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S2PfceNE0003 63.5553 KAWITOS LAKE 010
CP8?- 1JGEOPHYSICAL REPORT ON
THE DOORI6AN PROPERTY
PETAWANGA LAKE AREA
DISTRICT OF THUNDER BAY
ONTARIO
BY
Shaun P. Parent
INTRODUCTION-
This report of geophysical activities is written, following completion of both V.L.F. Electromagnetic and Magnetometer geophysical surveys on a group of 6 claims;. This property is situated at approximately 88 16 longitude by 66 26' latitude in the mining district of Thunder Bay in the p r o v i n c e o f O n t a r i o.
PROPERTY-
The group of 6 claims has been called the Doorigan property, and hosts the ALPAMAYO showing consisting of copper, silver,and gold assays. The ground was staked in August, September 1989. Claims occur on claim map sheet Petawanga Ci-387. Claims are numbered TB 1122021, TB 1122022, TB 1122023, TB 1122024, TB1122025, TB1122026.
LOCATION AND ACCESSIBILITY-
group is found in the Mining district of T.S. Sheet 32P/8 Kawitos Lake 1:50000.
southwest of Kawitos Lakeon the Albany Kilometers north of Armstrong on the
The claim covered by N some 3.5 Krn i s some 14 O Kawitos lake is large enough to is accessible v'ia an old series
Thunder Bay, andisThe property occursriver ^system. It
C.N. railway line.handle tw i n eng i ne a i r c r aft. of drill roads.
The property
GEOLOGY OF AREA-
T'he area on which the property is located is found within the east uchi volcanic belt. Rock types are primarily mafic to intermediate rnetavolcanics. Interest to the site was drawn by an outcrop of a chlorite-- ga r ne t-mica schist in which a grab sample assayed values of l. 2'A copper. This showing was discovered in August 1989 during a prospecting traverse.
WORK PERFORMED-
Approximately 11.25 Krns. of baseline and crosslines were cut and blazed in August. 1989. Following this, 2 ground geophysical surveys were performed. The survey consisted of V.L.F'. electromagnetic and magnetic techniques.
V.L.F. ELECTROMAGNETIC SURVEY-
The electromagnetic method utilized a Peonies EM-16 V.L.F.instrument. The lines were traversed in a north-south direction whereby the instrument- operator always faced northeast when a reading was taken.
(1)
The V.L.F. receiver unit obtains readings.
(i) IN~PHASE- using a
A measured mechanical
range of f- 150 X clinometer. The
with a sensitivity to *~ IX in-phase component measures the
vertical component of tilt of the polarization ellipse major axis.
(2) QUAD-PHASE- A measured range of *- 40 X with a sensitivity to *~ IXwhich is measured using a graduated cylinder. The quad-phase measures the vertical component of ellipticity of the polarization ellipse.
BASIC PRICIPLE OF V.L.F. SURVEYING-
The V.L.F. EM-l6 is a simple receiving coil which is sensitive to the magnetic radiation transmitted by powerful military antennas located throughout the world. Each transmitter has a separate frequency, to which each V.L.F. receiver can be tuned, using plug in crystals. In surveying with the unit, the transmitting station should be at right angles to the direction of tyhe survey lines. In the case of this survey on the Doorigan property, CUTLER NAA 24.0 Khz. was used.
Due to its frequency rating, the V.L.F. unit will provide responses in both good and poor conductive horizons. Therefore, the V.L.F. survey is unique in the detection of both strongly mineralized and weakly mineralized conduct- i ve ho r i zons.
METHOD OF PLOTTING-
MAP l- shows stacked V.L.F. profiles of the surveyed lines. The in-phasnwhile the quad phase is a dashed
while profiles are plotted at a scale of lcrn ~ A conductive axis is drawn where the in-phase
to negative. Strong conductive axis are represented by solid lines, while weak axis are dashed.
component line.. Map f- 20X for component
i s r ep r esented by solid lines,scale is 1:2000,both components.forms a crossover from positive
MAP 3- This map shows the fraser filtered V.L.F. data. The fraset filtered map when contoured aids in the interpretation of the data as noise is eliminated. Near surface anomalies are amplified and are indicated by higher values.
