1987 ASSESSMENT REPORT GEOPHYSICAL Greenwood M.D. …

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1987 ASSESSMENT REPORT on a 1987 GEOPHYSICAL & GEOCHEMICAL SURVEY on the - SUN MINERAL CLAIM Greenwood M.D. N.T.S. 82E 2E Location: Three Km SW of Greenwood, B.C. Four Km SW of Phoenix, B.C. Owner : Sunnyside Resources Ltd, and 400-601 Cordova St, Operator: Vancouver, B.C., V6B 1G1 Consultant: L. Sookochof f , P. Eng . Sookochoff Consultants Inc. 609-837 West Hastings St, Vancouver, B.C. V6C 1B6 Dates of Work: February 1, 1987-April 15, 1987.

Transcript of 1987 ASSESSMENT REPORT GEOPHYSICAL Greenwood M.D. …

1987 ASSESSMENT REPORT

on a 1987

GEOPHYSICAL & GEOCHEMICAL SURVEY

on the

- SUN MINERAL CLAIM

Greenwood M.D. N.T.S. 82E 2E

Location: Three Km SW of Greenwood, B.C. Four Km SW of Phoenix, B.C.

Owner : Sunnyside Resources Ltd, and 400-601 Cordova St, Operator: Vancouver, B.C., V6B 1G1

Consultant: L. Sookochof f , P. Eng . Sookochoff Consultants Inc. 609-837 W e s t Has t ings S t , Vancouver, B.C. V6C 1B6

Dates of Work: February 1, 1987-April 15, 1987.

TABLE OF CONTENTS

ILLUSTRATIONS

FIGURE I LOCAT I ON FIGURE 2 INDEX

FIGURE 3a VLF-EM (Fraser Filtered) FIGURE 4 ARSENIC GEOCHEMISTRY FIGURE 5 SILVER GEOCHEMISTRY FIGURE 6 COMPILATION MAP

FIGURE 3 VLF-EM SURVEY - PROFILES

APPENDIX

A ASSAY RESULTS

1 . 1. 1. 1. 2. 2. 3 . 4. 6. 6. 7 , 8 . 9.

10. 11.

/ . Geophys ica l & Geochemical

Assessment Report on t h e

Sun M i n e r a l C l a i m

INTRODUCTION

During t h e p e r i o d of F e b r u a r y 1 , 1987 t o A p r i l 15 , 1987 a n e x p l o r a t i o n program c o n s i s t i n g of g e o c h e m i c a l and g e o p h y s i c a l s u r v e y s were carried o u t on t h e Sun m i n e r a l claim.

The pu rpose of t h e s u r v e y s w a s t o locate p o t e n t i a l m i n e r a l c o n t a i n i n g s t r u c t u r e s or massive s u l p h i d e zones known to e x i s t i n t h e a r e a . T h i s r e p o r t provides t h e results of t h a t work, t h e i n t e r p r e t a t i o n and t h e c o n c l u s i o n s t h e r e o f .

PROPERTY

The p r o p e r t y c o n s i s t s of a c o n t i g u o u s b l o c k of f o u r claims. P a r t i c u l a r s are as f o l l o w s :

C l a i m name U n i t s Record N o , Lo t N o . Sun 18 4535 Bev 2 36673 J u l y 18/91* Fanny Joe Mine ra l lease 7295 Sunnys ide 401 2879 May 11 /88

*Upon approval o f f o u r y e a r s a s s e s s m e n t w o r k a p p l i e d March 1 1 , 1987 and J u n e 8, 1987.

TIMBER AND TOPOGRAPHY

Surface e l eva t ions on t h e p r o p e r t y v a r y from 1200 t o 1600 metres above sea l e v e l on a n o r t h e r l y - f a c i n g m o d e r a t e l y - s l o p i n g h i l l s i d e , Most of t h e area h a s been r e c e n t l y logged w i t h sparse Ponderosa P i n e and Douglas F i r remaining on t h e h i g h e r slopes.

TRANSPORTATION AND SUPPLIES

A C.P. r a i l l i n e p a s s e s t h r o u g h 1 2 a i r k,m. t o t h e east. S k y l i n k A i r l i n e s h a s r e c e n t l y commenced f l i g h t service from Vancouver to Grand Forks . C a s t l e g a r , 90 k.m, ea s t of Grand Forks , is served d a i l y by commercial a i r l i n e . Most e x p l o r a t i o n s u p p l i e s are o b t a i n a b l e a t Grand F o r k s or Greenwood.

- WKON TERRITORY

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'2_ Island

125'

soale i: 10.000.000 loo 0 loo 200 900 4ooKm

I I I

FORT I NELSON I

I

3 SOOKOCHOFT CONSULTANTS INC.

SUNNYSIDE RESOURCES LTD.

SUN CLAIM GREENWOOD KD.

LOCATION MAP

c \

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LOCATION AND ACCESS

The p r o p e r t y i s l o c a t e d w i t h i n t h r e e km s o u t h w e s t o f Greenwood and f o u r km s o u t h w e s t of t h e f o r m e r l y p r o d u c i n g Phoenix Mine. Greenwood i s l o c a t e d on t h e s o u t h e r n T r a n s p r o v i n c i a l highway N o . 3 , 430 r o a d km east o f Vancouver, B.C.

Access from t h e n o r t h t o t h e p r o p e r t y is p r o v i d e d by t h e Lind Creek road o r i g i n a t i n g from Greenwood. Access from t h e s o u t h is v i a t h e a l l w e a t h e r Phoenix-Lone S t a r h a u l r o a d a l o n g t h e s o u t h o f M t . A t w o o d .

HISTORY

The h i s t o r y o f t h e area stems from t h e h i s t o r i c Phoenix mine which w a s i n p r o d u c t i o n o r i g i n a l l y f rom 1900 t o 1919 and s u b s e q u e n t l y f rom 1959 t o 1978. The mine produced a t o t a l o f 30 m i l l i o n grams o f gold, 92 m i l l i o n grams o f s i l v e r and 250,050 t o n n e s o f coppe r from 27 m i l l i o n t o n n e s mined.

O t h e r p a s t p r o d u c e r s i n t h e area i n c l u d e t h e Winnipeg w i t h i n f o u r km east o f t h e Sun. The Winnipeg produced some 53,430 t o n n e s g r a d i n g 7.7 grams p e r t o n n e g o l d (0 .2 o z / t o n ) . E x p l o r a t i o n and development o f t h e Winnipeg-Golden Crown ( a n a d j a c e n t p r o d u c e r ) is c u r r e n t l y b e i n g e x p l o r e d by Grand F o r k s Mines - C o n s o l i d a t e d Boundary.

Noranda Resources h a s comple t ed a d r i l l i n g program i n 1986 on t h e a d j a c e n t Crown g r o u p and are c u r r e n t l y expand ing t h e e x p l o r a t i o n program i n . The d r i l l i n g w a s l o c a t e d a p p r o x i m a t e l y one km n o r t h e a s t of t h e n o r t h e a s t c o r n e r o f t h e Sun c l a i m .

S k y l a r k i n 1986 carried o u t a n underground e x p l o r a t i o n program on a n adjacent p r o p e r t y t o t h e n o r t h o f t h e Sun claim. The l o c a t i o n of t h e work ings is a p p r o x i m a t e l y one km w e s t of n o r t h o f t h e n o r t h w e s t c o r n e r o f t h e Sun claim.

An e x t e n s i v e program h a s been r e c e n t l y comple ted (November 1986) on a n a d j a c e n t p r o p e r t y t o t h e s o u t h and s o u t h e a s t .

0 1 2 3 4Kn 4

S C A m Mllb N.T.S. DmWNm k5O.OOo 3- *In ser/e CIO-COW R G W : 2

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On t h e Sun C l a i m Group fo rmer e x p l o r a t i o n i n c l u d e d 4.7 km of a geochem s u r v e y i n 1979. The r e s u l t s i n d i c a t e d a number of anomalous areas ( g r e a t e r t h a n 20 ppb) i n go ld . S e v e r a l of t h e anomalous areas were r e p o r t e d l y known t o be o v e r l a i n by s h a l l o w o v e r b u r d e n a d j a c e n t t o bedrock e x p o s u r e s w i t h q u a r t z v e i n i n g and f r a c t u r e f i l l i n g s . The q u a r t z w a s o f t e n o b s e r v e d t o c o n t a i n p y r i t e (McLeod 1 9 7 9 ) . A l o c a l i z e d magnetometer and VLF-EM s u r v e y ( n o r t h c e n t r a l area) r e t u r n e d poor r e s u l t s w i t h i n a n area o f c o n s i d e r a b l e q u a r t z v e i n i n g w i t h some p y r i t e m i n e r a l i z a t i o n (McLeod 1 9 7 9 ) .

On t h e Sunnys ide claim a n unknown q u a n t i t y of s i l v e r - l e a d - z i n c ore w a s s h i p p e d i n 1934.

On t h e Fanny Joe r e p o r t e d ( 1 9 3 3 ) work ings i n c l u d e s e v e r a l open c u t s and a s h a f t sunk on a f o u r i n c h q u a r t z v e i n t r a c e a b l e f o r 300 f e e t m i n e r a l i z e d w i t h p y r i t e and lesser amounts of g a l e n a .

