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32D05NW0121 OM91-193 HOLLOWAY 010
GEOPHYSICAL SURVEY REPORT
OF THE
PERREX - IRIS J.V. PROJECT
HARKER AND ELLIOTT TOWNSHIPS
LARDER LAKE MINING DIVISION
DISTRICT OF COCHRANE, ONTARIO
FOR
ALEXANDER H, PERRON
DECEMBER 24, 1991 MARY MAHOOD-GREER
GEOPHYSICAL TECHNICIAN
ILLUSTRATIONS
LOCATION MAP - FIGURE l a). . . . . . . . . . . . . . . . . l a)
LOCATION MAP - FIGURE l b). . . . . . . . . . . . . . . . . l b)
ACCOMPANYING MAPS. . . . . . . . . . . . . . . IN BACK POCKETS
SCALE: l inch to 200 feet
DATE: November 1991
THE ALBERTA GOLD EXPLORATION CORPORATION
Perrex-Iris - J.V. Project New East-West Grid
Ground VLF-EM SurveyNSS ProfiledWest SheetMap No.: Iris-EW-91-EM-laW
Ground VLF-EM SurveyNSS ProfiledEast SheetMap No.: Iris-EW-91-EM-laE
Ground VLF-EM SurveyNSS - ContouredWest SheetMap No.: Iris-EW-91-EM-16W
Ground VLF-EM SurveyNSS ContouredEast SheetMap No.: Iris-EW-91-EM-lbE
Ground VLF-EM SurveyNAA ProfiledWest SheetMap No.: Iris-EW-91-EM-2W
Ground VLF-EM SurveyNAA ProfiledEast SheetMap No.: Iris-EW-91-EM-2E
Ground Magnetometer SurveyWest SheetMap No.: Iris-EW-91-Mag-3W
Ground Magnetometer SurveyEast*SheetMap No.: Iris-EW-91-Mag-3E
32D05NW0121 OM91 -193 HOLLOWAY 01OC
TABLE OF CONTENTS
SUMMARY. i)
INTRODUCTION l, 2
GENERAL GEOLOGY.
INSTRUMENTATION. 2, 3, 4
PRESENTATION AND DISCUSSION OF RESULTS 5, 6, 7, 8, 9, 10
CONCLUSIONS AND RECOMMENDATIONS. 10, 11
CERTIFICATE. . . . . . . . . . . . . . . . . . . . . . . . . 12
i)
SUMMARY:
This report is a Geological and Geophysical Survey, as
required by the Ministry of Northern Development and Mines for
assessment work purposes.
The report includes an introduction to the property,
general geology, field results and conclusions and recommendations
based on the field survey.
Technical data is provided in the Appendix pink sheet
found in the back of the report. Field data is compiled on the
accompanying plan map found in the back of this report.
GEOPHYSICAL SURVEY REPORT
OF THE
PERREX - IRIS J.V.PROJECT
HARKER S. ELLIOTT TOWNSHIPS
LARDER LAKE MINING DIVISION
DISTRICT OF COCHRANE, ONTARIO
INTRODUCTION
The claim group consists of sixteen (16) patented, three (3) un-
patented and one leased mining claim, plus a large leased single claim area
formerly consisting of eleven staked mining claims. This claim group is a
contiguous claim group and is located in the southeast corner and northwest
corner of Harker and Elliott townships, at 48 0 28' north latitude and 79 0 46'
west longitude. The property is approximately twenty-five (25) miles north-
northeast of the town of Kirkland Lake, Ontario. Access to the property is
via the Harker-Holloway access road (Highway 627) which is east of Kirkland
Lake and then north to the Harker-Elliott township line, and east on a bush
access road. (See Figure la and Figure Ib).
Ownership of the claim has been attested to by John E. Perron,
103 Government Road East, Kirkland Lake, Ontario, and was not independently
ascertained by the writer.
A northwest-southeast baseline was established at L 0+00 at the
No. 3 pin of claim 9739 for 1600 feet north and 2000 feet south. Picket
lines were extended at 400 foot line spacings perpendicular to the baseline,
with stations established at 100 foot spacings along the lines. Control tie
lines were cut at L 32+00 E, L 56+00 E and L-76+00 E. At w L 56+00 E
further lines were turned off at 24+00 S, 28+00 S, 32+00 S and 36+00 S.
