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42A82NW8188 2 .9683 CLEAVER 010
SUMMARY REPORT
ON THE
1986 EXPLORATION PROGRAM
ON THE CLEAVER TOWNSHIP
LARDER LAKE MINING DIVISION
PROPERTY OF
CLEYO RESOURCES INC.
PROJECT #6436
RECEIVED
MINING ILANDS SECTION
Timmins, Ontario by: Stephen Conquer, B.Se.
December 19, 1986 for: David R. Bell
Geological Services Inc.
TABLE 42A02Nweie8 2.9683 CLEAVER 010C
I.0 SUMMARY l, 2
2. O INTRODUCTION 3
3.0 LOCATION AND ACCESS 4
4.0 PROPERTY AND OWNERSHIP 4
5.0 PHYSIOGRAPHY AND CLIMATE 5
6.0 POWER AND WATER 6
7.0 ANCILLARY SERVICES 6
8.0 PREVIOUS WORK 6, 7
9.0 REGIONAL GEOLOGY AND STRUCTURE 7
9.1 REGIONAL GEOLOGY 7, 8
9.11 METAVOLCANIC ROCKS 8
9.12 METASEDIMENTS 9
9.13 INTRUSIVES 9, 109.2 REGIONAL STRUCTURE 10
10.0 PROPERTY GEOLOGY AND STRUCTURE 10
10.1 PROPERTY GEOLOGY 11
10.1.1 MAFIC FLOWS 11, 12
10.1.2 INTERMEDIATE TO MAFIC TUFFS 12
10.1.3 INTERMEDIATE TO FELSIC FLOWS 12, 13
10.1.4 FELSIC INTRUSIONS
10.2 PROPERTY STRUCTURE 13, 14
II.0 MINERALIZATION AND 14 MINERALIZED SHOWINGS
11.1 A-ZONE 14, 15
11.2 B-ZONE 15, 16
12.0 GEOPHYSICS 16 , 16a
13.0 CONCLUSIONS 17
14.0 RECOMMENDATIONS 18, 19
15.0 COST ESTIMATES 19, 20, 21
CERTIFICATE OF QUALIFICATIONS
REFERENCES
TABLE OF CONTENTS cont'd
List of Figures
Figure l
Figure 2
Figure 3
Figure 4
Figure 5
Figure 6
Figure 7
Figure 8
Figure 9
Figure 10
Location Map - Provincial
Location Map - Regional
Claims Configuration
Topography
Sand and Gravel Resource Map
Timmins-Kirkland Geological Compilation (OGS Map 2205)
A-Zone: Geology, Assays and Sample Locations
Magnetometer Survey
VLF-EM FRASER FILTER
Induced Polarization - Filtered Data: 7, Frequency Effect
List of Tables
Table l
Table 2
List of Maps Map 6436-86-3- Map 6436-86-4-
Map 6436-86-5-
Map 6436-86-5-
Map 6436-86-5-
Map 6436-86-5-
Map 6436-86-5-
Map 6436-86-5-
Claim Status
Previous Regional Exploration Activities
l Sample Location and Assay Planl Geology Map
1 Pseudo Sections L4E
2 Pseudo Sections L2E
3 Pseudo Sections LO
4 Pseudo Sections L2W
5 Pseudo Sections L4W
6 Pseudo Sections L8W
Apendicies
Appendix l
Appendix 2 Appendix 3
Sample Locations and Assay Results
Assay Certificates
Whole Rock Geochemical Results
Technical Data Statement
1.
.O SUMMARY
The Cleyo Resources-Cleaver Township property is
located in an area which has only seen sporadic exploration
since the early 1900's. In the spring of 1986, Mr. Cleo
Clement in the company of the property vendor, undertook a
site examination. From this property visit several grab
samples were collected, from which highly anomalous assay
results (0.10-0.20 range) were received. These encouraging
results, prompted Mr. Clement on behalf of Cleyo Resources
Inc. to approach the firm of David R. Bell Geological Services
Inc. with a request that a property visit be made and intro
ductory report be prepared. It was as a result of this visit
and report that the recommended exploration program was initi
ated. In light of the late start to the program and the early
arrival of winter, the proposed program could not be completed
and as a result, only the mapping and IP surveys were finished.
A minor amount of stripping was completed late in
the program, with these new exposures to be examined during
the recommended program.
The property was found to be underlain by a series
of interbedded intermediate to mafic flows. These flows show
a variety of flow features, strike northeast-southwest, dip
steeply to the south, and vary from non-magnetic to highly
magnetic.During the mapping program two auriferous zones were
located. One of these showings is located in the same outcrop
as the "Main Showing" that had been previously visited by the
author. Examination of this showing, which was limited by a
lack of good weather, found a highly brecciated, altered and
mineralized rock that gave assays of up to 0.088 oz Au/ton.
The second gold showing, also the site of some earlier trench
ing, was hosted by intermediate to mafic volcanics that have
2.
silicified and mineralized. Assays from this zone of
up to 267 ppb Au were received. The results from both zones
are found to be very encouraging in light of the limited
work that has been completed. These zones also show a cor
relation with either magnetometer, VLF-EM, or IP anomalies.
Due to these promising results, a three phase
exploration program totalling S263,000.00 has been recommended.
The initiation of this third phase will be contingent upon the
receipt of encouraging results from the first two phases.
..O INTRODUCTION
In October of 1986 the firm of David R. Bell Geolo
gical Services Inc. was contracted to initiate a exploratory
program. This program was recommended as a result of a prop
erty visit made during May of 1986 and a search of all pertin
ent company and government information. The McNeil-Cleaver
Township area is the location of several gold showings, but
at the time has received only sporadic exploration activity.
One showing in McNeil Township is hosted by mineralized rock
that contains visible gold.
B tour^-tlf o{
Tin hoi! t! DJiVi
Property Location
. J Vf^.'i S. fA-:'-::s-
Savld R. Bell Geological Services Inc.
CLEYO RESOURCES INC.
LOCATION MAP
PROVINCIAL
Tw^/Area cleaver Two..Mining DivisionRclorcooo*
; DrawnScale
Larder Lake
Ore f todOat* June 17/86
Bovine* ont.Project 6436N.T.S.ChocKod
^^J^iS^^TU
.0 LOCATION AND ACCESS (see Figure l and 2)
The Cleyo Resources property is located 29 miles south- east of the city of Timmins in Cleaver Township, Larder Lake Mining
Division, in the District of Timiskaming, Ontario. This claim
group is found in the west-central portion of the township at 48.13 degrees north latitude and 81.47 degrees east longitude.
Access to Cleaver Township is gained by travelling approx imately 30 miles on the Langmuir Road, an all weather lumber road that runs southwest from the town of South Porcupine. Once in the vicinity of the property, three routes can be used to access the
northwest, north-central and south-central portions of the claim group. These access routes can be travelled using a two-wheel .
drive vehicle, but spring and fall weather may necessitate a
vehicle with four-wheel drive capabilities.
4.0 PROPERTY AND OWNERSHIP (see Figure 3)
The Cleyo Resources, Cleaver Township property is com posed of 27 contiguous unpatented mining claims (see Table 1) which are held in trust by Mr. Cleo Clement of Timmins, Ontario.
The property was optioned from Mr. William Dellaire of Timmins, Ontario, in January of 1986 and at that time consisted of only 23 claims. After reviewing the results of previous geo physical surveys and noting the location of the primary showing, the author recommended that an additional four claims should be staked. The acquisition of these claims would give complete coverage of this principle showing and any possible strike exten sion. These claims were subsequently staked in April of 1986, bringing the total number of claims to the present twenty-seven.
At the present time the 23 original claims (various recording dates in 1983) are under extension until Dec. 31, 1986, and require 40 days of assessment credits. The filing of this report for linecutting and geological survey credits will fulfill the necessary requirements to keep all claims in good standing until their respective anniversary or next filing dates in 1987 and 1988.
KF.TTli ,-LAKES .PROVINCIAL PARK
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David R. Bell Geological Services Inc.CLEYO RESOURCES INC.
LOCATION MAP
REGIONAL
Twp/Ar*. CLEAVER TWP. Pro vine o ON TMining Division LARDER LAKE Pro)* C t 6430
DrawnScat* 1:266000
DraftedDate JUNE
N.T.S. 42-A
Shoat FtQ.1
i as 11!s ..- - — -J - -
David R. Bel! Geologlcat Services Inc.CLEYO RESOURCES INC.
CLAIMS CONFIGURATION
Twp/Arca C leaver Twp.Minim OMttoii Larder Lake Pro)*ct 6436
H.T.S. A 2A/3
TABLE l
CLEYO RESOURCES INC. - CLEAVER TWP. PROPERTY
PROJECT 6436
CLAIM STATUS
Claim No. Recording Date
L724470 June 30, 1983
L724474 July 25, 1983
L725147 September 15, 1983
L725148 September 15, 1983
L725149 September 15, 1983
L725150 September 15, 1983
L725151 September 15, 1983
L725152 September 15, 1983
L725153 September 15, 1983
L725154 September 15, 1983
L725155 September 15, 1983
L725156 September 15, 1983
L725158 September 15, 1983
L725161 September 15, 1983
L725162 September 15, 1983
L749741 August 23, 1983
L749742 August 23, 1983
L749743 August 23, 1983
L749744 August 23, 1983
L749745 August 23, 1983 .
L749746 August 23, 1983
L750507 September 15, 1983
L750508 September 15, 1983
L916183 April 30, 1986
L916184 April 30, 1986
L916185 April 30, 1986
L916186 April 30, 1986
*Claims under extension until Dec Report of Work submitted Dec. 9,
Next F iling Da te
June 30, 1986
July 25, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
September 15, 1986
August 23, 1986
August 23, 1986
August 23, 1986
August 23, 1986
August 23, 1986
August 23, 1986
September 15, 1986
September 15, 1986
April 30, 1987
April 30, 1987
April 30, 1987
April 30, 1987
31, 19861986
No. of Days Required
40
40
40
40
40
40
40
40
40
40
40
40
40
40
40
40
4040
40
40
40
40
40
20
20
20
20
5.
0 PHYSIOGRAPHY AND CLIMATE ( see Figure 4)
The Gleyo property is situated in an area of mixed topography. A general pattern of low relief dominates this region with the elevation ranging from 1050 to 1150 feet above sea level. In the west half of Cleaver Township an area of moderate to high relief is present, here the terrain attains a maximum of 1500 feet above sea level. This north trending area of higher ground is probably caused by the Middle-Precam- brian Sediments of the Cobalt Group.
The claim group is drained by numerous lakes and rivers of the Nighthawk River system. This river system flows north and eventually drains into Nighthawk Lake.
Vegetation and overburden are typical of Northern Ontario. Sand, gravel and moderate to well developed "B" soil horizons are found in the higher better drained areas of the claim group, where poplar, birch, spruce and local stands of balsam fir are located. The lower lying areas of this property are covered by clay and water rich organic soils. It is in these areas that stands of cedar, spruce and alder dominate. In all areas, numerous types of mosses and grasses are present.
As a result of the Northern Ontario Engineering Geology Terrain Studies that were completed by the Ministry of Natural Resources, several sources of sand and gravel were located in this region (see Figure 5). In fact one such source is located on the Cleyo property. This source is a north trending esker that is found in the southeastern portion of the property. The Ministry has estimated that these local sources have a medium to high poten tial for coarse aggregate. These coarse aggregates will be valuable if the construction of access roads or mining facilities is ever initiated.
The climate of the area is characterized by hot, humid summers and long winters. An abundance of snowfall, and extreme cold are common during the winter months.
f •NDA'OCKtVlt MlOUKClt MAP (ICtNO
i ^ R* BeH Geological Services foe.CLEYO RESOURCES INC.
SAND AND GRAVEL
RESOURCE MAP
Cleaver Twp.givWon Larder Lake
00.000DrsrtedData June 17/86
A2A/SEChecked M .B. R
Fig. 5
..O POWER AND WATER
The power requirements for any early stages of explora
tion or development would have to be supplied by diesel generators
Although a major north-south power line is located 12 miles due
east of the Cleaver Township property, it may be more cost effect
ive to construct a power line from Matachewan, which is located
approximately 21 miles to the southeast. This is due to the fact
that the appropriate sub-stations are already present and there
fore construction costs may be minimized.
An abundant water supply for any exploration or early
development programs is present within the boundaries of this
property. If greater quantities of water are required, then
accessing the larger lakes to the southwest, or Nighthawk Lake
to the north, should meet any foreseeable requirements.
7.0 ANCILLARY SERVICES
All goods or services that would be needed for any of
the various exploration or mining phases could be acquired from
the city of Timmins.
8.0 PREVIOUS WORK
Prospecting and exploration for gold had begun in the
Matachewan district in as early as 1909, but the attention of
the prospectors soon swung to silver, as the discoveries near
Gowganda and Elk Lake were made. When the news of a major gold
discovery within the Porcupine Camp (1909) became wide spread,
the Matachewan area saw a renewed interest in gold exploration.
Numerous occurrences were uncovered in the townships of Powell,
Cairo, Alma and Baden. As well as private exploration, several
geological and topographical surveys were conducted by govern
ment agencies during the 1910's, especially in the vicinity of
the then, most current gold discoveries.
