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GEOLOGICAL AND GEOCHEMICAL REPORT
~ ' ~ R " ' C E O L O G I C A L B R A N C H A S S E S S M E N T 1 % E B @ b D ' '
JANUARY, 1989 BY: TERRY CAMPBELL
(MARIE 1 TO 7 MINERAL CLAIMS)
OMINZCA MINING SliVISION
N.T.3. 5.3 N/02
SITUATED AT CU-ORDINATES: 55O 03' N 124O 53' W
NORANDA EXPLORATION COMPANY, LIMITED (NO PERSONAL LIABILITY)
SUMMARY ............................................ 3 INTRODUCTION ....................................... 4 LOCATION & ACCESS .................................. 4 CLAIM STATISTICS ................................... 4 TOPOGRAPHY 6 VEGETATION ............................ 4 REGIONAL GEOLOGY ................................... 5 LOCAL GEOLOGY ...................................... 5 PREVIOUS WORK ...................................... 5 GEOCHEMISTRY .......................................... 6 CONCLUSIONS ........................................ 8 RECOMMENDATIONS .................................... 8
APPENDIX I Statement of Costs
APPENDIX I1 Statement of Qualifications APPENDIX I11 Analytical Procedure APPENDIX I V Geochemical Resuits
Cost Breakdown
,-
Fig. 1 Location Map Fig. 2 Claim Map
(Located in Pocket Fig. 3 Geology Fig. 4 Geology Fig. 5 Geology Fig. 6 Geology Fig. 7 Au/Cu - Fig. 8 Au/Cu - Fig. 9 Au/Cu - Fig. 10 AuICU -
File) Map (Sheet 1) Map (Sheet 2) Map (Sheet 3) Map (Sheet 4) Soil Geochemistry Soil Geochemistry Soil Geochemistry Soil Geochemistry
1:8,000,000 2a 1 :SO. 000 2b
1:5,000 1 : 5,000 1:5,000 1:5,000 1:5,000 1:5,000 1:5,000 1:5,000
,r
F
The Marie property was acquired in the fall of 1987 to secure the drainage basins of several anomalous creeks. More ground w a s staked in the summer of 1988. Preliminary geologic mapping and soil sampling was conducted by Noranda personnel in 1988. 33.35 km of recon soil grid was established and 7.875 km of detailed sampling lines were added to the grid.
Soil geochemistry failed to outline any large areas of anomalous geochem, but several isolated copper and gold geochemical anomalies warrant further sampling and mapping.
1
r
The property was staked in the fall of 1987 to cover the drainage areas of creeks that were found to have anomalous gold vaiues in silt samples and pan concentrate samples. The Marie 5, 6 and 7 claims were added to the property in 1988 to cover a kink in an airborne magnetics anomaly. Preliminary geologic mapping and soil sampling were conducted in 1988. A large recon grid with baseline azimuth 090 degrees was established and detailed sampling was completed around anomalous samples.
The claims are located approximately 10 km south of Mt. Alexander, approximately 90 km northwest of Fort St. James.
Access to the property is via the #LOO logging road, off of the Leo Creek forest service road. Part of the property has been logged recently. The remaining logging trails provide good access to the lower lying areas of the property.
c~~~~~~_sTATI_..~.~~:~,
CLALm".-&.&e-F ___-_-_._-...- RECORD ..-_.__._.-._l_l_. # # U N I T S .-.- Marie 1 9176 20 Marie 2 9177 20 Marie 3 9193 16 Marie 4 9194 8 Marie 5 9649 18 Marie 6 9650 18 Marie 7 9651 9
DATE N O ~ . Nov . Nov. Nov. Aug . Aug . Aug .
____._-.- -- DUE 13. 1989 13. 1989 25, 1989 25. 1989 11, 1989 11, 1989 11. 1989
TOPOGRAPHY 6( VE2GELATfON:
The elevation ranges from 950 to 1537 meters. The property consists of pine flats and swamps to steep forested slopes.
