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32DMNW8986 2.14997 MORRISETTE 010
G
VICTORIA LAKE PROPERTYMORRISETTE, ARNOLD, LEBEL TOWNSHIPS, ONTARIOLARDER LAKE MINING DIVISIONO.P.A.P. FILE NUMBER OP92-282
FINAL REPORT
ftPR 2 1 Graham Long, B.Sc., Geologist
TABLE Of32D84NW8986 2.14997 MORRISETTE
Summary
1.0 Introduction,,,,,,,,,,.,,..,.....,,,,,,,,,,,....,...,,,......,,,.,.,,, 1
2.0 Property Location and Access,,,,,,,,,,,,,,,,,,,,,,,,,,,, l
3.0 Land Position,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 3
40 Previous Work,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 3
5.0 Geology.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 55.1 Regional Geology,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 55.2 Property Geology.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 9
5.2. l Stripped Zone * 1,,,,,,,.,,,,,,,,,,,,,,,,,,,,,,, 145.2.2 Stripped Zone *2,,,,,,,,,,,,,,,,,,,,,,,,,.....,,.. 16
6.0 Geophysics,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 186.1 Instrumentation and Survey Procedure,,,,,,,,,,,,,, 18
6.1.1 Magnetometer,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 186.1.2 VLF EM-16,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 19
6.2 Results,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 196.2.1 Magnetometer.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 196.2.1 VLF EM-16,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 19
7.0 Conclusions and Recommendations.,,,,,,,,,,,,,,,,,,,,,, 20
References.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 22
Figure l 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*1- Detailed Geology MapFigure 7 Stripped Zone*2- Detailed Geology Map
Appendix 1 Statement of QualificationsAppendix 2 Legend- Geological SymbolsAppendix 3 Sample DescriptionsAppendix 4 Assay Sheets
010C
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 l 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 conlsted 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.
20 PROPERTY LOCATION AND ACCESS
The 43 claim property is located approximately 1 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".
1111922 ^r982340:1 982341 ' 982342 '[ill 1524111,11930 ,1111929 ,1111926 "11925
982339I 1 982338' J1111525Jl111932i|.111IJ31J1111928 j 1111927 Uf 1*924
J.l 11 " -^
y iT"~TT~fIf!i|7r11j^536|y982328 j 9823~29i l Q82334' 1982335
-r--\-r — J ——MURDOCH CREEK FAULTZONE (APPX.LOCATION)
i iMISEMA LAKE-MIST LAKE FAULT ZONE 982327 j g8233^ l 992333 ,982336
EDHARGREAVES (APPX. LOCATION) *wo*/ | *" X| |
11 igo/r 1 y.
a KIRGOOD
KENAKOTT-KIRKLAND
VICTORIA LAKE
LEBEL TWP
982326 j 98233rTi982332 ( 982337
GAUTHIER TWP
VICTORIA LAKE PROPERTY
CLAIM LOCATION MAP
meters
500 1000
Figure l
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.
3.Q LAND POSITION
The 43 unpatented mining claim property Is held In good standing and 100^ 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 emmedlately 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 (S? 1.75 gold at S35/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 11thologies(see Table 1). All of the rocks, with the exception of proterozoic Intrusives, are Archean in age and have been metamorphosed to the subgreenschlst 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).
M'/
ONTARIO\ \ QUEBEC
\RIO l V
VABITIBI
J. a- GREENSTONE
Abitibi Greenstone Belt
100 Km
20 40 60 Mi
Middle Precambrian sediments
Granitic rocks
Mafic intrusions
r- Ultramafic rocks
Early Precambrian sediments
Figure 2. Geology of the Abitibi greenstone belt (after Goodwin end Ridler 1970)
ttttttttt t.t t t.t.t t,1 t 1LAKE ABITIBI t Vi
PAMOUR DOME
vvvvvvvvV.V VVVVfVVVVV VVVVV|VVVVV
vvvlvvvvv
V V VV W V V V V VVVVVVV
v vvvvvvvv w w v w v v
V Vvvvvvvvvv
vvvvvvvv vvvvvvvvvvvvvvVV VVV WWW VVVVVVVV VVVVVVVV VVVVVVVVVVVVVVVVVVVVVVVjMvvvvvwvvvvvvvvvvvvw^ vvvvvvvvvwvvvwvv
VV V V V V V V V***ti V V V V ,V\V V V V V V
VVVVVVV VVVVVVVvvvvvvvv
vvvvvvvvV*KIRKLAND vvvvv
vv LAKEVvvvvvvv y.^VVVVVV
VtVtVt*
LEGEND
UPPER SUPERGROUP
Alkalic Volcanics(Timiskaming Group)
Calcalkahc Volcanics(Blake River Group)
Tholeiitic Volcanics(Kinoievis Group)
Komatnlic Volcanics(Stoughton Roquemaure Group and Larder Lake Group)
LOWER SUPERGROUP
Sedimentary Rocks (Porcupine Group)
Calc-alkalic t Tholeiitic Volcanics (a Skead i Catherine Group) (b Hunter Mine Group)
CZ3 Komatiitic Volcanics (Wabewawa Group)
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 RecentOlaclaltllls, 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 ROCKS Diorite, gabbro, anorthositic 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 andesltic 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 1 in bavk pocket). These units, with the exception of the felsic intrusives, are sheared and carbonitlzed 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 carbonatlzed by the Mlsema Lake-Mist Lake fault zone which is another off shoot of the
10
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 LI l +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 MB. 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
ttorhsette
ntsema Lake - Mist Lake Fault
samples 507-510, Inclusive
LEGEND
V9 Tuff (intermediate)
36 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: l: 20 000 Figure 4.
