32D04NW0377 OP92-282 ARNOLD 010
VICTORIA LAKE PROPERTYMORRISETTE, ARNOLD, LEBEL TOWNSHIPS, ONTARIOLARDER LAKE MINING DIVISIONO.P.A.P. FILE NUMBER OP92-282
FINAL REPORT
Graham Long, B.Sc., Geologist
PiO i
TABLE OF CONTENTS
Page Summary i
1 .0 Introduction............................................................................................ 1
2.0 Property Location and Access........................................................ 1
3.0 Land Position......................................................................................... 3
40 Previous Work...................................................................................... 3
5.0 Geology.................................................................................................... 55.1 Regional Geology,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 55.2 Property Geology,,,,,,.,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 9 Q
5.2. 1 Stripped Zone * 1 ,,,,,,,,,,,,,,,,,.,,,,,,,,,,,,, 1 45.2.2 Stripped Zone *2,,,,,,,,,,,.,,,,,,,,,,,,,,,,,,, 16
6.0 Geophysics,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 186.1 Instrumentation and Survey Procedure.,,,,,,,,,,,,, 18
6. 1 . l Magnetometer.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 1 86.1.2 VLF EM- 16,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 19
6.2 Results,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 196.2. 1 Magnetometer,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 1 96.2.1 VLF EM- 16,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 19
7.0 Conclusions and Recommendations,,,,,,,,,,,,,,,,,,,,,,. 20
References.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 22
Figure 1 Claim Location MapFigure 2 Geology of the Abitibi Greenstone BeltFigure 3 Geology of the Timmins Kirkland Lake AreaFigure 4 Sample Location Map- Morrisette and Arnold TownshipsFigure 5 Sample Location Map- Island in Victoria LakeFigure 6 Stripped Zone* l - Detai led Geology MapFigure 7 Stripped Zone*2- Detailed Geology Map
Appendix 1 Statement of QualificationsAppendix 2 Legend- Geological SymbolsAppendix 3 Sample DescriptionsAppendix 4 Assay Sheets
Table 1 Table of Lithologies
SUMMARY
During the 1992 field season the Victoria Lake Property situated
approximately 10 Km northeast of the town of Kirkland Lake, and 1 Km
northeast of the town of King Kirkland, Ontario, was subjected to an
exploration program financed by O.P.A.P. grant No. OPG92-146 and the
author.
The program consisted of establishing a grid system along a strike
length of 2.8 Km, over a portion of the Murdoch Creek Fault Zone which has
remained relatively untested to date. A geophysics program consisting of
gradient mag and V1F was carried out over the grid as well as geological
mapping and prospecting. The remaining areas outside of the grid and
within the property boundaries were selectively examined for their
economic potential.
This report covers in detail the results of the exploration program.
1.0 INTRODUCTION
An exploration program carried out on the Victoria Lake Property,
held in good standing by Mr. Glenn J. Mullan, of Dubuisson, Quebec, was
carried out during the 1992 field season. The program conisted of
establishing a grid system covering approximately 2.8 Km of strike length
over a relatively untested portion of the Murdoch Creek Fault Zone, which
is a splay off of the Kirkland Lake main break.
Lines were spaced at 100m intervals and stations established every
25m.
Geophysics consisted of a gradient mag survey as well as a one
station VLF survey. Geological mapping and prospecting was carried out
over the grid as well as detail mapping and sampling of two stripped zones
produced by a previous company.
Ground outside of the grid system was selectively chosen for
prospecting and sampling.
2.Q PROPERTY LOCATION AND ACCESS
The 43 claim property is located approximately l Km northeast of the
town of King Kirkland and some 10 Km northeast of Kirkland Lake, Ontario
(see Figure 1). The ground is within the Kirkland Lake resident geologists
area and encompasses the intersection of Morrisette, Arnold and Lebel
townships. All of these townships are in the Larder Lake Mining Division,
District of Timiskaming and covered by N.T.S. map sheet 32D/4 The
intersection of the townships is located at latitude 48* 11'23" and
longitude 79*53'l O".
MORRISETTE TWP
982340,1 982341 ] 982342 '! 111152411 \\ 1930 , 1111929 , 1111926 ( 1111925
,__j__j__\,^Jr---A--r-'—^-^-982339, 1 982338 ' 1111525 Jl H1932-] 1111931J 1111928 j 1111W7 ]'rfl1924
MURDOCH CREEK FAULTJONE (APPX. LOCATION)
B MISEMA LAKE- MIST LAKE FAULT ZONE ED HARGREAVES (APPX. LOCATION)
Lia KENAKOTT-KIRKLAND
KIRGOOD
' l 982335
982327 i 982330 982333 l 982336
LEBEL TWP
982326 i 982331982332 , 982337
ARNOLD TWP
N
VICTORIA LAKE
,'JBIDGOOD MINE ROAD TO KING KIRKLAND j)
l ,^--*''* f,' a
_______\\ BIDGOOD *2 MINE________
VICTORIA LAKE PROPERTY
CLAIM LOCATION MAP
_____meters- -
O 500 1000
Figure
The property Is easily accessed by by taking the Bidgood Mine
road,from highway 66, northeast to the south end of McTavish lake where a
boat can be launched thereby accessing the central portion of the claim
group. This is also the best access to the peninsula and island located in
Lebel township. A gravel road leading north from the town of King
Kirkland, cuts the northwestern corner of the property and gives access to
old skidder roads and footpaths on the property.
An old road leading in a southwesterly direction from Esker Lakes
Provincial Parks road, and located just north of the North Arm of Victoria
Lake, leads to the Ronal Red Lake shaft area located at the most northern
portion of the property.
30 LAND POSITION!
The 43 unpatented mining claim property is held in good standing and
1005? owned by Mr. Glenn J. Mullan of Dubuisson, Quebec.
40 PREVIOUS WORK
As far back as 1936, the property was considered to hold high
potential for an economic deposit as is suggested by the add by Kenakott
Kirkland Gold Mines Ltd. appearing in the September 3,1936 issue of the
Northern Miner. The add states that the property is similar to those on the
West Kirkland Lake camp and contains similar host lithologies to those on
the Bidgood property lying emmediately to the south. A vague reference to
free gold is made in the add stating that the occurence is located at the
intersection of two shear zones located in the eastern portion of the then
existing property.
In 1947, Ronal Red Lake Gold Mines Ltd. carried out prospecting,
mapping and drilling in the area of the Ronal Red Lake shaft, on the George
Tough claim group, which is encomposed by the present day Victoria Lake
Property.
Numerous shears were discovered in the outcrop and as a result some
stripping in two locations as well as eight (8) x-ray drill holes were put
down. None of the core samples contained any significant amounts of gold,
but grab samples containing as much as 2.05 oz/t (S71.75 gold at 135/oz)
were reported.
More recently in 1989 the the property was subjected to a combined
airborne magnetic and VLF-electromagnetic survey carried out by
H. Ferderber Geophysics Ltd for Trinity Explorations Ltd. The survey
outlined 5 potential fault zones and three probable shear zones.
In 1990 under option to Pamorex Minerals Inc., the company stripped
and sampled two areas over the Murdoch Creek Fault zone. Of particular
interest was an assay of 0.18 oz Au/ton over a 3 foot length.
