summ rpt diamond study geol mag em bulk tests …...1174509 (3 claims) mcmurray township 1174480 (4...
TRANSCRIPT
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42CC2SE0004 2 16363 LAST HEELS 010
fir s n
. 163 63
SUMMARY REPORT
Firesand Carbonatite Diamondiferous Study
Geological. Magnetics. Electromagnetics. Backhoe Bulk Testing
Lastheels A McMurrav Townships. Northern Ontario
by
Frederick T. Archibald, B.Sc. Geologist Novembers, 1995
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42C02SE0004 2 16363 LAST HEELS 01OC
INDEX
Summary 1
Property A Location 3
Property Access 3
Topography 3
Location Plan of Claim Group (1'^1200m) 4 PLATE A
History 5
Chart 1- Gold Producers in Close Proximity to Property
Diamond Source Structural A Emplacement 8
Firesand Carbonatite Complex
Table of Lithological Units
Property Claim Description
Regional Geology
Geological 81. Structural Plan
Local Geology
Property Geology
Geological Plan
Economic Geology
Specifics of VLF Electromagnetic Survey
Results of VLF Electromagnetic Survey
Specifics of Proton Magnetometer Survey 25
Results of Proton Magnetometer Survey 26
9
10
11
12
14 PLATE C
15
17
20 PLATE K
21
22
24
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Backhoe Pits and Washing Plant 28
Backhoe Location Plan 29 PLATE B
Results of Bulk Sample Concentrate Analyses 30
Conclusions 81 Recommendations 34
References 36
Cost Estimate 37
Certificate 38
Sampling Program Map A Stats- 1174419 39
Microscopic Examination Results 40
Gold Analyses 43
Daily Journal of Work 44
Claim Breakdown of Work 45
Breakdown of Costs 46
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APPENDICES
Regional Structural Geology Plan Plate C
Local Geological Plan Plate E
Local Airborne Anomaly Plan Plate F
Proton Magnetics (1" to 100 meters) Plate G
VLF Electromagnetics- Dip Angles (1" to 100 meters) Plate H
VLF Electromagnetics- Field Strength (1" to 100 meters) Plate J
Photographs
Program receipts
Claim Abstracts
Claim Extensions
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Firesand Carbonatite Diamondiferous Study McMurrav-Lastheels Townships. Northern Ontario
Introduction-
During the months of August and October of 1995, F.T. Archibald Consulting
Ltd. was contracted by Elliot Feder to perform work over a group of claims in the
northeastern part of McMurray Township and the northwestern part of Lastheels
Township in order to delineate potential for diamondiferous sources. The work was
performed over a group of eleven claim groups totalling some 59 claim units. A total of
S31.856.14 was spent on the claim groups.
The author has many years experience both in exploration for diamonds and in
production mining of diamonds.in Africa (Liberia), South America (Surinam and
Venezuela), and Canada (Labrador). F.T. Archibald performed a B.Sc. Thesis at
Carleton University in 1977-1978, evaluating the heavy mineral suite associated with
diamondiferous bearing kimberlites and related materials.
In the summer of 1991, diamonds were discovered in the southwest corner of
McMurray Township, and consequencial studies by Tom Morris of the Ontario
Geological Survey have confirmed that indicator minerals in the area indicate
diamondiferous sources in the area are possible.
Areas chosen for concentration of prospecting for kimberlites (diamondiferous
host rocks) were on the basis of: 1) locations in the direction of glacial flow (up-ice)
from the original find, 2) closeness of proximity to deep seated fault systems 3)
closeness to ultramafic rock swarms (including peridotites and carbonatites). The area
in which the surveys were performed satisfies all of the above criteria.
The area was geologically mapped in addition to compilation studies of
airborne electromagnetics and magnetics. Some twenty-three kilometers of VLF
electromagnetics and twenty-three kilometers of proton magnetics were carried out
over the property. Several gold showings lying within the claim area were trenched
and sampled. A series of thirteen backhoe pits were dug in selected areas; in close
proximity to major deep-seatefd faults, at the junctions between faults, and in areas of
circular magnetic (ground and airborne) features. These samples were trucked to a
portable-mobile washing plant and concentrated by sluicing methods to a concentrate
which was sent to a laboratory for heavy mineral separation and identification.
During the sluice- plant concentration process, gold flakes were observed in at
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least six of the pits. One of these pits (Bulk #5), located at the northeast contact of the
Firesand Carbonatite Complex and the junction of the Firesand Creek Fault, indicated
higher than normal amounts of gold flakes and a possible source area for gold.
The proton magnetometer survey delineated a 400 meter circular conductor at
the edge of the Firesand Carbonatite Complex. This is significant and should be
further investigated by sampling and/or drilling.
On December 11th, 1995, the Ministry of Northern Development and Mines
(MNDM) announced the discovery of at least four or five parallel kimberlite dykes in
the Lagarde Hill area of McMurray-Lendrum Townships. These narrow dykes, flat and
steeply dipping, trend in a northeasterly direction and cut through the north part of
Ward Lake and through the north part of the claim group. These trends match up with a
major northeasterly trending fault which cuts the property. As well, this strike lines up
with the Firesand Carbonatite Complex. The fact that kimberlites have been
discovered in this area along with diamonds in the surficial gravels has indicated that
this area has potential for diamondiferous kimberlite pipes.
The original diamond discoveries and heavy-mineral tracings to date have
indicated that the diamonds are traceable upstream of Wawa Creek- Ward Lake which
also indicates that the property has significance as far as potential to find diamond-
bearing kimberlites in this area.
Although it is not known as yet whether the newly discovered kimberlite dykes
are diamoniferous, it is thought that these dykes could be secondary feeders from one
or more kimberlite pipes along a defined fault trend. Two promising targets could be
the Green-Emerald Lake anomaly or another circular airborne anomaly over claim
1174477.
Airborne magnetics show at least ten anomalous targets (four negative and six
positive) underlying the claim group. Another nine airborne targets are within six
hundred meters of the claim boundary. At least ten of the ninteen anomalies coincide
with fault structures; areas where it is expected to find kimberlite pipe structures.
Only six of the airborne targets have been prospected, and the rest are potential
areas which should be investigated by prospecting and bulk sampling. Significant
gold analyses in the pit operations should also be prospected.
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Property SL Location-
The property is located within McMurray Township (northeast corner) and
Lastheels Township (northwest corner). The survey was performed over a contiguous
group of ten claim blocks totalling some 55 units. These claims consist of unpatented
mining claims which need in excess of 322,000.00 assessment work performed
before November 5, 1995 through January 14, 1996 for another years extension of
time. Most of this group has extensions of three months to apply the work.
The claims are located in the Wawa area of the Sault Ste. Marie Mining District
of Northern Ontario. The claims are located on the Michipicoten Harbour (1:50,000 )
NTS41N-15 sheet.
The claim group consists of a contiguous to semi-contiguous group of claims
described as follows:
1174419 (2 claims) McMurray Township
1174416 (8 claims) McMurray Township
1174421 (4 claims) McMurray Township
1110143 (4 claims) Lastheels Township
1110144 (1 claim) Lastheels Township
1174510 (5 claims) Lastheels Township
1201471 (12 claims) Lastheels Township
1201472 (12 claims) Lastheels Township
1201473 (4 claims) Lastheels Township
1174509 (3 claims) McMurray Township
1174480 (4 claims) McMurray Township
TOTAL- 59 claims (323,600 expenditures needed to extend to Nov.5,1996 to
January 14, 1997)
Additonal claim groups are also recommended to be kept as they are in line of
strike with the new kimberlite dyke discovery. These claims have been picked up on
speculation at a cost of S2500. These consist of thirteen units and are numbered as
follows:
1174413 (3 claim) restaked number
1174420 (1 claim) restaked number
1174477 (8 claims) restaked number
1174412 (1 claims) restaked number
March 8, 1996
March 8, 1996
March 8, 1996
March 8, 1996
March 8, 1995
March 8, 1995
January 14, 1996
January 14, 1996
January 14, 1996
March 8, 1996
February 9. 1995
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PLATE A
f- CHABANNEL TOWNSHIP ESQUEGA TOWNSHIP
MCMURRAY TOWNSHIPLASTHEELS TOWNSHIP
SURVEY GRID
LOCATION PLAN
SURVEY GRID 8 CLAIMSSCALE
. ... _=H-_ . ^ O 400 aOO 1200 1600
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The following are in good standing until March , 1996 but should be kept in
good standing due to the close proximity and significant location. A total of approximately 32400.00 is needed to keep these claims in good standing until March
3 to 21, 1997. These claims are as follows:1174530 (2 claims) McMurray Township March 3, 1996
1174531 (2 claims) Chabanel Township March 21, 1996
1174532 (2 claims) Chabanel Township March 3, 1996
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Property Access-
The claim group is located some 229 kilometers northwest of Sault Ste. Marie,
Ontario.
The property can be accessed by several routes. The first is by Highway #101
east from Wawa for some 6 kilometers to the Firesand Creek Timber Access Road. The
property is located some three to four kilometers south along this gravel road to the
northern boundary. Lines 6 South to 5 North and Lines 16 South to 18 South bissect
this road. The road is presently being used year-round by a timbering operation to the
west of the claim group.
The other access is by way of the High Falls Road, south of Wawa for some five
kilometers along Highway #17, and then by gravel road to either the Surluga Road or
to another road 500 meters before the townsite of High Falls, where the Leroy Lake
trail can be accessed by ATV or skidoo vehicles to the southern portion of the property.
This trail joins up to the Firesand Timber Access Road.
