DD RPT 30 FRY LAKE€¦ · lykx geolog f -interval k l (units - m eters) e a y g from -to k f e l y g p l r r r p l r r r p l r r p l r p l r r r r r n l p l r r r p l r r 108.70

52oe3Nweei5 ae FRY LAKE 010

DIAMOND DRILLING

AREA: FRY LAKE REPORT NO: 30

WORK PERFORMED FOR: Umex Inc.

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

CI

Pa Pa

Pa Pa

Pa Pa

Pa Pa

Pa

Pa

a d. m No.

844440/ 912796

8444S9/ 912795

844440/ 912796

844441/ 844438

844436

844442/

Hole No.

BAM88-7

BAM-88-8

BAM-88-9

BAM-88-10

BAM-11

BAM-12

Footage

176.56m

169

129

169

178

178

.47m

.93m

.77m

.92m

.92m

Date

Aug/88

Aug/88

Aug/88

Aug/88

Aug/88

Aug/88

Note

(1 )

(1)

O )

(1)

O )

(1 )Pa 844437

Pa 844440/Pa 912796

BAM-88-13 200.25m Aug/88 (1)

NOTES: (1) #W8803.280, filed Feb/89

LYNX Geosystems I ne

PROJECT IDEM : BAMAJI COLLAR NORTHING: -250.00 CLAIM # : P a 844440/Pa 912796

UMEX INC. BAMAJI LAKE PROPERTY

DRILLHOLE/TRAVERSE : BAM88 7

START DATE COLLAR EASTING TOTAL LENGTH

88/ 8/13-350.00175.56

COMPLETION DATE : 88/ 8/U COLLAR ELEVATION: 390.00 CORE/HOLE SIZE : BQ

PAGE: 1 DATE:

GEOLOGGED BY GRID AZIMUTH

ROD t 335.00

KEY

KEY

P

PLRR

PLRR

PL

pLR RR

PLR

PLRRRR

F -INL (UNITS =AG FRO

FLG

OVB 0.00

10.60

SUL 10.60SUL 10.60

17.32

17.3217.32

21 .05

21 .80

LIT 21.80 LIT 21.80LIT 21.80

24.80

TEX 24.80

25.44

25.4425.4426.0626.06

SURVEY FLAG

000001002003

T E R V A L -METERS)

M - T 0'

10.60

17.32

17.3217.32

21 .05

21 .0521.05

21.80

24.80

24.80 24.8024.80

25.44

25.44

30.15

30.1530.1526.3626.36

SURVEY POINT FORESIGHT AZIMUTH VERTICAL ANGLE NORTHING EASTINGLOCATION (DEGREES) (DEGREES)

0.00 335.00 -47.0052.43 337.00 -46.0098.15 338.00 -41.00171.30 343.00 -38.00

CORE y, T YPI- QAL TEX- GRAIN FRAC- STRUCTUR-1 ALTERATION MINS ORE-TYPE MINSRECOV- M ROCK FYING MIN TURES CHARACS TURE H H H H H ANY H H H ANYERY I TM TM MAT TX TX F C '/o M T ID STK DIP A A A A A MIN A A A MIN

( X ) X TYPE 1 2 QM1 1 2 F F C P # TK 1 AZM RT QZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM QM2 TX TX S R S 0 DIP F T ID STK DIP KF MU CL EP HE HA PR MO SL HAQUAL MEM V Q LC- 3 3 4 0 N H 1 S ML I 2 AZM RT HHHHHHHHDESIG AGE COL R D P C STRUCTUR-2 AAAAAAAA

OVB P

MFVL AX CL AX5 FG MX 2 3 P L/ 25 V* Q) O DTPI DG PF CL2 WF LB L) DT

MINOR PY AND PO CONCENTRATED WITHIN EPIDOTE/CARB PILLOWSELVAGES.

TRON QZ FX QZ PO FO 4 5 P FO 53 I) F + P+ D) DT /""c^TT ̂7""]DA BI FX 10 /\ V ' - J --k/

OCCASIONAL BLUE QTZ EYES; WEAKLY TO MODERATELY FOLIATED, RARE /f^'^ i^DIORITE VEINS; WEAKLY SILICIFIED NEAR LOWER CONTACT. f .' . - r' 1 "^

MFVL CL AX BR IR 3 4 P L/ 47 P= D) l 'PI DG PF FR V - ^ l' '

TRON QZ FX MG LB 4 5 P FO 35 P= fJNT*,Mp jf^Ol-OGICAl SURVEY,AL LA MF L/ 18 A^SbSSMENT FILES (

POSSIBLY ALTERED GRANODIORITE, APPEARS LEUCOCRATIC AND O^FlCf i HORNBLENDE RICH; SEEMS TO CROSSCUT QUARTZ AND FELDSPAR VPORPHYRITIC TRONDJHEMITE; TWO PHASES OR TWO TYPES OF INTRUSIVE f)FP 1 C 1QQ3

MFVL CL AX FG SF P FO 48 0=0) '-'"AL DA L/ 35

SHEARED, CARBONATIZED MAFIC VOLCANIC. RECEIVED

TRON QZ FX PO FM 3 4 P FO 50 P= D) SEAL LB L/ 50 O B)

SILICIFIED, LOCALLY SHEARED TRONDJHEMITE WITH SHORT SHEAREDMAFIC VOLCANIC SECTIONS.STRONGLY CARBONATIZED, VUGGY SHEARED MAFIC VOLCANIC?; ABUNDANTEUHEDRAL PY CUBES.

LYUX GEOLOG

F -INTERVAL K L (UNITS s METERS) f. A Y G FROM -TO

K FE LY G

PAGE: Z D ATE: 68/HOV/25

N L

PLR TEXNLNL

P LR TEX R TEX

P L

P LR TEX R TEX

P LR TEX R TEX R TEX

P L R

P L R R

P LR LIT R LIT

26.06

30.15

30.1530.15

31 .65

32.25

32.2532.25

35.78

37.06

37.0637.06

38.40

38.4038.4038.40

43.01

43.01

47.60

47.6047.60

50.00

50.0050.00

26.36

32.25

32.2530.65

32.15

35.78

35.7835.78

37.06

38.40

38.4038.40

43.01

43.0143.0143.01

47.60

47.60

50.00

50.0050.00

52.30

52.3052.30

CORE

DRI

XRECOV- M ROCKF p Y ic r\ i

{ X

ROCKQUALDES1

J

) X TYPE

FOR EN RTMEM V Q

G AGE

X MFVLAL

MFVLAL

BIOT ITE RICHX MFVL

ALX MFVL

AL

TRONAL

UMEX INC. BAMAJI

LLHOLE/TRAVERSE : BAMSS,? (CONTINUED)

TYPI- GAL TEX- GRAIN FRAC- STRUCTURFYINGT M T ui n

i

LC-COL

CL

BIAB

i n

2

TM3

BICB

CLAX

MINU A THn 1

QM1

QM2

BI2AX5

, LOCALLYBIABBIAB

QZMA

CLAXCLAX

FXBI

BI2AX5BI2AX5

QZ3FX5

TURESTX T"

1

TX3

BKVU

FGIR

1 A

2

TX4

SF

BNFO

CHARACS TUREt r* w u

F

S0

2

STRONGLYFGVUFGIR

FOWP

BKFOBNFO

MG

2

2

4

u * n

F C P X T K

R S 0 DIP FN H 1 SML ID P C

N

3 P

CARBONATIZED.3 D

3 D

5 P

- 1

T ID STK DIP 1 AZM RT

T ID STK DIP2 AZM

o T p Mr tupO 1 K U Li 1 U ft

FO

FO

FO

FO

U/L/

RT-2

60

56

56

56

7037

iALTERATION MINS ORE-TYPE M1NSH H H

QZ BI CY

KF MU CLH

T)

0)

Q)

Q)

P +

H

CB

EPH

P =

B)

B)

B)

B*

H ANY H K H ANYA M T U A A A M 1 IdnniNA n n n t n

MG XX PY CP GL YY SUMMARY

HE HAH H

CB c)

CB< )CBO

QZP) 1*

PR MO SL HAH H H H

DT

D)

D)

D =

D) SEBT

INCREASING DEFORMATION AND SILICIFICATION DOWN SECTION PAST 33.38m

MFVL P AL AB AX AX5 IR FO

TRON QZ SE SF SH P FO 58 l'AL LG FX MY BK L/ 41

HIGHLY SHEARED, SERICITIZED TRONJ, DECREASING INTENSITY TOWARDS LOWER CONTACT.

MFVL AX CL AX5 FG MX 2 3 PPI DC PF CL2 UF LB

NUMEROUS CARBONATE VE1NLETS, STRINGERS AND POSSIBLY PILLOW SELVAGES; BIOTITE ALTERATION HALOES ADJACENT TO TRONJ AND GRANODIORITE DIKES.

DT

TRON QZ FX BK MFAL MA LB

POSSIBLY ALTERED FELSIC TUFF.

U/ FO

L/

66 I) 54

18

SE D*P*

TRON QZ FX BR IR 3 4 PAL LA MF

MEDIUM TO COARSE GRAINED AND LEUCOCRATIC; SILICIFIED BUT NO SULPHIDES.

MFVL AX CL AX5 FG MX 2 3 P V) E)PI DG PF CL2 LB LF

MASSIVE TO WEAKLY FOLIATED, LAMINATED/BANDED MAFIC VOLCANIC WITH NUMEROUS CROSSCUTTING THREADS OF CARBONATE AND QUARTZ.

W) X)

D*

LYNX GEOLOG

F -INTERVAL K L (UNITS s METERS) E A Y G F R O M - T O

K FE LY G

PLRR

PLR TEXR TEXNL

PLRRRRNL

PL

PLRRRRR

PLRRRR

PLR TEX

P

*

52.30

52.3052.30

55.48

60.0060.0060.00

62.63

62.6362.6362.6365.6565.65

68.22

68.92

68.9268.9268.9268.9268.92

74.87

74.8774.8774.8774.87

96.64

96.64

98.97

'

55.48

55.4855.48

62.63

62.6362.6362.63

68.22

68.2268.2268.2265.8065.80

68.92

74.87

74.8774.8774.8774.8774.87

96.64

96.6496.6496.6496.64

98.97

98.97

108.70

UHEX INC. BAMAJI

DRILLHOLE/TRAVERSE : BAM88- 7 (CONTINUED)

PAGE: 3 DATE: 88/HOV/25

CORE RECOV- c p y

C X )

X TYPI- OAL TEX- GRAIN FRAC- STRUCTUR-1 ALTERATION MINS ORE-TYPE WINS M ROCK FYING MIN TURES CHARACS TURE H H H H H ANY H H H ANY

X TYPE 1 2 OM1 1 2 F F C P # TK 1 AZM RT QZ B! CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM OM2 TX TX S R S O DIP FQUAL MEM VOLC-3 340NH/ SML IDESIG AGE COL R D P C

T ID STK DIP KF MU CL EP HE HA PR MO SL HA2 AZM RT HHHHHHHH

STRUCTUR-2 AAAAAAAA

TRON BI OZ QZ2 FM PO 3 5 P FO DA FX FX4 UF HO U/

MASSIVE TO WEAKLY FOLIATED QUARTZ- FE LDSPAR - B IOT I TE (TRONDJHEMITE?) PORPHYRY.

MFVL AX CL AX5 FG MX 2 3 P VCPI DG PF CL2 LB LF

LOCALLY BRECCIATED BY INTENSE QT Z - CARB - B I OT I TE VEINLETS WITH PY AND MINOR PO.

X MFVL AX CL AX5 FG MX 2 3 D PI DG PF CL2 LB LF

46 I + F2 45

50

VC 50 V1

TRON OZ FX QZ4 SF SH 3 5 P FO AL MA BI FX3 WP - U/

SHEARED, SILICIFIED, WEAK TO MODERATELY SERICITiZED TRONJ PORPHYRY; FAIRLY HOMOGENEOUS TEXTURE; RIBBONS SERICITIZED FELDSPAR HALO OF SERICITE ALTERATION.

