EARTHUNT RESOURCES INC.
R.R. 2,
ONTAI
(705)
41P11SE0426 63.6121 CHURCHILL
FORT KNOX GOLD - SHININGTREE PROJECT
GENERAL GEOLOGICAL/GEOCHEMICAL OBSERVATIONS
A geological reconnaissance was undertaken in the
southeast quadrant of Churchill Township and in
adjoining Asquith Township between the hamlet of Shiningtree
and Chlorus Lake. The work was accomplished in mid-September
and the latter half of October, 1990, and was greatly
facilitated by a network of logging access roads connected to
Highway 560. The logging activities were confined to the
1980*3, well after M. Carter of the O.G.S. conducted his
mapping surveys. Extensive areas of clear cutting now
provide many new rock exposures.
Our recent field work principally involved an
examination of outcrops in an area extending from the
Gosselin claims in the Speed Lake area to the Herrick
(Kingsley Vein) claims at Michiwakenda Lake. This is a
distance of about 3 miles (4.8 km) and traverses a t hick
stratigraphic section with pillowed and komatiitic basalts at
the base, succeeded by rhyolite and iron formation in the
Perkins-Cochrane Lakes area. The aforementioned rocks are
capped by mixed flows, sediments and iron formation of the
Temiskaming equivalent Ridout series (see attached map).
The field work was designed to provide a preliminary
assessment of Fort Knox Gold's recently acquired claims which
cover both the Gosselin and Herrick gold occurrences.
Stripping, washing and sampling was done on the Gosselin
south zone, shaft area and main quartz zone near Speed Lake.
The work was concentrated on the south zone where host
rocks to gold mineralization are of two types: a silicified,
weakly pyritic felsite unit, and bull quartz veins in dark
green komatiitic rocks (see attached sketch maps). The bull
quartz is locally rusty and contains minor - up to Q.5% -
pyrite and chalcopyrite and reportedly visible gold.
Although no gold was seen, the size of the deep, wide pit in
the 'D' trench gives validity to the old reports. Drill
cores from under this trench gave up to 0.05 o.p.t. gold
over about five feet (1.5 m). The pink, hematitic, pyritized
wall rocks to the bull quartz veins commonly carry J.% - 3%
pyrite, and on geochemical analysis gave up to 991 p.p.b.
gold. By contrast, the bull quartz gave a high value of 391
p.p.b. gold.
2. . .
llil
010
ip ojo--2-
At the Gosselin shaft, visible gold can be readily seen
in samples from the old shaft sunk on a quartz vein which
occurs at a contact between komatiite and a felsite intrusion
(see whole rock analysis ST-WR-90-6). The quartz is banded
with carbonate, sericite, chlorite, fuchsite, and trace
amounts of fine-grained pyrite. One grab sample from the
shaft dump gave 1851 p. p. b. gold.
The most significant gold values obtained on the
Gosselin claims were reported in the 1980's by Onitap
Resources. The gold occurs in the same felsic intrusion
exposed at the shaft and in the Gosselin south zone where
Fort Knox conducted its recent backhoe stripping. According
to Onitap drill logs, a fifty foot (15 m) section of core
from a silicified, pyritic section of the felsite assayed
about 0.05 o. p. t. gold. The core from this hole may be
available for examination.
The Kingsley vein on the Herrick claims was channel-
sampled over a length of about 1000 feet (330 m). The
results of this sampling are attached to this report. The
vein was stripped over a length of about 1200 feet (370 m)
by Unocal Ltd. in the summer of 1989. The Herrick structure
is in places a knife-sharp crack filled by a grey and white
banded l foot (0.3 m) quartz vein or a quartz breccia vein up
to 6.5 feet (2 m) in width. Locally, where the structure is
up to 16.5 feet (5 m) wide, it is best described as a quartz
stringer stockwork. At the Herrick, fine visible gold was
seen - in samples on the mine dump - in white alabaster-
textured quartz and in association with very fine-grained
acicular arsenopyrite and ser icite-rich bands in the quartz.
There does not appear to be a direct relationship between
gold and the amount of sulphides. In fact, the sulphide
content is generally low ( 11) a nd a number of high grade
samples (e.g. 122869-873 incl.) showed only traces of
metallic mineralization.
A number of gold showings are known on the Churchill
claims, about 3/8 miles (0.6 km) south of the Herrick. The
structure is complex in this area, which is underlain by
carbonate facies iron formation, altered rhyolite and mafic
intrusive rocks. The gold occurs in quartz veins, the most
interesting of which are hosted by iron formations. At the
Pet vein, which produced gold in 1981, the host is banded
siderite-chert iron formation while to the north, the iron
formation hosting the Cochrane veins is sulphidic, chert-
oxide facies. The setting is reminiscent of that of the
Agnico Eagle mine near Joutel, Quebec.