12N
502 LEBEL TOWNSHIP
LEGEND
V6 Andesite
V9 Tuff
M1 Schist (sericitized)
. 507 Sample location and number
Shear
VICTORIA LAKE
505
NOTE: all of the rocks on the island have been carbonatized
SAMPLE LOCATION MAP - ISLAND IN VICTORIA LAKE after Map No. 53a, Township of Lebel SCALE: l : 400 Figure 5.
13
deformation zones. The agglomerate unit has a strike of approximately 057*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 l 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 > l cm, 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 1n a quartz feldspar porphyry on line 8+00 E at station l +50 S. No economic results were obtained from assaying the vein material, but It 1s 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-andeslte 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 l +50 5 (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-felslc 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 serlcitized and carbonitlzed 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 ^8. 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
15
VlO.undeformed
•i. ••k'-'
pyroclasts from 2 mm- J O cm in length, long axis trending at 072* Az.
small lapilli, 2cm long, replaced by pyrite.
^WATER FILLED 6 .522
pyritized bombs10-20 cm long, 5-10 cm wide.
" ""x^^^v^/X* f WATFRFIIIFD ^ ^Jpfejfe. " FtN^X ^i^-^SirX ''"^' ,.^"" "fif;*:*:.-^
, rt — ...w. ' ' : '-*^. ..^-w^sw^"' "'-^??^c*. r ^.-.'^^W^-'r '•HSSSSWBStSS^***"
LEGEND
VI O Agglomerate
Ml Schist (sericitized)
•2? Overburden
:^ Shear
\ Fault
j— Strike and dip
* 507 Sample location and number
Op
G
Fu
qv
Graphite
Gossan
Fuchsite
Quartz vein
undeformed block, slightly rotated within shear
glacially polished
Note: all of the above rock unit has been carbonatized to some ^ extent, therefore it is not mentioned on the map.
STRIPPED ZONE * 1 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 IX. 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 serecitlzed, moderately carbonatlzed and iron stained. The unit is highly sheared at 360*Az and
contains up to l% disseminated pyrite locally.
17 N
LEGEND
Agglomerate
Basalt
Overburden
Pillow structure
Brecciated
Hyaloclastite
Sample location and number
Pomorex channel sample 0.18 oz Au/ton over 3 feet
STRIPPED ZONE *2 DETAILED GEOLOGY MAP SCALE 1:200 Figure 7.
18
60 GEOPHYSICS
6.l 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.
19
6.1.2 VIF FM-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. l 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 l +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 FM-1 fi
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.
AMax-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 l Sp., Arnold and Katrine Townships,0ntario Department of mines. Accompanied by Map No. 2061, Scale, 1 Inch to 1/2 mile.
Jensen, L.S., 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, I960, 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; r'n 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.C.1989. 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, HI., 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 prophets 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, 8p., 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: l 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
SYMCOLES UTHOLOOIQUES
KOCHCS VOiCAHlOUlS ARCHftHHlS
V A*cAti tttctrujutt mdiwmtntt*
VI *0cA*f vtktnt^uti Itluquti eu tntttmtditirtt
vi rwiru
Vt tttthtM nttctnqutt mlttmtdititt* tu mtliutt
Vf JUXHiHt
V7 ttitht :Vf AtChtt fyttlttltqitl Htdjttr/n
V* AX VIO
VI 3 Ktehtt t
KOCMfS SlDUMHIAafS ARCHlltmlS
S Mecltti ttdantnttitt tndtltraunttt
fi
M(9
fft Otftftlrtt
fOKMAIIONS Of flf ARCMlfNHlS
FI Fetmttitfl dt /#f mdtttimtntt
ffmmon at it, naiuttt
FI ffnatttx tt Itt Hr*M F4 fffmutta rf* /*r ftrtofitltt
nn cttuwttttM OutflMt 11
Atf+tt. I'M'* ttttitt tl
ft"*9ltwi dt Iff
fi Qttemm tt tulrti Itttitl t ctftoftttrt
