area : report no: 26 bell lake work performed ......notes: (1) w9230.0052, filed dec/92. 52gtssweeea...

D 52Gi5swaee2 ae BELL LAKE 010

DIAMOND DRILLING

Area : BELL LAKE Report No: 26

WORK PERFORMED FOR: NORANDA EXPLORATION CO. LTD.

RECORDED HOLDER : SAME As ABOVE: OTHER [ ]

CLAIM No,

430682

430682 and 312526

HOLE No,

S92-1

S92-W1

S92-W2

S92-W3

S92-W4

S92-W5

S92-W6

S92-W7

FOOTAGE DATE NOTE

1507' MAY-JUNE/92 (1)

750-1077' JUNE/92 " (wedged from S92-1 at 750')

900-1222' " " (wedged from S92-W1 at 900')

790-1137' " " (wedged from S92-W1 at 790')

850-3067' " " {wedged from 92-W1 at 850')

2743-2763' " " (wedged from 92-W4 at 2743')

JUNE-JULY/922723.5-2848' (wedged from 92-W4 at 2723.5)

2676-3317' JULY/92 (wedged from 92-W4 at 2676')

NOTES: (1) W9230.0052, filed DEC/92.

52Gtssweeea zs BELL LAKE

NORANDA EXPLORATION COMPANY, LIMITED (no personal liability)

REPORT ON GEOPHYSICAL SURVEYING

AND DIAMOND DRILLING 1992

GROUP 51 - SIMAX OPTION

N.T.S.

NORTHWEST ONTARIO DISTRICT

•y""?*"?

. ' ! .f-.———

\; !i '",f

^ IH; O^ 5 --3— i: -n2 on

roz:SCO

2.

6 rn

PROJECT NO. 1392 THUNDER BAY, ONTARIO JULY 21, 1992

JOHN GINGERICHSR. GEOPHYSICIST

REG FELIXSR. PROJECT GEOLOGIST

Table of Content*

1.0 INTRODUCTION

2.0 LOCATION AND ACCESS

3.0 PROPERTY DISPOSITION

4.0 GEOLOGY

5.0 PREVIOUS WORK

6.0 PERSONNEL

7.0 INSTRUMENTATION7.1 Magnetometer Survey7.2 Large Loop TEM Survey7.3 Borehole PEM Survey

8.0 DISCUSSION OF RESULTS8.1 Magnetometer Survey8.2 Large Loop TEM Survey8.3 Borehole PEM Survey

9.0 1992 DRILL PROGRAM9.1 Discussion of Results

10.0 CONCLUSIONS AND RECOMMENDATIONS

List of Attachments

Figure 1 Location MapFigure 2 Property MapFigure 3 BHPEM Type Response CurvesFigure 4 Borehole PEM SystemsFigure 5 Modelled X-Y Data

Map 1 Magnetometer ValuesMap 2 Magnetometer Contours b. InterpretationMap 3 Longitudinal Interpretation

Appendix l Geonics TEM 57 3-Component ProfilesAppendix II Crone BHPEM 3-Component DataAppendix III Drill Logs, Cross Section, Geochemical Analyses

Page

1

1

1

2

3

4

4455

6677

88

13

Scale

1:1,000,000 1" - tt mile

1:4,800 1:4,800 1:4,800

1.0 INTRODUCTION

A total of 16 km of grid establishment 18 km of total field magnetic surveying, 10 km of Large Loop TEM, 6 holes BHPEM and one drill hole were completed between March 1st and July 13, 1992. The work area straddled the Group 51 - Simax property boundary in the vicinity of Claw Lake.

The objective of the work program was to evaluate the eastern extension of the NBU-Sturgeon Lake stratigraphy focusing at the top of alteration as defined by whole rock geochemistry. Previous work had concentrated on the north dipping (SOo) structural trend associated with the Lyon Lake- Sturgeon mineralization (NBU Horizon) and the Santa Maria footwall stringer zone. The vertical extent of the alteration zone remained relatively untested.

2.0 LOCATION AND ACCESS

The Group 51 - Simax properties are located immediately east of the Lyon Lake-Sturgeon Lake mines which along with Mattabi, lie in the Sturgeon Lake mining camp located 50 km north of Ignace and 250 km northwest of Thunder Bay, Ontario.

Ski-doo or knodwell access to the properties is via old drill roads which extend from the Sturgeon-Lyon Lake mine roads. The property can also be accessed by float/ski plane to Claw Lake.

3.0 PROPERTY DISPOSITION

There are 3 claim groups within the work area. The Group 51 claims are original Mattagami Lake Exploration holding staked in 1969. The Santa Maria block are patents recently optioned form Simax Oil and Gas. The Norex claims are recently staked lands which tie onto the east and south sides of the aforementioned patent blocks.

Group 51:

Group 51 consists of 42 patented mining claims which are 100% Noranda owned.

205364-366 3225735-740 6225742-745 4225780-783 4312518-523 6312525-529 5325402-404 3325406-407 2330289-291 3330311-314 4330342 J.Total 42

90*

STURGEON LAKE PROPERTIES

NORTHWEST ONTARIO

LOCATION MAP

GROUP 55L—

r-TV^ 01/2 1

NOREX CLAW LAKEGEON

AIM HEAR

Simax Option:

Noranda has the right to earn l OG^t of the Simax Oil and Gas, Santa Maria property subject to a 2 y* Net Smelter Return and payments of 1105,000 over 4 years and exploration expenditures aggregating $500,000.

Claim Number

PA 430679 PA 430680 PA 430681 PA 430682 PA 430683 PA 430684 PA 430685

Claim Number

PA 430686 PA 430687 PA 430688 PA 430689 PA 430690 PA 430691 PA 430692 PA 430693

Total - 15

Norex:

The recently acquired '\QQ')k Norex claims are:

Block Units Recorded

1144050114404911440511144048114514911957391195740119574111957421195743

121212161616161214

Total- 117

October?, 1991 October?, 1991 October?, 1991 October?, 1991 June 17, 1992 June 17, 1992 June 17, 1992 June 17, 1992 June 17, 1992 June 17,1992

4.0 GEOLOGY

The South Sturgeon Lake volcanic belt is a north-facing, steeply dipping sequence of mixed Archean tholeiitic to calc-alkaline volcanics approximately 25,000 feet of thickness within the Wabigoon Greenstone Belt of the Superior Province. The volcanic pile overlies gneissic Archean basement and is capped by 3000-4000 feet of Timiskaming-style sedimentary rocks. Mattagami personnel subdivided this belt into several laterally extensive mappable units which have been grouped into three volcanic cycles by Franklin et a) (1977). The majority of the Sturgeon Lake area massive sulphide deposits occur within or at the top of felsic voclaniclastics that are thought to delineate the termination of the lowermost volcanic cycle.

Relatively mild deformation has affected the South Sturgeon Lake region. The sequence is a steeply dipping, northward facing homoclinal sequence, the result of a major period of folding about an east-west axis. The fold axis of this synclinal structure lies near the north shore of Sturgeon Lake. A second mild deformation around a north-south axis produced a gradual concave arching towards the east with resultant changes in strike from 90* on the Mattabi area to 12Qo in the Lyon Lake area. A penetrative axial planar cleavage associated with the east-west axis is pervasive and partially well developed in the fine grained tuffaceous rocks.

Regional metamorphism is greenschist and locally almandine-amphibolite rank (Trowell 1964).

Within the Sturgeon Lake mining camp, three mines were put into production with some production also from the F-Group pit.

Deposit Tonnage x 10* WtZn *fcCu WtPb OptAg

Mattabi 12.55 8.28 0.74 0.85 3.31F-Group 0.38 9.51 0.64 0.58 1.92Sturgeon 3.95 6.53 1.24 0.63 3.42Lyon Lake 3.17 8.67 1.26 0.99 4.50

5.0 PREVIOUS WORK

The area was first examined by Mattagami Lake Mines in 1969 with an Airborne INPUT survey carried out by Questor Surveys Limited. Later, INPUT surveys were completed in the Post Lake and Harmon Lake areas north and east of the original flying. More recently, the OGS (1991) re-flew the belt using the Aerodat HEM system.

Most of the ground geophysical work was done on the property was by Mattagami Lake Exploration, which later merged with Noranda, and by Falconbridge Copper which later became Minnova.

Exploration on the Simax group was originally carried out by Santa Maria Mines which lead to the discovery of the stringer zone mineralization which was drilled by Falconbridge, Noranda and Minnova.

1969: Group 51, 84 claims originally staked after completion of the Questor Airborne Survey. Ground mag and JEM surveys were completed on reconnaissance grids over defined anomalies.

1970: Group 51 grid established and surveyed with mag and JEM. Five holes were drilled with no significant results.

1971: Radem, VLF, soils and mapping completed.

1972: Follow up Crone CEM was completed plus 5 diamond drill holes. Holes 72-9 and 72-10 intersected the NBU horizon but no mineralization present.

Drilling by Falconbridge on the Simax property following up an IP survey intersected one hole of economic (?) mineralization G.64% Zn, 2.62'*. Cu/14' (LLM-17).

1973-74: A total of 7 holes were drilled along the NBU contact. Best results were 0.1 Tfc Zn, 1.77-* Cu/4.5' in hole 51 -14,1.45**. Zn/16.5' in hole 51 -15 andl .01 (* Cu/12' in hole 74-16.

1974-75: Mattagami optioned the Santa Maria claims and carried out IP, mag, VLF and VEM surveys. Two holes were drilled and their previous holes were deepened. In this area, the best mineralization corresponded with the IP zones.

1976: Four additional holes were drilled on the depth extent of the Santa Maria mineralization. It was found the magnetic high areas were associated with magnetite alteration which was generally sulphide poor.

1982: Two additional deep holes were drilled on the J. Hinzen model of a proximal volcanic contact.

1983: An additional deep hole (51-26) was drilled.

1985: Hole 51-27 was drilled but appears to have stopped short of the alteration zone.

1986: Minnova drilled 9 close spaced, shallow vertical holes on the Santa Maria block. No significant results.

6.0 PERSONNEL

The ground geophysical surveys were undertaken by R. Swire, C. Ritchie, B. MacLachlan, G. Doucet and C. Sedleski. All are employees of Noranda Exploration Company, Limited, 960 Alloy Drive, Thunder Bay, Ontario.

Field supervision was provided by R. Swire under the direction of J. Gingerich, Sr. Geophysicist.

Linecutting was contracted to Stares Contracting of Thunder Bay (807-623-2171, 622-4454).

Data research and compilation was completed by R. Felix, Sr. Project Geologist and W. Reid, Sr. Research Geologist. The diamond drilling was contracted to Midwest Drilling Ltd. of Winnipeg, Manitoba. The corelogging and sampling was carried out by W. Bellinger and C. MacDougall, employees of Noranda and by M. Leahey of Bayshore Geology Inc. of Thunder Bay under contract to Noranda.

Field supervision was provided by R. Felix and J. Sullivan, District Geologist.

7.0 INSTRUMENTATION

7.1 Magnetometer Survey

The survey was undertaken with the Scintrex MP-3 proton precession magnetometer. Measurements of the earth's total geomagnetic field (accuracy of .1 gammas) were taken at 50 foot stations. Diurnal corrections were made by integrating the magnetic variations recorded every 30 seconds by an MP-3 base station with raw field data.

7.2 Large Loop TEM 57 Survey

The PROTEM EM 57 is a time domain system which can operate in both fixed or moving loop mode. Fixed loops can be variable in size from up to 500 x 1000m. The moving loop uses an 8-turn 5x5m square.

The transmitter outputs a bipolar rectangular current with a 5096 duty cycle. Repetition rates are 3 Hz, 7.5 Hz and 30 Hz with a maximum output current of 20 amps at voltage taps of 20 or 40 volts.

The receiver the time rate of decay of the magnetic flux along 3 axes on 20 geometrically spaced time channels for each base frequency ranging from 6 ms to 80 ms. Base frequencies available are 3, 7.5, 30, 75 and 285 Hz with signal synchronization provided by either reference cable link or quartz crystal lock. Integration time varies with base frequency from 17.5 sec to 70 sec. The accuracy of the reading varies with ground conditions and signal stacking. Under most conditions, noise envelope of (1dBz7150ms)mV.

For surveying on the property, 2 large transmitter loops were used at the 30 Hz repetition rate. Surveying was done on 800 ft spaced lines with some in loop readings taken from Loop #1.

7.3 Borehole PEM Survey

The Borehole Pulse Electromagnetic equipment will evaluate the size, conductivity and approximate shape and position of the conductors near a borehole. The anomaly patterns from conductors intersected by the borehole are different from those caused by external conductors (Figure 3). The method is capable of detecting a massive sulphide body from a drill hole that cuts the weaker, fringe mineralization surrounding the body. The method is independent of directional changes in the borehole.