X QZVN N VQ WH

PH

MFVL AX CL AX5 FG MX 2 3 PI DG PF CL2 LB LF

FO

4436

QTZ/FELDS OF QTZ *

43

51

X)

VI X)

B* Q +

QZ D) P)

D) + T

D + + T

SE D) PS

QZ V +

TRON SE OZ P FO 54 L+ < •^AL LG FX AG L/ 70

STRONGLY SERICITIZED, DECREASING IN INTENSITY TOWARDS LOWER CONTACT WHERE TRONJ TEXTURE BECOMES APPARENT;PY IS VERY FINELY DISSEMINATED, ALTHOUGH OCCASIONALLY OCCURS AS COARSER DISSEMINATIONS WITHIN QUARTZ VEINS; A VFG SILVER MINERAL PRESENT (GALENA?); ALSO MINOR SPHALERITE

2 3 P

DTD?

MFVL AX CL AX5 FG MX PI DG PF CL2 FG HO

FINE GRAINED, POSSIBLY PILLOW SELVAGES REPRESENTED BY QUARTZ+CARB BANDS WITH BIOTITE SELVAGES; ABUNDANT WISPS, THREADS OF CARBONATE; LOCAL PATCHY EPIDOTE AND SERICITE ALTERATION.

AND

TRON QZ FX OZ5 PO MX 3 5 PU/ 20 PW F1MA BI FX3 HO L/ 46

FELDSPAR PHENOCRYSTS WITHIN FINER QUARTZ/FELDS/BIOTITE MATRIX.

MFVL AX CL AX5 FG MX 2 3 P

C* DT

LYKX GEOLOG

F -INTERVAL K L (UNITS - M ETERS) E A Y G FROM -TO

K FE LY G

PLRRR

PLRRR

PLRR

PLR

PLRRRRRNL

PLRRR

PLRR

108.70

108.70108.70108.70

109.78

109.78109.78109.78

110.30

110.30110.30

11 1 .30

111 .30

119.65

119.65119.65119.65119.65122.90122.90

130.30

130.30130.30130.30

133.85

133.85133.85

109.78

109.78109.78109.78

110.30

110.30110.30110.30

111.30

111.30111 .30

119.65

119.65

130.30

130.30130.30130.30130.30123.35123.35

133.85

133.85133.85133.85

136.25

136.25136.25

UMEX INC. BAMAJI

DRILLHOLE/TRAVERSE : BAM88 7 (CONTINUED)

PAGE: 4 DATE; B6/HOV/15

CORE X TYPI- OAL TEX- GRAIN FRAC-RECOV- M ROCK FYING MIN TURES CHARACS TUREERY l TM TM MAT TX TX F C X M

( X ) X TYPE 1 2 QM1 1 2 F F C P it T K

STRUCTUR-1 ALTERATION MINS ORE-TYPE MINSH H H H H ANY H H H ANY

T ID STK DIP A A A A A MIN A A A MIN1 AZM RT QZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM OM2 TX TX S R S O DIP FQUAL MEM V Q LC- 3 3 4 O N H l S ML IDESIG AGE COL R D P C

PI DG PF CL2 FG HO


STRUCTUR-2 AAAAAAAA

TRON OZ FX MG MO P PHLA Bl GR L/ 39

LEUCOCRATIC TRONJ/GRANODIORITE, LOCALLY CATACLASTIC WITH SEVERAL B10TITIC CARBONATIZED MAFIC VOLC SECTIONS; SHEARING EVIDENT AT LOWER CONTACT.

FR FO 54 F2MFVL CL BI SF AL UB SH

SHEARED SILICIFIED MAFIC VOLCANIC, SHEARING INTENSITY INCREASES TO LOWER CONTACT WITH TRONJ; POSSIBLE CONTACT WAS LOCUS OF SHEAR; MINOR SERICITE.

DT

D)

TRON P-AL MA

SHEARED SILICIFIED TRONJ, INTENSITY DECREASING CONTACT. POOR SULPHIDE CONTENT.

MFVL AX CL AX5 FG MX 2 3 PPI DG PF CL2 WF LB

LOCAL PODS OF QUARTZ AND SILICIFICATION.

FO L/ TO

5640

PY

LYNX GEOLOG

K L (UNITS * METERS) E A Y G F R 0 M - T 0

1C FE LY G

LRRRR

PLRR

PLRRNLRNL

PLRRR

PL

PLR

PLRR

PLRRN

'

136.25136.25136.25136.25

138.85

138.85138.85

HI. H

U6.95H6.95H6.95

H7.91H7.91

H9.72

H9.72H9.72149.72

154.33

156.07

156.07

158.50

158.50158.50

166.86

166.86166.86169.35

138.85138.85138.85138.85

141.14

141 .14141.14

149.72

147.91147.91147.91

148.50148.50

154.33

154.33154.33154.33

156.07

158.50

158.50

166.86

166.86166.86

170.87

170.87170.87169.77

UMEX INC. BAMAJI

DRILLHOLE/TRAVERSE : 8AM88- 7 (CONTINUED)

PAGE: 5 DATE: B8/HOV/Z5

CORE RECOV ERY

( X )

ROCK QUAL DESIG

X H ROCK I X TYPE

FOR EN RT MEM V Q AGE

TYPI- OAL FYING HIM TM TM MAT

1 2 QM1

TM OM2 LC- 3 COL

TEX TURES TX TX

1 2

TX TX 3 4

GRAIN FRAC- CHARACS TURE F C X M F F C P (K TK

S R S 0 0 N H 1 R D P C

DIP F SML I

STRUCTUR-1 ALTERATION MIN! H H H H H 1

1 AZH RT OZ

T ID STK DIP KF 2 AZM RT

STRUCTUR-2

BI CY

Ml) CLH

CB MG

EP HE H H

; ORE^NY H MIN A XX PY

HA PR H H

TYPE MINS H H ANY A A MIN

CP GL YY

MO SL HA H H H

SUMMARY

AL GA FX FGLOCALLY QUARTZ VEINED, SILICIFIED, SER I C I T I ZED ; LOCALLY BRECCIATED TRONJ: INTENSELY SHEARED AND SILICIFIED; INITIAL 40CM ARE QUARTZ VEINED AND BRECC IATED- - POSSI BLY ALTERED MAFIC VOLCANIC.

MFVL AX BI FG LB AL AU FX BR FO

BIOTITIC, LOCALLY SERICITIC, DECREASING IN INTENSITY DOWN

FO FG

QUARTZ VEINED SECTION.

5 FO 25 V+ F3U/ 24

MAFIC VOLCANIC;

LYNX GEOLOG

F -IN K L (UNITS E A Y G FROM

PAGE: 6 DATE:

T E R V A L METERS)

T O

K FE LY G

170.87

170.87170.87170.87

175.56

175175

5656

175.56

UMEX INC. BAMAJI


CORE X TYPI- QAL TEX- GRAIN FRAC-RECOV- M ROCK FY1NG KIN TURES CHARACS TUREERY I TM TM MAT TX TX f C X M

( X ) X TYPE 1 2 QM1 1 2 F F C P # U

STRUCTUR-1 ALTERATION HINS ORE-TYPE MINSH H H H H ANY H H H ANY

T ID STK DIP A A A A A HIN A A A MIN 1 A2M RT QZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM QM2 TX TX S R S O DIP FQUAL MEM VQLC-3 340NH/ SML IDESIG AGE COL R D P C

T ID STK DIP KF MD CL EP HE HA PR HO SL HA2 AZM RT HHHHHHHH

STRUCTUR-2 AAAAAAAA

AL GU AX FO

FO MXMFVL AX CL PI DG BI

WEAK PERVASIVE SILICIFICATION AND THIN QUARTZ VEINLETS; PILLOW SELVAGES AT LOW ANGLE TO C.A. END OF HOLE-175.56 m; CASING LEFT IN; CORE STORED AT UMEX MINE

LYNX Geosystems l ne

PROJECT IDEN : BAMAJI COLLAR NORTHING: -200.00 CLAIM #: Pa 844439/Pa 912795

PAGE: 1 DATE:UMEX INC.

BAMAJI LAKE PROPERTY



88/ 8/15-500.00169.47

COMPLETION DATE : 88/ 8/16 COLLAR ELEVATION: 390.00 CORE/HOLE SIZE : BQ


ROD * 335.00

SURVEY FLAG

KEY

KEY

P

PLRR

PLRRRRRRRRR

PLRR

PLRR

PL

F - I N TL (UNITS =AG FROM

FLG

0.00

10.04

10.0410 .04

16.54

16.5416.5416.5416.5416.5416.5416.5423.0026.32

30.94

30.9430.94

42.98

42.9842.98

58.55

000 001 002003

E R V A LMETERS)

T 0

10.04

16.54

16.5416.54

30.94

30.9430.9430.9430.9430.9430.9430.9423.2027.82

42.98

42.9842.98

58.55

58. 5558.55

69.20

SURVEY POINT FORESIGHT AZIMUTH VERTICAL ANGLE NORTHING EASTING LOCATION (DEGREES) (DEGREES)

0.00 335.00 -47.00 58.37 337.00 -46.00 113.20 341.00 -41.00 168.00 344.00 -38.00

CORE y. T YPI- QAL TEX- GRAIN FRAC- RECOV- M ROCK FYING MIN TURES CHARACS TURE ERY I TMTMMATTXTXFCKM

( X ) X TYPE 1 2 QM1 1 2 F F C P # T K

ROCK FOR EN RT TH QM2 TX TX S R S 0 DIP F QUAL MEM V Q LC- 3 3 4 0 N H 1 S ML I DESIG AGE COL R D P C

OVB P

TRON QZ FX QZ4 MY MG 2 5 P

STRUCTUR-1 ALTERATION MINS ORE-TYPE MINS H H H H H ANY H H H ANY

T ID STK DIP A A A A A MIN A A A MIN 1 AZM RT QZ BI CY CB MG XX PY CP GL YY SUMMARY

T ID STK DIP KF MU CL EP HE HA PR MO SL HA 2 A ZM RT H H H H H H H H

STRUCTUR-2 AAAAAAAA

FO 60 \ -

LYN* GEOLOGUMEX INC.

BAMAJI


PAGE: 2 DATE: 88/NOV/25

f - INTERVAL- K L (UNITS * METERS) E A Y G F R 0 M - T 0

K FE L Y G

RR

PL

PLR

PLRRRNLNLNL

PLRR

PLRRR

PLRRR

PL

PL

58.5558.55

69.20

72.24

72.24

76.45

76.4576.4582.4282.42

91.00

92.64

103.95

103.95103.95

106.57

106.57106.57106.57

107.71

107.71107.71107.71

110.86

113.33

69.2069.20

72.24

76.45

76.45

103.95

103.95103.9582.7282.72

91.62

93.57

106.57

106.57106.57

107.71

107.71107.71107.74

110.86

110.86110.86110.86

113.33

114.40

CORE X TYPI- DAL TEX- GRAIN FRAC- STRUCTUR-1 ALTERATION MINS ORE-TYPE M1NS RECOV- M ROCK FYING HIM TURES CHARACS TURE K H H H H ANY H H H ANY

( X ) X TYPE 1 2 OM1 1 2 F F C P # TK 1 A2M RT OZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM QM2 TX TX S R S 0 DIP F T ID STK DIP KF MU CL EP HE HA PR MO SL HAQUAL MEM V Q LC- 3 3 4 0 N H 1 S ML I 2 AZM RT H H H H H H H H

WEAK TO MODERATELY SHEARED AND SERIC1T1ZED, POOR SULPHIDECONTENT.

TRON OZ FX OZ IH PA PMA MF FX MG

TRON OZ FX QZ4 SH MY P FO 40 I+ SE D)AL GA SE FX3 WP P*

LOCALLY STRONGLY SHEARED AND SERICITIZED

TRON QZ FX OZ MG WP P FO 62MA MF FX HO WF

AS AT 42.98m, FAIRLY CONSISTENT WEAKLY FOLIATED TRONJ/GDWITH SHORT SECTIONS OF QUARTZ - FE LDSPAR PORPHYRY.XENOLITH?

X MFVL AX BI FO FG N F1 P1 D*AL DG CL

X TRON QZ FX QZ SH MY D FO 54 Is SE D) QZAL MA MF FX BR WF P* P+

X TRON QZ FX QZ4 SH BN 2 5 D FO 35 \ * Q Z D)AL GA SE SE2 PO WF Q

TRON QZ FX QZ4 SH BN 2 5 P FO 35 Is QZ D)AL GA SE SE2 PO Q+ Q+ PS

STRONGLY AL T E RED , SHE ARED WITH UBIQUITOUS BLUE QUARTZ EYES;ABUNDANT SERICITE, SILICA AND SOME HEMATITE AND EPIDOTE.

