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Work History page 07
Mentioning eleven assessment files surveying on and near
project 507.
T-542 Rusk Porcupine Mines Ltd. 1941- 57.
T-556 Hollinger Cons. Gold Mines Ltd. 1958- 60.
T-620 Sylvanite Gold Mines Ltd. 1940.
T-770 see Hollinger 556
T-1532 Mill Hill Mines Ltd. 1973.
T-1647 Thomas Herbert 1975.
T-1941 Texas Gulf Canada Ltd. 1979-85.
T-2378 Preussag Canada Ltd. 1981.
T-2645 Noranda Exploration Co. Ltd. 1984.
T-2738 Gowest Amalgamated Resources Ltd. 1984-94.
T-2913 Mintek Resources Ltd. 1989.
File T-1941 applying geophysical and geological mapping,
along with overburden drill holes is most helpful.
File T-556 Hollinger Cons. Gold Mines Ltd. tested a HEM
conductor ( DDH C-10 and C-ll ) intersecting pyrite bands in both
diamond drill holes put down. Diamond Drill Holes C-10 and C-ll
now situates on claim 1177828 ( NW 1/4 ). DDH M-5, in 1961, now
located on claim 1177829 intersected graphite. Another DDH M-6
situated on claim 1189887 tested a magnetic high. The hole
logged as "very fine grained serpentinite containing fine
tetrahedrons of magnetite and locally pyritic."
Reference PLAN-1 situates claims and picket lines.
Regional Geology page 08
A base of Keewatin Basalts and Andesites is overlain by rhyolitic and pyroclastic volcanic rocks. The latter contain variable amounts of Iron Formation and intrusive peridotite- pyroxenite ultrabasic sills.
Overlying the volcanic rocks are a thick sequence of Timiskaming type sediments, largely greywacke with lesser Argilite.
To the south and west, a batholitic granite intrusion borders the claim group.
Invading the rock sequence are narrow diabase dykes intruding post depositional fractures, having a NS preferential direction, also interpreted running NE. Another set of separate diabase dykes run M\ and may be present on the property.
Ancient folding and extensive shearing complicate the- rock sequence.
Property Geology
The survey area mostly covered by glacial till averaging 20ft ( 31 overburden drill holes by Kidd Creek Mines Ltd, 79 ). The limited outcrop exposed on the property;
BL 6500N, near and along highway 144. BL 6500N, 8625E to 9125E. TL 5000N, 6000E to 6400F.L 7750E, 6900N.L 7000E, 6450.N.L 10125E and 10000E/ south of 5800Nand minimal exposure along the power line.
The exposed rock consists predominantly of mafic volcanics and diabase. As seen in outcrop, the rocks tend to strike NE and dip moderately to steeply to the NW. Pillows found north of highway 101 show tops are to the SE, therefore showing overturned units ( Barnett 1985 ).
The western portion of the grid interpreted as felsic to intermediate rocks of the Kamiskotia volcanic complex. Bedrock information is available from the four drill holes put down by Hollinger Gold Mines Ltd. ( 1960-61 ). Two NE conductors drilled and logged as narrow pyrite bands.
Property Geology (continued)
West of the Kamiskotia volcanics are rocks of the Tisda]'- group, here composed mostly of mafic volcanics and ultramafic* ( Barnet 1985 ). In the Tisdale group, the ultramafic horizon^ run NE, agreeing with the high magnetic susceptibility.
Maintaining that the faults predate the dykes and therefore, did not displace the dykes but did control their propagation ( Barnet 1985 ).
Diamond drill hole M-6 by Hollinger Gold Mines Ltd., found roughly 6850N/ 6050E, examining a magnetic high, logged as "very fine grained serpentinite containing fine tetrahedrons of magnetite and locally pyritic."
Minor narrow quartz and carbonate veins are common. Several irregular to lenticular gash veins 10 - 15 cm wide crop out under the power line at 7600N 7320E. The vein material consists of milky white quartz and lesser buff to brownish carbonate. No sulfides seen in the veins ( Barnett 1985 ).
Surveying the east part of the grid, both Preussag Canada Ltd. ( 1981 ) and Hollinger Gold Mines Ltd. ( 1959 ), took part in extensive geophysical, geological mapping, followed with DDH investigation. An outcrop now situated on claim 495309, described by Hollinger "a small mass of intrusive pyroxenite occurs." "To the west of the pyroxenite, a few outcrops of andesite are present." "On one of these andesite outcrops, narrow quartz carbonate stringers are well mineralized and carry gold values." ( H. Michie, S.N. Scott 1958 ). DDH B.T.-7 found roughly 8990E/ 5790N on the grid, describes "fine grained dark green andesite lava, which is generally hydrothermal ly altered." "Alteration consists of feldspathization or syeni11zation in veinlets or stringers, silicification and an introduction of thickly disseminated crystals of melanite." "Epidote is abundant in tiny stringers throughout." "Flakes of brown to black biotite are common." "Some fine disseminated magnetite is present."
Geophysical Agenda pag*? 10
Due to water coverage baseline, 65N has a 300 m offset to the N at 7500E, which then becomes baseline 6800N. The combined baselines measure 3750 m 1 s, extending with an azimuth of N40DegT across most of the grid. Controlling the three most westerly lines is tieline 8000N, controlling the remaining easterly lines is tie line 5800N. All lines have an azimuth of N230DegT, separated by 125 m's and chained at 25 meter intervals. The baseline start point off of highway 144 (post #1, claim 1181995) situates the grid at the intersection of Bristol, Carscallen, Denton, Thorneloe Townships.
Therefore, starting Induced Polarization coverage completing 38.7 km using the Pol e-Uipo l o array. t'sing an a spacing of 50 meters reading nl to n6, covering the complete area with three (3) remote current electrod-- pits. The first remote current pit at 7125E.' 3200N reads the central portion of the grid ( 6500E to 7750E ). The second pit at 6125E/ 3600N, reads tho west portion of the grid ( 5375E to 6125E ). The third pit at 9125E 3900N, reads the east portion of the grid ( 8000E to 10000E ). The Time Domain I.P. survey used a TSQ-3, 3000 watt fixed transmitter for lines 6125E to 7750E ( inclusive ). Replacing the TSQ-3 Tx with a Huntec 7500 watt Tx, after thieves lifted the scintrex Tx. The Huntec 7.5 Kw transmitter resolves better signal' noise ratio for the remaining lines. Being in the rain season, a saturated water table furnishes low contact resistances. The only- drawback surveying immersed shear zones, is EM noise er.nted ( EM coupling owed to freshly watered clays ). The choice of array (with superior signal/noise ratio ) maps the property adequately over varying glacial till. References found in the addendum explains equipments and techniques applied.
The seventeen lines read, seen on sections l to 17, label and contour three elements. The three elements are IP effect, apparent resistivity and metal factors ( MF = IP/ R* 1000 ). Also seen on top of the sections are profiles of filtered elements, filtering from nl to n4 only. Also included in the report is a plan map at 1:5000, showing n3 readings. Profiling both chargeability and resistivity elements using a logarithmic sea le.
The survey started in August, 1994, ended in October of 1994. Thanks to roaming thieves, a three week period lengthens the survey duration, waiting for transmitter replacement.
Presenting 666 stations of IP survey read on project 507.
Section Evaluations page 11
L-5375E Section l
This 1400 m section shows underlying rocks with a high apparent resistivity widespread. A chargeability high occurs between 7375N and 7750N. This IP anomaly perhaps shows the north limit of an ultramafic unit. Another high IP effect happens at the north extreme of the line, attributed with a lower resistivity. Rating this anomaly good and obscured grid north, merits concern. The northern IP anomaly, perhaps shows another intrusive halo. The resistivity signature is similar to that seen grid east over the u11 rama fics . The mag refutes on the central portion only, perhaps related to the depth of the body. Defining the low resistivity between 7175N and 7325N as heavy till ( crews exan-.ined cedar suanip ). The power l i ne at 8210N is probi enia t i c .
L-5625E Section 2
Section 2 measuring 1600 meters, shows an apparent resistivity comparible to section 1. Central underlaying rocks showing deeper by roughly 25 meters. The resistive response to the west ( 6750 - 6900 K ) reflects the same response as on section 1. Explaining the higher resistivity with high-grade metamorphic rocks at 6750n to 690 ON. A chargeability high occurs at the same location, showing the presence of metallic minerals. A second chargeability anomaly between 7450N and 7630N happens with excessive noise. The noise reflects a fresh water saturated fault with clay content. The twin reaction at 7950N reflects the same contact. The double reaction happens when the potential electrode connects to the zone, followed by the current electrode. Interpreting the underlying rocks as ultramafics. The mag corresponds on both south and north limits. The powerline SL-CM at 8125N is problernat ic .
L 5875E Section 3
This 3.2 km section shows EM coupling noise at 7125N ( n3, n4, n5 and n6 ) and 7575N ( n3 and n4 ), giving the noise to water saturated shear zones. The broad resistivity high on the south portion shows ultramafics; metallic minerals on both extremes of the ultramafic explained with an IP effect. This unit measures over 1500 meters wide. The chargeability high seen at 6525N ( nl to n6 ) reflects the north contact and the other response at 7125N and 7575N, defines another ultramafic unit. The resistivity and magnetic response both agree. This unit is also obscured grid north. The powerline at 8075N is problematic.
