dd rpt 11 castlewood lake area...are recorded on the north wind map. an all-weather road connects...
TRANSCRIPT
42EI3ICM65 11 CASTLEWOOD LAKEO1O
Diamond Drilling
Area of CASTLEWOOD LAKE Report NQ 11
Work performed by: New Bidlamaque Gold Mines Ltd.
Claim NQ
TB.94954
TB 94938
'TB 94960
TB 97243
t NQ
l
6
2
3
5
7
Footage
351'
337'
401'
351'
351'
288'
Date
Feb/60
Mar/60
Mar/60
Mar/60
Mar/60
Mar/60
Note
(l)
(D
(D
(l)
(D
(l)
Notes: (i) formerly Martin Lake #17
AWL 005( 7- 69) rev. 9 72
DRILL ItfG PROGKAJffe
ONA**N LAK& MINIUG CLAIMS
BlOLAMAQUi. GOU) HINt.S LIMIT 11)
t s ma g c m i
L eke
Onaman L a it e
\EVV BIDuAMAQUE GOLD M'NES LTD
^ C C A " l O N
NEW BIDLAMAQUE GOLD MINES LIMITEDPORT ARTHUR MINING DIVISION ,
SOUTH ONAMAN AREA
ONTARIO
s : - .. E. N c - - r:- v . i s DECEMBFK, 953
DRILLING PKOGRAtffe REPORT
ONAMAN LAIU MINING CLAIMS
BULAMAQUt GOLD MttifcS LlMiTfcD
Summary
A drilling programme consisting of six holes
(I, 2, 3, 5, 6, 7) for a total footage of 2079.0 was
completed in March 1^0 on the 42 claim group of New
Bidlamaque Gold Mines Limited in the Onaman Lake area
of Ontario.
The holes were directed into a strong linear
conductive and aa*oetic ^one located in a previous
geophysical aurvey and were distributed over a 4,000
Coot length of this *one.
Sulphides encountered consisted principally
of pyrite and pyrrhotite with very minor amounts of
chalcopyrite and sphalerite and varied in core length
iron less than ten feet in a mineralised section to 165
feet (hole #2). In content, the sulphides ranged from
minor percentage amounts to massive (mainly pyrite).
- 2 -
Associated with eh* sulphides in places, are
bands of lean iron formation not exceeding four feet in
core length.
Samples for assay were selected after logging
and were run for gold, silver, copper* zinc, nickel and
cobalt without significant results.
Further work recommended should consist of
detailed geological examination of old trenches and pits
in order to re-sample the showings, having regard to
previous reports on the property, and to establish the
relationship of these showings to the drilled area.
Property Location and Access
The property consists of 42 contiguous
unpatented and unsurveyed mining claims in the Onaman
Lake area of Ontario, Port Arthur .Hining Division.
They are numbered as follows:
l.B. 97247 - 49 incl. 3I.E. 97242 - 44 incl. 3I.E. 94936 - 71 incl. 36
42
- 3 -
The group lies 3fc miles west of Onaman Lake
which ia 35 miles north - west of Geraldton, Ontario,
the east boundary of the nipigon Provincial Forest
coincides with the east boundary of the claims and they
are recorded on the North Wind map.
An all-weather road connects Ne^ah, on the
BeardBore - Longlac highway with Auden, a lumbering town
on the Canadian national Railway due north. At a point
approximately 30 miles north on this road and almost due
west of the claims, a bush road runs east nine miles and
connects with the claim group by a tractor trail. Ibis
road may be used by truck in summer acxi snowmobile or
tractor in the winter.
Best meaus of access is by bush plane from
Geraldton to a small lake fc mile north of the claim group,
History
First report of the showing ia contained in th*
Ontario Department of Mines Annual Report, Volume XL,
Part 4, by L. F. Kindle and the location is indicated on
the accompanying nap MOP.
- 4 -
Two trenched areas axe Mentioned one north of the other
and narrow quartz veins were encountered carrying pyric*,
chalcopyrite, sphalerite and galena. A parallel vein
6 feet vide 600 feet vest is poorly mineralised. The
locations of these showings are not identifiable.
Channel sampling by K. Springer in June, 1930
showed low values in gold.
The showing is also indicated on Map #47H which
accompanies O.D.M. Report, Volume XLVII. Part d, but it
i* not described in the report.
A report by G. W. Fancy dated September 1st,
1959 is available and describes a visit made to the
property by him on August 24th, 1959.
Regional Geology
The most up-to-date geological map of the axea
Is *47H (1938) by W. W. Moorhouse.
A continuous belt of Keewatin volcanics and
sediments joins two larger areas of similar rocks that
occur in the Sturgeon River area and in the area around
Nakina and north.
J '
In the region of the claim group, numerous exposures show
the belt to have a somewhat south - easterly trend.
Remnant lemiskaming sediments occur within this greenstone
belt and numerous bosses of Algoma granites and diorite*
are mapped. Ih* belt is about twenty miles wide and
bounded by Lake Nipigon on the west end a large granitic
mass near Lake Onaman to the east.
Local Geology
As indicated on ria*) #47H, the western claims in
the group are underlain by itimiskaming conglomerate, the
aain central claims by Keewatin volcanics and the east line
of claims by Algoma granite. The strike of rocks and
contacts is almost due north, although Fancy reports
observed strikes of south 400 cast with dips near vertical.
The same attitude is noted for three out of the lour
showings examined by him which is thus at variance with
the sulphioe *one as defined by geophysical survey and
subsequent drilling. He believes an en echelon vein
fracture system occurs.
Two of the drill holes terminated in biotite
granite and all intersected andesite and chloritic schist
derived from it, with variable amounts of associated sulphide*,
- 6 -
Core lineations indicate dip to be 400 - iO0 to the weat.
The property has not been napped geologically
but it appears that the contact of the granite with the
overlying andesite schist complex also dips approximately
A30 to the weat, and it is probable that this intrusive
contact was the locua of subsequent inovements. The origin
of the sulphides aw y be due to nore basic phases of the
intrusive at depth as these phases are prevalent both
within and apart from the granite stocks in the area.
Geophysical Survey
A complete coverage electromagnetic survey was
run over 36 claims of the property late in 1959. A strong
linear conductive feature was located with a north - i,outh
attitude in the middle of the claim group and this feature
was then covered by a magnetometer survey. A report in
detail on this survey by T. k. Gledhill, geophysicist, i*
available.
The 4one appear*, to the south, on lint 36^ and
is continuous, to the north, onto claim i.B. *7243, beyond
the limits of th* survey.
