strong penetrative foliation
TRANSCRIPT
ARIS SUMMARY SHEET
nDistrict Geologist Kamloops Off Confidential 89 04 06
ASSESSMENT REPORT 17592 MINING DIVISION Kam100ps
CLAIM S
OPERATOR S
AUTHOR S
REPORT YEAR
GEOLOGICALSUMMARY
SBSLAT 51 03 19 LONG
UTM 11 5659405 305851
NTS 082M04wSBS 1 5Minnovapirie I D Goutier F
1988 34 pages
119 46 13PROPERTYLOCATION
The property is underlain by northwest striking and northeast
dipping metavolcanics and sediments of the Devono Mississippian Eagle
Bay Formation No known mineralization occurs on the claims however
the Homestake barite silver deposit occurs 3 kilometres to the north
west and the steep gold skarn area occurs immediately to the south
Rocks range from mafic to felsic volcanics and sediments all of which
show a strong penetrative foliation
WORKDONE
o
Geological GeophysicalEMGR 20 0 km HLEM
Map s 2 Scale s 1 2500
GEOL 200 0 ha
Map s 2 Scale s 1 7500 1 2500
LINE 29 8 kmROCK 220 sample s ME
Map s 12 Scale s 1 7500 1 2500
o
r
oJuly 7 1988
h
LOG NO 0720 RD
ACTION
FilE NO
GEDIOCYGEXXHFHISIlffllND GEDIIriSICS
of the SBS Prqlerty
1dams lake B
NlS 82M4W
rat 510J5 N
FILMED J
lcnj 119046 W
GEOLOGICAL BRANCHASSESSMENT REPORT
Ian D PirieFrancoise Galtier
Minnava Inc
4th Floor 311 Water streetVanacmIer B
o
o
TAmE OFaNrENrs
Pacre
OF CLUSIONS AND ONS l
af 1
General 1
IIJC citiat 1 ro 1
RIysi 2
2
3
of lkJrX 3
RESJInS 4
GeJIClCJYe 4
ReJioMl SettirlrJ 4
GED 4
PrqleJrty Geology smGtid 5
an of units 6
C11loritized Intermediate volcanic group 6
lntermediate to Felsic volcanic group
mtJusive group 8
9
GEDHIYSICS 11
ERD GEDIQGY SBSsKARN l1
SKNRN ZONE 12
CONCLUSIONS ONS 13
BIBLIOGRAmY
ITEMIZED XBlSlWIFNENl
llI1IKR S CATIctlS
o LIS OF I2ffiIm
Paqe
mmE 1 2
rmmE2 9 1
LIS OF FIGURES
FIGJIm 1 Jxcltial 2 1
FIGURE 2 Clllm CalfiguratiCIl am GridIocatiCIl 3 1
MIFS
in pocket
1 Geology Grid Area 1 2500
n2 Lithogeodlanisb SiO TiOCaO MJO
3 Lithogeodlanisb Na20 K20
4 Lithogeodlanisb Ba 01 lb Zn
5 Lithogeodlanisb Au 1lg
6 Lithogeodlanisb As Sb
7 Lithogeodlanisb Fe2C3 MrO Al2C3 Zn
8 Max MiD II 444 Hz
9 Max MiD II 1777 Hz
10 Geology Skarn Area
ll Lithogeodlanisb SiO TiOCaO MJO
12 Lithogeodlanisb Na20 K20
13 Lithogeodlanisb Ba 01 lb Zn
14 LithogeodlemistrAu 1lg
15 LithogeodlemistrAs Sb
16 Litmcjeodlemisby Fe2C3 Mrt Al2C3 Zn
o
o
o
sumARY OF WKIlJSICR AND CR
Detailed mawing sampling an geophysics in an area of the SBS
property iniieated by reconnaissance to be prospected for volcanogenicmassive sulphides has confinned its ananalous nature however further
work will be required to establish drill targets
Reconnaissance to
neighbouring property has
work can now be planned
a skan1 zone projectedits presence and location
locate
confinned
from a
Detailed
INlRJIXJCTCW
General
Minnova Incorporated fonnerly Corporation Falconbridge Copper is
the registered owner of 108 claim units SBS 1 to 6 in the Skwaam BayAdams lake area of the Kamloops mining division British Columbia lhe
clain1s are divided into two grwps SKWAAM West an SKWAAM East
his report presents the results of detailed geological mappingand lithogeochemical sampling at a scale of 1 2500 on a 30krn line gridan reconnaissance geological mapping and lithogeochemical sampling All
work was ied out during October 1987
IDcatioo and lio
lhe claims are located on the south side of Skwaam Bay 30krn east
of IDuis CIeEk an approxinately 75krn northeast of Kamloops Fig 1
Access is by way of the Agate Bay road fran Highway 5 at louis Creek or bythe Adams lake mainline from the town of Adams lake Several logging and
skidder roads facilitate access to the prqerty
o Page 2
Ihvsicxmuhv
be property lies on the westeJnside of the1darns Plateau which
consists of high rolling plateau coontry incised by locally steep drift
filled valleys Elevations range fran less than 500m at lake level to
over 1500m up on the plateau Much of the SBS property lies at around
1500m but drops off steeply north and east into1darns Lake
Fairly dense forest cover occurs across the area with loggingcurrently active right on the property
30 c
period
be climate is moderate with temperatures ranging from 25 C to
Precipitation is low to moderate with a May to November sncwfree
nPnn3rtv and CJrmership
Figure 2 shows the configuration of the SBS claims and the
location of tile 1987 30km line grid Table 1 S1lIlU1Iarizes the pertinentclaim data All claims are 100 owned and operated by Minnova Inc
TAmE 1
Nane Record Units lbIth
SBS 1 6593 20 April SKWAAM West
SBS 2 6594 12 April SKWAAM East
SBS 3 6595 16 April SKWAAM West
SBS 4 6596 20 April SKWAAM Fast
SBS 5 6597 20 April SKWAAM West
SBS 6 6598 20 April SKWAAM East
Page 2 1
I
IJ
IP l
ctg
0I
z
IiI
oI
Iii
I
6
IU OJ0
00 80
1
c 0
6
0
o il9
il
lfJl
ollfJO
0P
6
Ih
IQ
I
@
6
III
oils
ro
f II
OzCo
9
IZtii
o
o
o
Page 3
Historv
he SOO claw were staked in April 1986 Prior to Minnova s
acquisition of the property exploration was restricted to a soil survey
carried cut by eraigmnt mines in 1977 AR 6890 Work on the propertyin 1986 by Minnova included reconnaissance mawing arrl lithogeochemicalsanpling along existing roads
SuIIInarv of WoJKDca1e
Line cutting 30kIn line grid Grid extends from I82 50N
to 11100N arrl from L78E
to L57E see Fig 2 for
location
GeophysicsMax Min II
30 kIn line grid Corrlucted by MWH usingtwo frequencies 444Hz
arrl 1777Hz
Geochemical 16 manooys sanpling220 rock sanples Pace and compass
traversing of roads and
grid area on the
property Analysis for CU
Ib Zn Ag Au Si02 Ti02 Cao
MJO Na20 K20 Fe203 Sb As
Al203 MnO Zr arrl Ea
Geology Pace arrl compass mappingalong roads and grid lines
on the property Mappingscale Grid 1 2500 SOO 5
1 7500
20 manooys
0
o
Ol
61 04
C C ro e
SBS 1I I
GRIDAREA
SBS 3 BS 4
LCP
t
SBS 5 SBS 6
NTS 82M 4W
SBS PRDPERTY
I CLAIM CONFIGURATION I
o
MINN VA
1I
2Km
I
tage OJ l
llJ
i
Ci
to
ij
Q
IIi
iI
0
FIGURE 2
CJ
n
Page 4
RESUIlIS
Geoloav
Reclional SettiIlCl
e rocks of the area belong to the Eagle Bay Fonnation which
lies along the western flank of the Shuswap Metamorphic Complex in the
Omineca Belt e Eagle Bay Fonnation is a multideformed sequence of low
grade meta sediments arrl volcanic rocks which range in age from Cambrian
to Pennian Schiarizza arrl Preto 1984 Intruded repeatedly the Eagle
Bay fonnation was affected by magrratism andor volcanism in Devonian
Cretaceous arrl Eocene time lis evidenced by a penetrative foliation and
