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42E11NW8488 2.15893 LEGAULT 010
. I 5093STURGEON BRIDGE PROPERTY
GEOLOGICAL SURVEY
LEGAULT TOWNSHIP
JELLICOE, ONTARIO
RECEIVED
JUL S 1993
toCO
CD
enCO
BY: BARBARA KOWALSKI
*
NOV. 10, 1992
42E11NW8400 2.15093 LEGAULT
TABLE OF CONTENTS
010C
TITLE
INTRODUCTION
LOCATION AND ACCESS
CLAIM STATUS
PROPERTY LOCATION MAP
SERVICES
PREVIOUS WORK
REGIONAL GEOLOGY
REGIONAL ECONOMIC GEOLOGY
PROPERTY GEOLOGY
DISCUSSION OF RESULTS
RECOMMENDATIONS
CONCLUSIONS
AUTHOR'S QUALIFICATIONS
REFERENCES
APPENDIX l
PAGE
l
l
1
1A
2
2
3,4
4,5
5,6
6
7
8
9
10
11
INTRODUCTION
The purpose of this report is to advance the geological
information on the property, by providing detailed geology and
interpretation, from which recommendations for subsequent ex
ploration programs may be derived.
The author conducted 5 days geological mapping and evaluated
other potential economic areas, on the new picket lines cut at
100 foot intervals, during September 14 to 18 and October 29,
1992.
LOCATION AND ACCESS
The Sturgeon River Bridge property is located approximately
six kilometers east along Provincial Highway 11, from the town
of Jellicoe, Ontario. It is accessed north on the Kinghorn Road
from the highway, to the CNR railway crossing, about 500 meters
southwest of the claim block.
CLAIM STATUS
Mr. Fred Checkley currently owns 100% interest in TB
786139, 40, 41, 42 and 45; TB 813417, 18, 20, 46, 47, and 48; TB
1082429 and 30; TB 1142809, 10 and 11 unpatented mining claims.
The claims are registered at the Mining Recorders Office in
mourni l .' . iv
iitvp Jxs~slMurchl*pn f. y|'xV~"~~~V^ C J^ i I,! ^ ^hiichcb^)
Mungo Pirk fi f* BARBARA''^' V 4*' \-.- , tvMims^.G-ON
- --- . .KjlilouZ/X
Uuli i- P - utm nK g*ry\*Mclnlyrt \ t
io^^5rt^'^^
*i "y/y^A ;'iy*'A*7^•^'jmfi\*{ m ^^lfx
July 1990 c STURGEON BRIDGE PROPERTY Legault Twp., Ontario
LOCATION MAP
Scale 1:600,000
Thunder Bay. The claims can be found on the Legault Township map
G-170 claim sheet. All claims are in good standing in acccor-
dance with the Ontario Mining Act.
SERVICES
The property has excellent infrastructure facilities and
utilities. The CNR crosses the width of the property and it is
situated approximately 1.7 km north from the Trans Canada High
way, Trans Canada Pipeline and powerline services.
PREVIOUS WORK
Limited and sporadic exploration work has been done on the
' property since 1934. The programs completed, were surface
prospecting, trenching, airborne and surface magnetometer and EM
surveys, three diamond drill holes, linecutting, geology, channel
sampling and assaying. Numerous showings of gold and copper were
found, both in the native state and in mineralization, however,
no definitive zones have been outlined.
REGIONAL GEOLOGY
The Beardmore-Geraldton metavolcanic-metasedimentary (here
inafter the term " meta " is omitted) terrain is situated on the
boundary between the Quetico and Wabigoon subprovinces of the
Precambrian Shield. It comprises three belts of volcanic-sedi
mentary rocks termed the northern, central and southern sedimen
tary belts (NMB, CMB and 8MB respectively). Local mafic and
felsic intrsuives occur within the volcanic-sedimentary sequences
and are all cut by a numnber of sub-parallel, east-west trending
regional faults. Although the sedimentary sequence is fault-
bounded, the original sedimentary sequence was deposited on a
cratonic margin. The environments of deposition are varied and
range from alluvial fan-braid plain in the NMB, through fan
delta-braid in the CMB, to a marine turbiditic assemblage in the
8MB (Barrett and Fralick, 1989).
REGIONAL ECONOMIC GEOLOGY
The sedimentary belts play a significant economic role where
several gold deposits are located.
Southern Sedimentary Belt (8MB)
In the SMB, the Letich and Northern Empire gold deposits,
both near Beardmore, are hosted in steeply dipping quartz vein
systems; the former in sediments and the latter in mafic vol
canics. The MacLeod Cockshutt and Hard Rock Mines near Ger
aldton, consist of quartz stringers in iron formation and quartz
viens associated with felsic intrusives. The Solomon Pillars
near Jellicoe, consist of quartz stringers associated with iron
formation. Regionally, structural relationships between fault
systems and lithologic contacts are important to these deposits
(Kowalski, thesis in progress).
Central Sedimentary Belt (CMS)
There are several precious and base metal occurrences, for
example, the Sturgeon River Bridge property is one which occur
within the CMB. The characteristic features which prevail
amongst other precious and base metal deposits, as described
above, occur within the belt. Historically, little exploration
activity in the area, has stifled the economic potential which
may exist in the belt (Kowalski, thesis in progress).
Northern Sedimentary Belt (NMB)
This type of limited exploration interest is best demon
strated in the NMB where the Brookbank gold deposit exists. This
deposit is the first known deposit to the NMB. Although many
other precious and base metal occurrences occur along its 50 mile
strike length, very little exploraiton activity had been reported
in the belt. Geologically, the Brookbank deposit is localized
along a sheared contact between polymict conglomeratic-sandstone
unit and pillowed mafic volcanics. A diorite intrudes the
volcanics and has caused incipient deformation, alteration and
mineralization in the sediments and volcanics. A splay fault,
from the regional Paint Lake Fault separates the sediment-vol
canic units on the property (Kowalski, thesis in progress).
