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4aF*4NW8829 63.454 MANITOUWADGE LAKE 010
42F84MW8829 63.454 MANITOUWADGE LAKE 010C
REPORT I K 0 E X
Introduction . . ... . . . ... .. .. . *,iY....*.**
Summary and Recommendations . . v .. v,,... . . * Pagia, ;1, 2
Property ... ..... .. . ........ *. ,j..,..W..-,;-..*.'^ :F^tgt;*^ ,.-:- -
Location and ^.cces sibility ...... ...:.,,,.,;' Page 2, -3"
Topography .. ... *...... . .... •.•.'•^••'.* .'.y-., . :* ,,Pajge : 3,V
r}eneral Geology ....... .. ,... ..-.. ...^ *...,. VPage Ij., 5
Geology of the Property ... *.. ...v . . r . ..; ...* ^P^ge 5f 6t
Survey Data ..... . . .. ... ..... .. .....,.. *. * " Page' 7
"; ' ' '. ' * ' : ' - ' ~
:;- ^ ;:- -:s -:j. a- 'w ' . - ,. : '.^ ' . - -'
". i . . " i- - '
PL-tN NO. l .... .......,y, ' Geological Plan . , -
-:t- j,!-
Paige Petroleum Limited 35 Richmond Street West, Toronto, Ontario.
Gentleman: - v ' " : J.^'^-^V --
The following report de-s^ltoeS' iite, V ;? \-:---'
geological survey carried out on the^eri claim group
held by Paige Petroleum Limited and -located itti^he.. ' " ' ~ - - .: -* -' " B.-" ' l - -
Manitouwadge Lake area of Thunder Bay i)tatri^t of-i*' ' '
Ontario, This survey was carl*laid out undap, the per**
sonal supervision of J.D. McCannell o-f 1^2sBftthurst
Street, Toronto, Consulting Geologist:-for J'aige f
Limited. Mr. McCannell was wi actlv^; pia^ili^ant i2t the
actual survey, working long hours, quitting only when
forced to by the coming, of darkness,- * - ; . ." "^' ~ "
Sunmary and liecommendations " "' '' ' ''•''•' '.s'. ;"" ,-
The geological., survey fmlled Jtd' reveal
any mineralization of interest on tha^property but the- 1 *'-- " ' - ' ' ' :.-'. '
fact that sulphide ore bqdifs ara known to occur.In . ,
gneissic rocks and the presence of sulphide1 ' - ' , T " . v
z at i on in the gneissic rocks on th^ adjoini|ig-. s ' ' : ' ' -- ' ^- ~
to the west would indicate the p o SSib 111 t j .of- * ' "- i- ' - -\' - - '. * -- - . -. " " ' ; , -. " '
mineralization being present on t he:.'property of Be.ige
Petroleum Limited. So much of the rock gurface being
marked by overburden would necessitate ^ross sectioning
the formation by diamond drilling.
2. ' . - - : ....: -' '. ' ' ;- ,: . ,. .-,
With the Information that is now available "
from geological and geophysical surveys-carried out on
the property, It is recommended that limited diamond ,"
drilling he done at the discretion of the consult Ing
geologist to test the resistivity anomalies *and the
possible extension to the .east of the sulphide \
mineralization on the adjoining property to, the West*
Property ' ' ' ', t^ : , "/:.