MAGNETIC METHOD-
The magnetic method utilized a GEM 8 portable proton precessior magnetometer. The crosslines were traversed with the receiving coil placed next to the chained station.
The magnetic method obtains one reading on a LED display. A measurement of the total magnetic field in gammas. Range of measurement of this instruent is from 20,000 to 100,000 gammas, with a resolution of *- l gamma.
.
'BASIC PRINCIPLE OF MAGNETOMETER SURVEYS-
The earths magnetic field resembles the magnetic field generated by 3 huge bar magnet. The portable magnetometer is used to identify suttle small spatial changes in this field, that occur close to the earths surface. Such anomalies are caused by magnetic: minerals such as magnetite and pyrrhotite. Rocks having a higher concentration of these minerals are said to be more magnetic, thus producing higher magnetic signatures. Rocks having a lower percentage of these minerals produce lower signatures.
METHOD OF PLOTTING-
MAP 2- Values in garnrnas were plotted for each station surveyed on a plan map, with a scale of 152000. Contour lines connecting areas of equal intensity were then plotted, at a contour interval of 250 garnrnas. A base level of 60,000 was chosen as a datum point. Areas on the map having a value less then 60,000 occur within the depression. Areas having a stron magnetic signature show tightly spaced contours.
RESULTS-
The V.L.F. ELECTROMAGNETIC and MAGNETIC survey results are plotted on Maps l, 3 and 2.
The V.L.F. ELECTROMAGNETIC method ou lined several conductive horizons. Map 4 shows a compilation of V.L.F. and sampling locations. The ALPAMAYO SHOWING is also out-lined.
CONDUCTOR A-- Although only occurring on two lines, it appears to have a bed r~ oc k sou r ce.
CONDUCTOR EI- This strong conductor shows both in-phase and quad-phase response. It dips to the south and may extend off the grid to the east. Trenches were attempted along the axis of this conductor at two locations but bedrock was not reached. The ALPAMAYO COPPER SILVER showing occurs some 40 meters north of this conductor.
CONDUCTOR C- A weak conductor probably the result of overburden.
CONDUCTOR D- A strong response due to a bedrock source.
CONDUCTOR E- Strong response which is oblique to the grid. Very likely due to a bedrock source.
CONDUCTOR F- A weak response apparently dipping to the north.
CONDUCTOR G- Overburden source.
CONDUCTOR H- A weak south dipping horizon?
CONDUCTOR I- Single line response due to overburden.
CONDUCTOR J- North dipping bedrock conductor.O)
{CONDUCTOR K- Weak conductor oblique to the grid lines, similar to E probably dueto bedrock.
CONDUCTOR L- Insufficient data to interpret this single crossover.
CONDUCTOR M- Weak bedrock conductor?
CONDUCTOR N- A single line bedrock conductor?
CONDUCTOR O- Weak overburden response.
MAGNETIC METHOD-
The GEM 8 magnetometer magnetic survey (Map 2) shows an zone of moderate response, which follows the axis of the V.L.F. conductor. A magnetic low occurs over the strongest portion of the V.L.F. The magnetic trend appears to continue off the eastern portion of the grid. Other smaller magnetic trends on the grid are probably related to the zones of mafic volcanics that occur within the felsic rocks.
RESULTS -
The strong V.L.F. conductor (EO is the main anomaly of attraction on the property, as it has an associated magnetic response. As well the ALPAMAYO SHOWING which is most likely an alteration zone occurs on the footwall side of .this* conductor. Assays from sampling of the showing and the trenches are found at the end of this report. A laboratory report of sample identification from the showing is also enclosed.
