010 TOWNSHIP: Penhorwood REPORT NO: 29 · •Property —————NAT-JUVER Sheet No. _S——— OF - Hole No __NR-92?-! Depth 81 Lithology Description (colour, grain size,

DIAMONL

43B01SW8S76 29 PENHORWOOD010

TOWNSHIP: Penhorwood

WORK PERFORMED FOR: Noranda Exploration Co Ltd

RECORDED HOLDER: SAME AS ABOVE

: OTHER { J

REPORT NO: 29

CLAIM NO..

1180960

HOLE NO.NR-92-1

FOOTAGE

397 m

DATE NOTE

April 4 92 (1)

NOTES: (1) ROW 9260 00091

Filed November 1992

NREVISED

PftOJ.N? 111N.T.S^..............DWG.N*

NAT RIVER

DRILL PLAN

PROJECT*.....SURVEYED IYinDRAWN IYi

....™...... ...™ DATEs..JULYJ0.1W2 .SCALii 1:5000

NORANDA EXPLORATION CO. LTD.OMICI i "t*/!* , ttrmt/f.

PRDJECTi NAT RIVER #111

SECTIQN 1768VSCALE) 1/2000

BRILL HOLE NR93-1

98/07/31

NDRANDA EXPLDRATIDN

LATITUDE 2 Q 50S (Imperial) 625S (Metric)W

L58W (Imperial) 1768i (Metric)

Surface

NORANOA EXPLORATION COMPANY LIMITED

DIAMOND DRILL CORE LOGSheet No. -OF. 15

DEPARTURE

ELEVATION

Test Depth

25" eastDIP AT COLLAR

-45'

TOTAL DEPTH 397m

- BEARING —^

CORE SIZE BQ

-100m

Dip

-M -38.5 0

Magnetic Beiring

Corrected Bearing

Project No.

Property

111NAT RIVER

Hole No —NR-92-1

20 300m

NTS 42B/1 TWP. Penhorwood Claim No. 1180960

CORE STORAGE TJitinins, Aunor Mine Site

REMARKS Casing pulled._______

Date started ,March 30/92

contractor Bradley Bros. Ltd

completed — April 4/92

Logged by Wayne Corstorphine

Depth 81 Lithology Description (colour, grain size, texture, structure, etc.! Alteration Mineralization Remarks

0.0-11.0

11.0-13.0

DIABASE DYKE

13.0-16.5

ALTERED BASALT

16.5-20.5

FELDSPAR PORPHYRY

Casing

Fine-grained becoming finer toward lower contact; moderately magnetic; massive, but well-fractured; homogenous; lower contact lost in broken core.

Partially altered "granitized" basalt or sediment, a hybrid zone. Inhomogeneous appearance due to fracturing and irregular pale buff green to pinkish discoloration patches and lineations and fractures. Some weak epidotization; basic groundmass is fine grained and generally massive; medium to dare green in colour. Some foliated shear sections; estimate lS-20% discolouration. 14.1-14.24 Very fine-grained, pink feldspathic dyke; non-magnetic. 15.62-15.74 Pink, medium grained feldspathic dyke. Contacts irregular and at high angle Ô0 .

Medium to coarse grained "granitic" dyke. Massive texture, weakly porphyritic, pale pink with greenish interspacial grains of hornblende. Little or no observable free quartz so probably svenitic. Some volcanic inclusion material; variable ratios of feldspar to hornblende changes colour locally. Minor disseminated pyrite;

Saussuritization alorn fractures and small shears. Some pink feldspathization. Minor quartz blebs.

Minor disseminatedpyrite 1-31scattered through core.

No retained evidence of bedding.

Trace to li disseminated fine grained pyrite.

Weakly porphyritic more m-cg syenite.

NORANDA EXPLORATION COMPANY LIMITED

DIAMOND DRILL CORE LOG Project No.

Property

-114-

Sheet No.

Hole No

.OF.

MP-&XVSR-

Depth b Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

20.5-30.6

ALTERED BASALT

Contacts are irregular, generally high angle orientations at 70-800 .

Similar to 13.0-16.5 in alteration and structure. More pyritic in places: 20.5-22.3 Pyritic section 20.5-21.6 Dark grey with many hairline fractures with pale alteration outline. Protolith questionable but groundmass has texture of mafic intrusive or volcanic - eve i grained, massive, near a salt/pepper texture 21.6-22.3 Strong epidotization at 801 pale pistachio colour. Irregular jumbled, wispy texture caused by epidote colouring of core. 22.3-30.6 Inhomogeneous, same as 13.0-16.5. Strongly silicified with frequent pinkish, aphanitic, fractured patches. Faint banding appears in places with depth. Sometimes the aphanitic, siliceous sections have appearances of primary chert bed distinctly interbedded with volcanogenic sediment? Lower contact arbitrary - gradational based on alteration.

No carbonate style alteration or veining Saussuritization, feldspathization, as for 13.0-16.5.

3-101 disseminated pyrite

5-lO% disseminated pyrite.

Small chalcopyrite grain in silicified or siliceous section at 24.6.

30.6-47.7

BANDED METASEDIMENT OREYWACKE- AROILLITE

Well banded on meso to fine scale. Core angles 70-800 . Colour varies between dark black to pale grey with sharp contacts in

l clear evidence. Individual laminae range in thickness from a few mm to several cm or mor3 Three types of bands- thinner, finer-texture l dark blackish bands of hard argillaceous roc c; weakly graphitic but non-conductive. Constitutes about lQ-15% of interval. Seconi type still fine-grained, grey, usually forming thicker bands- greywacke composition Both are very hard (siliceous).