The property of Palge Petroleum Limited
covered by this report consists pf 10 mining clftlies
located in the Manitouwadge Lake area, District of
Thunder Bay, Port arthur Mining Division, Ontario. The
claim group is located in the northwest section of the
Man*touwadge Lake mining area and adjoins to .the east
of the property of Sudbury Contact Mines Limited.- * : -"'"'.-'- l
The claims included in the group are further
described as follows: T.B. 14.8161^, 14.8165 and 48172 to
'-8179 Inclusive.. ' - -
Location and Access ' . ; -' -
The Manitouwadge Lake area is located. - ' - "-' i -"' ." ~
approximately 6^ airline miles southeast 9? Geraldton, '
Ontario and lj.0 airline miles northeast of He^on Bay* ' ,
The area is reached by air from either of the Atwo points
mentioned above and various airway companies operate
chartered flights into Manitouwadge Lake as well .aa;.^ ;
other small lalces in the general, vicinity. , He 11 cop t e*!*-
service is also available and is very usefal : for
3.S :.
reaching properties where there are iip- : " . .
for landing standard type aircraft** .;.'.f , '' ,
A truck road constructed by•' . " 'J* ^ ' T- '- ", ' : . - V'-.'.' •••/•-'.•f' '
engaged in lumbering in th* geaerai- are^. ejc'teads
Stevens, a point on the Canadian Na*tpriai Jtit^way, !--
south to Camp 12 located in the west/part : ofs , tHe
Manitouwadge Lake area mining camp. "58v^ral bush #-
service the Immediate area around Camp '12 j and a^e suitable
for truck travel. The distance from S t evens to G:4inp 12 .
is approximately 30 miles. ; A winter road also
north from Helmo on the Canadian Pacifie R^l^i
services logging camps in the south, part of the general;. ,•V ' ,- ' ' - J-'' .•".-.".*: "'.'i' -- - •'•..-'-•-''- ,. --, - ,
Manitouwadge area. . -,. - ;. i -;.,.:-. \,-.- .,;/^-; .^-;,.'.;.-;'---.;.'j 1 -;.' --i\..
The property of Palge ''P6f^ol9tM;;Ltmi;t*d v:;.^."\:
can be reached by a truck road extending east from ': ' ^,"- -- * "' ••'•-. - . ' ''" -" ' ,-t ! 'i
Camp 12 and which passes within onerfjaarter of.^'iii^d, -,: , ~
to the south of the Company 1 s ciaiW9 grpuj)^ The . ' r ^
distance from Camp 12-to the. property-;.is appro-Xilcift'tely " ; ,-
8 miles, . V:- ," ! . " ,. ' " : ;
Plans are underway to constjpii|t a Provincial
road into the Manitouwadge Lake fcrea and railroad ;
survey crews are presently surveying a rout -for a rail
line Into the area. ....; - ' , ; "^ r "^;":?- r'5'-"'" : . '
Topography , :' ;'". ; .- .'.-- .'', ' y -'- . : , ;
The topographical relief of tfeaq property
is fairly gentle, with gradual slopes to the .'north ; . -;
toward the eastern boundary of the property. Bock ,:
outcrop Is fairly abundant lin the western and'north- -, ' . * ' n -. ' : . ' v ' - ' v.
western part of the property, but there are;;very few
rock exposures to the south and east. Host ofthe
outcrops are low, flat, moss covered exposures. A :' '" . ' v i 1 *'" ' " "'" -' -,, ~ .r*
small spring fed stream flows from north to south ; ,
through claims ij.8l6!| and lj.8165. Where this irferearn *\
crosses the south boundary of the property, iVwas
two to three feel wide and contained f if cm three. *t o
eight inches of water in 'the early part of Jaly
a period of six weeks without more than a.couple of
hours rainfall in that interval. , ^
The entire property Is cohered with a
stand of second growth spruce, poplar, birch and ,- ; "'
jackplne, The spruce in the swamps arerag&s from
3 to 5 inches, and the Jackpine and poplar on the '
higher ground ranges up to from 10 to llj. inches*r-
General Geology ., , - - v', ^ ' - , ~- - * ~" ^
Very little Information has bebii
on the geology of the Manitouwadge Lake area* ,/A ,
limited amount of reconnaissance .work wasi conducted by
the Ontario Department df Mines and is shown on Map
?4l-j "Heron Bay and White Lake Area1* Sheet,; published
in 1932. This map accompanies XLI- Annual Report
the Ontario Department of Mlnei* Fart IV, 1932,
r~
The claims group discussed herein Is
located immediately to the north of that part of the
Manitouwadge Lake area geologized by the Ontario
Department of Mines and shows on Map l|l-j* - : , " '
M ap ip.- j s hows a b and of e arly., Pre o aiabr l4it
volcanics from l to 2 miles wide extending In an east-
west direction through the Hanitouwadge Lake area and
bounded to the north and south by an Algoman; type
grsnite. The property of Patge Petroleum' Liniited Is ,
located about three miles north of the contact asshown
on this map. The ore bodies found on the Qeco Hlft^a
Limited property are located on or near the north *
contact of this volcanic assemblage* However,'.' '-;:
preliminary examinations, of the Lun-Echo Mihes.Ltffiited ;
ground show that the copper-zinc mineralization is not
confined to this one contact zOne* -\ -- .- -;-.