5.0 GEOLOGY
5.1 REGIONAL GEOLOGY
The townships of Morrisette, Lebel and Arnold are located in the Abitibi
Subprovence which itself is located in the southeast margin of the
Superior Structural Province. The Abitibi Subprovince, more commonly
refered to as the Abitibi Greenstone Belt, encompasses the town of
Timmins , Ontario in the west, Val d'Or, Quebec in the east, and the towns
of Matagami and Chibougamau, Quebec in the North (see Figure 2).
The Abitibi Greenstone Belt is a folded geosynclinal belt consisting of
volcano-sedimentary lithologies(see Table 1). All of the rocks , with the
exception of proterozoic intrusives, are Archean in age and have been
metamorphosed to the subgreenschist facies. Numerous igneous intrusives
including stocks, dikes and sills crosscut all of the rocks of the belt. The
major structural features of the greenstone belt consist of the
Destor-Porcupine fault in the north and the Cadillac-Larder Lake fault in
the south (see figure 3). These two deep seated fault zones are responsible
for numerous gold deposits.
The volcanic rocks were formed during cycles of volcanism that
consisted of komatiitic volcanism followed by tholeiitic, calc-alkaline,
and ultimately alkalic volcanism. The rocks of each group are refered to as
a supergroup. A supergroup is divided into groups according to major
changes in the chemistry of the rocks (Jensen, 1981).
ABITIBI , l. /s- GREENSTONE Ji
Abitibi Greenstone Belt
Granitic rocks
Mafic intrusions
Ultramafic rocks
Early Precambrian sediments
Km
40 60 Mi
Middle Precambrian sediments
Volcanics
Munro Group(Goodwin and Ridler. 1970)
en
Figure 2. Geology of the Abitibi greenstone belt (after Goodwin end Ridler 1970)
LAKE ABITIBI t t'l 1^1 i l i
'BATHOLITH'••-t-^^^'-vV'Vii-^v/c;- s;-V-"-^^ ,\,:r^jl'.V'f
!^^\ \ xk-
It t t t t t t t \.K t tttttttl
^J\t t t t t t t \t t t t t t t tttttttltttttttl tttttttl
.,,,. ttttttt 1
v v v v v v LAKE V vvvvvvvvv
"- "
tit t t t t t |t t 1*i-'- 'N-./ 'J T l. t t t t t 11 t t |"'r''''.-VVt \ t t t t t V t t - ,: l l - , \
t tV ttttttt t'irs /V."^\
KENOGAMISSI ltt t t fiU;. -;V'^n ATI i^^i ITL i T l t t It TT, - '~. i x
~^ i ' .C* t -* l - ^ v~, ' '-., ^'''TTTTTTTTTT T I TT T I IT,^.,, ;: ^'^:'rr ;,;-,- MATACHEWAN VtttVttt t t ttVttt t t tt t t tt ttVt'f: "'-';'' ''T" '^^'Wt^tSVS-ROUND LAKEtVtVlVtVtVtV
t tt\^tt TttBATHOLITHttttttt t ttttttttttttttttttttt
LEGEND
UPPER SUPERGROUP
Alkalic Volcanics(Timiskaming Group)
Calcalkahc Volcanics
( Blake River Group) Tholeiitic Volcanics
(Kinoievis Group) Komatiilic Volcanics
(Stoughton Roquemaure Group and Larder Lake Group)
LOWER SUPERGROUP
Sedimentary Rocks ( Porcupine Group)
Calc-alkalic 4 Tholeiitic Volcanics
(a Skead S Catherine Group) (b.Hunter Mine Group)
Komatiitic Volcanics
(WabewawaGroup)
O 12 Mi
20 Km
Figure 3. Geology of the Timmins-Kirkland Lake area (after Jensen 1978)
8
Table 1: Table of Lithologies
CENOZOIC
Pleistocene and RecentGlacial tills, esker deposits, proglacial lacustrine sands and silts, aeolian sands, peat
Unconformity PRECAMBRIAN
ARCHEAN
LATE MAFIC INTRUSIVE ROCKS Diabase
Intrusive Contact
LATE FELSIC INTRUSIVE ROCKSOranite, syenite, and related porphyritic dikes and sills
Intrusive Contact
EARLY MAFIC AND ULTRAMAFIC INTRUSIVE ROCKSDiorite, gabbro, anorthosite gabbro, peridotite, and lamprophyre
Intrusive Contact
FELSIC TO INTERMEDIATE METAVOLCANICS Dacite, andesite, and rhyodacite
METASEDIMENTSLimy sandstone, quartzite, and quartzitic conglomerate; meta-arkose and arkosic conglomerate; pebble conglomerate and breccia; slate and chloritic conglomerate
Disconformity
EARLY FELSIC INTRUSIVE ROCKS Quartz-feldspar porphyry
Intrusive Contact
MAFIC TO INTERMEDIATE METAVOLCANICS Basalt and Andesite; interflow sedimentary rocks
(after Rupert and Lovell; 1970)
In the Kirkland Lake- Noranda area the supergroups are divided into upper
and lower sections. The lower supergroup consists of the Pacaud tuffs
which occupy the lowest and oldest stratigraphic horizon, followed by the
Wabewawa group, the Catherine group and the Skead group. These groups
represent komatiitic, tholeiitic, calc-alkalic and alkalic lavas.
In the Upper Supergroup, the basal komatiitic succession is refered to as
the Stoughton-Roquemaure Group on the north limb of the syncinorium and
as the Larder lake Group on the south limb of the synclinorium. The
overlying tholeiitic, calc-alkalic, and alkalic successions are refered to as
the Kinojevis, Blake River, and Timiskaming Groups respectively (see
Figure 3).
5.2 PROPERTY GEOLOGY
The Victoria Lake property lies entirely within the Kinojevis Supergroup
comprised of tholeiitic metavolcanics. The property is predominately
underlain by intermediate volcanics comprised of andesite flows with the
possibility of some andesitic tuffs. A mafic volcanic, pillowed basalt flow
, and an intermediate to felsic pyroclastic breccia, cut by quartz feldspar
porphyries occur in the northeast corner of the property in Morrisette
township (see Map l in bavk pocket). These units, with the exception of the
felsic intrusives, are sheared and carbonitized by the Murdock
Creek-Kennedy Lake Fault zone which is a secondary splay off of the
Cadillac-Larder Lake Main Break. A gabbro plug intrudes the intermediate
volcanic host rock in Arnold township, as well as in a portion of
Morrisette township, and is sheared and carbonatized by the Misema
Lake-Mist Lake fault zone which is another off shoot of the
Cadillac-Larder Lake Main Break. In Lebel township, the island in Victoria
Lake is sheared and carbonatized but is not believed to contain high
economic potential.
A cut grid of approximately 22 Km was established over the Murdock
Creek-Kennedy Lake Fault Zone. The baseline was positioned in order to
parrallel the fault, the wing lines were spaced at 100 meter intervals
with stations every 25 meters (see Map l in the back pocket).
With the exception of a small andesite breccia outcrop located at
L11 +00 W, 3+75 N , the western portion of the grid contains no outcrop,
thus leaving the geological interpretation to the geophysics surveys. Since
the area is magnetically flat, it is assumed to be underlain by
intermediate metavolcanic flows with the possibility of interbedded tuffs.
The eastern portion of the grid contains abundant outcrop (see Map 4 in
the back pocket). The predominant rock type is a pillowed basalt. This unit
does not appear to be of any economic importance although a few boulders
were observed to contain fine to medium grained euhedral pyrite in some
instances in quantities of H?5. It is known that massive sulphide deposits
will have halos of sulphides extending away from the deposits,particularly
in pillow selvages, therefore it may be possible to trace these minor
sulphide occurences along strike of a known structure, to an economic
occurence.
