RPT ON GEOPH SUR 1981 MAG VLF HEM...42A06SW0206 2.3973 BRISTOL 010 PRKUSSAG CANADA LIMITED TIMMINS...
Transcript of RPT ON GEOPH SUR 1981 MAG VLF HEM...42A06SW0206 2.3973 BRISTOL 010 PRKUSSAG CANADA LIMITED TIMMINS...
42A06SW0206 2 .3973 BRISTOL 010
PRKUSSAG CANADA LIMITED
TIMMINS WEST PROJECT
GEOPHYSICAL SURVEYS 3981 Mag, VLF, HEM
RECEIVED,'UN 3 01981
MINING LANDS SfcCi
INTRODUCTION
Magnetometer, VLF electromagnetic and HEM surveys
were undertaken over a group of contiguous unpatented
claims within the southwest part of Bristol township
and the northeast part of Thorneloe township in .the
Porcupine Mining Division of the district of Cochrane
(fig 1). Linecutting and geophysical surveys were initiated
in January, 1 981. Completion of the geophysics was
in late June, 1981.
The surveys represent an initial stage in an overall
objective to evaluate the gold potential of the claim
group which is well situated geologically on the western
extension of the prolific Timmins gold camp. Because
of overburden coverage over a large part of the area
it has not been amenable to evaluation by prospecting.
PH9Ee-r tY-J^fis? ription
The group consists of 109 contiguous claims as
shown on fig 2. Recording dates range from
December 6, 1977 to May 22,1981. The 25 earlier staked
claims were staked and recorded by J. Croxall and
D. Miller of Timmins and have been optioned by Preussag
Canada Limited. The more recent claims, largely in
Thorneloc township, were staked eind recorded for Preussag
Canada Limited. Geophysical surveys cover only
claims as listed in appendix.
Location and Access
The property is located in northern Ontario, 20 km
southwest of the city of Timmins; a main mining and
population centre in the area.
The property is readily accessible from Timmins
by way of highways 101 and 144. The latter crosses
the western part of the claims. Access roads for lumbering
1- D.
fUs/C tntrufirt
Ouortr porpfiyrr, gufrll frkupor
, fr/atpor fw^yrf,
Grey*oc*t, tittsiait, noil
Orgillilt onj minif
COnjiomtrolt
Ftllic Mtlostamitn/i
[f j UndirlOta
Mafic f lo* s on3 p f rofla tt ic
rex:*!
FIG. l
PREUSS AG CANADA LTD
t) Pioducjnq^Mlnti
I Doml Mint) Ud l An Ag Cv )
4 Hollnor Mint! Lid l Au AS l
it Mclnlyfi Porcupini Mind Ud tAu *g Cg )
II Pomour Porcuplni Mir.ji Ud l Au AI l
o P?JiJ*'.Ciut!?')Ji!DUli O iilei 10*1 mint (tuAg) 15 Poynoiltr mint Itu *j l
14 Aunof CoU Minij Lid
Ci Scottllh Ontario m i rt* (lu Ag)
t? Uonetol mini (Au *g l
it Bonvthit mint (AU)
19 Eiroulan mint (Av)
10 Ree) mint (Au)
IT Davidion-Titdoll Mint! Ltd (An Ag)
st Dtlnilt Minn Ud (Au At l
4t Fulltr mint i AU)
M Crown mint Ug Ajl
47 Vioona mine ( Au Ag)
49 NiQTit Howk Ptnintula mlntlAuAt)
to Naybob mint (Au Agl
to Mont'o Porcuplnt Min*t LK) (Aw*tl
*] Bowman mint ink) 64 Foymcr mint (Ay Agl
to Noronda Mines Ltd (AU Ag i
TO Preston Mines Ltd (Au Agl
71 Porcupine tokt mint (Au Ag)
Tt Buffalo Anktnti mint (AuAq)
to Coruoixum mind (AuA^)
loo Hollinger Comolidaltd
Coil Wins) Ltd (Au AJ w l '
Location Plan
Timmins \V?st Property
—t.0000 Vi O Win tt
IM.-
""" |P 6 19266 |P 6192671 9587
B IB90I l 495307 1 17773e
P J P \
52BJOX 3! 528302, "YP ' P/_ . ^0 'i2W30l| /S852----- -~
528298 1528299,5
594659 [5946BRISTOL TWP
THORNELOE TWP663865 663053 ' 686866
Optioned Cloims
P l P 'P 5l'5907i 5I59II l 5I59I3 not covered
by surveyl———| Wholly Owned '———' Preussog Claims
Total of I09 claims - 96 claims covered by survey
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loperations make ease of activities within the property
quite good. Most parts are within easy walking distance.
Topography is f]at except for outcrop areas in
the Bristol township claims. Otherwise spruce swamps,
cedar swamps and some spruce covered sand plains dominate.
