32Ei2seee73 se NOSEWORTHY 010DIAMOND

TOWNSHIP: NOSEWORTHY REPORT NO: 28

WORK PERFORMED FOR: Morrison Minerals Ltd.

RECORDED HOLDER: SAME AS ABOVE (xx)

: OTHER ( )

CLAIM NO.L1048177 L1048176

L1048185

HOLE NO.BB-89-02 BB-89-03 BB-89-04 BB-89-06

FOOTAGE101m 64m 69m

DATEFeb789 Mar/89 Mar/89 Mar/89

NOTES: (1) # W8908.302, filed Nov/89 (2) # W8908.305, filed Nov/89

APPENDIX C

DIAMOND DRILL LOGS

i

DDH BB-89-02, 03 AND 04

MMttyof Northern

Diamond Drilling

)JJ5riO 1*9 CMWtoMlMtfMMMrf WHnO* A

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———————!——————————————————;—————————

ssw, 325 0

. O. H.

AUROGIN RESOURCES LTD

BURNTBUSH AREAPROJECT 490

DRILLB8- 99 - 03 BB - W

SCALE l ! 500DRAWN BY:

n89CHECKED:

AUROGM RESOURCES IK. Noseworthy, Hurtubise IMPS, t Chabbil Like Aril

5mtrjLiOUip.Qi.6r.ULtt6aF.ilMARCH 1

(88-89-01 to B

TOTAL OVERBURDEN DEPTH downhole/vertical DATE DATE CLAIM

DDK NO. A1IIWTH DIP (i) (letres) STARTED COMPUTED NO.

16-89-01 -- -900 111.5 37.5/37.5 02/26/89 02/27/89 10482J1 east of Chabbii like

88-85-02 - -10" 101.0 18.5/18.5 02/27/89 02/28/89 1048177 '1851 nest

of Railage l.noseworthy Tup".

BB-89-OJ 055 -600 65.0 42.4/38.0 03/01/89 03/02/89 1048176 noseworthy Tup. *450i NH of Ranage Like

JB-89-04 - -90* 69.0 41,5/41.5 03/02/89 03/03/89 1048176 (sue Noseworthy Twp. set-up as 68-89-03) *450i Nw of

Ranage lake

989 8-89-06)

LIIHOL06IES

0-37.0 overburden 37.0-63.9 eg altered ultraiafie intrusive

(tilcosi-biotite-cirbonate rich), strongly lagnetic

63.9-69,0 as above, less altered with granophyric segregations

69.0-91.0 divine-rich ultniific phase with linor talcose altered inter vals

91.0-lll.S iific tuff, biotite

0-18.5 ovirburden 18.5-85.0 e.g. talcose uHraiafic, strongly

limnetic 78.0-85.0 contact zone with quartz

pyroxene pegiititic zone, linor garnets, tr py

85.0-101.0 fine-grained greywacke, quartz- biotite rich

0-42.4 overburden 42.4-42.9 'pegiatitic' quartz and pyroxene 42.9-64,0 ticacious fine-grained greywacke

0-41.5 overburden 41.5-58.0 altered ultraiafic (talcose)

56.2-58.0 contact zone; pegiatitic quartz-fsp-pyroxene

SAHPIES (NO CORE)

16kg saiple, 37. 0-79. Oi for disaggregation l diaiond analysis (88-89-01) -EE-890203 101.5-102.0 for Au, ICP EE-890204 97.5- 98.0 for Au, ICP EE-890202 72.1 whole rock analysis

(340S lagnetic anoialy)

16kg saiple, 20. 0-69. 5i for diaiond analysis (88-89-02)

EE-890201 28.4 whole rock analysis -EE-890205 50.0-50.5 for Au, ICP

(1150? lagnetic anoialy)

-TBB-89-03-001 40. 0-40. 3i 1 41. 0-41.851 till and basal till saiple for HH analysis

(1040y lagnetic anoialy)

(1040JT lagnetic anoialy)

58.0-69.0 fine-grained greywacke, linor siliceous dikes

MIROSIH RESOURCES LTD.

Nosexorthy, Hurtubise lnps. t Chabbie lake Area

SuinnLp.tIUiMOrJlLtt.aauiMARCH 1989

DDH NO. AZIHUTH DIP

TOTAL OVERBURDENDEPTH donnhole/vertical(i) detres)

DATE DATE STARTED COMPUTED

CIAINNO. IITHOIOGIES SAMPLES

88-89-05 - -90* 114.5 34.5/34.5 03/03/89 03/05/89 1048227south oh Chabbbie laki

O-34.S overburden34.5-114.5 olivine-rich ultraeafic intrusion

inhoiogeneous., included fragientsf?) of utasediients and ultruafics abundant granophyric segregations, ft* siliceous dikes

8kg saiple, 34.5-100i for diaiond analysis (66-89-05)

(500* tagnetic anoialy)

88-89-06 - -90" 86.0 43.5/43.S 03/06/89 03/07/89 1046165SK of Chabbie lake

0-43.5 overburden 43.5-86.0 c.j. ultraiafic intrusion

43.5-56.0 ueathered, cruibly in parts, clay-rich olivines preferen tially withered

56.0-86.0 peridotitic (pyroxene rich, *ith olivine less abundant donnhoU)

8kg taiple, 44.S-6S.Oi for diaiond analysis (86-89-06-01)

-8kg saiple, 65,0-86.Oi for diaiond analysis (88-89-06-02)

(SSOlf lagnetic anoialy)

86-89-07 -90" 46.5 24.5/24.5 03/09/89 03/10/89 1048165Hurtubise Twp.

