PDF Report

DRILLING REPORT
ON THE
YALAKOM PROPERTY
LILLOOET MINING D I V I S I O N
N.T.S.
51
LAT:S0
D.G.
02'N
92 0 / 2 E
LONG:
122'
Leighton, B.Sc.,
35'W
F.G.A.C.
September, 1 9 9 0
GEOLOGICAL
A§SESSMENT
ANCH
PORT
. '8
i
CONTENTS
Page
1.
2.
3.
4.
5.
6.
7.
Summary
Introduction
1.1 Location, Access and Physiography
1.2
Claims Description
1.3 History
Geology
2.1 Regional Geology
2.2
Property Geology and Mineralization
Drilling Program
Conclusions and Recommendations
References
Certificate of Qualifications
Statement of Costs
i
1
1
1
4
6
6
8
9
10
11
13
14
FIGURES
Figure 1. Location Map
Figure 2. Claims Map
Figure 3. Drill Hole Location Map
APPENDICES
Appendix I
Appendix I1
Drill Logs
Assays
2
3
in pocket
i
DRILLING REPORT
ON THE
YALAKOM PROPERTY
SUMMARY
The Yalakom Property is located on Big Dog Mountain in the
Shulaps Ranges, 240 kilometres north of Vancouver and 40
kilometres northeast of the Bralorne Gold Camp, southeast
B.C. The property, within the Lillooet Mining Division,
consists of eight reverted crown grants and two metric fourpost claims, owned 100% by Balsam Resources Inc.
The area is underlain by Shulaps Ultramafic Complex
peridotite and quartz diorite porphyry of the Blue Creek
Intrusives. A gold-bearing quartz vein system cuts the
porphyry. The No. 9 vein was explored in 1949 and 1950 with
980 ft. (298 m) of drifting. At that time a 165 ft. (50 m)
l e n g t h was r e p o r t e d t o average 0 . 9 4 0 2 . gold p e r t o n ( c u t )
across a 1.21 ft. (0.37 m) width, or 0.38 oz. gold per ton
across a mining width of 3.28 ft. (1.0 m) (Thompson, 1957).
Work by Phendler (1982) indicated reserves of over 4,000
tons with an average diluted grade of 0.77 oz. gold per ton.
Sampling carried out in 1983 suggested that gold
mineralization occurs in three zones or shoots. Zone 1
grades 1.294 oz. gold per ton over 1.403 ft. (0.43 m) for
160 ft. (48.7 m), Zone 2 grades 0.741 oz. gold per ton over
2.03 ft. (0.62 m) for 50 ft. (15.2 m) and Zone 3 grades
0.601 02. gold per ton over 1.43 ft. (0.44 m) for 35 ft.
(10.7 m) (Phendler, 1983).
Surface drilling in 1987 demonstrated the continuity of the
quartz vein system along strike and and that gold
mineralization was present; however, due to practical
difficulties, the drilling was unable to reach the projected
down-dip continuation of the main No. 9 ore shoot (Culbert
and Leighton, 1987).
In 1990, 123.7 m (460 ft.) of drilling was done in one
diamond drill hole collared near the No. 9 adit portal and
targeting the down-dip continuation of the main ore shoot.
The drill intersected dioritic rocks, probably belonging to
the Blue Creek Porphyries, and aplite dykes. All were cut
by a number of quartz veinlets to veins with minor sulphide
mineralization and alteration. A total of 27 samples were
taken of the quartz. Fire assay analysis of the samples
gave an average gold content of <0.002 oz/ton for the top of
the hole. From 97.69-118.26 m a grouping of anomalous
samples carried values up to 0.059 oz/ton (2.02 g/tonne)
ii
over 1.49 m (4.8 ft.). This group of anomalous values
appears to be equivalent to Phendler's Zone 1. While values
obtained are not as high as previously reported, the
continuance of gold mineralization within this zone is
indicated.
Further work is recommended. Future drilling should target
the extension of Zone 1. Phendler's Zones 2 and 3 have yet
to be tested by drilling; this should be included in
subsequent work.