Local Resources-
Power is available from power lines some five kilometers southeast of the
property. Good access is available from all-year roads; from Highway #101 some three
to four kilometers to the north and the High Falls Road some five kilometers to the
south. Water is available from Firesand Creek which bissects the central section of the
group in a southwesterly direction. Manpower is readily available from Wawa which
has an experienced labour force from at least five gold mines which have closed down
within the past few years.
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Topography-
The central portions of the property are generally flat and coveredby glacial till
overburden. The northwestern and southwestern sections are covered with slightly
undulating relief and minimal overburden. The eastern sections of the property have
high relief with steep ridges averaging ten to twenty-five meters in height.
Most of the central and western sections of the property have recently been
timbered (within the past fifteen years). The areas on top of the cliffs (east of the
Firesand Creek) on the eastern portions have not been timbered for many years due to
access problems.
Tree cover in the lower flat lying areas consist of spruce ranging from 4 to 12
inches in diameter. In the higher areas the tree coverage consists of mainly birch and
spruce ranging from 8 inches to 24 inches in diameter. Tree cover is sparse and
spread out; and it appears that the pine have been timbered-out. Over 1174510, there
has been a recent planting of jackpine which have been inadvertently been burned-
over and replanted with black spruce (1993).
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History-
It has been reported that a gold-bearing vein averaging 31.0 ounces per ton
was discovered on the north boundary of the Booth claims 3292 and 3293 in the
1920's. This showing strikes onto claim 1174419.
In 1936, J.H.Teare discovered 3 gold-bearing veins associated with northwest
trending iron formation, on the east side of Leroy Lake. One vein, some 457 meters in
length, assayed between 0.264 and 0.334 ounces Au per ton. Another assayed 0.197
ounces Au per ton. These veins are in line of strike with the southwest section of
1174416.
In 1961. Algoma Steel Corporation Limited summarized results of a low-grade
niobium mineralization within the Firesand Carbonatite Complex.
In 1962, the Algoma Central Railway completed an airborne magnetometer and
electromagnetic survey over the area.
In 1972, Algoma Steel Corporation drilled the outer rim of the Firesand
Carbonatite Complex to delineate calcite content for use in the sinter plant in Wawa
without success. At least three to four holes were drilled under claims 1110143 and
1110144. Between 1951 and 1972, some 4433 meters was drilled over the
carbonatite complex in some 39 drill holes.
In 1975, the Ontario Department of Mines under RT. Rupert completed a
geological mapping over the area.
Also in 1975, Kenting Earth Sciences finished an airborne survey over the area.
In 1976, International Minerals and Chemical Corp. drilled some 114 meters in
three holes to delineate the potential for apatite mineralization within the carbonatite
complex.
In 1979, AMAX Minerals Exp. explored gold showings in the area, and
discovered the Valenti showing of north-south iron formation with gold values. This
showing is in line of strike with claim 1174416 and is some 3.5 kilometers south of the
claim group.
In 1981 and 1982, R.P.Sage of the Ontario Department of Mines mapped the'
areas of McMurray and Lastheels Townships.
In 1983, R.D. Henderson completed manual stripping and trenching, and
geological surveys over the southeast portion of the property.
In 1986, Caviar Resources Limited worked on the Reed Lake claims to the
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southwest side of the property, uncovering values as high as 0.49 ounces Au per ton
from felsic metavolcanics paralleling a gabbro-diabase dyke. At the same showing
some three tons of ore was milled in 1909 (Sears, S.M., 1986). In 1987, Citadel
Gold Mines performed a geological reconnaissance of the west portion of the claim
group.In 1988, P.P. Sage of the Ontario Geological Survey ( MNDM ) studied and
reported on the Firesand River Carbonatite Complex.In 1991, G.C. Clement Jr. collected samples from the Dead Creek area of the
Michipicoten River and the Wawa Creek area on the southwest side of McMurray
Township. Of some sixty possible diamonds, two of them approximately 1.13 and 1.05
carats were confirmed as diamonds by the Royal Ontario Museum. One of these was
considered 1/2 of an octahedron, and was probably cracked in half during transport.
In the fall of 1993, Tom Morris of the Ontario Geological Survey, bulk sampled
the Dead Creek and Wawa Creek areas, and confirmed that chrome pyrope garnets
(G 10) and diopside minerals were present. In the summer of 1994, Morris confirmed
that diamond indicator minerals were widerspread and in the areas northeast and east
of the original discovery; indicating that the original discovery was not just glaciated
material but in fact from the Wawa area.
In the fall of 1995, Currie Rose Resources discovered four kimberlite dykes on
Lagarde Hill; along the boundary of McMurray and Lendrum Townships. These
became visible due to a washout caused by a busted beaver dam along Coleman
Creek.
In the same time, MNDM located another kimberlite dyke to the west of the
Curry Rose Resources discovery, called the Nichols Dyke, which is in line of strike with
the initial discovery and is possibly part of the same system. This dyke has been
diagnosed as harzburgite xenolith ultramafic type.
These discoveries initiated a staking rush over these townships and townships
in line of strike with the kimberlite dykes.
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Chart 1
Gold Producers Located in Close Proximitv to Feder Property
Name Rock Type Years Mined Tons Mined Oz. Au Mined
Golden Reed granite (mafic volc.cont) 1907-1908
Cooper Mine mafic volc.(porph.cont)
Grace-Darwin mafric volc(granite dyke) 1902-1937
Parkhill mafic volcanics
Minto sheared granite-diorite
S.B.Smith tuff(porph.cont)
Hillside tuff-basalt(porph.cont)
Deep Lake mafic vole.
Stanley mafic volc.(granite cont)
Surluga mafic-porphyry cont.
(148,245 tons @ 0.30 Au per toi
Jubilee sheared granodiorite
Mariposa mafic volc.(granite dyke) Van Sickle granodior(S tuff)
Citadel sheared granodiorite
1907-1908
1898-1939
1902-1937
1929-1938
1929-1942
1935-1936
1934-1935
1936-1938
1936
1968-1989
remaining)
1929-1930
1904
1936
i ORO. -man
3.0
4.889
45,528
125,778
184,600
9,228
200
2,790
1,963
90,155
2,462
9.0
9,228
6.0
1.303
17,586
54,301
37,678
1,536
224
1,633
84
8,019
421.8
16.9
1,712
e; nnn
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Diamond Source Structure and Emplacement-
Diamonds are located within kimberlite host rocks and possible lamproite sources. Ultramafic rocks such as peridotites and eclog'rtes fit similar descriptions as
kimberi'ites.Diamonds are found in garnet-bearing harzgurgite and lherzolite peridotitic
rock (Gurney, 1989). Although orthopyroxene rich pyroxenrtes and dunrtes are
possible ultramafic source rocks which could contain diamonds; with minus 40*fc and plus nint/fc olivine contents respectively.
Diamonds are thought to have formed before the emplacement of the kimberlite bodies, and during rapid magma transit to the surface xenoliths of wallrock containing the diamonds are picked up and transported.
It is thought that diamonds are formed at depths between 150 to 200 kilometers (peridotitic) and depths greater than 300 kilometers (eclogite) (Gurney, 1989). tt is also thought that during tectonic plate collision, carbon (calcitic limestone) or carbonate- bearing rocks rifted under the upper plates and gave rise to diamond- formation within the Upper Mantle. This is why Carbonatite complexes are important in exploration for diamonds. Many of the diamond-bearing pipes in the world are located in close proximity to Carbonatite complexes; which are associated with deep-seated fault structures.
Kimberlite occurs as cone- pipe structures (Kimberly Mine in South Africa), sill structures (Lesotho Mines), and as dyke structures (Sierra Leone). These rocks consist of forty to ninty percent olivine rich ultramafics with heavy mineral suites consiting of pyrope garnet, ilmenite, spinel, corundum, zircon, rutile, and chromite. Lamproites occur with the same mineralogy but occur as flat-lying bodies rather than "cone" shaped bodies.
Most kimberlite pipes range in size from 5 to 30 hectares and occur in clusters ranging from 6 to 40 pipes in one area (Gurney, 1991). Most pipes are oval shaped and are associated with deep-seated fault structures. Less than 5*^ of kimberiites are diamondiferous; and less than SW* of the diamondiferous pipes are of gem quality ' (Chris Jennings . 1994).
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Firesand Carbonatite Complex-
The survey has been based around the Firesand Carbonatite Complex due to
the fact that carbonatite complexes; especially calcitic bearing units, are important
structures which have been found to be located in close proximity to kimberlite
complexes. Studies of the airborne magnetics and electromagnetics indicate that the
Firesand Carbonatite Complex underlies portions of claims 1174509, 1174510, and
1110143.
The Firesand Carbonatite Complex lies within the Michipicoten Greenstone Belt
of the Wawa Subprovince and immediately north of the Kapuskasing Subprovince of
the Canadian Shield. This complex is controlled by a series of deep-seated faults
within the Kapuskasing Subprovince; namely the Wawa-Kapuskasing Fault to the
north and the Firesand Creek Fault to the east. These two faults are the most deep-
seated faults in the area, and are bissected by a series of ultramafic complexes
(peridotites and pyroxenites) in the area; and can therefore be host for other deep-
seated complexes such as kimberlites or lamproites.
The carbonatite is elongate in a northeasterly direction and is cut-off on the east
side by the Firesand Creek Fault. It has an outer rim of silicocarbonatite (calcitic) with
an inner core of dolomitic carbonatite (Parsons, 1961).
