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HI iiiiiiv i union i ii ilium iiiiiiiiiiiin HIW ^AwJEll 1 1. nJJj i!!'!''' ill""" "l" III
RESULTS OF IP TRAVERSING
ON THE TAGLIAMONTE CLAIMS,
CAIRO TOWNSHIP, MATACHEWAN, ONTARIO
for
REGENT ROCK RESOURCES INC.
RECEIVEDOCT 1 9 t988
by MINING LANDS SECTION
J. B. Boniwell
Exploration Geophysical Consultant
August 18, 1988
^fe BXGA III INTEW GONS
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* III lilll! 1 Illllll42A02SE8272 2.11724 CAIRO
LIST OF CONTENTS
Introduction
Description of Property
Details of Survey
Discussion of Results
Conclusions and Recommendations
Appendix
LIST OF DRAWINGS
DWG. NO. TITLE
EIC-1931 Locality Plan
-1989 Chargeability, Resistivity Pseudo-Section
-1990 " " "
-1991 " " "
-1992 " " "
-1993 " " "
-1994 " " "
-1995 " " "
-1996 " ' " "
-1997 Superimposed Results in Plan
IB
in010C
Page 1
2
3
4
8
12
SCALE
1:2,000,000
,500W 1 1250
600W 1 1250
700W 1 1250
800W 1 1250
900W 1 1250
1000W 1 1250
1100W 1 1250
1200W
1:2500
BXGAblBUR INTERNATIONAbCONSULTANTS IsTD.
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INTRODUCTION
A total of eight cross-sections have recently been
traversed by IP/resistivity on the 6-claim Tagliamonte property
in Cairo Township near Matachewan, Ontario. This work fulfilled
the recommendations stemming from a prior geophysical surveying
of this ground by magnetics and VLF seeking new mineral
possibilities in the area (see Excalibur report #88-RRR-1,
Geophysical Results from the Tagliamonte Claims, Cairo Township,
Ontario, by J. B. Boniwell, April 1988).
These latest results have been compiled into pseudo-
sections, contoured, and anomalies translated into plan for
purposes of presentation and interpretation. The significance of
data is evaluated herein, and the advisability of a follow-up
drilling subsequently determined.
BXGAbinilR INTERNATIONAL, GONSUbT&NTS IsTD.
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- 2 -
DESCRIPTION OF PROPERTY
The constituent claims number six and are identified as
follows:
L 892133-38 incl., Cairo Twp., Larder Lake Mining
Division, Ontario.
They are all registered in the name of Regent Rock
Resources Inc., 425 University Ave., TORONTO, Ontario, M5G 1T6.
Each claim is nominally of 40 acres, and is non-patented;
together they form a contiguous block in the northwest corner of
the township. Access to them is by bush roads from a point on
Highway 66 approximately 3.5 kms east of Matachewan. The total
distance from Matachewan to the property is in the order of
6 kms.
There exists an above-average amount of outcrop within
the claims area. Because of it, the ground is lumpy and locally
abrupt. In these conditions, drainages are confined, albeit
still swampy at the bottom of depressions. Several potholes
therein are filled with water. The land is forested with a
mixture of spruce, jackpine and poplar.
BXGAblBUR INTERNATIONAL CONSULTANTS bTD.
SCALE 1 : 2,000,000
Gowganda SCALE V - 8 miles
REGENT ROCK RESOURCES INC.
CAIRO TWP. PROJECT Larder Lake M.D., Ontario
LOCATION MAP
DWG.No. E.I.C. - 1931
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- 3 -
DETAILS OF SURVEY
The subject induced polarization (IP) and resistivity
surveying was carried out under contract; it was completed in the
period 25 July - 3 August 1988.
A dipole-dipole electrode array was employed for the
traversing, the 'a' spacing of the dipoles set at 25 m, the fna'
distance between dipoles being varied through the equivalent of
'ns 1,2,3 and 4. The station interval along line was maintained at
25 m; however the existence of the several ponds and small lakes
in the grid area curtailed coverage in places and effectively
confined the programme to eight consecutive cross-sections in the
property centre.
The equipment employed was of the pulse transient type,
viz. Huntec MK IV receiver working in conjunction with a 2 kva
Phoenix IPT1 transmitter. At the receiver, a 240 msec delay time
was interposed before integrating the obtained secondary signal
over the ensuing 100 msec period.