the lack of continuity of the units along strike the rocks of the EagleBay Fonnation were extensively deformed during the Jurassic folding event
related to the Colombian Orogeny Campbell 1973 and during the intrusion
of the Raft arrl Baldy batholiths in the midcretaceous later faults and
broad open folds cut through the major units and structures of the
fonnation
e Eagle Bay Fonnation is directly correlative with other
stratigraphic sequences occurring on the edge of the Shuswap MetamorphicComplex Based on lithological structural arrl age similarities the EagleBay Fonnation can be correlated with both the Barkerville and the KootenayArc Terranes Struik 1986
ffiOIERlYGEOImY
Detailed geological mapping and lithogeochemical sanpling were carried out
on the 30km grid e geological mapping along the grid was COl1fliled at
a scale of 1 2500 OUtcrop expJSUre is excellent along the old loggingarrl skidder roads that switch back across the grid but sparse 3 in
the forest COVered area Along with the geological mapping 175 rock
Samples were collected for major oxide arrl trace element analysis On
o
rlJ
o
Page 5
the southwestern cxmer of the property SBS 5 claw a brief
geological reconnaissance SUIVey was initiated and 45 lithogeochemicalsanples were cx llected for analysis
Ihe property is dominated by a XI1plex package of interlayeredmafic to felsic volcanic and volcanoclastic units Ihese units are partlyinterlayered with but lOOStly overlain by a turbidite sequenceconposed of
phyllitic argillite and minor carbonates In the following the two
sanpled portions of the SBS property are diI1 ed separately under
SBSGrid and SBS Skanl
Prooertv Geol SBSGrid
Ihe grid area is underlain by a XI1plex sequence of interlayeredintermediate and felsic volcanic and volcanoclastic rocks Ihis
succession has been regionally metamoqilosed to st facies and
intensively deformed A penetrative mineral foliation striking NW and
dipping NE obscures most of the prinary structures Ihe intennediate
rocks are strongly foliated and altered to green phyllite and schist
chlorite and sericite Rocks of l1IOre felsic affinities are ankeritic
Abundant carbonate phenocrysts probably pseudanoIphic after plagi lase
and limonite pseudanorphs after iron rich carbonate give the rocks a
characteristic brown tinge Detailed mawing has outlined 6 map units
Map 1 Ihese units were defined using field OOservation canbined with
lithogeochemical data Apperrlix 1 Ihe 6 units can be divided into 3
main groups
1 A chloritized volcanic and volcanoclastic group probablyandesitic in UJ1Llfition
2 An ankeritesericite intermediate to felsic group dacite to
rhyCMlacite and quartz porphyries
o
o
o
Page 6
3 An intrusive group mainly quartzlOI1Zonite to diorite
he penetrative foliation am the intense alteration superilrposedon the rcxks in the area hindered the determination of a definite
protolith for these units It does appear that each group Xlntains
lenticular horizonscxlpOSed of massive canponent am of their pyroclasticandor extrusive equivalent hese groops are in stratigraphicXlntinuity however the stratigraphic relationships between mapableunits remains undetennined Definite folds are difficult to outline due
to schistosity developej in the rcxks Folding evidence was only seen in
one area where northwest plunging folds are eQCJSErl Consequentlystratigraphic repetitions caused by unrecognized folds andor faults mayexist
lhroughout the area quartz veining is well developej It
Xlnsists of numerous crisscrossing veins and veinlets and of some majorveins up to 105m thick Besides disseminated pyrite which occurs in
rcxks of each unit the rcxks on the SOO Grid Xlntain little other visible
sulphide mineralization Locally malachite staining and small
chalcopyrite and galena blebs occur mainly at semple locations 103 243
261 266 272 292 294 295 and 348 he felsic quartz porphyry unit
5 1 appears to be the most favorable host for the mineralization
Descrivtial of rock units
Principal lithological units are sh in Map 1 and detailed in
the following
Chloritized Intermediate volcanic
his group includes units 2 1 am 2 3c am Xlntains mainlytuffaceous am aphanitic chlorite Iilyllite and schist Geochemically the
rcxks of this group have a low Si02 Xlntent between 55 and 62 combined
III
J
o Page 7
with Ti02 values greater than 75 amlCMer than 105 see appendix 1 for
data he rooks of this group are propylitized as evidenced by abundant
and pervasive chlorite and lcxal sericite developnent and by the presence
of numerous calcite pods swells am veinlets he most likely protolithfor the rocks of this group is amesitic lhe distinction between the two
members of this group unit 2 1 am 2 3c in the field is difficult
firstly because of their fine grained nature am secondly because they
seem to be of variable lateral extent am lenticular in shape he rocks
of unit 2 1 are aphanitic to fine grained chlorite phyllite with
occasional pyrite grains arrljor aJlL JItes of grains in the plane of
foliation Locally quartz and carbonate occur as diffuse stringersChlorite phyllites of unit 2 3c arecatpOSed of a fine grained chlorite
groundmass supporting slightly coarser quartz grains and volcanic
fragments Mediumgrained carbonate porphyroblasts as well as
calciterich pods are often fourrl in the phyllite sericite is generallynot abundant in these rocks Disseminated pyrite is between 1 to 5 and
limonite stains are occasionally well developed along fractures and
foliation planes
Intennediate to Felsic volcanic crrouo
n
Ibis group includes the rocks of unit 2 3a and 2 3s 3 0 and 5 1
hey are quartz feldsparsericite schists of various affinities Unit 2 3
is corrposed of quartzofeldspathic schists with variable amounts of
superinposed sericite and iron carbonate alteration hey contain variable
amounts of sericitealtered crystals or volcanic fragments 5cm in a
very finegrained light colored quartZ feldspar matrix he schistose
mediumgrained quartz sericite layers or partings may be the result of
hydrothennal alteration consequently some rocks of this unit may be an
altered versicm of rocks from other units Geochemically these rocks are
intennediate in corrposition with a wide range of Si02 and Ti02 content
Si02 between 62 and 70 and Ti02 between 30 to 75 The rocks of
this unit contain variable amounts of sericite and ankerite and outcropped