It is quite possible that more, de tailed ..
geological work will show the presence of other gpeeii-
stone horizons in the general area* " - .
Geology of the Property - -V . :
The property of Paige Petroleum Iiiioited is
underlain by a granitic gneiss which has beeij" intrude d -
by granite which has been later intruded by diabase
dikes. The gneissic rock Is a fairly dark coloured,
fine grained, well defined gneiss. Prom tisual
examination the dark minerals appear to .be biotite and
-
hornblende with minor amounts of chlorite and possibly
scant magnetite. Owing to the fine texture of the
rock it was impossible to identify the light coloured :- . "j-.
minerals. This gneiss had the appearance .of altered
tuff. ' . '
The granite is a fairly fresh looking,
normal granite. The diabase, that was observed in ,
one outcrop where it had intruded the granite at
approximately ri^ht angles to -the 'general strike of
the gneissic formation, was a typical 'diabasic dike
material. The strike of the gneiss is east and west
to which the granite intrusions . seem to ,
The contacts between the granite and the gneiss are,,-
well defined and parallel to the gneissosity* '
A thorough examination, of the property
with special attention to the electric- anomalies
failed to reveal any shear g one s or mineralized zones
of any interest. The rock of .the property is ov.erlain
by a mantle of boulder clay with a loamy top soil,
There are two linear swamp areas that trend slightly
ea.ot of north as shown on the accompanying geological
plan. The depressions which caused these swamps to
Torrr may be the site of faulting, and the g^rietral
topography of the area would incline one to believe
they were continuations of regional faults or sub
sidiary faulting, but there is no criterion -by which.
a definite opinion could be formed. . ,. :
a*
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42F84NW0029 63.454 MANITOUWADGE LAKE 020
63.454 MANITOUWADGE LAKE 020C
REPORT INDEX
Introduction .................*.....*...........* Page l
Summary and Recommendations ..................... Page l, 2
Property .................*.*.................... Page 2, 3
Location and Accessibility ................... .*. Page 3* k
Topography ...................................... Page ij.
General Geology ......*.......................... Page kt S
Explanation of Resistivity Method ............... Page St b
Interpretation of Resistivity "'Results .......... Page 7* 8
Survey Data ....................................* Page 9* 10
-"- -;c- iv x # -:;- *
PLAN NO. l *...... Resistivity Contours and GeologicalInterpretation.
(Drawing Ref. No. 2l±-5
* K x x -:* -st s-
GEO -TECHNICAL oevELopMeNT COMPANY LIMITED
PAge Petroleum Limited,85 Richmond Street West, Room 102i|.,Toronto, Ontario
Gentlemen:
The following report describes the results
of the electrical resistivity survey conducted over the
group of 10 mining claims held by Paige Petroleum Limited
and located in the Manitouwadge Lake area, District of
Thunder Bay, Ontario. This survey was conducted by Oeo-
Technical Development Company Limited during the period
April 18th to 26th, 195U- The results obtained on this
survey are depicted on Plan No. l accompanying this report.