40CM({ ilOMlHlAIHlS
HOCHIS MtlAMORfHIQUfS
Rochtl tntltmorphtqutt indtttrrmnttl
SchilltM Ml
MS Migmtmt
M? Gn*iKM8 Amp*,t,ol,lt
M3 Citmilat
M 10 Mr/nowM 1 1 Outrtiilt
Mil
HOCHfS INIKUSIVfS
AocAM mtruwtt Itlugutl mdt)ltrmn4n
IS l Q IF IE 1C l C l A
l M
IN IT t O \ P 18 IX l Z IR
Svtnnt
Sr^i'f* J ItUtptth tktltn
Srintlt tutruiqut t ItUtfilK llcllin
Grtnat
Gitmtt i ttidtptlfi ttftltn
Monjonitt quttlttqut
Monionitt
Momodioritt Qutrtiniut
ronj/if*Gitnodioritt
ftgmttilt
40/iM
Grtnopftftt
Hlitclat tl ItlMl Mrutif
Z Aoc/irs intiuttvtt mltfmtditatt mdtttrrmntt
IT Dtotat gvtrluqut
2 M MonltrJwitt
1O OioiiU
2L Lampfopn/r* inttimttitmt
Roct*t inlrunvtg mttigutl mtlttttmtnttt
3R Anoritionit
3L It/nfffoifttrft mtltgut ou HHMttrmtnt
30
4 ftochtl inlrulKftl vltrtmtl'Qvtx
tp ftudoltlt
4H45
40 Otmitt
41 - f,,t,tnat
Qouvtrntm MiniilMKM StcKivMI
wnlduOu4t*c* l Eft*'flit 41 des Rastouf c**
L^GENDE DE LA COMPILATION GEOSCIENTIFIQUE (2* *dllion, 1984)
K
JO
a
a
va
A
SYMIOLCS O'ANOMAIIES OEOCHIMIOUES ET(YMIOLEt O'ANOMALIEf MINENAIOGIOUES
DES ALLUVION*
SCDIMIHTSDIKIJIS SI AU
StO/MlHTSDCfOHDDfiAC
SOLS
tAUt SCHJJfHKAINCS
tAUXOtSIMfACI
l
SVMBCLES DES ANOMALIES (SEOPHYSIOUES
lib,mi* t*
ICVtCH fOtAKSAnOHfHOVOOUtl *v df r
UVtSOePOTfNTItl SfONTANt
lives (iicntOMAaneiiaufs ACKHNS 1*1 I
HOCHli
HIHlHAUXlOUHOS If A TTttl
fOltAOt All UVKX/HAMl /y y
Ststtmes stmi ttropofili
ifVf tLfCTROMAGNfTtQUf AfftlfN SYSTtMf INfUT Itt 2 ctfliv* Itvtc prodiMl conduction* - tpfSttur. mftott tlHictntv* tttfctntu* lttlSttntv*i*l6ttntv* ttltaa mtl* mtgntttqut (cotncnttntm Igt tnomt* mtgntoqut fUf- ttpottt
LfVfSftfCTROMAGNfTIQOfSAUSOl {ttsytttmes J ctatfs homonltut ft*et produit tortductinte rim* f ut rnfioifittisystemtftcKins vrmcnuicliwemt*
ttt tontt tit tofttt itnturt ff4oftt^fn^Qut$ toitn modt pu f snout
tCHAN nt i OHHAGf Of tt OC f ft S A TlQUf
SONQAGf At t UVKWHAtRC tt*c ptetontftuf tn mttrtl t 9tutt*l On ftwQurt qut to sonants ttuv&nnm sont
$yf tt coucht 3
i f . IfVfS MAGNfT/QutS {AXIS Df HAUTfS VAt(URS)
X y LfVf GRAVlMfTRtQUf tt) htut ytvmftnQut 1bi 6*j y9-
* f f tfVf ftADtOMfTRIQUf OUDf SfVCTQMfTfVt OfS RAY*J'/' ONSGAMMA ttturtmvmlbtthQnumlfiftftptxlurt'vum/ f * ituu~,lrtlfillnlmJi*lrtfitmtti,,*rttftonum itf l lotti it
SVMBOLES DES INTERSECTIONS ET ZONES MINERALISEES
____ tHTf*S(CTfONWH[RAttSff •r i "to "L**n**V*'4jn dv b ftXtfi^VF rrWu
ZONE MIHfRALISEfnaeti son* (s rf y rn t u
SVMIOLES DE BONDAGES
SQHDAGf VfATtCAi
* ** IP ivntfVo it'dtftntiCiliQn du *iX*J*0C **u dMSUS Oubott tt tmtovmiitft tonfrgt r**** ami 4ti O
consutits
SONDA Gf POUR Ai iMtN T A JVOrV l N t AUt cover* kibotog-Qu* nnc&wtt r ttt
r/ SOffOAGf tNCt Wf A VfC PRQJiCTIQN HORIZON TAi f ItlptotanJtur tonnut ttttptofonittuf mtonnut Sonatgt onrAfW irtrtc pt Of fi- 1 'On ttftf'nytttm at tt *
t/ * flunfo a Oew-KS LO J (*T*f4? C* t\jrnffO {J OvnttC
f J OB** Utint^ JVB ut tXio**l a* tl ne Aj^u/e su* *J CJ^'e t* ctxnow
toi fOutnauM tit son&ge tom
f vti routnti tf* twtftg* t**i* OMS 4rs okHPf a
SUFFIXES POUR US MINERAUX DCS ROCHES •VMBOLES STRUCTURAUX
1
B
P
Y
,r
t
^',.
Qrenat
hotnblende laic
COMPOSITION
le stquemelique
ORIGINE
volcanique
intrusive
l carbonate
•^ru-il* nafmnnnil*
m muscovite
n nepheline
o leldspath-poiasfique
p plagioclase
q quarli
r chloritoide
"A ifiikiti trtt t*t awn * tutlttt e* mtntiit fv* ***n* e* evarr/f
SUFFIXES POUR COMPOSITION. ORIGINE ET ALTERATION
ALTERATION
u*
O
Pn t
? 0*
SiltCiMe
pyiins4e
e'pidoiisteporphyrmsee
chloritisee
s staurotide l tremolite adinole
u amphibole Ondeierminet
v "ve me de
w tourmaline i lil li manna
1 leoliie
A aericiiisee
t) carbonalisee
* all4ration poussxiut r alteration indttermmee
( skarn^ corneenne
SUFFIXES POUR IES SUBSTANCES D'lNTERET ECONOMIQUE MINERAUX EI flOCHES
Am
*l
Ap
Alp
tt
It
It
Bo
CoCo
Ch
Cr
CICor
Ci
fu
arruanie
•nihophyiliie
•petite•rsenopyrne
ba'yttne
Miyl
bismuth
bornite
chakopyrtte
cnlnTJip.
chromne
corindon
covelline
Fuchine
Fp
FI
Gn
Go
Hem
llm
Ml
Me
Ml
M!
