AND - British Columbia
ASSESSMENT REKlRTON THEAND-ON THECARTHAGE GROUPC)w-\YMIR. B.C.LONGITUDE:ll7O 10' WOWNER : NITHEX J3XPUIRATION LTD.OPERATOR : NITHM EXPIDlUiTION LTD.August 31, 1983
TABLE O F CONTENTSSUMMARYINTRO DUCT I O NLOCATION AND AGCESSCLAIMSPRO P m T Y HISTORYREZIONAL GEDLOGYPROPERTY GE?JMGYV E I N SYSTEHS AND O R E M I N E R A L I U T I O NEXPLORATION APPROACHD I S C U S S I O N O F RESULTSCONCLUSIONSSTATEHENT O F COSTSREFERENCESSTATEMENT 3F QUALIFICATIONS,APPENDICES- GEDCHEMICAL ANALYSIS METJBDAPPENDIX 11 - GMCHEMTCAL ANALYSIS C E R T I F I C A T E SAPPENDIX IAPPENDIX 111- GEDLOGICAL F I E L D NOTES
TABLE OF FIGURESFollowing PageFigure 1LOCATION MAP (1:2,400,000)Figure 2ACCESSMC P(1:50,000)Figure 3C W I M MAP (1:50,000)Figure 4GEOLOGY MAP (1:31,680)Figure 5GEUMGY O F THE CARTHHGE GROUP ( 1 : 2 5 )Figure 6GEDCHINICAL RESULTS FUR COLD ANDS I L V m (1: 2500)Figure 7GEX)CHWICBL RESULTS FOR LFAD ANDZINC (1: 2500)Figure 8GEtICHEMICBL RESULTS FUR QPPElR (1:2500)-.24In Pocket11t
1. YAn exploration programme consisting of s o i l sanpling andgeologic napping was done on the Carthage C l a i m Group, locatednear Y m i r , B.C.The presence of a previously discovered s o i lanomaly was confirmed and a new anomaly was found.INTRODUCTIONIn 1980, Nithex Exploration Ltd. purchased several groupsof claims which l i e i n a north-trending b e l t just east of Y m i r ,The ground acquired a t t h a t time included the CarthageB.C.Group,During the summer of 1981, Nithex conducted line-cutting,s o i l sampling and geological mapping programmes over the CarthageGroup i n order to explore f o r gold and s i l v e r mineralization,This work delineated several anomalous areas and the followingreport describes a programme of d e t a i l s o i l sampling and geologi c a l napping c a r r i e d out over one of these anomalies.3,LOCATION ANI) ACCESSThe Carthage Claim Group i s i n the Nelson Mining Divisiona t l a t i t u d e 49 degrees 20 minutes N, longitude 117 degrees 10minutes W on N.T.S.sheet 8 2 / 6( i g u r e1 ) .Creek, f i v e km NE of Y m i r , B.C.( i g u r e2).It i s on HuckleberryAccess to t h e claimsi s gained v i a f i v e knr of d i r t road which leaves Highway 6 a tYmir, and then on foot f o r approximately two km.A l l roads lead-ing to the property have, apparently, been washed out o r areovergrown.
