rpt on the 1995 geophys program shining tree …
TRANSCRIPT
41P11NE0057 2.15036 BERNHARDT 010
2-1593 6
REPORT OH THE
1995 GEOPHYSICAL PROGRAM
FOR
KRL RESOURCES CORP.
ON THE
SHINING TREE PROPERTIES
LARDER LAKE MINING DIVISION, ONTARIO
RECEIVED
APRS 1995
MINING LANDS BRANCH
Submitted by: R.J. MeikleRayan Exploration Ltd. Feb. 28,1995
41P11NE0057 2.15938 BERNHARDT 01OC
PAGE NO.
1233455,67,8,99,1011,12131314,15,16,1718,1920,21,2223
Pig. lFig. 2Fig. 3Fig. 4Fig. 5
Appendix A Appendix B Appendix C Appendix D Appendix E Appendix F Appendix G Appendix H
TABLE OF CONTENTS
CONTENTS
Introduction Location and Access Properties Personnel Previous work Geophysical Program Magnetometer Survey VLF-EM Survey HLEM Survey I.P. Survey Survey Results Fi lo Option Perkins Prospect Cook Option O'Bradovich Option Certification
LIST OF FIGURES
LocationRegional Location Land Holdings Map Claim Location Map Grid Location Map
APPENDICES
Scintrex IPR-12/IP Receiver Scintrex IPC-9/IP Transmitter Scintrex OMNI Plus/Magnetometer Apex Max-Min II/HLEM Instrument Geonics EM-16/VLF Receiver ForPro Resources Ltd.-Linecutting Inv. Rayan Exploration Ltd.-Geophysical Inv. Fi lo Option - VLF Plan Map
INTRODUCTION
Rayan Exploration Limited of Timmins Ontario, was hired on a
contract basis by, KRL Resources Corp., to conduct a geophysical
work program on their "Shining Tree Area Properties". The
portion of the Shining Tree Properties covered by this work
program are situated within Natal, Knight, Tyrrell, and Macmurchy
Townships, Larder Lake Mining Division, Districts of Sudbury and
Timiskaming, Ontario (Fig.l).
The geophysical program was carried out on four separate
grids, - "Perkins Option, - "Pilo Option", - "Obradovich Option",
and the "Cook Option".
The program consisted of a Magnetometer, VLF-EM, HLEM and
an Induced Polarization Survey, all of which were carried out
during the months of Jan. and Feb., 1995.
The purpose of this project was to further test areas known
to contain significant gold and base metal mineralization. A
diamond drill program was planned to test any significant
geophysical results.
This report will outline the survey parameters used and
results of the geophysical surveys conducted on each of the four
separate properties.
LOCATION AND ACCESS
The four grids covered by this work program are located
within Natal, Knight, Tyrrell, and Macmurchy Townships, Larder
Lake Mining Division, Districts of Sudbury and Timiskaming,
Ontario.
The Shining Tree Properties, are located approximately 80
km. south from the city of Timmins, Ontario. Locally, the work
area is situated about 20 km. northeast of the village of Shining
Tree, or 20 km. west of the village of Gowganda (Fig.2).
During the survey period, the work crew stayed in the
village of Gowganda, and the property was accessed from there. A
25 km. ride on Highway 560, west from Gowganda provided excellent
access to the central portion of the property. This Highway cut
east west through the block.
From here, the remainder of the block was accessed by
snowmobile. In this area, a network of old logging and drill
roads heading north and south of the highway, were utilized. This
provided good access to much of the remainder of the property.
73
43 49
PROVINCE OF ONTARIO
FlQ#l
KLR KESOUPCES CORP.SHINNING TREE AREA PROP.
LOCATION MAP
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PROPERTIES
The Shining Tree Property currently being worked by KRL
Resources Corp. is made up of a variety of different claim groups
and option deals (Fig. 3). Of these, the current geophysical
program covered only four of the areas. A brief description of
the four claim blocks, as well as the type of geophysical
coverage is listed below.
FILO OPTION- 9 claim units located in Knight Township*- 44 claim units located in Natal Township- Geophysical coverage: HLEM and VLF-EM
PBRKINS PROSPECT- 30 claim units located in Natal Township- Geophysical coverage: Mag, Max-Min and IP
COOK OPTION- l claim unit located in Macmurchy Township*- l claim unit located in Natal Township- Geophysical coverage: IP and Mag.
OBRADOVICH OPTION- 19 claim units located in Macmurchy Township*- Geophysical Coverage: IP
PERSONNEL
The people directly involved in the geophysical program
covered in this report were all employed by Rayan Exploration
Limited, of Timmins, Ontario, and are listed below.
Wayne Pearson...................TimminsEddy Brunet.....................TimminsAural Chamont...................TimminsDonny McKinnon..................TimminsLanny Anderson..................Timmins
All work was supervised by R.J.Meikle.
Outright Purchases Decker Mckel Claim
Land Holdings ft Relative Aquisition Map Scale: 1 Inch - 1 life
Claim location Hop
Scale: 1 tech - l UBe
ppKVIOUS WORK
The following is a brief account of the work previously
filed on the Shining Tree Properties, which is currently held by
KRL Resources Corp.
A number of companies have been active in the immediate
area. Some of these include Timiskaming Nickel Ltd., Mcintyre
Porcupine Mines, Ecstall Mining Company and Getty Mines Limited.
These companies have worked the ground at different times between
1948 and 1976. A variety of different geophysical and geological
programs were conducted, some of which reported encouraging
results. Some of these results includes various geophysical
targets as well as assay results of .005 oz/Au., .02 oz/Ag., .02
oz/Zn. 024 oz/Pb and .13 oz/Cu.
Recent sampling of the property done by KRL Resources
limited has reported significant values in Au. and Cu. These
include Au. values ranging from .124 oz to 5.3 oz/ton, and Cu.
values as high as 6.lit Cu.
Overall, work previously conducted on the properties
indicates an excellent gold and base metal potential.
Grid Location Map Scale: 1 Inch - l Uile
GEOPHYSICAL PROGRAM
Rayan Exploration Limited was hired on a contract basis by
KRL Resources Corp. to conduct a geophysical work program on
their "Shining Tree Area Properties". This consisted of
Magnetometer, VLF-EM, HLEM and Induced Polarization Surveys.
These surveys were carried out during the months of January and
February, 1995. Four separate grid areas were surveyed. For the
types of surveys done in each area, refer to the "Properties"
portion of this report. A general description of the instrument
specifications, as well as the survey parameters used is
discussed in further detail below.
MAGNETOMETER SURVEY:
The magnetometer survey was carried out on portions of the
Perkins Prospect and the Cook Option. This includes 2.5 km. on
the Cook Option, and 20 km. on the Perkins Prospect, for a total
of 22.5 km.
An EDA Omni Plus Proton Precession magnetometer was used to
carry out the magnetometer survey. The instrument is
synchronized with an EDA recording base station to help eliminate
magnetic diurnal variation. This should ensure an accuracy of
less than 10 Nt.
6
The Proton Precession method involves energizing a wire coil
immersed in a hydrocarbon fluid. This causes the protons in the
proton rich fluid to spin or precess simulating spinning magnetic
dipoles. When the current is removed the protons precess about
the direction of the earth's magnetic field, generating a signal
in the same coil which is proportional to the total magnetic
field intensity. In this way, the horizontal gradient of the
earth's magnetic field can be measured and plotted in plan form
with values of equal intensity joined to form a contour map.
This presentation is useful in correlating with other data
sets to aid in structural interpretation. Individual magnetic
responses can be interpreted for dip, depth and width estimates
after profiling the data.
The following parameters were employed for the survey:
Instrument - EDA Omni Plus Proton Precession MagnetometerStation Interval - 12.5mLine Interval - 100mDiurnal Correction Method - EDA Recording Base StationData Presentation - Perkins Prospect and Cook Option
- Plan, Magnetic Contour Map- 1:5000 scale- Contour interval = 20 nano-teslas
7
VLF - EM Survey
The VLF survey was conducted on the Fi lo Option, and
consisted of 1.5 km. of survey to locate a previous VLF
conductor.
A Geonics EM-16 VLF, instrument was used, recording both the
In-phase (dip angle) and Quadrature values at 25m intervals.
The following is a brief description of the VLF method.
While VLF stands for Very Low Frequency, it is for mineral
exploration purposes a very high frequency compared to other
commonly used Electromagnetic Surveys. The commonly used
frequencies are in the order of 18-20 kilohertz. The VLF-EM
technique employs fixed transmitter stations located at various
places around the world to facilitate navigation. Because of
this, one has a limited choice as to what transmitter station
that can be used, depending on distance from and azimuth to the
transmitter station.
For this survey, Annapolis Maryland, (NSS) was used. It has
an operating frequency of 21.4 khz and an azimuth of
approximately of 160 degrees TN from the property. Very briefly,
the transmitting station emits a concentric, circular wave
pattern, expanding about the transmitter dipole. Being thousands
of miles away from the transmitter, we deal with the tangent of
this wave pattern which in this case would have a direction
normal to the azimuth of 160 degrees. Thus any conductors having
a general NS strike direction would be intersected by this signal
which induces a signal in the conductor which in turn opposes the
8
primary signal from the transmitter station. This elliptically
polarizes the resultant field enabling detection of the conductor
using a receiver coil to determine the attitude of the resultant
field at various points along the grid lines.
The resultant field dips away from the conductor axis on
both sides of the conductor producing a cross-over on the
conductor axis. For an NS conductor, a true cross-over would
occur where the field dips south and changes to a east dip as you
progress from west to east. For this survey, a +/- system is
used where a (-1-) dip angle means the field is dipping to the west
(indicating anomaly is to east) and a (-) dip angle means the
field is dipping to the east (indicating anomaly is to
west). This is the case only if all readings were taken facing
east as per this survey.
The quadrature values, while not useful alone, can help
distinguish between bedrock conductors which generally have a
smaller out-of-phase response than overburden or short wavelength
conductors. Also, the polarity of the quadrature is diagnostic,
ie; if the polarity follows or is the same sense as the In-phase
it gives more credibility to the conductor. Reverse quadrature
often indicate overburden responses.
The following parameters were employed for the survey:
Instrument - Geonics EM-16 VLFTransmitter Station - Annapolis, Maryland (USA)
-Call symbol NSS Frequency - 21.4 KHZAzimuth to station - approx. 160 degrees TN Reading Direction -All reading taken facing east Station Interval - 25m Line Interval - 100m
Data Presentation - Plan, profiled map. Fi lo Option- Scale - 1:5000- profile scale l cm - 20*- Appendix - H
HORIZONTAL LOOP EM SURVEY
The HLEM survey was conducted on both the Fi lo Option and
Perkins Prospect. A total of 3 km. on the Fi lo Option, and 5 km.
on the Perkins Prospect, resulting in 8 km. overall.
The Horizontal Loop EM survey was carried out with an Apex
Max-Min II instrument. These surveys are commonly called "Max-
Min" surveys in recent times.
The Max-Min II instrument can operate at five frequencies
(3555HZ, 1777HZ, 888HZ, 444HZ, 222HZ)., and is capable of coil
separations from 25 meters to 200 meters. Although it can be
used in the vertical loop mode as well as minimum coupled, it is
most often used in the Maximum Coupled, Co-Planer mode which is
in effect a Horizontal Loop Electromagnetic Survey.
The instrument records the "In-Phase" and "Out-of-Phase"
components of the anomalous resultant field from a conductor as a
percentage of the primary field strength. Both components are
used in the interpretation of the results. Generally, the larger
the ratio of peak negative responses between In-Phase and Out-of-
Phase, the higher the conductivity of the anomaly. A ratio of
1:1 is considered a medium conductor.
The purpose of reading more than one frequency is to obtain
more information about the conductor itself as well as the
10
conductivity of the overburden etc. The higher frequencies will
respond to weaker conductive features such as faults, conductive
overburden etc. As a result the signal from these frequencies
can attenuate very quickly, possibly not penetrating to the
bedrock at all. The lower frequencies having a longer wavelength
tend to penetrate deeper and generally only respond to anomalies
with a higher order of conductance,. Thus as with most
geophysical techniques it is a trade off as to depth of
penetration vs. conductance threshold detectable. The use of
multi frequency surveys helps to alleviate this problem at a
minimal extra cost.
The Max-Min survey was carried out using an Apex Max-Min
II instrument reading 1777HZ, and 444HZ with a constant coil
spacing of 100 meters. The Maximum Coupled mode was employed
with the coils co-planer. A reading interval of 25 meters was
used. Because of the relatively flat surface topography, no
slope or topographic corrections were necessary. The entire
survey was read with unit serial no. 1057 with twice daily phase
mix testing to ensure that the data would be consistent across
the surveyed area.
The following parameters were used for the HLEM survey.
Instrument: Apex Max-Min IIStation Interval: 25 MLine Interval: 100 MFrequencies: 444 Hz., 1777 Hz.Coil Separation: 100 MData Presentation: - Profiled Plan Map: Fi lo Option
: Perkins Prospect- Scale: 1:5000- Profile Scale: l cm. s 10 t
11
INDUCED POLARIZATION SURVEY
The Induced Polarization Survey was conducted the Perkins
Prospect, Cook Option and Obradovich Option. This resulted in a
total of 25 days of Induces Polarization being conducted.
Individually, this breaks down to 9 days on the Perkins
Prospect, 2 days on the Cook Option and 14 days on the Obradovich
Opt i on.
The IP method involves applying voltage across two
electrodes in a pulsed manner i.e. 2 seconds on, 2 seconds off. A
second "dipole" or electrode pair, measures the residual
potential or voltage between them after the voltage is shut off
or during the 2 second off cycle. The potential is recorded at
different times after the shut off. If, for example, there is
sulphide mineralization within the measuring dipoles, they will
be polarized or charges set up on the sulphide particles. This
polarization gives the zone a capacitor effect, thereby blocking
the current delay giving a higher chargeability reading.
A typical signature for many gold showings would be a
chargeability high, resistivity high and magnetic low. This would
be characteristic of a mineralized, highly altered carbonated
and/or silicified zone. However, this is by no means the only
geological setting for gold, therefore every profile should be
looked at individually and correlated with all other geophysical-
geological data.
12
Electrode Array
The electrode array used for the survey was the Dipole-
Dipole Array. In this array two current electrodes (CI, C2) and
two receiver or potential electrodes are moved down a line in
unison. In this case the "a" spacing or distance between each
dipole was fixed at 25 meters apart. For an Ns l reading, the
closest Ci and PI were 25 meters apart. The C1-C2 dipole remain
in the same place while the potential dipole (P1-P2) moves ahead
on "a" spacing and the array is ready for an N-l reading.
IP Survey Parameters
The IP survey was carried out using the following
parameters:
Method: Time DomainElectrode Array: Dipole-Dipole"a" spacing: 25 metersNumber of Dipoles Read: 1-4Pulse Duration: 2 seconds on, 2 seconds offDelay Time: 310 millisecondsIntegration Time: 120 millisecondsReceiver: Scintrex IPR-12Transmitter: lPC-9 200 kva.Data Presentation: Contoured Psuedo Sections on plates:
- Obradovich Option: 3 Plates- Perkins Prospect: 2 Plates- Cook Option: l Plate
Scale: 1:2500
13
SURVEY RESULTS
The geophysical program conducted on the Shining Tree
Properties for KRL Resources Corp. was successful in outlining a
number of areas of interest. The results obtained for the four
different areas surveyed will be discussed separately and any
significant geophysical responses occurring within them, will be
also be discussed individually and in further detail below.
FILO OPTION
The geophysical surveys conducted on the Fi lo Option took
the form of a VLP-EM and HLEM survey. This was successful in
outlining a previously detected VLF conductor running through the
grid in roughly a north south direction. The VLF results show the
zone to extend from L2N/275E to L4N/300E, and remaining open in
both directions. The HLEM conducted on these same lines shows a
one line conductor on L3N/274E, which is coincidental with the
VLF conductor.
There is an in-phase response on L3nX250e and L4nX162n, with
no quadrature response. This anomaly could be a result of
topography but should be investigated as it appears to line up
with the response on L2n.
If the HLEH/VLF conductor is the primary focus on this
property, there is sufficient data to diamond drill test it at
this time.
14
PERKINS PROSPECT
This ground was covered with a Magnetometer, HLEM and
Induced Polarization Survey. These surveys were successful in
outlining several areas of interest.
The limited amount of HLEM Survey was done to check out a
surface showing at approximately 930w7340n, reported to be a
Cu/Massive Sulphide mineralized zone. The I.P. Survey outlined a
a strongly chargeable/conductive anomaly on L3n7875-1000w, with
the strongest chargeability centred at 850w, coincident with a
weak HLEM conductor on L3nX950w. It is most likely that the
coincident IP/HLEM anomaly is related to the sulphide showing
approx. 40m to the north. The poor conductivity shown on the HLEM
survey and the strong chargeability on the IP Survey would
suggest that the mineralization is more likely of a disseminated
nature, rather than massive sulphide mineralization of any
significant width. There is a similar HLEM/IP anomaly on
L2nX!Ol2w, Lln/iosow, appearing to be the same continuous
anomaly. Because of the likely possibility that this anomaly is
related to the sulphide showing mentioned above, it should be
investigated further and explained.
The HLEM Survey also outlined a weak conductor running
parallel to and approximately 125 meters west of the above
described HLEM/IP Anomaly. It has a weak quadrature response only
on the HLEM Survey. The IP Survey response shows a narrow very
conductive zone coincident with the HLEM conductor but not
chargeable. This type of response parameter is indicative of that
15
associated with a fault zone. The Magnetometer Survey shows the
anomaly to be in a relative magnetic low on the east flank of a
parallel linear magnetic high.
The Magnetometer Survey shows both the east and west grids
on the Perkins Option to have a relatively complex magnetic
susceptability pattern with several linear grid north-south lows
and highs.
The I.P. Survey outlined several chargeability anomalies,
some conductive and others resistive. Generally there is good
line to line correlation of the different anomalous zones. The
various IP anomalies are described as follows:
Anomaly 'A f
This anomaly is a highly chargeable/conductive zone striking
across the east end of the grid at approximately 550w is
coincident with a power line, and is thought to be caused by it.