Chipolm ( 1973 ) r e p o r t s t h a t s e v e r a l p r o s p e c t p i t s and s h a l l o w i n c l i n e d s h a f t s have been e x c a v a t e d on t h e Sunnys ide Crown G r a n t . The p i t s are w i t h i n l i m e s t o n e and impure q u a r t z i t e i n beds s i x i n c h e s t o 36 i n c h e s t h i c k s t i k i n g 40" t o 45" W and d i p p i n g 20" t o 40" n o r t h e a s t e r l y . A f o u r f o o t sample across a h e a v i l y o x i d i z e d l e n s r e t u r n e d 3.92% l e a d , 6.63% z i n c , 0.13% c o p p e r , 4 . 1 4 o z / t o n s i l v e r and 0.02 o z / t o n g o l d . S e l e c t e d samples f rom t h e p i l e o f ore s t a c k e d n e a r t h e p o r t a l c o n t a i n e d more t h a n 50 oz s i l v e r p e r t o n .

GEOLOGY AND MINERALIZATION

The g e n e r a l geo logy of t h e p r o p e r t y as described by L i t t l e , G.S.C. Map 6 - 1957, K e t t l e R i v e r , E a s t H a l f , is of t h e A n a r c h i s t Group of greenstone, greywacke, l imes tone and p a r a - g n e i s s . The A n a r c h i s t g r o u p c o n s i s t s v e r y l a r g e l y of h i g h l y metamorphosed s e d i m e n t a r y r o c k s b u t i n c l u d e s also a l t e r e d g r e e n s t o n e s and p o s s i b l y a l so a l t e r e d i n t r u s i v e rocks . The s e d i m e n t a r y members o f t h e g r o u p are t h e a l t e r e d e q u i v i l e n t s of q u a r t z i t e , s l a t e and l i m e s t o n e , micaceous q u a r t z i t e s , mica s c h i s t s , and c r y s t a l l i n e l imes tone . The s h e a r e d g r e e n s t o n e s p o s s i b l y r e p r e s e n t b o t h i n t r u s i v e and e x t r u s i v e t y p e s .

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A second g roup of r o c k s w i t h i n t h e A n a r c h i s t series are l i g h t g r e y , g r a n i t i c r o c k s , q u i t e g e n e r a l l y g n e i s s i c , t h e o u t c r o p s of which have i n some cases a s l i g h t l y r u s t y appea rance . Q u a r t z and m i c r o l i n e predominate w i t h oligoclase and a lb i t ic -o l igoc lase g e n e r a l l y p r e s e n t . The g r a n i t i c r o c k s are i n t r u s i v e i n t o t h e s c h i s t s of t h e A n a r c h i s t series.

Another g r o u p of r o c k s w i t h i n t h e A n a r c h i s t series c o n s i s t s of wheared b a s i c i n t r u s i v e s which can i n loca l areas b e r e p r e s e n t e d as s e r p e n t i n e w i t h c o n s i d e r a b l e p y r i t e deve lopment i n a s s o c i a t i o n w i t h s h e a r zones .

F e l d s p a r porphyry ' 'dykes" are also common i n t h e area. The r o c k is d e s c r i b e d as a " p a l e p i n k t o f l e s h c o l o r e d , f i n e - g r a i n e d r o c k w i t h g r a n i t i c t e x t u r e . Q u a r t z is f a i r l y common and f e l d s p a r , s h r e a d s of b i o t i t e , h o r n b l e n d e , small i n d i v i d u a l s of a p a t i t e and some i r o n ore make up t h e b a l a n c e of rock".

L o c a l l y t h r e e d i f f e r e n t rock u n i t s are r e p o r t e d on t h e p r o p e r t y . A metamorphosed sed imen t - v o l c a n i c u n i t ; a medium-grained g r a n o d i o r i t e ; and a b a s a l t .

M i n e r a l i z a t i o n r e p o r t e d on t h e p r o p e r t y i s p y r i t e , p y r r h o t i t e , m a g n e t i t e , a r s e n o p y r i t e , g a l e n a , s p h a l e r i t e and c h a l c o p y r i t e . The m i n e r a l i z a t i o n is accompanied by nar row q u a r t z v e i n s i n t h e metamorphosed sed imen t - v o l c a n i c u n i t .

GEOCHEMICAL PROCEDURE

I .. Survey Procedure

A g r i d sys tem of n o r t h - s o u t h l i n e s a t 1 0 0 meter i n t e r v a l s w a s e s t a b l i s h e d c o v e r i n g t h e p r o p e r t y w i t h e x c e p t i o n t o t h e e a s t e r n and e a s t - c e n t r a l p o r t i o n . A more d e t a i l e d g r i d w a s p l a c e d o v e r t h e Sunnys ide and Fanny Joe r e v e r t e d Crown g r a n t s . Samples w e r e p i c k e d up a t 50 metre i n t e r v a l s a l o n g t h e g r i d l i n e s . Samples w e r e selected from t h e B h o r i z o n of t h e brown t o brownish-gray sandy-loam f o r e s t s o i l a t a d e p t h of commonly 30 c e n t i m e t r e s . The so i l w a s p l a c e d i n a brown w e t - s t r e n g t h p a p e r bag w i t h t h e g r i d c o o r d i n a t e s marked t h e r e o n . A t o t a l of 532 samples w e r e a n a l y s e d . Twenty-six l i n e kms of s u r v e y were comple ted .

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2. T e s t i n g P r o c e d u r e

A l l s amples were t e s t e d by A c m e L a b o r a t o r i e s of Vancouver , B. C. The t e s t i n g p r o c e d u r e i s t o f i r s t t h o r o u g h l y d r y t h e sample, Whereupon - 5 0 0 grams o f mater ia l i s d i g e s t e d w i t h 3 m l . of 3:1:3 HCL t o HNo3 t o H20 a t 90 deg . more or less fo r one hour . The sample is d i l u t e d t o 1 0 m l s . w i t h water, The samples w e r e t h e n a n a l y z e d by atomic a b s o r p t i o n f o r t h i r t y elements. Two e l e m e n t s - s i l v e r and a r s e n i c w i t h l o c a l i z e d g o l d were p l o t t e d .

3 . Trea tment of Data

I n a s s e s s i n g t h e d a t a r e s u l t s , t h e background, sub-anomalous and anomalous v a l u e s w e r e d e t e r m i n e d u t i l i z i n g a s t a t i s t i c a l s o f t w a r e program on a n I.B.M. computer .

The sub-anomalous t h r e s h o l d v a l u e , which i s a v a l u e n o t c o n s i d e r e d anomalous, b u t a n i n d i c a t o r of p o t e n t i a l m i n e r a l i z a t i o n , is t a k e n as one s t a n d a r d d e v i a t i o n from t h e mean background v a l u e . The anomalous v a l u e s or t h e pr ime i n d i c a t o r v a l u e s a re t a k e n af t w o s t a n d a r d d e v i a t i o n s from t h e mean background v a l u e .

The r e s u l t s o f t h e d a t a t r e a t m e n t w e r e as f o l l o w s :

A 9 (PPm) A s (PPm

Mean backgroud v a l u e . 4 5 9.0 Sub-Anomalous - 3 3 15.8 Anomalous t h r e s h o l d v a l u e - 1 9 22 .6

All values are in p a r t s per million.

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GEOPHYSICAL SURVEY

VLF-EM SURVEY

A s a b r e Model 27 VLF-EM R e c e i v e r i n s t r u m e n t manufac tu red by S a b r e E l e c t r o n i c s o f Vancouver w a s u t i l i z e d i n t h e VLF-EM s u r v e y .

The VLF-EM Receiver measures t h e amount of d i s t o r t i o n produced i n a p r imary t r a n s m i t t e d magne t i c f i e l d - i n t h i s case S e a t t l e a t a f r e q u e n c y 24.6 Khz - and a s e c o n d a r y m a g n e t i c f i e l d which may be induced by a c o n d u c t i v e mass s u c h as a s u l p h i d e body. The VLF-EM u n i t - d u e t o i t s r e l a t i v e l y h i g h f r e q u e n c y - c a n d e t e c t l o w c o n d u c t i v e zones s u c h as f a u l t or s h e a r zones , c a r b o n i z e d s e d i m e n t s or l i t h o l o g i c a l c o n t a c t s .

The major d i s a d v a n t a g e of t h e VLF method, however i s t h a t t h e h i g h f r e q u e n c y r e s u l t s i n a m u l t i t u d e o f a n o m a l i e s from unwanted s o u r c e s such as swamp e d g e s , c r e e k and t o p o g r a p h i c a l h i g h s .

The VLF-EM r e s u l t s are i n d i c a t e d i n p r o f i l e based on t h e r a w f i e l d r e s u l t s . The g r i d sys t em o f t h e geochemica l s u r v e y w a s u sed f o r t h e g e o p h y s i c a l s u r v e y w i t h r e a d i n g s t a k e n a t 25 metre i n t e r v a l s .

RESULTS - GEOCHEMICAL SURVEY

The geochemica l s u r v e y d i s c l o s e d a number o f l o c a l i z e d s i l v e r and lesser a r s e n i c a n o m a l i e s t o t h e east of a north-northwesterly flowing creek through the central portion of t h e Sun m i n e r a l claim,

L o c a l i z e d s i l v e r anomalies occur w i t h i n t h e n o r t h e a s t e r n p o r t i o n and a p p e a r t o t r e n d g e n e r a l y s u b p a r a l l e l t o t h e s t r u c t u r a l t r e n d as i n d i c a t e d t o p o g r a p h i c a l l y by t h e c r e e k or e a s t e r l y f rom t h e c r e e k zone , A p o r t i o n o f t h e s h a f t zone a t 9 0 0 s 500E i s covered by sub-anomalous ( . 3 ppm A g ) s i l v e r v a l u e s . G e n e r a l l y t h e anomalous s i l v e r v a l u e s ( . 45 ppm Ag) occur p e r i p h e r a l t o t h e s h a f t zone.

