p,it 63-545-0 (onn-^-c-03
TRANSCRIPT
42J*4SEM25 19 PIVABISKA RIVER 010
DIAMOND DRILLING
AREA: PIVABISKA RIVER REPORT NO: 19
WORK PERFORMED FOR: Noranda Exploration Co. Ltd.
RECORDED HOLDER: Same as Above [xx]: Other [ ]
Claim No.
P 802232/ 802235
Hole No.
FR-88-7
Footage
276.15m
Date
June 88
Note
(D
NOTES: (1) W8906-305, date filed June/89
(3) 0^1'^"^ Ma"Ur,a l tcv^ b
P,It 63-545-0 (onn-^-C-03
epo4 Or, Dr. /A n^^Sfc y s ^r
LA
TIT
UD
E.
t 2.00 C
DE
PA
RTU
RE
ELE
VA
TION
.
6.0
0
N
NO
RA
ND
A E
XP
LOR
ATIO
N C
OM
PA
NY
LIM
ITE
D
DIA
MO
ND
DR
ILL CO
RE
LOG
Protect N
o. .2
77
Hole N
o..
Su
rfac
e
DIP
AT C
OLLA
R-4
5"
BE
AR
ING
.180"
Ten
Deoin
12.19
Dip
-46"
Mjq
neiic
D
inin
gC
orrected B
ellin
gP
roperlyP
ivab
iska
Riv
er
3-8
4
76.20
TOTAL DEPTH
27
6.1
5CORE SIZE .
BQm
.23-4
2"
228.60 -40"
CORE STOR
AGE.
REMARKS —
—
Aunor Minesite,
Timmins, Ont.
276.15 -40"
NTS 42
J ^p
Pivabiska
R.. Area.... Mo
^p
B02232
D.,e
i,.r,ed
1
0/0
6/8
8_
__
__
__
__
__
co
mo
,,,.,, 13/0
6/8
8_________
,lrlclo, Norex
Drilling Ltd.__________
S. Parker
Com
Denin A
Lunoiogy
Oesen
otio
n (co
lou
r, grim
sue. te
nu
re, stru
cture, etc.)
Atte
ntio
nM
me
raiita
tion
OW, A-i
. ' AL SURVEY
0-11.58
11.58-58.86
Amphibolitic
Silicified
Mafic Volcani
Overburden (casing)
Dark green
with light
green siliceous
bands, fine
to medium grained,
moderate to
strongly developed
foliation e
40-50 to core
axis-strongly
amphibolitic with intervals
of medium
grained, recrystallized?
subhedral to
euhedral amphibole
crystals within
a cjtz
rich matrix.
Minor dark brown, fin*
grained, micaceous
bands within m.g. amphibolite,
-occasional whit*
concordant gtz/calcit* veins
and discordant, irregular
(deformed) gtz/calcit* veins
and stringers
e.g., 9
21.78m.-trace
(sporadic), medium-grained,
purplish anhedral
garnet crystals
e.g., 23.19m
12.65-12.82m: broken
core 18.17-18.33m:
abundant gtz/calcite
in irregular veins,
minor pyrrhotite disseminated
in mafic component.
(P 21.94m:
lcm gtz
bleb surrounded by
calcite@
28.58m: several
medium grainedgarnets
within calcite vein
-black mineral? in
veins 28.90-29.66m:
interval exhibiting dark
brown micaceous bands within m.g.
amphibole rich
rock.
-amphibolite, chlorite
and minor
micaceous ninerals
(biotite)-local
light green,
silicified zones
g., 26.15-26.21m
-carbonate (calcite)
is found
in association
th many
of the
gtz veins.
l
-trace medium
to fit
grained subhedral
pyrrhotite blebs
within core,
(rock is
weakly magnetic) 0
12.18m: medium
grained, anhedral
pyrrhotite bleb adjacent
to anhedral
pyrite bleb within
cor*.-minor
fine grained
anhedral, disseminated
pyrite.
R
(J 1389
C E l V E D
NO
RA
ND
A E
XP
LOR
AT
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CO
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AN
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ITED
DIA
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DR
ILL CO
RE
LOG
Protect N
o.277
Hole N
o
Dem
n 4
Urnoloqy
Descrtoiion (colour, grain site, ten
ure, structure, etc.)