The vegetation consists of mature stands of spruce, pine and balsam. togging has taken place in the lower areas of the property. Undergrowth is mainly small cedar. alder. willows and devils club.
2
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1 I r l 1
MARIE CLAIMS
Y* .
50
0 I00 200 K ILOIlEfRES
SCALE . I :a.ooo,ooo
LOCATION MAP REVISED
1-1 Marie Claims
DWG. No. NORANDA EXPLORATION 1 OFFICE: PRINCE GEORGE, B . C .
I
I
J ? ,; 5 I i:
The Marie property lies in a broad northwest trending package of rocks known a s the Quesnel Trough. These include Upper Triassic to Lower Jurassic volcanics and sediments which have been intruded by the gogem Batholith and numerous other felsic to mafic stocks, ranging in age f r o m Triassic to Cretaceous.
The Quesnel Trough is bounded to the west by the Pinchi Fault.
Outcrop on the Marie property is sparse. The observed outcrop indicates the property is underlain by basalts, andesites and some intrusive diorites.
The basalt is slightly amygdaloidal, calcareous and green in coior.
The andesite is Light urey.
-. !ne above units are intruded by diorite, possibly belonging the t h e i-iogem Bathoiith stock.
PLEV I 0 US W-QRK.;
A large amount of previous work has been performed on the Jean and JW group of claims. The earliest recorded work was d o n e by the N.B.C. Syndicate. Between the years 1969 and 1974, they did work leading up to 10,495’ of percussion drilling in 1974. In 1975, Cominco performed geophysics and 2499’ of diamond drilling on the property. Airborne Magnetic survey. In 1983, Cominco took 344 soil and 12 silt samples.
In 1981. Cominco and Noranda flew 355 km2 of
3
A total of 818 soil samples were collected on the Marie property during the 1988 field season. 33.35 km on recon soil lines were hip-chained and compassed. The soil lines are 500 meters apart and samples were taken at 50 meter intervals. 7.875 km of detailed soil lines were added to the grid to define anomalous values. Samples were taken at 25 meter intervals on these lines.
Method- -
The samples were removed with a soil auger from the ‘B’soil horizon, 20-35 cm below the surface. The samples were placed in kraft wet-strength paper envelopes, dried and sent to Noranda’s lab at 1050 Davie St., Vancouver, B . C. The samples were analyzed €or copper and gold. The results are plotted on Figures 4 to 8, located in the pocket file. Appendix I11 described the analytical procedure.
There are numerous small anomalous zones found throughout the property. The values for sold range from 10 to 340 ppb. Values >10 ppb are considered to be anomalous. The values for copper range from 2 to 490 ppm. Values >lo0 ppm are considered to be anomaious.
Gold,- 23 samples were found to be anomalous for gold.
Locarion-- - __ 6000E 12600N 6500E 12050N 6500E 12350N 7000E 11850N 8000E 10750N 8500E 8950N 8500E 9100N 9000E 9950N 9000E 11900N 9500E 7600N 9500E 9350N 9500E 9SOON 9500E 9800N 10000E 7650N 8900E 11625N 8900E l1850N 8900E 12000N 9100E 11775N 9100E 11850N 9300E 9500N 10100E 7675N 7525E 11375N 9700E 7525N
__ - _I_ _____ V_a_l-~~-_.C~~-b_AU) 40 40 40 30 30 70 50 40 240 60 20 340 60 40 40 20 30 20 50 30 30 30 70
4
The Gold anomalies on t h i s p r o p e r t y are sporadic and isolated.
C_oqrgr-- 41 samples were found t o be anomalous f o r copper.
