royal oak mines inc semple-hutt prop 1994 assessment …
TRANSCRIPT
42A03SE0018 2 1S9O9 SEMPLE 010
ROYAL OAK MINES INC.
SEMPLE-HUTT PROPERTY
1994 ASSESSMENT REPORT
GEOPHYSICS
RECEIVED
MAR 2 41995
MINING LANDS BRANCH
09
i*' V
W4
P.G. Harvey 'Project GeologistEastern Canada Exploration
4 January 1995
42A03SE0018 2.15009 SEMPLE
CONTENTS01OC
l .0 Summary and Conclusions
2.0 Property Description, Location and Access
Figure l Location Map
Figure 2 Claim Map
Table l Claim List
3.0 Past Work and Geology
4.0 1994 Program
5.0 Conclusions and Recommendations
6.0 List of References
Statement of Qualifications
Page
l
1
2
3
4
5
5
6
6
Appendix Geophysical Report, Maps and I.P. Pseudo-Sections
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1.0 Summary and Conclusions
During December, 1994, Royal Oak Mines Inc. hired M.C. Exploration Services Inc. to complete 12.0 km of Time Domain Induced Polarization (I.P.) and Total Field Proton Precession Magnetic (T.F.M.) survey work on their Semple-Hutt property located about 62 km south of Timmins, Ontario.
This work was successfill in outlining several areas which responded favourably to the I.P. survey, and work to determine the cause of these I.P. responses, consisting of drilling and/or trenching, is warranted.
2.0 Property Description, Location and Access
The Semple-Hutt property consists of 42 claim units (672 ha) located about 62 km south of Timmins (Figure 1). These claims are within Semple and Hutt townships, and are listed in Table l and shown in Figure 2. The property is owned by Royal Oak Mines Inc., P.O. Bag 2010, Timmins, Ontario, P4N 7X7.
Road access to the property is provided by the Langmuir Road, originating in South Porcupine, to where H crosses Wicks Road (Hwy 566), which provides access to the northern portion of the property.
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SCALE 1:600,000
FIGURE 1: Location Map
WIC
KS
RO
AD
(56
6)
1176
551
: 11
7655
2
ROYA
L O
AK
MIN
ES I
NC
.
94-S
elec
ted
Line
a IP
8 M
ag S
urve
ys
SEM
PLE
- H
UTT
TW
PS, O
NT
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TABLE l
CLAIM LIST SEMPLE-HUTT PROPERTY
Claim Number Number of Units Township
935135935136935140935143935147935155935156935157935159935160935161 1917638 1917639 1
1159037 1115903911590361159038115904011590411159042115904311765501176551117655211765531176554117555511755561203717 (1204612 1
SempleSempleSempleSempleSempleSempleSempleSempleSempleSemple
1 Semple1 Semple1 Semple
SempleSempleHuttHuttHuttHuttHuttHuttHuttHuttHuttHuttHuttHuttHutt
'i Semple/Huttl Hutt
Total 42 units (672 ha)
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3.0 Past Work and Geology
Work in the area of the property dates back to 1958, when Jonsmhh Mines Ltd. exposed what is now called the Decker Showing, a series of gold-bearing quartz veins within deformed mafic volcanics. This showing is about 500 m west of the area covered by this report (Rg. 2).
In 1962, geophysical and geological surveys and 5,095 feet of drilling was done by Hollinger, covering the Semple-Hutt property, with work ibcussing on a pyritic graphite horizon near the small lake in the southern part of the property. Work between 1972 to 1979 consisted mainly of geophysical surveys, and three holes were drilled by Essex Minerals in the area covered by and surrounding the current property.
The Decker Showing was re-worked in 1986-1988 by Pamorex Minerals, who did an IP. survey, mapping, sampling, as well as drilling seven holes totalling 2,442 feet. Assay results from drilling were disappointing, as they were not as extensive as those from surface sampling.
The property was covered by the Ontario Department of Mines in Map 2291 (1968). The map indicates the bedrock of the property to consist of a sequence of mafic, intermediate and felsic volcanics which have been folded into an east-plunging syncline, which has been subsequently cross-folded.
In 1992, the property was mapped by Royal Oak Mines Inc.
4.0 1994 Program
Between December 5 and 20,1994, MG. Exploration Services Inc. (P.O. Box 362, Porcupine, Ontario, PON ICO) completed 12.0 km of I.P. and magnetometer survey work, which was supervised by Richard Daigle.
The details of this work are in the Appendix, in a report written by R. Daigle, along with the pertinent maps and pseudo-sections.
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5.0 Conclusions and Recommendations
As covered in the Geophysical Report (Appendix) several areas were outlined by the I.P. survey which require further work.
Possible near-surface sulphide mineralization occurs at Line O at (H-25S and Line O at S+75N, two areas that require testing by mechanical stripping.
The high chargeability on Line 2E at 7+OON requires drill testing.
Lower priority additional work includes drill testing of the mag and resistivity highs on Lines O to 3E north of the baseline.
6.0 List of References
Hogan, J. (1988) Pamorex Minerals Inc., 1987 Exploration Summary Report,Decker Property, Semple Township.
Londry, D. (1987) Report on Geophysical Work, Decker Property, SempleTownship.
O D M. Map 2291 (1968); Semple and Hutt Townships.
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STATEMENT OF QUALIFICATIONS
I, Peter G. Harvey, of the City of Timmins, Province of Ontario, do hereby certify that:
1 I received a B.Sc. degree (Honours) in Geology from Lakehead University, Thunder Bay, Ontario, in 1985.
2 I have been employed as a geologist by various mining companies in Ontario since 1985.
3 I am the author of this report.
4 I have no direct interest, nor do I have any shares of any company exploring the properties described in this report, nor on any adjacent or surrounding properties.
Dated this U th day of'^^ 1995, Timmins, Ontario.
V4/1/J
Peter G. Harvey Project Geologist Eastern Canada Exploration Royal Oak Mines Inc.
APPENDIX
Geophysical Report
Maps
I.P. Pseudo-Sections
Geophysical Agenda
Royal Oak Mines Inc. of Timmins, ON, completed 12 kilometers of Time Domain Induced Polarization Survey on the Semple-Hutt Property. M. C. Exploration Services Inc. ( MCX ) of Porcupine, ON, completed eight sections of IP survey using the Dipole Dipole Array reading n l to 6 with a Dipole Spacing "a" of 50 meters. Crews accessed the property travelling 70 km's south down the langmuir bush road out of Porcupine, ON. The fixed transmitter located along the Wicks road supplied power for all eight lines where crews started surveying line 300E then progressed westerly up to line 400W. LineslOOE, 0+00, 100W and 200W were problematical when crews attempted to achieve sufficient current for good penetration. Penetrating the high contact-resistance ( from 10 to 30 Kohm's ) involved using up to four grounding rods with a water-salt-copper sulfate solution to finaly lower the contact resistance for adequate penetration. Production was cut back by 50% until line 300W was reached. The IP survey statisics is included on the following page.
A Total Field Proton Precession Magnetic (TFM) Survey was then requested by Royal Oak and carried out by MCX on Dec. 19th, 1994. The EDA PPM-350 in conjunction with the EDA PPM-400 base station was used to cover the similar 12 km*s of NS grid lines. The detailed TFM survey read 970 stations and is leveled with a reference field of 57925nT's. The base station was located on tie line 1100N/ 150W. The TFM data range for the survey is from 57031 to 59969nT's with a mean of 58043nT's.
Equipment specifications and survey procedures are featured in the reports addendum.
The main objective of the geophysical program is to attempt to delineate a geological setting which may host auriferous quartz vein within intermediate to mafic metavolcanics. The showing developed by Pamourex in 1987-88 is assumed to strike near N70DegT. The showing is recognized with the following; minor conductivity where trenching revealed a zone of erratic quartz-calcite veining in silicified, carbonatized and sheared andesite with the quartz and adjacent wallrock well mineralized with disseminated to euthedral pyrite ( J. Hogan, 1988 Exploration Summary Report ). The mapped east plunging synclinal structure ( ODM map 2291 ) which in turn has been cross-folded onto itself will concern geophysical interpretations.
IP Survey Statistics
line No.
