42G02NW2004 2.20158 BOURINOT

010

REPORTON

THREE DIAMOND DRILL HOLES

BY

ST LAMBERT DRILLING

FOR

DIABRAS EXPLORATION INC.

IN

BOURINOT TOWNSHIP

ON CLAIMS

1225321, 1225323 and 1225324

MARCH 2000

8

PREPARED BY: STEVE S. MUNRO, B.Sc. Tuesday, September 08, 1998

RECEIVED

MAR 2 f 2000

GEOSCIENCF ASSESSMENT OFFICE

42G02NW2004 2.20158 BOURINOT

TABLE OF CONTENTS010C

1 INTRODUCTION

2 PROPERTY LOCATION

3 DRILLING

3.1 Hole OKD-01

3.2 Hole OKD-02

3.3 Hole OKD-03

4 HOLE PLAN, LOG AND SECTION

5 THE DRILL CORE

APPENDIX 1 - PLAN MAPS, VERTICAL SECTIONS ft DRILL LOGS

3

3

3

3

4

4

4

4

5

1 INTRODUCTION

This report describes three diamond drill holes drilled by St Lambert Drilling on behalf of Dia Bras Exploration Inc. of Montreal, Quebec. The three holes were drilled on a contiguous group of claims in Bourinot Township, Ontario. The holes were drilled during the period March 10, 2000 through to March 18, 2000 and a total of 302m were drilled

2 PROPERTY LOCATION

The three drill holes were drilled on a contiguous group of fifteen claims, held by Dia Bras Exploration Inc. in Bourinot Township, Ontario. The group of claims is located approximately 50 kilometres southwest of the town of Kapuskasing, as illustrated in Figure 1.

4f1S'H

NTS: 4K/2

Figure 1 - Property Location Map

3 DRILLING

3.1 Hole OKD-01

Hole ODK-01 was collared on grid line 2+OOE at station 14+40N on clair^ number 1225321. The hole was drilled at an azimuth of 1800 and a plunge of 50 0 . Drilling commenced March 10, 2000 and was completed on March 12, 2000. The

core was logged by Roger Thomas on site during the period March 12, 2000, through March 15, 2000. A total of 102m were drilled.

3.2 Hole OKD-02

Hole ODK-02 was collared on grid line 21+OOE at station 7+40S on claim number 1225323. The hole was drilled at an azimuth of 2250 and a plunge of 500 . Drilling commenced March 13, 2000 and was completed on March 15, 2000. The core was logged by Roger Thomas on site during the period March 18, 2000, through March 23, 2000. A total of 100m were drilled.

3.3 Hole OKD-03

Hole ODK-03 was collared on grid line 8+OOE at station 4+50S on claim number 1225324. The hole was drilled at an azimuth of O0 and a plunge of 500 . Drilling commenced March 16, 2000 and was completed on March 18, 2000. The core was logged by Roger Thomas on site during the period March 18, 2000, through March 19, 2000. A total of 100m were drilled.

4 HOLE PLAN, LOG AND SECTION

Detailed drill logs, plan maps and vertical sections are included for each drill hole in Appendix 1 of this report.

5 THE DRILL CORE

The drill core was logged during the period starting March 12, 2000 and ending March 19, 2000, on site, by Roger Thomas. Details of the storage of the drill core is included with the drill logs in Appendix 1 of this report.

APPENDIX 1

PLAN MAPS, VERTICAL SECTIONS Z DRILL LOGS

DRILL HOLE LOCATION PLAN

Claim 1225321

Bourinot Township

At ifino N\

i1500 N

UOO N

1300 N

1200 N

1100 N

1000 NOCNK") SOO N

LO

(-vi 800 N

*- X700 N

600 N

500 N

400 N

300 N

200 N

100 N

n

f i 8 S i S 10) -,

n ri ln r

f \n r

; in r

i /ln : r

'NO) 8O

O (

n rn m r

' 1225318 j

l

s

1.

1

c ) - . — - — - — i — ̂

\4

i

\\

ODK-01"" Az^SO 6

Depth = 102m

1225321

p2s; 524

\

\\\\\\

|i

C\c\

LOC\ C\

250 500

(metres)

Scale 1:10,000

750 NT

FROM : DlflBRflS-EXPLORflTlON. . .... ,. ,. . PHONE NO. : l Mar. 20 2000 li:36flM P2

000* T- L2Ezo

Q O

TERBDftDEN

PARAGNEISS

MAFIC GNEISS

OIA BRAS EXPLORATION INC,HotoNunter OOK-01

Ctokn Ne: 1226821 Location: L2E

Mnttd:Mv 17,2000

O

M*iitar 10-12, aooo

90m

SCALE

m0.

s s Q(M

Q

DIAMOND DRILL HOLE LOG

Client: Dia Bras Exploration Inc.Driled by: St lambert Drilling Co. Ltd.Logged by: Roger D. Thomas, MSc, P.Eng., R. D. Thomas and Associates.

Hole No. OOK-01 Page 1 of 6

LOCATION:

Province: Ontario Township Bourinot Latitude/Longitude: 49" 07' 30.98" 82* 53' 53.94" Grid: Southern

Mining District:Claim No:UTM:Grid reference:

Porcupine122532117 5442898mN361500mE2+OOE 12+40N

SLU

DRILL HOLE CHARACTERISTICS:

Core Size: Depth of Casing: Total depth: Date Drilled: Date Logged:

NQ6m102mMarch 10 -12, 2000March 12 -15, 2000

Hole orientation. 180* Inclination: 50"

Date Log Printed: March 16,2000

Note Alphanumeric* to p

UJ

J, a

a:Q

SLL

es Wtowtng cohort (eg: greyish Mack(N2) of gieenah btack (5G3fl)} am MunMlt Color nunbereaftw: Goddard, E N , Trask, P. D., * Ford, R.. Rove, O N, S^oewdtf. J T. and OvMteck, R. li 1964: PoctKxfcr dmt; Geological Society of America, Special Pubticafon. Boulder,Colorado, US A.Mtnsel Products 1973 MunMM sol color chart*, Muneel Product*. Macbeft Color A Photometry Division of Kblmwgew Corporation. BaNEnme, Maryland. U 5A

Anguterty (VA-very angular, A * angular. SA s 9Uoengiihr, SR-tut*oiinded, R^ rDun(M,vvR^wrtnunded)i9aicooKingto: g. M C.{19^Conic*rtsoftclMrtfoTVisuaeriiMaonofrow

Q.

