Embed Size (px)
Citation preview
Table of C 42C13SVW0008 2.15930 WABIKOBA LAKE 01OC
Page
SUMMARYI.0 INTRODUCTION..........................................................................................................12.0 LOCATION AND ACCESS.......................................................................................... 13.0 PROPERTY DESCRIPTION ........................................................................................14.0 PREVIOUS WORK ......................................................................................................35.0 REGIONAL GEOLOGY ...............................................................................................46.0 LINECUTTING.............................................................................................................47.0 TRENCHING AND SAMPUNG.....................................................................................48.0 PROPERTY GEOLOGY..............................................................................................^
8.1 Introduction ............................................................................................58.2 LMiologies.............................................................................................^8.3 AMeration................................................................................................68.4 Metamorphism and Deformation.............................................................6
9.0 GEOPHYSICAL SURVEYS..........................................................................................?9.1 Introduction............................................................................................?9.2 Instrumentation.......................................................................................?9.3 Interpretation......................................................................................... 8
10.0 CONCLUSIONS AND RECOMMENDATIONS .............................................................910.1 Geology...............................................................................................910.2 Geophysics.........................................................................................^
II.0 Appendix!Assays. Whole Rock, Multi-Element Analyses and Sample Descriptions
12.0 Appendix IIStatement of Authorship and Qualifications
List of Figures and Maps
Figure 1 Location MapMap 1 Geology Sheet 1Map 2 Trench 146 E Sample LocationsFigure 2 IP Dipole ArrayLine 14200E Induced PolarizationLine 14400E Induced PolarizationLine 14600E Induced PolarizationMap 3 Contoured Magnetic SurveyMap 4 Magnetic Profiles along linesMap 5 Induced Polarization Anomaly Map
Scale
1:5000 1:250
1:5000 1:5000 1:5000 1:5000 1:5000 1:5000
SUMMARY
During the period of June 14 through to December 2,1994. a work program consisting of geological mapping and sampling, a magnetometer survey, an Induced Polarization/Resistivity survey, and overburden trenching l stripping was conducted on the North Limb claim group. This daim group is located along Highway 614 to the south of Summers Lake, approximately 15 km north of Highway 17 and extends 5 kilometres to the east of the highway.
The results of this work have shown that a strong alteration system is centred on a small quartz-feldspar porphyry stock referred to as the Armand Creek Quartz Feldspar Porphyry (ACQFP). The eastern portion of this stock extends onto the North Limb property. Despite disappointing results of samples taken from surface exposures, the geological similarities between this property and Hemlo warrant further work.
11
1.0 INTRODUCTION
During the period of June 14 through to December 2. 1994. an exploration program consisting of geological mapping, magnetometer and I.P. surveys, and overburden trenching/stripping/channelling was conducted on the North Limb property. The results of this work program are contained herein.;
Work focused on delineating a quartz-feldspar porphyritic unit with characteristics similar to the quartz-feldspar porphyry intrusion associated with the Hemto gold deposit
2.0 LOCATION AND ACCESS (Figure 1)
The North Limb property extends from the CP rail tracks on the west, across Highway 614 and an additional 5 km to the east. The property is situated to the south of Summers Lake a distance of 15 km north of Highway 17. The centre of the property is located 17 km northeast of the Hemlo Mines.
Access is by either Highway 614 or the Twist Lake timber road, which both pass through the property.
3.0 PROPERTY DESCRIPTION (Figurel)
The mining claims on which exploration work was performed are:
CLAIM NUMBERS # of units
TB 1183307 TB 1196882 TB 1010503 TB 1010504 TB 1010507 TB 1010510 TB 650898
650900651397651398651399651400653301653302653303653304653309653310
TB 653311 TB 653312 TB 653313 TB 653314 TB 653317 TB 653318 TB 653319 TB 653322 TB 1174289 TB 1174290
68
TB TB TB TB TB TB TB TB TB TB TB
11144
28 claims 46
O
0\
6M
o
HEMLO GOLD MINE SITE
FIGURE l : LOCATION MAPLUCATIDN MAP
The listed claims are held by Hemlo Gold Mines Inc.
4.0 PREVIOUS WORK
The following is a summary of previous work conducted on various portions of the North Limb property:
Mclntyre-Porcupine Mines, Von Klien option, 1962
Discovery of a number of copper-nickel and copper-lead-zinc occurrences. Electromagnetic conductors and magnetic anomalies were tested with 28 diamond drill holes, but mineralization was weak and discontinuous with depth.
Noranda Exploration Co. Ltd, 1976
Dotted Lake airborne survey completed over the area.
Pryme Energy (North), 1982
Work concentrated on the Mcintyre occurrence.
Oued Resources, 1983
Geological mapping , trenching and drilling was completed on a claim group to the east of the North Limb property. Emphasis was on stratabound gold mineralization within iron rich interflow sedimentary sequences. Drilling returned values of up to 0.025 oz/ton over 3 metres.
Norman Resources Limited, 1983
Geological mapping, soil geochemistry, airborne magnetics and VLF-EM covering an area immediately southeast of the present claim block. Soil samples were all low range with one sample returning 45 ppb. No major near surface concentrations of precious metals were discovered.
Kelly-Kerr Energy Corp., 1986-1988
Geological mapping, stripping, soil geochemistry covered an area in eastern portion of the present claim group.
Noranda Exploration Co. Ltd, Newjay Property, 1987-1989
Humus geochemistry and geology filed covering a portion of the current claim group. No anomalous Au values were found in the 23 rock samples analyzed. A weak Au humus anomaly is reported to overlie a felsic-mafic contact.
Noranda Exploration Co. Ltd, Norman Resources Property, 1989
Geological report, plans, soil/rock geochemistry and assays filed for a claim block located southeast of the present property. Several anomalous Au values were recorded from the soil survey samples but results were not considered encouraging.
Fowler/Shuman, Armand Lake Property, 1991
Property report covering prospecting and stripping on the adjoining property to the east.
Newmont Exploration of Canada Ltd., 1992
Geological and lithogeochemical reports for a claim group located 2.5 kilometres to the southeast of the present claims.
Hemlo Gold Mines Inc., 1994
Trenching and geological mapping of trenches 150E. 153E and 156E on the Fowler #1 property.
5.0 REGIONAL GEOLOGY
The North Limb property is located within the Archean Schreiber-Hemlo greenstone belt which forms a part of the Abitibi-Wawa-Shebandowan Subprovince of the Superior Province. The area contains a dominantly southeast striking sequence of metavolcanic and metasedimentary rocks bounded to the south by the Musher Lake Granodiorite pluton.
Supracrustal rocks consist principally of basaltic flows and subordinate tuffs, with intercalations of epiclastic arkosic wacke and siltstone. Interbeds of felsic volcanic tuffs and/or volcaniclastic sediments occur locally. Numerous small elongate quartz-feldspar porphyry (QFP) stocks intrude the sequence. Equigranular to porphyritic dikes and sills intrude the volcanics, sediments, and small QFP stocks.
6.0 UNECUTTING
16.2 kilometres of grid was cut on the North Limb property during December.1993, May, 1994 and November 1994 by Vytyl Exploration of Thunder Bay. Grid lines were oriented north- south and spacing varied between 200 and 400 metres with stations established at 25 metre intervals.
7.0 TRENCHING AND SAMPLING (Appendix l)
Two trenches completed in an earlier program one of which was sampled using a diamond saw to extract a channel sample across favourable rock types. A total of 11 samples were collected and submitted to Accurassay Laboratories of Thunder Bay for gold assays. Assaying was by fire assay with an atomic absorption finish. Selected samples were submitted to Chemex Labs Ltd of Thunder Bay for ICP analysis to determine whole rock and trace element composition.
An additional 13 samples were collected during prospecting of the property and were as well submitted for gold assays.
No economic gold values were encountered with the majority of the samples returning
8.0 PROPERTY GEOLOGY (Map 1)
8.1 Introduction
During the period from June 14 through October 25. 1994. geological mapping was conducted on the North Limb property by Paul Johnston, under the supervision of John Londry. Mapping was performed along cut grid lines.
Geological data from previous mapping was reviewed and updated where necessary.
8.2 LJthologies
8.2.1 Mafic Metavolcanics
Mafic volcanics that underlie the northern third of the property consist primarily of massive flows with minor pillow structures and flow breccia. Pillow structures noted north of the property dip steeply to the south and indicate a southerly top direction.
The mafic volcanics are dark green, fine grained, with varying amounts of chlorite and amphibole. Minor alteration consisting of minor feldspathic fractures and minor carbonitization is present proximal to the QFP stocks.
8.2.3 Clastic Metasediments
A 250 metre wide band of clastic metasediments consisting of siltstone, fine sandstone, and minor interbeds of heterolithic pebble to cobble conglomerate extends across the northern part of the property. The metasediments are grey to dark grey with light grey-brown coloured weathered surfaces. They are typically immature quartzo-fekJspathic sediments, containing minor biotite and amphibole, and rare garnet. Primary structures were not recognized in this mapping program.
8.2.5 Quartz Feldspar Porphyry Intrusion
A small elongate quartz-feldspar porphyry (QFP) intrusion, flanking the northern contact of the Musher Lake Pluton, occurs on the eastern portion of the claim group. The QFP is light grey to grey and weathers white to light brown. Previous mapping identified this unit as a felsic tuff, however, delineation of the unit through grid line mapping and trenching combined with the texture of the quartz and feldspar phenocrysts and ground mass suggests this unit is an intrusive body. The unit is discordant to the sequence of mafic volcanic and sedimentary units in the area. Quartz and feldspar phenocrysts are fairly uniform in size and are intergrown with the groundmass suggesting crystallization from a melt rather than deposition from pyroclastic material.