The Firesand Carbonatite is dated at 1008 to 1087 Ma for the complex (Gittins
et al, 1967).
There is a fenetic halo around the complex as indicated by the airborne
magnetics and the actual contact area of the complex. There is also a radiating pattern
of carbonatite and lamprophyre dykes around it.
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Table of Lithologic Units
Cenozoic
Recent- stream till
Pleistocene- glacial till
unconformity
Late Precambrian (Proterozoic)
Firesand Carbonatite- dolomitic core rocks
gradational contact
Firesand Carbonatite- silicocarbonatite rim rocks
intrusive contact
Diabase Dykes
Early Precambrian (Archean)
Felsic Intrusives- feldspar porphyry b quartz-feldspar porphyry
intrusive contact
Intermediate Metavolcanics- tuff flows
Mafic Metavolcanics- basalt flows
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Property Claim Description-
The claim group on which the survey was done is located within the northwest
part od Lastheels Township and the northeast part of McMurray Township. The claim
numbers, (together with number of units and anniversary dates) are as follows:
Lastheels Township
1110143 (4 units, March 8, 1996)
1110144 (1 unit, March 8, 1996)
1174480 (4 units, February 9, 1996)
1174509 (3 units, March 8, 1996)
1174510 (5 units, March 8, 1996)
1201471 (12 units, January 14, 1996)
1201472 (12 units, January 14, 1996)
1201473 (4 units, January 14, 1996)
McMurray Township-
1174416 (8 units, March 8, 1996)
1174419 (2 units, March 8, 1996)
These claims are contiguous as shown by the claims maps, and are unpatented
mining claims. The claims surround the southern and eastern portions of the Firesand
Carbonatite Complex, and parts of the complex underlie claims 1110143 and
1174509.
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Regional Geology-
The region was last mapped in 1981 and 1982 by P.P. Sage of the Ontario
Department of Mines (Preliminary Map # 2439 and 2441). Traverses in the area were
done at approximately 1/2 mile intervals but in some cases 1/4 mile intervals.
The area is underlain by felsic metavolcanics (mainly lapilli tuffs) and mafic
metavolcanics (andesites & basalts) which are located within the southern limb of the
Michipicoten Greenstone Belt. This belt occurs within the Wawa Subprovince of the
Superior Province of the Canadian Shield. There are four metavolcanic and
metasediment rock types recognised within the Michipicoten Greenstone Belt (R.P.
Sage, 1994). The belt is comprised of several sequences of Archean felsic to mafic
metavolcanics with interbedded clastic metasediments and chemical metasediments
(iron formation). The mafic and felsic metavolcanic units are of Archean age. These
units have been intruded by numerous stocks of granitic rocks and mafic to ultramafic
rocks. Northwesterly trending diabase cut all of the other units.
The Kapuskasing Structural Zone lies between Lake Superior to the Hudson
Bay Lowlands. The two major deep-seated faults are the northeasterly trending
Firesand Creek Fault and the Wawa Lake Fault -Kapuskasing Fault trending in an
east-west direction. The Wawa Lake Fault consists of fractured crustal material that
may host kimberlitic rock formations (T.Morris, 1994). The Firesand Creek Fault is
offset and hosts several peridotite, carbonatite, and ultramafic complexes. Proterozoic
lamprophyre dykes formed from alkalic magma emplacement extending from the
Wawa Lake Fault-Kapuskasing Fault (P.P. Sage, 1994). It is along these zones that
there have been several recent diamond discoveries; such as the high-grade pipe at
Attawatiskap. The Firesand Creek Fault lies at the contact between the overlying felsic volcanics, and the underlying mafic volcanics.
Structural faults and rocks with strong or negative magnetic responses were
plotted using 1981 vintage airborne and airphotos in combination (OGS series
810006-810034; 1:20,000). In 1994 and 1995 field reconnaissance of the surrounding
area using this datauncovered several plutons of peridotite, pyroxenite, and gabbro1.
The peridotite and carbonatite structures are favoured for diamond emplacement; and
most of these units are associated with the two major fault systems as mentioned
above.
Most of the overburden coverage was deposited by Late Wisconsinian
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glaciation with an ice direction at 165 degrees to 263 degrees (T.Morris, 1994).
Diamond discoveries have been located in the southwest corner of McMurray
Township and 1993 to 1994 studies by T. Morris of the MNDM-ODM have indicated
heavy mineral dispersment (diamondiferous assemblage) increasing up-ice in the
direction of Deep Lake and also in the Michipicoten River system draining from the
Firesand complex. The property lies within this area of dispersion. Also it is believed
that Monopros did a complex study of both the Coleman Creek area and the Dog Lake
area during 1993 and 1994; both areas drain from the Firesand complex and the
Wawa Lake-Kapuskasing complex respectively.
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PLATE Q
Eaquagg Twsp.Lostheals " Twsp.
FELSIC NTRWS(VE ROCKS -
MAFIC METAVOLCAIfcCS - bcwtt
FELSIC METAVOLCAMCS - tuff
CLASTIC METASEDJMENTS
CHEMICAL METASEDMENTS ULTRAMAFIC NTRUSIVE
FELSIC NTRUSJVE - porphyry
CAR80NATTTE
MAFIC ttfTKUSJVE - (floba**
contact
fault / shear
^.-v vvx-vfc
GEOLOGICAL PLAN 8
STRUCTURAL GEOLOGY
^ \ ^ ~ ^ N ̂ \2 -•** \ \ \ \ \ ^^J \
i- N*V4 \ .Vv^ \
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Local Geology-
In 1980 and 1981, R.P. Sage of the OGS mapped the area lithologies
surrounding the immediate vicinity of the property. In 1988 Sage studied and reported
on the Firesand Carbonatite Complex which covers the property in-part.
A general reconnaissance was done over the surrounding area; especially
around the Firesand Creek Fault and the Wawa-Kapuskasing Fault. The general trend
of the area is in a northeast-southwest direction; although in the southern sections of
McMurray Township north-south to southeasterly is the preferred direction. The area is
generally underlain by mafic metavolcanic rocks (pillowed basalts), felsic
metavolcanics (tuffs), and felsic intrusives (granite and porphyry). There are also
several areas of ultramafic intrusives consisting of gabbro, pyroxenite, and peridotite;
most of which are located along the Firesand Fault or in swarms around the
carbonatite complex.. The Firesand Carbonatite, some 2.5 kilometers X 5.0 kilometers
in diameter, is located close to the convergance of the Firesand Fault (west side) and
the Kapuskasing Fault (south side).
The central portions of the survey grid are covered by Recent and Pleistocene
glacial sand and gravel to a thickness of over thirty meters in sections. Sampling of this
material by backhoe indicated rounded cobbles (5 to 20 centimeters in diameter)
generally consisting of granitic rock, mafic volcanics, felsic volcanics, and carbonatite.
In areas where bedrock was encountered, a clay layer (light brown to light grey) was
observed for a few meters, mixed with coarse boulders, lying immediately above the
bedrock.
The ODM preliminary maps show the local geological trend to be in a
northeasterly direction when in fact the geological trend underlying the claim group is
north -south. To the north and northeast of the claim group the prominant direction is
northeasterly, and to the south and southwest of the property the prominent direction is
southeasterly. There appears to be a transition of directional trend in the central
section of the property; possibly affected by the carboantite complex which is one of
the oldest units in the area (R.P. Sage, 1988).
Geological reconnaissance of the areas surrounding the survey grid have
shown several airborne magnetic circular structures (highs and lows). Many of these
have not previously been mapped or have been incorrectly mapped. There are
several gabbro intrusive swarms located between Deep Lake to Leroy Lake (along the
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south side of Reed Lake); some of which include ultramafic fragmental complexes. A
pyroxenite complex is located on the east side of the claim block, and two peridotite
bodies are located to the northeast of the claim group. Stidies of the airborne
geophysics and air-photos indicate that the peridotite complexes are controlled by
both the Firesand Creek Fault and the Kapuskasing-Wawa Lake Fault. There is
another circular structure underlying the Twin Lakes (northeast side of the Firesand
Carbonatite within Lastheels Township) which is a primary target for diamond
exploration.
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Property Geology-
A detailed geological mapping of claims: 1174510, 1201471, 1201472,
1110143, 1110144, and 1174416 was undertaken. A grid consisting of some twenty-
three kilometers with lines spaced at one-hundred meters apart. The base line
consists of approximately three kilometers in length going through the central portions
of the claims ina northeast direction which is parallel to the regional geological trend
for the area.
The central part of the group is covered by thick glacial overburden material.
Processing and concentrating this overburden in the north sections of the claim group
(1174510 and 1201471) uncovered gold concentrations within the gravels. One pit
inparticular gavre rise to approximately 24 specks of gold per cubic yard in the upper
materials which is significant.
Most of the property, especially the eastern portions and southwestern portions,
have intercalated horizons of mafic and felsic metavolcanic flow units. Close to the
Firesand Fault there are coarse-grained flow units; some of which are possibly
ultramafic gabbro intrusive units. At least six diabase dyke units cut these other units in
a northwesterly direction.
In the northeasterly section of the claim group is a unit of pyroxenite (ultramafic
intrusive) complex which appears to be fault controlled. It occurs within claim 1201471.
In the southwest corner of claim 1174510 and the western portions of 1110143
are the northeast and southeast contacts respectively of the Firesand Carbonatite
Complex. These portions of the carbonatite are silicocarbonate rich. Most of the
carbonatite is overlain by glacial till however prospecting of the outer boundaries
uncovered bedrock in-place.