Anomalous s i l v e r va lues occur w i t h i n t h e Sunnyside-Fanny Joe area as a d e f i n i t i v e eastern t r e n d from t h e Creek Zone, The anomalous s i l v e r v a l u e s correlate i n p a r t w i t h a large sub-anomalous a r s e n i c area and s p e c i f i c a l l y w i t h anomalous a r s e n i c v a l u e s ( > 22.6 ppm A s ) .

S e l e c t e d s o i l samples were a s s a y e d f o r g o l d w i t h i n t h e c o r r e l a t i v e anomalous areas. Anomalous gold v a l u e s o f up t o 400 ppb o c c u r a t 1000E 2100s.

. Sookoch ff Consvltants Im. J

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VLF-EM SURVEY

The VLF-EM s u r v e y was c a r r i e d o u t w i t h i n t h e n o r t h e r n p o r t i o n o f t h e claim group and i n c l u d e d f o u r l o c a l i z e d s i l v e r anomalous zones .

I f t h e VLF-EM anomal i e s i n d i c a t e s t r u c t u r e s , t h e s u r v e y s d i s c l o s e d a c o n j u g a t e set o f s t r u c t u r e s . The p redominan t s t r u c t u r e s t r e n d n o r t h - n o r t h e a s t e r l y s u b - p a r a l l e l i n g t h e t r e n d o f t h e s t r u c t u r a l l y i n f e r r e d ( t o p o g r a p h i c a l ) c r e e k zone. A complementary set of s t r u c t u r e s t r e n d n o r t h - e a s t e r l y t o e a s t e r l y .

The s h a f t zone a t 900s 500E w a s n o t r e f l e c t e d w i t h i n a s t r u c t u r a l zone however, a n o r t h w e s t e r l y t r e n d i n g s t r u c t u r e is i n d i c a t e d some 1 0 0 metres to t h e n o r t h w e s t . The c r e e k i s a l so 1 0 0 metres t o t h e w e s t .

The s h a f t a t 150E 1620s is located w i t h i n a n o r t h w e s t e r l y t r e n d i n g s t r u c t u r e a l i g n e d w i t h a s h a f t a t O + O O 1380s which i s i n d i c a t e d t o o c c u r a l o n g a n o r t h e a s t e r l y t r e n d i n g s t r u c t u r e .

Two of f o u r l o c a l i z e d s i l v e r a n o m a l i e s w i t h i n t h e VLF-EM s u r v e y area are l o c a t e d i n a s s o c i a t i o n w i t h s t r u c t u r a l i n d i c a t i o n s . The known m i n e r a l i z e d zones on t h e S u n n y s i d e and Fanny' Joe a t t h e s o u t h e a s t p o r t i o n o f t h e p r o p e r t y were n o t c o v e r e d by t h e i n i t i a l s t a g e o f t h e s u r v e y however , t h e geochemica l anomal i e s g e n e r a l l y t r e n d i n a n e a s t e r l y t o s o u t h - e a s t e r l y d i r e c t i o n .

CONCLUSIONS

The geochemica l and g e o p h y s i c a l s u r v e y s w e r e s u c c e s s f u l i n d e l i n e a t i n g areas o f p o t e n t i a l economic m i n e r a l zones .

The geochemica l s u r v e y d e l i n e a t e d anomalous zones w i t h i n t h e Sunnyside-Fanny Joe work ings where known m i n e r a l zones w e r e n o t detected i n t h e s u r v e y . The known zones o f p r e d o m i n a n t l y b a s e metal m i n e r a l i z a t i o n may e i t h e r b e l o c a l i z e d or masked by ove rburden . The p e r i p h e r a l s i l v e r - g o l d a n o m a l i e s may e x p r e s s p e r i p h e r a l p r e c i o u s metal m i n e r a l i z a t i o n t o a c e n t r a l base metal zone.

c S m k o c h , Consultants Inc. J

-8-

RECOMENDATIONS

Geochemical, geophysical and geological surveys should be completed over the balance of the property. Upon compilation of the results, the prime correlative anomalous areas should be trenched, mapped and sampled., IP surveys would follow to test for potential economic mineralization at depth. Test diamond drill holes would test the prime zones.

.tted,

'f, P.Eng. st.

Vancouver, B.C. May 28, 1987.

-9-

CERT I F I CATE

I, Laurence Sookochof f , o f t h e C i t y o f Vancouver, i n t h e P r o v i n c e of B r i t i s h Columbia , d o he reby c e r t i f y :

Tha t I a m a C o n s u l t i n g Geologist and p r i n c i p a l of Sookochoff C o n s u l t a n t s I n c . w i t h o f f i c e s a t 609-837 West H a s t i n g s S t , , Vancouver, B.C., V6C 1B6

I f u r t h e r c e r t i f y t h a t :

1 . I a m a g r a d u a t e o f t h e U n i v e r s i t y of B r i t i s h Columbia ( 1 9 6 6 ) and h o l d a B,Sc. d e g r e e i n Geology,

2. I have been p r a c t i s i n g my p r o f e s s i o n f o r t h e p a s t twenty-one y e a r s .

3 . I a m r e g i s t e r e d w i t h t h e A s s o c i a t i o n of P r o f e s s i o n a l

4 . The i n f o r m a t i o n f o r t h i o b t a i n e d from s o u r c e s as c i ted u n d e r b i b e s u p e r v i s i o n o f t h e e x p l o r a t i o n p r o g r

E n g i n e e r s o f B r i t i s h Columbia.

P.Eng,

May 28 , 1987. Vancouver, B, C e

r

-1 0-

Sunnyside Resources Ltd 1987 SUN CLAIM GROUP

1987 GEOCHEMICAL AND GEOPHYSICAL SURVEY

STATEMENT OF COSTS - - - - - - - - - - --_I - - - --- --

The geophysical and geochemical survey was carried out on the Sun mineral claim from February 1 , 1987 to April 15, the value of the following:

GEOCHEMICAL AND GEOPHYSICAL SURVEY

M. Klein, A. Kabatoff February 1 , 1987 to April 15, 1987 20 days @ $290/day

Truck rental 20 days @ $40/day plus gas

Room and Board 20 days @ $35/man/day

Draughting and compilaton

Assaying

Report

$5,800.00

1,080.00

1,400.00

625.00

3,231.90

1,200.00

$13,336.90

1987 to

-11-

\

BIBLIOGRAPHY

1. Chisholm, E.A. G e o l o g i c a l Repor t on t h e Greenwood Mineral P r o p e r t y of S i l v e r F a l l s Resources L t d . , Oc tobe r 1, 1973.

2. C o c k f i e l d , W.E. ( 1 9 3 5 ) - Lode Gold D e p o s i t s a t F a i r v i e w Camp, Camp McKinney, and V i d e t t e Lake A r e a , and t h e Dividend Lakeview P r o p e r t y near Osoyoos, B.C.; G.S.C., Memoir 179.

3. Leroy , O.E. ( 1 9 1 1 ) - Map 16A, Pheon ix , B r i t i s h Columbia; G.S.C., M e m o i r N o . 21.

4. McLeod, J . W . - P r o p e r t y on b e h a l f o f March Resources L td . , November 8, 1979. G e o l o g i c a l R e p o r t on t h e Okum P r o p e r t y f o r George O ' B r i e n , J u n e 7 , 1 9 7 9 . G e o l o g i c a l R e p o r t on t h e Okum P r o p e r t y on b e h a l f of Midwest Pe t ro l eum L i m i t e d , Oc tobe r 6, 1978.

5. McNaughton, D.A. ( 1 9 4 6 ) - Paper 45-20, b r i e f r e p o r t and p r e l i m i n a r y map of t h e Greenwood-Pheonix area; G.S.C., O t t a w a .

APPENDIX

ASSAY CERTIFICATES

,C A N A L Y T I C A L LABORATORIES 852 E. HCISTINGS ST. VANC EH B.C. V6A 1Hb FHONE 253-3158 DATA LINE 2 3 1 - 4

G E O C H E M I C A L ICF' A N A L Y S I S

.SO0 6RAM SAMPLE IS DI6ESTED WITH 3ML 3-1-2 HCL-HN03-HZO AT 95 DE6.C FOR ONE HOUR AND 18 DILUTED TO 10 ML WITH WATER, THIS LEACH IS PARTIAL FOR MN FE CA P LA CR M6 BA TI B N AND LIMITED FOR NA AND K. AU DETECTION LIMIT BY ICP IS 3 PPM. - SAMPLE TYPE1 Pulp AUI ANALYSIS BY AA FRO# 10 6RAM SAMPLE.