Re s u 31 s jp f J1 revious Invest ig ations
The first recorded work on the property was undertaken
by Rusk Porcupine Mines in 1942 on what are now claims
495307, 495308 and 495309 in Bristol township. Pits,
trenches and 18 diamond drill holes {6,500 feet) were
completed. No assay results from the drill holes are
available, however channel samples in carbonatized andesite
produced assays of: 4.0 ft of 0.71 oz/T Au; 2.5 ft of
0.43 oz/T Au; and 3.0 ft of 0.24 oz/T Au. (ref. ODM
vol 66, pt. 7, 1957).
Various geophysically directed programs were undertaken
over scatered parts of the present property from 1951
to 1962 as follows:
1 - 3953 Dominion Gulf did a raag survey north and south
of the Tatachikapika River in Thorneloe Township. Three
holes intersected iron formation.
2 ~ 1959 - ]962 Hollinger drilled at least 20 holes
as follow up to magnetometer and EM surveys in Thorneloe
and Bristol Townships. A variety of rock types such
as basic volcanics, ultramafics, porphyries, iron formation
and slates were intersected. Assays are not available,
but massive pyrite and pyrrhotite stringers and carbonated
inctasediments with quartz and pyrite are recorded.
No recent exploration has been undertaken on the
property itself, but over the last ten years there has
been intermittent activity on the Holmer property immediately
to the north where a shear zone up to 150 feet wide
in carbonated metavolcanics carries gold in quartz-
tourmaline veins.
-5-
Survcy Sj^ecJ^f icaj:.jic)i^s
The surveys were completed on picket line grids
as shown on Maps. Baselines were oriented parallel to
what is believed to be the regional trend of the litho-
logies. Picket line spacings are at 120 metres.
The survey was carried out by Mr. F.A. Hodgkinson,
assisted by Mr. Beaulieu and Mr. G. Mason-Apps.
(a) Magnetometer Survey - Readings were taken at 30
metre intervals along the picket lines using a Scintrex MP-2
(see appendix) proton precession magnetometer. Readings
were corrected for drift by tying into the baselines
which had been read and corrected previously by using
the looping method of baseline correction.
(b) VLF Survey Readings were taken at 30 metre stations
with the Geonics EM-16 {see appendix) to record the
]n-Phase and Out-of-Phase components. The Cutler Maine ^
transmitter at 17.8 k Hz was utilized for the entire
survey. Signal strength from Panama station was extremely
weak and hence could not be used for Baseline "B" in
spite of its ideal locaion. Readings on Baseline A and
B were taken with the operator facing south in both
instances.
(c) HEM Survey - Readings were taken at 30 metre stations
with the Apex Parametrics MaxMin II EM system (see appendix)
j ri the horizontal loop mode. A coil sep^lration of 120
metres was used and readings at 444 Hz and 1777 Hz were
recorded. Since the topography is fairly level no corrections
were necessary.
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Survey Resjults^ a n d I n t c rp r c t a t i on
(a) Majgnet^icjs - Contoured magnetics are illustrated
on maps 2a, 2b, 2c.
The gr j d A area (maps 2a, 2b) is dominated by a
series of parallel and en echelon mag highs along and
adjacent to the baseline from line 1680E to the east
end of the grid. The strongest and most continuous of
these linear mag features exists from line 2160E to line
5880E with local intensities to greater than 42,0002^
above background at two locations - namely* at the baseline
on lines 3240E to 3480E and at 150N on line 5280E. The (
magnetic intensity and linearity of this feature is typical
of that caused by magnetite iron formation. Steep gradients
suggest shallow depths locally (see line 5280E) . However,
on line 3360E not only is a deeper source interpreted
from shallower gradient but the broad nature of the
anomaly is also more consistent with a thickening,
probably by folding.
The en echelon mag high from L 1800E to L 2520E
has similar characteristics to the previously mentioned
feature and is also attributed to a magnetite iron formation
source . Tt is interpreted as either an isoclinally
folded repetition of the main magnetite iron formation
zone or else a faulted segment. If the latter inter
pretation is taken, the fault would have to strike at
N70W in order to achieve the noted geometric relationship.
A third linear mag feature is at 240N on lines
3000E to 3360E. It is another stratigraphic feature
of iron formation character but of short strike length.
A series of north striking weakly magnetic features
marked by low cimplitude ( +1 0 00"^ above background) isolated
peaks and ridges coincide with what are interpreted
as diabase dikes. These occur randomly across the claim
group. The more prominent dike related magnetics occur
along or parallel to lines 240E, 480E, 4080E, 4440E
and 57GOK. Other possible dikes which occur as more
7
subtle features are along L120E, L1920E, L2640E, L3240E,
1,384 OE and L5160E.
1'he only other notable magnetic feciture on grid
A is an irregular pattern in the northwest under claims
586865, 586874, 586875 and 515915. The bullseye pattern
with anomalies to 1500"Zf above background suggests the
underlying presence of ultramafic intrusives such as
arc found to the immediate north and are responsible.for
the pattern seen on map 2c.