'- 1579572 l 579 573\\|-3 i l \\.598656
l- 'L i L ! L , \j
5126bl ' 5 | 265a 1512659. 512660 l 599066 .59906^7
Ifrd^-OAZ l 687043 \V ^—-—"^^""u^ 904 L i/ x ^ ;^/ -s 5 l 2 6 6 l ' 599069 ; i \ 3- , l i 669799 "ecqTQn ' ^ , 312616 l' 3 4 2 6 l 2/-CIA 342613' f ' V-1- v-- * --c-- }\\-L---i- r --LV--.r^ir--%-^v - - T---kv-~- \3X* l^^-'eW-l___- - -^ '^..^ r '""" 'l^^^M l re^70^l^ . 6^798 . 66379) \ ^342615 ^ 512663' '^--^""^
1 — "i "*/ r1 ' ——i-- -r -U - - - J- - - -- -- -l 565530 \ l' , 1 i \\ L -ro ^ T^ i L L j \ \ L L j_ m — . _ i ,\. ^ ^ .. U, ^/. j'-.J^t-, ^ .----.--.l\ L 7247
^ , ^ ^^^—.—. \ i P i \ \ ,r~ i ; 3 'l U. D '-l V^l__-J \ (P
.56 2.117 1562 118
62115 |562I20 l 562 l 12
l. .... J 545252562II4 1562121 1562.13
6S7068 667069 667070 66707l "TJTT^J l *IC i ~ -— ^- -__-^ '^T— " -
- , L . L ^ i /y U.^
—rv— —.667848 6(i7840 [667839 1667838
1 is3.a3s.^ww738908 |738907 |
l 1- I L 687347 667841 '
' L- 'i'
Sri 80=1 7/ 611 go j 521800l l- /l *~ ! U l
l ^ l l l l
fi7.lSlo l azieot 'fiJlSol '82/821 l
Claim Location MapScale; l inch to 1/2 mile
Taken from a June 1986 Figure la
' B|irntHil LAMPLUGH feoO'
\FREi
JLduramay llVIt. Blewett 125^0'-
Middleton^
HAVEUE
Miles 10Location Map
O 10 20 Figure Ib
-2-
The field surveys were performed by Mary Mahood-Greer with Wendy
Weller assisting.
GENERAL GEOLOGY
O.D.M. Sixtieth Annual Report of the Geology of Harker township
indicates that the bedrock is predominately mafic volcanics, with northeast-
southwest trending rhyolite flows and a small stock of coarse syenite.
The trend of the mafic flows appear to be northeast-southwest and
the most common mafic flow is a diabasic flow with a flow brecciated top. The
tops of these flows are facing south.
The other mafic flows can be andesite, basalt, pillow lavas, diabasic
lavas and some spherulitic lavas as well as some fragmental lavas and tuffs.
The shapes of the pillows indicate that the flows are facing south.
The rhyolite flows range from 100 feet to 300 feet and strike
N 75 0 E. They have steep dips and face south. (These flows have since been
under dispute amond reputed geologists and are now considered to be altered
inner flows of siliceous basalt).
The syenite occurs as a very coarse syenite with large phenocrysts
of feldspars and also as a smaller fine grained syenite occurring on the north
boundary.
INSTRUMENTATION
i) Electromagnetic Survey:
The VLF-EM method uses as a source, one of the main submarine
-3-
communications transmitters in the 15 to 25 kHz band found throughout
the world. These submarine communication radio waves travel in a single
mode parallel to the surface of the earth along the earth-air interface.
Without vertical conductors and travelling over flat ground,
the magnetic field component of this radio or surface wave is horizontal
and perpendicular to it's direction of travel.
VLF instruments are capable of picking up these structures
that change the direction of the waves by measuring the tilt angle of
the major axis of the polarization ellipse. This is illustrated by the
tilt angle being zero on flat ground, but when a conductor is present
the tilt angle will acquire a finite value. The direction of such para
meters as depth, depth extent, dip and width of the conductor is very
minimal.
The VLF easily illustrates the location of the upper limit of
dipping structures which can be seen or plotted as VLF profiles as areas
of greatest change in tilt angle per unit of distance.
The instrument used for this survey was an EDA OMNI-PLUS
Mag-VLF (V12F) unit. The sensitivity of this unit is - .\l for the
inpha.se and - .Yk for the quadrature. The operating frequency for the
OMNI-PLUS is from 15-25 kHz and the station selection is made by com
puter controlled data input.
For the purpose of this survey the station used was Annapolis,
Maryland, which has a frequency of 21.4 kHz. A second station was also
-4-
used, Cutler, Maine, which has a frequency of 24.0 kHz.
All readings were taken perpendicular to the station and the
topography was noted for further use in the interpretation of the EM
reaults.
i i) Magnetic Survey:
This system uses a backward motion of spinning protons of a
hydrogen atom within a fluid of hydrogen and carbon. These spinning
magnetic protons are caused to have two opposite poles by applying a
magnetic field using a current within a coil of wire. When the current
is stopped, the protons precess about the earth's magnetic field and in
turn generate a small current in the wire. This frequency of precession
is proportional to the earth's total magnetic field.
This instrument is read directly in gammas which is the abso
lute value of the earth's total field for that station.
The instrument used for this survey was an EDA OMNI-PLUS field
Magnetometer and an EDA 350 PPM Base Station Magnetometer, this instrument
has a .01 sensitivity.
The diurnal variation was monitored by a base station monitor
with a reference value of 58,800 gammas.