The primary Fault structure is the Firesand Creek Fault which cuts the main
portion of the claim group in a northeasterly direction. There are at least two other
major faults splaying off the Firesand Fault. At the eastern end of Line 4+00 South, the
Firesand Fault splays and also appers to cut at several angles. This area is of primary
interest for any deep-seated intrusions. Another area of primary interest is at a point
(between claims 1174510 and 1174509) where the Firesand Carbonatite Complex
adjoins up to the Firesand Creek Fault. This is also an area to observe for deep seated
intrusions. Preliminary maps show the Firesand Carbonatite crossing thre Firesand
-
Creek Fault but studies and ground geology show that it in fact adbuts up to the
contact with the fault and is probably also controlled by a fault splaying from the
Firesand Creek Fault to the south. Several ultramafic complexes in the area sucgh as
the pyroxenite immediately to the east of the carbonatite complex, and ultramafic
swarms south of the carbonatite complex indicate prime areas for diamond
exploration.
11 Mafic to Intermediate Metavolcanic Rocks-
these are prevalent on the east side and the north side of the claim group. They
are generally fine grained and massive to thinly laminated. They do occur interbedded
with layers of coarse grained flows. In some cases gold-bearing quartz veins occur
along the contacts between the coarse and fine grained fractions (east of Firesand
Creek @ L 9 to 13 South, and on the south part of claim 1174419). Pillow structures
are prevalent within the finer grained phases.
2)Felsic Metavolcanic Rocks-
these rocks are generally prevalent in the southwestern portions of the property,
and occur as interbedded layers up to fifteen meters in thickness. They occur as
massive flows and as feldspar crystal tuff l laminated tuff.
3)Mafic l U ltramafic Intrusive Rocks-
These occur as fine to coarse grained units; some of which are pyroxene rich
and some of which are olivine rich. It is generally dark grey to dark green in colour.
Two bodies of peridotite occur northeast of the property in the area of Sunrise Lake
and northeast of Sunrise Lake; occurring on the east side of Firesand Creek Fault and
to the north of the Kapuskasing Fault. The peridotite is generally serpentinite rich in the
outer sections. A pyroxenite body occurs on the east side of the property within claim
1201471 (east-central). A swarm of gabbro dykes and plutons occur in a northwesterly
trend (Reed Lake to Deep Lake) on the southwest side of the property. They are
generally fine to medium grained and hornblende rich. Some ultramafic fragmental^
occur on the southwest side of Reed Lake.
4) Felsic Intrusives-
These rocks generally occur as northeasterly trending dykes and occur as
quartz-feldspar and feldspar varieties. Large areas of this type cover areas to the
-
northeast of the claim area within Esquega Township. Granodiorite plutons are
prevalent west and southwest of the property; the largest units being the Jubilee Stck
and the Centennial Stock. These rocks have weak schistocity of 020 degrees to 040
degrees.
5) Mafic Intrusives-
these units cut all of the other units and exist as northwesterly trending and
northeasterly trending (discordant and concordant respectively). Lamprophyre Dykes,
black and biotite rich are prevalent radiating structures from the carbonatite complex.
Carbonatite-silicocarbonatite (calcitic) dykes, displaying fine grained grey to reddish
coloured layers, are also prevalent radiating from the carbonatite complex for a few
kilometers beyond the complex contact. Diabase dykes, both olivine rich and pyroxene
rich varieties, are found cutting all of the other units in a northwesterly direction. They
are from a few meters to sixty meters in width. They are generally coarse grained and
speckled appearance (feldspar and pyroxene lath mixture).
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Economic Geoloav-
The area has long been known for gold and base metals potential. Chart 1
shows a list of producers within McMurray Township and surrounding the claim group.
Most of the gold occurrences have been associated with the Jubilee Fault and fault
zones splaying off the Jubilee Fault (R.Rupert, 1988). Other gold occurrences
surrounding the claim group are associated with: northwesterly and northeasterly
trending iron formation, felsic metavolcanic units, carbonate rich mafic metavolcanic
units, and contact areas of diabase or gabbro units.
Recent exploration has indicated gold, copper, lead and zinc values associated
with the Wawa Lake-Kapuskasing Fault area.
Nickel-copper-cobalt has been associated with the peridotite complexes in the
area.
Iron has been associated with several northeasterly trending metasediment
(chemical and clastic) which occur north of the property.
Diamonds and diamond-indicator minerls have been found in close proximity
and in the direction of ice-flow from the property. Primary sources for diamond
structures (kimberlites and lamproites) are located with deep-seated magmatic
structures. The Firesand Carbonateite and Sunrise peridotite are two such structures
which have been influenced by the Firesand Creek Fault and the Wawa Lake-
Kapuskasing Fault which are again the oldest and most deep-seated fault structures in
the area. All kimberlites are fault controlled and carbonatite complexes are found in
the vicinity of many of them.
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Specifics of VLF Electromagnetic Survey-
The Crone V.L.F. electromagnetic unit utilizes higher than normal
electromagnetic frequencies and is capable of detecting small sulphide bodies and
disseminated sulphide deposits. It accurately isolates banded conductors and
operates through areas of high noise and interference levels.
This method is capable of deep penetration but due to the high frequency used,
its penetration is limited in areas of clay and conductive overburden. The components
of dip angle in degrees of the magnetic field component, field strength of the magnetic
component of the VLF field, and the out of phase component of the magnetic field are
measured at each station. The out of phase is only noted when readings reflect
abnormal character which signifies a strong conductor.
There are several different channels or stations available; each with a different
frequency. A channel used should be parallel to the general strike of the area. If this
cannot be determined or if two different strikes are found, then two orthogonal stations
are used to define the systems and conductors. In this case there are two orthogonal
strikes for the area; northeast being the dominant and northwest being the weaker.
The stations of Annapolis, Maryland and Seattle, Washington were used for the
survey.
The dip angle measurement measures the angle of inclination from horizontal
of the direction of the resultant V.L.F. or the amplitude of the major axis of the
pollarization ellipse. It is detected by a minimum on the field strength meter and is read
from an inclinometer with a range of plus or minus ninty degrees. A conductor is
designated by a "true" crossover pattern of the readings. The measurement is taken
from an audio null when the instrument is held in a vertical position; after turning
perpendicular to the direction of the alignment with the V.L.F. field. The V.L.F. field is
found by an audio null or minimum field strength measurement when the instrument is
held in a horizontal position. The accuracy of the dip angle measurement is plus or
minus one-half degree.
The field strength measurement defines the shape and attitude of the conductor
by the strength of the field in the horizontal plane or the amplitude of the major axis of
the polarization ellipse. It is the maximum reading obtained from the field strength
meter when the instrument is rotated in the horizontal plane; and is measured as a
-
percent of the normal field strength established at a base station. The field strength of
the V.L.F. stations drifts with time and must be corrected at a base station every few
hours. The field strength measurement has an accuracy of plus or minus two percent.
The out of phase component of the magnetic field, as a pecent of the normal
primary field, is sensitive to a low order of conductivity; lower than the dip angle
measurements. It is used to locate conductors of a low order of magnitude. The
reading is not recorded but the measurement pulse is recorded. It is a measurement of
the secondary field produced by a ground conductor which is in a different phase than
the primary field. This is the minimum reading of the field strength meter obtained
when measuring the dip angle. The measurement hads an accuracy of plus or minus
two percent.
The survey was carried out during October 13 through 15, 1995. Lines were
spaced at 100 meters apart and stations every 25 meters on the lines. A total of some
twenty three kilometers was traversed during the survey. The grid was run on claims
1174510, 1201471, 1174509, 1201477, 1110143, and 1174416. Stations used were
Annapolis , Maryland (21.0 Khz. frequency) and Seattle, Washington (24.1 Khz.
frequency).
The results are plotted at 1 inch to 100 meters. The dip angle readings are
scaled at 1" to 10 degrees for contouring, and the field strength contoured at
percentages of 1007o above the base station normal which is 100.
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Results of V.L.F. Electromagnetic Survey-
There are four northeasterly trending electromagnetic signatures and two east-
west electromagnetic signatures over claims 1174509, 1201472, 1110143, and
1174416.There is also one northeasterly trend across claim 1174510.
Field Strength Measurements-
The field strength over most of the property has a weak signature possibly due
to a great depth of overburden in this area. On claim 1174510 there are two moderate
field strength signatures paralleling each other in a northeasterly direction. One
corresponds to the contact area between the carbonatite complex and a felsic
metavolcanic flow unit. The other (more northerly) corresponds with the central part of
the felsic metavolcanic flow unit. On claim 1174509, a weak field strength occurs on
Line 5 North at 300 West. This has been enhanced by a junk pile of old automobiles.
On Line 1 South to 3 South, a weak filed strength corresponds to a swampy area
underlying the Firesand Creek. Similarly, on Line 12 South at 100 East there is a
weak field strength corresponding with the swampy overburden underlying the
Firesand Creek. Over the rest of the grid is a base reading with no overall signature.
Dip Angle Measurements-
There are essentially five linears, all with a weak signature, which cut across the
survey grip in a northeast and east-west direction. There are some discontinuous
trends which correspond with the five major linears.
Anomaly A- is a weak northeasterly trend traced for four hundred meters across
the south central portion of claim 1174510. It corresponds with the contact between the
carbonatite complex to the south and the felsic metavolcanic unit to the north.
Anomaly B- is a weak anomalous trend traced in an east-west direction across
the north part of claim 1174510; over a distance of over 500 meters (Lines 1 North to
Lines 6 North). It corresponds with the silicocarbonatite section of the carbonatite
complex, and also parallels the north side of a magnetic "circular" high within the
carbonatite.
