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82 o. 296 o. 120 o. 60 o. 500. 0. metres. LEGEND. 1. 2. Unaltered metasedimentary package. Quartzites with muscovitic partings, schist Highly fractured, silicified and stockworked unit 1 with rare chloritic alteration. Fractures often coated with limonite, manganese. - PowerPoint PPT Presentation
Citation preview
0 10
metres
TECK EXPLORATION LTD.K A M L O O P S , B R I T I S H C O L U M B I A
FIGURE DRAWN BY: S.A.SCALE: 1:200 BY: M.P. & J.P.
Ten Mile Creek Property
VAL CLAIM GROUP
Trench 99-02
SP-6 (10,<0.2,10)SP-7 (5,<0.2,10)SP-8 (5,<0.2,10)
SP-9 (<5,<0.2,15)SP-10 (15,<0.2,10)
11213 (10,<0.2,<5)
11214 (35,<0.2,<5)
11218 (1
25,7
.0,3
0)
2
358p
pm P
b
1122
1 (4
0,0.
2,<5
)
11220 (9
0,0.
4,<5
)
1122
2 (1
5,<0
.2,<
5)
1122
3 (1
35,1
.2,5
)
2
540p
pm P
b
1
058p
pm Z
n
1122
4 (2
0,0.
2,<5
)
1122
5 (1
5,<0
.2,<
5)
1122
6 (1
5,<0
.2,<
5)
1122
7 (1
0,<0
.2,<
5)
SP
-1 (
<5,
<0.
2,10
)
SP
-2 (
5,<
0.2,
20)
SP
-3 (
5,<
0.2,
10)
SP
-4 (
<5,
<0.
2,10
)
SP
-5 (
<5,
<0.
2,15
)
QUARTZVEINS
274o
120 o
60o
296 o 82o
3 60o
fault rubble 2a2a2a2alimonitic/manganese partings
2a
10 cmstockwork vein
rubbly
2cminor
2c,rare 2a
rubbly2c, sil
qtz
banded qtz
1
2b
2b
2b
SP-11 (30,<0.2,<5)SP-12 (45,<0.2, 5)SP-13 (<5,<0.2, 5)SP-14 (15,<0.2, 5)SP-15 (40,<0.2,10)
11212 (30,<0.2, 5)
BIG
FAULT
ZONE?
11216 (490,2.4,20)
1574ppm
Pb
11217 (230,0.6,55)
11215 (1.04
g/t,2.6,10)
11211 (230,3.0,25)
11210 (585,11.8,80)
4862ppm
Pb
11209 (350,22.0,45)
7888ppm
Pb
11208 (8,5.0,15)
1124ppm
Pb
2c, 2cbx
330 o
355o
limonitic/manganese
partings 3/4cm
limonitic partings
brecciated silflooded intrusiveblebby quartz,minor stringers
limonitic/manganesepartings in fractures
in silcified intrusive2-3cm quartz vein limonitic partings
1 79o
70o
2b2b
2b2b
1
2
1
Pod of Quartz withrandom limonitic
fractures ~1.5-2/cm
11207 (10,<
0.2,<5)
11206 (900,21.0,20)
9052ppm
Pb
11205 (20,<
0.2,<5)
11203 (15,<
0.2,<5)
11202 (5,0.2,<
5)
11201 (25,<
0.2,<5)
030
o
155 o
06 o
110o 40o
020
o
Mn
70 o
quartz str v
’lets
quartz
qv
quartz
dense limoniticpartings
parting in Qv
0.5gpt Au / 12m
Quartz is not homogenous white quartz but seems to have been at one time and was shot through with a pyritic silica, resulting in a grey matrix white quartz breccia, to in situ breccia and a white quartz crackle breccia, with limonitic matrix, some white quartz, with grey pyritic silica stringers.
START: 0m
10
20
30
40
50
11219 (5
0,<0
.2,<
5)
60
70 80 90 100m
11204 (25,<
0.2,<5)
T R
E N
C H
T R
A I L
LEGEND
Bleached and silicified. Contains ~5% evenlydistributed Fe oxide pods. Usually containsquartz stringers, veinlets or veins to roughly 10%.
Stockwork intrusive. Contains >30% quartz veins,randomly oriented. Intrusive component mayappear similar to 2a but may also be pervasivelylimonitically altered.
Silicified intrusion with rare veins or veinlets, inareas contains pervasive limonitic alteration
Unit 2c brecciated as a crackle or in situ breccia
Unaltered metasedimentary package. Quartziteswith muscovitic partings, schist
Highly fractured, silicified and stockworked unit 1with rare chloritic alteration. Fractures oftencoated with limonite, manganese.*black partings, intense fracturing
11240 (185,0.4,20)Sample no. Au ppb, Ag ppm, As ppm
2 12a...
2b...
2c...
2cbx..
1a...
Quartz
72o
gree
n-bl
ack
goug
e
3 60o
340o
70o80o
gouge
73o
75o
O/B
SP-5 Soil Sample
Jual Creek
trail t
o
cam
p
2500
3000
3000
VAL / JUALSOIL GRID
tren
ch
trail
Tr 00-14
Tr 00-12
Tr 00-5,5a
Tr 00-10Tr
00-6
Tr 00-11
Tr 99-1
Tr 00-09
Tr 00-8Tr 99-3
Tr 99-4
Tr 00-7
VAL CLAIMS
JUAL
CLAIM
S
0 500
metres
Tr 00-18
Tr 00-16
Tr 00-13
Tr 00-17
Tr 00-15
Trench 99-2