The entire survey operation was conducted by Claridge La
Rose Geophysics Ltd. of Bracebridge, Ontario.
BXGAblBUR INTERNATIONAL, CONSULTANTS I*TD.
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- 4
DISCUSSION OP RESULTS
A heartening amount of IP anomaly has been recorded in
this survey beyond the known horizonal loop em. (HLEM) anomalies.
Even more gratifying, much of this anomaly locates with favouring
features identified from the earlier geophysics:
1) the NW-bearing fault axis in the south quarter. This
structure given prominence in the prior interpretation has now
been further distinguished by polarization anomaly coinciding
with its locus. This correlation is distinctive along the
eastern reaches of the axis, especially on line 700W where a
clear anomaly has been picked up in depth (ns3). It is
accompanied by perceptibly lowered resistivities.
This particular event holds importance since it was
closely approached by the DDH #C51-2 wherein gold was assayed
(160 ppb) in the core at virtual hole bottom, the only known
anomalous gold value so far obtained on the property. On the
balance of evidence, it is believed this hole did not extend far
enough to intersect either the structural axis nor the main
source of the polarization associated with it. The hole however
had penetrated 3.2 m (10.5') into a felsic tuff before being
stopped, and this material has been logged (J. Watkins, 1976) as
containing 5X disseminated pyrite on the average. In the one and
only sample taken thereof, this mineralization proved to host the
above-noted gold assay.
BXGAMBUR INTERNATIONAL CONSULTANTS LTD.
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However in the overlying lithologic sections, a 5%
concentration of sulphides is fairly commonplace according to the
same log. Thus there is uncertainty about which polarization
response belongs to what source; moreover the graphite component
of the carbonaceous argillites in this hole has not been
specifically described, while measured core angles suggest a
prevalence of relatively flat dips, or of distorted strikes. All
this makes for uncertainty at the same time as it promotes the
intrigue of the setting and the need for a more precise
resolution of the inherent possibilities.
2) the low magnetic region in the south. At the south
extremities of line 800W, 900W, some very fair IP anomaly has
been encountered in correlation with a magnetic depression. This
is a new indication of mineral incidence in the area.
Interestingly, the anomaly involved again appears more related to
structure than to any individual lithology: on both lines the IP
expression is broadly and incompletely resolved (open to the
south) while exhibiting some sense of burial. This set of
circumstances would fulfill the existence of a source
mineralization centred upon and following in part the projected
major NNE fault which falls in between. At the same time there
is some evident tendency for the anomaly to be influenced by the
local stratigraphy and the syenite intrusion which borders to the
grid south. However a diabase dyke flanking the anomaly to the
west interrupts the flowering of any such budding relationship
here.
BXGAMBUR INTERNATIONAL, CONSULTANTS bTD.
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- 6 -
3) the separate incidences of perceived magnetic
abatement. The two specific locations 100S/1000W, 225S/800W
cited in the previous report are both supported by IP anomaly,
the first clearly and individualistically, the second
indistinctly in a compound expression. The first case is
particularly satisfying since it signifies potentially a new
mineral occurrence not before identified despite the lowered
resistivities which accompany it. The second case is not as
certainly established but again there is a resistivity low in the
setting. It retains an appeal in consequence.
All these events are important inasmuch as they occur
independent of the HLEM. Predictably the conductor axes
themselves provide IP anomaly and quite marked low zones in
resistivity in correlation. Resistivities of less than 50
ohm-metres, on occasion less than 10 ohm-metres, have been
recorded along these em. systems in a consistent fashion. The
highly conducting nature of these sections in fact has often
inhibited reliable determinations of chargeability within them.
Still looking beyond these conductors to outside
possibilities, there exists an array of IP anomaly in the west
that is additional to the specific features already discussed.
Anomalous conditions dominate virtually the whole of the line
1200W section south of the BL. Up to six separate peakings can
be recognized in this distance (350 m), and in combination they
constitute a sector that manifestly is widely mineralized.
Moreover it is to be noted that- this is a sector in the so-called
mobile zone close to the Montreal River-Narrow Lake break where
regional movement has been seen to have deformed country strikes.
BXGAMBUR INTERNATIONAL CONSULTANTS bTD.
- 7 -
A considerable potential for gold occurrence emerges here as a
consequence.