Section Evaluations (continued) page 12
L 6125E Section 4
This 3.0 km section with little EM noise shows good penetration. Interpreting an ultramafic unit from the obscured south extreme to 6825N. A high resistivity seen at 5500N explaines granite dyke, cross-cutting the section. The associated chargeability is intricate, perhaps explained by the edge of the swamp ( with conductive clays ) bordering the existing ridge. The second highest resistivity feature at 5100N to 5175N, shows high-grade metamorphic rocks. The weak resistivity between 6800N to 7250N, having low magnetic susceptibility reflects the depth of the cedar swamp. A chargeability anomaly happens at 7325N within a moderate resistivity low. The depth of the target would hinder the magnetic response. Basic e.xtrusives are suspect in this vicinity ( Barnet 1985 ). The power line at 7975N is problematic.
L 6500E Section 5
Measuring 2.975 km in length, the section shows ultramafics on the south half. A variable arising at 5850N, perhaps tells of a sheared unit. The first segment is obscured grid south and ends at 5750N; the chargeability for its' length is uniform until the north extreme ( 5750n for nl ). The N farthest negative IP effect ( 5850N ) shows an abiding contact and the other ultramafic segment, from 5900N to 6650N, shows a good chargeability at its' north limit ( 6325N to 6525N ). This IP effect is frequent, mapping the halo of the ultramafics. It is possible that both responding elements between 6650N to 7050N is starting from that of volcanic tuff. This low resistivity and chargeability signature can also confirm underlying sediments. At this location, dry ground with mixed forest is seen during the survey. Interpreting a underlay of ultramafics between 7125N and 7800N. Restraining the resistive response between 7125K and 7500N is an overlay of cedar swamp. The powerline at 7875N is problematic.
Section Evaluations (continued) page 13
L 6750N Section 6
Measuring 2975 meters in length, the section displays good penetration with little noise. Agreeing with the mag survey, two granite dykes contort the resistivity section, showing the dykes surface, projection at 5925N and 6300K. Layered resistive impacts imply sediments abide at the south extreme of the line. Implying a contact at 5325N and a chargeable zone between 5375N to 5525N showing the halo. This halo insinuates a south limit of an ultramafic unit. Another chargeability anomaly at 6350N to 6525N, marks the north limit of the intrusive. This IP response stronger near surface, implies good metallic content ( 5 9. theorization ); therefore, follows concern. The diffuse response, emerging grid north is due to dip and size of the body. The resistivity section implies volcanic tuff between 6600N and 7100N. The chargeability low of O mV/V seen between 7150N7 to 7325N, maps the water content of the cedar swamp. Giving this low to a cross-cutting fault, interpreting an intrusive unit starting at 7300N. The zone obscured grid north has a chargeability anomaly at 7500N mapping its' south limit. The powerline at 7775N is problematic.
L 7000N Section 7
Measuring 2975 meters, the section shows good penetration with little noise. Interpreting an ultrmafic unit from 5300N to 6775N. A high resistivity at 5450N along with a moderate chargeability, indicates the south limit with high-grade metamorphic rocks. The high resistivity response projected at 6400N is that similar to a granite dyke. The high resistivity between 6525K to 6625N, along with an IP anomaly, marks the north limit of the ul t rarr.af ic. The chargeability and resistivity response at 5250N insinuates sediments remain on the south end of the line. The chargeability and resistivity response between 6700N and 7150N imply volcanics abide. The low chargeability of O mV/V at 7250N ( n^4 ) insinuates a cross-cutting fault. Another ultramafic type response occurs between 7250N and 7850N. Both N and S extremes have chargeability highs. The powerline at 7700K is problematic.
Section Evaluations (continued) page 14
L 7250N Section 8
This 3 km section hindered by water coverage between 6400N and 6550N. Highway 144 at 5300N is problematic, changing the southern resistivity response. Ending this effect would show layered resistive impacts similar to that of sedimentary deposits. A resistivity low intrudes at 5775N, perhaps mapping a minor shear zone containing conductive clays. Interpreting the south limit of the ultramafic at 5700N with agreeing chargeability and resistivity. The north limit is undetecting due to the water cover. The high resistivity at the south edge of the pond starts from a cross-cutting granite dyke. Volcanic rocks conceivable between 66DON to 71 DON and thr- high chargeability at 6750N is repeatable. The high resistivity at 730CN is due to another granite dyke cross-cutting the section. The conforming chargeability and resistivity anomalies at 76 O ON show a south limit of another possible ultramafic unit. A larger intrusive with a centralized shallow mantle of volcanic extrusives are not dismissed. The powerline at 7650N is problematic.
L 7500N Section 9
The 3.0 km section inclined by highway 144 at 5500.N by potential electrodes only. Perhaps a calcium saturated ditch is responsible. Interpreting an ultramafic unit between 5700N to 5950N with high-grade metamorphic rocks at the south limit. Abiding high resistivities likely occur with local granite dykes cross-cutting the unit. Coincidal with the mag survey, another granite dyke happens near 6500N, using the chargeability highs to better map the S and N limit. The south portion of the line shows layered resistive impacts. Alike sedimentary effects, postulating extrusive volcanics between 6950N and 7300N. The chargeability anomaly at 7350N suggest a south limit of an ultramafic unit. The high resistivity anomaly at 7500N is that of a granite dyke or high-grade metamorphic rocks. The powerline at 7550N is problematic.
Section Evaluations (continued) page 15
L 7750N Section 10
Measuring 2900 meters in length, this section, the first of 17 lines read, shows little noise. Surface noise happening from 5775N to 5975N ( nl and n2 ) conforms to the receiver, maximum sensitivity. Beyond 4000 mV the IP2 will not function, securing its' low sensitivity. Surface conditions having beyond 5000 ohm/ meters becomes problematic. This zone from 5775N to 5975N starts over outcrop of high-grade metamorphic rocks; explaining this zone to be the south limit of an existing ultrumafic unit. Mag and chargeability both agree. A chargeability high with a moderate resistivity low seen at 6800N shows the north limit of the ultramafic, accent-ing another commendable target d t 7300N. This chargeability anomaly with moderate resistivity low arises south of a shear zone. North of 7600K, the apparent resistivity visage lessen to a great degree.
L 8000E Section 11
Line 8000E measuring 2100 meters, accented by two high resistivities that outcrop, postulating the south limit of an u 11 rarr.a f i c , roughly at 5400N. The north limit obscured by a fault at 6150N, attributes noisy IP effects; therefore, assumes the north contact between 6400N and 6600N. Accenting an IP effect at 6700N with weak low resistivity impact. This anomaly also emphasized on line 7750E.
L 8375E Section 12
Measuring 11675 meters, the section foremost anomaly shows the burned ridge effect at 5300N. This anomaly shows an intrusive burried ridge, with a possible fault contact. The broad and diffuse resistivity and IP effect at 5300N to 5925N coincides with the ultramafic unit mapped by the mag survey. The resistivity high, along with a chargeability high, possibly shows a segment of ultramafic rocks. The water coverage 'limits the north extent of the line.
Section Evaluations (continued) page 16
L 8750E Section 13
Section 13 measures 1550 meters, limiting an ultramafic unit at 5500N. The north limit veiled grid north for water coverage, interrupted survey crews. A chargeability high occurs at 5700N, near the south limit of the intrusive. Another IP high at 6150N, postulates a grid north limit, deja vu on earlier sections. A resistivity high borders the south extreme of the section. Agreeing is two narrow IP highs implying multiple contacts. Noise also arise at this location, postulating a near fault. The chargeability lows centering at 5425N and 6000N reflect the bogs observed. Enhancing the very high resistivities cleaving north is an outcrop ridge. A low resistivity abides within the said high. The anomaly stemed from blasting when crews established highway 144.
L 9125E Section 14
Surveying 150f) meters section 14, shows intrusive rock with extremely high resistivities. Postulating Syenite as a possible rock type, responsible for high resistivity values. I'ltramafics named on the pr e l imi na r y map P 118, coincide with resistivity lows at 5500N and 5850N. The magnetic survey does not refute the presumption. A chargeability high at the south extreme of the line happens with EM noise. Assuming the noise represents a water saturated contact. The IP anomaly at 5850N implies limited depth extent to a wide body. The resistivity limits interpretation with high resistivity impacts. The third IP anomaly at 6250N, along with EM noise, submits to a near fault contact. A four pole profiling method can lower the resistive response with better convergence.
L 9500E Section 15
The 1200 meter section shows primary voltages above allowable receiver sensitivity along nl from 5075N to 5375N. Postulating Syenite type igneous rocks responsible for such high resistivities. The resistivity low at 5500N coincides with ultramafics, observed on preliminary map P 118. The mag does not refute the presumption. The chargeability noise at the south extreme of the line suggests a near contact. The EM noise at 5800N positions a fault contact, also mentioned on section 14. The gathering of metallic effects at 5500N ( nl to n6 )and 5550N ( nl to n6 ) is the first allusion of a unit dipping grid south. Indistinct IP anomalies abide on both south and north limits. Excluding 5400N to 5900N, elevated outcrop abides on this line. As line 9125E, suggesting four pole profiling for better delineation.