It was not until 1923 that any gold discoveries were made in the Cleaver-McNeil Townships area. Three Indians named Isador, Micmack and Tom Fox uncovered a gold showing in the south-central part of McNeil Township. This discovery led to the uncovering of several more occurrences in McNeil Township and eventually, Mr. Dan O'connor located two gold showings in the west-central section of Cleaver Township. Apparently nothing of significance ever came of these discoveries.
The Cleaver-McNeil area received very little attention during the intervening years between the 1920's and the 1950's. When exploration activities again increased, the bulk of the work was concentrated in the west half of Cleaver and the eastern part of McNeil Township. The companies and their respective explora tion activities as conducted in Cleaver Township are listed in Table 2.
The only work that has been recorded for the vicinity of the present Cleyo Resources property, has all been completed since 1974. Stripping and trenching have been completed by J. Boissoneault and R. Rousseau on ground that is now covered by claims L724470 and L724474. Linecutting, magnetometer and VLF-EM surveys were completed in early 1984 under a previous option agreement. The assessment credits for this work are still valid and in fact are being used to keep the claims in good standing. These surveys have outlined several areas of interest that have as yet not been examined.
9.0 REGIONAL GEOLOGY AND STRUCTURE (see Figure 6)
9.1 Regional Geology
Cleaver Township, and subsequently the Cleyo Resources property, is underlain by rocks that are entirely Precambrian age. The majority of the bedrock belongs to the Abitibi Green stone Belt, which being Early Precambrian or Archean in age, is a tectonically differentiated portion of the Superior Province
l
iTABLE 2
CLEYO RESOURCES INC. - CLEAVER TWP. PROPERTY
PROJECT #6436
PREVIOUS REGIONAL EXPLORATION ACTIVITIES
Jjleaver Twp.
ompany
Airiax
1 mperial Oil
JFeck
Joranda
tomstate Res. td.
w 'Connor
Jiamothe , Charles
T'exmont
Lang, Bert W.
1cNeil Twp.
fcompany
Noranda
C)ominco
1
1
Activity Year Assessment File No.
trenching, assaying, Oct. 76-Oct. 77 429441
HLEM, Max-Min
ground EM and Mag 1982 420367
Seismic, mag, drilling 1980-1981 537428
for placer gold
mag, HEM 1981 2.4423
mag, EM ? 2.4762
correspondence 1924 330
EM, drilling 1956 T-643
EM profiles 1965 ?
EM 1966 63.1838
Activity Year Assessment File No.
EM, mag ? ?
EM, mag ? ?
ii
8
'f the Canadian Shield. Rocks of Middle and Late Precambrian
age are respectively represented by Cobalt Group sediments and minor intrusions of diabase.
The Abitibi Greenstone Belt, in the vicinity of Cleaver Township, is composed of variably metamorphosed igneous, sedi
mentary and volcanically derived rocks (Pyke, 1978).
9.11 Metavoleanic Rocks
The metavolcanic rocks of this area are represented by at least two cycles of volcanism. The ultramafic rocks occupy
the lowest position of each cycle, while the mafic, intermediate and felsic rock types sit in respectively higher stratigraphic locations. The lowest of these two cycles, trends in a north-
south direction through Fripp, McArthur, Bartlett and English
Townships. The dominant, or upper cycle, shows an east-west, as opposed to the expected northerly trend. This may in part
be the result of the intrusion of the Geikie Pluton, even though the regional magnetometer survey suggests that this east-west trend, is more typical of the Cleaver-McNeil area.
The ultramafic metavolcanic rock types are by far the most sparcely distributed. Massive, polysutured and spinifex textured flows are the most common of these rocks, while pyro clastic units are found locally.
The most dominant of all rock types in this area are the mafic to intermediate metavolcanics. Lithological varieties included within these units are the massive, pillowed and vario
litic flows. In conjunction with these flows, pyroclastic rocks in the form of tuff, lapilli tuff and volcanic breccia are found.
The felsic metavolcanic rocks are represented by massive
and pillowed flows as well as the aforementioned types of pyro clastic rocks. Centers of felsic volcanism are located in the
area of Douglas-Fallon-Fasken and McArthur-Bartlett-English-Hutt Townships.
.12 Metasediments
Metasediments apparently, form only a very small portion
of this section of the Abitibi Greenstone Belt, comprising no more
than five percent of the exposed area. Where noted by previous
workers, the Early Precambrian metasediments are found to be assoc
iated with the intermediate to felsic volcanics (Pyke, 1978).
Middle Precambrian metasediments are represented by the Cobalt
Group, which in this area is composed of arkoses, greywackes and
argillites. These rocks lie in a thin band that runs in a north-
south direction through Montrose, Hincks, Cleaver and Fallon Town
ships .
9.13 Intrusives
The intrusive rocks which are present in this area,
range in chemical composition from felsic to untramafic.
The major felsic intrusions, such as the Peterlong Lake
Complex, and the Adams and Geikie Plutons, are composed of feld
spar and quartz porphyries, trondhjemites, granodiorites, quartz
diorites and diorites. Smaller intrusions of the same relative
compositions are also present in this area along with intrusions
of syenitic composition such as the Fallon Stock.
A large zone of mafic to ultramafic intrusions, is found
in the central portion of the lower most volcanic cycle, sitting
at the contact between the mafic and the intermediate to felsic
volcanics. There appears to be a genetic relationship between
these intrusive bodies and the more "felsic" rock types, as is
noted by their close spatial association in the Bartlett-McArthur
and Zavitz-Hutt Townships area. These intrusives may be composite
bodies of the following, gabbro, gabbroic anorthosite, pyroxenite,
serpentinized peridotite, and quartz gabbro. Other gabbro intru
sions have been noted in McNeil Township. As a result of the
10
linear magnetic trends in the Cleaver-McNeil area and the mag
netic anomalies in Cleaver Township it is possible that other
mafic stocks or plugs may be located within the vicinity of the
project area,
9.2 Regional Structure
As previously noted, the volcanic rocks of this area
show two major trends. The lower cycle trends north-south, gen
erally dips to the east at 65 to 80 degrees (local variations
are present), while tops face east showing that these units have
not been overturned. Except for major north-south faults these
rocks do not appear to have been severely deformed, at least
folding on a large scale is not evident.
The upper volcanic cycle, has undergone deformation,
by both folding and faulting. Numerous anticlinal and synclinal
structures are located within Douglas, Zavitz and Hutt Townships,
These are crosscut and offset by the northerly and northwesterly
trending faults that transect this area.
Details as to the structural make-up of the Cleaver-
McNeil area are limited due to the lack of any detailed explor
ation by either government or private industry.
10.0 PROPERTY GEOLOGY AND STRUCTURE
During the course of the mapping program approximately
200 bedrock outcroppings were examined for geological, mineral
ogical and structural information. Although this sounds like a
substantial amount of exposure, it in fact represents only about
ID-15% of the entire property. In so far as this is the situ
ation, geophysical (magnetometer and VLF-EM) data from previous
surveys was used as an interpretational aid to develop a geolo
gical framework from which further exploration could be recom
mended.
11.
10.1 Property Geology (see Map 6436-86-4-1)
The Cleyo Resources-Cleaver Township property is
found to be underlain by rocks that are of early Precambrian
age. Through field examinations the following rock types
have been recognized; magnetic and non-magnetic mafic flows,
intermediate to mafic flows and minor felsic intrusions.
10.1.1 Mafic Flows
By far the most dominant rock types that were seen
during the mapping program, are the mafic flows. Visual clas
sifications, based upon colour and mode of occurrence, suggest
that these rocks are of basaltic composition. Major and trace
element geochemical analysis has for the most part confirmed this
assumption.The geochemically determined rock types were dominantly
found to be of the tholeiitic chemical trend, while being of
either basaltic or "iron-rich" basaltic composition. A few
exceptions were noted. One exposure located at L8W at 0+30N
is still of the tholeiitic chemical trend but is of andesitic
composition. This is not uncommon by virtue of the fact that
the exposure sits near a flow top environment and may only be
an isolated occurrence. The other exception, located on L16W
at 28+50N and while being of basaltic composition is found to
be of the calc-alkalic chemical trend. This analysis matches
with the magnetometer survey which shows a trend of lower suscep
tibility in the area.These basalts are found as both massive and pillowed
flows, while well developed sections of flow top breccia are
locally noted. The massive flows being green to dark green in
colour range from aphanitic to coarse grained in texture, with
the fine to very fine grained varieties being dominant. It is
only within the coarse grained sections that the mineraology can
be discerned, and then only the plagioclase feldspar from the
mafic (pyroxene-amphibole) component. Well developed sections
of pillowed flows are seen to top the massive sections, with
12.
^pndividual pillows attaining dimensions of at least four feet
in length and three feet in width. Locally the pillows may contain well developed vesicules which can be used for tops
determination. The selvages are seen to contain both vario
litic growths and hyaloclastite (glass shards). The flow top breccia are characterized by angular to sub-rounded flow brec ciated fragments in a chloritic matrix, which may contain both
variolites and hyaloclastite.All varieties of basalts, whether massive, pillowed
or flow breccias were found in both magnetic and non-magnetic phases. The magnetic and some non-magnetic sections have been chemically defined as iron-rich tholeiites, while the non-mag netic sections are represented by iron-rich tholeiitic basalts,
tholeiitic andesites and basalts, and calc-alkalic basalts.
10.1.2 Intermediate to Mafic Tuff
Only one exposure of tuffaceous rock was round during the course of the mapping program. This outcrop, located on L16W at 17+40N is composed of a grey to grey-green rock, which weathers to a buff colour and shows definite, clastic features when examined closely. The rock is composed of approximately equal proportions of rounded to sub-rounded quartz and feldspar clasts, that are supported by a chlorite-muscovite-carbonate rich matrix. Both orthoclase (pink) and plagioclase (zoned) are found to represent the feldspar minerals in the portion of the clasts.
10.1.3 In t ermediat e to Felsic FIows
Exposures of the intermediate to mafic flows have been located in the south-central section of the property. These exposures all appear to be part of the same northeast trending unit. This horizon is coincident with a zone of low
susceptibility, as is expected from visual examination,
rocks are characterized by their pale grey to green and
locally grey green colour, dominantly aphanitic texture and
lack of magnetic response.
Geochemical analysis of these rocks has returned rhy-
olitic compositions of both the calc-alkalic and tholeiitic
chemical trends. This is in agreement with the gross visual
aspects of these rock units.
An exposure of these flows is located at 6+OOW and
7+20S, these rocks are found to contain up to 102 fine grained
disseminated pyrite, and are extremely hard. At this time it
is unknown whether these features are of primary origin or are
a result of an alteration process. Samples from this outcrop
have been collected and analyzed, the results are discussed in
the mineralization and alteration section.
10.1.4 Felsic Intrusions
Two felsic intrusive exposures were located as a
result of the geological mapping. The first of these, located
on L8W at 0+80N, is a rock of intermediate composition, that
shows a dominantly grey colour with green to dark green mafic
clots, and has an aphanitic texture. The exact nature of the
mineralogy is undiscernable due to the microscopic grain size.
The second exposure is located at 15+OOW-5+85N. This
rock is of syenitic composition. This classification is based
on colour alone, as the fine grained nature of the rock does
not allow for mineralogical determinations. The pink colour
represents the dominant orthoclase feldspar, while the black
mineral (S-5%) represents the mafic component.
10.2 Property Structure
The Cleyo claim block is underlain by a northeast-
southwest trending series of intermediate to mafic metavolcanics,
with isolated felsic intrusions. Direction or tops determination
can be made due to the well developed and exposed flow structures.
These features or structures, are found in the form of flow top
breccia and pillowed horizons, and in conjunction with the ob
served grain size gradation in the massive flows, indicate
14.
4fea south facing (tops face south) sequence of variable magnetic
to non-magnetic volcanic flows. Since these rocks dip steeply to the south it can also be said that they are not overturned.
This information can be of incalculable value when trying to
determine possible extensions to known auriferous showings, as well as located areas of potential mineral wealth.
Two cross structures have been located via the surface
mapping. These structures have a northerly trend and are seen
to truncate and cause an offset to the geological continuity.
One structure a northeast trending shear zone has been located
on L8W at 15+85S. The exact extent of this shear is unclear,
but striking at 027 0 and dipping at 080 0 E it is believed that
it extends northwards to the baseline, as is also shown by the
offset in a southwest trending VLF-EM conducting (L12E at 3+OOS
to L12W at 12+50S). The second mapped structure is found in the vicinity of the principle showing at 0+40W and 1+10S, and
has a strike of 156 0 and a dip of 82 0 to the southwest, with a relative movement of west block-south and east block-north
being noted.
11.0 MINERALIZATION AND MINERALIZED SHOWINGS
All rock types, as mapped during this program display at least minor degrees of metallic mineralization, whether it
be primary pyrite or magnetite as in the mafic volcanics, or secondary pyrite as seen in the breccia-alteration zones, with
pyrite being the dominant form. Two areas of interest were located, but received only a limited degree of exploration due
to the early snowfall. Anomalous assay results were received from grab sampling that was independently conducted at both
locations.
11.1 A-Zone
The "A-Zone" was located in the same outcropping as the previously named "Main Showing", but these two targets at
15
present appear unrelated. A diagram of the A-Zone (Figure 7)
showing sample locations and assay results has been included.