58.86-98.33
SilicifiedMetasedimen(Greywacke?
with Graph!Interbeds
-amphibole crystals
produce crenulation
texture (ie.,
intense micro
folding) '
6 30.58m:
medium grained black mineral?
within gtz/calcite
vein (trace
garnets) 39.68-40.30m:
mg, amphibole
rich vol,
with interstitial
qtz, trace
calcite-2cm
irregular clusters
of large
grainedamphibole
mosaics consisting
of approx.
90* amphibole,
10* gtz.
Fragments of
the a"Bove
m.g. vol.
occurwithin
the f.g.
vol. eg.,
44.10m (flow
texture?)44.67-44.78m:
light grey,
altered cherty
(silicified) zona with minor disseminated
pyrrhotite/pyrite.
-Light grey to
bluish, fin*
to medium
grained, strongly
developed foliated
8 35-45
to core
axis.-contains
black intervals
of graphitic
argillaceous metasediment eg.,
978.95m-locally,
small scale
folding developed
in foliation-minor
bluish gtz
veins and
fragments e.g.,
8 79.80m and
75.85m respectively.
Pfooeriy
Pivabiska
River
3-84
Alteratio
n
49.18-49.25m: light
grey silicified
zone similar
to that
from 44.67-44.78m.
-moderately silicified
and locally
argillaceous-strongly
graphitic in
sections
Mineralization
Hem
ams
9 50.0m,
minor pyrrhotite associated with
gtz/calcite vein 9
51.31m, medium grained
anhedral pyrite/pyrrhotit s
located adjacent to a calcite vein.
t
852.28m:
minor anhedral
pyrrh
otite.(w
eakly
m
agnetic)
-locally
up to 21
combined
fine
to
medium
grain
ed,
anh
edral
pyrrh
otite
/ pyrite
in
clu
sters
and dissem
inated
e.g
., @
61.58m-p
yrrh
otite
is
stron
gly
m
agnetic.
- listinct co
lou
r c lange
from green
grey at co
ntact
sections
of uiit m
ay be s efficien
tlyra
ph
itic to
be
conductive 5 ourcec o
ntrib
utin
g to
th
e
HLEM
z n
om
aly.
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LOG
Oeoirt ft
Uinoioqy
Descnoiian (colour, grain su
e. texture, structure, etc.)
98.33-102.3
Silicified
Metasedimen
(Greywacke?
58.86-59.13m: light brown
interval, -
transition into metasediment
Q 67.65m:
lent chloritic vein,
containingminor vugs
and It
pyrite77.72-85.04m:
argillaceous graphiticinterval
with up
to 5*
pyrite, no
pyrrhotite.
9 81.36m:
green amphibolitic
fragment ("2cm)
within metasediment.
92.97-93.20m: white
siliceous interval*
93.65-93.75: graphite
(broken core)
9 94.31:
gtz/graphit* (deformed)
94.2-95.43: graphite
(broken core) 0
96.78: white
calcite veining
-Light grey,
medium grained,
massive to weakly
developed foliation
S 30
to core axis
-abundant qtz
lenses define
foliation-locally,
foliation parallel
to core
axis '
99.45-99.50: blue
qtz vein 99.50-100.30:
dark argillaceous
interval within
light greywacke.
Alteratio
n
-high silica
content-abundant
chlorite on
cleavage planes
i No.
Moir N
eFR
-88-7
Pro
otrry
Pjv
ob
icl.?
Min
era
lizatio
n
-locally, 21
pyrite as
anhedral medium
grains, and
fine grained
anhedral pyrite
stringers. 8
63.40m: area
of abundant
pyrrhotite
77.72-85.04: up
to 51
pyrite in
medium sized
aggregates forming
bands parallel to
foliation.-pyrite
nodules at
81.45m.95.91-96.20m:
up to
51 fine
grainedeuhedral
pyrite in
veins (this
intervalis also
gtz-rich)
-minor, fine
grained subhedral
pyrite-minor
disseminated fine grained,
euhedral pyrrhotite
and sheared
pyrrhotite on
cleavage planes
(pyrrhotite is
magnetic)
Rem
arks
po pyrrh
otite
argillaceo
us
inte
rvals.
lyrrh
otite
icreases and
p 'rite
increases
a i you m
ove dow
n t lis
unit.
NO
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XP
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Sn
*ti Ha
-OF
.