300E
200E
100E
0+00
100H
200W
300W
400W
————— 1
samples taken
153
153
148
146
150
150
149
150
.J. 196 t(
—17 samj
.10 sam]
chai
—Currei
Vp (mV's) min-mean-max
4.6-334-3064
6.6-210-1437
1.4-298-3589
1.1-942-32K
1.2-810-15K
2.9-809-24K
1.4-1627-24K
1.3-2514-27K
ttal stations
ties lost due
ties lost due
ineling along
it Electrode i
lg (Amps) min-mean-max
0.37-2.72-1.8
0.38-1.90-4.5
0.24-1.80-3.2
0.18-1.20-2.8
0.19-0.78-2.8
0.18-0.89-2.5
0.20-1.0-2.77
0.22-0.8-2.60
read
to high contc
to low resist:
strata condud
il way s on N en*
SP (mV's) min-mean-max
-104|-2|117
-254 |-7 |236
-304|-5|236
-415 |-6 |453
-3481-31486
-121|-5|112
-224 1-1 |221
-175 |-2 |200
ict resistance
Survey Direct
S
N
S
N
S
N
S
N
ti
ivity ( current
or )
of traverse-
Project: Semple-Hutt, DplDpl , 0=1 to 6 S a ~ 50m' s, Dec 94.
Vp; Primary Voltage lg; Induced Current
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owln
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1 i
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552
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es
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Mag
Sur
veys
SEM
PLE
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WPS
, ON
T
HU
TT T
WP.
SEM
PLE
TWP.
IP Section Evaluations
Line 300E is the first of eight lines read and has four separate anomalies. The first most southern anomaly is obscured ( off line ) and has a chargeability effect reaching 7 V/mV's with an apparent resistivity of 85 to 245 ohm's/ 50 meters. This characteristic implies sediments underlie the south segment of line 300E. The second IP anomaly from SON to 25ON with lower IP effects ( than the afore mentioned ), happens within a high apparent resistivity and is characteristic to possible ultramafic intrusive type rocks. The third IP anomaly at 700N with IP high and moderately low apparent resistivity happens along a postulated felsicXintermediate to mafic contact. The fourth IP anomaly is obscured to the north and implies probable sediment type rocks from SOON to 900N. The response over this limited segment correlates with mapped intermediate to mafic metavolcanics ( ODM map 2291 ) thus attributing the lower apparent resistivity to graphite content. Section 300E will be used as a guide to what may be expected on the remaining eight traverses.
The high apparent resistivity responses on the west portion of the grid are nearer to surface comparable to line 300E. This is conformable to the east plunging synclinal structure. The sections show anomalies dipping south from line 300W to line 200E, thus implying that the synclinal structure undertakes an upright tilt near line 100E. The IP high/ resistivity low running along the south limit of the survey implies a felsic/ intermediate to mafic contact runs near 200S across all the lines ( 4W to 3E ). A similar contact runs from line 400W/ 875N to line 0/875N, then takes a sinuous trend crossing line 100E/800N and then line O again at 375N and is traceable up to line 200W to then become confined. This occurs in conjunction with the mapped cross-fold seen on ODM map 2291. The broad high IP effects at the north limit of line 300E implies this line runs along strike. Another along strike response is seen on line 400W where a prominent resistivity high occurs. A moderately high resistivity response interrupting the broad high postulates an ultramafic/volcanic contact. The abiding ultramafic ( ODM map 2291 ) on line 400W/50N agrees with the IP survey and is then projected easterly across the grid. The classical IP effect seen on lines 300E and 200E with associated apparent resistivity response infers an intruding ultramafic unit with an upright tilt. Several intense high apparent resistivities due to near surface ( or outcrop ) effects obscure the deeper n levels, these problematical areas occur as follows; L400W/ 100S to SOON, L300W/ SON to 550N, L200W/ 100N S SOON to 700N, L100W/ 150N Si 550N to 700N and LO/ 125N fie GOON to 700N. Two of these surface effects have corresponding significant IP effects located on line O at 25S and 575N. Other similar near surface targets occur on lines 100W/ 25N 6. 525N and 200W/ 25N S 475N 6 700N. The near surface high IP effect on line 300W/ 75S happens with a lower apparent resistivity implying a target within intermediate to mafic metavolcanics.
Magnetic Evaluation
The magnetic results on Plan l are contoured at a 50 nanoTesla interval and show discontinuous trends. A broad high magnetic susceptibility reaching 1398 nT's intruding from the west ( line O from 300N to 600N ) up to line O occurs in conjunction with a high resistivity/ chargeability anomaly which infers a probable ultramafic unit. Two narrower high magnetic trends intruding from the west also happen on line 400W at 125S and SON, the northern high mag at SON correlates with mapped ultramafic unit seen on ODM map 2291. These highs then take a sinuous SE trend and become diffused. The most north weak twin highs from line 100E to line 300E associated with high resistivity and chargeability infer that a probable ultramafic unit follows this sinuous trend. The weak high magnetic anomaly seen on line O at 150S implies probable sulfide mineralization. The two mag lows seen on line O from 525N to 450N and SON to SOS perhaps reflect alteration, however are likely dipole effects from the flanking mag highs. The high mag reaching beyond 1900 nT's above background seen at the north limit of line 300W correlates with the mag high mapped by D. Londry ( 1987 Geophysical Report ). This high magnetic trend was then associated with variable concentrations of disseminated magnetite appearing to confirm a localized, tight fold in the area of the main zone.
Implications
The IP survey delineates several targets of significance where further testing is warranted. The near surface effects can perhaps be investigated by stripping. Two prominent key areas suggesting near surface sulfide mineralization are as follows; Line 0/25S and Line 0/575N. Both of these targets are traceable on line 100W and happen near surface. The IP high resistivity low on line 200E at 700N merits drill testing, however it can perhaps be correlated with the near surface anomaly seen on line O at 575N. Drill testing of the mag, IP, and resistivity highs trending across lines O to 300E north of the baseline would confirm the source of the intrusive unit.
Recommending more TEM survey be done on the target area in an EW direction at 100m intervals. This type survey can be done on compass orientated lines and tied into existing cut lines. The mag and IP targets seen at the north limit of the gridded area are problematical and warrant further investigation.
R. J. Daigle. Dec. 27, 1994.
I, Richard Daigle of Timmins, Ontario
Certify
1. Three years of BLEM (max-min) evaluation under the supervision of Mr. J. Betz ( 1979 - 1981 ).
2. Five years conducting, evaluating Geophysical surveys for Kidd Creek Mines Ltd under supervision of Mr. D. Londry (1981 - 1985 ).
3 Six years contracting various geophysical surveys in Bathurst, N.B. ( 1986 - 1991 ).
4. Third year as geophysical evaluator for M. C. Exploration Services Inc., Timmins Ontario.
6. I have no direct interest in the property reported upon.
Timmins, Ontario. M// R. J. Daigle
SURVEY PROCEDURE
MAGNETICS
Theory;
The magnetic method is based on measuring alteration in the
shape and magnitude of the earth's naturally occurring magnetic
field caused by changes in the magnetization of the rocks in the
earth.
These changes in magnetization are due mainly to the
presence of the magnetic minerals, of which the most common is
magnetite, and to a lesser extent ilmenite, pyrrhotite, and some
less common minerals.
Magnetic anomalies in the earth's field are caused by
changes in two types of magnetization: induced and remanent
(permanent). Induced magnetization is caused by the magnetic
field being altered and enhanced by increases in the magnetic
susceptibility of the rocks, which is a function of the
concentration of the magnetic minerals.
Remanent magnetism is independent of the earth's magnetic
field, and is the permanent magnetization of the magnetic
particles (magnetite, etc. ) in the rocks. This is created when
these particles orient themselves parallel to the ambient field
when cooling. This magnetization may not be in the same
direction as the present earth's field, due to changes in the
orientation of the rock or the field.
The most common method of measuring the total magnetic
field in ground exploration is with a proton precession
magnetometer. This device measures the effect of the magnetic
field on the magnetic dipole of hydrogen protons. This dipole
is caused by the "spin" of the proton, and in a magnetometer
these dipoles in a sample of hydrogen-rich fluid are oriented
parallel to a magnetic field applied by an electric coil
surrounding the sample. After this magnetic field is removed,
the dipoles begin to precess (wobble) around their orientation
under the influence of the ambient earth's magnetic field. The
frequency of this precession is proportional to the earth's
magnetic field intensity.
Field Method:
The magnetics data was collected with an EDA PPM 350 proton
procession magnetometer, which measures the absolute value of
the earth's magnetic field to an accuracy of */- l gammas. The
magnetometer was carried down the survey line by a single
operator, with the sensor mounted on an aluminum pole to remove
it from any surface geologic noise. Readings were taken at
12.5m intervals.
The readings were corrected for changes in the earth ' s
total field (diurnal drift) with an EDA PPM 400 base station
magnetometer, which recorded readings every 30 seconds as the*
survey was being conducted. The data from both magnetometers
was then dumped with a computer and base corrected values were
computed.