0-24.5 overburden24.5-46.5 fine-grained tafic volcanic, very

linor dissei py, Ir cpy(2S05f lagnetic anoialy)

86-89-08 -90* 59.0 18.5/18.5 03/11/89 03/12/89 1048514Hurtubise Tup.

0-18.5 overburden18.5-59.0 fine-grained lafic intrusive, strongly

lagnetic, systei of fibrous talcose)?) o.tt-carb veinlels, no associated nail

(1950tf lagnetic anoialy)

Total 652.51

' \ ,V ^,_^—-'l /' \ . r'/' 1 - -'

•y A^

AUROGIN RESOURCES LTD.

Noseworthy Twp. Rammage Lake Area

Airborne Magnetic Signature Target BB-89-02

AUROGIN RESOURCES LTD.

Noseworthy Twp. Rammage Lake Area

Airborne Magnetic Signature

Targets BB-89-03 ^ BB-89-04

•set*.

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Lake

BASE LIME

AUROQIN'RESOURCES LTDBURNTBUSH AREA

PROJECT 490

SCALEDRAWN BY: CHECKED:

our.'.'

DDH -86-69

SCALE

AUROGIN RESOURCES LTDBURNTBUSH AREA

PROJECT 490ll firjet Mb- 3

Mtyxtt/c* Sut-**fta-n-o* (-iof ~)AA -91-O f tvtrite*!)

PRAWN BY: E.G. l CHECKED:

CONTOUR INTERVALMM.

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Ministry olNorthern Developmentand Mines

Ontario

DiamondDrillingLog

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AUKOG3N KKSOUKCKS LTD.

Chabbie Lake Area

Airborne Magnetic Signature

Target HH-89-06

,, nz ^,

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DDH BB-89-06

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PROJECT 490

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J

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AUROGIN RESOURCES LTDBURNTBUSH AREA

PROJECT 490

66-11-06*

SCALEPRAWN BY: f .

DATE:CHECKED:

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TABLE OF CONTENTS

Introduction

Previous Work

Location and Access

Field Methods

Preliminary Results

Conclusions and Recommendations

l

l

l

3

3

4

Appendix A

Appendix B

Appendix C

Appendix D

Table l

Figure l

Figure 2

- Petrographic and Hand Specimen Descriptions

- Airborne magnetics and Ground Magnetometer Surveys

- Diamond Drill Logs

- Analytical Results

- Summary of Diamond Drill Holes

- Target Location Map 1:250,000

- Diamond Drill Hole Location Map 1:50,000

Introduction

Aurogin Resources Ltd. drilled seven airborne magnetic targets, located approximately 50 kilometres northeast of Cochrane, Ontario. These targets were considered to have significant potential as diamondiferous kimberlite pipes.

Eight (8) diamond drill holes totalling 652 metres, recovering NQ core, were drilled between February 24 and March 12, 1989.

This drilling fulfills part of an option agreement between Aurogin and Morrison Minerals Ltd. whereby Aurogin can earn a 5(^ interest in the properties by drilling one hole on each of 12 targets and 1000 feet of follow-up drilling for each pipe that is confirmed as kimberlitic.

Previous Work

The targets were identified from a regional detailed helicopter- borne, high sensitivity magnetics survey flown by Aerodat Ltd. of Mississauga in 1986. This survey presented the twelve distinct circular magnetic "thumbprint" signatures in this area northeast of Cochrane. Only seven of these twelve targets were drill tested by this initial drill program (see Figure 1).

Location and Access

The targets are located in clusters across 25 kilometres in Noseworthy and Hurtubise Townships and the Chabbie Lake Area, within the Cochrane Mining Division.

Drilling was performed by Bradley Bros. Ltd. of Noranda, Quebec. Drill supervision was provided by the author with assistance from Steve Dawson, both of Aurogin Resources Ltd. Drill crews and Aurogin's geological crew were accomodated at a pre-existing Bradley camp located on the Inco Golden Pond road, accessible by all weather road from LaSarre, Quebec. Dave Rogers of Aurogin Resources Ltd. and Wally Boyko of Morrison Minerals Ltd. had the opportunity to visit the camp and examine core while the program was in progress.

Access to the property, as well as drill moves, was via helicopter based at the Bradley camp (Nordic Helicopters Ltd., LaSarre, Quebec). Ferrying distance to the drill sites ranged from 30 to 41 kilometres.