1
1. INTRODUCTION
1.1
Location, Access and Physiography
The Yalakom property is located 240 km north of Vancouver
and 40 km northeast of the Bralorne gold mine in the Shulaps
Range (Figure 1). The claims are on the eastern slope of
Big Dog Mountain at 2,300 m (7,550 ft.) elevation on the
north side of Blue Creek. Access is by gravel road from
Lillooet along the Gold Bridge Road for 22 km to Moha, then
along the Yalakom River Road for 58 km to the B:Lue Creek
road. The Blue Creek road leads onto the claims, to the
Elizabeth Mine (elevation 1994 m) and then to the No. 9 adit
of the Yalakom property, at 2,274 m (7,460 ft.) elevation.
The No. 9 adit of the Yalakom property is about 280 vertical
metres above and 1.5 kilometres to the west of the Elizabeth
Mine.
The property is located above tree line. Slopes are mainly
talus-covered permafrost soil, with little outcrop. Bedrock
is at or close to the surface on the upper flanks of the
ridge, but is obscured by loose rock. The mine is
accessible only during the summer and early fa1:L months due
to the high elevation.
1.2
Claims Description
The Yalakom Property consists of eight reverted crown
grants, and two four-post metric claims, owned :LOO% by
Balsam Resources Inc. The claims are within the Lillooet
Mining Division. Claims data is as follows:
Claim
Yalakom 1
Yalakom 2
Yalakom 3
Yalakom 4
Plateau 5
Plateau 6
Plateau 7
Plateau 8
True Blue 1
True Blue 2
Record
No
594
595
596
597
598
599
600
601
4440
4441
Lot No. Expiry Date*
(M/D/YI
Acreage/
Units
Mar.
Mar.
Mar.
Mar.
Mar.
Mar.
Mar.
Mar.
Apr.
Apr.
36.84
47.96
42.03
48.99
50.30
51.65
31.82
45.98
20 units
20 units
7408
7409
7410
7411
7416
7417
7418
7419
-
*on acceptance of this report.
1994
1994
1994
1994
1994
1994
1994
1994
1994
1994
0
p-..,
(0
?
!
~
I
BALSAM RESOURCES CORPORATION
LOCATION MAP
YALAKOM PROPERTY
N.T.S.
9202/E
October, 1 9 9 0
Scale:
1:7#500,000
Fig.
1
a
BaLBAN RESOURCES CORPORATION
CLAIMS MAP
YAIdKOM PROPERTY
N.T.S.
9202/E
Saale:
1:50,000
Oatober, 1990
FTS. 2
4
1.3
History
Prospectors first entered the Bridge River area from the
Placer gold was found in
Fraser River Canyon in the 1850's.
the area in 1863 and the first hard rock minera:L claims were
staked in 1896. Extensive exploration resulted in the
discovery of numerous small mines and prospects,,mostly of
auriferous quartz veins. By 1914, the Pioneer Mine went
into production, and by 1932, the Bralorne Mine also went
into production. Between 1932 to 1971 the Bralorne produced
5,474,000 tons of ore with a recovered grade of 0.52 oz.
gold/ton or 2,846,000 oz. of gold. From 1914 to 1962, the
Pioneer Mine produced 2,447,000 tons with a recovered grade
of 0.54 0 2 . gold per ton or 1,337,580 0 2 . of go:Ld. The
Bralorne-Pioneer gold camp was the major gold producing area
in British Columbia for some time.
Auriferous quartz veins were discovered in the property area
in 1934. In 1940 to 1941, these were rediscovered and
staked as the Elizabeth claims. In 1948, Braloime Mines
discovered boulders containing high grade gold on a talus
slope on what is now the Yalakom 2 claim. Trenching exposed
a 0.6-0.9 metre (2-3 foot) wide north-striking vein
traceable for 60 metres (200 feet). A total of 246 metres
(807 feet) of drifting was completed on this No. 9 vein in
1949 and 1950. Although the drift contained encouraging
values in gold, it did not produce the spectacular free gold
which had characterized the float. Bralorne Mines abandoned
the claims in 1953. A reserve of 800 tons containing 1,770
oz. of gold was calculated by W.H. White in 1956, based on
an earlier undated assay plan (White, 1957).