Md
Mo
Ol
IcUtpalhfluorine
gale ne
graphite
homilite
ilmcniie
magnate
maiachiie
marcasite
mica
miner a ui decora lil s
molybdenite
olivine
Pn penllanoMe
PC pierre de constructionPm pierre ornemeniale
Py pyritePi pyrophylliie
Po pyrrhotine
Ra minerau* redioactifs
Sh scheelite
Sd siderose
S* silica
Sp sphaerite
Sm spodumene
Su sullures (indeiermtnetl
Ta tanialtie
'
9 a *
XX/
a a t a
* a * 4
9 a * *
*///
+ /X• a t 0
ir " ^^
a a f a1//0/
S
9 tX 54
f
1t a
/Va a
/Y
jfe^
AHlCUReMfNIS lil aeU. Ibl mi i illlt^tmtni.
CONIOUKS GfOLOGlOUtS III ttnnu Ibl fobltilt luptttumi. Mdtpttx turn gtophyiiQutl lAIR SOU
SIKAIIHCAIION SOMMtl DfffHMINl III hotnonttlt. Ibl intltntt Itl nattilt. Idlptndigt nan Mtlrmint. til /tnittgtt
STKAriHCAHOH. SOMMir HOU DtltHMlNl lil htiitonlllt. Ibl intltnff. M vtrtttllt. Idlflndlgt non ttlttnvnl
SCHISTOSHt OU ClIVAGf OU IOIIAIIOH lHtnSII III hotnonlll. Ibl tntlmt. It) *triml. Idl otndtgt non ttwimmt
SCHISrOSlK OU CLIVAGt OU fOl IA IION trim Sil111 hontontll. Ibl tntltni. Itl tnrlttil W ptndtgt non
GHtlSSOSirf lil tntuentili. Ibl intlintt. Itl
DIACIASCS di nomanliltt Ibl intltnlti Itlvtrttttlts. W trlttrmt mufepfej
LINt A1ION lil horaontllt Ibl mtlintt. ttl wtitllt. W flongti mn dtltimtntt
CONtACI Of COUlfCS
SVMIOLES GEOMORPHOIOOIOUES
SIKHS GLACIAIHIS lil Mil du momimtm tonnutbl tntonnu
MOKAIHf fKONIAlf
ISKfnS III tint fittulttntnt ttnnu. Ibl intonnu
UMIllS Of IHAHSGHfSSION MARINl OU Ol SUtMCKOCHCt LACUSIKl liltonnuf IblOfttumtt
CVMBOLES DES GlTES MINEMAUX
STOCKWORK
FltOttltnttriitt rofmt It mtnvwt t
SUFFIXES POUR STRUCTURES PETROGRAPHIQUES ET TEXTURES CARACTERISTIOUES
ffi potpftyie If
Q potphytiqw
* vartoMique
9 coussineeO amygdala*Mf A sp*ni|(B" riibene'e
* citaitiee y
A/t t, vr. t, •M/WO.IWIIOT* t W* tt fvnoti'U
sptwiulrtiqu*
so***^c^Sf'eaC^k
v*l A
AAAA^
A
lurbKJiieS
brecciform*
breche iccionique
breche intrusive
breche pvfoclasiiquebreche eipiosrvebreche de couleehyacioclastique
x**i.1"
HOU Im POIMM *m p+iHt m m* *nmn t rttatttt It anil
AMASMmtKAllStltninmlmitHmnuonl
AM*SMHtlUUStlmpo*~*tnvt~*tm*i**ni*tmirttnottiHIitintl
IN&ClOUKXNTMIHCHAllSt
IHTinStCTlOHMIHtKAltStlOAHS UN tONOACf
ISOOXAOt Of MHAMOH'HISMl it utmrttl dtt j eotnirt indtqut It ttnt tritium du gnat dt
yXXnXXt t/xc a
/X if
X* ,* i , *
///ffiy/f* '
rtdtctlrutll vlHiomf *MC"tftS in louit tnttt tt* it tolt tit lnogioOt ou iHiltl tttlionlt fntttnnn
LINfAMfNt (obltnu ptr pnoto tnierpttlMionl
f l 1 S
ANllfOnMlS III fltn Ivll diwinatt Itl fiin*ni
AHllfOXMfSOfVCXSti til fill* t,,tla*f**ni Ibl
SYNfORMCS III fltn tin! Mlttminl Ibl fittumt
SrWOHMtS OtVfHSes lllelinn*td*Kmni Itl
HIS DINIRAINCMINI III Otail. Ibl luttliti lite ov tint ptonytt tt ptndtfftt
Aft DC niSStUCNJ AYfC ftONGtl
fAllieS 1OHC S Df CISAAltMlNI III tf ffttu/ntt. ItHtltHta Itvtt etopnytttutt Idl Itl tvtt ttns di dtpllttmtnl. til i*tt illutttttfli fltin tndtqvi It tilt •"••1*41 Iflthtrriigt tiff potnltf font tar It tilt ttttvn di thtringt pttlumtt
—
rVHi* tbl mt,m*w. menf/le/*"* 4*(hit*,**
SYMBOLES DES INSTALLATIONS MINlCflCB
* tB 12-
* *u e-
B a
7* aX M
*y
4 k aj ff ft a
/ j*7
X5-
" k .