No alteration present in sediments.

20.5-29.5 and 13.0-16.5 are probably sediment (volcanogenic grey wacke) greenish cast. Fracture alteration by siliceous solution etc has masked the original nature of the protolith. There is not enough clearly dissimilar in nature to the groundmass in deeper rock which is clearly well banded sediment.

Rare, thin, fine grained pyrite mass or heavy dissemi nation over lcm. Occasional interval with fine-grained pyrite l-2%.



"Property

Sheet No.

Hole No -

HAT-RIVER

Depth ft Lithology Description (colour, grain size, texture, structure, etc.! Alteration Mineralization Remarks

47.7-50.7

COARSEMETASEDIMENTGREYWACKE

50.7-63.0

Non magnetic, no veining or alteration. Third type of band is volcanic in appearance - greenish cast, fine grained coarser textured - tuff band or small dyke. These are rare at l-2%.Suggestion of graded bedding places tops downhole or to south. Lower contact sharp at 8O0 tea.

Mixed, interbeds of fine greywacke (45-50%) and coarsely textured, locally magnetite bearing (disseminated grains) foliated metasediment. 600 core angles, brownish to greenish cast to course bands. Coarser textured lithotype locally has appearance of conglomeratic rock with rounded heteroliths up to lcm floating in medium grained, micaceous-looking groundmass. Consider protolith to be coarse muddy arenite.S-7% mica, in general, some bands are chloritic. MM sized grains in groundmass. 47.7-48.3 coarse sediment 48.3-48.65 fine, siliceous sediment with thin laminae of coarse mica-bearing sediment 48.65-49.4 90% coarse sediment as in other sections. Intercalated, narrow laminae and irregular lenses of siliceous greywacke. 49.4-50.5 fine, siliceous greywacke 50.5-50.7 coarse greenish to brownish grey sediment with irregular poorly defined, fine greywacke. Internal contacts are generally sharp.

Uniform section of light to dark grey, wacke and argillite. Subtle, sharp bedding contac Minor, thin bands up to 15 or 20cm of the

Trace to j.% micro laminae and disse minated grains of py.


DIAMOND DRILL CORE LOG Project No111

Sheet No ——

Hole No

-OF.15

NR-92-1

' PropertyN&T RTVRD

Depth 8. Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

BEDDED GREYWACKE/ ARGILLITE (WEAKLY GRAPHITIC)

63.0-184.8

BASALT

coarser textured, micaceous sediment, less distinctive than those in 47.7 to 50.7. Minor pyrite as thin, concordant micro- laminae and coatings, widely dispersed occurrences. Core angles in weakly graphiti argillite beds 600 , some at 700 . Lower contact sharp at 600 . Marked by 4cm black graphitic argillite band. 62.5-62.96 Concordant feldspar porphyry sill, faint l-2mm feldspar phenocrysts, with anhedral outline, about 31.

Dark green, finely textured basalt. Relatively uniform, slight variations in texture - very fine to coarsely fine grained. Texture is generally massive in appearance but in detail is foliated. Non magnetic. Frequent, short intervals have "chloritic" appearance.Frequent paler sections of sharply defined feldspar porphyry, pale pinkish to grey colour. Somewhat pervasive alteration throu the dykes, e 67.85: 10cm fP, concordant, 60C

72.1-72.35, 78.0-78.6, 80.25-80.55, 80.7-80.9, 81.17, 81.5, 82.4-85.1 are all feldspar porphyry dykelets.

The volcanic is not very uniform in detail. Displays near banded variation from faintly defined chloritic laminae to greyish cast intervals, to salt/pepper, porphyritic textured phases.

59.4-91.44 Weak to moderately altered and veined section. Veining is random

Minor white carbonate (calcite) stringers - normally expected amounts. Some localized, weakly developed sericitization giving paler, yellow-brown discolouration.

No significant alteration or veining beyond normally expected amounts.

76.2 15m carbonate vein 2O0 tea.

Nil to trace pyrite only.

tea.

Pervasive calcite in groundmass.

good HCI reaction wherever a good


DIAMOND DRILL CORE LOG Project No. ————111———————

•Property —————NAT-JUVER

Sheet No. ___S——— OF -

Hole No ____NR-92?-!

Depth 81 Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

stockwork of thin, white, calcite-rich stringers {5%), locally to 101 over 10-20cm in one place.

90.3-91.0 Quartz-carbonate vein up to 2cm wide running parallel to core axis. At 90.9 large mass of white quartz-carbonate with splashed of chalcopyrite.

91.4-110.3 Variably textured and structured basalt. Local, thin, white veins 6 veinlets not beyond expected background amounts. Sows banded sections at 60-70 tea, caused by tectonic effects.

110.3-124.3 Well banded section of basalt. Banding caused by pale alteration lenses 60-700 tea. Most are less than l-2cm wide. Groundmass of basalt is massive to foliated.

Buff-green fromsericitizationor saussuritization?Discolouredbasalt reacts to HCIstrongly. Traces ofred hematite relatedto veining.Pervasive calcitethroughout groundmassof both paler bands Sdark, less altered,basalt.Alteration bandingis irregular and in-individually narrow -form pale, aphaniticinhomogeneous lenses.

Non-magnetic, no leucoxene visible. Occasional to more frequent sections of dark chloritic composition - usually very dark Frequent (51) irregular discolourations, carbonate=quartz veinlets etc. to make section inhomogeneous in appearance.