Heterolithic clastic units occur within and along the margins of the QFP and contain mafic volcanic and QFP clasts. Lenses of green mica and up to 5*K fine pyrite is common within the clastic unit. These clastic units appear to be related to the emplacement of the QFP and are interpreted as hydrothermal breccias.
8.2.6 Granodiorite Dikes
Narrow (10-200 cm) equigranular to moderately feldspar porphyritic dikes intrude volcanic, sedimentary and QFP units. The dikes occur across the property but appear to be more frequent near the QFP. Multiple phases of dikes are recognised but a consistent classification has yet to be established.
8.2.7 Granodiorite Pluton
The Musher Lake pluton is an arcuate granodiorite intrusion located south of the property. This pluton is weakly foliated near its contacts with the supracrustal rocks. Mafic xenoliths are common throughout the granodiorite. The pluton dearly post-dates the QFP as apophyses of granodiorite intrude the QFP. Irregular pegmatite dikes and pods are commonly observed in exposures of granodiorite.
8.3 Alteration
Intense alteration is associated with, and centred on the Armand Creek Quartz Feldspar Porphyry. Two main alteration phases have been noted. Early fracture controlled microcline alteration is overprinted by pervasive and fracture controlled muscovite (sericite). Green mica is associated with sericitic fractures and with clastic units interpreted as hydrothermal breccias. Weak alteration of the mafic volcanic country rock is present as diffuse feldspathic fractures and minor chloritization. A fine grained dike phase consisting of equigranular quartz and feldspar appears to be sericitically altered. Minor fine grained pyrite and trace sphalerite and magnetite is disseminated within the QFP. Pyrite is also within narrow veinlets that form the cores of alteration fractures.
8.4 Metamorphism and Deformation
Rocks in the area indicate amphibolite grade metamorphic conditions as indicated by amphibole in the mafic volcanic units. Garnet was the only alumino-silicate indicator mineral identified on the property. Chlorite does occur along with amphibole in the mafic volcanics and is pronounce adjacent to the Armand Creek Quartz Feldspar Porphyry.
The rocks have been strongly deformed as indicated by elongate clasts (in plan) in both the hydrothermal breccias and conglomerate units. Clasts do not appear to be elongated in the plane of foliation. Exposure was not adequate to allow mapping of geological structures such as folds or faults. Magnetic data was useful for interpreting the position of diabase dikes but the data does not indicate any major fault offsets. Magnetic contrast in rock types on the property are not sufficient to distinguish fold patterns.
Elongated quartz phenocrysts with the ACQFP indicate that it has be flattened. The overall shape of the ACQFP is lenticular and does K does not appear to be folded.
9.0 GEOPHYSICAL SURVEYS
9.1 Introduction
Approximately 4.4 kilometres of induced polarization (IP) and 13.0 km of magnetic survey were performed on the North Limb claims. One four man crew consisting of Noranda Exploration Company. Limited (no personal liability) personnel J. Maclsaac. D. Hancock, L Cross and H. Palomaki performed the work during the periods November 27 and November 29-December 2. 1994.
9.2 Instrumentation
9.2.1 Magnetometer Survey
A Scirrtrex IGS proton precession magnetometer system was used. Total magnetic field readings are taken with a precision of 0.2 nT or Gammas, although the accuracy is generally +I- 5 nT. Readings are corrected for diurnal variations using an identical recording unit set up as a base station in a non-anomalous area. Base station readings are taken every 30 seconds unless large or rapid variations are anticipated, in which case readings are taken more frequently.
For this survey base station readings were taken at a 30 second interval. Survey readings were recorded at 12.5 meter intervals along the line.
9.2.2 Induced Polarization and Resistivity Survey
The Dipole-Dipole survey was performed using an IPT1 transmitter, a 2.5 kilowatt Honda generator and an ELREC IP-6 receiver.
Survey parameters were 50 m dipole separations ("a" soarings) with readings recorded at six receiver separations (0=1 to 6). Figure 3 shows the plotting convention used to plot 'pseudo' sections which present chargeability and resistivity results.
IP chargeability represents the voltage retention capacity, or capacitance of the ground. It varies with metal, day or graphite content of the ground, grain size, and the degree to which grains are inter-connected. It is measured as an average of ten "windows' or time slices under the voltage decay curve of the ground being surveyed. The units are millivolts per volt (mV/V) or milliseconds (msec).
IP resistivity is a measure of the electrical resistance over a linear distance of the ground. This varies with metal, clay or graphite content, but is also sensitive to the bulk composition of overburden, bedrock and mineralization, and can be used as a lithological mapping tool. It is measured by combining the voltage measured between receiving electrodes wrth the current transmitted at the transmitting electrodes in a two dimensional approximation of Ohm's law (RSV7I) that is represented by the following formula:
Resistivity = pi * Voltage * n " (n+1) * (n+2) * a Current
Where pi is a numerical constant approximately equal to 3.14159. 'n' is a multiplier On this case 1 through 6) that represents the distance of the receiver electrode pair from the transmitter electrode pair and 'a' is the separation of the two electrode locations in the receiver
and transmitter electrode pairs (please see Figure 3). The resistivity units used for plotting are Ohm-meters.
Figure 2
Dipole-Dipole Arrayna
rfi
Plot Point
9.3 Interpretation
Line 14200E: Much of the survey line is affected by a near surface clay layer, however resistivities below this layer are sufficiently high that it is expected that 100 m or more of depth penetration was achieved. Narrow resistivity high anomalies occur at each end of the day layer.
At 10100N a moderate strength, well defined chargeability anomaly is present. The source is >50 m deep and good depth extent is indicated. There is no corresponding resistivity signature.
Line 14400E: A small portion of the survey line is affected by a near surface clay layer, however resistivities below this day layer are high enough that it is anticipated that MOO m depth penetration was achieved.
A single chargeability anomaly was deteded at 10050N. The anomaly is shallow and narrow and is not associated with a resistivity signature.
Line 14600E: A single chargeability anomaly was deteded at 10000N. The anomaly is shallow and narrow, but good depth extent is indicated.
u.o COLLUSIONS AND RECOMMENDATIONS .
10.1 Geology . .: ^ - . ' .
Similarities between the Armand Creek Quartz-Feldspar Porphyry (ACQFP) and the Moose Lake Porphyry associated wNh the Hemlo deposit are Naled below: !
(1) Early microcline event followed by Intense sericitic alteration within the core of the stock. Abundant tourmaline Is associated with sericitization.
(2) Green mica associated with felsic stocks.
(3) hydrothermal brecciation associated with felsic stocks.
(4) Small size dimensions, less than 5 km long, less than 500 metres wide. Both stocks appear strongly flattened but not folded. '. ' .
(5) Evidence Of multi-phase Intrusive activity with intrusive events predating and post-dating alteration events. . :
Mapping and trenching concentrated on delineating the ACQFP on the eastern portion of the property. In this area the Musher Lake Pluton has Intruded along the southern contact of the ACQFP. effectively removing the potential for mineralzatlon along this contact. Trenching was successful. in exposing complete sections through the ACQFP and the potential for mineralization In this area is small. Sampling results of the surface exposures of the ACQFP In this area has been disappointing. Additional mapping of the remaining property area would provide the Information necessary to evaluate the potential for additional porphyry systems.
10.2 Geophysics
The anomalies detected at approximately 10000N on all three survey lines represent a well defined target. Amplitudes are higher on Hnes 14400E and 14600E. but this Is probably because the anomaly Is nearer surface. Where the anomaly Is near surface Its character is clearly narrow. The best place to test the target is on Hne 14600E.
. Respectfully submitted,
Hemlo Gold Mines, Inc
-f^/}Paul Johnston Geologist Superior District
Hemlo. Ontario March 0,1005.
APPENDIX l
Assays, Whole Rock, Multi-Element Analyses and Sample Descriptions
uLA
B^t^
oN
OR
AN
DA
EX
PL
OR
AT
IVE
CO
MP
AN
Y.
LIM
ITE
D
PRO
PER
TY0
PR
OJE
CT
NO
.
1697
6
l W
Nu
- Olfl
e.
. Yt
dow
. R
tld
CER
T. N
O.
SAM
PLE
#
GR
ID R
EFER
ENC
EC
FA
ST
5
.'/)f
/l
N.T
.S..
DAT
ED
/ C
SA
MP
LE
RE
PO
RT
. D
ESC
RIP
TIO
NTY
PE
WID
THA
SS
AY
S
/l /
-f.
CO-O
RDIN
ATES
8AM
PU
R
ro
J./X
m.oc
c-x
(m.
H3
10••s
wt/
c/
'•/x
l/ l/ff
M ML?
lA
n n (1o •*
f -a
:r '"
-Tin/ i
*V
.W
Nor
n fe
rn,:
C:U
onn,
\tam
pf^.
fmi
i vj y i. o X "J' VI I/S l l IA l
o o65 ol 5
o-,-
8
z o
sio p S S
1 o"
ojcQa.