MFVL AX BI AX5 FG FO 3 4 P FO 40 PM F1 < * Q V *) DTAL DG PF PF3 QV LB VO 43 0+ V+ *)

SILICIFIED, WEAKLY SHEARED MV, STRONGER AT UPPER CONTACT:QUARTZ STRINGERS AND PATCHY MINOR EPIDOTE; UPPER CONTACT0 DEGREES TO C . A . ; BROWN AND GREEN AMPHIBOLE AT L/.

TRON QZ SE SH BN P FO 27 P* AK D*AL LA U/ 33 X+ B?

SERICITIZED, LOCALLY BLEACHED AND SILICIFIED, SHEARED TRONJ ORFELSIC/INTERMEDIATE VOLCANIC TUFF; DEFORMATION DECREASES DOWNSECTION.

MFVL AX CL FG FO P FO 26 PW O QZ **DG FX L/ 38 Os **

TRON OZ FX FM FM 3 5 P FO 36 DTLA BI LB

LYHX GEOLOG

f - INTERVAL K L (UNITS = METERS) E A Y G F R 0 M - T 0

K FE LY G

PLRNL

PLRRRRRRR

PLRR

PLRRR

PLKRRR

PLRRNL

114.40

114.40115.50

116.53

116.53116.53116.53116.53116.53116.53116.53

120.98

120.98120.98

123.50

123.50123.50123.50

130.85

130.85130.85130.85130.85

164.50

165.38165.38165.38

'

116.53

116.53115.85

120.98

120.98120.98120.98120.98120.98120.98120.98

123.50

123.50123.50

130.85

130.85130.85130.85

164.50

164.50164.50164.50164.50

169.47

165.68169.47165.68

UHEX INC. BAMAJI


PAGE: 3 DATE; SSfHOV/ZS

CORE X TYPI- OAL TEX- GRAIN FRAC-RECOV- H ROCK FYING MIN TURES CHARACS TUREERY I TM TH MAT TX TX F C X M

( X ) X TYPE 1 2 QM1 l 2 F F C P # TK 1


ID STIC DIP A A A A A MIN A A A HINAZM RT OZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM QM2 TX TX S R S O DIP FOUAL MEM V Q LC- 3 3 4 O N H l S ML IDESIG AGE COL R D P C

T ID STK DIP KF HU CL EP HE HA PR MO SL HA2 AZM RT HHHHHHHH

STRUCTUR-2 AAAAAAAA

FETF QZ FX FM FO 4 5 PLG SE PO

SHARP CONTACTS; COULD BE SHEARED ALTERED TRONJ.X TRON QZ FX FM FO 3 5 N

LA BI LB

FO

FO

40 11

53 X*MFVL AX FX SH QV 2 4 PAL GA CL FM LB

SHEARED, LOCALLY BANDED AND POSSIBLY BRECCIATED; SULPHIDES INCREASE WHERE QUARTZ PRESENT; TOWARDS LOWER CONTACT BANDING INCREASES, AND A GREYISH VERY FINE GRAINED MASSIVE ROCK IS PRESENT, WITH SOME GARNETS; ULTRAMYLONITE (?); LOCAL SERICITIZATION; FAINT OUTLINES OF FRAGMENTS LOCALLY MAY INDICATE BRECCIATION OR POSSIBLY ALTERED AGGLOMERATE; SEVERAL Z-FOLDS APPARENT.

FO 32 I?TRON QZ SE OZ4 SH PO PAL LG FX SE3 FM

COULD BE FELSIC TUFF, SEVERAL SHORT SECTIONS ARE VERY STRONGLY SHEARED AND PYRITIC; SOME CRENULAT IONS.

FOMFVL AX CL FO FG PPI DG FX CR LB

PERVASIVE WEAK TO MODERATE SILICIFICATION AT UPPER CONTACT DECREASING DOWN SECTION; ALSO SOME QUARTZ VEINS; CONTORTED PILLOW SELVAGES TYPICAL.

32 PW E)

FO 55 QWTRON QZ FX WF MG PMA BI HO

HOMOGENEOUS TRONJ/GD WITH LOCAL SHEARED AND BANDED SECTIONS; WEAK TO NIL SERICITIZATION; HAZY, WEAKLY ALTERED TEXTURE; LOCALLY GOOD DEVELOPMENT OF BLUE QUARTZ EYES AND PORPHYRITIC TEXTURE.

MFVL AX CL FG MX P GV 40 V) E+FX GV U/ 34

STRONGLY CARBONATI ZED, QUARTZ VEINLETS, STRINGERS, PO AND PY. END OF HOLE; CASING LEFT IN; CORE STORED AT UMEX MINE.

X MFVL AX CL FG MX D GV 40 V+ E+ FX GV U/ 34

X +

Q)

S)

DT

OZ D) DT S +

GN ET

D)

D*

QZ D* V) +T

QZ PW

QZ PW

OZ S)

Geosystems I ne




PAGE: 1 DATE: 88/NOV/25 A 9


88/ 8/18 250.00129.93



ROD * 335.00

SURVEY FLAG

KEY

KEY

P

PLRRRR

PLR

PLR

PLR

PL

PLRRRRRR

F -INL (UNITS =AG FRO

FLG

0.00

3.28

3.283.283.283.28

9.58

9.58

9.88

9.88

11 .40

11 .40

13.90

16.62

16.6216.6216.6216.6216.6216.62

000 001002

T E R V A LMETERS)

M - T 0

3.28

9. 58

9.589.589.589.58

9.88

9.88

11 .40

11 .40

13.90

13.90

16.62

22.82

22.8222.8222.8222.8222.8222.82


0.00 335.00 -46.00 61.57 337.00 -44.00 128.63 329.00 -42.00

CORE '/, T YPI- DAL TEX- GRAIN FRAC- RECOV- M ROCK FYING MIN TURES CHARACS TURE ERY I TM TM MAT TX TX F C X M

( '/, ) XTYPE 1 2QM1 1 2FFCP # TK

ROCK FOR EN RT TM QM2 TX TX S R S 0 DIP F QUAL MEM V Q LC- 3 3 4 0 N H / SML I DESIG AGE COL R D P C

OVB P

TRON QZ SE QZ3 SH PO 3 5 P


T ID STK DIP A A A A A MIN A A A MIN 1 AZM RT QZ BI CY CB MG XX PY CP GL YY SUMMARY

T ID STK DIP KF MU CL EP HE HA PR MO SL HA 2 AZM RT HHHHHHHH

STRUCTUR-2 AAAAAAAA

FO 45 12 < = -eT TO D) DTAL LG FX SE5 BK

STRONGLY SHEARED SERICITIZED TRONJ OR FELSIC TUFF. NUMEROUS STRINGERS AND FRACTURE FILLS OF B IOTI T E- -HALOE S AROUND FRACTURES; BLACK, HARD ELONGATE MINERAL POSSIBLY HORNBLENDE OR TOURMALINE.

D?

MFVL AXAL DG CL

POSSIBLY A XENOLITH.

FO FG

QFPO QZ FX QZ3 WF PO 3 5DA BI FX4 FM BK

QUARTZ FELDSPAR BIOTITE TRONJ ?

TRON QZ SE QZ3 SH POAL LG FX SE5 BK

POSSIBLE INCREASE IN THIN QUARTZ VEINS.

QFPO QZ FX QZ3 WF PO 2 4DA BI FX4 FM BK

FO

FO

FO

FO

43 F1

35 PU F2

48

40 PM

P=

B)

TRON QZ FX FM BR P FO 45 PM E+AL LG SE FO BK L/ 15

SIMILIAR TO 3.28m EXCEPT FEATURES LOCAL BRECCIATED SILICIFIED SECTIONS WHERE SULPHIDE CONTENT INCREASES. BRECCIATED APPEARING SECTIONS ARE CROSSCUT BY STOCKWORKS OF FRACTURES WITH HALOES OF ALTERATION POSSIBLY SILICA AND BIOTITE. GENERALLY LACKS THE QUARTZ EYES OF 3.28m. FRACTURES TEND TO BE LOW ANGLE TO CORE AXIS.

D*

D)

D)

D) O*

D)

PY t*

PY

GEOIOG

K L (UNITS z METERS) E A Y G F R 0 M - T 0

K FE LY G

PLRRRRRRRR

PLR

PLRRRRRNL

PL

PL

PLRR

PLRR

PL

22.82

22.8222.8222.8222.8222.8222.8222.8222.82

24.95

24.95

26.47

26.4726.4726.4731.6731 .6731 .67

34.21

43.95

44.50

44.5044.50

45.30

45.3045.30

46.15

24.95

24.9524.9524.9524.9524.9524.9524.9524.95

26.47

26.47

34.21

34.1134.1134.1133.1733.1733.17

43.95

44.50

45.30

45.3045.30

46.15

46.1546.15

47.11

UHEX INC. BAMAJI


PAGE: Z D ATE: 88/NOV/25

CORE X TYPI- CAL TEX- GRAIN FRAC-RECOV- M ROCK FYING MIN TURES CHARACS TUREERY I TM TM MAT TX TX F C X M

( X ) X TYPE 1 2 OM1 1 2 F F C P # TK


ID STK DIP A A A A A MIN A A A MINAZM RT QZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM OM2 TX TX S R S O DIP FQUAL MEM VQLC-3 3 4 O N H X SML IDESIG AGE COL R D P C

FR


STRUCTUR-2 AAAAAAAA

BN 17 V2MFVL AX CL FG AL AU 02 QV

CONTACT WITH TRONJ IS ARBITRARY; BASED ON CHLORITE, AMPHIBOLE CONTENT AND INTENSE SILICA FLOODING. VERY SILICEOUS YET MAFIC CONTENT WOULD INDICATE POSSIBLE VOLCANIC ORIGIN. SULPHIDES APPEAR RELATED TO SHALLOW FRACTURING AND QUARTZ FLOODING. LOCAL BROWN/REDDISH CAST IS POSSIBLY DUE TO PERVASIVE HEMATIZATION AS WELL AS B IOTI T E;OR I G INAL MAFIC VOLC TEXTURE OBLITERATED BY FRACTURING AND LIGHT GREY QUARTZ BANDS AND VEINS. CORE AQ FROM 23.47-26.50.

DS DTDT

SI

MFVL

L ICI FIED

FETF

AXDA

VAR

QZ

PFBI

IOL

FX

me

QZ5

VAFOMAF

MX

FM

1C

MF

3 4

VOLCANIC.

FO

FO

18 PW F1

45 V*

l fl|X GEOLOG

K L (UNITS = M ETERS) E A Y G F R 0 M - T 0

K FE LY G

R

PLRRNL

PLR

PL

PLR

PLRRRRRNLRNLNL

PLRR

PLRR

46.15

47.11

47.1149.0849.08

52.40

52.40

53.67

54.57

54.57

56.57

56.5756.5756.5756.5756.5757.50

57.9457.94

60.05

61 .47

61 .4761 .47

62.60

62.6062.60

47.11

52.40

52.4049.3849.38

53.67

53.67

54.57

56.57

56.57

61.47

61.4761.4761 .4761 .4761 .4757.80

58.5958.59

60.80

62.60

62.6062.60

63.95

63.9563.95

UHEX INC. BAMAJI


PAGE; 3 DATE: 88/NOV/E5

CORE RECOV ERY

( X )

ROCK QUAL DES1G

X M I X

FOR MEM AGE

ROCK

TYPE

EN RT V Q

TYPI - FYING TM TM

1 2

LC- COL

TM 3

QAL MIN MAT QM1

QM2

TEX TURES TX TX

1 2

TX 3

TX 4

GRAIN FRAC- CHARACS TURE F C X M F F C P # TK

S 0 R

R N D

SH P

0 1 C

DIP F SML I

T 1

T 2

STRUCTUR-1 ALTERATION MINi H H H H H y

AZM RT QZ BI

ID STK DIP KF MU AZM RT

STRUCTUR-2

CY

CLH

CB

EPH

MG

HE H

5 ORE' tNY H MIN A XX PY

HA H

PR H


CP GL YY

MO H

SLH

HA H

SUMMARY

FAIRLY SHARP LOWER CONTACT WITH PILLOWED MAFIC VOLCANICS.