Magnetics of grid B are dominated by a linear bullseye
pattern along the entire length of the grid from along
the baseline to the west edge of the grid. The 60,000"^
contour essentially marks the eastern limit. To the
east of this the magnetics are flat with not more than
100 7f variability throughout except where magnetic ridges
corresponding to the presence of diabase dikes are seen
{e.g. through the centre of claims 586236, 515914, 515911
etc and along the west side of claims 586887, 586886
etc) .
The bullseye pattern with highs locally to 6000 "if
above background correspond to a N30E trend and confirms
the presence of pyroxenite intrusives such as that rioted
in outcrop at 30E on L3480N. These intrusives are apparently
located somewhat randomly within non magnetic rocks
of volcanic origin such that magnetics between the pyroxe-
nilic intrusives decrease to background intensity,
b) VLF - Results of the EM-16.VLF survey are plotted
as profiles on maps 3a, 3b and 3c. Conductor traces
are illustrated by solid lines.
In the Grid A area a network of more than forty
parallel to sub-parallel conductors cross the entire
area from west to east. None have a configuration typical
of bedrock conductors close to the surface. However,
four (lettered A, B, C and D) show characteristic profiles
of deeper bedrock conductors with moderate to good conduc
tivity. Their symmetrical profile shape is typical
of near vertical sheet like bodies. Qualitiative data
is supplied by the HLEM data which is discussed in the
next section.
The remainder of the conductors are typical of
sources having weaker conductivity. Peak to trough
distances of greater than 120 metres and asymmetry of
the profile suggest Cciusative features related to variable
thicknesses of conductive overburden (i.e. buried overburden
filled valleys and edge effects). Nevertheless, the
conductive trends which range up to 1600.metres in length
are sometimes parallel to magnetic trends, and hence
could be related to either bedrock lithologies which
c'ire less resistant or to shears.
VLF EM results over Grid B are erratic and peaky
because of the presence of outcrop hummocks and sand
hills separated by swamps and overburden filled bedrock
troughs. Conductors are mostly sub-parallel conductors
and have characteristics typical of edge effects along
either outcropping and buried outcrop knobs, creek bottoms
or overburden troughs. Except in certain instances,
their continuity from line to line has been interpreted
somewhat arbitrarily assuming a strike direction sub-
parallel to the baseline i Poor directional coupling
of the grid in relation to the location of the Cutler
transmitter station hcis helped to compound the inter-
pretational problems in this type of terrain.
Typical of grid B conductors is the one which coincides
with the beaver pond on line 3000N at 300E. This feature
traces the creek val l ey both north and south of the pond
and can be attributed to the overburden filled valley
which is mapped between outcrop hills on each side.
A weak shear in the underlying trough could be responsible
for some enhancement of the anomalous amplitude but
~ Q ~
overburden thickening is the dominant force.
Qua]d tatj ve appraisal of these weak conductors
will be discussed in the next section covering HLEM
results.
c) HLEM - Horizontal loop EM results are plotted as
profiles on maps 4a, 4b, 4c and maps 5a, 5b, 5c for
444 hz and 1777 hz respectively.
In the grid A area (maps 4a, 4b, 5a and 5b), four
boncifide bedrock conductors are detected in the central
part of the grid to the north of the baseline. Anomaly
A is 110 metres long and is very narrow wi'th a vertical
or near vertical dip. Estimated depth is approximately,
40 metres. There is no mag association and conductivity
thickness values are low as evidenced by the rapid decrease
in IP/OP measured at 1777 hz and at 444 hz.
Anomaly B is directly on strike with anomaly A
and is probably on the same horizon. As shown on maps
4a and 4b it is composed of two thickenings for a 2000
metre strike length. It varies from O to 15 metres
in thickness. The thickest and most conductive part
of the body is at the eastern end on line 3240E at 240N
where it is calculated to have greater than 18 mho
conductivity -thickness and to have a 60 metre depth.
Immediately to the east on line 3360E a depth estimate
of greater than 44 metres and a conductivity-thickness
value of greater than 10 mho is calculated. Although
there is no magnetic response indicated for anomaly
B, the portion from L2880E to L3360E has a linear mag
high of greater than 12000 V parallel and flanking at
30 metres south.
Anomaly C is a 360 metre long conductor centred
at 4ON on line 3000E where is has its maximum calculated
thickness of approximately 20 metres. Conductivity-
thickness is approximately 30 mho and depth is 40 metres,
-10-
It Ides 150 metres to the north and parallel to the
strong magnetic feature producing the -44200"^
mag high of map 2b.
Anomaly D, which defines a short 20 metre wide
bedrock feature at 45N on line 3840E shows up on only
two picket lines. It has a conductivity-thickness value
of greater than 30 mhos and is estimated to be less
thc'm 45 metres deep. It appears to be on strike with
anomaly C but a direct magnetic correlation of up to
5000 o suggests a different causative source.