Diurnal corrections were applied by linear distribution of any
observed variation over the time between the base station, and the field
readings.
-5-
PRESENTATION AND DISCUSSION OF RESULTS
i) Electromagnetic Survey; NSS
The field data is presented on four plan maps, found in the
back pockets of this report. Map No.'s:
Iris-EW-91-EM-laW presented as profiled data
Iris-EW-91-EM-laE presented as profiled dataIris-EW-91-EM-lb-E presented as contoured data
Iris-EW-91-EM-lb-W presented as contoured data.
The VLF-EM data is illustrated as profiled data along the
survey lines and is plotted at a vertical scate of one inch = - 40/^
with the inphase and positives to the top and quadrature and negatives
to the bottom. See the accompanying plan maps for the conductor location,
It is also illustrated as contoured data which is calculated data mani
pulation, to more easily determine the conductor location.
Due to the many conductors found and all the differences they
project, they will be generally described below.
NSS-91-1 - has a magnetic association and may run parallel to conductor
91-3, - the north end may have conductive overburden inter-
ferdnce.
- At the south the axis deviates to the west and may be off
set by a east-west cross cutting structure, some of this
may be indicated by the magnetic survey.
NSS-91-2 - A low EM response with a strong magnetic disrupting magnetic
low to the west may indicate a structural change such as a
fault which is seen in the magnetic - north-south trend
which cross cuts the northeast trend of the mafic bedrock.
-6-
NSS-91-3 - May be conductive overburden, seems to be associates with
NSS-91-1
NSS-91-4 - A very weak EM response which is discontinued to the south
of L 12+00 S No magnetic response.
NSS-91-5 - Follows an inconsistent magnetic response which is rather
disruptive and is difficult to distinguish from any north-
south trending structures and the highly magnetic rock of
the surrounding flows.
NSS-91-6 - Does not have any magnetic association except for isolated
magnetic low in the same area as the crossover on the lines.
This may indicate the magnetic responses could be contoured
differently.
NSS-91-7 - Has a magnetic response associated with it, to a minor degree.
Large magnetic response to the north disguises any clear
association, - has a weak EM response.
NSS-91-8 - Same similarities to 91-7 with no clear magnetic associations.
Has a very weak EM response as well.
NSS-91-9 - A weak EM response with a negative inphase.
- No magnetic association.
- Possible topographically related.
NSS-91-10- Very strong positive EM response.
- With a negative inphase response on L 4+00 N
- To the west is a large magnetic deformation.
- Which clearly indicates a north south cross cutting structure
such as a fault or major shear zone.
NSS-91-11- Weak EM response with a varied magnetic response.
- Unclear whether or not the magnetic response is associated
with the EM anomaly or the complex magnetic susceptability
of the underlying mafic lows.
-7-
NSS-91-12 - Has a stronger EM response.
- Similar to 91-10
- Seems to occur just west of the fault as indicated by the
magnetic survey.
- Very weakly continues to the north to L 16+00 N.
NSS-91-13 - Broken up EM response with no reaction on L 4+00 S or L 8+00 N
- Magnetic survey shows some north south structural differences
although not very strong or continuous.
NSS-91-14 and 91-15 - Maybe parallel conductors or one in the same.
- 91-14 may end at L 0+00 or be an offshoot of 91-15. The
zones mapped out by the contouring are rather large EM res
ponses and could possibly be conductive overburden hiding an
anomaly below.
- 91-14 lies saddled between two magnetic highs.
NSS-91-16 - Has no magnetic response
- Is rather narrow in width with a high positive inphase and
positive quadrature.
- Does occur in a low-lying area but doesn't appear to be
topographically related.
ii) Electromagnetic Survey; NAA
The field data is presented on two maps, Map No.: IRIS-EW-91-
EM-2W and IRIS-EW-91-EM-2E, found in the back of this report.
The VLF-EM data is illustrated as profiled data along the sur
vey lines and is plotted at a vertical scale of one inch = - 407o with
the inphase and positives to the top and quadrature and negatives to the
bottom.
Due to the many conductors found and all the differences they
project, they will be generally described below.
NAA-91-A - Follows a sporadically north-south magnetic structure con
sisting of offsetting high and low magnetic susceptability.
- Could possibly be related to a topographical feature of a
swamp or low area.
- Occurs as a cross cutting anomaly to NSS-91-1, 91-2, 91-3,
may be indicative of a swamp and conductive overburden.
NAA-91-B - Occurs along a potential disrupting north-south magnetic low
at approximately L 20+00 S, 73+00 E.
- Occurs in common with NSS-91-1.
NAA-91-C - A small conductor which has minor magnetic association.
- Has common association to NSS-91-4.
NAA-91-D - Starting on L 16+00 N and carried through to L 24+00 S.
Follows a large low area of alder swamp and a creek system.
At 16+00 N a fault shear zone has been identified from pre
vious stripping. The conductor has some associated bearing
with the magnetic syrvey although the magnetic response is not
consistant with the VLF-EM target.