Onaman-Tashota Volcanic Arc
To the north of the sedimentary belts lies a volcanic arc
terrain called Onaman-Tashota located in the Wabigoon Subprov-
ince. This area is historically known to host many base metal
deposits and case studies are documented in the government files.
PROPERTY S ECONOMIC GEOLOGY
The property was previously mapped by Rainboth (1990), where
all the rock types were identified and described. The current
geological program provides a detailed examination of the speci
fic areas of deformation, alteration and mineralization on the
grid, as well as mapping the newly established grid, cut at 100
foot intervals. The area mapped in this program was completed on
ne numbers 5+OOW through to 31+OOE, 6+OOW, 10+OOW, 14+OOW and
all lines cut on claim numbers 1142809 through to 1142811.
Further to Rainboth's map, more pillowed mafic volcanics
were mapped with gabbroic, andesitic and dacitic variations
occurring in the volcanics. A unit of greywackes occur on the
westerly end of the grid are in sharp contact with the volcanics.
Diabase dykes occur on the property and were previously mapped by
Rainboth. Intrusions on the property are tonalitic dykes and a
diorite was identified on line 20+OOE. In this area is a deform
ed, altered and mineralized zone, called the FB Zone was defined.
The description and geophysical comparisons to the FB Zone are
provided below.
To the westerly end of the property, the Barbara La-ke Fault
or Jellicoe Lake Fault trends in the northeasterly direction. It
is at this fault that many disruptions and movements have oc
curred. It is possible that many or some of the gold showings on
the property could have been influenced by the fault. In order
to establish this theory, much more prospecting and power stripp
ing will have to be completed.
DISCUSSION OF RESULTS
The FB Zone identified during the survey is sheared,
carbonatized, silicified, sericitized and mineralized with
pyrite, pyrrhotite, chalcopyrite and bornite. The zone was
defined occurring from L4+OOE to L20+OOE and is shown on the
geological map. The probable cause for the presence of the zone
is due to the emplacement of the intrusive diorite/gabbroic rocks
which occur in close proximity to the mineralization. The
magnetometer signature indicates a favourable horizon for gold,
occuring on a flank of a magnetic high located on line 20+OOE.
The large diorite/gabbroic body to the east is also depicted by a
magnetic high. Corresponding with the zone is a weak VLF-EM
conductor located in close proximity in the swamp.
Grab samples were obtained from various locations on the
property. The assays ranged from 7 to 9790 ppb gold, 39 to
23,120 ppm copper, 3,700 ppm zinc, and 6,950 ppm lead. These
assays and locations are listed in Appendix 1.
RECOMMENDATIONS
It is apparent that more work should be done to establish
the economic potential of this FB Zone. The following work
program will enhance the property and provide further economic
indicators.
A) Power Stripping - The FB Zone should be further stripped from
Line 13+OOE to 20+OOE as shown on the geological map.
B) Sampling - Subsequent to the backhoe program, methodical
sampling should be done with the help of plugger and/ or ex
plosives. The reason for this method is to obtain the most
prestine sample possible past the weathering surface. It is at
the weathering surface where the majority of the precious and
base metals are leached away.
C) Geophysical - Further magnetometer and VLF-EM surveys should
be completed over the new picket lines.
D) Prospecting - Additional targets on the property where gold
and copper values were obtained should be prospected. The
purpose of this program is to establish a zone which has dimen
sions. If successfully achieved, then further power stripping
should be implemented.
The costs for the program, depend highly on the working
budget, therefore, expenditure costs are not included with the
recommendations.
CONCLUSIONS
The property is one of the more intriguing properties in the
area which has a favourable geological enviornment for precious
and base metal occurrence. Through dilegent and persistance
work, further zones on the property will be established and their
economic potential should be assessed as the FB Zone.
AUTHOR'S QUALIFICATIONS
I, Barbara Kowalski, conducted the mapping on the property
and am the author of this report. I graduated from McMaster
University in 1983, and am currently completing my M.Se. at
Lakehead University. I have been actively practicing continuous
ly each season for 9 and 1/2 years.
lA.
Barbara Kowalski
Geologist
FROM : PHOE NO. : P02
SUPPLEMENTARY PAGE TO BE INSERTED FOR OBOLOGICAL REPORT FOR B.
NELSON'S CLAIMS, NOVEMBER 10, 1992.
MAFIC METAVOLCANICS
1) Andesite - Medium to dark green when fresh, same when
weathered. Typically le fine-grained, massive textured and 10
pillowed with local pillow breccia. Typically le cross-cut by
thin less than 10 cm quartz-carbonate stringer* and has 1/2 to l \./.^,. --. , -r
fine-grained disseminations of l-2mm pyrite grains. Locally,
chalcopyrite may occur in pillow selvages as disseminations 1/2
to It.
CHEMICAL SEDIMENTS
1) Greywacke- Light grey when fresh, same when weathered and l*
typically softy and i* non-magnetic. The greywacke is inter
bedded with cherty buds that are less than 1m in width. Typi
cally, the greywacke has lets than 1/2X fine-grained sporadic
disseminations of pyrite.
2) Chert- The colour is variable from yellow, beige, pink, white
and grey when fresh and same when weathered, chert is typically
hard and i* either massive or fragmented. Usually the chert is
void of sulphides however occasionally fine-grained pyrite may
occur as disseminations up to 1/2* locally.
INTRUSIVES
1) Diabase- Cross-cutting the stratigraphy are diabase dykes.
OCT SB '93 l l:36PfiGE.002
FROM ; PHONE NO. : P03
There is one prominent dyke which nay prove lo be a t e conomic
value. The diabase is medium- to coarse- grained 2-3mm, and la
homogenously massive, it la green with a alight pink hue due to
feldspars that are present, it appears to weather a beige-brown
and IB* distinctive from other rock types on the property.
Typically, less than 1/2* f ine-grained disseminated pyrite occurs
throughout the unit.