The Carthage Claim Group i s located on Mineral T i t l e sReference Map 8 2 / (Figure6 3).Pertinent claim data a r el i s t e d i n t h e t a b l e below:Claim-Record NO.CarthagePatBeresfordDuff e r i nWild HorseX-rayRay Fr.Jo p l i nOronocoS oJ.M.RayGolden CalfRamseyMaude Fr.743744750751752753 )753")757758759765766767%)767")Anniversary 198319831983198319831983198319831983*Adjoining reverted Crown-grants which do not collectivelyexceed 61.78 acres a r e combined to form one recorded claim.The above information conforms with the records of theMining Recorder a t Nelson.5.PROPERTY HISTORYThe claims were f i r s t Crown-granted between 1900 and 1905.Prospecting and exploration work was done by many p a r t i e s overt h e years, but production of ore was never achieved.The mostIextensive exploration programme carried out on any of t h e claimswas t h a t done by t h e Y m i r Good-Hope Mining Co.Their work, con-s i s t i n g of road building, surface trenching, d r i f t i n g and u n d e r
Nithex Exploration Ltd.CMTtWGE GROUP,
NITHEX EXPLORATION LTD.CARTHAGE GROUPACCESS MAPP0 2000 4000 6000 8000 IOOOO
Nithex Exploration Ltd.Carthage GroupCLAIM MAP
ground diamond d r i l l i n g , was carried out on the X-Ray Groupbetween the years1944 and 1950. A t t h a t time, t h e group con-s i s t e d of t h e X-Ray, Wild Horse and Annie Maud Crown-grantedmineral claims.No major work was done on t h e claims u n t i l 1979, when theproperty was prospected by D. R. Cochrane.Nithex Exploration Ltd. purchased the Carthage Group i n1980, and carried out an exploration programme i n 1981 consisting of geochemical s o i l sampling and geologic mapping.6.REGIONAL GEDLOGYThe Y m i r area i s underlain by a s e r i e s of regionally andcontact- etamorphosed sedimentary anu volcanic rocks rangingi n age from Proterozoic t o Upper Jurassic (Figure4). Thisenkire sequence has been intruded by the Cretaceous Nelsongranites and g r a m d i o r i t e s and Tertiary Coryell plutonic rocks( i t t l e ,1960; McAllister, 1951).The non-intrusive rocks s t r i k e roughly north-south andr,dip o r are overturned steeply t o the west ( c l l i s t e 1951).Two phases of deformation have caused extensive crumpling and,locally, the structure can be very complex (F'yles and Hewlet ,1959; McUllister, 1951).Two major folds have been identified,howevsr, and these a r e the Baldy Anticline and the Laib CreekSyncline.Both a r e i s o c l i n a l folds which have axes trending
s l i g h t l y e a s t of north ( c l l i s t e 1951).r,Several faults t r a v e r s e t h e region.Most of t h e s e f a u l t ss t r i k e p a r a l l e l to t h e o v e r a l l formational s t r i k e with s t e e pe a s t e r l y dips (McAllister, 1951; L i t t l e , 1960).Towards t h esouth, near Salmo, t h r e e t h r u s t f a u l t s have been identified.These a l s o s t r i k e p a r a l l e l t o t h e general geology and d i p t ot h e e a s t ( y l e sana Hewlett, 1959).The Carthage Group i s underlain by s c h i s t s and m g i l l i t e sof t h e Ymir Group ana by g r a n i t e s of t h e Nelson I n t r u s i v e s( i g u r e s4 and 5).The Ynir Group sediments c o n s i s t of darkgrey, green, brown and black s l a t e s , shales, a r g i l l i t e s ,q u a r t z i t e s , p h y l l i t e s and schists.Near t h e contact with t h eintrusive, t h e sediments have been metamorphoses t o anaalusitemica s c h i s t s and chlorite-nicas c h i s t s ( c k l l i s t e r ,1951;L i t t l e , 1960).These rocks have been correlated with t h e Slocan Groupsediments by McAllister (1951) and a r e therefore considered t obe T r i a s s i c i n age."L i t t l e (1960) contends, however, t h a t t h elowermost p a r t of t h i s u n i t may be as o l d as Permian and t h euppermost as young as Lower Jurassic.I
The i n t r u s i v e rocks consist of porphyritic g r a n i t e (McBUister,1951), and, throughout the area, t h e r e a r e numerous s m a l l late-stagedikes and s t l l s ranging i n composition from a p l i t e t o lamprophym(Drysdale, 1917).3The metamorphism of t h e sediments i s not intense, except nearcontacts with i n t r u s i v e s (McAllister, 1951).During t h e courseof t h i s programme, t h e metamorphic grade was observed t o be modera t e l y intense with well developed f o l i a t i o n and occasional occurrences of porphyroblasts of andalusite.Two small i n t r u s i o n s ofNelson g r a n i t e ware noted on t h e property by Black (1982), andthese i n t r u s i v e s a r e t h e most l i k e l y source of t h e metamorphism.The most common rock-type observed i n t h e survey area i s agrey t o grey-brown o r r u s t y weathering, medium t o caarse-grainedmica-quartz (-graphite-andalusite)developed f o l i a t i o n .s c h i s t with moderate t o wellAlso f a i r l y common, i s a grey weathering,grey fine-grained t h i n l y laminated quartzite.These two rockt y p e s have been grouped together as Y m i r Sediments ( i g u r e5).No outcrops of i n t r u s i v e rocks were seen by t h e w r i t e r ,although boulders and fragments of paragneiss were observed alongt h e e a s t side of l i n e 3 75S (Figure 5).This i s not surprising,as t h e i n t r u s i v e contact has been observed by several geologistsIalong t h e eastern boundary of t h e Carthage Group (Drysdale, 1917;McBllister, 1951; L i t t l e , 1960; Black, 1981) (Figure 4 ) .