1
ii
IOCO CM
O)
NALYSIS
u. 0LU
CERTIFIC
g,^ O4
rt Q,
Q Di K Di
W Di
S Di D.
n) Di m Di
H O H of
M Ol-l c*
SH a-
O•Hea *Y
Pi Uu a w oPi U
SAMPLE DESCEIETIOU
o o o o o
o o o o oT HHHO
O O OO O
o o oo o o PI r-o TPI HH T
LO m in o in o PI in
o o o o o PI in
V
09 |v PI T CO
rv rv as oo o o o oo o
m ri oo H in in orv n
nmoTH
n o r* o riT fi PI fi f)
o o o o o
o o o o o o in TO rvrv T HO o T T T T rv
T T T T T O O O O OPI PI PI PI PI09 O9 OC 09 09 O O O O OPI PI PI PI PI
oH PI T in H
1 1 1 1 1 PI PI PI PI PI
1 1 1 1 1 r" H HH H bi fH Su EH (b
O O O O O
O O O O O 09 PI 0009 rv
oo o o oHHHHH
-- : ; :"'
O O OO Orv rv oo n
o in oin in ' oin ino T-.
oo oo oino ooo oTPI TO T
oo oin o OH ori rv
oo oo o o o oo oHH H
TO oo in mm ononoHHH
r- o orv o PIO PI T PI
OO 00 0
o o oo o
o o o T o ooo |vo rv
T T T T T O O O O O PI PI PI PI PI
09 09 00 00 00 00 OO 0 PI PI CNPI PI
H 03 -1 fi OH H
1 1 1 1 1"i ri n n n i i i i iHHHHH [u IH fu Cu tu
O O O OO
o oo o o o *9 rv mooH
O OO OO
o o o oo m ri o ri rv T fi fi PI fi
in oin o o T rvm oo T
o o o oo09 PI rv TPIin in T TT
o mrv ooo oo UIT no
o o o o o o o o o o
onoHo-*-^-*-*
noo PIO nPIPI PI PI
0 OO 00
o o o o o n THnoo HPI no rv rv rv rv o
T TT TT O OOOO PI PI PI PI PI
00 OOOO 0009 0 OO OOPI PI PI PI PI
H nHin M nT inn i i i i i m n n n T i i i i i HHHHH
O O OO O
o o o o oOOO OO 0
HH
0 0 00 O
o o o o orv in o 09 o H n nPl n
H
in o o o in o n PI os fi
T m n n o m T in H T
in o o o coTPI TOO
OOOO O o o o o o
o rv o n fi m H o rv ri
PIHHOH
TPIHOPIn n nm n
o o oo o
o o o o oo O rv H in
O O O T Orv rv tv o r-
T T TT T OO OOO PI PI PI PI PI
00 09 00 CO 00 O 0 OO O PI PI PI PI PI
T 00
1 l 1 1 T TT T 1 l 1 1 HHHH Ut fu bj tu
OOOOO
OO OO Oaa rv aoo9 ci
OOOOO
OOOOO OO PIO T
oo oin o
OOOOOHH PI PI H TO TlflT
OT Tino
aoooo oOOOOO
OOOOO O HHOPIO
H H H PI H
o o OD o inPI PI PI T PI .
OO OOO:
OOOOOninoonOHPIOPI
TT TT T OOOOO PI PI PI PI PI
0909 00 00 00 OOOOO PI PI PI PI PI
rv 000 TPlPinn i i i i T TT T
1 1 1 1HHHH
u CM Ui Ut CM
OOOO l '
OOOO " 'oOPIOl H H
OOOO
OOOOrv o PI rv lOPI VT
mom m1O fi T ^
OOOOo TOO rv rvfiOT
rv OHO o r- o o
OOOO OOOO
H
T oin o
PIOOH
0 TO fM nPlfi T
ooo o
OOOO x- O) PI H rv...;?^
*^9^A
T T T T:. .-.-::::: 'y :;:: OOOO ::...-::? '" PI PI PI PH \ ...::.
00 00 00 00 : OOOO ft PI PI PI PI ... ^f - '-'..
•*:"'' .-.-y'' 'y-
i PI n rv "': ...III :: •••:: . ,: .
in in m i ..-.-.H H H ;i- :
u Cu Cu (M
•i: H H H H ..::: ':: l 1 1 1
: : v: Ul Ul Ul Xi •i' -: :- 1 1 1 1
: -::.::: vi Ul KJ Ul
"'\.*frC"\
•:-. .^" * 10 IO 10 10 f.-' O O O O
':-. CD CD CD CO
.y:" - \ KJ K) 10 10
\ .-y^' ' :;:"~
; Ul Ul Ul Ul
H'HHHui o m Xk
vi UIOO
UlOOH
Ul UIUI vi OO vi O
o oooooo oUIXkHKJ
..o.
?SS5
H.H.
OXkOlO 1- 0 vi vi
.-' Xk Ul 10 O O OKJ vi
/k A
O OOO
o o o oOlHHIO
4k vlvlUI
Ul Xk H 10
' V; . . " o o o o.'-.J ' ' H HO H
- , : . ' vi o CD vi
n| rq n| lq n HUH rt^ i i i i i
Xk XkXk XkX.
UIUIKJ KJKJXk o co vi x.
X;K) 10 IO 10 10 O OO OO CO CD CO COCO
KJ KJKJ KJKJ OOO OO
Ul UIUI UIUI
..'ft
:ui vi oui o" Xk H vi U O
CO O vi COO
HKJHHKJ
Xk UIUI vi vi
oooobO OO OO
K) IOO HO
O K) O UICO Xk H CO vi Ul
KJKJKJ UIH
H KJCO XkUI
O HOOO
W KJXk vlui IO Xk Ul O vi
y\ y\ /v.
OOO OO
o o o o oHIOHHH
UIKJKJUIXk
O vIO 00 Ul Ul Ul vi O Ul
00000
OHO OH
iq n] iq nj i^
1 l l 1 1 Xk XkX. X. X.
H H O O X* CO Xk
10 K) KJ K) KJ O OO O O O COCO CD CO
KJ K) KJKJ 10 OOOO O XkXkXk XkXk
H UIMUI Ul 0
HHHHH O vi O Ci 0
O Xk CO vi O Ul Xk OO CI
Xk Ul Ul Ul H
Xk Xk vi H vi. H co o ui ui
"b oooo
0 OO 0 OHHHHKJ
HXkO OUI
OOOO OUI CO vi KJ O vi
HUIHH KJ
UIHO O CD CO Xk vi CO O
HHO OH
0 vIOOH Ui OO vi o
y\
O OO O O
OOO OH H vlui O vi
...M,.
CO XkO vi Ul0 HO 0 KJ
o oo o oOUIHHH O KJKJ H 0
HHHHH i i i i i
Xk Ul Ul Ul U
HUl Xk Ul KJ Ul HU)H
KJ KJKJ KJKJ OO OO O CO CO CO CO CD
KJKJ KJ K) K) OO OO O Xk Xk Xk Xk Xk
UIUI UIUI Ul
UIX. O vi o
Ul vi OO KJUl O OO Ul
XkHHHUl
UHHtj Xk CO WO vi 0
OO OO O
OO OO 0
1,,~HO XkXk CD vi CD CO X. CD
H Ul KJ Ul H
UICO O O Ul COOOHH
H..S
HU XkXk CD CO O UIKJ Ul
A y\ /k
OO O O O
HO O O O
KJUI UlXk ui
HO UlO O OUI H CO Xk
00000
O O OH H OUI vIO KJ
*q nj hg pq IT H HH HI- II i i i
Ul Ul Ul Ul U
H HO wh- 00 H
K) KJKJ KJKJ O OO OO CO COCO CO CO
KJKJ KJKJ K) OOO OO
Ul Ul Ul UIUI
Ul O Ul HUl
Ul OCO OXk CD UIUI X. O
K) UIKJ OK)
Ul vlUl OO O O vi HUl
O OO OO
O OO OO
KJ Xt KJ OKJ
Ul CO W vi O vj oo KJ O O
HKJKJUIKJ
CD vIKj UIUI O CD O O O
'0 KJH OKJ
CO XkXk HO Ui O O O X.
O O O O O
O O O O OH vi Ul HUl
Xk UIUI UIUI
O Ci KJ Xk O KJ O O Ul O
O O O OO
O Ul O O O vi vi vi Ul CO
1 1 1 1 1 1 KJ KJKJ KJ KJ
1 1 1 1 1 H Ul X. KJ HO
KJKJ KJ KJKJ O OO O 0 CO CO CO CD CO
KJKJ KJ KJKJ O OO O O
Ul UIUI Ul Ul
H 0 vIO vi CO
KJ CD O O O Ul HUl O X.
H Ul CO H O CD
KJHKJO Ul KJH UIX. CO
O O O OO
o KJUI ui roH KJUI O KJ
HH KJ COO 0 O
0 vi CD vi Ul -J OKJ OH
KJOO OHK) X. H O CD Ul X. O KJ O
KJH KJH KJ OO KJ vi
O COO Ul O O CD vi 00 vi
O OO O O
KJ Xk O Ul vi
KJ O O O O
o UIKJ o viO O O H Ul
o o o o o
SAMPLE DESCRIPTION
O hrfO M O M W *rJ
H) 3* S* C-fr
dP If H" KJ O LJ
ovi OPIO
Cr203 %
Fe203 4
KJ O
dPS j 0
o* g
O
Pi KJ O
t: t
: J
KJ O U)
CERTIFICATE OF ANALYSIS A9428541
Wlrrmj
.jilix Chemex Labs Ltd.^:^V'!?.B..ii^^^ An! "Vlcnl Cncrn| st9 ' GeocJwftisls ' Registered Assayors
':^;:i;^5iSiil^^'^ 212 Brooksbnnk Avo., North Vancouver i'KlaK&ZZ&f JL. Bntish Columbia, Canada V7J2C1
^/-uii-ASr' PHONE: 604-984-0221
To: NORANDA EXPLORATION CO, LTD. Page Numbor 1-A BAr venwirc jw Tolal Pages 1
MARATHON ONTARIO Cortilicato Dato20-OC T-B4
POT 2EO I|WOI(:|! No 1-B42854 1
POT2EO P.O. Number :
Project : 529 Account :
Comments: ATTN: JOHN LONDRY CC: JOHN SULLIVAN
I.YH-1-VHA connI,IHOO:O tiK/07/ni
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
1070 LITHIUM DRIVE. UNIT 2THUNDER BAY. ONTARIO P7B 6G3
PHONE (807) 623-6448FAX (807) 623-6820Page l
NORANDA EXPLORATION CO., LTD. Bag Service #8 Marathon, Ontario POT 2EO
July 26, 1994
Job #944710^
Project #505
Sample #30ay
123456789
1011 Check12131415161718192021 Check2223242526272829
Customerx *\
^1697-Ht^697-1 1^697-j|-1697-Kl^1697-Ll^i697-HJ182 3 -W*1823-V
- 1823-U,1823-T1823-T -1823-S o1823-R -1823-Q A823-P -"1823-O ^1823-N '1823-M,1823-L1823-K1823-K1823-J1823-11823-H1823-G1823-F1823-E1823-D1823-C
Goldppb
1019214159
137^^<59
11<5
142<5<515108
20^8
X5<5<5<5^1656<5
GoldOz/t
^.001<0.001<0.0010.0010.0020.004^.001<0.001<0.001^.001<0.001<0.0010.004<0.001^.001<0.001<0.001<0.001<0.001^.001<0.001<0.001<0.001<0.001^.001<0.001<0.0010.002<0.001
Certified By:
LAB
Q ,t*.f*
' i.. A
TI'-.