II
l
3
The PPM-350 is the latest addition to EDA's OMNIMAG* series of magnetometers and gradiometer. It is engineered to provide users with the latest state-of-the-art advances in microprocessor technology, including many features that are unique in the field.
Major benefits and features Include:* Significant increase in productivity* Lowered survey costs* Automatic diurnal correction* Programmable grid coordinates* Highly reproduceable data* Ergonomic design* Simplified fieldwork* Computer-compatible
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Specificationsl^ynamic Range. -.................. -... .18.000 to 110.000 gammas. RoHover display feature
. suppresses first significant digit upon exceeding 100.000 i * gammas.
Tuning Method........................ .Tuning value is calculated accurately utilizing a speciallydeveloped tuning algorithm
automatic Hne Tuning. ..................± 1596 relative to ambient field strength of last storedvalue
Display Resolution...................... .0,1 gamma ocesslng Sensitivity............. --...... 0.02 gamma
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Toh }e^nl Error Resolution................ 0.01 gamma
Absolute Accuracy . .....................± 1 gamma at 50.000 gammas at 230C12 gamma over total temperature range
tandard Memory Capacity ^ Total Field or Gradient................ .1.200 data blocks or sets of readingsP Tie-line Points....................... .100 data blocks or sets of readingsl Base Station......................... .5.000 data blocks or sets of readingsiSfcplay............... -.... - -..... -.... Custom-designed, ruggedized liquid crystal display with an
operating temperature range from -400C to * 550C. The display contains six numeric digits, decimal point, battery status monitor, signal decay rate and signal amplitude monitor and function descriptors.
JS 232 Serial I/O interface................ .2400baud. 8 data bits. 2 stop bits, no parityGradient Tolerance..................... .6.000 gammas per meter (field proven)
........................... .A. Diagnostic testing Idata and programmable memory)B. Self Test (hardware)
........................... .Optimized miniature design. Magnetic cleanliness isconsistent with the specified absolute accuracy.
Gradient Sensors ...................... .0.5 meter sensor separation (standard), normalized togammas/meter, optional 1.0 meter sensor separation
D avaMable. Horizontal sensors optional, ensor Cable ...................... -... -Remains flexible In temperature range specified. Includes
strairtrelief connector ^cllng Time (Base Station Mode) ..........Programmable from 5 seconds up to 60 minutes in 1
E second increments )peratlng Environmental Range........... -40-C to * 550C: 0-10096 relative humidity; weatherproofsower Supply .......................... Non-magnetic rechargeable sealed lead-acid battery
J. . cartridge or belt rechargeable NiCad or Disposable battery H cnrtrkkje or belt; or 12V DC power source option for b.nse l station operation. Battery cartridge/Belt Life................ 2.000 to 5.000 readings, for sealed lead acid power supply.
\, depending upon ambient temperature and rate of p readings j^yvelghts and Dimensions
f; instrument Console Only............... .2.8 kg. 238 x 150 x 250mmNICad or Alkanne Battery cartridge...... .1.2 kg. 235 x 105 x 90mmNlCad or Alkaline Battery Belt............1.2 kg. 540 x 100 x 40mmLead^Add Battery cartridge............ .1.8 kg. 235 x 105 x 90mmLead-Add Battery Belt................. 1.8 kg. 540 x I00x40mmSensor .............................. 1.2kg. 56mm diameter x 200mmGrddicnt Sensor O.Smseparation-standard)............ 2.1 kg. 56mm diameter x 790mm
^ Gradient Sensor*~ (LOmseparation-optionaO............. 2.2 kg. 56mm diameter x 1300mm
jndard System Complement............ Instrument console; sensor; 3-meter cable, aluminumsectional sensor staff, power supply, harness assembly, operations manual.
Base Station Option................... .Standard system plus 30 meter cableGradiometer Option .................. .Standard system plus 0.5 meter sensor
EDAmstnimentsinc. 4 Thomcfiffe Park Drive Toronto. Ontario Canada MJH1H1 Telex 06 23222 EDA TOR CiDte: mstrumcnts Toronto (41614257800
InU.SAE O A instruments me.5151 Ward Roadwheat Ridge. ColoradoUS A 80053(305)4229112
INDDCED POLARIZATION SURVEY
The Time Domain Method for Measuring IP
There are two basic systems or methods for the measurement of IP:
a) Frequency Domainb) Time Domain
In this'lecture we shall discuss the Time Domain method, its advantages and limitations.
The phenomena of induced polarization was reported in the literature as early as 1920 by Schlumberger. However, modern development of the method in the U.S. are generally dated to Bleil (1953). Khen a steady-state current into the earth is interrupted, it is observed that the voltage monitored at some point in the vicinity of the electrode generally does not immediately drop to zero. Instead, the voltage drops to some voltage V and thereafter decays with the time toward zero (see Figure 1).
CURRENT INTERRUPTION
Vc(t)
oo 00
FIGURE 1: Seheiiitle^lllustratlon of the transient type
The decay voltage or transient voltage indicates that the earth's resistivity is not simply resistive, but also has a reactive term too. The earth's resistivity is in general complex and might better be called an imped i vi ty. The term complex resistivity is more frequently being invoked to describe the total nature of the earth's resistivity. Modern time domain or transient techniques for measuring IP have developed from this very simple method of observing the IP response. A measure of the IP response, called CHARGEABILITY (M), is simply the amplitude of the secondary or decay voltage Vs (t) relative to the amplitude of the steady state voltage measured Vp while the current was on (see Figure 1).
The secondary voltage is usually much smaller then the primary voltage, so it is usual to express the secondary voltage in units of millivolts while retaining the units of volts for the primary voltage. Thus, the units of IP as measured using a pulse transient technique are often given a s mv/V. If the secondary voltage and the primary voltage are expressed in the same units, their ratio (i.e. Vs/Vp) is a dimensionJess fraction. Sometimes, therefore, the IP response (chargeability) will be expressed as a percent.
The definition of chargeability as suggested in Figure l indicates that it is a .function of time. Thus, there are an infinite number of possibilities for the definition of a single parameter which characterizes the measured chargeability or IP response. Much of the ongoing IP research today is centered around studying the total decay curve or, equivalently, the frequency spectra of the IP response, to determine additional information pertaining to the nature of the source of the IP response.
Modern time domain IP surveying instrumentation provides an efficient way of periodically repeating the experiment described in Figure 1. The time domain transmitter periodically pulses the current circuit. In addition, it com/nutates the polarity of the pulses. The transmitter waveform is illustrated in Figure 2. It is standard practice for the current ON time to be equal to the current OFF time. The ratio of the current ON time to the fundamental repetition period of the transmitter is often called the DUTY CYCLE and therefore when current on time equals the current off time the transmitter has a 50 percent duty cycle. An 8 sec repetition period (0.125Hz) and a 50 percent duty cycle is the most common IP transmitter waveform. However, there are some transmitters available for which both the duty cycle and the fundamental period can be varied.
II
PRIMARY TRANSMITTER WAVEFORM
SECONDARY VOLTAGE WAVEFORM
DEFINITION OF NEWMONT IP PARAMETERS 'M 1 a 'L 1
FIGURE 2: Definition of the Neumt IP Parameters t" and -M*.
Standard Definitions for Chargeability (M)
Figure l suggests that the IP parameter, chargeability varies with time and so it does. However r for practical reasons the entire decay curve is generally not sampled. Instead, the secondary voltage is sampled one or more times at various interals.
Because the secondary voltage is received at extremely low levels in many prospecting situations, measurements of its amplitude at any given time is extremely susceptible to noise. Therefore, the secondary voltage is usually integrated for a period of time called a gate. Thus, if the noise has a zero mean, the integration will tend to cancel the noise. Figure 2 illustrates the "Newmonf gates. The Newmont M factor is a standard time domain IP parameter throughout North America. The gate delay (i.e. the time after current interruption before integration starts), 0.45 sec was chosen to allow enough time for normal electromagnetic effects and any capacitive coupling effects between the transmitter and receiver to attenuate so that the secondary voltage consists only of the IP decay voltage.
Ill
In many, but not all, prospecting situations, the 450 msec delay before integration is sufficient time for any electromagnetic effects to have decayed away. The gate width is arbitrary but it is generally chosen to be an integral multiple of 60 Hz periods (i.e. 16.7 msec) so that the effect of 60 Hz noise is cancelled in the integration. The Newmont M gate width is 39 periods long while the L parameter is 78 periods long. The Newmont L factor as defined in Figure l is a parameter which helps to signal the presence of anomalous decay curve shape. The ratio of L to M (i.e. L/M) is unity whenever a typical IP decay curve is encountered. When L/M departs significantly from unity in a prospecting situation, the presence of EM coupling is strongly indicated. The reader is referred to Swift (1973) for an analysis of this parameter.