RECOMMENDATIGNS-
Further detailed exploration using trenching and geophysics should be carried out along strike and adjacent to the ALPAMAYO SHOWING and the V.L.F. c o n d u c t o r .
RESPECTFULLY SUBMITTED
S h a u n P . P a r e n t
MINERALS PRESENT-
63.5553 KAWITOS LAKE
DOORIGAN PROPERTY FACT SHEET
MAJOR: CHALCOPYRITE, SILVER- MINOR: GOLD
020
LOCATION-
PROPERTY -
GEOLOGY-
THUNDER BAY DISTRICT i l 88 15
The DOORIGAN property consists of 6 claims 1122021-1122026 which were staked by S. Parent in Sep t ernbe r 1989.
August
HISTORY-
From reconn prospecting in September 1989, the propertyshows little bedrock outcropping due to ground moraine cover. Known bedrock consists of well foliated granite gneiss, arnphibolites and some greenschist. A new showing of copper was discovered in August 1989. The ALPAMAYO COPPER SILVER SHOWING occurs in a garnet chlorite mica schist.
Although several oldcut lines exist some 200 meters eastof the showing, IT APPEARS THAT NO PREVIOUS FIELD WORK has ever been done on this property.
1989 FIELD WORK-- During August, September 1989 a grid was cut Ho cover the 6 claims 1122021-1122026. V.L.F. and Magnetometer surveys were carried out, as well as prospecting. Results of the V.L.F. survey indicate several conductive horizons. The main conductor occurs north of the baseline and within 40 meters of the ALPAMAYO SHOWING. The magnetic survey shows an interesting area of moderate magnetic response which follows the main V.L.F. horizon. Prospecting uncovered the ALPAMAYO SHOWING and surface blasting to -10 crn. proved copper silver mineralization. Assay results from grab samples are found at the end of this report, as wellas on the general compilation map. Two trenches in ground moraine were attempted in order to reach thebedrock. A thick clay layer and groundwater layer was reached before bedrock so the trenches were abandoned. Geochemical samples of the till were taken, and assayed. Theseare found at the end of the report.
RESEARCHED BY:SHAUN P. PARENT OCT. 89
Ontario
Northern Development Geological-
and Mines Survey
GERRY WHITE, GEOLOGISTMNDM435 S JAMES STREETTHUNDER BAY, ONTARIOP7C 5G6
nthHoorToronto, OntarioM7A 1W4Telephone 965-1337
LaboratoMel^ Report
O24B-S9
g*},
One sample the rock.
IDENTIFICATION
was submitted for identification of crystal forms in
The sample consists mainly of mm-sized flakes of chlorite with occasional biotite, One end of the sample is capped with a layer of massive chalcopyrite, which has altered in places to reddish- brown goethite, Distributed within the chalcopyrite are several small crystals of magnetite.
This is an interim September 7, 1989 possible .
Fee received: DEPT
report for samples entered in your name on ; additional work will follow as soon as
, Chief Analyst Hugh de Souza, Mineralogist September 7, 1989
Except by special permission reproduction of thne r wu It i mutt Includ* any qualifying remark* mad* by thli ministry with reference to any sample.
1270 (80/10)
Ontario
Ministry ofNorthern Developmentand Mines
Ministere du Developpement du Nord et des Mines
October 13, 1989
Mr. Shaun Parent 1-252 Algoma St. N. Thunder Bay, Ontario P7A 5A4
Dear Shaun:
The following are geochemical results for three samples from south of the Boylen, occurrence that you brought into our office during the first week in September.
Sample No. Au (ppb) Ag (ppm) Cu (ppm) Ni (ppm) Pt (ppb) Pd (ppb)
89-MSP-4
89-MSP-5
89-MSP-6
480
1540
250
7
19
10
1. 8%
5. 851s
3. 22%
60
74
42
<l
<l
<l
<l
<l
<l
If you require any further assistance, please do not hesitate to contact our office.