MFVL AX CL FG MX 2 3 PPI DG FX

SEVERAL CROSSCUTTING TRONJ DIKES. DOWNHOLE HALO OF BIOTITE ALTERATION

X TRON QZ FX N U/ 80 MA MF

QFPO QZ FX PO FM 2 5DA MF MX

FELDSPAR PHENOCRYSTS PREDOMINATE.

U/ L/

5447

MFVL AX CL PI DG FX

FG MX 2 3

F1TRON QZ FX QZ SH PO P FO 49 11AL MA BI FX AU U/ 51

QUARTZ AND FELDSPAR PORPHYRITIC ALTERED TRONJ OR FELSIC TUFF.

MFVL AX CL FG MX 2 3 PPI DG FX

UPPER CONTACT MARKED BY SEVERAL GREY AND WHITE QUARTZ VEINS. SECTION CONTAINS TWO SHORT DISCRETE ZONES OF STRONG BIOTITE ALTERATION WITH QUARTZ STRINGERS AND SULPHIDES. ZONES: 1) 57.50-57.80m

2) 57.94-58.59m X MFVL AX CL FG MX 2 3 D S+ F2

PI DG FX QUARTZ STRINGERS USUALLY CONTORTED.

X MFVL AX CL FG MX 2 3 D FO 35 S+ F2PI DG FX

X TRON QZ FX FO MG N U/ 65 MA BI WP L/ 53

TRON OZ FX SH AU 2 4AL MA SE WP

DEFORMATION INCREASES DOWN SECTION. TRONJ OR FELSIC TUFF.

P FO 54L/ 38

FAIRLY TYPICAL SHEARED

F1

FO 54 V+ F1OZBS QZ BI 023 BR FO PUG AX AX3 QV IR

CORRELATES WITH QUARTZ BRECCIA SHEAR ZONE IN BAM-06. CONSISTS OF ROUNDED, ELLIPSOIDAL BROWNISH FRAGMENTS HAPHAZARDLY

D)

D)

CT 0)

F1

D) D* D*

D) D*D*DT

D)

D+ D*

D)

LY^X GEOLOG PAGE: 4 DATE: 88/NOV/25

F -INTERVAL K L (UNITS * METERS) E A Y G F R 0 M - T 0

K FE LY G

RRRRRRRRR

PLRRRRNL

PLRRR

PLRRRRRNLRRRNLRRRR

62.6062.6062.6062.6062.6062.6062.6062.6062.60

63.95

63.9563.9563.9570.5970.59

72.56

72.5672.5672.56

103.25

103.25103.25105.87105.87105.87105.87

109.00109.00109.00109.00

125.95125.95125.95129.80

'

63.9563.9563.9563.9563.9563.9563.9563.9563.95

72.56

72.5672.5672.5671.5171 .51

103.25

103.25103.25103.25

129.93

129.93129.93106.17106.17106.17106.17

109.90109.90109.90109.90

129.80129.80129.80129.93

UMEX INC. BAMAJI


CORE RECOV ERY

( X )

ROCK QUAL DES1G

X M I X

FOR MEM AGE

ROCK

TYPE

EN RT V Q

TYP1 - FYING TM TM

1 2

LC- COL

TM 3

QAL TEX- MIN TURES MAT TX TX QM1 1 2

QM2 TX 3

TX4

GRAIN FRAC- CHARACS TURE F C X M F F C P # TK

S R 0 N R D

S H P

0 1 C

DIP F SML I

T 1

T 2

STRUCTl

ID STK AZM

JR-1 ALTERATION MIN! H H H H H 1

RT 02

ID STK DIP KF AZM RT

STRUCTUR-2

BI CY

MU CL H

CB

EPH

MG

HE H

5 ORE kNY H MIN A XX PY

HA H

PR H


CP GL YY

MO H

SLH

HA H

SUMMARY

DISTRIBUTED; SEPARATED BY BIOTITIC, CHLORITIC AND PYRITICFRACTURE FILLINGS. WHITE QUARTZ OCCURS AS PODS AND CONTORTEDOR BRECCIATED VEINS AND VEINLETS. BROWNISH CAST IN PART DUE TOBIOTITE CONTENT.POSSIBLY TWO GENERATIONS OF SULPHI DE - VERY FINE GRAINED AND ALATER COARSE FRACTURE FILLING TYPE. IRREGULAR TEXTURE MAKESCORE ANGLE MEASUREMENTS DIFFICULT.CALCITE MINOR CONSTITUENT. ANKERITE STAINING IS WEAKLYPOSITIVE. WtCLY MAGNETIC DUE TO PO OR POSSIBLY TRACE MAGNETITE

MFVL AX CL FO FG 2 3 P FO 51 V) E)PI DG FX 0V FO 55

LOCALLY SILICIFIED AND BIOTITIC AND CONTAINS SEVERAL SECTIONS OF BRECCIATED CONTORTED QUARTZ VEINS; FOLIATION DECREASING DOWN SECTION. SHEARED, SERICITIZED TRONJ OR FELSIC TUFF.

X TRON QZ FX ? SH AU N FO 65 AL MA SE WP U/ 80

TRON QZ FX MX WF 3 5 P FO 52 11 F1MA BI WP U/ 45

LOCAL QUARTZ VEINS AND SHEARED SECTIONS. BLUE OTZ EYES COMMON. SOME SECTIONS FEATURE HAZY ALTERED TEXTURE- SERICITE AND/OR SAUSSERITIZATION OF FELDSPARS AND WEAK SILICIFICATION.

MX 2 3 * FO U/

BIOTITE,

28 Q) 0+ 58

QUARTZ-

42 0) F +

MFVL AX CL AX6 FG PI DG FX FX3 WF

TYPICAL PILLOWED MAFIC VOLCANIC WITH LOCAL CARB SHEARED SECTIONS.LIGHT GREEN AND YELLOW ELONGATE ELLIPSOIDAL FRAGMENTS, WITH FRACTURES INFILLED WITH LATER QUARTZ. A VERY DISCRETE ZONE WITH POOR SULPHIDE CONTENT.

X OZBS QZ BI BR SH N FOLA

DISCRETE ZONE OF SHEARED, QUARTZ-CARB * BIOTITE RICH VOLCANIC, WITH 3-4X SULPHIDES. SOME COARSE EUHEDRAL WELL AS FINE DISSEMINATIONS.

X MFVL AX 02 SH QV N FOAL UG BI FG

SEVERAL THIN QUARTZ VEINS WITH SULPHIDES; PATCHES OF CALCITE AND COARSE AX CRYSTALS. QV'S 40 DECS TO C.A. AT 126.0m. LAST LAST 8 cm OF HOLE IS EPIDOTIZED TRONJ. END OF HOLE-129.93 m; CASING LEFT IN; CORE STORED AT UMEX MINE

MAFIC PYRITE AS

38 V* F1

4*

D*

Q)

D)

D+ D* D)







88/ 8/21100.00169.77

COMPLETION DATE : 88/ 8/22 COLLAR ELEVATION: 400.00 CORE/HOLE SIZE : 8Q


ROD * 335.00

SURVEY FLAG

000001002003

F -INTERVALL {UNITS s METERS)AG FROM - TO

SURVEY POINT LOCATION

0.00 55.47 110.34 162.15

CORE XRECOV ERY

( X )

ROCKQUAL DESIG

MIX

FORMEM AGE

ROCK

TYPE

EN RTV Q

FORESIGHT

TYPI- QAL TEX-FYITM

1

LC- COL

NGTM2

TM3

MINMATOM1

QM2

TURESTX

1

TX3

TX2

TX4

AZIMUTH (DEGREES)

335.00 335.50 338.00 342.00

GRAIN FRAC-CHARACSF CF F

S R0 N R D

X MC P

S 0H / P C

VERTICAL ANGLE (DEGREES)

47.00 -45.00 43.00 42.00

STRUCTUR-1TURE

aDIPSML

TK

FI

T1

T2

ID STK DIPAZM RT

ID STK DIPAZM RT

STRUCTUR-2

NORTHING EASTING

ALTERATION MINS ORE-TYPE MINSHA

QZ

KF

HA

B!

MU

HA

CY

CLH

HA

CB

EPH

H ANY HA

MG

HEH

MIN AXX PY

HA PRH H

HA

CP

MOH

H ANYA

GL

SLH

MINYY

HAH

SUMMARY

0.00

1.50

1 .501.50

12.40

12.4013.53

15.78

15.7815.7815.7815.7822.10

33.42

33.4233.4236.9237.5238.56

1.50

12.40

12.4012.40

15.78

15.7813.93

33.42

33.4233.4233.4233.4223.00

39. 16

39.1639. 1637.0638.3138.74

OVB

MFVL AX CL AX6 MX FG DG FX CL

S) E)

LOCAL THIN SHEARS WITH SOME QUARTZ AND CARB; BIOTITIC HALOES AROUND TRONDJHEMITE DIKES AND QUARTZ VEINS.

POZFP OZ FX DA MF

PO FM MX XE

U/L/

64 PM 37

QTZ-FELDSPAR TRONJ PORPHYRY ? RARE BLUE OZ EYES; FOL'N 55 DEG X MFVL AX CL FG WF N FO 51 FW

DG FX

MFVL AX CL AX6 MX FG FO 47

FOLIATION VARIES LOCAL BANDING, SOMETIMES CONTORTED; SMALL SCALE FOLDING APPARENT IN SOME SECTIONS; NUMEROUS BLEBS, STRINGERS AND GASHES OF CARBONATE. LOCAL BIOTITIC, OUARTZ-CARB VEINED SHEARS.

X MFVL AX CL AX6 SH BR D FO 65 V) F1

TRON QZ SE QZ3 SH FG FO 74AL MA FX SE1 WP U/ 68

SHEARED QUARTZ FELDSPAR TRONJ PORPHYRY WITH POOR SULPHIDE CONTENT.

X QZVNX MFVLX QZVN

SU FGBN FOFG FR

AW

L/ FO U/L/

65646570

•cT QZ V)

* * Q Z * * Q*

Q+ CB *) X* S) D*

P5 CB D) X* S) D)

4) D*

LYNX GEOLOG

P L R R R R R R N L R R R R R N L R N L

PL R R R N

UMEX INC. BAMAJI

DRILLHOLE/TRAVERSE t BAM88 10 (CONTINUED)

PAGE: 2 DAU: &B/NOW25

K EY

KE Y

F -INTERVAL- L (UNITS * METERS) A G F R 0 M - T 0

F L G

CORE RECOV ERY

( X )

ROCK QUAL DESIG

X M ROCK I X TYPE

FOR EN RT MEH V Q AGE

TYPI- OAL FY1NG MIN TM TM MAT

1 2 O M1

TM OM2 LC- 3 COL

TEX- GRAIN FRAC TURES CHARACS TURE TX TX F C X M

1 2 F F C P # TK

TX TX S R S 0 DIP F 3 it 0 N H 1 S ML I

R D P C

T 1

T 2

STRUCTUR-1

AZM RT

ID STK DIP AZM RT

STRUCTUR-2

ALTERATION MINS ORE H H H H H ANY H

OZ Bl CY

KF MU CLH

CB MG XX PY

EP HE HA PR K H H H


CP GL YY

MO SL HA H H H

SUMMARY

PLRRRRRRRRRRNL

46.36

46.3646.3646.3646.3646.3646.3646.3646.3646.8546.8546.85

54.07

54.0754.0754.0754.0754.0754.0754.0754.0747.2547.2547.25

54.07

54.0754.0754.0754.0754.0772.7572.75

74.5576.7576.7576.7576.7576.75

103.82103.82

107.14

107.14107.14107.14113.46

107,14

107.14107.14107.14107.14107.1474.5074.50

75.2378.0778.0778.0778.0778.07

104.44104.44

115.86

115.86115.86115.86113.76

PI DG FX FG

TRON OZ SE SH FG P FO 56 I* F+AL MA FX WP BN L/ 54

FAIRLY TYPICAL SHEARED TRONJ UNTIL 51.35m WHERE IRREGULAR "BRECCIATED"? TEXTURE IS EVIDENT, CONSISTING OF DARK RED/BROWNISH ROUNDED AND ELONGATE PODS OF SILICEOUS MATERIAL ENCLOSED BY MAFICS( AX, CHLORITE, POSSIBLY BIOTITE AND CARBONATE MATERIAL); TEXTURALLY RESEMBLES QZBR SHEAR ZONE BUT LACKS SECONDARY SILICIFICATION; GOOD SULPHIDE CONTENT AFTER 51.35 WITH PYRITE AND PO. SHARP I f W ITH SHEARED MAFIC VOLCANICS.INTENSLY SHEARED, BROKEN, RUBBLY, STRONGLY SERICITIC AND CARBONATED WITH IX SULPHIDES.

