l r he 'tl - ontario
TRANSCRIPT
DIAMOND DRILLING of the OPAP PIPE
SHARPE LAKE PROJECT
DIST, of TEMISKAMING ONTARIO
for
CONSOLIDATED PINE CHANNEL GOLD CORP.
l R he 'Tl
lain F. Downie P. Eng.. Thunder Bay, Ontario January 1998
31M05NE01752 18072 BUCKE 010
CONTENTS
LOCATION MAP l - includes property and basic ddh location map Scale about 1:35 M
LOCATION MAP II
INTRODUCTION
LOCATION AND ACCESS
PROPERTY
HISTORY
REGIONAL GEOLOGY
DIAMOND DRILLING AND PROCESSING
D.D. SUMMARY
MAP "A" - ddh. locations, ci. 118550
MAP "B" - ddh. location, ci. 1186973
NOTES
SUMMARY
CONCLUSIONS
STATEMENT OF EXPENDITURES
NOTES
APPENDIX I
APPENDIX II
Scale 1:14 630
Page l
Page l
Page 2
Page 2
Page 3
Page 4
PageS
Scalel:4K
Scale 1:4K
PageS
Page 8
PageS
Page 9
Page 9
d.d.h. logs, samples and sections
microprobe results
31M05NE0175 2.18072 BUCKE 010C
A Bucke Twp.
1 Lac Gfandin Proj.
2 Labrish Lake Proj..
Location Map I
- t
INTRODUCTION
Definition drilling of the OPAP Pipe is discussed. The work was carried out on behalf
of CONS. PIPE CHANNEL GOLD CORP..
The programme followed the signing of an option with holders of the lands to explore
the OPAP Pipe in the spring of 1995, subsequent land acquisition in the immediate area, an
airborne magnetic survey of Firstbrook Twp. Ont., and a programme of line-cutting and ground
magnetics on selected air'magnetic targets including the OPAP Pipe.
The work and this report were undertaken and completed with the knowledge and
approval of D. Hoffrnan, Pres. of Cons. Pine Channel.
LOCATION and ACCESS
Firstbrook and Bucke Twps. lie on the west side of Lake Temiskaming, Ontario. This
is at about 47 0 30*N. and 79 0 45'W. some 180 km. N. Of North Bay, Ontario.
Highway No. 11 runs N.-S. through Bucke Twp., and a number of Lot and Concession
roads, general access roads and tote roads render accessibility to most properties a formality,
with very little need to create "typical", bush road access except for a very few hundreds of
metres in rare instances.
PROPERTY
The property consists of two claims in Bucke Twp.:
CI. 1118550 N/2 LOT1. CONC. 4. andW/2.N/2 LOT 2. CONC. 4. 96 Ha
C2. 1186973 SE74,N72 LOT 2. CONC.4. 16 Ha
TOTAL 112 Ha
HISTORY
The OPAP Pipe lies within the Temiskaming Kimberlite Field, itself the southern part
of the larger Kirkland Lake - Temiskaming kimberlite province. Prior to Cons. Pine Channel
work, this field contained at least six (6) known kimberlite occurences: The Guiges, Nedelec
and Border occurences in Quebec, and the Bucke, Gravel and OPAP occurences in the area
of Hwy 11 adjacent to Haileybury and New Liskeard.
The area was flown by Monopros in 1982 and the anomaly over the Bucke Pipe
identified. Ground work further defined the anomaly but a diamond drill hole intersected
diabase under 41m. of overburden: the claims were abandoned. (Asses. Rpt 2.614-2).
Lac Minerals then acquired the ground (1984) and drilled a hole which intersected
kimberlite at 41 m. and continued in kimberlite until the hole was stopped at 346.5 m.. Later,
early 90's, KWG conducted work on the pipe, and it is believed that a diamond grade of
30C./100T. has been achieved. It is also believed that the stones show considerable resorption.
The Gravel Pipe, about 1km. To the e.s.e. was discovered and tested by Vera Cruz.
605kg. of K. from five drill holes returned only three micro'diamonds and four macro'diamonds.
John Ewanchuk and Keith Barron had a mutual interest in the area and joined forces to
acquire a land package (with R.L. Barnett) that was optioned to Bethlehem Resources in 1992.
Airmagnetics defined a number of anomalies: sk were drilled and no kimberlite encountered.
The holdings and data were returned to the partners. Eventually J. Ewanchuk, with funds from
an OPAP grant, drilled a short hole into the anomaly - the OPAP Pipe is the result, and the option
to Consolidated Pine Channel.
With the option came access to the air'mag survey of Bucke Twp., and a fairly complete
land - holding package was amassed to cover most of the "interesting" air'magnetic anomalies.
Further, a new air'mag was flown over Firstbrook Twp. and some new anomalies acquired;
unfortunately, none of these is too exciting.
REGIONAL GEOLOGY
The area is part of the Abitibi sub'province of the Superior Province of the Canadian
Shield. The Archean basement is about 2.7 b.y. and comprises metavolcanics (greenstones),
typical granite/gneiss shield rocks, and some sedimentary units.
The predominant structure is the NNW-SSE trending Temiskaming Graben which
contains most of the local Paleozoic carbonates as well as playing host to Lake Temiskaming.
The known kimberlite occurences lie along the flanks of this structure, although that may be
simply a function of the lack of overlaying, late debris, and the consequent ease of exploration.
DIAMOND DRILLING
The OPAP Pipe, a heterolithic, volcaniclastic diatreme - facies kimberlite breccia was
tested by sk d.d.h.'s for a total of 747m.. Of this 651.35m. is kimberlite. The 6.75m. of
kimberlite from OPAP-1 is retained for reference - it is extremely friable or rotten; it is of interest
as it lies under a cap of sts/arg. (Pre-Cambrian), is a diatreme - facies BX., and contains carb,
frags (Paleozoic); this latter is indicative of at least two, explosive, mixing events; the last failed
to dislodge the cap rock at the s. w. margin of the pipe, and caused some stoping under it. The
rock is described in detail in accompanying drill hole logs. (App.l)
The average S.G. of kimberlite from holes OPAP-2 to 5 inclus. Is just under 3.0 - 560m.
and 1565kg.. The rock in OPAP-6 is extremely friable and much was "ground" in drilling: the
"apparent" S.G. is about 2.0 -86m. and 175kg..
Drilling commenced early in Oct. 1995 and was completed early Nov. 1995.
D.D. SUMMARY
DDK No./ CO'ORDS AZ./ DEPTH START/END NOTES GRID___________DIP CASINCrm.)
AREA
OPAP-1 A
OPAP-2A
OPAP-3 A
OPAP-4 A
OPAP-5 A
OPAP-6A
3+50S1+45W
2+75S 0+95W
2+50S 0+25W
1+80S0+25W
1+80S 0+65E
1+80S1+25 W
N.A. -90
N.A. -90
N.A. -90
N.A. -90
N.A. -90
315 0-55 0
30.8/19.5 T.W./I.D.
149.65/17.35 T.W./I.D.
158.8/17.44 T.W./I.D.
157.25/11.44 T.W./I.D.
154.2/15.25 T.W./I.D.
96.0/7.9 I.D.
95-10-02 95-10-04
95-10-05 95-10-06
95-10-06 95-10-08
95-10-09 95-10-10
95-10-10 95-10-12
95-11-02 95-11-04
STS/ARG-24.05 K. Bx.-30.8
HVK. Bx.
PHVK. Bx
MPHVK. Bx.
MHVK. Bx.
HVKBx.-93.9 STS/ARG-96.0
SW/4N/2 LOT 2 RGB 4
SAME AS OPAP-1
SAME AS OPAP-1
SAME AS OPAP-1
CL. 11 86973
SAME AS OPAP-1
(r no. l
O
lo
CI, 1186973se/^n/2, lot 2,cone.4
Co rf f.
ef.ef. e'f/k - d. 4. h. o PS? P-
-j,
3 W c!
\(
Cb
Only OPAP-2 was tested with a magnetic susceptibility meter due to the failure of the
unit. Magnetism is not strong, but all core would attract a magnet from a few mm. away, and
in the odd spot from about lcm., and appears to be "normally" magnetised.
The magnetic anomaly recovered by a ground survey is a "negative"; considering the
"normal" magnetism of the rock. The ground signature may be attributed to the feet that the
kimberlite is in a "hole", and the surrounding, higher outcrop of sediments (magnetic on bedding
planes) and diabase are more magnetic than the diatreme rocks. However, it is possible that the
body as a whole retains and exhibits remanence.
As each hole was completed, with the exception of OPAP-1, a composite sample
(10-15cm. every 2-5m.) was taken: these are samples VR11458A - VR11462A for holes
OPAP-2 to -6 respectively.