- 7 -
The locations of the A, B, C and D showings described by
Fancy are indicated on the accompanying drilling map.
Holes 4 and 5 were spotted to b*s more or less coincident
with showings E and C. Ihe remainder of a total of five
holes were designed to test the main feature at best
indicated positions.
A second parallel magnetic ione lies between
lines 64N and 76!* and was not considered for testing by
drilling.
Drilling Results
Accompanying this report are logs and assays,
sections of individual holes and a surface plan inter
polation of the rock types intersected, as well as a
general location sketch of the drill sites.
The results of each hole are discussed below.
Hole 01
Drilled to depth of 351.0 feet. Casing -34.0
feet. Chlorite schist was encountered to depth of 107.6
feet. From 107.6 to 210.3 is a mineralized section of
chlorite schist.
- 8 -
Sulphides consist of pyrite and pyrrhotite in ratio of
60 - 40, occurring as numerous stringers, veinlets and
disconnected massive sections. Chalcopyrite is present
in minute amounts - one 5 foot sample gave 0.181 copper.
Quartz and carbonate are predominate as gangue minerals
in the chlorite schist host. The same rock type with
andesitic bands is found, increasingly contorted, to a
core depth of 249.5, where porphyritic quartz biotite
granite was entered.
Hole *2
Depth - 401.0 feet. Casing -9.0 feet.
Intercalated andesite and chlorite schist was
intersected throughout the hole containing a mineralized
section from 134.0 to 300.5 where sulphides (pyrite and
pyrrhotite) range from 5X to massive in volume. Pyrite
is more abundant than pyrrhotite. Very minor blebs of
chalcopyrite occur at random in this section and several
small sections of iron formations are present. Considerable
silification and/or introduction of quartz veins is noted.
Lineation varies from 60O - 8O0 to core. The
hole ended in carbonatized andesite.
- y -
Hole
Dfc^th - 331.0. Casing - 3.0 feet.
Intercalateu andesite and chlorite schist were inter*
sected to the bottom oi the hole. A short (169.2 - 177.1)
section occur* with 13* pyrite and ainor sphalerite, t h*
zinc percent is 0.3o across this section, with negligible
values in the other metal*. Considerable quartz and
carbonate is ^resent, one section 206.3 - 22^.0 being
almost entirely carbonatizad.
Hole f 3
ite^th 331.0. Casing - 6.0 feet.
i hi s hole was located to intersect a conductor
on the ^resumed position of shoving C described by Fancy.
Again interbanued andesite, chloritic schist ana
quartz - carbonate veins fora the gangue tainerals through-
out the hole, 'ihe anomaly can probably be attributed to
the narrow (63.3 - 6^.6) band of 10^ pyrite and pyrrhotite
at this horizon, ^o significant quantities of ore
sulphides were noted and no assays were taken.
- 10 -
Hole *6
Depth - 337.0. Casing -5.0 f**t.
The principal rock type encountered is chlorite
schist, with lesser amounts of identifiable andesite,
much silicified and carbonatized.
A mineralized section occurs from 176.7 to 265.5
containing pyrite and pyrrhotite in amounts from 2TL to
massive. Only minor blebs of chalcopyrite and sphalerite
were observed in the core. In all cases assays were
negligible. Iron formation is found in small bands
associated with the sulphides.
Hole *7
Depth - 288.0. Casing -41.0 feet.
This hole is the farthest one north, drilled
on a conductor cross-over obtained on strike beyond the
scope of the required survey, on ground later acquired by
the company.
Rock types are mainly chloritic schist, with
occasional bands of andesite and iron formation and the
hole entered biotite granite at 257.0 feet.
- 11 -
it la difficult to account foe the well
established conductor here in term* of sulphide content
which does not exceed 3*i (pyrite). Undoubtedly the chlorite
schist and iron toraation have both contributed to the
anomaly.
Keaarks
With the exception of Hole 17 ample sulphides
were intersected in the hole* to account for the conductor
magnetic features.
The results to be expected obviously do not
correspond to the assays from surface sampling, although
only hole #i apparently is located on one of the shoving*
reported in Fancy's report.
it MOBt be mentioned, however, that snow
conditions at the time of the geophysical survey
precluded checking t hoe showings in relation to the
conductors obtained.
Moreover, the locations of these showings,
having been referred to claim posts difficult to find,
cannot be relied upon.
- 12 -
A ground geological examination should therefore
be conducted over these showings for purposes of re-
sanpling and for establishing the location and relationship
to the drilled zone.
Ree ndations
It is therefore recommended that
(1) A geological property examination be aade for purposes
of sampling and locating the showings with respect
to the survey grid.
(2) The claims be held in good standing by application
of the assessment credits obtainable from the
geophysical survey and drilling progra:
Respectfully submitted,
SULMAC EXPLORATION SERVICES LIMITED
Toronto, Ontario.
April l, 1960
D. P. Robertson, B.A., P. Eng,
/Xc :~^-A
OF QUALIFICATION
I, DOnAU) ?t,1LS. KOBtKTSON, do hereby certify
that:
1. I aa employed as Chief Geologist by oulasc Exploration Services Limited, I or on to, at Suite 904, 30 Richmond Street West.
2. l aa a graduate of Queens University (1940) having been granted the degree of Honours B.A. in Geology.
3. l aa a anajher of the Association of Professional engineers of the Province of Ontario and a Fellow of the Geological Association of Canada.
4. Sulmac exploration Services Lisa ted conducted thegeophysical and drilling programmes referred to herein.
b. l have no interest, direct or indirect, in the properties or securities of New Bidlimaque Gold Mines Limited nor do l expect to receive any such interest whatsoever.
6. My information is based on Government publications, visits to the property, personal knowledge of the area and on ay duties as Supervisor.
Dated this first day of April, 1960.
i). F. Robertson, B.A., r. ^n
APPENDIX i
ASSESSMENT CREDITS
The following assessment credits are applicable
LO the groups of claims as a result of the drilling
programme.
Geophysical Survey Credits - Previously accepted on the
following basis:
36 claims
I.B. 94936 - 71
Days credits/claim - 40
fi"•4
04
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Group 3
15 claims
T.B. 97242 - 44 3T.B. 97247 -49 3f.B. 94954 - 59 5T.B. 94961 -62 2T.B. 94J65 l
li
Drill holes #1 and *6 on claim T.B. 94954 AXT core Footage 351 -t- 337 - 683
Drill hole #7 on claim T.B. 97243AXT core Footage - 233
Total 976
Days credits/claim * 976 a 6515
Drilled by Canadian Longyear Company UnitedDrawer 330 North Bay, OntarioDrilled February 25 - March 19, 1960 ( 6 holes).