]W^^r-"f-8i H -" . "k.J K - A- - '

-- i Y \'H)ml"n.im.''-A J j',! ,',' ,-J

0 Targets drill tested

Q Targets not drilled

AUROGIN RESOURCES LTD.

NOSEWORTHY S. HURTUBISE TWPS. AND CHABBIE LAKE AREA

DRILL HOLE LOCATION MAP

Scale 1:250,000 Mar 1989

Field Methods

The magnetic targets were located as accurately as possible from airphotos. A detailed ground magnetometer survey was done on each target area to accurately pinpoint the magnetic features on the ground. A Scintrex MP-2 Proton Magnetometer was used with frequent loops to a base station, to correct for diurnal variation. Most surveys were done over a couple hours/ so drift was not significant. Magnetic readings were generally taken at 10 metre intervals over pace-and-compass grids, until the targets were confidently located. Results of these magnetic surveys are shown on accompanying maps (Appendix B).

The magnetic anomalies ranged from 250 gammas (no. 7} to 1950 gammas (no. 8). Several of the "bull's eye" airborne anomalies could be resolved by the ground survey into more than a single magnetic high, with intervening lows.

In almost all cases, the drill holes were positioned directly over the maximum magnetic peak and drilled vertically. In several instances foresite and backsite pickets were established for potential inclined holes not requiring a drill move, should the initial vertical holes prove to be encouraging.

Overburden thickness ranged in the drill holes from 18.5 to 43.5 metres. A basal till sample was cored in hole BB-89-03. The till interval was sampled and panned for heavy minerals and examined for the presence of indicator minerals.

Preliminary Results

Details of each drill hole have been tabulated (see Table 1) . Drill logs appear in Appendix C. A cause for each of the seven magnetic highs was found.

Lithologies intersected in holes BB-89-01 (Chabbie Lake area), 02, and 04 (Rammage Lake, Noseworthy Twp.) are remarkably similar: a relatively homogeneous, massive, medium to coarse-grained ultramafic rock with moderate to extensive talcose and carbonate alteration which is associated with magnetite enrichment. In each of these holes fine-grained greywacke to tuffaceous sediment was intersected on the footwall of these mafic intrusive units.

Hole BB-89-05 (on Chabbie Lake) intersected highly heterogeneous lithologies. The slightly talcose-altered mafic intrusive contains strongly biotitized sediment horizons and/or fragments. Strongly magnetic, mylonitized horizons occur in abundance. Some contacts suggest fragmentation. Granophyric segregations and siliceous granitic dikes (?) become abundant downhole, as do biotitic sediment units or fragments.

Hole BB-89-06 intersected a less altered, massive, homogeneous, medium to coarse-grained pyroxenite (?). The upper 15 meters is quite weathered, breaking down into fine nodular rubble with interstitial bluish clay.

Hole BB-89-07, in Hurtubise Township, tested a more complex magnetic anomaly. A weaker magnetic high located near a weak airborne electromagnetic anomaly was drill tested. Fine-grained andesitic volcanic rock was intersected, containing up to X/2% finely disseminated pyrite and a trace of chalcopyrite. The upper 15 metres is denser, finer-grained and moderately magnetic.

Hole BB-89-08, in Hurtubise Township, tested a strong bull's eye magnetic anomaly. Strongly magnetic, coarse-grained, dark green chloritized gabbro was intersected. Narrow fractures contain fibrous serpentine, no wallrock alteration is associated.

Samples of the ultramafic intrusive in holes BB-89-01, 02, 05 and 06 were taken for disaggregation with caustic acid treatment and examination for diamonds at Lakefield Research Labs in Lakefield, Ontario. Representative pieces were taken at regular intervals to give 8 kg samples (see details on Table 1) or in hole BB-89-01, a 16 kg sample. Only a small quantity of residue was returned. No microdiamonds were identified in these residues. A brief description of these residues appears in appendix A.

Thin sections and hand samples were examined by Bruce Jago at the University of Toronto. Petrographic and hand sample descriptions follow in Appendix A.

CONCLUSIONS AND RECOMMENDATIONS

Initial analytical work on samples from the magnetic targets tested to date, has not yielded diamonds. The significance of the five untested pipe structures and a number of additional targets defined by the magnetic survey are being evaluated.

The northern holes showed more encouragement than the southern holes. Mafic to ultramafic intrusives were intersected in all of the northern holes.

No true kimberlitic rocks were associated with the seven magnetic targets drilled to date in this Burntbush area.

APPENDIX A

PETROGRAPHIC AND HAND SPECIMEN DESCRIPTIONS

Bruce Jago is presently working on his Ph.D. on calc-alkaline rocks and is continuing his research on kimberlites under Dr. John Gittens at the University of Toronto. Bruce completed his M.Se. on kimberlites at Lakehead University under Dr. Roger Mitchell, noted for his work on kimberlites. Bruce has had the opportunity to examine kimberlites and lamproites in the Kimberley area of South Africa, Argyle area of Australia and Somerset Island, Canada.