X TRON OZ SE SH BK D ' FO 56 I* F+ AL MA FX WP BN L/ 54

MFVL AX CL SF FG P FO 53 S) E*AL DG FX PI BN 22

ABUNDANT QUARTZ STRINGERS, FRACTURE FILLS; NUMEROUS CONTORTED QTZ+-CARB+-BIOTITE BANDS, POSSIBLE PILLOW SELVAGES; FOLIATION AND BANDS ARE SHALLOW TO CORE AXIS; SULPHIDES USUALLY FOUND IN BANDS WITH OTZ,CARB,B lOTITE; SEVERAL SHORT SILICEOUS BUT BIOTITE RICH SECTIONS MAY BE INT. VOLCANIC OR ALT'D TRONJ ALTERED TRONJ OR INTERMEDI ATE-FELS I C INTRUSIVE.

X INFI QZ BI FG WF N FO ? F1MA FX

MISSING CORE.AS PREVIOUS WITH SHARP DISCORDANT CONTACTS; THIS INTERVAL FEATURES MORE QUARTZ BANDS AND A CENTRAL STRONGLY SHEARED SECTION WHICH ALSO ENCOMPASSES A SHORT, B10TITIC MAFIC SECTION (XENOLITH?); COULD BE A DIORITE OR ALTERED TRONJ.

X INFI NMA

QUARTZ-FELDSPAR TRONJ PORPHYRY. X OZFP OZ FX MX PO

DA BI FM

FO L/

U/ L/

40 X) 27

2074

FI

TRON OZ FX MA BI

TEXTURE BLURRED WHERE SEVERAL SHORT ALTERED QUARTZ EYES PRESENT.

X OZVN QZ

WP MX P U/ 54 MG BN 65 WEAKLY SILICIFIED AND SERICITIZED; SECTIONS BUT LITTLE SULPHIDE; BLUE

I* F1

O?D) DT GN D) DT

Q?D) DT D)

D)D*

B* D)

B)

D)

DT

D*

GN DT

FG FR N U/ 42

LYNX GEOLOG

N(UNITS

T E R V A L METERS)

FROM T O

PLRRRR

PL

PLR

PLRRRRRRNLRNL

PL

PL

PLRRRRRR

115.86

115.86115.86115.86115.86

119.16

121.35

121.35

124.48

124.48124.48124.48129.10129.10129.10129.10

130.52130.52

137.50

139.53

140.74

140.74140.74140.74140.74140.74140. 74

119.16

119.16119.16119.16119.16

121.35

124.48

124.48

137.50

137.50137.50137.50129.75129.75129.75129.75

131.62131.62

139.53

140.74

141 .84

141 .84141.84141.84141 .84141.84141 .84

UHEX INC. BAMAJI


PAGE: 3 DATE: &8/NOV/25

CORE X TYPI- CAL TEX- GRAIN FRAC-RECOV- M ROCK FYING MIN TURES CHARACS TUREERY I TM TM MAT TX TX F C X M

( X ) X TYPE 1 2 QM1 1 2 F F C P # TK

STRUCTUR-1 ALTERATION MINS ORE-TYPE MINSH H H H H ANY H H N ANY


ROCK FOR EN RT TM OM2 TX TX S R S O DIP FQUAL MEM V Q LC- 3 3 4 O N H l S ML lDESIG AGE COL R D P C


STRUCTUR-2 AAAAAAAA

TRON AL

WA

QZ DA

FX MF

QZ3 FX4

SH FM

UP AU

3 5

L/

FO L/

DEFORMATION DECREASING TO LOWER CONTACT; SEVERAL LOW

62

66 PM F1 37

ANGLEFRACTURES WITH SERICITIC HALOES; ALTERATION MOST INTENSE BETWEEN 116.15-117.40m, WITH STRONG SILICIFICATION AND 3-4X PYRI TE .

MFVL AX CL DG FX

MX WF FG

QZFP QZ FX OZ4 MX FM P U/ 33 PW F1DA MF FX4 PO I f 2 5

QZ-FELDS TRONJ PORPHYRY WITH SEVERAL MAFIC VOLCANIC XENOLITHS.

FO 43 S) E+MFVL AX CL AX5 FG MX PP! DG FX FX? CV

TYPICAL MAFIC VOLCANIC WITH LOCAL SHEARED, BIOTITIC, QUARTZ * CARB VEINED/STRINGER ZONES; CARB STRINGERS ABUNDANT BETWEEN 128.0 AND 133.25; WEAKLY SILICIFIED TO LOWER CONTACT. POSSIBLY BRECCIATED, QUARTZ PODS, CARB STRINGERS; 3-4X SULPHIDES; CENTRAL ALTERED TRONJ DYKE; COULD REPRESENT QUARTZ BRECCIA ZONE; SOME CREAM/BROWN FRAGMENTS APPARENT.

X MFVL AX CL AX5 SH MX D FO 48 X) E+PI DG FX FX?

AS ABOVE BUT SHEARING AND ALTERATION LESS INTENSE.X MFVL AX CL AX5 SH MX D FO 55 S) E+

PI DG FX FX?

TRON OZ FX DA B I

MG FO 3 4 FR

MFVL AX CL AX5 FG MX PI DG FX FX? CV

FO L/

FO

59 V* 55

35OZBS OZ BI QZ2 BR CO PGU AX BIZ SH

WHITE QUARTZ BLOBS AND PODS MAY BE BRECCIATED QUARTZ VEINS; COARSE PY AND PO RELATED TO QUARTZ PODS AND THEIR SELVAGES; A MUCH FINER GRAINED PHASE OF SULPHIDE IS PERVASIVE THROUGH THE ZONE; BRECCIATION STRONGEST TOWARDS L/; SMALL SCALE S AND Z FOLDS PRESENT; L/ WITH QUARTZ VEIN SHARP; UPPER CONTACT WITH MAFIC VOLCAN ICS--GRADAT IONAL.

QZ D) V)

BT

X)

D*

D) DT D)

X)

S:

X)

BT

D) D) D)

D) DT D)

D*

PY D*

PY

LYNX GEOLOG


K FE LY G

PL

PLRRRNLNL

PLRRRRN

'

141.84

143.52

143.52143.52143.52155.53

158.00

158.74

158.74158.74158.74158.74160.63

143.52

158.74

158.74158.74158.74156.36

158.74

169.77

169.77169.77169.77169.77160.76

PAGE: 4 DATE: 88/NOV/25UMEX INC.

BAMAJI

DRILLHOLE/TRAVERSE : BAH88 10 (CONTINUED)

CORE X TYPI- QAL TEX- GRAIN FRAC-RECOV- M ROCK FYING KIN TURES CHARACS TUREERY I TM TM MAT TX TX F C X M

( X ) X TYPE 1 2 OM1 1 2 F F C P K T K


ID STK DIP A A A A A M1N A A A MINAZM RT OZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM QM2 TX TX S R S O DIP FDUAL HEM VQLC-3 3 4 O N H X SML IDESIG AGE COL R D P C

T ID STK DIP KF HU CL EP HE HA PR MO SL HA2 AZM RT HHHHHHHH

STRUCTUR-2 AAAAAAAA

OZVN QZ WH

BK FR XE

U/ L/

4033

O

MFVL AX CL AX5 FG MX P EPI DG FX FX? WF CV

ABUNDANT CARB STRINGERS WITH SULPHIDES, LOCAL QUARTZ VEINING WITH BIOTITIC HALOES; PILLOW SELVAGES OFTEN CONTORTED. SMALL SCALE l A ND S FOLDS.

X TRON QZ FX DA BI

D

S +

MX WF WP

X MFVL AX CL AX5 SH MX PI DG FX FX? WF

N U/ L/ FO

7056

F2 S =

P 'U/ 49 V* F1TRON OZ FX MX FM

MA BI 10TRONJ OR GRANODIORITE; LOCAL PERVASIVE SILIFICATION; FELDSPARS BLURRED - SERICITIZED AND OR WEAKLY SAUSSERI T I ZED: OCCASIONAL THIN SHEARED SECTION AND SEVERAL THIN QUARTZ VEINS. 169.77-END OF HOLE; CASING LEFT IN; CORE STORED AT UMEX MINE

X QZVN FR N L/ 30

D*


PROJECT IDEN : BAMAJI COLLAR NORTHING: -500.00 CLAIM #: Pa 844436





88/ 8/231000.00178.92



ROD * 335.00

SURVEY FLAG

000001002003

F -INTERVALL (UNITS s METERS)AG FROM - TO

0.00 1.20

PLRRRRRNL

PLR

PLRNL

PLRRRRRRR

1 .20

1 .201.201 .20

24.0024.0024.00

28.27

28.27

34.86

34.8637.43

39.56

39.5639.5639.5639.5639.5639.5639.56

28.27

28.2728.2728.2725.8225.8225.82

34.86

34.86

39.56

39.5638.48

54.20

54.2054.2054.2054.2054.2054.2054.20


0.00 335.00 -50.00 52.43 335.00 -48.00 116.43 336.00 -45.00 177.40 335.00 -43.00

CORE X TYPI- OAL TEX- GRAIN FRAC- RECOV- M ROCK FYING MIN TURES CHARACS TURE ERY I TM TM MAT TX TX F C !* M

C X ) X TYPE 1 2 QM1 1 2 F F C P # TK

ROCK FOR EN RT TM QM2 TX TX S R S 0 DIP F QUAL MEM V Q LC- 3 3 4 0 N H / SML I DESIG AGE COL R D P C

OVB P

MFVL AX CL MX WF P


T ID STK DIP A A A A A MIN A A A MIN 1 AZM RT OZ BI CY CB MG XX PY CP GL YY SUMMARY


FO 69 E* S) D)DG FX CV GV

INITIAL TWO METERS HAS 1X DISSEMINATED PYRITE; POSSIBLE RARE PILLOW SELVAGES; NUMEROUS TRONJ DIKES (Om WIDE); AFTER 11.0m CARB VEINLETS INCREASE IN INTENSITY.LOWER CONTACT SHARP WITH MAFIC VOLCANIC; MV BIOTITE ALTERED AT CONTACT

X TRON QZ FX BN SH F G N FO 70 S) AL MA MF U/ 80

TRON OZ FX AL DA BI

INITIAL TWO METERS

MFVL AX CL DG FX

CARB VNLTS RAREX TRON OZ FX

MA B I

WP FO P FO 54 PBN U/ 74SHEARED, SILICIFIED, SERICITIZED.

MX WF P GV

FO N WF MG

O

C*

P FO L/

SHORT SHEARED OCCASIONAL

I) F160 63 SECTIONS;

TRON QZ SE QZ? FM WP 2 5AL MA FX SE2 BN SH

INITIAL FOUR METERS WEAKLY ALTERED WITH 44m ONWARD-SHEARED, BANDED, SERICITIC; CROSSCUTTING QUARTZ VEIN;SILICIFIED AFTER 47m WITH INCREASE IN SULPHIDES; AFTER 52.5m DEFORMATION DECREASES; OCCASIONAL PATCHES OF FRESH TRONJ PORPHYRY ARE VISIBLE WITHIN ALTERED/SHEARED SECTIONS; POOR SULPHIDE CONTENT.