- Has strong associations the full length of the grid with NSS-
91-5 although 91-5 occurs 200 feet to east at the southern end.
- This conductor has a very strong inphase.
- With a double dip in the profile, this may indicate parallel
anomalous areas.
- Most likely caused by a fault or shear zone.
NAA-91-E - Trends northwest-southeast and appears to stop at the boundary
where the syenite starts.
- Occurs amongst a magnetic high with erratic responses.
-9-
- Seems to cross NSS-91-6 at a 45 0 angle.
Conductor 91-E may indicate the swamp in which it follows.
NAA-91-F - Strong response to North, weaker down on L 4+00 N 18+00 E.
- Plots out in same location as diamond drill hole identified
fault. Fault does not show up on Magnetic survey.
- Occurs as a offshoot of NSS-91-10. May be some structural
faulting.
NAA-91-G and 91-H - Occurs Nest of a north-south magnetic high that dis
rupts a east-west trending magnetic low that reflects the
east-west siliceous horizons, is a fault.
- Is a parallel conductor that maybe part of the same system.
- Over lies NSS-91-12 which may indicate 91-G is a part of 91-H.
NAA-91-I - Occurs along side 2 parallel magnetic highs, trending N-S.
- High inphase, low quadrature.
- Occurs in common with NSS-91-14
i i i) Magnetic Survey:
The field data is presented on two maps, Map No.: Iris-EW-91-
Mag-3W and Iris-EW-91-Mag-3E found in the back pockets of this report.
The magnetic data is illustrated as isomagnetic contours (contour interval:
100 gammas) on a map of corrected magnetic values recorded at each station.
The general magnetic trend appears to be in a northeast-southwest
direction with many north-south crosscutting structures evident. The area
between BL 0+00 and TL 32+00 E to the south has some very high magnetic
values and this is due primarily to the rock type occurring there. This
is a magnetic black mafic flows with pyroxene mineralization present.
-10-
Th e inner volcanic flows mapped out on the regional geology
maps can clearly be seen and are disrupted approximately at 9+00 E on
L 4+00 N, L 8+00 N, L 12+00 N and L 16+00 N. Other prominent north south
structures occur at TL 32+00 E 16+00 N and diagonally cross to approxi
mately 42+00 E on L 20+00 S.
The syenite stock on L 0+00 at 32+00 E does not clearly show up
due to the interference of the highly magnetic flows which lie in contact
with the syenite at L 4+00 S 32 * 00 E to 36+00 E.
CONCLUSIONS AND RECOMMENDATIONS
This survey provided some well needed information which was required
to locate and define north-south trending faults and cross-structures.
The previous surveys clearly indicated the general strike of the bedrock
but missed any north-south features. Work involving diamond drilling and stripping
has since turned up north-south faults, which have so far proven to have excellent
mineralization potential and are usually auriferous zones as well.
It was hoped this survey would clearly define the north-south structures
as it has and also indicate the east-west treading contacts.
It is where these structures meet that gold zones have been successfully
located.
The magnetic survey has provided some very strong targets but the general
trend was difficult to determine since the line spacing was 400 feet. It would be
highly recommended to combine the magnetic survey from both the east-west grid and
-li
the north-south grid onto one map. The old north-south lines would have to be
retied into the new grid, since the new grid has been accurately tied into the
new surveyed pins and claim lines.
This present survey has already had a datumn of 400 gammas added to the
magnetic values. This will enable the values to be directly related to the old
survey and successfully tied together.
December 24, 1991 Mary Mahood-GreerGeophysical technician
-12-
CERTIFICATE
I, Mary Mahood-Greer, of Kirkland Lake, Ontario, do hereby certify:
1) That I am a Geophysical Technician and reside at:
50 Dixon Avenue, Kirkland Lake, Ontario, P2N 3L1.
2) That I graduated from Sir Sandfor Fleming College at Lindsay,
Ontario, in 1978, with a diploma as a Geological Technician.
3) That I have been continuously engaged in my profession for
the past ten (10) years and I am qualified to write this report.
4) That I participated in this survey.