.j iV
i-\.
i
CER
T. N
O.
NO
RA
ND
A E
XP
LO
RA
TIO
N C
OM
PA
NY
. L
IMIT
ED
PR
OJE
CT
NO
. JT
O*r
PRO
PER
TY
—
GR
ID R
EFER
ENC
E _
^_
__
_^_
__
__
W
1823
'i.
,.''V
WU
. O
MIc
*
SA
MP
LE
RE
PO
RT
N.T
.S.
DATE
SAM
PLE
#D
ESC
RIP
TIO
NTY
PEW
IDTH
flpb/n
,C
O-O
RD
INAT
ESS
AM
PU
R
1 .
" tm
ri .
f '''
.. n
r^
,**
/\ :
* ••
'•••
•*'
1 t
J
S *
*
"l
1 Vi^
/'.i
.x/
-fj'"
) Vi/
'P
r*'
X/ 1--
'* /i-
A*
t s*
... t
,f*j-t
lsl^
-f u
t S.
%XI
M57
7570
A: J
r.A
u/x
it,S
W 5
80S
TA
Mft
6~-
t, '/o
5*89
3 09
Hs*
/*A
-n5.
77
t^i
t r/*
-X
5*87
73Q
S&O
9 VZ
O
2056
7875
"sr
rM
sr
Mlo
sr
no
's. r
n aA
uA/
-W
2.
rea
srrs
a
OLA
f^L
A-C
xvC
AA
x j
t5
^69
/4o
'L,-
V3
c; c
: c;
w.
n: C
jQem
ulN
wu
Foi
m:
C/f
enm
Mn
np
rtp
.fm
i
r
'
NORANDA :- ^XPLORATION . COMPANY l ; MTE(-flSBE SAMPLES " " -' "' ' - *' ; .
Property i Ao^^oa **1 T/Renzl) ' . . - ' . Hste Number* c) -
SAMPLE
/-r- a -y*i
(V
-3-H
-S
~6-7
-S-7-/o
-x/
' .
FROMmo tret
.'
-
-
-
.
*
-
TO
/-f
/•O
/-o/^o- 70
f,o^/.o .
.^/'O
/.sI'l.
'
-
-
m
WIDTHmorro*
*fe
tfh^9-fa^lo/Q'
1?^)
•^
3 r;- '- :--r"i ••-.' .- :" . ' '
. .'•-..-.-^ -.J-- .
. ^ ' ' *i - " - "* ' ' "
- page'"/Au Assays (grams/mt)
-
V&
ivf^
favZ
t -
Au
^A^Ao
VQ;
flu
'
--
'
-
m
-
-
*
*
- . .
-
- -
-
-
'
-
-
B .
-*-. .-i
*
m
-
-
\
'
.
t
- -
-
Final^o'K
s*1***At o-ffc'
m
. - -
VoU. r •sA^P*
ly**C ' 1
f pOf^
^H. i#~ - 1 ' - - f Q0 \* ^ l
P*l
ojj: s/
^^
*
•'
.
*
,-
-
.
--
—————
:,. ;.' .'.
- " . , . - * t
K rbf . X- PY
^rXei
i
. - - ' '
-
- - - -
.r
-
.
.
!^- "
- -'
-
.
.-/,
ACCURASSAY LABORATORIESA DIVISION OF ASSAYIAUORAJORY SERVICES INC.
1070 LITHIUM DRIVE. UNIT 2THUNDER BAY. ONTARIO P7B 6G3
PHONE (807) 623-6448FAX (807) 623-6820Page l.
NORANDA EXPLORATION CO., LTD. Bag Service f8 Marathon, Ontario POT 2EO
July 26,.1994
Job 1944731
Project f505
Accurassay
123456789
Sample fCustomer
9957-A 9957-B 9957-C 9957-D 9957-E 9957-F 9957-G 9957-H 9957-1
Gold ppb
Gold Oz/t
^<55
<5^^<5<56
< 0.001^.001<0.001<0.001<0.001<0.001<0.001<0.001KO.OOl
Certified By;
:^u :ACCUKASSAY LABS UTD.- 2/ l
! OACCURASSAY LABORATORIESA DIVISION OF ASSA Y L AGORA TOR Y SERVICES INC.
1070 LITHIUM DRIVE. UNIT 2THUNDER BAY. ONTARIO P7B 6G3
PHONE (807) 623-6448. FAX (807) 623-6820
Page l
NORANDA EXPLORATION CO., LTD. Bag Service #8 Marathon, Ontario POT 2EO
AccurassaySample f
123456789 Check
Customer
9957-J 9957-K 9957-L 9957-M 9957-N 9957-O 9957-P 9959-A 9959-A
July 29, 1994
Job 1944742
Project #505
Gold ppb
28
<52728
Gold Oz/t
<0.001 <0.001
<0.001 <0.001 <0.001 <0.001 ^.001 <0.001
\ Certified By;
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC
- ;\
1070 LITHIUM DRIVE. UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448FAX (807) 623-6820
Page'l
NORANDA EXPLORATION CO., LTD. Bag Service f 8 Marathon, Ontario POT 2EO
October 11, 1994
Job 19441152
Project f 529
Sample # Ac curassay Customer
123456789
1011 Check12131415161718192021 Check22232425262728
FT-2-3PT-2-6FT-2-7FT-2-8FT-2-9FT-2-11FT-3-2FT-3-4FT-3-5FT-3-7FT-3-7FT-3-8FT-3-9FT-3-10FT-3-12FT-3-13FT-3-14FT-3-15FT-3-16FT-3-17FT-3-17FT-3-19FT-3-20FT-3-22FT-3-23FT-3-24FT-3-25FT-3-27
GoldPpb
^<5^5<5<5<5<5<5<5^<5<5<5<5<5<5
. ^<5<5<5<5<5<5^<5<5<5
GoldOz/t
XO.OOl<0.001<0.001<0.001 CO. 001<0.001<0.001XO.OOlKO.OOlX0.001<0.001<0.001<0.001KO.OOlKO.OOlKO.OOl<0.001<0.001<0.001X0.001<0.001<0.001<0.001<0.001^.001<0.001<0.001
Certified By:
APPENDIX II
Statement of Authorship and Qualifications
The author of this report is Paul Johnston, l conducted the geological survey starting June 14 and completing on October 24,1994. My mailing address is:
P.O. Box 3197 Manitouwadge. Ontario POT2CO
l hold a B.Sc. (honours. (1987) from Carieton University and an a M.Sc (Minex. 1990) in geology from Queen's University, l have worked in exploration and mining continuously from 1987.
Ministry ofNorthern Development Report of Work Conducted
After Recording ClaimOntario
nedon ooieeM on ttJa form la obtained under Ae authority of tie IMngActTMalnfeniiaBMeXbeuaedton ermrid be dkei^ad to tt* PiovindeJ Managw. Mbiing LMd^
Sudbury. Ontario. P3E SA5. telephone (70S) 670-7284.
fnatructlone: - Please type or print and submit In dupicato.- Refer to the Mining Act and Regulations for ir
Recorder.- A separate copy of this form must be complel- Technical reports and maps must accompany- A sketch, showing the claims the work is assi
2.15930
42C13SW0008 2 15930 WABIKOBA LAKE 900
W\?^tv W.
VUV;VoU U, Aw
Work Performed (Check One Work Group Only)
Physical Work, Inducing OrMng
RehaWMation
Other Authorized. --*- WOnc
Assays
AssionniSfit fioni
Total Assessment Work Claimed on the Attached Statement of CostsNote: The Minister may reject for assessment work credit afl or part of the assessment work submitted if the recorded
holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.