2) Gabbro/Diorite- Dark green when freoh and weathered, massive
and coarse-grained. Locally plagioclase laths nay bc seen 2-4nw
in length. Usually, fine-grained pyrite is homogeneously dis
persed less than 1/21 as fine grains.
The alteration of the gabbro unit on surface la bilge-brown
and le typically mam i ve with a number oi quartz-carbonate
stringers throughout. The quartz-carbonate ve inlets may contain
galena, chalcopyrite and pyrite up to 5V locally. Hematite
particularly specularite may occur locally in the unit.
3) Tonalle Dykes- Pink to white both fresh and weathered sur
faces/ massive texture and very hard. Usually/ the dykes are
less than 1m in widths nnd may contain hornblende, biol:lte, and
some quartz. Plagioclase phenocrysts of 4mm in sizu occur.
Typically, the unit is void from sulphides.
ECONOMIC GEOLOGY
There are two areas of Interest on the property, that being
the quartz-carbonate veins that extend for several tens of feet
OCT 20 '93 l l :37PAGE.003
FROM : PHONE NO. : P04
on either side of the diabase dyke. The vein/ locally, is up to
1m in width and contains pyrite, chalcopyrite, and native copper.
It In olco gold-boating. A number of anxillary quartz-uaxLuuulw
veins filling in fractures occur nearly parallel to the east
strike. The west extension of the quartz vein that io located to
the vent nf the diabase dyke, a similar description of the vein
may be g1v*n with an additional enrichment of chalcopyrite and i- T-nir
native copper occurring within the pillow selvages of the mafic
volcanics.
There is no prominent halo of alteration that exists other
than ankerite alteration in these qutrtx-carhonahn vnino and
subsidiary veinlets.
OCT 20 '93 11:37 PAGE.004
REFERENCES
Kowalski, B., 1992: The Brookbank Gold Deposit, Beardmore,
Ontario (thesis in progress).
Rainboth, W., 1990: Sturgeon Bridge Property Geological Report,
Legault Township, Ontario. 10pp.
Walker, A.J., 1991: Sturgeon Bridge Property Magnetic and VLF-EM
Surveys, Legault Township, Ontario. 4pp.
WAWA ASSAYING INC.P.O. Box 1998 * Wawa. Ontario POS 1KO - 705-856-4443 127 Mission Road Fax - 705-856-2902
CERTIFICATE OF ANALYSIS N0- 1031S
CLIENT: MORNING DEW EXPLORATIONS LTD.
PROJECT i
TYPE OF ANALYSIS: Atomic Absorption
DATE: October 7, 1992
Reft 921007-1053
SAMPLE No.
16183
16164
16186
16186
16187
1618816189
16190
1619116192
Au i*t)b
4240
725
394
50
7
1070
730
65
149790
Ag Cu Zn Pb pDitf TJtifn Don Don
23120
1027
54.6 39 3700 6950
Certified By:
APPENDIX I
Sample No
16183
16184
16185
16186
16187
16188
16189
16190
16191
16192
Locat ion
L24+OOW, 6+OOS
L24+OOW, 6 + OOS
L12+OOW, 6+50S
L12+OOW, 6 + 50S
L10+OOW, 3 + OOS
L10+50W, 4 + OOS
L10+50W, 4+10S
L4+OOE, 10+OOS
L4+OOE, 10+OOS
L12+OOE, 10+OOS
Descr iption
Silicified (smoky grey
colour) mafic volcanic,
pyrite and chalcopyrite 2-3%
as fine disseminations.
Calcite and ankerite altera
tions in deformed mafic
volcanic, 2% fine- and
coarse- grained pyrite.
Malachite, azurite, chalco
pyrite, minor pyrite occur
ring within pillow selvages.
Same description as 16185.
Ankerite, ^ fine pyrite,
near contact with dyke.
Silicified, ankerite altera
tions 2-4% fine-grained
pyrite.
Same description as 16188.
Ankerite, weathered surface.
Ankerite, l/^ pyrite.
Fine pyrite, chalcopyrite,
galena and sphalerite in l
foot quartz vein.
t 4
42E11NW8408 2.15093 LEGAULT
2. 15093
STURGEON BRIDGE PROPERTY
MAGNETOMETER AND VLF EM SURVEY
LEGAULT TOWNSHIP
020
JUL 8 1993
JELLICOE, ONTARIO to
c"c J
BY: BARBARA KOWALSKI JAN. 10, 1993
42E11NW8400 2.15093 LEGAULT
TABLE OF CONTENTS
0S0C
TITLE
INTRODUCTION
LOCATION AND ACCESS
CLAIM STATUS
PROPERTY LOCATION MAP
SERVICES
PREVIOUS WORK
REGIONAL GEOLOGY
REGIONAL ECONOMIC GEOLOGY
PROPERTY GEOLOGY
GEOPHYSICAL SURVEY
MAGNETOMETER SURVEY
DISCUSSION OF RESULTS
VLF-EM SURVEY
RECOMMENDATIONS
CONCLUSIONS
AUTHOR'S QUALIFICATIONS
REFERENCES
PAGE
l
l
l
1A
3,4
5,6
Ei
7-9
9-1 2
12
13, 14
14
J. 5
INTRODUCTION
The purpose of this report is to advance the geophysical
information on the property and combine it with the geology, from
which recommendations for subsequent exploration programs may be
der i ved.
The surveys were conducted by F. Checkley. The magnetometer
survey was conducted from Oct. 31 to Nov. 23, 1992 and VLF EM
survey was completed from Dec. 5 to 12, 1992. Acceptable mag
netometer readings were obtained on Oct. 31, Nov. l, 15, 16, 17,
19 and 23. Magnetic storms causing drifts were encountered during
the other days, whereby, the data was discarded. All data was
corrected for diurn'al drift tay E(en Nelson.