Dec. 3 M ,Date Mary Mahood-Greer
. Geophysical Technician
32D05NW0121 OM91-193 HOLLOWAY 020
GEOLOGICAL SURVEY REPORT
OF THE
PERREX - IRIS J.V.. PROJECT
HARKER AND ELLIOTT TOWNSHIPS
LARDER LAKE MINING DIVISION
DISTRICT OF COCHRANE, ONTARIO
FOR
THE ALBERTA GOLD EXPLORATION CORPORATION
AND
PERREX RESOURCES INC,
MARCH l, 1992 ALEXANDER H, PERRON
PROSPECTOR
ILLUSTRATIONS
LOCATION MAP - FIGURE l a). . . . . . . . . . . . . . . . . l a)
LOCATION MAP - FIGURE l b). . . . . . . . . . . . . . . . . l b)
TABLE OF FORMATIONS - TABLE l . . . . . . . . . . . . . . . 2 a)
ACCOMPANYING MAP. . . . . . . . . . . . . . . . In Back Pocket
SCALE: l inch to 200 feet
DATE: November 1991
THE ALBERTA GOLD EXPLORATION CORPORATION
Perrex-Iris - J.V. Project New East-West Grid
Geological Survey Showing Prospecting Work
Map No. IRIS-EW-91-Geo-4-W
32D05NW0121 OM91-193 HOLLOWAY 020C
TABLE OF CONTENTS
INTRODUCTION, . . . . . . . . . . . . . . . . . . . . . l, 2
GENERAL GEOLOGY . . . . . . . . . . . . . . . . . . . . 2
TABLE l - TABLE OF FORMATIONS . . . . . . . . . . . . . 2 a)
GEOLOGICAL FIELD SURVEY AND PROSPECTING WORK. . . . . . 3, 4
CONCLUSIONS . . . . . . . . . . . . . . . . . . . . . . 4, 5
BIBLIOGRAPHY. . . . . . . . . . . . . . . . . . . . . . 6
CERTIFICATE . . . . . . . . . . . . . . . . . . . . . . 7
GEOLOGICAL SURVEY REPORT
OF THE
PERBEX - - IRIS J.V. PROJECT
HARKER AND ELLIOTT TOWNSHIPS
LARDER LAKE MINING DIVISION
DISTRICT OF COCHRANE, ONTARIO
INTRODUCTION
The Iris group has sixteen (16) patented, three (3) unpatented
and one leased raining claim, plus a large leased single claim area which
used to be elevan staked mining claims. This contiguous claim group is
located in the southeast corner and northwest corner of Harker and Elliott
townships. The property is twenty-five (25) miles northeast of Kirkland
Lake, Ontario. You can reach the property by the Harker-Holloway mining
road (Highvay 627) which is east of Kirkland Lake and then north to the
Harker-Ell iott township line, and east on a dirt road. (See Figure la and
Figure Ib).
The claims are presently owned by John E. Perron, 103 Government
Road East, Kirkland Lake, Ontario.
A northwest-southeast baseline was established at L 0+00 at the
No. 3 pin of claim 9739 for 1600 feet north and 2000 feet south. Picket
lines were cut every 400 feet at right angles to the baseline, with marked
pickets 100 feet along the lines. Tie lines were cut at L 32+00 E, L 56+00 E
and L-76+00 E. At T L 56+00 E further lines were turned off at 24+00 S,
28+00 S, 32+OOS and 36+00 S.
15795721 57937 3.j| Z6bl ^12650 15126591 512660 l 599066 .59906/7
-{512661 ' 599069 i \ \,
±TLL6.!!:.!:.l̂ L
G 6 9 7 a 3 '.* ?trr.l . . -tt-, - . .... .i 56 55 32
v562.1171562118
l .-f-L-~
L 7308 (E) L 1 97-38
- i.' l518JJJ0 iiecKlfe ,,. -- lo.-yrj b ' L '
,.,4 4,^ 6 oil 54152 5 9 '545256 '545255 l , -( l6(57068 667069 | 667070 ,66707-.- —l - - - - J. -r - ~
| t l Li -;54746.1 |54S?.5 8! 54 5 2 57
667848 i 6fi7840 [667839 1667838
o isiieoi snaoi i
Claim Location MapScale; l inch to 1/2 mile
Taken from a June 1986 Figure la \
Mil
CaUpbellCLIFFORD L
pKei
Miles 10Location Map-. o lo 20 Figure Ib
-2-
The geology and prospecting was then completed by Alexander H.
Perron by compass and pace traverses using the picket lines as control
points. Only the western half of the property was prospected. The eastern
half will be considered at a later date.
GENERAL GEOLOGY
The bedrock is mostly mafic volcanics, with northeast-southwest
trending rhyolite flows and a small stock of coarse syenite.
The trend of the mafic flows appear to be northeast-southwest and
the most common mafic flow is a diabasic flow with a flow brecciated top.
The tops of these flows are facing south.
The other mafic flows can be andesite, basalt, pillow lavas,
diabasic lavas and some spherulitic lavas as well as some fragmental lavas
and tuffs. The shapes of the pillows indicate that the flows are facing
south.
The rhyolite flows range from 100 feet to 300 feet and strike
N 75 0 E. They have steep dips and face south. (These flows have since been
under dispute among reputed geologists and are now considered to be altered
inner flows of siliceous basalt.)
The syenite occurs as a very coarse syenite with large phenocrysts
of feldspars and also as a smaller fine grained syenite occurring on the
north boundary. (See Table l for the stratigraphic assemblage).
-2 a)-
TABLE l
TABLE OF FORMATIONS
CENEZOIC
Pleistocene deposits - till, clay, sand, gravel.
ARCHEAN
Later Intrusive RocksDiabase - f.g. to e.g. equigranular diabase.