*ersons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)
r m nttttm a tt ei am tfhel **——-— -** — *~" lantai m m ail * O^.^ fc*—A— ai*- 4 ^^-^ ——— — —— — SlUIICelUuil Of DWIonCMi VIIOTBvC 560 NOtO WO. i OH fvVVFW
y Vwl at th* tbm in* covorad in INa woikraport wm raoontod In tfw cumnt hokJar'a name or haM under a banalldal by Hw cumaot facotdad tioMar.______
of Work Reportl certify thai l have a personal knootedgo of the facto set forth in this Work report, having performed the work or wttneaed same during andtor after Ma completion and annexed report is true.
a Pewon wfjfwyino
Office Uee Only
Details for (fork Reoort l Sil PC* T 35.00 2
1 Work Report! for Applying
Reserve
1
Claii Nuiber (see note 2)
TB 0.650.898
TB 0.650.900
T8 0.651.397
TB 0.651.398
TB 0.651.399
TB 0.651.400
TB 0.653.301
TB 0.653.302
TB 0.653.303
TB 0.653.304
TB 0.653.312
TB 0.653.317
TB 0.653.318
TB 0.653.319
TB 0.653.322
TB 1.010.503
1 of i lvalue of Assesient Clan! 1 (fork Done Units! l on this Clan
i ri
11i i i t1 —— i1
i
1 f
1 j111111
l
1 ! i
1.313.00
1.319.00
1.319.00
1.494.00
1.961.00
1.517.00
1.253.00
1.253.00
1.253.00
1.253.00
0.00
0.00
0.00
0.00
0.00
1 ! i 1. 502.00l l
value Applied to this Clan
- ^
JB
————————
300.00
400.00
400.00
400.00
Values Assigned froi this Claii
i
- j' .- s ai. 351. 00
! 1.517.00
1
i
1
1
400.00
1
TB 1.010.504! i i i 1.533.00 i ii * 1
1 !TB 1.010.507! t ! 1.7E3.0G il 1
j i IB I.OIC.SIoi 1 i/ 2.037.001 t it
1ii
iii
iB 1 .1*4.233! * I ! C. CO i i iTB 1.174.290
J 2- iTotal Nuiber
of Claiis
* CAA AAi . Duu . uu
4 ! l C. 00 1.600.00 1 111
i:
Reserve:Kork to be Claned at
a Future Date1.319.00
1.319.00
Q 1.319.00
1.494.00
1.253.00
1.253.00
1.253.00
1.253.00
1.502.00
1.533.0G
1.763.SO l
! 1.622.00 ! 475.00 !i l
-LRE CF! ve ft "1
i !1 1
li J ARR 3 193oi i i ii i i i!
i ii 1 ii i
i 1 i
i
i1
i
1 1
! i1 t
1
"~ i
20.392.00 ! 5.100.00 ! 5.100.00 15.732.00 • it iTotal Value Vork Total Value Total Assigned Total Reserve
Gone Vork ADD lied FroiCredits you are claning -n this report iav be cut back. In order to uniiue the adverse affects of such deletions, olease indicate froi which clans you wish to priorite the deletion of credits. Please urk ixi one of the following:i. p Cred-ts are to be cut back starting with the clans listed last, working backwards. j
r-i C'V ! 9 ! 1 Trail:*: ara i n ha ri:? ha.-i s.-^allv .v.-er all rlaiBc rnrfi:nait : r. Ht-.s ran.irt .if uari- ^-! 2-U3. j; Credits are to be cut back as pnonzec on the attatched aooerdix.
4. !x! Credits are to be cut back starting with the clans that have reserve credits.i LJtin the event that you have not specif-ed your choice of priority, option one will be ispleseate-j.Note 1: Exaiples of beneficial Interest are unrecorded transfers, option cayttits. Kiorandue of agreeientSPeteT.
with respect to the unira clans. , ro Note 2: If work has been oerfonea on patented or leased land, olease coiolete the following: en
*- : : :5j
to o ^
TuateII certify that the recorded holder had a beneficial interest in 'Sigratjre !the patented or leased land at the tise the work *as :er'oried. !
t3T705 268 9572 HBMLO TIMMINS 81003
St*tlMn0iit off CotteCvodtt
des ooOts aux fins ducrMHd'dvaluatlon
Mining ActfLol sur In mines
Transect*!) ttoM* detrsntacDon
' sry.2.15930
of thett*icajdon Mi fcm to cento*l undsr Bit eustasy
Mi costcfon anouuan vwu dt te Lot wr I
dsmlaSS&Davatapmam and Mnea. 4*i Roar. I9a deer Sveet Sudbuiy. ante*
u c**w pflM*nCi*jf OM tMnins flvMMSy mlntoblra du OantappMiMM du Noid at dat Mbm. is*, ma Oadv. 4* tap, Sudbwy
1. Olraet Coftts/CoAt* directs
MaJfHfoauvra
SupaivWon *ur to tamh
Total Dbaot Coal* Totsl dec eoOta
T( ToWotaM
2. Indirect Costs/CoOU One Nwwvot corti w not
Pour It raoboiraadMni dM travwB dt r|fi coott fndbKtt M MM DM adnWblw an tM qu*
-^s-
Swb Total of Indirect Coets Total partW dee eoOts tndbeets
IpMMMdMOI
(iMrivfDinecMidASwMM* dtHBjslr--:
Tto f rdsd newer w* be lequJied to venHy exiof costs iriHn 30 days of s reqiiMt tor
is not fnsda* *w UfewlBr ffsy isjMt for alM. SI Ml vaVMcadon nlMl W UN pu* dn imvR d*4
pmt ra|rtBrtout
i. Wort IBedwmiinti^yeajs of completion to dslmed st lOCWfc of the above Total Value of AtttumtMCnOL
t. Lwirsvauxde^wesdanslMclwawBwrfrtnllewsAivwnenlsom ren*OMsfsA100Kdslsvtfsurtab*susffl6flkimissdbcrtdld's^^
2. Woffcffladthree,foirorllveyeareattarooinplatianfaclaJrn*dSi Sim of the above Total Value of Assessment Credit See
2. LMMvauxdepoefeirofe.4uatieoMeinqBisi out lembounea i 50 * de to vtfaur tofato du crfd* d'eVahMtton
x 0^0-Vatour tooto du crtdld-i
x 0^0
Vertfylng Statement of Costs
vera fccuned wnee eonduoflhg anassmem wortc on ihe lands shown m fte accompanying Report of Work tarn.
______f em euthorhed
AtbBststfon ds I'ttst des coots
/aoeita par la present* :que lea montema Indkiute aont le plus exact poasMe et quo oaadepeneaa ont M engage** pour effiaduer tos traveux d*evaluatton
a qu'i tftre de.dam l
. J* sub autortsAI Jlk^*^ j J l eofflpv**!
nteke Olie oertfflcelton telra OAIM Mteiution.
12 (04W1J Nota : Dw* MM Jomiute. (tot pcrannM. to mwcuSn *ct mms* ui Mn* n*uir*.
OntarioMinistry ofNorthern Developmentand Mines
Ministere du Developpement du Nord et des Mines
April 24, 1995
Geoscience Approvals Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5
Telephone: (705) 670-5853 Fax: (705) 670-5863
Our File: 2.15930 Transaction /: W9540.00084
Mining RecorderMinistry of Northern Development 6 Mines435 James Street SouthSuite B003Thunder Bay, OntarioP7E 6E3
Dear Mr. Weirmeir:
Subject: APPROVAL OF ASSESSMENT WORK CREDITS OM MINING CLAIMS 650898 et *1. IN WABIKON LAKE AREA
Assessment work credits have been approved as outlined on the report of work form. The credits have been approved under Section 12 (Geology), Section 14 (Geophysical) and Section 17 (Assays) of the Mining Act Regulations.
The approval date is April 20, 1995.
If you have any questions regarding this correspondence, please contact Steven Beneteau at (705) 670-5858.
ORIGINAL SIGNED BY:
Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division
SBB/jl Enclosure:
cc: Resident GeologistThunder Bay, Ontario
'Assessment Files Library Sudbury, Ontario
_ - _ -1203259b
1224809203258RCCEiVED
APR'3 1995 MI94444 I|I9444I\\.
- J -Jr--i—"ll l l
~"]ll5T8tt|H07UI |HBTSI9
l T T 1224810
1203256 1154791|22496PkNEGROVE
^*\{ll7e8Sl i
^—l # —J—l 120924812092491207860 --- ---—i
1224804
- - - - -* -H- -.- -nAC!(9!br ! . X1196882
l 1174290 i1203281
1196847
i 1203282 l M97I56 il l !
I20Q356
WORK DONE ON
WORK RECORDED L
•^.OUTLINE OF CONTIGUOUSx —
v-V
M
O
i if
i
LO
RN
A
LA
KE
G
-59
8R
OU
S LA
KE
G-6
11
1830
37 l "i
—V
r "^
Tr-
r-r-
*^9
, i
lil
i it
iS
l 8 )
r53**
*--?--
t-?12
0215
8
1224
805
L' L
1LI
#W
HIT
E L
AK
E (
S,
PT.
) G
-62
3
WH
ITE
LA
KE
(N
. P
T.)
G
-622
o.
sH
zH
S
D *
O
p>
s-)
x
"H
w a
M m o 55 -H a o
^M^
S^
^^
^^
IH
^^•^
^^•^
W
l^
^^
^^
^
^^
^5
^p
^^
^
OD '^^
^^
^••M
^^
^^
k O CD ^^ C m
i 8-
Q.
9:
Ul
-*-
u,
0IT
3
o S-
3
3" —4s
3-
O"
i S
a-
o o rr CD1
Ul 2"
\ c
"U
) 3- CD
-z. 0 IT CD O
CD CD O
"D 3 CD O Q.
CD
Ul O*
-i
s -.
^ —^
3~ Ot s — CD 3) m 0 33 O m aj 3T -T o
S l/l — tQ U-J o" in 5" TT
CD Z z CD n 1
w Ul
0 51 n
o tn
Q 3 CL.
0 n n c o n Ul"
CO c Q Q CD" CD p.
H O Ul CD
ir o LO tr CD CD n 0 3 -o cF
o. —4s O 3 o o" c Ul
Ul O C n CD
Ul
-\ n _ 3 T1 i o o ^ o TJ -D
CD
Q Ul O U)" 3 o -o
88 i
w m Si
y f w m l * li 51 a o
SUBJ s l
0
ETRESSCAL
E NCH g o z Z
CO
!? S
O
^2l
SS
z2?