124.3-129.0 section.

Relatively homogeneous basalt

120.6-121.1 Beige to pale orange

green, alteration band. Possibly altered feldspar porphyry sill. Contacts are finer textured and hosting basalt banded and altered.

129.0-131.5 Development of pale, greenish buff alteration bands which give way at 129.6, to reddish, weakly hematized? basalt to 130.2. A short, banded, altered section follows as 129.0 to 129.6. Strongly hematitic band 130.5-130.9.

fabric is developed and pale grains are present in the basaltic groundmass.

Traces of disseminated pyrite.

Nil to trace pyrite.



Property —

Sheet No. ___6___ OF —NR-92-1

Hole No. ——————-——-——.

HAT RIVER


131.5-147.2 Weakly to moderately spotted ba Dark green spots at 1mm in size (S-5%). Sec is often near massive but locally shear foliated. Moderately magnetic throughout -

136.8-141.7 Weakly to moderately hematiz weakly to moderately foliated basalt (spotted). Reddish cast.

139.4-139.65 reddish pink dyke or strong alteration as 130.5-130.9.

After 137.0 magnetite diminishes and virtual disappears.

147.2-156.3 Reappearance of banded volcanic similar to 110.3-124.3. Inhomogeneous due t irregular, white veinlets of primarily calci composition (5-6%). Colour is paler green - almost chalky in appearance. Groundmass is calcite-rich (HC1 reaction) and paler, greyi red bands which are very irregular in size a distribution tend to be even richer in calci 147.2-152.5 calcite rich groundmass 152.5-154.7 disappearance of calcite with

development of ankeritereplacement alteration.Strong ankerite alteration ofpale buff colour.

All changes between footages are gradational in nature.

156.3-165.4 Basalt is less affected by alteration, returning to more pristine appearance. Distinctly coarser-grained, even textured; sub massive to only very locally foliated. Magnetite content still low but more continuous (still not very high about X-2% locally).

salt. :ion

jatchy. id

section a smallbe

eh colou-ndbe.

Ankerite alteration pervasive but erratic in concentration Core of alteration is 152.85-154.7. The central 0.5m is complete replacement

High frequency of l-3mm white carbonate (calcite) veinlets subparallel tea from 156.3-160.0. Still retains fine calcite throughout

Magnetite appears, patchy about 11 locally.

A magnetic response is frequently found at a carbonate veinlet, these may carry magnetite in small amounts or cause to concentrate this mineral at their contacts.

Minor occurrences of magnetite in this section.

Some pyritic concentrations locally. Mainly small semi-massive to heavily disseminated clots and wispy bands all about lcm in scale. Overall about l-2% concentrate

Nil, to disseminated pyrite grains only.

n.


DIAMOND DRILL CORE LOG Project No _ .., _ JU

Sheet No.

______ Hole No. -

-OF. -ts-

. Property NAT RIVER


184.6-210.2

INTRUDED ANDALTEREDBASALT

Section has look of metadiabase of fine texture. Lower contact arbitrary based on readily discernable "diabasic" texture. Same rock type continues but lacks homo geneity and distinctive groundmass texture unless carefully compared.

165.4-184.8 Dark green basalt, similar to non banded basalts above 156.3.

173.0-173.9 Feldspar Porphyry Sharp contacts 400 tea. Pale feldspar cryst 2C^ in greenish buff to pinkish buff ground mass. Massive textured numerous pale alteration lines following fracture breaks.

groundmass (HC1reaction).Local 0.5-15mm widereddish pink calciteveins - randomjagged orientation anshape.Normal white carbonat

IsWeaklv altered, carbonatized.

Nil sulfides in feldspar porphyry.

Localized leucoxene along fracture lines. Becomes more pervasive with depth, but it occurs only sporadically. Relatively uniform section with only local narrow zone of l-3cm displaying pale discolouration, fracturing and minor pyrite. Lower contact sharp at 450 to core axis.

Zone containing numerous pale, pinkish to whitish (less common), medium to coarsely textured feldspar-rich dykes. Some quartz but in low amounts (2t). The felsic dykes are massive with sharp, generally conformabl contacts varying from 45 to 7O0 tea. Intercalated basalt sections display, locall/ strong foliation to banding, above average magnetite content and hematitic to calcite- bearing groundmass in places. 151.1-186.15 Massive pale, feldspar-rich dyce dark blackish hairline stringers. Lower contact 4O0 . 186.15-189.85 Basalt; initial 0.3m tectoni-

Carbonate alteration variable - ankeritic here. Veinlets and some groundmass replacement of weak to moderate intensity

Generally low pyrite content, trace to it overall. Some local sections carry up to to 5 or 7% dissemi nated pyrite.

This section may correspond to the carbonatized zone in Utah's hole (NR-1-87) 200m to the cast. AT 186.7 Magnetite content becomes visible as black spots in basalt.



' Property

Sheet No

Hole No. -

.OF.

MPHIIVER

Depth 6 Lithology Description (colour, grain size, texture, structure, etc.)

eally and alteration banded, at lo* ri*-Alteration Mineralization Remarks

tea. Remaining part very homogeneous with a subtle banded to streaked texture over the foliation fabric. Strongly magnetic ( 5* magnetite).

189.85-190.4 Basalt, strongly magnetic, coarse magnetite grains about e-8%. Parts of groundmass, pinkish-feldspathized.