Sincerely,
Gerry WhiteStaff GeologistBeardmore-Geraldton DistrictMines and Minerals DivisionMinistry of Northern Development and MinesP. O. Box 5000Thunder Bay, OntarioP7C 5G6Tel. (807)475-1331
GW/clk
ACCURASSAY LABORATORIES LTD.P.O. BOX 604
KIRKLAND LAKE, ONTARIO, CANADA P2N 3J5 TEL.: (705) 567-6343
President: Dr. GEORGE DUNCAN, M.SC., PH. D., c. Chem (Ont.l, c. Chem (U.K.), M.C.I.c,, M.R.S.C., A.R.C.S.T.
Certificate of AnalysisPage: l
28984 Shaun Parent1,252 North Algona St. Thunder Bay, Ontario P7A-5A4
Date: . September l 19 89
Work Order l : T890287 Project j
SAMPLE NUMBERS Accurassay Customer
507285 Doorigan-1
Silver PP*
17
Copper PP*
^0000
Lead ppm
63
Zinc PP"
55
LF-30 Per: .^
ORIGINAL
ACCURASSAY LABORATORIES LTD.P.O. BOX 604
KIRKLAND LAKE, ONTARIO, CANADA P2N 3J5 TEL.: (705) 567-6343
President: Dr. GEORGE DUNCAN, wi.Sc., Ph, D., c. chem (om.i, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.
Certificate of Rnctlysis29113 shaun Parent
1,252 North Algoma St Thunder Bay, Ontario P7A-5A4
Date: September 19
Work Order ff : T890343 Project :
Page: l
___19 B9
SAMPLE NUMBERS Accurassay Customer
Copper Nickel ppm ppm
508132 DOORIGAN-l 12100 145
Lead ppm
66
Zinc ppm
50
LF-30 Per:
ORIGINAL
63.5553 KAWITOS LAKE
BOYLEN PROSKtUI httUI bHthl030
MINERALS PRESENT- MAJOR: CHALCOPYRITE, SILVER
LOCATION-
PROPERTY-
aeoLQSY-
THUNDER BAY DISTRICT 51 26 88 15
HISTORY-
The BOYLEN PROSPECT consists of 6 claims 1120979, 1120976, 1120977, 1122020, 1120975, 1040631
An outcropping consists of metavolcanics, metasediment^ and granite gneiss. The mineralization consists f. chalcopyrite, pyrrhotite, pyrite, galena, sphalerite and magnetite disseminated in the rnetavolcanic ar rnetasedirnentary rocks. The chalcopyrite disseminated in gabb r o (MRC 12, 1969).
M..J. Boylen Engineering offices carried out magnetometer and Magniphase E.M. surveys in 1961. Both surveys indicate a strong conductive horizon that appeared to outcrop Further trenching indicated mineralized copper boulders in trench l although bedrock was not reached. Several drillholes intersected interesting mineralization as wel as a wide carbonate alteration zone.
343-7
343-
343-9
343-10
203'- 208' CARBONATE ALTERATION ZONE Po, Py,227'- 255' CARBONATE ALTERATION ZONE Mt, Po, 27J ' - 296 ' CARBONATE ALTERATION ZONE
282'- 283' QTZ vein with heavy CPY mineralNO SAMPLE TAKEN
OZ/T Ag XCu96'- 98' 1.2' .20 4.01
140 '-161' CARBONATE ALTERATION ZONE150'- 155.5 5.5' Tr. 0.55155'- 156' 1.0' .13 2.27259'- 271 ' 12.0' Tr. 0.82
74'- 79' 5.0' Tr. 0.3179'- 84' 5.0' 0.4484'- 86' 2.0' 1.23 0.71107'- 110' CARBONATE ALTERATION ZONE195'- 198' 3. O 1 0.12
50'-- 54' 4.0' 0.2295'- 122' CARBONATE ALTERATION ZONE99'- 10 0.5 '1.5' 3.44106'- 113' 7.0' 0.82120'- 122" 1.5' 1.07
17.1'- 173' CARBONATE ALTERATION ZONE243'- 247' CARBONATE ALTERATION ZONE
Cpy , SphCpy, Sph
i zat i on
343-11
NO SAMPLES TAKEN MO FURTHER WORK HAS OCCURRED ON THIS PROPERTY SINCE THIS TIME.