Within this context also, the possibility opens up that
the diabse dyke immediately to the east acts as a locus for IP
anomaly along its flanks. There are anomalies for instance at
SON and 350S on the adjacent line 1100W section that fit this
category, and both expressions are fair and additional to prior
considerations. Again at the BL on line 1200W, a strong peaking
there the most northerly of the six peakings on the section
is tucked in against the side of the dyke. The one exception to
this rule in the coverage is at the northeasterly extremity of
the same line (1200W) where there appears no anomaly on the
dyke's furthest flank. This result may just possibly mean that
mineral fluids moving along the dyke edges came in from the south
and died out with distance northwards across the property.
BXGAblBUR INTBRNATIONAb CONSULTANTS fcTD.
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- 8 -
CONCLUSIONS AND RECOMMENDATIONS
The completed IP/resistivity surveying has fulfilled its
primary objectives, that is to detect other mineralized settings
in the area separate from the drilled conductors. In this
respect it can be said that results have exceeded expectations.
Encouragingly, all such possibilities perceived from the
preceding magnetic and VLF surveying have been enhanced by these
IP results. Chargeability anomalies up to 5 times background
have been observed in those places, as well as in one or two
additional localities outside the encompass of the horizontal
loop em. conduction. Host resistivities range from 500-5000
ohm-metres. As a consequence, a number of fresh and diverse
targets for investigation present themselves. In these, the
chief goal is seen to be gold mineralization.
To accomplish an adequate testing of the resident
possibilities, however, it is specifically recommended that a
programme of diamond drilling be undertaken which will be largely
cross-sectional in nature directed at the various mineral
indications provided by IP/resistivity. The holes and sections
which are prescribed are listed below.
DDK #RR-88-1: Collar at 40S/800W
to be drilled grid S at -500 for 100 m
BXGAblBUR INTERNATIONAL, CONSULTANTS bTD.
- 9 -
DDK #RR-88-2: Collar at 90S/800W
to be drilled grid S at -500 for 150 m
DDK #RR-88-3: Collar at 185S/800W
to be drilled grid S at -500 for 125 m
DDK #RR-88-4: Collar at 40N/1200W
to be drilled grid S at -50 0 for 100 m
DDK #RR-88-5: Collar at 25S/1200W
to be drilled grid S at -500 for 100 m
DDK #RR-88-6: Collar at 75S/1200W
to be drilled grid S at -500 for 100 m
DDK #RR-88-7: Collar at 125S/1200W
to be drilled grid S at -50 0 for 150 m
DDK #RR-88-8; Collar at 225S/1200W
to be drilled grid S at -50 0 for 100 m
DDH #RR-88~9: Collar at 280S/1200W
to be drilled grid S at -50 for 100 m
DDH #RR-88-10: Collar at 290N/900W
to be drilled grid S at -500for 120 m
DDH #RR-88-11: Collar at 450S/900W
to be drilled grid N at -50 0 for 125 m
EXGAblBUR INTERNATIONAL CONSULTANTS IsTD.
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- 10 -
This drilling amounts to 1270 m (4165 1 ). It is
considered a practical outlay for the area and for the potential
newly proffered by the IP results. Care has been taken to cover
as many bets as possible, including the lingering chance of a
zinc-rich base metal mineralization in the wider volcanic context
of the property geology. Most holes are relatively short in
order to stay fairly close to the various aspects of the targeted
geophysics, especially the perceived structural components.
As the exploration enters the drilling stage, it is
further recommended that:
i) the graphite component of any carbonaceous sediments
be duly noted and estimated volumetrically;
ii) physical measurements of the core be carried out.
Magnetic susceptibility and conductance
determinations need to be made fairly regularly to
establish characteristic relationships between any
intersected source and its geophysical response. The
causes of conduction, polarization and magnetic
anomaly require explanation here if effective
projections of mineral potential are to be made in
future.
iii) the exact locations of past drill holes be fixed with
respect to present grid co-ordinates.
BXGAblBUR INTBRNATIONAb CONSULTANTS IsTD.
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- 11 -
A budget total of S200,000 is foreseen to fund these
recommendations if carried out in full (see Appendix). It is
strongly recommended that the proposed drilling be implemented
this fall, and more or less as given, since time is of the
essence and the property clearly warrants this kind of testing.
JBB:sb
August 18, 1988
J. B. Boniwell
Exploration Geophysical Consultant
BXGAblBUR INTERNATIONAL CONSULTANTS LTD.