Petrographic Services 1517 -35 Charles Street , West, Toronto, Ontario, M5 S 1A1

March 28, 1989

Elaine EllinghamDuration Mines Limited,704 - 80 Richmond Street , West,Toronto, Ontario,M5H 2C7

Dear Elaine,

Please find attached the petrographic and handspecimen descriptions that you requested. None of the samples are of kimberlite nor even of weakly alkaline character. The protolith to these samples ranges from pyroxenite to gabbro to diorite although this can not be confidently ascertained in all cases. All rock samples have been altered to some extent although samples BB89 -01 - 72.5, BB89 - 01 - 79.0 and BB89 - 05 - 42.5 are relatively fresh. Others are intensely altered. In general, the alteration assemblage consists of chlorite - actinolite */- biotite */- calcite */- talc -t-/- pyrite. The relict primary minerals are pyroxene, apatite, zircon and rarely plagioclase. Magnetite occurs in only a few samples and imparts a weak to moderate magnetism.

I hope these reports meet with your satisfaction and that you will contact me if you or your collegues have any questions.

Yours truly,

Bruce Jago, H.B.Se.,M.Se. Consulting Petrologist

Number:BB89 - 01 - 72.5m

Rock Name: Pyroxenite

Rock Description:

This sample of drill core is a very grained, strongly inequigranular, dark hornfelsic and poikiloblastic - textured, rock. The mineralogy is dominated poikiloblastic amphibole and generally

dense, medium to coarse green to black coloured, basic igneous intrusive

by very coarse grained, interstitial, very fine

grained pyroxene. The amphibole is secondary and the sample is weakly carbonatized.

Thin Section Description:

In thin section, the primary mineralogy is dominated by weakly to moderately uralitized, fine grained, sub - equant to sub - prismatic, augite to ferroaugite with lesser, very coarse grained, weakly poikilitic and weakly to strongly sausseritized interstitial plagioclase, interstitial zircon and apatite and possible, relict orthopyroxene of indeterminable composition. Although the composition of the plagioclase can not be determined, it probably is an andesine to labradorite. The secondary mineralogy is dominated by very coarse grained, poikiloblastic, actinolitic amphibole with lesser calcite and sausserite. Actinolite has grown at the expense of augite and possibly orthopyroxene, although the former presence of the latter can not be determined positively.

Minerals Present

Augite - ferroaugiteOrthopyroxeneZirconApatitePlagioclaseActinoliteCalciteSausserite

Percent Abundance

60 - 65

Trace - l 5 - 7 30 - 351 - 22 - 5

Status

PrimaryPrimaryPrimaryPrimaryPrimarySecondarySecondarySecondary

Number :BB89 - 02 - 82.5m

Rock Name:Basic intrusive (see last paragraph this report)

Rock Description:

No rock provided for description.

Thin Section Description:

The primary mineralogy of strongly sausseritized, very inhomogenous, highly strained, indeterminable composition, grained, anhedral and broken partially resorbed zircon and igneous textures are poorly development of secondary minerals anisotropic metamorphic fabric

this sample now is dominated by coarse grained, compositionally

relict, poikilitic plagioclase of lesser but significant, coarse

prismatic apatite, anhedral to trace amounts of opaque. Relict preserved due to the strong

and to a strong, inhomogenous, The secondary mineralogy is

dominated by very coarse grained, randomly and strongly orientated, strongly intergrown, poikiloblastic actinolitic amphibole and biotitic mica with lesser, coarse grained, interstitial, poikilitic calcite and abundant sausserite. Radiation halos are weakly to strongly developed around zircon included in actinolite and biotite.

It is not possible to determine all of the primary silicate minerals due to the very coarse grained and very strongly developed secondary ferro - magnesian mineral assemblage. However, the primary assemblage probably would have included either or both of hypersthene and augite, minerals which are easily altered to actinolite and biotite under hydrous metamorphic conditions. The prolith probably was a pyroxenite, gabbro or ferromagnesian - rich diorite.

Minerals Present

PlagioclaseApatiteZirconOpaqueActinoliteBiotiteCalcite

Percent Abundance

40 - A51-21-2Trace - l35 - 4015-202-5

Status

PrimaryPrimaryPrimaryPrimary (?)SecondarySecondarySecondary (?)

fample Number:BB89 - 03 - 51.0m

Rock Name:Talc - chlorite - actinolite - pyrite hornfels

Rock Description:

This sample of drill core is an hornfelsic textured, talc- chlorite - actinolite - pyrite rock of probable basic, igneous intrusive origin. Very coarse grained, strongly intergrown poikilblastic talc and chlorite dominate the sample with lesser, fine grained, subhedral to euhedral pyrite and actinolite.

Thin Section Description:

Apatite as coarse, strongly resorbed prismatic grains and medium grained, anhedral zircon are the relict primary minerals in this thin section. The secondary silicate mineralogy is dominated by extremely coarse grained, strongly foliated and highly intergrown, porphyroblastic chlorite and muscovite, a member of the actinolite - tremolite series and very fine grained, highly intergrown porphyroblastic talc. Actinolite/ tremolite assemblages are growing at the expense of chlorite. The opaque mineralogy is dominated by fine to very coarse grained, poikiloblastic pyrite and very fine grained, anhedral magnetite. The latter occurs primarily along cleavage planes in highly strained amphibole.