22
2" z
*<
o
o a
O i-
5SS
SC
EE
5l|
:^? O.2
RAVEL
MITS
FO
ni 5
a
F ^
zm
n
o -
m
SQ
z
5 m z{2
Mso
*l
g n a
m
••5
en - 51
•*m
" o
i•*
m w
^ l
o g
i?S
?!
IB >
W
' 'r -
*x rt
05ff5
>
>O
O
m
m5
B"
O
Sz
c/)
O I en
•O
m 8 O m Z
:? z
o o
25
-c o x
CO i
CA •^
O S2 o o 30
O C/J
s z
z i
ss —
en8
!sm c
en
1 Z
C
3J
jMS
i1
MB
—
——
—
^p
-4
J IS
H
*
21 3
* 5
z5
m
i-
"*
O
Sills
3 *
a i
) en
o
en
a 5
H; S
g
0)
S
^i
^i
5i
C
W
H
Q I
.?r-
wr-
~3)
'*Z
?J
jgc
go
-c-m
;!3D
HajH
*m
JIa
zQ
i-".C
Bi*
l"a^
PS55
SS
f;g
SJg
Z
^n
g
1
C
2 -
Z
"*
D
z
EI
Ci e
n m
aj
0
2 0
fc
w
0
k
m
r- 5
2 c
5
w ^
m
hj•^
5
^"~
^
M Z
Z
-m
o-a
en
k -
5*n
0 ^
m
"
ut
*m "
i y 1 ! ?
\\
m O m O
42C13SWQOOB 2 15930 WABIKOBA LAKE
RES 0.
IP22-,
11.
OJ Oj
T—r" i - -i - r ~T - i - t - i - T - i - T - r - i - T - i- i - i - -t ~ i - r i - r - r - r - T ~t ~ T— i - i - T - i- i - i - r-T - i - i - \ - t T T - i - t - i- T - i - T - r~ T —T— ^ ~
\
i— i_L _L _i - J_i _u--j_ -i— J_ L— i- __L—i——L——
IP.22
RES .0
.11
.0 LO
CHARGEABILITY mV/V
APPARENT
RESISISTIVITY ohm-m
220
89+00 N ^ 90+00 N ( ( JM+00 N ( t 92+00 N ^ i 93+00 N 5 55 55 52 54 51 51 51 5
94+00 N 95+00 N 96+00 Nt -*- *- 97+00 N 98+00 N
0=1 41 ^.11 ^ 41 - 31
5 '('" 7 M VJ
59— -51 47 53 -59 5 51
0=2
0 = 3
0=4
0=5
0=6
41 3^5 52 41 41
51 43 57 51 54
41 45 59 71 99
34 33 41 -31 f
4 7 4' ' J l
^ 99+00 N H li
10 13
13 '.y ' 23
^ 100+00 N ( 101+00 N t j 102+00 N ^ ^ 103+00JN J
20 17 H i 3 43 32 21 21 32
^ It \x^\' v "l 21 li J i ' "
20 j IIV-Vl^l -10 l 5~ x 27 21 36
CHARGEABILITY mV/V
4 i l 7 l 5
55 7 )
5 C 'l 3
li l l 5 l 53
.-59 51/
l
M- i t- 5 5 10 ,, 13 /X; 7 * ' ' l S 'Y* 45 3 '51 / ^' , l i x/ 11i ; f ' ///7 '
ll'/t 1 3 /f JO -Si.// /f X
7 5 y 13 l . I I X^ II -^ / f / l ^~/ ( \ \ \ ^ \VV X
17 ' IJ ' ' 17 ' - IJ 4 17 II N II x 17 ' ' U N - - 3
li" " 14 v\ '3- -SO 13 l 4 } 4 2 \, X^i N-N
l* li H \ vv 2 ' - ' '
0=20=1
0=4
0=5
0=6
89+00 N 90+00 N 91+OON
lik 22k 70K 17k 19k 15k
92+00 N 9J+00 N 14k 9511 3UI
94+00 N 15*00 N 96+00 N 97+00 N 98+00 N 99+00 N 100+00 Nt-.*. -4. *-.***. t.*. f.
73lt ilk 14K Uk l IK 7347 J733 2510 2945
Ifll+OON 102+00 N 10J+00 N*.t**.**t-**-'25 4.11.) 4HJ 50JI 5420 MOI SiOt
APPARENT
RESISISTIVITY ohm-m
r.--2 n^ 1
0 = 4 0=5
0=6
11k Uk .^ 5514
14K ' , ' \
154 , 4JI2 - 7247 v - 15k x I2K , !4IIy - ' i \\ \ i i ' '] 7 123 ^ 1931 ~~~HK^^!*49 ; \ 1 U(
20K -'S MI4 -^- 1* 17K UK \ \ 3002 ~ 5711/f y s ^ \\\ ' ^M7I * SOt ~~ 27K 20K 'UK ^ X K7
'is ~ ~ . l , * Jil,ljk ( IOK 2IK [ 1 *k S 4102
\ \ \ ' /.'4|K Clk ~ 73K ' - 4195
4117 y H41 / ^ 9i5l 71k , 1412 . 2799 1909 , 1010 !MS Uk5 1125 1117 . 121 —— *52 2174 n-1
5*45 ' . Ilk 1*k 20K 14k J 4310 J194 , i?5l 1J4? 4312 - 7214 -, 1M7 , 2 2'.5 , M52 " 1792 0 = 2/ . \ ^ - \ / /i \* i ." - ' ; ' \ \ i --MO l 17K' !7K l I2K ' 5111 \ 4205 1910 l!0| \ 5IJO 4214 ?9|7 7441 l l'32 - 114?
! l ' l ! - ' \ l ~ -' \ " . \ ''~'2k l ?W 15K l 559) ^5IOJ 7144^ l'14 . 7131 5307 5003^ 3173, ^ 5411 -/-15k
17K , \#. s m '7 4727 27r 10*5 , 3I'2 I903~ , ' KW4 b309 ( , IK - 14K
0--1
0 = 4
,lilt 7135 S4I1 l 24JJ IUI 3311 25*5 II7J v 710J 6205 UK o--6
niter
* * *
Dipole-Dipole Arraya na a
* * * * r^D~1* * * * * _L _L.
* * * * * * \
.^930plot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS 10 = 6 WINDOW :
CHARGEABILITYInterval 27., 105!RESISTIVITYLogarithmic 1. 1.5, 2, 3, 5, 7.5, 10...
INSTRUMENTSRECEIVER : BRGM ELREC-6 TRANSMITTER : PHOENIX IPT-1
Scale 1:500050 O 50 1 00 15
RECEIVED
APR 3 K 95
MINING LAND: .
NORTH LIMBINDUCED POLARISATION
LINE 14600EDate : DECEMBER 1994 Property : 505 NTS : 42 D/9 Survey by : NOREX
hemlo goldMints Inc. *J
NCH
p- l - 1 - l l - l ' l l ' T l l 1 I'l I " l l ~ T ' T T I'l I'l I'l l l I I T ' l ' T ' I r
\
i i.i i i i i.i i i i i i . j i i i.i i i . i i . i . i . i i i i . i . i. . i i.i i i i i i i i i i
CHARGEABILITY mV/V
APPARENT
RESISISTIVITY ohm-m
42C13SW0008 2 15930 WABIKOBA LAKE 230
SHOO N 92+00 N- i - - . ^ . i .71 27 lf 4
9.1+00 N 14+00 N 41 4 ? t 5 M
95+00 N 96+00 N 97+00 N l J t j 1 16 42 46
98+00 N 5)9*00 N 100+00 N 101+00 N 102+00 N 10.1+00 N.t-**-*f*-**~t-4**tt*(.t.|*
i l i 5 l C li 14 It 11 M i 2 tt j 9 J 'CHARGEABILITY
mV/V
n=1
0=3
n-e
j 1 12 11, 45 41 41 41
44 55 41' ^"/fi-\:tf^ ) 'V il l l l J/' 2.1 l 1 2 - " 14 j \ S l 4 \ i J I J l( 3 b5i25 J l - l 4
/. S'/ 'l27 21 J 6 y 55 l l ; l li ' 47/11 II ' /, 2 5
V , \ 5 M \ 4 l
. 45 J l '41/74 l l - X 21J * J 5 J 1 2 t l l
J5 ill 47/49 11 ' ' ,, ! 0 X 14
j'l- 41 4 5" - J 5 J 7 J 2 5 t 14 14 14 14 14 7 t Si
\^\\
o-'J
0=6
iJI+00 N 92+00 N 9^+00 N 94+00 N 95+00 N 96tOO N 97+00 N 98+00 N 99+00 N 100+00 N 101+00 N.t*t*-t't*4~* f*--*. t-**-. ^^^.^.|.^**. + **-*-^•l•^*t*7151 1014 7IH 1102 1151 4752 4770 4?7J 400* 44!7 4SU 5147 t7ll I25J *57I M71 7171 MOO 421s j]tO Hit ?WJ JII5
102+00 N IflJ+OO N^,*tt.i.i? 2447 2J69 )I05
APPARENT
RESISISTIVITY ohm-m
2071 - 1157 , 1115 12/10=1 6*5* I4M WJS l *
0=2 W JjIS \ 11k ^
prr} 1511 1527 1117 -" 5515 . 4110 *7)1 304i , 2172 21*7
1i75 - 250*v
Ilk l IMS 27JO -- 2MJ \'l44l ' 2J06 2444 -' J5I4 4541 50J5 75tl •- ' " x x - -' ' " , /
^ SJM 5511 H17 ' IK
47U ,- 5047 ^ IJIJ 7UI *MI x 2HI 2271 U4l . l?2t IS40 JII7 1201
\ 7MI 5125 - 5510 ~- 1'75 15*4 " 14*4 ' 111* 57*7 l ' 100 \\ v J2M - 2120 0 = 2\ \ f i . \ \ i f .^ ' - ' i' i O ; 'i-I2K\ 5S1I 11*5 IJOJ ' IM ( 1*2 /, 515) 1115 ?J'I ^ KJ - 4*71 0=3\ \ i - ' i i u ^ 1 1 \. \ ^ t i - . .v
J77I 7517 ,' 5 705 l 7152 - 1577 4111 . 4211 S 7401 5705 7501 C004 M14 / Uk " 14K 1121 4SJI . 5537 4*22 , 1 704 -- 2304 JU! , ' !H29 7tM - 1511,
7M5 , Mil iOIO l lOK ' *447 (421 477J ^ 44IJ 7370 7S5~) ^ 7055' ~ ", f
H42 Mil 7054 MJ7 1151
tlk Ilk __ 10K IMS Mi 5i57 ' IJS2 - JMJ \ tjl4 -- ilOS 2500 4J21S' f -^ i .' - - ' . s \ - x '1 S - 71 " HJ5 ' 41)01 " 1 512 H25 ^ 5*16 ' UOJ 211J 4417^ . - - . s - x
Illl 5474 74J7 Mil ^ 14K 10K 7iSl - 7111 " HJ5 ' 41)01 " 1 512 H25 ^ 5*16 ' UOJ 211J 4417 ri-G
Dipole-Dipole ArrayQ nq
plot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS 10 = 6 WINDOW :
CHARGEABILITYInterval 27.. } Q7.RESISTIVITYLogarithmic 1. 1.5, 2. 3, 5. 7.5. 10.
