BATEMAN 010 DIAMOND DRILLING TOWNSHIP: BATEMAN … · PURE GOLD RESOURCES LTD. 020 J l l l l l l...

BATEMAN

DIAMOND DRILLING

010

TOWNSHIP: BATEMAN REPORT NO:55

WORK PERFORMED FOR: Pure Gold Resources Inc

RECORDED HOLDER: Same as Above [xx]: Other [ ]

Claim No.

KRL 865481

KRL 865495

KRL 865496

KRL 865441

KRL 865447

KRL 865437

KRL 865433

Hole No.

87-01

87-02

87-03

87-04

87-05

87-06

87-07

Footage

174.7m

224.39m

157.58m

157.58m

287.53m

152m

306.64m

Date

Jan/87

Jan/87

Feb/87

Feb/87

Feb/87

Feb/87

Feb-Mar/87

Note

(D

(D

(D

(D

(D

(D

(D

NOTES: (1) #90-87, filed in April/88.

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ss BATEMAN

DIAMOND DRILL REPORTLOGS AND SECTIONS

1986-1987 WORK PROGRAMME

HOYLES BAY PROPERTY

PURE GOLD RESOURCES LTD.

020

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ASSeSSMENT fJL- l

RECEIVED

y

l l l l l l l l l l l l l l ll Eugene Flood

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DIAMOND DRILLING PROGRAM

ON THE

HOYLES BAY PROPERTY

BATEMAN TOWNSHIP

ONTARIO

FOR

GOLDEN RIM RESOURCES LTD.

JANUARY - MARCH 1987

B.Se. Geology April 10, 1987

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l. INTRODUCTIpN

Golden Rim Resources holds a block of 127 claims in Bateman Township, Kenora Mining Division.

Noramco Exploration Inc. entered into an agreement with Golden Rim Resources to explore the potential for gold mineralization on the claim group. From the end of September to the beginning of November 1986, Noramco Exploration Inc. carried 1500 metres of diamond drilling which was completed by the beginning of March, 1987.

The Following report outlines the work done and the results obtained in the winter 1987 drill program.

2 ' SUMMARY AND RECOMMENDATION

Seven holes for a total of 1500 metres of BQ core was drilled on the Hoyles Bay property between January 15 and March 3, 1987 by M&B Drilling. While drilling improved the results obtained from surface sampling, no economic gold mineralization was intersected. Structural influences are considered to be the main contributing factor for the localization of gold. Sixty percent of the gold values greater than 100 ppb were located directly at lithological contacts in areas of magnetically interpreted faulting. Geochemical l y anomalous gold mineralization (95-455 ppb Au) was encountered in virtually every rock type. As there is no correlation of anomalous zones between drill holes, no evidence for a lithologic control exists. Follow up drilling using these guidelines and available geologic and geophysical data, is recommended in the following areas;

1) Between L22E and L26E, 2 + 50S to 4 + 50S, a section of an otherwise continuous E.M. anomaly has been dislocated to the north. A corresponding break in the magnetic response indicates faulting.

Eight I.P. anomalies were registered in this small zone. The high chargeability, low resistivity readings indicate a high concentration of sulphides in chert.

2) Two parallel continuous I.P. anomalies are found in the sediments south of the above area. These are;

a) L22E to L25E, 7+75S to 8+50S.High to very high resistivities and chargeabilities wereregistered.Spectral I.P. data indicates fine-grained sulphides arepresent.One of the station anomalies was rated a priority by thegeophysicist in charge of the survey.


b) L22E to L25E, 6+OOS to 7+OOS.Moderate to high resistivities along with low to high chargeabilities were encountered. Spectral I.P. data indicated the presence of fine-grained sulphides. Two of the four station anomalies were rated a priority to be drilled.

3) An E.M. conductor with significant continuity shows a break in its magnetic signature in an area where previous drilling intersected 680 ppb and 1020 ppb gold. The area in question is between L36E, 7+25S to 7 + 25S and L37+50E, 8+OOS to 8+75S. Two I.P. anomalies, one of which has a priority rating are co incident with the E.M. anomaly. The high to very high chargeability response is due to coarse-grained sulphides as determined by spectral data.

4) Immediately south and roughly parallel to the area above is a zone defined by four I. P. anomalies, three of which have a priority rating. The area is between L36E, 8+25 to 8+75S, and L37+50E, 9+50 to 10+25S. The source of the moderate chargeability is fine-grained disseminated sulphides as determined by spectral data.

5) South of the above I.P. anomaly is an E.M. conductor in mafic volcanics. The conductor has 3 corresponding I.P. anomalies of moderate to high chargeability and low resistivity. As there is no magnetic correlation, this conductor may represent a dilational shear zone with sulphides.

6) The area between L15E and L17E, 2 +75S to 4 + 50S defines a break in an E.M. conductor and it's corresponding magnetic signature. Also located within this zone are two I.P. anomalies of high to very high chargeability and low resistivity. The response is due to coarse-grained sulphides. The low resistivity may be the result of alteration in this zone of potential faulting.

7) In the north central portion a fold structure has been interpreted to exist based on ground magnetics. From L26E, 4+25N ti 6+50N, to L28E, 3+75N to 6+25N to L30E, 4+50N to 6+50N, there exists a broad formational feature with a large volume of chargeable material. I.P. spectral data from two priority rated anomalies located within this zone indicated fine-grained sulphides at depth. Therefore, fine-grained sulphide mineralization localized in a fold structure presents a target. A detailed ground magnetometer survey, with lines at 50 metre intervals, over this fold structure would prove very useful in delineating its true shape, and thereby further defining the target.


3 ' PROPERTY, LOCATION AND ACCESS

The property consists of 127 contiguous, unpatented raining claims in northern Bateman township, Kenora Mining Division, Red Lake, Northwestern Ontario. The claim group is approximately 16 kilometres north-northeast of the townsite of Red Lake.

Access may be gained by road, water and air. The Road branches north off Highway 125 approximately l north of Balraertown which is 9 kilometres northeast by Red Lake. Pine Ridge road turns east off Nungesser Bateman township and transects the entire property, lumber roads provide excellent access to the interior, forms the southern property boundary and is accessible float plane, from Red Lake or Cochenour.

Nungesserkilometreroad fromroad intoNumerousEast Bay

by boat or

4. WORK DONE

The drilling was done under contract by M&B Drilling of Powell Rover B.C. between January 15 and March 3, 1987. Over this time period, a total of 1500 metres of BQ core in 7 holes was drilled as listed below. All core was logged and a total of 900 samples, representing approximately half the core, was split and sent for assaying.

The core is presently stored in racks at the Old Buffalo Mine site, just outside the southern boundary of the town of Red Lake.

Drill logs, sections and a plan showing the drill hole locations are included in this report {see figures 1-8).

TABLE l

Hoyles Bay Drilling

Hole No. Co-ordinates Length Angle

NHB-97-01 L6W: 0+25N

NHB-87-02 L8E: 2+75E

NHB-87-03 L10E: 3+45N

NHB-87-04 19*38E:3*50N

NHB-87-05 L24E: 5+38N

NHB-87-06 18*50E:10*25E

NMB-87-07 L20E: 13+50N

174.7m

224.4m

163.4m

163. 4ra

298.2m

157.6m

318.0m

-45

-49

-49

-50

-50

-50

-65

Azimuth

90

130

130

130

145

130

130

Claim No.

865481

865495

865496

865441

865447

865437

865433

Total 1499.7m


5. RESULTS

A summary of all significant assay results is presented in Table 2 in the Appendix.

NHB-87-01: The hole was collared to test an E.M. conductor, an interpreted fault zone, and a mineralized lineament. A 5 metre section of massive sulphides was intersected between 151.4 and 156.3m and is considered to represent the E.M. anomaly. Consistently low gold assays ranging from 10-52 ppb were obtained from this zone. A fault breccia intersected between 124.1 and 124.7m corresponds well with the location of the magnetically interpreted fault. The lineament which to the southwest contains gold mineralization was not intersected. Approximately 7C^ of this hole consisted of felsic volcanics, a unit which had not been identified during the fall mapping program. This unit was subsequently intersected in the next five drill holes. No significant gold values were obtained from this hole.

NHB-87-02: The objective was to intersect an E.M. anomaly and two magnetic highs.The massive sulphides intersected between 71.59-91.97m and 174.1- 211.0m were responsible for the E.M. anomaly and the two magnetic highs. While these sections were barren, anomalous gold values were intersected. A sulphide bearing chert unit at the tip of the hole returned a value of 680ppb Au over 0.6m (10.1-10.7). A check assay however failed to verify the original assay. The contact zone between a mafic tuff and chert unit yielded 278 ppb Au over 2.4m (172.6-175.0). Mineralization included thin fuchsite and blue quartz veins along with pyrite and pyrrhotite. A 30 metre wide ultramafic intrusion was intersected near the beginning of the hole. This rock type was not recognized during the mapping program. Ultramafic intrusion were also intersected in holes #5,6 and 7.

NHB-87-03: This hole was designed to test a "massivesulphide" I. P. response in the vicinity of a potential faultstructure.Massive sulphides (pyrrhotite, magnetite and pyrite) wereintersected between 72.6 and 82.9m.

NHB-87-04: This hole was drilled to test for an interpreted structural break between two iron formations.Virtually the entire hole was comprised of an intermediate to felsic volcaniclastic unit. A 0.9m section (59.5-60.4m) containing three thin quartz veins and trace fuchsite ran 268 ppb Au (averaged). No other significant gold assays were returned.

NHB-87-05: The objective was to test an I.P. anomaly flankingand apparent fold structure as outlined by a ground magnetometersurvey.The source of the high resistivity anomaly is considered to be afelsic volcanic unit which comprises over 85% of this hole.


Certain sections of this volcanic unit displays intense potassic alteration. A value of 250 ppb Au over 0.9ra (177.1-178.Oro) was obtained from an mafic dike which contained irregular quartz veins and 1 ^ disseminated pyrite. No other anomalous gold values were obtained.

NHB-87-06: The purpose was to test a short isolated E.M. anomaly with a correponding magnetic high.A chert unit intersected between 54.8 and 60.0m containing 10% pyrrhotite is considered to be the source of the E.M. anomaly. Ultramafic intrusions containing disseminated magnetite comprise 60% of this hole. The cumulative effect of these intrusions are considered to be responsible for the "bull"s-eye" magnetic high. No significant gold values were obtained.

NHB-87-07: This hole was designed to test a short isolated E.M. conductor with a corresponding magnetic high. A chert unit with 15% pyrite and pyrrhotite, intersected between 34.57 and 41.46m is considered to be responsible for the E.M. anomaly. Weak to moderately magnetic ultramafic intrusions comprise approximately 15% of this hole. This, along with the pyrrhotite that is weakly disseminated throughout most of th hole would account for the magnetic high. Two horizons intersected anomalous gold values. A wacke unit with l* pyrite produced an assay of 150 ppb Au over 0.58m (144.9-145,48m) and 303 ppb Au over 1.8m (135.0-136. 8m) . The best section from this last interval was 455 ppb Au over 0.9m (135.0-135.9ra) . Downhole of the wacke unit a section of chert containing 5% pyrrhotite and 2% pyrite produced an assay of 360 ppb Au over 0.75m (148.95- 145.7m). Interesting alteration included S-10% sericite in the intermediate tufaceous into and trace molybdenum on fracture surfaces in the upper two wacke horizons,

6. CONCLUSIONS

Four of the seven drill holes in this program intersected zones of gold mineralization greater than 200 ppb. These are;

NHB-87-02: 10.1-10.7m ppb fold in a section of chert containing 5% pyrrhotite and 1.^ pyrite.