De
em
A
Uin
oio
gy
ffoieci H
a.
Pio
oerty
277M
oir No
FR-8B
-7
Pivabiska River
3-84
OescriD
iion (colo
ur, g
rain s
ite, textu
re, structu
re, etc.)
102.39-108. Silicified
Micaceous
Hetasedimen
108.80-196. Anphiboliti
Mafic Volca
.1
Dark grey,
fine to
medium grained, massive
to weakly developed
foliation 3
35-40 to
core axis,
-minor qtz
veins parallel
to foliation,
-minor calcite
associated qtz
veins.-locally,
minor medium-grained
anhedral garnet
crystals eg.,
102.22m-minor
amphibolitic intervals
eg., 106.50m
105.48-106.05:} 106.60-107.16:)
Broken core
107.73-107,83:}
Dark green,
with brown
micaceous bands,
fine to
medium grained,
massive to
weakly ic
developed fabric
0 35-45
to cor*
axis.-fabric
is defined..by brown micaceous bands,
gtz/calcit* veins, and allignnent
of amphibole crystals
-first 4.5m of unit
contains abundant qtz (minor
calcite) stringers and
irregular veins.
Quartzy veining is present,
although less
abundant past this interval.
113.45-113.55m: qtz/calcite vein
114.11-118.83m: example
of massive, homogeneous,
amphibolitic vol with
little gtz
veining.-texture
similar to
that from
11.58-58.86-euhedral
amphibole crystals
are common
in m.g. sections.
highly amphibolitic
minor micaceous
minerals-trace
calcite-minor silicification
-minor (locally
l*) anhedral
disseminated-pyrite
and sheared
pyrite on
cleavage plane:
-minor, medium
grainedanhedral
pyrrhotite and
pyrite blebs.
.
-similar to
that from
11.58-58.86
Deo
tn 4
U
ino
ioq
y
NO
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XP
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D
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LOG
Descrip
tion
(colo
ur, g
rain size, textu
re, structu
re, etc.)
-abundant (*5*)
irregular, wispy
qtz/ Fe-carbonate/calcite veins,
blebs and
stringers eg.,
6 131.28
-abundant medium grained
(recrystallized?) amphibole
bands created by a mosaic
of euhedral
amphibole crystals
eg., 9
145.85 f
170.14: i/2cm wide wavy
qtz/carbonate vein.173.52-176.59;
green, medium grained,
massive, recrystallized
amphibole, mica
qtz-rich volcanic. Becomes
finer grained
towards lower contact.
Very distinct differences
over the
finer grained,
foliated, amphibole-rich volcanic.
0 178.34:
4cm irregular gtz/Fe-carb bleb
9 179.90:
pinching and swelling m.g.
amphibole band*
189.58-189.67:
192.42-192.49:
qtz/calcit* veingrey
qtz vein 193.10-193.43:
strongly foliated
interval i
40 to
core axis
(sheared pyrrhotite on
cleavage planes)
193.94-195.16m: foliated,
amygdaloidal, siliceous,
amphibolitic vol. -medium grained
(qtz?) amygdaloids
195.16-196.63: silicified,
altered zone
with minor py/magnetite 9
195.56m and an
increase in pyrrhotite/pyrite down section
Alteratio
n
-highly silicified.
• OF ,
,277H
oi* N
oFR
-8B-7
Pivabiska River
3*84
Min
era
lizatio
n
132.14-132.64:
up to
30* massive pyrrhotite,
3* medium sized anhedra
pyrite blebs
-zone is
highly magnetii due
to pyrrhotite
-abundant calcite
162.46-162.82: minor
fine grained
euhedral to
subhedral white
sulphide mineral
(arsenopyrite?)
-trace chalcopyrite
blebs at
179.78
Remarks
-up to
3* pyrrhotite
in veins and
disseminati throughout.-medium
sized anhedral
magnetite crystals with
associated pyrite.
NO
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Dra
in ft
Uin
oio
qy
196.63-211.
Sulphide Ircn
Formation
(MassivePyrrhotitePyrite,SilicifiedZones
and Qtz)
Descrip
tion
(colo
ur, g
rain size, textu
re, structu
re, etc.)