Only two other types of anomalous responses are
noted for Grid A - namely weak out-of-phase responses ,
and local high in-phase peaks. The former type of response
is widespread and is illustrated on maps 4a, 4b, 5a
and 5b as dashed lines defining axes of weak out-of-
phase trends. They vary from single line anomalies
to ten line anomalies and are typically quite readily
traceable. The lack of in-phase response and decrease
in intensity from 1777 hz to 444 hz puts their cause in
the category of overburden filled bedrock troughs adjacent
to bedrock ridges. The lack of significant response
at 444 hz confirms this interpretation although bedrock
shears could be coincident with some and could be partially
responsible for the trough and ridge configuration of
the bedrock surface.
VLF anomalies are seen to coincide exactly with
the weak HEM responses.
Positive in-phase responses occurring from L1680E
to L3480E and from L4680E to L5760E are the only remaining
cinomalous responses. These are directly attributed
to nuignetite in magnetitic iron formation. The fact,
that amplitude of the readings remains constant at both
444 h z and 1777 hz and that no anomalous out-of-phase
response is produced substantiates the interpretation
of narrow magnetic, non-conductive tabular bodies. Positive
] P responses are produced only when either the transmitter
or receiver is directly over the magnetic body. Unlike
a true conductor, no anomalous readings are noted when
the body is straddled by the two instruments.
-31-
For Grid B (maps 4c and 5c) anomalous responses
arc produced by effects of variable overburden thicknesses
and by effects of magnetite in the bedrock. As with
Grid A, overburden features are defined by negative
out-of-phase responses. The majority are parallel or
sub-parallel to the regional stratigraphy and are hence
believed to be related to a bedrock topography dominated
by differences in hardness of the volcanic and intrusive
units. Conductors to the south of the baseline from
L1320N to L3120N coincide remarkably well with the south
edge of pyroxenite intrusives. Two others in the vicinity
of 81OE on L1800N correspond very closely with an inter
pretation conforming to a bedrock ridge along the diabose
dike defined by magnetics on map 2c.
The remaining anomalous feature of Grid B coincides
with highw^^y 144 from 360N to 1560N and has a character
typical of a grounded wire. The negative out-of-phase
response is normal for an overburden response but the
f]at bottom to the profile indicates a flat cylindrical
source. It is concluded that the grounding of the wire
causes it to take on the conductivity character of the
overburden or hence only an out-of-phase response.
Summary
Results of the mag, VLF and HEM surveys illustrate
a si nip] o pattern of magnetics and conductivity as follows:
(a) grid A shows a predominant E-W lithologic trend
dominated by a strong mag feature over the eastern two-
thirds of the grid. The intensity of the magnetics
is typical of magnetic iron formation for the most part.
However, an ultramafic flow or intrusive is interpreted
for a shorter mag feature at the north edge of the main
mag high;
(b) magnetics in the central part of grid A indicate
cither a thickening by folding or else a repetition
of magnetic horizons;
.../l 2
-12-
(c) associated with the wide mag zone of grid A are
four moderate bedrock conductors with little to no coinciden
magnetic response;
(d) diabase dikes show up as weak north trending magnetic
ridges;
(e) weak conductive trends conforming to edges of bedrock
ridges occur throughout the gird;
(f) no conductors of merit are noted on Grid B. However,
a number of weak features related to buried bedrock
topography are recognized;
(g) irregular magnetic features of Grid ,B are coinbident
with pyroxenite sills which are partily exposed in the
northern part of the grid. Diabase dikes show up as
magnetic ridges striking due north.
Ontario
APPENDIX I
Ministry of Natural Resources
GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT
File.
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 Survcy(s) ____Y^IL'... MfL?JL 21EI"L....—,. —— Township or Area . Br i s tol b Thor ne loe Twps
Claim Ilolder(s). ... Preussag .Canada.^LjJlit
Survey Company^. Pr
Author of Report . T T E. Warden __ _ - ————^^————-——— Address of Author. JkiLl ^Righrnon^ St . VI, Penthouse FI^
Toronto, OntarioCovering Dates of Survey _ .^,j.an,JL. - Jnnp, 2 Q, 1981
(linecuttirig to office)
Total Miles of Line Cut-. ____ 85.5 miles (136.8 km)
.
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.
ENTER 20 days for each additional survey using same grid.
DAYS per claim
40Geophysical
VLF - Electromagnetic
- Magnetometer—
— Radiometric,——————
Other_________20
20
Geological.
Geochemical.
AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)
Magnetometer_____Electromagnetic _____ Radiometric .-———
DATE:.
(enter days per claim)
SIGNATURE:Author of Report or Agent
i* -J fcO wt/3u
Res. Geol.^ ,
Previous Surveys File No. Type
_ Qualifications....