Anomaly 'B'
This anomaly is quite resistive with moderate chargeability
for the most part with a strong chargeability on Lln7687w. It
strikes from L3nX675w - LOn/eBOw, open on both ends.
Anomaly ' C'
This is a broad, mod. chargeable/resistive anomaly parallel
to and on the east flank of the conductive HLBM/IP anomaly 'D'.
16
Anomaly 'D'
This is a strongly chargeable/conductive anomaly with a
coincident HLEM response. It extends from L3n7950w - Lln/lOSOw,
open on both ends. As mentioned under the HLEM results above, it
could possibly be related to a sulphide showing at approximately
340n7930w which contained significant Cu values.
Anomaly ' E'
This is a mod. resistive anomaly, strongly chargeable on L2n
and mod. chargeable on Lln,L3n, at approx. 13w, open to the
north.
Anomaly ' F'
This is a weakly chargeable/resistive anomaly extending from
L3S/2030W - L9S/2060W, open to the south. It is broad on L4s and
there is no response on L5s where the resistivities quite low.
While the magnetic survey does not indicate any obvious reason
for the interruption between L4s and L6s, there must be
structural feature such as a fault in this area.
Anomaly 'G'
This is a strongly chargeable/mod, resistive, one line
response on L7S/2280W.
17
Anomaly ' H'
This is a nod. chargeable/resistive anomaly on a contact
with a conductive area to the east, running grid north-south
along the west end of the grid lines at approx. 2800w. The
contact is quite apparent with the unit to the west being quite
resistive, while the resistive unit has a higher background,
possibly due to grain size, and or wide spread disseminated
mineralization. Anomaly 'H' appears to be a distinct, linear,
more mineralized zone on the contact.
One of the more obvious priority targets would be Anomaly
'D'. It should be explained by trenching and or drilling to
determine if it is related to the sulphide showing.
The remaining I.P. anomalies described above should be
prospected and the ones with higher chargeability explained by
trenching and or drilling. A compilation with available
geological information would help resolve the geology and
possibly explain the rather complex resistivity. Discussions with
KRL field personnel indicate that the geology is quite complex
with diabase and gabbroic dikes cutting through the property. It
is important to attempt to identify which I.P. and Magnetic
responses are associated with them.
The NW tending anomalies in the southwest part of the grid
should be tested as possible extensions of the I.P. anomaly on
the Cook grid, coincident with the gold occurrence and appearing
to be on strike to the southwest.
18
COOK OPTION
The Cook Option grid was covered by a Magnetometer Survey
and an I.P. Survey. The Magnetic Survey shows a complex magnetic
susceptability pattern of linear, grid n-s highs and lows. It is
difficult to correlate with the I.P. anomalies.
The I.P. Survey outlined several anomalies described as
follows:
Anomaly 'A f
This is a broad weakly chargeable/mod, resistive anomaly on
Lls725e-130e, L3S/606, L4S/506, L5s/?, open north and south, and
to the east on Lines 4s and 5s. It was not detected on L2s which
is underlain by Ashburn Lake which appears to have a conductive
lake bottom, possibly masking the anomaly if it does exist on
this line. The I.P. Anomaly appears to be in a relatively
magnetic low area.
Anomaly 'B'
This anomaly is a strongly chargeable/conductive zone on L3s
from l7Se, open to the east and along strike.
Anomaly ' C'
This is a strongly chargeable/mod, resistive anomaly on
LSs/lSOw-open to west, and mod. chargeable/mod, resistive on
L4S/150W and L5S/125W. The anomaly is not fully covered to the
west on all lines. It is tending NW and is coincident with a
known gold occurrence on LSs/lBBw, which is believed to trend NW
as well.
19
Anomaly 'D f
This anomaly is a strongly chargeable/resistive zone on
L5S/10OW-25W. It has a 2000nT coincident magnetic response.
The above anomalies should all be followed up. The highest
priority would probably be Anomaly C which is possibly coincident
with the gold occurrence outlined by extensive trenching. The
I.P. Survey suggests that the zone extends in a NW/SW direction
off the property. As such the response on L4s and L5s should be
explained.
Anomaly 'B' is quite chargeable and conductive and could be
caused by massive sulphides and or graphite. There is not enough
coverage to resolve the strike direction at this time.
Anomaly 'D' is strongly chargeable and resistive. It does
not appear to be similar to 'C', but it is on strike and should
be explained.
20
OBRADOVICH OPTION
The I.P. Survey indicates that the property is highly
resistive for the most part with the exception of a conductive
area in the NE part of the grid east of the baseline on Lines 2s
to 4s, and on the west ends of lines 10s to 15s. There is a
relatively low resistive area in the central part of the grid
approximately 400m wide from L9s to L13s where it narrows and
extends to L17s.
The I.P. Survey outlined numerous chargeability anomalies,
most within the resistive areas. It is difficult to correlate the
anomalies from line to line. Some of the more weakly chargeable
zones within the resistivity highs could be caused by rock
type(grain size etc.), and or disseminated sulphides. Much of the
weaker chargeability anomalies within the resistivity highs
marked on the I.P. sections may in fact be indicative of the
background and not anomalous. The more discrete and more
chargeable zones will are described below as well as any
chargeability anomalies within the conductive areas.
It is important to keep in mind that some of the reason for
the complex and irregular resistivity pattern may be caused by
the change in topography in the area with numerous bedrock ridges
and overburden filled valleys in between.
The following is a description of some of the more
prospective anomalies:\
21
Anomaly 'A'
This a mod. chargeable/mod, resistive anomaly on L1S/25W and
weaker on L2S/60W. It is in contact with a conductive area to the
east.
Anomaly 'B'
This is a HW tending, resistive anomaly in contact with a
lower resistive unit to the east. It has the strongest
chargeability response on L4S/105W and LSs/Oe with more moderate
chargeability on L6S/756 and L7S/256, assuming they are the same
zone.
Anomaly 'C'
This is a NW
tending anomaly running from L9S/5806 - L12S/7126. It is strongly
chargeable and very resistive within a resistive unit.
Anomaly 'D r
This is a NS tending anomaly running from L14S/5206 -
L20S/4806. It is moderately chargeable and resistive. It appears
to be a distinct linear zone within the broad resistivity high
area.
Anomaly 'E'
This is a one line response on L14S/76. It is strongly
chargeable and moderately resistive.
22
Anomaly ' P'
This is interpreted to be a NW tending anomaly running from
Lds/GOe to Llls/3306. It possible that it continues to the SE and
is the same feature as Anomaly 'E' but the resolution between is
not good enough. The anomaly may also extend to the NW but
resolution with the high resistivity unit is poor. It is
strongly chargeable, and moderately resistive on Lines 9s and
10s.
There are several anomalies not described above which could
be of interest and should be interest. The anomalies should be
prospected and a thorough compilation of all data be done to
prioritize them. A magnetometer survey should be done to help
correlate and resolve the geology. It is important to attempt to
explain as many anomalous responses as possible to differentiate
between true chargeability responses caused by mineralization and
background type responses caused by different rock types etc.
CERTIFICATION
I, Raymond Joseph Melkle of Timmins, Ontario hereby certify that:
1. I hold a three year Technologist Diploma from the Haileybury School of Mines, Haileybury, Ontario, obtained in May 1975.
2. I have been practising my profession since 1973 in Ontario, Quebec, Nova Scotia, New Brunswick, Newfoundland, NWT, Manitoba, Germany and Chile.
3. I have been employed directly with Teck Corporation, MetalIgesselIschaft Canada Ltd. Sabina Industries, .S. Middleton Exploration Services Ltd., self employed 1979-1985 (Rayan Exploration Ltd.) and currently with Rayan Exploration Ltd.
4. I have based conclusions and recommendations contained in this report on knowledge of the area, my previous experience and on the results of the field work conducted on the property during 1995.
5. I hold no interest, directly or indirectly in this property, nor do I expect to receive any interest or considerations from the KRL Property other than professional fees for services rendered.
Dated this 28th day of February, 1995 at Timmins, Ontario.
Meikle
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APPENDIX A
T
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IPR-12 Time Domain Induced Polarization/Resistivity Receiver
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Brief Description
The IPR-12 Time Domain IP/Resistivity Receiver is principally used in exploration for precious and base metal mineral deposits. In addition, it is used in geoelec- trical surveying for groundwater or geothermal resources, often to great depths. For these latter targets, the induced polarization measurements may be as useful as the high accuracy resistivi ty results since it often happens that geo logical materials have IP contrasts when resistivity differences are absent.
Due to its integrated, lightweight, micropro cessor based design and its large, 16 line display screen, the IPR-12 is a remarkably powerful, yet easy to use instrument. A wide variety of alphanumeric and graphical information can be viewed by the operator during and after the taking of readings. Signals from up to eight potential dipoles can be measured simultaneously and recorded in solid-state memory along with automatically calculated parameters. Later, data can be output to a printer or a PC (direct or via modern) for processing into profiles and maps.
The IPR-12 is compatible with Scintrex IPC and TSQ Transmitters, or others which output square waves with equal on and off periods and polarity changes each half cycle. The IPR-12 measures the pri mary voltage (Vp), self potential (SP) and time domain induced polarization (Mi) characteristics of the received waveform. Resistivity, statistical and Cole-Cole parameters are calculated and recorded in memory with the measured data and time.
Scintrex has been active in induced polar ization research, development, manufac turing, consulting and surveying for over thirty years. We offer a full range of instru mentation, accessories and training.
r
r
The IPR-12 Receiver measures spectral IP signals from eight dipoles simultaneously then records measured and calculated parameters in memory.
Benefits
Speed Up Surveys
The IPR-12 saves you time and money in carrying out field surveys. Its capacity to measure up to eight dipoles simultaneous ly is far more efficient than older receivers measuring a single dipole. This advantage is particularly valuable in drillhole logging where electrode movement time is mini mal. . -
The built-in, solid-state memory records all information associated with a reading, dis pensing with the need for any hand written notes. PC compatibility means rapid elec tronic transfer of data from the receiver to a computer for rapid data processing.
Taking a reading is simple and fast. Only a few keystrokes are virtually needed
since the IPR-12 features automatic circuitresistance checks, SP buckout and gainsetting.
High Quality Data
. One of the most important features of the IPR-12 in permitting high quality data to be acquired, is the large display screen which allows the operator easy real time access to graphic and alphanumeric displays of instrument status and measured data. The IPR-12 ensures that the operator obtains accurate data from field work.
The number and relative widths of the IP decay curve windows have been carefully chosen to yield the transient information required for proper interpretation of spec tral IP data. Timings are selectable to per mit a very wide range of responses to be measured.
rl APPENDIX B
r r
r r rr r
IPC-9/200U
INDUCED POLARIZATION AND D.C. RESISTIVITY TRANSMITTER
2.0 SPECIFICATIONS
Maximum Output Power
Output Voltage
Output Current
Meter Ranges
Automatic Cycle Timing
Automatic Polarity Change
Pulse Durations
Period Time Stability and Accuracy
Open Loop Protection
Synchronization Output
Internal Power Sources
External Power Sources
200W defined as when current is on and into a resistive load.
Switch selectable at nominal settings of IS, 150, 210, 300, 425, 600 or 850 V.
1.5 A maximum.
Switch selectable at 50 mA, 150 mA, 500 mA, 1500 mA full scale with accuracy of 3X of full scale.
T:T:T:T; on:off:on:off.
Each 2T.
T is switch selectable at l, 2, 4, 8, 16 or 32 seconds.
Crystal controlled to better than 0.002 percent of the selected pulse duration.
High voltage is automatically turned off if the output power is less than 2 W. This can be overridden manually for testing purposes. This protection is not effective at the 15 V output.
Optically isolated, suitable for external synchronization of the lPR-1l multichannel IP Receiver.
Two battery packs are standard, each containing 4 GC 660-1 lead-acid gel-type batteries giving 24 V at 12 Ah.
One Penlite battery, Eveready E91 or equivalent.
24 V DC supply at maximum 10A.
2 -
APPENDIX C
l iiiji ii ! ! iiiiiijjjii^It:::::::::!:: ::M::I:IS:!!:II|! •.ilill iTitits^tii^nittti^itiiiitfiti^irniiiiii^tiitiiiljirilN-iHiHIiiHttiiiitmill\lKl I : Hi Hjf! l:!i!!i Hiiti I!j!lli[!i!!:i!!!Hi:m!ii:ili :}ii ! : :ii i !i
APPENDIX D
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PiKMiiI?^^iilllSil^^i?lill^f''ilil
Five frequencies: 222, 444, SSB, 1777 and 3555 Hz.
Maximum coupled C horizontal-loop 3 operation with reference cable.
Minimum coupled operation with reference cable.
Vertical-loop operation without reference cable.
Coil separations: S5, SO, 1OO , ISO , SOO and 25Om Cwith cable 3 or 100,200,300,400, BOO and BOO ft.
Reliable data from depths of up to ISO m C BOO ft 3.
Built-in voice communication circuitry with cable.
Tilt meters to control coil orientation.
^IPlii^
APPENDIX E.
r r r r r r
VLh (PLANE WAVE) EM INSTRUMENTS
VLF EM
EMI6One ol the most popular and widely used electromagnetic instruments, the EM16 VLF receiver makes Ihe ideal reconnaissance EM. This can be atlributed to its field reliability, operational simplicity, compactness and mutual compatibility with other reconnaissance instruments such as portable magnetometers and radiometric detec tors.
The VLF method of EM surveying, pioneered by Geonics, has proven to be a simple economical means of mapping geological structure and fault tracing. The applications are many and varied, ranging from direct detection of massive sulphide conductors lo the indirect detection ol precious metals and radioactive deposits.
FEATURES• The EM16 is the only VLF instrument that measures the quad phase as well as
the in phase secondary lield. This has the advantage ol providing an additional piece of data for a more comprehensive interpretation and also allows a more accurate determination ol the lilt angle.
• The secondary fields are measured as a ratio to the primary lield making Ihe measurement independent of absolute lield strength.
• The EM16 is the only VLF receiver that can be adapted to measure VLF resistivity.
SpecificationsMEASURED QUANTITY In phase and quad phase components ol vertical mag
netic field as a percentage ol horizontal primary field, (i.e. tangent of Ihe tilt angle and ellipticity)
SENSITIVITY I n phase :1150'/. Quad phase: i 407.
RESOLUTION 1V(
OUTPUT Nulling by audio tone. In phase indication from mechan ical inclinometer and quad phase Irom a graduated dial.
OPERATING FREQUENCY 15 25 kHz VLF Radio Band. Station selection done by means of plug-In units.
OPERATOR CONTROLS On/Off switch, battery test push button, station selector switch, audio volume control, quadrature dial, inclino meter.
POWER SUPPLY
DIMENSIONS WEIGHT
6 disposable 'AA' cells 42 x 14 x 9 cm Instrument: 1.6 kg Shipping : 5.5 kg
VLF RESISTIVITY METER
EMI6/I6RThe EM16R is a simple, button on attachment to the EM16 converting it to a direct reading terrain resistivity meter. The EM16R interfaces a pair of poten tial electrodes to the EM16 enabling the measurement of the ratio of, and the phase angle between, the horizontal electric and magnetic fields of the plane wave propagated by distant VLF radio transmitters.
The EMI6R is direct reading in ohm meters ol apparent ground resistivity. II the phase angle is 45', the resistivity reading is the true value and the earth is uniform to the depth of exploration (i.e. a skin depth). Any departure from 45" ol phase in dicates a layered earth. Two layer interpretation curves are supplied with each in strument to permit an interpretation based on a two layer earth model
This highly portable resistivity meter makes an ideal tool for quick geological map ping and has been used successfully for a variety ol applications
• Detection of massive and disseminated sulphide deposits• Overburden conductivity and thickness measurements• Pefmalrost mapping• Detection and delineation ol industrial mineral deposits• Aquifer mapping
Specifications EM16R ATTACHMENT
MEASURED QUANTITY
RESISTIVITY RANGES
PHASE RANGE
RESOLUTION
OUTPUT
OPERATING FREQUENCY
INTERPROBE SPACING
PROBE INPUT IMPEDANCE DIMENSIONS
WEIGHT
• Apparent Resistivity ol Ihe ground in ohm meters• Phase angle between E x and Hy in degrees
• 10- 300 onm meters• 100 - 3000 ohm meters• 1000 - 30000 ohm metersO 90 degrees• Resistivity. ±2"/. full scale•Phase . ±0.5"Null by audio (one. Resistivity and phase angle read from graduated dials.15-25 kHz VLF Radio Band. Station selection by means ol rotary switch.10 meters100 MO in parallel with 0.5 picofarads19 x 11.5 x 10 cm.(attached to side olEMI 6)1.5 kg (including probes and cable)
r r r r r r r r
APPENDIX F
FORPRO RESOURCES LTD. 7052352474P. 01
FORPRO *MtetagExploratkwAFomtry
RESOURCES LTD.
