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NORANDA EXPLORATION CO. LTD.tt Karr*MAMT M
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SARGENT 1-72
2640
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