Section Evaluations (continued) page 17
L 9750E Section 16
This 1200 meter section displays a similar resistivity low as seen on section 15. This low resistivity from 5650N to 5900N has an invading resistivity high at 5750N; the invading resistivity high attributes high-grade metamorphic rocks. The encompassing resistivity low coincides with the mapped ultramafic on preliminary map P 118. The mag survey does not refute the presumption. The two good chargeability anomalies at 5550N and 5825N show both zones are dipping grid north. On the south portion of the section, the primary voltage surpasses the receiver sensitivity. Suggesting a syenite type intrusive, responsibly losing ri] and n2 for the 400 nv?ter stretch (5000N to 5400N ). An IP high shown at the north extreme is unclear. The neg.-it.jvt- IP effects at 5750N, implies a near fault, contact. For better IP delineation, four pole profiling suggested.
L 10000E Section 17
This 17th out of 17 sections measures 1125 meters. The traverse depicts very high resistivities widespread. This high resistivity perchance originates from syenite type igneous rocks. Compared to section 15 and 16, thus section shows a narrower resistivity low from 5625N to 5800N. This low invaded by a resistivity high, suggests high-grade metamorphic rocks. As on previous sections, the low occurs where presumed ultramafics abide ( map P 118 ), the mag survey also agrees. The chargeability high at 5500N happens within a moderate comparative resistivity low. The IP high is marginal to the south of the better resistivity low. Another IP high at the north extent of the line remains indefinite. The twin IP anomalies embellish an ultramafic unit, deja vu signature. For better delineation with such high resistivities, four pole profiling suggested.
n3 Plan Evaluation page 18
Inhibiting the property are Acid Intrusives and High-Grade Metamorphic Rocks showing High Resistivity visage. These eminent highs overshadow noticeable low resistivities. Therefore, interpreting moderate low resistivities meaningful in detecting good conductivity structures. Devising plan 2 in three apparent resistivity responses; low, moderately low and high. The low resistivity, reflecting chiefly bedrock lows; the moderately low resistivities, show lingering structural breaks; the high resistivities, show Syenite type intrusives.
A notable moderate resistivity low extends from 5375E/ 7200N to 10000E/ 5800N, bisects the survey area. The magnetic survey admits to a structural break along this concurring feature. Another moderate low resistivity from 6500E/ 7850N to 7750E/ 7600N represents another structural break. The magnetic survey does not refute a break at this same location. Occurring at 6125E/ 5900N, an isolated moderately low resistivity is subject to the depth of the spruce bog. Accenting two moderately low resistivities revealing good conductors. The first zone begins at 7500E/ 7300N continues westerly. Showing another conductor at 7750E/ 6900N that runs westerly. Assuming contour traces on plan 2 because of large line spacing.
The high resistivity features on the east side of the grid reflect Syenite Type Intrusives. Fragments of the intrusion persists westerly, enduring up to line 6750E @ 6325N. The Syenite granites are often sodium-rich and carry minerals; therefore, attribute high resistances with high IP effects.
Showing a possible target of economic mineralization is the IP effect at 7750E/ 6800N, corresponds with an apparent resistivity low. Highlighting another IP effect of interest from 6750E/ 7400N to 7000E/ 7400N, which also coincides with an apparent resistivity low. Other dispersed high chargeabilities indicating metallic substances, merit concern. Relating these areas of concern at positions; 6750E/ 6450N, 8000E/6000N, 8000E/ 6615N, 9125E/ 6000N 6 6200N, 9500E/ 5600N fc 5900N, 9750E/ 5400N to 5600N and 10000E/ 5500N to 5700N. These scattered anomalies happen along geological contacts.
Implications page 19
Economic interests insinuate follow-up on the conductor situated on line 7750E/ 6800N. This zone should be delineated both east and west on the grid. The Dipole Dipole array is the preferred choice for its' favorable sensitivity and selectivity . This choice array is also symetrical, establishing plot points. Conductivity and Chargeability elements on the anomaly seen from line 6750E to 7000E @ 7400N is of concern. This zone also merits detail work; therefore, complimenting 6 to 8 km of IP, using the Dipole Dipole array reading nl to n6.
After investigating the conductors nature and extent. Diamond Drilling is commendable.
Compiling past work ( developing precious metals ) with the recent IP data collected is commendable. Resourceful DDH*s intersecting mineralization on the east portion of the grid, deserves attention.
THE INDUCED POLARIZATION METHOD
Induced Polarization (IP) is the measurement of a residual voltage in rocks that remains after the interception of a primary voltage. It includes many types of dipolar charge distributions set up by the passage of current through consolidated or unconsolidated rocks. Among the causes are concentration polarization and electrokinetic effects in all rocks and the phenomenon of overvoltage in rocks containing electronic conductors such as metallic sulphides and graphite.
The term overvoltage applies to secondary voltages set up by a current in the earth which decays when that current is interupted. These secondary effects may be measured by pick up or potential electrodes.
IP as we generally know it is a method of prospecting for low grade sulfide ores where metallic particles, sulfides in particular, give an anomalous response. Barren rock (with certain exceptions) gives a low response.
In practise, IP is measured in one of two ways: In the pure form, a steady current of some seconds (nominally 2 seconds) is passed and abruptly interupted. The slowly decaying transient voltages existing in the ground are measured after interuption. This is know as "pulse" or "time domain" IP. The factor Vs/Vp is the integrated product for a specified time and several readings are averaged thus suppressing noise and coupling effects. The resultant "m" or chargeability is essentially an unitless value.
The second method entails a comparison of the apparent resistivity using sinusoidal alternating currents of 2 frequencies within the normal range of 0.1 to 10.0 cps. The factor used to represent the IP effect by this method is the Percent Frequency Effect (PFE) and is defined by(R1-R2)XR1 x 100*fe where RI and R2 are the apparent resistivities at the low and high frequency.
OSE and LIMITATIONS
The effective depth of penetration of any IP survey is a function of the resistivity of the surface layer with respect to the resisitivity of the lower layer. All arrays have different effects from this resistivity contrast - some are less affected than others. When the surface layer is 0.01 of the lower layer, the effective penetration is very poor hence the term "masking".
The size of the target therefore becomes important when detection IB desirous under a conducting surface layer. Frequency methods are the most adversly effected by masking as inductive coupling can be much greater than the measured response.
The IP effect was initially developed for the prospecting of large porphyry copper ore bodies. Since that time, it has been successfully adapted for the search of sulfide bodies in the Canadian shield and elswhere. However, its usefullness is probably over-extended as a sulfide detector when exploring for gold. Therefore, it becomes a tool for structural mapping based on the differences in electrical properties of the rock and the target.
THE GENERAL POLE-DIPOLE ARRAY
The use of the pole-dipole array is much less common that the dipole-dipole or double dipole array but it has distinct advantages. The most noteable advantage is the much stronger current density obtainted from the single current pole on the traverse. This results in the strongest potential voltage measureable from any of the arrays. This stronger signal to noise permits operation in noisier areas and areas of thicker overburden. The most common form of this array is the THREE ARRAY or a pole-dipole array where 0=1.
wirftctl "2
"l Ot Hi 02 M3 Oj
tftopli *f Ifct diets
ii!
HIM l!
luiiiuiiun inUJIIIIIUlll
Major Benefits* Two Dipoles Simultaneously Measured
* Solid Stale Memory
* Automatic Primary Voltage Ranging
* Automatically Calculates Apparent Resistivity
* Computer Compatible
* Software Packages Available
- 3-
1. START UP
Turn on the Instrument using the ON/OFF switch.
2. BATTERY VOLTAGE CHECK
Press the BAT key. The unit Is supplied by 6 1.5 V D size dry ceOs.
BAT s 9 .0 : new batteries
BAT s 5.6 : change the batteries.
3. LINE CHECK
Press the Rs key, then select the electrode to be checked by pressing the
corresponding push button. Resistance between this electrode and the reference
electrode is displayed in k.ohm.
A. ARRAY SELECTION
Press the EL Array key and then the ROLL key to select the desired elec
trode array. Seven electrode arrays are available (see table 1 and fig. 1).
5. INTRODUCTION OF PARAMETERS
Press the P.Tx key to Introduce the parameters relating to the transmitter
(when a parameter has been Introduced, press the ROLL key to Introduce the next
one ; the CLEAR key can be used to rub out an erroneous value).
In the dipole dipole array, these parameters are :
X - AB : Abscissa (m) of the center of AB with respect to a fixed origin.
D : Dipole length (m) (AB r MN s D)
PROFIL : Integer number, allowing to Identify the measurements made on a same
profile, during storage.
l : Intensity of current (mA) for further computation of resistivity.
TIME : Injection tine. Introduce the number 1 or 2 ; the display will show 1 000
or 2 000 (ms).
Then, press the P.Rx CO and P.Rx Ci keys to Introduce the parameters
relating to the corresponding receiving line. In the dipole dipole array, this parameter
is :
X-MN : abscissa of the center of MN.
6. START AND STOP OF MEASUREMENTS
The acquisition of data Is triggered by pressing the start/stop key. The
instrument first synchronizes with the receiver signal The synchronization Is perfor-
mec o r. the higher level signa! channel. During this time "SEARCHING" is displayec. If
the synchronization has been successful "OK" is displayed ; if not, "NC SIGNAL" is
displayed, try again, anc check the transmitter Is working well.