Summary and Hecommendations
The electrical resistivity survey Indicated
several structural features which should prove very help
ful in the further exploration of this claims group.
A north-east trending fault structure has been
interpreted as extending in a north-east direction through
the west portion of the property. This fault appears to
be offset by an east-west fault extending through the
central portion of the claims group.
Several anomalies showing quite low resistivity
readings were delineated by the resistivity work and are
interpreted as representing shearing or fracturing* These
zones all follow linear trends of relatively lower resistiv
ity and are identified on the accompanying Plan by the
letters "A", "B M , "C", "D", "E" and "P". The resistivity
readings obtained over some sections of these interpreted
BED -TECHNICAL DEVELOPMENT COMPANY LIMITED
-2-
sWar or fracture zones are sufficiently low to suggest
the presence of at least disseminated sulphide mineraliza
tion*
Other zones of low resistivity obtained through
out the surveyed area do not appear to be associated with
any strong structural features and could be the result of
topographic rather than geologic conditions.
It is recommended that the next step in the
exploration of this claims group be confined to a preliminary
geological examination and some prospecting concentrating
the work in the areas of lower resistivity. The north-
south traverse lines used for the electrical resistivity
survey should provide excellent control lines for this
work. Diamond drilling can best be planned after the
preliminary geological work.
In the event that overburden conditions make
surface examinations impractical, it is recommended that
limited diamond drilling be carried out in the northwest
corner of the property to cross-section the zones of low
readings outlined by the resistivity work.
Property
The property of Paige Petroleum Limited covered
by this report consists of 10 mining claims located in the
Manitouwadge Lake area, District of Thunder Bay, Port
Arthur Mining Division, Ontario. The claims group is
located in the northwest section of the Manitouwadge Lake
CEO -TECHNICAL DEVELOPMENT COMPANY LIMITED
-3-
•^^raining area and adjoins to the east of the property of
Sudbury Contact Hine s Limited.
The claims included in the group are further
described as follows: T.B. I|.8l6[|., I|8l65 and 14.8172 to
U8179 inclusive. .
Location and Access
The Manitouwadge Lake area is located approxi
mately 75 airline miles southeast of Geraldton, Ontario
and i^.0 airline miles northeast of Heron Bay. The area
is reached by air from either of the two points mentioned
above and various airway companies operate chartered
flights into Manitouwadge Lake as well as other small
lakes in the general vicinity. Helicopter service is
also available and is very useful for reaching properties
where there are no lakes suitable for landing standard
type aircraft.
A truck road constructed by companies engaged
in lumbering in the general area extends from Stevens, a
point on the Canadian National Railway, south to Camp 12
located in the west part of the Manitouwadge Lake area
mining camp* Several bush roads service the Immediate
area around Camp 12 and are suitable for truck travel.
The distance from Stevens to Camp 12 is approximately
30 miles. A winter road also extends north from Helmo
on the Canadian Pacific Railway and services logging
camps in the south part of the general Manitouwadge area*
GEO -TECHNICAL DEVELOPMENT COMPANY LIMITED
"k-
~ The property of Paige Petroleum Limited can
be reached by a truck road extending east from Camp 12
and which passes within one-quarter of a mile to the
south of the Company's claims group. The distance from
Camp 12 to the property is approximately 8 miles.
Plans are underway to construct a Provincial
road into the Manitouwadge Lake area and railroad survey
crews are presently surveying a route for a rail line
into the area.
Topography
The topography of the claims group is quite
flat with a gentle slope to the north. The nature of
the topography does not suggest much outcrop but it is
quite possible that detailed prospecting will locate
rock exposures. A small stream flows in a southerly
direction through the claims group but it is not known
whether it maintains a flow of water during the summer
season.
general Geology
Very little information has been published on
the geology of the Manitouwadge Lake area. A limited
amount of reconnaissance work was conducted by the
Ontario Department of Mines and is shown on Map 14.1-J
"Heron Bay and White Lake Area" Sheet, published in
1932. This map accompanies XLI Annual Report of the
Ontario Department of Mines, Part IV, 1932.