'909 Government RoadP.O. Box 1513
South Porcupine, Ontario. . PON 1HO
PHONE: (70S) 239*2474
Oat* 30
Invoice 5 98
sr.i/* A/ c. ov ve /L A- c . . L/^g *^ X V
DESCRIPTION AMOUNT
s*/ rf. 7- r/*
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/O.0 0
OST *R1 01 849669
APPENDIX G
RAYAN EXPLORATION LTD,676 MURRAY STREETTIMMINS, ONTARIO
P4N 7B2 TEL (705) 268-4866
28 Feb.,1995 Job # R236 Inv.# R236-3
In Account With: KRL Resources Ltd.1022 - 470 Granville St.,Vancouver, B.C.V6C 1V5
Attention: Mr. S. Young
Invoice re: Geophysical Surveys "Shining Tree Project'
At A Rate Of:
F i lo option;
Final billing
HELM Survey - 5km @ $l60.00/km VLF Survey - l.5km @ 380.00/kin'
Perkins option:
= S 800.00 = 3 120.00
HELM survey - 5km @ SlSO.OO/km' * S 800.00 Magnetometer Survey - 20km @ 380.00/km^ 31600.00 I.P. Survey - 8 days @ 31250.00/day = 310000.00
- l day @ 3900.00/day = 3 900.00
Cook option:
Magnetometer Survey - 2.5km @ 580.00/km^ S 200.00 I.P. Survey - 2 days @ 31250.00/day = 3 2500.00
Q'Bradovich option:
I.P. Survey - 13 days @ 31250.00/day = 316250.00 - l day @ 3900.00/day = 3 900.00
Report and plotting = 3 500.00;
Subtotal.... . . . . . . . . . . . . . . . . . . . . . . . . . . = $34570.00GST 74...... . . . . . . . . . . . . . . . . . . . . . . .... ~ S 2419.90
Total................................. = $36989.90Less advance.......................... = S 19260.00
Balance Owing......................... = $17729.90
GST # R116488156
Yours truly,
R.J. Meikle
APPENDIX H
CONDUCTOR AXIS
-- 2
CROSSOVER * TO - WEST TO EAST
ALL READINGS TAKEN FACING EAST
KLR PESOUPCES CORP.Propart.u; F l LO PROSPECT QRID-B
.s PROFILED VLF-EM ANNAPOLIS NSS 21.4 KVA
Ministry of
Ontario
Report of Work Conducted After Recording Claim
Mining ActOft aflat tom to oMejntd under tfw u0iori*y of ttio *
ettouU to detected lo the PiovlncW UeMQef, MMnQ Lends, If r. Ontario. P3E 6AS. Haphoin (706) 670-72M.
^PUNEDOST2-15936BERNHARDT
i type or print and submit hi dupecata. w Mining Act and Regulations for P
Recorder.- A separate copy of this form must be compMsd for each Work Group.- Technical reports and maps must accompany this form hi dupicats.- A sketch.
900
(Check One Work Group Only)
Total Assessment Work Claimed on the Attached Statement of CostsNote: The Minister may reject for assessment work credtt aN or part of the assessment work submitted if the recorded
holder cannot verify expenditures daimed in the statement of costs within 30 days of a request for verification.
and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Nun* i
(attach a schedule H mcMssry)
^^AflAIM^hMAIj&M ftf ftaai JjfTJai iMft^vM^t * ^~.—. U^iA^ ^*— 4 ^^-^ •^u^^a^k^ueiuiicauuii or BenencMi imeieai see note NO. i on reverse
l certify that at ttw lreport were recorded in tie current holder's r or held unotoabenefcW
Dale WCertification of Work Report
l cattily that l have a personal knootedfje of the facto set forth in this Work report, rieving performed the wortt or i*tti Ma completion and annexed report is true.
O241 (OM91)
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IBCredits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (^) one of the following:
1. D Credits are to be cut back starting with the claim listed last, working backwards.2. D Credits are to be cut back equally over all claims contained in this report of work.3. D Credits are to be cut back as priorized on the attached appendix.
In the event that you have not specified your choice of priority, option one will be implemented.
Note 1: Examples of beneficial Interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.
Note 2: If work has been performed on patented or leased land, please complete the following: //\ \
l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.
Signature Date
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Les credits que vous reclamez dans le present rapport peuvent etre reduits. Afin de diminuer les consequences defavorables de telles reductions, veuillez indiquer I'ordre dans lequel vous desirez au'elles soient appliquees a vos claims. Veuillez cocher ( ^) I 'une des op tions suivantes :1. D Les credits doivent etre reduits en commencant par le demier claim sur la liste.2. D Les credits doivent etre reduits egalement entre tous les claims figurant dans le present rapport.3. D Les credits doivent etre reduits selon I'ordre donne en annexe. Si vous n'avez pas choisi d'option, la premiere sera appliquee.
Note 1 : Examples d'lnterets beneflclaires : cessions non enreglstrees, ententes sur des options, protocoles d'entente, etc. relatif aux claims.
Note 2: SI des travaux ont ete executes sur un terrain falsant I'objet de lettres patentes ou d'un bail, veuillez rempllr ce qui suit:
Je certifie que le titulaire enregistrd possedait un inl6ret b6neficiaire sur le terrain faisant I'objet de lettres patentes ou d'un bail, au moment ou les travaux ont et6 executes.
Signature Date
Vti Si is•5^S S
2. a
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itm S
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^
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Valeur des travaux d'evaluation
executes sur ce claim
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NO
-AN?; C;-;;
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Les credits qua vous reclamez dans le present rapport peuvent etre reduits. Afin de diminuer les consequences defavorables de telles reductions, veuillez indiquer I'ordre dans lequel vous desirez au'elles soient appliquees a vos claims. Veuillez cocher (**) I'une des op tions suivantes :
1 . D Les credits doivent etre reduits en commencant par le dernier claim sur la liste.2. d Les credits doivent etre reduits egalement entre tous les claims figurant dans le present rapport.3. CD Les credits doivent etre reduits selon I'ordre donn6 en annexe. Si vous n'avez pas choisi d'option, la premiere sera appliquee.
Note 1 : Examples d'lnterets beneflclaires : cessions non enreglstrees, ententes sur des options, protocoles d'entente, etc. relatlfs aux claims.
Note 2: SI des travaux ont ete executes sur un terrain falsant I'objet de lettres patentee ou d'un bail, veuillez remplir ce qul suit:
l Je certifie que le titulaire enregistre possedait un interSt ben6ficiaire sur le l Signature ' [ Date l
Ontario
Ministry ofNorthern Development
fend Mines
Minister* du Devetoppement du Nord et dee mines
Statement of Costs for Assessment Credit
Iztat des coOts aux fins du credit devaluation
Mining Act/Lol sur les mines
Transaction No./N" de transaction
2*1593 6Personal Information collected on this form is obtained under the authority of the Mining Act. This Information will be used to maintain a record and ongoing status of the mining daim(8). Questions about this collection should be directed to the Provincial Manager. Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 8A5, telephone (705) 670-7264.
Les renseignements personnels contenus dans la presents formula sont recueillis en vertu de la Loi sur les mines et serviront i tenir a jour un registre des concessions minieres. Adresser toute queslton sur la collece de ces renseignements au chef provincial des terrains miniers, ministers du Developpement du Nord et des Mines, 159, rue Cedar, 4* etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.
1. Direct Costs/Couts directs
Type
WagesSeJaJres
Contractor's and Consultant'sFAAA Drortsd* (•entrepreneur et os I'expert-— — ——— isvOflVVti
SuppHesUesd Foumtturas utillsees
Equipment Rental Location de materiel
Description
Labour Main-d'oeuvreField Supervision Supervision sur to terrain
Typ* j Gd?"yt,(.A b
fu^/kjrCHZ.
^'faisJfffreType
Type
Amount Morrtant
1W?
/J^J "
Total Direct Costs Total des couts directs
Totals Total global
&1&
&KS
2. Indirect Costs/Couts Indlrects* * Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les coOts Indirects ne sont pas admlsslbtes en tarn quo travaux d'evaluation.
Type
Transportation Transport
Food and Lodging Nourrlture et hebergementMobilization and Demobilization Mobilisation et demobilisation
DescriptionTyp*
,; ^F^nt *- -- C i \}
,: ,^F'K j
i^Iiiii^UN^
Amount Montan!
'C 6 ~"
1~*J
|W4,vcn :'
Sub Total of Indirect Cosls Total partlel des coOts Indirects
Amount Allowable (not greater than 20M of Direct Costs) Montant admissible (n'excedant pas 20 H des couts directs)Total Value of Assessment Credit Valeur totale du credit (Total of Direct and ANowsM* d'evaluation Indirect eetU) (Total dM eaOts draete
Totals Total global
te?tf
Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.
Note : Le titulaire enregistre sera tenu de verifier les depenses demandeas dans le present etat des couts dans les 30 jours suivant une demands a cet effet. Si la verification n'est pas effectuee, te ministre peut rejeter tout ou une partie des travaux d'evaluation presentes.
Rllng Discounts
1. Work filed within two years of completion is claimed at 10007o of the above Total Value of Assessment Credit.
Remises pour depot
1. Les travaux deposes dans les deux ans suivant leur achievement sont rembourses d 100 o/b de la valeur totale susmentionnee du credit devaluation.
2. Work filed three, four or five years after completion is claimed at SOo/o of the above Total Value of Assessment Credit. See calculations below:
Total Value of Assessment Credit Total Assessment Claimed
x 0.50
2. Les travaux deposes trois, quatre ou cinq ans apres leur achievement sont rembourses d 50 o/fc de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous.
Valeur totale du credit d'evaluation
x 0,50Evaluation totale demandee
Certification Verifying Statement of Costs
l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.
that as . K.(Recorded Holder. Agent, Position in Company)
to make this certification
Attestation de I'etat des couts
J'atteste par la presents :que les montants indiques sont le plus exact possible et que ces depenses ont ete engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.
am authorized Et qu'a titre de je suis autoris6(titulaire enregistre, representant, poste occupe dans la compagme)
faire cette attestation.
Signature
0212(04/91) Nota : Dans cette formula—v. f, lorslfu'il desii
Data
designe des personnes, le masculin est utilise au sens neutre.
ASSESSMENT WORK CREDIT FORM
FILE NUMBER: 2.15936
TRANSACTION NUMBER: W. 9580. 00147
DATE: APRIL 27, 1995
Claim Number Value of Work Performed on this Claim
L. 12008251131942/1131941/1131940 x1145897''1146533/1185723X12025621200167^1185697 71185616X1204267120426512042661131050^1134040 "1134042 -'1134041^1133932^1134039"1134043^-1133933^1133936^1133935^1193304 x1134045""1134046^1133937^1133938^341433^
1131076 '1131077 71131056/1131057 ^
0189025202520630
12601890
0504076041260
000
15351537156210371037687687
10071037837
307015351535153515353598270525934871
50,985
OntarioMinistry ofNorthern Developmentand Mines
Ministere duDeveloppement du Nord et des Mines
May 02 , 1995
Geoscience Approvals Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5
Telephone: (705) 670-5853 Fax: (705) 670-5863
Our File: 2.15936 Transaction #: W9580.00147
Mining RecorderMinistry of Northern Development St Mines4 Government Road EastKirkland Lake, OntarioP2N 1A2
Dear Sir:
Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMSL. 113 1942 BT AL IN NATAL, KNIGHT AND MACMURCHY TOWNSHIPS
Assessment work credits have been approved as outlined on the attached Assessment Work Credit form. The total credit approved has not changed from the original submission, however, the credits now reflect more accurately where the work was performed.
The credits have been approved under Section 14, Geophysics, Mining Act Regulations.
The approval date is April 27, 1995.
If you have any questions regarding this correspondence, please contact Lucille Jerome at (705) 670-5855.
ORIGINAL SIGNED BY:
Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division
\ LJ/jlEnclosure:
cc: Resident Geologist Cobalt, Ontario
ssessment Files Library Sudbury, Ontario
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NOTES
400' surface rights reservation along the shores of all lakes and rivers
Port of township closed to slaking effective May 8. 1978, Section 38 (f) of the Mlnlnq Act
SIIHI-ACI- AND MINING Klbins ON CHO WUIN THh loWNSHIh WITMUKAWIJ
PROSPtCTING', STAMUG OU I, bAl.fc ON l.rASh SECTION 3U r*b.O. I9BO, T l Ir MINING Ac l
AT 1:4? P.M.
•••PAHT O f OHUi-H NHW K/& ' Kf u(-| (if L' HY UHDEH O MLOI 90 MtH r^-r^TlVf AtJ KH AT ?:OO AM t-^T
l HE INFORMATION THAT APPEARS ON THIS MAP HAS F1FEN COMPILED FROM VARIOUS SOURCES AND ACCURACY IS NOT GUARANTEED THOSE WISHING TO STAKE WIN ING CLAIMS SHOULD CON SUIT WITH THF MINING MfcCORDER, MINISTRY OF NORTHERN DEVE1OP WENT AND MINES, FOH AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEHEON
Geology Reference- COBALTRESIDENT GEOLOGIST
MOND TP.
RAYMOND TP M. 244
I20I235 II93300
T I09498c|i \ s. i 1 **' 31"; io94'
UXl^ l^—~r^v-i—
MACMURCHY TP
LEGENDHIGHWAY AND ROUTE No OTHfcR ROADS
TRAILS SURVEYED LINES
TOWNSHIPS. BASELINES ETCLOTS, MINING CLAIMS, PARCELS ETC
UNSURVEYED LINESLOT LINESPARCEL BOUNDARYMINING CLAIMS ETC
RAILWAY AND RIGHT OF WAY UTILITY LINES
NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OH COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT
n i ]
DISPOSITION OF CROWN LANDS
TYPE OF DOCUMENT
PATENT. SURFACE ft, MINING RIGHTS
" .SURFACE RIGHTS ONLY .... MINING RIGHTS ONLY ...^..
LEASE, SURFACE ft MINING RIGHTS.-. SURFACE RIGHTS ONLY ,. .
" .MINING RIGHTSONLY ....., LICENCE OF OCCUPATION ORDER IN COUNCIL
RESERVATION .
CANCEi.LbU —........... . .....^..
SAND
SYMBOL
e e
ByT
oc
SCALE 1 INCH -40 CHAINS
i- M in i oon 4OOO 60OO 8000
O JOG METHtS
1000l l KM)
200013 KM)
TOWNSHIP
NATALMAX l *' mi .
MN R ADMINISTRATIVE DISTRICT
TIMMINS : 'MINING DIVISION
LARDER LAKE 2 .159,3LAND TITLES/ REGISTRY DIVISION
SUDBURY
6
Ministry ofNaturalResources
Ministry ofNorthern Developmentand Mines
Ontario
Oat* SEPT 1973Number
G-998
l41P11NE008VTlSMBbERNHARDT 210
y. ..
C/l C/1 CD
•-Q
H
o
J'"& 1
-... '
NOTES
4001 lurfoct right* fMtrva,tlon along the *hor*t of oil laku and rlvtrt.
Township closed to staking effective May 8, 1978, St c 38 If) of The Mining Act
on ill Crown Und l* tttt twnihlp ig out, ul* or M. Ordsr NMI
2i06as,
hv ordir
Mninifi*
A M.O. WU
. i W rt 7'^ " E- B- 1
i (HftMrwi frfc stiking stcUon 3i \m. Or4tr IK2-19 lit ttftctivi |.|,U.
AND MIMNO MOHTB WITHDRAWN PROM PROSPCCTING.'ftTAKMt, SALE OR LEAK. SECTION 98 Of THE MWNO ACT R8O OSO ORDfKVu-TI/M NWT " EFFECTIVE MAY *TlM 4t4E PM
\
THB INFORMATION THAT , APPEARS ON THIS MAP
L H AS BEEN COMPIIKD ' FROM VARIOUS SOURCES,
AND ACCURACY IS NOT GUARANTEED THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON
"THIS MAP SHOW8 THE APPROXIMATE LOCATION OF THE BOUNDARIES OF THE AREA WHICH 18 THE SUBJECT OF CURRENT LITIGATION. THE EXACT LOCATION WILL BE SHOWN FOLLOWING CONFIRMATION BY THE PARTIES TO THE ACTION,
geology reference-COBALTRAYMOND TP M. 244
RhSlDBNT nLEGEND
HIGHWAY AND ROUU No
OTHER ROADS
t RAILS
SURVEYiD LINtSTOWNSHIPS BASt LINES ETC LOTS MINING CLAIMS PARCELS, ETC
UNSURVtYED llNES LOT UNCS PARCEL BOUNDAHY MINING CLAIMS FTC
RAILWAY AND RISH! O^ WAY
UTILITY LINEb
NON PERENNIAL STKEAM
^LOODING OR FLOODING RIGHTS
SUBDIVISION
3RIGINAI SHOHEUNt
IjAHSH OR MUSKEG
INF S
it.
*.
DISPOSITION OF CROWN LANDS
TYPE Of DOCUMENT
PATENT SURFACE 4 MINING RIGHTS
SURFACE RIGHTS ONi.Y
MINING RIGHTS ONLY
SURFACE 4 MINING RIGHTS
SURFACE RIGHTS ONLY
MINING RK.HTS ONLY
LICENCE OF OCCUPATION
CROWN l AND -ALE
OHDFR-IN-COUNCIL
RESEHVATiuN
CANCELLED
SAND A GRAVEL
SYMBOL
0
e9mB BT cs oc
o
SCALE 1 INCH 40 CHAINSO MX 'tWO t 00 •000
O "j6ft 400 *'-T 100 l "M
Ai RES HECTARES
40
TOWNSHIP
KNIGHT
\
*M i 7* M eh 10*64 8T
COPY OF THIS MYl AR AHCHIVCD JUNE 16/92
TYRRELL TP M. 253
DISTRICT
TIMISKAMING-MINING DIVISION
LARDER LAJ(E
i i
lut
Ministry of Natural Resources
Ontario Surveys and Mapping Branch"bauT' " " T,,,, " l PlmTNo" ~
ft "il t , BIO "••n i ''j " T o onto M. 228
4lP11Nt0067 2 16836 BtRNHARDT 220
KNIGHT T OWNS PH P
1777 H: \\.
\*tf*
^
\tf O O
TOO ^\*
so
^\) ^ ^fr*- f. "*
41P11NEOO&7 2 1S936 BERNHARDT 230
** 20r~ BT ——— I
QUADRATURE
IB 20 -xl
IN-PHA8E
QUADRATURE— — —
HLEM LEGEND
INSTRUMENT: APEX - MAXMIN 11 MODE MAXIMUM COUPLET! CO-PLANAR
READING INTERVAL :25 M
COIL SEPERATIDN 100 M
FREQUENCY. 177? AND 444 H,
PROFILE SCALE- leu- 10*
CONDUCTORS
QQOO
MED
POOR
TOPO LEGEND
D Claim Po*i A**um*d
CI 41 m Llni
1593 6APR 3 J995
Cll.nt: KRL RESOURCES CORP.Property F I LO PROSPECT - NORTH GRID B
Titl. HORIZONTAL LOOP
SURVEYProcmmmmd :
RJM
OaiiJAN. 1995
ProvtnciONT.