Multiple Gate Time Domain Receivers
The foregoing discussion suggests that there is more information in a time-domain decay curve than a simple chargeability. Indeed, contemporary research in the IP method is now directed toward an analysis of the entire waveform. In order to obtain more information on the decay curve shape, most IP instrument manufacturers make a receiver which is capable of measuring more than one gate along the transient. Figure 3 schematically illustrates one-half of a time domain waveform and 4 arbitrary along the secondary voltage. The gate definitions are arbitrary, subject only to practical considerations mentioned earlier. However, the gates which are farther out in the decay curve necessarily must integrate a signal of much lower amplitude. As a result, it is usual to increase the gate widths by some multiple of the first gate width. Figure 3 suggests a binary increase in the width. Some instruments choose the gate widths and calibration constants so that whenever a decay curve having the standard shape of an IP response is measured, the chargeabilities measured at each gate are the same.
FIGURE 3: Figure 3. typical chargeability gate definition on a Miti gate tlae doBiln IP receiver.
Pole Dipole Array
The use of the Pole Dipole array i s much Jess common then the Dipole Dipole array but it has distinct advantages. The most notable advantage is the much stronger current density obtained from the single current pole on the traverse. This results in the strongest potential voltage measurable from any of the arrays. This stronger signal to noise permits operation in noisier areas and areas of thicker overburden.
This array is set up similar to that of the Dipole Dipole array except that one current electrode is fixed at geometric infinity or lOa ( 10 times the potential dipole ) across strike. The plot point is mid way between the on line current and the centre of the potential electrodes.
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lil Ol "l 02 MS Oj Us
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ADVANTAGES
1. Good SP rejection. The strong signal to noise ratio effectively eliminates the SP effect*2. Not susceptible to "masking" effects. This is the recommended array in areas of conductive overburden.3. A fairly sensitive and selective array.4. Returns highest Vp of all arrays. Hence it is ideal for work in noisy areas.5. Relatively faster than Dipole Dipole.6. Low inductive coupling.
DISADVANTAGES
1. Asymmetrical response - peak is only over the source when the spacing "a" is less than the depth of investigation. There will occur a double peak with the stronger of the two on the current side of the potential. This requires that moving current be always kept in the same relative position to the measuring dipole.2. Requires communication between current on line and transmitter.
SIX DIPOLE TIME DOMAIN IP RECEIVERThe TDR-6 induced polarization receiver is a highly cost-effective instrument far me detailed measurements of induced polarization and resistivity phe nomenon. Up to six dipoles can be measured simultaneously, tfuis increasing survey production.
A wide input voltage range, up to 30V, simplifies surveys over the narrow shadow conductors of large resistivity contrast. Input signal indicators are provided far eoch dipole. AB date are displayed on a 2 x 16 character LCD module and any selected parameters can be monitored on a sepoiuJe analogue meter tor noise valuation during (he stacking/averaging.
Ahhough me TDR-6 receiver is automatic tt alaws ful control and convnu-fwt^^v^bu' f fjt •IflvkA* L mrlnn MKopvwo* of CM nines during m
Smxe the nput siyiiuJ synchronizes vie receiver at eoui cycle, the transmit ter liming stability is not critical and any standard time domain transmitter can be used.
Data are stored in internal memory with a capacity of up to 2700 readings ie.. 450 stations. The dab formal b directly compatible wHh me GEOSOR IP Halting System without me necessity of on instrument conversion program.
FEATURES
JWide input signal range
jutomohc self-potential cancellation
Stocking/averaging of Vp and M tor high measurement accuracy in noisy environments
High rejection of power line interference
Continuity resistance test
Switch selectable delay ana integration time
MuhSwindow chargeability measurements
Digital output tor data logger
1 Six channel input provided
1 Compatible wHh standard time domain transmitters
1 Alpha-numeric LCD display
' Audio indicator tor automatic SP compensation
SPECIFICATIONS
Dipole*Input Impedancehput VaEagT (VP)
-accuracy-resolution
Se* Potential (SP) -range-accuracy
Automatic SP Compensation Charaeobfey (M) -range
-occufucy-resolution
Automatic Stacking May IWIntonation Time (each gote) Tod OorgiW^ TimT^ SyncKfonifuliuii Signal Filtering - Power linn
^ -C*er mtornal Test Ground fciiiitonm Tert Transmitting Time
Controls - push bufen
- rotary- rotary
I/O part libility
Memor* CapocriyData Outo* i
-compatibi TvnpcnAm Rongt 'CpcralinQ
-fltoroQC Po-.^&ppr,Weight'0"1
l to 610 megohmlOOuV - 30V (outomafic).25110 microvolt±2.0 vohIt 1.0 ve*SOOmV/V.251.1 mV/V2to32cydesProgrammablePiogi unuimbleDuring integration lime fer at gatesFrom channel l or 6Dual Natch 60/180 Hz or 50/150 Hz. 100 dBAnti-aba. RF and spie rejectionsVp - l vok.M-30 mV/VO - 200 k ohm1. 2. 4 and 8 SK. pulse duration ON/OFFl . J J B;-.. AnnLn'rL iljtjLl lll'H l liimnooro nine uumum waranm^*|Two Knes 16 abhanumeric LCDSix - monitoring input signal and courseresistance testingResetStart-StopRs-tM^fedDisplayDipole16key-4x42700 reodmm (450 stations at 6 azotes)RS232C baud rate programmableGE060FT P System-SOXto+SOK-401Cto*o01C Four 1.5V DaJU31xl6x29cm|lZ25x6.25x11^in.) 6^ kg (14.3 bs)
A ANDROTEX LIMITEDGEOPHYSICAL INSTRUMEWiS 16) 677^9i9 i^ CANADA
* -- ~M - .*"^*K^- .
Figure 2The TSQ-3 Transmitter and Motor-Generator Set
Tine Domain: T * 1,2.4 or 8 seconds, switch selectable
-T-H
Frequency Domain: T - ^ and f - 0.1, 0.3, 1.0 or 3.0 Hz.f
H—T-
Figure 3The TSQ-3 Output ^veforms
The Motor-Generator Set consists of a reliable Briggs and Stratton
four stroke engine, coupled to a brushless permanent aagnet alter
nator. The transmitter design employs solid-state components both
for pouer switching and control circuits. Output waveforms and
frequencies are switch selectable; square wave continuous for
frequency domain and square wave Interrupted for time domain. The
programmer Is crystal controlled for high stability. While care
still must be taken when working with high voltages, the TSQ-3
features overload, underload and thermal protection for maximum
safety. Stabilization circuitry ensures that the output current
is automatically controlled to within 0.1Z for up to 20Z external
load or 10Z Input voltage variations. Voltage, current and
circuit resistance are presented on a LED digital display.
Basically, the Motor-Generator and Transmitter function as
follows. The motor turns the generator (alternator) which
produces 800 Hz, three phase, 230 V AC. This energy is trans
formed upwards according to a front panel voltage setting in a
large transformer housed in the TSQ-3. The resulting AC is then
rectified in a rectifier bridge. Commutator switches then control
the DC voltage output according to the waveform and frequency
selected.
2. TSQ-3 Transmitter Console ft Motor - Generator Specifications
Transmitter Console
Output Power 3000 VA maximum
Output Voltages 300, 400, 500, 600, 750, 900, 1050, 1200,
1350 and 1500 volts, switch selectable
Output Current 10 amperes maximum
Output Current Stability
Automatically controlled to within 0.12
for up to 20Z external load variation or
up to 10Z input voltage variations.
Stabilization Over- range Protection
High voltage shuts off automatically If the control range of 20Z is exceeded.
Digital Display Light emitting diodes permit display up to 1999 with variable decimal point; switch
selectable to read Input voltage, output
current, external circuit resistance, dual current range, switch selectable.
Current Reading Resolution
10 mA on coarse range (1-10A), l aA on fine range (0-2A)
Frequency Domain Vaveforn
Square wave, approximately 6Z off at each polarity change
Frequency Domain Standard: 0.1, 0.3, 1.0 and 3.0 Hz, switchselectable.Optional: any number of frequencies inrange 0.1 to 5 Hz.
Time Domain Cycle Timing
t:t:t:t; on:off:on:off: automatic
Time Domain Polarity Change
Each 2t; automatic
Time Domain Pulse Durations
Standard: t-1,2,4,8,16 and 32 seconds Optional: any other timings
Time and Frequency Stability
Crystal controlled to better than 0.1Z with external clock option better than 20 ppm over operating temperature range.