LocktA.on---..- 5500E 11700N 7500E 11650N 8000E 8OOON 8000E 8550N 8000E 8650N 8500E 10300N 8500E 10350N 8500E 11200N 8500E 11350N 8500E 11650N 9000E 11950N 9000E 12000N 9500E 9500N 10000E 7800N 10000E 8150N 10500E 9150N 10500E 9750N 10500E lOOOON 10500E 10750N 11OOOE IOlOON 1 1 O O O E 10550N 11000E 10950N
580OE 12000N S9OOE 11700N 8900E 11775N 9100E 11900N 9200E 11950N 9300E 9600N 9300E 9625N 9300E 9650N 9400E 7525N 9600E 7550N 9800E 7625N 9900E 7650N
10100E 7900N 6000E 12600N 6475E 12375N 80252 10750N 9025E 9950N 9600E 9675N 9700E 9225N
Value (pDm Cu2 110 110 110 490 150 150 130 220 110 160 120 120 290 160 110 190 130 110 170 110 110 240 110 130 280 100 240 130 210 190 110 100 240 120 100 170 150 140 160 100 150
_.----.- ~
The copper anomalies on this p r o p e r t y are sporadic and isolated.
5
C-O-NG!.-USI-Q!.N~-
A total of 64 soil samples were found to be anomalous for gold or copper. The anomalous samples are scattered throughout the property. A f e w of the anomalous values are concentrated in small groups.
Establish a detailed soil grid around the anomalies located at 8OOOE. 8 5 S O N and 5000E, 8650N. The grid should consist of two lines: 7900E. S450N to 8750N and 8100E, 8450N to 8750N. (See Figure 8)
Prospect and map around the mini grid that surrounds 9500E, 9500N. (See Figure 7 )
Establish more recon soil lines: 10,000E, 10,000N to 12,000N; 11,50OE, 10,OOON to 11,000N; and 12,000E. 10,000N to 11,000N. Samples should be taken at 50 m e t e r intervals.
6
A > WAGES: Geology - 6 days B 815S/day Linecutting - 8 days @ S100/day Soil sampling - 8 days @ S100/day
B ) FOOD, ACCOMMODATIONS 6 TRANSPORTATION: 22 days @ SSO/day
C> COST OF ANALYSIS: 8 1 8 soils for Cu, A u 13 S8.75/sample
D ) COST O F REPORT PREPAZATION: A u t h o r 5200.00 Drafting 8200.00 Typing s 50.00
Total Cost
S 930.00 5 800.00 S 800.00
s 1,100.00
S 7,157.50
7
RF'PENDIX
STRTEMENT O F RURLIFICQTIONS
I, T e r r e n c e C a m p b e l l , of P r i n c e G e o r g e , F ' rovince o f B r i t i s h C o l u m b i a , d o h e r e b y c e r t i f y t h a t :
1. I am a g e o l o g i s t r e s i d i n g at 7748 G l a d s t o n e D r i v e , P r i n c e G e o r g e , B r i t i s h C o l u m b i a . .
2. I am a 1'305 g r a d u a t e of t h e U n i v e r s i t y uf B r i t i s h C o l urflbia, B. Sc. ( G e o l o g y ) .
3. I a m a member i n g o o d s t a n d i n g clf t h e B r i t i s h C o l u m b i a Yukon C h a m b e r of Mires.
4. I p r e s e n t l y h u l d t h e p u s i t i o n or' F i e l d G e o l c g g i s t w i t h Norarrda E x p l o r a t i cln Company, L i m i t e d (no p e r s u n n a l l i a b i l i t y ) and h a v e been i n t h e i r e r n o l u y since 1'386.
T e r r e n c e C a m p b e l l
APPENDIX I11
FINRLYTICRL METHOD DESCRIPTIONS FOR GEOCHEMICRL RSSESSMENT REPORTS
Revised:01/86
The methods listed are presently applied to analyse geological materials by the Noranda Geochemical Laboratory at Vancouver. (March, 1984)
Preparat ion of Samples
Sedirnents and soils are dried at approximately 80% and sieved with a 80 mesh nylon screen. The -80 mesh (0.18 mm) fraction is used for analysis.