190.40191.05 Feldspar-rich dyke as for 184.5-186.15.

191.05-194.5 Feldspar-rich dyke as for 184.5-186.15 etc. Two narrow grey siliceous bands over last 0.4 meters.

194.5-195.4 Dark blackish grey, fractured quartz-rich section. Fractures display radiating beige-red alteration - cores carry heavy pyrite mineralization. Lower 0.3-0.4 is quartz poor.

195.4-196.5 Highly feldspathized basalt similar to 190.4-191.05. 50-601 pervasive groundmass replacement by feldspathic alteration.

196.5-197.1 Feldspar-rich section same as 184.5-186.15 etc.

197.1-197.4 Highly feldspathized basalt similar to 195.4-196.5. Narrow pyritic stringers subparallel to core axis over last 0.3m which are highly silicified resembling somewhat 194.5-196.5.

197.4-198.25 Pink feldspar-rich section as 184.5-186.15. Small basalt lens at 198.0 15c m wide.

S-7% pyrite associated with fracture/alteration in grey-black quartz vein.

in

This section almost has appearance of felsic porphyry it is so altered.

5-8% stringer pyrite in fractures.


DIAMOND DRILL CORE LOG Project No ————111

Sheet No.

— Hole No

.OF. -15-

Property ————--MAT"RIVERDepth 8. Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

198.25-210.2 Predominantly basalt in variousstages and degrees of feldspathic alteration.A number of feldspar-rich dykes/sills as follows:200.9 10cm, sharp contacts201.35 10cm, sharp contacts201.8 30 cm with feldspathized basalt bordersplus carbonate and minor pyrite. 5-8cm carbanatequartz vein paralleling core axis.

202.45 10cm pink feldspathic dyke: Intervening section between 201.8 and 202.45 is dark and siliceous similar to 194.5-195.4 with pyrite filled fractures. The feldspathic section at 202.45 has a low contact angle with the dark siliceous section which is uphole, contact at 200 .

AT 201.25 Splash chalcopyrite in feldspathized basalt.

S-6% pyrite stringers in dark siliceous section, possibly quartz vein in 201.8-202.45 interval

203.0-203.6 Feldspathic dyke, last 0.3mm mixed with wispy basalt.

204.44-204.6 Feldspathic dyke; bordering basalt for 0.4-0.5m. Contains 10% ankerite veining.

206.0 10cm feldspathic dyke material.

206.25-206.9 feldspathic dyke Basalt sections between the numerous feldspathic lenses are foliated to alteration banded and randomly veined by pale ankerite. Some feldspathic veins too.

205.6 onward, calcite reappears in basalt groundmass.

Leucoxene visible in some altered basalt sections particularly: 198.25-199.6 which is strongly altered and moderately to well veined with veinlets of various composition. Note that the pink feldspathic dykes have inconsistent contact angles, i.e. upper and lower contacts are not parallel although they are usually subconformable to fabric in host basalt/fabric caused however by stresses related to deformation and intrusive activity.



Property —

Sheet No ___10__ OF

Hole No —

-NAT-RIVER

Depth a Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

210.2-238.0

BASALT

238.0-251.6

ALTEREDBASALT(ANKERXTXZED

Overall texture is contorted (brittle) and haphazard.

206.9-210.2 Moderately to weakly veined and banded basalt. Basalt still a dark green colour, fine-grained, non-magnetic; but still contains faint feldspathic component in the groundmass.

209.0 Diffuse occurrence of pink feldspathic fragments and much quartz- carbonate vein material across 0.3m.

Lower contact gradational, arbitrarily place at end of feldspathic dyke occurrences.

Return to normal basalt flow section. Contains 5% intrusive white carbonate and quartz veinlet material very randomly distributed and at all angles to core axis Maximum size of veins is 2cm, average l-5mm. Non-magnetic basalt. Dark green, fine-grainsd, mainly massive but frequent foliated to near banded sections, some weakly brecciated (short intervals -co.3-0.5m). Lower contact gradational, arbitrarily place J where ankerite alteration starts.

At approximately 238.0m there is an increase in the amount of carbonate veining and size of veinlets. Veinlets are ankerite- rich. Basalt exhibits strong fabric, some alteration induced banding and fragmentation suggestive of stress zone. Colour variation from dark, greyish green of basalt to pale white of veins and altered borders of buff colour.

240.4-245.1 Section contains intervals of

White calcite veinlets reappear in basalt.

Breccia Zone 0.3m

No significant alteration other than pervasive calcite throughout basalt groundmass.



Ankerite alteration mainly as veins throu ghout the section - estimate 101. Basalt groundmass also ankeritized. Occasional narrow irregular, ragged quartz-carbonate vein

Sparse sulfides, nil to trace or 13; locally of disseminated pyrite.


DIAMOND DRILL CORE LOGSheet No. .OF.

11 15Project No.

IllHole No.

MR-92-1

PropertyKAT RIVER

Depth 8. Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

251.8-310.9

BASALT

feldspathic dyke material similar to 189.85-206.9. Local intervals of highly altered and tectonized basalt similar to sections in 184.8-210.2 interval. Intense replacement feldspathization locally.

245.1-251.8 Variably altered (ankeritized) basalt. Foliated to alteration banded. Groundmass coarsening. Minor feldspathic bands - lost at 250.9- 251.1. Core angles at 600 . Lower contact - diminished alteration.

Similar to 210.2-238.0. Dark green, fine grained but variably textured, slightly coarser sections present. Irregularly veined by sporadic white quartz and carbonate-quartz stringers. Non magnetic.