From (•j)

0.00 4.00 OVERBURDEN, sand

4.00 32.00 PARAGN&SS: interbanded 4tTX. felsic and 60* mafic layers.Mafic layers: Dark greenish Mack (5GY2tt) 0.5 - 6 m thick, fine- to

medium-grained, moderately magnetic, variable texture from massive to poorly banded; composed of 80 - 70*4 Mack amphibole, 5- 20* plagioclase, 30-40ft dark green, very fine-grained matrix, trace-1% pyrrhotite; amphibole is chloritized; may include 5 - 20 mm thick. felsic (see below) layers and lenses. CA*70*.

Fetefc Layers: White to greyish pink (5R8/2), 0.5 - 2 m thick, fine- to medium-grated. non-magnetic, massive to poorly banded; composed of 10* quartz. 40*. K-spar, 40* ptogiodase, 10* biotAe; included tNn layers and up to 60 mm thick enclaves of mafic layers (see above).

@ 1 1.25: 8 mm chloritized, serpentiirized (?) Seam in mafic layer,

@14. 11 10-15 mm quartz vein containing IVo pyrrhotite atcontact with mafic host rock.

@ 1 5.40: well developed banding, CA-300 @15.50: 15 - 20 mm breccia zone composed of l - 2 nun, briDtant

green (5G6/6), angular fragments in a very fine-grainedmatrix. Trace pyrite (non-magnetic) Host rock is felsicgneiss. CA-55"

15.95-16.25: felsic bands are pate reddish brown {10R5M) (hematized). 16.10: banding is folded. 1 7.25-1 7.30: breccia zone at contact of mafic and felsic bands, highly

chloritized.17.30-17.73: moderately hematization of felsic bands. @1 8.00: 20 mm shear zone containing 2 mm seam of calcite and a

2 mm seam of 50"fc pyrrhotite with calcite. Parts are hematized.CA=20^

18.20-19.00: mafic band is medium-grained. (3)19.00: mafic bands change from being moderately to sttghtly

magnetic. 20.00-20.35: abundant 1 mm calcite filled fractures in mafic band.

CA-40".

inQ.

Hfm^mw^au f i!i! i li IIPforfi

;^!m}!: : :

4.00

32.00

32.00

K3iKiJ^lffliJli

32.00

102.00

S lil l m illli imiilts i tit! li!

PARAGNEISS, coni 22.15-22.20: moderately hematized and abundant seams fiHed with pate

green, very fine-grained material. 23.20-23.75. highly sheared to brecciated: moderately hematized.

carbonatized and chJoritized; trace fine-grained, pyrrhotite as 0.5 mm disseminated clots and as coatings on irregular, fine fractures.

25.70-27.30: felsic band wrfth very weH developed compositional banding, CA-50".

@27.32: 2 mm seam filled with pale green, fine-grained material, CA*50" panto! to banding.

27.68-27.95: sfigHUy hematized. Q27.72: 2 mm seam filed with fine-grained, green material, CA*4Q'. @29.5: laige, 7 mm books of biotite developed at contact of mafic and

felsic bands.

CONTACT, arbitrary

MAFIC GNEISS with minor felsic bands. Dark greenish grey (5GY4/1) to greyish black (N2), finery fofated to, in places, banded, to massive, fine- to medium-grained, in places porphyritic; coarser phases are less foliated. Composed of 30-4096 anhedral lo sobhedral. black amphibole. In part altered to chlorite; 20-30** very fine- grained feldspar; 40-50"* very fine-grained matrix; trace to tt biotite (7). Very slight to nl carbonatization. Very sbghtry magnetic. Felsic bands constitute -eSfc of rock. Coarse-grained, irregular. 5-40 mm thick, composed of 40ft hematized K-spar, 60* plagioclase.

35.10: well developed foliation, CA-60*. 36 42-37.20: wen developed foliation, C^57". 49.18-4922: <2% fine-grained, disseminated pyrrhotite, rock is slightly

magnetic.47 10-47.30: 2% fine-grained, disseminated pyrrhotite, rock is

moderately magnetic.

Rep 01

iS^^/Jji!??**^

38.80

mmUm -i ;!:* v-K-i (iatte'i*-: ̂

23^IWl?Jii3

3900

f ST :-::-"i.?:---^:-:3-v^---:-H ^ *--:**t:K* ;-?^.V;

iif^^nl)?s5*i

X 'i j' *; -?'-.?-X -i^X f .\^. .:?5*-:i,*KX*o ***--*jk#'Jtfc\

LL

ti

32.00 102.00 MAFIC GNEISS, coni 47.95-48.00: <2% fine-grained, disseminated pyrrhotite, rock is sKgMty

magnetic. 49.09-49.37: abundant, irregular, fine fractures 0*1 mm) filled with

quartz. ©53.70:30 mm highly foialed section composed of 10 x 30 quartz

lenses, pale green material, trace pyrrhotite; CAs4Q0 . 55.10-56.90: fairly abundant micro fractures fined with calcite;

various CA. 58.00-58.30; fairly abundant micro fractures fitted with calcite;

various CA. 59.28-59.55: abundant *c1 mm micro fractures filled with calcite;

various CA. Q60.83: marked increase in magnetic attraction from slight to

moderate Increase is caused by increase in pyrrhotite content to1*. It is fine-grained, disseminated.

68.88-69.18: fetelc band (as above); CA of both contacts andcompositional banding *50".

©69.25: felsic bands become slightly hematized, moderate reddishorange (tOR6/6) m colour.

70.56-71.12: felsic band, 8 mm wide, parallel to core axis. ©70.13 10-15 mm felsic band sHghtJy deformed (boudinage 7),

71.45-71.85: abundant micro fractures fitted with calcite, various CA71.85-72.00: felsic band, highly fractured to brecciated.@71.99:10 mm wide shear. CA-30.72.00-72.08: abundant micro fractures fitted with calcite, various CA.Q78.75: decrease in magnetism from moderate to slight.72.25-72.58: compositional banding in felsic phase is deformed.©72.50: felste bands become sDghtJy hematized, moderate reddish

orange (10R6/8) In colour. 72.58-72.78: mafic phase is quite green (serpentinization ?). Overall

colour is greyish green (5G5/2). Q73.70: composMonai bandog CA-10 C .

Rep 02 68.00 66.35

o.

Q N

8

Ifl

Q. XLU

d

Q

Oa L.