Flanking the basalt to the south, is an intermediate to felsic pyroclastic
breccia or agglomerate. The pyroclasts range in size from lapilli to bomb
sized fragments and have been sericitized and carbonatized in the
ntsema Lake - Mist Lake Fault
samples 507-510, Inclusive
LEGEND
V9 Tuff (intermediate)
3G Gabbro
q-cc v Quartz-carbonate vein
/x Shear
. 507 Sample location and number
SAMPLE LOCATION MAP - MORRISETTE AND ARNOLD TOWNSHIPSafter O.B.M. 20 17 5800 53300 SCALE: 1: 20 000 Figure A.
12Nt
502 LEBEL TOWNSHIP
VICTORIA LAKE
505
NOTE: all of the rocks on the island have been carbonatized.
LEGEND
V6 Andesite
V9 Tuff
Ml Schist (sericitized)
. 507 Sample location and number
Shear
SAMPLE LOCATION MAP - ISLAND IN VICTORIA LAKE after Map No. 53a, Township of Lebel SCALE: 1: 400 Figure 5.
13
deformation zones. The agglomerate unit has a strike of approximately
057 D Az, and an approximate width of between 75 to 100 meters. The
quartz feldspar porphyry units cut the mafic volcanic rocks but were not
observed to cut the agglomerate. South of the agglomerate unit there are
no outcrops, therefore deriving an interpretation from the magnetic map
(see Map 1 in the back pocket) the response appears to be that of an
intermediate volcanic, most likely an andesitic flow unit.
The quatrz feldspar porphyry units found on the east grid, contain
phenocrysts of alkali feldspar ranging in size from 1-2 mm to Hem, the
latter crystals taking on hexagonal shapes, in a groundmass of medium
grained quartz and alkali feldspar. A few quartz veins containing minor
amounts of pyrite were discovered in a quartz feldspar porphyry on line
8+00 E at station 1+50 S. No economic results were obtained from
assaying the vein material, but it is evidence that the system contains
hydrothermal fluids and that the intrusive could have forced the fluid into
the existing fault zones carrying with it and concentrating already
existing mineralization.
A timbered shaft occurs on line 3+00 E at approximately 0+95 N. The
shaft is partially filled in and is described by E. K. Fockler (1947) as being
an old test pit put down on calcite veining on or close to a
porphyry-andesite contact. This is the earliest reference made to the
shaft. It was most likely put down by earlier prospectors to which Fockler
describes their work as being desultory.
14
5.2.1 Stripped Zone *1
This stripped area is centrally located 16 meters west of Line 4+00 E,
station 1+50 S (see Figure 6.) The 5-10 meter wide trench has a trend of
approximately 285*Az and was stripped and washed as part of an
exploration program carried out by Pamorex Minerals Inc. in August of
1990.
The stripped area exposes a shear zone which is believed to be a portion
of the Murdock Creek-Kennedy Lake Fault Zone. The shear has an overall
trend of approximately 55*Az (range: 48'-67'Az), dips steeply to the
north, and has an exposed width for approximately 38 meters. The host
rock is an intermediate-felsic tuff breccia or agglomerate. Undeformed
portions of the rock unit show felsic pyroclasts ranging in size from
lapilli to bomb size, with the long axis of the pyroclasts paralleling that
of the predominate shear, hosted by an intermediate aphanitic matrix.
The main shear zone is highly sericitized and carbonitized thus giving it
a buff brown color. Graphite can be found in the central portion of the
shear as well as in secondary shears trending at oblique angles to the main
zone. The principle mineralization occurs as fine grained euhedral pyrite
disseminated in amounts ranging from trace to ^9?. An exception to the
overall disseminated pyrite can be found on the west side of the trench
where a gossaned area occurs. The agglomerate appears to have been
effected by an influx of iron rich fluid. Numerous lapilli and bombs have
been replaced by pyrite. Although samples from this area did not yield any
economic gold assays, they were anomalous compared to other samples
from the stripped area. This pyrite enriched zone could be an important key
VI O, undeformed
small lapilli, 2cm long, replaced by pyrite.*v"fc
*\v, WATER FILLEDf1 ''"^^^*^^" G * 522•*J-. i j* -** ^
523 i?
pyroclasts from 2 mm-10 cm in length, long axis trending at 072* Az.
\,-*;#.*V
^r'X-*//S^- .^SSfc-i X// Vi***-.-,, -'.i? 'v'V.-./^ --^^ ^-^ -Jta^•520 r-^-if ^^ A V'j: s
undeformed block, slightly rotated within shear.
"*o
/^B19* .4^•".•..V-tii. ,vrf. ^-' m
pyritized bombs10-20 cm long, 5-10 cm wide.
LEGEND
V10 Agglomerate
Ml Schist (sericitized)
,vv:.i; Overburden
^~ Shear
^ Fault
^o Strike and dip
* 507 Sample location and number
Gp
6
Fu
qv
., -. \je-\j /s//, -' -..V" i ' ...•:tu^,. *~. vi*- ^^ s y .i tvjj.- -^fc
^^fe^/ WATER NLLED " ^^^^^^^^^5,^
^' .^^;m... ^4^.s.af^''^Vflsw^^*-*^' "S5p*^-^*^f ̂ ^
.rt* i'^'i'TV'.^'J. -...
^^\
'^,.
Note: all of the above rock unit has been carbonatized to some extent, therefore it is not mentioned on the map.
15
Graphite
Gossan
Fuchsite
Quartz vein
STRIPPED ZONE * l DETAILED GEOLOGY MAP SCALE: 1:200Figure 6.
16
in future work in the area.
5.2.2 Stripped Zone *2
This stripped area is centrally located on line 2+00 E at station 1+50 S
(see Figure 7). The 6-22 meter wide trench has a trend of 322"Az, and was
stripped and washed as part of an exploration program carried out by
Pamorex Minerals Inc. in August of 1990.
This stripped area exposes the Ronal Red Lake showing which is a
sericitized shear zone trending approximately 305*Az (+X- 10'). The shear
is weakly mineralized with disseminated pyrite rarely exceeding 195. In
the southern portion of the stripped area, Pamorex obtained a gold assay of
6240 ppb (0.18 oz Au/ton) over 3 feet (see Figure 7). They also report the
same shear averaging 2400 ppb (0.07 oz Au/ton) across 3 to 4 feet for
approximately 35 feet along strike before being cut off by another shear
zone.
The host rock is an intermediate-mafic pillowed basalt. The basalt is
locally brecciated and locally contains well preserved pillows as well as
hyaloclastic texture. In the northern portion of the stripped area the
contact between the basalt and the overlying agglomerate is exposed for a
distance of just over 4 meters. The contact strikes along 042"Az and dips
50" to the north. The agglomerate is strongly serecitized, moderately
carbonatized and iron stained. The unit is highly sheared at 360"Az and
contains up to ^disseminated pyrite locally.
,.—**fc*\./~\ V10 17
LEGEND
WATER FILLED
Agglomerate
Basalt
Overburden
Pillow structure
Brecciated
Hyaloclastite
Sample location and number
Shear
Fault
Pomorex channel sample 0.18ozAuXtonover3feet
STRIPPED ZONE *2 DETAILED GEOLOGY MAP SCALE 1:200 Figure 7.