This showing is located within a dark green, brecciated, car-
bonatized and magnetic rock that shows silicified and carbon-
atized fragments with 1 0-157, f ine grained disseminated pyrite.
Due to the types and degree of alteration and mineralization,
it was believed that these rocks would contain at least anoma
lous quantities of gold. The assays of up to 0.088 oz Au/ton
that were received from grab sampling of this zone show that
this was in fact the case (see Appendix I). This showing is
coincident with an T.P anomaly. (See the geophysics section
for a further description)
11.2 B-Zone
The second target or the "B-Zone", located at 6+OOW
and 7+20S, is the site of previous trenching. As is the case
with the A-Zone, the B-Zone has not received a thorough nor
complete examination. This showing is found within the inter
mediate to mafic volcanics, and is distinguished by the apparent
silicification, silica filled fractures and S-7% pyrite mineral
ization. Grab samples collected from this showing have returned
anomalous assays of up 267 ppb Au (0.008 oz Au/ton, This showing
is found to be coincident with a southwest trending "mag" depres
sion (L4E-5S to L8W-9S), as well as a similar trending VLF-EM
conductor (see Figures 8 and 9).
The IP survey has highlighted an area that shows
slightly higher chargeability. This zone is also coincident
with the Mag and EM, but the exact form is unknown as the sur
vey boundaries prohibited a full disclosure of this anomalous
zone. It is these multiple-overlapping anomalous zones, along
with anomalous assay results that place the B-Zone as a very
promising exploration target, which will require a thorough
field examination next season.
very fine-fine g magnetic mafic f
-0018
C(
(fine grained, blac "\tnagnetic mafic flo
0053
/•brecciated, altered, •| mineralized rock ^extent unknown
—•Fault
-0015-0014
very fine-fine grained, vesicular magnetic mafic flow
magnetic
Sample No.
6436-0014-0015-0016-0017-0018-0019-0020-0021-0022-0023-0024
6436-0051-0052-0053-0054-0055-0056
Assay Results ppb Au o z Au7ton
107
141977
0.08834
5493433494902210
9600.1080.0280.0420.036
*samples 6436-0051 to -0056 collected
David R. Bell Geological Services Inc.CLEYO RESOURCES INC.
A-Zone
Geology, Assays and Sample Locations
Twp/Aroa C leaverMining Division Larder LakeRoforonoooDrawnScalo
.s.w.c.l n"56 T Draftod S .W.C.Date Dec.. 1 986
Province On t.Proleot 6436N.T.8. - 42A/2 S 3 ChockedShoot 7
16
The "Main Showing" as described in a previous report (Conquer, 1986) did not receive any further examinations during this phase of exploration. Although this showing would appear to be of less importance than both the A- and B-Zones, it should still be examined during any further phase of exploration.
The anomalous assay results in conjunction with the coincident geophysical anomalies present both the A- and B-Zones as high priority exploration targets, that should receive a more detailed examination during the next field season.
12.0 GEOPHYSICS (see Figures 8-10 and Maps 6436-86-5-1 to -6)
An orientation Induced Polarization survey was con ducted as part of this exploration program. This newly acquired geophysical data was used in conjunction with previously acquired "mag" and VLF-EM data was used to interpret geological and miner alogical trends.
When the A-Zone was found, it was observed that the pyrite content was not high enough to produce a VLF-EM response, but with the observed 2-^3^ pyrite concentration, would be suf ficient to give an IP response. This survey did outline an elliptical zone that extends for approximately 1,000 feet from 3+OOW to 7+OOW and is about 500 feet wide straddling the base line. Also from this survey a second weak but distinct charge able zone was located. As previously mentioned, this zone is coincident with other anomalies that highlight the B-Zone.
The structure which is inferred to be associated with the B-Zone is shown to be at least 5,000 feet long by the VLF-EM and the mag surveys. This does not appear to be one continuous structure, but may be composed of several dependent sections.
Several other parallel to sub-parallel structures can be inferred from the mag data, but apparently lack the similar EM association as is found with the B-Zone. An attempt should be made to further delineate the B-Zone geophysical structure in light of the current evidence.
— 8+00 S
David R. Bell Geological Services Inc.CLEYO RESOURCES INC.
INDUCED POLARIZATIONFILTERED DATA
K FREQUENCY EFFECT
Twp/Area Cleaver TownshipMining D ivision Larder LakeReferencesDrawn S. W. C.Scale I "e400'
Drafted S. W. C.Dato ec. 1986
Province OntarioProject 6436N.T.S. 4 2A/2, 3CheckedSheet 10
16a
ft Analysis of the magnetometer date reaffirms what has been seen from the mapping and that is a series of magnetic to
non-magnetic flows. At least within the confines of the Cleyo
property, a definite magnetic trend can be seen to exist. This
trend shows that the southern portion of the property is domin ated by a series of highly magnetic, presumably, "iron-rich"
tholeiitic basalts. While other highly mganetic "zones" are
defined, they decrease in both length and width becoming only
isolated occurrences. As has been shown by the geochemistry, a correlation can be drawn between the high magnetic suscep
tibility zones and the tholeiitic basalts, as well as the less susceptible or non-magnetic zones and the calc-alkalic rocks.
•C
O
— 40+00 N
- 20-t-O" N
-,.,. ..^'1 ; V— 20-t-OO S
~ 40+00 S
59,00'J
59,500
;:0,,000
59,000
59,500
60,000
zn.l - n
degression
David R. Belt Geological Services inc. iCleyo Resources Inc.
MAGNETOMETER SURVEY
Twp/Aroa Cleaver TwpMiiinq Oiv's io " : Larder LakeR o f ? r -? o c o sOrawn:S.W.C. DraftedSca'u - l": I000 1 'Offer Dec. 1 986
r.iC'i': Ontorio Ject 6436 |S'- 42 A/2, 3 f
-f. llS n f w t a
— 40-*-00 N
- 20+0^ N
— Baseline
- 2O+00 S
- 40 + OO S
David R. Bei! Geological Services inc.Cleyo Resources Inc.
VLF-EM FRASER FILTER
T w p/A r ;* o : Cleaver TwpM in: "q D i vis ie r*; Larder Lake
D ' s w f ' S.W.C- S -j 3 i fi : l " ; 1000* ' D 3 ; e : Dec. 1986
O rov : nce: Ontario " O ro;'';t : 6436
h H e t
17
.3.0 CONCLUSIONS
The geological mapping program which was completed
over the 27 claim Cleaver Township property of Cleyo Resources, was done so for two reasons. First, to gain a better under
standing of the local geology, mineralogy and stratigraphy such that a better insight could be gained into the source of and to
extend to the gold bearing zone of the "Main Showing." Second,
to locate other areas of possible economic significance. This
mapping program was in fact only one part of a previously recom
mended multiphase exploration program.It was found that the property was underlain by a
series of magnetic to non-magnetic basalts, intermediate to mafic flows and tuffs and localized felsic intrusions. These rocks have a northeast-southwest strike, dip steeply to the south and show a tops up configuration. From geochemical analysis it would appear as if the basalts, both magnetic and non-magnetic varieties are of the iron-rich tholeiitic trend, while the intermediate to mafic flows were magnesium-rich tholeiites.
The amount of structural data acquired through the mapping, precludes any meaningful interpretation beyond the mention that cross-faults or structures are known to exist. Their influence on any auriferous zones is at present unknown, and will only be understood as a result of future exploration.
In light of the completed work, two promising aurif erous zones were located. Both the A- and B-Zones were only examined in the most precursory fashion, due to the sudden arrival of winter. These zones have given definitely encour aging results, such that further work is a necessity. There fore the following recommendations are made.
18.
.4.O RECOMMENDATIONS
With the discovery of two gold bearing zones on the Cleyo Resources property, it is recommended that a two and possibly three phase exploration program be completed, such that these showings can be properly evaluated. The work that has been completed to date was only a small part of a larger scale program, that due to deteriorating weather conditions, could not be completed.
The first phase will consist of linecutting and geochemical sampling. The lines will be cut to facilitate completion of program segments from all phases of work. The sampling and subsequent analysis of the humus and "B"-horizon material across both A- and B-Zones, will serve to generate a "geochemical signature", which it is hoped can be used to show the aeria^. extent of these auriferous zones, as well as a base against which future geochemistry results can be compared. This work by its very nature must be completed before the stripping is started and the overburden is forever disturbed.
Phase two is designed to actually open up and physi cally examine both showings plus geochemically investigate other areas on the property. This phase will consist of strip ping, trenching, sampling, assaying and geological mapping. Through this work an overall geological picture can be developed, so as to further define the potential economic significance of these showings.
The other areas of interest that are outside the principle showings and that are either geologically or geophy- sically inferred should be examined. This examination may be best completed via geochemical sampling, especially in areas of poor exposure and shallow overburden (less than 20 feet).
The budget for the geochemical sampling has been calculated for coverage of the entire property. This may in fact not be practical due to overburden thicknesses, but it should be included in the planned program.
19,
Diamond drilling is proposed for the third phase of this program, and will be contingent upon the results of the two previous phases. At the present time a 5,000 foot drill program is envisioned for the two known showings. The planned footage is based upon an equal split of 2,500 feet per showing, Program modifications may be made upon in field results.
The above recommended three phase program is esti mated to cost S263,000.00
15.0 COST ESTIMATES
Phase I
Linecutting
-estimated @ 5 miles for grid extension and detailed lines-5 miles @ $325./mile 1,625.00
Orientation Geochemistry Survey on the Detailed Grid,-^-^^^-^—^
-50 foot sample intervals-360 samples of both humus and B-horizon therefore 720 samples
-720 samples @ 76 samples/day = 9 .6 days-9.6 days @ $200./day
Soil Analysis
-720 samples @ $ll./sample
Supervision
-3 days @ 3300./day
1,920.00
7,920.00
900.00
Meals and Accommodation
-13 man days @ $40./man/day
contingencies Phase I total
520.0012,885.001,288.50
S14,173.5O
20.
II
Stripping and Trenching
-20 days @ $l,000./day 20,000.00
Assaying
-200 samples @ 511. /sample 2,200.00
Geological Mapping
-geologist and assistant
-20 days @ 5500. /day 10,000.00
Property Geochemistry
-100 foot sample interval
-1,689 samples @ 75 samples/day-23 days @ 5200. /day A, 600. 00
Soil Analysis
-2,409 samples @ 511. /sample 26,499.00
Supervision
-10 days @ 5300. /day 3,000.00
Meals and Accommodation
-53 man days @ 540. /man/day 2,120.00
Supplies 2,000.00
Secretarial
-5 days @ 5160. /day 800.00
Report and Drafting
-10 days @ 5500. /day 5.000.0076,219.00
102 contingencies 7,621.90 Phase II total 583,840.90
21
III
Diamond Drilling
-5,000 feet @ 330. /foot all incl . 150,000.0010^ contingencies 15,000.00Phase III total S165,000.00
Total
Phase I 14,173.50 Phase II 83,840.90 Phase III 165,000.00
263,014.40 say $263,000.00
Respectfully submitted by,
December 19, 1986 Stephen Conquer, B.Se. Timmins, Ontario
CERTIFICATE OF QUALIFICATIONS
I, Stephen W. Conquer, hereby certify:
1. that I am a geologist employed by David R. Bell
Geological Services Inc., 261 Third Avenue, Timmins, Ontario
2. that I am a graduate of the University of Waterloo, holding a Bachelor of Science
degree (1979)
3. that I have been practising my profession as
a geologist since 1979
4. that I do not have nor do I expect to receive
either directly or indirectly, any interest in this property or the securities of Cleyo
Resources Inc.
rTimmins, Ontario Stephen W. Conquer, B.Se. December 19, 1986
REFERENCES
Conquer, S.W. 1986 Introductory Report on the Cleaver Township,
Larder Lake Mining Division, Property of Cleyo Resources Inc., Project #6436 - internal Company Report)
Cooke, H.C. 1919 Geology of Matachewan, District Northern
Ontario, Geological Survey, Department of Mines, Ottawa
Guy, Kenneth 1984 Report on a Ground Magnetic and Electro
magnetic Program for Melrose Resources Ltd.
Hopkins, Percy E, 1924 Notes on Gold in McNeil and other Townships,
Ontario Department of Mines, Volume 33, pt.3 pp 37-40
Lee, Hulbert A. 1979 Northern Ontario Engineering Geology Terrain
Study, Sand and Gravel Resources Map, Kirkland Lake, Ontario Geological Survey, Map 5032, scale 1:100,000
Pyke, D.R. 1978 Geology of the Peterlong Lake Area, Districts
of Timiskaming and Sudbury, Ontario Geological Survey Report 171, 53p, Map 2345, scale 1:50,000
REFERENCES cont'd
1968 NTS 42-A "Timmins" Surveys and MappingBranch, Department of Energy Mines and Resources, scale 1:250,000
1970 Map 8442 G "Radisson Lake" AeromagneticSeries, Department of Energy Mines and Resources, Geological Survey of Canada
l scale 1'^ mile
•i,
l 1970 Map 84476 "Peterlong Lake" Aeromagnetic
Series, Department of Energy Mines and
• Resources, Geological Survey of Canada scale l"=% mile
l 1975 NTS 42a73 "Peterlong Lake" TopographicSeries: Surveys and Mapping Branch
l Department of Energy Mines and Resourcesscale 1:50,000
1975 NTS 42a72 "Radisson Lake" Topographic
• Series: Surveys and Mapping Branch Department of Energy Mines and Resources
. scale 1:50,000
l
l
l
l
l
l
DAVID R. BELL GEOLOGICAL .SERVICES INC.