The PEM method utilizes a single turn transmitter loop, laid out on surface and a receiver probe that is sent down the borehole (Figure 4). For holes up to 500 meters in depth, the standard 480 watt, 24 volt output transmitter is used. The transmit loop is approximately 100 meters x 100 meters with more than one loop being used in order to obtain directional information. Alternating a single large collar loop encompassing multiple drill holes can be used. For deeper holes (down to 1200 meters) a 2300 watt, 115 volt output PEM transmitter is required, usually driving a transmit loop of approximately 500 meters x 500 meters. A standard PEM receiver is coupled with a reel and cable to the downhole probe.

Multiple loop configurations can be used to assist determination of the defined conductor with respect to the borehole. More recently the development of the XY probe allows 3-component measurements which provide much more diagnostic information as to conductor location. The use of 3-component probes eliminate the need for multiple loop surveys. Examples of type responses are shown in Figure 5.

BOREHOLE PULSE EM TYPE RESPONSE CURVES

HOLE INTERSECTING CONDUCTOR - HOLE OUTSIDE CONDUCTOR

Secondary Field

CRONE GEOPHYSICS LTD. BOREHOLE PULSE-EM SYSTEMS

3607 WOLFEDALE RD.M1SS1SSAUGA. ONT.CANADA, L5C 1V8

HECEIVCK Ri

METHOD

ReadingCOMpOMBt

Ik Loops

TRANSMITTERIk

24V to 115V

BOREHOLE

ISOLATED BOREHOLE

One hole is read from an array of transmit loops to acquire directional Information

Axial dB/dt

100m x 100m to 300m x 300m

Up to 200m from hole, dependent on size of conductor

MULTIPLE BOREHOLES

conductor

Multiple closely spaced holes are read from one large loop.

Axial dB/dt

300m x 300m to 1000m x 1000m


I

UNDERGROUND BOREHOLE

Underground holes are read horn large transmit loops on surface

Axial dB/dt

300m x 300m to 1000m x 1000m


Tx Power Supply tWtolUV

vouMZ nairnMVtollSV

8.0 DISCUSSION OF RESULTS

8.1 Magnetometer Survey

The survey defined an area of moderate magnetic relief ranging from 59100 nT to 60500 nT. Magnetic trends are northwest-southeast consistent with interpreted geologic strike.

Within the survey area, several discontinuous magnetic anomalies are mapped which appear to truncate or dislocate against a series of northeast structures. These northeast structures are evident on the regional airborne magnetics (Figure 3) and are thought to possibly define synvolcanic structure related to the conduits of hydrothermal solutions (black smokers) essential for massive sulphide mineralization. Thus, one would expect to find alteration pipes and 8M mineralization local to these structures.

The structural corridor bound by NE1 an NE2 appears to define the limits to the Santa Maria stringer zone mineralization. The broad magnetic anomaly M1 which lies at the alteration contact, bound by NE1 and NE2, corresponds with the weak locally massive sulphide mineralization intersected in shallow drilling near the Group 51 south boundary. Investigating the depth extent of this mineralization is considered an exploration priority.

The structural corridor bound by NE3 and NE4 lies in an area of limited exploration. Within this corridor is located the Claw Lake Cu, Zn, Ag showing reported in the government mapping of this area. There is no obvious magnetic target within the area of coverage, however the eastern limits of the structural zone is not fully resolved. Therefore it is essential that grid coverage be extended to the east.

Several of the defined stronger magnetic anomalies (> 1000 nT) appear to have extensive strike O 400m) and a narrow wavelength response indicating a near surface feature. These anomalies M2, M3 and M5 are interpreted to map mafic intrusives.

There is generally no conductivity associated with the intrusives. However, several small target conductive TEM responses (15-channel, 7-channel) were defined along the south flank of M3. An intermediate strength, small dimensional conductor is also located on the north flank of M4. This anomaly appears to map sulphide mineralization associated with a chert unit intersected in hole LLM6 and LLM7.

The chert unit may possibly define the eastern extent to the mineralization associated with M1.

Airborne Magnetics

Evaluation of both Norex and OGS airborne magnetic data indicated that there appears to be a strong correlation between BM mineralization and the intersections of the top of the alteration with northeast trending footwall (synvolcanic faults?) structures. Interpretation of the airborne magnetics (figure 3) identified several strong northeast structures in the Claw Lake area. One of the structural zones coincides with the Santa Maria stringer mineralization.

Re-examination of previous drilling indicated the possibility of mineralization in the area is steeply dipping. A core relogging and lithosampling program confirmed alteration and lithology is vertical to south dipping in the Santa Maria area. It appears that a major flat lying, south (5Qo) dipping thrust fault imparted a schistosing and structural alteration which was incorrectly thought to define the eastern extension to the Sturgeon Lake footwall stratigraphy. Thus, much of the deeper drilling in the area never reached the top of the alteration and stopped within the hanging wall stratigraphy.

6

Subsequent to this re-examination the Santa Maria property was optioned and additional claims staked in the Telephone Lake area.

8.2 Large Loop TEM 67 Survey

The Large Loop TEM survey was undertaken to investigate the possibility of deep seated conductors in the vicinity of Claw Lake.

The survey failed to define any significant conductors although several near surface small conductive zones were defined.

C1: Conductor C1 is a small dimensial, discontinuous conductor {IB-channel) located atapproximately 500S extending from 160 to 172E. The conductor appears to map the up dipextent to the massive sulphide mineralization intersected in holes 51-15 and 51-14.The conductor lies on the north flank of magnetic anomaly M1. The width of M1 (400') issignificantly larger than C1 indicating a greater extent to the disseminated sulphide andmagnetite alteration zones associated with the Santa Maria mineralization.The stringer mineralization of the Santa Maria Main Zone lies immediately below Ml.

C2: Anomaly C2 is a small dimensional, discontinuous conductor flanking magnetic anomalyM4. The conductor displays fair conductivity (10 channels) although the short wavelengthresponse indicates small conductive zones.Conductor C2 appears to map local increases in sulphide mineralization within the chert horizonintersected in hole 51-18.The geophysical signature is similar to anomaly M1-C1 and possibly maps the strike extent tothe Sturgeon Lake horizon.

The ground geophysical programs were undertaken in the immediate vicinity of the Santa Maria stringer mineralization. Surveying has mapped the strike extent of the Sturgeon Lake stratigraphy to the east shore of Claw Lake where other synvolcanic structures are inferred (NE3, NE4). There has been no DEEPSEARCH methods applied east of the survey area and continuation of coverage should be considered a top priority.

8.3 Borehole PEM Survey

The BHPEM surveying undertaken on the properties was plagued with instrumentation problems resulting in excess expenditures. The first program undertaken in March was abandoned after a short in the 1600m BEM cable was discovered. The second program undertaken in early June failed as a water leak into the directional probe shorted the unit. The third program undertaken in late June resulted in marginally useful data as the conductive bodies lay at the detection limits of the directional probe.

In total, hole 51-26 was surveyed three times, 51-27 three times, 51-28 twice, 51-25 once, 51-20 once and 92-1 once.

HOLE

51-20

51-25

51-26

51-27

51-28

92-1

LOOP NO.

#3

#1

#2, 3, 5

#1,4,5

#4,6

#7

COMPONENTS

1

1

3

3

3

3

DEPTH

243

1035

840

960

1208

1100

Surveying in holes 51-25 and 51-20 failed to define any anomalous responses.

Hole 51-26: BHPEM surveying defined a strong, long wavelength off-hole conductor located approximately 120m from the hole. Directional probing indicates the conductor is located west and down dip (below right) of a point 730m down hole.

Hole 51-27: BHPEM surveying defined a weak conductive zone located 60m east (left) of the hole at a point 880m down hole.

Hole 51-28: Several conductive zones are resolved at the bottom of the hole (1030m, 1130m) and one inferred beyond the hole's limit. Directional information is incomplete, but suggests the conductive zones lie within 30m of the hole likely down dip trend west.

Hole 92-1: There are several short wavelength conductive responses located near the top of the hole. Most are related to steel wedges. The only legitimate off-hole anomaly is located at 290m down hole. The conductor corresponds with a massive sulphide zone intersected at 1100' down hill in the first hole.The up-dip extension of this hole corresponds with a zone of magnetic, weak, sporadic conductivity zone defined by the TEM 57 survey.

9.0 1992 DRILL PROGRAM

During April - July, 1992 a stratigraphic drill hole was completed to test the 'top of Mattabi' sodic depleted felsic pyroclastics underlying the Simax Option property. The target horizon was the -600m elevation, 300m below any previous drilling.

The field work was undertaken from April 27-30 (drill mob and camp setup) and from May 21 - July 13, 1992 (drilling). One hole was completed encompassing 1744 meters.

The hole was drilled utilizing NO rods and equipment. Core was produced and logged in Imperial units. There was great difficulty in controlling the dip of the hole and two first attempts were each abandoned at 53.9m. Drilling continued to be extremely difficult with several wedges (10) being set and seven wedged holes abandoned as the hole failed to deviate as planned and rods broke in the hole.

Sampling was done on a maximum 3 foot interval over areas of sulphide mineralization. A total of 39 samples were submitted to TSL and Accurassay Labs Ltd. for Cu, Zn, Ag analyses by standard atomic absorption techniques. In addition, 35 core samples were collected approximately every 100

8

32NQV19 Aid:

MINING RECORDERPATRICIACLM i7o a

ill -CLMl 20!PO 225783 ;

Afgff IT iPlUKit i* 3 12527 Ps 31VJI4

CLM 202

7, 430680 (430431,430*82

1144050^|uo.i' B CLM

Pa l Pa l Pa I06J1 :4J06B9 4306SO 14J069I

1144049

1144048

227IS3 i 227)80 2059181 J059II

feet and submitted to TSL Labs for whole rock determinations.

Location of S-92-1 (S92-Z1) can be found on Maps 2 and 3. The drill log, cross section and geochemical analyses are appended to this report.

9.1 Discussion of Results

The drill hole was collared in the footwall felsic lapilli tuff stratigraphy. Weak to moderate chlorite-garnet alteration appears to be ubiquitous and occasional 'rhyolite breccia' zones were intersected. Of particular note is a 1.5m section of 'stringer type' sulphide mineralization intersected at 378m hosting up to tt chalcopyrite and 1 -2*K sphalerite. Best assays were 1.14** Cu and 1.23"* Zn over 2.05m. Good looking chloritic sericitic altered felsic fragmental* with patchy sulphide mineralization were intersected from 690m (S-90-W4) to 933m (S-90-W7). The felsic-mafic metavolcanic contact was finally reached in S-92-W7 which finished at 1011 meters (3317 feet). The contact was faulted and not mineralized. A downhole PEM survey revealed an off-hole anomaly at 290m downhole. This corresponds to a 1 -2m wide sulphide zone.

Whole rock determinations exhibit sodic alteration from 120m down hole to at least 820m down hole, approximately 75 meters south of the felsic-mafic metavolcanic contact.