18
6.Q GEOPHYSICS
6.1 Instrumentation and Survey Procedure
6.1.1 Magnetometer
The Proton Precession Magnetometer, GSM-8, was used to carry out the
magnetometer survey on the Victoria Lake Property. The proton
magnetometer uses the precession of spinning protons or nuclei of the
hydrogen atom in a sample of hydrocarbon fluid to measure the total
magnetic field intensity.
The total magnetic intensity, as measured by the proton magnetometer is
the magnitude of the earth's field vector independent of its direction. The
measurement can be expressed as a length (ie. 50,000 gammas) of the
earth's field vector. A local disturbance, say 10 gammas, would add (or
subtract) to the undisturbed field of 50,000 gammas in the usual manner
of vector addition. Since the proton magnetometer measures the magnitude
of the resultant vector (whose direction is almost parallel to the
undisturbed total field vector), that which is measured is very nearly the
component of the disturbance vector in the direction of the undisturbed
total field. Thus the change in total field intensity is called the anomaly
(Spence, 1989).
The data was collected at 25 meter intervals using a GSM-8 Proton
Magnetometer. Base readings were taken approximately every hour and
then used at the end of the day to correct for the fluctuations in the
earth's magnetic field. The data was plotted on a map scale of 1: 5000 and
contoured at a 100 Nt interval.
6.1.2 VLF EM-16
The VLF transmitting stations operating for communications with
submarines have a vertical antenna. The antenna current is thus vertical,
creating a concentric horizontal magnetic field around them. When these
magnetic fields meet conductive bodies in the ground, there will be
secondary fields radiating from these bodies. The VIF Em-16 measures the
vertical components of these secondary fields (Spence, 1989).
The Cutler, Maine transmitter station was chosen because of its
favourable orientation to the geology and structure of the property.
Readings were taken at 25 meter intervals along the cut lines of the grid,
using a Geonics EM-16 with both the in phase and quadrature being
recorded. Profiled data as well as Fraser filtered data were plotted on a
scale of 1: 5000, copies of which accompany this report.
6.2 Results
6.2.1 Magnetometer
The total field survey was useful in outlining the basalt unit in the
eastern portion of the grid system. Of special interest would be the 360
meter long magnetic low trending along 075* Az between lines 1+00 and
4+00 east. The western portion of the grid is relatively flat and might be
interpreted to be underlain by intermediate metavolcanics.
6.2.2 VLF EM-16
The Vlf survey was successful in delineating a number of anomalies, the
strongest and most interesting of which trends along 065' Az. This trend
coincides approximately with the trend of the Murdoch Creek Fault Zone
20
and more than likely represents the fault itself.
7.0 Conclusions and Recommendations
The exploration program carried out on the Victoria Lake Property,
consisting of 43 unpatented mining claims and. located at the junction of
Morrisette, Arnold and Lebel townships in Ontario, has proven that the
ground holds tremendous gold potential. The program has confirmed that
the essential elements for an economic deposit exist. In Morrisette
township the stripped zones expose auriferous, highly sheared and
carbonitized fault zones related to the Murdoch Creek Fault Zone. The
stripped areas contain quartz stringers and veins, disseminated pyrite
mineralization as well as chromium mica alteration. The volcanic host
rock also contains quartz feldspar porphyry intrusives containing
mineralized quartz veins.
The spatial association of felsic intrusive bodies with gold
mineralization is well known. Studies have shown that the emplacement of
an intrusive body will cause dehydration of the host rock at the contact
while remobilizing mineralization away from the contact area. These then
enriched fluids can accumulate in fractures and fault systems and in many
instances form economic deposits.
Prospecting in Lebel and Arnold townships turned up other shear systems
on the property. In Arnold township a quartz carbonate vein was discovered
within the Misema Lake- Mist Lake Fault Zone. Further work is required in
the area where the sample was taken in order to properly assess the zone.
21
The island dividing Victoria Lake and McTavish Lake is essentially all
sheared and carbonatized but appears to hold low potential for an
economic deposit.
In order to evaluate the full potential for a gold deposit on the property,
the western portion of the grid system should be continued to the north
boundary.
A Max-Min survey should be carried out over the entire grid system in
order to delineate any mineralized fracture systems that the VLF and
magnetometer surveys could not detect. Targets of interest should then be
drill tested.
22
REFERENCES
Cattalini, S., Chartrand, F. 1990. Massive Sulphide Deposits in Northwestern Quebec. In The Northwestern Quebec Polymetallic Belt. Edited by M. Rive, P. Verpaelst, Y. Gagnon, J.M. Lulin, G. Riverin and A. Simard. The Canadian Institute of Mining and Metallurgy, Special Volume 43.
Campbell, R.A., Report on the Combined Airborne Magnetic and VLF-Electromagnetic Survey on the Murdoch Creek Fault Property of Trinity Explorations. Lebel, Morrisette, and Arnold Townships, Larder Lake Mining Division, Ontario. H. Ferderber Geophysics, 14p., 1989.
Colvine, A.C., et al. 1988: Archean Lode Gold Deposits in Ontario; Ontario Geological Survey, Miscellaneous Paper 139, p. 136
Easton, R.M., and Johns, G.W. 1986: Volcanology and MineralExploration: The Application of Physical Volcanology and Facies Studies; P.2-40 in Volcanology and Mineral Deposits, edited by John Wood and Henry Wallace, Ontario Geological Survey, Miscellaneous Paper 129, 183 p.
Grabowski, G., Lovell, K, Guindon, D., and Bath, A.C. 1988. Kirkland Lake Resident Geologist's District-1987; in Report of Activities 1987, Resident Geologists, Ontario Geological Survey, Miscellaneous Paper 138, p251-284
Hogg, W.A., Geological Report No. 29,1964 15p., Arnold and Katrine Townships,0ntario Department of mines. Accompanied by Map No. 2061, Scale, 1 inch to 1/2 mile.
Jenson, L.5., 1981: Gold Mineralization in the Kirkland Lake- Larder Lake Area; p. 59-65 in Genesis of Archean, Volcanic-Hosted Gold Deposits, Symposium Held at the University of Waterloo, March 7, 1980, Ontario Geological Survey, MP 97, 175p.
Meyer, G., Grabowski, G., Lovell, H., Guindon, D., and Bath, A.C.1990. Kirkland Lake Resident Geologist's District-1989; in Report of Activities 1989, Resident Geologists, Ontario Geological Survey, Miscellaneous Paper 147, p255-272
23
Meyer,G., Grabowski, G., Lovell, H., Guindon, D., and Bath, A.C1989. Kirkland Lake Resident Geologist's District-1988; in Report of Activities 1988, Resident Geologists, Ontario Geological Survey, Miscellaneous Paper 142, p267-300
Pearson, V., Leve geologique de la propriete Lebel, Canton Lebel et de Morrisette, Kirkland Lake, Ontario, 93p. October 1988. Exploration Brex Inc.
Rupert, R.J., and Lovell, H.L, Geological Report 84, 27p.,1970, Geology of Bernhardt and Morrisette Townships, Ontario Department of Mines. Accompanied by Map 2193, Scale, 1 inch to 1/2 mile.
Spence, I., 1989: Geophysical report, Conglomerate Lake Property, High Frontier Resources.
Turcotte, R., and Lambert, R., Val d,0r Geophysique, Leve Geophysique propriete de Exploration Brex Inc., Project Lebel et Morrisette, Province de Quebec, Mai 1988, 8p., Vlf report with accompanying map.