Once synchronized, the equipment displays the SP values of both channels,
anc then :
. Primary voltage (V) in mV
) in 1. Standard deviation of V (E) m % s F or channe,
. Total chargeability (M) In 'et
. Number of pulses jsed (N) (mln. 3, max. 99) '
3y pressing the ROLL key, it is possible to read the data obtained on chan
nel 1, without stopping the acquisition.
To stop the acquisition, press the START/STOP key.
7. READING OF RESULTS
. By pressing RESULT CO (resp. RESULT CD, one obtains the averaged values of
Self Potential SPO (mV) and apparent resistivity ROD (ohm.m) (resp. SPi, ROD. W
the intensity value has not been introduced, the display will be RO s **, l = Q**.
- 5 -
. Then, by pressing ROLL, one obtains averaged values of Primary Voltage VO (mV),
standard deviation E f.%), total chargeability M ft.) (resp. Vi, E, M). If primary
voltage Is less than 1 mV, chargeability is not displayec ( M s ****).
. Then, by pressing ROLL again, one obtains the partial chargeabBlties of the cor
responding channel : M1, M2, M3 and M4 In the 2s program Ci.).
The two letters ST appearing at the bottom right of the display remind the
operator that he has not stored the last measurement.
8. STORAGE AND RECALL OF DATA
The STORE CO and STORE C1 keys permit to store the data of the corres
ponding channel. The number of the memory zone where the data will be stored is
displayed. Press CONFIRM key, or modify the number is necessary. The two letters
S" then dlsaopear of !*e display.
The RECALL key permits to recall the data corresoondlng to a giver memory
zone number : If the number displayed is not correct, modify It and press CONFIRM
key.
The data recalled will be displayed through RESJLT CO key whatever the
channel CO or Ci was actually used to obtain them.
The recall of a memory zone modify the parameters Introduced a-jring the
last measurement. Check them before starting a new measurement.
To clear the whole memory, press VCLEAR key, then CONFIRM key.
9. SERIAL LINK
. Transmission conditions : . speed 1 200 bauds
. format 8 bits, 1 stop, no parity
. ASCD character
. end of message LF, or CR LF.
. To establish connection, press the REMOTE key. - r - 2 emits a C character.
. Reading of values of a memory zone : R xxx, where xxx Is the number of the zone
to be read (C to 280^.
- 6 -
The H parameters stored In each zone are successively :
- a number characterizing the array (see table 1)
- the Injection time (1 or 2s)
- the l, S.P. V, E values
- the four geometric parameters (see table 1)
- the four chargeability values M1, M2. M3, M4
Note : The total chargeability M Is not transmitted. Its expression, In terms of partial
chargeabllltles are :
- for the 1s program M * ( 120 M1 * 220 M 2 * 420 M3J/760
- for the 2s program M * ( 120 M1 * 220 M 2 * **20 M3 * 820 M4)/! 580
TransmittersALTERNATOR
TRANSMITTER DUMMY LOAD
SPECIFICATIONS
Power input:
Output:
Cuircnt regulation:
Output frequency:
96 — 144 V line toni-iilr.il 3 ph.™-. 400 II? (from lluiitec generator set)Voltage 1"" - W)" V dr in 10 steps Current 04- K. A regulated"Less than ?O tt, change for±102. load changeOOWill* in 1 117 (time domain.coniplrx iesisli\ it\)00ti2 r)ll? lo 4 117 (lre(|irencydomain) sele( tahle on front panel
FrequencyaccuracyOutput duty eye le:
Output currentmeter:Ground resistancemeter:Input voltage meter:Dummy load: Temiwralure range
±50ppm -30c Cto *600 CO 5 to O 9)75 in increments of O 0625 (lime domain) O 9375 (complex resistivity) 0.75 (frequency domain)
Two tanges: 0-10 A and 0-20 A
Two ranges: 010 kn. 0-100 kl)
O-15OVTwo levels 2 k W and 6 kW-J4oClo^500C
Size 53cm x 43 cm x 43 cm Weight 50kg**Sm.iMer currents are obiain.WJr. Nit cHitMc/e the ciirrrnr
regulation range the fransniiirrr w/Lige is regulaled, mn the current
Specifications subject lo change without notice.
96 — 144 V line lo line 1 phase. 400 Hz (Ironilluntec generator set)
Voltage 150 - 22DO Vdc in B steps Current 02 — 7 A regulated** Less than *0 W, c hange lor ± I D'S, load change00()75 Hz to 1 H/ (time domain, complex resistivity) 00625 Hz to 4 11; (frequency domain) selef tahle from front panel An additional range of frcqiK-ru ies bc'lxveen O 78 and 5 O H/ is avail able and can be selected by an internal switch
±50 ppm - 30"C lo 16()0C O 5 lo O 9375 in increments of O 0625 (lime domain) O 9375 (complex resistivity) 0.75 (frequency domain)
Two ranges: 0-5 A and O 10 A
Two ranges: 0-10 kfl. 0-100 kn
O 150VTwo levels: 500 kW and 1 75 kW- 34"C to * 50"C53 cm x 43 cm x 29 cm26kg
SPECIFICATIONS
Output: 120 Vac 400Hz 3 phase 18kVA Maximum
Engine: 186 kW ait cooled twin cylinderhxir cycle piston engine with electric stall
f uel: Regular grade gasoline, lank capa city 14 L to give 2 h duration
Alternator: Star connected aircraft type, hell driven, forced air cooled
Output: 120 Vac 400Hz 3.5 kVAmaximumEngine: Briggs A Stratton 6 kW air cooled,
single cylinder four cycle piston engine with manual start
F uel: Regular grade gasoline, tank capa city 3.8 L to give 4 h duration
Alternator: Delta connected heavy duly auto mobile type, belt driven, air cooled
Construction: Tubular protective carrying frame with resiliency mounted engineand alternator
Size 51 cm x 48 x 76 cm Weight (dry): 61 kg
I, Richard Daigle of Timmins, Ontario
Certify
1. Three years of HLEM (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.
Dated
Timmins,Ontario. Mr. R. J. Daigle
Ministry ofNorthern Developmentend Mines
Ontario
Report of Work Conducted After Recording Claim
Mining Ae*
B^*J*kt^^vIVUmlMr
i coMadad on Ms form le obtained under ilw authority of ttt* ooBactton ahouU b* dtocted to Hw Provincial Mem Sudbury. Ontario, P3E 6AS. lalaphona (706) 670-7264.
Instructions: - Please type or print and submit in dupGcate 42*0*11*083 21*015 BRISTOL- Refer to the Mining Act and Regulations for 10*41*1. /mo vi imny
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.
.SQCU
d HoUwfs) OfentNo.
?0Jtttpttont Mo.
TowniMpMnei M or Q Plan No.
TocWork Performed (Check One Work Group Only)
Work Group Type
Qeotechnicel Survey
(ndudlng OrMng
Other Authorized
AssaysAssign mont bom
Total Assessment Work Claimed on the Attached Statement of Coste 33.^0/00Note: The Minister may reject for assessment work credit all or part of the assessment work submitted rf the recorded
holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.
Person* and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address
/^4*A4hAh A a nil a Aala Hf •men 4i vdivauiv n
Certification of Beneficial Interest * See Note No. 1 on reverse aidel cwtMy ttat at the tbm the work was performed, the cWms covered In tN* wortt
CertHKiauon of Work neport
orAganKSIgmtum)
OMI l hw* a peraoral knowtodo* of ttw tecta art forth In (Ms Work report, taring peffomwd the work or wttrMs complotlon md amend report Is trm.
i during andtar
and Adoraaa of f^afaon Caiwyino
Certltad By (Sgntfura)
For Office Uae Only
Details for tort Reoort t NEGNT94.343 Paqe l
Mork Reoortt iC'.aii Nuiber li of i for Aoolving li see note 2) IClaii!