Rock specimens are pulverized to -120 mesh (0.13 mm). Heavy mineral fractions (panned sarnPles) are analysed i n its entirety, when it is to be determined for gold without further sample preparation. See addendum.
CIna 1 y s i 5 o f Sam P 1 e s .
Decomposition of a 0.200 g sample is done with concentrated perchloric and nitric acid (3:1), digested for 5 hours at reflux temperature. Pulps o f ' rock or core are weighed out at 0.2 g or- less depending on the matrix o f the rock, and twice as much acid is used for decomposition than that i5 used for silt or soil.
The concentrations of Rg, Cd, Co, Cu, Fe, Mn, Mo, Ni, Pb, V and Zn (all the group R elements of the fee schedule) can be determined directly f r o r n the digest (dissolution) ~ i t h art atcmic absorption spectrometer (OR). R Varian-Techtron Model RR-5 c w Model RQ-475 is used to measure elemental concent rat ions.
Elernents Reauirins Specific Decortiposit ion Method
Rntirnony - Sb: 0 . Z g sample is. attacked with 3.3 mL of (5% tartaric acid, 1. 5 mL cortc. hydrcchlclr-ic acid and 0. 5 rtiL of conc. nitric acid, then heated in a water bath for- 3 hours at 35'3 C. S b is determined directly frorn the acid solution with an RR-475 equipped with electrodeless discharge lamp (EDL).
Rrsenic - R s : 0.2 - (3 .4 g sample is digested with 1.5 mL of 70 'I: perchloric acid and 0.5 r~iL of conc. nitric acid. R Var-ian 00-475 equipped with an Qs-EDL measures the arsenic concentrat iort clf the digest.
-1-
Barium - Bar 0.1 g sample is decornpclsed with conc. perchloric, nitric and hydrofluor-ic acid. Fltorriic absorption using a nitrous oxide-acetylene flame determines Eca from the aqueous solution.
Bismuth - Bi: 0.2 g - 0.3 g is digested with 2.0 ml of perchloric 70% and 1.0 m l of conc. nitric acid. Bismuth is determined directly from the digest into the flame of the RQ instrument c/w EDL.
Gold - nu: 10.0 g sample (Pan-concentrates see below) is digested with aqua regia ( 1 part nitric and 3 parts hydrochloric acid). Gold is extracted with Methyl iso-Butyl ketone (MIBK) from the aqueous solution. Gold is determined from the MIBK solution with flame QQ.
Magnesium - Mgr 0.05 - 6.10 g sample is digested with 4 ml perchloric/nitric acid ( 3 : l ) . Rn aliquot is taken to reduce the concentration to within the range o f atomic absorption. The RQ-475 with a nitrous oxide flame determines M g from the aqueous solution.
Tungsten - U: 1.0 g sample sintered. with a carbonate flux and thereafter leached with water. The leachate is treated with potassium thiocyanate. The yellow tungsten thiocyanate is extracted into tri-n-butyl phosphate. This permits colourimetric comparison with standards to measure tungsten concent rat ion.
Uranium - U: Rn aliquot, taken from a perchloric-nitric (3: 1) decomposition, usually from the niulti-element digestion, is diluted with water and a phosphate buffer. This solution is exposed to laser light, and the luminescence of the uranyl ion is quantitatively measured on the UR-3 (Scintrexc).
LOWEST VRLUES REPORTED IN PPM
Rg - 0.2 Mn - 20 Cd - 0.2 MID - 1
co - 1 Ni - 1
c u - 1 P b - 1
Fe - 100 v - 10
Zn - 1
Sb - 1
Qs - 1
Ba - 1 0
Bi - 1
au - 0.01 (10PPB)
w - 2
u - 0.1
APPENDIX IV
NORRNDR VUNCOUVEH LUBDRUTDRY
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