Minerals Present

ApatiteZirconChloriteMuscoviteTremolite/ActinoliteTalcPyriteMagnetite

Percent Abundance

Trace - l Trace - l 40 - 45 20 - 25 15-20 10 - 15 1-2 Trace

Status

PrimaryPrimaryPrimarySecondarySecondarySecondarySecondarySecondary

Handspecimen Description^

The mineralogy of these handspecimens is, in part, interpreted from the examination of thin sections BB89 - 01- 72.5, BB89 - 02 - 82.5 and BB89 - 03 - 51.0.

Handspecimen number:BB89 - 01 - 79.0m

This sample of drill core is a very dense, medium to coarse grained, strongly inequigranular, dark green to black coloured, hornfelsic, basic igneous intrusive rock. The mineralogy is dominated by very coarse grained, poikiloblastic amphibole, very fine grained, roughly equigranular pyroxene and irregular, interstitial calcite. Brown, lensoid - shaped grains may be zircon. The amphibole is secondary, the sample is weakly carbonatized and non - magnetic.

The protolith to this sample probably was a pyroxenite.

Handspecimen number:BB89 - 02 - 22.0m

This sample of drill core is a dark to medium - green, hornfelsic intergrowth of very coarse grained, porphyroblastic, platey green chlorite and brown biotite, prismatic actinolite and fine grained, felted interstitial chlorite - actinolite - talc (?) assemblages. Highly irregular, light green patches may be relict, now intensely sausseritized plagioclase. The rock is moderately magnetic and pyrite occurs as fine to medium grained, anhedral to subhedral grains and cubes. All silicate minerals in this sample, with the exception of relict plagioclase are secondary.

The protolith to this sample probably was a gabbro, pyroxenite or pyroxene - rich diorite.

BB89 - 05 - 42.5

This sample of drill core is a medium grained, green and white mottled, hornfelsic intergrowth of hypidiomorphic, dark medium to dark green, equant to prismatic, actinolitic amphibole, brown platey biotite, fresh to strongly sausseritized, inter stitial, irregular to sub - prismatic plagioclase and rare, lensoid - shaped, brown zircon. Biotite, amphibole and sausserite assemblages are secondary while zircon and plagioclase are primary. The sample is not magnetic and does not react with 5 % hydrochloric acid.

The protolith to this sample probably was gabbro or pyroxene - rich diorite.

a pyroxenite,

.BB89 - 05 - 73.5m

This sample of drill core is a weakly carbonatized, relict porphyritic textured, muscovite - bearing equivalent of sample BB89 - 05 42.5. The strongly zoned crystals are intensely sausseritized and biotized, relict, possibly zoned plagioclase phenocrysts. The matrix mineralogy has been altered to a hornfelsic intergrowth of primary zircon, possible relict primary plagioclase which has been strongly sausseritized and porphyroblastic actinolite and biotite. The rock is not magnetic and reacts very weakly with 5 % hydrochloric acid.

The protolith to this sample gabbro or pyroxene - rich diorite.

BB89 - 05 - 85.25m

probably was a pyroxenite,

This sample of drill core appears to be compositionally and texturally equivalent to the matrix of sample BB89 - 05 - 73.5. The sample is bounded at one end by a muscovite - chlorite - rich fracture surface and is traversed at the other by a four to five centimeter wide zone of intense ductile deformation. Within this zone, chlorite - rich folium are strongly developed as are sub- equant to augen - like porphyroblastic plagioclase (?). The latter are weakly to moderately sausseritized and rotated in the strongly foliated, chlorite - rich matrix. The sample is weakly to moderately magnetic and does not react with 5 % hydrochloric acid.

The protolith to this sample probably was a pyroxenite, gabbro or pyroxene - rich diorite.

BB89 - 06 - 47.5m

This sample of drill core is a light yellow to dark green mottled, coarse grained, hornfelsic intergrowth of weakly to moderately chloritized (?), porphyroblastic actinolitic amphibole and interstitial, wholly sausseritized plagioclase. Relict igneous textures are poorly preserved to absent and primary minerals are not preserved. The sample is not magnetic and it reacts strongly with 5 % hydrochloric acid.

The protolith to this bearing pyroxenite or gabbro.

sample probably was a plagioclase-

- 06 - 50.15m

This sample of drill core is a less intensely chloritized (?) and sausseritized , mineralogical equivalent of sample BB89 - 06 - 50.15. In spite of the less intense nature of the alteration, no primary minerals are preseved. The sample reacts vigorously with 5 X, hydrochloric acid and is not magnetic.