GEO -TECHNICAL DEVELOPMENT COMPANY LIMITED
-5-
The claims group discussed herein is located
immediately to the north of that part of the Manitouwadge
Lake area geologized by the Ontario Department of Mines
and shown on Map ^1-j*
Map lil-j shows a band of early Precambrian
volcanics from l to 2 miles wide extending in an east-
west direction through the Manitouwadge Lake area and
bounded to the north and south by an Algoman type granite.
The property of *aige Petroleum Limited is located about
three miles north or the contact as shown on this map*
The ore boditss found on the Geco Mines Limited property
are located on or near the north contact of this volcanic
assemblage. However, preliminary examinations of the
Lun-Echo Mines Limited ground show that the copper-zinc
mineralization is not confined to this one contact zone*
It is quite possible that more detailed
geological work will show the presence of other greenstone
horizons in the general area.
Explanation of Resistivity Method
The method used by Geo-Technical Development
Company Limited is a form of the earlier resistivity
methods modified by some eight years' experience in the
field.
In essence, a known current is put into the
ground and readings are taken at 50 foot intervals along
the picket lines by sensitive vacuum tube voltmeters
GEO -TECHNICAL DEVELOPMENT COMPANY LIMITED
-6-
"measuring the voltage drop across this interval. Calcu
lations translate these voltage readings into resistance
values in terms of ohm-centimeters. These are plotted
on the map.
Due to the inhomogeneity of the medium being
examined, in short, the complexity of the geology and
structure, interpretations are based on experience and
a knowledge of the geological conditions in the area being
tested with this particular method. Where the latter are
unknown, the interpretation must, of necessity, be limited
or very tentative.
However, without any geological information it
is generally possible to differentiate between banded
rocks such as volcanics, sediments or gneiss and large
bodies of massive intrusives, due to the difference of
electrical conductivity between the various flows or
beds. Strike trends, folding, etc., are therefore readily
picked up. In some cases, rock contacts may be inferred.
Shear or fracture zones are relatively better
conductors due to their higher water content. Where
extreme low resistivity values are found, graphite or
sulphides are indicated. Graphite is found in schist
or shear zones or sedimentary horizons, nhich are shown
by electrical methods as, generally, narrow low linear
trends. Unfortunately, from the point of view of inter
pretation, sulphides may be present with the graphite or
may occur in shear zones giving similar low linears.
GEO -TECHNICAL DEVELOPMENT COMPANY LIMITED
-l-
Interpretation of Resistivity Results
The results of the electrical resistivity
survey conducted over the property of Paige Petroleum
Limited located in the Manitouwadge La* e area, Ontario,
are depicted on Plan No. l accompanying this report.
The results of this survey can be considered
encouraging and several structural features were delin
eated which should serve as a very useful guide in the
further exploration of this property.
The contour plan of the electrical resistivity
results shows a definite break in the east-west structural
trend which is believed to be a result of north-east fault
ing. This fault structure is also suggested by topographic
lineaments which stand out quite sharply in aerial photo
graphs of the area. The resistivity survey suggests this
north-east faulting to be offset about 800 feet by an
east-west fault. The movement along the east-west fault
appears to be left-hand.
The resistivity survey has Indicated several
east-west conducting zones following linear trends of
relatively lower resistivity and interpreted as repre
senting shearing or fracturing. The most significant
of these zones are identified on the accompanying Plan
by the letters "A", "B", "C", "D", "E" and "F". Low
resistivity readings obtained over some of these zones
suggest the presence of at least disseminated sulphide
mineralization.