-brown pyrrhotite,
bronze pyrite,
white to
milky quartz,
green silicified
zones and
mafic components,
fine to
large grained
sulphides, predominantly massive
with local
zones of
weakly developed
fabric f
50 to
core axis,
(a very
homogeneous interval)
202.44-204.93: highly
altered, brown
to green,
fine grained
silicified volcanics,
moderately developed foliation
9 50
to core
axis. Total
of 81
combined sulphides
(pyrrhotite >
pyrite) within
gtz rich
mafic volcanics.203.86-204.38:
silicified, mafic vol
with a
fine network
of gtz/carb veining producing
a brecciated texture.
No sulphides.
9 209.96:
lea Fe-carbonate fragment
within massive
pyrrhotite interval.
9 211.48:
folding of gtz/mafic bands near massive
sulphide/mafic volcanic contact.
-the mafic
intervals are
highly silicied
196.63-202.44: 80*
massive pyrrhotite,
12* medium to
large grained
anhedral pyrite
blebs and
nodules, St
medium to l
arge sized
gtz eyes,
trace mafic
components. Pyrite
and gtz
gives rock
a spotty
texture. 199.31-199.69: siliceous
interval with
only 30t
pyrrhotite, S*
pyrite. The
remainder i*
silicified mafic
vol.
204.93-209.03: silicified volcanic wit) sulphide
content increasing
drastically towards
bottom of
secti Abundant
gtz veins
and blotches.-5*
sulphides grading
into massive sulphides
(pyrrhotite/pyrite) similar to that
from 196.63-202.44. 209.03-211.70m: massive
sulphide interv
similar to that
from 196.63-202.44. Pyrite
modules occur
locally and
are not
evenly distributed
throughout the
massive
This unit
represents the
Drincipal cause
af the
near :oincident
HLEM and
magnetic anomalies.
n.yrrhotite
NO
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LOG
Sn
vri No
Protect No
27
7M
oir N
oFR
-88-7
-OF
.
Pro
piriy
Pivabiska River
3-84
Oeotn ei
Litnoiogy
Descrtonon (colour, g
rain su
e. texture, stru
cture, etc.)
Alteratio
nM
ine
raliia
tion
Rem
ans
21
1.7
0-2
76
.15
Silicified
AmphiboliticMafic
Volcanic
Light green,
fine to
medium grained, weak
Q to
moderately developed
foliation e
30-45 to
core axis.
-abundant qtz,
qtz/calcite veins and
stringers, generally
paralleling foliation
-locally, small
intervals (10-20cm)
contain massive
sulphides (po)
similar to previous
unit, eg.,
215.77-215.96 and
irregular po/py bands
interbanded with the
volcanics eg.,
213.36-213.47 218.82-218.88:
milky qtz
vein-minor
vugs in
pyrite vein*
eg., 9 212.35
229.52-232.95: medium
grained, strongly
foliated (recrystallized?)
amphibole rich,
with minor micaceous
minerals. Similar to
medium grained texture
noted in
first unit.
Silicified, minor
qtz/calcite stringer
stockwork, and
trace fine
grained po/py blebs.
229.96-230.02: heavily
silicified interval.
232.95-234.51: dark
grey, fine
grained, foliated,
silicified, highly
altered interval
with abundant
qtz/calcite veins.
Tight folding
of qtz
veins S
233.55m. Light
green, carbonated
(calcite-rich) breccia
texture from
233.77-233.85. g
252.47: medium
grained black mineral,
weakly magnetic
(magnetite?) 254.06-254.24:
altered qtz/carbonate
veining260.28-260.44:
80* milky
qtz, minor
calcite, minor pyrrhotite
veining. 262.43-262.46:
milky discontinuous
qtz vein
moderately silicified
strongly amphibolitic
calcite is
associated ith
the majority
of f
qtz veins.
-local intervals
of massive
pyrrhotite, 51
pyrite, and
minor amphibole
blebs eg.,
215.77-215.96-locally
2* fine
grained pyrrhotite
in veins parallel
ing foliation
eg., 8
212.76-locally,
l-4cm sized
irregular pyrrhotite/ pyrit* clusters
eg., 219.48215.52-215.60: massive
pyrrhotite similar
to that
from 215.77-215.96 220.12-220.16: massive
pyrrhotite
minor irregular
pyrrhotite/pyritediscontinuous
veinsand
stringers.227.85-227.88:
pyrrhot teminor pyrite blotch238.29-238.33:
irregular pyrrhotiteblotch.239.14-239.16:
pyrrhot .teminor pyrite v
ein
242.03-242.06: pyrrhot .te
minor pyrite vein.