The protolith to this sample probably was bearing pyroxenite or gabbro.

a plagioclase-

LAKEFIELD RESEARCHA DIVISION OF FALCONBRIDGE LIMITED

PHONE (705)652-3341 TELEX NO. 06962842

FACSIMILE NO. (705) 652-6365

March 21, 1989

Mr. D.P. Rogers Aurogin Resources Inc. Suite 70480 Richmond St. West Toronto, Ontario M5H 2C7

Dear Mr. Rogers:

The enclosed vials contain the residues from the first five samples treated by caustic fusion. As I reported by phone, no microdiamonds are present in any of the samples. We will store the additional crushed, untreated samples from BB8901 (~5 kg) and BB8902 (~ 8 kg) as you requested.

In addition to some spinel, mica or chlorite and traces of a white, clear mineral (zircon?), the residues may contain a white powder from the chemical reaction, metal scale from our pots, and traces of plastic from the impeller of the stirrer used when we water leach the fusion product. A few coarse rock particles remain which may have been protected somehow from complete dissolution.

Yours truly

LAKEFIELD RESEARCH

RB:jm Encl.

R. Buchan, P. Eng. Head, Mineralogy

185 CONCESSION STREET, P.O. BOX 430 LAKEFIELD, ONTARIO, CANADA KOL 2HO

DESCRIPTION OF RESIDUES

BB-89-01 sample contains minor apatite, biotite, spinel, few sulphide grains, few "clean" striated plagioclase grains and a tourmaline fragment

BB-89-02 grains identified include apatite, a small yellowish zircon euhedra, quite a bit of magnetite and 3 reddish probable garnet grains (Fe-rich) could be of metamorphic origin (?)

BB-89-03 abundant orange ragged grains are probable brick contaninant, abundant cloritized mica

BB-89-06-02 minor contaminants, also black glassy non-magnetic grains fairly common

Note: most samples contain a significant quantity of contaminants introduced during the caustic acid dissolution. These include metal scale flakes, blue plastic shavings, translucent rod to tear-shaped grains etc.

APPENDIX B

AIRBORNE MAGNETICS, AIRPHOTOS AND GROUND MAGNETICS MAPS

APPENDIX D

ANALYTICAL RESULTS

•k wm 1S& feh H ttChemex Labs Ltd.

A(*iy*f*4SO MATHESON BLVD.,B.. UNIT 14, MISS ISSAIKH ,

ONTARIO. CANADA I.4Z-IRJ

PHONE (416) 190-0)10

To.AUROGIN RESOURCES LTD.

704 - 10 RICJM3ND ST. , W.TORONTO, ONM5H 2C7

ProJ*cl : BBUSH Common: ATT'N: K KU.INOHAM

**P*|C NoTot. DU t Invoice t : P.O. f

CERTIFICATE OF ANALYSIS A8 9 l 268 3

SAMPLE DESCRIPTION

EE-890201 EE-890202

PREP CODE

205 205

232 232

SiO296

51 .80 41.09

A12O396

6.24 7.00

Fe2O3i

6.05 10.79

r15.66 24.39

C*O

^16.85 4.16

Na2O96

1.16 0.26

K2O36

0.66 1.91

TiO296

0.34 0.33

*

P20596

< 0.01 0.04

MO96

0.12 0.15

BaO96

0.02 0.04

LOI96

1.82 8.00

TOTAL96

100.75 98.16

/7

CKRTIHU'ATION

Chemex Labs Ltd.450 M4THKSON BLVD.. E.. UNIT (4.

ONTARIO. CANADA UZ-IRJPHONE (416) 190-0110

To:AUROOIN RESOURCES LTD.

704 - tO RICHMOND ST.. W. TORONTO, ON MSH ZC7Coontail: ATT'N: E ELLINGHAM

A8912684

CERTIFICATE A8 9 1 2 6 8 4

Al'ROOIN RESOURCES LTD.

PROJECT : BBUSH

P .OH :

Samp l ei inbmitted to our lab in Mitiiiiauga, ON. Tbii report vat printed on 16-MAR-8 9.

SAMPLE PREPARATIONCHEMEXCODE

2052 3 2

NIMBERSAMPLES

33

DESCRIPTION

Rock Geochcm: Cruih.ipHi.rinj jTotal ICP digeition

* NOTE l:

The 32 element ICP package it luiiablc for trace metal i in toil and rock lamplei. Element! (or which the nitric-aqua rejia diccttion it potiiblr incomplete are: Al, Ba. Bc. Ca. Cr, Ga. K. La, Mj. Na, Sr, Ti. TI . W.