172.6-175.Oro, 278 ppb gold averaged over the contact between a mafic tuff (blue quartz veins with pyrite and pyrrhotite) and a chert unit (5% pyrite and pyrrhotite).

NHB-87-04: 59.5-60.4m, 268 ppb gold obtained from a felsic volcanic unit with quartz veining and trace fuchsite.

NHB-87-05: 177.1-178, Om, 250 pb gold in a mafic dike with quartz viewing and disseminated pyrite.


NHB-87-07: 135.0-136.8m, 303 ppb gold in a wacke unit with 13; pyrite. The interval 144.9-145.48, also from this same wacke unit, returned an assay of 120 ppb gold.

148 . 95-149 . 7m, 360 ppb gold from a section of chert containing 5% pyrrhotite and 2% pyrite.

Gold mineralization, as revealed by drilling, is found in all of the respective rock units on this property. The auriferous zones were accompanied by quartz veining and/or sulphide mineralization. Gold bearing horizons did not correlate between drill holes. It is thus considered that the localization fo gold mineralization is structurally controlled. Further evidence to support this view lies in the face that six out of the ten gold values greater than 100 ppb were located directly at a lithologic break. Rock contacts represent zones of weakness which may act as conduits for mineralizing fluids during a hydrothermal flooding event. Unfortunately, the drilling does not discern any specific formational boundary as being of particular interest. What perhaps is of more importance to the mineralization model is the presence of crosscutting structures, the intersection of which may prove favorable for the localization of gold mineralization. Structural breaks impinging on forrnational interfaces may then represent viable targets for future exploration.

94*40*

BATEMAN TWR

51* 10*

LEGEND

6 Felsic intrusive rocks5 Mafic intrusive rocks4 Chemical metasediments3 Clastic metasediments2 Intermediate metavolcanics1 Mafic metavolcanics

1000m

NORAMCO EXPLORATIONS MC.

GOLDEN RIM RESOURCES INC.

HOYLES BAY PROPERTY GEOLOGY

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CERTIFICATE OF QUALIFICATION

I, Eugene Flood, do hereby certify:

1. that I am a geologist and reside at 2045 Courtland Drive Burlington, Ontario. L7R 1R7

2. that I graduated from Lakehead University (Thunder Bay, Ontario) in 1985 with a Bachelor of Science degree in Geology

3. that I have practiced my profession continuously since graduation

4. that the report on the Diamond Drilling Program on the Hoyles Bay Property, Ontario is based on my personal knowledge of the geology of the area, field work carried out by and supervised by me and on a review of published and unpublished information on the property and surrounding area.

Cuxafc/inJi—

Eugene Flood,B.Se. April 30, 1987

APPENDIX


TABLE 2

SUMMARY OF ASSAY RESULTS FROM DRILL CORE

HOYLES BAY PROPERTY 11446

Sample* Host Rock Hole* Interval Width Assay Check Average SampleppbAu Assay Assay Descrip.

1762 Chert 87-02 10.1- 10.7m

0.6m 680 Nil 340

1872 Mafic Tuff

87-02 172.6- 0.9 173.5m

225 380 303

4968 Mafic Tuff

87-02

1873 Chert 87-02

173.5- 0.6m 174.1m

174.1- 0.9m 175.0m

200

1872-4968-1873 87-02 172.6- 2.4ra175.0m

385 250 307380 210

278

4791 interm. 87-04 59.5- 0.9m 210 345 Felsic V 60.4ra 170

4931 Mafic 87-05 177.1- 0.9m 250 Dike 178.0m

9612 Wacke 87-07 137.2- 0.9m 455138.1m

268

5* po. l^fe py . < f l % c p y 5 % chlor.* sericite

Thinfuchsitebluequartzbands .Smallchertinterbandl* py+po

Bluish quartz veins with py+po.

5* py* po

Weighted Average

3 thin qvs Trace fuchsite.

Irregular qtz veins l* dissem.PY

3^ PY15Sfecarbonate

l ll Sample# Host Rock Hole# Interval Width Assay Check Average Sample

PpbAu Assay Assay Descrip.

l 9613 Wacke 87-07 138.1- 0.9m 150 life py ™ 139.0m fracturi

surfaces

l 9612-9613 87-07 137.2- 1.8m 303139.0m

l 9624 Wacke 87-07 147.26- 0.58m 120 5*^ py147.84m

1 9629 Chert 87-07 151.37- 0.70m 360 5*^ po 152.13m 2*5; py 10'chlorite

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1111111111111111111

t

Hole!

1

2

1

2

3

4

1

2

3

4

1

2

3

4

5

1

2

4

5

6

7

Metreage

26.2m

193.8m

228.4m

106.7m

169.2m

107.0m

121.34m

50.91m

48.17m

121.65m

30.5m

32.0m

10.7m

23.2m

26.2m

7.9m

7.9m

39.0m

39.6m

38.4m

38.4m

SUMMARY OF PREVIOUS DRILLING

ON THE HOYLES BAY PROPERTY

Year Company

1948 Sadie Red Lake Mines Ltd

1948

1948 Dewson Mines Ltd

1948

1948

1948

1956 New Dickenson Mines

1956

1956

1956

1957 McDonald Property

1957

1957

1957

1957

1959 New Dickenson Mines

1959

1959

1959

1959

1959

SignificantResults

850 ppb Au/ 3. 1min FeldsparPorphyry

Unsampled

7

7

7

7

7V

7

?

7*

7

7

7

7

7

7

7*


Holet Metreage Year Company

30.2m 1959 Cull Property

16.0m 1959

7.4m 1959

23181 49.7m 1966

30604 125.0m 1966

30605 142.7m 1966

30607 185.1m 1966

INCO

INCO

INCO

INCO

Significant Results

1 assay of 2040 ppb Au2 assays of 1360 ppb Au5 assays of 680 ppb Au6 assays of 340 ppb Au Mo s t assays from sheared andesite

1 assay of 2040 ppb Au2 assays of 6080 ppb Au l assay of 3040 ppb Au All assays from andesite with sulphides

l assay of 1700 ppb Au l assay of 680 ppb Au Assays f rom andesite


DR\U LOCATION

I145

l

l'* 5600

8-03-1987::13:42

NORAMCO EXPLORATIONS INC

DIAMOND DRILL LOG

NHB 87-01

Property: Hoyles Bay J1446

Partner:

Azimuth: 90 degrees

Logged By: E.Flood

Date Started: Jan.15/1987

Core Size: BQ

Drill Company: M&B Drilling

NTS:

Clain f:

Dip:

Casing:

mnm 865481

-45 degrees

Out

Date Conpleted: Jan.18/198?

Core Location: Buffalo Hine Site

Overburden: 14.05 netres

Township: Balenan

Coordinates: L6H , fl*25N

Length: 174.7 netres

Elevation: Surface

Date Logged: Jan.19/1987

Samples Shipped: Jan.20/1987

Acid Dip Tests

l l, 15,85 c -49 deg. l 3 . 121.95 D -44 deg.

l 2 , 62,5 g -46 deg, t 4, 174,7 B -41 deg,

Purpose

Conclusions

Recointendations

To intersect an E.H, conductor,To intersect an interpreted fault zone,

Massive sulphides were intersected between 151,4-156,3. This does not correlate with the E.H.conductor on surface, A fault zonelfault brecciaibroken core) was intersected

Follow up drill locations are dependant on assay results,

8-03-1987:;13:42

NORAMCO EXPLORATIONS INC.

DIAMOND DRILL MG -t SUMMARY

NHB 87-01

Page 2

z:zzzzzzzzzzzzzzxzzzrz:zz::zErzzzzzzzzzzzzzzzzz:::zz::xzszzzziE:z::c:'r:::::;:E:iixx::23:;:xs': i:::tcez::a;:zE:zt::zzE!:x::3:zz

Fron(B) Tod) ——————-—-Description———————————"—:—*——-T---—-Mineralizationls)——-•, i ' '';, ' ' " ! v j,' . . .

' , , '"' ' "' ' ' r,' '-'" ^ -'-' \- '. , i''~, : ' ' ' ''- :'-

0,0 14,1 OVERBBRDES ; ,i ; ' ^

14,1 22,0 FELSIC VOLCANIC . .', . '

22,0 28,1 INTERKEDIATE VOLCANIC

28,1 49,1 FELSIC VOLCANIC

49,1 50,1 HAFIC DYKE

50,1 56.6 FELSIC VOLCANIC

56,6 57,8 HAFIC DHE


Pyrite Kit)

Chalcopyrite Kit)•' ' , *! '"' : ' ' : .

"Pyrite

"Pyrite

Pyrite Kit)

Pyrite ((Hinfringe)

::zz:;czzxzzzzEzx::zzzzEzrrzzzzzzzzzzzzz"-———Alterationlsl——-———-

Silica O Sericite {(It)

Garnet (21)XelloB-Green Sericite (l Chlorite

Silica Ufi-W)Chlorite (H)iellow-Green Sericite (U)

Carbonate ((HI

Biotite^ellov-Green Sericite (241Carbonate Kit)

Carbonate (I Garnet Kit)

Silica U0-15t) Chlorite Kit)

-f)3-1987::13:42


DIAKOND DRILL LOG - SUHKARY

NHB 87-01

Page 3

Proitlsi) Tola) -———————-Description—————-—...............——---™KineralizationU)——-—————Alteration(s)--————..———.—.——Description————

61,8 65,4 DIORITE HITH QUARTZ AND FELDSPAR PHBNOCRYSTS


102,5 104,4 HAFIC DYKE


151,4 156,3 MASSIVE SULPHIDES


•MineralizationU)——

Pyrite ((14 in stringe)

Pyrite K(U) Chalcopyrite (((14)

Pyrite (14 fracture fi) Chalcopyrite

Pyrite ((14) Chalcopyrite (((H)

Magnetite (50*) Pyrrhotite (35*) Pyrite (154)

Pyrrhotite (14) Pyrite (W Magnetite ((U)

Silica (1-2U Chlorite ((14)

Yellow-Green Sericite (54) Chlorite (U)

Carbonate (2-54 ubiquitou) Chlorite 0

Silica i 204)Yellow-Green Sericite (24) Carbonate K14)

Carbonate ( -trace) Garnet ( -trace) Chlorite ( -trace)

Chlorite (1-24) Garnet ((14)

174,7 END OF HOLE,

B-03-1987::13:43


DIAMOND DRILL LOG

NHB 87-

Page

01

4

From To ———————-W ( B)

0,0 14.1 OVERBURDEN


-Description-

Light GreyFine GrainedFoliation at 30 Deg, Cai,Lower Contact at 40 Deg, Cai.Weakly Fractured (2 Fractures/Metre)li Carbonate Veining at 30 Deg, Cat, - Avg, Hiclth 2iPyrite: WPyrrhotite: mChalcopyrite! (l*.Silica Alteration:Sericite Alteration: ( l\Non Kagnetic

Alteration produces a brecciated texture

22,0 28,1 INTERMEDIATE VOLCANIC

Grey to GreenFine GrainedFoliation at 30 Deg, Cai,Lover Contact at 50 Deg, Cai,Heakly Fractured (l Fractures/Metre!(H Carbonate Veining at 70 Deg, Cai, - Avg, Hidth 3cnPyrite: WGarnet Alteration: 24KelIon-Green Sericite Alteration:Chlorite Alteration: 151Non Kagnetic

Saiple Froi To Width Au Ag Cu Zn Pb Sb As Ko No, (g) (B) (z) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)