0
@
rUIIS DI MINI lAVtt CMfVAlfMlHtl III *tfHfil. tbl tnclint
fUITS OIXPIORAIION ISANS CMfVALfMlHIl IIIvtilictl Ibl tncltnt
runs AIANDONNIS
IHAHCHtf
GKAVICXCS OU SAtlllntS III It lipKl,loindonnti
MINI A citi ouvfnr
GALIRHS OfXflOIAHOH A /LAW DfIADIJI III in ullfi Ibl Ibtndonntt
GALtAlfS DF FHOOUCJIONA FLANC Df Ctn utlgt. Ibl Ibtndonntt
CHANJItKS SOUrtHHAIHS ptlond** tt
tAtlMlNIS
HALOl Df MINtKAI
fAHC A OfCMtrS
r.i.0* tV
cor t AU
Off AU 1
. ***.l
APPENDIX 3
Sample*501502
503504505506507508509510511512513514515516517518519520521522523524
525526527528529530531532
Rock Type
Y67Y9?
Y67Y9?
Ml
M1
Ml
MlV9
Y9
Y9
V9
Y9
MKY9)
MKY9)M1(Y9)MKY9)M1(Y9)Y10MlM1MlMlMI(YIO)Y10MI(YIO)
MI(VIO)V10qtz-ccveinMI(YIO)MlV7qtzveinqtz-cc vein
Alterationwk ser, strccwksll.strser,strccstrserstrser,mod ser , mod ccstr ser, modccwkccstrccwk ser, wkccmodccmod ser, strccstr ser, strccstr ser, modccstr ser, modccstr ser, strccstrserstrseratr ser, wkccstr ser, strccstr ser, strccstr ser, modccFe stainedFe stainedFe stained,str ser, modccFe stained, str serFe stained
str ser , mod ccstr ser ,Fe stainedstrccFe stained
Minerali2ationtrpytrpy
Fe stainedtr cpy,Pbs,pytrpynonenonetrpytrpynonetrpytrpytrpy2*pytrpy1*pyJ-2*pyGp, ISKpytrpytrpytrpygossangossantrpy
trpygossantrpyTr py, tr OptrpyISpytrpytrpy
Twp
LebelLebel
LebelLebelLebelLebelLebelLebelLebelLebelMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisette
MorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteMorrisetteArnold
Au Assyi pph43
xl11210001324O4
5
10
3
4
9191806
197893106O34
APPENDIX 4
16-NOV-92 RAPPORT R 130 Ref. Dossier 510-RY Page 1 De 1
Numero AU PPB
1052110522105231052410525
919
180619
1052610527105281052910530
1053110532
7893106
1 O
LES UBORATOIRES XRAL 150,13e RUE ROUYN-NORANDA QUEBEC J9X 2H6 TEL (8191764-9108 FAX: (8191764-4673Membre du Groupe SGS (Soclete Centrale de Surveillance)
Nuiwro
1050110502105031050410505
1050610507105081050910510
1051110512105131051410515
1051610517105181051910520
11-SEP-92
AU PPB
RAPPORT R 96 Ref. Dossier 312- Pag* 1 D* 1
43
11
21
•d•el•e!
1324
45
1034
LES LABORATOIRES XRAL 150. 13e RUE ROUYN-NORANDA QUEBEC J9X 2H8 TEU (819)764-9108 FAX: (819)764-4673Monbre du Groupe SGS (Soclete Generate de surveillance)
Ontario32D04NW8986 2.14997 MORRlSETTE 300
Ministry of Ministere duNorthern Development DeVeloppement du Nordand Mines et des Mines
Geoscience Approvals Section Mining Lands Branch Willet Green Miller Centre 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5
Telephone: (705) 670-5853 Fax: (705) 670-5863
Our File: 2.14997 Transaction #: W9380.00046
June 14, 1993
Mining RecorderMinistry of Northern Developmentand Mines4 Government Road EastKirkland Lake, OntarioP2N 1A2
Dear Sir:
RE: APPROVAL OF ASSESSMENT WORK SUBMITTED FOR GEOPHYSICS, GEOLOGY AND PROSPECTING ON MINING CLAIMS L 1111524 IN ARNOLD, LEBEL AND MORRISETTE TOWNSHIPS.
The assessment work submitted on the above mentioned Report of Work has been approved under section 6 (5) of the Mining Act Regulations, as of June 9, 1993.
Please address any inquiries to Dale Messenger at (705) 670-5858.
Yours sincerely,
Ron C. GashinskiSenior Manager, Mining Lands Branch
:es and Minerals Division
/jl losures:
cc: i /(ssessment Files Office I/Toronto, Ontario
•ASSESSMENT FILES
JUN 2 2 1993
Resident Geologist Kirkland Lake, Ontario
Ministry ofNorthern Development
Ontario
Report of Work Conducted After Recording Claim
Mining ActPersonal Information collected on this form is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury. Ontario. P3E 6AS, telephone (70S) 670-7264.