Efficiency .78
Operating Temperature Range
-300C to *50eC
Overload Protection Automatic shut-off at 3000 VA.
Underload Protection Automatic shut-off at current below 85 mA
Thermal Protection Automatic shut-off at internal temperature of 850C
Dimensions 350 x 530 mm x 320
Weight 25.0 kg
Motor-Generator
Type Motor flexibly coupled to alternator and installed on a frame with carrying handles.
Motor Briggs and Stratton, four stroke, 8 HP
Alternator Permanent magnet type, 800 Hz, threephase 230 V AC at full load.
Output Power 3500 V A maxim""
Dimensions 520 an x 715 m x 560 mm.
Weight 72.5 kg.
Total System
Shipping Weight 150 kg includes transmitter console, otor-generator, connecting cables and reusable wooden crates.
In Table l the maximum output current from the transmitter at certain values of load resistance is given for each position of the output voltage selector switch. The maximum load resistance limit occurs because of the built-in underload protection which shuts off the transmitter if the output is less than 85 mA. Figure 4 is a graph of output current vs voltage.
3. Theory of Operation
Power is supplied to the TSQ-3 transmitter through the alternator input connector from the three phase, 800 Hz alternator driven by {
a single cylinder, 4 stroke 8 HP engine. The main advantages of this brushless, permanent magnet alternator are: high efficiency, high overload capacity, short circuit immunity and minimum main tenance. The 10 m long input cable has four conductors, three for i
the three phases and the fourth to connect the alternator housing and the back pack to the TSQ-3 grounding lug. An additional grounding lug is provided on the mounting frame of the motor- generator which must be grounded as well. :
Figure 5 is a block diagram showing the basic function of the TSQ-3 transmitter.
Two of three input phases are sensed by the Overload Sensors. In case of an overload, the Protection Circuits open the solid-state Input Switches. The same action takes place if the output current drops below 85 mA, which is sensed by the Open Loop Sensor. If the current stabilization range of 20Z is exceeded, the Over-Range Sensor initiates the same action.
Ministry ofNorthern Developmentand Mines
Ontario
Report of Work Conducted After Recording Claim
Mining Act
42A03SE0018 2.15009 SEMPLE
Personal information cotected on this form is obtained untor the authority of the Mir this coSection ahould bo dtaodod to aw PIUVMUUI Manaijor. Minlno Landa. Mlnii Sudbury. Ontario. P3E 6A5. telephone (705) 670-7264.
Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for requirements of finny assbssmen
Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the., claims the work is assigned to. must accompany this form.
or900
,. jnny
Otoi6*4 fV/s/ 7X7
Telephone No. 340 '
Mining DMrion TowneMp/Area
-tloTTUorGPIenNo.H -1100
From: Ta 20Work Performed (Check One Work Group Only)
WorkGroup
S Geotechnical Survey
Physical Work. Including Dnlhng
Rehabilitation
Other Authorized Work
Assays
Assignment from Reserve
Type
{•ftoflLfS't+t Z*r**f - Z.fi *Ji Hy
RECEIVED
— MH 3 4 1:335 —
MIMNS i.AN:JS BR^MCM
Total Assessment Work Claimed on the Attached Statement of Costs
Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded holder cannot verify expenditures claimed In the statement of costs within 30 days of a request for verification.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)
Name Address
iUtu f/MU) fa , M ft*nti\\.C. Se/vici* live-. a*.
(attach a schedule H
tt^M^Jlni^l irij m m\m mt * C^^ Eifi*a fcl 4 **n ——--—-^^ ^B-a nenenciai imeresi see note NO. i on reverse srae
l certify that at the tbm Ilw i oowBred In thto wortc l hi ilw currant holder's ram or Md under a banefcW Internal
by the currant recanted hohtar.
(Sgnrtura)
Certification of Work Reportl certify that l have a personal knowledge of the tacts set forth in ttite wo* report, ra^ performed tte its completion and annexed report to true.
i during and/or after
Name and Address of Person Certifying
For Offlce Use OnlyTotal Value Gr. Recorded
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Credits you are claiming in this repon which daims you wish to priorize ttw1. D Credits are to be cut back st 2. PT Credits are to be cut back ei 3. D Credits are to be cut back as
In the event that you have not speci
Hotel: Ei to
Note 2: H
lamplesof
tmr- 1-iy uec
arting witli qually ovei t priorized
Red your c
work has been performedlor
vei
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ut back. In order to minimize the ac of credits. Please mark (•J one oti the claim listed last, working bac r all daims contained in this report on the attached appendix.
shoice of priority, option one will b
Iverse effects F the followingkwards. of work.
0 implement*
of such deletions, please indicate from:
V
i.
iMnofeViduin of 80roont0ntSf 010** wttn rospoct
t
1*
(tented or leased land, please complete the following:
1 certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.
Signature Date
Ministry ofNorthern Development
OntarioMinisteredu Devetoppomont du Nord el des mines
Statement of Costs for Assessment Credit
Etat des coOts aux fins du credit devaluation
Mining Act/Loi wr les mines
Transaction NoJN* da transaction
Pet it information coBected on this form is obtained under the authority of the MMng Act TMs information wM be used to maintain a record and ongoing status of the mining daim(s). Questions about this collection should be directed to the Provincial Manager. MMngs Lands. Ministry of Northern Development and Mines. 4th ROOT. 158 Cedar Street. Sudbury. Ontario P3E 6A5. tetophone (705) 670-7264.
Las renseignements poreonnsli contemn dans la presenta formufe sont racuolBgenvertudelaljolsiirfesailnssetaervlrortatBnlraiourunregistre des concessions minieres. Adresear toute questton sur la coiece de ces rensBMjnements au chef provincial daa terrains miniars. mlnisisro du DeVBtoppement du Nord el des Mines. 159. nw Cedar. 4e etage. Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.
1. Direct Coats/Coots directs
Type
Contractor** and Conauttanf a
Plotted*
et de I'expart-
Suppiaa Ueed
Equipment RentalLocution ds)
Labour Main-d'oeuvreField Supervision Supervision sur to terrain
type
Typa
Typa
Amount Montant
Totals Total global
2. Indirect Costs/Gouts Indlracts** Note: When ctoJming RehabMation work Indbecti Bis are not
Pour to remboursemant des travaux de rehabMatton. les cools indbeds ne eont pee admtssMes en tent qua travaux devaluation.
lo. no'
Total Direct Costs Total dee coot* directs
Type
FOOQ 4WIOLodging Nounftureet
Typa
WAR 2 41SS5
3j.A^-.;S HRAi ICH J
Amount Montant
i
afUa(n
Sub Total of Indirect Coste Total partial dee coots Indlracts
hen 20* of Direct Coats)pw 20 9t QM 4**^4MsV obvcts]
Total Value of t (ToMafDincti
Totals Total global
10,JIO'
Note: The recorded holder wii be required to verify expendttures claimed in this statement of costs within 30 days of a request for verification. H verification is not made, the Minister may reject for i all or part of the assessment work submitted.
Note : LeUtutaireenregistrAseratemi de verifier tas cto present etat des coots dans lea 30 Jours auivant une demande a eel 0ffet.Silaverificao^n'estpe8effectuea.lemUiistrapeutreietertout ou une parfe des travaux d'evatuatkm preaenlaa.
Hllng Discounts Remises pour depot
1. Work filed within two years of completion is claimed at lOtWb of the above Total Value of Assessment Credit.
1. Les travaux deposes dans tos deux ans suivant tour acheveimnt sont remtnureasalOOttdetavaleura^auvmntianritedu
2. Work filed three, four or five years after completion is claimed at SOT* of the above Total Value of Assessment Credit See calculations below:
2. L^ travaux deposes bois, quatreoudiu} ans apreskwrachevernerrt sont rembourses a 50 to de la valaur totals du credit d'evatuation susmentionne. Voir toe caJculs oMeasous.
Total Value of t :Credtt
x 0.50
Valaur du crMt d'*valua0on
X 0.50 -
Certlflcation Verifying Statement of Coste Attestation de I'etet dee coOts
l hereby certify.that the amounts shown are as accurate as pi siUe dtheswere incurred white conducting assessment work on the lands shown on the accompanying Report of Work form.
O - J l^ieeT t**-f*j^i _ l am authorizedthat as ito *
Hoktor . Agent Position(Recanted Hoktor. Agant. l
to make this certification
in Company)
J'atteste par la prteente :que'les montants indiques sont to plus exact possible-et que ces depsnses ont ete engagees pour effectuer les travaux d'evaluatJon sur tos terrains indiques dans la formute de rapport de travail cHoint
Et qu'a tJtre de _____(ftutaato enragistnft. i^vtosntsVst, povto oocupA
a faire cette attestation.