279.7-280.0 Narrow ankeritic section (weak) with quartz infilling basalt breccia interval.

Some sericitic discolouration.

Moderately veined with ankerite stringers.

No significant alteration.


Nil to trace disseminated pyrite grains.

281.4-282.15 Pale buff coloured (to grey buff) ankeritized zone. Contact discrete, upper 450 lower 80-900 . Cloudy quartz patches- minor, occurs in one 10cm section.

section282.15-292.5 Basalt-typical of general Local irregularities filled with quartz and carbonate (S-4%) - open space breccia-type of pattern.

292.5-293.05 Diabase dyke, upper contact 55 lower 45 , weak to moderate magnetic respons

293.05-294.0 Basalt

294.0-294.44 Dark greenish red, feldspar


DIAMOND DRILL CORE LOGSheet No. ___ __ OF .

Project No.

Property —

Hole No. ___.HR-92-1

HAT RIVER"Depth 8. Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

porphyry dyke.

294.44-295.25 Basalt section. Displays breccia texture and plastic deformation and minor, banded alteration.

235.25-295.9 Diabase dyke, moderate to strongly magnetic response. Upper contact 4O0 , lower 250 .

295.9-300.7 Sheared basalt, subparallel to core axis 15-200 . Occasional pink feld spathic bands l-2cm wide in plane of shearing. Basalt is moderately altered by calcite replacement in groundmass and by carbonatized bands. Grades in to coarsely mottled, semi-banded, green, to pale grey- green basalt containing much calcite and minor ankerite. Minor splashes of leucoxene

300.7-306.0 Well mottled basalt - churned up appearance but with tightly packed, cohesive look. Variably altered groundmass, strong disseminated calcite component in groundmass, pale, splotchy look caused by carbonate.

306.0-308.0 Deep reddish felsic dyke. Mottled pink red and dark green. Feldspath! composition. Local shear banding. Contact sharp, upper 2O0 , lower irregular mixed with basalt.

308.0-310.9 Tightly fractured, brittley stressed basalt. Continue to be in general deformation zone. Local wispy, pinkish to b alteration patches. Minor calcite veinlets. Calcite still strongly present in groundmass

Nil sulfides.

Strong calcite groundmass alteration, minimal ankerite.

sige


DIAMOND DRILL CORE LOGSheet No

13-OF.

15

Project No. TUTHole No. — ~NR-92-l

'PropertyIffiT "RIVER"

Depth ft Lithology Description (colour, grain size, texture, structure, etc.! Alteration Mineralization Remarks

310.9-317.8

ALTEREDBASALT(ANKERITIZED)

317.8-331.4

MASSIVE BASALt

Gradational into more intensely altered basalt.

Strongly ankeritized basalt. Inhomogeneous appearance due to variable groundmass alteration, veining and fragment* structure. General foliation fabric 156.00 in more uniform sections of 600 . Numerous coarse knots of white ankerite and quartz. Texture pale ankeritized basalt is close to spinifex but protolith considered to be basalt. Leucoxene grains visible. Several buff coloured sections of more intense carbonatization. Lower contact gradational.

Fine-grained, even textured, dark green basalt. Massive texture to groundmass. Initial l meter contains 5-7mm wide quartz vein running along core axis. Fine, pale discolouration lines criss cross core - following fracture lines. Gradually dissipate by 323.5 meters. This unit is different from previous basalt sections. More massive, even grained, uniform texture groundmass. No calcite in groundmass. Non magnetic. Has fine salt-pepper (oophitic) texture, white feldspar in dark green horn blende groundmass. Last 1.5m becoming paler with carbonate groundmass and weak vein alteration.

Ankeritization, some quartz vein material,

d Intense groundmass alteration.

Nil to trace pyrite, trace chalcopyrite.

328.8-329.0 Pale green - buff groundmass alteration Quartz vein l-2cm wide at 329.0. Heavy cpy concentrati in in form of vein clust sr pyrite also present. Several small grey

S-7% pyrite,Hi chalcopyrite.


DIAMOND DRILL CORE LOGSheel No ———-———— OF .

15

Project No.

• Properly _

Hole No.. NR-92-1

NAT"RIVER

Depth ft Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

331.4-3S0.7

ALTERED FLOW BASALT

350.7-397J

ULTRAMAFIC8

331.4-332.6 Initial meter strongly foliated coarse texture with centrally located low angle quartz vein (20-300) following the low angle fabric of stress zone. Foliation gradually dissipates by 332.6.

332.6-345.8 Dark green fine-grained basalt somewhat inhomogeneous appearance due to fine "disturbed" breccia-like structure - more like a flow breccia - numerous dark blackish wisps, lines etc.

345.8-349.6 Groundmass becomes paler with distinct beige cast locally. Numerous white ankeritic veinlets ( 5*) - very irregular, filling fractures? Also present are pinkish feldspathic sections of small size - few cm 0.4m in one instance. Fabric is variable from massive to foliated usually at high cor angles 60-700 . Last 2.5m coloured, ankeritis replaced basalt. Lower contact distinct, bo contact rocks strongly foliated. This secti basalt feldspathized and beige coloured from carbonate alteration.

Soft, dark blackish colour; fine, paler whit ish vein component lacing groundmass is anke rite d lesser calcite. Unit is essentially non-magnetic - only local isolated responses

quartz veins over last three meters. Small but heavy pyrite concentration with most of these veins.

Alteration appears more calcite-rich. Low angle quartz vein at 331.75.