DATE RECEIVED! NAY 29 1987 DATE HEFORT MAXLEDr )Ad @ 7 ASSAYER. /<$?a. DEAN TOYE. C E R T I F I E D 8 . C. ASSAYER

SOOEOCHOFF CONSULTANT P R O J E ( , I - SIINNY SIDE F1 1 e # 87-122:K F s a e Q

SAMPLE# no CU PF IN A6 N I CO NN FE AS U AU TH SP CD 58 E1 V CA P LA CR M6 BA T I 8 dL NA K W AUt PPN PPM ppn ppn PPn PPM PPM ppn I PPM PPM ppn ppn ppn ppn PPM ppn PPM x x ppn PPM I PPN 1 PPR x I 1 PPM PPB

800E 15005 1 14 4 71 . l 44 6 284 1.66 4 5 ND 3 30 1 2 2 29 .25 ,130 8 25 .27 188 .09 6 1.40 .03 -06 1 - 800E 1550s 1 11 7 60 .1 36 5 429 1.44 7 5 ND 1 39 1 2 2 25 .45 ,135 6 20 .20 173 -08 3 1.23 .03 .Ob 1 - BOO€ 16005 1 19 7 55 -1 54 8 169 2.07 7 5 ND 3 23 1 2 2 40 .23 .019 9 40 .46 102 . l ? 2 1.58 -03 .Ob 1 - 800E 1650s 1 16 6 87 . 3 56 7 176 2.13 3 5 ND 4 30 1 ? 2 37 .29 ,157 12 30 .30 140 .12 3 2-12 .04 - 0 4 1 - EOOE 17005 1 24 3 26 - 3 34 4 338 1.05 6 5 ND 1 60 1 2 2 21 1.01 ,026 4 20 .21 65 -05 3 -88 .05 .04 1 - 800E 17505 1 32 14 126 . l 54 9 390 2.37 29 5 ND 2 24 1 2 2 42 - 3 6 ,055 11 45 .59 70 .09 2 1.18 .03 .OB 1 - 800E 18005 1 14 6 118 .1 59 8 854 1.79 11 5 ND 2 24 1 2 3 27 .20 .368 5 26 .22 137 .I1 3 2.50 .03 .05 1 - 800E 19005 1 12 8 104 .3 37 7 311 1.79 9 5 ND 3 23 1 2 2 28 -30 .344 6 25 -26 121 . lo 4 1.93 .03 .04 1 - 800E 18505 1 14 9 149 a1 94 10 404 2.03 8 5 ND 3 15 1 2 3 33 .14 ,123 6 51 -37 110 a10 3 1.36 a03 ,OS 1 -

BOO€ 19505 1 16 8 125 e3 55 7 257 1.86 7 5 ND 4 27 1 2 2 31 .32 ,171 11 32 .35 102 010 2 1.73 -03 *05 1 -

BOOE 20005 1 35 9 100 .2 89 8 254 2.55 9 5 ND 6 22 1 2 2 45 2 8 .113 14 38 '57 123 -11 5 2.24 .03 .08 1 - BOOE 20505 1 15 5 67 .1 81 8 180 2.02 5 5 ND 4 22 1 2 2 33 .23 .075 10 46 .37 94 .I1 5 1.66 .03 -04 1 - BOOE 21005 1 17 9 49 .1 119 10 210 2.12 9 5 ND 4 16 1 2 2 35 .17 ,095 9 54 .41 76 ,11 2 1.85 .03 .03 2 - 800E 21505 1 20 6 49 .1 123 11 237 2.34 9 5 NO 3 20 1 2 2 41 .24 ,086 12 93 -58 95 .09 2 1.22 .03 .04 1 - 800E 22005 1 18 11 101 .1 305 14 614 2.38 12 5 ND 3 18 1 2 2 36 .20 .243 7 74 .47 143 -11 3 2.33 -03 e 0 4 1 - BOOE 22505 1 24 7 76 -1 185 15 278 2.54 7 5 ND 4 19 1 2 2 40 -21 .OB4 12 103 .63 105 -11 4 1.86 e03 S O 5 1 - 800E 23005 1 27 15 101 .1 277 19 436 3.30 14 5 ND 3 21 1 2 2 51 .23 .091 8 127 1.05 141 .13 2 2.41 .03 -06 1 - 8COE 24905 1 11 6 59 .1 122 12 356 ! . e 9 ? 5 I 2 15 ! 2 2 31 -14 -114 b 127 .57 158 .09 5 1.21 .Ox -03 1 - 800E 23505 1 11 7 77 - 1 173 15 379 2.32 9 5 ND 3 12 1 2 2 38 -12 .178 6 135 .64 158 -10 5 1.78 -03 *OS 1 -

800E 24505 1 14 12 66 -2 118 11 296 2-02 9 5 ND 2 18 1 2 2 32 .15 .171 6 81 . I 6 160 .12 3 2.13 -03 S O 5 1 -

800E 25005 1 17 8 87 .1 343 24 691 2.65 9 5 ND 3 21 1 2 2 43 -16 .152 8 131 .81 171 .12 3 2.13 a03 a07 1 - 800E 25505 1 22 9 86 - 3 244 18 247 2.77 11 5 ND 3 15 1 2 2 46 .15 .lo6 8 150 .81 125 . lo 2 1-99 a 0 2 *07 1 - 800E 26005 1 15 11 52 . l 148 11 313 1.96 6 5 ND 2 21 1 2 2 34 .28 .lo0 9 79 .54 108 .09 3 1.42 -03 -05 1 - EOOE 26505 1 13 10 48 .l 334 27 272 2.65 9 5 NU 3 29 1 2 2 30 .25 .353 6 170 .56 259 .08 2 1.42 .03 .04 2 - BOOE 27005 1 15 9 68 .1 372 17 194 2.32 6 5 ND 4 23 1 2 2 35 .34 .ME 11 93 .66 110 .12 4 2.27 .03 .04 1 - 8OOE 27505 1 17 9 46 .1 147 12 206 2.26 4 5 ND 3 15 1 2 2 38 .16 ,054 9 55 .50 99 .14 2 2.25 .03 SO4 1 1 800E 28005 1 15 9 56 .1 155 14 179 2.42 7 5 ND 3 16 1 2 2 39 .17 ,149 8 69 .55 133 .13 3 2.45 .03 .04 1 3 800E 28505 2 61 9 80 . l 214 16 257 3.90 15 5 ND 4 17 1 2 2 71 .21 ,054 13 208 1.31 109 -09 2 1.88 .02 .OS 1 5 BOOE 29005 1 24 9 66 , l 147 13 276 2.59 18 5 ND 4 13 1 2 2 46 -17 .071 11 85 .67 84 .14 2 2.34 .03 .04 I 3 BOOE 29505 1 24 11 106 .I 219 14 415 2.18 49 5 N D 5 18 1 2 '2 39 .31 .I26 10 81 ,64 110 .12 3 2.46 .03 .Ob 1 1

800E 30005 1 17 11 66 . l 148 15 661 2.38 20 5 ND 3 18 1 2 2 38 -20 ,198 7 78 .58 132 .12 3 2.22 .03 -03 1 1 STD C 20 59 37 134 6.9 70 28 1005 3.?4 41 15 8 36 48 18 17 19 64 .47 ,102 36 58 .E8 171 .OB 37 1.72 .07 .13 13 - 900E 1000s I 25 10 124 - 3 36 8 340 2.19 3 5 ND 5 22 2 2 2 39 ,21 .I27 13 26 .39 130 .12 4 2.33 -03 -06 1 - 900E 10505 1 25 11 102 .1 49 7 346 1.87 13 5 ND 3 17 1 2 2 32 .15 ,104 9 25 .30 158 .11 - 2 2.02 .03 -05 1 - 900E 11005 1 26 13 117 . 2 41 9 315 2017 9 5 ND 4 17 1 2 2 39 , I6 ,108 10 32 .39 167 a11 2 2.09 e 0 3 S O 5 1 -

900E 11505 1 34 10 195 .3 80 10 290 2.31 12 5 ND 4 22 1 2 2 40 .20 ,093 12 41 -47 209 .12 2 2.26 .03 -09 1 - 900E 12005 1 14 9 99 . 2 34 7 300 1.64 8 5 ND 2 20 1 2 2 27 .16 .252 5 19 .22 130 ,10 4 1.86 .03 .Ob 1 -

c

C '

(.

(

c

c

c

t

SAMPLE#

900E 1250s 906E 13005 900E 13505 900E 14005 960E 1450s

900E 15005 900E 1550s 900E 16005 900E 16505 900E 17005

900E 17505 900E 18005 900E 1850s 900E 19005 900E 19505

90oE 20005 900E 2050s 900E 21005 900E 21505 900E 22005

90M 22505 9 0 E 23005 900E 23505 STD C 9OOE 2400s

900; 21505 900E 25005 90oE 25505 900E 2600s 90OE 26505

900E 27005 900E 2750s 900E 2800s 9ooE 28505 900E 2900s

900E 29505 900E 30005

MO CU PB ZN PPM PPM PPW PPM

1 26 8 112 1 21 8 123 1 14 9 90 1 19 9 81 1 21 9 63

1 23 8 57 1 18 5 68 1 15 7 94 1 15 7 81 1 1 1 6 69

1 23 10 82 1 21 9 101 1 32 10 60 1 25 10 76 1 10 6 76

1 13 7 57 1 22 io 85 1 24 8 58 1 23 10 117 1 12 10 176

1 16 17 196 1 14 6 93 1 16 9 127 20 59 36 133 1 14 12 118

1 11 8 148 1 9 8 6 0 1 19 10 79 1 11 9 76 1 17 10 56

1 5 2 2 6 1 15 9 49 1 14 9 48 1 12 8 52 1 17 8 57

1 29 9 84 1 8 6 3 5

SOOKOCHOFF CONSULTANTS F'ROJkCT - SUNNY SIDE FILE # 87-1223H Faqe 1 0

~6 NI co MN FE as u AU TH SR CD SB B I v CA P LA CR t16 [ t ~ TI B ni N& K Y Aut PPM PPM PPM PPW I PPW ppn PPM PPM PPM PPM PPn PPM PPW x x PM PPM 1 PPM I PPM z x 2 PPI( PPB

.3 40 9 398 2.31 7 5 ND 4 19 1 2 2 46 .17 ,130 10 35 .46 178 .12 2 2.39 .03 .06 1 -

. 2 44 8 315 1.91 4 5 ND 3 17 1 2 3 35 .15 ,078 8 30 .37 123 .lo 2 1.84 .03 .06 1 -

.I 39 7 433 1.87 6 5 ND 3 27 1 2 2 32 .20 ,083 7 25 .34 157 .09 2 1.53 .03 .06 1 -

.1 44 7 472 1.88 5 5 ND 4 27 1 2 2 33 -22 .119 10 25 .36 187 .lo 3 1.74 .03 .07 1 -