Date Claim Holder
MINING CLAIMS TRAVERSED List numerically
See attached list(prefix) (number)
6 •o B
837 (5/79)
GEOPHYSICAL TECHNICAL DATA
GROUND SURVEYS li more than one survey, specify data for each type of survey
Number of Stations ___ i2j04 _________ __________ Number of Readings VLF S. Mag 4204, Ijifc
Station interval .........AOjl^res __ ___________ Line spadng -120jnetres ____________ 'HEM; l cm ^Profile
Contour interval Mag 250 gammas
H
aWyto
.H
Oi
Instrument .Accuracy — Scale constant ___r—zDiurnal correction method. Return to base station regularly
Base Station check-in interval (hours)__ 2 hours_________________Base Station location and value Established base lines for Grid A S B
Instrument _ Apex Parametrics Max Min II
Coil configuration ____Horizontal Loop
Coil separation _.......Accuracy .^ . ^ ...... ... L A/ 2 . ?erCenfc .
120 metres
, Method: CD Fixed transmitter CD Shoot back 0 In line CD Parallel line 444 hz S, 1 77 hzFrequency__.O
W J ' ' (specify V.L.F. station)W Parameters measured IP and OP at both frequencies
Instrument ^^
Scale constant _ ^Corrections
Base station value and location _____...,.__________
Elevation accuracy.^ —
Instrument —Method LI Time Domain CD Frequency Domain
Qp; Parameters- On time__..^^. ._....^..._______________ Frequency_____
N tx 2 H
t—*
2 fe ti-i i—(D [ii Power __U ^ Electrode array ~-
Off time ______._____________________ Range —Delay time __ ^. _____________________
Integration time ___._....__._____________
Electrode spacing _—. -^—- - —
Type of electrode ____...____
Instrument___......_....___..._..—.,......_.__.___________________ RangeSurvey Method _ ,, . ... ......... ....-..,.......-..—.......-_—.__________________.
Corrections madeM
Instrument_
Values measured _ ......_- -^__ __________Energy windows (levels) __—————^—————-Height of instrument___. _.,._ ____________________Background Count. Size of detector-_.-...._._______________________________________Overburden —..——...__... ......^. . — — .^..____————.—-———-—--———---.———-—-——.—--^
(type, depth — include outcrop map)
THKKS (SEISMIC, DRILL WELL l/KiGJNG ETC.)of survey__,- .^ _ .YML—J™,--—.————
Instrument_______Geon ic^ JEM^G^_
Accuracy___......__.Parameters measured.
Additional information (for understanding rcsnlis) Transmitter = Cutler Maine 17.8 k Hz - all readings taken facing southerly
Type of survey (s) -.-.—....- -..—... _—-..—.-—...-_———~—————————Instrument(s) __—..-..—_-————————————————————————
(specify for each type of survey)Accuracy__________.-__.___..____..__________..——
(specify for each type of survey)Aircraft used____^.....,..—... . —....____..._.______________Sensor altitude___ ——^—Navigation and flight path recovery method ...m.
Aircraft altitude____.___.________________________ Line Spacing ——. Miles flown over total area__ _^______.--_____________Over claims only..
GKOCHKMICAL SURVEY - PROCEDURE RECORD
Numbers of claims from which samples taken..,
Total Number of Samples. Type of Sample.
(Nature of Material)
Average Sample Weight——————— Method of Collection———————--
Soil Horizon Sampled.
Horizon Development. Sample Depth————.Terrain——————
Drainage Development——————.—————
Estimated Range of Overburden Thickness...
ANALYTICAL METHODSValues expressed in: per cent d
p. p. m. CDp.p. b. D
Cu, Pb, Zn, Ni, Co, Ag, Mo, As,-( circle)
Others.—-^————--——-.----.-—--.——--^————
Field Analysis (.-Extraction Method. Analytical Method- Reagents Used——
Field Laboratory AnalysisNo. -————-———-.
SAMPLKI'RKl'ARA'riON(IncliiHes drying, screening, crushing, ashing)
Mesh size of fraction used for analysis -—-——.
Extraction Method.Analytical Method — Reagents Used ———
Commercial Laboratory (- Name of Laboratory.— Extraction Method- Analytical Method.. Reagents Used ^^———
.tests)
.tests
.tests)
General- General .
M3N3NG CLAIMS TRAVERSEDAPPENDIX II
Number c
5P63 9266
P619267
P495307 20 c
P495308 20 d
P495309 2 0 d
P515901 20 d
P51S906 80 d
P535907
P515908
P535909
P515910
P515911
P515912
P525913
P5 3^914
P53 935
A P553050
P553053
P553052
P553053
P553054
P553055
P553865
P fi S 3 8 C 6
P530884
P583234
PS86228
P586229
P586230
P586231 ^
)f Days that can be Applied
ays P 5 86232 so
P5.86233
PS86234
' P586235 ays
P586236ays
P586237ays
P586238ays
P586239ays
P586240
P586261
P586264
P586265
P586864
P586865
P586866
P586867
P&86868
P586869
P586870
P586871
P586872
PS86873
P f Q C D "~1 A ^5 O O O 7 T
P586875
P586876
PS86877
P586878
P586879
P586880
P586881
f P586882 ,^
to Each Claim
days P586883 80
P586884
P586886
P586887
P586891
P586892
P586893
P586894
P586900
P58.6901
P586902
P586904
P586905
P586906
P586910
P586911
P586912
P586914
P586915
P586916
P586918
P586919
P586920
P586922
P586923
PS86924
P596926
P586927
P586928
P596927
f 9 3 Claims
days
CM
Godfrey Twp.-M.284
23M. BASE LINE 22 M.