Df 332.6-344.5 Heavy calcite in groundmass

344.5-349.6 Ankeriti alteration, pale dis colouration but still greenish colour to b'asalt.

5-8% very fine pyriteto

sed th an of

Pervasive ankerite veining at 8% throughout ultra mafic.

X-2% pyrite - coarse splashes.

Sparse pyrite but local concentration over a few cm of

Ultramafic carries abov 11 disseminated pyrite as 1mm grains.


DIAMOND DRILL CORE LOGSheet No. ———n——OF.

10

Project No.

Properly —

Hole No.. NR-92-1

\T-RIVER:Depth ft Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

397.0

352.4-353.2 Pink, cloudy coarse looking texture. Mainly feldspar with chloritic fractures. Lower contact distinct at 8 O0 .

353.2-354.6 Grey feldspar porphyry dyke.Lower contact phenocrysts .

70 leached. Cloudy feldspj

X-2% disseminated pyrite.

J.% disseminated pyrite.

354.6-363.0 Ultramafic, massive to coarsel imbrecciated structure. 81; white ankeritic veinlets.

363.0-363.5 Pale, pink feldspar porphyry. Phenocrysts poorly defined. Hard surface. Contacts sharp, upper at 450 , lower at 450 ,

No alteration.

but reverse direction to upper, quartz veining.

Minor

363.5-397.0 Uniform section of ultramafic. Inhomogeneous texture from well foliated to weakly foliated 350-450 tea. Ankerite wisps patches and veins comprise S-10% of material in the unit - variation produces inhomogenei to rock's appearance. Throughout the ultra mafic there are narrow l-5cm intervals of greener, chloritic material.

END OF HOLE


J.% pyrite grains.

ty

Ministry of. ; Northern Development and Mines

Report of Work Conducted After Recording Claim

Mining ActOntario

Personal InfdMRtlon collected on this form Is obtained under the authority of the Mir this collection should be directed to the Provincial Manager, Mining/ands, Minis Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264.

l ' . . - 12B0ISW8576 29 PENHORWOOD 900

Instructions: - 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.

Recorded Holder(s) Noranda Exploration Company ,Address P.O. Box 1205, 60 Shirley St

'Limited (no personal liability)

. South,Mining DivisionPorcupine

Dates Work Frc Performed m: March

Timmins Ontario P4N 7J5Township/Area

ftsres/Se weU/Kenocra mincr/Penhorwood

Client No. 176208

Telephone No.

(705) 26R-QfinnM or Q Plan No.

M 1 074/G 3247/G 3239/G 324

30, 1992 To: April 4, 1992

Work Performed (Check One Work Group Only)Work Group

y

i. * Geotechnical Survey

Physical Work, i Including Drilling

RehabilitationOther Authorized Work

Assays

Assignment from , Reserve ,,. i i

Diamond I

"hhlTAnin CEOLOGiCAL SlIRVPYPUt****'*'*-' ULVL-v v*-"^*- ****i

CIS -ASSESSMENT FILES

rillin^jGtJoie^^NR 92-

—— RECEIVED ——*"~ r

01 , 397.0 metres

*. RECORDED s

Illl ^ 1 101?JUL 0 l \JJc-

Receipt

Total Assessment Work Claimed on the Attached Statement of Costs S 20.200.00

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

Bradley Bros. .Limited1 j .' :

i i

Address

48- 14th Street, P.O. Box 2367, Rouyn-Noranda, Que. J9X 5A9

(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

• i j 1 t OD *^*JV^\vi {^ 1 1 1 ^^ ^-

Recorded WMX or Agent (Signature)

lil.Certification of Work Report

l certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after Its completion and annexed report Is true.

Name and Address of Person Certifying -

W. Corstorphine c/o P.O. Box 1205, Timmins Ontario P4N 7J5elepone No.

(705) 268-9600

Date

For Office Use OnlyTotal Value Cr. Recorded Date Recorded

Deemed Date

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Sign

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Ontario

Ministry ofNorthern Developmentand Mines

Ministers du j/eloppement du Nord des mines

Statement of Costs for Assessment CreditEtat des couts aux fins du credit devaluation

Mining Act/Loi sur les mines

Transaction No./N" de transaction. caw

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 clalm(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 renseignements personnels contenus dans la presente formule sont recueillis en vertu de la Lol sur les mines et servlront a tenlr a jour un registre des concessions minleres, Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains miniers, minlstere du Developpement du Nord et des Mines, 159, rue Cedar, 4e etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/CoQts directs

Type

Wages Salalres

Contractor's and Consultant's Fees Drolls de I'entrepreneur et de 1 'expert- consell

Supplies Used Fournltures utilities

Equipment Rental Location de mattrlel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

Type

Diamond Drilling

Type

Type

Amount Montant

2,134.0C

17, 726. (

-

Total Direct Costs Total des coOts directs

Totals Total global

2,134.00

0

17,726.00

1^.,,,'Ô.f

19,860.0

2. indirect Costs/CoOts Indirects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les couts indirects ne sont pas admlssibles en tant que travaux d'evalualion.