R R. 2, MILLBROOK
DOUG HUNTER, M.SC. ONTARIO. CANADA
CONSULTING GEOLOGIST LOA 1 GO (715) 932-31 30-3-
Zinc mineralization was observed in chert and carbonate
units associated with iron formations both east and west of
Perkins Lake. A siderite-rich chloritic fragmental outcrop
at the southwest corner of Perkins Lake resembles the iron
formation exposed at the Pet vein workings. The Perkins Lake
sphalerite-pyrite showing occurs within a relatively thick
felsic volcanic unit which has been mapped by Carter over a 4
mile {6.5 km) strike length. A pyrite-rich horizon examined
on the shore of Cochrane Lake is associated with an A.E.M.
anomaly (beneath the lake) which is directly on strike of the
zinc mineralization at Perkins Lake. There appears to be
potential in this environment for volcanogenic massive
copper-zinc sulphides.
In summary, the following points are emphasized:
i) The geological relations at Shiningtree are poorly
understood and detailed work will improve the situation
dramatically;
ii) Our field work has given us a good grounding in order to
undertake a meaningful compilation of the economic geology;
iii) Very little systematic base metal exploration has been
performed and there are some new zinc showings which have not
been evaluated;
iv) Komatiitic basalts seem to be more important in the
Shiningtree area than previously thought. These are
potential hosts for volcanogenic Cu-Ni deposits;
v) Gold mineralization in the Shiningtree area is
widespread and occurs in a wide variety of geologic
environments. Documentation is poor and research/compilation
could be very imformative.
Respectfully submitted,
A. Douglas Hunter
November, 1990
R R 2, MILLBROOK
DOUG HUNTER.M.Sc. ONTARIO. CANADA
CONSULTING GEOLOGIST LOA1GO (705)932-3130iblished 1928
Swastika Laboratories
A Division of Assayers Corporation Ltd.
Assaying - Consulting - Representation
Page l of 3
Geochemical Analvsis Certificate OW-1688-RG1
' " V
Company: FORT KNOX GOLD RES. INC. Dale: NOV-20-90
Project: Copy 1. 22 FRONT ST. W, TORONTO M5 J 1C4
Attn: WAYNEWHYMARK 2. FAX TO 4 1 6-869-0778
We hereby certify the following Geochemical Analysis of 90 ROCK samples
submitted OCT-30-90 by D. HUNTER. ^ ,,
tfOTf G-nCfFt itJ SAMPLES ABE. M flRKCD u/lTH A Gr.
Sonple
Nirrber
ST-VR-90-1 122801
ST-VR-90-2 122802
ST-VR-90-2 122803
ST-VR-90-2 122804
ST-VR-90-3 122805
ST-VR-90-4 122806
ST-VR-90-4 122807
ST-VR-90-4 122808
ST-VR-90-4 122809
ST-VR-90-4 122810
ST-VR-90-4 122811
ST-VR-90-4 122812
ST-VR-90-4 122813
ST-VR-90-4 122814
ST-VR-90-4 122815
ST-VR-90-4 122816
ST-VR-90-4 122817
ST-VR-90-4 122818
ST-VR-90-4 122819
ST-VR-90-4 122820
ST-VR-90-4 122821
ST-VR-90-4 122822
ST-VR-90-4 122823
ST-VR-90-4 122824
ST-VR-90-4 122825
ST-VR-90-4 122826
ST-VR-90-4 122827
ST-VR-90-4 122828
ST-VR-90-4 122829
ST-VR-90-4 122830
Au Au check Au 2nd Au check Ag As Cu Ni Zn VM
ppb ppb ppb 2nd ppb ppm ppm ppm ppm ppm ppm
16 55
92 57
24 14 0.3 84 163
Nil 0.1 44 108
21 30
Nil 0.1 42 1040
31 L- II 532-61 0.1 19 86
7 L- H 5 32,6*5 0.1 45 80
237 L- " '5316*1 1.4 122 123
96 L- U S 3 16? 0.4 160 77
Nil t.-ll53^6<:^ 0.4
3
69 - G-
72-6-
31-6-
62-6
93 -6-
141-6
110-6
377- Gr 549
38-6
45- 6
144 -Gr
336- Gr
86-6
160-6
127-6
387-6 343
165 -C- 2
55-6
Certified by- a JJ
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705)642-3244 FAX (705)642-3300stablishedl928
Swastika Laboratories
A Division of Assayers Corporation Ltd.