1989 FIELD WORK-- During August 1989 recutting of the original Boy l enQr i d was done in order to resurvey the prospect with Mag anc V.L.F. Results of both surveys indicated a good strong conductor which dips steeply to the south and extends across the clain group. This conductor appears to be the result of the carbonate alteration zone. Another weaker conductor occurs along the southern flank of the grid. A grab sstrnple was taken from th* area in the vicinity of trench 3. Assay results are found at the end of the report. In July 1989 the prospect was visited by John Mason and Gerry White of The Ministry of Northeri- Development and Mines. Samples from the trenches were obtained and sent to the O.G.6. for Assay. Results are found at the ent of the report as well as on the general compilation map.
REFERENCES-M.J. BOYLEN ENGINEERING OFFICES i SEEBER GROUP) NTS 52 P8/NW/NE
ONTARIO GEOLOGICAL SURVEY, MINERAL RESOURCES CIRCULAR 12, 1969 P.P. 341.
ONTARIO GEOLOGICAL SURVEY, MINERAL DEPOSITS INVENTORY RECORD FILE TBO 120
PARENT SHAUN, BOYLEN PROSPECT NTS 52 P8/NW/NE FILE 2.12714
RESEARCHED BY:SHAUN P. PARENT OCT. 89
ACCURASSAY LABORATORIES LTD.P.O. BOX 604
KIRKLAND LAKE, ONTARIO, CANADA P2N 3J5 TEL.: (705) 567-6343
President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Ch*m (Ont.i, c. cn*m (U.K.). M.C.I.C., M.R.S.C.. A.R.C.S.T.
Certificate of Analysis
28772 Shaun Parent1,252 North Algoma St,Thunder Bay, OntarioP7A-5A4
SAMPLE NUMBERSAccurassay Customer
506137 l 506137 l
Gold ppb
2844
Date: July 28
Work Order l : T890210 Project :
Ooid 02/T
0.0010.001 Check
Page: l
___19_89
LF-30
ORIGINAL
Per:
ACCURASSAY LABORATORIES LTD.P.O. BOX 604
KIRKLAND LAKE, ONTARIO, CANADA P2N 3J5 TEL.: (705) 567-6343
President: Dr. GEORGE DUNCAN, M.SC., PH. D., c. chem (Om.i, c. Chsm (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.
Certificate of RncilysisPage: l
Shaun Parent1,252 North Algoma St.Thunder Bay, OntarioP7A-5A4
SAMPLE NUMBERS Silver Accurassay Customer ppm
Date: 19 89
Work Order tt : T890210 Project :
Copper ppm
Nickel ppm
Lead ppm
Zinc ppm
506137 3900 880 11
LF-30 Per:
ORIGINAL
Ontario
Ministry ofNorthern Developmentand Mines
Ministere du Developpement du Nord et des Mines
September 15, 1989
Mr. Shaun Parent 1-252 Algoma St. N. Thunder Bay, Ontario P7A 5A4
Dear Shaun:
The following are geochemical results for eight samples that John Mason and myself collected from the Boylen Occurrence on July 26, 1989.