LOCATION AND ACCESS
The Sturgeon River Bridge property is located approximately
six kilometers east along Provincial Highway 11, from the town
of Jell i coe, Ontario. It is accessed north on the Kinghorn Road
from the highway, to the CNR railway crossing, about 500 meters
sout h west of the c l ei i m bloc k.
CLAIM STATUS
Mr. Fred Checkley currently owns 100X interest in TB
786139, 40, 41, 42 and 45; TB 813417, 18, 20, 46, 47, and 48; TB
• p'li'v •'•'•".; * ir""^f^B-lMnnll^JlM
iiW
urehlion f 3 i ''- t ^*
. Odd* 1^ ' OlllnpU ' Di* ion . B^,... i^fti
Uv.l4Vy 'ixjndn . wn*ot
July 1990STURGEON BRIDGE PROPERTY
Legault Twp., Ontario
LOCATION MAP
Scale 1:600,000
10B2429 and 30; TB 1142809, 10 and 11 unpatented mining claims.
The claims are registered at the Mining Recorders Office in
Thunder Bay. The claims can be found on the Legault Township map
G-170 claim sheet. All claims are in good standing in acccor-
dance with the Ontario Mining Act.
SERVICES
The property has excellent infrastructure facilities and
utilities. The CNR crosses the width of the property and it is
situated approximately 1.7 km north from the Trans Canada High
way, Trans Canada Pipeline and power l i ne services.
PREVIOUS WORK
Limited and sporadic exploration work has been done on the
property since 1934. The programs completed, were surface
prospecting, trenching, airborne and surface magnetometer and EM
surveys, three diamond'dr i 11 holes, l i nee ut t i rig, geology, channel
sampling and assaying. Numerous showings of gold arid copper were
found, both in the native state and in mineralization, however,
no def i n i t i ve z ones have been out l i ned.
REGIONAL GEOLOGY
The Beardmore-Geraldton metavolcanic-metasedimentary (here
inafter the term " meta " is omitted) terrain is situated on the
boundary between the Ouetico and Wabigoon subprovinces of the
Precambrian Shield. It comprises three belts of volcanic-sedi
mentary rocks termed the northern, central and southern sedimen
tary belts CNMB, CMB and SMB respectively). Local mafic and
felsic: intrsuives occur within the volcanic-sedimentary sequences
and are all cut by a numnber of sub-parallel, east-west trending
regional faults. Although the sedimentary sequence is fault-
bounded, the original sedimentary sequence was deposited on a
cratonic margin. The environments of deposition are varied and
range from alluvial fan-braid plain in the NMB, through fan
delta-braid in the CMB, to a marine turbiditic assemblage in the
SMB.
REGIONAL ECONOMIC GEOLOGY
The sedimentary belts play a significant economic role where
several gold deposits are located.
Southern Sedimentary Belt CSMB)
In the SMB, the Let i eh and Northern Empire gold deposits,
both near Beardmore, are hosted in steeply dipping quarts vein
systems; the former in sediments and the latter in mafic vol-
c a n i c B ,. T h e Mac: L. e o d C o c k s h u tt a n d H a r d R o c k M i fi e s near 6 e r -"
aldtori, consist of quarts stringers in iron formation and quarts
viens associated with felsic intrusives. The Solomon Pillars
near Jell i coe, consist of quarts stringers associated with iron
formation. Regionally, structural relationships between fault
systems and lithologic contacts are important to these deposits
(Kowalski, thesis in progress).
Central Sedimentary Belt CCMS)
There are sever'al precious and base metal occurrences, for
example, the Sturgeon River Bridge property is one which occur
with in t h e CMB. The characteristic features which prevail
amongst other precious and base metal deposits, as described
above, occur within the belt. Historically, little exploration
activity in the area, has stifled the economic potential which
may exist in the belt (Kowalski, thesis in progress).
Northern Sedimentary Belt (NMB)
This type of limited exploration interest is best demon
strated in the NMB where the Brookbank gold deposit exists. This
deposit is the first known deposit to the NMB. Although many
other precious and base metal occurrences occur along its 50 mile
strike length, very little exploraiton activity had been reported
in the belt. Geologically, the Brookbank deposit is localized
along a sheared contact between polymict conglomeratic-sandstone
unit and pillowed mafic volcanics. A diorite intrudes the
volcanics and has caused incipient deformation, alteration and
mineralization in the sediments and volcanics. A splay fault,
from the regional Paint Lake Fault separates the sediment-vol
canic: units on the property (Kowalski, thesis in progress).
Onaman-lashota Volcanic Arc
To the north of the sedimentary belts lies a volcanic arc
terrain called Onaman-Tashota located in the Wabigoon Subprov-
ince. This area is historically known to host many base metal
deposits and case studies are documented in the government files.
PROPERTY fc ECONOMIC GEOLOGY
The property was previously mapped by Rainboth (1990) and
further geological work was completed by Kowalski (1992).
Pillowed mafic volcanics were mapped with gabbroic, an-
desitic and dacitic variations occurring in the volcanics. A unit
of greywackes occur on the westerly end of the grid are in sharp
contact with the volcanics. Diabase dykes occur on the property
and were previously mapped by Rainbath. Intrusions on the
proper t y are tonal i t i c dykes and a diorite was identified on l i ne
"'O+OOE. In this area is a deformed, altercvd and mineralized
zone, called the FB Zone was defined. The description and
geophysical comparisons to the FB Zone are provided below.
To the westerly end of the property, the Barbara Lake Fault
or Jellicoe Lake Fault trends in the northeasterly direction. It
is at this fault that many disruptions and movements have oc
curred. It is possible that many or some of the gold showings on
the property could have been influenced by the fault. In order
to establish this theory, more prospecting will have to be
c o m p l et ed.
GEOPHYSICAL SURVEYS
The geophysical surveys were completed over L8+OOW through
to L.32+OOE at 100 foot spaced lines and extending from Base Line
3+OOS through to on a few lines during the magnetometer survey to
16+OOS to 17+OOS. In addition, further lines to the north from
LG+OOW to L20+OOW were completed to Base line 0+00.