Seel*1:5.
Ch.ck.d.RJM
TownshipKNIGHT
NTS.
Draw l no444-177?
MAYANEXPLORATION LTD
OBOPHYBCt TIMMINS. ONTARIO
(7061-266-4866
>
M9 CHO.Nil Ni2Ni3Ni4
3.2 4.2 4.3-bl b-l
3 -*--'3.^.%(
2 4.B 4.411^ 9.5 t*.3.1
H.9 CHO. Nil
Ni3
Ni4
RESISTIVE
RESISTIVITYNil 327-0
Ni2 50!
Ni3 604-0582.0
Ni4 845.078
• 051B.O
2.IK
RESISTIVITY NU N.2 Ni3 Nt4
(?V4 ( of .25^ .liftM9 CHO.
Nil
Ni2
Ni3
Nt4
.9 .1 .3 , .0 -4
.2 ^J_ -^ti 0 - 9 l.| .B
ne CHO..1 -.1 .1 -.3 -.3 -.5 -.t ..e 1.7 Z. 8 t.fl Nit
-.4 1.0 -.9 -.B -.S --7 -2.|N.4 At2 3.0 Hit
l.3 \-.fl -B -B -1.4.2 .a"———— - 0 ^ -
.b
. -. -. .. . .
-.S --7 -2.|N.4 At2^ .t /^8~^~.r-T*.'V. -B
Ni4
SIONA1 OUT TO CGNDLCTIVE
UAKE BOTTOM SEDIMENTS
RESISTIVITY
100* , 7^H , 5(JM t 2 5,M t Of .
139.0 100. 0^84.0BBJLJi5
, IOpE . 125E
RESISTIVITY 0 212 .0 238 .0 Nil
97 1 - o soo . oNi3
M9 CHO-Nil
Ni2
Hi3
NI4
ojxurrtvc
RtSISTlVlTYNil
Ni2
Ni3
Ni4
2.3K S.6K
ISfE , 1
RESISTIVITY 277.0441.0 Nil
MK444.0 Ni2
02.0 Ni3
O Ni4
,IOpN t 7^H f 50f50H
M9 CHO.Nil
Ni?
Ni4
\-f.-i b , 8 . 7.1 . 10.2M9 CHO.
NHNi2
Ni3
a 7.9 12.2 Ni4
^2|H ^ Of
RESISTIVITY
>
^1593 6RECEIVED
APR 3 1995
MINING LANDS BRANCH
KRI RESOURCES CHRP
SUE: vi-Y
ELHJK GRID
MAC:MLJRLIIY TWP.SHINING l REE AREA
RE ATE l OF' l l:2500
M9 CHO.Nil 7.2
M9 CMC
Ni2
Ni4
"timi.o i .h/Mr A/zA. y
Ni3
Ni4
KtblSIIVIIYNil
Ni2
Ni3
NU
RESISTIVITYS.flH .9.9K 2B.3K I3.2K 11 .9H I2.7K ^TjJ^ 7.7N Nil
10.6H 4.Mtl.BK 13.SK IS.OK 12.IK I3.7K 19.SK Ni2
3 - bKN* . •CjJ'llt—*-l* 14.2K 13.BK 17.OK 24.2K Ni3
S.5K 3\inB-3K l/T^XflNw 11.6K 16.1K ?T.5K Ni4
INt 100 S
INDUCED POLRRIZflTION SURVEY
DIPOLE-DIPOLt BRRRY
N - 1. 2. 3. 4. ... •R* 8PHCINO - 25.0 HETHE8
BKEIVtR, KINTCX IPN-IZ TlHf OOHAIN
RX'TX TIMIND: 2*** ON 2*M OFF PLOTTID M1NOOH BLICCi *f
BCIH11VX IPC-B M* WATT
KRL RESOURCES CORP.
COOK GRID MflCMURCMY THP.
J.SCRLE r l : 2500
OflTE : JRN. 1995 KEF i L1S
RRYRN EXPLORflTION LTD
LINE : 200 S
INUUC1 U rUl.nKI7flXJ SURVEY
DIPOLE-DIPOLE flRRHY*
S* i*L\ r
ttmn mvt N r 1. t. 3. 4. . --
•H* 8PRCIMO s 25. O METRES
9CINTEX l W* l? TIME DOMAIN
RX-TX TIH1NB Zaw ON ZMC OFFPLOTTED M1NDOM S. ICC rt
TKM4BHITTER 9C1NTHEX IPC 8 2BB MAU
KRL RESOURCES CORP.
COOK GRID MRCnURCHY TNP.
DflTE J JflN. 1995 RFF : L2S
SCRLE - l : 2500
RflYflN EXPLORflTION LTD
LINE 300 S
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE HRRflY
M rCIHTN ; 1. 2. S. 4. .-.
•A* BfWCINO , tt.O H ETKEB
RBCCIVDti BCINTCX IPN-IS Tit* O*VMN
RX TV T1MIM1 ?..c, ON ZMC OFF
tCIMIMW IK-B BM MATT
KRL RESOURCES CORP.
COOK GRID MflCMURCHY TWP.
DflTF : JflN. 199S REF : L3S
SCflLE - l : 2500
RflYRN EXPLORflTION LTD.
l I NE : 400 S
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE RRRRY
N - l . 2. 3. 4. ... "fl- SPRCINO - 25.0 HETRE8
NKCXIVOli BCINTCX im-12 TINE DOMAIN
RX-TX TIMIND. ZM. ON 2w OFF PUTTTED MINDDM SLICE *B
TNAMMITTEM. 9CINTfKX l PC-8 2W MATT
KRL RESOURCES CORP
COOK GRID MflCMURCMY TWP.
ORTE i JflN. 1 995 j
SCfll F - l :
RflYRN LX
L INE : 500 ( ]
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLF RRRflT
N ; l. 2. 3. 4. . .. •A' 6PRCINO ^ 25.0 METRES
NECEIVCM BCINTEX 1PR-12 TIME DOMAIN
MX-TX TIMIND. ZM* GN 2~* OFF PLOTTED WINDOW *.tCt *t
BCINTIVX IPC-I M* MATT
KRL RESOURCES CORP.
COOK GRID MflCMURCHY TWP.
DHTE : JHN. 1995 KEF : L5S
SCflLE - l j__2500
RRYflN EXP1 ORflTION l TD
240
41P1fNeQ06T a 16B3B BERRHARDT 250
-?c
00
'O
<
ERASER Ell If.RED I.R. CHARGEABILITY
-r,
FRASER FILTERLD l RESISTIVITY
*i
LEGEND
DATA: FRASER FILTERED CHARGEABl L lTY/RESl ST l V lTY
SOURCE: I .R. DIPOLE-DIPOLE SURVEY
"A* SPACING- 25M
N - l -4
TIME DOMAIN
CONTOUR INTERVAL - 2 MILLISECONDS (CHO)
200 IK 5K l OK l SK ?OK (RbSlbllVITY)
FILTER METHOD: FRASER. 'B'. TRIANGLE
aa*
Cll.nt. RESOURCES CORP.
Proparty COOK PROSPECT
FRASFR FILTERED
CHARGEAB L lTY RFS ST l V l TYPracmmmmd
RJM
OoLiFEB 1995
Pr-ov l nciON!
Sea 11l 5.000
ChackedKJM
Town*hl pMACMUKCHY
NTS4IP/NW
Dr-eiw t ny r r C
MAYANEXPl ORA'l ION LIDCON l MAC! /CONRJl 1MJ UtOH fYSICS
TIMMINS. ONTARIO
(70S l 268-4HBB
119 C MR.Nil
Ni2
N"3
N:4
14^5M | 140,OM [137( SH t138) OH Z^SH tt zgon ,n pn i yii n yn .11 goN ti OT^N t i o^on .logan ,t oj .85pn ,B25n ,80pn 725H TOOH ajpn espn eesn BOOM .57pn .sspn .
3.3 y4.2 5-1
5.4\ 7.lXl
IO/SS A hr
-.9 OJI 8-1 VB.7 ,9.0,
*19PH
119 CHO. NilNi2
B.B Ni3
.6 Nt4
RESISTIVE
RESISTIVITY
975H . 9SpN , 925M117,5* l 15,DN L 1ZJ5M li
Nil 885.0 V2,.1K 2.5(^.0, /-2
, 525N
Ni4
/X3PN.5^*^Ki^k. 4N
18.SK I2.7K 17.3K 22-SK 36.BK
IK 20.BK 23.OK 1B-5K 31-
.SK\0\2K 34 -SK 25 -2K 32 -2K
S.oVuB.2K 36.8H 41-6K 10.
RESISTIVITY Nil
Ni2
Ni3
Al/TSIT l .4K Nt4
LINE 300 N
INDUCED POLRRIZRTIONSURV F Y i. 159
DIPOLE-DIPOtE RRRflY
-CL-..J5LMPTN
N s 1. 2. 3. 4. . •IT BfflClNO - 25.0
RECEIVED
APR 2 6 1995
MttMMG LANDS
EtVKR: 8CINTEX IW-12 TIME DOMAIN
RX-TX TIMING 2Mo ON Za.e OFF PUOTTH) MINX* SLICE *9
TWANBHITTOI 8CINTICX 1PC-9 ZM HATT
KRL RESOURCES CORP
PERK INS GRID NATAL - KNIGHT TOWNSHIP
rDRTE : 21/01/95
SCRLE r l :
REF : L3N
2500
RflYRN EXP.
MS CMC.Nil
Ni2
Ni3
Ni4
RESISTIVITYNil
11.4
M ^BZbH (6Dp375H l 350H l 325M13QOM12TSM
. 4 4.3 8JB .5.4 , 2-5 2.6 . 1.46.7 0.4 B.'/ .b. 4 b. 5 B. O
RESISTIVE
M9 CHG, N "
CONDUCTIVE
^
Ni4 18.9K\i.8K
11.SK 22.9K IB.4
.4K 30.2K2B.9K
5K30.BK 33.4K
.IK 20.SK 29.7K
ra a4.IJM.M l.t
LINE : 200 N
INDUCED POI RRIZflTION SUKVf Y
DIPOLE-DIPOLE ARRRY
t . m
N t 1. 2. 3. 4. ... R' Bf BC I NO : 25.0 HETRE8
INTCX im-12 TIIC PDMAIN
KX-TX TlHINOt 2*M ON 2**c GTT PUDTTTO HINDON BL1CC. *9
BCINT1CX irC-9 ZW HATT
KRL RESOURCES CORP.
PERK INS GRID
NATAL - KNIGHT TOWNSHIP
REF : L2N
SCRLE - l : 2500
DflTE : 21/01/95
RRYRN EXP.
>
M9Nil
SU MOON 137.5H 13SOM.iag.5H 130 -.T - l -T ' \f*j-l
12.8 10.^ ^-4 6- 7 6.8^ 5.5 6-9 4.4 4. \ ^ , \*, 5 ^ 4-S 3.4
;.T\ir.^\N6.V f*S?l 4 -G /fe.7 /i.3 5.6 rfjt.2 B^0^\.2 4. *\ 3.4.1
N:4 5.0 7.8 S. B-
RESISTIVE
,147,51*,
RESISTIVITYNil
Ni2 Ni3 N)4
B.7K 16.7K30.OKBB.2K40.8K37.BKfB.
21 -IK I6.4K 28.IK 5B.4K 3B-7K 33.SK
19.OK IB.SK 30.BK 83-BK 48-2K 13.
20.8K 25.SK 32.SK 75.4K 17.BK
135,ON J 2^5*4.1 gqON.UTjStUlSjOH,
n9 CMC-Nil
Ni2
N:3
N:4
8
M g 8.0 '.d 7.4 - i -HIJ2 \6-3 7-''
8.3 f.
7.3 6.9
7.3
.J
S5PU 525H 50PH 475H 4SpH 425M 40QH .375H^^fH^^——*-——f—— 4* ——-\————T -"T" ^*"——f————'————1
M9 CHG.3 .4.8 7.B NH
l Ni2
Ni3
Ni4
RESISTIVE CONDUCTIVE CONDUCTIVE RESISTIVE CONDUCTIVE
^
KtSlhTIVIl YNil
N-.2
N-.3
Ni4
14.BK 14. l K 28. l K 43. OK 23.6K 33
9.OK 17.IK 20.6K 45. IK 26.BK 25.BK
6.VJJ 9\6K24-2K2S.2K24.4K26.4K
11.2K 7.4K13.3K 32-4K I5.4K25.8K
4K
KRL RFSOIMT.S C(JRP
I.R. SURVEY
PERK INS PROSFDECT -
NATAL S KNIGHT TWPS
SHINING TREE AREA
EAST PART
M9 CHO.
^•QfflL42^^?50HBjSNBMH J.75h
Nil
Hit
Nt3
Ni4
16.1 S.IM9 CHG.
Nil
tO. l 12.20.2 9.9
Ni3
N:4
RESISTIVE lm,B75H ,8SpH ,B25N ,60pH t 72SN
RESISriVlTYNU Ni2
Nt3
Nt4
LINE : IDD N
INDUCED POLRRIZRTION SURVEY
DIPOLE-DIPOLE flRRRY '
N s 1. 2. 3. 4. ... SrPClNO - 25.0 METRES
•IVO* 8CINTEX IPR-1Z TIME OQHAIN
RX-TX T1HIND ZMO IX 2*ae OFFPU3TTB3 MINDOM SLICE *8
SCINTHEX IR--B ZBB HAII
KRL RESOURCES CORP
PERK INS GR H)
NATAL - KNIGHT TOWNSHIP
REF : LIN
: 2500
DflTE : 23\Dl\9b
RRYRN EXP.
LINE : O N
INDUCED POLRRIZRTION SURVEY
OIPOLE-DIPOlE RRRflY
N - l. 2. 3. 4. ... •FT SPHCINO - 2 b.D METRES
RECEIVER SCINttX IW-1? TIME OOMAIN
RX-TX TIMING Z..B ON 2mc OFT PLOTTED HINDON SLICE *9
TRANSMITTER SCINTREX IHC-9 ?BB HATT
KRL RESOURCES CORP.
PERK INS GR I [J NATAL - KNIGHT TOWNSHIP
DflTE : JHN. 1995 K it : l ON
SCRLE r. l : 21)00
RRYRN EXPLORRTION LTD.
l (JO ( :
INDUCED POLRRIZH1 ION SURVEY
DIPOLE-DIPOLE flRRflY
N i l . 2. 3. 4. ... R* srnciNO s 25.0 METRES
RECEIVER SCINTEX l PR-IZ TIME ULMAIN
RX-TX TIMING 2**c 01 ;Me cn-PCOTTED M1NDON SLICE. *B
rRANBMMTER STINTREX IPC-9 200 WATT
KRL RESOURCES CORP.
PFRKINS GRID
NATAL - KNIGHT TOWNSHIP
DflTE : JflN. 1995 KEK : l IS
J5CRI L l : 2500
RRYRN LXPI ORRTION l TO.
\ A f r: i OF i
26041P11NF0067 2 16636 BfcHNHARDT
M9 CMC.NH N'2NO
Ni4
RESISTIVITYNil Ni2 Ni3 Ni4
8.8 7.2 9-1 -*^7.
13.9 ^frvl B 8.0 7. B 6.4 6.2 l 13.7 13.6Nl\ R. l 7.7 7.8 6-2 B^fl.
4.6 .6.6 6.3 7.0 , 8 -7 10.1 B.86.7 5^9 *.2 JO* ^?9\ 8-8
3 10 0.1 8.0
28S0^282SH gBqON r27]5H 275,0* ,272) 5N 270,0* 287,5* 285,0* 8^5* |8qOH .257,5* 25^0* 2*^^01* JttfS*JMgM^*H ,?4 VH 1ZS]SH ^-3|?H ,M?5-N 290,0* tg27,5W 225,0* 22^5* 220,0* 217,5* (21 5,0* 21 2,5* f l qOH .207,5*
.8 3.7 3.8 8.0 4.7 4.g. J.3 3.8 3.0 /g/4 3.2/5.1 4-8 4.8 4\ 3-0 *-8 3-t
8.7 . 5-1 4.3. 2.8-9.8
2.33.4
.8.^.2 -9.2 -3.8 -4.5 r3.3
*- 3 4.3/3.2 10 2 -ax- 9 -s. j -5.1 -4 .a4.8 4.2/3.2 3-2 4.0/^2^-2/1 -3\8 -4 -4 /-g . ^T wS
———— RESISTIVE ——
^^
31.2K 16.BK20.4K29-4K 54.8K 10.6K23.1K 13-SK I1.7K31.3K 14-8K20.5K74 SK 23 . 4K 17 .OK 28 .
11 .7K I0.1K 21.5K 13.4K 48-2K 26.5K 31 .9K I6.5K 18. 9K 30- 7K 16-BK 34-OK 28. 2K
465^JJ.522 .0 488^D 560 79^JLfift2^. OJ719 .0
OK +-.IIJB3.0.3K 1.4(407/0413.0
RESISTIVITY 4-4K 3.9K Nil
4.2K Ni2 NiS N)4
L INE : 500 S
INDUCED POLflRIZRTION SURVEY
DIPOLE-DIPOLE RKRflY
N - 1 . 2. 3. 4. ... *fl* 8PWCINO : 25.0 HETRE6
RECElVtR. 9CINTEX IPR-12 TIME DOMAIN
RX-TX TIMIKD 2.*c ON 2..o OFF PUTTTCD MIMXM SLICE *8
9CINTTCX IPC i ZW MATT
KRL RESOURCES CORP.
PERK INS GRID
NATAL KNIGHT TOWNSHIP
TDflTE : 19/01/95 REF : L5S
SCflLE r l: 2500
RRYflN EXP.
M9 CHO.
* r .