:i ;^iliiiill:^r^almtitmte

32.00

102.00

f;1:;t6l?^

mMM102.00

ii!i| \ m 1 # | lil! Hi i! 1 i linsNlfel&f* 5 *p Z sj5 ;;;i iOMv;.;;: i; i^ttijs ?jv;:j?; ;; mv^s^'tet j |f: i,m f p?? ttufppH-; 5 si;;- s; y; ;:.; ? 5M;W;^;:*teMi*itiBn; S ^m;ffiJ?8SM; i ;fc K::*i i ;f*ii:' ; ^:Sa0^ j His p *; s; ivsiji^iifiSffSfWBSw is immmxxix ? ss jap j *^ji^SiJliiS? s fj^li! i5M;5; iK;igvUP? j|H??|S ilJBs ?? ?si*?J?:SSM.?sli.?* MiBKSl ?4ji*^

MAFIC GNEISS, coni 73.00: several 1 nnm cateBe filled fractures, CA^550 . 78.33: 5 mm fracture filled with quartz and brilliant green (5G6/6)

material; CA^SO0 . 79.32-84.48: felsic bands constitute 4W of rock; they are moderately

hematized, moderate reddish brawn (10RSM) in colour and medium- to coarse -grained

81. OS-81. 60: felsic band is highly fractured to brecciated; fractures are sub-parallel 1o GA and filled with calcite and chlorite; contacts oftMs unit may be shears, CA^SO0 .

Q83.25: 35 mm thick possible shear contact between mafic and felsicbands; highly carbonatized, trace leucoxene (?)

Q83.52: 40 mm shear zone as above (Q83.25). 83.90: compoatkma) bandmg. CA^550 . ffi86 1 0* becomes slightly to moderately magnetic88.20-88.58: abundant calcite filed micro fractures, various GA, Q90.45: becomes slightly magnetic.QB0.68: bands of inteimediale composition become present and

constitute 30K of core These are medium) light grey (N6) fine grained, massive to weakly banded, non-magnetic to slightly mnnn^^ln ^nmnmrn** nf Arm* ^ mm*r ^HGl- Mr&Ak n*w*v^Kift\x^f A tfiWmagnetic, composed of icnb K-spar, 3tnb DOCK amphibole, 10?* biotite, 50K plagioclase, trace pyrrhotite.

^90.88: mafic bands become moderately magnetic. @91.73: felsic bands become sightly hematized, banding becomes

irregular. 94.00-95.00: banding CA^O'\ 95.90: banding CAMO . 99.88-100.33: shear zone with quartz seams to 30 mm wide oontaining

5ft sulphides (pyrite and pyrrhotite) disseminated on fractures, in veins and in wait rock. Host rock is mykmitized to greyish greenaphanitic material; in places hematized.

Q99.10: becomes moderately magnetic.101.95-102.00: ^ fine-grained, disseminated pyrrhotite.

EOHMagnetic anomaly explained by pyrrhotite in malic gneiss. lOOft core recovery

IlllililliIfjsfijSij;?*? fi

: ^Ji i' ' ' ̂ ^^^^ '-*^-

*l:-i::-:t*iA : S? ?j-J^:inifft iji

i--:- 5: ^'i.-y--^ v-J^ :- '-i^y-

^p^^^^U^ j!*SS?)OfSf~; sls*4Mg|5H^ :~a:-:-.-:-.UiW:-:);-s* -

;iiSi*;HS i;

iWxtaiii'M sjitfejjj^ll|!(^!

CORE BOXING AND STORAGE Page 6 of 6

;:-H^^i^

hjjttSilfe^^12

3

4

5

6

7

8

d

10

1)12

13

14

15

16

17

18

19

20

^Wi;;illt

liliii!!4.00

11,95

15.25

19.68

24.00

28.50

33.00

37.38

41.62

45,95

50.32

54.72

59.17

63.50

67.80

72.08

76.50

80.75

85.00

89.29

^tiiis||!s|iis-s;;| 3:*?5i;.:**???s?.:*.;s"s-"". ij-^5 jix:S-;:-*x:-i-i-iv - y*.mmmmm

11.95

15.25

19.68

24.00

28.50

33.00

37.38

41.62

45.95

50.32

54.72

59.17

63.50

67.80

72.08

76.50

80.75

85.00

89.29

93.58

lliiM l-— ••^-'-''^x '-fii"f*~ " "' ~" " "

StJvJfciiJ'ifs'i^ii i!

Paragneiss

Paragnelss

Paragneiss

Paragneiss

Paragneiss

Paragneiss

MaAc gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

Mafic gneiss

tnfiekJ

(n field

fn flett

In field

Infield

Inffeld

Infield

In Held

Infield

In field

Infield

Infield

Infield

Infield

Infield

Infield

Infield

Infield

to field

Infield

s?-Sw.?H-???j|t:'iHjKS--.** ::-: J f- J -::-r*;-s-x*:'-j;:**.- -T-:

*i* .". i^ f.;* **s*i* *f3*

fKBMwii21

22

23

24

25

26

27

28

29

30

31

32

33

34

35

36

37

38

39

40

!;l|;liH;s?Ws|3i3.*'- lv ̂ -i *-? a^.**^ *?.r*f.*

tiliRiiitP93.58

98.20

i^!!tHt!!pii *SjB5fipjfc*n;*.?-P T JFftejMlilPll i

98.20

102.00

K^sjlslillllllfif

Mflfic gneiss

Mafic gneiss

In field

In field

-

DRILL HOLE LOCATION PLAN

Claim 1225323

Bourinot Township

o 250 500

(metres)

Scale 1:10,000

750

FROM : DIRBRRS-EXPLORRTION..... . ..... PHONE NO. : Mar. 20 2000 11-.41RM P9

225* T

FELSIC ONEJSS

DIA BRAS EXPLORATION INC.HotoNumbw: OOK-02

CWm Not 1226323 Loortton: L21E 7-KJOS

Mi MM* 14*15-19.2000

Mm

SCALE

o*-*o.

(M

O

R

DIAMOND DRILL HOLE LOG

Client: Dia Bras Exploration Inc.Drilled by: St Lambert Drilling Co. Ltd.Logged by: Roger D. Thomas. MSc., P.Eng., R. D. Thomas and Associates

Hole No. ODK-02 Page 1 of 6

LOCATION:

Provii Ontario BourinotTownship:

Latitude/Longitude: 49" 06' 29.88"W 82" 52* 8 02"WGrid: Southern

Mining District Claim No: UTM: Grid reference:

Porcupine122532317 5440958mN 363600mE21+OOE 7+OOS

DRILL HOLE CHARACTERISTICS:

Core Size: Depth of Casing: Total depth: Date Drilled: Date Logged:

NQ45100mMarch 13 -15,2000March 18 -23,2000

Hole orientation: 225T Inclination: 50"

Date Log Printed: March 19, 2000

(La: oGoddanl. E. H. Trask, P. O ,, de Fort, R., Rove, O N , SJngiwaM, J T and Owbw*. R. M. 198* Rw*^*ixc^iart; GwfegtealSoc^ of America, Spw^PuMcal^BouWef. CotanfeU.SAMun^lfroducU 1973: Mutudttoi ctaof chatlt; Mantrtl Producte, Madxm Colcr 8. PHrtomOy DMOonrtKoimofgmCorporetloo, BiKmnK, Maryland. U.S.A.