INSTRUMENTSRECEIVER : BRGM ELREC-6 TRANSMIHER : PHOENIX IPT-1B
Scale 1:500050 O 50 100 150
(maters)
NORTH LIMBINDUCED POLARISATION
LINE 1440 OEDate : NOVEMBER 1994 Property : 505 NTS : 42 D/9 Survey by : NOREX
hemlo oldMines Inc. ^S
42C13SWQOOB 2 15930 WABIKOBA LAKE
kES
CHARGEABILITY mV/V
APPARENTRESISISTIVITY
ohm-m
240
n=1
n=4 0=5
r- r - i " T - r - i " r i - T i 'T - i - t t t -1 r - i i ' i ' i - r - T - i r - T * i i - r - i t t i " i ' l l J ' i ' t T i i i i - i r i - r - i T -
4. . t --i-- i —l -4 . l -4- . l .-l . i - J.,- i- . L - i-—l - t— l- L - l - i - l - l - l --J— J- --i . l - i-—l —t - i --1 - l— 4 ——l - -1—4 - l .-l . l... L., l . l l . 4. . J - l - l- . t- i -4. . 4—4-. l-. 1-.-,
IP.2J
KES .0
.0
91+00 Nr t -T- t t - t *
64 41 44 46
92*00 N 9.1+00 N t * t * i . 94+00 N^ f 95+00 N ( ^ 96+00 N ( 97+00 N . ^ 98+00 N ( ^ 99+00 N 10 10 75 11 10 21 1) 21 25 l 21 li 1 1
t 1 00+00 N ( J01+OON l 67 15 15
41 57 53
10 Kg* 41 i*ss IDS ^™ M//X/ -2 l -49 -17
i"2 r ':H^ i ^"" 11 - '" 21^ ~^~i t~~t 1 1 r~ J * r—; 11 r " 5 J" -15
^ 102+00 N ( ^ 10J+00 N j 104+00 N ^105+00 N11 6 56 Si St 51 57 67 63
13 v x 2 3 59 46 -35 54 57 77 61
CHARGEABILITY mV/V
7 -7 a^ 54 y*y.,\1 -^ -. 1 7 y.. , (O//x 10 y- 4 l y . U ^v 2 3 59 46 -35 54 57 77
, 4 5 - ' S "^"54 l ~ f~\ ' j'l /'li' U - ['o 11 \V 1 t ^ S l 6 "5 6 41 49 \ 6 l 71( i C J S .' . i V \\ - \ \ ' \l l
45 r 6 4 ' 42 11 13 4 31f~ -^.
ii i" *i^ 14 ; 4i
^ \ \ l l l l f \ 4 li 17 l l \ 4 7 \ l 7 5 9 — ' 5 l 43/71 19 62
11 41 4 l ' l l 25 2 n-6
^ 91+OON 4411 (710
H92+00 N-, -f * -
1115 (107 7119
9J+OON ^ *- ~ t - *- 94+00 N 95+00 N^ 96+00 N(711 5110
i 5610
4117
Till MJ2 7111
4777
1711 .. JJ21
5111 (^TM5 ^ 2152\ \ \ ~^\ ~^
4*11 1075 (UK x xlWI
7011 5101 7J1l\ 12K
5244
1511
5114 4101 4172 5251
^97+00 N
(111 7191
^ 98+00 N
74W 1570
99+00 N-*--*- *-
10K UK
100+00 N-t- ^-*-
1107 5921
101+00 N-^-^-^
Uil Jill
102+00 N--* * *-
1554 1114
10^+00 N*-i- -*
4121 TM
104+00 N-*- -i— -*
1110 1141
105+00 N-*--*---*-
7161 1142
1170 (7S5
Sill
5411 (111 (Oil
5057 7(17
lZS — III! ,- 1020 2154 , 1511 4041 v
Ull — 1101 UJJ — 1214 ~"~ 1512 M75 f (442 ^ 4111\ / ' 7
4017 KIM M21 -- 4M4^ 44Z5 ^ Sill ,
4415 .. 4711 ' (lit S515 (007 5105 /I170
MM
Sill -. 151! Sill 4(11
1010 ,, 7150
\ \1070 I4K\\
(154 mO I5K
SIM (713^ (420 (til 7001 5515 7511
"TIM 1071^ 1110 ' 1400 ^ 6111 7IN
7155 -^ JM , -" 15K
(711 ' , 1IK I7K s (191' J l Vi// •^ 1 4K 20K
6524 1554X X \ \ "li,
5711 (711 5136 l 10(4 V 4167^ VV-' \\
1114 2511 - - 2517 - 4111 , 5131 . 1111
2441
H56 ^
1071 ' 1U
1IK
14K~"(™/.
17K ' Sill
1411//
7415 (141
7511 5145
5105 4107
Sill
4110 7750
W\(M44 — 4111 \ 1490 . x 17St 1741 ,' 12K
(111 5111
(110
11(3
7M4
5506
APPARENTRESISISTIVITY
ohm-m
SIM 1411 2171 — INI ^ 17H " 1740~
M5I f 7141\\ - J '
- 8516
"\!\ 1041l \ -
- 14K ISJI
MM UK
7011 7075
(MS
till
1211 5177
1115 \ 1500 \ 4746\ \\ \\ /, ,- - \
5915 ^ 4014 x 1155 ' ' I IK^ 1715 ' 1111
15K 1011
I4K
n-4
n=5
RlterDipole-Dipole Array
* *
* * *
* * * *
* * * * *
* 4i * * * 4
15930plot point
DIPOLE LENGTH : 0=50 DIPOLE SPACINGS -.0 = 6 WINDOW :CHARGEABILITYInterval 27., 105!RESISTIVITYLogarithmic 1, 1.5, 2, 3, 5, 7.5, 10...
INSTRUMENTS RECEIVER : BRGM EL TRANSMITTER : PHOENIX
Scale 1:50(
RECEIVEDIPT-1B
APR 3 1995o10 150
i LANDS BRANCH
NORTH LIMBINDUCED POLARISATION
LINE 1420 OEDate : NOVEMBER 1994 Property : 505 NTS : 42 D/9 Survey by : NOREX
hemlo oldMints Inc. w/
o8COLU
O
O
00mUJ!
o
oco " inU
JooTT
mLJ
OinUJo
o
oinUJoo00O
O
CO
10600N
*-
Q
LU
O
OO
O
CN
-775
-8o
*v
en
o
to
o
O o
C/) -
o
15930
(NSLjJ
OLi.
DQ
UJ
lSi
5sL2 0)
0Q
UJ OZ
)o•z.
OJ^ c
--o out
-
- -c BX
.Q
-
10- l ..r^
s^I*^
00
Q.
O5
Q
MINING LANDS BRANCH
•i
JO.