SAMPLE LOCATION SHEET
1H1KD A VI . I-UIlt C
l If flNS. OUT AMD
K H 9JS
Cleyo Resources—Ijir,.mM PROJECT Wo. 6436
llt'P..MTS: 42A/2 and 3
^Mpte /Jo.
136-0001
-0002-0003
1 -0004-0005
| -0006
* -0007
1 -0008
-0009
- -0010
| -0011
-0012
| -0013-0014
| -0015
-0016
| -0017
-0018
1 -0019-0020
. -0021
1 -0022
- -0023
1 -0024
-0025
| -0026-0027
l -0028
" -D029
1 -0030'
ncjid Wtwib(yi
CRC-SWC-001
-003-004
-006-008
-010
-Oil-013
-016 '-019
-022
-024
-026-029
-030
-031
-032
-033
-034-035
-036
-037
-038
-039
-040
-041
-043a-044
-045
-046
Location
L4E/9+30N
LAW/O+^N
L4W/7+60N
L12W/5+36N
8+20W/1+37N
9+20W/6+20N
11+50W/1+80S
11+50W/1+20S
L8W/5+44S
8+80W/8+90S
7+20W/16+80S
L8W/15+85S
L8W/15+85S
0+45E/1+75S
0+35E/1+70S
0+32E/0+88S
0+36E/0+85S
0+34E/0+73S
0+24E/0+51S
0+24E/0+51S
0+44E/0+20S
0+54E/0+02S
0+54E/0+02S
0+56E/0+11S
51+20W/23+60N
•jO+SOU/^^-l-ftnN
55+20W/10+40S
464-40W/40+40S
44W737-fOOS
43W/34+60S
Au ppb
43
2011
466
35256
4
3
a414110
71419
0.0??pz AU/ ton
34
549343•349
4900
4
aa
wriiM,^.Rocfe
. AM&U&LLBT
AT
FT
FT
FT
FT
FT
FT
RC
FT
FT•DC
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BTFTBT
FT
FTFT
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DAVID R. BELL GEOLOGICAL SERVICES INC.
l l l
THIRD AVI . tunt eI'O* 1750
SAMPLE LOCATION SHEET
CMPAW: Clevo Resources Inc.
K H 7J5
PROJECT Wo. 6436
lC'P. (AREAJ: Cleaver Township : A 2A/2 and 3
JJPU to.6436-00311 -0032
-0033
| -0034-0035
1 -0036-0037
1 -0038-0039
1 -0040
-0041-0042
1J ————
1 ————-1
|
1:
1 ———.
TMU lUe*CRC-SWC-049
-051
-054-057-058-059-060-061-062-063
-064-065
L)
—— ——— ——— —— ——— L.
LocationL16W/20+70N15+10W/5+10N
BL/14+50W
LO/7+OOS
LO/17+10S4+30W/10+OOS
4+30W/10+OOS
6+OOW/7+20S
6+OOW/7+20S
6+OOW/7+20S
6+50W/7+40SL4W/4+90S
1 .
Au ppb
41^1
^ 146
4!25
193221
12267
2728
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•^ r^\ \ A iy D ELL -WniTE ANALYTICAL LABORATORIES LTD.y P .O. BOX 187. HAILEYBURY. ONTARIO TEL: 672-3107
(Errtifiratp nf AnalgBtB2 DATE: November 13, 1986
' OF: Rock (li) RECEIVED: November 1986i FROM: M r - Stephen Conquer, David R. Bell Geological Services Inc.
PROJECT; #6436
Sample No. Gold ppb Oz. Gold
6436-0008 2566436-0014 106436-0015 7 6436-0016 146436-0017 196436-0018 776436-0019 0.088** 6436-0021 549**6436-0022 343**'6436-0023 349** 6436-0024 490**
** Checked
-
*
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BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-31O7
(Brrttfirate of AnalgBtaNO. 2133 DATE: December 10, 1986
SAMPLE(S) OF: Core (5) RECEIVED: December 1986
SAMPLE(S) FROM: Mr. Stephen Conquer, David R. Bell Geological Services
_________________________________________PROJECT: #6436_____________
l
i i i i i i i i i
Sample No.
6436-003789
6436-0040l
I ACCORDANCE WITH LONG.ESTABLISHED NORTH A'CAS CJSTOM, UNLESS IT IS SPECIFICALLY STATED
tr-EBWISE COLD AND SILVER VALUES REPORTED ON t ME*L SHEETS HAVE NOT SI-EN ADJUSTED TO COMPEM.
IE FOR LOSSES AND GA'NS INHERENT IN THE FIXE ASSAY PROCESS.I
Gold ppb
19322112
26727
BELL-WHITE ANALYTICAL LABORATORIES LTD.
rr
CERTIFICATE OF ANALYSIS
TQ: DAVID R. LT.LL GEOLOGICAL SERVICES J MCATTN: STHMU. ' i c o'OUE^.?ol THIRD /.VENUE T I f, M INS, ONTARIOP'*?,' IE e
CUSTOMER NC.
DATE SUSMITTED5-NOV-86
621
REPORT 30104 REF. FILE 25683-H3
13 ROCK PROJ. 6436
WERE ANALYSED AS FOLLOWS:
AU PP3l.'RMAJ tMG P P ',P PP.",CA PPMMN P P MF- E P P y.CO P P MNI PPMCU PPM2N PPMURMIN PPMMO PPXPD PP3A G PPMCD PPMf' T PPBP B P P M
METHODFADCPWRCCPDCPDCPDCPDCPDCPDCPDCPDCPW RDCPFAOCPDCPDCPFADCPDCP
DETECTION LIMIT1.0000.01C
100.00010.000
100.0002.0002.0001.0001.0000.5000.500
10.0001.0002.0000.5001.000
10.0002.000
X-RAY ASSAY LA
DATE 19-NCV-86 CERTIFIED BY
l
l
iX-RAV ASSAV LABORATORIES LIMITED -1885 LESLIE STREET - DON MILLS, ONTARIO M3B 3J4 - (416) 445-5755' TELEX 06-986947
19-NOV-P6 REP
SAJ'.F'LE
6436-CG016436-OLD26436-00030436-C00464 36 -DC 056436-0006(.436-00076436-00096436-00 106436-00116436-00126436-00136436-0020
2 ft T 3C104
AU PP3
432011
t,66
3543
C lCIci34
REF*riLE
MG PPM
37000170002000029000350002900013000320001900
19000220006900
21000
25688-H3
P PPM
490110044057C44030047048050
500940630560
PACE 1 OF
C A PPM
890032000200002600015000200004300680037CO4100
3^000240005200
l lK-RAY ASSAY LABORATORIES LIMITED - 1885 LESLIE STREET - DON MILLS, ONTARIO M3B 3J4 - (416) 445-5755' TELEX 06-986947
l11111
VL9-NOV-&6 R
SAMPLE
64 3 6 -GC 016436-OCDt6*3^-00031)436-01,0';6436-000:;6436-00066436-ODD?6 43 6-00 OP6436-0 D 1 D 6436- DC 116436-00126436-00136436-0020
LPOr.T 30104
;v- r PH
1000l 4 0 0 14001 - 0 013001 8006EO1300160
110015007801000
REF. FILG
r E P P M
7600075000 B 20 005300090000990005400010000011000 80000960003300086000
2568C-H3
CO PPK
4451
325 55428544
40341037
PACE 2 O F
N! PPW,
7460 5156597526264
20278
22
lX-RAV ASSAY LABORATORIES LIMITED * 1 885 LESLIE STREET * DON MILLS, ONTARIO M3B 3J4 * (416) 445-5755 * TELEX 06-986947
19-NOV-66 RIP
s AMP L L
6436-OCOl6436-00026436-00036436-00046436-000564? 6-00 066436-CC076436-00096436-0010t-436-00 1 16436-00120436-00136436-0020
:;''.T 30104
CU PPI'.
100.160.90. C69. D
ISO.94.091.069.069.077.044.013.037.0
KEF.FIL
ZN PPM
120.1400.leo.110.160.150.85.0
160.17.0
120.140.59.0
140.
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MO PPM
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X-RAY ASSAY LABORATORIES LIMITED - 1885 LESLIE STREET * DON MILLS, ONTARIO M3B 3J4 - (416) 445-5755' TELEX 06-986947
l
19-iNGV-BG RCPCfU 30104 R c F . F l l E 2568E-H3 PACE 4 CF
SAK.PLE AG PPM CD PPM PT PPB PS PPM
o436-CGOi6OG-OG026436-00036A3&-00046436-00056 A 36- OD Ot.6436-OC076436-00096436-00106 43 6 -OC: li6^36-00126436-00136436-0020
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X-RAY ASSAY LABORATORIES LIMITED * 1885 LESLIE STREET - DON MILLS, ONTARIO MSB 3J4 - (416) 445-5755 * TELEX 06-986947
ll l l
l l l l
CERTIFICATE OF ANALYSIS
TO: DAVID R. BELL GEOLOGICAL SERVICES INC.ATTN: STEPHAN CONOUER CUSTOMER NO. 621l 261 THIRD AVEMUETIMMINS, ONTARIO DATE SUBMITTED
1E3 20-NOV-86
REPORT 30316 REF. FILE 25895-PH
13 PULPS ON HAND RE:WO#25688
UERE ANALYSED AS FOLLOWS:
METHOD DETECTION LIMITC02 Z WET 0.010S S XRF 0.010
X-RAY ASSAY LABORATORIES LIMITED-TXTz^^ DATE 08-DEC-86 CERTIFIED BY~..r..VT. .
•KM ASSAY LABORATORIES LIMITED -1885 LESLIE STREET - DON MILLS, ONTARIO M3B 3J4 * (416) 445-5755' TELEX 06-986947 i 1
08-DEC-86 REPURT 30316 REF.FILE 25895-PH PAGE l OF l
SAMPLE C02 Z S 2
6436-0001 0.73 NIL6436-0002 4.1i 0.156436-0003 2.25 NIL6436-0004 3.19 NIL6436-0005 1.72 NIL6436-0006 2.77 NIL6436-0007 0*27 NIL6436-0009 0.33 NIL6436-0010 0.43 NIL6436-0011 0.08 NIL6436-0012 4.46 NIL6436-0013 2.77 NIL6436-0020 0.60 NIL
t-TTAY ASSAY LABORATORIES LIMITED * 1885 LESLIE STREET * DON MILLS, ONTARIO M3B 3J4 * (416) 445-5755 - TELEX 06-986947
X X RRRRR A LLXX XX RR RR A AA LL
XX XX RR RR AA AA LLXXX RR RR AA AA LLXXX RRRRR AAAAAAA LL
XX XX RR RR AA AA LLXX XX RR RR AA AA LLLLLLLX X RR R AA AA LLLLLLL
XRF - WHOLE ROCK ANALYSIS
DAVID R BELL GEOLOGICAL SERVICES INC.AUn: STEPHAN CONQUER CUSTOMER No. 621261 THIRD AVENUETIWINSi ONTARIO IiATE SUBMITTEDP4N 1E8 5-NOV-86
REPORT 3O1O4 REF. FILE 25688 19-NOV-86
XRF W. R. A. SUMS INCLUDE ALL ELEMENTS DETERMINED. FOR SUMMATION ELEMENTS ARE CALCULATED AS OXIDES.
X-RAY ASSAY LABORATORIES 19-HDV-86
SflKPLE
M36-OM1
H3&-0032
6136-0033
6436-0004
4436-0005
M34-000&
6436-0007
6436-0009
6436-0010
6436-0011
6436-0012
6436-0013
6436-0320
5102
49.
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49.
49.
52.