Type

Transportation Transport

Food and Lodging Nourrlture et hibergementMobilization and Demobilization Mobilisation et demobilisation

DescriptionTypeTruck Rental/Gas

-Ts-fteeeftdm-| JUL311992

Receipt . ____

Amount Montant

340.00

r

Sub Total of Indirect Costs Total partial des couts Indirects

Amount Allowable (not greater than 20W of Direct Costs) Montant admissible (n'excedant pas 20 W des coOts directs)Total Value of Assessment Credit Valeur tolale du (Total of Direct and Allowable devaluation Indirect coat*) (Total del eoflti di

creditrecti

Totals Total global

340.00

340.00

340.00

2Q200.0(et Indirect! tdmlislblei

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

Note : Le titulaire enregistre sera tenu de verifier les depenses demandees dans le present etat des codts dans les 30 jours sulvant une demande a cet effet. Si la verification n'est pas effectuee, le mlnistre peut rejeter tout ou une partie des travaux devaluation presentes.

Filing Discounts Remises pour depot

1 . Work filed within two years of completion is claimed at 10007o of the above Total Value of Assessment Credit.

1 . Les travaux deposes dans les deux ans suivant leur achevement sont rembourses a 100 "A de la valeur totale susmentionnee du credit devaluation.

2. Work filed three, four or five years after completion is claimed at 5007o of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimedx 0.50

2. Les travaux deposes trois, quatre ou cinq ans apres leur achevement sont rembourses a 50 Vo de la valeur totale du credit devaluation susmentionne. Volr les calculs ci-dessous.

Valeur totale du credit devaluationx 0,50

Evaluation totale demandee

Certification Verifying Statement of Costs

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

that as Lands/Project Coordinator(Recorded Holder, Agent, Position In Company)

to make this certification

Attestation de l'6tat des coQts

J'atteste par la presente :que les montants Indiques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux devaluation sur les terrains Indiques dans la formule de rapport de travail ci-joint.

, am authorized El qu - 6 , itre de je suis autoris6(titulaire enreglstrd, repr6senlanl, poste occupd dans la compagnie)

a faire cette attestation.

Signature Date

0212 (04/91) Nota : Dans cette formule, lorsqu'il deslgne des personnes, le masculln est utilise" au sens neutre.

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REFERENCEAREAS WITHDRAWN FROM DISPOSITION

M.R.O. -MINING RIGHTS ONLY

S.R.O. - SURFACE RIGHTS ONLY

M.+ S. - MINING AND SURFACE RIGHTS

®

Description

400 RESERVE

SEC 43/70

SEC. 36/SO

Order No.

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ORDER OF THE MINISTER #33/87 DATED MARCH S O'fl?

WITHDRAWS MWWG AND SURFACE R*HTS UNDER SECTION

36 OF THE MINING ACT RSO '980

SAND AND GRAVEl

GRAVEL

GRAVEL PIT

GRAVEL

PILE 38729

FILE 15555 v.6

FILE I 06ZT4

QUARRY PERMIT *22B05 ISStlED FOR THE REMOVAL OF THE

OUARTZ JULY l M7.

QUARRY PtRMIT 9 22808 ISSUED F OR TME REMOVAL OF

QUARTZ 3EPT 10, 1 987

CANCELLED PATENT ANQ LEASED CLAIMS

i-THIS TWfi SUBJECT TO FOREST ACTIVITY IN 1992/93. FURTHER INFORMATION AVAILABLE ON FILE.

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER. MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON

REEVES TWP.

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LEGENDHIGHWAY AND ROUTE No. OTHER ROADS

TRAILS

SURVEYED L INES:TOWNSHIPS. BASE LINES, ETC.LOTS. MINING CLAIMS. PARCELS. ETC

UNSURVEYED LINES:LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY UTILITY LINES

NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES

TRAVERSE MONUMENT

OISPOSITION OF CROWN LANDS

SYMBOLTYPE OF DOCUMENT

PATENT. SURFACE A MINING RIGHTS.

" . SURFACE RIGHTS ONLY___.

.MINING RIGHTS ONLY____.LEASE, SURFACE ft MINING R IGHTS™

" , SURFACE RIGHTS ONLY.___." .MINING RIGHTSONLY.__,_.

LICENCE OF OCCUPATION ,. ORDER-IN-COUNCIL ___... RESERVATION ____....^

CANCE LLEO ^^,

SAND ft GRAVELt AND USE Pt'RMIT . Ifc-

MININO RIGHTS IN PARCELS PATENTED PRIOR TO MAY 6. 1913, V ESTED IN O RIGINAL PATENTEE BT THE PUBLIC LANDS ACT. R.5.O. 1970. CHAP. MO. M C. U. SUBSEC 1.

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AUG 101992

ACTIVATED ..ANUARY \O, i'l

TOWNSHIP

PENHORWOODM.N.R. ADMINISTRATIVE DISTRICT

CHAPLEAUMINING DIVISION

PORCUPINELAND TITLES/ REGISTRY DIVISION

SUDBURY

Ministryof L andNatural Management

Resources B ranchOntario

Olti MARCH 1985

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REFERENCES

AREAS WITHDRAWN FROM DISPOSITION

M.*.O. - MINING RIGHTS ONLY

i-R.O. - SURFACE RIGHTS ONLY

M.* S. - MINING AND SURFACE RIGHTS

ftmw CMwM*.