MAGNETOMETER SURVEY
A Scintrex MR l instrument was used during the survey and
the data was read at 20 foot intervals along the north-south
lines. Base stations were established on Base line 0+00 at 14+OOW
and on Base line 3+008 at G+OOW, 4+OOW, 0+00, 4+OOE, 8+OOE,
12+001;::., 16+OOE, 20+OOE, 24+OOE and 28+OOE. Base stations were
read e t interval? of 30 to 50 minutes. Sensitivity levels were
d e t ter mi ne d to be 20 gammas.
DISCUSSION OF RESULTS
Several small magnetometer h i g h gamma i'ea d :i rigs of over :l. v 301.)
through to over 2,300 were encountered. Comparably, there were a
number of magnetometer lows established with gamma readings of
ove Y negat i ve 3,0OO gammas. Variation s of gamma reading s was
established on almost each line along the grid. The importance
of the data is to look at the magnetometer results with relation-
ship to the geological data and establish trends.
Area l
A large, broad magnetometer anomaly exists on the south side
of the grid. This area predominates in a cedar swamp. Within
the swamp, an occasional outcrop of pillowed mafic volcanics
occurs with pyrite and a deformed and altered outcrop of vol
canics occurs on L13+OOE, 14+OOS. The magnetometer high gamma
readings continue eastward across the grid and across the diorite
outcrop. There is no pronounced outlined of the diorite defined
by the magnetometer data. From L4+OOE to L12+OOE, approximately
Base line 3-+OOS to 12+OOS a large magnetometer low occurs in the
area. An area of outcrop reveals a deformed and altered zone
called the FB Zone, The shear zone is comprised of ankerite,
sericite, silica alterations and mineralised principally with
pyrite, pyrrhotite, chalcopyrite. An abrupt north-south change
occurs just east of L12+OOE from magnetometer low to high (see
map for specific: gamma readings).
Area 2
The second area of interest is the south side of the broad
magnetometer high occur ing within a swamp. A few lines were
extended with the survey and a magnetometer low was encountered
on L.KH-OOE at 16+QOS to 17+OOS. This low corresponds with an
outcrop area of fine-grained mafic volcanic. It is altered with
ankerite and mineralized with pyrite and pyrrhotite.
Area 3
A diabase dyke occurs at approximately L10+OOW and is
reflected partially by an interception of gamma readings. In
addition along LB+OOW strong and low gamma readings were obtained
at 5+209 (high), 5+40S (low), 6+20S (high). These readings are
explained by the content of pyrrhotite (with magnetite) minerali
zation. On the west side of the diabase dyke at line 12+OOW,
5-i-GOS, 700-720 gamma readings correlates with a contact between
pillowed mafic volcanics, mineralized with chalcopyrite and a
shear zone defined by ankerite, silicification, sericitization
and is mineralized with pyrite and minor chalcopyrite.
Area 4
A 1580 gamma reading was obtained at L32+OOW, 13+75S which
was exposed and revealed a 2 foot felsic dike to the north of a
15 foot wide balsaltic rock striking N75E. This area requires to
be prospected and determine if any deformation, alteration or
m i n e r a l i z a t i o n e x i s t s in t h e a r e a.
VLF EM SURVEY
A Crone Radem VLF'-EM Receiver was used, utilising Cutler
Maine, 17.8 kHz transmitter station. Sensitivity of the instru
ment is l "/.. D ip angles were only determined through the survey.
Sixteen conductors were determined and are described as follows:
Conductor A
Occurs in area 4 described in the magnetometer data above.
This conductor should be pursued further to east to determine its
extent and its significance as it is recognised by the data to be
a s t r o n g c o n d u c t o r .
Conductor B and D
Conductor B occurs on L32+OOE at 11+20S. It is not known
how far east the conductor extends, however, it continues west
ward to approximately L28+OOE where it is discontinued. Cond
uctor D may perhaps be the remnant continuation of conductor B.
Conductor B occurs within a magnetometer low whereas conductor D
occurs within a magnetometer high. These two conductors are
/o
shown in the data to be weak, however, should be pursued with
prospecting as there may be a structure trending in a northwest
erly direction coinciding with the high and low magnetics.
Conductor C
Conductor occurs on L31+OOE to L30+OOE and is to be con
sidered as a weak anomaly with no significant magnetic signature.
Conductor E
This conductor extends from L25+OOE to L14+OOE from Base
line 9+OOS to approximately 8+OOS. It occurs partially within a
magnetic: high and it may signify the presence of a porphyritic
dyke or the presence of a quarts vein. This area should be
i nspected.
Conductor F7 , G, H, I
Conductor F occurs from L19+OOE to L20+OOE just south of
Base line 9+OOS. Conductor G occurs from L18+OOE to L16+OOE,
conductor H at L17+OOE to L1G+OOE, arid conductor I occurs on
L15+OOE, 13+OOS. These conductors are all weak and may represent
dykes or veins.
Conductor J
It is located from L10+OOE to L9+OOE next to the Base line
9+OOS. The conductor occurs within magnetometer high area
between two magnetometer lows. A quarts vein and a porhyritic
dyke occur nearby and may have bearing to the existence of this
n
conductor. It however, should be investigated.
C on d u c t o r s K, L
These two conductors are located on Line 0+00, 11+40S and
12+40S. These are very weak conductors.
Conductor M
It is located between lines 2+OOW and 3+OOW just south of
the Base line 9+OOS. It cross-cuts the trend of the magnetometer
data, however, coincides near the transition from a magnetometer
high to a low to the south. Although, it appears from the data
the conductor is weak it should be further investigated by
prospecting.
Conductor N,D
Conductor N is located at 2+OOW, 13+75S and is a very weak
conductor. Conductor O is located at LG+OOW, 2+20S and is deter
mined to be a\ very weak conductor.