Bralorne assay plans appear to record only significant gold
assays and cover only 50 metres (164 feet) of the total 250
metre (820 foot) length of the adit. Assays reported showed
0.37 metres (1.23 feet) of uncut 1.45 oz/ton go:Ld or diluted
0.91 metres (3.0 foot) width of 0.38 oz/ton gold with high
grades cut to 3 oz. gold (Thompson, 1957).
Based on Bralorne's sampling, Phendler (1982) estimated
reserves over 400 tons grading 0.77 oz. gold per ton
(assuming 20% dilution on the 1.23 feet vein) calculated as
follows:
a) Tonnage calculation (above the level)
165 ft. x 165 ft. x 1.50 ft. =
10 cubic feet per ton
4,083 tons
b) Grade Calculation:.
0.94
02.
Au/ton diluted 20%
= 0.77
oz Au/ton.
5
Phendler proposed extraction by resuing, a type of cut-andfill stoping wherein the vein is extracted first and the
stope is widened to a practical working width with the
material remaining in the stope.
In 1983, the backs of No. 9 adit were systematically sampled
under Phendler's supervision (Phendler: August 22, 1983). A
continuous quartz vein system exists throughout. Three gold
bearing zones were delineated. Results are tabled below:
Zone Footage
from
Portal
1
2
3
Length
105-265'
365-415'
600-635'
160'
50 '
35'
Width
0.89'
1.53'
0.93'
Uncut
Grade
(oz/t Au)
2.019
0.983
0.926
Diluted
Grade
(oz/t Au)
1.294/1.40
0.74 1/2.03
0.601/1.43
'
'
'
Overall, 13 of 135 samples assayed more than one ounce gold
per ton. These results indicated that the gold-bearing
quartz vein is continuous throughout about 244 metres (800
feet) of the adit.
bulk (175 kg) sample of selected vein material indicated
no problems with treatment, and recovery in the 85-90
percent range (Phendler, 1982). Limited surface work by
Phendler (1982) suggested that the vein can be traced for
400 metres on surface.
A
In 1984, three diamond drill holes explored the No. 9 vein
below the adit level. Several gold-bearing quartz veins
were intersected, with the best reported intersection of
1.09 oz/ton gold across 0.2 metres (0.7 feet) in hole 84-1.
Phendler (1984) concluded that mineral Zone 1 rakes to the
south and projects down-dip for at least 35 metres (115
feet), and estimated an additional 1670 tons of drill
indicated reserves at 0.38 oz/ton gold. More generally the
drilling showed that the veins are present, some with
appreciable gold content.
In July, 1987, a program of surface diamond drilling as
outlined by Culbert and Leighton (1987), was initiated.
This program had the objective of approximately outlining
the downward continuation of main ore shoots within the No.
9 vein. Four diamond drill holes totalling 600 metres were
done. This drilling demonstrated the continuity of the
quartz vein system but, due to practical difficulties, the
holes did not reach the target - the projected down-dip ore
shoot extension area (Culbert C Leighton, 1989). Core
samples gave values to 4.94, 4.18 and 3.57 g/tonne over
unknown thicknesses (Gaba et al., 1988).
6
2.
2.1
GEOLOGY
Regional Geology
Most recent government mapping indicates that the region,
from west of Gold Bridge to northeast of the Yalakom and
Bridge Rivers, is underlain by three complexly imbricated
terrances, separated by lenticular north-northwest trending
fault zones. The terranes are:
- Permian(?) to Jurassic Bridge River Complex - now defined
as comprising Bralorne Intrusives, Bridge River Assemblage,
Shulaps Ultramafic intrusives and the Cadwallader Fault Zone
rocks (variably metamorphosed and structurally imbricated
chert, argillite, mafic extrusives and intrusives greenstone, greenschist, blueschist, diabase, gabbrolimestones, clastic rocks and serpentinite);
- Permian(?) to upper Triassic Cadwallader Terrane - arcderived volcanic and sedimentary rocks (basalts, volcanic
wackes and argillites);
-
late Triassic to Middle Cretaceous Methow Terrane clastic
sedimentary rocks and limestone.