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- 12 -
APPENDIX
Costs
Total costs for the recommended drilling stage on the
property are estimated at $195,000.00 as follows:
i) diamond drilling:
1270 m at SIIO.OO all-up
ii) assaying:
1000 samples at S12.00 (Au only)
100 samples at S7.50 (Zn)
iii) geological logging, sampling,
on-site supervision:
25 days at $350.00
iv) subsistence, transportation, supplies:
$139,700.00
12,000.00
750.00
8,750.00
1,750.00
v) geologic compilation, reporting, drafting: 3,500.00
vi) management, incl. assessment submission,
physical measurements on core:
Contingency
3,500.00
169,950.00
25,500.00
8195,450.00
EXGAblBUR INTERNATIONAL CONSULTANTS bTD.
Ontario
Ministry ofNorthern Developmentand Mines
Ministdre du Developpement du Nord et des Mines
300Whitney Block, Room 6biu Queen's Park Toronto, Ontario M7A 1W3
Telephone: (416) 965-4888
November 30, 1988 Your file: W8808-490 Our file: 2.11724
Mining RecorderMinistry of Northern Development and Mines4 Government Road EastKirkland Lake, OntarioP2N 1A2
Dear Sir:
Re: Notice of Intent dated November 15, 1988Geophysical (Induced Polarization) Survey submitted on Mining Claims L 892133 et al in the Township of Cairo
The assessment work credits, as listed with the above-mentioned 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,
W.R. CowanProvincial Manager, Mining LandsMines fc Minerals DivisionR™RM:plEnclosure
cc: Mr. G.H. FergusonMining and Lands Commissioner Toronto, Ontario
Regent Rock Resources Inc. 425 University Ave. Toronto, Ontario M5G 1T6
ONTARfO 3SOI.OGICAL SURVEY
ASSfcSSMENT FILES OFFICE
DEC l 1983
R E C e l v E D
Resident Geologist Kirkland Lake, Ontario
Mr. J.B. Boniwell 10 Hurontario Street Mississauga, Ontario L5G 3G7
Mmisivy.'oiNorthern Deve\opmen\
Mines
Ontarioa^LMi mj
Technical Assessment Work Credits
Date
November 15. 1988
File2.11724
Mining Recorder'* Report of Work No.
W8808-490
Recorded Holder
Regent Rock Resources Inc.Township or Area
Cairo Township
Type of turvey and number of Assessment days credit per claim
Geophysical
Rfldinmptrir Hays
Inrlnred polarization 20 riay^
Other . riays
Section 77 (19) See "Mining Claims Assessed" column
Geological riays
Genchemiral riays
Man days f] Airborne i i
Special provision RI Ground Q
O Credits have been reduced because of partial coverage of claims.
fi Credits have been reduced because of corrections to work dates and figures of applicant.
Mining Claims Assessed
l 8 92133 892135-136 892138
Special credits under section 77 (16) for the following mining claims
5 days Induced Polarization
L 892134
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 above 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)
Ministry ofNorthern Developmentand Mines
Report of Work
Ontario
^rPOx^.
Instructions: - Please type or printf- If number of mining claims traversed
exceeds space on this form, attach a list.Not*: - Only days credits calculated in the
"Expenditures" section may be enteredin the "Expend. Days Cr." columns.
- Do not use shaded areas below.Type of Survey(f)
Claim Holder(s)Induced Polarization/resistivity
Township or Ar*a
Cairo Twp.Prospector's Licence No.
Regent Rock Resources Inc.Address
Survey Company425 University Ave. , Toronto, Ontario, M5G 1T6--————
TBate of Survey (from A to)
Claridge La Rose Geophysics Ltd. ___ p&y | flo. | 3?. \ 8a3yv i Xw i ff f̂'ay | Mo. j Yr.