17011702

1703

1704

1705

1706

1707

14,18 14,7914.79 15,40

16,77 17,84

20,21 20,43

20,88 21,34

24,09 24,70

25,91 26,52

0,61 20,0000,61 5,000

1.07 nil

0,22 30,000

0,46 15,000

0,61 nil

0,61 nil

Chloritic alteration produces a brecciated teiture

8-03-1987:;13;43


DIAMOND DRILL LOG

NHB 87-01

Page 5

ProB lo -Description-

Upper contact 15 deg.can 701 core recovery 22.87-25.91

28.1 49.1 FELSIC VOLCANIC

Light-GreyPine GrainedPoliation at 30 Deg. Cai.Lower Contact at 70 Deg. Cai.Weakly Fractured (l Fractures/Metre)Silica Alteration: 10-154Chlorite Alteration: ItHellow-Green Sericite Alteration: ItSon Magnetic

Upper contact 50 deg.cail, SB lost core:30.5-32.0(iislatch)randoB chlorite veining produces brecciated teiture

SaapJe ProB To Width Au Ag Cu Zn Pb No. IB) (B) (B) (ppb) (ppb) (ppb) (ppb) (ppb)

Sb As Ho (ppb) (ppb) (ppb)

1708

1709

1710

1711

1712

1713

28

32

33

35

37

41

.35

.32

.54

.00

.80

.46

28

33

33

36

38

41

.96

.23

.84

.13

.11

.77

0.61

0.91

0.30

1.13

0.31

0.31

nil

nil

nil

nil

45.00

nil

49.1 50.1 HAFIC DYKE

Dark GreyPine GrainedMassiveLover Contact at 50 Deg. Cai.Weakly Fractured (2 Fractures/Metre)Ut Carbonate Veining randon angles -- Avg. Width 2nPyrite: Ut

8-03-198?::13:43


DIAMOND DRILL LOG

NHB 87-01

Page 6

FroB IB)

To Description

Carbonate Alteration; (H Non Kagnetic

Upper contact 70 deg.caxweak pervasive carbonate alteration


Light-GreyFine GrainedFoliation at 25 Deg. Cat.Weakly Fractured (l Fractures/Metre lBiotite Alteration: 54Yellow-Green Sericite Alteration: 21Carbonate Alteration: (HNon Magnetic

Upper contact 50 deg.cassoffle sections appear brecciatedl DID wide fuchsite sean associated with carbonate,Lower contact irregular,

56,6 57,8 KAFIC DIKE

Light-GreyFine GrainedKassiveWeakly Fractured !8 Fractures/Metre)(U Carbonate Veining at 70 Deg. Can, -- Avg, Width fatPyrite: (HCarbonate Alteration: ttGarnet Alteration: (HNon Kagnetic

Saiple Froa To Width Au Ag Cu Zn Pb So. (a) (i) (g) (ppb) (ppb) (ppb) (ppb) (ppb)

Sb As Ho (ppb) (ppb) (ppb)

1714 53,81 54,12 0,31 nil

1715 56,10 56,40 0,30 nil

1716 57,49 57,8 0,31 nil

8-03-1987;:13:44


DIAMOND DRILL LOG

NHB 67-01

Page 7

Froj) (B)

To (i)

-Description-

carbonate occurs as fine phenocrysts Lower contact irregular


Light-GreyPine GrainedWeakly Fractured (5 Fractures/Metre)(H Carbonate Veining randoa — Avg, Hidth lwPyrite: U4 in stringersSilica Alteration: 10-154Chlorite Alteration: (14NOB Magnetic

Upper and lover contacts are irregular

61,8 65,4 DIORITE WITH QUARTZ AND FELDSPAR PHENOCRYSTS

GreyFine to Kediuia GrainedMassiveLower Contact at 45 Deg, Cai,Weakly Fractured (6 Fractures/Hetre)(It Carbonate Veining randoi angles -- Avg, Width 2mPyrite: (14 in stringersSilica Alteration: 1-24Chlorite Alteration: (14Non Magnetic

There are 3 separate intrusions within this unit; Diorite with predominantly feldspar phenocrysts

Saiple No,

FroB To Hidth Au Ag Cu Zn Pb Sb As Ho (i) (B) (B) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) tppb) (ppb)

1717 58,69 58,99 0,30 5,1

1718

17191720

63,57 63,87 0,30 nil

64,33 x 64,94 64,94 65,55

0,610,61

nil nil

H3-1987;:13:44

NORAMCO EXPLORATIONS INC*

DIAMOND DRILL I.OG :

NHB 87-01

Page 6

Proa (B!

To In)

-Description

Felspar PorphyryThe two dioritic phases are interniied

65.4 102.5 FELSIC VOLCANIC

Light-Grey to Dark-GreyFine GrainedFoliation at 25 Deg, Cai.Weakly Fractured 12 Fractures/Metre!(tt Quartz Veining at 80 Deg, CaiPyrite: ((ttChalcopyrite: ((ttKelloM-Green Sericite Alteration:Chlorite Alteration: ttDon Magnetic

101.0-102.5 20', chlorite 1-2* garnets sone carbonate veins.

....................................

No, uartz phenocrysts

sued ct sub-unit 63,64-64,23

1721

e! 1722 - Avg, Width 2cB

1723

54 1724

1725

ated (priuary) 1726

(B)

68,90

70,73

78.96

79,88

81.71

83.23

To (B)

69.21

71.65

79.57

80.18

82,01

83,54

Width(B)

0,31

0,92

0,61

0,30

0.30

0,31

:::::::::;:rr:::;:r:r:;:::r:rr:::::::::rr::rrrrr::::;rr:;:::

Au Ag Cu 2n Pb Sb As Mo (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)

15,000

nil

nil

nil

nil

nil

1727 87.50 88.11 0.61 nil

1728 89.33 89.63 0.30 nil

1729 92,68 92.99 0.31 20.000

H3-1987::13:45


DIAMOND DRILL LOG

NHB 87-01

Page 9

Pron To (B) In)

-Description- Sanple Pros To Width Au Ag Cu 2n Pb Sb As Ko No, d) (g) (B) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)

102,5 104,4 HAFIC DUKE

Dark-GreyFine GrainedMassiveWeakly Fractured (2 Fractures/Metre)1-21 Carbonate Veining randos angles -- Avg, Width 2aBPyrite: tt f racture fillingChalcopyrite: ( (ttCarbonate Alteration: 2-51 ubiquitous phenos,Chlorite Alteration:Non Magnetic

1730 93,90 94,21 0,31 nil

1731 96,04 96,34 0,30 nil

1732 101,22 101,83 0,61 nil


Light-GreyFine GrainedFoliation at 30 Deg, Cai,Weakly Fractured (7 Fractures/Hetre)(tt Quartz Veining - Avg, Width 8cBPyrite: ( tt

1733 106,86 107,32 0,46 nil

1734 123,17 123,48 0,31 nil

1735 124,09 124,70 0,61 nil

8-03-1987::13:45

NORAMCO EXPLORATIONS INC,

DIAMOND DRILL LOG

NHB 87-01

Page 10

Front To ——— -— —— - —— Description ——————————— W ( B)

Chalcopyrite: ((1*Silica Alteration; 20*fellow-Green Sericite Alteration: 2*Carbonate Alteration; {1*Non Magnetic

118.60-128.66 Silicif.zone Bell fracturedTr. fuchsite in silicified zone 127.5124.09-124.70 fault brecciaangular felsic vole. frags. cenented together byquartztcarbonate*sericite*chlorite12cn Bilky qv 125.61-126.07132.06-132.51 Bilky qv jFoliation becomes progressively betterdeveloped doBnhole.

i

151.4 156.3 MASSIVE SULPHIDES

Kellow-BroBnWeakly Fractured (3 Fractures/Metre)Magnetite: 50*Pyrrhotite: 35*Pyrite: 15*Carbonate Alteration: -traceGarnet Alteration: -traceChlorite Alteration: -traceStrongly Magnetic

Saaple No.

1736

1737

1738

-1739

1740

1741

1742

1743

174417451746174717481749175017511752

Fr (

125

127

132

133

142

146

149

151

151151152152153153154155155

OB B)

.61

.44

.01

.23

.07

.04

.09

.09

.40

.83

.13

.74

.35

.96

.57

.18

.79

i

126

127

132

133

142

146

149

151

151152152153153154155155156

ro(B)

.07

.74

.62

.54

.37

.34

.39;

.40

.83

.13

.74

.35

.96

.57

.18

.79

.25

M'

Wl

{

0

0

0

0

0

0

0

0

000000000

dthB)

.46

.30

.61

.31

.30

.30

.30

.31

.43

.30

.61

.61

.61

.61

.61

.61

.46

(

20

5

5

10205220204020515

Au Ag Cu 2n Pb Sb As Mo ppb) (ppb) (ppb) (ppb) (ppb) (ppb) fppb) (ppb!

nil

nil

nil

.000

.000

.000

nil

nil

.000

.000

.000

.000

.000

.000

.000

.000

.000

First 0.4n pyrite rich

8-03-1987::13:46


DIAMOND DRILL LOG

NHB 87-01

Page 11

Froii (B)

To IE)

No distinct banding developed Some graphitic alt.present


Light-GreyFine Grained(tt Quartz Veining randoaPyrrhotite: ttPyrite: 14Kagnetite: (HChlorite Alteration: 1-2*Garnet Alteration: (ttModerately Magnetic

This unit is less altered and not as veil foliatedas the felsic volcanic unit above the tassive sulphides174,70 E.O.H.Rythaic discontinues banding develops near end of unit,This tay represent tuffaceous bedding,Trace fuchsite and potassic alteration,Last 0,3m of unit displays graphitic alteration,

ition ————— - ———— Saaple No,

•hotite+iaagnetite

1753

ivg, Width IBB 1754

1755

1756 1757

Projs

156,25

158,54

161,13

162,65 163,26

To(B)

156,71

159,15

161,59

163,26 164,02

Width(B)

0,46

0,61

0,46

0,61 0,76

Au Ag (ppb) (ppb)

nil

nil

nil

20,000 5,000

Cu Zn Pb Sb (ppb) (ppb) (ppb)

As Mo (ppb) (ppb)

1758 168,60 168,90 0.30 nil

174,7 END OF HOLE.

6-03-1987;:13i46


Sanple Cements

Sample No,

1701

1702

1703

1704

1705

1706

1707

1708

1709

1710

1711

1712

1713

1714

1715

1716

1717

W8

Promla)

14.18

14,79

16,77

20,21

20,88

24,09

25,91

28,35

32,32

33,54

35.00

37,80

41,46

53.81

56,10

57,49

58.69

63,57

Toi*}

14,79

15,40

17,84

20,43

21.34

24,70

26,52

28,96

33,23

33,84

36.13

38.11

41,77

54,12

56,40

57,80

58.99

63,87

Width(n)

0,61

0.61

1,07

0,22

0,46

0,61

0,61

0,61

0,91

0,30

1,13

0,31

0.31

0,31

0.30

0,31

0.30

0,30

"••"•Kcidi Ko

Thin qvs (Hpy tr.cpy

Tr.py/cpy

Thin qvs tr.py/po/cpy

Tr, fuchsite py/po

Thin qvs seric.Tr.py/cpy

l-2taag,l-2tgarn,Chloritized

ttpy Tr.po 2igarn,3cB qv

Thin qvs well silicif.tr, py

Brecc.teit.silicif.Tr.fuchs

Prin.volc, breccia n/thin qvs

PriB.volc.brecc.Thin qv w/po

Thin qv with po/cpy

Brecc.teit.prod.by.chlor.alt,

Tr, fuchsite strongly sericit,

sericitized with biotitespots

50*silic,5tcarb,l-2tpy string,

2ipy fract.fillings&dissei,

ttpy stringers 2cn vide qv

NHB 87-01

Page 13

8-03-1987;:13:47


Sanple Consents

NHB 87-01

Page 14

Sanple No.