Conductor P
It occurs from L16+OOW at 6+20S through to L20+OOW at 5+40S.
This conductor may coincide with a quarts vein or a porphyritic
dyke. It is considered from the data to be a moderate condutor.
F u r" t h e r D :J.;;:, c L\ ; :., s :i. on o f D a t a
An area of perhaps utmost significance may lie between LS-i GOE
through to Ll+OOE occuring south of the Base line 9+OOS. A
prominent south dip occurs hear e which may be indicative of a
strong conductor lying to the south of the exisiting lines
(coinciding with a magnetometer low). An abrupt change in dip
occurs at LO+00 from south on the east side and north on the west
side of L.CH-OOE:, This may be a reflection of a hidden N-S (ap
proximate) trending fault. A prominent north dip occurs from
LI +OOW to L3-i'COW before it dissipates westward.,
It is suggested by the data that a possible conductor
indicating the existance of a structural feature occurs here,
c o in c i d i n g wit h s i g n i f i c a n t m a g n e t o m e t e i" data.
RECOMMENDATIONS
The following work program is recommended with respect to
the findings of the new data encountered in this program..
A) The VI....F"---EM data should first be pursued along the lines that
extend to the railroad and beyond such that the cross-over may be
defined and the strength of the dip of the south side of the
c ond u c t or may be d e t e r m i n ed. The area wh i c h shoul d be c o ve r ed
occurs from LO-KX) to 1,.20-i-OOE. Depending if a conductor is
located, should it be successful, then lines should be cut
further south at 1.00 foot spacings and a detailed VI...F"-EM and
mag en tome ter program should be pursued. Further VI... F'-EM and
magnetometer data should be extended eastward as to cover the
extent of t h o conductors A and B.
B) All t h e conductors c: o i n c i d i n g wit h magnetometer signatures be
prospected with a corresponding detail structural analysis (that
i R, detail of strike, dip and possible plunge determination of
nearly all the outcrops, then a map showing all data should be
compiled and interpreted).
C) l n t h e area o f t h e mag n e t o mete r h i g fi, t here lies a p r o m i n e n t
cedar swamp. A geobotanical survey should be pursued in the area
between Ll-i-OOE to 13-i-OOE on l y south of the outcrop area in the
swamp. The tap r oot s of those trees wh i c h are large, should
extend and reach near or at. outcrop. The analysis should be done
for Au and Cu (depending on assay prices).
D) A complete compilation of the data accumulated should then be
done whereby /x numhor of winkie drill hole targets can be sited.
COMMENTS
The programs of mechanical stripping, geology, geophysics,
plugging and assays all indicate an area where gold exists. It
is a matter of pin pointing the exact location where gold may
exist over considerable lengths and widths.
Although limited, the program recommended can be completed
with the next OPAP grant whereby, gold can be established to
o c c u r i n economic dimensions.
CONCLUSIONS
The property :i. s one of the more intriguing properties in the
area which has a favourable geological envi ornment for precious
and base metal occurrence. Through di l egent and persi stance
work, further zones on the property will be established and their
e c en n o m i c p o t e n t i a l s h o u l d b e a s s e s s e d a s t h e F B 2. o ne.
A U 7 H O R' S Q U A L l F T C A TIO N S
I y Barbara Kowalski, conducted the mapping on the property
and am the author of this report. I graduated from MeMaster
University in 1983, and am currently completing my 1*1,, Se. at
L a k e h e a d U n i v e r s i t y. l have bee n actively p r a i: t i c i n g c o n t i n u o u s -
l y ea c: h s e a s o n f o r l O y e a r s.
B a r b a r a K o w a l s k i D -si - v
Geoloqist
REFERENCES
K o w a .1 B k i , B. y 1 9 9 2: T h e B i- o o k b a n k G o l d D e p o sit, Bear d m o r e,
(D r rt a r i o (t h e s i s i n p r o g r e s s) .
Rainboth, W, y 1990s Sturgeon Bridge F'roper t y Geological Report,
Legault Township, Ontario. 10pp.
Walker, A.J.. , 1991: E) turgeon Bridge Property Magnetic and VLF-EM
Surveys, I.... e q au 11 Township, Ontario. 4pp.
42E11NW8400 Z . 15993 LEGAULT 300Ontario
Ministry ofNorthern Developmentand Mines
Ministere du Developpement du Nord et des Mines
October 21, 1993
Geoscience Approvals Section 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5
Telephone: Fax:
(705) 670-5853 (705) 670-5863
Our File: 2.15093 Transaction #: W9340.00133
Mining Recorder Ministry of Northern Development and Mines 435 Janes Street South Suite B003Thunder Bay, Ontario P7E 6E3
Dear Sir/Madam:
Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS TB786139 ET AL IN LEGAULT TOWNSHIP
The deficiencies in the original submission have been rectified.
The assessment work credits for Geology, Section 12 and Geophysics, Section 14 of the Mining Act Regulations, have been approved as outlined on the attached Assessment Work Credit Form.
The approval date is October 19, 1993.
If you have any questions regarding this correspondence, please contact Lucille Jerome at (705) 670-5855.
Yours sincerely,
Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division
cc: Resident GeologistThunder Bay, Ontario
./Assessment Files Library v Toronto, Ontario
ASSESSMENT WORK CREDIT FORM
FILE NUMBERl 2.15093DATES October 20, 1993RECORDER'S REPORT NUMBERS W9340.00133
RECORDED HOLDERS Fred Checkley CLIENT NUMBER: 117469
TOWNSHIP OR AREAS Legault Township
CLAIM VALUE OF WORK DONE VALUE APPLIED VALUE ASSIGNED RESERVE ON THIS CLAIM TO THIS CLAIM FROM THIS CLAIM
TB786139 908 O 908786142 1994 O 1994813418 3756 O 3756813420 2219 O 22191082429 1675 O 16751142809 344 O 3441142810 344 O 3441142811 343 O 3431194764 O___________H5&3_____________P.