Angularity (VA - my annular, A * angUar. SA * subangular. SR * sUrowxj^R^rconderi. Wl*wrtroufMtod)i*acecidBigl(): Powera. M. C. (1963): Compwteon chart far visual aaUmMm of rouwlrwsB, Journal of SuHnurtary Petrotagy. v. 23.p. 117- lift

Q.

a CM

0.00 45.60 OVERBURDEN: sand, lew coarse pebbtes and small cobbles of gneiss (local Knotogies) and a few Paleozoic limestone. NotW

4580 100.00 FELSIC GNEISS: moderate pink (5R7M) to light red (5R6/6), oxidized to Kght brown (5YR5/3) angular sand, non-magnetic, poorly developed compositional banding, CAMO0; generaly fine-grained although large, anhedral K-spar crystals are present in places. Composed of 10-20* anhedral quartz. ID- 40% anhedral-subrtedral K-spar, 20-60* subhedral plagioclase. S-15% biotite, trace very fine-grained metaWc mineral Rock has been epidotized and hemafized as noted below. In places rock has a greenish hue probably resulting from chloritization of biotite.Note that even though the cone has crumbled to a grus throughout most of the note, the recovery has been excefcrrt except In the places note below.

45 60-40 20: rock is quite rotten, highly oxidized and half of a hascrumbled to grus.

47.OtM7.20: several 30 mm anhedral crystals of K-spar. 47.2(M7.95:20* cnloritized biotite. 47.95-50.45: rock is rotten and is recovered as grus. 48.00-51.00:1.15 m lost core. 51.35-51.50: moderately hematizad; core is very broken. 53.50-53.60: mafic band as below (55.25-55.37). 54.12-54.25:6036 mafic band as below <55.25-55.37) 54.36-54.55: moderately hematized. 55.25-55.37: mafic band: dark grey (N3), f ne-grained, massive,

non-magnetic: 40** plagioclase. 6016 black amphibole; contacts: upper CAMS", tower CA*ti00 , not paraflet.

55 52-58.90: moderate hematizaUon, core commonly broken wMiepidote, chlorite and Calcite (T} on fractures.

58.90-59.05: aphanitic, greyish red to very dusky red (10R3/2), mylonitic (T} Zone. Core is broken but appears to be a 30 mm section of fractured unaltered gneiss contained in the zone. Contacts are sharp, wavy and coated with chlorite. CA*480 .

59.90-60.00: aphanitic zone as above (58.90-59.05).

Rep 02 5780 57.95

Rep 01 58.88 58.95

DJT-4

CL

CE

**t**#^.

*-.- '-

45.60 100,00 Felsic Gneiss, coni60.5041.90: colour change from red to while. 6218-63.00: lost core; rock probably similar to thai below (63.00-63.18) 63.006318: greenish Mack (5GY2/1), very fine-grained, mafic band

containing feldspar inclusions. Possibly a dyke; core is ground,sfgtrHy magnettc and contains 5*fc medium- to coarse-grainedbiotite.

Q83.75: rock has become pinkish grey (5YR8/1) to very tight grey (N8)in colour. Redder sections are restricted to crumbled core andalong fractures.

64.08: biolite content increases to 20-30tt, commonly cMoriHzed 64.08-67.20: banding Is well developed and is wavy and subparaNel the

core axis.67.75-89.00: core very broken and partly crumbled. Red in colour. 69.33-69.39: mafic band composed of 60* Mack amphibole and 40**

plagioclase. Non-magnetic. 69.97-70.05: mafic enclave in half of core, composed of 60* black

ampMbote and 40*. plagioclase; non-magnetic. 70.70-72.16: mafic-rich section containing eO-80% Uack amphibole,

20-35*) plagioclase, and D-5% K-spar; amphibole is moderatelycitforttizecl; non-magnefc.

72.12*73.35: core very crumbled and weathered. 73,35-73.m mafic-rich section: 90*96 black amphibole and

10* feldspar 73.70-78.20: core very crumbled and weathered; intact core pieces to

0.05 m long, mainly of maflc-rtch phase as above (70.70-72.16). 78.20-78.90: felsic gneiss, very Ight grey (N8); fine- to medium-grained,

weakly fofiated; non-magnetic; composed of ID-15% quartz, 10-35-*, K-spar, 30-50*16 plagioclase, and ID-20% cMoritized biotite.

(@J78.90: core becomes very broken into 5-10 mm pieces with a few0.03 - 0.10 m pieces being present; core has aJso turned quite redin colour; mafic parts are green from chloritization. Considerablemissing core as below.

75.00-78.00:0.3 m missing core.

ntHOL

45.60 100.00 Felsic Gneiss, coni. 78.00-81.00:1.0 m missing core. 81.00-84.00:2.0 m missing core. #85.10: foliation CAMS*. 85.30-86.20: moderately silicified, pervasive and as 6-8 mm masses;

also epkJolized and chtonlized as coatings on fractures; rock ishighly fractured.

88.20-89.20: moderately hematized, core recovered mainly as10-30 mm fragments

89.20-89.40:WgMy fractured; chloritization as abundant fracture WHngs. 89.40-90.00:0.60 m missing core90.00-91.30: NgHy fractured with abundant chlorite filled fractures. 091.10:8 mm seam of very dark red (5R2/B), aphanic material;

CAF20" 91.30-9160: moderately sMIcMed as above (85 30-88 20); moderately

abundant cMoritized fractures.91.60-92.65: moderately sJHcrtied as above (85.30-8820). 92.65-95.80: moderate to high cMoritizatfon, chlorite occurring as

irregular masses, as 1-30 mm seams (CA?500), and as coatingson micro fractures. Core is retrieved as 10-20 mm pieces and asa "day* with a tew 0.10 m sections being preserved. Feldsparsare moderately to highly hematized.

95.00-100.00: some of the "day* material has the colour of malachitealthough R does not effervesce in add (X may be too cold). Acursory inspection did not reveal the presence of sulphides.

95.80-100.00: highly chtoritized and hematized throughout. Core isreturned as coarse sand grains and "day", with a few 0.05-0.08 mlengths of sold core. Drillers described i as having clay likesections.