Turcotte, R., and Lambert, R., Val d'Or Geophysique, Leve Geophysique propriete de Exploration Brex Inc., Project Lebel et Morrisette, Province de Quebec, Mai 1988, Sp., Mag report with accompanying map.
Watson, G.P., and Kerrich, R., 1983: Macassa Mine, Kirkland Lake; Production History, Geology, Gold Ore Types and Hydrothermal Regimes, p.56-74 in The Geology of Gold in Ontario, edited by A.C. Colvine, Ontario Geological Survey, Miscellaneous Paper 110, 278p.
Map No. 53a, Township of Lebel, Scale: 1 inch to 1,000 feet.
APPENDIX 1
STATEMENT OF QUALIFICATIONS
l, Graham G. Long, residing in the city of Rouyn-Noranda, in the province of Quebec, hereby certify that:
1. l am an exploration geologist and have been practicing my profession since 1988.
2. l graduated from Concordia University, Montreal, Quebec, with a Bachelor of Science degree in Geology in 1988.
3. l am a member in good standing of the Northwestern Quebec Prospectors Association.
JANUARY, 1993
Graham G. Long, B.Sc., Geologist
APPENDIX 2
SYMBOLES UTHOLOGlQUES
RQCHES VOLCAfffQUfS ARCHEENNES
V ftocftet votcentques mdetermmees
VI Aocnes voicanrqvet falsigues ou intermediates
V2 fthyoM.
V3 Trachyte
V4 Daota
V5 H off f t volceniquet mtarmediaires Ou /netiques
V6 Andante
V7 Sasaita
V8 ftochei pyioctastiQues indetermnees
V9 fu/
VlO Agglomerai
VI 3 floc 1*1*t volcamoue* uHremalique*
ftOCHfS SEDIMENTAtRES A/tCHfEfV/VfS
S Roche* sedimmntaires indeiermineei
St Conglomeiat
S 2 4*-* 01*
53 (?I'*utv*c*r
54 Argi/itt. share, ardinse. pttylrade
S 5 Quart t He
fQRMATlQNS Df fCft ARCHEENNES
FI fotmaiion da far indetermmee
F 2 Formation da tar sullurae
F3 formation da tar OMydea
F4 formation da far carbonatae
ftOCHES SEDiMEWAlXES fftOTEftOfOlOUES
P Roc t** * teaim+ntiiret tndeiarmmeet
n Arkose
P3 Cf*ui**c**
P4 Queritite tt gf f t
PS Argiliie. shale ardoite at pnyt/ade
P6 Fcrmetion de fer
P7 Oo/omt* et muir e t rochet a carbonetas
P8 Tillitt
ftOCHfS SEOlMfNTAIRES PALfOZOtQUfS
ftOCHfS MfTAMQttPHlQUfS
M ftocffs /nfitmorpfiiqucs t
Ml Schisie
MS Migmatite
Hit
MB
M9
MIO
Ml 1
M12
1
IS
1O
IF
IE
IG
1C
1A
1M
IN
IT
ID
IP
18
IX
12
IR
2
2T
2M
2O
2L
3
3G
3N
3R
3L
30
Gne/ss
Amphioolite
Gnnula,
Mrlonitf
Quirlitte
Miibre
aocHes inrmsivES
Rochet trtttusives fitsMtues indelerminees
Srenae
Syenite Quannque
Syenite t teldspeth tlcelin
Syenite qutrtltqve e teldspith tlcelin
Gnnite
Ctenite e teldspeth elcelm
Montonitt QuMftntjue
Momontte
Momodiofire QUirtiiQue
Tonalite
Granodiorite
Pegmatite
Aloilile
Aplite
Crenophyfe
Rhyolite et leifite intrusive
Roches intrusive* inlermediiirer tndeterminees
Diorite guirltitfue
Moniodiortte
Diorite
Limpropnyre intermediate
Rocttfs intrusive* maliQues indtteimmets
Cibbro
Ivorite
Anortnosne
lamprophyre rrtettque ou nidelermine
Diabase
4 ftoches mirusives vttratnafiques
4P Peridotite
4H Hornblendite
Serpentinite
Dunite
4S
40
4Y
e ultramatique
l Gouverrtemtni du Quebecl Mini*l*f* da l En*(gie ei das Raaiourcesl 5*cl*ur d*t m*fi**
LEGENDE DE LA COMPILATION GEOSCIENTIFIQUE
(2e ddilion, 1984)
SYMBOLES D ANOMALIES GEOCHIMIQUES ETSYM80LES O'ANOMAIIES MINERALOGIQUES
DES ALLUVIONS
SK SEDIMENTS Df RUISSEAU
f- StOIMCNTS DC fONO DE LAC
SO SOLS
IS fAL/X Of SURfACl
ve
K
ML
fA
SVMBC LES DE.S ANOMALIES GEOPHYSIQUES
f f basset valours
r* LCVE DE POLARISATION PttOVOaUEf a** de hevM
f f LEVESDEPOTeHTIELSPONTANC
LECTROMAGNfTlQUeS Afft/ffl/S (tt TURAIf* ase let SYM* ** cowanttonnels id) mufti frequence* texcluanl f /tvfl/ri
potntilM indique la mode puisttoue ih)
•f ' f 'f ' 0 - La t- ^ f (bf radiophase. f pha
A j9 A ,'. AFMAG /ef SYSiemeS muti requence^ts j f H) large ur d'anomelie rapponee: le ^fi f^ direction du leve (gf sysfemes en
' auires syslemes semi-aeroportes
HOCHES
MINI RAUK LOUHOSIBA TTCEI
FORAGE ALLUVIONNAIRE
Les tonal di lortlt tineurs geocfurmguet font delimiters pir ant ligne di contour nnlermant I'idtrtiiticanort du genre di leve it fitemmpue pit li tymbole dta etimerta fmterfl.