as pale tan 2 3a to pale green 2 3s phyllites and schists he well
o
c
o
Page 8
layered quartzofeldspathic schist contains 1 to 5 disseminated pyriteThe pyrite ocxurs in two forms 1 as rarrlan disseminated irregular and
very fine grains ani2 as scattered subeuhedral coarser grains be
pyrite altered to liIronite gives a spotty awearance to the rocks
Numerous quartz cartxnate veins aniveinlets cutthrc1ugh the rocks of this
unit
he rocks of unit 3 0 have a finEMJrained rroderately foliated
crystalline grcinitic awearance with superinposed patchy sericite andor
feldspathic alteration Ibis unit is brown weathered due to the
alteration of its Fecarbonate rich mineral Geochemically this group
includes rocks with a high silica content 70 combined with a
relatively low 25 Ti02 content hey are derived from volcanic
rocks of felsic affinities probably rhyCMlacite to rhyolite in
corrplSition
he rocks of unit 5 1 are soft anischistose highly sericitic
quartz porphyry schists The quartz porphyries range in size from 1 to 10
mm and can reJresent 20 to 25 of the rock They are supported by a
pervasively sericitized and intensively foliated grounlmass The
subrounded non flattened nature of the quartz phenocrysts resulted in a
distinctiveIlutrqJy altered surface Occasionally rocks of this llllit
specifically at sanple location 294 exhibit spotty malachite stainingand cany srrall amounts of chalcopyrite
Intrusive
he intrusive group includes weakly foliated granitic textured
fine to medium grained rock of porphyritic dioritecorrplSition he rocks
are UJlI of medium to ooarsegrained subeuhedral quartz and
plagioclase mystals in a medi ined sericitized plagioclase and
quartz rich Ilabrix he intrusives are Ilainly sill like bodies and are in
more or less conrdant contact with the adjacent sericite phyllites and
schists
o
o
o
Page 9
A total of 175 rock saIllles were taken during the SUlVey of the
gridded area Sarlples were of fresh rock representative of the outcropfrom which they were taken weighed 1 1 2 to 2 llJs and were analyzed for
CU Fb Zn Ag Au As Sb SiCTi02 cao MgO Na20 K20 Fe203 Al203MnO Zr and Ba
All samples were analyzed at Min En labs in North Vancouver
Major and minor elements were analyzed by ICP using a fused pelletLithium Borate flux and aqua regia digestion cu Fb Zn Ag As and Sb
were analyzed by ICP after an aqua regia digestion and Au was analyzed bystandard wet geochemical procedures with anlA finish
All elements are plotted on 1 2500 scale maps in the back pocketNotes on their significance follow this paragraph All were viewed takinginto nsideration statistics derived from reconnaissance of the entire
property done in 1986 and summarized in table 2
Si0 Ti0CaO MgO Map 2
bese elements are generally lithologically related although cao
and MgO may inlicate cartJonatization and chloritization respectively
Both Si02 and TiCalmost without exception confirm the presence
of an intennediate to locally felsic volcanic package Weak MgO
enhancement with respect to the property backgrourrl shows no obvious
spatial pattern cao enrichment is both weak and rare
Na20 K20 Map 3
bese alkalis are highly mobile during hydrothennal alteration and
hence are useful inlicators of such be grid area shows considerable
Page 9 1
Qffi OJ
tIl P rlQ Q tIl Q II 111
rp p fJ 0111 111 0 rl Q tIl U
rl 111 l l CIl NCIl CIl m CIl e 0 QJ
0 e l 0 rl CIl0 l 0 N rl N N
P P g P 111 J P a 111 l III ll0 0 0 0 Q III a 0 ll III
p p p l 0 NUI rl 0 Q l CIl
m g 15 l rl l cj 0 0 111 1110 rl 0 l QJ rl Q
III u Q a 0 J
m 1l 1l u 1l N III UI rl p P IIIOJ Q rl Q N III 1l rl 00 CIl UI UI UI UI a rl 111 tIl YcJ UI III 111 tIl 111 N Of u
Q a a N a III rl 0 N l 0 corl 111 N V be Q rl N UI
111 II 111 N tIl UI l 111 ltIl be bO bO tIl UI 0 N N a lN N N UI N Q r N 41 0 Q
0 0 tIl 1l UIv
III Q l 1l JUI 0 CIl r l 111 l UI
P UI tIl rl CIl a p CIl l 1110 r r N 0 0 1l III 0 rlP 00 0 rl P III g t N Y rl III
0 0 0 N rl III N Y 1l Y III Ql t 0 111 a l III co a Jr N UI 0 N N Of 0 co 0111 111 l 111 J g 0
a 111 e a l
I111rl
Q l p0 0
l N l l Pf UI UI UIcJ III bO rl
IH l Q Q rl Q Q l IIIf 0 0 0 r 0 l 0 0r l l Po Po l 0 l l
NH
i 0 Po e111 be bO l l Po l bO bO 111 l
0 fil d l l UI rl UI rl UI l l rl UI rl r UI rl rl0 0 J J rl 0 0 J l J J Jt J J Q r Q r 111 Q J J Q 0 r rl Q r r0 0 III III t r 111 t III III
il IPo tIl CIl 41 41 1l tIl UI 0 41 a 41 41
H t
H
IQ
Il
0co 0 III co
g cot t N co
Nt N t Y
00 t III t 00 Y N 0 0t 0 t
0 Y 0 0 co t coco 0 t III 00 N N N JOJ III 0 III I t I I J I I I I I I III
N Y III N N Y coI I I I co co co co co co
I co co co00 III Y co III Y co co co co co co N co l
0JH
mlIII Y t III Y
co III 00 00 00 N co
J t co 00 N III III Pl0 co N N N III co co
UIIII
r
N rr r r r r r r r r r r r r N r Y
10 m a a a a a a 0P Po Po Po Po Po NPo Po Po Po Po Po Y Y OJa N N 0 0 NOQ 0 0 0 0 N 0 NO Na l j be 111 r N 111 be g 4N f j JcJ Po N IQ H cJ N
o Page 10
soda depletion which does not appeiar to be stratigraphy related and will
require further checking Potash enrichnent is less obvious but where
present is related to the soda depletion
Ba OJ lb Zn Map 4
lhese elements are the direct pathfirxiers for base metal barite
massive suliride deposits believed to occur in the area In the case of
lb the analytical method is different fran that of Table 2 now standard
ICP as opposed to fusionjICP therefore the statistics were not valid
Consequently an arbitrary threshold value of 5Dwn was established on
nsideration of the data
o
All elements show rnnnerous ananalies especially Cu up to
1598ppm and Zn up to 988ppm Ibis is nsiderecl very encouraging and
warranting further exploration
All 1g Map 5
Gold and silver values are generally quite low although two Agvalues of 4 8ppm H100 351 and a 6 1ppm 294 are strongly anomalous
Numerous other values are greater than the threshold of 1ppm OITerall the
results are nsistent with known systems in the area where precious metal
values are rarely very anomalous unless right in the heart of a
mineralizing system
As Sb Map 6
lhese elements were not run in the original rermaissance
therefore no statistical data is available CUrsory examination reveals
that Sb values are unifonnly low while the majority of As values are less
than 2Oppm qonsequently several As anomalies are apparent most notably
o sample 325 2il8ppm 324 203wn and 327 75ppm lhe close proximity
o
o
Page 11
of these sample numbers gives some cause for suspicion of contamination