Reserve lUnitslf P'IP
—————— l—-IP
————— '-l—IP —————— l—
/IP l —————— 1-' IP
/IPIPIP
/IPf I P/IPt I P
X P
————— i—f I P/i?x P'i?/IPi'ip
i —————— I-I ' IP
'IP/IP
ipIP
x IPIPIP
/IP1
/IP/IP
IP/IP/ p/p/p
0.495.3071 1
0.495.308! 1
0.495.3091 1
0.530.8841 1
0.583.2341 1
0.849.9631 1
0.649.9641 1
0.649.9651 1
0.757.6591 1
0.764.9451 1
0.916.8151 1
0.916.8161 1
0.938.3831 1
0.998.3841 1
1.159.6321 1
1.159.6331 1
1.159.6341 1
1.159.6351 1
1.159.6361 1
1.159.637! 1
1. 153.638] 1
1.159.639! 1
1.159.6401 1
1.159.6411 1
1.159.642
1.159.643
1.176.341
1
1
1
t. 177.8071 1
1.177.8081 1
1.177.8091 1
1.177.8111 1
1.177.8141 1
1.177.8211 2
1.177.8221 1
1.177.823
1.177.824
1
1
1.177.8251 4l
1.177.8261 2
1.177.8271 2
1.177.828 0
' IP 1.177.829J 1
i P
P
1.177.8301 2
1.177.831
X P 1.181.409
P' P
. P——————— h-
: IPi i.- Pp
1.181.410
1
14 1
1.181.4131 1 1
1.181.9351 2 1
1.183.2141 1 i i1.189.528
1.189.544
1
hrl
lvalue of AssesKntI lork Cone l
on this Clan. 523.00- 513.00
567.06
169.00
0.00
371.00
375.00
284.00
432. OP
0.00
C.OC
153.00
223.00
331.00
344.00
462.00
435.00
203.00
263.90
365.40
405.00
182.00
246.00
260.00
368. OG
257.00
51.00
0.00
0.00
270.00
0.00
0.00
1.073.00
243.00
577.00
0.00—————————
1.306.00
358.00
236.00 1 —————————
1.323.00
71.00
608.00
0.80
297.00
0.00
64.00
-yHtOO
0.00
value Aoclied to this CJiii
. 400.00——— *S* ———— 1
ieuc 44WW ttL fecO —————*^ * 371.00
375.00
284.00
400.00
151.0&
400.00————————— 400.00
—————————— , 400.00
400.001 ————————— ,
400.00————————— 400.00
400.00
400.00
400.00
400.00
368.00
257.00
51.00
160.001
160.00
160.00
141.00
400.00
338.00
231.00
229.00
831.00
158.00
42.00
400.0C
237.00
64.00
67*. 44rW
4C&.00
l values Assigned iReserveiior* to be: l froi this Clan i CiiiKd at i
523.00
513.00
567.00
fc- 16032.00
8.00
223.08
331.00
62.00
; '35.00
:
5.0C
270.00
1.073.00
102.00
577.00
368.00
127.00
7.00
492.00
566.00
60.00
•ttrftG
a Future Date '———————— 1i1———————— |
!
1 1 1
1
————————————— j!
i 5 it ii! it l ti
!1
1t 1
11
————————————— 1i
————————————— 11xr:-~™ —— — i
" - f
1
t
ii
i i 1l
l
l
l
—————————— !1i!l
! i —————————— 1
li—————— i!
. ————————————————————— 11 11
i 1 ————————————————————— 1
1i ————————————————————— i
111
iiiiii i i
iiiii
i —————— ii l—————— i
i i\ ————————— !
l———— i!
—————————— ii1
1 l
1 1
i
i
! i ^ —————————— !1 i
338.00
0.00
331.00 1
IP 1.189.5521 2 !-4-
I-IP 1.189.5531 1-i- 4- -t
Details for Bork Reoort l KEOKT94.049
1 172.001 ————————— i! 0.00i
172.00 1 ————————— i
1i
Page 2
Mork Reoortt IClaii Nuiber It of lvalue of Assestent for Applying K see note 21 Clan! lork Done
Reserve Units! ! on this Clan
/IP 1.189.5621 1
P 1.189.5801 1
P 1.189.532
P 1.189.593
/IP 1.189.764
/
fi
i
i
P 1.189.861
P 1.189.886
P 1.189.887
3i4
4
6
6
P 1.189.8881 4
P 1. 183.9141 1
P 1.189.915
P 1.198.802
P 1.198.803
IP 1.198.804
x P 1.201.162
1
1
1
1——
1
.ti
————————
c*-58*
Total Hunter of C'.aits
———
287.001 ———————— i ————————— i
Value Applied to this Clan |
287.00o.oo ;i0.00
0.00
1.200.00————————
119.00
1.742.00 1.483.00————————— ————————— i
64.00—————————
1.083.00
1.411.00—————————
1.645.00
1.961.00 2.358.00
1.772.00
0.00—————————
0.00
439.00
0.00
0.00
108.00
i ————————— i
—————————
—————————6i^
1.600.00
400.00
400.00
400.00
6K- QioO
! ———————————————————— 1
tt*-
piffle ac ^iitoctWrWTM ^irmrM-
Total Value Vork Total Value Done Vork Applied
Values Assigned 1 Reserve -.Vork to bel froi this Clan ClaiKd at
a Future Datei
1 i
———— O~~ 'ft*
259.00
172.00
1 ———— i
'
160 i
39.00 1———— ' ————
ir ~i L. ————— 1 ——————————— l
ftfTtt-ttMt;
i
i "- - V
———— i —— r— ——V- ,^'-^- i- J
5
i 11
- - -- . - . .
—————————
7iUrOG
7.509.06 j 0.00
Total Assigned Total Reserve Froi
i
ii 1
i
(Credits you are claiming in this reoort HV be cut back. In order to unicize the adverse affects of sue* deletions, please indicate froi which clans you wish to ononze the deletion of credits. Please urk it! one of the following:
i n li.! j Credits are to be cut back starting with the clans listed last, working backwards.
i "-12.1 l Credits are to be cut back equal lv over all clans contained in this reoort of work, l u
i n13.1 i Credits are to be cat back as oriohzed on the ittatched aooendix. } LJl n14.1x1 Credits are to be cut back starting with the clans that have r:ser.- e !?*-I "-Jlin the event that you have not specified your choice of priority, option one will be nolewnted.
Mote t: Exanles of beneficial Interest are unrecorded transfers, option oayients. Kiorandui of agreements, etc.with respect to the lining clans.
Note 2: If work has been performed on patented or leased land, please coHlete the following:
I certify that the recorded holder had a beneficial interest in Signature the patented or leased land at the tiK the work was performed.
Date
Ministry o* ' Norttiarn Oavatoprnant
Ontariodu
tf^^a^^bMMt^MBfeAM^ jfe. ftbMMiuevaMjppemani ou Nora ei des mines
Statement of Coste for Assessment CreditEtat des coflts aux fins du credit devaluationMining Act/Loi sur tes mines
NoJN* de transaction
JL i 5of Via
on this form te obtained inter the authority Las
be dtaectad to the
Act Thia information w* be used to maintain a record and of the mining cteim(a). Questions about Ms coftsction should
recueBs en vertu de te Lot sur teadans te preiente formute eont
ager. MMngs Lands. MMsny of NorthernDevelopment and lines. 4th Floor. 159 Cedar Sheet. Sudbury. Ontario P3E 6*5. telephone (705) 670-7264.
et eerviront ft tenir ft jour un regtelre tt gyssaon sur te i ^ ^
au chef provinaal des terrains mMers. rnMslere duDevatoppement du Nord el des lines. 159. rae Cedar. 4* etage. Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.
1. Direct Costa/CoOts direct* 2. Indirect Costs/Coflts indirects
Type
Contractor**
etdofexport-
MairHroeuvreHeld Supervision Supervision sur to terrain'DP*
M.AJC.U
TUP*
Amount
Total Direct Coats Total dee cotte direct*
Tow globalirk Indkecl coats are not
Pour te remboursement des travaux de rehabMatton. toe coots IndMects ne eont pas admlsaxitea en tantojue travaux tf evaluation.
Type
Food 4wd
f f.
AmountMontant
Sub Total of Indkect Coat* Total partM daa cotte Indirect*
(hot (n-. man 20* of mn* Casts) DM 20 H di
Total Value of Aae (ToM of Una. and
T* Total
6TiL
Nose: The recorded holder wtt be required to verify expenditures daimed inMkS* Ml^tmm^f* f^ jtsiMtm HaMkaM ^A jtmtm jrf m fin m i m at Inr nn.iBr niiriM Mma aufleraoni 01 CUBUI wnran jo oays or a reojuesi lor vumnauuu. n verification te not made, the Minister may reject tor assessment work al or part of the assessment work submMed.
:Ledlutain sgistrej tes dApsruosdanundses dans to present Mat des coots dans tot 30 Jours sutant une demande ft eel •Hot. Si ta vdnficstion n'oslou une partto des travatn (revaluation presarass.
Fling Dtacount* Rcmlios pour depot
1. Work Mad within two years of completion is daimed at 100* of the above Total Value of Assessment Credit
1. Las travaux deposes dans tes daux ans suwant tour achevement aontmeftionrfe
2. Work fled three, four or five years after completion is daimed at 504* of the above Total Value of Assessment Credit See calculations below:
Total Value of Ass**x 0.50 -
2. Las travaux deposes trote.qualreoucinqansaprestour achevement sont rembourses ft 50 4b de la vatour totate du credrt d'evaluation susmantionne. Voir tes cak
Vatourx 0^0 -
Certification Verifying Statement of Costs
l hereby certify:that the amounts shown are as accurate as possible and these costs were Incurred white conducting assessment work on the tends shown on the accompanying Report of Work form.
that asAgM. Portion
Attestation de I'etat des coots
J'atteste par la present*:quo to* montants indiques son! to phis exact possible at qua ces depanses ont ale engagees pour effectuer tea travaux d'evaluation sur to* terrains indiques dans la formuto de rapport da travel cHoint
i am authariyad Et qu'a tJtre de to suis autorisa
to make this certification a fair* cede attestation.
Stonebre
Note: Dans oMle tomwto. toraquTdfeigM das pwsormas. to •st tuffite au sens neutre.