These are intruded by late Cretaceous to Oligocene felsic to
intermediate stocks and dykes, including outliers of the
Jurassic Coast Plutonic Complex (including the Bendor
Pluton) which lies some 30 kilometres to the west of the
claims.
The pre-mid Cretaceous Shulaps Complex is the main rock type
underlying the claims and forms a wedge against the Yalakom
Fault to the east. The Shulaps Complex consists of two main
members; a serpentinite melange overlain by rhythmically
layered harzburgite, dunite and orthopyroxenite. The
Shulaps and Bridge River Complexes together are now believed
to constitute a dismembered ophiolite sequence.
All strata are locally overlain by Eocene volcanic and
sedimentary rocks, and Miocene to Pliocene plateau lavas of
the Chilcotin Group.
The regional structure is dominated by northwest to north
trending faults that reflect a complex history of midCretaceous to Tertiary compressive strike-slip and
extensional deformation. The major faults are the Yalakom
Fault to the east of the property, which runs into the
Bridge River Fault a small distance south of the claims; and
the Marshall Creek fault to the west. These mid-Cretaceous
to Tertiary structures are superimposed on poorly understood
older structures.
7
The brittle faulting and lenticularity of the Bridge River
complex may be attributed to an earlier deformational
history, perhaps in a subduction zone or accretionary prism
setting.(Schiarriza et al., 1990)
Mineralization in the area is concentrated in a wedge
between the Yalakom-Bridge River Faults and Marshall Creek
Fault, and is broadly associated with Late Cretaceous to
Eocene intrusive activity. Mineralization type:; include
mesothermal auriferous quartz veins (such as those at
Bralorne-Pioneer and Elizabeth-Yalakom), as well as veins,
disseminations and stockworks of molybdenum, copper and gold
along the northeast margin of the Mission Ridge Pluton. The
ultramafic Shulaps Complex contains small chromite
concentrations and has been prospected for jade,,magnesite
and chrysotile. Cinnabar occurs locally as disseminations
and veinlets near the Bridge River Fault (Schiarriza et al.,
1989)
The most important mineralization type in the area has
historically been the low-sulphide auriferous quartz veins
which were the main producers of the Bralorne-Pioneer gold
camp. Mineralization in the Bralorne-Pioneer area is
spatially related to the Bralorne augite diorite which
occurs as a number of elongated stocks situated along a
regional fault zone known as the Cadwallader Shear. The
host rock to the auriferous veins is a differentiated
diorite mass that is characterized by chlorite-talcserpentine schist along the Cadwallader shear. The shear
zone and similar plugs trend north-northwest from Bralorne.
The ore veins at Bralorne-Pioneer occupy tension fractures
that obliquely traverse the structural lens between the
Cadwallader and Fergusson faults. Most of the veins strike
eastward and dip steeply north; however, a less numerous
set, productive in the Pioneer Mine, strikes northwestward
and dips steeply west. The veins are displaced by
occasional northerly-trending faults and common:ly
anastomose.
The vein material is massive milky white quartz which is
commonly ribboned roughly parallel to the strike and dip of
the vein with sulphides, chlorite and sericite partings,
particularly in the ore shoots. Accessory vein minerals are
calcite, ankerite, siderite, scheelite and mariposite. The
quartz veins in oreshoots carry up to 3 % sulphides,
consisting of mainly pyrite and arsenopyrite with very minor
amounts of sphalerite, galena, pyrrhotite, chalcopyrite,
tetrahedrite, stibnite, molybdenite and commonly visible
native gold and gold telluride.