VO•fr
NO
OtO
LNO
OZO
LNOOOOL
DQN
0086N
0096N
OO
6N
Z6N
0006NO
Q88
N0098
NOO
t-8NO
OZ8
bJ O
O
CM (D CD
UJ
O
O
O
COUJ
o
oCDinUJ
o
oCOo
oUJ
O
OCM
LU
O
Oom
Oin ea
UJ
o
oCOo
oCOUJ
o
oo
oCM
N0008
42C138WOOOB 2 15030 WABIKOBA
PRECAMBRIANPROTEROZOIC
MAFIC INTRUSIVE DIKES 13a diabase dike
ARCHEAN
[ 13 l LATE FELSIC INTRUSIVES 12a aplite 13b pegmatite
GNEISSIC COMPLEX INTRUSIONS lla unsubdlvlded lib granite gneiss Ile paragneiss lid naflc gneiss
l 10 l FELSIC PLUTONIC ROCKS 1———' lOa granodiorite (le Cedar Lake Pluton)
l Ob monzonite (le Go*an Lake Pluton)
~~| MAFIC PLUTONIC ROCKS "" 9a gabbro
MAFIC DIKES J 8a diorite dike Bl lanprophyre 8z xenollth-bearmg lanprophyre
FELSIC DIKES7a quartz-feldspar porphyry dike7b feldspar porphyry dike7c Irregular Feldspar porphyry dike (popcorn porphyry)7d equigranular dike
FELSIC INTRUSIVE STOCKSbo quartz feldspar porphyry stock6b fine grained quartz-feldspar porphyry stockfad hydrothermal breccia related to QFP stock
~1 CLASTIC SEDIMENTARY ROCKS 5a cobble conglomerate 5to pebble conglomerate5c pebble-bearing sandstone and pebble conglomerate Sd pebble-bearing sandstone
pebble-bearfrig sandstone and siltstone 5f sandstone 5g fine sandstone and stltiton*3h fm* t MM ton* and roncton* 8" MWfMt *M gr*y Mtsten* Sp flMOl M*MMW Mi pelitic MMMtont
CHCMICAL SEDIMENTAIY ROCKS 4a chert4b cherty siltstone 4c chert-magnetite iron formation 4d chert sulphide iron formation 4e barite-rich sediment
3 l INTERMEDIATE VOLCANIC ROCKS - — 3a massive
3b pyroclastic ash 3c pyroclastic lapilli 3d pyroclastic bonbs
FELSIC VOLCANIC ROCKS 2a massive 2b pyroclastic ash ?c pyroclastic lapilli Se pyroclastic bombs
l j MAFIC META-VQLCANIC ROCKS— ^ la massive floe
le amygdaloidal flowIf tuffIp pKlowed floeIs ultramafic flos-It tuff breccia
( ' natfflers r parentheses art neorCAPS capitalized Modifier* are coarse gramed or ntente
PIIIHMV FEATUKSq quartz-eye beftrmgfx feldspar crystal betrlngr nudetane rip-up ctait tovarmgs rcmrtane clast hearingax torecaated
NETAMORPHIC N9CIMLS
cardjeritechloritecuFVWigtonltegarnetkyanitenagnetrtesMewHtestaurolite
M.UMTHM NMDMLS
kt (notiteep epidotefd feldsparff feldspathic fracturesft feldspathic itoanorkgr. green Mcahn KeMotrfte
•i jliclflcatlor.•r aericrteaf ttrlctiltlc fracturei• a fftricrtlc etockoKirk tn tourHolln*
(CQlc ilicati) band* ted amphibole
i fracture ipletely anphltooiitljed rock
SULPHIDES. ETC
anhydrite gold
tpea
chtlcapyrtto'
nalachit* nolybMnupyrrhotite pyrite sphalerite teuuridei
f.159 SO
IrSOOO
or t hi LimbHenlo North East
Date
Geologist 1
Feb 6, 1995
P Johnston
i0
iVJn H•r
33iTJ
CO
CO COen
3Dmorn••M
mQ
.5408000 .N
/IP^'^fjQ)11 jLt^aJi. " 4±* ^ -^
Golden Giant Mine
li5409100 N
en00 CD-^ o o
cn CD CD A en o
5409100 N
Clam Post 2 \ 246n at 353 degrees!
TRENCH 14
5409050 N
FT-2-i
FT-2-9 FT-2-10
FT-2-11X 9900 N
cln 11644205409050 N
LEGEND
FT-4-14
SAMPLE LOCATION
SAMPLE NUMBER
DUTCRDP
CUT GRID LINES
CLAIM POST
5409000 N
u
cln 1010510
U
(Li
5409000 N
O 5 10 15metres
IVlD
APR 3 1995MINING LAMPS PDAMr|f
co oo4* O O
m
nmuiNMii42C138WOOOB 2 15930 WABIKOBA LAKE 270
tn-cooo-l*enOm
Trench 146l hy__ II Kum* DM* Nw 03/99
1*90
D*g Ne
Ld O O 00
LJ O O Or-O
LU O O C\j
LJ O O
LJ O O CO
LJ O O 00
LJ Ooo
LJ C O C\J
LJ O O
LJ O O CD
LJ O O 00
LJ O O O LO
LJ O O C\J LO
LJ OO
LO
LJ O O CO LO
LJ O O 00'LO
LJ O O O CO
o o
LJOo-T CO
I-Jo
CO
LJ O O GO CO
LJ O O O
M11200N -i1200N
l l / o o MU vJlN
E TB653301
TB653302
a
10000N
TB1010503
9800N-
TB1174289
9600N-
9400N-
9200N-
9000N-
8800N-
2:TB1010507
.4 f
- 10800N
- 1, 0600N
-10400N
8600N-
8400N-
-10200N
-10000N
vr- v.
sv^
x
)
JC
8200N-
•LI711.3
711147.17B-i1B.Im.1•LI
O7
VI•1.1•J.im.!•J.IMl J OB.7•LS•4-t
M7.iTIM J*1JMiTM.ITIM
•i. i1MU•LImTIL*•t.*0T.4M?.l•LI•J
•V.I•uM. fauv.*•LIa*.)•M.* OLS•LI
•m.iTM.1 WJ
•7W.7•XI•7.1 744.1m.t7B.7 7M.1 7M.1
••LJ IB.7 TM.1 7*J
JB.I 7M.1
•TIL t
JMUMLt
ni.fMl7M 7M.I TM.t ITT.f 711. l•7.*•1 l 717.1 rm.* 7M.Im t•H. *BJ.3
ML7 •1.1 W.I
Mlni
117*.* II*.* 7M * Td.* 7M l 7O.5 711.5 IM.I
7B.
m.
-9800N
-9600N
-9400Nmi.*It 1.7
on.t774.1 01.1 M. l MI.I174.4 711.*at174.1Ml
-9200N
7M.3 7M.7 7*1.1 5JS.7 M4.1
•7.*•LIML t•Lt7*74LI
71IJ MI.1 Ml.5•4.17117M.*IR.IM7JmTJL!
515.1MM•LIMB.f TMJ Ml.l 071
571.1at.iBtJai.iMi.5O75
•1.3ni.s4*4.t•LI 5B.J•L7•LI
-9000N
•M.I O4.I MS. 7 Ml.l Ml.] Ml.l 171.1•1.5•7.1auMl.lTIM 7M.I•m.t
•LI7*7.1•1.3 Ml .3 Ttl.l•ML7 07m.*TJL! 7SLI
8800N
8600N
S-8400N
RECEIVED
APR 3 1995
HMN6UNDS BRANCH
8200N
714.3
LJ O O 00 CN
LJ Oo o
LJ O O C\i
LJ O O
LJ O O CO
l
LJ8'OO'i
LJ O O O
LJ O O C\J
LJ O O
LJ O O CO
LJ O O 00
LJ O O OLO
LJ O O CN LO
LJ O O
LO
LJ O O CO LO
LJ O O 00 LO
LJ O O O CO
LJ O O CM CO
LJ O O
co
I
LJ O O 00 CO
LJ O O O
42C13SW0008 2 15930 WABIKOBA LAKE 280
Instrument : SCINTREX MP-3Profile Scale SOOnT/cm
Reduced Profile Scale SOOOnT/cmProfile Base Value 400
Datum : 58000
Scale 1:500050 O 50 100 150 200
•M
(meters)
NORTH LIMB/FOWLER 1&2MAGNETIC SURVEY
TOTALPROJECT : N LIMB.FOW1&2 NUMBER : 505,529,530
BASELINE AZIMUTH : 90 deg
DATE : NOVEMBER/1994 NTS : 42-D-9 SURVEY BY : NOREX
RLE : M529FOWM
hemlo goldMines Inc. ^X
J.-,
FB653310
LU O O OO CNI
11200N-
1 1000N-o -————
0800N-
TB653303
oeooN- -;
10400N-
TB653304
TB653309
ICbOON
10000N- t
9800N
TB1174289
9600N-
9400N-
9200N-
9000N-
8800N-
8600N-
8400N-
N-
LJ O O 00 OJ
LJ O OO
LJ OO CN
LJ O O
LJo oCDm
LJ o o00
LJ O O O
LJ O OCN
LJ O O
UJ O O CD
LJ O O 00
LJ OO O
LJ O O CN LO
LJ O
LJ O O CD
LO
LJ O O 00LO
LJ OO O CD
LJ O O CN CD
LJ O O
CD
UJ O O CD CD
LJ O O 00 CD
LJ O O O
LJ O O CN
LJ O O
LJ O O CD
J LJ O O O
LJ O O CN
LJ O O
LJ O O CD
LJ O O 00
l1
LJ O O O LO
LJ O O
LJo o
in LO
LJo oCD LO
LJ O O 00 LO
LJ O O O CD
LJ O O CN CD
LJ O O
CD
LJ O O CD CD
35" T3 70CO
CD COen
LJo o o
11200N
- 11000N-
-10800N
-10600N
-10400N
-10200N
-10000N
-9800N
-9600N
-9400N
-9200N
-9000N
8800N
l: - 8600N
•: -8400N
:: -8200N
m o mma
LJ o o o
N
'2.I5S30RECEIVED
1995
muiNG LANDS BRANCH
Instrument : SCINTREX MP-3Contour Intervals : 50 nT
Datum : 58000
Scale 1:500050 O 50 100 150 200
Sm——^K (meters)
NORTH LIMB/FOWLER 1&2MAGNETIC SURVEY
TOTALPROJECT : N LIMB, FOW1fc2 NUMBER : 505,529,530
BASELINE AZIMUTH : 90 deg
DATE : NOVEMBER/1994 NTS : 42-D-9 SURVEY BY : NOREX
FILE : M529FOWM
hemlo goldlime* Inc. ^J
29042C13SW0008 2 15930 WABIKOBA LAKE