B*

DT

D) D*

D)

D)

SE F/

SE PW

LYNX GEOLOG

F - I N T E R V A K L (UNITS ' METERS) E A Y C F R O M - T O

K FE LY G

PLR

PLRR

PLRRRNL

PLRRRRRRRRRRRR

PLRRR

PLR

P

*

54.20

54.20

56.55

56.5556.55

60.67

60.6760.6760.6763.54

64.97

64 .9764 .9764.9764.9764.9764.9764.9764.9764.9764.9764.9764.97

68.68

68.6868.6868.68

74.34

74.34

78.33

'

56.55

56.55

60.67

60.6760.67

64.97

64.9764.9764.9764.07

68.68

68.6868.6868.6868.6868.6868.6868.6868.6868.6868.6868.6868.68

74.34

74.3474.3474.34

78.33

78.33

92.20

UHEX INC. BAMAJI


PAGE: 2 DATE: 88/KOV/2S

CORE X TYPI- GAL TEX- GRAIN FRAC-RECOV- M ROCK FYING MIN TURES CHARACS TUREERY I TM TM MAT TX TX F C X M

( X ) X TYPE 1 2 QM1 1 2 F F C P * TK

STRUCTUR-1 ALTERATION HINS ORE-TYPE M1NSH H H H H ANY H H H ANY

T ID STK DIP A A A A A MIN A A A MIN1 AZM RT OZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TH QH2 TX TX S R S O DIP FOUAL MEM V Q LC- 3 3 4 O N H l S ML IDESIG AGE COL R D P C

MFVL AX CL FG MXDG FX

QUARTZ VEIN AT UPPER CONTACT.


STRUCTUR-2 AAAAAAAA

PW

TRON 02 SE OZ2 FM WP 2 5 PU/ 80AL MA FX SE2 BN SK

SHEARED, PERVASIVE UK TO MODERATE SILICIFICATION; SEVERAL THIN WHITE CONCORDANT VEINS.

MFVL AX QZ FG SF 3 4 P FO 42 V* F*AL DG BI QV SK

GREY QUARTZ PODS, VE INS-IRREGULAR, POSSIBLY BRECCIATED; MAFIC VOLCANICS SHEARED BUT BIOTITE DEVELOPMENT NOT AS HIGH AS PREVIOUS BAMAJI HOLES TO WEST.

X TRON OZ SE QZ? FM WP 2 5 N U/ 27 AL MA FX SE2 BN SH L/ 28

TRON QZ FX FO BR P FO 47 E* F1AL DA BI SH FG FO 55

BETWEEN 66.47--68.53, BANDED AND BRECCIATED TEXTURE CONSISTING OF PORPHYRITIC AND GREY ALTERED TRONJ ALTERNATING WITH PATCHES OR LENS/BANDS OF AX, CARB, CHLORITE RICH ROCK; OCCASIONAL THIN STRONGLY BIOTITIC SHEARS.A THIN APPROX 1cm ENVELOPE OF GREY/WHITE QUARTZ CAN USUALLY 8E FOUND SEPARATING THE MAFIC AND TRONJ PORTIONS/BRECCIA FRAGMENTS; BETWEEN 67.77 AND 68.53 QUARTZ HAS BLEACHED APPEARANCE; TEST FOR FECB SLIGHTLY POSITIVE;THE QUARTZ HAS A SUGARY, SUCROISIC TEXTURE, VERY DIFFERENT FROM VEIN QUARTZ; SULPHIDES (MOSTLY PY) MAY REACH 1-2X LOCALLY; FAULT BRECCIA? RESEMBLES QUARTZ, BRECC, SHEAR ZONE EXCEPT HOST IS TRONJ AND SULPHIDES VERY POOR; **** BAMAJI AU SHOWING ****

MFVL FOAX FX AX5 WF MG 3 4 PDA BI FX3 MX

INITIAL TWO METERS ARE MED GRAINED, AFTER WHICH UNIT IS FOLIATED AND CONTAINS NUMEROUS CARB STRINGERS; MOD SIL'D, SHEARED AND PYRITIC NEAR L/ WITH TRONJ.

TRON OZ SE FG WP P U/AL MA FX SH FO

WEAKLY ALTERED, SHEARED AS AT 64.97; COULD BE INT

I* F1

O D'

P?D) D*

t) DT CB D)P) D*

36 S) F2

MFVL AX CL FG MX 2 3

4070

FELSIC TUFF.

S* E)

CT

D)

D* PY

LYNX GEOLOG

K L ( E AY G

K FE LY G

LRRRNLNLRNL

PLRRR

PLR

PLRRRR

PLR

PLRR

PLRRR

UNITS * ME

FROM'

78.3378.3380.4080.40

85.88

88.8488.84

92.20

92.2092.2092.20

96.73

96.73

97.32

97.3297.3297.3297.32

100.25

100.25

105.00

105.00105.00

106.29

106.29106.29106.29

TERS)

- T 0'

92.2092.2081.0581.05

86.58

89.8389.83

96.73

96.7396.7396.73

97.32

97.32

100.25

100.25100.25100.25100.25

105.00

105.00

106.29

106.29106.29

107.94

107.94107.94107.94

UMEX INC. BAMAJI


PAGE: 3 OfUE; 88/KOV/Z5

CORE RECOV

ERY ( X )

ROCK OUAL DESIG

X M ROCK I X TYPE


TYP1- QAL FYING MIN TM TM MAT

1 2 QM1

TM QM2 LC- 3 COL


1 2 F F C P # TK

TX TX S R S 0 3 4 0 N H X

R D P C

DIP F SML I

T 1

T 2

STRUCTUR

ID STK D AZM

ID STK D AZM

STRUCTUR

1 ALTERATION MINS ORE H H H H H ANY H

RT OZ

IP KF RT -2

BI CY CB

MU CL EP H H

MG XX PY

HE HA PR H H H

TYPE HINS H H ANY A A MIN

CP GL YY

MO SL HA H H H

SUMMARY

PI DG FX WF GVINITIAL 3 METERS, CARB AND QTZ STRINGERS-MASSIVE AND UNALTERED AFTER THAT EXCEPT FOR LOCAL EPIDOTE BANDS/PATCHES. SHEARED BIOTITIC, CARBONATI ZED, PYRITIC MAFIC VOLCANIC.

FG SH WF GV MX MG WF

2 3MFVL AX CL PI DG FX

X TRON QZ FX MA B!

SHEARED, BIOTITE AND PYRITE RICH HALOES X TRON MX MG

MA WP

TRON QZ FX WF WPAL MA BI FM

WEAK ALTERATION (SERICITIZATION). SHEARING AND GRAIN SIZE VARIES LOCALLY; TEXTURE PRESENT.

FG FO

FO

U/

U/ L/

FO U/

S+ F3

69

7164

50F1

GOOD TRONJ PORPHYRY

MFVL AX CL MG FX

WEAK TO MODERATE SERICITIZED MAFIC VOLCANIC.

TRON QZ SE OZ2 SH BK 2 A P FO 61 V1AL LG FX SE4 CR FG U/ 80

INTENSELY SERICITIZED, SHEARED, WEAKLY CARBONATI ZED, STRONGLY QUARTZ VEINED; POOR SULPHIDES; COULD BE ALTERED INTERMEDIATE FELSIC TUFF; SHARP CONTACTS; LOWER CONTACT WITH MAFIC VOLCANIC SLIGHTLY BIOTITIC; OCCASIONAL QUARTZ EYE.

MFVL FG MX PPI DG

TYPICAL, LOCAL CARB VE1NLETS.

F1TRON OZ FX FG WP PAL DA BI PA IR

BRECCIATED, SHEARED UPPER CONTACT, SIL'D, CARBONATIZED AND UPPER CONTACT QUARTZ VEINED, BLOCKY.

MFVL AX CL FG BN P P + E*AL DG FX CO F1

UPPER CONTACT SHEARED, BIOTITIC WITH QUARTZ PODS (BRECCIATED VEINS?"); FROM 107.00--107.94, CARB-OTZ-BIOTITE STRINGERS ARE CONTORTED, FOLDED, CRENULATED.

S* Q +

D) D)

PY

LYNX GEOLOG

K L (UNITS ' METERS) E A Y G FROM -TO

K FE LY G

LRRRRRRR

PLRR

PLRR

PLRR

PLR

PLRR

PLR

PLRRRRR

107.94107.94107.94107.94107.94107.94107.94

112.64

112.64112.64

115.38

115.38115.38

118.57

118.57118.57

124.53

124.53

128.19

128.19128.19

129.20

129.20

132.34

132.34132.34132.34132.34132.34

112.64112.64112.64112.64112.64112.64112.64

115.38

115.38115.38

118.57

118.57118.57

124.53

124.53124.53

128.19

128. 19

129.20

129.20129.20

132.34

132.34

152.57

152.57152.57152.57152.57152.57

UHEX INC. BAMAJI


PAGE: 4 DATE: 88/HOV/E5

CORE RECOV ERY

( X )

X TYPI- OAL TEX- GRAIN FRAC-M ROCK FYING MIN TURES CHARACS TUREl TM TM MAT TX TX F C X M


T ID STK DIP A A A A A MIN A A A MINX TYPE 1 2 QM1 1 2 F f C P TK 1 AZM RT QZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM QM2 TX TX S R S O DIP FQUA L MEM V Q LC- 3 3 4 O N H 7 SML IDESIG AGE COL R D P C

T ID ST K DIP KF MU CL EP HE HA PR MO SL KA2 A ZM RT H H H H H H H H

STRUCTUR-2 AAAAAAAA

UA BI LF L/ 10 FAIRLY TYPICAL EXCEPT FOR SEVERAL SECTIONS; 108.90-110.78 AND 111.78-112.64 WHICH FEATURE VARIOUS SIZES OF ELONGATE SUBANGULAR QUARTZ FRAGMENTS (LAPILLI?) GIVING THE ROCK A TUFFACEOUS TEXTURE; THESE SECTIONS ARE NOTICEABLY BETTER FOLIATED AND APPEAR TO HAVE SEVERAL SHARP CONTACTS WITH THE TRONJ PORPHYRY; THE LOWERMOST UNIT HAS BROWNISH CAST POSSIBLY FROM BIOTITE; FOLIATION MEASURMENT IS FROM LOWER TUFF UNIT;

P) E =MFVL AX CL FG CV PPI DG FX MX

TYPICAL CARB STRINGERED MAFIC VOLCANIC WITH BIOTITIC CONTACTS UITH TRONJ (LOWER CONTACT).

FO 58 PW F1

F1

TRON QZ FX FM WP PAL MA BI SH PA

PATCHY LIGHT AND DARK GREY COLOUR/ALTERATION; PYR1TIC BETWEEN 117.8--118.2 AND BLOCKY AT LOWER CONTACT.

MFVL AX CL AX4 MX WF PDG FX FX3 FM

SLIGHTLY COARSER GRAINED THAN USUAL MAFIC VOLCANIC, BUT HOMOGENEOUS; A FEW CARB VEINLETS NEAR LOWER CONTACT.

TRON QZ FX FX2 FM PO 3 5 PU/ 81 PM F1DA BI QZ4 MX L/ 55

TYPICAL QUARTZ-FELDS TRONJ PORPHYRY, RARE BLUE QUARTZ EYES.

AMPH AX FX AX6 MG MX 3 5 P V sDG CL FX3

QUARTZ VEINS IRREGULAR, SHALLOW TO CORE AXIS; DOMINANTLY AX CRYSTALS WITH INTERSTITIAL PLAG.

TRON QZ FX FX2 FM PO 3 5 PU/ 29DA BI OZ4 MX L/ 62

AS ABOVE EXCEPT NOT SILICIFIED OR QUARTZ VEINED.

C*

c*

D)

LYNX GEOLOG

K L (UNITS = METERS) E A Y G F R 0 M - T 0

K FE LY G

RNLNLNLNLNL

PLRRRR

PLNL

PLRR

'

132.34133.46

136.32

137.61

141.94

145.09

152.57

152.57152.57152.57152.57

159.50

163.36

166.36

176.11176.11

'

152.57135.00

137.13

138.61

142.84

146.00

159.50

159.50159.50159.50159.50

166.36

163.58

178.92

176.58176.58

UMEX INC. BAMAJI


PAGE: 5 DATE: BB/NOV/25

CORE X TYPI- OAL TEX- GRAIN FRAC-RECOV- M ROCK FYING MIN TURES CHARACS TUREERY I TM TM MAT TX TX F C X M

( X ) X TYPE 1 2 OM1 1 2 F F C P # TK



ROCK FOR EN RT TM OM2 TX TX S R S O DIP FQUAL MEM V Q LC- 3 3 4 O N H l S ML IDESIG AGE COL R D P C

PATCHS CARB-QTZ-EPIDOTE.X

X

X

X

X

MFVL

TRON

MFVL

TRON

TRON

AXDGQZMAAXDGOZMAOZMA

CLFXFXBICLFXFXBIFXBI

FGLFMXUFFGLFFGWFMXWF

MXGVMG

MXGVMX

MG

20

20


STRUCTUR-

U/

FO

U/

U/

•2

V) E)

80

42 V) E)

80

60

S+ D) PYQ) ** O

S+ DQ)

TRON QZ FX FG UP P FO 64 PM F1 AL UG BI HO FO L/ 49 F?