Total Miles of lin* Cut
N/AName and Address of Author (of Geo-Technicat report)
——-———3. B . Boniwell, 10 Hurontario St., MISSISSAUGA, Ontario, L5G 3G7Credits Requested per Each Claim in Columns at rightSpecial Provisions Geophysical
For first survey: -Electromagnetic Enter 40 days. (This includes line cutting) . Magnetometer
For each additional survey: - R"diometric
using the same grid: i -m\ •Other ( Ir)
Enter 20 days (for each)
Geological
Geochemical
Man Days ^^^ Geophysical
FiY Ft /fjI.Vi" J* - '" "^ P^TMlectromagnetic *tdJ8nter J6f.al(s) here . . ! i 0* jj
r^wS ' -' - 'lagnetometer
^ " OCT 21 J966 ^ iadiometric/o?. X -̂ ) ty~ ' ) ther
C~^T\ Geo1 'gical
~~ —————————— -CTBfhemical
Airborne Credits
Note: Special provisions Electromagnetic credits do not apply to Airborne Surveys. ; Magnetometer
; Radiometric
Days per Claim
20
Days per Claim
•••"••"'
Days per Claim
——————
Mining Claims Traversed (List in numerical sequence)
Expenditures (excludes power stripping)Type of Work Performed
Performed on Claim(s)
Calculation of Expenditure Days Credits
Total Expenditures
InstructionsTotal Days Credits may be appo choice. Enter number of days cr In columns at right.
l at the claim holder's er claim selected
DateOct. 19 '88
Recon Agent (Signature) l"
Certification Verifying Report of Work
Total numb*r of mining claims covered by this report of work.
l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, or witnessed same during and/or after its completion and the annexed report is true.
performed the work
Name and Postal Address of Person Certifying
•T. R. Rnniwell, 10 Hurontario St.,
MISSISSAUGA, Ontario, L5G 3G7Date Certified19 Oct. '88
Certifi
1362 (85/12)
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rMinistry ofNorthern Developmentand Mines
ntario
Geophysical-Geologlcal-Geochemlcal Technical Data Statement
File-
l l
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
Type of Survcy(s). Town ship or Area.
Claim Holder(s)—
Induced Polarization
Cairo Township, Ontario
Regent Rock Resources
___425 University Ave. , Toronto,————..
Survey Company Claridge La Pose Geophysics—————
Author of Report J . B. Boniwell——————————————
Address of Author 10 Hurontario St., Mississaugat Ont.
Covering Dates of Survey .23 July - 3rd August ' 88————((incoming to office)
Total Miles of Line Hut N/A_____;_________;—————,
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.
Geophysical—Electromagnetic.—Magnetometer——Radiometric——
DAYSper claim
(IP) 20
Geological.Geochemical.
AIRBORNE CREDITS (Special provision credit* do not
Magnetometer. .Electromagnetic.to airborne surveys)
omctric ____
Oct. 17/88
(enter dayi per claim)
SIGNATURE:A\'
Author of Report or Agent
Res. Geol.. .Qualifications.
Previous Surveys File No. Type Date Claim Holder
MINING CLAIMS TRAVERSED LUt numerically
L 892133 """"(pYe'fixf
892134(number)
892135
892136
892138
l
1j
TOTAL CLAIMS.
B37 /8S/12J
INDUCED rO!.-\R!7AT10\-
RF.SISTIVITY GRAVITY ELECTROMAGNETIC MAONF.TIC
GROUND SURVEYS — If more than one survey, specify data for each type of survey
NumbT of St^ti""* Number of Readings ,
Station interval Line spacing
Profile srale
Contour interval
Instrument
AcC'irary — Srale ronstant
Diurnal rorrerfion method
Base Station check-in interval (hours)
Rase Station location and value
Instrument
Coil configuration , . ,
Coil separation
AccuracyMethod: D Fixed transmitter D Shoot back Q In line
Frequency .(•pecify V.L.F. tution)
Parameters measured.
Instrument
Srale ronstant
Corrections made
Rase station value and location
Elevation arruracy
Instrument . ,. , .,. .
Method fD Time Domain D Frequency Domain
Parameters — On time 1 sec ' Frequency
-Off time 1 sec Range..
- Delay time 240 IPS
— Intepration time 100 msO
Power 2 Kva ,
F/lectrod** a.rrny r5ipolG~d!LDolG
Electrode spacing . 25 m , . . . . . ,- , ..., ,
Type of electrode ————— porous pots ———————————————————————————————
1
1
1
1
1
1
1H
D Parallel line
1
1
1
1
1m1̂m
l1
1
Ministry ofNorthern Developmentand Mines
Ontario
Report of Work(Geophysical, Geological, Geochemical and ExpenditJitures)
O f "i '-7 Of** (V^nin^Apt JL v 'W
instructions: — Please type or print.— If number of mining clarms i traversed
exceeds space on this form, attach a list. Note: — Only days credits calculated in the
./S "Expenditures" section may be entered in the "Expend. Days Cr." columns.