am further sanpling shoold be done
Fez03 total iraI Al2O3 Zr Map 7
hese elements are generally lithologically controlled am all are
consistent with an intennediate to felsic volcanic package Several
anomalous Mn02 values are iOOicated however their significance is
uncertain at this time
GIDIHYSICS Maps 8 9
A Max Min II survey was corrlucted over the grid area by MWH
Geophysics Ltd A 150m coil separation was used IWo frequencies 444
am 1777 Hz were recorded at 25m intervals alonJ the grid lines
At each station secant measurements were taken to correct for
nominal coil spacing irregularities induced by rough terrain he in
phase am outof phase values read as a percentage of the prinmy field
strength were recorded for each frequency
seriOllS problems were encountered during the survey due to
topography forest company road construction am slash burning As a
result the data is quite noisey am has several gaps in it However no
anomalies seem to be present on either frequency
IroPERlY GIDlilGY SBSsKAml
A skarnified phyllite lies in a turbiditelike sequence in
contact with meta volcanic rocks in the SW part of the property he
sedimentary sequence isconposed of interlJedded argillaceous limestone am
black phyllite with discontinuous horizons of calcareous phyllite he
meta volcanic rock sucxession contains basalts am cherty tuff in contact
with a more intennediatefelsic volcanic am volcanoclastic package Map10
o
o
o
Page 12
hese units appear in stratigraJt1ic cxmtinuity A penetrativefoliation is well developed in the argillaceoos am calcareous rocks am
in the tnyllites It strikes similarly to the foliation in the rocks of
the rest of the property NW diwing NE Small scale folds are
ubiquitoos in the skanUfied tnyllite however neither large scale folds
nor top imicators were fami during this brief survey
Skarn alteration is develqxrl at the ntact between the two units
where thin light grey and green phyllite layers banded tuff and
tnyllites hQ9t gaet and epidote associated with quartz and calcite
he skamified phyllite ntains aImrlant pyrite and pyrrt10tite in nasses
with minor scattered blebs of chalcopyrite am trace galena A distinct
asbestiforrn anphibole probably pyrophylite fills tension fracture veins
in the massive greenstone
Porphyritic quartz monzonite to quartz diorite Ixxlies were found
in close proximity to the skamified phyllite Quartz veining is locallyabundant in tl1e granitic textured rocks rot the relationship between the
skarn development and the presence of the intrusive bodies in their
vicinities have not been yet clearly established
LlJHJGEXHEMI SRARN zcm
Using the procedures ootlined in the Litho section on the gridarea page 8 45 rock sarrples were taken during the skarn zone
reconnaissance am analyzed by the same methods for the same elements
since the mnnber of sarrples is not statistically valid no attenpt has been
made to thus define anomalous and backgnx1rrl nor since the geology of
this area is atypical of the property as a whole are the statistics shawn
in Table 2 valid However the precious metal values along with Sb and As
are readily interpretable and the najor elements will provide an irrportantbase of data for future work as well as enhancing the geological
interpretation All data are displayed on Maps 11 through 16
n
I
o
Page 13
It is apparent that Sb As arxi Ag all display extremely noisey arxi
high values as might be expected in a skarn Unfortunately Au is not
unduly high
Other element patterns generally back up the geological division
into mafic volcanic intrusive felsic volcanic and limeyphyllite sediment
nfCllJSIrn8 AND REXXHlENIl1TIONS
W9rk on two areas of the SBS claim block during 1987 has providedboth an insight into the geology of the p and encouragement to
continue exploration
In the area vered by a grid a better handle on the corrqlex
intennediate to felsic volcanic package has been obtained Although no
clear cut stratigraphic markers were established variations in texture and
alteration mineralogy can be seen In addition the major and trace
element lithcpgeochemisby strongly suggests widespread hydrothennal
activity No geophysical conductors were fourrl but gaps in the survey
should be filled when possible
UleSSPBCIed presence of a skarn zone projected from an adjacent
property was confinned Details of the stratigraphy rerrain to be worked
out with further work Strongly anomalous values in Ag Sb and As are
very encouraging A grid should be established for detailed explorationin the area
o
o
BIBlJrelWHY
Schiarrizza P A am Prete V A 1984 Geology of the Adams Plateau
Cleazwater area B C Ministry of Energy Mines Pet Res
Map 56
stJuik L C 1986 Imbracate1Terranes of the CariJxO Gold Belt with
cprrelations am inplications for tectonics in southern
British Colanbia Canadian Jcxrrnal of Earth Sciences vol
23 pp 1047 1061
Vollo N B 197 Soil SUlVey of the CI claw Assessment Report 6890
o
o
lDHIZID asr
LINECUITING 29 8 kIn @ 310 per kIn
GIDHIYSICS 8 days @ 550 per day
GIDUXY
F Gootier 20 days @ 350 per day
GEXXHEM
220 roCk sarrples @ 20 each
WR Ag Au Ol Ib Zn
SarrplingD Small
A Ross
10 days @ 150 per day6 days @ 150 per day
SUPERVISION
I Pirie 3 days @ 400 per day
TRUCK 22 days @ 60 per day
FOOD AcxxMDATION 38 marrlays @ 50 per day
INIERmEIATION at1FUIERAND REroRl WRITJR
2 days @ 400 per day
DRAFTlliG 5 days @ 150 per day
MISCELIllNFXXJS
Allocatin SKlWMEIST 65
SKlWMWEST 35
22 040
11 868
9 238 00
4 400 00
7 000 00
4 400 00
1 500 00
900 00
1 200 00
1 320 00
1 900 00
800 00
750 00
500 00
33 908 00
o
o
1l1lHR S CUALIFICATIOOS
I Francoise Goutier certify that
1 I am a geologist residing at 302 880 W 71st Avenue Vancouver
Be
2 I have a BSc in Geology fran the Universite de Montreal Quebec
1982 and a MSc Econanic Geology fran the University of British
Columbia Vancouver Be 1986
3 I have practised my profession since 1982
4 Ipersonally carried out or supervised the work reported herein
Francoise GaItier
0
o
o
Gertlflcate of qualifications
1 Ian D Pirle certlfy that
1 Iam an ElliPloration Geologist resLding at 4580 44B Avenue DeltaB C
2 Ihave a BSc Hons in Applied Geology from the Univemlty of StrathclydeGJasgow Scotland 1977 and a HSc Geology Geochemistry from queen s
Universlty at Kingston Ontarlo 1980
3 Ihave practised my profession since 1977
4 IpersonaJly carrled out or supervlsed the work reported hereln