CCHANTILL ONNAGllSOLf
fCHAH TIL L ONHAGf DC BLOC IRK A TIQUf
f f f f ti-S f i Jt t ^ ^ rf
x/-
LfVf eLECTmMAGNfriauEACHIEN SrSTEMCINPUT III3 ctniux llvec pfOduit conductivity - 4p*nset*r. mltatl Ibl3 cirtiun Id 4 ciniu* tdl 5 ciaiuf tel 6 cima* If! Ino- mlli* mtgnetiqu* coincident! lg! inomat* rmgntoqui fux- lipost*
LEVtS ELECTROMAGNf TIQVES AU SOL tllsWemf* A cidres honioniau* llvec produn conductivite-toaiS' icuf. mhosllblsystfmes t cidns vtniciuxlcisrstemex
tn mode pulsatotre
LFVES MAGNETlQUfS f AXES DE HAUTES VALEURSI: Illllnlnttbllusol
L6VE CRAVIMfTfttQUf: talhaut grawnttnqve Ibtbas&m-
...ASONDAGE ALL UVIOHNAIRC lint molonMut In mtttn t onjchil. On i&nanpj&a que las lonoagcs aluvxynjott soni repottes sufti coucfts 3
LEVE RAOIOMETRIQUE OU DE SPfCTDMfTWf DCS HAY- OfllS GAMMA: til uranium Ibl thonum id nppon untnmm/ thorium (di lolillilpotisvum
SVMBOLES DES INTERSECTIONS ET ZONES MINERALISEES
^,HAUS f E
T de i* substance if^vu et tonQueur ae la i&a ll*'
SYMBOLES DE SONOAGES
SONDAGE VERTICALlapremie'e couche bthologique renconltee v est droite ei * numero d'xJennticjtion du somtige #u Jessus on
e si un fournal de sondage e*nie tons Jes dossiers
SOMOA Gf POUH AL IMfN T A TIQN EN EA Ut a premie ft coucne lifhofogtQve renconnee y esr mdiguee adrone et lg numero a'ldentiltcttton du sondage AU itessus dusymboie f un fournal de sondage e*tsit oans tes dossiersconsultts
SONDA Gf INCL fNt A VEC PRQJEC J ION HOWZQN TAL f (eiprofondevrconnuetbipratondtufincQnnua Sondage inclmt nvec pro/efi'On ttontoniiie df la tt rtcmpfe La frototKleitr vtmcj** du mrvr rerra^i y est en metres a gauche et le nurr&o d'^entificatfon JkjdessuS Ou A dt&te Ce num&o O dont'tcatori e*actorwn a cat* donnf dons us dLsse consumes et ne figt/re sur /j cane Oe cixnomfon t}ue fes iQwniuM df sondage sont a
SUFFIXES POUR LES MINERAUX DES ROCHES SYMBOLES ST1UCTURAUX
b
c
d
e
f
gh
i
biotite
chlorite
disthene
epidote
feldspath jindeterrr
grenat
hornblende
talc
1
h
m
n
une) o
P
Q
'
carbonate
sericite paragonite
muscovite
nepheline
fekJspath-potassique
plagioclase
quaitichloriloide
s
1
u
V
W
a
yt
staurotide
tremolite adinole
amphibole (mdeteiminet
"ve me de
tourmaline
sillimanite
pyroxene
teolile
SUFFIXED POUR COMPOSITION. ORIQtNE ET ALTERATION
0
0y
s1*
Ift
COMPOSITION
felsique
mafique
ultramalique
OfllGINE
se di mentai re
vofcanique
intrusive
w
aU
rr
e
j 0*
ALTERAriON
amphibolide
Sihcifi4e
alb ii, see
pyniisee
* p idol is**
porphyrin***
ctilonnsee
A"
x
r
t.
*
ertcitisee
carbonatite
serpentinite**
alteration potass iq ne
alteration indelermmee
skarn
corneenne
SUFFIXES POUR LES SUBSTANCES D'lNTERET ECONOMIQUE
MINERAUX ET ROCHES
Am
Ay
Ap
Asp
Ba
Be
Bs
Bo
Cp
Cn
Ch
Cr
Ci
Cor
Cv
amianie
anthophyllite
apatite
arsenopyrite
barytine
beryl
bismuth
bornite
chalcopyrite
chalcosine
chert, jaspe
chromite
cordierite
corindon
covelline
Fp
FI
Gn
Gp
H err
[1m
Mt
Me
Ma
Mi
MdMo
feldspath
fluorine
galene
graphite
i hematite
ilmenite
magnetite
malachite
marcasite
mica
min^raux decoratits
molybdenite
Pn
PC
Pm
Py
Pi
Po
Ra
Sh
Sd
Si
Sp
Sm
Su
Ta
pentlandite
pier re de construction
pierre ornementale
pyrite
pyrophyllite
pyrrhotine
mmerauB radtoaciits
scheelite
siderose
ftilK*
sphalerite
spodumene
sullures (indetermines)
lanial'te
* a t/i* /'
. * e * .
T f f 9* f
a a t .1
+/ / /t t t tt
-f///U * * mf
"T~/ / /*
'aa*
-f//a * t tt-t-/ f*^
* * c rf
//o/
f
t t/ 71
1C •i
f
1* t
,/ /"tr i.
a * '
f ff f
*2sfc.
AFFLfUREMfNTS (a) 'sole, fb} aire d'aftlewements
CONTOURS GEOLOGIQUES /al connu (bt piobablx ou presume. ictd'apresievetgfophystques(AIR SOL)
STRATIFICATION. SOMMET DETERMINE (alho/uontale. fbl inclmee. (c) verticale. (di pendage nondetermine, (si renversee
STRATIFICATION. SOMMfT NON DETERMINE {a)hontoniafe. {b) incline*, fcf vertical*, td) pendage nondeter mint
SCHISTOSITE OU CLIVAGE OU FOLIA TIQN {Plan SI t(al honionttl. fbl incline . (c) vertical. Id) pendage nondetermine
SCHISTOSITE OU CLIVAGE OU fOLIA JION (Plan S2Ila! horitontal. (b) melin*, {ci vertical tdl pfitdage nondetermine
vet tic ale
DIACLASES (a) horttontales. (bf incline**, (c) verticates. (d) sysiemes multiples
LINEATION la) horizon! alt (b) mclmee. {ci verticale. (di plongee non determmee
CONTACT DE COULffS
SYMBOLES GEOMORPHOLOQIQUES
STRIfS GLACtAIRCS la) sens du mouvement connu.fbl mconnu
MORAINE FFtONTALf
fSKERS (al sens d*tcoutemenr connu. ibf mconnu
UMITfS DE TRANSGRESSION MARINE OU OfSUBMERGENCE LACUSTRE (a)connue. (b)presumee
SYMBOLES DES GJTES MINERAUX
STOCKWORK
/fxXXXXm a
XXa a
X*
f/'fyx
mt y /v
r lw*" ' * "
* aa a-
* aH e-
B B
/t aX M
A
ISOGRADE DE MfTAMOftPHlSME Le tomfnef d** point f s mdiQutt le sent cr&ssant du grade de meiamofprttsme Le nom du{dest mtntraKev't
edit de t isograde ou iHilsl esttsontf presttntfsi
LINEAMENT fobtenu par pftoto interpretation/
PLIS
ANTIFQRMfS (a) plan a*iat dtftrmtn* (t) pietum*
ANTlFORMfS OEVfRSfS talplen t*ialdeierm.i*. (bf prtfsumt!
SYNfORMES fa) plan etiml Mlermm*. W pfeittvntt
SYNFOHMES DfVtflSfS f ml plan a..*/ otffcvm-W. fbipresumt
PUS D'ENTRAINEMENT fat de*tre. (bf tenfttrt (ulrlistt avfc otj sans plonyea tt pendayet
AXC DE PLISSEMENT AVfC PtONGEf
FAILLES. ZONES Df CISAiLLfMCNT (a) CWM* (b/ presumee. (cj d aor f s leves geopf^YSiQues. id! incline*, (e) avrc tens de deolacement. (H avec aftais-tment (Itrcercte plem indique le cortt at'a-lltH. igt faifitt df
de charnage presumee
SYMBOLES DES INSTALLATIONS MINltflCC
PUI7S Df MINE lAVfC CHfVALfMENT. fat v*n*atfbl incline
PUITS o EXPLORATION ISANS CHEVALEMENII /a;vertical. Ibl incline
PUITS ABANDONNfS
TRANCHE f
GRAVIERES OU SABLItRES (a) en f.pto'tn** ft fabandonnet
MINE A cifi OUVERTOl olivine
i
SUFFIXES POUR STRUCTURES PETROGRAPHIQUES ET TEXTURES CARACTERlSTIOUES
tfMi turbidite*
iittuii L\ brechi'orme
A breche tecionique
A breche intrusive
A breche pyroclastique
m breche explosive
A breche de coulee
A hyacioclastique
UlQ
(D
0
acH
*
porphyre 'p'*
porphynque
variolinque.
amygdalaire
a spinifex
rubanee [
cisailiee C
it ae W.- df 0ft
iiQ~.. 4 5O".. rf*
spherutttique
S^^UiQi\dcnO /r/v
X
F1LON lin vttns fOfrm tt dimtnvon l
H-ON tm pouvmnt tom tuimtti tn inim ttmtraon t Fmehmim dtltctntt
AMAS M/NtRAL/Sftfn ynin tom* tt dimtnsnnl
AMAS MINCRALISf Ir* pom** itrm pim***ttn-tion i rtctitat at it ant l
moice ou POINT MINEKALISE
INTERSECTION M1HERALISEE DANS UN SONDAGE
GAlCHieS OEXPLORA1ION A fLANC Of COIIAU tADITI ftt tn uttoe. fbf totndonntt
GAlCRtfS DC PRODUCTION A FLANCOf COTCAUItt en ustge. Ibl tbtnoonnft
CHANTIfHS SOUTCKRAIN3 pralondnx en meuel
BATIMENTS
HALDC DE MINIRAI
f ARC A DECHETS
APPENDIX 3
Sample *
501
502
503
504
505
506
507
508
509
510
511
512
513
514
515
516
517
518
519
520
521
522
523
524
525
526
527
528
529
530
531
532
Rock Type
V6? Y9?