Early Intrusive Rocks
Syenite - e.g. syenite and syenite porphyry,mafic syenite, quartz syenite, aplitic syenite.
Pyroxenite - m.g. to e.g. pyroxenite, augite porphyry, lamprophyre.
Kinojevis Group VolcanicsSiliceous Horizons - metasomatized basalt,
rhyolite, tuff, cherty and carbonaceous metasediments.
Basalt - pillowed flows, variolitic flows, flow breccia, hyaloclastite.
-3-
GEOLOGICAL FIELD SURVEY AND PROSPECTING HORK.
The field work was drawn up on the Map found at the back of the
report. For information not mentioned here refer to the plan map for
details.
The claims found in Harker township were covered by new growth
of poplar and spruce as well as some areas of replanted spruce. This area
was previously cut. The ground is dry with a gently sliping terrain of
glacial debris and some sand and gravel.
The areas covered in Elliott township are covered by a primary
mixture of spruce and balsam fir with large areas of alder and windblown
deadfall. Elliott township had more areas of wet sections caused mainly by
small brooks and beaver creeks and low runoffs.
Most of the outcrops found and examined were basalt and andesite.
They were massive fine grained to course diabasic flows. They had a massive
blocky texture and pyrite in a disseminated cube form was seen and was less
than W.
Flow breccia texture was found over the property. Classic textures
can be found on a large bald outcrop between L 4 S and L 8 S approximately
17 E. Inner flows between the lava flows and flow brecciated basalts were
seen about L 4 S l 8 W. The most important area prospected was an attempt
to follow the lower horizon of rhyolite/siliceous basalt which occurs about
the same place as L 8 S. The outcrop about L 8 S 14E to 20E was closely
examined and flow banding was noted in a hard dense fine grained grey to
black rock. This banding could be traced over a few feet across the rock.
-4-
Vesicles were also noted, many of them filled with quartz. Flow ba
was also found just east of the baseline about L 8 S. Some old previous
unexamined trenches were located and flow banding was seen. An other old
trench was found north of L 8 S 24-W. It also had a dark grey-black very
hard massive rock, with a fine grained texture.
This same zone was located near L 4 N 4-W. Minor banding may have
been seen but mostly just quartz filled vesicles.
No more outcrop was found throughout the areas of Elliott township.
A large area occurring between L 4 N and L 4 S about 12 E to 20 E
was found to be the centre of the mafic flow. This texture was more coarse
with long black crystals of hornblende, very similar to a coarse diabase.
Some inner parts were nearly that of a grabbroic texture.
A complex series of fault was mapped out about L 8 N 16-E. This
was noted by piecing together the scattered outcrop and mapping out a space
between the northeast-southwest diabase dykes and the east-west rhyolitic
zones. The very massive diabasic flows appear to separate the rocks and
is cut off itself from any westerly extension.
CONCLUSIONS
The geological survey and prospecting work was performed for two
reasons, one of which was to properly locate the new east-west grid in
relation to the new boundary survey which was surveyed in the spring of
1991. The prospecting was done to try and figure out the inner layered
zones of rhyolHe/siliceous horizons between the basalt flows. Previous
-5-
mapping by J. Satterly maps the rock as a rhyolite. Present day examina
tions have called the rock many different labels from a rhyolitic-chert
to an altered siliceous basalt. There has never been any serious prospect
ing carried out to try and determine what the rock is.
The conclusion made after finding some of the old trenches which
have never been prospected since the late 40's was that from physical
examination the rock was indeed an igneous volcanic rock primarily rhyolite.
The vesicles were very common and many were not filled. The bending was
very difficult to see and had probably lead to the misinterpretation of the
classification of the rock in the first place. From the surface, the banding
can in places indicate altered pillow structures which have the appearance
of being very warped. But after prospecting the zones the flowing lines
take on the appearance of flow banding.
This rock type was very difficult to class and samples were taken
and shipped off to Ottawa for chemical analysis. In particular neutron
activation analysis. As well thin sections are being prepared to further
assist in the proper classification of the rock. It may well be that only
by these methods will the rocks be properly identified.
Respectfully submitted,
March l, 1992 Alexander H. PerronProspector/President
-6-
BIBLIOGRAPHY
JENSEN, L. S. - 1978 - Geology of Thackeray, Elliott, Tannahill and DokisTownships, District of Cochrane, Ontario. Geological Survey Report 165, 71 p. Accompanied by Maps 2367, 2368, Scale 1:31680 (l inch to 1/2 mile).
Parsons, G.E. - 1948 - Summary of Preliminary Report, Iris Gold Mines,Harker Townships. Summary of assay results and vein descriptions, dated December 1948.
Satterly, J. - 1951 - Geology of Harker Township, District of Cochrane,Ontario Department of Mines, Vol. 60, Pt. 7 p. 1-47 and Map No. 1951-4.