.jesuisautorise la oompagnia)
0212 (04/81) Nota: Dana oatta tormula. toraqu'H dteigne daa i Via maacuBn eat utaM au sens nautre.
OntarioMinistry ofNorthern Developmentand Mines
Ministere du Developpement du Nord et des Mines
Geoscience Approvals Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5
Our File: 2.15909 Transaction /: W9560.00001
March 28, 1995Telephone: Fax:
(705) 670-5853 (705) 670-5863
Mining RecorderMinistry of Northern Development fc Mines60 Wilson Avenue1st FloorTimmins, OntarioP4N 2S7
Dear Sir:
Subject: APPROVAL OF A881 WORK CREDITS OH MINING CLAIMSP.935159 ET AL IM SEMPLE AMD HUTT TOWNSHIPS
Assessment work credits have been approved as outlined on the original report of work. The credits have been approved under Section 14, Geophysics, Mining Act Regulations.
The approval date is March 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/J1 closure:
cc: Resident Geologist Timmins, Ontario
/Assessment Files Library Sudbury, Ontario
Royal OakMines Inc.
Eastern Canada Exploration Division P.O. Bag 2010 Timmins. Ontarin MN 7X7
Tel (71)5)360-1141 Kiv (715)360-1:32
l August 1994
Ontario Mining Recorder's OfficesMinistry of Northern Development and Mines
2.15909
RE: Authorization of Paul Coad, Richard Labine, Peter Harvey, Reno Pressacco and/orDiane Carter to act as agent for Royal Oak Mines Inc. when dealing with the
____submission of work reports-^——^^—^^^——^^—^-^—^^^—^^^—^—^^-^—
Tfiis is to certify that Paul Coad, Richard Labine, Peter Harvey, Reno Pressacco and/or Diane Carter are authorized to act as agents for Royal Oak Mines Inc. for the purpose of tiling assessment work credits and their distribution for a period of one (1) year or until further notice.
Yours truly,
ROYAL OAK MINES INC.
Ross F. BurnsVice President, Exploration
RFB/lha
RECEIVED
MAR 2 41995
MINING LANDS C RAriCH |
Royal Oak Mines Inc. is listed on the American and Toronto Stock Exdianges - Symbol RtflO
THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED 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
ZAVITZ TWP.
90Mp r r r r r1177362 l 1177381/4 1177374 l M77694 l II77SOI , II77SO8
! /! ' l l J* 4- ^1^1177810
l .rf*^jllV809r—r--fjr-\7T-\iI7730S
|| l I2046ia M 28943
. ~ - -p-
. JIY ill773?l |(I773IB l M77J96(10 UNITS) fl)^ ______|^___i^ l l
l' IF/!,-. N/7320 j M7MI9 iiirrsw 1117738* i\ i w 11177377 i
-,. ^.
l "379 11773161177396 1177
(16 UNITS)
1131)041 1176*10 l H7633I . II7833E
I823571182356
1182355
de UNITS)
. J H6704* l l li. l l,I76S8S l 1 176884 \T~" \~ ~ ~"
——l l /l1153691 1 )670*1' i
T i' r1133137 f 1,3,091 l 1131096 l H33I36 | II39IS3 f
l 11 j
13818* j IISI090 j 113*093
^ l j___J___J___ -U, ^____(
200
HALLIDAY TWP.
LEGEND
HIGHWAY ANO ROUTF No OTHER ROADS TRAILS SURVEYED LINES
TOWNSHIPS, BASE LINES, 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 i SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT
i i i i-fefc
DISPOSITION OF CROWN LANDS
TYPE OF DOCUMENT
PATENT. SURFACE ft MINING RIGHTS , SURFACE RIGHTS ONLY...,. , MINING RIGHTS ONLY .....
LEASE. SURFACE fc MINING RIGHTS- " .SURFACE RIGHTS ONLY.. . " .MINING RIGHTS ONLY..........
LICENCE OF OCCUPATION .._....,...ORDER IN COUNCIL ........^.........RESERVATION .......... . .... ..CAI^CiLLED .- .
SYMBOL
e d
... B
... a-. T . OC
Tllia TW19 aUBueCT TO PUREST ML 11 VI l f
SCALE 1 INCH - 40 CHAI
ttt Tn loon 4000 60OO 80
O J 60 METHtS
1000l l KM)
3000(2 KM l
© THI5 TWP IS SUBJECT TO FORtSl ACTIVITY IN I39S/96 f urt men INFORMATION AVAiiAait ON ut i
TOWNSHIP
HUTTMN.R AOMINISTRl'
TIMMINSMINING DIVISION
PORCUPINELAND TITLES/ REGISTR
SUDBURY
-r V"" [(f'CL
lli
! ' - 199)
.; uiVijioN
RECEIVED
MAR 2 41995DIVISION
MINING LANDS BRAMCU
Ministry ofNaturalResources
Ministry ofNorthern Developmentand Mines
Ontario
0*1*JUNE, 1992
A( TIVATEP JULY IB, ISBZMY DC
MY O W,
Numbui
G -3948
lOJip OD
ol
0410
o o
UJ
.0
ro
THF INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCr.S AND ACCURACY IS NOT GUARANTEED THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON BULT WITH THE MINING RECORDER MINISTRY OF NORTHERN DEVELOP Mf NT AND MINtS FOR AD DITIONAI. INFORMATION ON THE STATUS OF THE l ANOS SHOWN HFREON
o
ENGLISH TWP. M'787
GO 10iio: LUo
l
SOTHMAN TWP. M-II2I
NOTES
400' surface rights reservation along the shores of all lakes and rivers.
ut
m/95TO.y -
Ai eas withdrawn fruni staKing jnder Section 43
.t the Mining Act(R S O 19/0)
Order File
(Ri) wit / r i 18*60
Date Disposition
10/4/7* SMO
MINING AND SURFACE: RIGHTS WITHDRAWN FROMt-KOJKL.riNG, ^TAKING OUT. SALE OR LEASE IVJDf K SECTION 35 ^ THE MINING ACT R.S.O 1990 Ohtr. i n^ W -r 4-t- J4 NCR DATED 94-MAY-02
'fcD AKPI'. /4. I9UO PC
LEGEND
PR SURf ACt RIGHTS ONLY LEASE
LICENSE OFbCCUPATION
CROWN LAND SALES
LOCATED LAND
CANCELLED
MINING RIGHTS ONLY
SURFACE RIGHTS ONLY
HIGHWAY 4 ROUTE NO.
ROADS
TRAILS
RAILWAYS
POWER LINES
MARSH OR MUSKEG
MINES
)Of•*a*
2.159
TOWNSHIP OF
SEDISTRICT OFS
PORCUPINEMINING DIVISION
SCALE : 1 INCH - 40 CHAINS (1/2 MILE)DR. R W NOBLf
PLAN NO-j | 00
ONTARIODEPARTMENT OF MINES AND NORTHERN AFFAIRS
210
O O
B
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c J
l l l l l l l l J i l J
r j
FL 1100 N
BASELINE
c t (]l f- i* Id Mn') t \( t K ' rnl r. ur ri58000nT Base Subtracted
l, '.O nl interval, '. 7 O b O - r y50 nl' 1 -P'-n 1.
H( n ', 10f- n l Interval. ', 7800 - r,9800 nl'--t'rri '., '.00 nl Ir.tfrval, '-8000 -S9hOO nf-,
3L.6 "tatir,n,1 l OON/ I'.OW, S/y^Snl kf:( Md9/0 'jurvfypH ritotir,n , M. an ')84^nl'5
btiO'lfinl to M'^'K-'n! Mrignrtir K'nriqe.
IN'.IRUMLNI'.