Y6? Y9?
M1
Ml
Ml
M1
V9
Y9
V9
V9
Y9
MKY9)
M1(V9)
MKY9)
M1(V9)
MKY9)
V10
Ml
Ml
Ml
Ml
MI(YIO)
V10
MI(YIO)
MI(VIO)
Y10
qtz-cc vein
MI(YIO)
Ml
V7
qtzvein
qtz-cc vein
Alteration
wk ser, strcc
wk sil, str ser,
strcc
strser
strser,
mod ser, modcc
str ser, modcc
wkcc
strcc
wkser.wkcc
modcc
mod ser, strcc
str ser, strcc
str ser, modcc
str ser, modcc
str ser, strcc
strser
strser
atr ser , wk cc
str ser, strcc
str ser, strcc
str ser , mod cc
Fe stained
Fe stained
Fe stained,
str ser, modcc
Fe stained, str ser
Fe stained
str ser, modcc
str ser, Fe stained
strcc
Fe stained
Mineralization
trpy
trpy
Fe stained
tr cpy,Pbs,py
trpy
none
none
trpy
trpy
none
trpy
trpy
trpy
258 py
trpy
158 py
1-2*py
Gp, 1*py
trpy
trpy
trpy
gossan
gossan
trpy
trpy
gossan
trpyTr py, tr Gp
trpy
15? py
trpy
trpy
Twp
Lebel
Lebel
Lebel
Lebel
Lebel
Lebel
Lebel
Lebel
Lebel
Lebel
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
Morrisette
MorrisetteMorrisette
Morrisette
Arnold
Au As?3v( oob
4
3
0
1
1
2
1
^
^
^
1
3
2
4
O
4
5
10
3
4
9
19
180
6
19
78
93
10
6
O
3
4
APPENDIX 4
XRAL 16-NOV-92 RAPPORT R 130 Ref. Dossier 510-RY Page 1 De 1
Numero AU PPB
1052110522105231052410525
919
180619
1052610527105281052910530
1053110532
7893106
•O
1•d
LES LABORATOIRES XRAL 150, tie RUE ROUYN-NORANDA QUEBEC J9X 2H6 TEL (819)764-9108 FAX: (819)784-4673Membre du Groupe SGS (Societe Generate de Surveillance)
[XRAL 11-SEP-92 RAPPORT R 96 Ref. Dossier 312- Page 1 De 1
Numero AU PPB
1050110502105031050410505
1050610507 1050S1050910510
1051110512105131051410515
1051610517105181051910520
43
•O11
21
1324
el
45
103
LES LABORATOIRES XRAL 150, 13e RUE ROUYN-NORANDA QUEBEC J9X 2H8 TEL (819)764-9108 FAX: (819)764-4673Memtare du Groupe SGS (Societe Generate de Surveillance)
l l l l l l l l l l l l i l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l i l l l l l l l l l l l l l l l l l l l i l l l l l l l l l l l l l l l l l l l lo o4-oCN
O O4- O)
o o4-00
o o
o o4- co
Oo4-LO
o o
o o4- ro
O o4-CN
O O4-
Oo4- o
o o4- cn
o o4-00
Oo4-
o o4CD
O O4LO
Oo
o o4 ro
O O4CN
O O4
o o4o
UJo o4
LU O O4CN
LoJ O O
ro
UJo o
LU O O4-LO
LU O O4- co
UJo o4-
LJ o o4-00
LJ O O4-
LU O O4- o
64-OON
54-OON
44-DON
3+OON
24-OON
14-OON
-Baseline
1+OOS
24-OOS
34-OOS
812
64-OON -
54-OON -
44-OON -
34-OON -
2+OON -
14-OON -
BaselineAZIMUTH 057*
14-OOS -
44-OOS
54-OOS
64-OOS
*94
.897 \ ..917
.899 \ .913
.888 N .901
3+OOS
VICTORIA LAKE
2+OOS -
5+OOS -
6+OOS -
o o(M
OO-hO CM
O O4-
o o4-00
o o
o o4- co
o o4-LO
o o
o o-t-
o o+(N
Oo4-
o o4- o
o o4-O)
o o4-00
o o4-
o o4-CD
O O4- in
o o
o o4-
o. o4-CM
oO4-
o o4- o
LU Oo4-
LU O O4-CM
LU O O4- ro
LU Oo
LU O O4-
LU o o4-CD
LU O O4-
LU o o4- cx)
LU O O4-CD
LU O O4- o
i i l i i i i i l i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i
DECLINATION 11*30'W BASELINE AZIMUTH 057*
LEGEND
INSTRUMENT: GEM SYSTEMS GSM-8PROTON MAGNETOMETER
SURVEY BY: D. FERDEBER CONTOUR INTERVAL: 100 NANO TESLAS
MAGNETIC DEPRESSION
ADD 57,000 NT TO EACH STATION
100
SCALE 1:5000
200i
METRES
400
VICTORIA LAKE PROPERTY
MAGNETIC SURVEY
MORRISETTE TOWNSHIPDISTRICT OF TIMISKAMING, ONT.LARDER LAKE MINING DIVISION
DATA BY: D.F.
DRAW BY:
APPROVED BY:
SCALE: 1:5000 METRIC
DATE: JANUARY. 1993
NTS: 32 D/4
MAP No.