A summary log of S-92-1 and the accompanying wedged holes is as follows:

Hole: S-92-01A

Dep: 16000E Lat: 1900S Dip: -77* Azi: 030* Start: May 22/92 Finish: May 24/92

O 80' (24.6m) Overburden80 177' (53.9) Lapilli Tuff

177 Hole abandoned - excessive deviation

Hole: S-92-01B

Dep: 16000E Lat: 1900S Dip: -77* Azi: 030' Start: May 24/92 Finish: May 25/92

O 80' (24.6m) Overburden80 177' (53.9) Lapilli Tuff

177 Hole abandoned - excessive deviation

9

Hole: S-92-01

Dep: 16000E Lat: 1900S Dip: -82* Azi: 030* Start: May 24/92 Finish: May 31/92

O 82

156158313

520528

687806

879889

8931507

82' 156'

158' 313' 520'

528' 687'

806' 879'

889' 893'

1507'

(25m) Overburden (47.6) Footwall Lapilli Tuff

- chlorite-garnet alteration (48.2) Massive "Dacite' Intrusive (95.4) Brecciated "RhyoWte/Rhyodacite" Felsic Volcanic (158.5) Footwall Lapilli Tuff

- chlorite-garnet alteration (161) Mafic Dyke (209.5) Intermediate Tuff - Lapilli Tuff

- weak chlorite-garnet(245.7) Massive to locally brecciated 'Dacite* Intrusive (268) Rhyolite Breccia

- mod - int. chl-garnet alteration, tr py(271) Rhyolite Agglomerate(272) Silicified Rhyolite Fragmental

- 2-5% diss. pyrite (459.5m) Felsic Tuff

Abandoned because of failure to deviate correctly

Hole: S-92-W1 (Wedged from 92-01 at 750')

Start: June 1/92 Finish: June 3/92

750814.5876.8886.3

814.5' (248.3m) Felsic Tuff - chlorite-garnet fracturing876.8' (267.3) Felsic Breccia/Fragmental - chlorite-garnet matrix886.3' (270.2) Felsic Agglomerate with quartz flooding/qtz veining

1077.0' (328.4) Blue Quartz Eye Felsic Tuff1077.0' Hole abandoned due to steepening

Hole: S-92-W2 (Wedged from 92-W1 at 900')


9001222

1222' (304.9m) Felsic TuffAbandoned because of steepening

10



7901137

1137 Felsic TuffAbandoned because of steepening



850 1057 Felsic Tuff 1057 1110 Lapilli Tuff Fragmental 1110 1188 Mafic Dyke Swarm 1188 1207 Felsic Lapilli Tuff 1207 1257 Mafic Dyke Swarm 1257 1480 Felsic Lapilli Tuff 1480 1494 Mafic Dykes 1494 2216 Felsic Tuff - Lapilli Tuff

- weak to moderate chl, biotite, garnet alteration,occasional quartz eye rhyolite

2116 2265 Diorite Dyke 2265 2313.25 Felsic Lapilli Tuff Altered

- with moderate sericite, moderate silicification, someblue quartz eye

2313.25 2336.2 Mafic Dyke 2336.2 2479.9 Felsic Tuff

- silicification with sericite, garnet, anthophyllite 2479.9 2487.5 Diorite Dyke Fault Zone 2487.5 2607.5 Felsic Tuff

- with sericite garnet, magnetite 2607.5 2617.1 Garnet Chlorite Zone 2617.1 2663 Quartz Eye Crystal Tuff

- with moderate sericite, magnetite 2663 2729 Lapilli Tuff

- with sericite garnet, chlorite2729 2788.9 Blue Quartz Eye Felsic Lapilli Tuff 2788.9 2809.25 Mafic Dyke Intermixed Volcanics 2809.25 2968 Agglomerate Lapilli Tuff

- chlorite with moderate sericite, garnet 2968 2998 Feldspar Crystal Tuff 2998 3067 Felsic Lapilli Tuff

- moderate to pervasive sericite, garnet, chl

Drill rods broke in hole - lost

11

Hole: S-92-W5 (wedged from 92-W4 at 2743')

Dep: 16000E Lat: 1900S Dip: -82* Azi: 030' Start: June 26/92 Finish: June 28/92

2743 2763 Felsic Tuff2763 End of Hole - Abandoned because of cored wedge.

Hole: S-92-W6 (wedged from 92-W4 at 2723.5')

Dep: 16000E Lat: 1900S Dip: -82e Azi: 030* Start: June 28/92 Finish: July 2/92

2723.5 2848 Felsic Tuff2848 End of Hole - Abandoned because of excess vibration and loose

wedge. Hole: S-92-W7 (wedged from 92-W4 at 2676')

Dep: 16000E Lat: 1900S Dip: -82* Azi: 030* Start: July 2/92 Finish: in progress

2676 2727 Felsic lapilli tuff with ser, gar, cbl, bio alterationdiss. po 4 mag

2727 2766 Blue quartz eye lapilli tuff with sil, chl, alteration 2766 2897 Felsic lapilli tuff - as above 2897.0 3060.2 Felsic Tuff - lapilli tuff breccia with garnet, chl, sil, ser

alteration3060.2 3065.8 Fault Zone Breccia - ser. graphitic 3065.8 3317.0 Int. Tuff - bio, chl, calcite unaltered

3317.0 End of Hole

Assays: none significant

12

10.0 CONCLUSIONS AND RECOMMENDATIONS

BHPEM surveying defined a strong off-hole conductor located approximately 120m west of hole 51-26 at a point 730 meters down hole. Within this region, there remains sufficient room to allow a yet untested 'Mattabi size' ore deposit. A drill hole is proposed to drill test the off-hole anomaly.

The 'top of the Mattabi' alteration was intersected 125m east and 220m below the original target in hole S-92-1 at about -1100 meters. The contact of the felsic with the mafic metavolcanics was faulted and not mineralized. A 1.5 meter section 'of stringer type' sulphide mineralization was intersected at 378m downhole with best assays of 1.14ft Cu and 1.23ft Zn over 2.05 meters. An off-hole PEM anomaly corresponds to this sulphide zone. Whole rock analyses confirmed the sodic depletion alteration in the felsic fragmentals intersected. The up-dip extension of this hole corresponds with a zone of magnetic, weak, sporadic conductivity defined by the TEM 57 survey. Further exploration along this horizon is highly recommended.

Finally, geologic mapping, geochemical surveying and EM surveys east of Claw Lake covering the eastern extension of the favourable geology located on Group 51 is recommended.

Respectfully submitted,

NORANDA EXPLORATION COMPANY, LIMITED (no personal liability)

John GingerichSr. Geophysicist -

FelixThunder Bay, Ontario Sr. Project Geologist July 21,1992 Northwest Ontario District

13

APPENDIX III

DRILL LOGS

Proj f 1392

Hole f 892-l

Length 1507

Casing 80

Core Size BO

Claim Nuaber

DIAMOND DRILL RECORD

Property Siiax Option

Azimuth 53

Inclination -82

Elevation O

Grid Reference 16000 B 1895 6

Grid Azimuth 23

Surveys Acid, Troparl

Instrument Used

Drilled by Midwest

Logged by w. Bellinger C.McDougal M.W.Leahey

Started May 23,1992 Finished June 2. 1992

Date Logged May 24 -June 3,1992 Core Storage Campsiteon Claw Lake

Remarks Hole dropped 5 degrees In 1507 feet

Attach Location Sketch Signature

892-116000,-1895 SIMAX OPTION O ELEVATIONxxxxxxxxx xxxxxxxxx xxxxxxxxx xxxxxxxxx xxxxxxxxx

82 (OVERBURDEN)

82 156 (Footwall Lapilli Tuff chl,garnet tr py.cpy)Mottled light gray to green felsic lapilli tuff composed of rounded to stretched ellipsoidal fragments of gray felsic to green chloritic clasts In a Moderately chloritic Matrix, a* 2-1Oam pink garnet porphyroblasts. Bedding 50*70 degree to ea. tr py,cpy

156 158 (DacitlC Ash Tuff)Light gray, fine grained dacltlc ash tuff with a l nor Uu chloritic spots

158 313.8 (Brecciated Rhyollte-Rhyodaclte)Light to aedluM gray, fine grained aasslve rhyolite breccia brecciation consists of 2-5 ea angular rhyolite clasts held together by weak green chlorite and eallte fracture fillings ("Brick work alteration"), Minor garnet porphyroblasts local

313.8 520.2 (Footwall Lapilli Tuff chl garnet tr po cpy)Medlui gray to Bedim green felsic lapilli tuff exhibitingweak to Moderate chloritic alteration, with Minor calcite,biotite and 1-10 MI pink garnets In the Matrix. LocallyInterbedded with thin qtz eye crystal tuff horizons andseveral diabase dykes. Lapilli fine grained Massive rhyolite1-5 ea Minor qtz velning with IK po local tr cpy bedding 30-60 degrees to ea345.5 354.4 (Mafic Dyke)376.2 378.2 (Mafic Dyke)464 475 (Mafic Dyke)

520.2 527.9 (Mafic Dyke)MedluM grained with Minor qtz calcite velning

527.9 687 (Intermediate Tuff Lapilli Tuff wchl garnets)MedluM gray , fine to Medlua grained Massive and bedded dacite tuff Interbedded with lapilli tuff horizons weak to perservasive chloritic alteration and si nor

development of garnet porphyroblast*, bedding 35-45 degree* to ea

667 806 (Dacite MftMlve to Local Bx)Hedlua to light gray, Cine grained aasslve to weakly brecciated dacite, weak chloritic alteration oocurrt as fracture fillings, ilnor garnet porphyroblast*, minor bedded to lapilli tuff horizons locally observed, bedding 30 degrees to ea

606 679 (Rhyolite Breccia-Agglomerate chl garnet)Mottled aedlui to dark gray, coarse,clast supported rhyolite fragmental composed of 2-6 ea fine grained aasslve subrounded felsic clasts, weak to local Intense chlorite with (5aa) pink garnet porphyroblast* In aatrlx. poorly developed bedding 35-40 degrees to ea

679 869 (Rhyolite Pyroclastic Breccia)Strongly brecciated variably sized (U-5 ea) light grey, fine grained aasslve to weak flow banded rhyolite clasts supported In a dark gray fine grained tuffaceous aatrlx crude bedding defined by clasts orientation 25 degrees to ea

669 907 (Rhyolite Flow Breccia? sil chl)Variably sized (to l Oca) angular to ellipsoidal, fine to aedlut grained massive rhyolite clasts In a moderately silicified to chlorltlzed V- biotite aatrlx. bedding 35 degrees to ea, tr - 5K py,po

907 959 (Qtz Eye Dacite chl biotite)Dark gray to green, fine grained massive volcanic with U-5* blue qtz eyes (aa*) in a weakly to strongly clhlorltlzed V- biotite altered matrix. Locally 1-2 ea clasts enchanced due to chlorite clotting. Qtz eyes decrease below 927 where unit Is more altered weak foliation 70 degrees to ea

959 1036.5 (Footwall Lapilli Tuff chl biotite)Medium gray to dark green lapilli tuff composed of a-3 ea subrounded ellipsoidal clasts of fine grained rhyolite -dacite In a moderately chlorltlzed biotite altered matrix. Local bedding a O* to ea, domlnately 35-45 degrees to ea

1038.5 1196 (Felsic Tuff wsll garnets chl bio)Dark to medium gray, variable chlorite and biotite greatest In middle of unit, weak silicification, rounded garnets .5-1 ma Foliation 30 degrees to ea 1158.75 1160 white quartz vein barren

lonal hairline calcite filled fracture*

1196 1240. 5 (Mottled cherty Felsic fragmental cnl local ser bio)Mottled green to yellow graf colour, matrix biotite chloritic, fragments tillfied and or sericitic, local small garnets, upper contact 40 degree* to ea, lower contact 70 degrees to ea1215.75 1216.5 Semi -massive lense or matrix filling 2* cpy 5* ZnS 11 to foliation 30 degrees to ea 1226. 5 1229 white barren quartz vein 40 degrees to ea 1237.5 1238.25 white quartz vein few blebs of po,cpy 30 degrees to ea

1240.5 1246.5 (Mineralized Section-Seal Massive Po.Cpy ZnS)Exhalite horizon sulphides sub 11 foliation 30 degrees to ea

po,py 2* cpy K Zns

1246.5 1383.25 (Felsic Tuff garnets fracture alteration rare OB)dark to medlun gray colour, euhedral to rounded garnetsthroughout, local more chlorite foliation 30 degrees to eaweak bleaching along fractures 40 degrees to earare quartz eye1355.75 1356.5 white quartz vein

1383.25 1393 (Felsic Tuff Chl Sheared Mafic Dyke)dark gray to green lower contact 90 degrees to ea

1393 1507 (Felsic Tuff Lapilli Tuff wsll garnetlight to medium gray chlorite rims around lapilli lotted appearance, foliation 25-30 degrees to ea 1437 local tr py, cpy 1507 W) OF HOLE


ProJ f 1392 Property siiax Option

Hole f S92-V1

Length 750 -1077

Casing

Core Size BO

Clali NiMber p fi

Azliuth 059

Inclination -78

Elevation -737.41

Grid Reference 16060.21 B 1772.66 S

Grid Azlsuth 029

Surveys Acid, troparl

Instrument Used

Drilled by Midwest Started June 3,1992

Logged by M W LEAHBY Date Logged June 4-5,1992

Finished June 4,1992

Core Storage caipelte on Claw Lake

Renarks Wedge at 750 feet, hole lifts for 142' then steepens


944.25 977 Mafic Dyke Swangreen to light brown In colour944.25 951 Green Mafic Dyke fine to edit* grained951 958 Mafic Dyke brown ft green coarse grained,

calcite In Matrix 958 966 Mafic Dyke fine to aedlui grained, lower contact

foliated 45 degrees to ea for last 1.5* 966 977 Volcanics intermixed with Mf le dykelets

977 1077 Lapilli Tuff Fragmentalbrown to green In colour, stretch laplIll/fragments ion -lev, local foliation near dykes

1077 END OF HOLE


ProJ f 1392

Hole f S92-WW1

Length 900 - 1222

Casing

Core Size BO

Clala Nuftber

Property Sliax Option

Azltuth 59

Inclination -73

Elevation -1736.85

Grid Reference 16080.17 B 1736.85 8

Grid Azlauth 29

Surveys Acld,Tropari

Instruient used

Drilled by Midwest Started June 4, 1992 Finished June 7,1992

Logged by H w Leahey Date Logged June 5-8,1992 Core Storage Catpslte onClaw Lake

Renarks wedge at 900 only one subsequently bypassed, arc universal bullnosed 924 - 928.5 ft 1062 -1066 feet hole lifted 3 degrees In 112 feet then steepened