59M!
ASSESSMENTGROUP
No lASSESSMENT
GROUPNo3
ASSESSMENT
GROUPNo2
PROPERTY SKETCH
NEW BIDLAMAQUE GOLD MINES LIPORT ARTHUR MINING DIVISION
SOUTH ONAMAN AREA
ONTARIOScale l" - 2640' Jan. I960
CHLORITE SCHIST
MINERALIZED ZONE
CHLORITE SCHIST
for assays
END OF HOLE
NEW PIDLAMAQJliD.D,H #1
SE-J1ION ,-6 * CON j.RG. GRID tiAST SCALt L" - 50'
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schist incluaioi
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of irregular atr.ii gy masses pyrite and minor pyrrhotite. Pyrite aaaaive t iae grail *d W^HFtirt^A*
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Schistosity 70*90*.
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to d*ri^ 1^*;
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— - —
-228.5
T3270 ~-243.5
2*9 !T—
—
—
FOR
MA
TION
SA
MP
LE
NO
.
Ch lor i ta achiat abundaolw
hit* carbonate.•ea t car ad grains pyritajl
schiibacostts proftaasivsly ww
ith dapth. 216-217.5xo
likaf—Br
sppasrs frajBMrotal^craaJKY .
.jfiUtrtx.aM
ktt jip 3Jft of cock
f tom 770-5 to 2)1.
Irregular pate ha a of pyiritast 226.3. dull vhita qufrrtaw
ith cy pssvf carbonata andut m
f chloritic schistiocluaiooa fro* 228.5 to
A229.7, ninor pyrita in quarts A
ndaaita fioa gralnad.•assiva* carrying abundcsrboasta and scsttaradftraina of pyrita.
Cut
Is t s whits c*f^M
)ostastrin
fsrs. C
ontact wit
chlo
ritic achiat grada-tioosl ovar 2*.C
hloritic achist, cosrs ajrsinad w
ith abundantcarbooata. F
oliation tt 60-iO
Oto cora axis but
locslly coot or t ad.S
chistosity bacosws
prograssivaly strongarw
itjr dapth.
t- int
•X -
i
LE
NniH
FT.
Sss^la
tosityW
Q1A
6302
6)63
6304 ,
6303 J
630i6307
r630T 6309 6310 6311f A
* X
——
63136314 6513
— —
-
l
AN
ALY
SIS
*
Dapth
Fast103-
A08-
1 OB-113113-
•/o
Gold
Chit.
Nil
Mil
.118 lu
llil8
?ul H41
123-133 133-142 U
f- 151 15S-16I ia-lT
3
173- 18C 180-192195^101201-206206-211 2H
-2MiT--
•-
Mil
Nil
Mil
Mil
Sil
Nil
Mil
LM
ilM
il "
Nil
Nil- —
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Sillar
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Ml
BIL
Mil
NJJl
1*04,,0.020.03 0.03 0.02
0.020.030,07M
il
- -
-- —
-
--
LENG
TH
FE
ET
Copparl
0.04
J). 06
0,03^ MOJM
0*.02 0.030.02 0.030.02 0.040.050.18*0^14 0.02---——
PRO
GR
ESSIVE TO
TALS
FEET X PER C
ENT
Zinc1
Nona
Nona
-Jrs^a M
oo* M
opa^JIO
ftSL
0.02M
ona NonaM
OM
Mona
Nona
Nona
Nona
Nona
Nickal
1
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. Ww
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ons- ..
r.lk!M
-^"^^•^**
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Cobalt
IT .
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0,01.H
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racaNona ^
Kona T rae a
woaa ...
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Nona Iraca
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v^^V
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..
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PR
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ER
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SU
LM
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SA
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LIN
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LE
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PT
Ho
Grid
351. 0 'ANG
LE -...44.— STRIKE
SH
EE
T
NO
.—1
.
CO
-OR
DIN
AT
ES
ELEVATION
31+OO
E
L3CP
TH
F
EE
T
H*** ?tafcr-i*
307.0
302. O^L
l o t-i t*.
LV
*
prvavnt at *0-TO^ to
axi*. i:;uart!t pturaocryi
"locally-appaar to ba ax a tv
t fetter** grains of pyrTla oo**rv*d. C rani U
, bio
tlta, m
asaive.wTth por pl*y r i t ic gr aa i t a gradatiooal over l*,
aaita, porphyritic u
artt-biotit*.W
AASiva qua^te w
ith pink talds- .3-322*0
Dull
vnoN
ph
yritic
^
uai
m
v
'1
arp . **^i1 i **a g
•v fittarff
ph*•j
H**** —
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M 1
• l*fl^
* ^
w
iBM
^^t J
A^
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va ac lava^p
M
) rock v
aria
j
oil a
t ion vtMti
SA
MP
LE
NO
.
Ci,
rainedno—to
—
aaa-ii^
r it.^.
xW
trvn
r
la--
LF
NT
iTH
f T.
f1 l
AN
AL
YS
IS
1,'k
--
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LE
NG
TH
FEE
T
PR
OG
RE
SS
IVE
TOTA
LSFE
ET X
PER
CE
NTJ
white
ODCJaiiai
MAO. PROFILE
CHLORITE SCHIST
MINERALIZED ZONE
CHLORITE SCHIST
END OF HOLE
NciWD. D.
-*-5C'N, 4^ * 5U'E /RG. GR ID S
SOALt i 1
PR
OP
ER
"*"
HO
LE
N
O.
SU
LM
AC
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XP
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SE
RV
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S
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in*.
DE
PT
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LE
SA
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LIN
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RE
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E
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VA
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N.
SH
EE
T
NO
.
ST
RIK
EC
O-O
RD
INA
TE
S89+30N
46+SOtt
DE
PT
H
FE
ET
FO
RM
AT
ION
SA
MP
LE
NO
.
LE
NG
TH
FT
.
AN
ALY
SIS
LE
NG
TH
FtE
T
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X P
ER
C
EN
T
Caaiof
3ft.OA
M3E
SIT.&
,_ __
•aa* "abundant ea_
and acattarad narrow carboaat* atrlngara
J* faw ac* rita,
^ ^
SCHIST, Jina.grainad fait to ^
foliation^at^TO
-SJP to cora.
Abundant ^
carbonata - law acattaj
laaay patch** of o^i
T32.