Storen, R. - 1947 - Preliminary Report of Iris Gold Mines Ltd., HarkerTownship, Larder Lake Mining Division, Province of Ontario, Engineers report dated November 1947.
-7-
C.ERTIFICATE
I, Alexander H, Perm, Of* K.trWa.n.d' La.Ke,, On,ta,ri.Q, dp hereby
1) That I am a third (3) generation prospector in the familyand reside at 114 First Street, Kirkland Lake, Ontario P2N INS.
2) That I have been continuously engaged in my profession for the past forty (40) years, and I am qualified to write this report.
3) That I performed this survey.
Date Alexander H. PerronPresident
L I6*OO N "
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32D05NW0121 OM91-193 HOLLOWAY 200
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Outcrop f"' PillowsGeological boundary inferred
assumedFault Trench
PRECAMBRIAN
6 l Mafic dykes a) diabase
5 j Felsic Intrusive Rocks b)syenite, quartz syenite
Rhyolite a) massive b) banded
\ l Basalt, Andesitea) pillowed b) flow breccia c)spherulitic
Report S Map by: Alex Perron
KEY MAP
THE ALBERTAEXPLORATION
PERREX-IR1SNew East West Cr
GEOLOGY SURVEY showing
Prospecting WorkWest Sheet
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INSTRUMENTATIONStation used: NSS Annapolis
Contour interval: IO units
Contoured by: W. K. Weller
Report by Mary Mahood-Greer
HARKER
Harker Q\La*t
OPERTY
THE ALBERTA GOLDEXPLORATION CORPORATIONt '
PERREX-IRIS J.V. PROJECTNew East — West GrJ d
GROUND VLF SURVEY l' i
NSS ContouredEast Sheet
HARKER-ELLIOTT TOWNSHIPLARDER LAKE MINING DIVISION
DISTRICT.OF COCHRANE, ONTARIO200 400 60Qft*t
Scale: l inch to 200 feet
PE R R O N S'Kirkland Lake Canada
l99tlMfl9 No.: IRIS-EW-9I-EM
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INSTRUMENTATIONInphase Quadrature VLF ConductorInstrument used EDA OMNI-PLUS
Mag-VLF (VI2F) Station used- Cutler, Maine Frequency: NAA 24.0 kHz Vertical scale linch?*407o Plotted by: Wendy Weller
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KEY MAP
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PROPERTY
THE ALBERTA GOLDEXPLORATION CORPORATION
PERREX-IRIS J.V. PROJECTNew East West Grid
GROUND VLF-EM SURVEY NAA - Profiled
West SheetHARKER-ELLIOTT TOWNSHIP
LARDER LAKE MINING DIVISIONDISTRICT OF COCHRANE, ONTARIO
200 feet O 200 400 600 feetl
Scale: l inch to 200 feet
PE R R O N S'Kirkland Lake
32D05NW0121 OM91-193 HOLLOWAY
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\INSTRUMENTATIONStation used: MSS Annapolis
Contour interval: l O units
Contoured by. W. K. Weller
Report by Mary Mahood-Greer
KEY MAP
PROPERTY
THE ALBERTA GOLDEXPLORATION CORPORATION
PERREX-IRIS JV PROJECTNew East-West Grid
GROUND VLF SURVEY NSS Contoured
West SheetHARKER-ELLIOTT TOWNSHIP
LARDER LAKE MINING DIVISIONDISTRICT OF COCHRANE , ONTARIO
200 feet 200 400 SOOfeet
Scale l inch to 200 feet
PERRONS'Kirkland Lake Canada
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INSTRUMENTATIONIsomagnetic contoursBase station value*. 59770 bInstrument used- EDA OMNI-PLUSField Mag 8 EDA 350 PPMBase station Mag
Datumn subtracted' 58,000 b Contor interval - 100 gammas or
500 gammas Contoured by- Mary Mahood-Greer
LEGEND
^ 500 b
500 -1000 b
1000-1500 b
1500-2000 b
2000-3000 b
3000-4000 b
< 4000 b
Report by Mary Mahood-Greer
KEY MAP
WestMARKER-ELLIOT .
LARDER LAKE MINiN-.- , DISTRICT OF COCHRANE ,
200 feet O 200 400
Scale: l inch to 200 fee
PE R R O N S'Kirkland Lake Canada
Drawn by: Mary Mahood-Greer i Date: November 19911 Mao No. ; IRIS-EW-91
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o
INSTRUMENTATIONInphase ; ^.^Quadrature ——EM ConductorInstrument used: EDA OMNI-PLUS
Mag- VLF (VI2F) Station used: Annapolis, Maryland Frequency- NSS 21.4 kHz Vertical scale: linch s± 40 0Xo Plotted by: Wendy Weller
Inphase
Quadrature
PositiveNegative
Report by- Mary Mahood-Greer
KEY MAP
l ^- *—-i-- —- —y
PERT r
*
THE ALBERTA GOLDEXPLORA TION CORPORA Tic A
PERREX-IRIS J.V. PROJECTNew .East — Wes* G-r : a
GROUND VLF-EM SURVEY NSS-Pro f i led
East SheetHARKER-ELLIOTT Tu/, , ,m-
LARDER LAKE MINING . . iGN DISTRICT OF COCHRANE .