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8
6
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12.7
13.2
14.0
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123
12.4
13.6
14.1
12.2
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7.13
5. 50
5.84
4.50
4.20
4.50
5.49
3.88
0.72
5.64
6.26
3.97
1.04
KGD
7.05
3.30
4.24
4.90
5.82
4.94
4.37
5.01
0.48
4.30
3.73
1.38
3.52
REPORT 30104 REFERENCE FILE 25688
NA20
1.21
0.64
3.64
2.70
2.98
2.52
4.71
1.67
5.17
146
2.57
3.16
4.35
K20
0.09
3.12
0.42
0.38
0.09
0.13
0.17
0.71
1.47
0.15
0.32
2.39
0.25
FE203
14.2
10.9
14.4
12.4
15.6
16.6
15.1
18.3
1.60
17.5
15.5
4.43
15.6
two
0.18
0. 20
0.23
0.21
0.21
0.28
0.19
0.27
0.03
0.23
0.21
0.11
0.15
T102
1.22
1.69
1.49
1.26
1.47
1.24
1.57
1.87
0.12
1.82
1.63
0.68
1.62
P205
0.11
0.25
0.13
0.13
0.11
0.08
0.12
0.14
0.02
0.14
0.22
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PAGE l
CR203 LOI SUM
0.02 4.62 99.4
tt. 01 6.7? 99.3
O.Oi 4.70 98.7
0.01 6.31 99. l
0.01 5.08 99. l
0.01 5.93 99.4
a. 01 1.85 98.8
m 01 3.85 99.2
0.01 1.39 99.7
'CO. 01 2.54 99.5
0.01 7.23 99.3
CO. 01 4.47 100.1
tt. 01 3.16 99.2
X-RAY ASSAY LABORATORIES
SMPLE
6436-0001
6436-0002
6436-0003
6436-0004
6436-0005
6436-0006
6436-0007
6436-0009
6436-0010
6436-0011
6436-0012
6436-0013
6436-0020
RE
10
no
10
20
10
20
20
20
90
10
20
120
30
19-f,'OV-86
SR
220
60
80
60
60
ao60
160
60
120
40
50
40
Y
30
20
10
30
20
30
30
30
50
30
30
20
30
ZR
50
100
80
120
80
70
110
110
140
90
90
160
90
REPORT 30104 REFERENCE FILE 25683
KB
20
20
20
20
20
30
20
30
20
20
20
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130
800
220
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140
120
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PAGE 2
X-RAY ASSAY Lfcl'OOttESJEIS3: CATiD;; LOT KITH C:,,-.J;:Y iiinuncfiTiou GRAPH ifaVIH R. L-ELL CTOLOOIC^ i^VICES INC ( Pf;OJ: W36 )
19-DEC-84
SA!?LE S\r,::j'. CODE AL203 t,30 FE203*MHT102
6436-0001^136-0002W 36-000364&-00046436-00056136-00066436-00076436-0009M36-OOIO6436-00116436-00126436-0013M36-0020
1 BT -52. 042 fiT M. 833 FT 44. 76', FT 46. 695 FT 43. 206 FT 43. 977 FI 44. 558 FT 39. 55S' RC 87. 69
10 FT 40. 87li Fi 46.2512 DC 73. 4913 FT 43. 96
CODE REFERENCE - JENSEN
UK - ULWili'nC KOMATIITE UK -FT - IRON F:ICH BftSALT NT -AT - THO.EIITIC A;-;DESITE DT -RT - THOLEIITIC RHYOLITE BT -AC - CflLC-f'ilMLIKE AMESITE K -RC - CALC-ALKOE RHYOLITE DC -H - NOT DEFINED
27. 36 30. 6115. 26 29. 91IS. S-0 36. 3421. 92 31. 3322. 71 34. 0919. 62 36. 411&. 79 36. kb19. 73 40. 714. 33 7. 98
17. 92 41. 2016. 04 37. 719. 10 17, 42
16.04 40.00
CATION PLOT
BASALTIC KOfttTIITEHIGH MAGNESIUfl BASALTTHOLEIITIC DACITETHOLEIITIC BASALTCALC-ALKALINE BASALTCfiLC-ftLKftLlNE DACITE
L S. JENSEN (1976): A O CATION PLOT FOR CLASSIFYING SUBALKALIC VOLCANIC ROCKS. ONTARIO DIV1S10M OF MINES, MISC. PAPER 66.
E. C. GRUMSKY (1981): HO. 16 AN ALGORITHM FOR THE CLASS IFICATION OF SUBALKALIC VOLCANIC ROCKS USING THE JENSEN CATION PLOT. SUMrtftRY OF FIELD KDRiC ONTARIO DIV. OF MINES, MISC. PAPER 100.
X-RAY ASSAY LABORATORIES 19-DEC-86 JENSEN CATION PLOT GRAPH l
DAVID R. BELL GEOLOGICAL SERVICES INC ( PROJ: 6436 )
FE203+TI02+MNO
10
20
30
40
50
60
70
BO
90
AL203
90
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10
HGO
X-RAY ASSAY LABORATORIES
SYMBOL TABLE
CODE SYMBOL CODE SYMBOL
1 -Q
2
3 A
4
5 x
6 4
7 *
8 x
9
10 y
H
12
13 i
14
15
16
17
18
19
20
21
22
23
24
25
26
CERTIFICATE OF AMALYSIS
m
TO: DAVID R. BELL GEOLOGICAL ATIK: l).*. BELL 261 THIRD AVENUE TIXtMINS* ONTARIO P'*N 1E8
SERVICES INC.CUSTOMER MD.
DATE SUBMITTED 3-DEC-86
621
REPORT 30513 REF. FILE 26052-G1
PROJ. 6436
WERE ANALYSED AS FOLLOWS
AU PPB GOZ XWRKAJ K KG PPM P PPM S ZGA PPM KN PPM FE PPM CO PPM NI PPM CU PPM ZN PPM WRMIN PPM MO PPM PD PPB AG PPM CD PPM PT PPB PB PPM
DATE 19-DEC-86
METHOD FADCP WETW RDCP DCP XRFD:PDGPDCPDGPDCP DCPD:PH RDCPFADCPDCPDCPFADCPDCP
DETECTION LIMIT1.0000.0100.010
100.00010.0000.010
100.0002.0002.0001.0001.0000.5000.500 10.0001.0002,0000.5001.000
10.0002.000
X-RAY ASSAY
ERTIFIED BY
LABORATORIES LIMITED
v-,-.;4* .J-.
X-KAY ASSAY LABORATORIES LIMITED - 1885 LESLIE STREET - DON MILLS, ONTARIO M3B 3J4 - (416) 445-5755 - TELEX 06-986947
1 1 11111111111111111
19-DI-C-86 REPORT 30513 R E F . F I L E 26052-01
SAKPlL- AU PP3 C 02 'i M G PPM
6436-0025- CI 2.00 29000o436-CC?i. 4 0.56 23000 6/, 36-CU27 CI 0.18 38000 6436-002:. CI 2.05 160000*36-002? CI 4.41 240006436-0030 CI 0.69 15000 6436-0031 CI 1.31 350006436-0032 CI 4.65 400006426-0033 CI ?.29 29000 6436- 002*- 46 0.23 10006436-0035 CI 3.45 210006436-0036 25 0.38 1000 o436-00-'.2 2 ti 6.41 15000
PAGE 1 OF
P PPM
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6 A 36 -00 2 56436-00266436-00276A36-OD2E,6436-00296436-00306436-OG316436-00326136-00336436-00346436-00356436-00366436-0042
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•DEC-86 REPORT 30513 ^EF.FILE 26052-G1 PAGE 4 OF 4
SA".PLE A3 PPM CD PPM PT PPf, PB PP^
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XRF - WHOLE ROCK ANALYSIS
MVID R BELL GEOLOGICAL SERVICES INC.ftltn: D. R FELL241 THIRD AVEKJETIKiilNS,?W 1 E8
CUSTOhER No. 621
DATE SUBMITTED 3-DEC-84
REPORT 3O513 REF. FILE 26O52 19-DEC-86
XRF W. R. A. SUMS INCLUDE ALL ELEMENTS DETERMINED.FOR SUMMATION ELEMENTS ARE CALCULATED AS OXIDES.
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X-RAY ASSAY LABORATORIES 19~DEC-86 JENSEN CATION PLOT GRAPH l
DAVID R. BELL GEOLOGICAL SERVICES INC ( PROJ: 6436 )
FE203+TI02+MNO
10 90
20
30
80
70
60
50
60
70
BO
90
50
40
30
20
10
~r70AL203 10 20 30 40 50 60 BO 90 H60
X-RAY ASSAY LABORATORIES
SYMBOL TABLE
CODE SYMBOL CODE SYMBOL
In 14
2 c
3 A
4 *
5 -^
6 4
7 . ,, *
B x
9 - a
10 y
11
12 .
13 T ,
15
16
17
18
19
20
21
22
23
24
25
26
l
7+00*1 S+oo^l.—J__________L..
RESISTIVITY (APR) IN OHM FEET
N ' l
N-2
N =3
N =4
N =5
FREQUENCY EFFECT (APR) IN "/o
N- l
N =2
N =3
N =4
N *5
METAL FACTOR (APR)
N = l
N =3
N *4
N "5
RESISTIVITY (APR) IN OHM FEET
N * l
N *2
N *3
N =4
N =5
FREQUENCY EFFECT (APR) IN "/o
N = 2
N = 3
N =4
N =5
METAL FACTOR ( APR)
N = l
N =2
N =3
N *4
N =5
COMPANY : ...CJE.O
PROPERTY : r. L T&ft- .
NO-
ap 6^36-86-5-2
ELECTRODE CONFIGURATION —X-*-————N X———*-*-X—*
PLOTTING POINT X= /OO
SURFACE PROJECTION Or ANOMALOUS ZONES
PROBABLE l l l l l l l l l
POSSIBLE / / X / /
INSTRUMENT
CONTRACTOR
DATE SURVEYED
ocToae/? Sil- J9 At*
s^OPERATOR
FREQUENCIES^ .
NOTE CONTOURS AT LOGARITHMIC INTERVALS I.,1.5,2 .3,5-,75 , !0 O
PHOENIX IPV-I IPT-1
REMY BELANGER ENRG.
APPROVED
~DATE^ December 19, 1986
INDUCED POLARIZATION AND RESISTIVITY SURVEY
_. ^J____...... .i_.
a-3
RESISTIVITY (APR) IN OHM FEET
N *l
N "2
N *3
N Z4
N Z5
FREQUENCY EFFECT (APR) IN 0Xo
N * l
N =2
N *3
N =4
N =5
METAL FACTOR (APR)
N = l
N =2
N =3
N =4
N =5
COMPANY : CLzo
PROPERTY^
T/ 'M rt /X/ 5
LINE NO.-
Man 6436-86-5-6
ELECTRODE CONRGURATION —X—**————N X———•~—X—*-
\
POINT
SURFACE PROJECTION OF ANOMALOUS ZONES
PROBABLE l l M l l l l l
POSSIBLE / / / / /
INSTRUMENT
CONTRACTOR DATE SURVEYED
OC.T.
FREQUENCIES^ V-Q
NOTE CONTOURS AT LOGARITHMIC INTERVALS l , 1.5,2 .3,5,7 5 , 10.0
PHOENIX ! p V-! |PT-|
REMY BELANGER ENRG.
APPROVED
OPERATOR DATE: December 19, 1986
INDUCED POLARIZATION AND RESISTIVITY SURVEY
ICfOOfJ
RESISTIVITY (APR) IN OHM FEET
580 N "
N*
N *
N *
N *
FREQUENCY EFFECT (APR) IN 0X0
N s l
N =2
N =3
N -4
N '5
(O 11+00*1
METAL FACTOR ( APR)
XN * l
N =2
N =3
N =4
N *5
COMPANY
PROPERTY :
!NE NO.-
6^36-86-5-5
ELECTRODE CONnGURAT ION ——X-*-*————N X———*"^-X—*-
______i . t.
PLOTT'NG POINT •y x*
SURFACE PROJECTION OP ANOMALOUS ZONES
PROBABLE M M l l l l l
D OSSI8LE / X S / /
INSTRUMEN""
CONTRACTOR
DATE SURVEYEDay-
FREQUENCIES. . 25
NOTE CONTOURS AT LOGARITHMIC INTERVALS l ,i.5,2 .3,5.,75 , '00
PHOENIX IPV-Ij p T- l
REVY BELANGER ENRG. APPROVED
OPERATOR Ke-'Hy DATE: December 19, 1986
INDUCED POLARIZATION AND RESISTIVITY SURVEY
r EE"
N s '
V =2
N-3 j
N s4 j
N *5
FREQUENCY EFFECT (APR) IN "/o
N * l
N =2
N *3
N -4
N *5
METAL FACTOR ( APR)
N = l
N =2
N =3
N =4
N =5
COMPANy:
^ VE NC - 3. +00
r L E C"*" RODE COS' tr 'GURA"l"ON'
• V x=
SURFACE PROJECTION 0^ ANOMALOUS ZONES
FREQUENCIES-
DROBABLE l l l l l l l l l N'O^E CONTOURS AT LOGAR'TMM'C 'NTERVALS
i , '5,2 ,3 ,5 , 7 5 . '00
ENRG.
DATE SURVE V E: A-PROVED
3.*-178(0
OPERATOR fi z f* f DATE December 19, 1986
INDUCED POLARIZATION AND RESISTIVITY SURVEY
L' S'
e
8-\ '
i'
I-
oy
?/ r*oo±b/vex*//. /voof9 /voo/s fo&j-hSOP-/-/ s OOL^ 2*
re ve
*T ' ' ' ' I l l l l
t
o//voo+8l O
/.H
RESISTIVITY (APF) IN OHV FEET
N *l
N *2
N =3
N *4
N *5
FREQUENCY EFFECT (APR) IN 07o
N - l
N =2
N -3
N "4
N *5
METAL FACTOR (APR)
N * l
N =2
N -3
N M
N -5
COMPANY :
PROPERTY : TO//?
LINE NO.- o
o A/ y/^yf /o
Map 6436-86-5-3
ELECTRODE CONFIGURATION -—x-*-————N X———*~--X—*-
PLOTTING POINT
SURFACE PROJECTION O 17 ANOMALOUS ZONES
PROBABLE M l l l l i M
D OSSIBLE / / / / /
FREQUENCIES^ . V-O /y~
NOTE CONTOURS AT LOGARITHMIC INTERVALS 1,15, 2 .3,5,75 , !0.0
INSTRUMENT : PHOENIX IPV-IIPT-!