_
_
^
Scattai cubaa o
Fp
/rlta. AKOK8IIE,
fina gralnad,•aaaiva locally waak.•chlatpalty.
70
P-tO
C
OI
* trfro* vaak to
i Abundant
quart^aod
134.0"Qr, dark gray
daaaa with chloritic andbam
ia rut by narrow quatta * _
^
carbooata atrlngaraSI pyrtta aa IrraguU
rvainlat* and
-4
-t"
1-4
PR
OP
ER
-"
HO
LE
N
O.
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
Bidlaa*4ua cold MID*.
SAM
PLIN
G
RE
CO
RD
2
DE
PT
H
401*
AN
GL
E
*45
O
ST
RIK
E8
45
Og
SH
EE
T
Mn
DE
PT
H
FLE
T
T3
4.T
131. i
142.d
FO
RM
AT
ION
aloft* wa*k fracturaaand acalatoaa planaa. C
halcopyrite aa _
_
diaaaaAnatad gralna
and floa aigjragataa ob- aanrad at 133.0 CHLORITIC SCHIST, w
ith 35 - 401 diaaaaioatad ajraiaa and Irra^ular baoda of pyrita chlorita duck.UON
baodad. of
wall
fina BMigaatita and
ricti banda ofquartz ygita
SAMPLE
NO.
uartg, dark gf•y,
5*101 irregular band* of pyrlta
CHLORITIC SCHIST, 4at)c
Eraan ahiatoalty
to cora. 51 diaaaainata t
Pjrtlta IKON PIFO
MAIIOM, wall
baodad at 4(X* to core
- lo p lac aa wall
c OP t or t a l. 31 narrow banda
of pyri :aand
pyrrbotita. Quart*
,ia
dark tray and daaae.
LE
NG
TH
FT
.
AN
AL
YS
IS
V,
' ~~ ——
—T"
LE
NG
TH
FE
ET
IT
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X
PE
R
CE
NT-t-
•4-4...... —
4. -t-
SU
LM
AC
E
XP
LO
RA
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N
SE
RV
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S
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D
PROPER- a** Bldlaaw
qua Cold ttlnaa
SA
MP
LIN
G
RE
CO
RD
2__
__
. D
EP
TH
401*
AN
GL
E J
!**0._
_ S
TR
IKE
S
45
OE
E
LE
VA
TIO
N —
——
SH
EE
T
NO
.
HO
LE
N
O.
^C
O-O
RD
INA
TE
S89+50*
46*506
•HIM
of pyrlta and. pyrrhotite.
Pyrite t
pyjccfaotit*.J,a lil Q
uart*, dark tray, with
li diaaaadnatad ar* of
pyrrhotite QUULTZ,
FO
RM
AT
ION
SA
MP
LE
LE
NG
TH
FT
.
CHLCm
niC SCHIST,
darkw
ith 3Xirragular
35i ch
ar1tle ach
iatkock vall-baD
dad at A
0 cora. 10-201 irrag
baodAof
- iO;20
fan narrow banda of •aynatltaIEOM
FORMATION( narrow
- 174
•inor pyrite iod
banda of pyrlta andrhotitaSCHIST,
vi tlh 3C lfioa pyrita and ninor
—
pyrrbotlta. A faw
—
acattarad araina or cluatara of chocolate
AN
AL
YS
IS
*y.
LE
NG
TH
FEE
T
l"
t
t
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X P
ER
C
EN
T
.__
j
—_____
-i-
.j__
_.
__.
PR
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ER
TV(
HO
LE
N
O. .
SU
LM
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XP
LO
RA
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N
SE
RV
ICE
S
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D
Bidlaa*qu* Cola rfjnas
SA
MP
LIN
G
RE
CO
RD
DE
PT
H
401*
AN
GL
E
"45
** S
TR
IKE
S4
5O
S
EL
EV
AT
ION
——
SH
EE
T
NO
.
DE
PT
H
FE
ET
15*. 0
-111*0-
171.4
215.0
FOR
MA
TION
HUMITE
liftht to daik
narrow stringers of
pyrite sad aln
or
SA
MP
LE
NO
.
pyrrhotite, ainor chloriticschist inclusion
1M
M2M
KT1C 110N
FORMATION
with arch contorted fin*
gray banda of magnetite
grains and irregularblabs of pyrite andpyrrhotite up to IX•inor chloritic schist.cixm
rric scniri, with l to z.quarts, pjrrita and pyrrhotite irregular banda and diaaaaU
natadgrains laaa than 31 topyrite: pyrrhotite,
7:1174.0 - 174.5Q
uarts drilled whita to
gray with 51 y e lo le t s
of pyrite and pyrrbotitaa fracture fillin
g.
UUSJTI&, sMditm
to oarkgray,
101 carbonatesulphides 201 avaragaIrragular banda anddiaaaeinatad bands ofpyrite and pyrrhotiteR
atio pyrite: p/rrb
otlt
3: l. acattaraa suouta
b lobe ol chalcopyrite w
51
ii,tb
LE
NG
TH
FT.
-.-—.
AN
ALY
SIS
*
(-
•A*--
LE
NG
TH
FE
ET
PRO
GR
ESSIV
E TO
TALS
FEET X PER C
ENT
- — -—
-- ---- -
r -
-
- - -----
230.5
240.t
242.5
249.3
233.5
l f
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
uev *idlaa*que Cold .i!**. S
AM
PL
ING
R
EC
OR
DSH
EE
T
NO
.
o.D
EP
TH
TO
RM
AT
ION
AN
GLE
"45
__
_ ST
RIK
E.
SA
MP
LL
NO
.
with the pyrrhotite
202.0 - 204.5 l dark gray quart* Pyrrhotite and pyrite auiphldaa average 601•ut varying 3 to 901
J yrita: pyrrhotite. ;2.
Liilit gray quart*
217.3 - 211.3. HatrU
of aaction la light gra;' quart* and carbonate SULTUDftS avaraga 351 hut varying 3 to 731 pyrite: pyrrhotite,
1:2. Natrlm
601 light gray ".
quarts aoa* daoaa gray•actions.
Hiaor chloritic
aehiat iacluaiooa. gULPTUOKS 601 pyrite: pyrrhotite,
3:1 ajatrixof ligh
t gray quarts C
MLO
iniC SC
BliT, wall
foliated at tO0 to coca C
ontain* course crystal of pyrite diaaavlnatad 151 quart* and creaejy carhoaata In hand*. QUM
tT-i. dull white to
gray Ml laaa than 31
itlgiaatnateil •r*^•tringer* of pyrite,
jp/xrhotlte ratio 6:1
l
chlocitic aehiat incluafLon251.S - 232.4
._ _
_.