LIGHT BROWNISH-GREY, ALMOST BLEACHED COMPARED TO USUAL MEDIUM DARK GREY COLOUR; INITIAL AND FINAL APPROX 75cm RELATIVELY UNALTERED GRADUAL TRANSITION; SILICIFICATION AND SERITIZATION ARE MAJOR ALTERATIONS; MINOR CALCITE, TEST NEGATIVE FOR FeCB.

D)D*

PY


PROJECT IDEM : BAMAJI COLLAR NORTHING: -440.00 CLAIM #: Pa 844442/Pa 844437





88/ 8/26450.00178.92

COMPLETION DATE : 88/ 8/27 COLLAR ELEVATION: 400.00 CORE/HOLE SIZE : BO


ROD * 335.00

SURVEY FLAG

000001002003

F - I N T E R V A K L (UNITS = METERS) E A Y G FROM - TO

K FE LY G


0.00 55.47 110.34 177.40

CORERECOV ERY

( X )

ROCKQUAL

XMI X

FORMEM

FORESIGHT

TYPI -ROCK

TYPE

EN RTV Q

FYT Ui n

1

LC

INGT Ml n 2

TM- 3

QALMINHATnn l OM1

OM2

TEX TURESTX T X

1 2

TX TX3 4

AZIMUTH (DEGREES)

335.00 334.00 339.00 339.50


-46.00 -44.00 -39.00 -35.00

GRAIN FRAC-CHARACSF f * "r t* F F

S R0 N

A n C P

S 0H /

TURE

K T K

DIP FSML I

T 1

T2

STRUCTUR- 1

ID STK AZM

ID STKAZM

RT

DIPRT

NORTHING EASTING

ALTERATION MINS ORE-H

OZ

KF

H

BI

Mil

H

CY

CLH

H

CB

EPH

H ANY H

MG XX PY

HE HA PRH H H

TYPE MINSHA

CP

MOH

H ANYA M 1 UA n i H

GL YY

SL HAH H

SUMMARY

PL R

P L R N L

P L R R

P L

P L R R R R R R R

0.00

2.46

2.46

5.02

5.02 11.64

2.46

5.02

5.02

30.15

30.15 12.02

30.15

30.1530.15

32.27

AL2 34.85

34.8534.8534.8534.8534.8534.8534.85

32.27

32.2732.27

34.85

36.18

36. 1836.1836.1836.1836.1836.1836.18

OVB

TRON QZ FX MG UPDA MF MX BK

TYPICAL QTZ-FELDS TRONJ PORPHYRY.

AMPH AX FX AX5 MG WF iAG CL FX3 HO EQ

MAFIC VOLCANIC; POSSIBLE COARSE FLOW? X QZVN

WH

FO

PU

60 V* f *

CT

LOCALLY AX PORPHYRITIC.N L/ 54

U/ 65

TRON QZ FX MG UP P U/ 80 L/ 47

WEAKLY SIL'D AT UPPER CONTACT; PITTED AND LIGHTER GREY CAST TOUARDS LOWER CONTACT.

AMPH AX CL AX5 FM UF DG BI

FO

f* F 1

59 P) F2AMPH Bl AX AX3 SH BR 2 4 PAL UG SX SX1 FM

SHEARED, STRONGLY B IOTI T l C , CARBONATIZED WITH PODS OF QUARTZ (BRECCIATED QUARTZ VEINS?); POSSIBLY MINOR ACTINOLITE; POSS MAFIC FRAGMENTS - VERY FAINT; STRONGLY SULPH1DIC; 34.85 - 35.59m INTACT AND PART OF THIS SECTION; FROM 35.59 - 36.18, UNSURE IF BELONGS IN THIS BOX AS CORE WAS SPILLED; TEXTURALLY SIMILIAR BUT NOT 100X SURE IT BELONGS HERE; UPPER CONTACT GRADATIONAL.

FI

N DT

LYNX GEOLOG

K L (UNITS s METERS) E A Y G F R 0 M - T 0

K FE LY G

R

PL

P ALZLRRR

PLRR

PLRR

PLRR

PLRNLN

PLRRRR

PLRR

'

36.18

36.38

37.47

37.4737.4737.47

38.68

38.6838.68

42.10

42.1042.10

44.80

44.8044.80

49.57

53.8253.82

54.55

59.94

59.9459.9459.9462.50

62.80

62.8062.80

'

36.38

37.47

38.68

38.6838.6838.68

42.10

42.1042. 10

44.80

44.8044.80

49.57

49.5749.57

59.94

54.3054.30

55.39

62.80

62.5062.5062.5062.80

95.20

95.2095.20

UMEX INC. BAMAJI

DRILLHOLE/TRAVERSE : BAM88J2 (CONTINUED)

CORE y, T YPI- QAL TEX- GRAIN FRAC- STRUCTUR-1RECOV- M ROCK FYING HIM TURES CHARACS TUREERY I TH TM MAT TX TX F C X M T ID STK DIP

( X ) X TYPE 1 2 QM1 1 2 F F C P it T K 1


ALTERATION MINS ORE-TYPE MINS H H H H H ANY H H H ANY A A A A A MIN A A A MIN

AZM RT QZ BI CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM QM2 TX TX S R S O DIP FOUAL MEM V Q LC- 3 3 4 O N H l S ML IDESIG AGE COL R D P C


STRUCTUR-2 AAAAAAAA

CORE LOST

MFVL AX CL DG FX

FG FO CV

FO

MFVL BI QZ BI4 SH 0V P FO AL UN CB 021 CV BK VO

STRONGLY SHEARED, BIOTITIC, QTZ VEINED, CARBONATIZED PYRITIC, FAIRLY SHARP UPPER AND LOWER CONTACTS ie. VERY DISCRETE ZONE.

FOAMPH AX FX AX5 MG UF PAG CL FX3 HO EQ

GRADUAL GRAIN SIZE REDUCTION TO LOWER(GRADATIONAL)CONTACT WITH MAFIC VOLCANIC.

53 S'

26 V1 F 26 F?

53

V*MFVL AX FX MX FG PDG CL UF

LOCATION OF LOWER CONTACT WITH TRONJ UNKNOWN AS CORE MISSING !N BOX #8 FROM APPROX 43.20-45.45m

TRON QZ FX FM WP P FO 76 PM F1AL DA MF FO HO L/ 62

UPPER CONTACT NOT EXACT; SECTION IS JUMBLED UNTIL 48.86m; WEAK TO MODERATELY SHEARED, PERVASIVELY SIL'D, MINOR SERICITE.

MFVL AX FX FG DG CL WF

CONTAINS SEVERAL THIN 0V X TRON

X TRON

FXTRON QZ AL LA

CORE BETWEEN 62.50 TO STRONGLY SIL'O;

MX GV 'S AND

S)

MINOR SULPHIDES.N VO

U/N U/

FG FO P FO BK U/

-62.80 IS MISSING, CONTAINS l i O F WEAKLY SERICITIZED; MOD SHEARED;

334980

65 PS80

UNIT; MOD TEXTURE

BLURRED; CONSISTENT BREAKDOWN OF MAFIC AND CORE MISSING

FELDSPAR MINERALS

MFVL AX FX FG MX 5 PDG CL WF GV

UPPER CONTACT UNKNOWN; CORE JUMBLED UNTIL 65.37m LOCALLY PILLOWED; PATCHY EPIDOTE; LOCAL CONCENTRATION OF

P)

V) Q)

P1 D= DT PY

S*

C*

S)Q)

OT

D)DT

D*

0)

S)Q)

LYNX GEOLOG


K FE LY G

RRRR

PLRRRR

PL

PLRRRRRRRRR

PLRRRRRRRNL

PLRRR

'

62.8062.8062.8084.45

95.20

95.2095.2095.2095.20

100.55

104.80

104.80104.80104.80104.80104.80104.80104.80104.80104.80

113.82

113.82113.82113.82113.82113.82113.82118.20118.20

123.02

123.02123.02123.02

'

95.2095.2095.2089.11

100.55

100.55100.55100.55100.55

104.80

113.82

113.82113.82113.82113.82113.82113.82113.82113.82113.82

123.02

123.02123.02123.02123.02123.02123.02119.34119.34

128.89

128.89128.89128.89

UHEX INC. BAMAJI

DRILLHOLE/TRAVERSE : BAH88 12 (CONTINUED)


CORE RECOV-C l\ 1

( X )

ROCK DUAL DESIG

X TYPI- GAL TEX- GRAIN FRAC- M ROCK FYING MIN TURES CHARACS TURE

X TYPE 1 2 QM1 1 2 F F C P # TK

FOR EN RT TH QM2 TX TX S R S 0 DIP F HEM VQlC-3 3 4 0 N H X SHL I AGE COL R D P C

T1

T 2

STRUCTUR-1

ID STK DIP AZM RT

ID STK DIP AZM RT

STRUCTUR-2

ALTERATK H H H

02 BI CY

KF MU CLH

DN tH

CB

EPH

UN!H t

MG

HE H

; (^NYn j r XX

HA H

)REH

rf A PY

PR H

TYPE 1H H 1A A

CP GL

HO SL H H

11NS \NYn i nYY

HA H

SUMMARY

PY AND PO RELATED TO CARB/QTZ PATCHES/BANDS - PILLOW SELVAGES? 67.45 - 73.0 -- INCREASED CARB STRINGERS AND QTZ PODS AND GASHES; LOCAL WEAK SIL'N; OCCASIONAL TRONJ DIKE CORE JUHBLED -- CORE IS MAFIC VOLCANIC; 0.5m MISSING.

TRON QZ FX FM SH P FO 70 PHAL MA BI BK L/ 70

MOD SHEARED, PERVASIVELY SIL'D, WEAKLY SER1CITIZED TRONJ. SEVERAL SHORT MAFIC VOLCANIC XENOLITHS -- STRONGLY PYRITIC AND CARBONATIZED; TYPICAL LIGHT AND DK GREY, BANDED AND SPECKLED ALTERED TRONDJHEMITE.

MFVL AX FX DG CL

FG MX WF GV

3 5 FO 48 V) F?TRON QZ FX FM PO AL AG BI SH LB

SHEARED(MYLONITIC), WEAK-MOD SERICITIZED, LOCALLY WKLY SIL'D TRONJ; NUMEROUS BLACK LAMINAE(FRACTURE FILLINGS?) PARALLELING FOLIATION - BIOTITE AND/OR CHLORITE; ABUNDANT QTZ EYES; NUHEROUS QTZ VEINS, VEINLETS, WITH PYRITE; BOTH LOWER AND UPPER CONTACTS FEATURE ALTERED MAFIC VOLCANIC WALLROCK; CORE FROM 106.5 - 112.0 IS MIXED UP BUT SEVERAL CONTIGUOUS SECTIONS EXIST WITHIN THIS SECTION AND HAVE BEEN SAMPLED AS UNITS; UPPER AND LOWER CONTACTS ARE DEFINITE; APPROX 1.45m OF CORE IS MISSING FROM THIS SECTION.

MFVL AX FX MG FO P FO 40 S) F1VA DG BI PA IR L/ 38

MEDIUM GRAINED COARSE FLOW OR MAFIC INTRUSIVE; SHARP L/ WITH FINE GRAINED PILLOWED HAFIC VOLCANIC FLOWS; VARIABLE PLAG CONTENT; OFTEN VARIOLITIC; SHARP L/ INDICATES THIS UNIT IS DISCRETE ROCK TYPE, EITHER FLOW OR INTRUSIVE; LOCALLY THEREAPPEARS TO BE CLASTS(XENOLITHS? ); VERY IRREGULAR, PATCHY TEXTURE; LOCALLY RESEMBLES THE AMPHIBOLITE FOUND AT 5.02 H. SIMILAR TO PREVIOUS ALTERED TRONDJHEMITE;

X TRON OZ FX QZ3 FG FO N U/ 41 AL LG SE SE2 AU SH FO ?