Anomaly C- is a weak northeasterly trending signature which is outlined
between Line 8 South and Line 6 North, and is traced for some 1400 meters across
claims 1174509 and 1110143. This trend corresponds with the southeastern contact of
the carbonatite complex with the mafic metavolcanic flow units (basalts).
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Anomaly D- is a weak to moderate trend which trends in anortheasterly
direction from Line 18 South to Line 2 North. This trend corresponds with the swamp
overburden surrounding the Firesand Creek. This trend cuts across claims 1201472,
1110143, and 1174416.
Anomaly E- is a weak to moderate anomaly which trends northeasterly
between Line 2 South and Line 11 South. Located on claim 1201472, it corresponds
with part of the Firesand Fault system. This trend cuts rock units such as: diabase
dykes, porphyry dykes, and mafic metavolcanics.
The VLF electromagnetic survey has not delineated any significant conductor
trends, but has delineated at least one major fault-shear zone coinciding with the
Firesand Creek Fault.
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Specifics of Proton Magnetometer Survey-
The survey was completed with the use of the Exploranium-Geometrics
"Unirnag" proton magnetometer. It has a digital readout with a sensitivity of plus or
minus ten gammas.
The accuracy of the readings is increased by averaging two or three readings;
or until the readings settle out to a normalized reading. The range selector is changed
up or down in areas where there is high magnetic noise, or until a station with a
normalized reading is found.
The "World Gamma Range" setting on the instrument was brought down to a
scale relative to the regional magnetics of the area when plotting the final resultant
readings. The instrument requires no calibration once the proper range setting is
found. The average range setting for this area is 58,000 gammas. When plotting, the
58,000 setting is set at zero. Every few hours the readings are checked at a base
station on the base line and changes are noted and calibrated at the end of the day.
Results are plotted at 250 gamma intervals; after plotting corrections for daily
and diurnal drift. Base plans are plotted at a scale of 1 inch to 100 meters. Station
readings are taken on lines spaced at 100 meters apart with stations every twenty-five
meters. The field work was completed during October 13 to October 15, 1995. A total of
approximately twenty-three kilometers was traversed during the survey. Intervals of fifty
meter lines was carried out over Emerald-Green Lake.
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Results of Proton Magnetometer Survey-
At least four anomalous signatures were outlined by the survey; the most
significant over the northern portion of Emerald-Green Lake.
Trend A-
This anomaly is a weak signature trending in a northeasterly direction across
the central portions of the survey grid; and over claims 1174416, 1110143, 1201472,
and 1201471. This trend corresponds with the outer contact of the southeast section of
the Firesand Carbonatite Complex. This is probably outlining the iron-rich contact
areas of the complex.
Trend B-
This strong magnetic signature, trending in a north-south direction, traces the
bottom edge of a cliff between Line 14 South and Line 19 South; over a distance of
some five hundred meters. It corresponds with a carbonate rich coarse grained mafic
metavolcanic flow unit. It is located on claim 1174416.
Trend C-
This is a strong circular magnetic signature; somewhat oval shaped, located
between Lines 00 and Line 4 North. Located on the north side and under Emerald-
Green Lake, it is located within the boundary area of the silicocarbonatite section of
the Firesand Carbonatite Complex (southeast side).
There is significance to this structure as it is possible for a deep-seated
ultramafic complex to be pushed up through the fractured portion of the carbonatite
complex. If this unit is a diamondiferous kimberlite plug, it would be the minimum size
to be of economical interest; as it is some 400 meters round. This anomaly is a good
drilling target; to be drilled from northwest to southeast. Other similar circular features
should be looked for in close proximity to this one as kimberlite dykes always occur in
swarms and are associated with major fault systems.
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Conclusions of Magnetics and VLF Electromagnetics-
The geophysics have been useful in delineating the contact areas of the
carbonatite complex. They have also been useful in delineating fault structures and
several possible diamondiferous and gold target areas.
The electomagnetics have not been of much use probably due to the thick
overburden cover in the central portions of the survey grid. However this survey has
been useful in delineating some of the major fault systems which cut the claim group.
The magnetics have been useful in delineating a circular anomalous trend
some 400 meters round; a trend which occurs on the southeast flank of the carbonatite
complex and also centred on the north side of Emerald-Green Lake. This trend lies in
an area susceptable for intrusion of an ultramafic complex. This circular or ovoid
structure becomes a prime target for kimberlite.
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Backhoe Pits and Washing Plant-
Some thirteen pits were dug down to a maximum depth of 5.5 meters or until
bedrock was reached. Areas were chosen on the basis of: closeness to anomalous
area (airborne or ground geophysics) in conjunction with deep-seated fault systems. It
is a known fact that kimberlite pipes occur in close proximity to fault systems.
The pits were dug in an attempt to reach the basal gravels. Concentrates of
heavy minerals from basal materials is more accurate in locating local source areas,
whereas heavy minerals in the surficial materials can have travelled for great
distances.
Approximately two to two and a half cubic yards of material were washed from
each set-up. The material was loaded using a Caterpillar 330 backhoe, and
transported using a five-ton dump-truck to a local area for washing.
The washing plant consisted of a five-meter length of sluice boxes which were
designed from a pilot gold-alluvial processing plant. Thre author has designed alluvial
plants for production purposes for the past fifteen years, and has worked on many gold
and diamond alluvial projects.
The material from each pit was processed independently. Each pit consumed
approximately three hours to process.
The material was panned down to a concentrate which was sent to a lab for
heavy mineral separation and microscope work to detail the heavy mineral suite.
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Backhoe Pits- Bulk Sampling Program - Firesand Carbonatite Project
Contents 40 to 50 percent cobble (rounded) content. Cobbles consist of granitic-felsic volcanics- mafic volcanics. Brown colour. Some mafic volcanic bedrock fragments. Some gold specks observed in sample concentrates. Some 2.5 cubic yards sluiced and concentrated October 18, 1995. Dug to 5.2 meters depth.
Contents averaging 607o cobbles (rounded and rock fragments) with coarse sand matrix , brown colour with low clay content. Dug down to bedrock. Some specks gold observed in concentrates. Some 2.5 cubic yards washed and concentrated in sluice on October 18, 1995. Dug to 4.5 and 5.0 meters depth.
Pit F-3
Contents 5007o cobbles to 5-10 cm. diameter with clay matrix. Clay light grey and ancient-looking; similar to diamondiferous clays. Bedrock at 4.0 to 4.5 meters depth. Up to ID-15% os sample mixed with bedrock fragments of mafic volcanics. Some gold specks observed Some 2.5 cubic yards washed (sluiced) and concentrated October 18, 1995.
Pit F-4
Contents 40 to 5007o cobbles; rounded granite- felsic volcanics- mafic volcanics. Cobbles up to 3 to 8 cm. diameter. Heavy black sand concentrate and 2 to 5 specks gold each pan of concentrate (total of approximately 60 in 2.5 cubic yards of material washed). Dug to depth of 5.5 meters; no bedrock encountered. Sluiced and concentrated October 18, 1995.
Contents up to 6007o cobbles averaging 2 to 10 cm. diameter. Rounded cobbles of generally felsic volcanics with minor mafic volcanics. Beige colour with low clay content. Bedrock fragments (10 to 1507o content) up to 0.2 meters diameter. Some granitic cobbles. Dug to depth of 5.0 meters. Some 2.5 cubic meters washed and concentrated on October 18, 1995. No specks gold observed.
Pit F-6
Contents 20 to 3007o cobbles; rounded and averaging 3 to 5 cm. diameter. Cobbles mainly granitic with some mafic metavolcanics.carbonatitic, and felsic volcanics. Beige colour with no clay. Dug to depth of 5.5 meters. No outcrop
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encountered. Pit lies on north side of Emerald-Green Lake and over centre of magnetic ovoid "high". Some 2.5 cubic meters washed and concentrated on October 18, 1995. No specks gold observed.
Pit F-7
Contents 25-3007o cobbles; rounded and averaging 3 to 6 cm. in diameter. Majority granitic in nature. Appears to be of recent outwash. No bedrock encountered. Matrix of fine sand and clay. Pit on west side of Firesand Creek. Dug to depth of 5.5 meters. Hole caving in due to high water content. Material slumped with water. Some 2.5 cubic meters washed and concentrated on October 19, 1995. No specks gold observed.
Contents 25 to 3007o cobbles. Beige colour with some organics layers. No bedrock encountered. Cobbles mainly granitic and mafic volcanics. Pit on west side of Firesand Creek at junction of Firesand Fault and Lyre Fault. Dug to depth of 5.5 meters. Some 2.2 cubic yards washed and concentrated on October 19, 1995. No specks of gold encountered.
Pit F-9
Contents 20-2507o cobbles, average size 2-4 cm. diameter, rounded, coarse sand matrix, mainly granitic gravel, some silt-clay, west side creek draining south side carbonatite and into Firesand Creek complex. Located northwest side Megut Lake. Depth 5.5 meters. Some 2.5 cubic yards material (saturated), washed and concentrated October 19, 1995. No visible specks gold encountered.
PitF-10-
Contents 2507o cobbles, mafic metavolcanic & granitic cobbles(rounded), ave. cobble size 3 to 6 cm. diameter, brown coloyur, some organic layer, some red-oxide layers. West side of Firesand Creek (at edge Megut Lake), Dug to 5.5 meters depth. Some 2.5 cubic yards of saturated material washed and concentrated October 20,1995. No visible specks gold encountered.