.I 33 7 432 1.83 3 5 I D 3 30 1 2 2 35 .24 .089 0 24 .35 135 .10 3 1.74 .03 -05 1 -

.I 49 9 352 2,li 5 5 ND 4 23 1 2 2 43 .23 ,053 10 36 .42 110 .lo 2 1.44 .02 .05 1 -

.1 34 6 373 1.73 5 5 NO 5 30 1 3 2 33 .22 .089 10 24 -31 150 .l0 2 1.47 -03 .06 1 -

.l 35 7 518 1.97 6 5 ND 4 23 1 2 2 36 .20 .085 10 29 .36 125 .lo 3 1.43 .03 .07 1 -

.1 37 6 377 1.74 2 5 ND 3 25 1 2 2 32 .22 ,084 10 30 -33 131 .09 5 1.25 .03 .07 1 -

.I 50 7 359 1.71 3 5 ND 3 22 1 2 2 30 .21 ,112 8 35 .29 149 .09 3 1.12 .03 .OS 1 - -3 75 8 209 2.21 7 5 ND 4 21 1 2 2 38 .18 ,126 9 35 -41 204 .I1 3 1.99 .03 -08 1 - . 2 74 8 398 2.11 ? 5 ND 4 22 1 2 2 36 .18 .119 9 33 .40 188 .ll 8 1.94 .03 .07 1 - .I 61 10 373 2.38 7 5 ND 5 28 1 2 2 46 .35 .Ob5 15 50 .66 98 .10 4 1.32 .03 .ll 1 - - 2 45 5 156 1.51 6 5 ND 2 53 1 2 2 28 .39 ,075 7 19 .27 174 -09 5 1.25 .03 .07 1 - .1 43 5 226 1.71 8 5 I D 3 19 1 2 2 30 .16 ,151 8 25 .28 148 .09 2 1.51 ,03 .05 1 - .1 53 7 198 2.21 4 6 ND 6 28 1 2 2 43 .24 .053 15 35 .40 140 . I 2 3 1.56 .03 .06 1 - .2 54 9 776 2.36 10 7 ND 4 21 1 2 3 41 .20 .091 12 30 .40 186 .13 2 1.98 .03 -08 1 - .1 32 7 303 1.81 6 5 NO 2 19 1 2 2 34 .23 .073 5 29 .34 92 .09 2 1.25 .02 .06 1 - .1 65 9 782 2.14 26 5 ND 2 22 1 2 2 35 .21 ,271 6 36 .36 270 .10 3 1.92 .03 -08 1 - .1 47 7 631 1.88 4 5 ND 4 20 1 2 4 28 .34 ,145 7 25 .24 105 .ll 11 2.10 .04 .08 1 -

b.0 69 28 1029 3.98 40 14 8 36 48 18 17 21 64 .48 .lo1 36 55 .88 173 .OB 37 1.73 .07 .13 15 - .1 50 7 335 2.00 8 5 ND 4 25 1 2 2 29 .73 .064 10 33 .32 111 .12 7 1.96 .04 .OS 1 -

72 8 239 2.33 10 5 ND 4 24 1 2 2 41 .23 .127 10 41 .51 173 a12 3 2.23 -03 e08 1 -

* 1 77 7 316 2.18 2 5 ND 6 31 1 2 2 36 .29 .lo4 14 32 ,38 174 e l l 2 2.05 -03 SO7 1 -

1.3 44 6 241 2.01 5 5 ND 4 26 1 2 2 25 -90 -052 11 27 .28 85 a1 0 11 1.78 e03 -04 1 -

.i 73 8 4231.88 5 5 no 3 :a : 2 2 26 .3c.099 6 53 .3e :a3 .:e 4 1 . ~ 0 ,os .os ! - - 1 130 12 447 2.04 6 5 ND 2 14 1 2 2 32 .14 ,060 5 147 .52 111 .10 4 1.41 .03 .OS 1 - .l 136 11 524 1.90 10 5 ND 2 16 1 3 2 35 .1? ,062 5 61 .36 93 .lo 3 1.47 .04 .04 1 - e 1 110 10 453 2.22 12 5 ND 5 20 1 3 2 40 .25 ,082 12 87 -53 125 -10 6 1.56 e03 a 0 6 1 - e 1 268 19 295 2.78 12 5 ND 3 18 1 2 2 48 -17 ,045 8 107 -68 108 a13 3 2.10 .03 e04 1 - .l 26 7 218 -96 5 7 ND 1 6 1 2 2 20 .07 .025 2 52 .13 25 .OS 4 .25 .04 .02 2 - .1 160 15 266 2.36 6 5 ND 4 15 1 2 2 41 .14 .043 9 82 .56 99 .13 2 1.92 .03 a 0 5 2 2 .1 111 12 239 2.13 3 5 ND 4 13 1 2 2 34 .09 .14S 6 57 .35 112 .15 2 2.92 .04 .04 2 3 .l 175 13 243 2.38 2 5 ND 3 18 1 2 2 41 .28 .033 7 107 .56 84 .12 2 1.83 .03 .02 2 1 .l 135 14 326 2.18 2 5 ND 3 12 1 2 2 38 .12 .Ob8 7 62 ,45 99 .14 2 2.14 .03 .OS 1 1

.1 47 8 447 2.72 5 5 ND 3 11 1 2 3 44 .12 .21? b 40 .39 112 .17 2 2.64 .OS .Ob 1 1

.l 91 9 133 1.49 4 5 ID 2 13 1 2 2 31 .16 ,016 5 62 .33 61 .I1 2 .94 .03 .04 2 1

Q c: SOOKOCHOFF CONSULTANT PROJECT - SUNNY SIDE F I L E # 87-12Z;H Faae 11

SAtPLE4 NO CU PB ZN A6 NI CO t N FE RS U AU TH SR CD SB PI V CA P LA CR H6 EA T I B AL NA I: W AUt PPM wt wt PPR PPH ppn PPH cpn x wt PPI( PPH w n ppn ppn pp t ppt ppn x x PPM PPH x PPH z wt x x x pp t PPB

lO0OE 10005 1 22 15 136 .5 28 7 460 1.94 8 5 ND 4 19 1 2 2 31 .18 ,196 10 24 .:3 150 .10 2 1.92 .03 .OB 1 -

l00OE 11005 1 31 49 136 .8 50 10 28: 2.64 14 5 ND 5 15 1 2 2 45 .I5 -133 1 1 40 .3 13: .lo 2 2.1: -02 .08 I - IOOOE 11505 1 20 16 109 .4 26 7 636 1 . 7 4 5 5 ND 4 25 1 2 3 29 . ? I .I59 8 23 .28 200 ,I2 2 2.43 .04 .06 1 - ~ O O O E io505 1 24 23 is1 .e 31 7 22; 2.12 io 5 ND 4 16 I 2 2 37 .17 .OB& io 2: -37 129 .i i 2 1.99 .E .07 i -

~ O O O E 1200s 1 24 15 161 .4 39 io 694 2.18 1; 5 ND 3 16 I 2 2 41 .ib ,121 e 29 .40 1;: .ii 4 2.03 .o: .05 I -

lOOOE 12505 I 22 8 77 .1 34 6 410 1.92 5 5 ND 3 20 1 2 2 39 -19 ,100 8 51 .40 124 .IO 3 1.82 .02 .07 1 - IOOOE 13005 1 19 17 105 . 2 53 7 3% 1.86 8 5 NO 3 17 I 2 2 '34 .I6 . I20 8 29 .37 154 .09 16 1.84 .O3 .05 1 - 1000E 13505 1 10 11 1:: .: 27 6 379, 1.68 8 5 ND 2 23 1 2 2 25 .15 ,289 5 24 .23 190 .09 2 1.78 .02 .05 1 - lOO0E 14005 1 2: 6 94 . 2 46 7 389 1.85 3 5 ND 4 25 1 2 2 31 -22 .157 1 1 26 .33 232 .ll 17 2.06 .03 .05 1 - IOOOE 14505 1 26 8 73 . 2 39 9 426 2.36 3 5 ND 4 29 1 2 2 45 .25 ,110 14 66 .71 209 -15 23 2.61 .04 .09 1 -

1000E 15005 1 29 9 68 . 1 60 10 445 2.25 2 5 ND 5 26 1 2 2 39 .22 ,079 14 30 .39 181 .I4 24 2.68 .03 -08 1 - lOOOE 15505 1 18 6 79 - 1 14 6 521 1.70 5 5 ND 2 11 1 2 3 31 -12 .lo5 6 14 .17 75 .09 2 1.14 .03 .05 1 - l600E It005 1 18 13 74 . I 23 6 745 1.88 11 5 ND 3 29 1 2 2 35 .27 ,076 8 21 .30 128 .lo 2 1.53 .02 .Ob 1 - 1OOOE 16505 1 18 6 80 .1 26 6 81: 1.82 6 5 ND 4 19 1 2 2 33 .18 .127 10 21 .SO 153 .09 3 1.42 -03 .07 1 - lO0OE 17005 1 18 11 87 - 2 17 5 657 1.58 5 5 ND 2 17 1 2 2 28 -15 ,066 7 13 .21 123 .08 15 1.31 .03 .06 1 -

(

(

IOOOE 17505 lOOOE 18005 1OOOE 1850s lO0OE 19005 lOOOE 19505

1000E 20005 1OOOE 20505 lOOOE 21005 lOOOE 21505 1OOOE 22005

1 17 10 85 .2 33 6 405 1.88 3 5 ND 3 23 1 2 2 :2 .17 .136 1 16 4 82 . 2 59 8 289 1.93 5 5 ND 3 20 1 2 2 32 .19 .116 1 10 3 52 - 1 29 5 341 1.33 5 5 NU 2 17 1 2 2 25 .13 ,107 1 27 10 90 .2 68 10 267 2.49 7 5 ND 5 29 1 2 2 41 .22 ,131 1 14 4 58 .2 28 6 561. 1.57 6 5 ND 3 21 1 2 2 29 .16 .070