. l
i "l
ELE
VA
TIO
N.
FT
.
AN
AL
YS
ISLLN
GT
M
FEET
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X
PE
R
CE
NT
i T
i _ _
_
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
PR
OP
ER
T
HO
LE
N
O.
** iidlaaaqu* Cold Xinaa
DE
PT
H401'
AN
GLE
SA
MP
LIN
G
RE
CO
RD
-450
SH
EE
T
NO
.
ST
RIK
E
DE
PT
H
FE
ET
FO
RM
AT
ION
PR
OG
RE
SS
IVE
TO
TA
LS
259.5SCHIST,_ _
foliation •t~5Cp to cor Laaa carbonate and
than pravlou***C
tion
. V
jft.t* and pyrtt*
291.5to
ll vtd.tr to w
Uk calorT
t*
j)yrrfcotrt* F
ynrtotit* occur* a*
29172
t, pyrita aa caaraar grain*, C
aalcopyrtt* la admit*
quantity *t 2i(T.5.
Lot* carbon*t* in afrTagara and fractura*.
hooayyalloif colour . j.inoatloi at 70~to cor*,
30075QUUETZ,
HttlaT
pyrrfcotitaT
iaaTll aaaatva **ctloo*Ita~
——
—
—of pyriti at 219TZ
TO
a tocoaraa cB
ilcopyrlt*, ctibtc pyrita and w
tnor
PR
OP
EF
v
HO
LE
N
O.
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
Haw Bidlaa*qua Cold Hine.
SA
MP
LIN
G
RE
CO
RD
o2
DE
PT
H
401*
AN
GL
E _
_^
45_ S
TR
IKE
S
45O
B
EL
EV
AT
ION
-——
SH
EE
T
NO
.
a*
.^C
O-O
RD
INA
TE
S
^89+SO
K 46+30K
DE
PT
H
FE
ET
329.0
360.0
379. 5
A01.0
FOR
MA
TION
CHLORITE SCHIST, w
allfoliated at 63O to car*dH
ltaiOA
1
^1 flU
artScarbonate la alnute w
hibaoda.
LlttU
to no•ulphldaa.
Fairly
uaifocai linaatioa.CH
LOtniC SCHIST.
cootortad follafcioo,li t t la to ao •ulphidaa.CHLORITE SCH
IST.uniform
acfciatoaity.(30 to cor*.
Noaulphidaa.
Soaia barronquarts aactiooa
iBaaJ.c volcanic^ probablj aodaaita but *uchcajfboojjti**4.
ScfttarJ
narrow quarts stringer t j
Faintly dafinad linaatiat 7 O0 to cora
1
- fisp or HOU -D
rillad by - Canadiao J
March 1 -4
. 19*0
HC
UlB
Bo' -
t. B.
94938
Loiftad by - D. Kurd
D. t. Robar
SAM
PLE
.
NO
.
- ' —
——
-;
——
—
L. ^
UK
xikyaar
•00
LE
NC
.TM
FT.
iaayi*M
O.
6316A
631?
631JL
631i
63206321
63226321
61246325
6326
iti)epthft tt t133-143^IM
-133
r!53-163Ii3
- .n
r!73 ^
O73-
^183U
S-193
. 193* 1QX
i203-213
.113-i 2?3^23-
H21T233-241-
AN
ALY
SIS
•k
Cold
^?t.
•il
Kll
HU
MIL
Hil
fill
Nil
auMil-
-Jill
mi
h
'k
Silver
Oca.
0.02
Hil
Q, 02
Jill
0,52
l*il
Traca
•f&l
0*U2[ M
il ^
o.ol
LE
NG
TH
FE
ET
Copper1
0.04^0.03
.0.03
0.04
[O..M.0.06
O.iJl
i), 04 H
0.04
0.05
0.04
.. ....
PROCFE
Zinc1
wontM
ooa
Mooa
ffonaT ras a0.08
0.04
Trace
Nona
HQoa,0.04
SRESSIV
E TOT
ET X PER C
EN
Nicfcfl
1
MOM
Nona
Scoa
Jkma
-
Moaa
Hooa
.Jtoot-
Mono
Moo*
Mooa , .
Nona ^
ALS
TCobalt^j
IkM*
Booa
Hone
tflfMvaB
Tract
Xrac*
NOB*
MOMM
OfM
MOD*
Hone
O
O
PR
OP
EP
~V
HO
LE
N
O.
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
SA
MP
LIN
G
RE
CO
RD
DEPTH 331*0* ANGLE * 43O
STRIKE J|*j
SHE
ET
N
O.
^ **^7^^ w
___
•cSiat, foil*-
,grain* pfrltut, M
inor l*o*L
*Ait* ^u*rt* a
HJM
to •a
ialy
*t c favof
Chlocicc Schi*t.
at•t* a f aw *cattara4
pyrlt*,
IJJM
to U
*4iMH
fin* to pttdiua
••ction.
Chloric*w
ith
CO
-OR
DIN
AT
ES
L72+VOH
32130E
MG
TH
LE
T
—---
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X
PE
R
CE
NT
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
PRO
PER
TY
fedV
lidl
HO
LE
N
O.
SA
MP
LIN
G
RE
CO
RD
laat
3
DE
PT
H 3
51
.0*
AN
GL
E -
45
O
ST
RIK
E (G
rid)
EL
EV
AT
ION
.
SH
EE
T
NO
.
L72+OON CO
-OR
DIN
AT
E^
^
throujhou
of cor*. Minor
ray quarto with teat
natMOE
PJilt*
ilarita I; 10
of *ina vita choaolata
tphalarltatn
latt of chalcopyrite t iu
:2:ly.
ilU fla*rto •odlva
alood. Saattorod
lorlta •chiat scat ca ita last tbaa li.
_ ty
aa t sty t I:
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
PROPERTY Ne*
HO
LE
N
O.
DE
PT
HjL*L-.
AN
GLE
*
SA
MP
LIN
G
RE
CO
RD
0 Bft*t
ELE
VA
TIO
NC
OL72+OOK
SH
EE
T
O-O
RD
INA
TE
S
DE
PT
H
KLE
TF
OR
MA
TIO
N
229.0w
ith scattered
schistchlorite
givingrock
somewhat mottled appearance.
Slightlinea t ion
tu iock wjLth
dark, mafic grains orient*
at 706 to core
axis.fey narrow
(l-2toa) pyriu
trinketa. Andetite
fine to
grained oaasive. contact,
dhenti Atit*
1
SA
MP
LE
NO
.