i i i i i i i i i i i i i i i i i i i "i i i i i i i \ i i i i i i i i i i i i i i i i i i i i i i i i i r~in r~i i i i i i i i i i i i i i i i i i r i i i i i i i l i i i i i i i i i i i ' i i i i i i i i i i i i i i i i i i i i
o o4- oCM
O O4-cn
o o4- oo
o o4-
o o4-CD
O O4-LO
o o4-
O O4- ro
O O4-CN
O O4-
o o4- o
o o4-CT)
O O-hco
o o4-
B:o o4 co
o o4-LO
Oo
o o4- ro
o o4- CN
O O4-
o o4- o
LU O O4-
LU O O4-CM
LaJ O O4- ro
LaJ O O
LU Oo4-LO
UJo o4- co
LU Oo4-
LUo o4-00
LUo o4-O)
LUo o4-o
64-OON
54-OON
44-OON
34-OON
24-OON
14-OON
l-Baseline
14-OOS
24-OOS
34-005
BaselineAZIMUTH 057*
44-OOS
54-OOS
64-OOS
+1J3U+25 +8IJ f+16
VICTORIA LAKE
64-OON H
54-OON H
44-OON H
34-OON H
24-OON H
14-OON H
14-OOS H
24-OOS H
34-OOS H
.. 4+OOS H
54-OOS H
64-OOS H
o o4- oCN
O O4- cn
O O4- oo
o o4-
o o4-CD
O O4-
O O
o o4- ro
O O4-CN
O O4-
o o4- o
o o4-CD
O O4- co
o o4-
o ofCO
o o4-LO
Oo 4-
o o4-K)
O O O 0004-4-4-CN T- o
LU O O4-
LU O O4-CN
LU O O4- ro
LU Oo4-
LU O O4-
LU O O4-CD
LU O O4-
LU o o4- oo
LU O O4-
LU Oo4- o
.L-U4-I-. l l i l l i i l i l l i l l l i l l i l i i l i l i i i i i j i i i i i i l l l l l l l
DECLINATION 11'30'W BASELINE AZIMUTH 057*
LEGEND
INSTRUMENT: GEONICS EM-16 SURVEY BY: D. FERDEBER STATION: CUTLER, MAINE, 24.0 KHz OPERATOR FACING NORTH
PROFILE SCALE: 1cm = 50?S IN PHASE AND QUAD.
IN PHASE QUADRATURE
————--1 — — ••••i AXIS OF ANOMALY (WEAK. MODERATE, STRONG)
100
SCALE 1:5000
200
i
METRES
400
VICTORIA LAKE PROPERTY
VLF-EM SURVEYPROFILED DATA
CUTLER, MAINE, 24.0 KHz
MORRISETTE TOWNSHIPDISTRICT OF TIMISKAMING, ONT.LARDER LAKE MINING DIVISION
DATA BY: D.F.DRAWN BY:APPROVED BY:
SCALE: 1:5000 METRICDATE: JANUARY, 1993NTS: 32 D/4
MAP NO.
2
l l l l i i l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l i l l l l I l l l l l l l l l l l l l J l l l ( l l l .1 l l l ( l l l l l l l l l l l l l l l l l l l l l lo o4- o(N
O O4- cn
o O+DO
Oo4-
o o4-CD
O O4- LO
o o
o o4- ro
O O4- CM
O O4-
o o4- o
o o4-
o o4- oo
o o4-
o o4CO
o o4-LO
Oo4-
o o4- ro
o o4- CN
o o4-
o o4- o
LU O O4-
LU Oo4-CNI
LU O O4-
UJ O O
UJo o4-
LU o o4-CD
LU O O4-
LU o o4-00
LU O O4- cn
LU o o4- o
6+OON
54-OON
44-OON
34-OON
24-OON
14-OON
-Baseline
1+OOS
24-OOS
34-OOS
Baseline7 ' AZIMUTH 057'•17
'4+UDS"
54-OOS
64-OOS
VICTORIA LAKE
64-OON -
54-OON -
44-OON -
34-OON -
24-OON -
14-OON -
14-OOS -
24-OOS -
3+OOS -
44-OOS -
5+OOS -
64-OOS -
oCM. CM
O O4- oCM
O O4- cn
o o4- oo
o o4-
o o4- co
o o4-
o o4-
o o4- ro
O O4- CN
Oo 4-
o o4- o
o o4-
o o4- co
o o4-
o o4
o o4-LO
o oo o4- 4-
O O4- CN
o o4-
o o4- o
LU O O4-
LU O O4-CM
LU O O4-K)
LU O O
LU O O4- m
LUo o4- co
LUo o4-
LUo o4- oo
LUo o4-
LUo o4- o
l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l t l l l l l" l l l l l l l l l l l l l l l l l l l l l l i l l l l l l l l l l l l l l l l l l l l l l l l l l
DECLINATION 1T30*W BASELINE AZIMUTH 05T
LEGEND
INSTRUMENT: GEONICS EM-16 SURVEY BY: D. FERDEBER STATION: CUTLER, MAINE, 24.0 KHz OPERATOR FACING NORTH
CONTOUR INTERVAL = 10 UNITS
...AXIS OF ANOMALY (WEAK, MODERATE. STRONG)
100
SCALE 1:5000
200
i
METRES
400
VICTORIA LAKE PROPERTY
VLF-EM SURVEYFRASER FILTER DATA
CUTLER, MAINE, 24.0 KHz
MORRISETTE TOWNSHIPDISTRICT OF TIMISKAMING, ONT.LARDER LAKE MINING DIVISION
DATA BY: D.F.
DRAV1/N BY:
APPFtOVED BY:
SCALE: 1:5000 METRIC
DATE: JANUARY, 1993
NTS: 32 D/4-
MAP NO.
3
T l—l l l l l l I l l IIII -j—j—ri—i—i—i—i—i—n—i—i—i—i—i i i i i i i i i i i r~i'' ' ' ' i i i i i i i i i i i i i i i T~I—i—i—i—i—i—r~i i i i i i rni i i i i i i i i i i i i i i i i i i i i i i i i r~i i i i i i i i i i i r
o4- oCM
6+OON
5+OON
4+OON
3+OON
2+OON
1+OON
-Baseline
: 1+OOS
2+OOS
3+OOS
4+OOS
5+OOS
6+OOS
oCO
o o4-CD
T
O o
O O
00
O O4-
Oo00
o o4- to
^z.
Oo 4-
o o4-LO
o o4-CD
o oNt-
AU.
o o4-K)
Ak
o o4-o o
0o
o o
0o:Lcti
o ooooo oooo4- 4- 4- 4-
ooo ooo4-4-4-
o o4-
o o4-o o4-
o o4-
LU O O4-
LU o o•4-
UJo o4-
UJo o4-
LU O O4-
LJ o o4-
LU o o4-
LU O O4-
Ld O O4-
LJ Oo 4-
0o
0olo
0o0o-f-oo
0o-fr-
0o 0o0o
0o0o 0o 0o
+5
LU O O
LU O O
CM
LU O O
LU LUO . OO O
UJ
CD
LU O O
aseline AZIMUTH 057-
64-OON -
"5+OON -
4+OON -
34-OON -
24-OON -
1+OON -
LU O O
LU O O
oo CD
LU O O
O
l li t i i i i i i r i t i i i i i i i i i i i l i l ' ' i i l ' ' ' l ' ' ' ' l ' ' ' i i i i i i i i i i l i l i l i i i l i i l i i i l i i i i i i i l i i i i i i i l i i i l i i i l i i i f i i i f l l M l l l l l l l l l l l f l l
lg10
li
1+OOS -
2+oos -
-34-OOS.-
4+OOS -
5+OOS -
6+OOS -
LEGEND
Y5 BasaltY6 AndesiteY l O Agglomerate (including lapilli tuff)Ml SchistQFP Quartz feldspar porphyryB Exploration shaft
SL Pillow structureqv Quartz vein
i ^ Fault l ShearA Pyroclastic breccia
HJH Claim post^ Swamp/;/, x Outcrop: large, small^ Stripped zone
.v. Old road~* x
O Diamond drill hole collar
100
SCALE 1:5000
200
i
METRES
400
VICTORIA LAKE PROPERTY
GEOLOGY MAP
MORRISETTE TOWNSHIPDISTRICT OF TIMISKAMING, ONT.LARDER LAKE MINING DIVISION
DATA BY: D.F.
DRAWN BY:APPROVED BY:
SCALE: 1:5000 METRICDATE: JANUARY. 1993NTS: 32 D/4
.III.