11,583 11,583 11,583
Ministry ofVlorUAp Developmentandmmes
Ontariot
Report of Work Conducted After Recording Claim
Mining Act
Transaction Number
du'used tor ooTrPersonal Infv Jon collected on this form is obtained under the authority of the Mining Act. This Information wttlthis collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Ftoor, 160 Cedar Street,Sudbury, Ontario, P3E 6A5, telephone (705) 670-7204.
Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining
Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form In duplicate.- A sketch, showing the claims the work is assignedJof must accompany tbis form.
event No. CWJ/7 ( phont No*
Recorded Holders) "
?rt J A. {Are rAddress
,0, Ao* /2 ^ r/rjTownshlp/Area
J 4 f
Mining
e,M or Q
/ 7 GDates Work Performed
From:H
To:
TWork Performed (Check One Work Group Only)
13
Work Group
X Geotechnical Survey
Physical Work, Including Drilling
Rehabilitation
Other Authorized Work
Assays
Assignment from Reserve
Type
dfn let/If A / . h tbhS't'tiiAe 1-ff , l/Lf frftrfAv Ss (* i
' ' ; v
* 4*
' f
"RECEIVED"JUL 8 1993
MININnu.ND6DnAMftM
f
f*.
Total Assessment Work Claimed on the Attached Statement of Costs i l o
Note: The Minister may reject for assessment work credit all 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.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name
/~ C k f t K /f yf h. Ck,,J(Jij* ' f^ P L4^fl 1 \ f\ J
Address
P-0, ftofi /2 ?
P.O. '-k** m610 PC* L
fi }f ft S& /ne r f C/sl',
tfrcts'pto0st 0sifa j .,/c Rj.At*/*/ TAu*d;fc*,ti
f 'f
(attach a schedule if necessary)
Certification of Beneficial Interest * See Note No. 1 on reverse side
1 certify that at the time the work was performed, the claims covered In this work report were recorded in the current holder's name or held under a beneficial Interest by the current recorded holder.
Date Recorded Holder or Agent (Signature)
Certification of Work Report /1 certify that 1 have a personal knowledge of the facts set forth in this Work report, having performed the work or witneesed seme during and/or after Its completion and annexed report Is true.
Name and Address of Parson Certifying
C, fox J21Telepone No. Date f Certified "By (
ftFor Office Use Only
Total Value Cr. Recorded Dst* Recorded Mining Recorder
Date
Sent
Received StampCo
CTJ
OntarioDevelopment
lines
MJi-istere duf ^ppement du Nord*. .rt mines
Statement of Costs for Assessment Credit
fetat des coOts aux fins du credit devaluation
Mining Act/Lol sur les mines
Transaction NoJN* d* transaction
2. 15093Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands. Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury. Ontario P3E 6A5, telephone (705) 670-7264.
Les renseignements personnels contenus dans la presente formule sent recueillis en vertu de la Lot sur les mint* ei servtront a ttnlr a jour un rtgistre des concessions minieres. Adresser loute question sur la cdlece de ces renseignements au chef provincial des terrains mlnlers. ministers du Devetoppement du Nord et des Mines. 159, rue Cedar. 4* etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.
1. Direct Costs/Gouts directs
Type
Wages Salalre*
Contractor'* and Consultant's Fee*Drolte de ('entrepreneur et d* ('expert- conaell
Supplies UsedFournlturesutlllaaaa
Equipment Rental Location de material
Description
Labour Main-d'oeuvre
Field Supervision Supervision sur le terrain
Type
1 1 f ft In fi f 6 1
Type 1 '
Fi ri, J* Off it t
f}/ v f- h si;
Type
I/A P
Amount Montant
1 00
Totals Total global
qoo
z/lo
Total Direct Coata Total des couts directs
2. Indirect Costs/Couts Indlrects* * Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work. Pour le remboursement de* travaux d* rehabilitation, le* couts Indirect* ne sont pa* admissible* en tant que travaux d'evaluatlon.
Type
Transportation Transport
Food and Lodging NourrKur* et hebergementMobilization and DemobilizationMobilisation et demobilisation
DescriptionTypa
Aufa
fi
7
DC/^difr*- neUclVcl
JUL 8 199:
MINING EANDS Una
Amount Montant
/9?2
So
~
MCH
Sub Total of Indirect Coats Totsl psrtlel des coOts Indlrects
Amount Allowable (not greater than 20H of Direct Coal*) Montant admissible (n'excedant pas M H des eoOta directs)Total Value of Assessment Credit Valeur total* du crMK (Total of Direct and Allowable d'evaluatlon Indirect costal Total dM eatta dbeete
Total* Total global
l tt Lv\'
5V. ,
fyrt2Wiffi^IttK
tt In
Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.
Note : Le titulalre enreglstre sera tenu de verifier les depenses demandeas dans le present etat des coOts dans les 30 Jours survant une demande a cet effet. Si la verification n'est pas effectuee. le mlnlstre peut rejeter tout ou une partle des travaux d'evaluatlon presentee.
Filing Discounts
1. Work filed within two years of completion is claimed at I000xb of the above Total Value of Assessment Credit.
2. Work filed three, four or five years after completion is claimed at 500xb of the above Total Value of Assessment Credit. See calculations below:
Total Value of Assessment Credit Total Assessment Claimed
x 0.50
Remises pour depotCO CO
cr1. Les travaux deposes dans les deux ans sutvanT tourjKMvement sent
rembourses a 100 H de la valeur total* susmentjppneeAJ cfsdtt (revaluation.r~* ~"•^ rv; ^ '
2. Les travaux deposes trois. quatre ou cinq sjfiaprfi leu* achievement sont rembourses a 50 M da la valaur totale du; grdoTl (^valuation usmentionne. Volr les calculs cl-dessousT* ' - c
Valeur totale du credit d'evaluatlon (Equation total* demand**x 0.50 -
Certification Verifying Statement of Costs
l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.
that as o, -ecHolder.(Recorded Holder. Agent, Position in Company)
to make this certification
Attestation de I'etat des coOts
J'atteste par la presents :que les montants Indlques sont Is plus exact possible et que ces depenses ont ste engage** pour effectuer les travaux d'evaluation sur les terrains Indiques dansSaJormule de rapport de travail ci-joint.
l am authorized Et qu'a titre de je suls autorise(tltuialre enregtotre, representant. poete oocupe dan* la eompagnle)
a faire cette attestation.