PitF-11-
Contents 20-2507o cobbles, beige colour, red oxide layers, some organic layers, cobbles to 3-6 cm. diameter 4 rounded. West side Firesand Creek on shore of Megut Lake. Saturated with water and fine silty-sand matrix. Dug to 5.5 meters depth with no bedrock encountered. Fluvial-glacial material. Washed and concentrated October 20, 1995. No visible specks gold encountered.
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Pit F-12-
Contents 1507o cobbles, beige colour, coarse sand matrix, mafic rich cobbles avering 1-3 cm. diameter. Water saturated material. Pit at west side creek draining carbonatite (south side) complex into Firesand Creek complex. Dug to 5.5 meters depth and no bedrock encountered. Wsahed and concentrated October 20 and October 21, 1995.
W.C.-1-
Contents 25-3007o cobbles (rounded and sub-angular). Cobbles of granite, mafic volcanics, porphyry, felsic volcanics. Bulk sample of 300 kilos of material from 21.0 meters below high bank on river edge; at point on inner side ox-bow. High degree of black-sand concentrate. Some specks gold visible. Garnets visible. Concentrated October 17, 1995.
S.P-1-
Contents 5007o cobbles (rounded and sub-angular). Cobbles of porphyry, granite, mafic volcanics, felsic metavolcanics, peridotite. Till sample concentrate of 140 kilos from Sunrise peridotie and North Sunrise Peridotite. Some specks gold visible. Black sand concentrate coarse grained. Concentrated spring of 1995.
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PLATE B
PIT l
1201473
PH 2
PIT 3
NM0IO
PIT 4' •PITS
washing plont
1201471
PITH
BACKHOE-PITTINC LOCA
• PIT
SCALE 9^=5
O 200 4OO mfrra
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Conclusions A Recommendations-
A detailed exploration program consisting of geophysical and geological
surveys with follow-up gravel bulk sampling programs was carried out over the claim
group surrounding the Firesand Carbonatite complex to investigate the potential of a
deep-seated mantle source which would lead to emplacement of kimberlite rocks.
Although no sources were outlined, several significant anomalies for both gold and
diamonds were outlined by the surveys.
Although sparse kimberlite heavy-mineral suites were detected by the surveys,
some isolated heavy minerals associated with kimberlites, picroilmenites, were
isolated from two of the thirteen backhoe pits.
One of the samples , WC-1, did not indicate any kimberlite trace-elements but is
in close proximity to a surface kimberlite recently discovered in the Lagarde Mountain
area. This indicates that kimberlite indicators might be missed if they are they are
collected up-ice or in areas with thick overburden capping.
The electromagnetics have located several fault systems which kimberlites
might be associated with.
The magnetics have located a kimberlitic-type target on the southeast contact of
the Firesand Carbonatite complex which is probably covered by an overburden cap.
Kimberlite indicator minerlas were not encountered in this area possibly due to the fact
that this anomaly is at depth and does not surface. This target is of a large enough size
to be of sgnificance. It is recommended that this target be diamond drilled.
Alluvial gold values of significance were encountered in the northern section of
the claim group in the area being drained by the Firesand Creek. Indications are that
there is a source area for the gold in this area and that further investigations are
needed to find these sources.
Several gold bearing vein systems in the west side of the property were
sampled but returned low gold values (See Chart C). However, one gold-bearing vein
system on the southwest boundary, the Booth Showing, indicates that there is a
significant gold-bearing vein system which possibly carries on to the claim group. This
area should be investigated by further prospecting and sampling.
At least six airborne targets have been defined on the present group of claims,
and another four on adjoining claims which are held by the same owner. Another three
-
targets are located on the claim boundary areas. Sixof these anomalies , two of which
are negative magnetic anomalies, are associated with two fault structures crossing the
property. One is the Firesand Creek Fault and the other is the fault which has been
associated with the kimberlite dykes. It is suggested that these areas in specific be
prospected and in cases of overburden cover be sampled using till-sampling
techniques. All of these zones surround the Firesand Carbonatite Complex which
increases the significance of these targets.
It is recommended that S2500 be spent on picking up adjoining claims to the
northwest of the group surveyed, and that another S2400 be spent to keep another six
claims in good standing for another year. This would bring the group to a total of
approximately 79 claim units.
It is recommended that the next phase consist of geological mapping, VLF
electromagnetics, magnetics, and bulk testing of the northwesterly group of claims; in
specific the area that is cut by the Kimberlite Dyke Fault.
December 11, 1995
Toronto, Ontario FT. Archibald, B.Se. Geologist
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References
Archibald, C.W. April 1991, Qualifying Report for Firesand Resources Ltd.
Archibald, FT. January 1995, Summary Report McMurray-Chabannel Twsps.(Private)
Baird, D.S., April 1937 Planet Gold Mines Limited Report (Hillside Mine)
Canadian Mines Handbook, 1994-1995.
Johnson, E.M. 1937. Report of Claim 10294 (Wawa Gold Fields North)
Joyce, C.S. July 1967 TSL Certificate of Analysis for Algoma Ore Division
Kuryliw, C.J. July 1970 Geology Plan for Pango Gold Mines Ltd.
Kuryliw, C.J. June, 1970. Magnetometer Survey for Pango Gold Mines Ltd.
Melkman, A.C. August, 1934. Wawa Goldfields Development Plan
Morris, T.F. Nov.1994 OGS OFR 5908 Results of Overburden Sampling for Kimberlite
Heavy Mineral Indicators and Gold Grains, Michipicoten River- Wawa Area
OGS MRC 13, 1971. Gold Deposits of Ontario pg. 27-35
OGS OFR 5283, 1979 Hillside Mine pg. 116-118
OGS OFR 5283, 1979. Wawa Goldfields South pg.119-120
OGS, 1981. Wawa Area Airborne Electromagnetics 8* Magnetics (81006-81034 incl.)
Ravenbeck-Sonic Soil Sampling Inc. March 1993. Report on Investigation of Existing
Abandoned Mines Within Resident Geologist district of Wawa for MNDM, Vol. 1-3
Robinson, H.S., Sept.1928 Report on Mammoth Metals Property
Reward, C. April 1964 Diamond Drilling for McMarmac Red Lake Gold Mines Ltd.
Rupert, R.J. Sept. 1973 Hillside Mine Plan
Rupert, R.J. Sept. 1988. Citadel Gold Mines Inc.-Wawa Goldfields Mine Plan 4 Report
Sage, R.P. 1988, OGS Study 47- Firesand River Carbonatite Complex, Algoma Dist.
Sage, R.P. 1982 OGS P.2439 Geology of Chabannel Township
Sage, R.P. 1982 OGS P.2439 Geology of McMurray Township
Sage, R.P. 1982 OGS P.2442 Geology of Lastheels Township
Sage, R.P. 1982 OGS P.2440 Geology of Esquega Township
Sears, S. July 1986. Geological Mapping of Reed Lake Claim Group, Caviar Res. Ltd.
Sears, S. July 1986. Geophysical Survey of Reed Lake Claim Group, Caviar Res. Ltd.
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Cost Estimate PHASE 1
17 kilometers magnetics——————— S3060 17 kilometers geology——————— S306017 kilometers electromagnetics--—— S3060 assaying—————————~-——— $1500
travel/food/board/supplies -————— S2500pitting/washing plant———————— S3300
Total Costs———————— S16.480
PHASE 2diamond drilling (ten targets)
@ S20 per foot including geologist- S60.000
Total Cost of Phase 1 and Phase 2 including 1507o contingenies-- S87.952.00
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Certificate
l, Frederick Thomas Archibald, of the Town of Thornhill in the Region of York of the Province of Ontario, Canada, hereby certifies the following:
1. That l am an exploration consulting geologist and geophysicist2. That l have practised my profession in Canada for the past eighteen years,3. That l have personally been on the property and managed the programs,4. That l am a geological graduate of Carleton University, Ottawa, with a degree
of B.Se. Geology (1978).5. That the following report is a product of field work done on the property6. That Elliot Feder has advanced some 322,616.93 towards expenditures7. That l was commissioned by Elliot Feder to manage the work program and
write a report on the following group of 59 claim units8. That the field work was completed prior to November of 1995.9. That proper extensions were applied for prior to submitting these reports for
assessment purposes10. That it is believed the work was submitted prior to deadlines and that
sufficient assessment was submitted to apply at least one years extention on the 59 claim units
Dated at Concord, Ontario this 23rd. day of December, 1995.
Signed:
-
Breakdown of Work
Contracting - geological mapping (23 km.) S4140.00Contracting- geophysics (46 km.) S8280.00Casual Labour S9655.00Heavy Equipment Rental S3940.75Equipment Rental S 750.00Supplies S 152.06Travel Expenses S1562.60Maps b Abstracts b faxing charges S 373.22Room/Board/Subsistence S1494.27Assaying charges S1508.24 TOTAL————————————-————S31.856.14
Claim Number 1201473 (4) 1174510 (5) 1201471 (12) 1110143 (4) 1201472 (12) 1174416 (8) 1174419 (2) 1110144 (1) 1174509 (3) 1174421 (4) 1174480 (4)1174530 (2)
1174531 (2)
1174532 (2)
Assessment Performed On Claim Assessment Reserve Applied1112 1600
7032 2000
3639 4800
4030 3200
7527 4800
5756 5756
853 853
684 8001223 2447——— 1600—— 1600——- 800—-- 800—— 800
TOTAL———— 31856 31856
-
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F. T. ARCHIBALD CONSULT Ir-13 DATE; OSCErlSER J, 1V75
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OCT 31 '95 02:59PM CHAUNCEY ASSAY LABSCHAUNCEY ASSAY LABORATORIES LTD.