These samples were submitted to Kennecott Canada Inc. for processing at the
laboratory in Thunder Bay, Ont. Processing consists of crushing to -1mm., screening to two
fractions (0.25-0.5mm. and 0.5-lmm.), magnetic separation in a rolls magnetic separator to
remove manetic material, concentration in a heavy liquid (Sodium poly-tungstate:S.G. ~ 2.95),
retrieval and washing of concentrates ^2.95 S.G.).
The resulting samples are observed under microscope and picked for any minerals of
the following; garnets, chromites, ilmenites, clino'pyroxene (chrome diopside), orthopyroxene
(enstatic) and olivine. The "picks" are then subject to a further (representative) selection and
these are submitted to R.L. Barnett for microprobe analyses.
Final picks are as follows:
SAMP. NO PYROPE ECLOG.GT. CPX OPX CHROM. OLIV. TOTAL
VR11458A
VR11459A
VR11460A
VR11461A
VR11462A
e.g. composite
40
24
36
41
41
44
226
14
4 11
16
1 20
15
5 76
13
7
10
21
10
61
28
23
21
31
24
127
1 96
69
83
9 123
10 100
44
20 515
These pyropes generally are G.9. garnets (macrocryst suite) with only three (3) of 226
creeping into the diamond stability field. Eclogitic pyrope is typical upper mantle. Chrome
diopside lies largely within the diamond stability field (or along it's margins) -. the exception
in this survey. Olivine and orthopyroxene are typical macrocryst suite or uper mantle. Chromite
is typical upper mantle with but three (3) of 127 edging into the diamond stability field.
These results suggest that the OPAP Pipe could be diamondiferous, although the
apparent (?) lack of ilmenite suggests that it may be rich enough in iron to have passed into the
"mags" upon magnetic separation, possibly hinting at strong resorption.
Given the location of the pipe, its quite good size, and relatively shallow depth, even a low
content of low value stones could make this of occurrence of no small interest.
NOTES:
i) The core was sampled - put in buckets, four to a sample and 25kg. per bucket.
ii) Four 50kg. (1/2 samples) lots from holes OPAP-2 to -5 inclusive were forwarded to
Vancouver. It is the author's understanding that the balance is in storage at the
facilities of Devex Exploration in La Ronge, SK.,
iii) It is understood that the two samples each for fusion were submitted to de Beers
(sent to RSA?) and to Lakefield laboratories. It is further understood that no
diamonds were recovered at either facility.
SUMMARY
Six diamond drill holes were drilled on the OPAP kimberlite in Oct.(Nov.) 1995.
Indicator mineral chemistry suggested that there were some hope of recovering diamonds.
(Supposed?) attempts at diamond recovery reportedly failed to return any stones.
CONCLUSIONS
It would appear that the OPAP Pipe is non-diamondiferous. However, all fusion
samples came from the first samples in the holes tested - the upper part of the pipe - and so it
would appear that with so much material remaining ^1.2 tonnes?) that some tests of deeper
material may be worthwhile.
Res
lain F. Downie, P.Eng., Ont
STATEMENT OF EXPENDITURES
COST OF DIAMOND DRILLING: 747m. at S73.007m. 54 531.00
Mob. and de mob. 2 000.00
Cost of buckets: 68 at S4.007bucket 272.00 (core trays were recovered (?) and are reuseable)
GEOLOGIST: supervision 15000.00
SUBSEQUENT reports and supervision (samples/lab) 2 500.00
Transportation: one month truck rental plus fiiel (est. 4200km. at 40c7km.) l 680.00
Accommodation and meals for 35 days l 730.00
Laboratory treatment for HM concentrates
5 samples at S750.007sample 3 750.00
5 samples picked at S250.007sample l 250.00
Final selections for probe 515 grains at S4.007grain 2 060.00
515 microprobe analysis at S12.00/grain 6 180.00
TOTAL 90 953.00
NOTES:
i) Devex is a subsiduary of CONS. PINE CHANNEL and so costs are not easily realised.
However, other contracts overseen by the author saw prices vary from S69.007m. to S83.007m. at
the time. I am sure that CONS. PINE CHANNEL/DEVEX can justify the "contract" estimate
used.
ii) Mob. and de mob. are pro-rata ( and probably low) as other targets were drilled - the
actual cost from La Ronge and back is probably in the region of S8-10K.
iii) The rates for laboratory are Kennecott standard, and can be verified, as can the rates
for microprobe analysis.
Respectfully,
Distribution of costs: 20.6407o to CI. 1186973 79.3607o to CI. 1118350
I, lain F. Downie, resident at 2035 Montrose Place, in the city of Thunder Bay, Ontario,
declare that
i) I am a graduate of the University of Toronto having obtained a B.A.Sc.(Geology)
from the Faculty of Applied Science and Engineering in 1962.
ii) I am a member in good standing of Professional Engineers Ontario and have been
continuously since graduation.
iii) I am a practising exploration geologist and that I have practised continously since
1962, the last five years as a consultant primarily to diamond companies.
iv) I hold no interest of any kind, direct of indirect, in this property and I do not expect
to receive any such interest or payment above my normal fees.
lain F. Downie P.Eng.Ont.
APPENDIX I
CONSOLIDATED PINE CHANNEL DRILL LOG
DDK NO. CO'ORDS
DEPTH
:OPAP-1 13+503 1+45W :30.80m.
PROJECT AZIM DIP CORE
/(X
-.SHARPE LAKE, ON:N.A. START:95-10-2:-90 :BGM
END : 95-10-4 CLAIMrSW/4 N/2 LOT 2 RGB 4 BUCKE TWP.
O - 19.5
19.5 - 24.05
24.05 - 29.55
29.55 - 30.80
30.80
Casing
Arkosic Sandstone - Siltstone - Argillite apparently shattered in situ: clay-filled fractures.bedding essentially across the core, kimberlite in fractures: 21.95; 23.45 - 24.65
Heterolithic, Volcaniclastic K. Bx.. rotten, friable but containing autoliths, and xenoliths of overlying seds., argillite, greywacke, diabase, gneiss, and rare carbonate frags,(pebble-size, angular).
The carb, frags under the Proterozoic Cap indicate a prior eruption (at least one) to bring the younger rocks back into the diatreme, and a later eruption mixing with the older deposit and failing to broach the Proterozoic rock near its margin.
Clay/(K. Bx.)probably major water influx from surface bringing clay down and mixing with the rotten K.. The fine mud plus K. "blocks" probably indicates proximity to diatreme wall.
E.O.H.
lain F. Downie, P. Eng.
CONSOLIDATED PINE CHANNEL DRILL LOG
DDK NO. CO'ORDS
DEPTH
: OPAP-2 I2+75S 0+95W :149.65
PROJECT : SHARPE LAKE, ONAZIM :N.A. START: 95-10-5DIP :-90CORE :BGM
END : 95-10-6 CLAIM iSW/4 N/2
M k 4C U~ctf
LOT 2 RGE 4BUCKE TWP.
O - 17.35
3.0 - 17.35
17.35 - 149.65
Casing
Casing: Boulder Till - mixed bag of boulders.
Heterolithic, Volcaniclastic K. Ex.. a massive or uniform appearing gray rock. an almost uniform mix of Pre-Cambrian and Paleozoic rocks . Pre-Cambrian gneiss , granite, diorite, diabase, arkosic siltstone, argillite (uncommon), greywacke predominate; with arkosic siltstone/f ine sandstone having the highest frequency. Cobalt conglomerate is noted - pebbles in fine matrix as cobble size clasts .
Generally the smaller, more angular frags, are most common and the Pre-Cambrian ones dominate. Larger frags, are more rounded and comprised mainly of carbonate rocks. Carb. and Db. frags, to 7cm. are observed: carb, is limestone and/or dolomite - both are buff in colour and may be fossilif erous .
The carb, frags, are often serpentinised with a rim of lighter material a few mm. thick around a finer band of green, translucent serpentine a few mm. thick within this and next to "fresh" carbonate.
Calcite veining is common at high angles to the c .a. .under a lens it can be seen that the "matrix" also contains a fine, xenolithic content - usually tiny frags, of gray/green siltstone down to and under 1mm. in diameter. K. often comprises less than 50 !fc of the rock and always less than 65%.
The K. is of at least three (?) generations: autoliths a) rare clasts, angular, of medium to dark gray K. with microcrysts and rare microphenocrysts (of olivine?), b) a gray/green, very f.g. K. with microcrysts and occasional microphenocrysts of olivine: these clasts are usually sub'angular, c) a brown, v.f.g. K. with macro- to microcrysts and rare microphenocrysts. Perfectly round (spherical?) ones are noted (< l cm. generally) but no concentric foliation is seen. Quite angular ones ( < 2 .5cm.) contain micro to fine ( < 4mm.) macrocrysts; some of the latter are broken at the rim of the clast, or protruding from it. These forms may indicate two generations from a single magma.