gDat Ian Pirie
CJ
olIlIftIDlX I
CAL1NAUSIS L1SlIIC
o
SAMPLE NO AL203 BA CAO fE203 K20 HGO mm2 NA20 5102 5R TW2 ZR
d85500113 12 0 203 7 2 3 96 3 48 4 89 0 19 3 09 56 8 0 03 0 62 0 012
l855002 17 66 0 038 5 79 4 9B 1 69 3 71 0 21 4 76 57 B9 0 04 0 75 O OOB5855003 13 09 0 006 13 6 10 99 0 21 4 91 0 45 I 47 77 0 08 0 56 0 01
5855004 16 75 0 061 7 39 65 2 45 3 53 0 29 3 62 55 66 0 03 0 77 0 012
5855005 11 52 O 13 63 16 17 0 18 5 35 0 68 1 64 47 31 0 02 0 66 0 012
5B55006 14 39 0 021 12 8 10 3 0 56 3 23 0 52 2 48 42 68 0 06 0 58 0 0075855007 11 6 0 005 15 62 12 11 0 08 5 59 0 66 1 06 41 97 0 02 3 51 0 025
5855008 6 82 0 011 16 55 12 2 0 3 9 07 0 64 0 66 44 12 0 01 0 59 0 0065855009 15 45 0 02 9 56 11 14 0 73 5 62 0 4 3 06 45 95 0 06 2 59 0 0135855010 12 16 0 193 14 53 5 59 2 71 8 56 0 28 0 96 44 83 0 02 0 6 O5855011 14 27 0 159 1 17 2 14 5 27 0 39 0 07 2 82 70 59 0 01 0 29 0 023
5855012 4 4 0 011 13 05 26 72 0 11 7 08 0 61 0 27 42 89 0 02 173 0 0115855013 12 41 0 034 6 73 2 61 0 57 2 58 0 27 4 96 60 91 0 02 0 58 0 01358S5014 13 66 0 007 15 47 9 45 0 11 2 9 0 55 2 75 44 25 0 06 0 59 0 003
58S5015 17 4 0 059 10 46 5 92 2 13 6 16 0 27 2 41 51 74 0 03 0 95 0 0055B55016 14 86 0 013 10 84 8 5 0 47 5 03 0 67 3 42 53 04 0 03 0 75 0 0055855017 14 96 O 13 69 7 14 0 11 4 22 0 4 2 65 51 25 0 06 1 19 O5B55018 10 03 O 15 09 14 67 0 11 6 12 0 87 0 58 43 49 0 02 101 O OO lS8S5019 11 38 0 06 4 32 4 8 1 42 3 56 0 19 3 35 67 49 0 01 0 69 0 024S855020 13 66 O 12 6 5 93 0 08 5 51 0 33 3 83 51 1 0 04 16 0 008S8S5021 15 53 0 005 13 92 8 23 0 19 3 27 0 4 2 58 50 4 0 02 0 64 0 009S8S5022 18 62 0 009 5 74 12 31 0 15 5 17 0 27 4 27 48 03 0 07 0 92 0 006S8S5023 9 43 O 16 67 15 15 0 1 4 67 0 65 0 12 42 48 0 03 0 42 O58S5024 16 74 0 009 8 09 12 94 0 2 5 54 0 3 2 16 44 45 0 07 0 99 OS8S5025 14 79 0 123 2 53 2 06 3 63 0 63 0 09 2 66 69 8 0 01 0 33 0 0215855026 14 33 0 094 2 4 2 91 3 17 0 58 0 09 3 67 69 39 0 01 0 31 0 0258S5027 15 08 0 18 1 22 1 92 5 46 0 38 0 09 2 14 69 76 0 01 0 31 0 027
58S5028 15 25 0 136 0 17 3 69 2 65 0 57 0 11 2 88 71 59 0 01 0 4 0 018
S8S5029 15 49 0 063 1 43 6 49 169 1 73 0 35 3 33 66 29 0 02 0 49 0 018
S855030 15 72 0 101 1 1 4 47 2 2 0 95 0 11 3 99 68 53 0 02 0 47 0 015
S8S5031 15 93 0 193 0 14 4 52 4 49 1 22 0 06 2 01 68 52 0 01 0 45 0 02
S8S5032 15 43 0 056 1 42 4 53 1 08 0 95 0 08 5 79 67 3 0 03 0 46 0 017
S8S5033 14 47 O 12 7 11 04 0 12 3 86 0 4 2 77 50 27 0 04 0 93 0 017
SBS5034 13 72 0 014 11 33 11 53 0 23 6 59 0 53 2 67 46 22 0 03 3 32 o m
5BS5035 14 77 0 128 0 06 4 12 3 93 0 6 0 23 1 91 71 62 0 01 0 32 0 02
5B55036 14 35 0 121 2 65 162 3 49 0 58 0 1 2 71 70 33 0 01 0 28 0 015
SBS5037 14 85 0 168 1 11 2 27 5 11 0 43 0 07 2 97 69 93 0 01 0 3 0 017
5BS5038 15 58 0 096 173 6 57 2 88 5 89 0 2 2 62 61 01 0 01 0 66 0 011
58S5039 13 94 0 172 0 81 2 93 4 76 0 49 0 06 2 41 71 19 0 01 0 22 0 019
5BS5041 14 45 0 148 116 3 83 3 57 0 55 0 11 3 62 68 95 0 01 0 32 0 023
5B55042 14 5 0 149 0 7 3 49 4 4 0 36 0 07 3 38 69 47 0 02 0 3 0 022
5855044 14 76 0 11 0 62 3 13 3 43 0 6 0 1 3 01 71 05 0 01 0 31 0 019
S8S5045 14 83 0 153 0 91 2 86 4 59 0 42 0 08 3 15 69 47 0 01 0 31 0 022
S8S200 14 79 0 1 4 74 3 93 2 9 1 36 0 35 3 25 64 11 0 01 0 36 0 021
S8S204 17 07 0 07 0 19 6 14 2 88 0 66 0 2 2 42 67 19 0 01 0 58 0 019
S8S205 13 75 0 089 3 06 3 75 2 33 1 57 0 34 3 37 67 75 0 01 0 34 0 02
58S206 15 32 0 051 2 1 5 38 1 82 2 3 0 21 3 46 65 66 0 01 0 64 0 015
S8S207 18 51 0 081 151 6 36 4 12 4 54 0 3 2 17 58 89 0 01 103 0 01
S85208 14 62 0 08 5 44 5 37 2 53 2 72 0 21 2 34 58 82 0 02 0 57 0 013
5BS209 18 1 0 096 1 49 8 15 3 66 2 8 0 09 1 94 60 52 0 01 0 75 0 017
S8S211 16 01 0 071 5 49 7 49 3 76 1 17 0 62 1 01 56 29 0 01 0 71 0 014
0585212 16 97 0 104 2 19 6 59 4 16 2 98 0 25 1 42 62 24 0 01 0 71 0 012
jS8S213 16 11 0 122 0 85 5 87 3 43 1 98 0 27 2 73 65 68 0 01 0 55 0 02
S8S214 18 13 0 15 0 22 6 22 5 36 1 83 0 17 0 61 63 76 O 0 81 0 014
S8S215 14 12 0 084 0 83 2 29 3 05 0 35 0 21 2 66 73 99 0 01 0 16 0
58S216 13 76 0 058 2 61 2 29 3 04 0 55 0 15 2 47 71 72 0 01 0 16 O
S8S217 13 84 0 062 0 33 182 3 75 0 52 0 16 1 25 75 93 O 0 14 O5BS218 16 68 0 067 2 71 6 75 3 11 2 07 0 22 2 35 62 47 0 01 0 69 0 015
S85219 6 48 0 027 7 84 5 99 1 36 3 73 0 9 1 18 69 48 0 02 0 24 Oc nt 1I 11 t n 177 I n Ii 71 I I n Q fllIQ Cj 1 1 Q n III n iiQ n n
8AMPLE NO AL203 BA CAO FE203 K20 MUO MN02 N 20 SlOt SR IIO IR
OSB822116 31 0 12 0 1 2 75 5 41 0 89 0 09 0 12 71 52 O 0 25 0 009
S8S222 3 0B 0 022 0 05 1 41 0 91 0 15 0 09 0 02 91 BB O 0 04 0 005J
SBS223 lB 43 0 11 0 12 B 34 4 02 0 B2 0 16 1 36 63 43 0 01 0 76 0 013S8S224 15 39 0 092 2 13 4 32 2 23 0 72 0 12 4 14 67 14 0 01 0 42 0 027SBS225 16 59 0 103 2 35 7 35 2 6 2 19 0 19 3 86 60 B6 0 01 0 63 0 015
SBS226 17 12 0 127 1 28 5 4B 3 99 1 78 0 1 2 13 64 42 0 01 0 64 0 019
SBS227 12 B4 0 108 6 64 4 47 3 08 2 97 0 5 1 96 61 98 0 02 0 29 0 015
SBS228 13 78 0 113 0 29 3 23 3 54 0 78 0 27 1 74 73 57 0 01 0 4 0 015SBS229 18 15 0 031 0 5 7 31 3 53 5 64 0 23 0 4 60 96 0 01 0 85 0 005SB9230 8 27 0 018 0 13 3 79 1 99 I91 0 1 0 13 80 86 O 0 36 0 005S8S231 16 29 0 109 0 78 5 55 3 19 1 75 0 19 3 02 66 15 0 01 0 44 0 022SBS232 14 5 0 099 3 8 4 74 2 94 1 59 0 22 3 05 65 43 0 02 0 45 0 013
SBS233 15 28 0 103 2 09 4 11 2 82 0 73 0 17 3 67 67 76 0 01 0 4 0 017
SBS234 16 13 0 135 0 57 3 79 3 72 0 7 0 13 2 B 69 2 0 01 0 35 0 029
SBS235 15 51 0 07 0 43 5 21 I99 0 5 0 28 4 69 19 0 01 0 46 0 022
9BS236 14 97 0 105 0 93 3 4 2 47 0 64 0 05 4 2 70 46 0 01 0 3 0 02S9S237 14 35 0 059 3 45 4 6 1 59 1 72 0 15 5 05 66 1 0 02 0 4 0 019
SBS23B 13 08 0 056 2 33 2 14 4 28 1 47 0 35 0 07 71 97 0 01 0 15 O
S8S239 14 09 0 096 0 4 2 94 2 44 0 56 0 14 3 67 72 36 0 01 0 26 0 019
S9S240 16 03 0 077 2 Bl 7 24 2 6 2 59 0 29 2 71 61 26 0 01 0 74 0 014
S9S241 14 92 0 099 1 29 4 66 4 57 1 31 0 23 0 35 69 94 0 01 0 39 0 022
888242 13 81 0 127 1 38 2 98 3 23 0 92 0 11 2 46 7223 0 01 0 26 0 016
SBS244 15 42 0 082 0 08 3 05 5 14 0 B9 0 3 0 14 72 34 O 0 25 0 007
SBS245 15 07 0 102 0 15 2 87 2 9 0 53 0 11 3 51 72 16 0 01 0 27 0 017
SB8246 15 45 0 09 2 26 7 35 2 03 2 03 O IB 3 65 61 94 0 02 0 74 0 01
S88247 14 22 0 113 3 12 3 76 3 64 0 94 0 24 2 1 68 08 0 01 0 3 0 019
OSBS248 15 62 0 078 2 45 6 83 2 2 I75 0 14 3 7B 62 11 0 02 0 75 0 015
SBS249 14 55 0 111 2 43 3 18 3 61 0 97 0 1 2 32 69 55 0 01 0 3 0 024
SBS250 15 22 0 097 3 74 5 39 2 74 2 07 0 16 3 12 63 1 0 02 0 45 0 015