OMNI IV PPM '',0, pr.rtoblt unit OMNI IV PPM 400, base station unit
PLAN l RECEIVED
MAR 2 41995
"cole 1-5000 .0 o___'in irm__isn 200
(meters)
i 2.15909
220
ROYAL OAK Mines Inc.Magnetic T.jrvey
Semple Hutt Chim Croupnip*: V Mutt Iwp ,. M!',: H l'
l Joh,upio,' Mining l)ivi .ionM i Lxploruti^n Ajrvi'.f;.. Iri'. DI;'. I'J'J4
JW
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CD CD
C JoCN- J
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CD
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CD CD
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l i l l i l
CD ro
BASEL INL
Interpreted Contact
Mag High
Mag Low
IP Interpreted Anomaly
o0)
H *- (U
n(SI(S)O)
(Y
2.15909
Anomaly Classification
l low FffectPoorly Chargeable mV/V. IP effect Low Apparent Resistivity, rho
.: ' '] Moderately Low Lffect
Moderately High fffeU
High tffectGood Chargeability mV/V. IP effectHigh Apparent Resistivity, rho
Dipole Dipole n---1 to G. a^
Array
Scale 1:H50 100
rRgCEIVED
000
Royal Oak Inc.1994 Compilation MapSemple- Hutt Claim Group
SernplK K Hutt l wps NIS4I r'/NW
Porcupine Minincj Divr.ionM. C Lxplorutiori ServK.nta Ini. [ )tn. 1 9'J4
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IP RES MF 21, 68K., 244
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Interpretation
Chargeability mV/V
Interpretation
Resistivity ohm/meters
Interpretation
Metal Factorip/rei * 1000
- -r -~ r - r - r — r - i t - T - r i T - r - T - i i i T - i T'? i - i t i T i - T T - 1 - r i r - i i i i t i i i i i r i i i i i i i i
\\
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o n
filter0=1
0.4
0=6
filter0=1
0=2
0=3
0=4
0=5
o-*6
filter
0=30=4
n^.5
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10 10 10 a tt JO 20 10 10 JO 40 20 10 10
i n i 10 io io 40 n a m u so M io n1 9 M M 10 10 tt 90 M a 10 V V 10 10 B
d. ."^p."r12
n
Topo
Interpretation
ChargeabilitymV/V
Interpretation
F^esistivityohm/meters
Interpretation
Metal F actor ip/res * 1000
400W
Dipole-Dipole Arrayno
Q-50M
rf plot point
RECEIVED
MAR 2 41995
l liternl r\2 n3 n4
ntervals Profiles Resistivity , 250 ohm/meter - - — - Chargeability . 1 O mV/V Metal Factor , 10 X
INSTRUMENTSAndrotex TDR6, Time Domain Receiver
1 /60mSec Total Interqrotion Time, 80mS Delay f^ ( 80+80+80+80+160+160+160+320+320+320 ) mSec
Scmtrex ISQ-3 Fansmitter BSecond Total Duty Cycle. 25ec On/Off Time
INTERPRETATION[ J Low Effect
' Poorly Chargeable mV/V. IP effect Low Apparent Resistivity, rho
[:\ / -'v | Moderately Low Effect
Moderately High Effect
High EffectGood Chargeability mV/V, IP effectHigh Apparent Resistivity, rho
50Stale 1,5000
50 100 150 200 250 300
(meters)
Royal Oak Mnes IncInduced Polarization SurveySemple- Hutt Claim Group
Hutt Twp. Ml S: 41 P fPorcupine Mining Division
M. C. Exploration Services Inc. Dec 1994
IP RES19 4flK
H
9 6. ^4K^
0 0
MF363
-
182.
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0.
MF KES IP
Topo
Interpretation
ChargeabilitytnV/V
Interpretation
jjs
Resistivity
erpretation
etui Factor /res * 1000
T - i i r i i i i i i i i i i i T t i T i i T i t i i i i t -f i i i i t i i i i t i i i i "T—r - r —i——i—i——i—r - i t i i t i
\\
\\ \
t—t- -r T —T T Z\
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L1B2 l 24K
L
Lo Lo
filter
0=1
r.-2
0-3
0=6
filter
0-1
o*2 0=3
0=4
0=5
0=6
filter
0=3
0=4
3*OOS MX) i HOOSt t 4 l l *
MX) 1*00 N 2*00 N1-114-
MDN 4*00 N StOONIt IS 11 10 14 IS II 12 10 14 10 13 1) U 12 10 14 SI
6+00 N^S 7 4.1
7*00 N* 4- *
71 It 11 14 71
10+00 N l i l filter
4+00 S 3+00:* 2+OOS 1*00 S 0*00i . i . , . , . i . i . . i .U J24 1101 1S.1I in \m J074 UH
1*00 N 2+00 N 3+00 N t - i 4+00 N 5+OON . i . i .2W 2* 1JK 1SK 17K 17* 25K J* 31K 4JK
6*00 N 7+pON
MK J&K
117, .71
8*00 N 9+00 N 10*00 N . ~ - t -F" . i . t- ~-IV VI ttt 14* 207 410 d| ter
IU 1M 101 s 417 0=1f
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0=6
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l H 1 1 l 10 90 filter
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40 li li B12 Jl II
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(-1210B7D2 K) 70 40 40 40 O a
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9 6
Topo
Interpretation
ChargeabilityrnV/V
Interpretation
Resistivity ohm/meters
Interpretation
Metal Factor ip/res * 1000
L JOOW
Dipole-Dipole Array
j ina Q i 8*r i
plot point
Filter* m
* * n2* * * n3
* * * * n4
Cont. Intervals Profiler Resistivity , 250 ohm/meter — -- — — Chargeability ; 1 O mV/V Metal Factor , 10 % ———————
INSTRUMtNTSAndrotex TDRb. Time Domain Receiver
1 7bOmbec Total Integration Time, BOmS Delay, r^ ( 80+80+80+80+160+160+160+320+320+320 ) mSec
Scmtrex TSQ 3 Tansmitter SSecond Total Duty Cycle, 2Sec On/Off Time
INTERPRETATIONi J Low Effect
Poorly Chargeable mV/V. IP effect Low Apparent Resistivity, rho
[ ~ ^' r' -\\ M oderately Low Effect
W////^ Moderately High Effect
High EffectGood Chargeability mV/V. IP effectHigh Apparent Resistivity, rho
50Scale 1-5000
O &Q 100 ISO 200 2bO JOO
(meters)
Royal Oak Mines hieInduced Polarization SurveySemple- Hutt Claim Croup
Hutt Twp. NTS: 41 P j N WPorcupine Mining Division
M. C. Exploration Services ho Dec 1994
IP RES18, 2123
8.8. 1062.
'Oj 0
MF143
71.
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0.
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. , 14J
Topo
Interpretation
ChargeabilitymV/V
Interpretation
Resistivity ohm/meters
Interpretation
Metal Factor ip/res * 1000
_ 4~ t i . 4 l t l l l l l "T IT l l l l l T l -t I "-'J - i i i i i i i t i i i i i i t i i i i i i i..., l)
t t l
3*005 t .2*005 f IKlOb i 0+00
filter *' 7 10 ** * J l 4 J i iliOON ?*pON WON 4*ON WXJN 6*00 Ntltt.ft**f*t* --f - * -* ' l , ( * t .
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5 2 I I
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14 17 9 l 4S * 16
B e
l opo
Inter prrtutiOM
( h oryeabilitymV/V
Inti r [ir ctutiori
ohiTi/ineters
Intrrpretalion
Metal l actorip/reb * 1000
L l Oi)| .
Dipole Dipole Array
ripoint
SOM
Lent Intervals Profiler Kebiblivity , /'bO ohm/muter Chargeability . 1 O mV/V Metal fa. tor , 10 7,
INSlklJMINISAndrotex lUKb, l mie Domain Receiver
l/hOm'iec lotal Intergrution hint, HOm'* DelayMl ( aniflOt80t80HbOi IbOi IhOtj/Ot VOOA) ) mSei
Scmlrex ISO, S l ansmitterlotal Duly (ydc. -"..ec On 'Oil lime
IN FI KI'RI IAIION
LOW LtfcctPoorly Chorguablc mV/V, IP effortLow Apparent Resistivity, rho
Moderately Low btfect
Moderately High t ttect
High r (tec tGood Chargeability mV/V II' effectHigh Apparent Kcsibtivity, rho
St ale 1 iiOOO M o 50 i oo i so ?oo pso joo
(motors)
Royal Oak Mines IncInduced Polari/ation SurveySemple Mull Claim Crnup
Hutt fwp. NIS 41 P f N WPorcupine Mining Division
M C [ xplnration Services Inc l)o(, 1994
IP RES 11-, 1885,
4
5.5. 943.
•i H
0^ Oj
MF 70.
35.