S92-W1 SIMAX OPTION 16080.1? B 1736.85 8 •1736.85 l WEDGE 900

902 943 (Blue Quartz Bye Tuff user chl gar bio)light gray, weak sericite, chlorite garnet 11 to foliation,foliation 25 degrees to ea, blue quartz eyes l-2am .biotitealteration of lapilli908.6 909.5 Lamprophyre Dyke tr py on each contact914 943 tore strongly foliated924 928.5 arc universal bullnosed no core940.6 941.1 Mafic Dyke

943 993.75 (Dyke Swan)943 951 Mafic Dyke green fine to medium to grained

Irregular calcite velnlets throughout 951 966 Mafic Dyke brown and white coarse grained,

calcite In matrix, local calcite veins 966 985.25 Mafic Dyke green coarse to fine grained,

Includes BOM biotite rich volcanics 40 dagroosto ea

985.25 993.75 Contact Zone Intermixed Mafic Dyke ft Biotiterich Volcanics 5 degrees to ea

993.75 1172 (Lapilli Tuff fragmental bio)brown green lapilli tuff fragmental, dirty looking biotite matrix, abundant chlorite mafic dykes, fragments vary from .5mm 2.5cm, fragments matrix supported 1034.75 1040.25 Mafic Dyke brown 8. green, fine to medium grained

lower contact 25 degrees to ea 1058 1062 Mafic Dyke green medium grained, 3" inclusion of

tuff, calcite and quartz velnlng, contact 20degrees to ea

1062 1066 arc universal bullnosed no core 1152.1 1155.5 Mafic Dyke green .5" quartz vein minor py.cpy on

lower contact1158.8 1160 minor py In chlorite patch 1166 l" massive py,cpy,Zns stringer vein 20 degreesto ea *"

1172 1222 (Felsic Lapilli Tuff wMblo gar ser)light gray mottled salt ft pepper, weak to moderate biotitealtered lapilli elongated fragments, small garnets throughoutsection 1mm size, Inlal fracture controlled sericite alterationbeyond 1212 patches of sericite alteration1175 1175.6 Mafic Dyke coarse grained1189.8 1202.25 Mafic Dyke medium grained biotite rich

upper contact 25 degrees to ea, foliation 30 degrees to ea

1222 END OF HOLE


Proj t 1392

Hole f S92-X1

Length 790 - 1137

Casing

Core Size BQ

Claim Umber

Property Sliax Option

Azimuth 59

Inclination -74

Elevation -776.63

Grid Reference 16065,09 B 1764.05 S

Grid Azliuth 29

Surveys Add, Troparl

Instrument Used

Drilled by Midwest Started June 7, 1992 Finished June 9,1992

Logged by H V Leahey Date Logged June 8-10,1992 Core Storage Campsite onClaw Lake

Remarks wedge at 790 feet .hole lifted 6 degrees In 87 feet then steepened



Pro j f 1392

Hole f S92-XX1

Property Sliax option

Aziiuth 60

Grid Reference 16074.63 B1747.19 8

Grid Azltuth 30

Length 850 - 3067 Inclination -68 Surveys Acid Troparl

Casing Elevation -832.89 Instruient Used

Core size BQ

Clala Number p /)-

Drilled by Midwest Started June 10,1992 Finished June 26,1992

Logged by M W Leahey Date Logged June 11-26 Core Storage Caipsite onClaw Lake

Remarks 4 wedges In hole 850,902,957,1057 total 6 In stringcore barrel stuck at 3069 300 rods broken off unable to retrelve new wedge at 2752 to bypass steel, contlnatlon naaed S92-Y1


S92-XX1 16074.64B•1747.198-832.896VBDG8S 4SPBC XXI

853 677.4 (Felsic Bx Fragmental wser qtz velnlng gar cbl)light gray In situ brecciation, chlorite ft garnet throughout weak to Moderate sericite alteration of Matrix, fragments or pseudo-fragments l-S ci variable shaped B7i 872 quartz vein white cbl patches no sllphldes

877.4 898.25 (Felsic Agglomerate wser sil chl frag local gar)light gray to light green In colour .fragments 1-8 ea chlorltlzed and rimmed with biotite, bleached weak sericite,silicified, local euhedral pink garnets 877.4 881.2 green marker foliation 30 degrees to ea, clast ft

matrix support brown biotite In mtx 877.7 898.25 py to 3* In patches along foliation

898.25 964.1 (Blue Quartz Bye Lapilli Tuff wMser gar)light gray salt ft pepper texture, small blue quartz eye .5- 1mm Inltal fracture controlled weak sericite alteration, garnets 5mm appear reabsorbed or corroded, foliation 28 degrees to ea 905.2 905.75 coarse green ft brown mafic dyke 917.4 919 med to coarse grained mafic dyke 50 degrees to

ea 924 964.1 weak to moderate sericite, large 2-3 cm chlorite

patches902 904 bullnosed by wedge no core 957 958.4 bullnosed by wedge no core

964.1 996 (Lapilli Tuff Fragmental bio chlgray brown in colour, Intermediate in composition or altered fragments ,5mm -2 cm, dirty bio matrix, foliation 35 degrees to ea

996 997 (Fault Zone Breccia)strongly sheared 15 degrees to ea, fragments elongated

997 1007 (Green Mafic Dyke)

( '

1007 1109.8 (Lapilli Tuff fragmental bio chl .5" cpy vein)gray brown in colour, Intermediate In composition or alteredfragmenta .5mm -2 cm, dirty bio chl matrix, foliation 35 degree*to ea1038.6 1040.5 Green Mafic Dyke1064.25 .5M cpy vein1065.25 1066.25 Mafic dyke carb veins

1109.8 1187.5 (Mafic Dyke Swan Intermixed Lapilli Tuff Fragmental)1109.8 1119.75 medium grained Mafic Dyke carbonate veins1119.75 1126.6 Lapilli Tuff Fragmental1126.6 1137.5 coarse grained Green Mafic Dyke1137.5 1155.6 Lapilli Tuff Fragmental1155.6 1187.5 fine to medium grained Mafic Dyke

1187.50 1207.25 (Felsic Tuff Lapilli Tuff wser bio lapilli)light to dark gray wser alteration along fractures, biotite alteration of lapilli 1200.75 1201.25 Lamprophyre Dyke

1207.25 1257 (Mafic Dyke Swarm)dark gray and brown fine to medium grained mafic dykes, pink garnets near lower contact

1257 1297.5 (Felsic Fragmental Silicified chl bleached fragments)gray unit with green fragments, l-8mm chl bleached fragments biotite local qtz veins

1297.5 1374 (Blue Qtz Bye Felsic Lapilli Tuff wser gar bio)light gray colour, weak sericite, 2-3mm grnets throughout, blotltlzed lapilli, poor foliation 40 degrees to ea 1357 1358 Lamprophyre Dyke 1361.2 1361.6 Lamprophyre Dyke

1374 1404 (Felsic Tuff large gar)dark gray, large 2-3 cm garnets, faint follatoln

1404 1479.9 (Felsic Lapilli Tuff wser bio large gar)light to dark gray, weak sericite, biotite throughout foliation 30 degrees to cm1448 1448.75 Mafic Dyke bio1449 1452.1 Mafic Dyke bio

1463.3 1465.8 Mafic Dyke coarse grained

1479.9 1494 (Mafic Dyke)coarse grained, green

1494 1505.75 (Felsic Volcanics Altered sil Mser wchl kspar Fedol gar) gray, yellow-gray, tan alteration f rot fractures to local pervasive areas Moderately sericitic silicified, weak cbl, large garnets 2-3MM, kspar near dyke, earthy Fedol? In section foliation 20 degrees to ea

1505.75 1514 (Dloite Dyke kepar alt dlssea py)light greenish gray, top and bottom k-feldspar alteration along fractures, l* dlssea py In dyke

1514 1527.8 (Felsic Volcanics Altered sil Mser wchl kspar Fedol gar) gray, yellow-gray, tan alteration froM fractures to local pervasive areas Moderately sericitic silicified, weak chl large garnets 2-3ra, kspar near dyke, earthy Fedol? In section foliation 20 degrees to ea

1527.8 1535 (Mafic Dyke)coarse grained, calcite veins

1535 1569.25(Felslc Volcanics Altered sil Mser wchl Kspar Fedol gar) gray, yellow-gray, tan alteration fro* fractures to local pervasive areas Moderately sericitic silicified, weak chl large garnets 2-3M, kspar near dyke, earthy Fedol? In section follaton 20 degrees to ea

1569.25 1621.4 (Felsic Lapilli Tuff gar chl wser)light gray weak sericite local, abdunant corroded garnets .5*B-1.5oi, foliation 35 degrees to ea1577.25 1584 Diorite Dyke salt ft pepper texture l* dlssea py

cubic xtals .5m

1621.4 1685.1 (Diorite Dyke)light coloured, Massive fine grained salt ft pepper texture dlsseM cubic .5MM py K, near lower contact garnets and xenollths of volcanics

1164 1671 Felsic Lapilli Tuff ainor py nail garnet* 1683.9 1685 Mafic Dyke

1685.1 1722.4 (Felsic Tuff Lapilli Tuff l* py cbl bio gar) light gray to dark gray , garnets corroded 1- chlorite biotite throughout py in patches locally to K foliation 45 degrees to ea 1717.4 1718.25 Mafic Dyke, Dykelets

1722.4 1749.5 (Mafic Dyke)fine to coarse grained. Inclusion of Felsic Tuff a Lapilli Tuff 1733.75 1745 local py

1749.5 1885.9 (Felsic Lapilli Tuff Agglomerate veer bio chl alnor py)light to dark gray lapilli 2-8 ea, weak sericite, garnets .5-lma biotite chlorite throughout, foliation 40 degrees to ea 1769.2 1775.4 Mafic Dyke coarse grained soae py.cpy

In fractures1779 1779.45 Mafic Dyke Coarse grained 1783 1783.4 Laaprophyre Dyke

1885.9 1978.75 (Diorite Dyke IK dissen py)light to dark gray diorite dyke, fine dlssea py

1978.75 1999.5 (Blue Quartz Bye Lapilli Tuff Agglcwerate gar bio chl ilnor py) aedlua to dark gray, ,5-laa small subrounded blue quartz eye, fragments chlorltlzed and rlaaed with biotite, garnets 1-1. SM foliation 35 degrees to ea

1999.5 2036.5 (Diorite Dyke 1.5-2* py dlssea)light to dark gray green colour ,1.5-2* dlssea py 2033.1-2036.5 Mafic Dyke fine grained green

2036.5 2116 (Intermixed Felsic Vole i Mafic Dykes) ^2036.5 2044.6 Blue Quartz Bye Lapilli Tuff Agglomerate bio

l* py, lau quartz eyes foliation 40 to ea 2044.6 2049.8 Green Mafic calcite veins 2049.8 2056.75 Lapilli Tuff l* py foliation 40 degrees to ea

local qtz veins sub 11 to ea2056.75 2058.1 Brown Mafic Dyke calcite veins 11 foliation 2058.1 2061.5 Tuff Lapilli Tuff bloltlzed fragaents 1-2* py 2061.5 2068 Green Mafic Dyke 2* py on lower contact

2068 2070.8 Tuff Lapilli Tuff2070.8 2078.9 Mafic Djrke quartz patches2078.9 2081.5 Lapilli Tuff 2* PT2081.5 2085.5 Mafic Dyke2085.5 2095 Altered Tuff Lapilli Tuff sil ter2095 2100.7 Green Mafic Dyke2100.7 2106.75 Altered Tuff Lapilli Tuff ell bleached fractures

foliation 40 degrees to ea 2106.75 2110.25 Green Mafic Dyke 2110.25 2116 Lapilli Tuff Agglomerate altered fragments

foliation 40 degrees to ea

2116 2265 (Diorite Dyke 1-1.5 dlssea py)fine to medlm grained, biotite abdunant.low angle quartz and calcite velnlets 15 degrees to ea, 1-1.5* dissem py 2125 2" quartz vein2220.25 2222 shear zone foliated 25 degrees to ea contains

31" laminated quartz veins

2265 2313.25 (Felsic Lapilli Tuff Altered wMser Msll some BOB)light gray, dark gray, yellow gray colour, fracture alterationand pervasive patches, weak to moderate sericite, Moderatelysilicified,win foliation 30 degrees varies from 0-40 degreesto ea2274 2276 pervasive sericite, calcite veins2279.65 2287.25 Mafic Dyke medium to coarse grained2284 2285 2 py velnlets rimmed with chlorite 10 degrees

to ea 2290. l 2292 Green Mafic Dyke

2313.25 2336.2 (Mafic Dyke bio 21 py In Vole Zenollths)biotite rich .foliated 23-40 degrees to ea Intermixed vole 2328 2330.5 Felsic Lapilli Tuff 2K py 2332.75 2333.5 Felsic Lapilli Tuff 2ft py