Instruction*: - Please type or print and submit in duplicate. jfr * X Tt V w 4- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining
Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.
Work Performed (Check One Work Group Only)Work Group
JtGeotechnical Survey
Physical Work, Including Drilling
Rehabilitation
Other Authorized Work
AssaysAssignment from Reserve
Type
V^tv*. ^O^VAV ^Qx^xtrK YWji*Sifci*Sl ^MF C""\*^A\\C^!s ^^^SjAt*. ^J X^^Cfc^S*^C^ *Si ' ' vi O ^"^*S ^^ ^^1
REl " lx '-^
APR 9, 7 W*
MINING LANDS ohn; *-
Total Assessment Work Claimed on the Attached Statement of Costs o Note: The Minister may reject for assessment work credit all or part of the assessment work submitted If the recorded
holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address
(attach a schedule if necessary)
Certification of Beneficial Interest * See Note No. 1 on reverse side lRecordeO Holder or Agent (Signature)
v 'j'tV1 '
-X——l
1 certify that at the time the work was performed, the claims covered in this work report were recorded m the current holder's name or held under a beneficial interest by the current recorded holder
Date
Certification of Work Reportl l certify that i have a personal knowledge o! the facts set forth m this Work report, having performed tbe^brk or witnessed same during and/or arte'
,!S corrr'etiC- ana annexe; 'epc~. 's t".e
"- "i
For Office Use Only
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Statement of Costs - "Murdoch Creek Fault Prospect"
Summer, 1992 Program
Item - Description
A) Survey Costs (020,617.50)
- linecutting (14 miles 8 0375/mile * 7V3ST)- geological (2 geologists @ 20 field days)
s 10 days on grid, 4 on stripped reconnaisance off grid, island in peninsula, etc.
- prospecting (l prospector 6 5 field days)- geophysical (VLF, l station; NAA)- geophysical (gradient magnetic)- final report (5 days)- 32 rock sample assays- equipment rentals (boat rental: l month)- drafting fees for maps (10 hours @ 025/hour)- drafting supplies for sketches (mylar, etc.)- consumeables (flagging, sample bags, topofil
Cost
- 05617.50 . 38000
areas, 6 on Victoria Lake,
" $750 . 02000 . 02000 . 01000- 0350 " 0500- 0250
0501) ' 0100
B) Support Costs (02550)
- vehicle mil eage (1000 km in- food S accomodation (30 days
Subtotals:
Ontario total @
9 00.30/km) 075/day)
030002250
Total allowable for assessment credits:
The above cost breakdown has been derived from information supplied by the author at my request.
:.V,\'No LA-0? ^' ''33. av St-Ph.lippe. Dubuisson (Quebec, J9P 4N7 (819} 738-4082
, REFERENCESAREAS WITHDRAWN FROM DISPOSITION
M.R.O. - MINING RIGHTS ONLY
S.R.O. SURFACE RlGHTSONLY
M.+ S. - MINING AND SURFACE RIGHTS
Description Ordar No Dat* Opposition File
Section 36/90 NBff^G/79 53 ^9 SRSMR 160705
Settion 36/00 NRW 56/80 3 - l 80 M R O. 160705
SAND and GRAVEL
GRAVEL FILE 46l2d
DATE OF ISSUE
1993
LABDEH LAKE MINING RECORDER'S OFFICE
NOTES
THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON.
Surfoce rights on Mtnmy Claim L 10772 *emporarily withdrawn. File 1 43155
Mining Claims outlined thus L^^-* are subject to rights and privileges granted by Mining Court Order — April 1,1946. Fife: 19697.
NOTICE OF FORESTRY ACTIVITYTHS TOWNSHIP t AREA FALLS WITHIN THE ———
TIMISKAMING MANAGEMENT UNIT.M-mM..m. ANDlifiYYE"SUBJEcTTO"FOr^sfRY OPERATIONS. THE MNR UNIT FORESTER FOR THIS AREA CAN SE CONTACTED AT: P.O. BOX 129
SWASTKA. ONT.POK ITO 705.649-3???
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LEGEND
HIGHWAY AND ROUTE N.