-
o^
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' ~- -~- \
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T'"] l - T l l
Topo
Interpretation
Chargeability mV/V
Interpretation
Resistivity ohm/meters
Interpretation
Metal Factorip/res * 1000
i i i . i . i . i i i ~ l ^t i i i i i i i i i i i , i.i i i i i
MF 70
REb IP M
94J
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n*5
n-6
7-tOON . t(t to
4 * 4" - * * * . t . l
49 44 44 4
20 40 O 0-20 30 K 10 10 b s J 7 n- 1
31 4 \\ 40 -20 50 17 K -3
4,5OO,e^ -14 -31 42V 31 ^ 3 1 \^ l l -11 10 21 -1 -45 17
1|'W j g —— 4 4 14 - 40 \
filter 1Kn-1 239n*2
n-3
3*005 2+00 S.—f:—^ t ^.. . .. ±.. *in 132 1M 392 MO
1+00 S 04004—— . l . -4-—————. t 4 -
HO 1215 1M3 1714 1125 1420
7+00 N ft+UON* . * . t . *HI 43/ 4(6 429
2+OON 3+OON 4+00 N ^00 N 6+00 N- -1— -' * * - * ' ^ ' - 4——' * - - * . i . i . i15H 131* 1305 1254 117) 10W 747 710 m 5M
*4 71 1*7 272 420 342 272 —— 207 321 3M - S61 - 371 365 2J4..___200 - 2*2, 2U - 2*4 245 - - 2)3 202 ;S^ ~~~———.^^ ____ ___ S ^—————~- \^ __ —— v——~ ^~^72 13* f 417 ~\,, M 5(6 JB^. *fi"—^(h v 311 7 i M ,— K3 \^522 -^*00^--44I ~--- 502 314 313 4* 405 *7\ 202
111 J79 f/9B W? 770 ^ llll^l^NN Ut.___/25 ( 11(2 1222 "^ /W --^ W^IOB l g4 ,~^ 5(P~~ 529
" tfil " 1404 913 1003 '";i2 54*
9*00^ ( ^ 10+00 N
* " ' ** * filter304 20t 201 . 213 HI
130 401 2lJ 316 37)
,'19 505 m "' 2(4 3*7
Ut
ta
0=3 n-4
n-b
n-6
. 3+00^
filter " ' **
n-3
1+00 S - * .3 70
CHOC 1+00 N 2+OON i+00 N 4*00 N WC N frtOn N /tOON IWX N-* ^*— * t * * **.* t *-i .-* . t- i — --^ -^-f'lti.i.i.t.tit't*O H 49 61 3 12 SO 40 -1 S -2 l 21 II 37 I I II M It 10 17
10+00 NM ^ 1J filter
40 1 O 20 -B -11-45 30 K
20 1 -19 -39 -l( -95 34 l J
-12 23 11 It 12 35 4
15 51 i M
19-^11 V JJ^-^" l'
\- y - v^\^^l 2 j IS II II U II N 7 J 12
41 94 II 11 li J1 Ml ^ i l
n-5
n-4
n^b
n h
l ri p o
Interpretation
'.hcirgeabilitymV/V
Interpretation
Kebistivity ohrri/meters
Interpretation
Metal Factor ip/res * 1000
Dipole Dipole Arrayno
MT
plot point
h liter* nl
* * n/ * * * n ^
* * * * n4
Cont Intervals Profiles Resistivity , ^50 ohni/mi'tnr Chargeability , 1.0 mV/V Metal Factor , 10 %
INSlKUMtNTSAndrotex IDK6, lime Domain Receiver
l /bOrrijoc lotal Intergration Time, ROrriS Delay ( 80+80*80+80+160-t 160*1MH.y(H.VO-K5?0 ) rni.ec
Sciritrex FSO J farv.mitter RSecnnd lotal Duty Cycle, S '.^c O n/Off lime.
INItKf'KI IAIION
l Low EffectPoorly Chargeable mV/V, IP eftec.l Low Apparent Rebibtivity, rho
- .' ,-:.-| Moderately Low ttfect
Moderately High tffect
High LffectGood Chargeability mv/V, IP effectHigh Apparent Resistivity, rho
'.cole 1-hOOOjon
M.
(meters)
Royal Oak MinvsInduced f'olari/atnui SurveySemple Hutt Claim Croup
Hutt Twp. MIS- -11 l' ' N WI'orujpine Mminq Divisionl xploration Servi(.cb hi, iJec, l'H-1
IP RES 6.4, 2184.
MF
3 2J 1092 J 20-
Oj
l opo
Interpretation
Chargeability inV/V
Interpretation
im/meters
t pi ctation
tul l actor
rej, * 1000
OJ
T ' ——T ~ T~ T T t l 1 l l l l T——f — T l l l l l l l l r l l i l i p p i
..l . l l . l l l l l l l l l l l l l l l l l l l l -J t
II 1 1 1 1 1 1 1 1
--. - -
1 1 1 1 1 1 i 1 1 1
Ml J9
.0
n
KLb /IB4
u.109i!
L
.0
IP .b 4
J i
LO
4 t ' . 4 ^ ijl . i , i . i i' "f . "'l i 'i ' i * i* i
filter J filter
n-4
2 l ^.-- 3 i ——34 ' v 11 l y Ib lb,J4 Jl
"/'TfCN 3J\\ W W K VU\\ ffi 70 70 4(1 40 Df] , .' . l l
1,' ' d i A\\ U )) ) ' '-. ,44 44 52 51 -— ' 4( 41 vN l6 3t 42 It 41 44 '4 ( 19 ^^ 5 b ' Id
. .-^.. t . , . l •; 'r IV
^ 3+OD S t 2+00 i,filter "* " l 77 ' ™ * M
1*00 S 0+00 j 1*OON t ( ^*OON
504 VI 1!A/ 16/4 I(M 1920 189? IM
.MX) N *t.1174 liM
4+00 N **i1400 1510
'tOO N iU/b Ut/
5=^x1 r ^-;"--, ~ .^ 20(2 H Ut y 121* - 933 ^- bft4
/•(K) N
/•i' UM
Ml) 46J
H'di N 9KX) N i
Vi ,2t 566 D21 tiller
//tt 106 266 J04 Jtt4 Ml n . l
Wl 2*4 J// W? -DI- i, .'
ilfl *M .M/ 5/6 - 1100x
r64 j't *) 7 1141
//U SO, /(W
'(B ID4? 1446
n 4
3+OOS
filter
n-i)
0+00 1+00 N 2+00 Nl . l . l . * . l . - 4
45 ?3 l/ ?( 39 4 13
3+00 N t+on N*4 . i . * t
(O 40 40 JO
•itflO N t,i(X) N
l II / 4 !
/•(K) N MX) N
i l) h U II 4 III D li 10
lO'UI N
'" " tilt, l
H l l ,,|l/ 10 10 10 31 It II 10 30 W) 19 26 l 'j l I I .' l 'l le, t i B rt , u li
40 20 10 10 tl 54 45 -20 40 10 H) 10 /n 60 l li / j t l ' DM II,''h ., n'
i 9 9 10 10 51 4 J 73 2 1 1 0 40 10 40 ID 2TI Mi /S ; , Mi h 4 D 4 l/ B J *, 2 n i
30 10 16 21 19 13 11 20 10 i w /i) /n in , ; f r, n ,- h l i/ u , i - ,, ^' " \ lK \ 5/ 1 21 l 14 12 12 41 40 10 J Jfl 4(1 .-H 4/ 11 III J/ j h In II M-',
l Ib l/ U~'-94 29 13 50 II 12 25 35 l 75 it '4 id 4u III 'i y h. 14 M h ,, -1,
lopn
Inter pollution
(.hurgeubilityITlV /V
Kt '.islivityohm ruclerb
r 111. r i' 11 t a 11 ("i r i
l
'.001
Affljy
O H(J J II IIri l M
l i
lilt'
Cont Interval 1 . I'mfile.^!;() ohm nu.tfi
( hrjrgeability , l O mv 'V M'.tal (actor . 10 7,
IN'.IK'llMl Nl 'Arnlrottjx IDKf), linn Donidin Kt i i ivt i
l/hOrnSi'i lotal Inttrqrutmn linn , H(iin', l)nlayMl ( 80i80t80tBOt IhOHhOi lh()i'.'(M I'mVO J rrr.c.
l .f inlren IMJ ^ lari'.mittci
lotal iMjty Cy( li , ; l ,t i i)n Off linn
IN l l K'l'l'l IAIK 'I
i ci* r Itci ll 'ooily ( hurgf uhli 1 nA li' i ttt i tl o w Appijrcrit K( .1 .tivity rtin
Modi'iijtcly l nw l Hi l
Modi rah ly i lnjii l ffi i t
High l Ile. l
Ilnjli A()|Hj|i ut K'( iijtivily
' ,i ijli l M K H)
l) l}() 10(1 ISO 'Od
nl Oak Mil H -x hieiJu(,ed 'o iji i ijlii 'li ' iijf vt ,
NWluit l w p N '- 1
M'i if u|)iiit Miniiuj l )ivr.uiii
l ")hrutji 'i i rf 'i vi' ( . lin l )f (