96.00-100.00:1.2 m tost core, probably between 98.00 and100.00 m acQOfdmg to dnHers.

Note: the last tO-20 m of the hole was difficult to dnH because the core tube had to be puled every 0.1-0.3 m because of fhe blocky nature of the day and broken rock.

Rep 03 78.57 78.64

U-

•••'•Hiij;'

!:|p100.00

*t***za- :;? ins li i in^-i^^-;;:v:?:?.-^i;.i'::-i:-::j;.; ifit :-:"*^ ;."i :| K ;: *: : -J 5? s: ^:IW^E|iplPVfff^^;r:.: xS:; ^:;.:^-:; :-v5 -;J;i;-5ii ::?^xf*-;:;-i"i:iwi"4i*- ^^^"^i'HivtK-"^??.-^': ??ii-i^;i — *?:ii :5i :J— ^5Wvryi"::*?-;~iSVxJf ?ii"--: :;;i i*Si-f.:; v'-: S^S^:;;ti^i; ; :̂:: j/:^?:"-"-^^:^^*

E OHHole was drilled to test negative anomaly. Anomaly shown to be the result of weathered non-magnetic rock in a probable fault zone. The lack of core recovery and presence of clay in the lower part of the hole is interpreted to be indicating the fault zone. The day is probably fat* gouge

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CORE BOXING AND STORAGE Page 6 of 6

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Felsic Gnefs*

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21

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DRILL HOLE LOCATION PLAN

Claim 1225324

Bourinot Township

100 N

1225321

100 S

ZOO S

300 S

400 S

500 S

600 S

700 S

600 S

900 S

1000 S

1100 S

1200 S

1300 S

1400 S

1500 S

ODK-03

Az^OO0

Depth = 100m o

oo

1225324

ooOO

m m

1225325

250 500

(metres)

Scale 1:10,000

750 N T

FROM : DIPBRPS-EXPLORPTION... . . . ... . . PHONE NO. : l Mar. 20 2000 ll:47flM PIS

FELStC-frfTERMEDlATE GNEISS

ULTRAMAFIC DYKE INTERMEDlATi-FELSIC

GNEISSULTRAMAFIC

DYKE

INTERMEDIATE

DIA BRAS EXPLORATION INC.

CWm Ne: 1225324 Locrton: 1864*208

r- ,-tCL

DIAMOND DRILL HOLE LOG

ru

l

CRenf Dia Bras Expforation Inc.Drilled by: St Lambed Drilling Co Ltd.Logged by: Roger D. Thomas, MSc., P.Eng., R. D. Thomas and Associates

Hole No. ODK-03 Page 1 of 9

LOCATION:

Province; OntarioTownship: BourinotLatitude/Longitude: 49" Off37.74"N7820 53' 22.31"WGrid: Southern

Mining District: Claim No: UTM: Grid reference:

Porcupine122532417 5441238mN362100mE4+20S8+OOE

DRILL HOLE CHARACTERISTICS:

Core Size: Depth of Casing: Total depth: Date Drilled: Date Logged: Date Log Printed:

NO3m100mMarch 16 -18,2000March 18 -19,2000March 19, 2OOO

Hole orientation: 000* Inclination 50"

Note: Alphenumwics in pamtthN, Sing*^,J.Ta^

Cokvado, U.SA MunaalPredKlB 1973; Munw***cokx chart* Miiiw*F*roducte,Mac*^C^

= wry angubr, A * aMgukr, SA - autwnoutar, SR - aubronnded, R - ioiaoMWR"WBlw)iiiKhd)i*acccrdBiBto: Poiws.M. C (tO3): CompartaondartIbr*mlaatlmaHonof roundnas*; JoMtnalrfS-JtnefihryPirtrology.v 23,p.l17-1IO.

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0.00 2.50 OVERBURDEN: sand

2.50 44.32

a a

FELSK-WTERMEDMTE GNEISS: BgW grey (NT) w4h vailing amounts of black (N1) and moderate reddish orange (10R8/6). Well developed compositional banding, composed of 1-3 mm mafic bands and 5-10 mm fetsic bands. Texture is fairly uniform overall, but locally it is variable; fine* drained, equigranular. Fatty uniform composition of 20* quartz. 2OTfc K- spar,SO%plaaJoclase> 9%Mofleand1%tlac4(arnplribole. Biotite occurs as smaB (*:l-2 mm) flakes; amphibole occurs as 2-3 mm subhedral crystals. Trace pyntKrtte associated wit* amphibole. In places. K-spar occurs as 5-20 mm rounded anhedral crystals, the most abundant occurrences are noted below. Overall, rock is non-magnetic to moderately magnetic; the felsic bands are generally non-magnetic whereas the mafic bands are moderately magnetic. Magneo^m is related to pynhotMewhk^ is in turn related to the amphibole. Core commonly recovered as 0.2-0.4 m lengths with longer pieces being common. Very hard rock to drill.

3.83-4 50: rock changes from HgM grey (NT) to moderate reddish orange (1 ORB/6) and marie mineral content increases to 15* UoUte and black amphibole. CA of compositional banding a 50'.

4.50-4.71 :COTB is broken Mo 10 mm diameter pieces. Most fracture faces are coated with pate greenish mineral and are sHckensided.

4,71-e.Oft rock is moderate reddish orange (10R6/8) in colour.4.88-4.94: several 25 mm anhedral, rounded K-spar crystals,S.23-5.32:40mmtrrtckmaficbarKlco^lpt>sedof20%bwtite30%c}llof(te,

45% plagioclase. 5*. K-spar and TPh pyrrhotite, aN fine-gained. Pyrrhotite is disseminated and very fine-grained. CA^aO".

5.48-5.90: several 15-30 mm anhedral, rounded K-spar crystals.6.00-10.40: decrease in intensity of orange colour of rock.9.70-10.10:5* biotite and Mack amphibole.@9.60: compositional banting. 0=70'.11.70-12.52: 5*. biotite and Mack amphibole12.30-12.48: slight increase in redtfteh colour to patches of moderate

reddish orange (10R8/8).18.53-20.60:5% mafic minerals, moderate orange pink (10R7M) in colour.20.23-20.38: broken core.

Rep-01 1273 13.10

en *-*Q.

x ft-

1Z 50 44.32 FELSIC-iNTERMEDIATE GNEISS, coni.

20.60-21.10: IS-20% biotite * amphibole; medium orange pink (10R7/4)in colour.