SBS251 15 16 0 10B 153 4 15 3 25 I 0 12 3 17 67 32 0 01 0 42 0 02
SBS252 15 33 0 134 1 96 5 7 3 73 1 25 0 12 2 11 66 84 0 0 0 41 0 018
SBS253 15 75 0 097 2 92 6 86 3 4 0 72 0 37 2 84 64 2 0 01 0 5 0 015
SBS254 14 64 0 103 0 84 3 14 3 37 0 59 0 11 2 64 72 01 0 01 0 29 0 02
SB8255 15 48 0 129 0 44 3 2 3 75 0 82 0 16 2 9 69 95 0 01 0 35 0 026
SB8256 15 65 0 103 1 6 3 24 2 5 0 96 0 05 4 61 67 83 0 01 0 37 0 026
SBS257 4 22 0 084 3 07 3 16 3 3 0 B2 0 27 2 B 69 11 0 01 0 35 0 019
S8S258 18 17 0 185 107 8 92 5 44 2 84 0 16 0 4 59 04 0 01 0 69 0 008
888259 15 43 0 108 1 39 4 79 3 52 1 57 0 18 1 83 67 7 0 01 0 41 0 02
SBS260 15 32 0 095 2 44 5 13 2 62 1 2 0 15 3 35 65 66 0 01 0 46 0 019
SBS261 15 31 0 07 3 67 3 9 2 25 0 71 0 15 4 03 64 05 0 02 0 42 0 031
SBS262 14 65 0 095 I59 2 86 2 49 0 56 0 13 4 4 69 05 0 01 0 33 0 021
SBS263 15 96 0 137 2 4 09 2 95 1 16 0 14 3 47 65 32 0 01 0 41 0 021
SBS264 13 84 0 088 2 98 3 78 2 71 0 96 O OB 2 94 67 57 0 02 0 31 0 018
SBS265 13 29 0 065 2 56 2 74 2 17 0 98 0 15 3 96 69 34 0 01 0 19 0 018
SBS266 16 55 0 068 3 7 14 28 I92 4 7 0 42 2 55 51 18 0 02 0 6B O
S8S268 15 4 0 138 1 65 4 93 4 13 0 8 0 17 2 25 66 37 0 01 0 45 0 021
SBS269 14 47 0 07 0 49 2 49 1 77 0 32 0 09 5 11 72 45 0 01 0 26 0 016
S8S270 14 56 0 093 1 73 3 42 2 72 0 58 0 26 3 62 68 7 0 01 0 33 0 021
S8S271 15 66 0 117 162 6 73 3 44 0 75 0 31 2 62 64 59 0 01 0 64 0 016
888m 14 74 0 112 181 3 51 3 06 0 67 0 19 3 5 68 96 0 01 0 35 0 015
S8S273 15 4 0 219 0 23 2 99 2 46 0 44 0 1 4 6 70 82 0 01 0 31 0 018
S88274 16 13 0 066 5 83 8 15 1 33 3 84 0 23 4 2 51 88 0 03 0 61 0 007
j SBS275 17 34 0 085 I71 5 61 4 15 2 31 0 25 1 35 63 93 0 01 0 69 0 014
S8S276 15 94 0 068 3 34 5 89 2 51 1 72 0 24 3 43 62 72 0 01 0 71 0 012
S8Sm 16 77 0 056 181 6 55 2 88 0 99 0 23 2 63 64 17 0 01 0 71 0 013
SBS278 14 74 0 066 149 5 13 2 74 196 0 28 2 17 67 72 0 1 0 54 0 013
SBS279 15 84 0 071 129 6 09 3 15 2 0 17 2 2 65 78 0 01 0 59 0 018
SBS280 16 8 0 096 143 6 2 3 34 1 14 0 18 2 38 65 38 0 0 0 65 0 02
SBS281 17 34 0 093 0 86 6 45 2 76 1 21 0 11 3 35 64 47 0 01 0 8 0 017
qRq R I r5 O r 4q 1 7q o I 7q r4 OR o 01 o rR o 017
8AMPLE NO AL203 BA CAO FE203 K20 HOO MN02 NA20 8102 8R TI02 ZR
dB82B316 51 0 09B O lB 10 31 3 2 4B 0 21 13 62 8 0 01 0 78 0 013
BS284 14 79 0 125 0 82 3 04 2 61 0 8 0 05 4 55 70 55 0 02 0 29 0 02SB82B5 15 93 0 09 0 25 3 32 3 2 0 62 0 22 3 32 70 18 0 01 0 4 0 0288B8286 16 4 0 072 2 28 5 94 1 86 0 95 0 12 5 OB 63 8 0 02 0 65 0 0258B8287 16 49 0 OB3 3 12 3 27 2 61 0 73 0 07 4 28 65 92 0 02 0 53 0 029
SB82BB 15 Bl 0 101 1 68 3 55 3 01 0 67 0 11 4 4 67 8 0 01 0 37 0 0278B8289 17 0 133 2 61 7 46 4 34 2 42 0 27 1 4 59 42 0 01 0 9 0 0148B8290 13 45 0 OB2 0 04 3 2 3 63 1 2 0 1 0 11 75 B6 0 01 0 14 O
8B8291 13 95 0 084 0 51 6 62 2 36 2 05 0 18 2 25 69 61 0 01 0 2B 0 028B8m IB 76 0 208 0 43 4 49 5 62 0 B5 0 05 2 21 64 51 0 01 0 43 0 0318B8293 17 46 0 072 0 79 12 02 2 44 4 B3 0 22 1 4 57 35 0 01 0 B6 0 015
SB5294 12 67 0 069 0 04 B 9 1 94 2 4 0 15 1 69 6B 67 0 01 0 24 0 017
8B8295 15 52 0 051 0 62 7 76 197 4 45 0 26 2 49 63 57 0 01 O B 0 018B8297 15 IB 0 09 2 19 7 39 3 3 2 63 0 2 1 3B 63 66 0 01 0 63 0 014
5B529B 14 B 0 OB7 3 62 4 97 2 B5 1 03 0 16 2 99 65 17 0 02 0 45 0 015
SB8299 15 59 0 076 3 5B 6 76 2 53 4 02 0 23 3 22 5B 63 0 02 0 5 0 0118B8300 13 9 0 113 2 61 415 3 71 O BB 0 16 2 15 67 72 0 01 0 3 0 02
8B8301 15 BB 0 131 12 5 7B 3 65 I76 0 11 2 69 65 71 0 01 0 46 0 0178B8302 14 5B O OBB 0 15 3 39 3 33 0 76 0 12 2 72 72 27 0 01 0 29 0 019
8B8303 16 25 0 116 2 14 7 25 3 29 1 5 0 12 2 55 63 23 0 01 0 7B 0 0138B8304 12 3 0 029 0 07 9 64 2 0 55 0 06 2 B4 69 76 0 01 0 33 0 0228B5305 17 9B 0 171 0 62 3 29 4 33 0 B2 0 06 3 1 66 98 0 01 0 39 0 0295B8306 16 9B 0 07 0 17 6 08 3 04 0 67 0 1 2 B7 66 9 0 01 0 62 0 021
8B8307 13 43 0 063 2 05 I99 3 08 0 42 0 14 2 37 73 54 0 01 0 15 O
8B830B 17 19 0 068 3 86 12 47 2 25 3 67 0 39 2 53 53 93 0 02 0 67 O
8B5309 14 67 0 068 0 06 2 37 M3 O BI 0 17 0 1 74 3 O 0 24 0 005
OB5310 15 27 0 074 O BB 4 5 2 BI 0 77 0 17 3 14 69 54 0 01 0 44 0 019
j8B8311 16 03 0 082 2 99 6 B 2 33 3 22 0 25 2 74 61 99 0 01 0 69 0 008
8B8312 16 03 0 059 2 37 7 97 2 61 3 69 0 2B 2 11 61 1B 0 01 0 63 0 007
5B8313 15 29 0 094 1 6 6 41 3 24 0 94 0 27 1 94 66 B2 0 01 0 54 O OIB
5B8314 12 4B O OBl 3 09 3 B2 3 09 0 9B 0 39 1 6B 70 81 0 01 0 28 0 019
8B8316 12 77 0 05 2 44 2 52 1 88 0 88 0 18 3 88 71 9B 0 01 0 22 0 014
8B8317 14 52 0 089 2 31 3 1 2 15 0 59 0 08 4 32 69 31 0 02 0 32 0 023
8B831B 14 B4 0 093 4 98 3 0B 1 5B 1 41 0 1 5 1 65 47 0 03 0 47 0 021
8B8319 IB 92 0 142 0 38 6 2 4 75 2 26 0 16 2 53 6154 0 01 0 7 0 012
SB8320 20 21 0 126 0 47 6 25 3 65 1 6 0 17 4 67 59 52 0 01 0 78 0 03
8B8321 12 62 0 077 3 65 3 65 2 9 1 03 0 27 2 52 68 29 0 01 0 32 0 013
5B5322 17 17 0 069 0 32 6 44 2 16 2 0 07 5 44 63 14 0 01 0 72 0 017
8B8323 14 41 0 123 2 4B 8 83 2 28 3 38 0 37 1 92 6153 0 02 0 7 0 009
8B8324 14 74 0 095 2 B 6 BI 2 29 2 52 0 26 2 95 63 12 0 02 0 66 0 011
8B8325 17 09 0 076 0 4 B 25 2 63 3 19 0 45 2 29 62 06 0 01 0 77 0 009
5B8326 16 23 0 128 2 33 7 97 3 06 1 61 0 29 2 89 61 23 0 02 0 76 0 011
8B5327 14 8 0 126 1 83 3 49 4 06 0 85 0 09 2 21 69 07 0 01 0 31 0 022
5B532B 15 58 0 068 4 41 6 85 2 35 2 71 0 25 2 65 58 07 0 02 0 62 0 01
8B8329 19 18 0 078 0 35 7 91 3 56 3 17 0 21 1 94 60 07 0 01 0 86 0 015
SB5330 14 79 0 052 2 33 6 49 2 01 2 54 0 27 3 47 64 68 0 01 0 51 0 018
8B8331 16 61 0 07 2 81 8 35 2 87 0 73 0 37 2 19 62 37 0 01 0 75 0 014
8B8332 16 57 0 087 0 78 8 13 4 08 1 67 0 43 0 77 64 21 0 01 0 74 0 012
5B5333 14 13 0 055 5 22 5 91 3 09 162 0 52 2 07 60 86 0 01 0 59 0 008
8B8334 14 5 0 083 2 03 3 2 I92 0 48 0 09 4 57 69 47 0 02 0 31 0 02
8B8335 13 81 0 078 1 93 2 62 2 24 0 7 0 13 4 17 71 62 0 01 0 26 0 021
1B8336 13 69 0 076 2 27 4 27 2 83 0 82 0 34 2 61 70 34 0 01 0 3 0 016
SB8337 14 46 0 132 2 03 3 11 3 05 1 07 0 2 3 21 70 06 0 01 0 29 0 023
8B533B 13 92 0 087 0 8 2 6 2 18 0 43 0 17 4 18 73 16 0 01 0 22 0 016
8B8339 16 32 0 228 0 42 5 18 5 02 122 0 2 0 3 68 14 0 01 0 52 0 027
8B8340 16 36 0 165 0 85 4 43 3 6 0 89 0 09 2 94 67 51 0 01 0 54 0 022SB8341 16 26 0 OB8 2 86 5 2 18 1 17 0 15 4 73 63 29 0 02 0 71 0 0228B8342 13 B3 0 093 0 08 2 56 2 34 0 45 0 06 3 64 74 38 0 01 0 22 0 013
8B8343 14 69 0 102 1 28 4 06 3 18 0 68 0 19 3 1 69 65 0 01 0 33 0 021
8RSlli 16J13 0 iO 1A3 B Lib
SAMPLE NO AL203 BA CAO FE203 K20 MGO MM02 MA20 5102 5R TlO2 IR