Sample No. Au (ppb) Ag (ppm)
89-MBO-l <2 <2 (TR. 2-1, middle south)
89-MBO-2 5 <2 (TR. 2-2, 10 ft. north of 2-1)
89-MBO-3 290 2 (TR. 3-1, south end)
89-MBO-4 105 <2 {TR. 3-2, 6 ft. north of 3-1)
89-MBO-5 <2 <2 (TR. 3-3, 11 ft. north of 3-1)
89-MBO-6 2 <2 (TR. 4-1, south end)
. . . 2
Mr. Shaun Parent September 15, 1989 Page 2
Sample No. Au (ppb) Ag (ppm)
89-MBO-7 14 <2 (TR. 4-2, 10 ft. north of 4-1)
89-MBO-8 8 <2(TR. 4-3 - 20 ft.north of 4-1)
Base metal results are still pending and will be forwarded to you when we receive them from our Toronto lab.
Sincerely,
Gerry White Staff Geologist Beardmore-Geraldton District Mines and Minerals Division Ministry of Northern Developmentand Mines
P. O. Box 5000 Thunder Bay, Ontario P7C 5G6 Tel. (807)475-1331
GW/clk
Ontario
Ministry ofNorthern Developmentand Mines
Ministere duDeveloppement du Nord et des MinesSeptember 25, 1989
Mr. Shaun Parent 1-252 Algoma St. N. Thunder Bay, Ontario P7A 5A4
Dear Shaun:
The following are base metal results for eight samples from tffeBoylen Occurrence. Gold and silver results for these samples weresent to you on September 15, 1989.
Sample No. Cu (ppm)
89-MBO-l 91 (TR. 2-1, middle south)
89-MBO-2 570 (TR. 2-2, 10 ft. north of 2-1)
89-MBO-3 5600 (TR. 3-1, south end)
89-MBO-4 6850 (TR. 3-2, 6 ft. north of 3-1)
89-MBO-5 333 (TR. 3-3, 11 ft. northof 3-1)
89-MBO-6 900 (TR. 4-1, south end)
Pb (ppm)
30
16
26
16
Zn (ppm)
70
67
50
39
28
30
. . . 2
Mr. Shaun Parent September 25, 1989 Page 2
Sample No. Cu (ppm) Pb (ppm) Zn (ppm)
89-MBO-7 405 10 20 (TR. 4-2, 10 ft. north Of 4-1)
89-MBO-8 715 ^0 39 (TR. 4-3 - 20 ft. north of 4-1)
I apologize for the delay. If you require any further assistance, please do not hesitate to contact our office.
Sincerely,
Gerry White Staff Geologist Beardmore-Geraldton District Mines and Minerals Division Ministry of Northern Developmentand Mines
P. O. Box 5000 Thunder Bay, Ontario P7C 5G6 Tel. (807)475-1331
GW/clk
63.5553 KAWITOS LAKE
JO
300
IHIS SUUMITTAL CONSISIEO OF VARIOUS REPORTS, SOME
OF WHICH HAVE BEEN CUEEED FROM THIS F1EE. THE CUEEEU
MAIERIAE HAD BEEN PREVIOUSLY SUBMIT!ED UNDER HIE
FOEEOWING RECORD SERIES (HIE DOCUMENIS CAN BE VIEWED
IN THESE SERIES):
rb r.
r1122021
1122023
1122
022
V4
AL
PA
MA
YO
S
HO
WIN
G
1122
020
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AM
AY
O
CO
PP
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HO
WIN
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CH
LOR
ITE
G
ARN
ET
MIC
A S
CH
IST
GR
AB
SA
MP
LE1 2 3
VA
LUE
SAu
(p
pb)
48
01
54
0
25
0
Ag
(ppm
;
7 19
10
Cu
35
1.8
5.8
53
.22
Zn
(pp
m)
55
N/A
N/A
LEGE
ND
A
ALP
AU
AY
OC
u S
HO
WIN
GM
AG
NE
TIC
TR
EN
Dtow
__ V
LF
CO
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UC
TOR
A
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MA
GN
ETI
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ND
H
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DO
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IGA
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PR
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TY
SC
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: 1:5
000
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MAP
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5 10
20
DIS
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UkK
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13
83
36
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339
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LEN
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240' -
242'
242*
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OZ
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11.9
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42
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2'8
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131 '4
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