jL---i--- -l--- —— t****. .9*9.* ' 506703 , 508702 595996 5959 57 i 598958 , 5989591 595960 595961 , J l——— li"-P~ ' P f P |P 1522255,522253 l , ^ '' —— .4 — - M .. J____j.. - - -u,- - - -——| P T
553206/5532051853201 |983200 l~- - t~p- ~ ~r~P~ ~T V ~T p |~p Tp l P P P | P | P l P U 28 , 60J
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5M.-
4M.- -
5532,6 1553217 J5B32I8 Tp __ - l - - J-- __J '
p j P l P j jl l .460315 ,479904 \f_i_ ^.
553221 1653220 J 553219 |—- —— 4p- f, /p \
3M
2M.
l M.
148 1147 553203 1553196 j,P
f ; ' i 11 553207/8532041983202 |S53I99 .
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Thorneloe Twp. - M. 313
K. K.42A86SW0206 2.3973 BRISTOL 200
THE TOWNSHIP OF
BRISTOLDISTRICT OF
COCHRANE
PORCUPINE MINING D IVISION
SCALE: 1 -INCH-4O C HAINS
DISPOSITION OF CROWN LANDS
PATENT, SURFACE AND MINING RIGHTS ..__ *" , SURFACE RIGHTS ONLY_______. O" , MINING RIGHTS ONLY _______. 9
LEASE, SURFACE AND MINING RIGHTS___ B" t SURFACE RIGHTS ONLY^______. HH , MINING RIGHTS ONLY ________ H
LICENCE OF OCCUPATION____________ T
ROADSIMPROVED ROADSKING'S HIGHWAYS
RAILWAYSPOWER LINESMARSH OR MUSKEGMINES
CANCELLED
, NOTES
400' Surface Rights Reservation along the shores of all lakes 8, rivers
Areas withdrawn from staking under Section 43 of the Mining Act t R.S.0.19701.
Order No. F ile Date Disposition164584 Surface Rights Only.
DWE OF ISSUE
FEB101982
This township lies within the Municipality of the CITY Of TIMMINS.
PLAN NO. M-264ONTARIO
MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH
roNOJ
cO)Q
Bristol Twp. M.264
5M-
61265553865 5586S7P-J 58^880 , ,, (
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Me Keown Twp. M.299
2-3973 BRISTOL
THE TOWNSHIP OF
THORNELOE
DISTRICT OF COCHRANE
PORCUPINE MINING DIVISION
SCALE: 1-INCH 4O CHAINS
LEGEND
PATENTED LAND
CROWN LAND SALE
LEASESLOCATED LAND
LICENSE OF OCCUPATION
MINING RIGHTS ONLY
SURFACE RIGHTS ONLY
ROADSIMPROVED ROADSKING'S HIGHWAYS
RAILWAYS
POWER L INESMARSH OR MUSKEG
MINES
CANCELLtDPATENTED S.R.O.
ce
NOTES :
400' Surface Rights reservation along the shores of ali lakes and rivers.
Reservation for Deputy Chief Ranger's Headquarters site shown thus •••••••vi F ile 1 10657
Flooding rights on Mattagami River 8 Kenogamissi Lake are r eserved to Ont. Hydro- L.O. 7598
File 1163 vol.3
Areas withdrawn from staking under Section
43 of the Mining Act t R.S.O. 1 970.) Order N- Fil*—— Pu l ffi Disposition
FEB10882
Ministry of Natural ResourcesTORONTO
S.R.O.
SAND and GRAVEL
( j) M.N.R. GRAVEL PIT 256 , FILE III46T
g) GRAVEL FILE 143834
5) M.N.R. GRAVEL RESERVE
This township lies within the Municipality of the CITY of TIMMINS.
PLAN NO. M.3I3ONTARIO
MINISTRY OF NATURAL R ESOURCESSURVEYS AND MAPPING BRANCH
\ \ ?,9??