33 Chauncey Avenue, Toronto, Ontario, HSZ 2Z2 Tel s (4161 239-3527 FAX: C416) 239-4O12
P.I
CERTIFICATE OF ANALYSIS
RECEIVED FROM:
REPORT NO.t
DATE RECEIVED:
FRED ARCHIBALD
AR-22O
OCTOBER 24. 1995
DATE: OCTOBER 31
SAMPLES OFs CONCENTRATES
ATTENTION: FRED ARCHIBALD
SAMPLE NO
F-1F-2F-3F-4F-5F-6F-7F-8F-9F-10F-11F--12F-13WC-1
SAMPLE WEIGHT grams
153.949.6
345.1 235.284. l 100.7 237. Qisa.o175.O 301.2 147. l 101.0 498.2 55.9
MI HEAVIES 7.
15.0 7. 2.7Q 7. 3.48 7. 9.43 7. .66 7. 1.73 X
16.69 7. 4.83 7. 1.36 7. 3.43 '/. 2.39 7. 2.4Q 7. .03 7. 3.85 7.
MI HEAVIES Au micrograms
S36 205 22O 2.121 315 134 520 55763 417 144 17O6553
MI HEAVIES Cr ppm
41 174672872 1154452
1O963
1O8SO
'-' 5 19O
* Or HAD TO BE DONE FOR DIAMOND INVESTIGATION
J. van Engelen Mgr.
-
REPORT
ON
MICROSCOPIC EXAMINATION
OF
FOURTEEN HEAVY MINERALS CONCENTRATES OF TILL SAMPLES
Fourteen heavy minerals concentrates of screened till samples were microscopically examined to determine their mineral constituents, with emphasis on any diamond indicator minerals that might be present, and, if present, to determine the chemical compositions.of these indicator minerals utilizing the scanning electron .'microscope, and from these compositions to determine whether these indicators were derived from a potentially diamondiferous source.
The fourteen samples are numbered F-l to F-13, inclusive, and WC-1.
Sample F-l;
Approximately 8 0* of the sample is magnetite, and 15% is pink to amber coloured almandine garnet. Augite and orthopyroxene are abundant. Epidote, sphene, and diopside occur in minor amounts, particularly the diopside. Ilmenite also occurs in minor amounts, as fresh fragments that lack the alteration crust typical of picroilmenite.
Sample F-2:
Magnetite comprises approximately 55% of the sample, and pink to amber coloured almandine garnet about 4(^. The remaining 5% is comprised of several grains of black coloured augite, a few grains of diopside, and minor epidote, sphene, zircon, and orthopyroxene.
Sample F-3:
Magnetite comprises 7 0-BO* of the sample. Pink to amber coloured almandine comprises lS-20% of the sample. Several grains of ilmenite are present, however none display the crustal surface which is typical of picroilmenite. Minor epidote is present, along with several grains of diopside, zircon, and orthopyroxene. Three fragments are present of a pale blue to dark blue coloured mineral which may be topaz or apatite. Trace amounts of tarnished sulphide grains are also present.
Sample F-4;
Magnetite and ilmenite together comprise about ^ 0% of the sample. The ilmenite displays fresh surfaces rather than the crustal surfaces which would identify it as picroilmenite. Pink almandine
-
comprises about 2(^ of the sample, and orthopyroxene about 5%. Minor augite is present, along with minor amounts of sphene, zircon, and epidote. Trace amounts of tarnished sulphides are also present.
Sample F-5:
Magnetite comprises about 70* of the sample, and pink coloured almandine a further 25*. Minor to trace amounts of epidote, diopside, zircon, and orthopyroxene are present. One cleavage fragment of ilmenite was identified. A portion of its surface is vaguely crusty, suggesting that it may be picroilmenite.
Sample F-6:
The predominant mineral is magnetite, which comprises about 75% of r the sample. Pink coloured almandine comprises a further 20*. : Minor to trace amounts of augite, sphene, zircon, orthopyroxene, and epitote are also present.
Sample F-7:
Approximately 70* of the sample consists of magnetite and ilmenite, with the magnetite more prevalent. Pink almandine comprises about 25% of the sample. The balance consists of minor amounts of orthopyroxene, epidote, zircon, and sphene, and traces of diopside. One grain of ilmenite displays a crustal surface which vaguely resembles that of picroilmenite.
Sample F-8:
The predominant mineral is magnetite, which comprises about 75% of the sample. Pink almandine comprises a further 20*. Minor to trace amounts of orthopyroxene, augite, sphene, zircon, epidote, and diopside are also present.
Sample F-9:
Magnetite is the predominant mineral, comprising 70-75% of the sample. Pink coloured almandine comprises a further 20*. Minor to trace amounts of orthopyroxene, epidote, zircon, sphene and diopside are also present.
Sample F-10:
Magnetite comprises 70-80* of the sample, and pink almandine about 20%. Minor to trace amounts of orthopyroxene, augite, sphene, zircon, epidote, and diopside are also present.
Sample F-ll:
Magnetite comprises 70-8O* of the sample, and pink almandine about 20%. Minor to trace amounts of orthopyroxene, augite, sphene, zircon, epidote, and diopside are also present.
-
3.
Sample F-12;
Magnetite is the predominant mineral, comprising about 75% of the sample. Pink almandine comprises about 2 0% of the sample. Minor to trace amounts of orthopyroxene, augite, sphene, epidote, zircon, and diopside are also present.
Sample F-13:
This sample did not produce a suitable heavy minerals concentrate. It does, however, contain several grains of fresh pyrrhotite and pyrite.
Sample WC-1:
.-Magnetite is the predominant mineral, comprising about 1 0* of the sample. Pink almandine conprises a further 25%. The balance of the sample consists of minor to trace amounts of orthopyroxene, augite, sphene, zircon, epidote, and diopside.
The microscopic examination of the fourteen heavy minerals concentrates failed to identify any pyrope garnet or chrome diopside, two of the commonest diamond indicator minerals. Picroilmenite, another common indicator mineral, was identified, but only in small amounts, one grain in each of two samples - F-5 and F-7. Sphene, a common rock-forming mineral, can also be a diamond indicator mineral under certain circumstances. However, it is far less reliable than pyrope garnet, chrome diopside, or picroilmenite. Sphene is present in samples F-l, F-2, F-4, F-6, F-7, F-8, F-9, F-10, F-ll, F-12, and WC-1.
Sulphides are present in trace amounts in Samples F-3 and F-4, and as several grains of fresh pyrite and pyrrhotite in Sample F-13.
The distinct lack of any pyrope garnets and chrome diopsides, combined with the presence of only two grains of picroilmenite strongly precludes any possibility that the site of this suite of samples might represent a glacial dispersion train. Any further diamond evaluation work on these samples in not considered warranted, and therefore no microprobe analyses were undertaken.
The abnormally high Cr values have no direct correlation with the garnet (almandine) content, the diopside content, or the
-
magnetite content. It is unlikely that the Cr is derived from a mantle source. The high Cr values are likely due to oxides derived from mafic and/or ultramafic rocks from a crustal source.
November 10, 1995 Toronto, Ontario E. A. Gallo, B.Se., F.G.A.C.
-
DAILY
-
Daily Field Log of Work Schedule- Feder Group (Mcmurray-Lastheels Twsps)
May 5- P.C.Deslisle and F.T.Archibald study area and traverse1201473,1174510,1174480,1174812. Study air photo and magnetics. East- west traverses every 400 feet.
May 6- P.C.Delisle and F.T.Archibald study area and traverse 1201471 and overpyroxenite area-east-west traverses every 200 feet.
May 7- P.C.Delisle & F.T.Archibald study area and traverse 1201472 and 1110143 May 8- P.C.Delisle A F.T.Archibald study area and traverse 1174416 A 1174419 area August 27- F.T.Archibald layout linecutting grid over claim group: 1174416, 1110143,
1110144, 1201472, 1201471August 28- F.T Archibald prospects group 1174419, lays grid over 1174510-1201473 Sept.1- F.T.Archibald prospects 1174480,1174812,1110143. 1110144 October 12- F.T.Archibald prospects 1201472 (northwest traverses) October 13- F.T.Archibald A Bouchard prospects 1110143 (northwest traverses) October 14- F.T. Archibald A Bouchard prospects 1174416(northwest traverses October 15- F.T.Archibald A Bouchard prospects 1174419 (northwest traverses) October 16- F.T.Archibald A Bouchard prospects 1174480,1174510, 1201473 October 17- F.T.Archibald A Bouchard set up washing plant on 1201471 October 18- F.T.Archibald 4 Bouchard start backhoe digging 1174510 October 19- F.T.Archibald 4 Bouchard backhoe digging 1201471 A 1201472 October 20- F.T.Archibald A Bouchard backhoe digging and washing plant operation
claim 1174416 .1110143, 1174509 October 21- F.T.Archibald backhoe digging 1174416 and washing plant
operationOctober 22-^/1".Archibald prospect 1174419 October 25-P.C.Delisle and B.Bouchard prospect and map 1174419, sample trenches
-
vfi O
l- Oex.