One outcrop of grey-green fine-grained c h l o r i t e (?)-nicas c h i s t was noted a t 2 7 5 / 1 5 0(Figure 5).This rock e x h i b i t sa f a i r degree of kaolinization, probably due t o a l t e r a t i o n by anearby quartz vein.Drysdale (1917) reported t h a t quartz veinsi n t h e Y m i r a r e a frequently contained kaonlinite, both i n t h ew a l l rocks and i n t h e veins themselves.The probability of aquartz vein occurring nearby i s f u r t h e r enhanced by t h e presenceof a geochemical anomaly a t 2 755/1 753 (Figures 6, 7 and 8).8,VEIN SYSTEMS AND ORE MINERALIZXTIONGold, s i l v e r , lead, zinc and copper mineralization occurson t h e property i n quartz veins, stockworks ana zones of r e t i c u l a t i n g q u a r t z v e i n l e t s which p a r a l l e l t h e s t r i k e and d i p oft h e country-rock sediments,Sd,phi.de minerals i n these veinsc o n s i s t of fine-to coarse-grained disseminated p i t e , pyrrhot i t e anci s p h a l e r i t e with minor chalcopyrite and galena l lack,1981).These zones can be several f e e t thick, but a r e usuallyq u i t e narrow, i n t h e order of 0.5 t o 1 f o o t wide ( M c l l i s t e r , 1951).The main zone of quartz veining on t h e Carthage Group, asevidenced by t h e l o c a t i o n of geochemical anomalies and o l dworkings, starts a t 4 00S/0 50 and trends northeast t o t h eCarthage Claim on a bearing of approximately 025 degrees ( i g u r e5).There a r e many trenches and a d i t s i n this portion of t h e property,some or' which have dumps containing mineralized boulders.A
sample of vein material taken by t h e w r i t e r from one of thesedumps a t 1 75S/1 00E assayed 0.006 oz Au/ton and 2.37 oz g / t o n .There i s evidence of another mineralized zone on t h eproperty which s t r i k e s approximately 160 degrees and t r a v e r s e st h e X-Ray C l a i m from 3 0 0 / 2 0 0t o 1 0 0 / @ 5 0 .Geochemicalanomalies i n gold, s i l v e r , zinc, copper and, t o a l e s s e r degree,l e a d occur along t h i s zone and w i l l be discussed i n g r e a t e rd e t a i l i n a l a t e r section of -this r e p o r t (Figure 6 , 7 and 8 ) ,9.EXPLORATION APPROACHI n t h e summer 1981, Nithex Exploration Ltd. conducted aprogramme of geochemical' s o i l sampling and geological mappingover t h e Carthage Group claims.A sampling grici was cut overt h e property, consisting of a 1.5 km long base l i n e bearing 025degrees with cross l i n e s 100 metres apart.These c r o s s l i n e swere sampled a t 25 metre i n t e r v a l s and t h e samples were analysedf o r copper, lead, zinc, s i l v e r and gold ( i c h a r d s o nand Black, 1981),This s o i l sampling programme outlined several geochemicalanoiualies.The l a r g e s t of these anomalies i s located on t h eX-Ray and Carthage claims i n a northeast-southwest trending zone.Many trenches and a d i t s a r e present i n t h i s a r e a and it i s pobably t h e main zone of mineralization on t h e property a s described