NU N)2
N:3
N:4
.5 5.7 3J. 4.4 4-44-8 4.1
-5 8 U .8 87X^4.8 5.4 AJ .8 l. 7/2.6X5 A 7.9\5.fl XS^O \
8^ 3.4 J.7 1.4, 2.8 4.1 4-1 B.t 3^5 .7.8 7.5^ 5.5 5-1
( -.T tUl—T.8 3.0 yt—**fl 3 -V3 l-7/ /fTo^NS.l f.4/ LO 2\0
3.8 J,.,? 4.S 2.5
— CONDUCTIVE CXNXCTIVE RESISTIVE —
RESISTIVITYNil N:2 Ni3 Nl4
p 230-0,482.0 318.OJ7I 05 '12.0
15.055 i.O 80X415
1K7B8. 0^77.0538. 055.0 98j67pTi5 ,0 S v— -*^ — O o O l *
l.gK l. OK .OK l.gK l
RESISTIVITY NUNig
1.7K Ni3 I.IK Ni4
LINE 600 S
INDUCED POLRRIZflTIONSURVFY
DIPOLE-DIPOLE flRKHY
-*—
N s l. 2. 3. 4. ... fl" SPflCINO r 25.0 METRES
HECEIVOt; SC1NTEX IPR-13 TIK DOMAIN
RX-TX TIMING- 2**e CM 2*.e OFF PU3TTBD HINDOH 9LICE *9
aciNncx I PC-S 28t WATT
KRL RESOURCES CORP.
PERK INS GRID
NATAL - KNIGHT TOWNSHIP
DATE : JAN. 1995 REF : L6S
SCRLE r l : 2500RflYflN EXPLORflTION LTD.
M9 CHO.
1^^ OH
NH Ni2 Nt3N:4
6-0 5.8 4.8 5.8 5.8 5.3 B.I 8.8 . 5.1 5.7 4.8 5.3 5.5 5.9
7.5 5V8 4-8 4.9 3^*. 12.4 "Vi 8^Bl 4.7 4.6/ 2.5 2^\ 5.4 5-6
2 5
*v
RESISTIVITYNU Ni2 Ni3 NI4 4.3K
^2^)0.5K ejTK^B^ajL^ .9ITT5.7K /fr^lK 10*^14^91^
.2K f**. B 5.3K—4.8K 7.4K
1B.3K 16 4)llf8KI4.2K 25.2K 10.lA 10.0IO2.6K 17.6K 12-4K
8 5.
3
mgK
3K
12-
5-5 4.5 BJI 6.8
1 S. 5X7 -g B.O
4.7/7.8 7.3
2 /7.0 7.6
4
SM.gO^OH 197,5^,183,0*
4.4K S.2K9-7K S.gK
*K M^*lCjB^3K iTTaK A ^""^ ^
V 7^4*^8 {J 4 0 . 4 K
4K 13. 2K li .OK
M9 CHO. Nil
Nig
Ni3
N:4
- ^" " 1
RESISTIVITYN:l
Ni2
NO
Nl4
LINE : 700 S
INDUCED POLRRIZflTION SURVEY
DIPOLE-DIPOLE flRRflY
DCTTH rtniTN r l. 2. 3. 4. . -.
*fl* SPflClNO - 25.0 MFTRfS
RECEIVER SCINTTtX I PR J? TIME IXJMAIN
RK.TX UHfMi, 2^K OH l**c UT MIMBt BLICf. tt
CINHCX IPC-B Z* WATT
PERK INS GRID
NATAL - KNIGHT TOWNSHIP - . .., ^ . .DHTE : JflN. 1995 REh : L7S
RflYflN EXPLORflTION LTD.
M9 CHO.
g 1 2, 5H f2 1 QDM ZM5H 2050M ,1 8'{5H .1 9SOH1925M1800H
Nil N'2 Ni3Ni4
3.2 3.2 /45.2 3.8 4-1 4-1 4.7 7.7 5.1 4.9 3.2 3.1 3.5 7.3 6.9
.S^^^B 3.^ 5.4 4-3 /.7 7.3\4.8 4 .7 ~~*-l- -4^t^ 5 .O^YTSv 6 .9V4 yfS.S S.8^±A 7 .8(^5)5^ ^ 5.4 Sji 5.9 ^.7^x5/1 9-1
.8 3.7 6-0 5.6/7.0 5.9 6.9 9 .4 4 -2 /fTl 7.4 l 4 V l .9 \ V.2^- 8.3
RESISTIVE
gg^DN ,g 17,3^ 21 i^OM f 1 2,5H 21 qOH 207,^ 20^QH ^D^SM 20(jOH 197,5^ 195fON 132.SM^1 g^OH
9 CHO, Nil Ni2 N'3 Ni4
RESISTIVITY RESISTIVITY9K 9.2K {jr 4-6K
?lK J l-6K
/•/W 14 . t K Ni4
LINE : BOO S
INDUCED POLHRIZflTION SURVEY
DIPOLfL-DIPOl E HRRflY
N - 1 . 2. 3 . 4 . ... •fl" SPflClNO r 25.0 METRES
sciNTcx IPR-JZ TI^ DOMAINRX-TX T1MIMG 2..c ON 2..c OfT PUTTTED N1NQCM SLICE. *9
TRANSMITTER SCINTHEX IPC-9 Ztt WATT
KRL RESOURCES CORP.
PERK INS GRID
NATAL - KNIGHT TOWNSHIPDOTE : JflN. Khf : lflS
bLHLE - l :
N EXPLORflTION LTD
KRL RLSOURCES CORP
I.R. SURVEY
RK INS PROSPECT
NAIAL 8 KNIGHT (WPS
I1NING TREE AREA
ATE ? D I C.. :2b00
M9 CHO.NU Ni2 Ni3 Ni4
RESISTIVITY
N:2 NU Nl4
220| OH |21pH21 OH 21 ^5Nl
SK
4K
RESISTIVITY .5. OK 2.7K 3.9K N:l IK 8.Hr~5^2K N:2
~.8K N:3 17.BK N:4
LINE : 900 5
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE
N r l . 2. 3. 4. 6PHCINO - 25.0
RECEIVER SCINTEX IPR-1?
RECEIVED
APR 2 6 1995MtTRES
MtNIMaMNDS BRANCHRX-TX TIMING 2**c ON ?..t err PUDTTED WINDOW SLICE *aTRANSMITTT3? SCINTWEX IPC-9 200 WATT
KRL RESOURCES CORP .
PF-RKINS GR I [J NAIAI - KNIGHT 1DWNSHIP
DflTE : JHN. 1995 KFh : L9S
sem.f. - i: ?bnoRflYflN EXPLOKHTION LTD-
M9 CHO.2.5 4.1 2.9 2.6 2.5 2
OM
B 3.0 2.5 2.8 8.1 2.2 3.7 5.1 6^4, 4-0 5.8 4.7 4.0 1^8 2 f l yS 2.6\ 5-2\ 2.3 4\D 5-1 5.2 5.8 5.0 4.8 4
*Cl~-XXT^TXS^T^H/ 3 B^ J*l 5' 2 5' 5
- 0 ^\ .2^.0 \4.7X2U? O 5.7 4.6
4.7 3.8 2.8 2.4 2.7 2.4 3.42 2.5 2.4 /4-r9^ 2.6 3.1 1-3
3\2.5 2.7 ('l .5 1.2\ 3.3^/5 .2 5.7\ 2.3 2.3\ 1.8 Ll~ .3 . 31 -.
M9 CHO, Nil
Ni2
N:3
9 N)4
RFSISTIVECODLCTIVE CONPUCTIVt
RESISTIVITYNU
Ni2
Ni3
Nt4
10-4K 23.9K 20.SK 47.4K
13.2K26-1KZ2.1K
13.9K22.2K
10.811
7,* l O 767 ^870.0*58.0 438^0^18 -O 887.0.0751.
l-OMIB7.0 79-MWB4-Oy V l.
• 0. fThCSSvdsOB.O 720X0*4^0
5* aqOM^S* 255rP*^5^5*j25qO* i247^*245tO*^24^8* t240(OM237) S* )235fO*^32r5*^30)0* |22-{5* 22^0*^22,5*22qO* |217( 5*j215) 0* 2^5* 210,0* 207,5* 205,0*202,5*^200,0*
17.0KRESISTIVITY
506.0 836^0 T Tf+Q l -OK
.0631 .06177^ l .4K
276M3 509 JO.6K NO
.0 Ni4
LINE : 100 N
INDUCED POLRRIZRTION SURVEY
DIPOI f- DIPOLE flRRflY
N - 1. 2. J. 4. ... "W SPflCINO s 25.0 M.ETRE8
RECEIVER 9C1NTEX 1PR-12 TIME OOMAIN
RX-TX T (MIND 2..o CM ZMC OTT PIOTTED HINDON SLICE #9
TRANSMITTER SCINTHEX IPC-9 281 WATT
KR RESOURCESj:pRP.
PERK INS GRID
NATAL - KNIGHT TOWNSHIP
nflTE : JHN. 1995 REF i L1NW
SCRLE - J : 2 \^
RRYHN EXPLORRTION LTD.
275,0^272^ 270^ 267,5*265,0* 262,5^26^0* 25PM 255,0^,2^^
M9 CHO.Nil
Ni2
Nt3
Nt4
2.1 4^ _ 4.2 5.4 4.1 3.0 5.4 4.8. 7.3 ^.7 5. t J .I 6-3 5.5 5.5 5.2 3.0 3-5 4-6 4.8 5.4 4.4 4.8 4.4 5.9 2. S 3-4 2.3 2.8 5.0 7.5 6.4 7.9 .4.45.7 4. 2.7 1.3 2.7 2,8 2.6 3.8 2. B 2.2 2.0.S 7. S .B 5,fl 8.2/5-5 4.3 5.2 4 9 S.I 4-1 4-B 4.6 4-7
6.4 7.3 IMl 57*-" S. 4 IxT^xjUl — 4Ui 4.8 4-B 5 . 4 Irf-K 5 . 0 4-4 .4 6.4 7.8 610 4.1-^5^7 /TU /^TBTX 3\ 6-1 5-1 xf^B 2.1 3.V 4.5 6.2
3.^" 4.7
.9/5.5 4.8 3.9 3.3 2.1 /6U. 4.8
8.4 t .l/Z.jf 1 /fc 3.7 1.4 6.1 fi.6 l 1 .6 /2.6 4 .8 3.1/^rrrm 0 ^-N.
119 CHG. H.4 11.9 NU
S.I 8.1) N i Z
N:4
7(^8.3
.Si 7.3
RESISTIVE CONDUCTIVE HT8ISTIVF
RESISTIVITYNil
Ni2
Ni3
Ni4
28^0* ,2B2,8* .280,0* .277,5* .275,0*.272,5*^0* 267,5* .265,0* 26^5* 2^^
*7KRESISTIVITY
3K 4.2K14.9K NU
BIT B.SK Ni2
6-6K Nl3
3K 7.BK M-79K Ni4
2928*2800*28 .272,8
M9 CHO.NU Nt2
Ni3
Ni4
28 25 Hl2BQOW 2575* 255.0*2523*2500* 8475* 245.0* 2425* 24QO* 237.5* 238.0* 1323N 2300* 22 (S* 225.0* .2223* 2200*2178* 218.0* 2125*2100*2075* 2050* 2025* 20QD*D* S Y f * S *S f /* S y S s s 7 s7 'S S S" r f/* . i . i i /*/ s s /*/ y f f y f f*/ s /V s /'7 s S S V s 7 f s f 7~7\ ?
7-3 . 9.5, vajl .7.1 7.0 7.B .4.6. 3.1, S.3. 8..S.7 S.3 2.2 2.0 2.3 5.3 .6 2.5 2.0 2.7 2.6\ |
6 2.2^~T*8 3.4 2.V
8.3, 6.4 , *.l 7.2 7.4 8.5 ,0\ (.1 \6.7 7.4 8^1
d 6.9 /.S 7.54-1 2/V. 4.8 6.2 7.2 6-3 6-S/' 4-3 5.9 5-7 5.2
119 CHG. N: l
N:2
N.3
Ni4
7 ... RESISTIVE CTNXfTIVE RESISTIVE
2B25W29QO* ll . . p i j- f
RESISTIVITY
^
NU 12.SK 19.OK 14.SK 10.7K
Ni2 14-4KS4.4K B/AK41
NiS 21.OK 12.8K20.8K
Ni4 7.8K 42.4W4
20. BK .0538
^' K 75.3K 87.2K 33.7K 27.BK 43.SK 6B-4K 93. IK 74.6K 3.2.K
3.0 BS.SK 26.SK 40.OK 32.8K 40 .9K 68-OK101 .8K 2.BK
643.0. 22.7K24.1K 42.3K 34.3K 35.3K 77.6K 3.0K 5^*38.1K21
18.3K24.9K40.5K29.5K36.0K l .
SK 29.7K 80.OK 21 .BK 38.SK 20-6K 27.4K 16.2K 19.SK T^.SK
.9K62.7K27.1K 23.BK 35.BK 29.SK 25.BK 14.IK 16.OK 10.OK
32.0K28-4K 30-6K 18-lK 39-9K Z2.8K 21.SK 10.1K 22.2K 1B.OK
RESISTIVITY NU Ni2 Ni3
,1K 18-IK 19.6K 10.BK 13 . IK 37.3K ZO-8K 20-6K 26-7K 16-5K 15.OK 14.6K 35.9K IB.IK N.4
* .288,0*^3^8*^80,0* 247,5* 245,0* ^4^5*^4^0*^37,5* Z35,0* 232,5*23^0* 227,5* 225,0* 22^5* Z Z^OVI Zl^SHZ^OH 2 1^5* 210,0*^07,5*205,0*20^5*200,0*^9^5*^9^0*
M9 CHO.Nil
Ni2
N:3
6.4 4. 3.8 4'8.
8.B^~TKS\3y6 l .y S .3^y.4
^.7) \V-^g.T ' 4.8
3.0
a.ni -B-
3.1 8.4
5.5 .B 3.0 2-3 2.83.0 3.4 3.5 3.2 l 4.8 4.3 3.9 2-V 3.3
K r.9 4,5 J./ Z.fi 2.li \ 4.7 4/0 J.W 4^
3.8 6.1 3.9 5.1 4.6 5.7 5.1 4.0 4.7 5.2 5.6 4.7 5-0 5.2 4.4 4.4 5.9 4.0 5.2 b.9 3.4
4-4 4.3 4-1 5.1 5.3 tf-^ 4.11 7 \trhi i f 4** *.k M^-^.M 4.5
M9 CHG. NU
Nt?
N:3
MM
ODMXCTIVE RESISTIVE
RESISTIVITYNU
Ni2
NiS
Ni4 400
15.4K 13.7K
IK 20.OK fl.OM
15.4K 15.9K\\
K 12.BK 14. SK
5. IK 6-5K.3.5K 4. OK 3.5K2.7K 3.8K
M9 CHO-NU Ni2
Nt3
Nl4
^PM^SMISP^M^^SM^DM^^S^
.2 l.J 2.1 3 .1. 4 .8 .B.B .5.4 4-4 5-9
8.8
.5 3.5 4.1 5-4 5.1 ^4, 6.5, 4.3 3.
B4.8\3.3 \X.4 r^\ 5-1 5.5 5 .5 /2 .8
"T.7 4.4\ 3.3) S.ev-^6.5 7.0^4.7,^3.
3 4.2 4^—4.5 3.8\ 8-4 6 .* k. 2 t
-1 7. fi 10-10-D 9.3 5.1 5.2 4.7 T^b 12.01/5/3 5.8 5.9
5.8
i.B 6.2
M9 CHO. NU
N:2
N:3
N:4
CtNXCTIVt —— RESISTIVE — RESISTIVE
290(O
RESISTIVITYNU 2.SK
Ni4 l
* 257,5* 233,0*25^5* 25qp*^47t 5* )24SfO*H242tStt24pfO* jJSTjSM^S^pW^SSjSM/SqOM^I 15*^2^0*^2^5* (22j}OMJ!jTjSJJ 215^1* 21^5*^21^0*^207,5*^20^0* 20^5*^10^0* \97,5*^95,0*
KKSISTIVITY 7K ,9j7K 18-BK 18-2K 17.7K27.0K 5,^ 18 . 2K 6 - 2K 3.SK 2.5K 2 .flH^UJK, 3 .gK^T^K^^BK^BK 5.PJ. 9-OK 4.9JS 12.8K. ^.ZK 6^7JJ 11 .OK 12 .7K 20 . IK 26 .6K 7 JIL 3 .6K 11 . IK NU
B-WlB-M 37. BK 19.BK SO.BK 22.SK 12 . W^Aff l . Btt/^^^^K^^t^a^K^fci^K ^HT^UK 6.}Xw7BTl\ QJK^K-Vt. 1 3 .7X^-/K25 .OK 25.4K 17.7K 11 .6K 14.3K 27.BK "1.6K N:2
4K58-6K 41.OK 52.SK 32.7K 41 .2K ffX^)4.pl^y7K 13 ^^wW^rtl'i p vBtJ^^O^-i^TK 8^Ma.9K aLwfls .2K 12 . IK 12 .STTiT .3K 43 .OK 26 .6K 8/^R ^.?7K 36 .3K 41 .4K Ni3
m2B.7K5B.BK 9 . BM 12 h/Nl&A* B WT^. BKkN^W^eW 6 -9K 19 -9K r^lTl6 -7K BCVK 19 .6K 14 .SK 10-6K 29 -8K 26 -SK 39 -6K 10 .8V 6 .Bk/20 .2K 50 . IK Ni4
CHtiNilNit
NiS
Ni4
3025*^00
B.O |.0 J9. 4.B B.I1.1 ** 7j^W |3 i
.4-7 4-B 6\.l 7.1 (B.I ViLJ^i
ZB25* 2800* 2775* 2750* 2725* 2700* 2673* 2B90M 2823* 2800* 2815* 2550* 2525* 25QOM 2475* 245.0*24^3* 2400* 'l 1 75* 2350lt 232iH 2JUOH 2278* 2250*itttS* 220.0*1115* J ^IHIIIHI fi'i | i | i'T*''i'*y [ y ?~?^f~^ f~f?~ f '/*7 y fs Y f /~ft ' ''I'l'i' 1 '' T^l^H
7^7 5.a 4.4 7.6 /.l) 5^ b.7 2.7 3.2 3?a74.fl 6,.0 B.B 7.l Tj^ ^^^
l TTTX 6:5—7.4 (fl"-"S\ 6.B 6 ^ jt.Z 3 .5 4^0-^-2 6/2 7.0 7.4 (f?TJ*r*^\l f
^U B\L JUO 7.3V8X 6.7X4-1 4-.^ 4-2 49 5U\7.2 B.B 7.^1^-7 10.J//1.:
ZSH^2J t)ON 200,0^
9.^X4.6 4-8)7.2 7.K B.7 .B .1
0.4POOR
CONTACT
-l 1.5 2.5 --1 tits 6
na CHO.NUNi2
7.7 9.1 \7.5 6.5 4.8 4.5 5.2 6.1 S. .6.7 Ni4
RESISTIVE 7 ——- RESISTIVE
RESISTIVITYNU
Ni2
Nt4
B.IK 14.4K 9,
10.BK 16-9K
14.6K 13
11 -3K
. BK
OK
19.8K
104. 8K 49. BK 10. SK 21. SK 19. OK 30.