OTHER ROADS
TRAILS
SURVEYED LINESTOWNSHIPS BASfc LINES ETC LOTS, WINING CLAIMS PAPOt LS
JNSURVEYED LlNtSLOT LINESPARCEL BOUNDARYMINING CLAIMS ETC
RAILWAY AND RIGHT Of WAY
UTILITY LINES NON PERENNIAL STREAM FLOODING OR FLOODING W'C^s SUBDIVISION OR COMPOSITE. PL AN
RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT
DISPOSITION OF CROWN LANDS
TYPE OF DOCUMENT SYMBOL
PATENT, SURFACE 4 MINING RIGHTS ® o' 0
SURPACt RlGHTSONl V B
. MINING RlGHTSONLY Q
LEASE.SURFACE 8. MINING RIGHTS © or B" .SURFACE RlGHTSONLY B
" , MINING RlGHTSONLY y
LICENCE OF OCCUPATION L.O.or YORDER IN COUNCIL OCRESERVATION 0
CANCELLED ®
SAND St GRAVEL ... . (*)
WOTS MINING RIGHTS IN PAHff ,S "i ' f N ' f r . PM -)B T WA. f,
1*13 VtSTfO PN ORM.lNA. "ATtN'M B- "-'t f O B l <
LANDS AC' R S O '9'0 CHAP 380 Stt 63 SuBSti '
SCALE; 1 INCH ^ 40 CHAINS
O 1000 ?OOO •ooo 6OOC aooo
o ?ooMETRES
1OOOt-K M
TOWNSHIP
MORRISETTEMN R ADMINISTRATIVE DISTRICT
KIRKLAND LAKEMINING DIVISION
LARDER LAKELAND TITLES/ REGISTRY DIVISION
TIMISKAMING
MinistryofNatural
LandManagement
BranchOntario
ltitt JANUARY 1995
CIRCULATED FEB. 26, 1990 G-3217
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; 2+OOS
3+OOS
4+OOS
5+OOS
6+OOS
VICTORIA LAKE
6+OON -
' 5+OON
4+OON -
3+OON -
2+OON -
1+OON -
^
DECLINATION 1T30'W BASELINE AZIMUTH 057'
1+OOS -
2+OOS -
3+OOS-
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
4+OOS :
5+OOS -
6+OOS -
l'. 14997
100
SCALE 1:5000
200
i
METRES
4OO
VICTORIA LAKE PROPERTY
Oo o o
32DMNW8986 2.14997 MORRISETTE 230
ooooooooooooooooooooooooooooo goooooooooooooooooooooooooooo+ I A 1 1 1 1 i ^L. -4- -1— -r- "T" "4~ ~T~ ~T~ "T" -1- —1- -4- l "T" "l l~ "l "T" "T" "T" *T-
"T" "l "T" 1^ *^ l^ "T" i^ ^^ fc^-i , ' * L,^ *rv\ t^ rr\ tr\ *H- hO r^i f~^ CD CO P*-* CD LO "^T" t1*") C\l ^ — O * — ^N ^J *^J LO CD P"- 00 0) O OQ p** CD u j ^r r j tN i — 'wj vy^ "^ i v*-' " ' ^ ' * ^ v—* * ^-^
, 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 t i i i i t i r i i i i i i i i i t i t i l l i l l l l l l l l l 1..-I 1 1 .J-l— LI ...Li 1 1 1 J.-I 1 1 1 1 .1 i 1 1 1 l. 1 1 1 1 1 1 1 1 1 1 1. J 1 1 1 1 l. 1 1 1 1 1 1 1 1 1 1
MAGNETIC SURVEY
MORRISETTE TOWNSHIP DISTRICT OF TIMISKAMING, ONT. LARDER LAKE MINING DIVISION
DATA BY: D.F.DRAWN BY:APPROVED BY:
SCALE: 1:5000 METRIC MAR MoIV 1 t\ 1 IX \J *
DATE: JANUARY. 1993 ANTS: J2 D/4 '
l l l l l l l l l l l J 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 J l l l l l l l l l I I l l l ] l l l l l l l l l l l l l l i l l
O O4- oCN
O O4-en
o o4-00
O O4-
o o4-CD
O O4-LO
Oo o o4-
O O4-CM
O O4-
o o4- o
o o4- cn
O O4-00
o o4-o o4- to
o o4-LO
o o4-o o4-
O O4- CN
O O4-
o o4- o
LJ O O4-
LJ O O4-CM
LJ O O4-
LJ O O4-
UJo o4-
Ld O O4-CD
llJOo4-
UJo o4-00
UJo oH-O)
UJo o4- o
64-OON
5+OON
44-OON
3+OON
24-OON
14-OON
-Baseline
1+OOS
2+OOS
34-OOS
44-OOS
5+OOS
64-OOS
BaselineAZIMUTH 057'
VICTORIA LAKE
6+OON -
5+OON -
4+OON -
3+OON -
2+OON -
1+OON -
DECUNA710N BASEUNE AZIMUTH 057'
14-OOS -
2+OOS -
34-OOS -
4+OOS -
54-OOS -
64-OOS
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
AXIS OF ANOMALY (WEAK. MODERATE, STRONG)
O O4- o
Oo4-O)
o o4-00
O O4-
o o4- co
Oo4-LO
Oo4-o o4-
O O4-CS
O O4-
o o4- o
o o4-O)
o o4-00
Oo 4-o o4- co
o o4-
Oo4-
o o4- ro
O O4-04
O O4-
o o4- o
LJ O O4-
LU O O4-(N
LU O O4-
LJ O O4-
LaJ O O4-LO
LJ O O4-CD
LJ O O4-
LJ o o4-00
LJ O O4- cn
l l l l l l l l i i i i i i t 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 t i i i t i i i i i l i i i l i i l i l