I n August of 1983, a s e r i e s of d e t a i l s o i l samples weretaken i n order t o more f u l l y define t h e continuity and extentof t h i s anomaly.These samples were taken a t 25 metre i n t e r -v a l s along cross l i n e s c u t 25 metres a p a r t between t h e recorenaissance lines.A total of 85 samples were taken betweenl i n e s 1 OCS and 4 00S and between 0 5W and 2 00E (Figures 5,6 , 7 and 8).The r e s u l t s have been p l o t t e d on 1:2500 scale maps( i g u r e s6, 7 and 8).Gold and s i l v e r have been p l o t t e dtogether (Figure 6) as have lead and zinc ( i g u r e7).Copperwas plotted on a separate map ( i g u r e8).10.DISCUSSION OF RESULTSA s was mentioned befbre, most of t h e work done, t o date, ont h e property has been confined t o a zone which starts a t 4 0 0 /B50E and trends northeast t o t h e Carthage Claim.Several p i t sand a t l e a s t four a d i t s have been excavated along t h i s zoneindicating t h e probable existence of sulphide mineralization.Not surprisingly, there a r e a number of geochemical anomaliesi n t h i s area.These anomalies, detected by both t h i s y e a r ' sprogramme and t h e reconnaissance programme conducted i n 1981,a r e probably due t o naturally high metal occurrences i n t h es o i l and t o contamination from previous exploration a c t i v i t i e s .Consequently, care was taken t o minimize possible contamination
caused by sampling too close t o waste dumps and roads.High values were obtained f o r gold and zinc near t h ebase l i n e between l i n e s 2 00S and 2 50S.This anomaly l i e svery close t o a small plug of Nelson Intrusive and t h e r e a r esome mineralized quartz boulders s c a t t e r e d throughout t h e a r e awhich may account f o r t h e high metal content of t h e s o i l .There i s an a d i t a t 1 7 5 / 0 t 2 5 but, since it l i e s downhillfrom t h e anomalous samples, no conta.mination from t h e wastedump i s suspected.There i s another anomalous zone on t h e pmperty whichs t r i k e s approximately 160 degrees and t r a v e r s e s t h e X-2ay C l a i mfrom 3 00S/2 00 t o 1 00S/O 50 .Anomlously high values f o r gold and s i l v e r were detectedalong t h i s zone i n a s e r i e s of d i s c r e e t , r e l a t i v e l y discontinuousoccurrences.The geochemical r e s u l t s f o r copper and zinc suggest,however, t h a t t h i s is, i n f a c t , one continuous zone.Thesemetals, due t o t h e i r g r e a t e r mobility, b e t t e r r e f l e c t t h e l e n t i c u l a r s t r u c t u r e of t h e anomaly.It appears t h a t t h e r e may bepods of h i g h e r g r a d e mineralization along the zone which a r edetectable by gold and s i l v e r geochemistry.The lower-gradesections of t h e s t r u c t u r e a r e detectable by base-netal geoc,hemi s t r y only.