106. 9K 14. BK 30-SK ZB-2K 23. BK
30.4K 30.0K 38.BK 38.2K 6/3. l K
54.8K34.BK5a.4K 11.9H/2.BK 4.4
,6K 2^3.98f. IK 4.1K/8.8
4K T^K7.1K
7.4lfTal3K \ .Q
yi9.0
woe.o huei'3vOJ91-0 Nij
IKJ21 JO/ l -5K Ni4
RESISTIVITY NU
nRl l j i-: VE: Y
i rNA Al rM h f 11 GUT WP C
i N i NI AKh A
AIT (Jl
LINt : O N
INDUCtl) POLflRIZflTION SURVEY
DIPUIE-DIPOLE BRRflT
N - l . 2. 3. 4. .. . 'H* S^HflNO r 25.0 MFTRFS
HECEIVER SCINTEX IPR-12 TIME UOMAIN
RX IX IIMINP. ?..c DN 2..c CFTWlftOW -'i ICE *9
i*.INiftx ipc-a ?0e HAH
KRL RESOURCES CORP.
PERK INS GRID NATAI - KNIGHT TOWNSHIP
: 25/U1/90 REF : LOE
5CRLL ^ l^ 2500
RRYRN EXP.
INE . 15936NUUCED POlRRIZRTION
SURVEY
DIPOI E-DIPOLE flRRflY
RECEIVED
APR 2 6 19 )5
-H" SPflCINO - 25.0 METRE SMtNING LrtNUb U
POINTN - l . 2. 3. 4.
RECEIVER. SC1NTEX IPR-U TIME ODHAIN
RX- IX l IHIKC ZMO ON ZMC OFT
PLOTTED HlNDOM a ICE *9
TRANBHITTER SCINTHEX JPC B 28* KATT
KRL RESOURCES CORP.
PERK INS GRID
NAIAL - KNIGHT TOWNSHIP
OflTE : JflN. 1995 REF J L1S
SCHLE - l : 2500
RRYRN EXPlORRTION LTD.
ANCH
l INL 200 S
INDUCED POLflRIZRTION SURVEY
UIPOLE--DIPOLE flRRflY
N z 1. 2. 3, 4, ... •fi' SPflCINO r 25.0 MCTRE8
RECEIVER 9CINTEX IPR-iZ TIME DOMAINRX-TX TIMING 2*M ON 2m* OFFPLOTTED NINPDH 3LICE. *9
TRANSMITTER 3CINTNEX IPC-B ZBB MATT
KRl RFSUURCES CORP
Pb.RKINS GRID NA1AL - KNIGHT TOWNSHIP
: 21/01/96 REI- i L2S
SCfll K l : ^
RRYRN EXP.
l I NE : 3DD S
INDUCED POLRRIZRfION SURVEY
niPDLL DIPOLE flRRflY
J?L
N - l . 2. 3. 4. ... •fi* SPHflNO s 25.0 METRES
RECEIVER SClNTtX IPR-12 TIME DOMAIN
RX-TX TIMING ZMe ON Z**o DFTPLOTTED MINOQW SLICE ** 1HANBMITTER SCINTICX IPC-8 2M NATT
KRl RESOURCES CORP
PLRKINS GRID
NAIAL. - KNIGtri IOWNSHIP
DHTE : 20/01/95 REF : 1.3S
SCfll.t - l : 2500
RRYHN EXP.
I NE 400 S
INDUCED POl RRIZRTION SURVEY
nipni F-nipni F RRRRYa . M a*11
N l . ?. i . 4 . . "H" SPH(INC - 25.0 MtFRtS
RECEIVER SLINltX IPR-12 TIME DOMAIN
HX-TX TIMING 2..c ON ZMC OFTPLDTTEU MIKUM 9 i a- taTRANBMITTER 9CINTTCX IPC-9 ZBB WATT
KRl RESOURCES CORJ3 .
PARKINS GRID
NATAL KNIGHT TOWNSHIP
DflTE JflN. 1SS5
SCRI h l t
REF : L4S
2500
RRYRN EXI1 ORRTION LTD.
roc jC.J
5gmO)-H
^ *c ji )
ui(.0-H
UJJjC/)PI
1r 1
f
m
, . | i i ..( ) (J i )( ) r j t i
in m in~i* i* i*C/) U t d)-i \ 1
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( tini-( 1 1
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i t-t/)
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( A)
t J
( J
mt-( n
• - (nl J C Jl J l i
in ini- i-
(0 ( li
i U( J1 J
1 11I-
( n
i (D• J ( }() i J
111 IIIi- ' t*
(/i C./)
m
oos
L 200S
2. 159L .5005
L 400'
600S
/OOS
l 800S
L 900S
LIOOOS
V'-f^-t- t i ^*—-J-/4 ^ t. - .- to uj/^ k ~ V- '\ •~C) rj X \ O O^ io\ l"
t\y*-ft -t- t * *--VL.* \ *•K * t y- t^y i-^ ^ *- x^ (7i m j
L l IOOS
L l200S
L l300S
L 14005
L l500S
600S
L I700S
l 8OOS
(^ * l * t \f l t t t
n il) i H) i (U tt* i* P
l f t t fr l
i .'i 411 *- l^
l l 1^1 ^( hU ^ , *V '-'t J
l b 8 S KK l 8 li 8t * -J ^ fell* *TKV(0
V ooT
V t. ,, ui i . * t/ *- ri r* * *
290
OOS
L 200S
L 300S
L 4003
L 500S
L 600S
L 700S
L 800S
L 900S
LIOOOS
oos
LI200S
LI300S
LI400S
LI500S
LI600S
L l 7005
L l BOOS
L l 900S
LEGEND
DA I A FRASER HLTFRFD CHARGEAB l L l TY/RES l ST l V l TY
SOURCE: l.P DIPOLE-DIPOLE SURVEY
"A* SPACING- 25M
N - l -4
TIME DOMAIN
CONTOUR INTERVAL - 2 MILLISECONDS (CHG)
200. IK.5K. l OK. I5K.20K (RFSISTIVITY)
FILTER METHOD FRASER. 'B'. TRIANGLE
na i IB ei
l l l t-, i . t KLR HCh'X CORP.
f lJpttl t 11 ON
V l Y
H":' '..; Jr f
i_ ..
RAYANl'! l if-,M l l T J l lil
, .f i|l( A i i i i V 4V l II H J l* l Ut 1C SK i
' l MM .l r i il-l l AMI i
.rt" i . ' M itihh
34043
———D
P^RKTM0 "
KNIGHT TWP.
INSTRUCT EDA OMNI ^RC'ON PRECESSION MAGNETOMETER
PARA^eTERS MEASLFED EARTH'S TOTAL MAGNETIC FIELD (NANO-TESLAS)
READING INTERVAL 12 5 M
CONTOUR INTERVAL 20 NANO TESLAS
DILFNAL GDRRECTION *1ETHOO RECORDING OMNI 9ASE STATION
DATUM SUBT^*C^ED f^ROf* AL^ PLOTTED READINGS 57002 nT
PEAK MAQhE~:C H I3H
PEAK
\ l
TOPQ LEGE^4D
D Claim Post Assumed
MACMJRCHT TWP. TYRRELL TWP.Claim L inne
C Hydro L l ne
3 6 RECEIVED
APR 3 1995
v-
CI lent. KRL RESOURCES CORP.Property ~ t R K I N S S ;K•tt;,
TOTAL n
Proceaaed RJI*
DateJAN 1535
Prav t nee ' ON'
Seal e.l 5.220
CheckedRJW
Townahlp
N.T S4IP/NH
MAG
RAYANEXPLORATION LTCOONTRACT/COMBJLTNQ OEOPHYSKS
TIMMINS. QNT/SRIO
(7B51-26B-4866
4IP11NBOOS7 2.15936 BERNHARDT 300
I77Y 444 Hz
NATAL TWP. KNIGM TWP.NATAL TWP. KNIGH1' TWP.
310
I P - PHAGF QUAUR A TURE
X* 20 10 0 10 20 -x
CONDUCTOR -15 AXIS
HLEM LEGEND
IN-PHASE
INSTRUMENT APEX - MAXMIN li
MODE MAXIMUM COUPLED. CO-PLANAR
READING INTERVAL ?5 M
COIL SEPARATION 150 M
FREQUENCY. 444 H.
OUAORATURE
CONDUCTORS
GOOD
NED
POOR
TOPO LEGEND
D Claim Past Assumed
Claim Lin
2-1593 RECEIVED
APR 3 1"5Mfriiiar. L AMDS BRANCH
s* i aa IM
KRL RESOURCES CORP.P, op.rly PERK IN0) PROSPECT
HORIZON l"Al LOOP
SURVEYocossed
R.JM
DotJAN 199H
Pr-uvince
Seals
CheckedRJM
TownshipNATAL
NTS
rirewlng
RAYAN:XPLORATION L uCONTRACT /CQNBU- TTJO OeOPHYSCS
TIMMINS ONTARIO
17051-268-4866
7^
M47V17, 7' KNIGHT TWP.NATAL TWP. KNIGHT TWP.
,xd'WV\^TA- - -
\0
1,00 \(J O
-500
ft v.^u
^o^
41P11NEOOS7 2 16838 BERNHAHDT l320
IP-PHASE QUADRATURfc
** 20 r
10 0 IB) 20 -X ~T~ 1
,- ~~ o
10
CONDUCTOR -15 AXIS . '
31 a
- I07-10 f -l
IN-PHASE ~—————— -——
QUADRATURE — — - - — —
CONDUCTORS
HL.EM LEGEND
INSTRUMENT APEX - MAXMIN 11
MODE MAXIMUM COUPLED CD-PLANAR
READING INTERVAL -26 M
COIL SEPARATION 150 M
FREQUENCY 444 H.
GOOD
MEDPOOR
TOPO LEGEND
LJ Claim Po*i At lumi
Claim Line
2*1593 6RECEIVED
APR 3 1995
MINING LANDS BRANCH
aa* i aa
CI lent KRL RESOURCES CORP.Property PERK INS PROSPECTTitl, HORIZON lAL LOOP
SURVEYProcessed
RJM
OaLiJAN 1995
Prov l nee*ONT
Scall 5.000
CheckedRJM
Towneh t pNATAL
NTS
Draw l rig
RAYANEXPLORATION LTD
TIMMINS. ONTARIO
I70BI -2B8-4866
O
r-*^
t
\ iCP
\^*'o
yCP
l l.-v-
ffi ^ **i1-5. V*
en .j)(P r4*- r*
^
,o (pi !i *. ^ri o)r*
ffi
\
, ^ U "^ * ^ ^ *l* ^ * IP *en ip o" *- "SiP O -J t-a
(P. d* ^
'-.o
LE.GFND
DATA FRASER FILIfRED RESISTIVITY
SOURCE. IP DIPOLE- DIPOLE SURVEY
'A* SPACING- 25M
N - 1-4
f l Ml DONA l N
CONTOUR I NTERVAL - 200.1K.5K.1BK...[OHM-MI
FILTER METHOD FRASLR B TRIANGLE
^ JB.1593APRS 1995
MINING LAMPS n B A f,r|(
20* tea
CI lent KLR RflSOURCES CORP.Property PERK ING PROSPECT
FRASER F LTFRFD
ProcRJM
Dot.FL'B l 995
Provl neeDN1
Sea 11l b
RJMTawnshi p
NAIAL/KN1GH1N l S
II P/NW
Dr-ow i rigf FREG
RAYANEXPLORATION LIDCONTRACT/CONSU TMO OtOPHYSCS
TIMMINS ONlARItJ (7051-268-4866
41P11NCOO!./' 2 1661fi BERNHARDT
•Wliiiwii*i"i"""'^~-.-..— -..1P11NE-OQ67 2 1E.636 BERNHARDT
340
DATA: FRASER FILTERED CHARGEABILITY/
SOURCE: l.p. DIPOLE-DIPOLE SURVEY
"A* SPACING- 25M
N - l -4
TIME DOMAIN
CONTOUR INTERVAL - 2 MILLISECONDS (CHG)
FILTER METHOD: FRASER 'B'. TR IANGLE
APRS 1995
M
CIl.nt RESOURCES CORP.
PERK INS PROSPECT
FRASER FILTERED
CHARGEABI L l TY
Dot.FEB 1995 Townvhlp
NATAL/KNIGHT RAYAHEXPLORATION LTD.CONTRAC1YOONMXTNO
TIMMINS. ONTARIO
(7161-268-4806
to
•5-'
O \V
ntf'i V
to
oto -i
i•s l l t,Vi
tO to
tot') -7-
o
\
V
V
V- -
41P11NF00572 15936 BERNHA&DT 350
LEGEND
DATA. ERASER FILTERED CHARGEABILITY/
SOURCE: I.R. DIPOLE-DIPOLE SURVEY
SPACING- 25M
N - l -4
T l ML DOMAIN
CONTOUR INTERVAI 2 MIL! lSFCONDb (CHO)
FILTER METHOD. FRASER "B 1 . TRIANGLE
1593APR 3
O
CI lent RESOURCESPr-op*rty PROSPECTTitli FRASER ri TE:RE:D
CHARGFAB T YProc
RJM
Da t-eFEB 1995
Pr-ov l ncaON
Seal-l.b.000
CheckedRJM
NATAL/KNIGHTNTS
4IP/NW
Drew lngFFCHG
RAYANEXPLORAIION l TDCONTRACT/consul rMO oeow-fr-acs
TIMMINS. ONTARIO
(7051-268 4B66
V-
I-o f '
en •7
r-'
i t i
\V
if
fiV
fi "
•A fi
fiV
t
V
, .^U^ * ft S *(J Ip
s
V
41P11NE0067 2 1 6036 BFRNHARD1 360
LEGEND
DATA: FRASER FILTERED RESISTIVITY
SOURCE: I.R. DIPOLE-DIPOLE SURVEY
A' SPACING- 25M
N - I-4
ME DOMAIN
CONTOUR INTERVAL - 20B.1K.5K.1BK...(OHM-M)
FILTER METHOD FRASER "B . TRIANoJRECEIVED
" APR 3 1995
MINING LANDS BRANCH
2-1593 6
CI lent
Propariy
KLR RESOURCES CORP
PFRKIN5 PROSPECT
FRASER FILTERED
RFSI SI I V ITYVoceaaad
RJM
DateFEB 1995
Prov i nee
Seall 5.000
CheckedRJM
Township NATAL/KNIGHT
NTSl P/NW
Dr-ow l nofTRCS
RAYAMEXPLORA1ION LTDCONTRACTxCONSULTMO QEOHHY
TIMMINS ONTARIO
(7051-268-4866
L IOOS
L 200S
L 300S
L 600S
L 700S
L 800S
L 900S
LIOOOS
L l IOOS
LI200S
LI300S
LI400S
l. I500S
LI600S
LI700S
LI800S
LI900S
L2000S
L2IOOS
41P11NE0067 2 16838 (SERNHARPT 370
K) O O
mCO
CJfj
m
IJU-DC/)IT]
r~r— ^
i n
r--c Jr )
IT1P.
(J)\
roCJr j
m"^C/)
H
COOO
rn"^CO
H
p.rjC J
111~Jf.
CO^
UlCJC)
r ri"it-C/)
1
U)f J( 3
in"^c/)
i
- iC )( J
IT]~i*
C/)H
(JOt )f j
rn~t*CO
H
-tr1O O* OD t— ^~-f — fc
o — rcr -i* ir
i- 1
f RASf:R r l LI LKM l) l P CMARGI AH l l. l ir
CJ C)
mC/)
H
au.D C/)
mC/)
}
CJo
mC/)
m
noCJr )
mC/)
-l
COo o
inCO -H
CJ
rnCO
Ul
CD
rnC/)
en c j o
III
CO-H
-J O
rnCO-l
00 O CJ
mCO-H
ui uP el R
O at 10 y-4
ot — o a
l RASf R f" l FL.RLD P RLSl ST l VITY
IOOS
L 700S
L 300S
L *KXK:
L 500S
L 600S
L /OOS
L 800S
L 900S
LIOOOS
OOS'
L l 2005
LI300S
LI400S
L l500S
LI600S
LI ZOOS
LI800S
LI900S
L2000S
L2IOOS
LEGEND
DATA: ERASER FILTERED CHARGEABl L lTY/RESl ST l V lTY
SOURCE l.P DIPOLE-DIPOLE SURVEY
A' SPACING- 25M
N - l -4
TIME DOMAIN
CONTOUR INTERVAL - 2 MILLISECONDS (CHG)
200 IK 5K l OK l5K 20K
(RfcSISTlVIFY)
LTER METHOD FRASER. 'B 1 . TRIANGLE
J2.15S3
CI lent. KLR RESOURCES CORf*Praper-ty OBRADOV CM OPTIONTitl.
