1
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) 112 1 8 (1 2 5 , 7 . 0 , 3 0 ) 23 5 8 p p m P b 11221 (40 ,0.2,< 5 ) 11220 (90,0.4,<5) 112 22 (15 ,<0.2 , < 5) 11223 (135,1.2 ,5) 2540ppm Pb 1058ppm Zn 11224 (20,0.2,<5) 112 25 (1 5 , <0.2, < 5) 112 26 (15 ,<0.2, <5) 11227 (10 ,<0.2 , < 5) S P - 1 ( < 5 , < 0 . 2 , 1 0 ) S P - 2 ( 5 , < 0 . 2 , 2 0 ) S P - 3 ( 5 , < 0 . 2 , 1 0 ) S P - 4 ( < 5 , < 0 . 2 , 1 0 ) S P - 5 ( < 5 , < 0 . 2 , 1 5 ) QUARTZ VEINS 274 o 120 o 60 o 296 o 82 o 3 6 0 o fault rubble 2a 2a 2a 2a limonitic/manganese partings 2a 10 cm stockwork vein rubbly 2c minor 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 FAU L T ZONE? 1 1216 ( 4 90, 2. 4, 2 0 ) 1 57 4p p m Pb 1 1217 ( 23 0, 0.6,5 5 ) 1 121 5 ( 1.04 g /t , 2. 6, 1 0) 1 1 211 ( 23 0 , 3 . 0,2 5 ) 1 1210 ( 5 85, 1 1 .8 , 8 0) 4 862p pm Pb 1 120 9 ( 35 0, 22 .0 , 45) 7 8 8 8 p p m P b 1 1208 ( 8 ,5. 0 , 15 ) 1 124p pm Pb 2c, 2cbx 330 o 3 5 5 o limonitic/ manganese partings 3/4cm limonitic partings brecciated sil flooded intrusive blebby quartz, minor stringers limonitic/ manganese partings in fractures in silcified intrusive 2-3cm quartz vein limonitic partings 1 7 9 o 70 o 2b 2b 2b 2b 1 2 1 Pod of Quartz with random limonitic fractures ~1.5- 2/cm 1 1207 ( 1 0, < 0 . 2,< 5 ) 1 1206 ( 9 00, 2 1. 0, 2 0) 9 0 5 2p p m P b 1 1 2 05 ( 20 ,< 0 .2, < 5) 1 12 03 ( 15 ,< 0. 2, < 5) 1 1 202 ( 5, 0 . 2 , <5) 1 1 2 01 ( 2 5 ,< 0 .2,< 5) 03 0 o 155 o 06 o 110 o 40 o 0 2 0 o Mn 70 o q u art z str v’l et s q uar tz qv q u ar t z dense limonitic partings parting in Qv 0.5 gpt 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 1 121 9 (5 0 , < 0 . 2 , < 5) 60 70 80 90 100 m 1 120 4 ( 25,< 0. 2,< 5) T R E N C H T R A I L LEGEND Bleached and silicified. Contains ~5% evenly distributed Fe oxide pods. Usually contains quartz stringers, veinlets or veins to roughly 10%. Stockwork intrusive. Contains >30% quartz veins, randomly oriented. Intrusive component may appear similar to 2a but may also be pervasively limonitically altered. Silicified intrusion with rare veins or veinlets, in areas contains pervasive limonitic alteration Unit 2c brecciated as a crackle or in situ breccia 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. *black partings, intense fracturing 11240 (185,0.4,20) Sample no. Au ppb, Ag ppm, As ppm 2 1 2a... 2b... 2c... 2cbx.. 1a... Quartz 72 o green-black gouge 3 6 0 o 3 40 o 70 o 80 o gouge 73 o 75 o O/B SP-5 Soil Sample Jual Creek trail to camp 2500 3000 3000 VAL / JUAL SOIL GRID t r e n ch t r a il Tr 00-14 Tr 00-12 Tr 00-5, 5a Tr 00-10 Tr 00- 6 Tr 00-11 Tr 99-1 Tr 00-09 Tr 00-8 Tr 99-3 Tr 99-4 Tr 00-7 VAL CLAIMS JUA L CLAI MS 0 500 metres Tr 00-18 Tr 00-16 Tr 00-13 Tr 00-17 Tr 00-15 Trench 99-2

metres

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DESCRIPTION

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

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Page 1: metres

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