The geochemical r e s u l t s f o r l e a d do not r e f l e c t t h i sanomaly as c l e a r l y , although t h e r e i s a general trend observa b l e between l i n e s 2 W and 1 75S,The existence of a mineralized zone which caused t h egeochemical anomaly i s supported by an outcrop of kaolinizedp y r i t i f erous c h l o r i t e-nica s c h i s t a t 2 7 5 / l 5 0(Figure 5)Xaolinite was noted by Drysdale (1917) as a common ganguemineral i n veins and f a u l t s in t h e Y m i r area.The k a o l i n i t eoccurs i n both t h e veins and t h e wall-rocks.CO NCLUSIU NS--1.The d e t a i l s o i l sampling programme conducted over t h eCarthage Group Claims confirmed t h e existence of a northeastsouthwest trending geochemical anomaly located i n t h e v i c i n i t yof t h e g r i d base l i n e .The source of t h i s anomaly i s probablydue t o t h e quartz veins described by previous workers althought h e s e veins have y e t to be investigated by t h e writer,2.Another anomaly, locat3d between 3 0 0 / 2 0 0and 1 00 /0 25W, w s s detected on t h e property.The source o f t h i sanomaly i s not known,3,Both anomalies a r e open-ended and require more d e t a i lsoil-sampling, geologic mapping and,d r i l l - t a r g e t s can be defined,-x--,possibly, trenching before-
12.STATEMENT OF COSTSPre-fieldFieldAssistantVehicle.50 d a y s @ 210.90/day3.00 days 8 210.90/day3.00 days 8 I 90,00/day3.90 days 8 30.00/day 105.00630.00270.9090. 00 100.90Equipment and SuppliesReproduction and Office Costs333.75Assays12. 50Geochemical Analyses 85.90 SanplesTotal 2,842*751.COCHRAN, D. R., (1979), llProspecting Assessment P-aport onPortions of the Carthage Group and Gibralter and InkemanReveFted Crown-pant ed Mineral Claims. 'I2.COCKFIELD, W. 3., (1936) !!Lode Gold Deposits of Y m i r Nelson Area, B r i t i s h Coltrmbial', Geological Survey ofCanada Memoir 191.3.BLACK, R. G., (l981), Unp iblishedmemos and progressreports t o Nithex Exploration Ltd.4.DRYSUiLE, C. !J.,(1917), I1Ymir Mining Camp, B r i t i s hColumbiatt Geological Survey of Canada Memoir 94.5.LITTLE, H. !J., (1%0), ItNelson Map Area, West Half,Geological Survey ofBritish Columbia (82F/id1/2)Canada Memoir 308.,,",,
6.McALLISTHl, A. L., (1951), I1Ymir b p Area, B r i t i s hColumbiaM,Geological Survey of Canada Paper 51-47.MINISTRY OF MINES ANNUAL REPORTS, 190011903, 1905,1917, 1930, 1934, 1944-1750.8.RICHARDSON, P. W. and BLACK, R. G., (1982), uAssessment Report Describing t h e S o i l Geochemistry Programmeon the Carthage Claim Groupft.9.IJALKER, J. Fa, (1934), llGeology and l i n e r a l Depositsof the Salmo Map Area, British Columbia1', Geological.Survey of Canada Memoir 172.10.(1980), "A Summary of Ecploration Potentialof Claims i n t h e Y m i r Gold Campu, -Private Report t oNithex Exploration Ltd.WOLFE, R.,
l, , STATEMENT OF yUALIFICATIONSI, David W. Iiennie, hereby c e r t i f y :1. That I am a geological engineer residing a t #313505 Second S t r e e t , Nelson, B.C.-2. That I am a r e g i s t e r e d Professional Engineer i nt h e Province of B r i t i s h Columbia (1982).3. That I a m a graduate of t h e University of B r i t i s hColumbia and hold a bachelor of Applied Sciencedegree i n Geological Engineering (1979).4. That I have practiced my profession continuouslys i c egraduation.5. That I have not received d i r e c t l y o r i n d i r e c t l y ,nor do I expect t o receive, any i n t e r e s t i n t h eCarthage Property o r Nithex Exploration Ltd.6 . That I, personally, c a r r i e d o u t t h e f i e l d work andprepared t h i s r e p o r t on t h e request of NithexExploration Ltd.