4
LC
NG
TI1
TT
.
|j
V,
-J...i
AN
ALY
SIS
ft-::.i.
'i
-——
-
LE
NG
TH
FE
ET
-
-
,
PR
OG
RE
SS
IVE
TO
TA
LS
FE
ET
X
PE
R
CE
NT
with carbonate sradatlonf l
owe 2'i aiaor tchiatoM
i
Utt UM
D IX M before.
chlorite achUt w
ith 40V
vhlce to gn
j quartz and ; *l*or pink feldspar
itr*cul*r Mi
with
of pyritegrains of chalcopyrite
, aaaociated with the
li pyrite quart* appeare to
narrow irregu a MMli angle e
he a vain.At
cfialcopyrlte chlorite achiat at contact.
1.
ar
PR
OP
ER
T
HO
LE
N
O.
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
M*v B
idlaMqtie G
old ifioei S
AM
PLIN
G
RE
CO
RD
JL
__
__
DE
PT
H 3
51
.0*
AN
GL
E J
"*5C
_
ST
RIK
E C
*le
E
LE
VA
TIO
N_
__
SH
EE
T
NO
..
CO
-OR
DIN
AT
ES
L72-MM
B 52+50C
DF^TTH
FO
RM
AT
ION
331.0 A
adeaite l IM tra
ined
•eaaive. S
catteredgraiae m
d narrow (1*0)
•triag*r0
of p
yrite.
lode it loca
lly eehiatoi351.0
lad e
f hole.
Mot**:—. . ^
— -
-- — --
Loffod by Don Hard
Jack Kirk
*tarto
4 10 M
ardi oO^ Liaiafaod 11 H
ardi 60lo
taatAJlx
ill coBtrofitort;
Ctfta
g raw
Mrod.
^D
rilled
on C
laim # T
.B.
9A960
SA
MP
LE
NO
.
1.
-
1
r -
-
- — h
- - i
.-
\- - i
1 F
NG
TH
FT
Soapli
Mo.
iJ112a..
^ 6333
- -- ------ i.
-
AN
ALY
SIS
'k
Depth
ffffff
169-173
255-27*t
••/iGold
Ova.
-jii1
Mil
i 4 -
; •••-;;
i
•i
Silve
r0**.0*.(H
-
0.07
1
LE
NG
TH
FE
ET
Copper
Q. C*
0.10
.j.-!:---- -r.ii)
- -----.
M l"it .il 1i
-
l
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X
PE
R
CE
NT
Zinc
0.3*
0.03
nicke
l
•ooe
Hone
i . . ... .—
it 1
,. i
...
Cobalt
HOMO
Mono
—
—
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
PROPERTY NW
Bidlaaaqu* C
old Minaa
SA
MP
LIN
G
RE
CO
RD
SH
EE
T
NO
.
HO
LE
N
O.
DE
PT
H
33
7.0
A
NG
LE
"
^
ST
RIK
E
Grid
E
LE
VA
TIO
NC
O-O
RD
INA
TE
SL92+OOH
49*501
DE
PT
H
KL
ET
Andes, x Le f ip* grained
Chloritic sch
ist foliation
at 700"line ftc&
iiicd acattarad
- -lino gf a i nod pyrita
FO
RM
AT
ION
-ccoaay ^uartat and
— tttd
-of
.——
——
——
- —
——
——
- -.
-- - --.^
-|4,.
^ i Ile*
by Lengyaar bed.; "~"
Hoi th R
ay, Ctiit.
Logged byfrun Kurd
—
J. B.
Started Kareh 5/607700
Drilled
on Claia # T
.B.
54954
Ulo o4 O lO
UJo o*K) 10
OVERBURDENCONDUCTOR
ANDESITE
CHLORITE SCHIST
ANDESITE
CHLORITE SCHIST
IRON FORMATION, 30Xo PYRITE CHLORITE SCHIST
IRON FORMATION, 3*fc PYRITE
CHLORITE SCHIST
ORANITE
END OF HOLE
NEW RIDLAMAQUED. D. l:. #7
SECTION 104 * OON r RG. GRID EAST SCALE l -50'
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
PROPERTY Nav BidlM
MqiM
Cold Kin.*
SAM
PLIN
G
RE
CO
RD
SH
EE
T
NO
.
HO
LE
N
O.
DE
PT
H2
88
AN
GLE
ST
RIK
E
iaat
EL
EV
AT
ION
CO
-OR
DIN
AT
ES
^104*00 M
&+00&
DE
PT
H
FE
ET
~4T.no
FO
RM
AT
ION
Collar
_AMDESITg,
aa** grained.
Locally waakl . Minor *hita
.rHLOKITlC SCHIST,
to wMk foliation
70 * SO0 to M
loor pyrtta. _ Scatter
of whit* carbon*
q8 uarts,8
raw oiirr mr
carbonate atriogara, ——
~
SCHIST,Scbiatoaity atroag atcato
aty
0^ - S
Ortto cor a axia.
_ narrow
and lanaa* of white qua11* with minor carbonate. Scattered iraTaa of~p
~*ith
iman r ^
^
oFTioa^ainad^jH
i aod dark gray quart*. 31 acattarad fioa pyrit laodim
at ftO0 - 9CP to cor a axi*.
31 Toe lch
loritic band*,
PR
OG
RE
SS
IVE
T
OT
ALS
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
PROPERTY Maw Bidlaaaqua Gold M
ince S
AM
PLIN
G
RE
CO
RD
2——
——
DE
PT
H
MB
* A
NG
LE
.J^
lA0
— S
TR
IKE
S
**t
EL
EV
AT
ION
——
SH
EE
T
NO
.
HO
LE
N
O.
CO
-OR
DIN
AT
ES
104+OOM
50*00*
DE
PT
H
FE
ET
213.0
213.9
217.
257.0
2M.O
FO
RM
AT
ION
__
SCHIST, aa
~bafora.ntOM
FORMATlOM
. aa b^fora,
acattarad pyritj 31CHOKITIC SCHIST, w
ithnarrow baoda of iron
pyrita aa bafora. CHLORITIC SCHIST, w
ith- 10X narrow laoaj
and carbonataA faw
acattarad aarrow
baoda of •agnttlt*.
^Schiatoaity at SO0
NO
.
lFN
GT
HA
NA
LY
SIS
LtN
GT
H
FE
ET
PROGRESSIVE TOTALS FEET X PER CENT
appro*, to c or a axia.