FRASER E ETERED
CHARGEAB L. l Y RES l ST l V I'Y
RJM
Dot.FEB 1995
Pravl neeONT.
Sea lel 5.000
CheckedRJM
TownehlMACMURCHY
NTS4IP/NW
DrowinyFhCHG
MAYANLXPLURAIION LTDCONTRACT/CONiULTMO OEOPHYSCS
TIMMINS ONTARIO
17051-268-4866
V ,.
Mi Mi. N:. M:-
C 3 .t *~ r~~~^ -3: : .. .t
/
V ' /
K !\l \ . l r—ii NO
___A A,
AAt \
l 3
2*1593 6RECEIVEDAPRS 1995
LAMPS BfUMCH
2s" :Cp* "5* 5QK 25* DE 2SE
RESISTIVITY M:' 1S2.3W52.BK 44. 6K 3C.8K 25. OH *5 .7*79-lK 6t.'
i MK :35.0lC6l BK36 : * " 2* 83 .61 32 . IK 74 .6*1
Mtl- •.19.5*52.8*66.9* BE. IK S"1 . 4K TO-W 74.
* 1
———— - ———— -4 ——————————————— ——— 1
t
:75H ISpM 125* 100M 75* 5QW . 25M Qj
.:, -se ioptRES:S' : . :* v
f" *6 ir 31 .an Hil
s -44 -SK 69- 4K N:2
' :c .6M 55 . 3K 54 .OK N:3
' :K 6C.4K 25. OK 79. OK M:4
t
RA-** '.•'.ND i**c ON 2. .c OF11
^-C — ET W^CO S. CE *S
-J^V^SH I ' ' tK SCiSTREX I PC -5 298 **~~r
,, — — j, — s-- r- — — — — . ~ f-~ — , — , ' < -~s *Vt— "— , , - — — — . ~-S — ' . _ i\: — ^J^^-J-.—- — ^ -^— !
K ^ i ' — * k f ' — * r — * _ -^ 7 — | fc . *- j "" - - _ j T r — '
DflTE : J^ 1 S95 ^E r : L5S
Sffl !r - *: ^^^C^J W ' " _ . — — * i— ^^ *— /O
RflrRN EXPL^RRTI^N
——————————————————— /-1
tt S CMD. 1 M9 CHD. Mtl 10. a 8-9 l^ 9-0 8.4 6.2 fl,.6 A 2 3 1 0 J T. 2 4-2 NU
Mi2 11.5 J9. S 9.2 8.6 IJjjO 9^K 6 .6 T*^ 8or V*./* -S N:2
Mt4 .'.C ^7.8 lKT""tl.5 12-3 ( g^^^fsi 5 . j/ ^5 6. f /3.7 M:4
175M LSfM .12SM ,10pM , 75,M , 5BJM , 2S,M 0| 25,E SCjE 7^E
RESISTIVITY RESISTIVITY ! Nil 29.6K 44.5W.Q6.7K 33.7K31.7K I3.1K 17.6Ht3.5K 25.5K 9 .SK B.IK Mtl
Mr2 41 .4K 73.0K 64.2K 40.9K27.7K29.OK70.4K24.isK 11.5K22.2K VsK N:2
Ms3 68.4K 44.9K 62.1K 30.7K 49.4KS6.6K24.1K 10.2K^3.5K IC^Mt^^ZK N:3 Mi4 42.1K 41.1K 49.1K 46.9K 99.9K25.6K 10.3K 17.2K J*ftK^*^T5 . 4K Nt4
LINE : 70C S
:NDUCED PSLRR^RTIONSURVEY
DI P OLE-DI P 3LE FRRRY
. i . JL. -i.
r©^ rCh*-. '\ t '\ - 1
N : 1 . 2. 3. 4. . . . •P- SPflCIND : 25.0 fICTKES
(CCEIVER SCINTEX IPW-1? TINE DOMAIN
RX-TX TIMING ZMC ON Zmme OFF PLOTTED MINDOM SLICE *S
TTWNSWITTB? SC1NTREX fPC-9 2M MATT
KRL RESOURCES CORP.
OBRADOVICH GRID MACMURCHY TOWNSHIP
nOTP * IflKJ 1 QQ^ I? F" f * 1 *7^w" " t. •vOPii99w RW' 'L/O
SCflLE r 1 : 2500
RflYRN EXPLORRTION
l
iSPN 125M topx 7SM 50M 2SM F f ' ' * r y y V x /'y
75E' y S s s s S\2SE
M9 CHD.
M9 CHD.Mtl N:2 Mt3
6.1 1,2 .p 13. L y8.6 . 7.2 8-1 6.6
Nil N:2N:3
N:4
7-t 6.0 6.7 S.9 V9.9 9.4 9.3 ip.3 10.J 64 9.4 JO.l 6.4,^y.6
7.9 8B.I
.9 9.9 9.4 9.3 11).3 10.J 64 9.4 10.16.B^-*,0 lO^T^ 9-9\ 10-3 Vi 8-3 1^-9 10-3
.4 7.0/9.8 ^J9 10^1 11.5 11^/8.6^0^^8 ^r*^7.V 10.1 9.9 "3^3. ^TlVl.7Ng.2 7.9 i
H9 CHD. NUN:2
3 10.8 Mi3x. " ~— .7N9.2 7.9 9.9 MM
LINE : 800 S
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE RRRflY
N r l. 2. 3. 4. . - . •ft* SPRCIMO r 25.0 METRES
•IVBl- 9CIN1EX im-12 TIRE DOHA IN RX-TX TIH0B: 2mmm ON ZMO OFF PLOTTB3 MINDOM SLICE: *V TMNBHITTBt: 9CINTNEK 1PC-B 211 MATT
RESISTIVITYMsl M:2 NO Ni4
ISM ,12S* ^OpM , 75,M , S^M , 2S,M , PC , 2SjE f , ^E l ODE [12SE
RESISTIVITY.7* 11 .BK 19.BK 57.4K 58.BK42.2KBB.lt W.BMfi.4^ 24.SK 24.6K Mil
22^B 17.6K 1B-4K 18-4K 20 .BK 59.0K 47.4K 45-61 CT^B t6-6K 63.6K 18.tK M:2 tt. 4* 15.2K 10.TK 22.OK 20.9K 16.4K 42 .2* S*.4Mfi^K 32. IK 90.SK 36.6K Mi3 r XS.fK 13.0K41.6K 1S.1K24.TK21.4N tS.4MS4.MI6.8K 27.SK29.1K 18.SN Ni4
KRL RESOURCES CORP
OBRADOVICH GRID MACMURCHY TOWNSHIP
DATE : JAN 1995 REF t L8S
SCflLE - l: 2500RflYRN EXPLORRTION
17SE ^DDE 22SE 25DE 27SE , 30pE . 325E ,35pE , 37SE 40DE 42SC 4BBJE 4)75E
i 8 * 9 8' 77. t 8. 8 9.
. 4 7^8 Utf.8 9C9 v B .4 l***-v 7 .0 7 9 .3\ li .2 l B. B t/^6 11.
17S
RESISTIVITYMtl
Ni2
M:3
M:4
16.IK 32.2K 15. IK 10.6K
fl.6K32.iK 13.2K 137.SK 33.BK 24.SK
9.4K62.6K 19
RESISTIVE
325 , 375E | 425E ) 4SpE ,475E , SODE ,S2SE
8K 22.7K 31.4K29.2K IB.OK 17.SN IS.8K 1B.3K i-7K,15.3K 9.SK 26.OR .BK 26.2K 27.9K 32 .3K 20.OK 21 .9K 4B -2K 28.OK 1S.2K 19.4K 10.BN2B.1 25.6K 37.BK 33.3K 30.3K 21.2K 47 .BK 54 .7K 42.TK 17.9K 16.6K 14 .2N tK44.5K 47.9K 31. SK 30-OK 39-6K 47 . IK 72-9K 44.2K 13.M tt.4N 20.4*
'SE .700E
15.IK 4K 9JBK12.SK17.4K14X1K 1S.4K 3K 21 .tK 12.OK 21.4K
RESISTIVITYMtlM:2 Mt3 Ni4
LINE : 900 S
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE RRRflY
fi.
N r 1. 2. 3. 4. ...- SPBCINB : 25.0 METRES
iIVBt: SCINTEX IPR-12 TIWE DO**IN RX-TX TIMING: 2aac ON 2MC OFFPLOTTED MINDOM SLICE. *9 1VMNBMIT1BI: aCINTHEX IPC-9 2H MATT
KRL RESOURCES CORP
OBRADOVICH GRID MACMURCHY TOWNSHIP
DflTE : 29/01/95 REF : L9S
SCflLE ^ l: 2500RflYflN EXP.
s
LINE : 1000 S
225M
M9 CHD.
N:2 N:3 N:4
62SE 65DE 67SE ,70pE40pE , 425E , 45DE , 475E SSPE . 575E .60|
9.5 6.4 1CU3 B. 38.8 9.0 B.6
.3 8-6 8-B 6.6 8.5 6.6 8.5
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE RRRRY
fi.
COOUCTIVE !
22S
RESISTI^ RESISTIVE
175 OE , 12SE , ISpE , 17SE , 20pE ,22SE , 25pE ( 32SE t 37SE | 40pE t 425E | 4SpE ( 47SE , 50pE | 575E | B2SE ,65pE ,675E | 7SpE , 77SE
RESISTIVITY
N:2 N:3 Nt4
• 9K.4i2Kr.BK ^2.4K 10.2K 41 .3K 16-3K 25-4K 36.6* 86.2H 31 .IK f4.BTrr^^K |TM 1B.3K 14.OK 21.OK 29.OK 8^7K 33.In 52 .OK 4 l
t 16.5K 1374TT3.0K 16.6K 18.7K 25.2K 15.TK 17.7* 17.2K 42.IK 57.4K l 23.IK 12-3K 14.3K 30.OK 13-3K 27 .BK 20.BK 6.4* 30.SK 19.4K 40.8K
96.9K59.8K27.4K 9.5K-.5K 5-4K 44 .614 08. OK 35. 2K
57. 7K 48. 9K 63. SK
S -2K 16 -SK12 .2K
.7K 15. 9K 19. SK 7.BK51.SK 65. IK 45.4K 32.IK 12.ON IS .SK 25 -7K 17 . IK 20.OK
RESISTIVITY
Mt2
M:3
M:4
N z l . 2, 3. 4. ... 'W 5PRCINC : 25-0 METRES
BEEE1VER SCINTEX im-12 TlfC DOMAINRX-TX TIMING. 2MB ON 2*w OFFPLOTTS) MINDOM SLICE *9
SC1NTRCX IPC-9 2W WATT
KRL RESOURCES CORP.
OBRADOVICH GRID MACMURCHY TOWNSHIP
DflTE : JRN. 1 995 REF : L10S
SCflLE - l : 2500RflYflN EXPLORflTION LTD.
:SN
-s20DK ,17SH t;SDH )125* , 100M 75H SE
' s s A ' ' ' ' iv^ X/ y j
N : ,
N-.2
M-2
N: 4
6.8 .4.6 4.5 ,6.6 SJ 7.6^ 6.1,12-2
S. 2 9.arTV9.7 13^2^:6 9
M : ;
N:2
-Ch
K r l . 2 . 3. 4 . . . . •fi- SPACING - 25.0 METRES
RECEIVER SCINTEX IPR-12 TIME CDWIN
RX-TX TIMING 2nc ON ZMC OFF PUDTTHD MltOOM SLICE *9
TRANSMITTER SCINTREX IPC-9 2H MATT
175* | 125M StM
2.7K 2.2H 2.9K 5 6K,9.0K 7.9K S-9K. 9.9K. ITT
N:2
l .3*
N: i
N:2
N:3
N:4
KRL RESOURCES CORP.
GBRADOVICH GRID MACMURCHY TOWNSHIP
DP'E : 29/01/95 REf : L IS
SCflLE - l : 2500RflYRN EXP.
200 s
M9 CHG.
Mi2 N:3M:4
INDJCED POLRRIZRTION SURVEY
OIPOLE-CIPOLE
fi___fi
6.7 ^ 4.81/2-1.8 -.5 -1.0 N:4
RESISTIVE CONDUCTIVE
RESISTIVITY
N:2
M:3
N:4
N : l . 2. 3. 4. ... SPHCINO : 25.0 HETKES
rive? SCINTEX m*-12 TI*E DOKAINRX-TX TIMING 2—e ON ZMC OFF PLOTTED MINDOH SLICE *9
SCWTHEX tPC-8 2H MATT
KRL RESOURCES CORP
OBRADOVICH GRID MACMURCHY TOWNSHIP
DflTE : 29/01/95 REF : L2S
SCflLE - l : 2500RRYRN EXP.
200H
H9 CHD.
17SM I50M 12SM i y s s s s y s s
ll
LINE : 300 S
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE RRRRY
(
Nil
Mi2
N:4
*f
(l{
20pM
RESISTIVITY ITYMtl Ms2N:3
N:4
14. BK 63 .ON 44 .BM 54. OK 2S.2K65.OKS4.OKZl.OK
22. SK 66. IK 26. 4K S.2K 24.9K38.2K
fi fi
Pi — l* Z* J* 4* *** R* SPMCIMC r 25.0 NETftCS
. 9CINTEX IPR-12 TIME DOMAIN RX-TX T1HING ZMC ON 2**c OFF PUTTTH) MIMOOM SLICE *9
*ITT9- SCINTKEX IPC-9 2H MATT
KRL RESOURCES CORP
OBRADOVICH GRID MACMURCHY TOWNSHIP
DATE : JRN 1995 REF : L3S
SCflLE - l : 2500RflYflN EXPLORflTION
LINE : 500 S
17SH l SON .1250 topn 7 ' 1 S Y S S S s S S 1S S S*S\
f!9 CHD.
N:2
N:3
N :4
6.7
9.3
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE
M:4N r l . 2. 3. 4. .. .
R- SPflClHO r 25. O METRES
RESISTIVE
17S*i t 125M t
RESISTIVITYMM
N'3Nt4
16.3K 32.3K 33.BK 12-9K 19.3K4B.5K37.2K 46.9K22.4K 27.3K3S.9K2U9K22.BK
33-3K25.6K53.4K 30. 3K 12 .OK 46. BK 42. IK 39 .6K 17. BK 11 .9K
OE 25E
RESISTIVITY .&K 2. OK N:l ( f. I K Nz2
Nt3Ni4
SCINTEX Cm-12 TIME OOMACN RX-TX TIMING 2mmc ON ZMC OFF PL0TTED HINDON SLICE *9 TRANSMITTB? SCINTfCX IPC-9 20 MATT
KRL RESOURCES CORP
OBRADOVICH GRID MACMURCHY TOWNSHIP
DRTE : JHN 1 995 REF : L5S
SCflLE - l : 2500RRYflN EXPLORflTION
380
f
V' i1
l
20pM | l75U 1SPM.12SM.10PM 7S.W SQM 2 5, M OE 2S,E
rift CMC. f19 CHO.Mn ^ '3^^^s^^ji^^^7i/'/^//^:/1/^ 4; 0 2 '^ l '? 7* 8 W t|
Mt4 17.6 IBrS— a^S~f3vK\2n .9 1^6/7/4/7 *r6 \3.4X^io MM
*
2Qpl ,17SM ,ISpM ,12SM t100M 75^4 SIJM 2S,M OE 2S( E
RESISTIVITY RESISTIVITY Nil 19.3K 36.7K 30.6K 6^4K^2 .4K 29 .BK 3^4* 2^5* 1*2K.22.2K Mtl
Ns2 16.2K47.2K22.0K 12.9K 17.9K^^B^-6<1I1{^f7^l^^J.l^A:3l^ Nil
Mt3 17.8K53.2K26-2K 1 7 . 4K7(^^p 71^24T2K 12 -9Xx^5^8^1K Ms3
| M:4 25.0K59.3K30.6K 2JZJP^sIK34.0K 27 .3K l ^.tK^&f/K.VK 1N4
!
LINE : 400 S
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE RRRflY
. 1 . V - ' -
fi fiNv
•TIH^VMTN r 1. 2. 3. 4. ...
•W SP9CIMO z 25.0 flETRES*
RECEINCR SCINTEX IPR-12 TINE DOMAIN
RX-TX TIMING: 2we ON 2~c OFF PLOTTED MINDOM SLICE *9
TMNBHITTER 9CINTNEX IPC-9 2BB MATT
KRL RESOURCES CORP.
OBRADOVICH GRID MACMURCHY TOWNSHIP
DflTE : 29/01/95
SCflLE -
RflYflN
REF : L4S
1 : 2500
EXP.
,1ft,.' ? ' ifcfcw,,
,325E , E ,425E 50DE52St
MS fur,.,650.C t ,725E , 75pE , 82SE
Nil
Nl2
Nl3
Ni4
7.3 .4.8. 3.3. .8,4 9.4. 14.4 . 9..4 .6.5, 4.8 5.4, 7.3 .8. 4.6 2.9 2.6 9.2.4.7 J. 52.7 3.9 t
l I 1 l
B.I A .a L .6Wr^1.4 8.4 6.8\ S.4 Sfa
M9 CMC..8 N:|
N:2
N:3
Ni4
LINt
INOlin UK i
-X.l
MotrtH roim
l Ope , Itig , 15pC , 1 711 ,tO(H
RESISTIVITYNil
Ni2
Ni3
Nt4
59.9K 10121.7K35.IK
4V.9K72. SK 8
-dK 47. JK 17.OK 22.SK
N - l . 2. T. 4. •W SPHCINO - Z5.0
30.SK 9.SK 13.IK 10.IK 8.-1K^8^8JJ!t.IK^aV7K 5.6K T-SK 6.JK 8.4K 14.1K 99.8K 18.1K 40-4K 11.IK 26.5K 1K21-2K 8Q1K34.6K 13.4ITli.8*|R IJ^N^lKJ.A* oB^ilCiC^K27. 8K 18.8K I8.8K 21.9K 31 .OK 18.7K27.8K 12
26.4K 17.4K 19.9K 18.0K174N 12\K-rf^lK 1S.3K 17.0K 24.7K 91.9K 18.8K 14.8K 43.4K 20.0K 43.BK 11.2K48.5K 12 K7S.2K 10.1K28.8K27.8KI9.9K2B.8K 18.7K 24 .OK 39. IK 28.9K 90.8K 17.BK 90.BK 28.7K 45.SK 15.0K 38.9K 39.6K
DOMAIN
norm WINDOW ft ter .9l II l t
KRL K'f . .1 i. Ji '
OGRAIXJVIOI (i MACMURCH f T (.M.