20.90-21.40: abundant irregutar fractures, some fWed with chlorite. Q21.00: compositional barring becomes less pronounced. 21.95-22.22: several chbrile+calcjte coated fractures,

mainly low CA^O, 23A 22.75-23.00: fine- to very fine-grained, moderate redctsh orange

(10R6/8) with a few chlorite coated micro fractures, irregular; smalltrace calcite on fractures.

25.67-25.84: fine to very fine-grained; abundant chtorite+cafcite coatedmicro fractures; pale reddish brown (10R5/4).

26.63-26.89: mafic bend, equigranular, homogeneous, wet banded(CA-700), moderately to highly magnetic: composed of 3096 blackamphibole, 2CT* chlorite after amphibole. 40* plagioclase. 9**, K-spar, and 1ft pyrrhotite as t mm disseminated clots. Uppercc^act b gradational.

20.09-27.05: as above rj26.83-26.89) except 20** K spar; nightyfractured, CA-irregular.

27.05-27.06: felsic; no mafic minerals.27.06-27.12: mafic band as above (26.83-26.89). 27.12-27.16: mafic band as above (26.69-27.06). Q28.30:40 mm duMneter mass of moderate reddish orange

(10R6/B) K-spar.@28.53: compositional banding becomes pronounced. 29.08-29.90: many parallel, wavy fractures at 10-20 mm spacing*;

CAs30"-409 ; moderate hemafeatior.30.47-30.54: mafic enclave as above (226.85-26.89) in half of core. 3l.30-3t.46: well banded, CA*700 . 3t 46-31 54: moderate reddish orange (10R6/6) tend; CA*600 .

2-3^ mafic minerals. 32.15-32.74: well banded but folded. @32.50: rock becomes predominantly moderate reddteh orange

(10R6/6) in colour.

(M LL

tf)

l :l•i'iiifit!iaiiipf

2.50

Iliiilliu^H4432

iFELSrC-WTERMEDIATE GNEISS, coni

33.40-33.46: mafic band as above (26.83-27.05), 0/^=30". Q33.43- fracture coated with chtaHe CA-30" but perpendicular to

band above. Q33.58: rock becomes weH banded.37.52-37.80: abundant fine wavy fractures at 8-10 mm spatings;

generally coated with quartz+cHorite to t mm thick. Trace very fine-grained, disseminated pyrrhotite and as 1-2 mm replacementsof amphibole. Rock sheared to mytonrtized.

37.80-38.35: increase in pervasive slldticatiort with correspondingdecrease in mafic mineral content

38.35-38.58: high pervasive sib'cifrcation; feldspars are coarse-grained, subhedral (recrystalfaed 7).

38 58-39.68: rock is highly deformed and altered Abundant irregular, wavy fractures fiHed with 1 mm seams of chlorite; moderatelyabundant 2-5 mm seams of Mack, aphanitic material (chlorite 7), in one place forming a 80 mm x 30 mm mass on the side of thecore. Rockgeneraly appears to be brecciated to mytonitized. Trace-1% pyrrholNe throughout; moderate to highly magnetic.

Q39.68: rock becomes well banded and colour starts to revert to grey. 41 .70-41 .80: mafic band as above (26.83-26.80); trace disseminated

fine-grained pyrrhotite; moderately magnetic. Q41.84: 15 mm seam in broken core. Lower contact is sharp, possibly

sheared. CA*50". Seam b probably a mylonitic zone. Composed of dark grey (N3) aphanitic material with 5** pyrrhotite coating fractures and disseminated in rock.

©42.25: moderately well banded, CAM2C 43.85-44.32: abundant micro fractures fiHed with chlorite; most

abundant CA-40" but are offset by perpendicular fractures at CA=70^

Q44.25: well developed banding. CA^SO ' .

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PHI44.32

44.32

40.45

46.45

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46.45

59.43

Mi! li IB S 18lflS*!P m um\ III;! li lil^sy|Bi^|i^iii ili^il^U i ? |0|; y pff |j;j*f "? LiSiH w! JH H&JiiiMiJ&siife' LM^jijut? 1 S s*Ji* a fe 1W

CONTACT: sharp, fairly straight. CA*1 00 . Truncates Feldspar crystais ingneiss. Micro fractures in gneiss cross contact tool dyke. There does not appear to be any contact metamorphism or alteration of gneiss atongcontact

ULTRAMAFIC DYKE: Mottled greyish black (N8) vrifh greyish yellow green(5GY6/2) spots of oNvfne. Homogeneous, uniform, porphyritic, highly magnetic sllghVy carbonatized. Composed of SD-60% subhedral rarelyeuhedral, 5-8 mm diameter, rarely embayeci crystals of olrvine in very fine-grained, black groundmass.

CONTACT: Sharp, straight, same as upper contact, CA*20*. Adjacentgneiss is unaltered but contains abundant micro fredures up to 0.05 m from contact

mTBUMEDIATE^ELSIC GNEISS: tight grey (NT). We* developedcompositional banding, composed of 1-3 mm mafic bands and 5-10 mm felsic bands. Fine-grained, equigranular. Falrty uniform composition of 10*quartz, 1094 K-spar. 604* plagioclase, 1 9* biotite and Itt black amphibole. BnMe occurs as smafl ^1-2 mm) flakes; ampMbote occurs as 2-3 mmsubhedral crystals. Trace pyrrhotite associated with amphibole. Overall, rockisnon-magnettcto moderately magnetic; the felsic bands are generally non-magnetic whereas the mafic bands are moderately magnetic.

^46.90: banding, CA*56C . Q47.38: rock turns moderate reddish brown (10R4/B) in colour. ©48.40: banding CA^480 . 48.79-49.38: moderate pervasive silicification; abundant micro fractures

coated with chlorite on 8-10 mm spatfngs. CAB'20". 51.38-51 .48: core very broken; numerous calcite coated micro fractures. 53.70-53.88: abundant chlorite tcalcfte coated fractures. 53.70-53.88: abundant chlorite-* calcite coated fractures; ^ pyrrhotite

as 1 mm x 5 mm lenses on fractures; CA*30".

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48.45

59.43

59.43

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59.43

69.94

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llltlPiPl 8tH M!j| |p! iyS5}g|!||MfsmC:Hsmsfe s**f jpjisijjsjiSggil P

INTERMECHATE-FELStC GNEISS: cont@54 15 banding CA*500 . Q55 02* one 3 mm band is pitted and contains calcite55.10 55.40: broken core. 56.86-57 22: moderate pervasive silification.57.22-57.50: broken core, moderately pervasive silification, low

chloritization and carbonatization as coatings on fractures. 57.50-58.10: moderate pervasive sNttffcalion.©58 35 15 mm quartz vein, CA^^O0 . G59.00: rock becomes dafk grey (N3) to oltve Mack (5Y2/1) with very

few red, felsic layers. Also becomes moderately to highly magnetic mainly resulting from the presence of 1 mmdisseminated masses of pyrrhotite. Olive colour is the result ofgreen alteration of mafic minerals.