BIOTITE .
____
grained, ahaarad at cool act
Porphyritic with quartz
phtoacryata. ...J
-2MD OF H
OU -
Taat takan at 250' s -4:
*
by Caoadian
Loggad by -J. Kirk* IL
Prlllad on Clain Wo. T
——i....
- TOO J
BOOMAO. PROFILE
- 300
UJ 100 ^
o o . ±lO
in o o**- m
OVERBURDENCHLORITE SCHIST
ANDESITECONDUCTOR
CHLORITE SCHIST ANDESITE
MINERALIZED ZONE
ANDESITE
CHLORITE SCHIST
ANDESITE
CHLORITE SCHIST ANDESITE
CHLORITE SCHIST CARBONATE
CHLORITE SCHIST ANDESITE
CHLORITE SCHIST
ANDESITE
END OF HOLE
NEtt EIDLAMAQUED.D.K. #3
SECTION 64 r OON ERG. GRID CAST SCALE l - 50'
PR
OP
ER
'
HO
LE
N
O. —
H
Bidlaoaque
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
SA
MP
LIN
G
RE
CO
RD
G
ridS
HE
ET
N
O..
nD
EP
TH
3
51
.0*
AN
GL
E -
45
O
ST
RIK
E
JJflg
t E
LE
VA
TIO
NC
O-O
RD
INA
TE
SL64+OOM
Sl+O
OE
OE
PT
H
0.0-6.022. S
H.1
t
61 ft
Ol.U
OO
e J
™- ——
- -
115.4
116 742X
0
127 4
f- ft f m S
223.0
FOR
MA
TIO
N
Cai Ing
CHlo*iti^ "chiff w
ithn4ri*nv i*i**y ffTiw
^r**-oi quart* carbonate,scattered fine fryt * t* —
—
^. .
. BMia i ct finn
^•aVO
V
OK
py* X V
V a
^lo
rtttc schiat foita^
tlon at 700.Andes i UB finn grainedvnatver "locally w•^fcly-^
QuartiL, w
hite W light
grey 601 with included
andesite and chloritic•chist, 101 pyrrhotite
'and pyrite in the quart* w
ith a few scattered
grains of chalcopyriteapd sphalerite i*uart* vein type*
9f ^^
QMS s i ve f aa before
Am
i* A Lfcit f in* atr a ineid
Qtlerirti^
•cKjat,. —
-^ "
*
^
tfc
*P
*- ^
*
^B
"^** ^
t ^
Andesite ma d s lv* f f ne
SA
MP
LE
NO
,
T
-t --4-1
1 1
f 11k
LE
NG
TH
FT.
——
——
-
——
-
lo
j'4
AN
AL
YSIS
•/i
r
-
•i
-..
- ——
-
...
LL
NG
TH
FEE
T
i!Tj'iiiht 1
PRO
CFE
..—.-
5RE
SSIVE
TOT
ET X PE
R C
EN
--H
-
4LS
T
•—
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
PROPER New Bidlam
a^uf!
HO
LE
N
O.
5______ D
EP
TH
351.O
* A
NG
LE
^.
SA
MP
LIN
G
RE
CO
RD
G
rid- S
TR
IKE
E
aa
t E
LE
VA
TIO
N.
SH
EE
T
NO
.
CO
-OR
DIN
AT
ES
Lfr+OOM 51+OQE
DE
PT
H
FtE
T
223.0
223*2
261.0
FO
RM
AT
ION
grained, locally weakly
•chiatoae. Few scattered
*- ~ white quarts aod car-booata.Chlorite
achiatf folia*
tion ao0 ainor white
SA
MP
LE
NO
.
-4-41/2 )dull white with
and 401 band of pyrrhotite and
sphalerite at 6:4:1.Sphalerite 10 darkchocolace brownChloritic schist abuaddniwhite quartz limTcat-~bonate.A
odesite fine grained
auwaive,
locally achivtoi w,M
t 3Q
1.7 m
Mtrin
yir
(l-2iOB
)COAIMI pyrrhotite aod chalcQpyil to.-.——
.——-
LE
NG
TH
AN
ALY
SIS
•k•/o
LtN
GT
H
FE
ET
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X
PE
R
CE
NT
-f-
•— -—f
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
PROPER New B
idlanaqua C
old Kin
.* S
AM
PL
ING
R
EC
OR
Do
Crid
i____ D
EP
TH
3
31
.0*
AN
GL
E r
L-^
-_ S
TR
IKE
R
**t E
LE
VA
TIO
N —
——
SH
EE
T
NO
.
HO
LE
N
O.
CO
-OR
DIN
AT
ES
L6+OOH 51+OOE
DE
PT
H
302.0
351.0
351.0
FO
RM
AT
ION
Ch
loritic
Sch
ist, fo
lia
tion fa
ir to w
aak at 50-
iO0 ftch
iato
aity bacooas
waakar w
ith dapth.
Afld
Mita
fia
a g
rain
ed
aaia
lvt.
FrwB 334.6 to
— "*—
*—
"Mfc
k itm
ftfj V
^
— 2nd o
f Hol^ —
VB
&A
AW
V
^
WW
NiW
AV
KI
MM
FH
^
nor to *y*
BB
^^f o
y v*
cm L o
—
— *s 1.
Kirk
Sta
rted: M
arch 14/60C
oa
sted
: M
arch 16/60
or Iliad
on ula
ia # r.i.
SA
MP
I E
NO
.
AC
i9 —
—
- H
j — -
-t
!4960
LEN
GT
H
FT.
- —
——
— 1
-
f.
ri
-.. -,
i—..
AN
AL
YS
IS
'A
r- .--l
r~ "
'"
•'C
LEN
GT
H
FE
ET
— -
PR
OC
FE
•— —
SR
ES
SIV
E T
OT
/
ET
X P
ER
C
EN
- .--
1-
'
l
-- — --
!^LS
T
-...
-
OVERBURDENCHLORITE SCHIST
ANDESITE
CONDUCTOR
CHLORITE SCHIST
NEW ' IDLAMAQ'JED.D.v #6
SEC, ION j l * CCN* ERG. GRIJ EAST SCALE i" - 50'
MINERALIZED ZONE
ANDESITE
CHLORITE SCHIST ANDESITE
END OF HOLE
174-194 194-214 214-234 234-254 254-26o
Nil Nil Nil Nil Nil
•* i
I i -i c o Nil
C. 04 C.C4^ * '-. ' —
C.Cv C. 00
None N me : one
;oi -It_y.