1719

1720

1721

1722

1723

1724

1725

1726

1727

1728

1729

1730

1731

1732

1733

1734

1735

t

ProB li!

64.33

64.94

68.90

70.73

78.96

79.88

81.71

83.23

87.50

89.33

92.68

93.90

96.04

101.22

106.86

123.17

124.09

125.61

To In)

64.94

65.55

69.21

71.65

79.57

80.18

82.01

83.54

88.11

89.63

92.99

94.21

96.34

101.83

107.32

123.48

124.70

126.07

Width(B)

0.61

0.61

0.31

0.92

0.61

0.30

0.30

0.31

0.61

0.30

0.31

0.31

0.30

0.61

0.46

0.31

0.61

0.46

....................................................i.......™

2-5*py IStbiotite

15tbiotite Tr.py Sea wide qv

2-5tpy Htpo Tr.cpy

5ci qv Tr.py sericite silicif.

Thin qvs Strong silic.&seric.

l-2*po Thin qv Tr.cpy

Strongly sericitized Tr.py/po

Silicified

Tr. fuchsite Sen qv w/ tr.py

Tr. fuchsite sericitized

Tr.cpy

Tr. fuchsite thin qv silicif.

Broken core silicif.

Eeavily chloritized l-2igarn.

2 qvs tr.py carb. frac. fillings

SOB wide qv broken core ;

Fault breccia

12 ea vide silky qv

8-03-1987:;13:4?


Saiple CoBBents

NHB 87-01

Page 15

Sanple Mo,

173?

1738

1739

1740

1741

1742

1743

1744

1745

1746

1747

1748

1749

1750

1751

1752

1753

t,

From (K)

127.44

132.01

133.23

142.07

146.04

149.09

151.09

151.40

151.83

152.13

152.74

153.35

153.96

154.57

155.18

155.79

156.25

158.54

To (ID)

127.74

132.62

133.54

142.37

146.34

149.39

151.40

151.83

152.13

152.74

153.35

153.96

154.57

155.18

155.79

156.25

156.71

159.15

Width(B)

0.30

0,61

0.31

0.30

0,30

0.30

0.31

0.43

0.30

0.61

0.61

0.61

0.61

0.61

0.61

0.46

0.46

0.61

r:izrzrrr;zrrmr:rr:rrr;c:;rir:rrr::

Tr. fuchsite in silicif.zone

45ca qv with tr, black lineral

Hipy strongly silicified

IflcB qv broken core

Thin fuchsite seas sericitized

Sen qv K.alt.llpy.tr.cpy.shrd

Graph. alt, Itpy

60lpy 3fllpo lOtoag

?0',po 20lpy lOtaag

80*po lOtoag lOtpy

85*po lOtnag Stpy

SOUag 15tpo tr.py 5tgarn*chlr

45^po 45'.nag Ifliunk, alt. tr.py

55tpo 25^nag 20khl*garntcarb

50hag 30lpo ISigarn S^py+chlr

55*nag 20tpy 2fl*po Sigarnets

5*.po Stgarnets contact zone

Slpy stringers 20khlor. barnett

Q8-03-1987::13:47

Sample Proa To WidthMo. (B) (B) (B)

1755 161,13 161,59 0,46

1756 162,65 163,26 0,61

1757 163,26 164,02 0,76

1758 168,60 168,90 0,30


Sample Cements

NHB 87-01

Page 16

Reiarks

2tpo stringers tr.py

2-5*po ttpy Thin qvs

2-5tpo 2-5*garn,l*py

2-5tpy garn,graph,

AZIMUTH: 090 degrees NHB 87-01ifij rio" t——ST

20

40

60

80

100

120

140

OVERBURDEN

FELSIC VOLCANIC INTERMEDIATE VOLCANIC

FELSIC VOLCANIC

MAFIC DYKE FELSIC VOLCANIC

MAFIC DYKE FELSIC VOLCANIC

DIORITE KITH QUARTZ AND FELDSPAR PHENOCRYSTS FELSIC VOLCANIC

MAFIC DYKE

•FELSIC VOLCANIC

•MASSIVE SULPHIDES

•FELSIC VOLCANIC

END OF HOLE: 174.7 wter*.

-. 160

. 180

.. 200

.. 220

-. 240

NORAMCO EXPLORATION

Hoy!63 Bay #1446 D i amond Dr i 11 Sect i on

NO! NHB 87-01 ]Log by: E.FloodLocation: L6M , 0+25N Date*. Jan. 18/1987Azliuth: 090 degreesDip! -45 degreesDate Drawn: 08-09-1987GEOCOM CORELOG 100

Depth! 174.70 MetersCI alK: KRL 865461Scale: 1 : 1000

P


PR\U HOLE LOCATION

13.0 t-

Sc.le'. 1-5000

8-03-1987:;13:48


DIAMOND DRILL LOG

NHB 87-02

Property,

Partner:

Azimuth:

Logged By:

Date Started:

Core Size:

Drill Coapany:

Hoyles Bay 11446

130 degrees

E, Flood

Jan.23/198?

BQ

H4B Drilling

NTS: 52N/4

Cliii f: 865495

Dip: -49 degrees

Casing: Out

Date Completed: Jan.30 198?


Overburden: 8.23 letres

Township: Bateaan

Coordinates: L8E , 2*75H

Length: 224.39 netres

Elevation: Surface

Date Logged: Jan.24-Feb.l 198?

Saiples Shipped: Feb.2 198?

Acid Dip Teats

j 1. 60.98 B -49 deg. l 3. 182.93 D -34 deg.

l 2. 121.95 B -39 deg. f 4. 224.39 B -32 deg.

PurposeTo intersect an E.H.anomaly and tvo aagnetic highs.

Conclusions

Recommendations

The Bassive sulphides intersected between 71.59-91.97 and 174.1-211.0 vere responsible for the E.H.anonaly and the tvo aagnetic highs.

Structural breaks in the Bassive sulphide stratigraphy ae outlined by the ground sag.survey should be drill tested

8-03-1987;:13:48


DIAMOND DRILL LOG -- SUMMARY

NHB 67-02

Page 2

Frond!) TO(B) ————————-—Description-

0,0 8,2 OVERBURDEN

8,2 14,9 FERRUGINOUS CHERT

14,9 19,2 MAFIC VOLCANIC

19,2 19,5 MYLONITE



34,5 64,7 ULTRAMAFIC INTRUSION

-Mineralizationfsl-

Pyrrhotite ( 5-101) Pyrite ( 2-5*1 Magnetite { 2-51} Chalcopyrite

Pyrrhotite l It) Pyrite KUt) Magnetite {((11) Chalcopyrite {((li)

Magnetite ( 5t banded) Pyrite ((l stringers)

Magnetite (21) Pyrite Ut) Pyrrhotite (It) Chalcopyrite {((It)

Magnetite ((It) Pyrrhotite (((It) Pyrite (((It) Chalcopyrite (((It)

Magnetite (5t) Pyrite (((It) Pyrrhotite (((It) Chalcopyrite (((It)

•Alteration(s)-

Chlorite ( 10-15t) Yellow-Green Sericite { It)

Carbonate f 2-5t disseii.4)

Chlorite l St)

Chlorite (St)

Biotite (2t) Silica (2t) Epidote (It)

Carbonate ((It on fract,

B-03-198?::13:49


DIAMOND DRILL LOG -- SOMME!

NHB 87-02

Page 3

Froi(n) Tola)


•Description-

66, l 92,0 IRON FORMATION


71,6 80,0 MASSIVE SULPHIDES

80,0 92,0 FERRUGINOUS CHERT KITH MASSIVE SULPHIDES

92,0 151,0 INTERMEDIATE TO FELSIC VOLCANICLASTIC



•Hineralization(s)-

Hagnetite i 2\ thin convol) Pyrite ( (l\ on fractur) Pyrrhotite (Ut thin strin)

Pyrrhotite (2-51 stringers) Magnetite (2-51 bands) Pyrite (li stringers)

Pyrite (75*1 Pyrrhotite (W) Magnetite (St)

Pyrite (Ul) Pyrrhotite (M) Chalcopyrite (HW Magnetite (((U)

Pyrite 111 dissea.) Chalcopyrite ((H in qvs) Pyrrhotite (Ut dissen.)

Pyrite UM)

•Alteration(s)-

Chlorite ( 2-54) Garnet (2*) Carbonate O

Chlorite (W

Carbonate O

Biotite Ufll) Chlorite (54) Garnet (It) Carbonate O

Carbonate O Chlorite O

Chlorite OSilica OYellow-Green Sericite O

08-03-1987::13:50



NHB 87-02

Page 4

Pronto) Tola) --—————.—.-Description——————————————————Mineralizationfsl————————Alteration(s)—————————

170,3 174,1 MAFIC TOFF

174,1 178,0 CHERT KITH MASSIVE SDLPHIDES

178,0 207,8 MASSIVE SDLPHIDES HITHIN CHERT


211,0 212,8 MAFIC DYKE

212,8 215.2 FERRUGINOUS CHERT

215,2 224,4 INTERMEDIATE TUFF

Pyrite (W) Pyrrhotite KU) Magnetite KW)

Pyrrhotite 115*) Pyrite (10t) Magnetite (2-5*)

Pyrite (65i) Pyrrhotite UO-151) Magnetite UOt) Chalcopyrite K(tt)

Magnetite UOt) Pyrrhotite Pyrite (H)

Pyrrhotite (U) Pyrite (W Magnetite i H)

Pyrite Kit on fract.) Magnetite {(H thin seasosl

Garnet (U) Carbonate U

Biotite O

Garnet (2'.) Chlorite (W

Silica (2', in two zone)Garnet (WKelJow-Green Sericite (24 on foliatio)

H3-198?::13;50


DIAMOND DRILL LOG - SOKKARK

NHB 87-02

Page 5

FroB(io) Tola) •Description- Mineralizationis) -Alteration(s)"

224.4 END OF HOLE,

8-03-1987::13:50


DIAMOND DRILL LOG

NHB 87-02

Page 6

FroB To(n) (i)

0,0 8.2

8,2 14,9

srrrrrssssrssssssrrrrsrirrssrsrssrrrsBsssBSSSSSsssrsrsssssrs

OVERBURDEN

FERRUGINOUS CHERT

Dark-GreyFine GrainedLower Contact at 32 Deg, Cai.Weakly Fractured (4 Fractures/Metre)n Carbonate Veining at 55 Deg. Cai. -- Avg, Width 2naPyrrhotite: 5-10*Pyrite: 2-54Magnetite: 2-5*Chalcopyrite: UllChlorite Alteration: 10-15*Uel Ion-Green Sericite Alteration: H

SaipleNo,

17591760176117621763176417651766176717681769

::;t::::

From(B)

8,238,849,45

10,0610,6711,2811,8912.5013,1113,7214,33

To(B)

8.849,4510,0610,6711,2811,8912,5013,1113,7214,3314,94

Widthd)

0,610,610,610,610,610,610,610,610,610,610,61

Au Ag(ppb) (ppb)

15,000oil5,000nil5,0005,000dinilnilnilnil

Cu Zn Pb Sb As Ho(ppb) (ppb) (ppb) (ppb) (ppb) (ppb)

Hoderately Magnetic

10,83-11.08 95*Bag,5*po,Tr.cpy, 11,13-11.38 60lpy Mpo 15toag ISkhlor,


Dark-GreenPine GrainedLover Contact at 38 Deg, Cai,Weakly Fractured (4 Fractures/Metre)2\ Carbonate Veining randoa -- Avg. Width 2amPyrrhotite: ItPyrite: (UtMagnetite: (mChalcopyrite: ((HCarbonate Alteration: 2-5* dissea.&in phenos,Weakly Magnetic

1770177117721773177417751776

14,9415,5516,1616,7717,3817,9918,60

15,5516,1616,7717,3817,9918,6019,21

0,610,610,610,610,610,610,61

nilnilnilnilnilnilnil

Iron stained fracture surfaces

8-03-1987:113:51


DIAH08D DRILL LOG

NHB 87-02

Page 7

Proa d)

To (B)

-Description

Unit begins to develop a foliation over the last 15ca

19,2 19,5 HKLOMITE

Banded Black to WhitePine GrainedFoliation at 40 Deg, Cai,Lower Contact at 25 Deg, Cai,Weakly Fractured (9 Practures/Hetre)30* Carbonate Veining at 40 Deg, Cai. - Avg, Width IpMagnetite: 5t bandedPyrite: (l stringersChlorite Alteration: 51Moderately Magnetic

Thin discontinous banding; aagnetic black band/carbonate/chlorite Mylonitic teiture Hylonitized aafic volcanic?