The oreshoots are 10 times more persistent vertically than
laterally and have generally sharp lateral cut-offs in gold
values. Average stoping widths ranged from 3 to 5 feet with
8
stopes widening as much as 20 feet at vein junctions. No
noticeable change occurs in vein mineralization over a
vertical range of over 6,000 feet. The longest and most
productive veins are up to several thousand feet long;
oreshoots varied considerably in length, but few exceeded
800 feet.
Wall rock alteration along the veins consists predominantly
of argillization, chlorization and carbonatization,
constituting envelopes of a few inches to 10 feet wide that
contain no gold.
2.2
Property Geology and Mineralization
The Yalakom claims are underlain by peridotite of the
Shulaps Ultramafic Complex intruded by irregular dioritic
porphyries, chiefly quartz diorite, probably belonging to
the Blue Creek Porphyries. The peridotite is typical of
that in the rest of the Shulaps ultrabasic compltex. Most of
it is intensely serpentinized.
porphyry on the east. The alteration of the porphyry along
parts of the zone, especially at its northern end, is due to
Smaller outcrops, some of which may be continuous with the
main masses, range in appearance from distinctly porphyritic
to equigranular, and in composition from quartz-rich diorite
to diorite. Some contain introduced quartz. Abundant white
aplite veinlets are also present.
9
e
The veins at the Elizabeth and Yalakom prospects; occur in
stocks of Blue Creek Porphyry cutting Shulaps harzburgite
(Schiarriza, 1990; Culbert & Leighton, 1989). The veins are
typically ribboned and occupy steeply dipping northerly
trending shears. Alteration along the margins i.s minimal,
consistig mainly of pyritizatization and silicification.
The veins contain visible gold and up to a few percent
sulphides (mainly arsenopyrite, pyrite and cha1c:opyrite).
Some malachite and azurite is present. Mapping by the B.C.
Ministry of Mines indicates that the Elizabeth and Yalakom
veins appear similar to the mesothermal gold v e h s at
Bralorne-Pioneer Mines (Minfile).
Historic reports suggested (White, 1957) that the No. 9 vein
is substantially narrower than the Elizabeth v e h , but is
higher grade and a greater part of its length contains gold.
More recent mapping indicates that the No. 9 vei.n is
actually a series of parallel veins rather than a single
quartz vein. Mineralization appears to be concentrated
along partings of chlorite and carbonaceous material (Gaba
et al., 1988). The best mineralized shoots were believed to
occur in places of cross fracturing and small st-rike
deflections, and the vein was reported to dip at
approximately 70° west. Alteration along the margins is
minimal and consists mainly of pyritization and
silicification.
Work in 1987 failed to intersect significant mineralization;
however, narrow quartz veins intersected below Phendler's
Zone 1 shoot suggested a probable downward extension to the
main gold-rich vein (Culbert & Leighton, 1989).
3. DRILLING PROGRAM
e
In 1990, one diamond drill hole (DDH 90-1) was drilled on
the Yalakom property to a depth of 123.7 m (406 ft.) at
235O/-4Oo.
The hole was collared 25.5 m (84 ft.) at 078O
from the No. 9 adit portal. The drill core was logged by
Michael Lancaster. The drill intersected diorite to quartz
diorite with some hornblende+/-feldspar porphyritic
sections, probably belonging to the Blue Creek Porphyries,
and some aplite dykes. These were cut by a numher of quartz
veinlets to veins (to 1.46 m maximum, avge. <2 c:m). The
quartz veins carried trace to ~ 0 . 5 %pyrite, with sporadic
traces of chalcopyrite, molybenite or arsenopyrj-te ( ? ) . A
few veins showed dusty black sulphide ribboning along the
contact with the host rock. Some calcite veining was also
noted. Minor alteration includes kaolinization,
argillization and limonitic staining. A total of 27 samples
10
were taken of the quartz and sent for gold analysis (Fire
Assay-AAS) (See Appendices I, 11). Most sample:; returned
values of <0.002 oz/ton, with some values up to 0.059 oz/ton
over 1.49 m (2.02 g/tonne - Sample 1837). There does not
appear to be any obvious correlation between go:Ld content
and sulphide content. The anomalous values are concentrated
towards the bottom of the hole (Samples 1830-1838, taken
between 97.69-118.26 m), and appear to be equivalent to
Phendler's Zone 1. While the values obtained are lower than
those previously obtained, they still indicate the presence
of anomalous gold mineralization at depth.