" "" — Do not use shaded areas below.Type of Survey(s)
Induced Polarization/resistivityClaim Holder(s)
Township or Area
Cairo Two.
Regent Rock Resources Inc.Prospector's Licence No.
Address
Survey Company425 University Ave., Toronto, Ontario, M5G 1T6
Claridge La Rose Geophysics Ltd.[Date of Survey (from a to)23 ,07 . 88 l 03 . 08 88^Day j Mo. ] Yr. J Day j Mo. j Yr.
(Total Miles of line Cut
N/AName and Address of Author (of Geo-Technical report)
________J. B. Boniwell, 10 Hurontario St., MISSISSAUGA, Ontario, L5G 3G7Credits 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)
Men Days
Complete reverse side and enter total(s) here
Airborne Credits
Note: Special provisions credits do not apply to Airborne Surveys.
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
-Other (IP)
Geological
Geochemical
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Electromagnetic
Magnetometer
Radiometric
Days per Claim
20
Days per Claim
Days per Claim
Expenditures (excludes power stripping)Type of Work Performed
Performed on Claim(s)
Calculation of Expenditure Days Credits Total
Total Expenditures Days Credits
S -h 15 -Instructions
Total Days Credits may be apportion choice. Enter number of days crauitt In columns at right. l l f
Date Oct. 19 '88
\Recorded 1Vj^
cM a t the claim holder's rjer claim selected
1Kbld^pr Agent (Signature)ES&l^rtl'
Certification Verifying Report of Work
Mining Claims Traversed (List in numerical sequence)Mining Claim
Prefix Number
L892133L892134
L892135
L892136
L892138
Expend. Days Cr.
Total number of mining claims covered by this report of work.
For Office Use OnlyTotal Days Cr. Recorded
Date Recorded
Date Approved as Recorded
Mining Recorder
Branch Director
l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto or witnessed same during and/or after its completion and the annexed report is true.
performed the work
Name and Postal Address of Person Certifying
.T. R. Roniwell,—10-Huron.tflrifiL-Stt
HTSSISSAUGA, Ontario, L5G 3G7Date Certified19 Oct. '88
Certifi
1362 {85/12)
AREAS WITHDRAWN ' ^OM DISPOSITION
M.A.O. - MINING RIGHTS ONLY
S.M.O. -SURFACE RIGHTS ONLY
M.* t. - MINING AND SURFACE RIGHTS
MIMN3 AND SURFACE HfiMTS NOT OPENTO STAKING, APPLICATION UNDER SECTION 3 l(b) JUNE I2J997.
GL4MM - PCNOM AfUCAlKM UMOeR rUBLJC UU08 ACT
hJMD UU KMHIT
NOTES
AREA WEST QF WEST MONTREAL RIVER
CLOSED TO STAKINO SUBJECT TO SEC. 3B(f)
OP THE WININO ACT, CO SEPT. I9T8
CTDV ANOTICE OF FOPrTrtS TOWNSHIP 7 ARE* PUONSKl FOREST MANA
AND MAY BE SUBJECTTHE MNR UNIT FORESTCONTACTED AT; P.O. BC
SWASTIKA. ONT. POK ITO 705-642-3222
42AWSE0272 2. H724 CAIRO
Alma Twp.
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DATE OF ISSUE
OCT 211988
HlGHW'V A;4D ROUTE Na
OTHER ROADS
TRAILS '
SURVEYED LINES:TOWNSHIPS. BASE LINES. ETC.
i.. MINING CLAIMS. PARCELS. ETC,
JNSURVEYED LINES:LOT LINESPARCEL BOUNDARY -MINING CLAIMS ETC
RAILWAY AND RIGHT OF WAY
UTILIT\ LINES
NON-PERkNNIALSTFEAM
. .CODING OR FLOOD'NG RIGHTS
SUBDIVISION OR COMPOSITE PLAN
K5SERVATIONS
ORIGINAL SHORcLIKE
MARSH OR MUSKEG
MINES
TRAVERSE MONUMENT .
DISPOSITION OF CROWN LANDS
OF DOCUMENT
^ATENT, SURFACE ft M, KING. s-jsFAce R IGHTS.MINING RtGHTbO.LY .....
LEASE. SURFACE 4 MlfllNG RIGHT? .