GEO -TECHNICAL DEVELOPMENT COMPANY LIMITED
-8-
The "A", "B", "C" and "D" shear zones are
located west of the interpreted north-east trending
fault and cut off quite sharply against it. The "E"
and "P" zones are located east of the fault in the
northeast part of the property. These two structures
are somewhat weakly defined and probably represent
fracturing rather than shearing. The fact that they
do not appear to be continuous along strike tends to
confirm the presence of fracturing rather than shearing.
A broad zone of low resistivity underlies a
large part of Claims T.B. l±Bl6l± and Ij.8l7li. The broad
nature of this zone of low readings suggests topographic
influences, although the low reading obtained on Line
28 4 00 E stands out quite sharply and could be caused
by geologic rather than topographic conditions. It is
possible that a zone of fracturing extends through
this area but the extent to which it would influence
the resistivity readings is somewhat masked by topo
graphic effects.
Other minor anomalous conditions observed
throughout the ai rveyed area could, in part, be caused
by weak fracturing but are believed to be the result of
topographic influences.
GEO -TECHNICAL DEVELOPMENT COMPANY LIMITED
-9-
Survey Data
An electrical resistivity survey was conducted
over the property of Paige Petroleum Limited located in
the Manitouwadge Lake area, District of Thunder Bay,
Ontario.
The survey was conducted by Geo-Technical
Development Company Limited during the period April l8th
to 26th, 195U* and the results are shown on Plan No. l
accompanying this report*
An east-west base line was established through
the central part of the property and north-south traverse
lines were turned off at lj.00 foot intervals. Electrical
resistivity readings were taken at 50 foot intervals along
these north-south traverse lines. These readings are shown
on Plan No. l to the east of the traverse lines and areIj.
expressed in ohm-centimetera x 10 .
A total of 6.614. nil's of line were surveyed by
the electrical resistivity method which required 66^ station
readings. The claims covered by the electrical resistivity
survey are numbered T.B. I;8l6fy, 1^.8160 and i|8l?2 to 1^.8179
inclusive.
The number of eight-hour man days required to
complete this work is as follows:-
f
GEO -TECHNICAL DEVELOPMENT COMPANY LIMITED
-10-
Line cutting and chainingLaying spread wireOperating resistivity surveyCalculation 6 InterpretationDraftingOffice Typing 4 Supervision
Totals
(8 hour) Attributable to Man Days Assessment Work
16 x k 2 x b
20 x 52 x k7x46 xk
.180
828
53 212
Respectfully submitted,
GEO-TECHNICAL DEVELOPMENT COMPANT LIMITED
J. D. McCannell,
May 31, Toronto, Ontario
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PAIGE PETROLEUM LIMITEDGEOLOGICAL PLAN
MANITOUWADGE LAKE AREA
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LINES CUT AND CHAINED, RESISTIVITY READINGS OBSERVED
RESISTIVITY CONTOUR
FAULT ZONE INFERRED FROM GEOPHYSICAL SURVEY
SHEAR OR FRACTURE ZONE INFERRED FROM GEOPHYSICAL SURVEY
ELECTRICAL RESISTIVITY ANOMALY
CLAIM BOUNDARY AND CLAIM POST LOCATION
J , ^jfZ- ——o —— —l— ——O —— o1- -J V-IJLL - ̂ __
LOCATION MAPSCALE l"- l MILE
MAC Li O D COCKkHUTT
ELECTRICAL RESISTIVITY SURVEY OVER PROPERTY OF
PAIGE PETROLEUM LIMITEDRESISTIVITY CONTOURS AND GEOLOGICAL INTERPRETATION
MANITOUWADGE LAKfc AREANAMA CREEK SECTION
DISTRICT OF THUNDER BAY
PQRT ARTHUR MINING DIVISION ONTARIO
GEOPHYSICAL SURVEY BY
GEO -TECHNICAL DEVELOPMENTPLAN N 0 l
SCALE 200'
COMPANYMAY 1954
LIMITED
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B3.4E4 MANITOUWADGE LAKE24 - S - S4J