CHEMEX CODE

I OOS 545 565 585 595 6056 15 6 256 35 6456 5566568569

707 27 37 5767 778

5 795S 25 S J584

NXMBER SAMPLES

3333333333333j33333333333

ANALYTICAL PROCEDURES

DESCR 1 PT 1 ON METHOD

Au ppb: Puie 10 g sample FA-AASMo ppm: 24 element, rock A core ICP-AESW ppm: 24 element, rock A core ICP-AESZn ppm: 24 element, rock A core ICP-AESP ppm: 24 element, rock A core ICP-AESPb ppm: 24 element, rock A core ICP-AESBi ppm: 24 element, rock A core ICP-AESCd ppm: 24 element, rock A core ICP-AESCo ppm: 24 element, rock A core ICP-AESNi ppm: 24 element, rock A core ICP-AESB* ppm: 24 element, rock A core ICP-AESPe %•. 24 clement, rock A core ICP-AESMn ppm: 24 element, rock A core ICP-AESCr ppm: 24 clement, rock A core ICP-AESMI 9b: 24 element, rock A core ICP-AESV ppm: 24 element, rock A core ICP-AESAl *to: 24 element, rock A core ICP-AESBe ppm: 24 element, rock A core ICP-AESC* ty. 24 element, rock A core ICP-AESCu ppm: 24 clement, rock A core ICP-AESA| ppm: 24 element, rock A core A ASTi •*: 24 element, rock A core ICP-AESSr ppm: 24 element, rock A core ICP-AESNa ft: 24 element, rock A core ICP-AESK 'ft: 24 element, rock A core ICP-AES

DETECTION LIMIT

51

102

IO22

0. 511

100.01

11

0.011

0.010. 5

0.01l

0. 5O.OI

10.010.01

UPPER

LIMIT

10000 10000 10OOO 10000 10000 10000 10000 10000 10000 1OOOO 1000025.0 10000 1000025.0 1000025.0 1000025.0 10000

200 10.00 10000 10.0020.0

Chemex Labs Ltd.CltwnUI* * 0*oolM*iUtt *

410 MATHESON BLVD.. E.. UNIT 14, MISS ISSAlOA , ONTARIO, CANADA L4Z-UJPHONE (416) 190-0110

To :AUROGJN RESOURCES LTD.

704 - 10 RICHMOND ST. , W.TORONTO, ONM5H 2C7

Projtci : BRUSH Common: ATT'N: EELLINOHAM

••Pate No. -.t-A To). P*j*i) D* l e Invoice P.O. l

CERTIFICATE OF ANALYSIS A8912684

SAMPLE DESCRIPTION

EE-890203EE-890204EE-890205

PREP CODE

205205205

232232232

Au ppb FA+AA

< 5< 5< 5

M) ppm IW ppm (ICP) ,(ICP)

,

223

< 10< 10< 10

Zn ppm (ICP)

51106456

P ppm (ICP)

630860590

'

Pt ppm (ICP)

1246

146

Bi ppm Cd ppm (ICP) (ICP)

!

11

242

< 0.5< 0.5

0.5

Co ppm (ICP)

151123

Ni ppm (ICP)

492979

'..;

Ba ppm (ICP)

820350

1250

t

v .

Fe % (ICP)

2.502.783.44

Vii ppm (ICP)

359455436

Cr ppm (ICP)

141235256

CERTIFICATION

Chemex Labs Ltd.To:AlROGlN RESOURCES LTD.

Analytic*! CtttffW*!* * 0*ooD*ml*U * ft*gl*tM*d4SO KUTHESON BLVD., E., UNIT 54, MISSI SSAIOA .

ONTARIO. CANADA L4Z-IR5PHONR (416) 190-0)10

704 - 10 RIOMCttO ST. TORONTO, ON M5H 2C7

PioJ.el : BRUSHConnwnl*: ATT'N: E ELI.INUHAM

W.

••Pai* No. :l Tol. Pt|Ci l Dtlt Invoice P.O. l

CERTIFICATE OF ANALYSIS A8 9 1268 4

SAMPLE DESCRIPTION

EE-890203EE-890204EE-890205

PREP CODE

205205205

232232232

Vfe ?6 (ICP)

1.721 .151 .81

V ppm (ICP)

4671

104

Al 96 (ICP)

7.775.627.94

Se ppra (ICP)

6.040.0

138.0

Ca 96 (ICP)

1.493.281.45

C\i ppm (ICP)

293866

Ag ppra !TI *ft AAS (ICP)

< 0.5< 0.5< 0.5

0.220.230.39

Sr ppra (ICP)

719521424

Na 96 t ICP)

3.061.582.24

K 96 (ICP)

1.880.863.70

.ft ———

CERTIFICATION :

RESOURCES

Suite 70480 Richmond Street WestToronto. Ontario, Canada M5H 2C7

Tel. (416) 362-1474 Fax. (416) 362-1933

Gordon Stollery,ChairmanMorrison Minerals Ltd.,1501 - 200- King Street West,TorontoM5H 3T4

April 3, 1989.

ASSESSMENT FILES OFFICE

NOV021989

R E C E t V ED

Dear Gordon:Please find enclosed one copy of our report covering thediamond exploration play.

Unfortunately, the northern group of targets turned out to be barren pyroxenites and the test work gave no real encouragement. I want to reflect on the data and program for a while in order to determine if there is any further

work warranted.

Many thanks for your co-operation on this project.*J aa l ^ V

Yours truly,

David P. Rogers Aurogin Resources Ltd,

DOCUMENT No.