" ,SURFACc RICH "SONL''. _ ,
" , MINIf J RIGHTS ONLY....—
L'CENCEOF OCCUPATION . ___ .
ORDER-IN-COUNClL .. .... .........
RESERVATION..... ..,....... —
CANCELLED ,................ ...
SAND 4 GRAVEL . __ .....,........
SYMBOL
^ c*
....rf ....... CT
. __ .. _ .-^. B
.,. __ ,...LA*-~
, .......... _ . Of
WOTI: WININO M IGHTS M PARCELS P*~fcNTto PHIO* T O MA*
1*13. V tSTIti i* ORIGINAL P ATfNTEE i 1 THC *Utj' LA W Of ACT F .; o |97O CMA* 3*O, SCC *3. i -J M l C
SCALE ,ti' V - -'1C
•(ITTOO 6000
O 200 lOOOl l KM)
2UOO (2 -M t
j TOWNSHIP
CAIROJM M.R. ADMINISTRATIVE OISTRffT
KIRKLAND LAKEMINING DIVISION
LARDER LAKELAND TITLES/ REGISTRY DIVISION
TIMISKAMING
Ministry of Ministry ofNatural Northern DevelopmentResources and MVies
OntarioOat* JULY 1984
G-3209
o o
600K
400N
200N
OS
200S
400S
600S
700So oCD
O O
oo f\J
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o cOD
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LEGEND
Interpreted fault showing
relative movement and
basis for projection.,... M - Magnetics V - VLF EM tNSS) G - Geology
Projected geologic contact,
Magnetic horizon.............
H LEM conductor showing width ,,
Old DDH with identification C
showing horizontal extent... 0
IP anomaly showing peak,
relative amplitude and lateral extent,. . ,.. ... . ..
Proposed DDH with identifier and horizonta projection ,.........
Limits of l P coverage .
WKMed Strong
88-2
200m
-2500
REGENT ROCK RESOURCES INC.
CAIRO TOWNSHIP PROJECT
LARDER LAKE MINING DIVISION
ONTARIO CANADA
PLAN of INTERPRETATIONSHOWING i P RESULTS
Date - AUGUST 1988 DWG. Mo E.l.C. - 1997
42A02SE027a 2.11724 CAIRO aio
325S
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4171 2167 177 12.0
4841
3536
100 2796 1566 396! 4290
14.0
353 77.0
5085
2534
2-9 3.1 5.1
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5.9
ri = 2
n = 3
n = 4
320
SURVEY SPECIFICATIONSDELAY TIMF ' 2 40 m secINTEGRATION TIME t l 00 m secCONFIGURATION * D l p o l e-D l p o l e Array
DIPOLE SEPARATION - 2 5 meters
PLOTTING SPECIFICATIONS
HORIZONTAL SCALE : 1=1250
CHARGEABILITY
RESISTIVITY
Contour
10 msec contour
1 msec contour
Re n g e
Above 2500
2500 - 500Below 500
O
! n t e r v a l
0000 ohm-fn
2500 ohm-m500 ohm-m100 ohm-m
•" o- fc ,-*f -*-
DATA ACQUISITION i
DATA PROCESSING iJOB NUMBER -
TESLA-10 LTD TC-1044
REGENT ROCK RESOURCES INC
CAIRO TOWNSHIP PROJECT
IP PSEUDO SECTION
LINE '- 5 00W
Dwg N o . E.I.C.-1989 Date i 15-Aug-88
ro u Q
O) o O
APPARENT CHARGEABILITY
(msec)
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306 220 527
266
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4-4 3.0 0-9 9-4
SURVEY SPECIFICATIONSDELAY TIME ' 240 msecINTEGRATION TIME ' 100 m secCONFIGURATION - D l p o l e-D l p o l e A rrayDIPOLE SEPARATION - 2 5 meUrs
PLOTTING SPECIFICATIONS
1 O 250HORIZONTAL SCALE :
CHARGEABILITY
RESISTIVITY
Contour
10 msec contour l msec contour
Range
Above 2500
2500 - 500 Below 500
I n i: e r v a l
0000 ohm-m2500 o hm-m500 o h m~m100 o hm~m
DATA ACQUISITION
DATA PROCESSING JOB NUMBER
TESLA-10 LTDTC-1044
REGENT ROCK RESOURCES INC-
CAIRO TOWNSHIP PROJECT IP PSEUDO SECTION
LINE 700W
Dwg No. E .I,C. - 1991 Date i !5-Aug-88
2.11724 CAIRO 240
450S 425S 400S 3753 350S
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100
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n = 2
n = 3
n = 4
SURVEY SPECIFICATIONSDELAY T IME i 240 msecINTEGRATION TIME : 100 msecCONFIGURATION : D lpo i e-Dl po l e ArrsyDIPOLE SEPARATION ' 25 meters
PLOTTING SPECIFICATIONSl:1250HORIZONTAL SCALE '
CHARGEABILITY i
RESISTIVITY
Contour-
10 msec c ontour l m sec c ontour
Range Interval
Above 2500 10000 o hm-m 2500 ohm-m
2500 - 500 5 00 ohm-m Be l ow 500 100 ohm-m
DATA ACQUISITION
DATA PROCESSING JOB NUMBER
TESLA-10 LTD TC-1044
REGENT ROCK RESOURCES INC
CAIRO TOWNSHIP PROJECT
IP PSEUDO SECTION
LINE : 800W
Dwg No . E.I.C.- 1992 Date i 15-Aug-88
2.11724 CAIRO 250
LU a: LU o: o, Q.