2336.2 2479.9 (Felsic Tuff sil wser on fractures gar antho py In dyke*)light to dark gray, thin bedded 2-5mm ,chlorltlzed lapilli withpyrite to 2K, corroded garnets 3* distribution .5mm to 2cm Insize, local anthophyIllite with garnets, slickenside on somefractures2396 2407 large 2 cm garnet ft anthophyllite2415 2417 large 2 em garnet ft anthophyllite2352.6 2352.9 Mafic Dyke 1.5-2* py2371 2372.5 Mafic Dyke2421 2429.75 Mafic Dyke fine grained calcite veins 30 degrees

to ea 2437.5 2441.5 Mafic Dyke local 2* py, cpy on fracture

2479.9 2487.5 (Diorite Dyke Fault Zone blocky)light green graf, qtz pebble* lower contact 28 degrees to ea

2487.5 2607.5 (Felsic Tuff veer gar dieses tag)light gray to green user dlsseM Magnetite euhedral .5u-lMM in size local to 54, corroded garnets ,5-lme, sandy texture,weak bleaching, Fe stain, below 2567 Increased fracture alteration sericite 5* garnets2550.25 2552 Mafic Dyke coarse grained 30 degrees to ea 2559.5 2562.5 Mafic Dyke Medlun to coarse grained 2* py

2607.5 2617.1 (Garnet Chlorite Zone) corroded 50* of rock I-

2617.1 2663 (Quartz Bye Crystal Tuff wMser dlese* iag)light gray, yellow gray dlsse* euhedral Magnetite, subroundedgray quartz eyes, foliation 30 degrees to ea2620.6 2623.5 Mafic Dyke DlsseM py to 2*. py veinlet on

fracture2628.65 2628.9 Mafic Dyke coarse grained 2629.4 2629.9 Mafic Dyke coarse grained

2663 2729 (Lapilli Tuff wser gar dlssea Mag chl)light gray to dark gray, weak sericite, chlorite, dlssea agnetlte 24 In is* euhedral crystals, foliation 35 degrees toea, local pervasive sericite In Matrix, local Minor py2664.5 2665.5 garnet chlorite zone2686.5 2687 serpentine amphibole alteration2709.9 2711.2 BQB unit2720.35 2720.75 serpentine amphibole alteration

2729 2788.9 (Blue Quartz Bye Felsic Lapilli Tuff sil wMser 54py 3{aag)light gray yellow gray bleached, top 20*silicified, blue quartzeyes euhedral to subhedral l-2tt 5* distribution, dlsseM agnetlte 34 foliation 35-45 degrees to ea2730.75 2734.33 104 py alnor po In Matrix of Lapilli Tuff2734.33 2762 54 py dlsses and streaked along foliation2729 2729.95 Mafic Dyke green finegrained2740.6 2741.2 Mafic Dyke 14 py2742.35 2743.85 Mafic Dyke2755.75 2756.65 Mafic Dyke i/4" py on fracture2760.3 2760.9 Mafic Dyke aaphibole xtal on edge2761.5 2761.75 Mafic Dyke

2762.25 2769 Mafic Dyke2782 2788 garnet* reappear to 2ca, magnetite stringer* and

rims around fragment*

2788.9 2809.25 (Mafic Dyke Intermixed Vole)green colour .fine to ledlui grained, dlssea py UX, local biotite on contact, calcite veins 2793.35 2794.5 Lapilli Tuff 2799.65 2800.8 Lapilli Tuff 2802.75 2807.25 Lapilli Tuff

2809.25 2968 (Agglomerate Lapilli Tuff cbl wMser gar)light to dark gray, felsic to intermediate compositionchlorite, weak to Moderate sericite alteration, 1mm garnet*foliation 40 degrees to ea2825 2830 Mafic Dyke calcite veins2833 2834.5 Mafic Dyke2834.5 2836.4 py 3* In VOlC2836.4 2844.5 Mafic Dyke fine to coarse grained qtz vein2869.7 2880.35 Mafic Dyke2892 2900 py 3* In VOlC

2968 2997.75 (Feldspar Xtal Tuff cal chl ve inlet*)•edlui to dark gray, 1-2** Irregular feldspar crystals, calcite chlorite velnlets throughout 2996.1 2997.25 Mafic Dyke green2997.25 2997.75 Contact With 2 2M quartz veins

2997.75 3067 (Felsic Tuff Lapilli Tuff Breccia gar local MPser chl) light to dark gray, local moderate to pervasive sericite alteration, chlorite In fractures, In situ brecciation, 6- 10H corroded garnets foliation 40 degrees? to ea 3015.1 3016.25 Mafic Dyke bio chl 3016.25 3028.5 Persavlve sereclte alteration 3020.4 3024.9 Mafic Dyke

3067 END OP HOLE

Core Size BQ


Pro) f 1392

Hole f S92-Y1

Property Sitax Option

Azimuth 47


Grid Azlauth 17

Length 2743 - 2767 inclination -59 Surveys Acid, Troparl

Casting Elevation -2552.40 Instrument (teed

Claim NiMber f A 8

Drllled by Midwest Started June 27, 1992 Finished June 28, 1992

Logged by M v Leahey Date Logged June 28, 1992 Core Storage Caapslte onClaw Lake

Reaarks wedge at 2757 to bypass 300 feet of rods and stuck corebarrel In hole wedge slipped cored 3.5' of steel


Option16409.53 B977.08 8•2552.40

xxxxxxxxxxxxxxxxxxxxxxxxxxxxxxvwwwwv

2743 2763 (Blue Quartz Bye Lapilli Tuff wMeer chl 2X py tr po) light gray to dark gray In colour, 2* py tr po, quartz eyes 1-1.5 tat, weak to Moderate sericite, local silification, foliation 40 -45 degrees to ea 2743 2745.5 Step bit CUt2749.25 2750.5 Mafic Dyke coarse grained bio on contacts 2751.3 2752.65 Mafic Dyke green coarse centre fine contacts 2755 2757.2 Mafic Dyke green fine to coarse grained 2760.4 2760.S Mafic Dyke green 2761.25 2761.5 Mafic Dyke

2763 2767 (Mafic Dyke a Sil Lapilli Tuff)

2762 2765 step bit cut, wedge slipped 3.5' of steel wedgecored

2767 END OF HOLE

DIAHOND DBJLL RBOORD

Pro j t 1392

Hole f 692-YYi

Property Slaax Option

Aziauth 46


Grid Aziiuth 16

Length 2723.25 - 2848 Inclination -59 Survey* Acid, iroparl

Casing Elevation -2526.69 Instrurent Used

Core Size BQ

Clal. Nuiber p fa

Drllled by Midwest started June 28, 1992 Finished July 1,1992

Logged by H W Leahey Date Logged July 5,1992 Core Storage Caapelte onClaw Lake

Reaarks wedge at 2728 to bypass 300' of rods, core barrel andYl wedge. At 2848 binding and vibration caused abdondbent of wedge

Attach Location sketch Signature

SIMAX OPTION 16405.71 B1009.97 8-2526.69

2723.25 2729.25 (Lapilli Tuff wser gar chl dlsses sag)light gray to dark gray, weak sericite, chlorite, dlsees sagnetite, local concentration of garnets l-2s* foliation 45 degrees to ea 2728.75 2729.25 Hafio Dyke green sedlui grained

2729.25 2778 (Blue Quartz Bye FBlslc Lapilli Tuff MPser 5*py dtaag) light gray, yellow gray, bleached silicified throughout unit, blue quartz eyes euhedral to subhedral l-2s* 3* distribution, diseea and stringer sagnetite 3*, oderate to pervasive sericite alteration, foliation 40 - 45 degrees to ea2729.8 2733.75 10* py ilnor po in latrlx of Lapilli Tuff 2733.75 2778 5* py trace epr 2739.5 2743.25 Mafic Dyke 2747.25 2749.1 Mafic Dyke bio on lower contact 2750.5 2751.6 Mafic Dyke coarse grained 2753.65 2756 Mafic Dyke coarse center fine on contacts 2757.95 2758.95 Mafic Dyke 2759.75 2760.25 Mafic Dyke 2761.65 2763.35 Mafic dyke foliated, quartz vein

2762 2762.65 with amphibole cpy crystals

2778 2803.9 (Felsic Lapilli Tuff wsll wser bio gar aag stringers)light to dark gray, local 1.5 -2 M silicified bleaching around fragments, weak sericite. Irregular sagnetlte stringers and dieses sagnetlte 3*. biotite throughout section, py 1-3* 2782.2 2783.65 Mafic Dyke coarse grained it py 2785.1 2787.5 Mafic Dyke coarse grained If py bio on

contacts 2788.65 2795.6 Mafic Dyke aedlui to coarse grained 1.5-2* py,

i/4 M py.po on fracture 2803 2803.9 Mafic Dyke coarse grained biotite

a803.9 2848 (Felsic AggLoterate bio wMser sil)light to dark gray, gray green, weak to oderate fracturecontrolled sericite, soae calcite velnlets, biotite rl**ed andbleached fragments 2-4 os2816.15 2818.25 Mafic Dyke thin calcite veins2826 2827 Mafic Dyke coarse grained2831 2836 Maf lo Dyke coarse grained2842 2847 Mafic Dyke Vole Xenolith!2848 END OF HOLE


Pro j f 1392

Hole f S92-Z1

Property Slaax Optiono

Azltuth 47


Grid Azliuth 17

Length 2687.6 - 3317 Inclination -62 Survey! ACID, TROPABI

Casing Elevation -2481.67 Instruient Used

Core Size BQ

PA 3/^-5*21 6

Drilled by Midwest Started July 2,1992 Finished July 13,1992

Logged by H W Leahey Date Logged July 5-13 Core Storage Caapslte onClaw Lake

Reaarks wedge at 2676 ceaented In place


SXMAX OPTION 16398.39 B 1034.96 8

-2481.67 WEDGE 2676 892-21

2687.6 2695.8 (Felsic Tuff Lapilli Tuff vser gar dlssem mag stringers) light gray, gray brown, salt a pepper testure, elongated lapilli, corroded garnets, po fragments local, dlssem and stringer magnetite, strong foliation 45-50 degrees to ea

2695.8 2726.25 (Felsic Lapilli Tuff cbl bio gar dlssem mag 3*)light gray, green gray, black biotite Inmatrlx and rilling fragments, chlorite large garnets concentration 1-2**, foliation 40 degrees to ea

2726.25 2766 (Blue Quartz Bye Felsic Lapilli Tuff 4*py tr cpy sil chl wNser) weak sericite except moderate to pervasive sericite at top light to medium gray, bleached patches and slllfled, blue quartz eyes 1-1.5 mm subhedral to euhedral 5* distribution 2728.8 2725.5 sulfldes 10* 11 to ea, quart vein

2726.8 2727.5 patches py, po2728.8 2731.5 Mafic Pyke coarse center fine contacts 2739.1 2741.5 Mafic Dyke green coarse centre fine contacts

biotite on lower contact 2744.6 2748.6 Mafic Dyke green xenolith of slllfled

volcanic 2746.2 2746.6 at 2747.75 po Zns patch 2749.65 2750 Mafic Dyke2750.5 2751.6 Mafic Dyke 1/4- quartz vein biotite on contacts 2755.5 2758.4 Mafic Dyke green coarse center fine contacts,

biotite on bottom contact 2264 2266 SK py trace cpy follatlo 25-40 degrees to ea

2766 2818 (Felsic Lapilli Tuff gar bio wser chl dlsse* py) light gray medium gray, large garnets .2mm-lorn, fragments 2-6cm unsorted, fragmented elongated with depth foliation 50 degrees to ea2777.75 2780.2 Mafic Dyke green coarse center fine contacts 2781.2 2782.75 Mafic Dyke green coarse foliated 53 degrees to

ea calcite velnlets 2788 2789.25 Mafic Dyke green coarse grained 2" quartz vein

at base 2794.45 2795.6 Mafic Dyke green coarse center fine contacts,

biotite on contacts, narrow calcite veins 2805 2806.4 Mafic Dyke green 2808.35 2808.50 Mafic Dyke Irregular contacts 2809.45 2810.1 Mafic Dyke coarse grained Irregular bottom

contact 2810.55 2810.65 Mafic dykelet

2818 2856.1 (Mafic Dyke Swam Intermixed Lapilli Tuff)green, coarse grained, calcite veins red brown biotiteon contacts2818.65 2818.8 Vole Inclusion2821.25 2821.6 Volo Inclusion2622.5 2826.9 Vole Inclusion Lapilli Tuff2826.9 2827.65 Foliation 50 degrees to ea2841.75 2843.75 Lapilli Tuff Agglomerate contact2849.55 2856.1 Haflc Dyke green coarse grained 2* py2851 2852 Quartz Vein ft Vole Xenolith