Saiple Proa To Width Au Ag Cu Zn Pb Sb As Ho So, (B) (B) (B) !ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)

1777 19,21 19,51 0,30 nil


Light-Grey to Dark-GreyFine GrainedLower Contact at 45 Deg. Cai,Weakly Fractured (7 Practures/Metre)5* Carbonate Veining randoB -- Avg, Width lOcaMagnetite: 21Pyrite: ItPyrrhotite: UChalcopyrite: ( (\\Chlorite Alteration: 5i ^Moderately Magnetic

1778177917801781178217831784

19,5120,1220,7321,3421.9522,5623,11

20,1220,7321,34 -21,9522,5623,1123,78

0,610,610,610,610,610,550,67

nilniloilnilnilnilnil

NORAMCO EXPLORATIONS INC. NHB 87-02

08-03-1987::13:51 DIAMOND DRILL LOG Page 8

Proa To ———————————Description——————————— Saaple Froa To Width Au Ag Cu Zn Pb Sb As Mo (B) i t) No, (B) (B) (B) (ppb) (ppb) (ppb) ippb) (ppb) (ppb) ippbl (ppb)

Weak pervasive carbonate alteration

23,1 34,5 HAFIC VOLCANIC

Dark-Green 1785 23,78 24,39 0,61 5,000Fine GrainedWeakly Fractured (5 Fractures/Metre) 1786 27,44 28,05 0,61 5,00051 Carbonate Veining random -- Avg, Width 2mMagnetite; m 1787 29,73 30.34 0,61 nilPyrrhotite: (WPyrite: (M 1788 31,40 31,71 0,31 nilChalcopyrite: ((UBiotite Alteration: 2 1 1789 32,62 33,23 0,61 nilSilica Alteration: 2iEpidote Alteration: It 1790 34,15 34,45 0,30 nilWeakly Magnetic

Core is pervasively carbonated except where irregularyelloK silicification occursWide carbonate veins often contain K-spar and biotite23,62-24,24 Brecciated texture29.16-29,32 Mafic Dyke30,79-34,15 2-5tepidote34.15-34,45 101 lagnetite in convoluted Beans

34,5 64,7 ULTRAMAFIC INTRUSION

Dark-Grey 1791 34,45 34,96 0,51 nilFine to Medium Grained 1792 34,96 35,87 0,91 nilWeakly Fractured (4 Fractures/Metre)2* Carbonate Veining random -- Avg, Width 2m 1 793 54,27 54,88 0,61 nilMagnetite: 54Pyrite: Wl 1794 55,79 56,40 0,61 nil

8-03-198?::13:52


DIAMOND DRILL LOG

NHB 87-02

Page 9

FroB In)

To IB)

-Description

Pyrrhotite: (WChalcopyrite:Carbonate Alteration: (It on fract. surfacesModerately Magnetic

Core is very soft,greasy.talcose,"soapstone"34.45-34.98 contact zone much gore felsic than rest of unitslightly harder,possibly silicified.very iagnetic,55

deg.fol.54,38 Trace oolybdenuD in qv 55,79-58,84 eany thin qvs.Tr.cpy.Very chloritized, Sheared texture displayed on fracture surfaces, Lower contact is not well defined

:r:::r::::r::;:::::::;;::::rrs::;:

....................... gjnp].

No, 1795 1796

, surfaces 1797 1798

e Frdi d)

56,40 57,01 57,62 58,23

:r:r:z:r:

To d)

57,01 57,62 58,23 58,84

:::::r:r

Width(B) 0,61 0,61 0,61 0,61

nw ny

(ppb) (ppb) nil nil nil nil

Cu (ppb)

Zn Pb(ppb) (ppb)

Sb(ppb)

AAno(ppb)

Ko (ppb)


Dark-GreyFine GrainedFoliation at 60 Deg. Cax,Weakly Fractured (3 Fractures/Metre)Magnetite: 2* thin convol.seamsPyrite: (U on fracture surfacesPyrrhotite: ( l\ thin stringersModerately Magnetic

pervasively carbonated

66.1 92.0 IRON FORMATION

-Sub Units-


08-03-1987::13:52 DIAMOND DRILL LOG Page 10

Proa To ———————--Description--—-——————— Saiple Froi To Hidth Au Rg Cu Zn Pb Sb As Mo(B) (m) No. in) (B) (i) (ppb) (ppb) (ppb) (ppb) (ppbl (ppb) (ppb) (ppb)


Banded GreyFine GrainedHeakly Fractured !4 Fractures/Metre)(U Carbonate Veining at 50 Deg, Cai, -- Avg, Width InnPyrrhotite: 2-51 stringersHagnetite: 2-5t bandsPyrite: H stringersChlorite Alteration: 2-5*Garnet Alteration: 2*.Carbonate Alteration:Koderately Magnetic

Magnetitetpyrrhotite+chlorite+garnet bands Neak perv.carb.assoc,with chlorite^garnets Sone sections of relatively massive chert

71,6 60.0 MASSIVE SULPHIDES

Banded KellowHediuB to Coarse Grained(\\ Carbonate Veining - Avg. Width 2niDPyrite: ?5tPyrrhotite: MMagnetite: 5iChlorite Alteration: HStrongly Magnetic

Uchert

80,0 92,0 FERRUGIMOIIS CHERT HITH MASSIVE SULPHIDES

Dark-Grey


08-03-1987::13:53 DIAMOND DRILL LOG

FroB To - ————————— Description —————————— (B) M

Medium to Coarse Grained Weakly Fractured (2 Fractures/Metre) 14 Carbonate Veining -- Avg, Midth IBB Carbonate Alteration: Strongly Magnetic

Section 79.98-84.15 204py,204po,i04Bag,soBe banding Section 84,15-91,9? 254mag,lfl4po,24py.tr,cpy, Hell banded -displays sone soft sediient deformation, Convoluted banding

92.0 151,0 INTERMEDIATE TO FELSIC VOLCANICLASTIC

Light-GreyFine GrainedFoliation at 60 Deg, Cai,14 Quartz-Carbonate Veining at 45 Deg, Cai, -- Avg, Width

3CBPyrite: 04Pyrrhotite: (14Chalcopyrite: ( (ttMagnetite: ( d\Biotite Alteration: 104Chlorite Alteration: 54Garnet Alteration: 14Carbonate Alteration:Weakly Magnetic

91,97-94,82 14py,14po, strongly chlor.pervasively carb,94,82-103,29 relatively sassive flow103.29-108.54 rel.fine fragaentsdn scale)

Saiple No,

1851185218531854

1855

1856

1857

18581859

1860

1861

Proi (B)

95969899

103

104

109

115116

118

126

.70

.30

.50

.40

.00

.30

.30

.9.0

.30

.60

.20

969899

100

103

104

109

116117

119

126

To (B)

.30

.50.

.40

.80

.70

.90

.60

.30.10

.50

,8D

NHB 87-02

Page 11

Width Au Ag Cu 2n Pb Sb As Mo (B) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)

0201

.60

.20

.90

.40

0,70

0

0

00

0

0

.60

.30

.40

.80

.90

.60

nilnilnilnil

nil

nil

nil

nilnil

15,000

nil108.54-117.68 coarse fragmental(CD scale)

8-03-1987:113:53


DIAMOND DRILL LOG

NHB 87-02

Page 12

Proa (B)

To d)

-Description-

117,68-127,44 rel.fine fragaents 127.44-134.15 coarse fragments 134,15-151.04 fine to coarse fragnents Trace fuchsite in different locations

Saiple frog To Width Au Ag Cu Zn Pb Sb As HoHo, (B) li) (B) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)

1862 137.20 138,10 0,90 nil1863 138,10 139,00 0,90 nil

18641865

145,10 146,00146,00 147,00

0,90 nil 1,00 20,000

151,0 163,7 HAPIC VOLCANIC

Dark-GreyPine GrainedFoliation at 70 Deg, Can.Weakly Fractured (2 Practures/Metre)2i Quartz-Carbonate Veining randoi -- Avg, Width SBBPyrite; H disseo.Chalcopyrite: (tt in qvsPyrrhotite: (tt dissee.Carbonate Alteration:Chlorite Alteration:

Trace specular hematite? in qv at 160,11 Unit is tuffaceous in sections


GreyPine GrainedFoliation at 75 Deg, Cai,Weakly Fractured 13 Fractures/Metre)(li Quartz-Carbonate Veining at 30 Deg, Cai, - Avg, Width

leu Pyrite: ((tt

186618671868

1869

1870

156,70 157,60157,60 158,50158,50 159,10

159,60 160,20

160,40 161,00

1871 166,20 166.S

0.90 5,0000,90 80,0000,60 65,000

0,60 60,000

0,60 45,000

0,60 nil

4958495949604961

166,77167,40168,00168,60

167,40168,00168,60169,20

0,630,600,600,60

nilnilnilnil

B-G3-1987::13:54


DIAMOND DRILL LOG

NHB 87-02

Page 13

Froi (B)

To (B)

-Description-

Chlorite Alteration: Silica Alteration: Kellov-Green Sericite Alteration: Don Magnetic

Coarsening upvards sequence of fine U2n) to coarse()2cn) uphole i

Saiple Frog ToMo, d) d)

4962 169,20 169.804963 169,80 170,30

Width Au Ag Cu Zn Pb Sb As Ho(B) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) Ippb) (ppb)0,60 nil0,50 nil

170,3 174,1 MAFIC TDFP

Brown-GreyFine GrainedFoliation at 75 Deg, Cai,Heakly Fractured (4 Fractures/Metrell* Quartz Veining -- Avg, Width hunPyrite: UtPyrrhotite: UtMagnetite: (UtGarnet Alteration: ItCarbonate Alteration:Heakly Magnetic

Upper contact is irregularQuartz veins are blueSulphides assoc.vith thin cherty interbandsCarbonated fracture surfacesTrace fuchsiteLover contact not veil defined

496449654966496718724968

170,30 170,70170,70 171,30171,30 172,00172,00 172,60172,60 17.3,50173,50 174,10

0,40 5,0000,60 20,0000,70 5,0000,60 10,0090,90 303,0000,60 200,000

174,1 178,0 CHERT WITH MASSIVE SOLPBIDES

light-Grey Fine Grained

18731874

174,10 175,00175,00 175,90

0.90 306,000 0,90 nil

8-03-1987;:13:54


DIAMOND DRILL LOG

NHB 87-02

Page 14

Froa (B)

To In)

Pyrrhotite: 15*. Pyrite; 104 Magnetite: 2-54 Biotite Alteration: Moderately Magnetic

-Description- Saaple Proa To WidthNo, (B) (B) (B)