059.05: 10 mm dyke (?) as below (59.43-69.94). .©59.13: rock is highly fractured; chlorite -t calcite on fractures, CA*259

CONTACT: Sharp, truncates crystals in gneiss; slight decrease in size ofolivine crystals toward contact in dyke, otherwise no contact metamorphism or alteration. Contact is very irregular and at low core angle (contact is present in core from 59.1 2-59.73).

ULTRAMAFIC DYKE: Da/fc ofrve brown (5Y274) to olive Mack (5Y2/1) depending on the olivine size and content; fine- to medkim-grained; strongly magnetic; composed of several phases with average composition of 47* 5-8 mm diameter, moderate greenish yellow (10Y7/4), subhedral crystals of olivine, 2OTt subhedral 1-3 mm orthopyroxene, 3*ft 1-3 mm diameter mineral altered to while serpentine, 10"* black, irregular fine-grained masses (xenotfths 7), 20* aphanitic groundmass, small trace sulphide. High pervasive carbonatization.

59.43-60.66: fine-grained phase. Olivine is 1 mm diameter. 604)0-61.06: abundant calcite coated micro fractures, commonly CA-200

also 1 mm wide, rarefy 3-5 mm wkle, CA^00-20", mainly in coarse phase.

a*;5;;*?H*St?.

tllfPifiiIfflpypItefi

n CMQ-

59.43 69.94 ULTRAMAFIC DYKE, coat 61.05-69.25: coarse-grained phase.64.0S64.80: while, serpentinized mineral constitutes 5* of rock. 09.00-69.20: very coarse-grained. 69.2549.94: fine-grained.

69.94 CONTACT: simiar to upper contact except the dyke appears to be corroding into the gneiss. S rnm above the contact is a carbonate+serpentine coated fracture parallel contact at CA*23"

69.94 100.00 INTERMEDIATE GNEISS: very pate orange (10YR8/2), we! banded, slightly magnetic resulting from pyrrhotite associated with black amphbote, fine grained, composUonaJty banded; overall composition of 50** white feldspar, 30* biotite, 10* pink feldspar, io* black amphibole, trace pyrrhotite associated with amphibole.

970.10: banding CA*460 .970.48:40 mm wide, highly sfltified zone.71.37-71.54: moderately sllcMed; broken core resulting from a few

cftlonte+calcite coated fractures.71.35-74.45: rock is predominantly moderate reddtoh orange (10R6/6).972.80: banding CA*4S0 .73.84-74.13: abundant caJcite+serpentine coated fractures, resuKng In

broken core; CA*600 .78.18-78.21: mafic minerals altered to tight greenish material

(serpentine 7).978.40: banding CA-40".78.65-79.08: bamfng is folded.79.16-79.22: moderate pervasive silicification.60.40-80.58: core is broken resulting from low GA, chtorite+caltite

coated fractures.981.70: Increase in mafic mineral content, mainly biotite,

content to 20*.

S!

co in

IIP69.94

100.00

100.00

iiflffil i 1 f j jliii ill 1 1111 111 t 11 j l i| ji fi i

INTERMEDIATE GNEISS, contQ80.60: bandkig becomes moderately folded; felsic bands become

moderate reddish orange (10R6/6) in colour and represent *:10ttof core.

64 87-86 00* core broken by fractures at CA*0"87.00-96.33: core is recovered in long pieces, commonly ̂ .5 m

94.67-94.91: moderately sBfcWed; moderate reddish orange (10R6VB) incotoun contains <5% mafic minerals.

96.33-96.82: core very broken by low core angle fractures (CA-1 70)coated with serpentine (very slippery).

96.33-97.58: rock is moderate reddish orange in colour; moderatepervasive siacrfteattoa

99.10-100.00: rock is well banded with laiity constant CA*40".

EOHMagnetic anomaly shown to be the result of magnetic ultramafic dykes in the drill hole.Excellent (10091) core recovery.

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CORE BOXING AND STORAGE Page 9 o(9

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Felsic Gneiss

Ultramafic dyke

Felsic GneissFelsic Gneiss

Felsic Gneiss

Ultramafic dyke

unramafic dyke

Ultramafic dyke

Felsic Gneiss

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Felsic GneissFelsic Gneiss

iiiHiif." "" " jiiioiiiw^ ̂ " v '

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Field

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Declaration of Assessment Work Performed on Mining Land

t, SubMCtfon 64(2) and 66(3), R.S.0.1990

Transaction Number (office use)

Assessment Files Research Imaging

(ction 65(2) and 66(3) of the Mining Act. Under section 8 of the Mining Act, th ment work and correspond with the mining land holder. Questions about th development and Mines, 3rd Roor, 933 Ramsey Lake Road, Sudbury, Ontaric

42G02NW2004 2.20158 BOURINOT 9QQ

For work p*rtorm*d on Crown Lands before recording a claim, use form 0240. i typ* or print in ink.

t a^artted holdofW (Attach a list if necessary)_____

'**** D i/i i?PA c /^y^/gpyi-fV^n——Ud^.L/l

Client Number

:ax Number'-IHOS

•••m* Client Number

Telephone Number

Fax Number

2. Type of work performed: Check (*Q and report on only ONE of the following groups for this declaration.~i Geotechnical: prospecting, surveys, rj Physical: drilling stripping, n Rehabilitation

assays and work under section 1 8 (regs) trenching and associated assaysVork Type

J 1 ('i l^i 0 i/i C^ \J (~\ H ( si f. ( C. Gtf. O^]^\i t/* \ —^ •J

atesWork From -~ To erformed D** (b 1 Month S | Y**t 2.OQC2 Dty /^| Month 3*1 Y*" iOOO

liobal Positioning System Data (if •vaUatte) Township/Am f) -s/xt^ */

MorG^tanNumbv

Office UseCommodityTotal $ Value of ft . j 7 Workaaimed r Sr"5 W /ONTS Reference ' '

Mining Division -ff^l/^^c^jResident Geologist -^- X . District /V/X-TX-^XX^I

3 lease remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report

5. Person or companies who prepared the technical report (Attach a list if necessary)

-W Telephone Number (ft*!) 7

\ddressl f O

Fax Number

.ame ^ K L?