CONTRACTOR REMY BELANGER ENRG.
DATE SURVEYED APPROVED
_ ^ y o*.i o.a.'g^ ago- SLJL- /v86 ^x7.
OPERATOR ""' OATE: December 19, 1986
INDUCED POLARIZATION
AND RESISTIVITY SURVEY
6*1 5/OO/v;
RESISTIVITY (APF) IN OHM FEET
N
N * Z
N =4
N =5
FREQUENCY EFFECT (APR) IN 0Xo
N * l
N =2
N *3
N =4
N Z5
S+OOAJ ~7-f-odA/ S-f-oo*/ *?-f-oo*S
.8
METAL FACTOR ( APP )
N " l
N ^2
N ^3
N Z4
N -5
375-
RESISTIVITY (APP) IN OHM FEET
N
a lo
&S1
aa?
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/f-too rt
N =3
N *4
N *5
FREQUENCY EFFECT (APP) IN 0Xo
N z l
N =2
N =3
N *4
N *5
METAL FACTOR ( APP)
N = l
N =2
N *3
N =4
N '5
COMPANY : C LjE.ro
PROPERTY '
LINE NO-
6^36-86-5-1
ELECTRODE CON^'GURATION —X~*-*————N X———*-^X—^
PLOTT'NG POINT
SURFACE DROJECT:ONO c ANOMALOUS ZONES
PROBABLE l l l l l M l l
D OSSIBLE / / / / /
FREQUENCIES^
CONTRAC T OR
DATE SURVEYED
3 f-
NOTE CONTOURS AT LOGARITHMIC INTERVALS ! , :5,2 .3,5,75 . 'O C
! PV-ItPT-l
REVY BELANGER ENRG.
APPROVED
OPERATOR DATE: December 19, 1986
INDUCED POLARIZATION AND RESISTIVITY SURVEY
42A82NW8108 8 .9683 CLEAVER 900
March 20, 1987 Your File: 521/86 Our File: 2.9683
Mining RecorderMinistry of Northern Development and Mines4 Government Road EastKirkland Lake, OntarioP2N 1A2Dear Sir:RE: Notice of Intent dated February 9, 1987
Geological Survey on Mining Claims L 724470, et al, 1n Cleaver Township
The assessment work credits, as listed with the above-mntloned Notice of Intent, have been approved as of the above date.
Please Inform the recorded holder of these mining claims and so Indicate on your records.
Yours sincerely,
J.C. Smith, A/ManagerMining Lands SectionMineral Development and Lands BranchMines and Minerals Division
Whitney Block, Room 6610 Queen's Park Toronto, Ontario H7A 1H3
Telephone: (416) 965-4888
DK/raccc: Cleo Clement (In Trust)
1165 McLean DriveTimmins, Ontario
Mr. G.H. FergusonMining i Lands CommissionerToronto, Ontario
Stephen Conquer 261 Third Avenue Timmins, Ontario P4N 1E2Resident Geologist Kirkland Lake, Ontario
Encl.
Ministry ofNorthern Developmentand Mines
Ontario
Technical Assessment Work Credits
t
AMENDED
Dm
February 9, 1987
Flit
2.9683Mining Recorder'* Report ofWorkU- 521/86 ,
Recorded Holder
CLEO CLEMENT (IN TRUST)Townthlp or Area
CLEAVER TOWNSHIPType of survey and number of
Assessment days credit per claimGeophysical
Elartrnmagnetir Hays
Magnetometer riays
Rariinmetrir riays
Induce^ polarization riays
Other. riays
Section 77 (19) See "Mining Claims Assessed" column
40Genlogical riays
Rftorheminal days
Man days | | Airborne l l
Special provision [X] Ground (5T)
j l Credits have been reduced because of partial coverage of claims.
Q Credits have been reduced because of corrections to work dates and figures of applicant.
Mining Claims Assessed
L 724470 724474 725147 to 56 inclusive 725158 725161-62 749741 to 46 inclusive 750507-08 916185-86
Special credits under section 77 (16) for the following mining claims
20 DAYS GEOLOGICAL
L 916183 - 84
Mo credits have been allowed for the following mining claims
Q not sufficiently covered by the survey Q insufficient technical data filed
The Mining Recorder may reduce the abeve credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 80; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.
628 (85/12)
Natural Resources (Geophysical, Geological,
Geochemical andgca, i
Expenditures) CT"^ l (SL~, /\ Ct lJ CX. l /O^" ) l U?
' W .
The Mining Act
exceeds space on this fort Note: — Only days credits calq
"Expenditures" section in the "Expend. Days Cr." co*rafhns.
— Do not use shaded areas below.Type of S ^^
Claim Holdensj
Cleo Clement (In Trust)Address
1165 McLean Drive, Timmins, OntarioSurvey Company Date of S
David R. Bell Geological Services Inc. Day r
Township or Area
Cleaver TownshipProspector's Licence No.
M 20951 *
Survey (from Si to)
i/io. | Yr. j uay | "N2 86rTotal Miles of line Cut
25 milesName and Address of Author (of Geo-Technical report)
Stephen Conquer c/o 261 Third Ave., Timmins, OntarioCredits Requested per Each Claim in Columns at rightSpecial Provisions
For first survey:Enter 40 days. (This includes line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Days
i iW-entef'totaHs) here "X.
iff OB tt wi ' ^y ^s*-*^vv^
* *""-^--"^)
Airborne Credits ^
Note: Special provisions credits do not apply to Airborne Surveys.
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Geoph
'JL;. O1
Geolog
Geoch
ysical
:tromagnetic
jnetometer
Jiometric
ter
cal
mical
Electromagnetic
Magnetometer
Radiometric
Days perClaim
40
Days per Claim
Days per Claim
Expenditures (excludes power stripping)Type of Work Performed
Performed on Claim(s)
Calculation of Expenditure Days Credits
Total ExpendituresTotal
Days Credits
InstructionsTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.
Date
Dec. 9/86Certification Verifying Report of Work A.
Mining Claims Traversed (List in numerical sequence)Mining Claim
Prefix Number
724470724474725147725148725149725150725151725152725153725154725155725156725158725161725162749741749742749743749744749745749746750507750508
Expend. Days Cr.
Total number of mining claims covered by this report of work.
For Office Use OnlyTotal Days Cr. Recorded
Date rded, o, o ,-rir1 tt 1986 Mining Recorder
i.rl hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.
Name and Postal Address of Person Certifying
Stephen Conquer, 261 Third Ave.. Timmins OntarioDate CertifiedDec. 9/86
1362 (81/91
Ontario
Ministry of Natural Resources
GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT
File.
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
l*o
Type of
Township or Area. Claim Holder(s)—
GeologicalCleaver TownshipCleo Clement (In Trust)
Survey Company David R. Bell Geological ServicesInc Author of Report Stephen Conquer________________*
Address of Author c/o P.O. Box 1250. 261 Third Ave.Covering Dates of Survey Sept 12/86-Dec 19/86
(linecutting to office) Total Miles of Line Cut 25 miles____________
SPECIAL PROVISIONSCREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.
DAYS~ i-i per claim Geophysical
—Mapnefnmptpr
— R adiometric ...,,,,..,--Other
t f\
r^nrr^miral
AIRBORNE CREDITS (Special provision credits do not apply to airborne survey i)
Magnetometer. .Electromagnetic(enter days per claim)
DATR- Dec. 19/86 SIGNATURE
Res. Geol. _ Qualifications.Previous Surveys
File No. Type Date Claim Holder
MINING CLAIMS TRAVERSED List numerically
L72447.0.....(prefix)
.U.2M7A.,,L.725.14.7,
L725.H8,
L725.14.9, L72.51.5.Q,
L725m,
L725.15.2,
liZmSA, L72.5.1.5.5,
L7Z5.15.6. L.725.158..
L.7,25.161.
L.7,2.5.1.6.2..
(number)
M tt
3U7.4.9.2.4.3.......,....,..,..,
L7.4.9.7.4.4....................L7.4.9.7.4.5........................L7..4.9.7.4.6.....................L750507
TOTAL CLAIMS 27
837 (5/79)
GEOPHYSICAL TECHNICAL DATA
GRQUNJj^SUKVKYS - If more than one survey, specify data for each type of survey
Number of Stations
Station interval
Profile scale
val I,ine sparing
*rval
Instrument —.
Accuracy — Scale constant.
Diurnal correction method.
Base Station check-in interval (hours)
Base Station location and value
lZQ
SwW
Instrument —Coil configuration
Coil separation _
Accuracy —————
Method:
Frequency,—-——
Q Fixed transmitter D Shoot back CD In line d Parallel line
Parameters measured —
-s)
(specify V.L.F. station)
lO
Instrument -——
Scale constant ——
Corrections made.
Base station value and location
its
Elevation accuracy.
Instrument
ZO
N
QttCc z
w
Method D Time Domain
Parameters — On time .—.—.
- Off time ——.
— Delay time ——-
— Integration time.
Power.
Electrode array — Electrode spacing .
Type of electrode
Frequency Domain
Frequency _____
Range ——^-————
SELF POTENTIAL
i Instrument_________________——————————————————————— Range. Survey Method ______________————————————————————————————
Corrections made.
RADIOMETRIC
Instrument -——-Values measured .
l*i Energy windows (levels) —
Height of instrument ____________________________ Background Count .
Size of detector _____________________________________________•lOverburden
(type, depth - include outcrop map)
OTHERS (SEISMIC, DRILL WE] ,L I .OGGING ETC.)
Type of survey ,—.——---^——-^-^—-————-—-———
Instrument --——-———--.-———^—~———-^————
If Accuracy-————— i Parameters measured.
Additional information (for understanding results).
AIRBORNE SURVEYS
"* Type of survey(s)
Instrument(s) ——(specify for each type of survey)
Accuracy^———————————————(specify for each type of survey)
Aircraft used-——————————^^——————-—^^^-^—^—^^—
Sensor altitude.Navigation and flight path recovery method.
T? ________________________________________
Aircraft altitude________________________________Line Sparing
Miles flown over total area_______:__________________Over claims only..
or.(^Hjrir..ivijijrtij aur
Numbers of claims from which samples taken
TotaJ Niimher of Samples
Type of Sample(Nature of Material)
Average Sample Weight
Method of Collection.
Soil Horizon Sampled.Horizon DevelopmentSample Depth.,Terrain
Drainage DevelopmentF-StimHtpd Range of Overburden Thickness
SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)
Mesh sire of frartion iiserl for analysis.
General . —
i VE, I - riUJL.r,lJUK.tt KE.C.UK1J H
—— ANALYTICAL METHODSValues expressed in: per cent D
p. p. m. CDp. p. b. D
Cu, Pb, Zn, Ni, Co, Ag, Mo, As.-(circle)
Olhprs
Field Analysis (. tests)
Extraction Method
Analytiral Method
Reagents I Iserl
Field Laboratory AnalysisNo. (. . tests)F.vtrartion Methorl
Analytical MethodReagents Used
nommerrial Laboratory ( tests)
Name of Laboratory
F.Ytrarlion MethoH,
Analytiral MethoH
Reagents IJs*"d .
General . ————————————————————————————
li
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
j
1
FALLON TWR
o:
UJ
UJ O
K VL8B3I9B | L 833I97 l^'^LT 'L l
849537,649340
-- -J i 1867133 r/867136 l ~B67I37 l "867136
849543^ — - .4- -- J
IB49S38f. .v. i . l1867131 !A86713Z ' L867133 l L*67I34
l
— JL— — -L ~ -
"18672101867^29,867228 .867122
867116:8313796 .183795 168/3794 1867123
.L - - +L- -749700 749899 1 74
-749695.749694
867Z3S 867234 A |- — -|7427BS[ 742784 6723318"496IIJ
LLp N.ghthawki - -i L l /L
, .l 858944 l |B58
j^L-- V-
—' ' 763148 j V,7^3147753206 753193
l-l- -
^ 4 . ^4 .. j. t^L ^L .T^L J f \
N\ i-/- j.-/ri. - j838964 j 842761 | 6-\ ('Z7SZ | 856*70'
60 0 36'W'
HINCKS TWR
42A92NW8I08 3.9663 CLEAVER 200
NOTES
400' surface r ights reservation along the shores of all
lakes and r ivers.
AREAS WITHDRAWN FROM
M.R.O. - MINING R IGHTS ONLY
S.B.O. - SURFACE RIGHTS ONLY
M.+ S. - MINING AND SURFACE RIGHTS
DMcription Or d w No. Dm Disposition Fit*
•4*
©or 0"
LEGEND
PATENTED LAND
PATENTED FOR SURFACE RIGHTS ONLY
LEASE
LICENSE OF OCCUPATION
CROWN LAND SALES
LOCATED LAND
CANCELLED
MINING RIGHTS ONLY
SURFACE RIGHTS ONLY
HIGHWAY * ROUTE NO.
ROADS
TRAILS
RAILWAYS
POWER LINES
MARSH OR MUSKEG
MINES , ^
'used only with summer resort locations or when space is limited
LO.
C.S.
Loc. C.
M.R.O. S.R.O.
TOWNSHIP OF
CLEAVERDISTRICT OF
TIMISKAMING
LARDER LAKEMINING DIVISION
SCALE : 1 INCH - 40 CHAINS (1/2 MILE)
DR.