dB534515 71 0 131 1 06 5 22 3 07 1 0 06 3 17 67 48 0 01 0 62 0 014
B5346 15 74 0 106 0 82 7 12 3 1 2 14 0 29 1 71 65 76 0 01 0 66 0 0125B5347 15 9 0 074 1 05 5 74 3 56 2 7 0 2 117 66 03 0 01 0 6 0 0165B5349 12 51 0 039 1 97 3 49 2 0 75 0 46 3 52 71 74 0 01 0 21 0 014
S8S350 IB 51 0 064 0 35 9 26 2 93 4 55 O ll 2 28 5B 62 0 01 0 74 0 0075B5351 11 88 0 071 1 1 2 29 3 82 0 76 0 64 0 07 76 86 0 01 0 13 O5B5352 13 83 0 209 1 91 2 42 2 41 0 73 0 2 3 59 71 1 0 01 0 25 0 017
5B5353 16 83 0 097 0 75 7 04 2 84 1 39 0 12 3 47 64 03 0 01 0 78 0 013
5B5354 15 94 0 103 3 1 3 9 3 5 1 18 0 16 3 13 64 14 0 02 0 72 0 0175B5355 13 69 0 113 5 56 7 39 1 81 2 89 0 23 3 32 57 93 0 03 0 5B 0 0095B5356 1701 0 116 145 8 38 3 1 2 78 0 25 2 73 60 19 0 01 0 59 0 009
5B5357 13 81 0 058 4 36 5 65 2 23 1 74 0 2 2 76 62 38 0 02 0 4 0 013
5B535B 15 56 0 077 3 56 5 11 418 1 13 0 23 1 32 63 03 0 01 0 41 0 0175B5360 14 22 0 132 2 34 2 93 3 07 0 49 0 11 2 82 69 26 0 01 0 27 0 021585361 15 66 0 127 112 2 61 3 67 0 66 0 06 3 12 69 65 0 01 0 32 0 022
5B5362 14 89 0 133 2 53 3 18 4 5 1 3 0 09 1 5B 68 27 0 01 0 32 0 023
5B5363 14 29 0 133 1 4 5 99 3 34 I B8 0 2 1 47 67 92 0 01 0 3B 0 009
585364 15 51 0 09 2 64 5 35 2 85 1 9B 0 15 2 47 64 06 0 02 0 54 0 017
5B5365 15 97 0 09 0 52 4 27 3 75 2 51 0 13 1 87 67 43 0 01 0 55 0 019
5B55040
5B55043
5B51243
5B51267
5B51296
5B51315
58534B
OB51359
o
6AMPLE NO TOm NA K AS A6 B CU PB 6B III AU PPB LINE DEP
dB6500193 59 6 57 0 8 10 I 10 21 I lB 5
B65002 97 52 6 45 t 2 21 7 29 IS I 2B 518B85003 92 6B 1 21 2 3 15 52 17 3 45 5
6B65004 97 06 6 07 1 7 9 6 36 11 I 21 10
6B65005 97 17 182 2 6 13 5 76 12 4 19 5
6B85006 87 65 3 04 2 1 4 13 10 15 2 53 56865007 92 25 114 5 5 14 10 4 34 3 44 15
6B65008 90 97 0 96 1 8 9 I 24 13 I 17 10
6865009 95 19 3 79 5 8 45 25 230 5002 742 101 606B65010 90 43 3 67 2 3 19 6 37 95 II 13 56865011 97 21 8 09 0 6 7 I 20 30 13 29 5
6865012 96 9 0 38 4 5 I 5 964 69 14 32 20
6B65013 9I 6B 5 53 2 4 65 2 22 63 B34 51 5
6B65014 89 81 2 86 2 9 58 22 34 48 1743 78 5
6865015 97 51 4 54 2 4 13 7 4 16 27 21 56865016 97 63 3 B9 2 4 99 B 25 68 12 60 5
6865017 95 6B 2 76 3 4 12 7 I 200 I 29 56B65018 92 0 69 2 6 12 9 27 20 2 51 106B65019 97 29 4 77 2 2 13 3 22 15 2 30 5
6B65020 94 69 3 91 3 8 18 I I 21 2 II 156865021 95 19 2 77 1 5 22 2 18 4 I 22 56865022 95 57 4 42 2 4 4 35 29 16 2 128 5
6B65023 89 72 0 22 1 9 9 9 I II 2 41 5
6B65024 91 49 2 36 2 5 21 42 34 28 4 140 5
6865025 96 68 6 29 0 8 3 I I 10 I 10 56865026 96 98 6 84 0 8 12 I 8 8 2 24 10
06865027 97 17 8 2 0 5 4 I 4 9 I 24 5
6865028 97 48 5 53 0 3 I 3 I 7 2 43 58885029 97 39 5 02 1 1 7 15 5 24 5 70 5
6865030 97 68 6 19 0 6 I 6 I 12 3 42 5
6865031 97 56 6 5 0 3 10 7 I 14 2 46 5
6 65032 97 14 6 87 0 5 2 5 I 11 3 36 56B85033 96 61 2 B9 2 3 6 2 153 II I 16 106B65034 96 22 2 9 2 2 19 14 16 22 4 78 5
6B65035 97 69 5 84 0 4 48 I 13 30 2B58 37 5
6B65036 96 27 6 2 0 7 6 2 3 12 I 21 5
8B85037 97 22 B OB 0 4 5 2 6 10 1 23 5
6B65038 97 25 5 5 1 5 5 26 3 28 2 169 20
6B65039 97 01 7 17 0 6 I 2 18 9 I 27 10
6B65041 96 75 7 19 0 9 6 3 6 10 I 22 5
6865042 96 87 7 78 0 6 8 2 9 B 2 23 5
6B65044 97 16 6 44 0 7 7 I 9 II I 19 5
6B65045 96 8 7 74 I 10 2 10 77 2 26 10
6B6200 95 93 6 15 1 2 18 9 19 23 I 42 10
6B6204 97 52 5 3 0 6 7 9 74 18 2 128 15 9985 5900
6B6205 96 38 5 7 1 3 21 8 144 53 2 54 5 9985 5900
6B8206 96 96 5 28 0 9 9 16 30 28 4 74 5 9980 5860
6B6207 97 53 6 29 0 9 23 19 31 32 4 114 10 9865 5700
686208 92 74 4 87 1 2 15 18 20 35 3 66 5 9840 5820
6B6209 97 61 5 6 0 7 4 22 9 20 5 84 5 9825 5975
6B6211 92 63 4 77 1 6 4 9 7 63 3 118 20 9775 6180
0686212 97 64 5 58 I 10 16 42 26 I 79 10 9750 6380
6B6213 97 62 6 16 0 7 13 15 50 50 I 110 5 9760 6450
6B6214 97 27 5 97 I 2 13 316 47 1 200 5 9700 6520
6B5215 97 75 5 71 0 7 6 5 5 34 2 28 5 9690 65006B5216 96 B2 5 51 0 7 B 5 3 32 I 26 10 9690 6400
6B5217 97 8 5 0 5 10 4 4 21 2 25 5 9630 61806B6218 97 14 5 46 0 9 5 9 14 30 2 97 5 9625 6200
6B5219 97 24 2 54 1 9 33 5 23 102 2 51 5 9625 6200
6B5220 97 66 5 68 0 6 2 8 39 23 2 112 15 9610 6260
SAMPLE NO TOm NA K AG AS B CU PB SB ZN AU PPB LINE DEP
dBS22197 57 5 53 0 4 5 3 B 12 2 27 5 9595 6305
8S222 97 72 0 99 1 6 13 1 12 m 3 22 5 9595 6305585223 97 57 5 38 0 5 1 9 48 20 3 99 5 9600 6350SBS224 96 73 6 37 0 9 4 B 57 17 2 41 5 l575 63 lOSB6225 96 74 6 46 1 1 15 31 24 1 81 10 9575 6 150SBS226 97 0B 6 12 0 7 2 14 29 18 4 76 5 9525 6500585227 94 88 5 04 1 6 25 8 38 47 1 31 5 9520 6530SBS22B 97 72 5 28 0 6 6 4 61 52 2 23 15 9460 6500SBS229 97 62 3 93 0 5 12 13 130 18 1 55 10 10710 6820SBS230 97 56 2 12 0 7 10 3 81 22 2 33 5 10580 6875SBS231 97 51 6 21 0 4 5 3 27 9 1 21 5 10550 6830SBS232 96 86 5 99 0 2 3 3 7 B 1 31 5 10150 6B30SBS233 97 17 6 49 0 4 1 3 41 21 1 77 5 10030 68008B8234 97 58 6 52 0 2 5 1 2 6 1 26 5 9910 6880SBS235 97 68 5 99 0 6 6 2 22 20 1 29 5 9750 6800SBS236 97 57 6 67 0 8 15 2 12 84 1 121 10 9740 67808B8237 97 51 6 64 0 4 4 1 33 23 1 60 5 9700 6790
8B8238 95 89 4 35 0 8 17 17 36 19 4 87 5 9650 6815SBS239 97 59 6 11 0 5 4 5 34 14 1 47 5 9580 6810SBS240 96 37 5 31 0 4 3 2 2 9 1 11 5 3375 68108B8241 97 78 4 92 0 3 5 2 7 60 1 71 5 96BO 6770SBS242 97 54 5 69 0 2 5 1 26 21 1 80 5 96BO 67306B6244 97 7 5 28 0 7 18 13 31 13 4 94 5 9620 6780S8S245 97 72 6 41 0 7 7 2 87 15 1 25 10 9550 6700SBS246 95 75 5 6B 0 6 12 13 26 13 4 75 5 9580 6720SB6247 96 54 5 74 0 3 3 1 2 8 1 14 5 9500 6700
OB8148 95 75 5 9B 0 5 16 11 1 19 1 61 5 9400 6710SBS249 97 15 5 93 0 4 6 2 7 26 2 33 5 9190 6850SBS250 96 13 5 B6 0 4 11 5 4 11 2 51 5 9220 6810SBS251 9626 6 42 0 6 1 2 1 14 1 43 5 9215 6725SB8252 97 62 5 B4 0 4 5 2 97 6 1 21 10 9460 6660SBS253 97 67 6 24 0 2 5 1 2 9 1 14 5 9480 6600SBS254 97 77 6 01 0 3 1 3 8 5 1 21 5 9400 6610SBS255 97 21 6 65 0 8 10 2 23 27 1 20 5 9375 6620SBS256 96 96 7 11 0 4 15 16 61 9 4 93 5 9265 6590SBS257 97 03 5 93 0 5 1 8 2 14 3 70 10 9315 6660SBS258 96 92 5 84 0 3 2 1 14 7 1 24 5 9375 6500SBS259 96 97 5 35 0 6 8 1 7B lB 1 20 5 9290 6490SBS260 96 47 5 97 0 5 12 B 2 14 1 49 10 9140 6580SBS261 94 6 6 28 0 9 7 3 417 33 1 42 5 9270 6430SBS262 96 1B 6 B9 0 4 6 1 16 B 1 14 10 9375 64008BS263 95 69 6 42 0 6 1 7 37 13 2 4B 5 9260 6475
SBS264 95 3 5 65 0 5 5 3 B 11 1 32 5 9350 6480
SBS265 95 49 6 13 0 3 9 1 72 21 1 14 5 9450 6400
SBS266 96 07 4 47 0 9 lB 23 280 18 6 156 10 9480 6420
SBS268 96 31 6 38 0 3 1 2 21 10 1 21 5 9450 6300
SB6269 97 53 6 B8 0 2 1 1 6B 8 1 14 5 9460 6330
SBS270 96 03 6 34 0 5 2 1 183 31 1 49 10 9315 6200