Signature Date
r
Ci
SI -e (NJ
So
Co
v/ CJN
vj
OD ON
I IIOv.
i"
-si
Iff Hi1
•\\
iV
i
N*O
Work
to
be
Claimed
at
Cre
dits
you
are
cla
imin
g in
this
repo
rt m
ay b
e cu
t bac
k. I
n or
der t
o m
inim
ize
the
adve
rse
effe
cts
of s
uch
dele
tions
, pl
ease
indi
cate
from
w
hich
cla
ims
you
wis
h to
prio
rlze
the
defe
tion
of c
redi
ts.
Plea
se m
ark
(s)
one
of t
he f
ollo
win
g:
1.
O C
redi
ts a
re t
o be
cut
bac
k st
artin
g w
ith t
he c
laim
lis
ted
last
, w
orki
ng b
ackw
ards
.
2.
D C
redi
ts a
re t
o be
cut
bac
k eq
ually
ove
r al
l cla
ims
cont
aine
d in
thi
s re
port
of w
ork.
3.
D C
redi
ts a
re to
be
cut b
ack
as p
rioriz
ed o
n th
e at
tach
ed a
ppen
dix.
In t
he e
vent
tha
t yo
u ha
ve n
ot s
peci
fied
your
cho
ice
of p
riorit
y, o
ptio
n on
e w
ill b
e im
plem
ente
d.
Not
e 1:
Ex
ampl
es o
f ben
efic
ial I
nter
est a
re u
nrec
orde
d tra
nsfe
rs, o
ptio
n ag
reem
ents
, mem
oran
dum
of a
gree
men
ts, e
tc.,
with
resp
ect
to t
he m
inin
g cl
aim
s.e
Not
* 2:
If
wor
k ha
s be
en p
erfo
rmed
on
pate
nted
or
leas
ed la
nd, p
leas
e co
mpl
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the
follo
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g:
l cer
tify
that
the
reco
rded
hol
der
had
a be
nefic
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nter
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in th
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ased
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TOWNSHIP
LEGAULTM.N.R. ADMINISTRATIVE DISTRICT
NIPIGON 8 GERALDT
MINING DIVISION
THUNDER BAYLAND TITLES/ REGISTRY DIVISION
THUNDER BAY
JUl
^MINING
Ministry ofNaturalResources
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Branch ^O
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Oltl F EBRUARY, 1 981
DATE:
SEPTEMBER. 1989
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LOCATION MAPO 1mile
XLEGAULT TWP.
786T786
PARTRIGE LAKE
TB 813446
VEZINA LAKEBOULDERS
SAND and BOULI
TB 786141
TB 786140TB 8134474+00 N —
TB 813417
r- POND '-,
TB 786139
- , JVTB 8134204 + 00 S _
6+00 S —
786142
1 1 i ijyi i i * m i Ft il l l l 1 J.I l l l l l l l M l M M l l l l l l l LI l
POWERLINE
TB 1082429
TB 813418
TB 786145
LEGENDDiabases
Gabbro
/Tonalite(0uartz, Feldspar, Porphyry, Dyke)fMafic Metavolcanics(Vesicular)
\PilTowsT
Massive Mafic Volcanic
Fine-Grained Mafic Volcanic
Coarse-Grained Mafic Volcanic
PARTRIDGE LAKE
GalenaPyriteChalcopyritePyrrhotiteQuartz,CarbonateEpidote
Pop, B i r J ac k pine,Spruce,Balsam,Birch
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20+00 N
16+00 N
12+00 N
_ 8+00 N
4 + 00 N
( 076 tf ) Base Line
4 + 00 S
TB 813446
VEZINA LAKEBOULDERS
SAND and BOULDERS '
TB 786141
TB 813447 TB 813448
TB 813417
TB 813420
BIK Spf ^
TRENCHES
_ 12+00 S
TB 786142
OLD ROAD
16400 S
i lall 111 u 11 iS rl M M l l M l l l l l l M l l l l l l l l l l l l l l l l lit M l l l l M l l l l l M l l l l v V -v \s v \s \X i-11 ijK u-n i 11 M 11 11 l M l l l I.! l l l l l l t M L l l t l l l l l/l l M l M l M lt l l l l l l l l l l l l l l I.I l If l lL'.'.'"J l l l l t l ri M i l l l l l
POWERLINE
TB 1082429TB 1082430 20+00 S
TB 813418
24+00 S
LEGENDSYMBOLS
go .. - -.. -.. Bedding
Shearing
. Outcrop
Outcrop Area
Geological Rock Contact
Gabbro
./Tonalite(Quartz, Feldspar, Porphyry, Dyke)
*Mafic Metavolcanics(V^sicular)(Pillows)
Massive Mafic Volcanic
Fine-Grained Mafic Volcanic
Coarse-Grained Mafic Volcanic
Diorite
- tocoSturgeon Bridge Property
LEGAULT TOWNSHIP ONTARIO
Swamp(Cedar, Black Spruce)
Claim Post
Claim Line
Road Creek
Fault
. . Diamond Drill Hole
Railway
Powerline
GEOLOGYGalenaPyriteChalcopyritePyrrhotiteQuartz,CarbonateEpidoteJackpine,Spruce,Balsam, Birch
Updated from Rainboth (1990) by B.Kowalski
JUL 8 1993
MINING LANDS BRANCH
Property holder F.Checkley
Scale: r-200 Date: Sept.1992
8 + 00 S
PARTRIDGE LAKE
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