Telephone Number

•.ddress*,xi -f^

Fax Numberr*- 1 Q

Telephone Number

^ddress Fax Number

Certification by Recorded Holder or Agent, do hereby certify that l have personal knowledge of the facts set forth in

(Print Nune)ni s Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after itsompletion andiignature of Reo

.gent's Address"- 3.01 - f?CC•41 (03^7)

, to the best ofoMea kloldef DC

f yC ., /,7 N - Al/ p P/**! K*^

f

o*i

my knowledge, the annexed report is true.taent —~

- ,Ko&ol. St&r-lootou^L

/ d t**;* t M **7Telephone Number

JmJ W'*i76S~

Date ^/ - yn^r 7-ofojFax Number(^fi,) 3^i '-/v^r~**"* -^

RECEIVEDMAR 2 1 2000

GEOSCIENCE'ASSESSMEMTntcipe

recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mmin was performed, at the time work was performed. A map showing the contiguous link must accompany thi

/, DOM-Cbld^Claim Number. Or If

.vas done on other eligible ,,ng land, show In this

,;umn the location number idicated on the claim map.

i

3

3

TB7827

1234567

1234568

.225*311i ;us~ ^i3IJ^S" 'S/ 4-/i ^5 0 t^* ^ 1 ^^^ j ^^ ̂ ^ J -^ * *

(225- 1 1 f.I215-ZC7iZiri ( ?\22S~3 i ^\12mo(2AST3^ t/2zr^^^ll^S" 5^3/o2^ Ufi^^r 3^^"/a^r 5^^Column Totals

Number of Claim Units. For other mining land, fat hectares.

16 ha

12

2

1C

1C

(C

1 C

Ik

/k

?6/6/^/6/d

//^H,1C1C

2HO

Valin of work performed on thisdalm or other mining land

926,825

0

S 8,892

•f.

~

—

/^ l*! 0!—

lo' >^^

II 'Y S" c/~

—

^3 *"l i 0

Value of work applied to this dalm.

N/A

524,000

5 4,000

33^76-^00

^—-•~

C^lOO6,^(0022.5^7

Value of wor^" assigned to other mining daims.

524,000

0

0

-

-

-

C HOO

\(e 1^7

22 S*\l

Bank. Value of work to be distributed at a future date

52,825

0

54,892

/"v

i;

-

-

(0, 7*1 ^-

^,r6011 , tYTH

--

20 . ? d

. do hereby certify that the above work credits are eligiblejer

(PiMFidNwM)^section 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim

are the wprk was done.ature of R/-HjE&rdedyftolderorAoent Authorized In Writing Data ;

^f ) ysmtInstruction for cutting back credits that are not approved.

ne of the credits claimed in this declaration may be cut back: Please check K) in the boxes below to show how you wish to ntize the deletion of credits:

D 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.Er 2. Credits are to be cut back starting with the claims listed last, working backwards; orD 3. Credits are to be cut back equally over all claims listed in this declaration; orD 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):

*.: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary:' ^^^^^

Office Use Only————-——————-—-——-.———ved Stamp

3/97)

Deemed Approved Date

Date Approved

Date Notification Sent

Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

RECEIVEDMAR 2 1 2000

GEOSCIENCE ASSESSMENT _____OfFICE

ntario Ministry ofNorthernD*v*topm*0t Statement of Costs

for Assessment CreditTransaction Number (office use)

^formation collected on this form Is obtained under (he authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the ^ct, this information b a public record. This Information wB be used to review the assessment work and correspond with the mining land holder. Questions

this collection should be Directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor. 933 Ramsey Lake Road, Sudbury jo, P3E 6B5.

Work Type

C/i^woit^ (Jrim/Kv-j

AO^GII^\ / Su#i:r{S\}ior\Jc/ O r

Units of work Depending on (he type of work, 1st the nurnber of houra/day worked, metres of drfflng, Uometres of grid fine; number of samples, etc.

lot ^

/L/ 0{*yf

- 'i i

Associated Costs (e.g. supplies, mobilization and demobilization).

.

j(A n b (fan }? Aoi^tf

Transportation Costs

Food and Lodging Costs

6(.n(ae.(c{. AoTc(

**~6

Cost Per Unit of work

^?^.rr

* S~ 3 r

Total Value of Assessment Work

Total Cost

'x?7.VJ?

f 7 LJ^O

*l L,of1 s"3ro

ciie.

sr*?^Hi, *ilO

alculations of Filing Discounts:

Work filed within two years of performance is claimed at 100^ of the above Total Value of Assessment Work. If work is filed after two years and up to liy&^rs;after performance, it can only be claimed at 500Xo of the Total Value of Assessment Work. If this situationrappiles to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0.50: Total S value of worked claimed.

jte:Work older than 5 years is noKeligible for creditA recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

rtification verifying costs:

S4 C. O C. Mi(.v\r o_____, do hereby certify, that the amounts shown are as accurate as may reasonably(ptoasa print fulnam*) ,

determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying

;laration of Work form as(n*oord*d

•i±yl am authorized to make this certificatior

0197)

\

Date

MAR 2 1 2023GEOSCIENCE ASSESSMENT _____OfFICE_____

Ministry ofNorthern Developmentand Mines

July 26, 2000

Steve MunroDIA BRAS EXPLORATION INC.#201-1750 BRIMLEY ROADSCARBOROUGH, ONTARIOM1P-4X7

Dear Sir or Madam:

Subject: Transaction Number(s):

Ministere du Developpement du Nord et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (888)415-9845 Fax: (877)670-1555

Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Submission Number: 2.20158

StatusW0060.00122 Approval After Notice

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact JIM MCAULEY by e-mail at james.mcauley@ndm.gov.on.ea or by telephone at (705) 670-5880.

Yours sincerely,

ORIGINAL SIGNED BYSteve B. BeneteauActing Supervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 15103 Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.20158

Date Correspondence Sent: July 26, 2000________________________Assessor:JIM MCAULEY^^^^———^^^^^^—^^^^

Transaction First ClaimNumber Number Township(s)/Area(s) Status Approval Date

W0060.00122 1225321 BOURINOT Approval After Notice July 23,2000

Section:16 Drilling PDRILL

The 45 days outlined in the Notice dated June 8, 2000 have passed and the information provided (photocopies of invoices) has been reviewed.

The assessment credit is being approved for the amount indicated in the original submission. The TOTAL VALUE of assessment credit that will be allowed, based on the information provided in this submission, is S43,410.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

Correspondence to: Recorded Holder(s) and/or Agent(s):Resident Geologist Steve MunroSouth Porcupine, ON DIA BRAS EXPLORATION INC.

SCARBOROUGH, ONTARIO Assessment Files Library Sudbury, ON

Page: 1Correspondence ID: 15103

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