The matrix is cryptocrystalline, gray and contains numerous macro and microcrysts of serpentine: larger macros contain fresh olivine in a matrix of dark brown serpentine (? - and mica?), and larger still contain olivine in a cocoon of serpentine and often magnetite formed in the "typical" olivine parting. Macros > 0.5cm. are not common.
There are autoliths with xenoliths (cores??) and smaller, sparse pelletal lapilli. In addition there are fresh olivine micro-Xmacrocrysts, presumably the result of disaggregation of larger macros. INDICATORS: - one tiny C.D. ( < 172mm.) in an autolith.very few pyropes - macros of highly altered material: very fine red to purple matter in an aphanitic, creamy matrix, usually entirely within a kelyphitic rim.some opagues too small to identify - probably magnetite. rare small macros of phlogopite.
The entire rock is strongly magnetic - normal magnetism.
149.65 E.O.H.
lain F. Downie P. Eng.
DDK NO. CO'ORDS
DEPTH
:OPAP-3 -.2+408 0+25W
: 158. 8m.
CONSOLIDATED PINE CHANNEL DRILL LOG
PROJECT : SHARPE LAKE, ONAZIM :N.A. START: 95-10-6DIP :-90 END : 95-10-8CORE :BGM CLAIM: SW/4 N/2
4
O - 17.4
17.4 - 118
Casing
Pelletal-textured, Heterolithic, Volcaniclastic K. Bx.
- immediate impression is that this is like OPAP-2 .- the rock is a slightly darker gray; there are fewer
(?) carb, xenoliths, but they are larger (2 exceed 30 cm.) and some exhibit the serpentine alteration noted in OPAP-2. P. C. xenoliths are as numerous as in OPAP-3 and roughly similar in size, but larger rounded ones are generally absent, and angular ones to 4cm. are present, some obviously (?) are derived from pebble/cobble conglomerate.
Generalisation: angularity decreases assize increases.
- carb, veining is lower in content, but varies greatly in attitude - to sub parallel to c. a..
- closer examination reveals a distinct greenish cast on the gray.
- there are more small, dark argillite frags, and fewer ss/sts . .
- occasional, tabular (angular) clasts of carb, are seen.
- the matrix is weakly calcitic locally.Macrocrysts of fresh to
serpentinised olivine are common sub 'angular rather than sub 'rounded. megacrysts are present, but macros are predominant and usually < !X2cm. .
- there are rare fine macros of phlogopite.Most noteworthy is that the brown K. of OPAP-2
is now quite prominent. Oval or round (to rare amoeboid) lapilli are more common and autoliths, attain sizes of > 2.5cm. - the smaller ones ( < 172cm.) are usually angular. Macro-rich clasts are common; micros are very common and microphenocrysts are rare.
completelybut are
Occasional
Some round lapilli (?) exhibit a faintly concentric foliation. Again round and angular forms may suggest two events from a single magma.
"Gray" K. autoliths are rare and all noted are angular and micro- to finely macrocrystal with rare microphenocrysts.
The gray-green K. is not noted.Partial mantles of brown K. on macros and
lapilli are not uncommon.The more one sees, the more one suspects that
the brown K. may be part and parcel of the final eruptive event with small, angular clasts forming from the larger, preexisting autoliths.
118-135 As Above - Variation on a theme- contains more frequently occurring large carb. -
and P.C. xenoliths: P.C. ones are common.
135 - 158.8 As for 17.4 - 118- at 138.7 a dykelet (6-8cm.) of brown K. containing
micros, macros and megacrysts of olivine and fresh olivine (including laths) developed from disaggregation of the aforementioned macros and megas. Rare microphenocrysts are seen.
- indicators are noteworthy for being absent.- the rock is strongly and "normally" magnetic.
158.8 E.O.H.
lain F. Downie P. Eng,
CONSOLIDATED PINE CHANNEL DRILL LOG
DDK NO. :OPAP-4 PROJECT :SHARPE LAKE, ONCO'ORDS rl+803 AZIM :N.A. START:95-10-9
0+25W DIP :-90 END :95-10-10 DEPTH :157.3m. CORE :BGM CLAIM:SWX4 NX2
/V. Bi**A* T^3- LOT 2 RGB 4BUCKE TWP.
O - 11.4 Casing - boulders of ss/sts and one of Is..
11.4 - 41.5 Macrocrystal, Pelletal-textured, Heterolithic, Volcaniclastic K. Bx..
- chaotic, heterolithic bx..- xenoliths vary from mm. scale to cm. scale with most in the 0.5 - 2.0cm. range. P. C. fragments outnumber Paleozoic carb, frags. 3:1 and xenoliths form 35%+X- of rock. Carb, clasts exhibit reaction rims with a band of dark green serpentine marking the limit of inward penetration.
- angular frags, tend to be small and increasing size co'incides with decreasing angularity.
-K. is formed of gray microcrystalXmacrocrystal matrix: the mesostasis in cryptocrystalline and presumably of serpentine with mere traces of calcite.
- macrocrystsXmicrocrysts are of olivine or their serpentinised pseudomorph^: some have lighter rims (< l X2mm) St some are partially or wholly mantled by brown K. (see later in text). Microphenocrysts are noted, but rare. Gold glints may indicate the presence of phlogopite (v.f.g.).
- magnetite is common in macrocrysts of olivine and the whole rock is quite magnetic.
- K. clasts - autoliths - and lapilliXglobular aggregates are common: gray and greenish gray autoliths are small ( < 0 .5cm. generally) and uncommon, and tend to be sub'rounded to angular. Brown microcrystal (rarely microphenocrystal) K. is formed as clasts varying from < 2mm. to several cm. - clasts exceeding lcm. are uncommon and those < 0.5cm. predominate. The matrix of the Brown K. is calcitic, cryptocrystalline - probably(?) finely phlogopitic - with micros and microphenos of olivineXserpentine. Macrocrysts are uncommon and rarely > 0.3cm. Pelletal lapilli are uncommon and form on small macros of olivine or xenoliths.
- a pronounced system of white calciteXgypsum (anhydrite?) stringersXveinlets is ubiquitous across the core.
41.5 - 104 As Above - Variation on a theme.- no sharp change; a vague but noticeable variation:
it is slightly less chaotic - frags, are smaller, and carb, clasts less common, or at least less prominent.
- occasional, large autoliths of Brown K. (see preceding) are micro/macrocrystal ( < 3mm.) to 4x3cm. . Lapilli to just over lcm. are noted - usually on olivine macrocrysts.
- small, angular to rounded autoliths of Brown K. are common, gray K. autoliths guite uncommon.
- olivine, fresh - but generally serpentinised; and angular to sub'rounded frags, of fresh olivine are ubiguitous - presumably from shattered larger macros which exhibit typical olivine parting with serp./mag. around fresh olivine.
- calcite/gypsum veining is less regular and at random orientation -42.9 lcm. dykelet of Brown K. at 30 degrees to c.a..
- carb, clasts exhibit alteration rim with inner ring of dark green serpentine.
- angular clasts (. 5cm.) of conglomerate (pebble) are seen. 49.5 - 49.5 - Brown K. dykelet sub'parallel to c.a.
- 56.0 - 56.5 - slightly finer phase, coarsening downward may indicate the top of a "bed". 63.4 - a large autolith or a dykelet ( > 1 0cm.) of Brown K. in friable matrix.64.4 - 64.8 - part of a dyke (let) of f. Brown K. parallel to c.a..67.45 - 68.3 - 5cm. dykelet of Brown K. at 5 degrees to c.a..70.85 - 71.25 - again - parallel to c.a.. 79.6 - 80.2 - f. Brown K. varies from parallel to across c.a..
- 82.6 - 87.6 - another, slightly finer and less chaotic phase, lighter gray coarsening downhole - possibly a bed.87.6 downhole - coarser; larger frags, of P. C . rock; darker; less calc./gyp. veining. 94.15 - 94.7 - f. Brown K. dykelet parallel to c .a. . 95.9 - 96.1 - f. Brown K. dykelet.
- 101.15 - 101.45 - finer "bed" grading to coarser downhole.
104 - 157.3 As Above - further variation.- there is a fairly abrupt increase in size and
frequency of carb, clasts; these are generally angular and vary from mm. to dm. scale.
- again a chaotic bx.- calc./gypsum veining is more regular once more, with fewer less radical departures from across the core. They vary from mm. to lcm. scale. 118.2 - 120.2 - f. Brown K. dykelet subparallel to c . a. .