1 21 7 69 .1 31 8 560 2.22 5 5 ND 5 23 1 2 3 42 .20 .0?6 1 27 12 127 .1 37 9 534 2,70 7 5 HD 3 19 1 2 2 48 .19 ,043 1 23 21 118 . 2 43 8 552 2.62 47 5 ND 4 21 1 2 2 44 .22 .OS6 1 22 53 104 .3 28 8 933 2.52 9 5 ND 4 17 1 2 2 43 .I6 .068 1 22 10 79 - 1 35 7 396 2.34 9 5 NU 4 30 I 2 2 41 -27 .024

7 29 8 37 5 18

11 42 7 25

11 26 8 28 10 30 11 22 12 33

-34 -40 .24 * 55 .31

* 33 .50 I48 .38 .43

187 168 127 168 143

167 152 171 130 174

.09

.09

.07 - 1 1 .08

.12

.14

.13

.13

.ll

2 1.67 2 1.59 15 1.07 3 2.19 8 1.34

4 2.01 2 2.10 14 2.17 15 2 . 3 14 1.73

.02 IO2 .03 * 02 .03

,03 .03 .03 .03 . 02

.Ob 1 -

.Ob 1 -

.06 1 - -09 1 - .os 1 - .07 1 1 .07 1 1 .08 1 2 .07 1 4 -10 1 1

I

c

(

(

c

c

lO0OE 22505 1 25 9 83 .3 33 7 642 1.90 13 5 NU 3 24 1 2 3 33 .21 .lo0 10 22 -33 236 .10 19 1.87 .03 .OB I 4 lO0OE 23005 1 36 13 264 .3 47 8 491 2.38 19 5 ND 3 24 1 2 2 39 .26 ,058 8 39 .48 150 .OB 3 1.85 .03 .07 1 I lO0OE 23505 1 25 10 124 .2 67 9 419 2-16 10 5 ND 3 24 1 2 2 36 .47 .070 10 50 .46 120 .09 3 1.56 .03 .12 1 1 lOOOE 24005 1 25 8 109 .1 111 13 385 2.53 6 5 ND 4 20 1 2 2 41 .31 .079 10 74 .58 128 .ll 14 1.88 .03 .08 1 2 lOO0E 24505 1 16 8 172 .1 73 9 919 2.03 5 5 NU 2 23 1 2 2 30 .37 ,178 7 63 .37 224 .09 2 1.61 -03 .07 1 1

l0OOE 25005 1 10 9 156 .l 126 13 377 2.06 19 5 ND 2 14 1 2 2 32 .14 ,127 6 91 .43 127 .09 3 1.45 .03 -04 1 1 1OOOE 25505 1 16 11 99 .2 110 11 472 1.87 11 5 ND 2 18 I 2 2 32 .30 ,070 6 68 ,40 99 .09 4 1.39 .03 -05 1 1 lOOOE 2600s 1 9 12 108 ,1 45 7 481 1.61 7 5 ND 2 14 1 2 2 29 .29 ,069 5 33 .31 85 .08 2 1.15 .03 .Ob 1 - lOOOE 26505 1 13 17 95 .1 78 8 782 1.72 4 5 ND 2 15 1 2 2 29 .32 .lo0 7 57 .39 106 .08 2 1.46 .OS .03 1 - lOOOE 27005 1 12 10 116 - 1 98 9 461 2.22 4 5 ND 3 17 1 2 2 33 .45 ,125 9 56 .48 103 .10 4 2.03 .03 .Ob 1 - lO0OE 27505 1 13 6 59 .1 63 8 436 1.65 2 5 ND 3 14 1 2 2 26 .12 ,168 5 35 .25 111 .lo 2 2.04 - 0 2 .04 1 - STU C 19 59 41 134 6.7 68 28 1005 4.01 41 16 8 34 48 18 16 19 63 .48 -102 36 59 .88 180 .08 37 1.72 .07 -13 13 -

Paae 12 c

SOOKOCHOFF CONSULTANT P R O J E C T -- SUNNY SX DE

fl0 CU PH 2N A6 NI CO IN FE AS U AU TH SR ED SB B1 V 'Pn PPH ppn PPI PPN PPN PPN PPN x PPN PPH P P ~ ppn ppn PPI PPM ppn PPI

SANPLEt I PPI

T I x

B AL NA K PPfl 2 x x

w &Ut PPfl PPB

~ O O O E 2800s lO0OE 28505 100OE 29005 lOOOE 29505 l0OOE 30005

1 16 9 69 . l 65 10 1087 1.91 9 5 ND 1 16 1 2 2 30 1 1: 10 43 , I 148 14 197 2.39 2 5 ND Z 13 1 2 2 38 1 15 8 48 - 1 157 2 291 2.61 3 5 ND 2 13 1 2 2 37 1 1 1 14 44 .1 107 11 j93 1.68 7 5 ND 1 18 1 2 2 28 1 15 1 1 78 ,1 75 12 964 7 . 2 6 10 5 ND 2 13 1 2 2 35

.19 .317 4 45 .38

.15 ,036 6 99 .49 - 1 6 .040 6 140 .4: .26 .042 4 66 .33 ,It ,169 t 55 .36

2:: 1:1 99 83 169

-12 .l: I11 I O 9 I 1 2

3 2.07 .?: .(I3 2 2.09 -03 .O? 3 1.91 -0: . 0 2 3 1.44 .03 - 0 2 4 2.0: .0! .05

2 2.27 .o; .08 3 1.18 .02 .05 5 2.38 .05 .08 5 1.98 .Oz .05 2 2.2: .03 .05

1 -

1 -

1 -

0 -

- _

1lOOE 10005 1lOOE 10505 ll0OE 11005 110OE 11505 1lOOE 12005

1 38 17 167 .3 50 9 344 2.53 6 5 NO 4 21 1 2 2 40 1 20 12 75 . I 27 7 234 1.89 4 5 ND 2 16 1 2 2 34 1 25 14 124 .6 35 7 254 1.94 7 5 ND 4 16 1 2 2 31 1 17 33 135 .9 29 7 497 1.93 9 5 ND 3 22 1 2 2 30 1 19 15 99 .4 38 9 337 1.95 6 5 ND 2 I 6 1 2 2 33

-23 ,084 14 33 .5? ,113 ,075 9 27 .39 .16 ,116 9 19 -30 .20 ,137 6 19 .29 .14 ,066 6 21 .39

202 96 112 146 134

.l:

.OB * 1: .10 .I1

1 - 1 - 1 - 1 - 1 -

IlOOE 12505 llOOE 16005 1lOOE 16505 ll0OE 17005 llOOE 17505

llOOE 1800s 11OOE 1850s llOOE 19005 11OOE 19505 1lOOE 20005

11OOE 20255 llOOE 20505 llOOE 20755 llOOE 21005 llOOE 21255

!100E 21505 llOOE 21755 1lOOE 22005 llOOE 22255 1lOOE 22505

1100E 23005 llOOE 23505 llOOE 24005 IlOOE 24505 llOOE 25005

1 12 1 1 1 18 1; 1 19 13 1 20 9 1 25 21

106 85

10: 92 101

. 2 22 6

.1 21 6

.4 26 6

.I 28 6

.2 30 7

.l 31 6

.1 19 7

.3 30 8 - 1 31 6 .4 26 8

473 1.44 5 5 ND 1 25 1 2 2 26 672 2.02 3 5 ND 3 14 1 2 2 37 999 1.71 5 5 ND 3 26 1 2 2 30 570 1.85 5 5 ND 3 17 1 2 3 32 409 2.23 15 5 ND 4 21 1 2 2 35

516 1.87 5 5 NO 4 23 1 2 2 31 1029 2.17 7 5 ND 2 29 1 2 2 33 461 2.56 7 5 ND 6 25 1 2 3 43 458 1.66 6 5 ND 2 27 1 2 2 31 1015 2.26 42 5 ND 3 21 1 2 2 40

.2: .dl7 5 18 .24

.14 ,108 9 16 .25

.30 -123 8 17 -27

.18 -086 9 24 .32 -17 -062 12 22 .35

.15 ,082 8 22 .26 ,16 .091 8 15 .31 .20 .133 15 27 -41 .19 ,080 8 22 .30 .:1 ,080 8 25 .37

.14 ,104 9 24 .38

.17 ,067 6 15 .24

.15 ,047 9 25 -36

.16 .Ob2 8 18 -30

.20 ,101 7 19 .28

147 179 187 159 172

160 257 227 108 164

168 118 121 137 164

.07 * 13 -10 .!O * 1 1

2 1.17 .02 .?4 4 2.36 - 0 3 .05 4 1.76 .0; -06 3 1.63 .03 .05 3 2.02 .02 '05

1 - 1 - 1 - 1 - 1 -

1 18 9 1 24 8 1 21 15 1 15 11 1 21 18

103 146 96 73 107

.ll

.ll

.12

.OB -12

,14 . 09 .10 .12 -09

01:

I 08 * 09 .ll .11

4 1.99 -03 .05 2 2.02 .03 .OS 4 2.45 .02 -08 2 1.30 .03 .04 2 L O 2 .02 .07

1 - 1 - 2 - 1 1 1 150

1 24 27 152 .6 27 8 819 2.57 162 5 ND 4 17 1 2 2 44 1 14 19 118 - 1 15 6 922 1.74 40 5 ND 1 15 1 2 2 33 1 18 35 139 .4 25 7 802 2.32 100 5 ND 2 16 1 2 2 42 1 20 88 127 1.1 23 8 1159 2.09 107 5 ND 2 16 . 1 3 2 35 1 18 28 191 .4 26 6 1241 1.77 45 5 ND 2 19 2 2 2 30