GEXlCHEMICBL AIUiLYSI3 METHOD
ACME ANALYT IC4L LABORATOR IES LTD.852 East Hast i n g s Street,V a n o u v e r , 6. C.GEOCHEM I CAL ANALYSES PROCEDUREC o e rL .e a d . Z i n c a n d S i l v e rThe s o i l samples a r e p r e p a r e d b y d r y i n g t h e sampleSamples60 c, a n d s i e v i n g the sample t o m i n u s 80 mesh.w e i g h i n g 0.5 grams a r e d i g e s t e d i n hot d i l u t e a q u a r e g i a in aat-b o i l i n g w a t e r b a t h a n d d i l u t e d t o 10 ml w i t h d e m i n e r a l i z e d water.T h e e x t r a c t e d s o l u t i o n i s a n a l y z e d b y atomic a b s o r p t i o n for Cu, Pb,Zn a n d 49.GoldThe m i n u sT h e samples a r e i g n i t e d o v e r n i g h t a t 600' .80 mesh p o r t i o n i s g r o u n d i n a r i n g g r i n d e r a n d 10 grams a r ed i g e s t e d w i t h d i l u t e hot aqua r e g i a .The c l e a r s o l u t i o n i s e x t r a c t e dw i t h methyl i s o b u t y l ketone.Gold i s determined i n the m e t h y l isob u t y l ketone e x t r a c t b y atomic a b s o r p t i o n .
APPENDIX 11GEUCHENICXL ANALYSIS C E X T I F I C A T E S
ACME ANALYTICAL LABORATORIES LTD.852 E. HASTINGS, VANCOUVER B.C.PH: 253-3158TELEX :04-53124DATE RECEIVED AUG 151383DATE REPORTS MAILEDA ,500 GM SAMPLE I S DIGESTED WITH 3 !L OF 3:1:3 HCL TO HN03 TO HZ0 AT 90 DE6.C. FOR 1 HOUR.THE SAMPLE I S DILUTED TO 10 MtS WITH HATER. ELEMENTS ANALYSED BY AA : CU, PB, ZN, M.SAHPLE TYPE : SOIL - DRIED hT 0 DEG C., -80 MESH.REGIA LEACH MIBK EXTRACTION, AA ANALYSIS,--ASSAYEHr; {,' pif::) 1.1:-.:i:t.J:F::' :1',. .I.".,".,'.ji::f.!." ,".A,.,. .J b ,i, ,.i.;,2"5:; f::j.t.251/J.l, .I,, 1:::; *. ::; (1):I, ,,I,.,-,,:r.I r-.("j.,;., K:::::i.I:.1, , , l'c::":; Ci . . '75,. .,. .-. %.%. :.'.L.rD E b N TOYE, CERTIFIED B.C.I.1:;:A:.A,.4.(::.I-.FBZ h1l' l/A6PF'M1!3 I (13[35 )(:6 5Q1 1SO1.3.71 '7r-l4F:* I 1F::,F-1. .ai,, .:%LtL-. (5.:y,-,.'L.q a', 662846474:.*-"-"Q-.IiASSAYERau*f3 'f:'.J:'i 0.525. i sC?I75eLI.55L-;J5c::.I2 (2251 (1165.-,L (1) ,&.I.f3 1:j r:'".:,Ib ,.:, -,i::!Wi:) 2?i [:2 .2I.5 r.; (1) .I.5 (:I) E2 .I"2 5 S 0 .I.'i' 5 F'.,:,.".I c-.L.):, ::. "[" .'Y,&,.1;: J,.)(:\1.Ec4" .:s,. 42('j"42 . ti25--1(11. (3
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765 766 767%) 767") Anniversary Date August 22, 1983 August 22, 1983 August 22, 1983 August 22, 1983 . In August of 1983, a series of detail soil samples were taken in order to more fully define the continuity and extent of this anomaly. These samples were taken at 25 metre inter- vals alo
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Can new technologies shak e the empirical foundations of rock engineering? D Elmo University of British Columbia, Canada D Stead Simon Fraser University, Canada B Yang University of British Columbia, Canada R Tsai University of British Columbia, Canada Y Fogel University of British Columbia, Canada Abstract The past decade has witnes
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Chapter III:British Enterprise in Bangkok. 93 1.The Role and Importance of British Trading Houses in Bangkok. 93 2.The British Trading Houses. 100 3.The British Banks in Bangkok. 124 A)Paper Currency. 128 B)The British Response to the Gold Standard,1902. 130 C)The Idea of a National Bank and the Effects on the British Banks. 136 4.Public Works. 147