DP.TE : Rt l
SCflLE - l :
RAYAN EXF'I GRA1
M9 CHO.
iP|L^I,i
Nil
Nl3
Nl4
H.8 10.0 .8.4 6.7 7.3
8.7 S.aN^.O 6-8 6 7.B 8.7X7.5 /*fTT\8
7.5 . 4-8 . 7 .2 11.2 11.0 .12.8 12.9. IS11.3
li.B
1/1.6 11.1 11.S
^4 7.7 5.2 2-6 ^ 3.B 3.,
•ffcj.5 7.9\ 3J.5 2.2 2.3 2-3 3:
N^Y^'V7 " (nrbr-•VwtXVW.S 4.1 3.1 2.2 .9 r*
2.8
-9 5 -2 x .6 y.8 4 .7
M9 CMC. Nil Ni2N)3
N:4
, 12SE , 15pE ,175C ,25pE 4 425g , 45pE , 47pe SOpt .JtBC .
RESIST i ve
^9yg ,65pC .67SE ,728e ,7gPC
RESISTIVITYNil
Ni2
Ni3
Ni4
32.BK 26.4K 97.7K 40-7W4
54.SK 38.OK 48-8K 12.
69.OK 46.4K 17.SK
82.3K IB.OK 18.BK 47.
K CB. SK B^KZS.BK 18.4K 38.OK 43.8K 73.2K SO.SK 34.SK 15. SK 21. SK IS .7K 21 .BK 25.4K 81.4K f 9. IN H.7K 13.2K 29.OK 4K 14.9K 17.SK 43.8K 23.OK 54.BK SB. IK 56.SK SK.8K 23 -3K 31-3K 85.8K 12. IK 20 . IK 27.8M 29.OK tO-IR 13.6K 30
BK 36.SK 24.2K 51.BK 28.OK 64.IK 48.BK 33.SK 20.OK 37.SK 63.OK 43.4K 11 . IK 20 .BK 40.9K 99.4W I7.2K 21 . 34.3K 45. IK 26.6K 60.OK 31.3K 48. IK 22.OK 19 .9K 30-9K 69.2K 34 . IK 32 .IK 11 .4K 31 .OK 62-2K 2l-8i 23. IK
LINE : 1800 .
INDUCED POLflRIZfll I MN SURVEY
DIPOLE-DIPOLE HRKHr
fi.
OCPTM^WIHTN - l . 2. 3. 4. . . .
•R* 8PHCINO s 25.0 Ml TIU!,
rive* SCINTEX IPR-IZ iiwRX-TX TIMING ?..c ON 2Mc (FrRJ3TTTT) MINTTM SI ICE *8
SriNTHEX IPT-H c-BB WAI l
KRL
OBRALJnVH7H i .f MACMURLIIY l (M i
OflTE ' f K l l
SCRLL
RAYAN EXPLORATION
MB CHO.Nil Ni2 Ni3 Ni4
RESISTIVITYNilNi2 NiS
Nl4
275E tfpE ,325E
38.tllt4.OK58.7K3l.8KI
48pe ,47Bt .SOpt ,S28f ffOf .575E ,BOpE
.8JM|,7K B.7)1 l*.SK 9.IK It.81118.OK OMK 7..5K,!l .4K 4|.8K
2B5S.OKtt^48.0K80.7K33.8K91.8Nf^ik^^29.aK27.5K ™8t.8W29.9^^*4/7.SK 18. .lK4B.tNtl*tKSS.3K82.1K40.1K3S.8AAp|8f9.1K9l.3K lB.2IT1t3.tN 88.4K 19.it^)K 2S-OK
4*14.0
B0.1K22.9K47.4N24).8KI4.2K88.8K49.9K 8.IB80.7K 31 .7J20.4K 30. 2K lt.4K 16.2K2i.8N tt, f*
RESISTIVITY N:lNi2
NiS
Nt4
1^00 S
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE RRKf-ir
otrrnfdntN 1 . Z . J . 4 . .
•R* SPfltlNO - ^b.O MLTKt'i
RECEIVER SCINTI--X [PR \ f T |MF
KK Tx T IMING Smm^ (M .'..c ()f>F ^i^^L U^^aU^pW ^^ 4^^B f ,^g)|K
IITTWi BCINTMK IK-B MB WATT
KRL RESOURCES CORP
OBRADOVICH GRID MACMURCHY TOWNSHIP
OflTE l / REF : I.19S
SCflLE ~ l : 2500
RAYAN EXPLORATION
4.9 4.6 5.46.1 S.I 8^3 7.3 7.9
5-3 5.s) 7.0 |fT~"8.9
S/T' 7.0 7.1 8.9 8.t
**;* i
M9 CHO./•-1 / 7- 4 i ^ /'6t 8T.3J.9^8-4 S.t
"SZ^ /*J*^X1'~*7 r' ^4r8XlU*. 74 I8M; 4,4\7.B /4.8 S.V 7.
RESISTIVITYNil Ni2 Ni9 Ni4
27SE SOpt ,325E ,38pe ,S'
5.BK28.1K I8.7K 8.JK 9^1K
7.7Kj|.6K41.8K28. 12.7R14.9KS9.7K
18.8K 18.8142.4K27.SK 9 <.7K18.7Ktl.7K3B.4K
Ml 23.IK 21.8118.IK|4.1K91.9Kll^8KxC
i
II0TIVC
, 578E , BOpE , 625E ,85tJ.J75E
RESISTIVITY NilNi2 NiS
6.SK 6.IK Ni4
' t- ; |r—————————————————— 44 ————
:A
————— '* "1
———— IJM ————t
f,.
"""T ——————— ~ ———————————————— T ———
i
INE : ?nnn
' iS
DIPOLE-DIPOLE RRRflY
-Ci. J?L
KPTN r* i K tN : 1. 2. 3. 4. ...
'H* SPflCINO : 25.0 METRES
RECZJVCR SCINTEX 1PW-I2 TIW DOMAIN
RX-TX TIM1NB: Zaae ON 2..c OFF PLOTTED H1NDDM SLICE *fl
TNANBHITTER SCINTREX l PC-9 ZW MATT
KRL RESOURCES CORF-
OBRADOVICH GRID MACMURCHY TOWNSHIP
DflTE REF : L20S
SCflLE - l : 2500
RAYAN EXPLORATION
\
RECEIVED
APR 3 1995 DC
5.1593 0^ ^8^
8.8 7.S 7-1 8.8y
y 4.9\8.4X.7 8.7 4.1 8^4 Kl~^l jrTt).8 8,2 4.8 4.8 4.8 8.0 5./ 7.t,JjX^t /^.f
4.8 M ••'8N**.,,t*9 4.7/6.8 S. 6--^ /.7 /CO
lKlaie-SK IB.2410.O 2Swtt.7K18.7K |^K32
OS NI4 14.0K lJ*\ 7.SK \7V2K f.l
RESISTIVITY •2K Nil
OK 30.SK Ni2 NiS
tf'7K18.2K 8.4*27.IK Ni4
^^^^^^
^*8^ll
^
LINE : 2100 S
INDUCED POLflRIZflTION SURVEY
DIPOLE-DIPOLE flRRflY
i m | .
1*1 r^x,/N r 1. 2. 3. 4. ...
•fl" SPRUNG r 25.0 METRES
RECEIVER SCINTEX IPR-12 TIMt DOHAIN
RX-TX TIMING 2..c ON 2..c CFF PLOTTED WINDOW airf *9
1HMMN1TTEM. BCINTHCX IPC-8 2M NATT j
^t^^^HMH^^Htji]tjBjim***H*~^^^^IWHRRcEs CORP '
OBRADOVICH GRID MACMURCHY TOWNSHIP
OflTE J / /
SCRLE r
REF : L21S
1 ! 2500
RAYAN EXPLORATION
N S41
41
h*
M
D S
A iK
i
i
'^*^^8HBiS5|p|
41P11NEOOt7 J 16036 BERNHARDT
IT* i IK;6.0 7.4 7.4 7.5 J. 2 7.0.1Q.6 B. 2 8.5 2.4 0 4.2 5.1 .6 V 4V.B,6.9 5.8 8.*. I.3.J 7.5 ,B.6 (5.6
.0 7.3 7.5—7.8
8.0 8.9 6-0 9.2
• \ 7 .0 /S~74\ 7.0\ 8.
CONDUCriVE
KLSIS1 1VHY
N . ^
N: j
N;4
46 O 104.1) 133
106.0 l^CL/
( 51JH i 2^H t OE t 25,1 t bljE t 7 5^ J
3-3K 3.2K 3.5K ^-SK, 15.BK V ^.OK, 9.0K..8
.9K
^
4.4K, 9.SK 10.
850/02K
4K28.5K 33.0K2S.3K24-2K22.9K I8.8K 42-2K 35-2K 25 .4K 30 .4K
(12.7K35.5K 33.8K26.4K 33.7K 19.SK 34 .SK 52 -OK 32 -6K 4B.7K22.6K
2K 16.OK 39.BK 33.9K 39.IK 25.SK 29.8K 39.BK 43.4K 47.6K 32.3K 13.5K
15.OK I6-4K 45.BK 45.4K 27.7K 39.7K 34.SK 33.4K 60.9K 28.2K 18.OK 12.3K
RESISTIVITY Nit
Ni2
Ni3
Ni4
•l
Kt ' t i '
K- l .
1 i 11 l f l l H , l. l
I lilt-
DRTt : 01 ,
K' h M
IN'l
ri9 r
6.0
7.fx a^il— lt j
a A.af /-.4- -^
• i ^.f B .6 Ip.*; 10,4 4-3 5.4, Z.:
3-9. s.B\i^Ti *ie,6 s-y/a /*n\ M'.2B *? y l o /i "'""^"••3 JR \i no * ^\ f ^^~ *t ci *\ * IS \ "* *^ *" *D v.W * \* l 3 ^g t * O
J ^— ^ \ ^_' l/3 xf?\0 10\3 TT*. 8.T1—8-:6 Ni4
CttCUCTIVE RESISTIVE
7H. 7| 50,E 30pE ,40pg
RESISTIVITY, SSfE
RESISTIVE
, 675E , 70pE . 7 5pE , 775E
BK l l .BK 11.9KZ3.8K S^SK B.IK ^.4K1Q.4K B.6K 4.9K Z^BK l .BM. S^SK 4.8
124-BK 14. SK 12.SK 12 .f^P^.il^/BWlS -SK\ fe .OK^JK\2\S^.r^^TT8JI^
.SK24.BK S^ 1S.1K20.7K ll\^4\Crt^K 8.SK 13.9K0 |||JK
28.SK 18.SK il.7K25.4K 16.2K 12^8*1 f^* 7.BK 5-1K BTjft fi
J0.2K
35 1 ^i.BK^.:46.BK4a.3K52.6K83.1K
2K53.0K7I.7K86-2K
41.8KSS.2Ni03.8K 7
BK SB.SK 94.OK 10.SK 1B-2K 11 .BK
9.711 2.7K?l 8.6K
RESISTIVITY N:l
N:2
Nt3
N)4
\
..JS1
Kill l H ' KM l- lv
HX l l IM It* *.. ill .
i-lll.il M l "* i' h . l 4 l
l (y/j i M i i 11 ^ ,. .' w i 11 -i
Mhh'-M l ' M MA-' ,'li Jh i l M
DHH o;-'NII.' -i 1 .
S( Ml t
,?5pH .ffSN , 125M . 10pn . 75.H . 51)H
M9 CHO.NJl
Ni2
Ni3
N:4
2 .R .6 1.3 1.0 J}. 1 -9 2. 9 - 6 1.3 fjf 1 .8 2.C
2.6 -5 -8 /rve-^1.6 .71.9 /c.o~2\y" .B
825E 33pC 37pE 40pE ,425E , 45pE , 473t
POOR CONTACTS
CONDUCTIVE RESISTIVE
, 175M ^ISpH , 12SH ^ IQpH
KtSISTlVlTYIf.SK li
ISTIVITY
••MM*,* .9K
27.BK
32. OK
N)3KM
L l Nl :
N l•H-
,i i nn K
RX U l IIMfJI) ., n l* i
PU)! It li WIUI vi t t
TMANSMI l m, I'iH* -
KRI
MALMURur 11 i'UWN^h l
DflTE : JRN 1995 REF : l 135
SCfll 1 :
RRYRN ^ *!
f19 CHO.NU HtZ
N:4 -6.1
8.7 8.8 7.8 6.B
MS CHO. NilNil**'
N 1 3
Nl4
COCXCTIVE RESISTIVE
RESISTIVITYOK 4B.6KB7.7K 5
.OK140.7K ll
50.0K 1B.2K
.3K 31 .7K 35 . IK 22 . IK 2B.3K 39-7K27.7K
9 -SK 29 .SK 39 . IK 61-7K22.4K
41.7K 35. SK 31. IK //tK 4.8K
IK 8.2K51.0W15.7K 38.1K24.6K 9-4K 51. BK 17. 8K 4.BK
25.SK 28.SK 55.M 12.4K4. IK 40. SK f 2. f N llslfiufr 19-3K 13.IK 38.2K 38.OK 18.IK fi
10.SRfO.8K 16.SK ff.IK IS.OK 37.IK 11.OK SO.IK 12.OK 13.6K IS.7K f O.IK 33.OK 18.SK 28.SK 15.SK 12.IK 17.SK
.IK, 4.4K 3.SK 6.9K3. SK /. SK S.7J
f0OK 4.SK S.fK/S^.SI
r 4- 7K 9 ' 9K5JK 3.8K
RESISTIVITY Nil Ni2 Ni3 N'4
l T P t- i l 1 l— i r ^'i
INDUCLD r H!
DIPOl
"H* !iKH. i M. '
RECEIVt H -4 INIt * II-K
FIX -IX IIMIN), . ,.. (rj .
PLOT mn ^IUUM ^ hi .-iSI (NIHI * id
OBRA[)f)vu:n iMACMURCHY I M
DflTE :
SCRI.E l :
KRYRN K
20pH , 173M ISpM , 128H , IQpM 25,H OE 7SK .fOpE ,225g 28pE USE .3002 ! ItSt MM ! 37SC 400E . 4ME , 43DC 478
na CHO.Nil
Nlf
NiS
Nt4
8.3
0 7.8 ?'*y*^xn-7\ sorrs.a
5.7 S .85.7, 6.3 ^5.3,8.4 7.4 7.1
CCftlUCTIVE
20pH i 175H | 15pH | 12SM | 10pM ( 73^ . IQpC . 17SE , 20pt , 22SC ,30pE , 323E ,40pt ,4fSC ,48pt 47SC .578E .BOpE .625E
RESISTIVITY
ON 40.IK 21 .BK 39.3K65.IK
Nil 171.0 lU.QJIJ.Om.O^B.BK 28.BK 23.SK 30.OK 25.2K If.fK 42.5K 19.7K[To 300^ 42.7K3B-ZK _
Ml' MfWmjO 408.544^^*^11^ 30-IK 72.SK ^OK 14.9K 40.IK 25.2K 28.SK
O**B*^
SO.IK 18.9K 8.OK 18.SK 14.7K a*3K 25. IK 15.2K 67.4K
.1K sW 9^K9!
80.SK \OK ^HSB
fS.BK 32.SK 14.9K33.2K B-SK 33-SK 29.3K 24 . IK
95.2K 42.BK 20.4K 15.9K 42.ZK 32.BK 42.9K
IK40.8K^5.3K 9.2K 68.SK 41 .BK 42-6K 2/3K
LINK :
INDUCE D I'OI RKI/M ' SUKVt r
DIPOLL -DI Pill L UK'"
. * . M t
..f:\Der (H rami
N : l . 2. i ^ •B' SPflClNI) . . i t i 1
REUEIVER SC INTFX im l i n K IM' t,
RX-TX I|MIM. /... IIM *~ l Pl.OTTfcJJ N IMJIX SI H l *'i
Vrf IMU! x M i i
KRL
OBRAUUVIf/H lil' 1 )!. MACMURCHY TOWNSHIP
9I/02/9S LIMf" i N
RflYflN [ X \' .
i M
RECAPR 3 1995
•MNNQLANDtMRANCH
C.7— -A .0
2.1593 6ID
..A
O S C
ACMURC O
na CHO.Nil
Ni2
Ni3
Ni4
SOpC S23E B5pE B79t 70pC 7SJg , 73pE 7 7 St 82
7.1
S.S. 4.4 4.4. l'* 3 -^. 1.9. 8.7 7.0 8.4
.3 4^3 /3^7 2.4 /S-8 4.|
1-9 S.I 4.3
M9 CH6. Nil
Ni2
NO
NM
isrrivc
RESISTIVITYNil
Nlf
Nl4
5IJE 75,ERESISTIVITY
4K 25. OK 28. IK Nil Nit
Ni4
LINE inno s
INDUCED POL RRIZHT 1HN SURVEY
DIPOl f.-DIFJ OLL RKKflr
-fiOcrTN r*iMr
N r l . 2. 3. 4, ..- •fi' 6PBCINO : 2b-0 METKtS
RBCEIVER: SC1NTEX IPR-1Z TIME DOMAIN
RX-TX TIMIND 2Mo ON 2Mo OFFpurrrec M IMDM SLICE *sTKANBHITTCH 8CINTREX IPC-8 ZM MATT
KRL RESOURCES CORP
OBRADOVICH GRID MACMURCHY TOWNSHIP
DRTE : JAN 1995 REF : L16S
SCRLE - l : 2500
RflYflN EXPLORRTION