PREUSSAG
TIMMINS WEST CLAIM GROUPGrid A
WEST HALF)
TOTAL FIELD MAGNETICSi—i i—i i—i ]—i l—t "1
Map 2a
Contour Interval - 250 gammas(l000gammas in areas of
high gradient )Operator - F. A. Hodgkinson
Instrument - Scintrex MP-2
Date - May 18I
515909
60323
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PREUSSAG
TIMMINS WEST CLAIM GROUPGrid A(EAST H ALF)
TOTAL FIELD MAGNETICS100 100 200 300 Metres
March 81 Scale l! 3,000
Map 2bNTS 42/A/5
Contour Interval - 250 gammas(l000gammas in areas of
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Operator - RA. Hodgkinson
Instrument- Scintrex MP-2
Date - May '81
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PREUSSAG
TIMMINS WEST CLAIM GROUPGrid B
TOTAL FIELD MAGNETICS100 100
March 81 Scale 1:3,000
Map 2c
Contour Interval - 250 gammas(lOOOgammas in areas of
high gradient )Operator - F. A. Hodgkinson Instrument - Scintrex MP-2
Date - June '81
59 735
55386659799
200 300 Metres
NTS 42/A/5
—— BOO W
—— 870 W
—— 840W
—— 810W
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—— 75OW
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—— 660W
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" — 5IOW
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PREUSSAG
TIMMINS WEST CLAIM GROUPGrid A
VLF EM515908
Map 3a
In-Phase Profile
Quadrature Profile
Profile Scale : l cm to IO GXo
In Phase Quadrature
Conductor Trace.515909
Operator-B.Beaulie (facing south) Instrument- Geonics EM-16 Date -May '81
\ 515915
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PREUSSAG
TIMMINS WEST CLAIM GROUPGrid A
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VLF EM100 200
March ' 81 Scale l: 3,000
Map 3b
•x In-Phase Profile
*——* Quadrature Profile
Profile Scale i l cm to I07o
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l
5
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300 Metres
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4440E
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Date - May '81
-2
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54ON
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42A06SW0Z06 2.3973 BRISTOL310
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—— 630 N
—— 600 N
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—— 42ON
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—— 180 N
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—— 570 S
—— 60OS
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4440 E
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42ON
39ON
360N
30ON
270N
24ON
21QN
(SON
I50N
I20N
9ON
60 N
3ON
00
305
60S
90S
I2OS
180S
2(0 S
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2705
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3305
36OS
39OS
42OS
45OS
48OS
5IOS
54OS
5705
6005
6 3O S
660 S
69OS
72OS
7505
78OS
8 tO S
87OS
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4440 E
—— 660N —— N0I-89I
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586912
586902
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PREUSSAG
TIMMINS WEST CLAIM GROUPGrid B
VLF EM100 100
March 81 Scale i:3,000
Map 3c
x In-Phase Profile
i——* Out-of-Phase Profile
Profile Scale i lcm to \07o
4- ve -ve
14
-23
-5
-14
-9
In Phase Out of Phase
Operator -B.Beaulie Instrument- Geonics EM-16 Date -June '81
\J6I9267 '
200 300 Met res
NTS 42/A/5
Conductor Trace —
9OOW
870 W
840 W
810 W
780 W
7SOW
72OW
69OW
66OW
63OW
6OOW
57OW
54OW
stow
48OW
45OW
42OW
39OW
36OW
33OW
3OOW
270 W
24OW
2IOW
18OW
150 W
i2O W
9OW
60 W
SOW
OO
3OE
60E
9OE
I2OE
t SO E
ISO E
2IOE
240E
27OE
300 E
330E
36OE
39OE
42OE
450E
- 480 E
- 5IOE
- 540E
- 57OE
- 6OOE
- 63OE
- 660 E
- 690 E
- 720E
- 75OE
~ 780 E
- 8iOE
- 840 E
- 87OE
- 900E
,
PREUSSAG
TIMMINS WEST CLAIM GROUPGrid A
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HLEM 444hz100 O
I—I t—l l—l l—l l—l l-iOO 200
March 81 Scale 1:3,000
Map 4aNTS 42/
)09
x In-Phase Profile Out-of-Phase Profile
Profile Scale ; l cm to I0 07o Instrument Max-Min HOperators- F A. Hodgkinson, B. Beaulieu
Coil Separation - 120metres
Axis of Very Weak Conductor (Centre of Overburden Trough)
Bedrock Conductor Trace
-ve
Out of Phase
i
West Sheet
586236
In Phase
Date- May '81
A/ 0 f-2322-9O93-2364-23T
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586884
586240 \ 586893586235
N02-235 3-24O
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300 Metres
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990N
960N
930N
870 N
/V
750N
T2ON
69ON
660N
63ON
GOON
570 N
54ON
5ION
48ON
450 N
42ON
33ON
27ON
240 N
l SON
60N