Mining RecorderMinistry of Northern Development 6 Mines60 Wilson Avenue, 1st FloorTimmins, OntarioP4M 2S7
Dear Sir:
Subject: APPROVAL OP ASS1 WORK CREDITS OH MINING CLAIMSP.495307 ET AL IM BRISTOL, CARSCALLEN, DENTON AND THORNELOE 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 May 30, 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/1J
cc: Resident Geologist Timmins, Ontario
Assessment Files Library Sudbury, Ontario
REFERENCE'.
AREAS WITHDRAWN FROM DISPOSITION
MAO - MINING RIGHTS ON 1. Y
iMO -SURFACfc RIGHTS ONLY
Mtl M INING AND SURFACE RIGHT
Owmpwpi Order No Oft* U itpocttion Fi"
SEC 43/70 hEB 1/66 M - S 1/ISwC
DANA AND JOWSEr PARK Rt StRVE ; K O
sec ib/ao wee/es N0v ib/es MHO
HESERVEP FOX PU0LIC USE SftO
SURFACE RIGHT S OWL Y WITHDRAWN FROM i l AKINC, ORDER IWNBW 94/B-* DATED 64 JUl Y O4 (WASIt DISPOSAL SITE)
AND
APPLICATION PENDING UNDER THE PUBLIC LANDS ACT NOTICE RECEIVED 92-DEC-ai SNOWMOBILE TRAILS
THIS IWP
IMF INhOHMAHON THAT AI'P( AHb ON THIS MAC MAS BEEN COMPllfn FROM VARIOUS SOURC.fS AND ACCURACY IS NO I GUARANTEED THOSF WISHING TO STAKF MIN INC. CLAIMS SHOUI D C.ON SUIT WITH THF MININC. RECORDER, MINIS l HY OF NORTHERN UEVtl OC MEN l AND MINES FOH A() OITIONAL INFORMATION ON THE STATUS OF TMP
200
CARSCALLEN TWP.
JOwser L lm bW
5M
4M
IM
REYNOLDS TWP.
nii? l
l l 740* l
LAKES PROV PARK
1190600
i P /' ' ' V L
1 4.04? /^----J-*-"]!5 !'^ '
:1 L M. i \ f i 2/0 P IP'4*7,, i' 4 '79V
95l*6B 9U)967 84S4OS
LEGENDHll.MWAY AMI HOUTt Ni,
O ' Ut " H( )A[ i
THAIl
SURVt vt D l INf l,TOWNSHIPS flASt L INf' Ml - LOTS MIMNC, CLAIMS HARC^FL^ F Tf
UNbUHVt t t D L INfl ()1 l INfPARC t l BOUNhAHvMININt, C.I AIMS F TC
HAILWAY AND MIGHT OF WAY ^
UTll IT Y i (NFS
NON PF RFNNIAL STRFAM
F LOOOlNCi OH F lOODING HIGH IS i
SUBDIVISION OR COMPOSlTF PLAN
RLSF RVATIONS
ORIGINAL SHORF LINf
MARSH OR MUSKF(, MlNf'
THAVt RSF MONIIMF S T
DISPOSITION OF CROWN LANDS
TYPE OFDOCUMtNT SYMBOL
PATfcNl SURFACE 4 MINING RIGHTS . .. .... -. 0
SURFACE RIGHTSONLY . ... ft
MINING NIGHTS UNLY .... Q
LfcASE SURFACfc 4 MINING RIGHTS..... . . B
SURFACE RIGHTS ONLY . .. H
MINING HIGHTSONLY ............... ....... y
LICENCE OF OCCUPATION .. ............. - .......-.. TORDER IN COUNCIL .......... ..., OC
MOIt MiNiN'i Hi itl^ iN KAHlll^ rAI^NltLt^KI'.lH IUMAT b
^.^ tti) VMTIO IN ONlClMAk PAT|NTi( |V THf PUCLICW**^ t*ND( ACT M IO 1*70 C H A* MO MC *3 tuMtC i
SCALt 1 INCH 40 CHAINS
1IMHI .'(MM •000
TOWNSHIP
DENTONM.N R ADMINISTRATIVE DISTRICT
TIMMINSMINING DIVISION
PORCUPINELAND TITUS/ REGISTRY 1
COCHRANE
Mmistryof
BranchOntario
0*i* M tt l * M l 'l 1C
Al I VAII l." 1 hi l
Ut "r ill6-3224
REFERENCESAREAS WITHDRAWN FROM DISPOSITION
M.R.O. - MINING RIGHTS ONLY
SR.O - SURhACE RIGHTS ONLY
M.+ S -MINING AND SURFACE MIGHTS
DMcription OreUr No Oat* Diipotition File
3F.C 43 HO 17/5 1 It S KO lk,4it)4
SAND AND GKAVt L.
GRAVEL F"f 14.5834
MN.R 6KAVKI Kfr'SfiW
MN R (.HAVirl PIT 25a HLt IU4C7
f J) I HIS TWP. SUBJECT TO FOREST ACTIVITIES IN ' 1994/95. FURTHER INFO AVAILABLE ON FILE.
NOTES
Rtiirvotion for Deputy Chief Ranger's Headquarters site thown thut l?......... File: 110657
Flooding Rights on Kenogamissi Lk S Mattagami R art rwerved to Ont. Hydro — L.0.7598. File; 1163 vol.3
i HIS TOWNSHIP UF.S WITHIN me MUNIQWVI 11 ^ 01THF CIT 1* "r "MMINS
(u IK APPLICATION PENDING UNDER PUBLIC LANDS ACT v—— NOTICE RECEIVED 93-MAR-30
(SNOWMOBILE TRAIL)
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 H6REON
Bristol Twp.
5M 4M IM
83*448 92J6OI | 9P380."
l 9560 T/ 105*076 ll (4 UNITS)
——-— -— -() (2 1JNIT3)
\ ^97639 l 1 1 / 827* |"796T30 ' R
(9JUNI1S)
5M
Me Keown Twp.
LEGENDHK.MWAV /TJI) HOIITI Nil
O IHI i HI )A[i',
l HAH -
SUHVI ^i l l) l INI '.
lOWNbHII". UASt l INf-S ETC -
l O!' MININI , l l AIMS PARCELS fc TC
UNSUHVI i MI MNI Sl O l l INI .PAIU l l HdiiNDAHYMININC, l l AIM 1. \ K ,
RAH WAV AND HlliHl m WAY f
Dill II Y l INI ' ,
NON I'f Hf NNIAI STHIAM
F l OiHMNi, i )H l l (HH)ING RIGHTS
sunn!viMiiN tin i f)MPOSiTi PLANHtM IU A l ION'
ORUilNAi ,HI 'ill l IM
MARSH DM Ml ISM-(i
MIM S
THAVI I'M MONUMI N f
DISPOSITION OF CROWN LANDS
JYPE OF DOCUMENT SYMBOL(f)or 0
eQ
L Q or
OC
PATtNI biMUAC t ft MINING RIGHTS
SUM! A( f MICiHTSONLY ..
MINlNd HK.HTSONLY ..
LEASE bUHi A( f A MINING RIGHTS.SURhACb RIGH1SONLY.- . ..
MININ(, HIGHTSONLY. .-..
LICENCE Of OCCUPATION ...-.. --
ORDfcR INCOONCIl . .
REStRVAllON
CANCf l l E O
SAND K, f.HAV i l
NOTf. MJNJhU HlUMIb IN PAHCfcl-6 PA l tN l tO ^HioH to MAr 6. IMHf MTi* M* OmaiNAU PATVNTil RV THK PUBLIC LANO* ACT * t O 1*70. CHAP MO. Of Q 03. OUMIC 1
SCAl l l INCH 40 CHAINS
4OUU hOOO 8000
l OOOl l " Ml
2000(J KMI
1601 5TOWNSHIP
THORNELOEM N.R ADMINISTRATIVE DISTRICT
TIMMINSMINING DIVISION
RECBVfr.D
i 19'JSPORCUPINE ' m *LAND TITLES/ REGISTftjlAMtttSiail ,u
MINING ANP SURFACE RIGHTS Rt-OHtNFD TO PROSPECTING, STAKING OUT, SALE OR LtASE UNDER SECTION 35 OF THE MINING ACT R.S.O.itt o ORDER NO. o-p.ee/9e NER
IHfACi HI6MTS WTTI190AWN
IT 7|00 AM f-6.T. ,. O (USfM INCU
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
MHWM AND SURF ACE RIQHTt RB-Ore*P TO PROSPECTING.
OOUT, SALC OR LeAWSECTION so of THEACT (U.O. IWO
ORKR NO, 0-P SO'M NER PAtEO 9t-NOV-Ot AT 7 00 AM/fet'i** "OJ P 4tO*Ot TO f--4t03!3 INC L AND P-4tO5(t)
KEY PLAN For O.B.M. Map
ao ir
to ir
4800
4800 88800
17 4000
17 4800
83800
83800
not to scale
Ul
l
S10f
^GODFREV TWP. G-Or-
"66000 mN
"?00 i
O) M
50
H48 1147
J*V
4-ONttS
II697O1 N l lli
, i(gtSlTS) \ 1 '
~" fp~ ,~i 'p ~" H' ^ 1 726367
1190994 l1 f '
^ ^ - J 1 1Krt TA k .^.^x^^^A. 1 i \
i 1
/253ro
p785)56
n
i ^ i
, 1
-fOtt a.^.^ 1 'CjOj^ |
1
1P- p.