157.3 E .O.H.
lain F. Downie P.Eng.
CONSOLIDATED PINE CHANNEL DRILL LOG
DDK NO. CO'ORDS
DEPTH
:OPAP-5 rl+SOS 0+65E :154.25m.
PROJECTAZIMDIP
CORE
:SHARPE LAKE,:N.A.:-90
:BGM
ONSTART:95-10-JO END :95-10-12 CLAIM:1186973
UIW73
O - 15.25
15.25 - 154.25
Casing
Macrocrystal Bx. .15.25 - 18.3 18.3 - 21.35 21.35 - 23.2
Heterolithic, Volcaniclastic K.
recovery recovery
80% recovery typical of previous holes; weathered, friable at surface.gray, serpentinitic, matrix with tnacrocrysts of olivine and its serpentinised pseudomorphs that range from angular to quite rounded, contains autoliths of dark gray K. with micro- and fine macrocrysts of olivine/serp. plus rounded (to amoeboid) to quite angular autoliths of Brown K. ranging from (few) mm. scale to > 3cm..pelletal lapilli are sparse to absent, chaotic bx. with P.C. xenoliths: gneiss/granite, diabase, varied sediments; and carb, clasts. Size varies from mm. scale to > > 3cm.; average is l-2cm.. O - 48.75 marked by large cb. clasts O 4cm.)
- about one every 3m. 48.75 - 99.65 fresher with rounded to quite
angular carb. frags. rarelyexceeding 2.5cm.
99.65 - 124.05 larger carb, clasts: > 4cm. to20 cm.
124.05 - 138.7 fewer, smaller carb, clasts(< 2 .5cm.)
138.7 - 154.25 larger carb, clasts: < 15cm.) entire unit exhibits an almost complete lack of carb. veining.also note an increase in content of coarser Brown K. clasts in the areas of large carb, clasts lower in the hole.
E.O.H.
P. Eng.
CONSOLIDATED PINE CHANNEL DRILL LOG
-t * t-*-"-**''DDK NO.CO'ORDS
DEPTH(vi.
e^( ^\
:OPAP-6-.1+8081+2 5W:96.0m.
rf fj k *1 M0 1o L df f 73
PROJECTAZIMDIPCORE
f
'2. C^^ /V 2^/o E .
: SHARPE LAKE,:315:-55:BGM
d* T-Jf
ON ^START: 9 5-1 1-02END : 95-11-04CLAIM iSW/4 N/2LOT 2 RGB 4 BUCKE TWP.
O - 7.90
7.90 - 93.9
93.9 - 96.0
96.0
Casinglargely boulders of ss/sts/arg. and one large Is.
lain F. Downi
Heterolithic, Volcaniclastic K. Bx.chaotic heterolithic bx. : extremely broken/friable,especially in upper 28m.quite similar to OPAP-5, possibly a lowerxenolithic content <25% composed of Dk. Gy. Arg.^6cm.), sts/arg., diabase, gneiss/granite,carbonates ^lOcm.): generally the xenoliths arefine, varying from mm. to cm. scale, but averaging1-1.5cm.autoliths of Brown K. are quite variable in size,content and form: they seldom exceed lcm. and mostare ^.5cm.. Dark grey K. is not common but farfrom rare.white calc/gypsum veining is totally absent.rock remains rotten and apparently uniformdownhole, but minor variations could be concealedby friability.in last 12-14m. there are a number of quite, goodlysized, sts/arg. angular frags, of extreme red-brownFeO (Jasperitic) colouration.olivine macros are fine and micros ubiquitous -often dark, serpentinitic.phlogopite occurs as uncommon small macrocrysts.ilmenite is rareno garnet or C.D. is seen.L.C. at 55 degrees to c.a. across bedding below.
Gray Lamellar Sts/Arg.bedding at 30-35 degrees to c.a.
E.O.H.
Dip Collar: -5645.7: -5391.45: -51
Dip of diatreme wall 75 degrees.
P. Eng.
100 kg. samples have 25 kg./pail 48 kg. samples have 24 kg./pail
DDK - OPAP-2-95
SAMPLERSH-2-1 SH-2-2 SH-2-3 SH-2-4
METERAGE SAMPLE SIZE (KG)17.37-52.4 52.4-86.9 86.9-124.5 124.5-155.75
100 100 100
- 50 kg. to Vancouver
364 Kg.
100 kg. samples have 25 kg./pail 48 kg. samples have 24 kg./pail
DDH - OPAP-3-95
SAMPLERSH-3-1 SH-3-2 SH-3-3 SH-3-4
METERAGE SAMPLE SIZE (KG)17.5-52.5 52.5-87.5 87.5-122.5 122.5-158.8
100 100 100 100
-50 kg. to Vancouver
400 Kg.
100 kg. samples have 25 kg./pail 48 kg. samples have 24 kg./pail
DDK - OPAP-4-95
SAMPLERSH-4-1 SH-4-2 SH-4-3 SH-4-4
METERAGE SAMPLE SIZE (KG)11.4-49.0 49.0-88.1 88 .1-124.2 124.2-157.28
100 100 100
- 50 kg. to Vancouver
383.4 Kg.
100 kg. samples have 25 kg./pail 48 kg. samples have 24 kg./pail
DDK - OPAP-5-95
SAMPLERSH-5-1 SH-5-2 SH-5-3 SH-5-4
METERAGE SAMPLE SIZE (KG)15.25-65.2 65.2-102.3 102.3-139.34 139.34-154.2
100 100 100-J!!
- 50 kg. to Vancouver
343 kg.
100 kg. samples have 25 kg./pail 48 kg. samples have 24 kg./pail
DDK - OPAP-6-95
_____SAMPLEfl_______METERAGE______SAMPLE SIZE (KG) SH-11-1 8.53-61.0 100 SH-11-2 61.0-93.9 75
175 kg.
'XL
***
'T*u
r#
f.-*at#
it0•T:/o
——
— — ' —
——
——
——
——
——
— 7
——
j-t — -j-^ —
——
— x —
~ ——
—
—
9t!s ——
— f.
*y ^y
^y^/^
^z/
^*z**t s W
|
eTfx e
^ ^J
I J
r
VI l
l
APPENDIX H
F.L. BHFMETT 'JEO 519 C-52 1475 12-01-V5 t'2:44PH C 25] tt l
2- l
GARNET - KENNECOTT CANADASAMPLE VR11462A
wt % CaO
o RLB
P.L. BHRNETT GEOLCG. IS 652 1475 12-01-95 02:45PM [25]
CHROME DIOPSIDE - KENNECOTT CANADA 6AMPLC VR114C&A
o.u
4 c -1 o
4 O-1•ri v
" "i * -o 3-5^ 30-^ w.U
0 2 S Jt.. O
n^ j* j±^ 2 .0
J 1.5-1.0-
0.5-
rt ft
-^
/l
^"
f-X
,-r^—r
^
— -
-^—
i\^
N
\\
\
s. *\-^-e
</ o
*-~fc^
?\o
- M 1
os-^ou
^X'
^
10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26
wt CaO
RLB
R.L. BHFMETT GEOLOG. 5i9 652 1475 12-01-^5 *2:45FM [25] 83
70
66 -
w Diamond InclusionO62-
ML.
O 58
50
46
CHROMITE - KENNECOTT CANADA SAMPLE VR11462A
l ^ ! ' l
o o00
oi . i - i . i . i . t fr t . i . i iO 2 4 6 8 10 12 14 16 18 20
wt *fc MgO
o RLB
R.L. BHFJETT GEOLOG. si;- c52 1475 12-01-9? 02:46PM [25] 84
70
60
d60M
Q40
#30
10
CHROMITE - KENNECOTT CANADA SAMPLE VR11462A
r 1 ' 1 1 | i I ! -| "' 1 | l , - | l , - i
Diamond inclusion Field*v - -
1 , 1
0 o o o/\
1,1,1,1.1,1.1.