DATE JULY I 986PLAN NO. G-3619
Ministry of Ministry ofNatural Northern DevelopmentResources and Mines
Ontario
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td.)
Mannm
me
....
....
....
....
..,.
....
....
....
..
Re
eve
-Do
bie
miie
. .
. . .
. ..
. ...
..
. . .
Syl
van
ite G
old
Min
es L
td.
. . .
.. . .
. . ..
. ..
.
Tec
k C
orp.
Ltd
. —
Tec
k H
ughe
s M
irin
g D
ivis
ion
kirk
land L
ake
min
e . ,
.. . .
. . ..
. . .
. ..
.. .
.T
eck-
H jg
he
s m
ines
.
T ro
t h e
wa
y-O
ssia
n m
ire
. . .
. ..
Tyr
an
ite M
ines
Ltc.
. .
. . .
. . ,
, , ,
.. .
. . . .
. . .
Upper
Canada M
ines
Ltd
.U
pp
er
Be
ave
r (A
rgo
na
ut)
^ne (
man
agem
ent
agre
em
ent
with
Lak
e B
eave
rhou
se M
ines
Ltd.
Upper
Ca
na
da
min
e U
nite
d O
ba
lski
Min
ing C
o. L
td.
West
field
Min
era
ls L
td.
Conia
uru
m m
ine
Wrig
ht-
Ha
rgre
ave
s M
ines
Ltd
. Y
oung-D
avi
dso
n M
ines
Ltd
.
The
lis
t of
pa
st-p
rod
uce
rs is
lim
ited
to m
ines
with
met
al p
rod
uct
ion
valu
ed i
n exc
ess
of
225,
000.
MIN
ER
AL
PR
OD
UC
TIO
N A
ND
RE
SO
UR
CE
S
Ir 1
97",
min
es l
oca:
ed w
ithin
the
Tim
min
s-K
irkla
nd L
ake
shee
t pr
oduc
ed g
old,
silv
er,
coba
lt, c
oppe
r, zi
nc,
lead
, ni
ckel
, iro
n, c
ad
miu
m, s
ulph
ur a
nd a
sbes
tos.
Bar
ite is
soo
n sc
hedu
led
for
prod
uc
tion
in Y
arro
w
l ow
nshi
s. T
he a
rea
also
con
tain
s de
posi
ts o
f m
oly-
b
de
njm
. ur
aniu
m,
tung
sten
, bi
smut
h,
palla
dium
, pl
atin
um,
mag
nesi
um, n
ephe
line,
mar
l, sa
nd a
nd g
rave
l. T
wo
kim
berli
te d
ikes
ar
e kn
own
to o
ccur
; on
e in
McC
ool
Tow
nshi
p, a
noth
er in
Gau
thie
r To
wns
hip.
Gol
d is
pr
oduc
ed a
t th
e P
orcu
pine
(lim
min
s),
Kirk
land
La
ke-
Lard
er L
ake
min
ing
cam
ps,
and
in H
islo
p To
wns
hip
sout
heas
t of
M
athe
son.
Fo
rmer
pro
duct
ion
incl
uded
the
Mat
ache
wan
and
Elk
Lake
cam
ps.
~\ he
lar
gest
pro
duce
r of
silv
er is
the
Kid
d C
reek
min
e no
rth o
f Ti
mm
ins.
Silv
er i
s al
so r
ecov
ered
at a
ll th
e pr
oduc
ing
gold
min
es,
in a
dditi
on t
o th
e op
erat
ing
min
es i
n th
e G
owga
nda
area
. Fo
rmer
pr
oduc
tion
incl
uded
the
Mat
ache
wan
, El
k La
ke a
nd C
obal
t (C
asey
To
wns
hip)
are
as.
Zinc
, co
pper
, le
ad,
cadm
ium
an
d su
lphu
r ar
e pr
oduc
ed
by
Ecs
tall
Min
ing
Lim
ited
{Kid
d C
reek
min
e).
Cop
per
and
zinc
are
pr
oduc
ed i
n th
e K
amis
kotia
are
a w
est o
f tim
min
s an
d at
the
Pot
ter
min
e ea
st o
f M
athe
son.
Cop
per
is al
so p
rodu
ced
at t
he M
cint
yre
Por
cupi
ne m
ine
near
Tim
min
s, t
he M
iller
Lak
e-0'
Bne
n m
ine
near
G
owga
nda
and
the
Upp
er B
eave
r m
ine
near
Lar
der
Lake
. M
inor
co
pper
has
als
o be
en p
rodu
ced
in t
he E
lk La
ke,
Mat
ache
wan
and
G
owga
nda
area
s.
Min
or l
ead-
zinc
was
for
mer
ly p
rodu
ced
m t
he
Mat
ache
wan
are
a,N
icke
l pr
oduc
tion
com
men
ced
in
1971
at
the
Te
xmon
t m
ine
loca
ted
sout
h of
Tim
min
s. N
oran
da M
ines
Lim
ited
will
sho
rtly
be
prod
ucin
g ni
ckel
fro
m L
angm
uir
Tow
nshi
p, s
outh
east
of T
imm
ins.
N
icke
l was
for
mer
ly p
rodu
ced
at th
e A
lexo
min
e, lo
cate
d no
rthea
st
of T
imm
ins.
Iron
ore
is p
rodu
ced
at t
he A
dam
s m
ine
of D
omin
ion
Foun
drie
s an
d St
eel
Lim
ited,
loc
ated
in
Bost
on T
owns
hip,
sou
th o
f K
irkla
nd
Lake
.N
early
all
the
asbe
stos
pro
duct
ion
has
com
e fro
m t
he a
rea
east
of
Mat
heso
n, a
nd m
ost
of t
his
has
been
fro
m t
he M
unro
min
e, a
pa
st p
rodu
cer
of C
anad
ian
John
s-M
anvl
lle C
ompa
ny L
imite
d. H
ed
man
Min
es L
imite
d is
prod
ucin
g as
best
os i
n W
arde
n To
wns
hip,
an
d C
anad
ian
John
s-M
anvi
lle is
cur
rent
ly p
repa
ring
a pr
oper
ty fo
r pr
oduc
tion
in
Gar
rison
To
wns
hip;
bo
th
loca
litie
s ar
e ea
st
of
Mat
heso
n.C
obal
t is
pr
oduc
ed
in t
he G
owga
nda
area
, an
d w
as f
orm
erly
m
ined
in
the
Llk
Lake
and
Cob
alt (
Cas
ey T
owns
hip)
are
as.
Tota
l va
lue
of m
iner
al p
rodu
ctio
n fro
m t
he m
ap a
rea
to th
e en
d o'
19
69
was
ap
prox
imat
ely
S3,5
51.0
00,0
00.
Qua
ntity
of
min
eral
s pr
oduc
ed i
s as
fol
low
s:
HO
W T
O
OB
TAIN
AD
DIT
ION
AL
INFO
RM
ATI
ON
Pub
lishe
d ge
olog
ical
m
aps
cove
ring
this
she
et a
re i
ndic
ated
on
Inde
x M
aps
2079
, 20
80 a
nd 2
081
of th
e O
ntar
io D
ivis
ion
of M
ines
, M
inis
try o
f N
atur
al R
esou
rces
, Tor
onto
, and
on
Inde
x sh
eets
31,
32,
41
, and
42
of th
e G
eolo
gica
l Sur
vey
of C
anad
a, D
epar
tmen
t of E
nerg
y,
Min
es a
nd R
esou
rces
, O
ttaw
a.P
ublis
hed
geol
ogic
al
repo
rts c
over
ing
this
she
et a
re l
iste
d in
B
ulle
tin N
o. 2
5 of
the
Ont
ario
Div
isio
n of
Min
es,
Min
istry
of
Nat
ural
R
esou
rces
and
in
the
Ind
ex o
f P
ublic
atio
ns,
Geo
logi
cal
Surv
ey o
f C
anad
a, 1
961,
197
0.T
opog
raph
ic m
aps
of th
e ar
ea c
an b
e ob
tain
ed f
rom
the
Div
isio
n of
Lan
ds, M
inis
try
of N
atur
al R
esou
rces
, Tor
onto
, or t
he T
opog
raph
ic
Sur
vey,
Dep
artm
ent
of E
nerg
y, M
ines
and
Res
ourc
es, O
ttaw
a.A
ir ph
otog
raph
s m
ay b
e ob
tain
ed f
rom
(he
Silv
icul
ture
Sec
tion,
D
ivis
ion
of L
ands
, M
inis
try o
f N
atur
al R
esou
rces
, Tor
onto
. Ont
ario
, or
fro
m
the
Nat
iona
l A
ir P
hoto
grap
hic
Libr
ary,
D
epar
tmen
t of
E
nerg
y, M
ines
and
Res
ourc
es,
Otta
wa.
Aer
omag
netic
map
s'co
verin
g th
is s
heet
can
be
obta
ined
from
the
Geo
logi
cal
Sur
vey
of C
anad
a.
Parti
al c
over
age
may
be
obta
ined
fro
m t
he O
ntar
io D
ivis
ion
of M
ines
.Th
e na
me
an
d o
wne
rshi
p of
man
y m
iner
al o
ccur
renc
es s
how
n on
th
is s
heet
are
giv
en o
n M
ap 2
148,
Ont
ario
Min
eral
Map
, 19
68.
Info
rmat
ion
on g
eolo
gy,
min
es a
nd m
iner
al o
ccur
renc
es m
ay b
e ob
tain
ed a
t th
e o
ffice
of
the
loca
l R
esid
ent
Geo
logi
st (
Tim
min
s.
Kirk
land
Lak
e or
Sud
bury
).M
inin
g cl
aim
map
s an
d ge
nera
l in
form
atio
n ca
n be
obt
aine
d at
th
e of
fice
of t
he M
inin
g R
ecor
der
at T
imm
ins,
Kirk
land
Lak
e, o
r .^
urlh
iirv
cir
st t
he D
ivi^
inn
nf L
ands
. To
ront
o.
ON
TAR
IO
DIV
ISIO
N O
F M
INES
HO
NO
UR
AB
LE L
EO B
ERN
IER
- M
inis
ter
of N
atur
al R
esou
rces
W. Q
. MA
CN
EE
, Dep
uty
Min
iste
r o/
Nat
ural
Res
ourc
es
G. A
. Jew
ett,
Exec
utiv
e D
irect
or, D
ivis
ion
of M
ines
E.
C. P
ye, D
irect
or, G
eo/o
gica
l Bra
nch
Adj
oins
Map
216
1 C
oral
Rap
ids
Coc
hran
e
Mal
oney
\
\ \
\ T-
ake
f \
G7 \
IGisf
V
KIN
GS
MIL
LN
l, R
EAD
ME
'it
|7 •'.'EDW
ARDS
win
Fal
ls..
. Gi
l lE
EF
Y
\(
Glc
Mei
Qto
sh
5C3'
Spr
ing
FR
EC
HE
VIb
LE
le ^
Au
BA
RN
ET
TH
AC
KE
RA
Y
tafe
—T
-Sil
J O
SNE
BO
E
MCKE
OWN
Gil
Gil
Gll
f
11 ^ P
fkR
AN
D
M/
SHE
BA
AR
GY
LE
94
Jiu.
Cu,
M
NO
RT
HR
UP
GIOc
way R
AT
TR
AY
12b
BA
NN
OC
KB
UR
N
^
MO
NTR
OSE
tHcf
t Lak
e IZb \
(Sin
clai
r M
l. Si
rtct
airV
i tot
e16
00"
W
l*b
V
14
i lO
b
S M
AllT
jAG
AM
I
CO
NN
AtIG
HT
\ lon
dond
erry
L
ake
\Qt
AS
QU
ITH
--^
B1""j
r
Adj
oins
Man
21B
fi S
udbu
ry C
obal
t
GE
OL
OG
ICA
L R
EL
IAB
ILIT
Y D
IAG
RA
M
42A
82N
W01
08
2.9
683
CLE
AV
ER
ME
TA
L A
ND
M
INE
RA
L R
EFE
RE
NC
E
21
0
Sem
i-det
aile
d an
d re
conn
aiss
ance
map
ping
; 1"
to
Y m
ile:
r to
1 m
ile;
1" t
o 2
mile
s
-— —
war
n ru
i'iu:
--^-
-^-
-— -^ -
t^-^
^jp
i^iii
^u^
^^
Buc
ke-p
^~"~
" "
~*'~
Fo
rmal
ionf
—
SE
CT
ION
—N
EW
LIS
KE
AR
D A
RE
A
SE
CT
ION
-HE
NW
OO
D T
OW
NS
HIP
AR
EA
13
12b
12b
Map
2205
TIM
MIN
S-K
IRK
LA
ND
LA
KE
Geo
logi
cal C
omp
ilat
ion
Ser
ies
CO
CH
RA
NE
, SU
DB
UR
Y A
ND
TIM
ISK
AM
ING
DIS
TR
ICT
S
Scal
e 1:
253,
440
or l
Inc
h to
4 M
iles
SE
CT
ION
—LA
RD
ER
LA
KE
AR
EA
l
11
'1C^ wtVj , \\l
I \
\}
.IHJf
c 1
N\3
l \
IF\I
'W
,
Al
\ 2i
H
ItJc*
^ 3
\
N
i la
'b l
\ ^
\IF\
l 'W
\
' ^ \
4
\ \ i
/i
\
\ /'
^le
W
le
Scale
, 1 in
ch to
4 m
iles
SE
CT
ION
—R
ED
ST
ON
E R
IVE
R A
RE
A
ID18
SO
UR
CE
S O
F I
NF
OR
MA
TIO
N
Geo
logi
cal c
ompi
latio
n by
D,
R. P
yke,
L. D
. A
yres
, an
d D
. G
. In
nes,
197
0,19
71.