2856.1 2907 (Agglomerate Lapilli Tuff gar cbl bio local sil user) edlui graf green, weak sericite soae tuff bands, small garnets .5*1**, black biotite riming fragments chl patches, chlorltlzed fragments foliation 40 to 70 degrees to ea 2861.45 2861.75 Mafic Dyke biotite 2874.25 2874.75 Quartz Vein barren white 2675.8 2880.65 Mafic Dyke Feldspar Porphyry? 2880.65 2872 Fault Zone right lateral calcite Infilling

2907 3060.20 (Felsic Tuff Lapilli Tuff Breccia sil gar chl MPser)light yellow gray to medium gray, corroded garnets In matrixwith chlorite, alteration bleaching sericite after biotite,sigmoidal foliation 50 degree* to ea2926.25 2937.1 Feldspar Xtal Tuff chl along fractures2945.5 2947.8 Mafic Dyke coarse biotite foliation 55 degrees

to ea2953 2957 garnet chlorite matrix 25S garnets 2960 2962 garnet chlorite 45* garnets 2962 2967 fracture controlled sericite alteration 2967 2975.75 garnet chlorite matrix 45* garnets l-2om

corroded2978.2 2981.75 Mafic Dyke brown green 2981.75 3016.45 Moderate to Pervasive sericite alteration In

situ breccia remlnant orglnal gray , few garnets 3016.45 3031 garnets H .5mm-lcm biotite

3065.20 3065.75 (Fault Zone Breccia sericite serpentine graphite)l-2oi fragments matrix sllckenslded sericite, serpentine, and graphite. Fault marks the end of altered felsic volcanics and start of hanglngwall Intermediate volcanics. Foliation varies from 35-50 degrees to ea

3065.75 3317 (Intermediate Tuffs bio chlorite calcite qtz veins velnlets)brown green unit, abdundant calcite quam veins,velnlets,blebs rimmed with chlorite,Irregular biotite bands .5-1.5mm along foliation, fine biotite In matrix causes brown colour, strong foliation 50 degrees to ea 3065.75 3071.9 Mafic Dyke green aedlum grained

3090.8 3091.1 Quartz carbonate vein barren3100.9 3101.2 Quartz vein r lined with calcite and chlorite3107.9 3109.5 Mafic Dyke green coarse grained3114 3116 po pr if folded schistosity calcite veins3119 3121 Mafic Dyke coarse grained calcite velnlets if po3143.4 3144.75 Mafic Dyke coarse grained 2f po3144.75 3146 few pink garnets laa3182.1 3182.4 Mafic Dyke coarse grained tr po3183 3183.1 Mafic Dyke carse grained3191.5 3192 Mafic Dyke coarse center fine contacts3192 3237 Lighter brown colour Increased fine biotite3258.75 3259.1 Crack seal quartz vein a quartz calcite vein3263.2 3264.25 Crack seal quartz calcite chlorite vein3277.4 3285.8 Mafic Dyke coarse grained biotite

3277.4 3281 foliation 50 degrees to ea3281 3283 quartz vein barren

3301.5 3301.75 py on fracure dlssea py In coarse grainedaaflc (pillow?)

3314.2 3314.45 fine po py 10* In gray tuff 3314.75 3314.9 fine po py 10* in gray tuff

3317 END OF HOLE

1983/5/30" 80RSURV **

SUUVEY DATA AND CALCULATED CO-OBDISATBS (feet)

PROPERTY'. STURGEON LAKE GR HOLE NO: 92-1 GRID: 51

Page l

DEPTH0.00

200.00300.00400,00600.00800.00900.00

1000.001200.001300.001400.001500.001600.001700.002100.002200.002400.002500.002600.002700.002800.00

BtCUMmOR-77.00-77.00-76.00-74.00-70.00-68.00-67.00-66.00-65.00-62.00-61.00-58.00-57.00-56.00-52.00-51.00-49.00-48.00-45.00-43.00-40.00

BEARING 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00

DATE:SURVEY IMSTRl*

BASTU1GS16000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000.0016000,00

C?*G

BY: ffiNT?

I*BBS;*.*?*aaai

NOKTHIHGS-1900.00-1855.01-1831.67-1805.78-1743.98-1672.31-1634.04-1594.16-1511.22-1466.60-1418.89-1368.13-1314.41-1259.21-1024.10-961.85-833.29-767.03-698.19-626.26 551.36

ELEVATION 0.00

-W2.tr

.72

.72

-578,91-769,63-858.02-949.

'1131,-1221.21-1309.09-1395.26-1479.59-1562.-1886.-1964.85-2118.06-2192.V6.-2265,49-2334.96-2401.22

.98

.59

1983/5/30** BORSURV **

SURVBT DATA AND CAljCUUTKJ) 00-ORDtRATBS (feet)

Page l

PROPBRTY: S1MAX OPTION HOLE MO: ^92- 1GELD: GRID ei

DATE: MAY 31,1992SURVBT BY: M. W. L. INSTRUMENT: TROPARI

COMMENTS:AZIMUTH GRID 26 DEGRESS 4 DEGREES BAST DBCLINATION

DEPTH0.00

164.00328.00656.00

.1148.001257.001350.001452.001507.00

INCLINATION-82.00-80.00-80.00-78.00-77.00-77.00-78.00-77.00-77.00

BEARING23.0023.0026.0029.0029.0029.00!29.0029.0029.00

BASTIUGS16000.0016010.0216Q2A.8316050.7316102.3616114.2516124.0116134.7116140.71

NORTHINGS-1895.00-1871.38-1845.47-1789.96-1696.82-1675.37-1657.77-1638.46-1627.64

BIRVATION0.00

-161.98-323.49-645.46

-1125.80-1232.01-1322.80-1422.38-1475.98

1983/5/30** BORSURV *-

Pag* i

SURVW DATA AND CALCULATED OO^ORDINATRS

PROPERTY: S WAX HOIK MO: 592-Wi GRID: GRID 51

DATE: JUM 2, 1992 SURVBT BY: M. W. L. INSTRUMENT: Tropari

DEPTH0. 00

'164. 0032B.OO656.00

^" 7-bQ.OO /72.0Q

790.50892.00900.00997.00

1022.001077.00

mCUNATION-82.00-80.00-80.00-78.00-78,00-75.00-74.00-73.00-73.00-73.00-73.50-74.00

BEARING23.0023.0026.0029.0029.0029.0029.0029.0029.0029.0029.0029.00

EASTINGS16000.0016010.0216021.8316050.7316060.2116062.7016065.09'16079.0716080.2016093.9516097.4516104.91

NORTHINGS-1895.00-1871.38-1845.47-1789.96

^-1778.86 .-1768.37-1764.05-1738.83-1736.79-1711.98-1705.68-1692.22

ELSVATXOX0.00

-161.98-323.49-645.46

^ -737.41-758.80-776.63-873.95-881.60-974.36-998.30

-1051.10

*tf

**

K

M

Q

: 8s1

c?sp;3

3 CMto o

O eo O

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op oo oo r^ r- r- r^r4 H rt r* f* r4 v.

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l l

t

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**4 CM

If)

oo

oo

gogggog

gS8888S

88

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4 l

l l

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CM IT) /* f"

9*-4 fo \o r* f- r*-

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*-( *~ *J *~,

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So vg ea to sr in o-

00 00 00 O* O *— *^

W" *-" 1-1 *-l *-*

88888888

CM

CM

CM

CM

CM

— C

MC

M

88888888

r*- r- r* r- .^ r^ r* i

t i

i i

i i

SO

O Q

O O

O O

O

O Q

O O

O O

OC

MC

MC

MC

MC

MC

N.C

M

*

1983/^/30" BORSORV ** x

SURVEY DATA AND CALCULATED CO-OUmNATHS (Cect)

PROPERTY: SIMAX HOLE NO: 592-X1 GRID: GRID 51

DATE: June 5, 1992 SUKV8Y BY: M. W. L. INSTRUMENT: TROPARI

Pag* l

DEPTH0.00

164.00328.00656.00750.00772.00

^r730; 50822.00877.00967.00

1037.001137.00

INCLINATION-82.00-80.00-80.00-78.00-78.00-75.00-74.00-69.00-68.00-69.00-69.00-69.00

BEARING23.0023.0026.0029.0029.0029.0029.0029.0030.0031.0032.0030.50

BASTINGS16000.0016010.0216021.8316050.7316060.2116062.7016065.0916069.9416079.8716096.6116109.7116128.31

NORTHINGS-1895.00-1871.38-1845.47-1789.96-1772.86-1768. 37 i-1764.05-1765.31-1737.76-1709.34-1687.95-1657.31

ELEVATION0.00

-161.98-323.49-645.46-737.41

. ̂258.80-776,63'-806.50-857.67-941.41-1006.76-1100.12

* aowusv M-

SUKVBY DATA AND CAUWUT8D CO-ORDINATES (Uct)

Page l

PROPERTY: SIMAX HOLE NO: 592-XXI GRID: GRID 51

COMMENTS:GRID NORTH 026 DfiCL 4ESECOND WliUUE AT 902 FIRST AT 790 ,T*'*P

DATS: JURE 10.1992 SURVEY BY: M.W.L.

TROPARI

DWTH0.00

164.00328.00656.00750.00772.0022CL5(L^

*850.00902.00927.00957.00

1007.00tesr. oo

es.i.**rrs**s*s*

INCLINATION-82.00-80.00-80.00-Y8.00-78.00-75.00-74.00-68~.00-67.00-67.00-67.00-65.00-ts. oo

UEAK1NG23.0023,0026.0029.0029.0029.0029.0030.0027.5026.0024.0025.0026. SO

EASTINGS16000.0016010.0216021.8316050.7316060.2116062.7016065.0916074.6316084.2016088.6016093.5616101.99

NORTHINGS-1895.00-1871.38-1845.47-1789.96-1772,86-1768.37-J.764.05-1747.19-1729.74-1721.02-1710.39-1691.89

ELEVATION0.00

-161.98-323.49-645.46-737.41-758.80-776,42-832.89-880.93-903.94-931.56-977 . 23

n.

1992/7/13** BORSURV "

SUMMARY LITHO LOG Page l PROPERTY: SIMAX HOLE NO.: 92-21

FROM TO C.A. LITHOGICAL UNIT

0.00 2687.60

2687.602695.60 48 Felsic Tuff Lapilli Tuff wser gar dlsse* *ag po

2695.60 2726.25 40 Felsic Lapilli Tuff chl bio gar disse* Mg 3*

2726.25 2766.00 38 Blue Quartz Bye Felsic Lapilli Tuff sil chl wMser

2766.00 2818.00 50 Felsic Lapilli Tuff gar bio wser chl disse* py

2818.00 2856.10 50 Mafic Dyke Swan Intermixed Lapilli Tuff

2856.10 2907.00 55 Agglomerate Lapilli Tuff gar chl bio sil wser

2907.00 3060.20 40 Felsic Tuff Lapilli Tuff Breccia gar chl sil MPser

3060.20 3065.75 vs" Fault Zone Breccia ser graphite

3065.75 3317.00 50 Intermediate Tuffs bio chl calcite qtz veinlets

33/7 '

2/7/13** BORSURV **

Page l

SURVEY DATA AND CALCULATED 00-ORDINATBS (feet)

PROPERTY: SIMAX HOLE NO: 92-21 GRID: GRID 51

DATE: July 3,1992 SURVEY BY: H.V.LBAHBY INSTRUMENT: TROPARI

COflENTS:GRID NORTH 026 DECL 4BWEDGE AT 2676 CEMENTED TO OVERCOME BINDING

^ a

DEPTH0.00

164.00328.00656.00750.00772.00790. 50850.00902.00927.00957.00

1007.001217.001265.001412.001497.001557.001657.001757.001857.002007.002097.002197.002247.002347.002395.002497.002547.002657.002676.002685.002707.002732.002762.002817.002877.002977.003087.003197.003297.003317.00

INCLINATION-82.00-80.00-80.00-78.00-78.00-75.00-74.00-68.00-67.00-67.00-67.00-65.00-66.00-66.00-65,00-66.00-65.00-65.00-64.00-64.00-64.00-63.00-64.00-64.00-63.00-64.00-64.00-63.00-62.00-62.00-57.00-54.00-53.00-52.00-51.00-49.00-46.00-45.00-44.00-44.00-44.00

BEARING23.0023.0026.0029.0029.0029.0029.0030.0027.5026.0024.0025.0023.5032.5026.0027.0027.0029.5025.0026.0026.0026.5020.0023.5020.0020.0019.0018.0017.0017.0017.0017.0017.0015.0015.0015.008.008.008.5011.5011.50