2 4 6 8 10 12 14 16 18 20
Wt 96 MgO
o RLB
wW59i' wt
t (t,
mt
000' K'i 496'
UZ'rrio'895'
WJCfl'oin
'9 000'fOO'9
SHOTin8Z'
18'il55 '5inIr'BTfO'
r/'Ir9
t OOO'fZi6i'i tlO'I
l UVtl IW
t urj Wt 509't 9(0"f
01)0' 9 ItO'
t WS
rO'OOTfi'95i'
i?'4lPt'S82'8
Zi'8150'
5iT*iL
isr T5T'w siri ooo' n t
9i6'4 rFO'I 666'4t 9rl'r ii ltd' ti W tt 2(3' ii W Ji 9ort i
900'9 000' 000'9t 900'9 i
80'OOi IIri'9 9i82' S2K'M !SSI'9 U
08'/ ^
SZ'8! li
IV li
fi'Tf frg
rrs '544i a j
OOO'tZ8rnin-*rio'sir 656'Zld'
4Wtf 00'i66'5
001}
6l
58
l]
If
UV MI'sot' url 000 'K t
900*01 tin J66'4t 500't ii Jro' tt Itll' tl 986' t1 iOO1 il lOO'f i
000'9 ilO" 000'9t i86'S t
fi'64 irif'i 38'K' Zi'8f'8I iO'8*'9 9t'C5'8 50-Zfil 91'90' 10'tfi'O? Z5'
t f
OOO'W590'!/fll'r6JO"
69fftlfTOO'HO'fTOO"
646'?
0019
M?8ei
Tt
651'881'
iSOO'OI
11t1tt
000 '9t
UITftTO50{Til0091
ot B urnim sOr t Kiniw i Or 9 WrITilll 9 Or ? WHUA 5 Or r DZ9?]TltA t O I WM18A i 8* i W9MIH J Of I Wrlisn T
W KJ/J
000 'rZion601'r00'
KfJtr 000'
580 'fISO'm '5
'OOT
L
'41 9'S'ST
'Tr
I
tit* mi own
H6'6 I/J'lt ?90'ri rso'i isrl 396'i fflO't r30'i
000'9 910't Z96'5
IT 'OOT06'9
srmiOi'9^'9
8K8Tro'
oroi
0nwnij83liIS
yIS
MS001GHhCOM
03JfOJJfOJD
Jll'lJC1S
iqidAOH '^i)Il8* 'S3SNW llOD^HH 'Mm
Hdit* :30 So-10-31 Sit'I 339 6IS '901030 11314*3 "l "d
WWi OOO'IZ
;?6'4 K!1i otnl 190't III't m'i ZOO'i zin
)0fl'9 HO'i 786 '5
ci '44U'k
orZf'4IOT ltnH'U
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91
m1i9Z'
t ooo n16ST4 ttl'
i W*i 910'i WO 'Ii Wi 000 'i otn
OQin 6NTj 154'i
?9'OOItnirtO'4lir i50 'iS*'Z266'81'U
u
w Mrw wt OM'K i 000 'H
Stt'4 i?i' IIO'Ol US'i w* t esrrj iiV t 610'i 99i' i nri zir t itr4 no' t Oifl'i ZOZ'5 t iSl't
[Z0'9 309 OOG'1* ^fl'l iW9 t fU'S
60'001 fi'J4or? is'?62' *r50'5Z ii'OZ;r? ;r?9Z'9 Ifl'iOt'8! 00 '41J!' irZ4'Tf on*
H 11
I'm 'SitI 4Z J3318M1H
Mr MI'
i 000 'HLU'i 9Z8'
j m'tt Wj W* J991s OtO'i m'i
ono'9 4ii)'i W5
10'OCIintriO'OZZ9'998':?6'6ISO'
iVUli
'W9HUA 'WM
Z9I'
nrt 000
SOO'OI 544t HZt 9!0i 5Ut ?99l 100i 01!
OGG'9 100t 464
60'001?f'9
iri9'4I5*'9Si1?
I9'tl19'
*ruu
3 1103]NHn
MI'
W'kZ i OOO'K
4IO'OI Ii4' * t 68J'f
t UO'i *U'i ftrl 500'
'f i 4Zl'fOOfl'9 010'
'S i 064'S
J9'464Z'9SZ"
58'il*rili' l91'JI10'Zt'U
31
'3dOiUd
0^ 91 W9MTHA 11 W SI DZ'HW 51 0* M W9tlW H flf CI W9HW liok zi twiiu n0^ II W9tilBH ]1 0^ 01 W W ISA 010* 4 W9HW 6
W WJ/J841' H/di OOO'K 0
SJt'6 640 I KOt 850 '^ 9Hi KO' HHt OU' lil iZO'l S3i cSfl' 11l 8U'I IS
000'9 iSO' 1*t iH'S IS
Z9'00! WS80't Ut!]JZ' DHt|08'81 33H?n 03Ji6'8 IOZ3K'ft fOZV*r ionH'U ZOiS
6
LO [53] UdSt*:~(? 5-5-10-31 Sif! 359 615 '001030
R.L. BHRNETT 5 ri-- e52 147! 12-01 -'^5 #2 : 45PM [253 8S
PYROPE, KEHHECOil CAHftM, WU62A, Hoveibir 29 199S, S.l.fi.
1S!02 411 102fl203 Uc?03 3f?0 7HGO 15HHO
CftO im 5 9
Si 5.9HOAl .670
Al 3.694Tl .002Cd .353FE .958KX. .06!
H6 4.121CA .7920 24.000
f/*f/FR
17 miUJA11 W1U2A19 YR11467A
70 VR114J2A
21 VR11462A
22 VtlKttA23 VRI1462A74 VRU462A
7.6'
02.94
SO9!
25.52.15.60
1
6.000tt
st
t
i
9.983l
.243
.m
17 40If 40
194020 40
21 4077 4023 40
14 40
1841.6?
.0025.022.967.71
19.52
.625.16
100.61
5,90' t
.091 6.000
3.76C *.000 l
.532 *
.911 t
,075 1
4. lil '.785 9.997
24.000 *.240.193
1"
41.
18.7
620
5100
5.995.005
3.083.013.8'?.782.039
4.10J.864
24.900
72H2411
5111J?6159
t
6,000ltttts
9.992t
.191
.lit
241
1966
20
5100
5.954.046
3.775010
.729
.807
.03J4.34!
.88824.000
D5209
.36
.4J
.73
.32
.27
.78.50
,
6.000lJttl
t
10.055i
.193
.162
?111.76
.0618.957.096.30
P. 58.25
6.40
100.41
6.001 *.000 6.001
3.707.m.305.75?
.0304.192
.965 9.98324.000 l
.188
.158
2141.67
.1318.686.97
6.3120,64
.225.40
100.02
5.994 4
.006 6.000J. 160 '
.014 '.793 t.759 t.C27 t
4.425 *.832 10. 01 i
24.000 *.178.151
2!41.88
.H19.667.04
1. 1720.41
.565. 5 j
100.19
6.014 J
.000 6.0143.158
.013.799
.141
.044
1.36).854 9.978
24.000 'J BO.m
2441.55
.18H. 557.406 20
20.39.28
5.55100.10
5.982.018 6
3.129.019
.842
.746
.8344.3)5
.856 1024.000
.
t
.009ititit
.002t
178151
R.L. BARNETT GEOLOG. 519 652 1475 12-01-95 02:49PM [25]
PKfiOPE, KEHNECOli WHAOft, mi462*, Kovubn 29 1995, S.l.8.
255102 41.32Ha? .19A20J 17.07C2C3 7.42FFO 6.02HSO 19.94
HHO .29CM 4.71SUH 100.4!
51 5.934 *AL .066 6. SCO*L 3.161 'I! .021 'CR .842 lFE .723 tm . 035 'H6 4.272 'Cft .955 10.0090 24.000 t
F/H .177 F/FR .151
25 YRUtttt 25 4024 mi442ft 76 4077 m um 2 7 4028 YB11467A H 4029 YI11462H 79 4030 VI11UM 30 4031 YRH462A 51 4032 YH11462A 32 40
2641.17
.38
18.27
7.604.4J
19. 86
.25
6.39106.15
5.943 i.057 4.01)0
J.ObO t.041 l.867 '.776 *.031 *
4.27} i.988 10.027
24.000 t.189 .159
2741.66
.45
11.75
7.02
6.34
19.74
.255.99
160.20
5.993 *.007 6. OOP
i. 172 '.049 '.798 *.763 l.030 J
4,233 '.923 9.948
24.000 t.187.158
2341.25
.J?I'.OS6.716.66
19.78.28
4.35100.50
5.933 t.067 4.000
J.Hi '.04? '.763 i.801 *.034 i
4.240 i.978 10.025
24.000 t.197
7941.59
.3616.216.866.5!
19. 77.2*
Ut99.68
6.C22 *.000 4.C22
3,157 i.059 ',?!5 l.791 *.029 *
4.267 '.949 9.968
24.000 t.197 .141
3041.70
.41
17. E27.336.57
1V.J!.2'
6,2099.70
6.048 i.000 6.043
3.045 '.045 i.840 *.79] l
.034 '4.189 *
.963 9.91624.000 i
.199
.Hi
3141.5?