.mil

:!' 4 . .' , -, ' *-*3 i 35748

4 ,- * .'r- -'N * .W h 18S45

•*t1 l4S;;ow a ' k "O '3^/48

OU**** A l If- NUA l ION . jf*f

^^|Â'nO *' -l d B l 1 H M ) ^ H . MR

i *" 1 i or r M ' - "* a i AKINS PUNA VUH A f r i ICATJON UNDER

••irm H l ANl'B ACT

1MI-. l WT SUHJITT 10 f (WtST A(*1 IV ITY IN 1992/93.

l I IHTHI H I WOHMAT ION AVAILABLE ON FILE

M ' C P ^ ^T7

M l s. ":i J4-. ; IIF

M T \ "li ^?6

MELROSE TWP

ea 93

Q-

i-

FREY TWP

^ ^^ft^^^4^ i**Hft^4#4^ PJOTSft+p

;———-(---... — —

J— — — — -4- — — — J- — — — — — _ —.-H..— — l P****W PA4M* IP.B04623 P.80463* l P

| __ __ : __ 'j TT njTICT755311 l l ^- — | 904622 lp.867633 IP.9S7SJ4

I- - - — — 34 \ 'IP76S3I6 IP.7S53B ^ i" ~"~ J P~ ~ ~ ~

— tV "~ — ~1p~ '— — '""T — — ~ l*.' — l ' . - l

1177122 j I I769B6 j "76987 j H76980 \ \ *

i \•- . ,m*6 j I'77II9 1177123 i 1176985 l 1176984 | H769835r- \Affm! ^-———liW &JT4KT ' 4*79*n ^ 9472651 'P i P.

^969.7698,PHARAND

w-\ ^ \s^ *(.3[fVi

KENOGAMING TVVPOP

LEGENDHIGHWAY AND ROUTE No. OTHER ROADSTRAILS —SURVEYED LINES:

TOWNSHIPS. BASE LINES. ETC. - LOTS, MINING CLAIMS, PARCELS. ETC.-

UNSURVEYED LINES:LOT LINES — PARCEL BOUNDARY - MINING CLAIM^ ETC. —

RAILWAY AND RIGHT Of WAY -*-UTILITY LINES -"NON-PERENNIAL STREAM —FLOODING OR FLOODING RIGHTS ^SUBDIVISION OR COMPOSITE PLANRESERVATIONSORIGINAL SHORELINEMARSH OR MUSKEG ^r*MINESTRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT. SURFACE ft MINING RIGHTS ____ —™.- * .SURFACE RIGHTS ONLY....... ______ ..M. ^

" .MINING RIGHTS ONLY ^......,..^...... __ . OLEASE, SURFACE ft MINING RIGHTS....—.— — — ™ B

" .SURFACE RIGHTSONLY,.^....^...™.,...... B" .MINING RIGHTSONLY........ __ .. _ .......w. B

LICENCE OF OCCUPATION . __ . ____ ... ___ .. __ . T ORDER-IN COUNCIL ..^™. _ . __ ............ ......... OCRESERVATION _____ ........ _ ....^. ___ ...™. _ . (J)

CANCELLED ___ .—— ———.—............™..^.^ *;SAND ft GRAVEL _____ ... _ m -——— .--.^ ———— —— — — ——— ..,,

NOTE: MINING mOMTI IM PARCEL* PATSNTIO PfllOft TO MAY f, 1*13. VOTED IN OM4OIMAC PATiNTK* *V THC PUftttC LAMOt ACT. HA. O. ?*T#, CHAP MO, KC *3. *UBStC i,

SCALE: 1 INCH - 40 CHAINS

f ECTO 1OOO 2OOO 4OOO •000

O TOOl l KMI

MOO(7 *M

TOWNSHIP

SEWELLM.N.R. ADMINISTRATIVE D ISTRICT

TIMMINSMINING D IVISION

PORCUPINELAND TITLES/ R EGISTRY DIVISION

SUDBURYMinistryof t-*ndNatural ManagementResources Branch

Ontario

Oil* MARCH,1985

CHFCKED BYAtt^. PLACED ON .E 90/O5/O8.

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t f fei

42B01S1V8576 39 PENHORWOOD 220

o

JQ

O) LJ

!SLJ

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINtNG RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON

MELROSE TP. M.E61

9 N1

S M

7 M

1 P ioaaz9S|P.I073I7I i

IPI03S97 , l jP.I03597i-l

i j.Vt(6UN,TM

Vi?*™ i - rV** rtS. i t-'f

(p ' Q

0'- ©*.59023

-ENHORWOOD TP. M.IC5

THE TOWNSHIP OF

DISTRICT OFSUDBURY

PORCUPINE MINING DIVISION

SCALE: 1-INCH-4O CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RKSHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLED PATENTED S.R O.

NOTES

4-00 surface rights reserve*^ of oil lakes or-^

Areas withdrawn from staking und*r S*ction 43 ol the Mining Act (R.SO 1970)

Ne FM* Daft Ditpotition

W,48/72 July 27/72 S.R. * M.R.Sec. 43 of 1h* M ining Act R.S.O., 1 970 ( Se.d Orchard) 1*313}

SAND AND GRAVEL

M.T.C. PIT 3A2 FILE 1 49632

BflKaaghlt- UBM* V- iiî.-

CHFCKEO B Y MCR aUGU.ST 2 i"9O DLACEO ON ACTIVE f .r AUGUST g/ '90.

PLAN N0.- r\/; If JE ' V j*

ONTAR1O

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

q•;*.-f

"3

tf

•"ft

42B0ISW857B 29 PENHORWOOD 230

Documents

010 TOWNSHIP: Penhorwood REPORT NO: 29 · •Property —————NAT-JUVER Sheet No. ___S——— OF - Hole No ____NR-92?-! Depth 81 Lithology Description (colour, grain size,

010 TOWNSHIP: Penhorwood REPORT NO: 29 · •Property —————NAT-JUVER Sheet No. _S——— OF - Hole No __NR-92?-! Depth 81 Lithology Description (colour, grain size,