4. CONCLUSIONS AND'RECOMMENDATIONS
The Yalakom property, located 40 km northeast o f the
Bralorne gold camp in southeast B.C., consists of eight
reverted crown grants and two metric four-post claims.
Gold-bearing float Led to the uncovering of a gold-bearing
quartz vein system, investigated in 1949 to 1950 by
drifting. Work in 1982 and 1983 indicated reserves of over
4000 tons with an average diluted grade of 0.77 oz. per ton
in three zones. Drilling in 1987 failed to intersect the
system.
A single drill hole in 1990 apparently intersected Zone 1 of
the mineralized quartz vein system. Values obtained within
the zone ranged from 0.006 to 0.59 oz. per ton (over 4.9
ft., or 1.49 m). While values are lower than previously
obtained, they are still important as an indication of
continued gold mineralization at depth.
Future w+rk should target the extension of Zone 1 at depth.
Phendler's Zones 2 and 3 have yet to be investigated by
drilling and should also be targeted.
1
11
5 . REFERENCES
B.C. Minister of Mines Annual Reports, 1946, 1949, 1950.
Culbert, R.R. and Leighton, D.G. (1989). Repori: on the
Yalakom Property for Balsam Resources Inc. Revised
October, 1989.
Culbert, R.R. and Leighton, D.G. (1986). Reporl: on the
Yalakom Property for Southern Lights Resources Ltd.
Revised February 6, 1987.
Karchmar, Ken, and Sorbara, J. Paul (August 1987). Report
on the AU-1, 2 and 3 Mineral Claims, Lillooet Mining
Division, British Columbia. Company report for
Petroflame International Resources Ltd.
Lancaster, M.F. and Hardy, J.L. (1987). Report on the
Yalakom Gold Property for Balsam Resources Inc. July
10.
Private company report.
Phendler, R.W. (1979). Report on Yalakom and Mix claim
Groups, Lillooet Mining Division, B.C. Priivate company
report.
Phendler, R.W. (1980). Report on Yalakom Claim Group,
Lillooet Mining Division, B.C. October 15,, Private
company report.
Phendler, R.W. (1982). Report on the Yalakom Gold Property,
Lillooet Mining Division, for Southern Lights Resources
Ltd. December 20. Private company report,,
Phendler, R.W. (1982). Report on Diamond Drill Program on
Yalakom Claims of Southern Lights Resources, October
20. Private company report.
Phendler, R.W.. (1983). Sampling program - Yalakom Property,
B.C. August 22. Private company report.
Phendler, R.W. (1984). Report on 1984 Drilling Program,
Yalakom Property, B.C. Private company report.
Schiarriza, P., Gaba, R.G., Glover, J.K., Garveir, J.I.
(1989). Geology and Mineral Occurrences of the
Tyaughton Creek Area. In B.C.E.M.P.R. Geological
Fieldwork, Paper 1989-1.
Schiarriza, P., Gaba, R.G., Coleman, M., Garver,,J.I.,
Glover, J.K. (1990). Geological and Mineral
Occurrences of the Yalakom River Area. In B.C.E.M.P.R.
Geological Fieldwork, Paper 1990-1.
12
Thompson, R.M. (1957). Letter Report on Elizabeth & No. 9
Property. September 23. Private company report.
White, W.H. (1957). Production and Exploration
Possibilities
No. 9 Vein
(Yalakom), September 29.
Private company report.