.4219,415,926.81
19.62.31
5.8?100.09
5.983 '.017 6.000
J. 280 i.052 i.673 '.8?] '.035 '
4.207 '.9D6 *.?73
24.090 '.205 .170
3241.48
.39:o.4j4.727.JJ
19.70
.285.61
99.94
5.941 '.029 6.000
3.470 '.042 *.536 '.381 '.034 '
4.220 '.864 9.997
24.000 *.217 .17!
R.L. BARNETT GEOLOG. 519 652 141 12-01-95 02:50PM [25] 810
HENNECOn CftNAOft, mW2A, Noveibtr 2? 1755, R.I.S.
335102 41.39T102 .42A2QJ 19.43(353 L. UtFEO 6.95H60 19.69HHO .30CHO 6.01Sun 100.25
Si 5.951 *H .049 6.000Al 3.277 i11 .045 'Cn ,v6t *
FE .8J4 'hit .037 tIK 4.220 'CA .926 1C. 0860 24.000 t
F/K .20?F/fH .1)1
53 Vfill462S 35 4034 KR11U2A 34 4035 YW462A 55 4036 mitiit 36 4037 mittZt 37 4038 m WH 3 8 (d39 Y81146?* 39 4040 Wl 44211 40 40
3*41.21
.6819.11
r., li'.05
19.49.28
4.2599,3:
5.981 *.019 6.000
3.249 t.074 t.JC8 '.854 {.054 *
4.216 '.969 10.005
24.000 *.211.174
3541.
t
21.J.
s.19.
5.100.
5.936.064
3.483.057.415J59.046
4.152.913
24.000
515305li0246389660
t
6.000ittiii
10.025i
.242
.195
34t
19J7
19
6100
5,960.040
3,259.071.611,908.035
4.173.958
24.000
(.27.65.39.55
.52
.39.27.19.05
t
6.000
10.013t
.224
.184
3)41.53
.49
20.58 l.iv
?.kOiy.69
.185.8*
100.31
5.955 *.045 6.flflfl
3.399 '.053 '.510 '.911 '.03' i
4.208 t.B?I 10.013
24.000 t.225.183
J841.60
.7021.11j.u7.54
29.05.J/
5.049?. 36
5.956 '.042 6.000
3.521 i.075 '.391 *.905 *.045 '
4.280 *.773 9.988
24.000 '.271.181
J'
41.
21,j.7,
19..
cV ,
9?.
5.972.028
3.546.052.401.912.043
4,140.814
24.000
5-48125S
5?34358181
i
6.000itttit
9.986'
.230
.187
H41,
,
21,i.8.
19.
5.100
5.934.066
3.624.072.251
1.011.047
4.151.859
24.000
616? '96tt5!SI396?54
t
6.000ttttit
10.022t
.256
.204
Of If MttlUA If
TK 'Ml 6Z JsqiJAON 'WHW 'MDHO linmiV '3iO!l*((
LIV Mliw H/J
i COO' f!W6 109'
i m't /U'i Ufl't 800'i (lO'f
000 1 IWi 596'?
SI'00!in?rSD'IZfll'ior8ffZ 80' If'Jf
If
0HD
NX3483li1*1*IS
mmmmOH
ton(G^JOIS
IItt [53] Wd05:30 Se-10-31 Sit'I 3S9 6IS '901030 113ITdHa 'T
R.L. BARNETT GEOLOG. 9 652 1475 12-01-95 02:51PM 125] 8 12
CLIMMMEHE, UHHfCQI' CftKflOft, VR114t2ft, Hwibtf 30 1995, R.L.B.
1S102 54. HT!02 .02A203 .74C20J 1.94FED 1.95MO 17.81HHO .09m 2 2. o?no .o?KftiO LO/5UH 100.J2
SI 1.975 iti .on 2.000Al .0071! .001CR .056FE .059N6 .961UN .005CA JS7N* .Onf. .001 2.0110 6.000 *
F/H .044F/Ffl .ObO
1 W1467A 42 402 VR1H42A 4! 403 mi462A 44 404 mi4i2ft 45 405 WlWft U 40i mm?* 47 407 VtilliM 4t 40a Kfill4(,2d 41 40
254. U
.H,?0
1.123. IS
18.92.02
?0,80.02.65
100.2?
im *.022 2.000.003 i.004 '.05! '.on *
1.019 *.001 '.805 i.041 '.081 2.010
6.000 '.094M
354.59
.2'2.54l.'J2. 74
17.46.U
19.07.04
1.94100.47
1.962 J.OJ8 2.000.070 '.008 l.042 '.082 '.946 '.004 *JJ4 '.155 *.002 2.024
4.000 1.091.084
4i4.13
.0?J.101.711,50
16.79.00
22. it.04
l.fli100.28
1.950 l.050 2.000.081 '.001 *.036 i.045 t.901 '.000 '.863 '.074 t.002 2.004
6.000 ',050.048
554.46
.112.997.67l.Jt
15.56.00
20.18.54
2. SO99.88
1.96? '.031 2.000.096 t.003 t.016 '.041 *.839 i.900 '.?82 '.175 '.002 2.015
6.000 t.049.047
655.19
.021.411.271.51
17. ?C-.06
2?. 99.04
1.05100.54
1.984 l.016 2.000.344.001.031.039.922.002.886.073.007 2.005
6.000 l.045.043
I54.80
.102.447.492.51
16.42.07
19.37.04
7. 55100.54
1.913 t.027 2.000.576 *.003 i.071 '.077 t.881 '.002 *.147 *.157 '.007 2.017
(.000 t.090.087
854.95
,113.352.501.43
15.35.04
19.88.02
2.65100.28
1.975 '.025 2.001.11!.003.071.043.822.001.766.185.001 2.00
b.OOO i.054.051
F.L. BmFNETT GEOLOG. 519 652 1475 12-01-95 02:52PM [25] 813
CLlHOPrilOXENE, tEHNECOIT CftKftOfl, WH62&, Hovaiber 30 1995, S.l.8.
95102 54.'102A20! 1.C203 LFEO 2.K60 19.mm 1 9.K20KA20m 11SI 1.963HI .037di .016II .002CR .037FE .038Hfi LOSSKM .000U .764Md .048t .0030 6.000
f/KF/PH
9 YP.H462A16 WU42A11 W1462*12 mi4(2ft13 VR1H42A14 VRJ146?A15 mum
160??4id905301660!68b4
t2.000
2.014t
.084
.inse 4051 4ft52 40534154 4055 4056 40
1054.
1.1.i.
16,
22.
1.100.
1.971.0?9.049.000.036.041.911.000.890.088.002
6,000
4600842634SB0096042503
t2.000
2.0Ui
.045
.043
1154.
1.2.2
16.
20.
i.100.
1.980.020.045.006.OSO.063.895.001.784.13?.002
6.000
83215279W420376(149636
t2.000
tlitittt
7.012l
.072
.06?
153
12l
li
20
1160
1.965.035.OK.006.058.090.945.001.809.103.002
6.000
2.98
22.14.03.96.41.04.73.04.H.01
t2.000
ttitjtit
i. mt
.091.088
1!54. U
.142.711.56i. 55
16.01.02
21.37.02
2.10ICO. 48
1.975 '.025 2.000.092 '.004 i.044 t.1)46 i.85! *.001 l.821 '.146 t.001 2.014
6.000 t.054.052
1454.
t
Ll.2,
17.
i?.
1.100.
1.971.079.C56.001.053.0)6.'40.001.768.122.00?
6.900
f!040188515J049?057550
12.000
it'ttttl
2.021t
.082
.015
1554.37
.1!i. 342.9?2.25
li. M.00
19. J9.03
2.24100.05
1.968 '.032 2.000.068 t.003 '.085 t.068 i.88! i.000 *.752 *.15? '.001 2.016
6,000 '.07?.072
wISO'
1SI*1*
ltt1t111t
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CHROME, WNECOt] HUM*, YRU4624, Hoveibit 27 1975, B.L,E.
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4.1621.117 10.000
24.040 '.112.154
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R.L. BARNETT GEOLOQ. 519 652 1475 01-09-96 09:22AM [353
PYROPE, CAUDA, YR114S8A, Jamry 4 1994, i, l. 8.
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R.L. BARNETT GEOLOG. 519 652 1475 01-09-96 09:22AM [351 810
mm, CANADA, must*, awry 4 mi, K.I.B.