256.53-257.15:
up to 3
-similar to that
rom 11.58-58.86
Ithough contains
iore sulphide
nineralization-calcite moreabundant than?e-carbonate
NO
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i NO277
Sri**i NO. "
OF
FR-88-7M
oir No
Pivabiska R
iver 3-86
Deoin 8.
Liinoiogy
276.1
5
Deserioiion (co
lou
r, grain
sue. textu
re, structu
re, etc.)
270.16-270.37: qtz/calcite vein with
minor mafic minerals, pyrrhotite
and pyrite.
272.79-273.10: pinching and swelling,
'lea wide calcite vein trending approx.
parallel to core axis.
End of Hole.
Alteratio
nM
ineralizatio
nR
eman
s
This texture
is exhibite l
locally in
other section
268.24-268.30: 70*
pyrrhotite, 30*
minor calcite/qtz,
mafic component.
•r*
eon
UJo oc\i
l l
P8O2232
Q90*
FR-BB-7
P 802235
P 80223
P 802234
-BLO
Pivabiska River 3-84 (Grid "G")
Collar Location: 50m North and 2OOm East of *3 Post P8O2232 Grid Co-ordinates: L2.OOE/6.OON Azl8O0 af-45*
at visio
POOJ M? 277MT.S.o*G. H;
LOCATION PLAN D.D.H. FR-88- 7
PROJECT: EOX RIVERsutvtrioiri.OAAWM Ifi——
OATnAUO/88- . son. riO.QOO
NORANDA EXPLORATION CO.LTDomen.
inistry of Northern Affairs and Mines
Report of Work
JUMENT6906*
OntarioMining A 42J84SE8825 19 PIVABISKA RIVER 90©
Name at- ,tal Address of Recorded Holder
Noranda Exploration Company, Limited (no personal liability)
Suite
Prospector's Licence No.
A-34387
1300-4 King St. West, Toronto, Ontario M5H 1B6Summary of Work Performance and Distribution of CreditsTotal Work Days Cr. claimed
for Performance of the following work. (Check one only)
[~~| Manual Work
J Shaft Sinking Drifting or other Lateral Work.
J Compressed Air, other Power driven or mechanical equip.
j Power Stripping
Diamond or other Core drillingLand Survey
All the work was performed on Mining Claim(s): P-802232 A 802235
Required Information eg: type of equipment. Names, Addresses, etc. (See Table Below)
Contractor: Norex Drilling Ltd., P.O. .Box 88, Porcupine, Ontario
Date Drilled: June 10 to June 13, J988_____.
DDH f FR-88-7
Bearing: Az 180 0Dip: -45 0Size of Core: BQLength: 276.15m (906.0 ft)On Claim No.: P-802232*235 feet k
ONTARIO GEOLOGICAL SURVEY"ASSESSMENT FILES
OFFICE
JUN O
RECEIVED
RECORDED
OCT 13
P-802235-*671 feet.t
Credits to be filed late*-: 906-340 = SS6- days i
Core stored at 60 Shirley St. So, Timmins, OntDate of Report
. Oct. 11/88Recorded Holder or Agent (Signature)
Certification Verifying Report of Workl hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.
Name and Postal Address of Person CertifyingR.C. Denommee, P.O. Box 1205
Timmins, OntarioDate CertifiedOct. 11/88
Certified by (Signature)
Table of Information l Attachments Required by the Mining Recorder
Type of Work
Manual Work
Shaft Sinking, Drifting or other Lateral Work
Compressed air, other power driven or mechanical equip.
Powtr Stripping
Specific information per type
Nil
Type of equipment
Type of equipment and amount expended. Note: Proof of actual coit mutt b* submitted within 30 days of recording.
Other information (Common to 2 or more types)
Names and addresses of men who performed manual work/operated equipment, together with dates and hours of employment.
Name* and addresses of owner or operator together with dates when drilling/stripping
Attachments
Work Sketch: these are required to show the location and extent of work in relation to the nearest claim post.
16'35'
34'
33'32'
Sf^
^w
fSfl i";-v
,^^i i^
ej^
tte, v'-^a
7-i*a3feii*SaE
3sfe?J .'L:1-.'-' '" \-: ".i!-,1;