Assaying - Consulting - Representation
Geochemical Analysis Certificate
Company: FORT KNOX GOLD RES. INC.
Project:
Aim: WAYNE WHYMARK
Page 2 of 3
OW-1688-RG1
Date: NOV-20-90
Copy 1. 22 FRONT ST.W, TORONTO M5J1C4
2. FAX TO 416-869-0778
We hereby certify the following Geochemical Analysis of 90 ROCK samples
submitted OCT-30-90 by D. HUNTER.
ALL
Sanplc
Nurtoer
ST-VR-90-4 122831
ST-VR-90-4 122832
ST-VR-90-4 122833
ST-VR-90-4 122834
ST-VR-90-4 122835
ST-VR-90-4 122836
ST-VR-90-4 122837
ST-VR-90-4 122838
ST-VR-90-4 122839
ST-VR-90-4 122840
ST-VR-90-4 122841
ST-VR-90-4 122842
ST-VR-90-4 122843
ST-VR-90-4 122844
ST-VR-90-4 122845
ST-VR-90-4 122846
ST-VR-90-4 122847
ST-VR-90-4 122848
ST-VR-90-4 122849
ST-VR-90-4 122850
ST-VR-90-4 122851
ST-W-90-4 122852
ST-W-90-4 122853
ST-\\R-90-4 122854
ST-VR-90-4 122855
ST-UR-90-4 122856
ST-VW-90-4 122857
ST-W-90-4 122858
ST-VR-90-4 122859
ST-VR-90-4 122860
Au Au check Au 2nd Au check Ag As Cu Ni Zn VRA
ppb ppb ppb 2nd ppb ppm ppm ppm ppm ppm ppn
7406 45
2057 80
422
339 30
8297 6994
2184 65
823
1073
79
117
175
1714
1577
11932 120
665 60
24754 27566 240
22766 22560 30515 28252
2157
161 135
281
6926 200
3051
1179
3703
6240
1104
6583 4800
110
989
1783
Certifie LS/CYX..-XA
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244 FAX (705)642-3300iblishedl928
Swastika Laboratories
A Division of Assayers Corporation Ltd.
Assaying - Consulting - Representation
Geochemical Analysis Certificate
Company: FORT KNOX GOLD RES. INC.
Project:
Attn: WAYNE WHYMARK
Page 3 of 3
OW-1688-RG1
Date: NOV-20-90
Copy 1. 22 FRONT ST.W, TORONTO M5J1C4
2. FAX TO 416-869-0778
We hereby certify the following Geochemical Analysis of 90 ROCK samples
submitted OCT-30-90 by D. HUNTER.
Saiple
Nutter
Au Au check Au 2nd Au check Ag As Cu Ni Zn VM
ppb ppb ppb 2nd ppb ppno ppm ppm ppm ppm ppm
ST-VR-90-4 122861
ST-VR-90-4 122862
ST-VR-90-4 122863
ST-VR-90-4 122864
ST-VR-90-4 12286S
ST-VR-90-4 122866
ST-VR-90-4 122867
ST-VR-90-4 122868
ST-VR-90-4 122869
ST-VR-90-4 122870
ST-VR-90-4 122871
ST-VR-90-4 122872
ST-VR-90-4 122873
ST-VR-90-4 122874
ST-VR-90-4 122875
ST-VR-90-4 122876
ST-VR-90-4 122877
ST-VR-90-4 122878
ST-VR-90-4 122879
ST-VR-90-4 122880
ST-VR-90-4 122881
ST-VR-90-4 122882
ST-VR-90-4 122883
ST-VR-90-4 122884
6103 ^\
2743 \ 120
3086
6926 5143
82 J
7954 7
13029 l
m" 124,2 VHE^.CK S *HMS
18103 19543 17966 194745623 1
12617 J
12686 12617 S
4114 ^-^
2825 /^
391 - G
305 - G-
991-6-
195-6-
14-6-
727 - C 6 .4 8
45-6-
3909 -G- 3703 140
23 1.4 190 77 129
ST-VR-90-5 122885 Nil 0.1 12 22
ST-VR-90-6 122886 147 - G
ST-VR-90-7 122887 Nil
ST-VR-90-8 122888 - GST-VR-90-9 122889 -G
ST-VR-90-10 122890 - 6-
0.1 10
16
107
15
8
25
15
107
460
735
Certified byP.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244. FAX (705)642-3300NOU IB '90 15:30 SWASTIKA LAB PAGE.01
P.O. BOX ID
I.C.A.