41S102 41.37no: .26A203 16.28:2C3 6. WFEfl 4. 4J1" 17,52KM .25CAD 4. MSUN 99.40
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24.000 *.217.171
R.L. BARNETT GEOLOG. 519 652 1475 11-24-95 02:25PM [3] 82
COOMk.O
CHROME DIOPSIDE - KENNECOTT CANADA SAMPLE VR11461A
5.04.5^
4.0-
3.5^
3.0-
25 f..\j2.0-
1.51.0 J
0.5-0.0
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10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26
wt CaO
RLB
R.L. BARNETT GEOLOG. 519 652 1475 11-21-95 03:5?PM [*5] 830
GARNET - KENNECOTT CANADA SAMPLE VR11461A
o RLB
R.L. BARNETT GEOLOG. 519 652 1475 11-21-95 03:54PM i 851 831
ECLOGITIC GARNET - K ENNECOTT CANADASAMPLE VR11 461A
o(9Z
^?
4-
5
u.zu
0.18-
0.16-
0,14-
0,12-
0.10-
0.08-
0.06-
0.04-
0.02-
A rtrt
O
-
8 10 12 14 16
wt CaO
RLB
R.L. BHRNETT GEOLOO. 519 652 1475 l l-21-±'5 03: 54PM [85]
ECLOGITIC GARNET - KENNECOTT CANADASAMPLE VR11461A
(M O
**
1.80-
1,60-
1.40
1.20-
1,00-0.80-
0.60-
0,40-
0.20-
A f\f\
O
8 10 12 14 16
wt CaO
RLB
R.L. EMRNETT GEOLOG. 519 652 1475 11-21-95 03:55PM 185] 833
70
66
Of 2'L. O
58
CHROMITE - KENNECOTT CANADA SAMPLE VR11461A
Diamcnd Inclusion Field
50
46
%Oo
.o ^ o ^ o
1 ' l ' l - l - l ' l l l——l——l——l——l——l—2 4 6 8 10 12 14 16 18 20
wt 96 MgO
o RLB
R.L. BARNETT GEOLOG. 519 652 1 4~5 1 1-21-95 03:55PM [85] 834
CHROMITE - KENNECOTT CANADA SAMPLE VR11461A
70
60 h
d50CM
Q40
10 -
1 1 1 l 1 1 1 l 1 l 1 l
Diamond Inclusion Field
- ^o c^O ^o o
"~
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,. i 1 1 1 1 1 1 1 1 1 1 1
1 1 i 1 1 ] 1
> x^
m
Oo
0 o
o
1 1 1,1
2 4 6 8 10 12 14 16 18 20
wt 96 MgO
RLB
R.L. BARNETT GEOLOG. 519 652 1475 11-24-95 02'-26PM [3] 83
s -
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R.L. BARNETT GEOLOQ. 519 652 1475 11-24-95 02:27PM [3] **4
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R.L. BARNETT GEOLOG. 519 652 1475 11-24-95 02:28PM [ 3] 85
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R.L. BARNETT GEOLOG. 519 652 1475 11-24-95 62:30PM **9
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R. L. BARNETT GEOLOG. 519 652 1475 11-24-95 02:31PM C3] 810
"l
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GARNET - KENNECOTT CANADASAMPLE VR1 1460A
14 f-
1ft
V///T/ Z
wt 96 CaO
o RLB
CHROME DIOPSIDE - KENNECOTT CANADA SAMPLE VR11460A
a. o4.5-
4,0-
W * KO 3'6W S A-^ o,u 0 25-/..O
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10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26
wt ** CaO
o RLB
70
66
062
O 58
CHROMITE - KENNECOTT CANADA SAMPLE VR11460A
Diamond inclusion Fleid
46
o0 o
ooo o
50
00
0
l . l l l l l li l l l
8 10 12 14 16 18 20
wt ** MgO
o RLB
CHROMITE - KENNECOTT CANADA SAMPLE VR11460A
70 j——'——i——-——i——'——i————i——'——i———Diamond Inclusion Field
60
O* 0Mu
#31
10
0 o
. l ! l . l l l ; l l l , l , l l l l
O 2 4 6 8 10 12 14 16 18 20
wt *K MgO
RLB
PWPE, KEKHfCan CAN&Oll, W1460ft, DtCSlbtr i mi, S.L.8.
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f /HF/Fh
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550438982234345843
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itittl
9.956t
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1 402 403 404 405 406 407 408 40
241,55
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19.19.34
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16
14
12
s 7TV 17
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ECLOGITIC GARNET - KENNECOTT CANADASAMPLE VR11459A
0CMCO
tf
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0.18-
0.16-0.14-
0.12-
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8 10 12 14 16
wt CaO
o RLB
ECLOGITIC GARNET - KENNECOTT CANADASAMPLE VR11459A
CMOpx
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1.60-1,40-
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8 10 12 14 16
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5.0
4.5
4.0
2.0
1,0
0.5
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10 11 12 13 14 15 IS 17 18 19 20 21 22 23 24 25 26
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o RLB
CHROMITE - KENNECOTT CANADA SAMPLE VR11459A
70 ——i—-r
66 1Diamond inclusion Field
C$2 o1 L o
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o RLB
CHROMITE - KENNECOTT CANADA SAMPLE VR11459A
Diamond Inclusion Field
60
d60M
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10
0* 00
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Ministry ofNorthern Developmentand Mines
Declaration of Assessment Work Performed On Mining LandMining Act, Subsection 85(2) and 68(3), R.S.0.19M
Transaction Number (office use).iyX)4ft
H*s Rtssarcrt Imaging
Personal information collected on this form is obtained under the ant*"""- -' Mining Act. the information is a ouhiio r.—— - - ^^iiiiiiiiillulimimMnMm Questions abc 933 Ramsey Li
Instructions
1. Recorded holder(s) (Attach a list if necessary)
900
35(2) and 66(3) of the Mining Act. Under section B of the ssment work and correspond with the mining land holder. Istry of Northern Development and Mines, 6th Floor,
claim, use form 0240.
2. 18072Client Number
Address56 IX* tL
Number
Client Number
Telephone NumberAddress
Fax Nurrfber~ M*
3z2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration.
D Geotechnical: prospecting, surveys, rea' Physical: drilling, stripping, assays and work under section 18 (regs) ^ trenching and associated assays
WorK TVDQ C5k i
L/ttltfa T* wl F rftfTl *O /\/**^ ^}
Day Month YetGlobal Positioning System Data (If available)
ir Day | Month j YearTownship/ Area
M or G-Plan Number
Gr 3+13
Office
Q Rehabilitation
UseCommodity
Total S Value of Work Claimed ^ A^\oNTS Reference
Mining Division \ .J*/ j L
Resident Geologist District jCjf-^Jr,^ I nJk^
Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.
3. Person or companies who prepared the technical report (Attach a list if necessary)Name
tax Number
Number
AddressPL- fl rf y
Name Telephone Number
Address Fax Numberl
Name Telephone Nurr -er ? . ^
Address Fax NumberGEOSClENCL ASbtSSWIENTO' r.-^p
4. Certification by Recorded Holder or Agent
l. do hereby certify that , nave knowledge of the facts set(Print Name)forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.
Date
Telephone Number Fax
j,
Recorded Holder 33.3 07oJohn Ewanchuk193 McKelvie Drive., P.O. Box 932, New Liskeard,Ontario, POJ 1POTel/Fax. (705) 647-7207Client Number 297989
o-.,
l i ;ksl o
RECEIV
a ASStSSMENT, .-.^^
01-23-1398 12:39Pr-; Bar-on larketms Int. l 90S 45525SS P.03b. Work to b* recorded ami diMriDuted. worx can only oe assigned to ciaims inai are conuguuuv iaajoming; i^ the mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany this form.
Mining Claim Number. Or K work *res done on other eligible mining land, enow In thb column the location number Indicated on the claim map.
*9
•8
•g12
3
4
5
6
. 7
8
9
10
11
12
13
14
15
TB7827
1234567
1234568
wjxxoJ' SS*7*?
L. 1 1 ^E fef ""7-3
L\ l \ f rTf
Number of CMm Unite. For other mining land, litt hectare*.
16 ha
12
2
32-V(87c**\
M-
Column Totals
Value or workperformed On tnit claim or other mining land.
(26.825
0
S 8, 882
x) *3to90.i?"
*9,S8*S-,3^
O
* 45:4-7* -So
v Mtio of wont applied to UiiJ claim.
N/A
(24,000
(4.000
A^O
J~ f
J b 00*0*0 i
^too-oo
Value of work •Mtgnetf lo othermininoclalmJ.
(24,000
0
0f
l . JWo " CO
oO
* l^co. 00
Benk. Vehie of work tobedWrtbuied""Crft *7 vo u t ^
S2.825
0
(4.692
/3^*KfO-lS'
^^ft-ir0
,
fif^lk^O' /
., do hereby certify that the above work credits are eligible under(Print Put Nam*)
subsection 7 (1) Of the Assessment Work Regulation 6/96 for assignment to contiguous dahns or for application to
the claim where the wort? was done.Signature at Record.* HoW*r or AgentHolder or Agent /uittKxte*d-"TTJriting
^^ (h . ^2——,—is for cutting back credit* that are not approved.