8BS271 96 51 6 06 1 1 I 4 158 58 2 41 15 9340 62l0
SB8m 96 94 6 56 0 9 5 6 9 9 2 30 5 9310 6160
8BS273 97 59 7 06 0 1 2 I 16 8 1 16 5 9325 6290
OSBS274 92 31 5 53 0 9 19 20 21 19 4 77 10 9500 6540
SB6275 97 45 5 5 0 9 6 9 3B 14 1 73 5 J9l0 60BO
SBS276 96 59 5 94 1 14 11 33 14 4 93 5 9B15 6110
SBsm 96 82 5 51 0 7 6 11 71 12 2 Ill 5 9880 6130SBS278 96 86 4 91 0 7 12 11 29 25 4 79 5 9820 6160
8B8179 97 12 5 35 O B 12 12 11 13 I 80 10 9675 6140SBS280 97 61 5 72 0 7 9 9 25 14 2 80 5 9610 6100
SBS281 97 47 6 11 0 6 6 11 lB 8 I 99 5 9600 6060r
SAMPLE NO TOm NA K AG AS B CU PB se IN u ppe LInE DEP
SBS283 97 68 4 3 0 3 14 17 84 9 I 152 5 9550 6150
OBS284 97 68 7 16 0 6 I 5 4 5 I 27 5 9500 6160c
SBS2B5 97 55 6 52 0 5 5 3 30 29 2 46 5 9490 6190SBS286 97 2 6 94 0 5 I 9 4 8 1 47 5 9370 6075SBS287 97 16 6 B9 0 6 1 5 4 10 1 35 5 9400 6175SBS2BB 97 54 7 41 0 6 3 5 10 7 2 39 5 9325 6100SBS289 96 94 5 74 0 9 19 16 79 17 1 98 5 9825 7180SBS290 97 81 3 74 0 5 6 7 5 5 1 30 5 9920 7210SBS291 97 91 4 61 0 1 1 B 96 6 1 53 5 9975 7250SBS292 97 59 7 B3 0 9 10 16 3BO 13 1 7B 5 9B35 7150SBS293 97 46 3 84 0 9 23 32 389 19 7 181 5 9865 7120SBS294 96 77 3 63 6 1 15 20 8445 50 4 151 5 9B35 7150SBS295 97 52 4 46 O B 20 24 103 120 6 400 5 9680 7090SBS297 96 68 4 68 1 9 13 281 lB 3 71 5 9680 7090SBS298 96 17 5 84 0 7 1 4 45 19 2 47 0 9660 7130SBS299 95 17 575 I lB 17 3 17 4 75 5 96BO 7150SBS300 95 71 5 B6 0 6 I 3 I 10 2 17 5 9300 70BOSBS301 97 39 6 34 0 5 3 7 1 9 3 49 5 9275 7150SBS302 97 73 6 05 0 1 1 I 2 8 I 16 10 9260 7220SBS303 97 24 5 84 0 7 5 10 13B 11 I 60 5 9625 7210SBS304 97 6 4 84 0 4 11 7 597 41 5 BI 5 9560 66BOSBS305 97 77 7 43 0 3 1 I 7 8 1 24 5 9525 6680SBS306 97 52 5 91 0 1 6 4 14 13 2 67 5 9610 6500SBS307 97 25 5 45 0 6 1 2 3 7B 1 25 5 96BO 6430SBS308 97 04 478 1 3 19 18 345 24 2 157 10 9650 6400SBS309 97 71 5 03 0 1 6 1 4 13 1 27 10 9610 6450
lSBS310 97 62 5 95 0 4 1 3 67 13 I 50 5 9630 6350S8S311 97 16 5 07 I 18 18 17 22 5 151 5 9600 6410SB8312 96 95 4 72 0 8 12 19 119 24 3 107 5 9925 62208B8313 97 17 5 18 0 6 2 6 53 16 2 91 5 9570 62208B8314 96 74 4 77 I 3 3 23 24 I 27 5 9540 6260SBS316 96 82 5 76 0 8 8 3 36 49 2 152 25 9490 6250S8S317 96 82 6 47 0 7 I I 6 11 1 18 5 9375 61908B8318 97 17 6 68 0 8 11 2 2 17 1 30 5 11050 7550SBS319 97 61 7 28 0 2 11 11 18 16 I 74 5 10970 7510SBS320 97 4B B 32 0 4 7 12 12 14 1 B2 5 10920 7550SBS321 95 36 5 42 1 7 2 59 26 1 25 10 11130 moSBS322 97 57 7 6 0 3 15 13 12 21 1 80 5 11050 7375SBS323 96 05 4 2 1 12 22 2 20 6 107 5 10625 6410SBS324 96 28 5 24 1 203 16 17 29 4 72 5 10080 6470SBS325 97 3 4 92 1 6 288 23 m 99 4 263 15 10630 6550S8S326 96 53 5 95 0 9 18 6 87 23 1 85 5 10700 6560S8S327 96 88 6 27 0 4 75 2 10 11 1 27 5 9l30 5980SBS328 93 6 5 0 8 22 15 24 16 3 114 15 9925 6030SBS329 97 35 5 5 0 6 21 19 Ill 214 4 755 5 9925 60508BS330 97 17 5 48 1 4 1 11 202 45 4 87 10 9855 60BOSBS331 97 14 5 06 0 8 14 8 52 19 2 114 5 9875 6050SBS332 97 49 4 85 0 7 13 10 33 31 2 101 5 9820 6060SBS333 94 09 5 16 1 2 14 3 10 33 2 37 5 9850 6010SBS334 96 69 6 49 0 6 8 1 6 11 1 39 10 9540 5975SBS335 97 6 6 41 0 6 20 1 53 13 I lB 5 9480 5970
nSBS336 97 58 5 44 1 1 9 1 131 22 2 34 5 9480 6075jSBS337 97 66 6 26 0 7 16 3 9 19 1 22 5 9480 6010
SBS338 97 77 6 36 0 4 5 1 8 14 I 19 5 9460 5980SBS339 97 59 5 32 0 5 1 5 36 16 1 64 10 9440 5925S8S340 97 42 6 54 0 4 1 2 29 12 1 42 5 9360 5975SBS341 96 47 6 91 0 7 13 7 3 12 3 39 5 3350 6010SBS342 97 69 5 98 0 1 4 I 5 5 1 14 5 9300 6000SBS343 97 28 6 28 0 4 2 1 10 12 1 20 10 9325 5900SBS344 97 11 6 41 0 5 I 11 2 12 3 9390 900
SAMPLE NO TOml NA K AG AS B CU PB SB ZN AU PPB LItlE OEP
SBS345 97 55 6 24 0 3 1 4 4 10 1 53 5 9510 58908S346 97 48 4 81 0 7 9 14 43 36 5 218 5 9890 5930
8B8347 97 05 4 73 0 7 18 15 86 34 3 231 5 9770 57B5SBS349 96 72 5 52 1 12 1 12 26 2 20 5 9680 5710SBS350 97 42 5 21 0 6 10 24 73 50 5 2B7 5 9650 57BOS86351 97 63 3 89 4 8 37 2 20 456 3 988 20 9625 5700S8S352 96 68 6 0 7 11 1 17 17 1 23 5 9525 5690SBS353 97 37 6 31 0 5 1 14 16 16 1 85 5 9400 5710686354 95 91 663 0 8 5 2 2 15 1 24 5 9325 5720686355 93 54 5 13 1 2 13 10 137 27 1 1 7 5 9615 58206B6356 96 62 5 83 O B 5 15 33 15 1 123 5 9835 72006B6357 93 62 4 99 1 1 11 9 27 19 4 53 5 9750 72906B6358 94 65 5 5 1 1 I 3 167 19 2 43 5 9675 72506B6360 95 67 5 89 0 7 1 3 21 8 1 22 5 9535 73756BS361 97 02 6 79 0 7 6 4 5 4 1 19 5 9500 74758B6362 96 82 6 08 0 9 9 4 14 12 2 23 5 9410 7800SB6363 97 02 4 81 0 9 16 13 15 16 3 84 10 10580 7280SBS364 95 68 5 32 1 5 14 17 13 1 63 5 10550 7320SBS365 97 1 5 62 0 8 17 11 33 16 I 88 5 9900 5650SBS5040 0 6 3 2 42 14 1 30 5
6B65043 1 6 11 5 4 6 1 10 5SBSI243 0 5 12 1 14 24 1 32 206B61267 1 7 II 7 67 104 1 77 10SB61296 2 8 11 243 52 2 61 56BSI315 0 4 5 3 22 22 1 19 5SB6348 7 9 9 I 9142 32 15 615 15 9770 5785
08B61359 0 5 5 2 99 11 1 53 5
I
COHPAIIY HlIlIlOVA IIlC HIll Ell lABS lCP REPORT ACT FW PASE I OF IPROJECT 110 325 705 NEST 15TH ST NORTH VANCOUVER B C VI 112 FILE NO 7 1317
tU1l L L It l l m L EPl g l I PI 7
2 B CU PB SB m AU rPBsas Ioa 4 a 3 i 89 78 3 29 20
Ql 1 6 2 4 142 25 I 36 5L 62 1 5 4 16 13 26 5 79 5
SBS I03 9 2 7 159B 20 4 76 15SBS 104 1 3 21 B 2B 33 I 66 558S 105 8 18 18 105 22 4 79 joSBS IOb 1 0 15 7 12 19 I 4 5
SBS I07 4 B 2 4 7 I 13 5SBS IOB 1 0 11 I 50 22 2 19 30
SBS 109 8 19 21 93 21 6 115 10598 110 4 j i 2i jo 1 29 5SBS lI1 9 B 3 97 19 I 26 10
o
ok ij fi
1
tl11
151st
I
Ifi f
o
II
t
v 705 NEST 151H SI NORTH VANCOUVER a c V1H lT2 FILE NO 7 1311I nlKE SRAV 604 980 5814 OR 1604 988 4524 TYPE ROCK SEOCHE DAIE SEPT 22 1987
R t
iL l l l50S lOB 16 37 103 2 00 33 3 53 67 15 3 BS 64 29 OJ 44 019 95 75
lS 101 15 74 103 1 39 4 68 3 21 13 14 3 81 6b 06 01 46 014 96 41
102 16 87 075 2 11 7 59 1 89 1 81 13 4 52 59 74 02 75 012 95 52
585 103 13 26 125 01 5 98 3 58 75 14 25 73 42 01 14 005 97 64
SBS I04 16 40 011 3 53 1 12 2 94 3 16 21 2 76 59 19 01 59 012 9b 06
SBS I05 16 BI 131 1 22 6 19 3 32 3 09 11 2 BI 61 5B 01 B7 016 96 23
saS I06 15 30 010 2 80 4 99 2 90 2 00 20 3 24 64 46 01 47 015 96 45
SBS t07 t4 91 079 1 30 1 19 2 50 51 06 4 81 70 44 01 26 021 96 75
SBS IOB 14 IB 083 2 39 3 28 3 04 1 13 24 3 18 61 92 01 29 018 95 16
S8S 109 16 55 101 16 7 76 3 24 3 59 18 1 77 62 89 01 75 016 97 61
sBs iio io os i6i ii i 9i iBs 66 oa 3 s3 6i 97 oi i3 oia 97 60S8S 111 14 68 103 2 49 4 45 3 16 15 11 3 58 65 56 02 36 015 95 32
IN EN lABS ICP REPORT IACI f26J PABE I Of J
f O
i f1 W
14 t
951
od