1875 175,90 176,50 0,601876 176,50 177,10 0,601877 177,10 178,00 0,90

Au Ag Cu Zn Pb Sb As Mo (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) nil nil nil

178,0 207,8 HASSIVE SULPHIDES MITHIN CHERT

KellovHediua Grained Pyrite: M Pyrrhotite; 10-151 Magnetite: 10', Chalcopyrite: (Ul Strongly Magnetic

10-154 chert

18781879188018811882188318841885

188618871888

1889189018911892189318941895189618971898

178,00178,70179,30179,90180,50181,10181,70182,30

182,90183,50184,10

184,90185,40186,00186,60187,20187,80188,40189,00189,60190,20

178,70179,30179,90180,50181,10181,70182,30182,90

183,50184,10184,80

185,40186,00186,60187,20

, 187.80•188,40189,00189,60190,20190,90

0,700,600,600,600,600,600,600,60

0,600,600,70

0,500,600,600,600,600,600,600,600,600,70

nilnilnil

10,00010,00010,000

nilnil

nilnil

10,000

nilnilnil

45,000nilnilnilnilnil

10,000

8-03-1987i:13;55


DIAMOND DRILL LOG

NHB 87-02

Page 15

:r;r:::::;;;:::::::::::::::::::;r:;r:;::rr;;:;::::r:;;rr:r::::::::r:::r::::r:::::::::::

From To —————————— Description —————————— Saipleis, i (ID) No,

189919001901190219031904190S1906190719061909191019111912191319141915191619171918191919201921192219231924 .19251926

207,8 211,0 FERRDGINODS CHERT

Dark-Grey 1927Fine Grained 1928

:r;;rr:r:

Froid)

190,90191,50192,10192,70193,30193,90194,50195,10195,70196,30197,00197,60198,20198,80199,40200,00200,60201,20201,80202,40203,00203,70204,30204,90205,50206,10206,70207,30

207,90208,50

Tod)

191,50192,10192,70193,30193,90194,50195,10195,70196.30197,00197,60198,20198,80199,40200,00200,60201,20201,80202,40203,00203,70204,30204.90205,50206,10206,70207,30207,90

208.50209.10

;::::a::

Width(B)0,600,600.600,600,600,600,600,600,600,700,600,600,600,600,600,600,600,600,600,600,700,600,600,600,600,600,600,60

0,600,60

Au Ag Cu Zn Pb Sb As Ho(ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)nilnilnilnilnilnilnilnilnilnilnil

10,000nilnilnilnilnilnilnilnilnil

35.000nilnil

10,00020,00010,000nil

nilnil

H3-198?:;13:56


DIAMOND DRILL LOG

NHB 87-02

Page 16

From (a)

To IB)

-Description-

Lower Contact at 50 Deg, Cai, Weakly Fractured 12 Fractures/Metre l Kagnetite: 10* Pyrrhotite: 5* Pyrite: l* Moderately Magnetic

Saeple Proi ToNo, (B) (D)

1929 209,10 209,801930 209,60 210,401931 210,40 211,00

Width Au Ag Cu Zn Pb Sb As KoIn) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)0,70 nil0,60 nil0,60 nil

211,0 212,8 MAFIC DYKE

Dark-GreyFine GrainedLower Contact at 75 Deg. Cax.Weakly Fractured (2 Fractures/Metre)((tt Carbonate Veining randon -- Avg, Width linWeakly Magnetic

1932 212,70 213,40 0,70 nil

carbonate phenocrysts


Dark-GreyFine GrainedWeakly Fractured (4 Fractures/Metre)Pyrrhotite: ttPyrite: ttMagnetite: ttGarnet Alteration: 2',Chlorite Alteration: ttHeakly Magnetic

193319341935

213,40214,00214,60

214.00214,60215.20

0,600,600,60

nil nil nil

215,2 224,4 INTERMEDIATE TDFF

Dark-Grey


08-03-1987::13:56 DIAMOND DULL LOG

From To — — — — — — -—Description ——— - — - —— ™ Sanple Prom d) (ml No, (B)

Fine Grained 1936 216,20

*

To(B)

217,10

Width(B) 0,90

Au tppb) nil

Ag !ppb)

NHB 87-

Page

(ppb) (ppb)

02

17

Pb(ppb)

nl iSt) AS(ppb) (ppbl (|

Ho

Foliation at 70 Deg, Cax,Weakly Fractured (4 Fractures/Metre)Pyrites (It on fract.surfacesKagnetite; (tt thin seansSilica Alteration; 2i in two zonesGarnet Alteration: l \Kellow-Green Sericite Alteration: 21 on foliation planesModerately Magnetic

Rough sorting of tuffaceous naterial frog fine to coarseuphole

224.4 E.O.K.

224,4 END OF HOLE,

08-03-1987:il3:57

Sample No,

1759

1760

1761

1762

1763

1764

1765

1766

1767

1768

1769

1770

1776

1777

1778

1779

1780

Hi

FroB IB!

8,23

8.84

9,45

10,06

10,67

11,28

11,89

12.50

13.11

13.72

14.33

14.94

18.60

19,21

19.51

20.12

20.73

21.34

To (B)

8,84

9.45

10,06

10,67

11.28

11.89

12.50

13.11

13.72

14.33

14.94

15.55

19.21

19,51

20,12

20,73

21,34

21,95

Width (B)

0,61

0,61

0.61

0.61

0.61

0.61

0.61

0.61

0,61

0,61

0.61

0.61

0.61

0.30

0,61

0.61

0,61

0.61


Sample Cements Page 19

* --Jt-- . - — .pAma y If OB H ••• — w**oAcKd ift B

2ipy, Hnag.Hpo,

5*py, tpo,

5tpo.(ltpy,Tr,cpy,llsericite

5*po,Upy,(ttcpy.5tchlor*ser,

25taag,5tpy,Tr,cpy,

2-54py*po Tr, garnets

Banded lag. seals l-2cn vide

carb, chlor. nag, alteration

2-5*py

2*py.*po.

Banded tag.Beans l-2ci vide

2cB vide carb. vein

Hell foliated last 15cn

Kylonitic zone.2ci qc vein

Upo

Hpo.Hiag.Hpy.(Ucpy

chlor, alt, prod, brecc.teit,

Upy, carbonate vein

8-03-1987::13:57


Sanple Contents

NHB 87-02

Page 20

Sanple No,

1782

1783

1784

1785

1786

1787

1788

1789

1790

1791

1792

1793

1794

1795

1796

1797

1798

Hi

Froa (K)

21.95

22.56

23.11

23,78

27.44

29.73

31.40

32.62

34.15

34.45

34.96

54.27

55.79

56.40

57.01

57.62

58,23

95.70

To (B)

22.56

23,11

23,78

24,39

28,05

30,34

31.71

33,23

34.45

34.96

35,87

54.88

56.40

57,01

57,62

58,23

58,84

96.30

Width(B)

0,61

0.55

0,67

0.61

0,61

0,61

0,31

0.61

0,30

0,51

0,91

0,61

0,61

0,61

0,61

0.61

0.61

0,60

Thin tag. and po.seais

10cB vide qv

8-03-1987:;13:57


Sanple Couients

NHB 87-02

Page 21

Sample No.

1852

1853

1854

1855

1856

1857

1858

1859

1860

1861

1862

1863

1864

1865

1866

1867

1868

m9

FroD(B)

96.30

98,50

99.40

103,00

104,30

109.30

115.90

116.30

118.60

126.20

137.20

138.10

145.10

146,00

156,70

157,60

158.50

159,60

ToID)

98,50

99,40

100,80

103,70

104.90

109.60

116.30

117.10

119,50

126.80

138.10

139,00

146,00

147,00

157,60

158.50

159.10

160.20

Width(D)

2,20

0.90

1.40

0,70

0.60

0.30

0.40

0.80

0.90

0.60

0,90

0,90

0.90

1.00

0.90

0.90

0,60

0,60

* m m . m . . v . . D ft WL 3 V If Q * . m * i. m m m m mtVClidi ho

lOci qv w?bio,tpy,Tr,po

Upy.Tr, fuchsite

3 ci qv, Tr, fuchsite

2*py.5-lfl*biotite perv.carb,

Itpy,

7 CD qv Kith py,2tgarnets

llpy.Tr,po.2-4cii qc veins

Trace fuchsite

Chalco-qtz vein Tr, fuchsite

Thin fracture w/talc.py.fuch.

silicif, zone Thin fuch.seans

ttpy, Thin qvs Fuchsite

Hpy, cpy+po frac, fillings

Sim cpy vein lipy dissei,

cpy in qv

py stringers pytgiatic qvs

cpy in thin pytgsatic qvs

py, fracture fillings

-03-1987;:13:57


Sanple Contents

NHB 87-02

Page 22

Sanple No,

1870

1871

4958

4959

4960

4961

4962

4963

4964

4965

4966

4967

1872

4968

1873

1874

1875

^76

nFro(B

160,

166.

166.

167,

168,

168,

169,

169,

170.

170,

171,

172,

172.

173.

174,

175.

175,

176.

'B l

40

20

77

40

00

60

20

80

30

70

30

00

60

50

10

00

.90

50

To (B)

161.

166.

167.

168,

168,

169.

169.

170.

170.

171.

172.

172.

173.

174.

175.

175.

176.

177.

00

80

40

00

60

20

80

30

70

30

00

60

50

10

00

90

50

10

Ui AHid(B

0.

0,

0,

0,

0,

0,

0,

0,

0,

0,

0.

0.

0.

0,

0,

0.

0,

0,

th)60

60

63

60

60

60

60

50

40

60

70

60

90

60

90

90

60

60

l-2*py. IflcB qv with py,

silicified chlor.seric.

Thin qvs Trace cpy/py,

Thin qvs Trace pyrrhotite

2-lcB qvs Trace pyrrhotit

Trace fuchsite

Trace fuchsite 1 qv

Trace fuchsite

Several thin bluish qvs

Several thin bluish qvs

Thin bluish qvs Tr, cpy/py

4 thin bluish qvs 2i garni

Fuch.qtz banding Itpytpo

Bluish qvs v/py+po.Fe.cari

Slpytpo

lOtpo, Itpy,

15tpo, Ifltoag,

20lpo 5tpy

.......... — .. — . ...... — — — ....... — ... —— ............................ — --....-..-...........

e

i

etB

b?

08-03-1987::13i58


Saiple CoKuente

NHB 87-02

Page 23

Sample No.

1877

1889

1894

1919

1923

1927

1928

1929

1930

1931

1932

FroB (B)

177.

184.

187.

203.

205.

207.

208.

209.

209.

210.

212.

10

90

80

00

50

90

50

10

60

40

70

To (B)

178.

185.

188.

203.

206.

208.

209.

209.

210,

211.

213.

Width (B)

00

40

40

70

10

50

10

80

40

00

40

0.

0.

0.

0.

0.

0.

0.

0.

0,

0.

0.

90

50

60

70

60

60

60

70

60

60

70

..............................

20*py lOipo

crude banding

90* chert 10* py.