7^^3^3 i "
1l
729331
ratistie(
09*60 00 mN
50
l 1200497 1200496
15 UNITS
120^520l? UNITS)
FT-n———p- ———I200b0l
16 UNITS
1200498
16 UNITS
P NO ^PEN GROUND H
l 949636 y 94MS7 \V \ \
'"*
^ 'IP 1'iosoiTo f v '"{^^^ —ip- — — —^V- — — —il l ' i M. k ...it.. . Ir m vr ,
UNSURVEYtD l INESIOT LINESPARCEL BOUNDARYMINING CLAIMS ETC
RAILWAY AND RIGHT OF WAY UTILITY LINES NON PERENNIAL STREAM FLOODING OR FLOODING RIGHTS : SUBDIVISION OR COMPOSITE PLAN ^ RESERVATIONS ORIGINAL SHORELINEMARSH OR MUSKEG . " '* MINES TRAVERSE MONUMENT
DISPOSITION OF CROWN LANDS
TYPE OF DOCUMENT
PATENT, SURFACE ft MINING RIGHTS SURFACE RIGHTSONLY .. .
.MINING RIGHTS ONLY . . LEASE. SURFACE 8, M INING RIGHTS.
SURFACE RIGHTSONLY , ..MINING RIGHTSONLY
LICENCE OF OCCUPATION ...... ...ORDER IN COUNCIL . ... .RESERVATION . CANCELLED . .,. SAND&GRAVEL ........ .,.., ..
SYMBOL9
...... e
B v
oc
(D(D
NOTE M INING RIGHTS IN P ARCELS PATENTED PRIOR TO MAV t 1813 VESTED I N ORIGINAL P ATENTEE tv THE PUBLIC LANDS ACT R SO 1 970, CHAP 380 SEC 03 SUtSfC 1
&00M*lr*t
10 O Chdnt - - - n t- —
400 O
1000 — M*lr*t
10 20 30 40 SO 10 TOChain*
1000 2000 3000 4000 iOM,———————— Ftfl
SCALE 1:20 000ZONE ' 17
APPLICATION PENDING UNDER THE PUBLIC LANDS ACT NOTICE RECEIVED 92-DEC-2I
APPLICATION W* CWWN LAND UNDER THE PUWJC LAND* ACT NOTWe RECEIVED 9J.MAY-4 ^^ CM EXCAVATION TOP SOIL HOCDMO STORAOE ETC-
THIS TWP SUBJECT TO FOR! AREAS DESIGNATED EXACT! Til
MAY 2 6 1995
MINING LANDS BRANCH
MIN8.
- } 'f r, W5
2.1601 5
TOWNSHIP
BRISTOLM.N R ADMINISTRATIVE DISTRICT
TIMMINSMINING DIVISION
PORCUPINELAND TITLES/ REGISTRY DIVISION
COCHRANEMinistry ofNaturalResources
LandManagementBranch
OntarioORIGINAL COMPILATION JULY 1 984
ACTIVATED JULY 13, 1992 8r DCREVISED
CHECKED BY C.W
Numb*i
G-3998
QCO Q) Q) GO
COocCO
o
00 CD CD CO
O
230
1O1SIUB 91091 Z C9003N90V2V
tMM9/ J ZU6BS
iiww
j^Z9S6*ll| j'
(sunn v) l j -ittwe jx'wwie ^~ - n ~ •~*~ ~ ~* -^ *" * "~* ^ "
^8968111 l , ^-^-—-l 9996911
RES IP MF 3382., 41 55-,
1691
1
O,
RESISTIVIIY
ohm/maters
OiRiargeabilityCM1
mV/V
etal factor /rae * 1000
2-1 2 8.
Oj Oj
-i—i—-T- T r i i i i i i t ' i fi i - r - t t i - r i T r T - i T ' r ' i i i i i i - r - i " i t - i - 1 t i t i i t i i t r i
L—l l l l I i l l l l l l l l l l J l . l . l . l l l . l . J . l l . I.. l . L -..L-. l l i l l l l l . l . l. l l l l l l i l I i __ .0 l O O
MF IP -55 r4 1
1691
Chargeability
Resistivity
^6(W)ON f t 70+00 N ( ( 71+00 N^ 72+00 N ( ^ /MO N ( f 74+00 N ( ^ 75*00 N ( t 76*00 N ( t 77*00 N /B+00 N TWO N 80+00 N 81+00 N
Port-upjno Mining Division M. C. Exploration Services Inc . Sept 1 99'
RE.S7775-
iiijii
3887Jiiijiii
0-.
IP MF76^ 7.,
'
3 8-j 35.
J
0. OJ
i — T -r t t r - r T - i— r T t r — T - r - T i i i i i t i i i i i r i i i i r t i r i i i i i i i t i i i t T i i T i r r - i - 7 r - T i i i t r - , , , T i i ' r T i i t i i p i
RESISTIVITY ohm/meters
OinCO irgeobility
mVA
rtal Factor
is res * 1000
4- - 4. _U ..J i i i i . i - i . i i i i - -i -. J. . J~ - J . i i i i i i i i i i i i i i i a - j. i i i i i i i i i .. L— j.- a i j i j__i_ i i i .j_ j ii. - L i i i i i i.i.i i i L . i t. i 1 ' ' ' ' ' - i J i.i-i L i .. a
7IP RES
77/5
L.3 i) u3887
LO LO ; o
/////^///^/)^^^ ?w''?frw///^ Chargeability
Resistivity55*00 N 56+00 N 57+00 N 59*00 N 59*00 N 60+00 N 61+00 N 62+00 N 65*00 N " 64*00 N 65*00 Kl 66*00 N b7*00 N 68KK) N 69+00 N /O+OO N 71+00 N 72+00 N 73+00 N__^ i 51+00 (^ ^
Porcupine Mining DivisionM C. Exploration Services Inc . Sept 1994
REb I P M F5498
2749
55., 81-,
8-| 4 1
0^ Oj 0.
RLSISIIVII'Y ohm/meters
ChargeabilityCO mV/V
:tul h actor /res * 1000
l t l l l l 1 ' l ' ' ' ' ' T, , , i i i l i l i i i i i i i i i i i i i l i l l i i i i ' l T l i i i l i i i i i i i i i l l i i i i i i i i i i i i i i i t i t i i r i i i i i i i i Mf- IP RES
i i i i l i r i r i i t i i --r i i - i - 8 ' r5 b -5498
l
\
\
41 1-28 r2749
L . J. . i l i i i i i i i i i i i i i i i i i i . l i i i i l --i - l i i i- i . l l i i i i i i i l l l i i i i i l i i i i i i i i i i i i i l i i i i i i i l . i l j . l
66+00 N 6/tOON 68+00 N bSKW N 70*00 N 71+OON 72*00 N 7^*00 N 7++00 Nt l t t ' ( . t . l t l t 4 lit t . ( . i l i l t t t *
38 47 58 69 74 74 62 53 49 44 35 28 24 23 24 31 3
75iOO N 7htOO N 7^7+00 N 78+00 N 79+00 N 33 25 3? 32 J8 26 26 21 21 16 filter
l ' 34 /V\V" i'^- "' '''^''l / b ' b J ^ ' 4 ' _— ___— —~' J ' ' ' *\. v—^' -— 4 l ^ x 68 .-^, 4 *^^±l.'^. 4 l i - 6 S y s 1^L---' 26 28-, 3^^, l fl n~1' X \ \ V ' ~~-~" ' 4 ~-^— '-I^n8 ' J ) * b 4."-' b — S1 f ''' JL* " 7f-1 "''"'' 6~\ ' i ^JJ^/s 4 2 '/~ V lT^~2 I ——2~6 J 4,4-^24 ?J,-^l8 "Ti"~—-2 n ~i
Jl \15 ~"56'~^6 2''"—- 7 — - '^ 6 l ^..^ 5 4/45 41 r J 4 18 15 12 21/41 -"^t 1 /.X/ l l 7 l l l i 9 S It S 3 /"\ 'l 4 l 1 l l n- .A-,,—x \.. .. . .-\(..s~^ S ri / /- ./(..y/Cr^XA48 48 47 \64____63^ 69^ (9-^ S 6 y 4 / "l '
27^^51 ^ *2^~- 4 9'" 4" 5 ~-; 5 l ,. 5 9 A J l' 2 2-'^ l 6 l lS ^ N VC \ (: 4 6 4 46 5 5 - 7 5 ^ 5 7 x 3 l v l b 1 15 2 4 ' 4 2 ''' l 4 18 l -25
18 l 2 X 3 -—''' 26 X X' 46 134 \ M l
13/29 21^/52^42 ( 2 4 ( l
l 8
s*i / /*.7 x \46' /9
n-4
0=6
RESISTIVITY ohm/meters
ChargeabilitymV/V
Metal Kit tor ip/res * 1000
MAY 2 6 1995
MININGFiTTel
** *
* * ** * * *
7?bOt.