-
EXPENDITURE
-
INVOICE # 95-25
F.T.Archibald Consulting Ltd. 668 Millway Ave. Unit 15 Concord, Ontario L4K 3V2
IN ACCOUNT WITH
Elliot Feder22 Snowberry Ct.King City , Ontario Re:McMurray-Lastheels Twsp. Claim ProjectJan. maps 98.67
maps 9.63 .:maps 10.12maps 1.15
May map purchase 24.71mileage 1200 X.35 420.00motel 395.77food/groceries 246.99supplies 29.46contract labour 750.00 (P.C.Delisle, geologist)X 3.75 days
F.T.Archibald contract 750.00 (3.75 days in field)washing plant rent 750.00 (Lilex Industries)- including pumps A hose
Aug. 27 hotel/food 127.0527 meals 54.3728 maps MNDM 5.65 28 gas 23.02* 28 meals 19.53 28 motel 60.48 28 gas 33.00*
Sept. 1 air flight 70.00 1 gas 32.00* 1 meals 25.75 1 meals 18.13 1 gas 31.03*
Sept. 1 mileage 1400 X .35 370.95 (less fuel)F.T.Archibald 600.00 (3 days in field-) coordination linecutting 5000.00 (B.Bouchard- 20 km. X S250)
Oct.12-21 mileage Timmins-Wawa-Toronto @ S0.35 per km.-1993 km697.55
FT. Archibald Oct. 12 to Oct.21 @ S200 per day (field)2000.00
October 12 motel 145.60 groceries 109.47 gas 22.03*
-
Nov.
1314
1516
1718
19
20
21
22
23
248
10
mealmealmealgasmealsuppliesgassuppliesmealmealmealmealmealmealDump truckgroceriesgasmealhelperbackhoelabourmotelmealgasgasgasgasP.C.DelisleB.BouchardMNDMMNDMmap printsMNDMMNDMGallo report
5.13 32.79 12.57 50.00* 12.82
1.37 34.01 80.22 13.88 12.57 12.57
3.98 5.85 9.49
775.00 14.40
7.00 13.61
190.00 1845.75 1320.00 67.63 3.84
25.00* 56.32* 30.80* 45.50*
200.00 165.00
15.58** 13.50** 40.15** 59.56** 94.50** 882.75**
Chauncey Lab 572.99** Chauncey Lab 52.50**
Geological Survey 23 km. 4140.00 Electromagnetic 23 km. 4140.00 Geological Surv. 23 km. 4140.00 Photocopy 33.12
TOTAL CHARGES———— S31.856.14
(15.5hr. @ S50perhr)
(Pierre Gravel)(15.0 hr. + floating charge)Barron Bouchard 8 X 165/day
* charges do not include GST on services
-
Jl/^LKER Drof ting 8c ftepro Producls
G.S.T. REGISTRATION NO.
R127537207
35 McCleary Court, Unit 24, Concord. Ontario L4K 3Y9 Tel.: (905) 660-9680 1-800-268-4866 Fax: (905) 660-9688
SOLD TO:
SALES ORDER NO
18631
TERMS
NET 15 DAYS
G ST. NO. CUSTOMER ORDER NO. TIME REQUIRED ^EOF
NO.OF ORIGINALS ENCLOSED
DESCRIPTION OF ORIGINALS
NO.PRINTS
OFF EACHTYPE OF PRINT REQUIRED
TOTALNO
COPIESUNIT
SO. FT.TOTAL SQ.FT.
PRICEPER
O. FOOTAMOUNT
X? 61r
SPECIAL INSTRUCTIONS
C On AccountC CashCH ChequeD C-arge Carci - V^sa M IC AMX
RECEIVED BY
-
OntarioMinistry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines
INVOICE
DATE:
"PLEASE QUOTE INVOICE NUMBER WHEN MAKING PAYKENT"
G-S.T. No. R124668666
Mining Recorder's Office Ministry of Northern
Development and Mines 60 church Street Sault Ste. Marie, Ontario P6A 3H3 (705) 945-6925
—PRINTS
—ABSTRACTS
2. —— —FAX FEES
—PHOTOCOPIES
—REPORTS
--—GEOLOGICAL MAPS
-PRELIMINARY MAPS
\ 1L
TYPE
@ $1.00 each
Q 5 1.02 each
@ $2.04 each page
@ Si. 02 each
@ 5 each
@ S each
@ S4-40 each
6 $2.20 each
-AEROMAGNETIC MAPS
— CERTIFIED COPIES
Payment Duo Upon Receipt
Cheques Payable to U '*- of France
cOO'd
@ 5 each
6 5 each
@ 5 each
6 $4.00 each
@ 52.04 each
SUB-TOTAL: G.S.T- P.S.T.
TOTAL:
3IMVK S S 03N OXIXIK OPtl (NOKIS6 -SZ-MOO
AMOUNT
TD
-
Ontario
Ministry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines
"PLEASE QUOTE INVOICE NUMBER WHEN MAKING PAYMENT"
INVOICE f
TO.-: ROM:
UHVL3VZ
G.S.T. No. R124668666
Mining Recorder's office Ministry of Northern
Development and Mines 60 church Street Sault Ste. Marie, Ontario P6A 3H3 (705) 945-6925
—PRINTS l
1M-——("ABSTRACTS
)4 ——|—FAX FEES
-PHOTOCOPIES
-REPORTS
——j—GEOLOGICAL MAPS
———PRELIMINARY MAPS
$1.00 each
$1.02 each
$2.04 each page
-AEROMAGNETIC MAPS
-CERTIFIED COPIES
Payment DuoUpon Receipt
Cneques Payable toM.T.'S*.^ cf F : nance
i y \j
TOO'd
i 51.02 each
e 5 each
@ 5 each
i 54.40 each
@ 52.20 each
@ 5 each
Q 5 each
e 5 each
@ S each
i $4.00 each
i 52.04 each
SUB-TOTAL: G.S.T. P.S.T.
TOTAL:
3IHVK S S 03N OMXIlv iO'cl (XOK)Sfi .?c- MOO
-
NOV 2 1 '95 09:3v3AM CHfiUNCEY ftSSftY LfiES P. 6
GALLO EXPLORATION SERVICES INC.
148 Allanhurst Drive Islington, Ontario M9A 4K7
Ph: 416-245-3511
r. account with Chauncey Assay Laboratories for the following rofessional services:
inocular microscopy of 14 heavy minerals concentrates of till anples (F-l to F-13, inclusive, and WC-1):
cv. 7-9 - Microscopy and identification of mineral grains
31 hours @ 525./hour ........... $ 775.00
:ov. 10 - Report Writing1/4 day @ 5200./day ........... __50.00
Sub total $ 825.00
GST 57.75
TOTAL DUE $ 882.75
November 10, 1995 E. A. Gallo, B.Se., F.G.A.C,
-
JH^LKER DrofHng 8cffepro Products
G ST. R
EGISTR
ATION
NO.
R127537207
35 McCleary Court, U
nit 24, C
oncord, Ontario L4K 3Y9
Tel.: (905) 660-9680 1-800-26M
866 Fax: (905) 660-9688
SOLD TO:
/T"-r-
SALES ORDER NO
15486
- LT
D.
TERMS
NE
T 15 D
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O.ST. NO.PRO
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Cb NO.
CU
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tH O
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TIME REQ
UIRED
NO. O
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ENC
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DESC
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N
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RIG
INALS
NO.PR
INTS
OFF EACH
TYPE OF PRINT R
EQU
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TOTALNO.
CO
PIESU
NIT
SQ. FT.
TOTAL
SO. FT.
PRIC
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TA
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SPECIAL IN
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G. ST
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THIS
AM
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REC
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CH
AU
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RIES LTD.33 C
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M8Z 222
TELEPHO
NE: (416)239-3527 - FAX.: (416) 239-4012
DUE UPON RECEIPT
GST l R123717001
Mr.
Fred A
rchibald 668 M
illway A
venue U
nit 15 i
16 C
oncord, O
ntario L4K
3V2
A 5053
Novem
ber B,
1995
PAGE DUF DAT f
Due U
pon Receipt
DESCRIPTION
14 Assays Au 14 Assays Gr 14 Heavy Mineral Separarions
(Screening And Examination Included)
Get. No:
AR-220 SAnple No:
F-1 to F-13, WC-1
ORDERED
SHIPPEDUNIT PRICE
EXTENDED PRICE
S 8.75
S 4.50
$ 25.00
$ 122.50
S 63.00
S 350.00
SUB TOTAL
GST
PST
TOTAL
535.5037.49
572.99
S 572.99
-
MOVING Sk HAULAGEREFUSE, BRUSH, SNOW REMOVAL
ROOF CLEANING
BOX 67, HAWK '^T. ONT. POS 1 GO
VALOIS SNOWPLOWING* Commercial (fe Residential *
BiU ValoisHawk Junction, Ontario
Phone 889-2011
Date.
X
Address-
Location rSt/L-^CwA
Invoice
157
Work Description
-
Elliot Feder
Kingnclty^ Ont. RT. ARCHIBALD CONSULTING LTD.668 MillwayAve. Units 15-16 Concord. Ont. L4K3V2
Tel: (905) 660-0501 Fax: (905) 660-7143
November l, 1994
Expenses incurred re: Claims 1110167 1174474 1174475 1174473 1174416-X1174471 1174471 1174472 1174470 1174421^t
^•-—1174512 1174477 1174481 1174530 1174420-V^—1174419 1174413 1174531 1174532
Map studies and preparations; field studies, etc.
map purchases 24.71mileage charge (1200 km.) 420.00motel 395.77food/groceries 246.99supplies 29.46contract labour (P.C.Deslisle) 750.00 (3.75 days)washing plant manufacture 750.00
TOTAL OWING as per contract $2615.93
sincerely,
F.T.Archibald, B . Se -Geologist
-
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