-
-
13
a
6. CERTIFICATE OF QUALIFICATIONS
I, D. G. Leighton, hereby certify that:
1.
I am a Professional Geologist with offices at 3155 West
12th Avenue, Vancouver, B.C.
2.
I am a graduate of the University of British Columbia,
B.Sc. (1968).
3.
I have practiced mining exploration for twenty-six
years, most of which was based in British Columbia.
4.
I am a member (Fellow) in good standing of the
Geological Association of Canada.
5.
I have no interests, directly or indirectlly, in the
properties or securities of Balsam Resources Inc.
6.
I have personally visited the Yalakom property, on
which this report is based, and supervised the most
recent phase of work carried out.
Dated at Vancouver, British Columbia, this
GB-A-L
,
1990.
D. G. Leighton, B.Sc., F.G.A.C.
3-a
day of
14
7 . STATEMENT OF COSTS
Labour
Geologist, 5 days at $250/day
(Between August 14-24, 1990)
$ 1,250
costs
Drilling
406' at $40/ft.
Site Preparation
S amp 1ing
3 1 samples @ $12.75
Freight/Supplies
Drafting, etc.
$16,240
5,000
395
500
2,000
$25,385
Overhead 10%
TOTAL
2.538
$27,923
APPENDIX I
DRILL LOGS
YALAKOM PROPERTY
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I
-
- - - ............
..
.
-_... . .
..........
.....
. . . . . . .
.
. . .- . . . . . . .
...
.......
. . . .
-
......
.
i
~
.
. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .
~
.................
,
.
- . . . -.
. . . . . . . . . . . . . . .
........
.
. . . . . . . . . . .
. . . . . . .
. . .
.....
...........
....
. . .
..-
.
. .
. . . . . . . . . . . __--.
.__
...
..
. .
..... -. ... .-
.-.
--
.
. .-
~
.-
...
..
-.
...
APPENDIX I1
ASSAYS
YALAKOM PROPERTY
To:
. .. .
CONSOLIDATEDBALSAM RESOURCES INC.
6017 LARCH ST.
VANCOUVER, B.C.
V6M 4E5
Comments:
Projaa
:
CERTIFICATE OF ANALYSIS
SANPLE
DESCRIPTION
1809
1810
1811
1812
1813
PREP
CODE
201
201
201
201
1814
201
201
1.815
1816
1817
1818
201
201
201
201
1819
1820
1821
1822
1823
1824
294
294
294
294
294
(Au
oz/T
I
I
<
0.002
<
0.002
0.002
<
<
<
0.002
0.002
201
201
201
201
201
201
201
201
201
201
1829
1830
1831
1832
1833
1834
201
201
201
201
201
201
201
201
201
201
1839
201
0.014
0.020
0.026
0.006
--I--
1
1
1
Page Number : 1
.
TotalPages:
Inmice Date: 23AUG-90
I
Inmice No. : I-9021086
P.O. Number :
A9021086
i
e
To: CONSOLIDATED BALSAM RESOURCES INC
Chemex Labs Ltd.
B.C.
6017
VANCOUVER,
LARCH ST.
Analyucal Chemtsrs .Geochemists * Regtslered Assayers
V6M 4E5
212 Brooksbank Ave North Vancouver
British Columbia, Caiada V7J 2C1
PHONE 604-984-0221
. .
I
CERTIFICATE
Comments:’
A9021 086
CONSOUDATED BALSAM RESOURCES INC
Project:
ANALYTICAL PROCEDURES
:HEMEX
CODE
UMBEI
9MPLE
DESCRIPTION
P.O. # :
Samples submitted t o our lab i n Vancouver, BC.
This report was p r i n t e d on 23-AUG-90.
A9021086
398
SAMPLE PREPARATION
DESCRIPTION
Assay r i n g t o approx 150 mesh
Crush and s p l i t (0-10 pounds)
-
31
iu o z / l :
1/2 a s s a y ton
METHOD
FA-=
DETECT04
LIMIT
0.002
UPPEF
LIMm
20.00