DOCUMENT No. .303

DOCUMENT No.FDOCUW8S

|**a*t*w*^v*-

DOCUMENT No

L-s

3, -Ut

MinistryNorand

ilppment

fttario

Report of Work

900lame and Vo'stel Address of Recorded Holder ^-.^.—-^^

(MINERAUX MORRISON LTEE ) MORRISON MINERALS LIMITED

C. P. 1657, Val-d'Or (Quebec)

Prospector's Licence No.T4969

J9P 5Y9Summary of Work Performance and Distribution of CreditsTotel Work Oays Cr. claimed

767.70tor Performance o* the following work. (Check one only)

Q Manual Work

Qshaft Sinking Drifting or other Lateral Work.

Q Compressed Air, other Power driven or mechanical equip.

Q Power Stripping

|Diamond or other Coredrilling

Land Survey

All the work was performed on Mining Claim(s): L 1048136Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)

Hole # BB 89-02; BB 89-03; BB 89-04

Drilling date: March 1989

Drilling Co.Bradley Bros LtdDrilling Date: March 1989

Exploration C.: Aurogin Resources Ltd Suite 70480 Richmond Street W. Toronto (Ontario) M5H 2C7

RECORDED^K-

AUG 25 1989

Certification Verifying Report of Workl hereby certify that l have a personal and intimate knowledge of the facts set forth in the ftepon of Work annexed/hereto, Inavmg performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person Certifying

Jacquelin Gauthier; Mineraux Morrison Ltee C.P. 1657 Val-d'Or (Quebec).-- ...~ Oat! Certified ^ Cert/ffed b/lSttnasanit"' jffl^J9P 5Y9

Table of Information/Attachments Required by the Mining Recorder

DSU'-!??!?|r\S ~' ' ' ' t' **~, s

UU .... i

ta of Report

March 1989

Type of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Power Stripping

Oinmond O' other cor*

—————————— ~ ——————— ——————

Specific information par type

Nil

Type of equipment

Type of equipment and (mount expended. Not*: Proof of actual cost mutt be submitted within 30 day* of recording-

S'enea core log .nowing. roai*e*. diameter ofrn,r number and Irvglm Of hole*.

————————————————— ———————— —————— m

f VOther information (Common to 2 or more types)

Name* and addresses of men who performed manual work /operated equipment, together

Names ana addresses of owner or operator together with dates when drilling/strippingdone.

- Mi!

Attachments

Work Sketch; these •r* required to (how

extent of work In relation to the

Work Sketch (as ebove) In duplicate

Nil

Mmistry olNorthern Developmentand Mines

OntarioMining Aet

Instruction* - Supply required data on a leparate form for each type of work to be recorded (tee table below).

- For Geo-tichnic*! work uti form no. 1362 "Report of Work (Geological, Geophysical, Geochemical and Expenditure*)".

lame end Pottai Address of Recorded Holder MDRRTCinM MTMRDATC ITMTTCn(MINERAUX MORRISON LTEE ) MORRISON MINERALS LIMITED Prospector i Licence No.

T 4969C.P. 1657, Val-d?0r, (Quebec) J9P 5Y9

Summary of Work Performance and Distribution of CreditsTottl Work Days C', claimed

for Performance of the following work. (Chtck oni only)

Q Manual Work

f ] Shaft Sinking Drifting or other Lateral Work.

Q Compressed Air, other Power driven or mechanical aquip.

Q Power Stripping

Diamond or other Core drillingLand Survey

All the work was performed on Mining CleimU): L 1048185;Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below) Tt E C O R

Hole BB 89-06 280 Feet

Drilling date: March 1989Drilling Co. Bradley Bros Ltd

Exploration Co. : Aurogin Resources LTd Suite 70480 Richmond Street W. Toronto (Ontario) M5H 2C7

ONTARIO GEOLOGICAL SURVE ASSESSMENT FILES

OFFICE

NOV02 1989

RECEIVED

Data of Report

March 1989Certification Verifying Report of Work 77 7

dile'eto, nVl hereby cen^y that l have a persons! and intimate knowledpe of the factl let forth in the Report of Work annexed^iereto, Having performed the work or witnessed same during and/or after its completion and the annexed report it trwe.

Name and Posta' Address of Person Certifying

Jacquelin Gauthier: Mineraux Morrison T.T^P

J9P 5Y9Date Certified

23-08-89

Table of Information/Attachments Required by the Mining Recorder ff

Type of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

Lend Survey

Specific information per type

Nil

Type of equipment

Type of equipment and amount expended. Note: Proof of actual cost mult be submitted within 30 day* of recording.

Signed core log showing; footage, diameter of core, number end angles of holes.

Name and address of Ontario lend surveyer.

Other information (Common to 2 or more types)

Names end addresses of men who performed manual work /operated equipment, together with dates end hours of employment.

Names and addresses of owner or operetor together with dates when drilling/strippingdone.

Nil

Attachments

Work Sketch: these ere required to show the location and extent of work in relation to the nearest claim post.

Work Sketch fat ebove) in duplicate

Nil

768 (85/12)