200 feet
\ rAR)C
OC feer
Scale: (inch to 200 e f
PE R R O N SKirkland Lake Canada
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Grid East N 53*E
SYMBOLSSurvey pin (located) ® assumed o Survey line (cut) ——— assumed — Township line - —— - —— - — Claim post o located " tie-on r Claim line — — — — — Grid control point * Road primary :::::i: bush ::::.v.v.::v.:
INSTRUMENTATIONInphase * ^.f^ "~;v^;^ Quadrature -^—- ~"";X, ' , EM Conductor —— — I— Instrument used: EDA OMNI-PLUS
Mag- VLF (VI2F) Station used: Annapolis, Maryland Frequency: NSS 21.4 kHz Vertical scale linch s± 400Xo Plotted by. Wendy Weller
Inphose
Quadrature
PositiveNegative
Report by-- Mary Mahood-Greer
KEY MAP
PROPERTY
1
THE ALBERTA GOLDEXPLORATION CORPORATION
PERREX-IRIS JV PROJECTNew East — West Grid
GROUND VLF-EM SURVEY
NSS-Profiled
West SheetHARKER-ELLIOTT TOWNSHIP
LARDER LAKE MINING DIVISIONDISTRICT OF COCHRANE , ONTARIO
200 feet 200 400 GOOfeet
Scale: l inch to 200 feet
PE R R O N S'Kirkland Lake Canada
Drown by Mary Mohood-Greer|Dote: November l99l|Mop No.: IRIS-EW-9I-EM loW
Magnetic North I00 WL 16*00 N
Grid East N 53 0 E
L 12* 00 N-r -r\-7 -i* ~* -n -w 'i* if -ii -ir -it -H *". ifi*w-" -* -H
SYMBOLSSurvey pin (located) ® assumed oSurvey line (cut) ——— assumedTownship lineClaim post o located * tie-on f-Claim line —Grid control pointRoad primary :::.".:: bush
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INSTRUMENTATIONInphase Quadrature VLF ConductorInstrument used: EDA OMNI-PLUS
Mag-VLF (VI2F) Station used: Cutler, Maine Frequency: NAA 24.0 kHz Vertical scale: Mncr^-40% Plotted by Wendy Weller
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Report by Mary Mahood-Greer
KEY MAPl 28+00 S
9+00
L 36*00 S
32D05NW0121 OM91-193 HOLLOWAY
CJ1 O)
o om
N
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K* NX
x\
THE ALBERTA GOLDEXPLORATION CORPORATION
PERREX-IRIS JY PROJECTNew East-West GridGROUND VLF-EM SURVEY
NAA-Profiled
East SheetHARKER-ELLIOTT TOWNSHIP
LARDER LAKE MINING DIVISIONDISTRICT OF COCHRANE, ONTARIO
200 feet 200 400 600feet
Scale: (inch to 200 feet
PER RONS'Kirkland Lake Canada
Drown by Mary Mohood-Greer| Date: November !99l|Mop No.: IRIS-EW-9I-EM-2E
L 16 + 00 N
2 E, fiv,s 7 * i IP t- 00 N
L 8* 00 S
L 12*00 S
LxJ6*00 S
L 20*0
24*00 S
l 28 + 00 S
2 + 00
32D05NW0121 OM91-193 HOLLOWAY
Magnetic North l O0 W
Grid East M 53*E
SYMBOLSSurvey pin (located) © assumed o Survey line (cut) ——— assumed —Township line - —— - — - — Claim post o located * tie-on f- Claim line — — — — — Grid control point * Road primary ::*.:::: bush ::::v.::::::::
INSTRUMENTATIONIsomagnetic contoursBase station value: 59770 bInstrument used: EDA OMNI-PLUSField Mag 8 EDA 350 PPMBase station Mag
Dafumn subtracted: 58,000 b Contour interval' 100 gammas or
500 gammas Contoured by: Mary Mahood-Greer
LEGEND
500 b
500 - 1000 b
1000-1500 b
1500-2000 b
j l 2000-3000 b
3000-4000 b
C 4000 b
Report by Mary Mahood-Greer
KEY MAP
THE ALBERTA GOLDEXPLORATION CORPORATION
PERREX-IRIS J.V. PROJECTNew Easf — West Grid
GROUND MAGNETOMETERSURVEY
SheetHARKER-ELLIOTT TOWNSHIP
LARDER LAKE MINING DIVISIONDISTRICT OF COCHRANE, ONTARIO
200 feet 200 400 600 feet
Scale: l inch to 200 feet
PERRONS'Kirkland Lake Canada
: Novembtf !99l|Mop No IRIS-EW-91-MolE