BASTINGS16000.0016010.0216021.8316050.7316060.2116062.7016065.0916074.6316084.2016088.6016093.5616101.9916137.7616146.9216176.7116192.4416203.7316223.7416243.4516262.3216291.1516308.9116326.5216334.6416351.1816358.5016373.4316380.5116395.7816398.3916399.7216403.3716407.7116412.7516421.6116431.5916445.0616455.7916467.0516479.5416482.41

NORTHINGS 1895.00 1871.38-1845.47-1789.96-1772.86-1768.37-1764.05-1747.19-1729.74-1721.02-1710.39-1691.89 1612.49-1595,25-1542.06-1510.52-1488.35-1451.12-1412.85 1373.28 1314.18-1278.16-1237.16-1216.81-1175.36-1155.24-1113.09-1091.93-1043.49 1034.96-1030.59 1018.68-1004.45-986.90-953.83-916.57-850.37-774.02-696.38-625.53-611.44

ELEVATION0.00

161.98-323.49-645.46-737.41-758.80-776.63-832.89-880.93-903.94-931.56-977.23

-1168.33-1212.18-1345.94 1423.29-1477.88-1568.51-1658.77-1748.65-1883.47-1964.02-2053.51-2098.45-2187.94-2230.90 2322.58-2367.32-2464.89-2481.67-2489.43-2507.56-2527.65-2551.45-2594.50-2640.46-2714.19-2792.64-2869.74-2939.21-2953. 10

lOfK VOU1ANKB

\ \ \\ \ \s \ \ \ \ \ X \

\\\\s\\s \ \s\\\\\\\

SURFACE PLAN

in. ix OH/U"S" *l-17

On/U* -*- gt ** **O

snmawm un HKUBOT

MAFIC VOLCANICS

METASEDIMENTS

- BARGE:. -SPRUCECONE

SPRUCECONE.*-*;'"**.^

MAFIC VOLCANICS

GROUP 55

^NGROUP 51PROPOSED GRIDCOVERAGE FOR

GEOPHYSICS

MAFIC VOLCANICS

No DEPLETION

MINNOVABIEDLEMAN

BAY PUUTON

GEON CLAW LAKE

SENT BY:THUNDER BAY. ONT. :11-13-92 : 11 = 19 :ACCURASSAY LABS LTD. - 807 623 0452: f* 2/3

ACCURASSAY LABSA DIVISION OF ASSAY LABORATORY SERVICES INC

' - ..'- :-~ 'si'^ :'': ' -.' '•-'•^•••-••#'.5' -v, '-'. '"e ; ;. s : .v-^ i ?:.--.?, ' - -. .'--v-i-c'v; :A. ^v.1-,!.' ' y -'•'••. -

NORANDA EXPLORATION CO. LTD. 960 Alloy Drive Thunder Bay, ON P7B 6A1

Attm Mr. R. Felix Project i

'

A Job t

#':"- ::^:Cppyr: ;sl;^f;igl^; t.:' ; ':; ,v : ^:-SeW*^,^;,^;4 ^^^' -.v.'i v :- V-VJL '.^ -;.5'.' -J\?'' • ••'.-' -'v•^^:-^:-:^V^^fe:^i:.'"'- ;^??;,A ; :;-": ^'.I'.'&r^.v*'-j^/'^C' ; ,i

PO924213T

••Ji;*' " - ' i.'•''v'r! '-'-.'..' • : '--'

K^':' .'''-.':- • '••••'•~-

Cor*cu AA

ppmZnAA

ppm

S-rl-1240.537041306

17650

32570296O

13120

';-.- i-'**vt':: - •••^- t*. . : ..v

' v ''"'"'

i

SENT BY:THUNDER BAY. ONT. '11-13-92: 11:20 :ACCURASSAY LABS LTD. 7. 807,623 0452:* 3/ 3

ACCURASSAY LABSA DIVISION OF ASSAY LABORATORY SERVICES INC.

NORANDA EXPLORATION CO. LTD. 960 Alloy Drive Thunder Bay, ON P78 6A1

i-''*-'Attnt Hr. R. Felix Project! 1 392

o^tt;.chem. Bay Division

Signed*

Jeffre Manag

-..' . -.. ' ..' l . 4 ~ l ".^ - - --f.. .. ' /J.- . , *f-'.•* ' '^. -m:'~f^ffi 3^^S- ; " ••..."^.•;'r . ;.;^:-\, ....^•.••^N •^-^::;^; ;S';-:,. j:^.--^^:^.^-^^^:-S:..•^-, - -' /r^;'*ffj' ^-"•^•'.'•^rii^fe^fe;:^

. f . i'i.

' '- : ,* .' . "l- J .

o JUN t?TSL LABORATORIES

2-308-48lh STREET. EASTSASKATOON. SASKATCHEWAN

87K6A4Q (306) 991-1033 FAX: (306) 2424717

SAMPLE(S) FROM

CERTIFICATE OF ANALYSIS

Noranda Exploration Co. Ltd. 960 Alloy Drive Thunder Bay, Ontario P7B 6A1

SAMPLE(S) OF Core

REPORT No, S4276

INVOICE #: 19467 P.O.: 81814/TB1894

R. Felix Project: 1392

S-l-100 S-l-200 S-l-300 S-l-400 S-l-500

S-l-600 S-l-700 S-l-800 S-l-900 S-l-1000

S-l-1100 S-l-1200 S-l-1300 S-l-1400 S-l-1500

ppm

.6

.2 <.2 .4 .4

.2

.4

.8

.6

.6

.4

.4

.4

.2

Cu ppm

63 5 2 l4

5 l567

525563

Zn ppm

63715758

100

7362319276

746587

12088

COPIES TO: R. FelixINVOICE TO: Noranda Expl.- Thunder Bay

Jun 11/92SIGNED UJU~-**^ \SV~**^

CTA

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report.

Page l of l

SAMPLE(S) FROM

M 2 iTSL LABORATORIES

2 -308-48* STREET, 1A8TSASKATOON, SASKATCHEWAN

87K6A4l (306) 931-1033 FAX: (306) 2424717


Noranda Exploration Co. Ltd. 960 Alloy Drive Thunder Bay, Ontario P7B 6A1

SAMPLE(S)OF Drill Core

REPORT No. S4393

INVOICE t: 19592 P.O.: 81738

A. Smith Project: 1392 -

2450'257026172730.75/2734.332734.33/2739.33

2745/2749 2894.25/2897

Ag ppm

<.2

Cu ppm

29

Zn ppm

34

Agozt

0505.0705

<.05 .05

Cu t

Zn

:.01

COPIES TO:INVOICE TO: Noranda Expl.- Thunder Bay

Jul 08/92SIGNED


CTA

Page l of l

JUI-68S2

TSL LABORATORIES J2-308-48* STREET, EAST

SASKATOON, SASKATCHEWAN87K6A4

O (30*) 931-1093 PAX: (303) 242-4717

SAMPLE(S) FROM


Norando Exploration Co. Ltd. 960 Alloy Drive Thunder Bay, Ontario P7B 6A1

REPORT No. S4340

SAMPLE(S) OF coreINVOICE #: 19527 P.O.: 81825/TB1929

R. Felix Project: 1392

Au ppb

S92-XX1-878S92-XX1-902S92-XX1-1015S92-XX1-1629S92-XX1-1979

S92-XX1-2037

ppm

.2

.2

.4

.2

Cu ppm

227444636

130

Zn ppm

73688690

180

140

COPIES TO: R. FelixINVOICE TO: Noranda Expl.- Thunder Bay

Jun 26/92SIGNED LAc^v^

CTA


Page l of l

JUL 3 o l*— LABORATORIES2-308-48th STREET, EAST

SASKATOON. SASKATCHEWAN87K6A4

O 006) 991-1039 FAX: (306) 242-4717


SAMPLE(S) FROM Noranda Exploration Co. Ltd. 960 Alloy Drive Thunder Bay, Ontario P7B 6A1

REPORT No. S4482

INVOICE #: 19683 SAMPLE(S)OF core P.O.: TB1984

Project: 1392 -

Ag Cu Znppm ppra ppm

S92-2084 < .2 20 49S92-2690 <.2 23 92S92-2982 < .2 6 9S92-XX1-3017 <.2 4 6S92-XX1-3062 < .2 2 4 1

S92-3196 < .2 32 62S92-3298 <.2 43 64S92-3314-3315 <.2 140 15

COPIES TO:INVOICE TO: Noranda Expl.- Thunder Bay

*— y. CTASIGNED ' ' ^" '*

For enquiries on this report, please contact Customer Service Department. Page l Of l Samples, Pulps and Rejects discarded two months from the date of this report.

NORANDA EXPLORATION LTD.Mft 1*T. Ott, mn

Laboratoire* TSL/A88AYBR8 Laboratories760 AV. DU CVIVM C.P. 6*5 MVni-MOIIMU gUBMC J9X 5C6 PHONE ffi 819-797-4693 FM tt 819-797-4S01

I.C.A.P. WHOLE ROCK ANALYSISLithiuB M*t*Ber*t* Fusion

wan ne. i T1588r*0* He. i l of lFil* He. t JN19W

t JW-2S-1992

B-l-400••1-700•-1-MO•-1*400•-i-iooo

y•-i-ueo•-i-iaoo•-I-DOO••1-1400•-1-1(00

•r j

173110

*7

70 41 9]

1.490.4* O.I 0.47 0.3

1.4 1.9 l.t 1.1 1.3

1.333.71 0.9 1.C O.S

fct/ta•S' i/**

NORANDA EXPLORATION CO TCDHMH MY. omuo vrm g. PBLXX n-192*PMJUM2 •

Laboratoirec T8L/AS8AYERS Laboratories760 *V. DU CUIVXB C. P. 669 ftOUYN-IKMMfM QUXNC J9X 5C6

mom t: 619-797-4653 PAX ft 619-797-4501

Z.C.A.P. WHOLE ROCK ANALYSISLithluB itat*Bor*t* Fusion

upon ne. s T1639P*0* 90. l l Of l

PI i* MO. t jvosnDato t JUL-12-1992

XXI-*7( XU-903xn-ioisXX1-162*

XX1-1979

XX1-2037

•r i

107216

222

44|

l.fl.C1.963.3I.!

O.I

TSL/92

NORANDA EXPLORATIONTHDHBCB WOT OW TV-192*

PKMI1992

Laboratoires TSL/A88AYER8 LaboratoriM780 W. DU CUIVRI C.P. 66S ItOUYN-llOMUIDA gWMC J9X 9C6 PNOMI fi 819-797-4653 PAX fi 819-797-4901

I.C.A.P. WHOLE ROCK ANALYSISLithiuB M*ta*or*t* Fusion

o. , T1638•e. i l of l

PU* Ho. i JT09MMM i JVL-08-1992

KXl-1202 XX1-1*00xn-1400 na-1992XX1-1417

xn-1782 XX1-2279

•r :

11089

146

10

LO!ft

0.911.342.923,10.1

1.09 S.94

T81/92'BIONID i

NORANDA EXPLORATION anvil. SMITH raoj.1392 ^

TBI19S7

Laboratoires TSL/ASSAYER8 Laboratories7*0 MT. DU CUIVXB C. r. 665 nOVm-MOMMM QUKBBC J9X BC6 PHONE f: 819-797-4693 FAX li 819-797-4501 Jtli

I.C.A.P. WHOLE ROCK ANALYSISLithiuB M*t*Bor*t* Puclon

JUCKMT Mo. . T1690

Pag* Mo. : l of lMl* Mo. l JY14Wtat* t JVL-20-1992

A1J T10

*

•r ; LOI

X

24*0257026172710.75/27S4.332734.33/2739.33

16.9210.!14.38.1

12.4

0.44 0.72 1.67 0.91 0.7C

0.93 0.1 0.3 O.I1.19

0.31O. It 0.21 0.1* 0.33

O.C 0.( O.C 0.06

1C11149

1.11.471.349.442.11

2749/2749 2894.29/2897

12.1 10.C

1.3 9.1

1.370.99

0.230.26

O.C 0.06

173112 3.65

•IONED lrat/92

HOt 1 1392

tit 19*4

BXPLORATIONAUG 2 6 1992

Laboratoiras T8L/A8SAYERS Laboratories7so AV. ou cuivu e. r. MS MUTO-HOMHM oimne J9x set

•t 819-797-4653 rM fi 619-797-4901

I.C.A.P. WHOLE ROCK ANALYSISLlthluB H*t*Borat* ruaion

mom MO. i T1783Ho. t l of l

•o. l AT07RAtat* l .AOO-12-1992

992-20M•92-2*90•92-29*2392-U-3017 M.' 1-90*2

S92-31M•92-929*•92-9314-991S

•r

137

1. 1.150.92.O.