2 2.82 .O? .05 2 1.36 .03 .03 2 1.49 .02 .OS 4 2.25 .03 .05 4 1.56 .03 .05

4 2.15 .02 .05 3 1.27 .02 .04 2 1.14 .02 .03 4 1.87 .02 .05 2 1.73 .02 .04

2 1.83 .03 .ll 2 1.71 .03 .lo 2 1.42 .03 .08 2 1.00 .03 .04 3 -99 .02 .05

1 1 1 1 1 160 1 400 1 1

1 20 10 153 '2 25 7 1537 2.02 12 5 WC 3 17 1 2 2 35 1 16 20 89 .2 20 6 600 1.87 5 5 ND 2 11 1 2 2 35 1 13 10 BO .1 23 6 912 1.79 2 5 ND 2 19 1 2 2 36 1 24 16 81 - 1 41 8 392 2.37 9 5 NO 5 15 1 2 2 43 1 19 12 73 - 1 29 6 538 2.05 6 5 ND 3 13 1 2 2 38

1 26 19 111 .l 21 7 1334 2.19 10 5 ND 2 40 1 2 2 33 1 25 7 109 .3 27 7 878 1.93 13 5 ND 2 31 1 2 2 33 1 18 12 117 - 1 24 7 919 1.80 7 5 ND 2 29 1 2 2 31 1 15 7 112 .2 29 6 391 1-43 7 5 ND 2 18 1 2 2 26 1 21 8 71 - 1 38 8 371 2.16 3 5 ND 3 23 1 2 2 40

1 29 13 90 .4 64 7 141 2.21 2 5 NO 3 25 1 2 2 37 20 60 36 135 6.8 69 28 1019 3.99 41 17 7 34 49 18 16 19 64

l ! 1 1 1 1 1 - 1 -

. ! b ,124 8 :9 .26 -14 .Ob8 7 18 .27 .22 .041 6 24 .27 .15 ,079 10 35 .43 .11 ,068 11 26 .35

203 62 122 71 101

.36 ,050 9 22 .40

.33 .099 8 24 .37

.30 .139 6 22 .37

.25 .069 7 30 .29

.33 .078 13 44 .48

-21 .029 9 27 .39 .48 ,101 36 59 -88

302 219 270 95 112

.09 n o 9 -08 .Oh .07

1 - 1 - 1 - 1 - 1 -

l2OOE 10005 STD C

156 184

.12 * 08

2 2.36 -03 .08 37 1.72 .07 -13

1 - 12 -

i

SOOKOCHOFF CONSULTANT PRClJECT -- SUNNY S I D E FILE # €37- 1TZT.R

SAflPLE(I

1?00E 1050s 12OOE 11005 1200E 11505 126OE 20255 1200E 20505

1200E 20755 1200E 21005 1200E 21255 1200E 21565 1200E 21755

1200E 2200s 1200E 22255 120OE 22505 STD C 1?00E 22755

1200E 23005 1200E 23505 l2OOE 24005 1200E 24505 1200E 2500s

1250E 20005 1250E 20255 1250E 20505 1250E 20755 1250E 21005

1250E 21255 1250E 21505 1250E 2i755 1250E 22005 1250E 22255

1250E 22505 1250E 22755 1250E 23005 1250E 23255 1250E 23505

1300E 1000s 1300E 10505

tlO CU PB I N A6 N I EO t!N FE AS U AU TH SR CD SB 81 V C A f PPI PPN PPM ppn PPM Ppn PP~I ppn 1 PPR PPI~ PPII PPI PPR ppn PPI PPN P P ~ : 2

1 I? 7 9; - 2 !I 7 158 1.85 8 5 ND 2 25 1 2 2 29 . X . E 4 1 3 B 110 1.0 78 0 297 2.Z9 7 5 ND 4 27 1 2 2 36 .Zl .a93 1 10 14 13: .9 40 8 807 1.85 9 5 ID 2 20 1 2 2 30 .15 .155 2 24 10 12: .: :4 7 1142 2.27 1 1 5 ND 4 17 1 2 2 37 .15 .1:9 2 18 te 130 .? 27 8 659 2.76 11 5 ND 4 17 1 2 2 46 .i7 ,147

1 15 3 65 . 2 16 5 769 1.45 2 5 ND 1 16 1 2 2 29 -17 .Ob9 1 17 19 139 . 3 17 6 1503 1.65 16 5 ND 2 14 1 2 2 29 .13 ,151 1 18 8 75 .1 17 7 818 1.98 9 5 ND 2 14 1 2 2 36 .15 -089 1 19 8 76 .1 13 5 621 1.85 13 5 ND 1 14 1 2 2 33 .17 ,088 1 16 7 68 .1 13 7 745 1,75 8 5 ND 1 1 1 1 2 2 32 .13 ,069

1 x 7 1 20 6 1 16 4

20 58 37 1 16 5

1 28 5 1 16 2 1 25 7 1 24 7 1 15 9

103 132 1 :: 13: 84

68 86 61 170 260

LA cfi P P I PPfl

? :1 13 28 6 25

1 1 20 14 29

5 l b 6 16 7 20 5 14 5 16

.5 56 10

. 3 39 7 - 2 45 7 6.8 67 28 .1 50 6

. 2 42 8

.2 47 8 - 1 51 9 .1 42 9 .l 55 8

311 2.77 12 5 ND 5 19 1 2 2 47 833 2.10 12 5 NO 2 35 1 2 2 33 496 2.10 8 5 ND I 26 1 2 2 35 990 4.94 :9 15 7 35 50 17 15 21 65 571 1.71 5 5 ND 2 27 1 2 2 30

264 2.27 7 5 ND 4 24 1 2 2 42 556 2.00 6 5 ND 3 19 1 2 2 35 480 2.55 5 5 ND 3 27 1 2 2 47 831 2.39 37 5 ND 3 23 1 2 2 42 550 2.37 12 5 ND 3 20 1 2 2 41

. 20 .OB2 14 38 '35 ,116 9 24 .34 .071 10 32 -50 . lo0 37 59 .33 ,102 8 21

.26 .057 15 35

.20 ,132 7 34

.33 .031 12 54 -29 ,066 10 37 .26 ,045 10 44

MG

. 26 * 39 * ?9 ,51 * 37

a 20 .18 .28 .21 * 24

.52

.3 * 35 .90 s27

.45

.36 ,65 .46 .44

BA PPfl

187 202 167 254 182

112 180 112 96 70

140 261 185 177 155

151 156 139 130 100

TI B AL NA K Y RUt x ppn x x x PPI~ PPri

.09 5 1.61 .0: .66 1 -

. I 2 4 2.78 .o: .OB 1 -

.09 3 1.81 -0: .0b 1 -

.13 ? 2 . 5 5 -03 .O? 1 -

.14 3 2.53 -03 .07 1 -

'09 4 1.11 .04 .05 1 - .12 4 2.02 .03 .05 3 1 .lo 5 1.63 -03 -04 2 1 ,09 4 1.30 .03 .04 5 1 .09 4 .98 .03 -05 1 2

I 13 -09 .ll .09 -10

,13 .10 * 12 - 1 1 .ll

3 2.32 . 02 '07 1 8 5 1.82 .03 .Ob 1 2 2 1.93 - 0 3 .06 1 1 36 1.80 .07 -1: 14 - 17 1.51 '03 .Ob 1 10

4 2.01 .03 .Ob 1 6 4 1.82 .03 .05 1 1 2 1.50 .03 - 1 1 1 3 4 1.77 -03 .07 1 5 6 1.74 .03 .Ob 1 1

1 22 6 146 .2 29 7 1271 2.06 11 5 ND 2 21 1 2 2 33 .16 .221 7 18 .26 255 -13 14 2.55 .03 .Oh 1 - 1 8 6 80 .1 7 41221 .99 4 5 ND 1 18 1 2 2 22 .18.036 3 8 .12 113 .07 21 .68 .04 .04 1 - 1 18 7 94 - 2 30 7 762 1.96 9 7 ND 3 18 1 2 2 35 .l5 ,122 8 25 .31 158 .ll 18 1.84 .03 .04 1 - 1 13 4 96 - 1 15 5 1218 1.47 6 5 ND 1 15 1 2 2 29 .18 .063 4 13 .19 148 .09 17 1.11 .04 .04 1 - 1 15 11 102 .1 26 7 823 2.23 11 5 ND 2 16 1 2 2 38 .15 .094 7 23 .34 158 .13 3 1.89 .03 .06 1 - 1 3a in 80 -4 43 9 4422.51 12 5 ND 4 22 1 2 2 44 :loo 12 15 .qn 132 .is ~ 2 ~ 5 3 .03 '07 1 - 1 17 6 84 . 2 31 7 614 1.90 9 5 ND 2 17 1 2 3 36 .19 ,075 7 29 .36 138 .09 3 1.4: .03 .Ob 1 - 1 30 8 71 . 2 52 8 228 2.58 11 5 ND 5 18 1 2 2 45 .19 .OB6 14 38 .49 125 .14 2 2.62 .03 .05 2 - 1 18 9 174 - 3 32 7 689 1.91 23 5 ND 3 20 1 2 2 33 .l8 ,084 8 23 .30 154 .11 2 1.86 -03 .05 1 - 1 17 9 89 .1 23 5 714 1.77 14 7 ND 2 20 1 2 2 33 .22 .077 8 20 .27 133 -09 22 1.43 .03 .05 1 - 1 14 6 111 .l 19 5 llb3 1.75 4 5 ND 2 23 1 2 2 30 .24 ,107 9 15 .27 235 .10 5 1.77 -03 .09 1 - 1 18 21 106 .l 21 6 1323 1.83 12 5 ND 3 24 1 2 2 34 .35 ,122 1 1 19 .29 223 .lo 18 1.52 .04 .07 1 - 1 35 7 89 .1 44 9 350 2.83 , 8 5 ND 6 22 1 2 2 50 -23 .lo1 18 30 .53 99 .16 24 2.78 -03 .09 1 - 1 18 13 83 ,1 34 6 882 2.07 7 5 ND 3 22 1 2 2 40 .25 ,056 9 30 .38 135 .I1 2 1.45 .03 .Ob 1 - 1 25 25 116 - 1 35 9 1085 2.70 8 5 ND 2 29 1 2 2 50 .37 ,055 9 24 .56 170 .14 5 1.99 -03 .ll 2 -