ION
00
60S
330-
BIOS
84O
8?O S
9OOS
93OS
96OS
28 80 E
3773PREUSSAG
TIMMINS WEST CLAIM GROUPGrid A(EAST HALF)
HLEM 444hz100 300 300 Metres
March '81 Scale i: 3,000
Map 4bNTS 42/A/5
(——x In-Phase Profile
,——* Out-of-Phase Profile
Profile Scale ! icm to I07o Instrument Max-Min H Operators - F A. Hodgkinson, B. Beaulieu
Coil Separation - 120metres
Bedrock Conductor Trace
Axis of Very Weak Conductor (Centre of Overburden Trough)
4- ve -ve-3
3
O
4320 f
-l
444O E
-4 -l
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Date- May'81
X -l
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99ON
960 N
93QN
9OON
87ON
84 ON
8ION
780 N
7SON
T20N
69ON
660 N
630 N
600 N
570 N
54ON
5ION
48ON
45ON
42ON
390N
36ON
33ON
300N
270 N
24ON
2 ION
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I5ON
I20N
9ON
60N
3ON
OO
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60S
90S
/?OS
150 S
ISO S
2105
240 S
270 S
N02-027 __ m r ——
33OS
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4805
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63OS
66OS
6 90S
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750 S
78OS
8IOS
84OS
8 70S
9OOS
N
PREUSSAG
TIMMINS WEST CLAIM GROUPGrid B
HLEM 444hz100_____________O
100 200
March 81 Scale i:3,000
Map 4c
x——x In-Phase Profile* —— * O ut-of- Phase Profile
Profile Scale \ l cm to I07o Instrument Max-Min HOperators - F A. Hodgkinson, B. Beaulieu Coil Separation - IZOmetres
3840N r
Date - June '81
Axis of Very Weak Conductor (Centre of Overburden Trough)
-ve
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O 9 X
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300 Metres
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510 W
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360 W
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2 tO W
180 W
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3OW
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3OE
6OE
9OE
1 20 E
i 50 E
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2IOE
24OE
270E
3OCE
33GE
360 E
39OE
4 2O E
450E
480 E
5IOE
54OE
57OE
600E
63O E
66OE
690 E
72OE
7 50 E
78OE
8IOE
84OE
87OE
90OE
PREUSSAG
TIMMINS WEST CLAIM GROUPGrid A(WEST HALF)
HLEM 1777hz100 Oi-l l—l l—l t—l t-rq^
100 200 300 Metres
March 81 Scale l : 3,000
Map 5 aNTS 42/A/5
——x In-Phase Profile——* Out-of-Phase Profile
Profile Scale ". l cm to I07oInstrument Max-Min H.Operators -FA. Hodgkinson, B. Beaulieu
Coil Separation - IZOmetres
Axis of Very Weak Conductor (Centre of Overburden Trough)
Bedrock Conductor Trace
I2OON
II7ON
II4QN
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IO8ON
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IO2ON
990N
960N
—— 93ON
—— 9OON
West Sheet
586236
In Phase Out of Phase
Date- May 81
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TIMMINS WEST CLAIM GROUPGrid A(EAST HALF)
HLEM 1777hz100 100 200 300 Metres
March 81 Scale i:3,000
Map 5bNTS 42/A/5
,—— K I n-Phase Profile f'-—* Out-of-Phase Profile
Profile Scale i l cm to I0 07o Instrument Max-Min H Operators - FA. Hodgkinson, B. Beaulieu Coil Separation - I20metres
Bedrock Conductor Trace
Axis of Very Weak Conductor (Centre of Overburden Trough)
-f ve —*- ve
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O
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n Phase
Date-May'81
Out ot Phase i
N0 l-922 504OE 2-921
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960 N
93ON
9OON
870 N
84ON
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78O N
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69ON
660N
63ON
6OON
57ON
54O/V
5ION
480 N
450 N
42ON
390 N
36ON
33ON
SOON
270 N
24ON
2 ION
I8ON
/50N
120N
9ON
60N
SON
oo
3OS
60S
90S
12OS
150 S
180S
2IOS
240 S
27OS
3OOS
33OS
36OS
39OS
420 S
45OS
48OS
5IOS
54OS
5 70S
GOO S
63OS
66O S
69OS
72OS
7SOS
78OS
8IOS
84OS
87OS
9OOS
N
PREUSSAG
TIMMINS WEST CLAIM GROUPGrid B
HLEM 1777hz100 100 200
Marcti '81 Scale 1:3,000
Map 5c
x——x In-Phase Profile .——* Out-of-Phase Profile
Profile Scale l l cm to I07o Instrument Max-M in IEOperators -FA. Hodgkinson, B. Beaulieu
Coil Separation - IZOmetres
l Date - June !8I
Axis of Very Weak Conductor (Centre of Overburden Trough)
In Phase Out of Phase
300 Metres
NTS 42/A/5
900 W
-ve
840W
e tow
78OW
75O W
72OW
69OW
66 O W
6 30 W
6 00 W
57OW
54OW
5 IOW
48OW
45OW
42O W
390 W
36OW
33OW
3OOW
270 W
2 to W
180 W
1 50 W
t 2O W
9OW
6OW
3OW
OO
30 E
60 E
90 E
1 20 E
iso e
18OE
2IQE
2405
27OE
3OGE
330E
36OE
390E
4 2O E
450E
48OE
5IOE
540E
57OE
6OOE
63OE
66OE
6 90 e
720E
750 E
78OE
810 E
84OE
87OE
9OOE