Includes lOcu nafic dyke

crude aagnetite-py, banding

crudely banded Bag.+poOOt)

208.92-209.10 nassive sag

85Uiag, 15tpo. Tr.py

SQlmag. 30lpy,

po seass chlor.alt.

magnetite bands

*

AZIMUTH: 130 degrees NHB 87-02"lo 5f1

20

40

- BO

. BO

. 120

140

.. 160

180

- 200

• - 220

-. 240

1

FERRUGINOUS CHERT

MASSIVE SULPHIDES

FERRUGINOUS CHERT KITH MASSIVE SULPHIDES

OVERBURDEN

FERRUGINOUS CHERT MAFIC VOLCANIC MYLONITEFERRUGINOUS CHERT

MAFIC VOLCANIC ULTRAMAFIC INTRUSION

MAFIC VOLCANIC

IRON FORMATION

INTERMEDIATE TO FELSIC VOLCANICLASTIC

•MAFIC VOLCANIC•INTERMEDIATE TO FELSIC VOLCANICLASTIC

•MAFIC TUFF-CHERT KITH MASSIVE SULPHIDES

•MASSIVE SULPHIDES NITHIN CHERT

•FERRUGINOUS CHERT-MAFIC DYKE

'FERRUGINOUS CHERT 'INTERMEDIATE TUFF

END OF HOLE: 224.4 meters.

NORAMCO EXPLORATION

Hoy!es Bay #1446 D i amond Dr i 11 Sect i on

NO; NHB 67-02 | Log by: E.FIoodLocation! L8E , 2+75N | Datei Jan.30 1987Azliuthi 130 degreesDip! -49 degreesDate Drawn: 08-09-1987GEOCOM CORELOG 100

CIaIn: 8B5495Scale: 1 : 1000

ft̂3

zoo o-i

Oo

c

in

C*

-*--r

X

2.

of

O•zor00

Jtt

8-04-198?::l?:49


DIAMOND DRILL LOG

NHB 87-03

Property: Hoyles Bay 11446

Partner:

Azinuth: 130 degrees

Logged By: Eugene Flood

Date Started: Feb.l 198?

Core Size: BQ

Drill Company: KiB Drilling

NTS: 52H/4

dais}: 865496

Dip: -49 degrees

Casing: Out

Date Completed: Peb,3 198?


Overburden: 14,99 tetres

Township: Bateaan

Coordinates: HOE , 3+45N

Length: 15?,58 netres

Elevation: Surface

Date Logged: Peb,2-5 198?

Samples Shipped: Feb.6 198?

kid Dip Tests

f 1. 14.99 o -55 deg. j 3. 117.6 B -49 deg,

l 2, , 58,8 i -49 deg. l 4. 157,58 l -45 deg,

Purpose

Conclusions

Reconnendations

To test a "massive sulphide" I.P.response,

The massive sulphide unit from 70.1 - 80.0 is considered to be responsible for the I.P.anoiialy,

Follov up drill locations are dependant on assay results

-04-1987::17:49


DIAMOND DRILL LOG -- SUMMARV

NHB 87-03

Page 2

Fronts) Tola) — ————

0,0 15,0 OVERBURDEN


-Description———————-———-———.—-—Mineralization(s)-


70,1 80,0 KASSIVE SULPHIDES HITHI8 CHERT


81,9 86,8 MAFIC TO INTERMEDIATE FLOH

86,8 87,5 MASSIVE MAGNETITE

87,5 89,2 MASSIVE PYRITE

Magnetite (5t) Pyrite (1-2*1 Chalcopyrite UUt)

Magnetite Pyrite W) Chalcopyrite UM)

Magnetite Pyrite M)

Magnetite HOU Pyrite 15*)

Magnetite (95*) Pyrite (5*) Chalcopyrite ((Ut)

Pyrite (95V) Magnetite Ut) Chalcopyrite KUt)

•Alteration(s)-

Silica (25*,) Chlorite (10*1 Carbonate 15*1 Biotite (24) Epidote l (l*.)

Chlorite (10-154) Carbonate O

Chlorite (W Garnet Km)

Carbonate O Silica O Chlorite O

Epidote U(U)

-04-1987::17:49



NHB 87-03

Page 3

To (B) •Description————————-—---—-——-———JlineralizationU)—————--——Alteration(s)-

89,2 92,1 MASSIVE MAGNETITE WITH PYRITE IN CHERT

92,1 135.7 INTERMEDIATE TO FELSIC VOLCANIC

135,7 157,6 INTERMEDIATE TO FELSIC VOLCANOCLASTIC

Magnetite Pyrite (5-10*1

Pyrite (54) Magnetite (51) Chalcopyrite UW)

Pyrite HW Magnetite

Silica (5*,) Chlorite (W Epidote {(li)

Chlorite (51) Biotite (21)

Biotite (10*,) Chlorite (It) Garnet Kit)

157,6 END OF HOLE,

8-04-1987;:17:49


DIAMOND DRILL LOG

NHB 87-03

Page 4

FroB To

0.0 15.0 OVERBURDEN

15.0 64.8 HAFIC VOLCANIC

-Description-

Dark-Grey to Dark-GreenFine GrainedFoliation at 45 Deg. Cai.Weakly Fractured (3 Fractures/Ketrel{H Carbonate Veining random -- Avg. Width IDDRagnetite: 54Pyrite: 1-21Chalcopyrite: ( (ttSilica Alteration; 25*Chlorite Alteration: 104Carbonate Alteration: 54Biotite Alteration: 24Epidote Alteration: (14Moderately Magnetic

Several silicification zonesjlS,55-16,46 27.44-33.2335.98-37.5 52.8-62.515.55-18.60 5-104 py18.60-19.51 High cone, of epidote and brown carbonate.Several sections with a vuggy texture;44.97-46.95 47.87-48.48 62.80-63.26

SanpleNo,

19371938193919401941194219431944

194519461947194819491950

195119521953

195419551956

From(D)

14,9915,8816,4617,0517.7918.5219,4020.29

24,7025,5826,4627,3428,2229,11

29,9930,5831.46

34,1037,0437,93

To(n)

15,8816.4617,0517,7918.5219,4020,2921.17

25,5826.4627,3428,2229,1129,99

30,5831.4632,05

34,9937,9338,95

Width(D)

0,690,580,590,740,730,880,890.88

0.880,880,880,880,890,88

0,590,880,59

0,890,891,02

Au(ppb)

25,00020,00035,000nilnil

45,000nilnil

nilnilnilnilnilnil

nil5,0005,000

nilnilnil

Ag Cu Zn Pb Sb As Ko (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb!

1957 39,98 40,57 0,59 5,00(1958 40,57 41.45 0.88 nil

1959 42,48 43,36 0,88 nil

-04-198?::17:50


DIAMOND DRILL LOG

NHB 87-03

Page 5

Proa To ———— — ——— - — Description ———————— - — - SaBple(B) (B) No,

19601961

1 19621963196419651966196?1968196919701971

Proa(B)

43.3644.1044.9845,8646,7547,6348,5149,3950,2751,1652,0452,92

To Width(B)

44,1044,9845,8646,7547,6348,5149,3950,2?51,16 t52,0452,9253,80

(B)0,740.880,880,890,880,880,880,880,890,880,880,88

Au Ag Cu Zn Pb Sb As Mo(ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)nil5,000nil

10,000nilnilnilnilnil

10,000nilnil

197219731974197519761977197819791980198119821983

54,6055,2756,1557,0457.9258,8059,6860,5661,4562,3363,2164,09

55,2756,1557,0457.9258,8059,6860,5661,4562,3363,2164,0964,78

0,6?0.880,890,880.880.880,880.890,880,880,880,69

nilnilnilnilnilnilnilnilnil

10,00nilnil


Dark-GreyFine GrainedWeakly Fractured (4 Fractures/Metre)li Carbonate Veining randoB -- Avg. Width In

1984198519861987

64,78 65,5665,56 66,4466,44 67.3367,33 68,21

0,780,880,890,88

nilnilnil

15,000

-04-1987;:17:5Q


DIAMOND DRILL LOG

NHB 87-03

Page 6

FroB To ———————— -— W (B)

Magnetite: 5* Pyrite: tt Chalcopyrite: ((tt Chlorite Alteration: Carbonate Alteration: Moderately Magnetic

—Description —————

10-15*

•- ———— SaBple No,

1988 1989 1990

Proa (i)

68,21 68,80 69,38

68 69 70

To (B) .80 .38 .07

Width (B) 0,59 0,58 0,69

:xri:r::

Au (ppb)

45,000 10.000 25,000

Ag (ppb)

PUWU

(ppb)Zn

(ppb)Pb Sb As Mo

(ppb! (ppbi (ppb) (ppb)

Sections have a vuggy texture Coarse pyrite cubes up to lea

70,1 80.O MASSIVE SULPHIDES WITHIN CHERT

Brown to KellowKediun GrainedWeakly Fractured (2 Fractures/Metre)Strongly Magnetic

Section 72.66 - 80,11 crude banding 40 deg, Cas.40*po,40*iiag,54py,15*chert,Tr,cpy.Section 78 -80 70* py 15* lag 5* chert

19911992199319941995

199619971998199920004701470247034704470547064707

70,0770,5671,1571,7472,32

72,9173.5074.0974,6875.2675.8576.4477.2577.9178,5079,0979,67

70,5671,1571,7472,3272,91

73,5074,0974,6875,2675,8576,4477,2577,9178,5079,0979.6779,97

0,490,590,590,580,59

0,590,590,590,580,590,590,810.660,590,590,58

: 0.30

nilnil

10,000nilnil

nilnil

10,00030,00010,00015,000nilnil

10,00015.000nilnil

0JM1.9 FERRUGINOUS CHERT

Dark-Grey 4708 79,97 80,56 0,59 nil

8-04-1987::17:51


DIAMOND DRILL LOG

NHB 87-03

Page 7

FroB To —— - ———— - —(B) (i)

Fine GrainedWeakly Fractured (214 Carbonate VeiningMagnetite: 154Pyrite: 54Chlorite Alteration:Garnet Alteration: (Strongly Magnetic

Fractures/Metre)randoa -- Avg, Width IBID

54{H

SaapleNo,

470947104711

Fr(

808181

OBB).56.14.44

i

818181

To(B).14.44.91

Hi'(000

dthB).58.30.47

Au ' Ag Cu Zn Pb Sb As Ho(ppb) Ippb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)nilnil

5,000

81,9 86,8 HAFIC TO INTERMEDIATE FLOW

Dark-GreyFine GrainedFoliation at 52 Deg, Cax,Weakly Fractured (7 Fractures/Metre)Kagnetite: 104Pyrite: 54Carbonate Alteration:Silica Alteration:Chlorite Alteration:Moderately Magnetic

84,98-85,77 strongly chloritizedWeakly brecciated texture to nost of the core

86,8 87,5 MASSIVE MAGNETITE

BlackFine Grained(14 Carbonate Veining randoB -- Avg. Width IBBMagnetite: 954Pyrite: 5*.