2.14 1.S1 0.67

Sil

•IOHD

Ministry ofNorthern Development

Mines

Report of Work Conducted After Recording Claim

Mining ActPersonal information collected on this form is obtained under the authority of the Mir this collection should be directed to the Provincial Manager, Mining Lands, Minis Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264.

Transaction Number

se BELL LAKE 900Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining

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.

S * \ . A . s 1 311/1392Recorded Holder(s) /S/OT J ACT 4 CX/) /O r** fl*A- (0xtW)*foy

Noranda Inc./Simax Gas fit Oil Inc. ' /./mWlT^ "Address c/o 960 Alloy Drive, Thunder Bay, Ontario P7B 6A1Mining DivisionPatricia

Dates Work Performed Fr0m: March 1,1 992

Township/AreaBell Lake

Client No. f .176211/? Q*7fe;?o6JTelephone No.

(807) 623-4339M or Q Plan No.

G-2533

TO: July 13, 1992 i l;

Work Performed (Check One Work Group Only)ro

X

Tot

Work Group

Geotechnical Survey

Physical Work, Including Drilling

l

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

al Assessment Work

Diamond Drilling {Hole S-92-1

Claimed on the Attached Statem

Type ;;t.

C

) (u);2o) ;-

"ONTARIO GEOLOG!UAI-;H. j•YMO . A^^^S^^^N * r'lLciO

8 r- r-4 i ; i \ C U ) i- 1, ii ( iMrV ——————

nt of cKyECIET li&LOOO,... in ....*~i- • •~- -

' — ~s'- *~

n.5* ^j ̂ n s-,:

7i ^ 5) "i i ~ o jt. ( :c* mZ ,30 --

t '

. ! -\;\ - ' i : ,-,:;

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

vi id west Drilling -

vi. Leahey, Bayshore Geology

\. Felix (Author), J.Sullivan

W.Reid,W.Bellinger,C.MacDougall,S. Stares

Address

1 80 Cree Crescent, Winnipeg, Manitoba R3J 3W1

692 Dalhousie Drive, Thunder Bay, Ontario P7C 5T9 i

c/o 960 Alloy Drive, Thunder Bay, Ontario P7B 6A1 !' !

c/o 960 Alloy Drive, Thunder Bay, Ontario P7B 6A1

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse side1 certify that at the time the work was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial Interest by the current recorded holder.

Date

Nov. 18/92

Recorded Holder or Agent (Signature)

/^j^ j//^\^s*^-J

Certification of Work Reportl certify that l have a personal knowledge of the facts set forth in this V Its completion and annexed report is true.

Name and Address of Person Certifying

}ecilia M. Barrett, 960 Alloy Drive, Thunder Bay, OntarioTelepone No. Date

807)623-4339 Nov. 18/92

york report, having performed the

P7B 6A1Certified ByJSignalure)

work or witnessed same during and/or after

- . . -. ' i ,., . - . ,- . -. - ' -,.

——*^~, '

For Office Use Only

^201000 Deemed Approval Date

Fet. 17.Date Approved

. 17/93Date Notice for Amendments Sent

RECORDED

NOV 19 1992

0241 (CW9I)

-OO52.

Work Report Number for Applying Reserve Claim Number

Number of Claim Units

Value of Assessment Work Done on this Claim

Value Applied to this Claim

Value Assigned from this Claim

Reserve: Work to be Claimed at a Future Date

Pa 312526 1 180,900 180.900

Pa 430682 20,100 20,100

201,000 201,000

Total Number of Claims Units Total Value Work Done Total Value Work Applied Total Assigned From Total Reserve

Credits are to be cut back starting RESERVE CREDITSt •-ir'l'-lO'^TJ •"V-MI-M'.'M

1 certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed. . -,. , -, -

. B **l M t II f^\ t I O

Signature: ^y^-? '*V^c Date: November 1 8, 1 992

P P * Ul a O' *^K O u

Page 1

Ontario

Ministry of* Northern Development

and Mines

linistere duiloppement du Nord

et des mines

Statement of Costs for Assessment Credit

Etat des couts aux fins du credit devaluation

Transaction No./N 0 de transaction

Mining Act/Lol sur ies mines

Personal information collected on this form is obtained under the authority of the Mining Act. This Information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines. 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) 670-7264.

Les renselgnements personnels contenus dans la presents formule sont recuelllis en vertu de la Lol sur les mines et serviront a tenlr a jour un registre des concessions minieres. Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains minlers, ministers du Developpement du Nord et des Mines, 159, rue Cedar, 4e etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

———————————————————————1311/1393————1. Direct Costs/CoOts directs

Type

Wages Salalres

Contractor's and Consultant's FeesDroits de ('entrepreneur •t de ('expert- consell

Supplies Used Fournltures utilise**

Equipment Rental Location de materiel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

Type Drilling, dip tests

Engineering

Type Sample bags, boxes, etc

Type

Amount Montant

5.600

5,600

172,000

10,800

2,300

Total Direct Costs Total des couts directs

Totals Total global

••'••l-:^"^M

;ii|200!;

ift9rROft

^JÎfgSt*!i2i30pi!

i sn j wvvM

2. Indirect Costs/Gouts indlrects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work. Pour le remboursement des travaux de rehabilitation, Ies coQts Indirects ne sont pas admisslbles en tant quo travaux devaluation.

Type

Transportation Transport

Food and Lodging Nourrtture et hebergementMobilization and Demobilization Mobilisation et demobilisation

Description

Type Ground

Fixed Wing

Amount Montant

1,100

900

Totals Total global

2,700

Sub Total of Indirect Costs Total partlel des couts Indlrects

Amount Allowable (not greater than 20H of Direct Costs) Montant admissible (n'excMant pas 20 M des coats directs)Total Value of Assessment Credit (Total of Direct and Allowable Indirect costs)

VaJeur totals du creditdevaluation(Total d* coott direct*

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification Is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Le titulaire enreglstre sera tenu de verifier Ies defenses demandees dans le present etat des couts dans les 30 jours suivant une demande a cet effet. Si la verification n'est pas effectuee, le minlstre peut rejeter tout ou une partie des travaux d'evaluation presentes.

Filing Discounts

1. Work filed within two years of completion is claimed at 100(ft of the above Total Value of Assessment Credit.

2. Work filed three, four or five years after completion is claimed at 500X) of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimed

x 0.50 -

Remises pour dep6t ~- i~ g

1. Les travaux deposes dans lesûâns suivanQgur achevement sontrembourses a 100 "H. de la valeur totals ftkmentlonnee du credit d'evaluation.rj *~* ni ^

2. Les travaux deposds trols, qiu^r^tCplnq ensures leur achevement sont rembourses a 50 to de^2a vaîr totale' du credit d'evaluation susmenttonne. Voir les calci® cl-dessous. *^*

Valeur totale du credit d'evaluation Evaluation totale demandeex 0,50 -

Certification Verifying Statement of Costs Attestation de I'etat des couts

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that as riHc AHminictrgfftiffioi{RecofdedHoToer, Agent, Position In Company)

to make this certification

J'atteste par la presents :que les montants indiques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-jolnt.

l am authorized Et qu'a titre de je suls autoris6(titulaire enreglstre, representant, post* occupe dans la compagnle)

a falre cette attestation.Signature Date

NOV. 18/92

0212 (04/81) Nota : Dans cette formule, lorequ'll designs des peraonnes, le masculin est utilise au sens neutre.

rfAFIC VOLCANICSSWAMP LAKE. Y

PROPOSED DRILL HOLE

. CLAW LAKE \\ INTRUMAFIC INTRUS.

MAFIC VOLCANICFELSIC VOLCANICS

FELSIC TUFF

MAFIC VOLCAN

\. \ S. V V

\\\ \ \ \ 2̂±-'^

MAFIC INTRUSIVE

x RHYO RAGMENT^L

MAFIC VOLCANICS

SURFAC PLAN

^I24 2.6* Cu/1.4 ft51-15

1.45* Zn, Cu/16.5 tt

alteredhorizon 7

no sulphides.03X Zn. 1 X Cu/12 ft

0.15X Zn 0.02X Cu/1 ft

51-18W 51-17

3* Cu/5 ft 0 alt'n ? no atpayi

-1,000 ft

MATTABI DEPOSIT DIMENSIONS

2,000 ft

off hoi* onomajv(no alt'n below)

•bort ?O 200 400 600 600 1000

SEMI-WASSIVE PY/Q.5' N.SA norandaPROPOSED DRILL,

NORANDA EXPLORATION Co., LTD. - THUNDER BAY

STURGEON LAKE0.1 X Zn/lfltt

Zn frog*.ehort 7

(PEM to 1800' only) PROJECThorizon ehort

no alteration(TOP OF ALTERATION)LONGITUDINAL

I

LONGITUDINAL *e, SURFACE PLANInterpreted by : W. REID

Project number : 2311

File number : 7311DRLP

52G15SW0B02 26 BELL LAKE MAPS

CLAW LAKE

\OOP ..(p.p. ( -] ^UTSIDE LOOP)

f+1 OUTSIDE NES TO SOUTH OF LOO

SUALL CONDUCTOR. CHANNEL RESPONSE"•"•" 1 2 '40: 45

400ft 800ft Oft l l L l l

STURGEON UKEMAGNETOMETER SURVEY .

PROJECT: STURGEON PROJECT | : 1392 BASELINE AZIMUTH : 300 D*g.

SCALE - 1 i 4800 / r ~ 400ft DATE : 3/19/92 SURVEY BY : CS/BM Quod\:

FILE: M1392FINORANDA EXPLORATION

MAP 2

iS Lapilli Tuff, ohl-gar Alt'n

Fault Ton* Lopim Tuff Dooltlc Aeh Tuff

Breaolated Rhyoltte/ Rhyodoalto

Lopllll Tuff, ohl-f gor tr po.apy f j

f

0.3* "l / Intermediate Tuff/ lapilli Tuff wW cbl- gar

locally breodated wk ehl

l ll l

RhyollU areoola mod ohl.gor.tr py

Felelo Breoola Fragmental wmr qta vein* o hi gor

RhyollU Flow Breoola ill, a W 1-5* py.po

lue Quarto Ey* L eye DooKe ohl bio

/ Blue Quarto Ey* Lapilli Tuff gar *Mt*r Qti

Lopllll Tuff Fragmental blo ohltfW* BnTuff ohl bla

Lapilli Tuff Fragmental bio ohl

looal garnet* Moflo Dyke Swarm Lopllll Tuff Frogman

weeF blo lapilliFelelo Tuff Lapilli Tuff

* \ 'Moflo Dyke/Swarm gar

Cherty FeltlA Vela Green

Ohl bl*aoh*d frag

iy* r*l*1o Lapilli Tuff w**r gor gar

[•la Lapilli Tuff wmer bio large gar

ill Mw wohl k^xir fadol oar Dlortt* Dyk* k* pa/ alt d1it*n( py t F*ltlo Vole AA til Mnr/wohl kvpar f*do! gar

Dyk* oolott* v*lnt

tle Veto Alt til H**r wohl taar

f Fettle Tuff Lapilli Tuff ehl blo gar py to IS i

' \ l il 1\ Moflo Dyke looal py f t

Felvla Lapilli Tuff Ago.! w*er blo ohl minor py epy

j f t J t

l

. \ DlarlU (by** dltnm py to/lX

(li 1Blue Quartz Ey* F*l*lo Lap Aggl gar minor py bio

Diorite Dyk* t. 5 - 2X qltMm py

Felvta Vote * Uaflo DykM

CHorft* Dytw 1-1.5 X dlmftm py

Moflo Dyke blo py 2* In Volo ZenofHht

;f relate Tuff til wt*r on foso gar ontho py h dyk*

Ey* Xtal Tuff wM**r dlM*m mag

l/u*1"'0 ^P"1' Tuff ohl bla oar dltttm mag 3X

J* Btu* Quartz Ey* Fiblc Lapilli Tuff *ll eh l tffbtr

Fel*le Lopllll Tuff gar blo mer ohl

Dyke tflee*m py

l Mafia Dyke Swarm Inttrmlxtd Low l II Tuff

/ Agglornorate Lapilli Tuff glr ehl blo tl!

rrtH.lba'"H!lffTYJapf* 1 TWMSnWSlJflg8 Feldspar Xtal Tuff o* on fracture*

f •rrtd.lba'rWrYjapf* 1

Felilo TJff Lapilli Tuff Brvoolo gar ohl ill MP.*r Tuff nllclt* chlorite vetnlete

Intermediate Tuff* bto ehl calcite q t velnlvt

NORANDA EXPLORATION Co. LTD

SECTION 16000E

SIMAX OPTION

Na20 VALUES PLOTTED

DATE: SEPT 1 6/9252G15SW0002 26 BELL LAKE

area : report no: 26 bell lake work performed ......notes: (1) w9230.0052, filed dec/92. 52gtssweeea...

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