Pole Dipole Arraya
i
l
no
plot point
.LGrNU
Coni Inervl's,Resistivity , 500 ohm/meter Chargeability , 1 O mV/V Metal Factor , 5 7,
Profiles
Instruments. URGM IP2(Rx ), Scmtrex ISQJ(Tx) IbSOrnSec lotol Intergration Time, 420rr6 Delay 8Second lotal Duty Cycle. ?Ser On/Oft Time
Porcupine Mining Division M C", Exploration Services' IPX, C'*ep1 1994
KLS IP MF 6966., 61 96, ,
3483
KtSISIIVIIY ohrn/meterb
hurgeability niV/V
3tal f actor /ros, * 1000
48
OJ
I l l l l l l l l l l l 1 i p i i i i i p i i i i i i i i t i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i 1 l 1 l l I l l l l I l l l i i i i i i i i i l l l l t l l t l l l r-- , ,
1 l l l l l l I l l 1 l l l l . i l l J l
46 i 6 1 ,6966
48 i J481
Chargeability
Resistivity
filtern^l
n-2
n J
9*2
51+00 N W+OON tftOON 1)4*00 N &+00 N 56+00 N 'i/.OO N ifr+OO N KMOO N bO+00 N bl+00 N 62+00 N 6iHX) N 64+00 Nt t * i f t i l l * t * l ' t l ' l * * l |t|(l*tttt(tft(t*t|-*— -l————* t * l * t -* t t t t
NOKANDA L'XIWltA'nON Co LtdInduced I'olan/ation Survey
I'tojerl SO/NfS 42A f) l t ,
Porcupine Mining DivisionM C Lxploraiion bervi(..es Iru L*:pt 1 CJ(
KLb IH 4907 9 i
MF17*-,
.2454 4 b , 86
Rr.,lSllVITY otiin/ meters
argeabihtyCO rnV/V
ital Factor/res * 1000
r i i i i t i i i i i i i i i i i l l l l l T l ! l 1 l l l i i i i r t i i i i i " i ' r ' l i i i i T i r i i i i i i i i i t r i i i i i i i P i i i , t , ,i i i i i i i t i i
Mi-
XX
h- --i---*-
J. l l l l l l l l l\
l l l l l l ll — j. - l l l i —l——l - l i l l l l l —l——U l l l l . l l l l l i. . l l l l l i i l l l l l -l l l ..l l . i . l 1 l l l l l l l l l l 1 l l l l l l . l l i L., i.
IP 9 490/
8 h |.4 b i /4M
l O
_____ _ —. . — a . — z- --"—i f~f ' s .'"*". - .r. 4" *.~ •Vt*^~*rt-~' * ' l i^jt^r SIX 'X////// '////////AT/ ivv,- i**••i..:T
4' 4 4 ' l 37 X4 8 r b l 41 48 s) 67 . ^3-^^ 5.7 7 8f ) f -^ N ~" 7 ' ^ ^- - '" —"
* 2 b 7 7 4 ' J ' 3 ' -" ' * ' 8-23 , 740 SO 40 60 S , 4 9 — - 46X3 7 J t 4 6 4 4 b f 6 5 ^ 6 "' -, 7 6 . "7—7 l.r^^' 6 ^.. 8 6 r 6 l ^V 3 6 i 2 — ~ 60 60 t l 6 5 _ - 45 ___ .4 2 31 ^ __ 3 3/19 l 2 5/17,^3
70 , 3 7 ~— 3 t 3 3 3 3 \ 2 6 \ \ ^ju ^\^-^^^ v -- . .-.Jiin \ ^l ' 89 "75 61-'-84- 71-' 5 6 ~ 48 V 18^ / l . - ^ j /^ s
'42 39 29 27 74^16 17' 24 27' X5 7 7 l n40 40 20 Ih ' \ l t 14 32 28 31 4 46' b l
^ 2 8 N \ l
~ 2 2
RFSISIMFY
ohmXrneters
Chargeability
Metal r actoripXres * 1000
MAY 2 fi 199.S•JUC i ,, ,
67501
Pole Dipole Arraynu
Hlter *
V60* ^
50M
LLGLND
ProfilesCont Inervl'sResistivity , 500 ohm/meter Chargeability . 1 O mV/V Metal F'actor , 5 %
Instruments; BHGM lP2(Rx ). bcmtrcx 1580mSec lotal Integration Time, 4^0mS Delay. SSecond Total Duty Cycle, ?Sec On/Off Time
low effect
mod.low effect
mod.high effect
high effect
bO O
Section 6bcale 1 bOOO
bO 100 1bO ?00 JOO
(meters)
NOKANDA UXfWKATION To LtdInduced Polarization Survey
Project 507N1S: 42A b f b
Porcupine Mining DivisionM. C l xploration bervice^ Inc.. bepl
RES 2993.,
1497.
KtSlbTMTYohm/meters
O argeability 10 mv/v
•tul Factor 'res. * 1000
Mr 8 9^
4 "i
i i i i l i i i i i i i i i i i i ' 'l l T l l I l l i l
I l l l l l l l l l ' l i i i i i i i i i i i i i l l l l . l . l l l l l l __L l l l l J. --l l l l l l l l l l l l l l l l l l l I l l l l l l l l l l l i l
Porcupine Mininy DivisionM (, l jxploration t^rviccb Inc V:pt 190
RE.S IP MF 4710-, 88 8, ^. , , , , , , , , , , , , i , i , ,
2355
0.
' l l
4 4.
RFSISriVIIY ohm/meters
rgeability fnV/V
ti ul factor68 * 1000
l l l
oJ oJ
i i i i t i r i i i i t i i i i l i l i t i
l l l l l l i l l l l i i i l i i l . i i i i i l i l l l i l l l l i l l l l l l l i l l
filter
T^/7/TZHT^ y '-*-: * -^-''-' ~"' - V- V ' - - ' l JM '/]S.-?~ - - -. '-j ^'-- ."t*. ,jv ' -^ •-.'.-.•V-T7 t -.y i-.-'y f-^'tov'*-1.1 * yrff///^
4 51*00 N ^ , 52*00 N ( . 5J+00 N ( - M+00 N ( 55*00 N ( . 56*00 N ( 5?*00 N ( 58*00 N ( WtOO N t 60*00 N 61*00 N 62*00 N 280(1 1846 2/55 2248 2416 2/66 3258 3805 4282 2861 2/13 16/1 1501 1350 1280 1218 1134 1181 I2li 1348 1502 1683 118 2073 282/18 2806
' ' ' ' T" ' ' ' ' ' ' ' ' ' l l . i l , , , , , , ,
' ' ' ' r r , , - , ,
i l - i i i i i i i i' ' ' ' ' ' ' ' ' ' ' ' -i . . , , , , ,
' ' ' ' ' ' i i i , ,
mm'tm*5* :±::-^:f:: ^^m^msmaz^s^ - ^ ~~.—-' ——— —— '————*— ' ~—* .-^-- -- * ^'.' .'. ^^//7jj)j f r ~i i 11, . 1 .,———^L ' . * i f i * ' -; - ,.'. **t~T~— —Bggja^j^^^^/ag^L'a^^atT, ~...,\^ s rrr^.
2375t00 N- , . 67^ N. , . f*00 N , . 6BJOO N ( 70,00 N
-l——r~ r --, r i-t—t -r- i—r~i T - i -T - T |—T-I-T-T r~ "i i -r" i -f —T T-I i'i——t -~i—r-r i T-I r - r-i - t - t - i l r-f-r-'-r- ' T - i i i i t - r i T - t - i r - i - T i i i i i i l l
*jPAlt , .-*J?M -*- 70+00 N ( 71+00 N 3 2* 26 25 27 l* 32 IS
72+00 N 73+00 N—*-—t.—.—*.- -* *- —*1 0 l 13
, 7**oojlL t . T5*®^2 2* 36 37
^ 76+00 N^
21 3 1
77+00 N 24 3.1
78+00 N 79*00 N 80+00 N . 8.1^
25 2 3 filter
2 J J 2 2 2
51+00 N 52+00 N1
53+00 N ^__54+OON ^ ^ 55+OOJ^ ^__ 56+00^
11 12 12 13 14 13 12 12
5/+OD N 59+00 JJ 59*00 N ^ 60*00 N
l l 11 13 12 12 12 11
61400 N 62+00 N
l 11 to
63*00 N ^ 644QO N
70 B 10 K)6&JOON 66*00 N 67+00 N
0 (O 80 W i
. ®JOO N 68+00 N ( ^ 70*00 N
11 1 14 17 21^ 71+00 ^ __ 72+00 N 73+00 N 74+00 N
33 55 28 2 IS 16 14 2
76*00 N 77+00 N 78+00 N 79*00 N80*00 N 81+00 N
2* 35 2t 13 21 1* 2 t 31 22 13 12 16 17 li It f]|t er
21 26
17 1 t / 0 J 1 2 f~80~ ~-J1 11 It It 13 ___M 13 M 14 IS 14 14 ^ l l ' 1 J 12 li 13 12 li/ 60 B B 60 rt\l l \ 70 ^90 13 14 ^^/^~**\ ' 7 2 i t-—T 4 ]j^^^^W^i^^4.——-x J4 X^xl7 17 l \ fi 5 8 ( l J 2 8 l^||S^Wn 2 iffl^^^Httl'* ^-2 5\ -l ^18——- lT~—II——li 0=2
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