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n =
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n -
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n =
3
n =
4
SURVEY SPECIFICATIONS
DELAY TIME
: 240
msec
INTEGRATION TIME
' l 0
0 msec
CONFIGURATION
' Dipole-Dipols Array
DIPOLE SEPARATION
'- 25 meters
PLOTTING SPECIFICATIONS
HORIZONTAL SCALE
- 1
:1250
CHARGEABILITY
'
RESISTIVITY
Contour
10 msec contour
1 msec contour
Range
Interval
Above
2500
10000
ohm-m
2500 ohm-m
2500
- 500
500 ohm-m
Be low
500
100
ohm-m
DATA ACQUISITION
DATA PROCESSING
JOB NUMBER
TESLA-10 LTD
TC-1044
REGENT ROCK RESOURCES INC
CAIRO TOWNSHIP PROJECT
IP PSEUDO SECTION
LIN
E
:900
W
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1 25S
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n =
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SURVEY SPECIFICATIONS
DELAY TIME
: 240
msec
INTEGRATION TINE
' TOO
msec
CONFIGURATION
' D l
p o
l e-D l
p o
l e
Array
DIPOLE SEPARATION
: 25 meters
PLOTTING SPECIFICATIONS
HORIZONTAL SCALE
: 1=1250
CHARGEABILITY
RESISTIVITY
Contour
10 msec contour
1 msec contour
Range
Interval
Above 2500
10000 ohm-m
2500 ohm-m
2500
- 500
500 ohm-m
Below
500
100
ohm-m
DATA ACQUISITION
DATA PROCESSING
JOB
NUMBER
•^ l
TESLA-10 LTD
TC-1044
REGENT ROCK RESOURCES INC
CAIRO TOWNSHIP PROJECT
IP PSEUDO SECTION
LIN
E
MO
OO
W
Dw
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o .
E.I.C
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994
Date
:
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2944 ""5966 3152 2093
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B5872 B2988 B6045 J 0212 ^5555 ^ 551 ^3362 B5477 n - 1
4190,^ 6603 n ^ 2
^
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3.7 3.6 3.6 4.
4-6
25.23.2
n = 2
n - 3
n - 4
SURVEY SPECIFICATIONSDELAY TIME : 240 msecINTEGRATION T IME : 100 msecCONFIGURATION : D l p o le-Dlpol e ArrayDIPOLE SEPARATION - 2 5 meters
PLOTTING SPECIFICATIONS
HORIZONTAL SCALE ' 1:l 250
CHARGEABILITY
RESISTIVITY
Contour
10 msec contour
1 m sec c ontour
Range Interval
Above 2500 10000 ohm-m 2500 ohm-m
2500 - 500 500 ohm-m Be l ow 500 100 ohm-m
DATA ACQUISITION :
DATA PROCESSING 'JOB NUMBER :
TESLA-10 LTD TC-1044
REGENT ROCK RESOURCES INC
CAIRO TOWNSHIP PROJECT
IP PSEUDO SECTION
LINE :1200W
Dwg N o. E.!.C. - 1996 Date : 1 5-Aug-88
42A02SE0272 2.11724 CAIRO 230