471247134714471547164717

81,9182,6183,5084,3885,2686,14

82,6183,5064,3885,2686,1486,80

0,700,890,880,880.880,66

5.00^nil

15,00nilnil

15,0014718 86,80 87,49 0,69 53,C

8-04-1987::17:5i


DIAMOND DRILL LOG

NHB 87-03

Page 8

FroB (B)

To (ID)

-Description- Saaple No,

Chalcopyrite: Strongly Magnetic

Upper contact irregularCoarse pyrite cubes up to leo wide

87,5 89,2 MASSIVE PYRITE

Hello*Kediun to Coarse GrainedWeakly Fractured (2 Fractures/Metre)Pyrite: 95*Magnetite: 14Chalcopyrite: ((HEpidote Alteration: ( (l\Weakly Magnetic

ttchert

89.2 92,1 MASSIVE MAGNETITE WITH PYRITE IN CHERT

BlackFine GrainedP, Carbonate Veining -- Avg, Hidth 2mmMagnetite: 50*,Pyrite: 5-101Silica Alteration: 5iChlorite Alteration: 2 \Epidote Alteration: (ItStrongly Magnetic

471947204721

From (B)

To (o)

87,4987,9188,49

87,9188,4989,16

Width Au Ag Cu Zr, Pb Sb As Mo (B) (ppb) (ppb) Ippbl (ppb) (ppbl (ppb) (ppb) (ppb)

0,42 40,0000,58 15,0000,67 15,000

47224723472447254726

89,1689,8690,5591,1491,73

89,6690,5591,1491,7392,07

0,700.690,590,590,34

30,00015,00015,000nilnil

92,m5,7 INTERMEDIATE TO FELSIC VOLCANIC

Grey 4727 92.07 92,90 0,83 30,0

8-04-1987::l?:52


DIAMOND DRILL LOG

FroEi (B)

To (B)

Pine Grained

-—Description--———— OdSplcNo,

4728

Froi (a)

92.90

To (B)

93,79Foliation at 45 Deg. Cai.Weakly Fractured (3 Fractures/Metre)(tt Carbonate Veining randoio -- Avg, Width 2mPyrite: 5*Magnetite: 5*Chalcopyrite: ((ttChlorite Alteration: 5*Biotite Alteration: 2*Hoderately Magnetic

Pervasive strong carbonate alteration 95.48-111.89 Wpy 97.26-97.66 Hafic Dyke

SanpleNo,

4728

47294730473147324733473447354736473747384739474047414742474347444745474647474748

Froi(a)

92.90

94.1894,9695.8496,7397,6198.4999,37

100,25101.14102,02102,90103,78104,66105,55106,43107,31108,19109,07109,96110,84

To(B)

93,79

94,9695,8496.7397.6198,4999,37100.25101,14102.02102,90103.78104.66105.55106,43107,31108.19109.07109,96110,84111.72

WidthIn)0,89

0,780,880.890,880.880.880.880,890,880,880.88

, 0,880,890,880.880,880.880.890.880,88

Au(ppb)

15,000

10,000nilnilnilnil

15,000

nil5,0005,000nilnilnil

5,000nil

5,000nilnilnilnil

NHB 87-03

Page 9

Cu Zn Pb Sb As Ko (ppb) (ppb) (ppb) (ppb) (ppb) ippb) (ppb) Ippb)

4749 112,31 113,19 0,88 nil

47504751475247534754

118,48 119,36119,36 120,25120,25 121,13121,13 122,01122,01 122,89

0,880,890,880,880,88

nil nil nil nil nil

8-04-19871:17:52


DIAMOND DRILL LOG

NHB 87-03

Page 10

Froi To In) (ID)

-Description-rrsrssi:

SanpleNo.

47554756475747584759'476047614762476347644765476647674768

FromIn)

122.89123.77124.66125.54126.42127.30128.18129.07129.95130.83131.71132.59133.48134.36

r:r:r:rer:

Tod)

123.77124.66125.54126.42127.30128.18129.07129.95130.83131.71132.59133.48134.36135.24

Widthla)0.880.890.880.880.880.880.890.880.880.880.880.890.880.88

Au Ag Cu Zn Pb Sb As Mo(ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb) (ppb)nilnilnilnilnil

15.00015.00035.000

nilnilnilnilnilnil

135.7 157.6 INTERMEDIATE TO FELSIC VOLCANOCLASTIC

GreyFine GrainedFoliation at 60 Deg. Can.Heakly Fractured (l Fractures/Metrel(H Quartz Veining at 60 Deg. Cai. -- Avg. Width 4fflnPyrite: MMagnetite: ((UBiotite Alteration: 101Chlorite Alteration: HGarnet Alteration: (liNon Magnetic

140.70-145.3 l-2*py (lliag.perv carb.chloritic alt.

8-04-1987::17;53


DIAMOND DRILL LOG

NHB 87-03

Page 11

Froffi d)

To d)

-Description-

145.3-148.48 relatively fine fragments Ulci) 148.48-154.70 relatively coarse fragments Olcul 154.70-155.79 relatively nassive felsic flow

Saaple From To Width Au Ag Cu Zn Pb Sb As Ho lo. d) (B) (D) (ppbl (ppb) (ppb) (ppb) (ppb) (ppbl (ppb) (ppb)

157.6 END OF HOLE.

8-04-1987:;17;53


Sample Contents

NHB 87-03

Page 13

Salop No

1937

1938

1939

1940

1941

1942

1943

1944

1945

1946

1947

1948

1949

1950

1951

1952

1953

1954

le From(a)

14.99

15.88

16.46

17.05

17.79

18.52

19.40

20.29

24.70

25.58

26.46

27.34

28.22

29.11

29.99

A30.58

31,46

34.10

Tod)

15.88

16.46

17.05

17,79

18.52

19,40

20.29

21.17

25,58

26,46

27,34

28.22

29.11

29,99

30,58

31,46

32,05

34,99

Widthir,)

0,89

0.58

0,59

0,74

0.73

0.88

0,89

0.88

0,88

0,88

0.88

0.88

0.89

0.88

0,59

0.88

0.59

0.89

BSBBrBBsrrzzzzzzBBzzzzzzzszBZSESBBSssssBrsriBBrzzzBB

5-10tpy.silic, carb. nag.

5tpy. carb. nag.

5-10^py.carb.

2-5*py, silk. iperv, carb,

2tpy,epidote(ibrovn carb,

Jipy.epidoteibrown carb.

2tpy perv.carb.

2lpy, 21. 64-21.83 sass.nag,

Upy, perv.carb,

Itpy, vuggy core

2*py. Bilic.perv.carb, ;

Hpy.sihc. perv.carb.

Hpy. Bilic.perv.carb.

Tr.py.silic, perv.carb.

silic.perv.carb.

Hpy, vuggy core

Gtpy. perv.carb.

Well fractured vuggy core

8-04-1987::17:53


Sample Consents

NHB 87-03

Page 14

Samp] No,

1955

1956

1957

1958

1959

1960

1961

1962

1963

1964

1965

1966

196?

1968

1969

1970

1971

1972

.e Pron(a)

37,04

37.93

39.98

40,5?

42.48

43.36

44.10

44.98

45,86

46.75

47.63

48,51

49.39

50.2?

51.16

A52.Q4

52,92

54.60

To(ID)

37,93

38,95

40.57

41.45

43.36

44.10

44,98

45.86

46.75

47,63

48.51

49.39

50,27

51.16

52,04

52,92

53,80

55.2?

Width(B)

0.89

1.02

0.59

0.88

0.88

0,74

0,88

0,88

0,89

0,88

0.88

0,88

0.88

0,89

0,88

0,88

0,88

0,6?

Hpy. chlor. biotite

2*py.6ilic. chlor. perv. carb.

2tpy,silic,perv.carb,

2lpy,Tr,po,perv.carb,

Upy.silic, carb. bio. chlor.

2ipy. vuggy texture carb,

Hpy. vuggy broken core

Hpy .carbonate

vuggy broken core carb,

epidote biotite vuggy calcite

24py.8ilic.perv. carb.

24py.perv.carb.

2ipy.perv.carb.

2lpy,brown carb,

Yellow silicification biotite

Hpy, Biotite

Hpy.lfllbiotite stringers

Epidote chlor. nag, (talc seam

08-04-1987::17:53

Sample No.

1973

1974

1975

1976

1977

1978

1979

1980

1981

1982

1983

1984

1985

1986

1987

19880

1989

1990

Prom (B)

55.27

56.15

57.04

57.92

58.80

59.68

60.56

61.45

62.33

63.21

64.09

64.78

65.56

66.44

67.33

68.21

68.80

69.38

To

56.15

57.04

57.92

58.80

59.68

60.56

61.45

62.33

63.21

64.09

64.78

65.56

66.44

67.33

68.21

68,80

69.38

70.07

Width in)

0.88

0.89

0.88

0.88

0.88

0.88

0.89

0.88

0.88

0,88

0,69

0,78

0,88

0,89

0,88

0,59

0,58

fi, 69


Saople Coments Page 15

———— Remarks ————

Thin nag. seats

Carb.vein and nag.sean

epidote brown carb. lag. bio.

Tr.py. Biotite stringers

lOlbiotite stringers Tr.py,

biotite stringers Tr.py.

Broken core perv. carb, Bag.

vuggy carb. nag. veil chlor.

Tr.py.nag.Well chlor.

Thin nag seams chlor.

20taag.8eans chlor, carb.

lfl-15*iag,10*chlor,Tr,cpy,

20*,chlor. Tr.py. sag, Thin cvs

2 ea qv with py, chlor,

Hpy.tcpy. chlor,

Upy,

2tpy,5tniag,Tr,cpy,

25taag.2tpy.carb.veins

8-QH987::17:54


Sanple Connects

NHB 87-03

Page 16

Saap. No,

1991

1992

1993

1994

1996

199?

1998

1999

2000

4701

4702

4707

4708

4709

4710

4711

4712

4713

le FroBIK)

70.07

70.56

71.15

71.74

72.91

73.50

74.09

74.68

75.26

75.85

76.44

79.67

79.97

80.56

81.14

A81.44

81.91

82.61

To (D)

70.56

71.15

71.74

72.32

73.50

74.09

74.68

75.26

75.85

76.44

77.25

79.97

80.56

81.14

81.44

81.91

82.61

83.50

Widthd!

0.49

0.59

0.59

0.58

0.59

0.59

0.59

0.58

0.59

0.59

0.81

0.30

0.59

0.58

0.30

0.47

0.70

0.89

AcBarRB

254nag.254po.Wpy.

24py'po, Tr.cpy.ttiiag.

354po, 354mag, 14py,

254nag. 154po. 104py.Tr.cpy

504nag, 354po 104py Tr.cpy,

554i)ag. 354po. 54py.

504ioag.304po.5tpy. Tr.cpy,

504nag, 4Q4po. 104py

604jiag. 304po Iflipy.

40hag. 30tpo 5tpy

504nag. 304po. l-2*py.

30*py 104po

lOipy

304mag.24py.12cD pink cv

204uag. Trace garnets

Trace pyrite

154nag.l4py. Trace cpy.carb.

24py

8-04-1987;:17s54


Sauple CoBuentfi

NHB 87-03

Page l?

Saip No

4714

4715

4716

4717

4718

4719

4720

4721

4722

4723

4724

4725

4726

4727

4728

4729

4730

4731

le Fron(a)

83.50

84.38

85.26

86.14

86.80

87.49

87.91

88.49

89.16

89.86

90.55

91.14

91.73

92.07

92.90

A94.18

94.96

95.84

To(o)

84.38

85.26

86.14

86.80

87.49

87.91

88.49

89.16

89.86

90.55

91.14

91.73

92.07

92.90

93.79

94.96

95.64

96.73

Width(D)

0.88

0.88

0.88

0.66

0.69

0.42

0.58

0.6?

0.70

0.69

0.59

0.59

0.34

0.83

0.89

0.78

0.88

0.89

EsrrssrsssrrssrsssrsssssEsrsrsesssrssassrsssssrssssrrsssrsrsssrss^srsssssr

ncwarKo

5*py

5*py

2-5lpy. Trace epidote

Hpy Brecciated teiture,

95hag.5*py,

954py Shag,

854py ISkhert Trace cpy : ,

95tpy '

90*nag.lO*py. ^ ,

lfl*py lOkhlor.lO^carb.S^nag,

SOUiag.lOtpy.lOtcarb.

silic,l-2hag.Hepidote

90imag, 5^py. Stcarbonate

151 pyrite

10* pyrite.

20-254 pyrite ,

15^ pyrite .

154 pyrite

8-04-1987::17:54


SaispJe CoBnents

NHB 87-03

Page 18

Sanple Pron No. (B)

4732

4733

4734

4735

4736

4737

4738

4739

4740

4741

4742

4743

4744

4745

4746

4747

4748

4749

96

97

98

99

100

101

102

102

103

104

105

106

107

108

109

A09

110

112

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