LJ O O4- o
l l l l l l l l
2. 14997
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
32D04NW8986 2.14997 MORRISETTE 240
l l l l l l l l l l l l lo o o
o o o
5o o o o o o o o
o o o o
H-o o
o oo o
o o o o o o
i i i i i i5o o
l l l l l l l l l l l l ( l l l l l l lo o o o o
o o o
o oLjjo o
UJo o
LjJo oUJo o
UJo o
LiJo o
IjJo oLjJo o
IjJo o
uJo o
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
BaselineAZIMUTH 057-
VICTORIA LAKE
6+OON -
5+OON -
4+OON -
3+OON -
2+OON -
1+OON -
DECLINATION 1T30'W BASELINE AZIMUTH 057*
1+OOS -
2+OOS -
3+OOS -
4+OOS
5+OOS -
6+OOS -
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)
2.14997
100
SCALE 1:5000
200
i
METRES
400
VICTORIA LAKE PROPERTY
VLF-EM SURVEYFRASER FILTER DATA
CUTLER, MAINE, 24.0 KHz
O O+ O r\i
O OH-
5 5o oO 0+ ±oo r-
5o oCD
Mil
5o o+lO
i 1 1 1
MORRISETTE TOWNSHIP555^5555555555 LULJLU LJ uj LJ uj LJ LU LJ DISTRICT OF TIMISKAMING, ONT.000 o OOOOOOOOOOOOOOOOOOOOO I ARDFR l AKF MINING DIVISION OOOOOOOOOOOOOOOOOOOOOOOOQ LMIAUI^n, LMPsIL IVlMNIIN'o UIVIOIUIN
+ + + -I- + + + + + + + + + + + + + + + + + + + + +^ (^ ^! ^Z ^ ' " O - ^_ DATA BY. DF SCALE: 1:5000 METRIC |^^p ^Oi
DRAWN BY: DATE: JANUARY, 1993 -7
1 , , , , | | | | | | | | | | | | | | | | | | | l l l l l l l l l l 1 1 1 1 | 1 | 1 | 1 1 1 1 1 1 1 1 1 1 1 1 | 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 t 1 1 1 1 1 1 t 1 1 1 1 1..I 1 1 1 IJ—l 1 L 1 J 1 1 -1 1 1 APPROVED BY: NTS: Z2 D/4 ^
32D04NWB986 2.14997 MORRISETTE S50
: : i J i i i i i i i i i i i i i^ ^5 50 O O Oo o o oo CD oo r^CM T- T- T-
1 1 1 15:ooCD
III)^oo4-LO
1 1 1 1 1^oo4-
1 i 1 1^oo4- ro
1 1 1 1 1 1 1 1 1 1 1 1 1 1 1^ 15 5 50 o 0 00 o 0 04- + 4- 4-C\I ^- O O)
1 i 1 J 1 1 1
^ B:O Oo o4- 4- oo r^
i i i i i i i5: 5:0 00 04- 4-CD LO
1 1 1 1 15:Oo4-
l i i5:OoK)
1 1 13:oo4-CM
l 1 1 1
^OOHh
i \ \- i i i iLJ
O OO 0+ 4-o *-
1 1 1 1LJOo•4-CM
1 1 1 1 1 1 1 1 1 1 1 1LJ UJ LJO O OO O O4-4-4-K) ^ LO
1 1 1LJOO4- to
i i i iUJoo4-h-
i i i i iLJOO4- oo
1 1 1UJOO4-O)
1 1LJOO4- o
^(M \
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
BaselineIMUTH 057"
VICTORIA LAKE
6+OON -
5+OON -
4+OON -
3+OON -
\
2+OON
1+OON
:
1+OOS -
2+OOS -
3+OOS -
4+OOS -
5+OOS -
6+OOS -
V5
V6
V10
Ml
QFP
B
SL
qvS
A
o
LEGEND
BasaltAndesiteAgglomerate (including lapilli tuff)
SchistQuartz feldspar porphyryExploration shaft
Pillow structure Quartz vein Fault l Shear Pyroclastic breccia
Claim post
SwampOutcrop: large, smallStripped zoneOld roadDiamond drill hole collar
100
T jT O".h
SCALE 1:5000
200
i
METRES
400
VICTORIA LAKE PROPERTY
^^5^^^5^^^^55^5^5^5^ UJL^UJLJLJLJUJljJUJLjjo oo o o o o o o r) o o o o o o o o o o o. o o o o. o o o o. o oOoOOOOOOO o O O O O OO OO O o O O O O OO O -O O O - o+ I 1 1 1 1 1 1 1 ^~"^ t 1 t 1 1 1 1 1 1 1 1 1 J 1^ 1 1 1 1 1 1 , -i- —L -L -J- -i- -4- -L -L i J. -j- -J- -J- -J— -f- —J- -J- -p ^- -4- -i- "p -p —p -p —p -p —p -j— -J-
.O.Q^ 00. 1^ CD LO ^t- rO . CN - -r- O. CD CO h- CD LO.NJ-.K) CM^- o t- CM rO.^.LO CD. r^ CO O) O
1 1 1 l l l 1 f 1 1 [ 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 t 1 1 1 1 1 t 1 1 1 t 1 1 1 1 1 1 1 t 1 1 1 M 1 1 1 1 1 1 1 1 1 1 1 ! 1 1 1 1 1 1 1 ! 1 1 ( 1 1 1 1 1 1 1 1 1 I.. 1 .1 l 1 1 1 l I 1 f 1 1 1 f t l 1 1 1 1 1 1 1 1 1 1 1 1 1 f 1 1
GEOLOGY MAP
MORRISETTE TOWNSHIP DISTRICT OF TIMISKAMING, ONT. LARDER LAKE MINING DIVISION
DATA BY: G-LDRAWN BY: G.L.APPROVED BY:
SCALE: 1:5000 METRICDATE: JANUARY, 1993 MAP No.NTS: 32 D/4- A
32D04NW8986 2.14997 MORRISETTE260