1 27 7 66 .5 52 7 267 1.87 5 5 ND 3 30 1 2 2 34 -29 ,017 12 28 .40 100 .ll 2 1.68 -04 .05 1 - 1 16 11 86 . 3 38 8 354 2.12 11 5 ND 3 21 1 2 2 37 .21 .099 8 29 .32 98 .11 16 2.00 .03 .05 1 -

SOOKOCHOFF CONSULTANT FROJECT - SI INIVY E i T DE F 11-E # 8;'- 1 ??::F?

SAWPLEt tl9 CU PR I N A6 N1 CO flN f E AS U RU TH SR CD SP BI V CA P LA CR M6 PPM PPN PFM PPM PPN PPM PPN PPH z PPR PPM PPn PPM PPI( PPN PPR PPM ppn x z PPM P P ~ x

Pane 14

1300E 1100s 1 l e 10 65 .3 47 8 22: 2.04 8 5 ND 2 19 1 2 2 33 -18 ,100 6 24 -30 1300E 1!50S 1 20 ? 80 - 2 40 8 215 1.97 6 5 #@ 3 29 1 2 2 34 ,29 . lo? D 28 .40 1500E XXS 1 16 7 110 . Z 23 6 911 1.77 8 5 N D 2 25 1 ? 2 :O . 20 .072 7 17 - 2 9 lj0OE ?OSOS 1 1: 6 96 , 2 13 5 774 1.62 8 5 N D 3 21 I 2 2 28 .15 ,126 6 8 -18 1300E 2975s I 13 32 144 .? 11 5 621 1.88 19 5 N D 2 23 1 2 2 2 .20 .I60 5 !? .?2

1300E 21005 1360E 212% 1300E 2150s 1300E ?175S 1300E 2200S

!!00E 22255 130OE 22505 1SOOE ?:?:s 1300E 23005 1300E 23255

1 16 10 118 . 4 12 6 1163 1.97 SO 5 N D 2 16 1 2 2 34 -17 ,128 1 18 20 125 .5 32 8 498 2.55 59 5 ND 15 1 2 2 45 .17 ,088 1 19 35 121 .1 27 6 629 1.94 41 5 N D 2 21 1 2 2 35 .24 ,066 1 20 10 142 .1 23 6 1009 2.18 16 5 N D 3 ?6 1 2 2 37 , 2 6 ,160 1 22 9 110 .1 23 9 970 2.48 13 5 N D 3 15 1 2 2 43 .19 ,119

1 27 8 11: - 1 26 9 1416 2.49 11 5 N D 1 16 1 2 2 45 -22 ,105 1 15 8 6: - 1 12 5 645 1.85 2 5 NO 2 1: 1 2 2 37 .I6 ,064 2 32 24 102 . l 36 8 600 2.79 10 5 ND 4 16 1 2 2 52 -19 .OR: 1 22 5 67 .1 26 7 64: 2.27 6 5 N D 3 14 1 2 2 42 .17 ,044 1 22 4 75 - 1 40 9 830 2.49 6 5 ND 2 20 1 2 2 47 .24 ,085

7 1; 9 27 9 24 9 18 8 ?2

8 22 5 11

10 29 7 24

10 29

I22 .41

,34 *? . ..d .re s d J

.39

.47 * 3 .43

*c , LJ

BA TI B AL NA K W AU1 PPb X PPM X X 1 PPM PPR

94 .I1 4 2.29 .o: -95 1 - 147 . l o 3 1.75 -01 .07 1 - 176 -10 4 1.91 .O: .Ob 1 - 149 .13 4 2.46 .04 .05 1 - 133 .12 4 2.1: -04 .07 1 -

136 97

141 287 109

107 65

101 76

150

a 11 a 12 * 09 .12 .13

. I 1

.11

.14

.11

.12

9 1.55 4 1.79 2 1.56 6 2.34 4 1.Q1

4 1.70 3 1.41 : 2.39

10 1.51 4 1.94

I O 3

- 0 2 .03 .03 .03

.03

.04 * 93 ' 0:. 3 02

1 ; 1 2 1 5 : 1 2 1 1

1 1 l ! 1 - 1 - 1 -

1300E ?:;os 1 19 15 56 .1 16 6 872 1.85 9 5 N D 1 15 1 2 2 38 .17 .073 6 16 .24 86 -09 2 1.09 .03 .04 1 - 1309E 24005 1 47 7 80 .1 26 12 750 3.47 6 5 ND 3 29 1 2 2 74 .31 .Ob3 9 43 1.06 213 .21 2 2.44 -03 .24 1 - 1300E 24505 1 3 17 104 -4 57 10 557 2.90 34 5 ND 5 24 1 2 2 SO .25 .OS7 15 44 .58 130 .14 2 2.22 .02 .09 1 - STD C 21 58 37 133 6.9 69 28 991 3.98 42 15 7 35 48 17 16 19 64 -49 ,100 37 55 .90 176 .08 37 1.76 .07 .13 13 - 1350E 20005 1 13 9 151 -2 16 7 823 2.26 6 5 ND 1 13 1 2 2 36 .14 ,200 6 21 .34 137 -10 4 1.59 .03 .06 1 -

1350E 20255 1 26 7 121 .3 22 7 325 2.39 5 5 ND 2 17 1 2 2 39 .17 .079 8 21 .44 182 .10 2 1.94 .OS .OB 1 - 1350E 2050s 1 16 9 118 .3 22 7 476 2.19 14 5 ND 2 22 1 2 2 36 .20 ,251 5 21 .26 149 .13 5 2.68 .03 .OS 2 - 1350E 20755 1 34 17 151 .2 21 9 650 2.55 16 5 ND 3 19 1 2 2 44 .18 .221 6 28 -54 177 .15 10 2.98 .04 .OS 1 - 1350E 21005 1 15 38 197 .3 16 4 563 1.74 12 5 ND 2 19 1 2 2 29 .19 .091 6 14 .24 lb2 . lo 10 1.86 .a4 .OS 1 - 1J50E 21255 1 19 128 275 1.0 27 7 1368 2-26 217 5 ND 2 18 3 2 2 36 -18 ,079 8 21 .33 251 .13 5 2.28 .03 '05 1 - 1350E 21505 1 19 8 90 .1 36 8 709 2.36 19 5 ND 3 17 1 2 2 43 .18 .141 7 26 .37 124 .12 3 1.92 .03 .06 1 - 1350E 21755 1 21 12 99 -1 24 7 901 2.56 7 5 ND 2 19 1 2 2 45 .23 ,093 8 24 -39 138 .13 11 1.99 .03 -06 1 - 1350E 22005 1 19 9 102 .1 20 7 1250 2.26 11 5 ND 1 13 1 2 2 40 .15 .OB7 7 17 .34 144 . l l 2 1.65 .03 .06 1 - 1350E 2225s 1 20 16 95 . l 18 8 1251 2.19 11 5 ND 1 16 1 2 2 39 . l8 ,067 7 18 .32 97 .09 4 1.37 -03 .05 1 - i359E 2 5 0 5 1 14 16 121 .1 15 6 1626 1.97 6 5 ID 1 16 1 2 2 41 .21 ,048 5 14 .31 170 . l l 3 1.19 .04 .04 1 - 1350E 22755 1 21 27 132 .1 31 7 493 2.28 8 5 ND 4 18 1 2 2 40 .19 ,063 10 23 .36 138 .14 3 2.52 .03 .05 1 - 1350E 23005 1 12 14 83 . l 20 5 1817 1.54 2 5 ND 1 17 1 2 2 32 .21 .OS5 6 18 .23 144 .09 5 1.05 .03 .OS 1 - 1350E 23255 1 24 7 78 .1 31 8 596 2.58 4 5 ND 3 15 1 2 2 48 .18 ,100 8 30 - 4 2 115 .14 10 2.30 .03 .OS 1 - 1350E 23505 1 18 4 71 .1 24 6 842 1.98 2 5 ND 2 15 1 2 2 38 .18 .080 7 20 -31 115 . l o 9 1.54 -03 .05 1 - 1400E 1000s 1 13 7 64 .1 28 6 317 1.83 4 5 ND 2 23 1 2 2 29 .17 .216 6 23 ,24 175 .09 10 1.63 .03 .04 1 - 1400E 1050s 1 11 6 65 .2 19 5 167 1.61 10 5 ND 2 13 1 2 2 28 .14 ,238 4 14 .18 73 . l o 10 1.75 .04 .05 1 - 1400E 11005 1 26 8 61 .4 49 9 141 2.40 3 5 ND 5 27 1 2 2 44 -25 ,050 11 33 -42 189 .12 3 2.22 -03 .07 1 -