Tlonc HoneNone None l r a c e
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
PROPER—
He* lid
lais^u
e
SA
MP
LIN
G
RE
CO
RD
HO
LE
N
O.
6
DE
PT
H 3
17
.0*
AN
GL
E *
45
O
ST
RIK
E
Grid
*
SH
EE
T
NO
..
CO
-OR
DIN
AT
ES
L32* 49+SOE
DE
PT
H
FE
ET
0-5,013.0
20. o
44.0
JI4*7
d5.5
FOR
MA
TION
SA
MP
LE
NO
.
CasingAndes H
e fine or*in*d
•as s i ve abundant crtanv IIw
hite cerbonat*C
hloritic fffihifttt veen, tib~ ""
^ , i
ffSa fC
^nig schistosity Pt 50rto cote satis.
Abundant 1
•tattered grains carbonatiteA
ndesite fine grained. ||
places *AHfc* and yellow
carbonate section iron l38.6-39. a few
scatteredgrains pyrite.C
hloric* schist,
sbundttflveinlets and lenses ofcreaser cA
ibonete goodfoliation at 70* - 60'A f*w
pemtt.*rm
d cub* H of
(.write.
j
651 with green chloritic
schist inclusions 31pyrite M
dift&eainAteti
grains and irregularpatches. pyrrhotite asirregular patches andalso dissem
inated ara inof ow
^paetitep a tewsteal 1 grains oi chalco pyrite observed.
Y
LE
NG
TH
FT.
AN
ALY
SIS
tt
t -
-- - —
—
jf-
tttt
LE
NG
TH
FEET
PRO
GR
ESSIV
E TO
TALS
FEET X PER C
ENT
^ — .-
.. ...- .^... .
PR
OP
ER
TY
NewS
ULM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
SA
MP
LIN
G
RE
CO
RD
SH
EE
T
NO
. -2.
HO
LE
N
O.
6
ng
PT
H 3
37.0
* A
NG
LE
-
45
S
TR
IKE
g
rid
E
LE
VA
TIO
NC
O-O
RD
INA
TE
SL92+OOM
49*
OLP
TH
F
EE
T
ailoritic ochi*t abundant
FO
RM
AT
ION
atbooata. a l*w narv*
.
-t-tax^d gy^jnt of4 *
*t*
fi friirich and.iX
OB
I l iO
3
JO
L
bll t
SA
MP
LE
NO
.
at-
litt—
pjucit*-jnd y yr the t i t*
^ut* Jw pyrrhotite 2;1
4uc*d fin* ftwjni
in thit ••ctioo.j
folia*Itloo *t 40' ea cox*
\-C1i*
hf
a*-Mv
VZ
pyrrhotite. fev-ae*tt*r*d
LE
NG
TH
FT
.
AN
ALY
SIS
LtN
OT
H
FE
ET
If-
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X
PE
R
CE
NT
-I-
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
— .
...... .
OM
mr-L
-IINO
r\C
HO
LE
N
O.
b
DE
PT
H
337.0
* A
NG
LE
-
45**
ST
RIK
Egrid
DE
PT
H
FE
ET
22
i.L
^7
.?. —.0
1^
23
5.0
FO
RM
AT
ION
Chlo
ritic kch
i^t.
we
ll(c li ut- fid
At. 60 o
td cor*
Apia
. '.ra
,t fVF
ff1^ u
ra^fiji
fiivii c\il^tt * w i-
t y r i tt i sfjji
insula
r band!
ul
'i^rt
*j3d ca
rbo
na
te*
I'tcs* 212
t0
C
U4H
V*
A^"*-P
-1 l3
' i'y
1"1
vijiirv, da^K
t^rvy 7U& v
i^t^ j
.f 'f 4 i
acts 1 r- 1
l M; i U
S i l
SAMPLE:
NO
.
J^54! .
h.ILK
A! finer
na
vtD
W ilA
f Lu
y*^
IB
th
e
v,rjH
fi(* ^-fia
lc"
y*tf^
f*
-t*rv
*d
*^5wc
i^t*tf
w1^
!tt*tt
VlttlO
Lit*
V
-VH
C*
Hfryrsh
ot.lt* 4 - ^
14 y*, ite
^AajtW
* i in
* ^ran
i04 w
ith sotfkor c
hio
iltita
ch
i*V(
1 ij^hC
ij T ''J
,M
*rt
*n4 cstbonatw i
f c-At fcitttttfxra
iue p
yrrh
otii.*.
iytt
r;to
i/yt iriot 1 tc
t)' 1
( uA
rrx ritill
uh
itf to
g
r*fn
-3
^i-
t- 1 ^ j
'
sch
ist.
inclu
muT
id
15 to
itMl*^
r*tch#"
i-yr-it* *P
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AiC
i^lttfftC
d
t. JJ O^if
idLX
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tl^hv
cilcklcoi. y it tv i\4iAvx
11
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NG
TH
FT
.
t
-. ..
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L^*V
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J
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RD
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VA
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tOO
S
^'^^SO
H
AN
ALY
SIS
y.
— -
11
*
r -
*j
4
. ..,
---
LE
NG
TH
FE
ET
1 -
' ,.. .
t i -'l;
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X
PE
R
CE
NT
--
^.
-.
. ..
.
-
.
-
1
PR
OP
ER
TY
HO
LE
N
O.
SU
LM
AC
E
XP
LO
RA
TIO
N
SE
RV
ICE
S
LIM
ITE
D
SA
MP
LIN
G
RE
CO
RD
DE
PT
H 337.0
* A
NG
LE
* 4
SO
S
TR
IKE
G
cliJ
E
LE
VA
TIO
N —
——
SH
EE
T
NO
.
DE
PT
H
FtE
TF
OR
MA
TIO
NS
AM
PL
E
NO
.
LtN
GT
H
FT
.
AN
ALY
SIS
•/o
LE
NG
TH
FE
ET
PR
OG
RE
SS
IVE
T
OT
ALS
FE
ET
X
PE
R
CE
NT
255^0a a lv*
with p
yrrhotit
JUK
Llfi l
4A.Q
-
244.4
cut t i TIEM
teh 21aod*, J0
1 pjtxiu*
11 Oy
•CB
ttttV9u
it t * C** cJnricopyrl te *
BC
hU
t
with depth.
25570 \nd* a H
e Tin* grained
, scattered floc
. Jdta** light
Qinor chloriui andV
ycli* id** wf tineL ^
ink
i.A h
ue.
l
J -____
^^
.. l
m.
___..
"t" i..