Pre
viou
s co
mpi
latio
n by
Gin
n,
et a
!, M
ap 2
046,
196
4.
Geo
logy
fro
m p
ublis
hed
map
s of t
he O
ntar
io D
ivis
ion
o! M
ines
, G
eolo
gica
l S
urve
y of
Can
ada,
and
unp
ub
lishe
d m
aps
of m
inin
g c
ompa
nies
.
Car
togr
aphy
by
C.
Harr
is a
nd a
ssis
tant
s, D
ivis
ion
o/"
Lane
's,
Min
istr
y of N
atur
al R
esou
rces
, 19
72.
ease
map
s co
mpi
led
from
Nat
iona
l To
pogr
aphi
c S
erie
s,
shee
ts 3
1 M
jNW
; 32
D1N
W;
32 D
/SW
; 41
PjN
W;
41
PIN
E;4
2A
INE
;42
AIN
W;4
2A
ISW
;42
AtS
E.
2030
Ki
om
etre
s
T~
T"
1
H
H
Scale
, 1 in
ch tt
4 m
iles
SE
CT
ION
—G
OW
GA
ND
A A
RE
A
FIG
UR
E 6
Map
220
5T
imm
ins-
Kirk
land
Lak
e G
eolo
gica
l Com
pila
tion
Ser
ies
Scale
, l in
ch to
200
mile
s
N.T.
S. r
efere
nce
31M,
32D
.41P
.42A
LE
GE
ND
CE
NO
ZO
IC
PL
EIS
TO
CE
NE
AN
D
RE
CE
NT
Till,
var
ved
clay
, sa
nd, g
rave
l, pe
at.
UN
CO
NF
OR
MIT
Y
MES
OZO
IC
INT
RU
SIV
E
CO
NT
AC
T
PA
LE
OZ
OIC
LO
WE
R A
ND
M
IDD
LE
SIL
UR
IAN
18
Tho
rnlo
e F
orm
atio
n: li
mes
tone
, do
l om
ite,
sand
ston
e.
Wab
i For
mat
ion:
lim
esto
ne.
Sha
le.
MID
DL
E A
ND
U
PP
ER
OR
DO
VIC
IAN
17
Daw
son
Poi
nt F
orm
atio
n; s
hale
. Fa
rr F
orm
atio
n: l
imes
tone
. B
ucke
For
mat
ion:
lim
esto
ne,
shal
e.
Giii
guen
For
mat
ion:
san
dsto
ne.
UN
CO
NF
OR
MIT
Y
PR
EC
AM
BR
IAN
LA
TE
P
RE
CA
MB
RIA
N
MA
FIC
IN
TR
US
IVE
R
OC
KS
16
Dia
base
: dik
es.
INT
RU
SIV
E
CO
NT
AC
T
MID
DL
E P
RE
CA
MB
RIA
N
AL
KA
LIC
IN
TR
US
IVE
RO
CK
S
15
Syen
ite,
neph
elin
e sy
enite
.
14
Dia
base
, gr
anop
hyre
: sh
eets
an
d di
kes.
MA
FIC
IN
TR
US
IVE
RO
CK
S
INT
RU
SIV
E
CO
NT
AC
T
HU
RO
NIA
N
SU
PE
RG
RO
UP
CO
BA
LT
GR
OU
P
Lorr
ain
For
mat
ion
13
Qua
rtzite
, ark
ose.
Gow
gand
a Fo
rmat
ion
12
Uns
ubdi
vide
d.12
a Fi
rstb
rook
Mem
ber:
argi
llite,
gre
y wa
cke,
silt
ston
e, a
rkos
e.12
b C
olem
an M
embe
r: co
nglo
mer
ate,
ar
kose
, gr
eyw
acke
, qu
artz
ite,
argi
l lit
e.U
NC
ON
FO
RM
ITY
EA
RL
Y P
RE
CA
MB
RIA
N
MA
FIC
IN
TR
US
IVE
R
OC
KS
*
11
Diab
ase:
dike
s.
INT
RU
SIV
E
CO
NT
AC
T
FE
LS
IC I
NT
RU
SIV
E R
OC
KS
C
Ida
Qua
rtz
porp
hyr
y, q
ua
rtz-
feld
spa
r po
rphy
ry,
feld
spar
por
phyr
y, g
ran
ophy
re,
fels
ited
Wb
Tro
ndhj
emite
, gr
anod
iorit
e,
quar
tz
mon
zoni
te:
sim
ple
bath
olith
s an
d st
ocks
tf10
c T
rond
hjem
ite,
gran
odio
rite.
Q
uartz
m
onzo
nite
, quart
z dio
rite
, a
plit
e,
pegm
atit
e,
mig
matite
: co
mple
x ba
thol
iths.
9 S
yenite,
monzonite,
feld
spar
porp
hyry
d
ME
TA
MO
RP
HO
SE
D
MA
FIC
A
ND
U
LT
RA
MA
FIC
RO
CK
S*
fi G
abbr
o, d
iorit
e, l
ampr
ophy
re.
7 P
eridotite
, dunite,
pyro
xe
nite
, se
rpentin
itef
6 C
ongl
omer
ate,
gre
ywac
ke, s
i/ist
one,
sl
ate,
arg
illite
^
5 G
reyw
acke
, si
ltsto
ne,
slat
e, a
rgill
ite
and
min
or p
ebbl
e co
ngio
mer
atet
INT
RU
SIV
E C
ON
TA
CT
ME
TA
SE
DIM
EN
TS
ff
ME
TA
VO
LC
AN
ICS
S
ALK
ALIC
M
ET
AV
OL
CA
NIC
S"
Tra
chyt
e,
/euc
itic
trac
hyte
; fle
ws,
ULT
RA
MA
FIC
ME
TA
VO
LCA
NIC
S
3 Se
rpen
tiniz
ed d
uniti
c an
d pe
rido-
FFLS
IC
ME
TA
VO
LCA
NIC
S
2a
Pyr
ocla
stic
roc
ks
INltR
ME
DIA
TE
A
ND
M
AF
IC
ME
TA
VO
LCA
NIC
S/
la
Inte
rmed
iate
How
s.1b
In
term
edia
te p
yroc
last
ic r
ocks
1c
Maf
ic f
/ow
s an
d py
rocl
astic
roc
ks.
If
Iron
form
atio
n an
d fe
rru
gino
us
cher
t(o
ccur
s as
a m
embe
r o; s
trat
igra
phic
units
1,2
,4,
and
5).
S
Sul
phid
e m
iner
aliz
atio
n.
aFor
mer
ly c
lass
ified
as
Nip
issi
ng i
n pa
rt.
^No
rth
-tre
nd
ing
dik
es a
re p
art of M
atac
hew
an s
war
m.
cFor
mer
ly c
lass
ified
as
Alg
oman
.
eFor
mer
ly c
lass
ified
as
Hai
leyb
uria
n.
fMay
in
part
be
com
pose
d of
ultr
am
afic
flo
ws.
in t
hese
gro
ups
are
subd
ivid
ed l
ithol
ogic
al/y
an
d th
e or
der
does
not n
eces
saril
y im
ply
age
rel
atio
n sh
ip w
ithin
or a
mon
g gr
oups
.
^For
mer
ly c
lass
ified
as
Tim
iska
min
g.
/For
mer
ly c
lass
ified
as
Kee
wat
in.
The
lette
r "G
" pr
eced
ing
a ro
ck u
nit
num
ber,
for
ex
ampl
e "G
14
", i
ndic
ates
int
erpr
etat
ion
from
geo
phys
i ca
l dat
a in
drift
cov
ered
are
as.
SY
MB
OL
S
Faul
t.
Line
amen
t.
isso'
Alti
tude
in f
eet
abov
e m
ean
sea
leve
l.
Rai
lway
with
sta
tion
or fl
agst
op.
Prov
inci
al h
ighw
ay.
Mot
or ro
ad.
= H
O
ther
road
.
Airc
raft
land
ing
faci
litie
s.
Larg
er c
omm
unity
.
Smal
ler
com
mun
ity.
Prod
ucin
g m
ine.
Past
pro
duci
ng m
ine.
Min
eral
occ
urre
nce.
Res
iden
t Geo
logi
st's
, Min
ing
Rec
orde
r's
offic
es,
Kirk
land
Lak
e, T
imm
ins.
Min
ing D
ivis
ion
with
bou
ndar
y.
Inte
r pro
vinc
ial
boun
dary
.
Dis
tric
t bo
unda
ry.
Tow
nshi
p bo
unda
ry.
A
B
Line
of
sect
ion.
SE
CT
ION
— T
IMM
INS
AR
EA
TH
E M
AP
IN
DE
X
The
red
lette
rs a
nd n
umbe
rs in
the
bord
ers
prov
ide
a lo
catio
n re
fere
nce
syst
em b
ased
on
that
of
Map
20
24, O
ntar
io M
iner
al M
ap.
(DinGO*fr-l
CMto CM-J
CO
-J00
UJ CO-J
Ul CO
TL 15 OON
— 40+OON
— 30+00N
— 20+OON
TL 25 00 S
A-ZONE assa resul ts
-0002 s;vOii' lot:. LI ion and number
20;AT Au assav (pph); Geochemical Rock
Gen l t vi cal Con t rir L"
sO '--n nviru-'Lic data
B D
Tree
S - spruce
P - pine
B - birch
F - b als am fir
A - alder
C - cedar
Pop - pop l a r
Thole i. i tic SuiteFT - iron-rich tholeiitic basalt BT - tholeiitic basalt AT - tholeiitic andesite RT - Lhol e i i. L i c T hyol i t., e
Cal c-Alka! i c Suit,.BC - cal.c-alkalir basalt AC - ea l c-a Ik a l i c a p.-k's 11 e RC - calc-alk-ilit: rhyolite Df; - cal c-alkalic dac i re
-OOH-0015-0016-0017-0018-0019-0020-0021 549 ppb-0022 343 ppb-0023 349 ppb-0024 490
10 ppb 7 ppbH ppb19 ppb77 ppb0.088 oz Au/ton3A ppb
r e;; i-i l l s
y? 1
Trench l-0038 221 pnb-0039 12 ppb-0040 267 ppb
Trench 2-00'd 27 ppb
— 10+OON
— Baseline
— 10+OOS
—20+OOS
30+OOS
David R. Bell Geological Services IncCleyo Resources Inc.
Sample Location and Assay Plan
Twp7Ar68 : Cleaver Twp.
Mining Division : L ardor Lake
•\ u u
{Drafted :4- -
,Dai*j . t)*.. , t LI ~ui
Prov : Ontario
Project No : 0 430
NTS fvlo : 4i? A/? ,o
--V- ^
Ht? . f 1 'i i-
5.9663 CLEAER
CD if)
OD
-J
O
-l
OJro S
* 00
UJ 00
UJ CD
TL 15 OON
— 40+00N
30+00N
20+OON
TL 25 00 S
MAFIC ROCKS
l l Noii-iT.a^ru: t i c
B -basal fs undif ferentIn
Bm -nia^s i ve f l ows
Bp -pill LiWL'd flows
Bpy -flow E ^p brooc i n
1U - t Vlf !'.H?.'PM:-i
[ "j M "l '.!H'I T/
H h.i :..i l t -i tind i t" l" f i.'i'iit. i .'i
Bm :!i,i':'. i vo f l ovs
j^ ill .'V.'J, l l ,^-:
INTEKMKDLATK - FELSIC ROCKS
Q Non-rr.agnet ic
A -andeaiteundifferentiatted
Am -mass i ve flows
FELSIC INTKLISFVKS
FI -uiuuibdivided
Geologi cal Contact
based on magneti c data and geology
based or. geol ogy a n ci g e o e h e m i s t r y
cla ini post, local I on and number found , assumed
e leva Lion contours hash marks show down slope
e s k e r
road
swampy ground
Trt^e Typ^ s
S - spruce
P - pine
B - birch
F - balsam fir
A - alder
C - cedar
Pop - poplar
vesicular
hyaloclastite
variolitic
magnetic
g - geophysically inferred
sh z - shear zone
vesr
hyal varmag
Scale
10+OON
— Baseline
10+OOS
20+OOS
—30+OOS
David R. Bell Geological Services IncCleyo Resources Inc.
GEOLOGY
Twp/Area : Cleaver Twp.
Mining Division : Larder Uko
References :
Drawn : '1./JJ -
Scale : i" fl'io'Drafted : y A '
Date : nr^, , t Hfin
PrOV : Ontario
Project Wo : 0430
NTS No : 4y A/? ,n
Checked : /,, '
Sheet No : n*i'^ "fi. . .^ , ^.* t
42A*2NWataB 2 .96B3 CLEAVER 230