TELEPHONE li 03-642-3244
FAX li 703-642-3300
WHOLE ROCK ANALYSIS
HiUBonti Fulton
SWASTIKA LABORATORIES
P.O. BOX 10
SWASTIKA, QNT
YOUR REFERENCE - RM6B8-WJ1
SAMPLE!
122901
122602
122803
122904
122863 - Gr
122886 - Gr
122887 -
122969- G-
122890 - GFort Knox
6B8-WJ1
6102
X
73.82
56.08
71,91
51.20
69.73
78.55
77.9B
50,31
44,63
42.74
A1203
X
14.26
13,64
13,44
7.82
13,61
12,41
12.17
13,77
9.76
6.27
Fi203
X
1,35
6.92
2.11
26.32
2.64
1.36
1.65
13,84
11,43
10,05
CaO
X
1.72
6,11
2.91
3,96
3.12
0,74
0,27
4,63
7,31
4,17
HgO
r,
0.23
2.17
0.29
3.48
0.67
0,19
0.41
7.09
20.19
24.60
NI20
X
3.73
5,40
3.71
0.09
3,57
2.39
3.13
3.10
1.22
0.04
T.8.L,
T.S.L,
T.B.L.
K20
X
1.30
0.58
1.52
0.14
2.24
2,38
2.38
0.26
0.10
tt.02
REPORT No. l H - 8428 -
Fill NO. l N009RA
1
Invoici No, t
Ti02
X
0.35
1,83
0,37
0.23
0,33
0.05
0.07
1,02
0.39
0.20
HnO
X
0.02
0.23
0.03
0.75
0,07
0.02
0.01
0.16
0,17
0.13
P205
X
0.14
0,34
0,14
0.08
0.18
0.12
0.10
0.18
0.20
0,22
LO!
l
2.77
4.78
3.76
6.14
3.93
1,67
1.23
6,22
4.91
11,48
T01AL
X
100,15
100,09
100,23
100,22
100.12
100,2?
99,40
100,57
100.33
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f!!, y.CHURCHILL TWP. - SlilNINGTREE AREA
Sample No,
10101
10102
10103
10105
10106
1010?
10108
10109
10110
10111
10112
10113
10115
10116
10117
10118
10119
10120
10121
Rock Type
J-'yritic "green" carbonate/south of road
Gosselin Zone
Fuchsite/carbonate vein
Quartz in tourmaline and very fine
grained pyrite
Pyritic QC vein and fuchsite
Pyritic QWMCT-Z VE! M -v
w\ S" \ i
H
H
Green chert with ruby
Massive pyrite
Carbonate facies I. F.
Pyritic fragmental with ruby sph.
Pyritic heavy pyrite
Herrick, brecciated qtz on dump
d H n n H
Pyritic fragmental N. end of zone
Pet vein area, massive
Brown-altered pyritic ( 2fo) quartz
vein (north of High Grade Zone).ilished 1928
Swastika Laboratories
A Division of Assayers Corporation Ltd.
Assaying - Consulting - Representation
Geochemical Analysis Certificate OW-1390-RG1
Company:
Project:
Attii:
FORT KNOX GOLD RES. INC.
WAYNE WHYMARK
Date: SEP-20-90
Copy 1. 22 FRONT ST.W..TORONTO, M5J 1C4
2. FAX TO 416-869-0778
3. HOLD
We hereby certify the following Geochemical Analysis of 20 ROCK samples
submitted SEP-17-90 by WAYNE WHYMARK.
Sample
Number
10101
10102
10103
10104
10105
10106
10107
10108
10109
10110
iolin
10112
10113
10114
10115
10116
10117
10118
10119
10120
Au Au check Au 2nd Au
ppb ppb ppb 2
Nil
24
1851
247
12274
28869 29555 33257
14
669
1334
789
1053
24
103
21
10
99
15154 15086
15223 13303
24
2770
check A
nd ppb pp
30789
0.
0.
0.
0.
0.
0.
2.
kg
m
1
4
2
1
3
2
6
Cu
ppm
10
38
13
46
22
21
95
Mi Zn
ppm ppir
13600
297
70
2160
89
177
9880 76
Certified by
G. Lebel l Manager
P.O. Box 10, Swastika, Ontario POK1TO
Telephone (705) 642-3244. FAX (705)642-3300KNOX Goi-D Re:sou.Rce.s
A
AND Recce.
Co Uec-UA
•11P1ISE042S S3.
geologyontario.mndmf.gov.on.ca |