Some of the credits claimed in this declaration may be cut back. Please check (*- ) in the boxes below to show howyou wish to prioritize the deletion of credits:
J3^. 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as Indicated. O 2. Credits are to be cut back starting with the claims listed last, working backwards; or D 3. Credits are to be cut back equally over all claims listed In this decl tra^
D 4. Credits are to be cut back as prioritized on the attached appendix
JAN 2 3 1998 .
Note: If you have not Indicated how your credits are to be deleted, credits will be cut followed by option number 2 if necessary.
For Office Use Only
GEOSCIENCE ASSESSMENT
Recvkvd Stamp Dnim4 Approved OM*
Dale Approved
Datv NollNcctton 9ant
Toul Velu* of CreMApprovM
JPN 23 '98 12=44
Approved tor Recording by Mining Recordar (Slpnttur*)
l 905 4552599TOTfiL P.03 PPGE.03
Ontario Ministry o!Northern Developmentand Mines
Statement ot Costs for Assessment Credit . 6004 O
srsonal Information collected on this form Is obtained under the authority of subsection 6(1) of the Assessment Work Regulation 6/96. Under - ictlon 8 of the Mining Act, the Information Is a public record. This Information will be used to review (he assessment work and correspond withe mining land holder. Questions about this collection should be directed to the Chief Mlnifrg^HHMHpMBBQBHHIMMM^M^HMMAL.i ^ ^ ,, , ^. ^T
f--: j i s,.' V.' \ fc-/
Work TypeUnits of Work
Depending on the type of work, list the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.
Cost Per Unit of work
Total Cost
\ssoclated Costs (e.g. supplies, mobilization and demobilization).
i
Transportation Costs
-RHCJFood and Lodging Costs tf 730
Total Value of Assessment Work
Calculations of Filing Discounts:
1. Work filed within two years of performance is claimed at 10007o of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 500Xo of the Total
Value of Assessment Work. If this situationapplies to your claims, use the calculation below:TOTAL VALUE OF ASSESSMENT WORK ^ ff}-0t * 0 - 50 ~ WYTb^ Total S value of worked claimed.
Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification Is not made, the Minister may reject all or part of the assessment work submitted.
Certification verifying costs:
l, fJ^ (TT/ , do hereby certify, that the amounts shown are as accurate as may(please print lull name)
reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on
the accompanying Declaration of Work form as
to make this certification.(recorded holder, agent, or stale company position with signing authority)
l am authorized
Date
Ministry ofNorthern Developmentand Mines
Ministers du Developpement du Nord et des Mines Ontario
March 26, 1998
KEITH MICHAEL BARRON 56 HARTFORD TRAIL BRAMPTON, ONTARIO L6W-4J8
Geoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5
Telephone: (888)415-9846 Fax: (705) 670-5881
Dear Sir or Madam:
Subject: Transaction Number(s):
Submission Number: 2 .18072
W9880.00040Status
Deemed Approval
We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.
If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice.
Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.
If you have any questions regarding this correspondence, please contact Lucille Jerome by e-mail at [email protected] or by telephone at (705) 670-5858.
Yours sincerely,
ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section
Correspondence ID: 12063
Copy for: Assessment Library
Work Report Assessment Results
Submission Number: 2 .18072
Date Correspondence Sent: March 26, 1998 Assessor:Lucille Jerome
Transaction NumberW9880.00040 Section:16 Drilling PDRILL
First Claim Number8000065
Township(s) l Area(s) BUCKE
StatusDeemed Approval
Approval Date
March 25, 1998
Correspondence to:Resident Geologist Kirkland Lake, ON
Assessment Files Library Sudbury, ON
Recorded Holder(s) and/or Agent(s):KEITH MICHAEL BARRON BRAMPTON, ONTARIO
ROBERT LAWRENCE BARNETT London, Ontario
JOHN RICHARD EWANCHUK NEW LISKEARD, Ontario
Page: 1Correspondence ID: 12063
""M05NE0175 2.18072 BUCKE200
\
DYMOND TOWNSHIPs "- , l ; ' ; v . ,
HARRIS TOWNSHIP
PQ5773t- V \J l l wI2Q27I9lo "1 1186377
" - \ ' 1112^63 l _. r- v ; "1
1118549
-TIMISKAMINGf i r ^ _j i
III&654 i- :^-! ^i;
1191097\ ' HAitEYBURY
\ \1198681 12^3328
.--1211533
*^
! M l' l ORTH
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,-.. n nml l Is."T2H483
J " '' \ w ' - i Y ; v ia . ' ] ^- ----TT.-T--
e i 91211484
TOWNSHIP
Ministry ofNaturalResources
Ontario
Ministry ofNorthern Developmentand Mines
i
INDEX TO LAND DISPOSITION
PLAN
G-34I3TOWNSHIP
BUCKE
M.N.R. ADMINISTRATIVE DISTRICT
TEMAGAMIMINING DIVISION
LARDER LAKELAND TITLES /REGISTRY DIVISION
TIMISKAMING
OATH OF ISSUE2 5 1998
Scale 1:20 000
1000Metres
1000 2000Metres
1000Feet
1000 2000 3000 4000 5000 6000 7000 8000 9000 10000——i i———————i i —i i———————i i- i ——i Feet
Contour Interval 10 Metres
SYMBOLSBoundary
Township, Meridian, Baseline.
Road allowance; surveyed ... shoreline...
Lot/Concession; surveyed, unsurveyed
Parcel; surveyedunsurveyed
Right-of-way; road\ railway ............................ '
utility.............................. *
Reservation .................................... *\*X*xwm
Cliff, PH, Pile...................................... ~ ,,,,,,,,..,,, r
Contour .......................................... 20Interpolated Approximate Depression..........................
Control point (horizontal) ...................................... A
Flooded land...................................... ^XXXXKX:OOC
Mine head frame .............................................. a
Pipeline (above ground)
Railway; single track............................... -i———'———*-double track .............................. -"———'——H-abandoned............................... -*— —— —"-
Road; highway, county, township .................... - - — -~^----access ..................................... - - -- ^ ^ :trail, bush ................................... -- —————-
Shoreline (original)................................. ..--"""•••••••••....
Transmission line
Wooded area...................................... -- -
DISPOSITION OF CROWN LANDSPatent l
Surface SK. M ining Rights Surface]Rights Only Mining Rights Only.
LeaseSurface 4 Mining Rights . Surface Rights Only Mining Rights Only.
Licence of Occupation
Order-in-Council.
Cancelled
Reservation
Sand S Gravel.
THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES. AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER. MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD- r ( r DITIONAL INFORMATION
.H
.B
. ..................oc
AREAS WITHDRAWN FROM DISPOSITIONMRO- Mining Rights Only SRO - Surface Rights Only
•' M + S- Mining and Surface Rights
Description Order No. Date Disposition File
rt-L-44/95 JUNE 1/95 MINING R'GHTS
THIS TOWNSHIP FALLS WITHIN THE TEMAGAMI COMPREHENSIVE PLANING AREA. SPECIAL WORKING CONDITIONS MAY APPLY TO EXPLORATION ACTIVITIES. FOR MORE DETAILS PLEASE CONTACT:
DISTRICT MANAGER, NORTH BAY DISTRICT MINISTRY, NATURAL RESOURCES
NOTES
FLOODING RIGHTS TO ELEVATION 999'ABOVE SE A LE VE L IN LAKE TIMISKAMING. FILE 139387
NORTH HALF LOT B CON. 2 SUBJECT TO SANITARY CONTROL OF CONSTANCE LAKE FOR TOWN OF HAILEYBUR Y.
STAKINGS OF MINING CLAIMS WITHIN TOWNSITES SHOWN THUS : ^ ONLY WITH CONSENT OF THE MINISTER.
JRPALF. KiCHTS WITHDKA^N UNOKR SKJ.36 Hf MINING ACT R.S.O. 1980 ORDER NO. W-OI/9I/ONT
(TrtANSCANADA PIP^UNF. RIGHT OK WAY AND BUFFER ZONE PARTICULARLY 40.E5 MF.TF.RS OR i i i! F'. ON flTHF-i SIDK OF CENTRF. LINE OF RIGHT OF
AUGUST 11,1935,ON THE STATUS OF THE LANDS SHOWN HEREON ARCHIVE J FER 27/97
Map base and land disposition drafting by Surveys and Mapping Branch, Ministry of Natural Resources.
The disposition of land, location of lot fabric and parcel boundaries on this index was compiled for administrative purposes only.
CD
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