F1 F1

MX P) E)MFVL AX FX AX6 FG PI DG CL FX3 LB

TYPICAL PILLOWED MAFIC VOLCANIC WITH PATCHY EPIDOTE ALTERATION; LOCAL SIL'N, NUMEROUS THIN OTZ STRINGERS; OCCASIONAL CARB STRINGERS; LOCAL PILLOW BRECCIA - FLOW TOP BRECCIA?;

D) DT

PY D)4*

SE

LYNX GEOLOG

K L (UNITS = METERS) E A Y G FROM -TO

K FE LY G

RNL

P

PLRRRR

PL

PLRRNLNLNLNLNL

123.02123.59

128.89

129.30

129.30129.30129.30129.30

130.00

131.23

131.23131.23135.98

146.41

U8.31

153.94

163.82

128.89124.38

129.30

130.00

130.00130.00130.00130.00

131.23

178.92

178.92178.92137.75

147.24

149.39

156.00

164.67

UHEX INC. BAMAJI


PAGE: 4 DATE: 88/NOV/Z5

CORE X TYPI- GAL TEX- GRAIN FRAC-RECOV- H ROCK FYING KIN TURES CHARACS TUREERY I TM TM MAT TX TX F C X M

( X ) X TYPE 1 2 QM1 1 2 F F C P # TK



ROCK FOR EN RT TM OM2 TX TX S R S O DIP FQUAL MEM V Q LC- 3 3 4 O N H l S ML IDES1G AGE COL R D P C

OCCASIONAL TRONJ DIKE.X TRON 02 FX MG 0V

HA BI XE FO

MFVL AX BI 612 FM

T ID STK DIP KF MU CL EP HE KA PR MO SL HA2 AZM RT HHHHHHHH

STRUCTUR-2 AAAAAAAA

FO U/

58 PM 40

TRON QZ BI QZ3 FM IR P FO 65 P) F2AL AU SX SX1 BR BN L/ 27

RESEMBLES QZ-BR-SH ZONE WITH SMALL CREAM/BROUN COLOURED SILICEOUS "FRAGMENTS"; UNIT IS A DISCRETE ALTERED TRONDJHEMITE WITH SHARP UPPER AND LOWER CTC'S CROSSCUTTING MV; ABUNDANT SULPHIDES, PY, PO, CP, GA, AND SP ; STRONGLY BIOTITIC.

MFVL BI AX BI3 FG FO AL UB CL HO

PU F3

P? E)MFVL AX FX AX6 FG MX PPI DC CL FX3 LB

NUMEROUS SHORT SECTIONS OF BRECCIATED, EPIDOTIZED MAFIC VOLCANIC 178.92-END OF HOLE; CASING LEFT IN; CORE STORED AT UMEX MINE

X

x

x

x

x

TRON

MFVL

INVL

TRON

MFVL

02DAAX

AXLGQZDA

FXBIFXCL

BIFXBI

HX

MGBRFG

MX

FO

FO

U/

FO

L/

60 PW

55

64

QV

QZ D* V+ t*

DT

S)

PM

PY

Or D* D* D= D)

D)

D* D*

DT

D* D*

O

LYNX Geosystems I ne




PAGE: 1 DATE:


88/ 8/29-416.00200.25



RDD * 335.00

KE Y

KE Y

SURVEY FLAG

000 001 002 003004

f -INTERVAL-L (UNITS * METERS)A G FROM - TO

FL G


0.00 46.33 98.15 146.90

FORESIGHT

198.73

CORERECOV-

E R Y( * )ROCKOUAL DESIG

XMI X

FORMEM AGE

ROCK

TYPE

EN RTV Q

TYPI -FYINGTM T Min in

1 2

TMLC- 3 COL

GALMINMATn t\ i QM1

QM2

TEX TURESTX TX

1 2

TX TX3 4

AZIMUTH (DEGREES)

340.00 345.00 343.00 345.00345.

GRAINCHARACSc f V Mr L A n F F C P

S R S 00 N H / R D P C

00

FRAC TURE

H T K

DIP FSML I


-43.00 -41.00 38.00 36.00

T1

T2

33.00

STRUCTUR- 1

ID STK DIP AZM RT

ID STK DIPAZM RT

STRUCTUR-2

NORTH1

ALTERATIONH

QZ

KF

H H

BI CY

MU CLH

H

CB

EPH

NG EAST!

MINS OREH ANY H

MG XX PY

HE HA PRH H H

ING

TYPE MINSHA

CP

MOH

H ANYA M 1 UH i H

GL YY

SL HAH H

SUMMARY

P

PLR

PLRR

PL

PLNLNL

PLRRR

PLR

0.00

5.71

5.71

7.67

7.677.67

8.78

9.63

12.20

14.83

19.58

19.5819.5819.58

27.06

27.06

5.71

7.67

7.67

8.78

8.788.78

9.63

19.58

13.05

15.68

27.06

27.0627.0627.06

29.57

29.57

OVB

TRON QZ FX FM SH P FO 65 PMAL MA MF BK UP L/ 60

INITIAL 1.5m SHEARED, WEAKLY SERICITIZED, AND BLOCKY;

FO 42 P) FMFVL BI CB 815 FG SH PAL UB QZ CV

STRONGLY CARBONATI ZED, BIOTITIC, SHEARED MAFIC VOLCANIC WITH SOME QUARTZ VE1NLETS AND PODS.

HG WF

FG MX 0V GV

TRONMA

MFVL AX CL DG FX

X TRONMA

X TRONDA

TRON QZ SE SE2 SH FG AL LG FX QZ4 WP BK

FO L/

U/

FOU/

37

30

62 l - 75

STRONGLY SERICITIZED, SHEARED TRON WITH QUARTZ EYES/AUGEN; LOCAL QUARTZ VEINS; VERY BLOCKY; VERY FINE DISSEMINATED PYRITE

TRON OZ FX FM SH PAL MA MF

AS ABOVE BUT COARSER AND NOT SERICITIZED OR BLOCKY.

Q)

cT

D* DT

D =DT

D)

DT

-xca..

DmOm^m0

•KXHMMK.

•"•••--"rs3Et.i

O0

cr^. _ kcr>COcw

V--

J;- i'

n f :

O wg 3mo02: SronB

3 ^m cfO 3D

I^

D) DT

LYMX GEOLOG


K FE LY G

PLRRRRRRR

PLRRRRRRRRRRRRRRRR

PLRRRR

PLR

PLR

'

29.57

29.5729.5729.5729.5729.5729.5729.57

43.48

43.4843.4843.4843.4843.4843.4843.4843.4843.4843.4844.0344.0344.0347.6547.6547.65

49.90

49.9049.9049.9049.90

55.20

55.20

57.00

57.00

43.48

43.4843.4843.4843.4843.4843.4843.48

49.90

49.9049.9049.9049.9049.9049.9049.9049.9049.9049.9044.9044.9044.9048.7448.7448.74

55.20

55.2055.2055.2055.20

57.00

57.00

59.65

59.65

UHEX INC. BAMAJI

DRILLHOLE/TRAVERSE : BAH88^13 (CONTINUED)

PAGE: Z D ATE: 88/HOV/E5

CORE RECOV ERY

C X )

ROCK QUAL DESIG

X TYPI- QAL TEX- GRAIN FRAC- H ROCK FYING H1N TURES CHARACS TURE I TM TM MAT TX TX F C X M X TYPE 1 2 QM1 1 2 F F C P # TK

FOR EN RT TM QM2 TX TX S R S 0 DIP F MEM V Q LC- 3 3 4 0 N H 1 S ML I AGE COL R 0 P C

T 1

T 2

STRUCTUR- 1

AZM RT

ID STK DIP AZM RT

STRUCTUR-2

ALTERATION HIM! H H H H H ;

OZ BI CY

KF MU CLH

CB MG

EP HE H H

5 OREVNY H MIN A XX PY

HA H

PRH


CP GL YY

MOH

SL H

HA H

SUMMARY

TRON QZ FX QZ3 FM UP WA MA BI FX3 WF LB

LOCALLY SILICIFIED, SHEARED UNIFORMLY TEXTURED, UBIQUITOUS FRACTURE COULD BE INDICATION REDUCTION; SULPHIDE

2 4 56 FO 53 V) F2 BT D)

AND BANDED; OVERALL FAIRLY TRONJ; SOME MINOR QUARTZ VEINS AND CONTROLLED SERICITE; GRANULAR APPEARANCE OF FABRIC DEVELOPMENT, GRAIN SIZE CONTENT NOT HIGH t1X; TOWARDS L/

FINER GRAINED AND FELDSPAR PORPHYRITIC WITH DARK GREYFINE MATRIX.

TRON QZ FX FG LB 2 4 P FO 40 0) OSA LA AX BR SF BN 35 0 +

WELL FOLIATED, SHEARED, LOCALLY BRECCIATED AND PYRITIC TRONJ; PYRITIC BRECCIATED SECTIONS CONTAIN MAFIC COMPONENT OF CHLORITE, ACTINOLITE AS WELL AS PERVASIVE CARBONATE; LOCALLY APPEARS TO BE SERICITE SCHIST; SILICIFICATION PATCHY; LOCAL BANDING ESPECIALLY NEAR OR WITHIN BRECCIATED SECTIONS; MINOR FRACTURE CONTROLLED ALTERATION (SERICITE). RESEMBLES SECTION IN HOLE 011--BAMAJI LAKE SHOWING.-- SEVERAL SHORT SECTIONS OF CREAMY WHITE BANDS WITH BIOTITE FRACTURES; SHARP LOWER CONTACT WITH MAFIC VOLCANICS (30 DEGREES TO CORE AXIS); FAIRLY SHARP U/ WITH WEAKLY ALTERED TRONJ. PYRITIC (4-5X), CENTRAL 25cm BRECCIATED, VUGGY, BANDED WITH CREAMY WHITE SERICITE AND QUARTZ BANDS AND FRACTURE CONTROLLED BIOTITE SEAMS{47 DEGREES TO CORE AXIS). PYRITIC 7-8X PY AND SOME PO; BANDED, CRENULATED; APPEARSLESS BRECCIATED BUT IS FINELY BANDED WITH MAFIC COMPONENTOF CHLORITE/ACTINOLITE.

D) SEP1

FO 20 S+ F1MFVL AX FX AX5 MG FO PWA DG BI FX3 LE EQ

COARSER THAN USUAL MAFIC VOLCANIC BUT WELL FOLIATED AND STRONGLY L1NEATED, VISIBLE ON BROKEN END OF CORE (ALIGNMENT OF PRISMATIC HORNBLENDE); COARSER GRAINED AND PLAGIOCLASE RICH AT LOWER CONTACT, COOKED UP MAFIC VOLCANIC".

c* DT

FO 50INFV OZ SE OZ2 FG SF PSA LA FX FX?

SERICITE MICA SCHI ST ; I NT-FELSIC VOLCANIC OR TRONJ PRECURSOR

F? F1

D*

MFVL AX FX BN FG P FO 45 V*MA MG MU FO VO 26 F2 P1

INITIAL 1 METER FAINTLY RESEMBLES ABOVE; COULD BE LESS ALTERED

SE P2

TO Q*

LYNX GEOLOG

F - I N T E R V A K L (UNITS s METERS) E A Y G F R O M - T O

K FE LY G

RR

PLRRRR

PLRNLRRRNLRR

PLRRR

PLRRRRNLRNLRRRN

*

57.0057.00

59.65

59.6559.6559.6559.65

61.57

65.7465.74

66.6066.6066.6066.60

67.1367.13

67.85

67.8567.8567.85

73.14

73.1473.1473.1473.1486.60

90.6090.60

102.35102.35102.35102.35

1

59.6559.65

61.57

61.5761.5761.5761.57

67.85

66. AA66. 44

67.1367.1367.1367.13

67.8567.85

73. H

73. H73.1473.14

130.66

130.66130.66130.66130.6689.23

92.6092.60

102.60102.60102.60102.60

UHEX INC. BAMAJI

DRILLHOLE/TRAVERSE : 8AM88 13 (CONTINUED)

PAGE: 3 DATE: &8/H.OV/25

CORE X TYPI- OAL TEX- GRAIN FRAC-RECOV- M ROCK FYING MIN TURES CHARACS TUREERY I TM TM MAT TX TX F C X M

{ X ) X TYPE 1 2 QM1 1 2 F F C P # TK

STRUCTUR-1 ALTERATION MINS ORE-TYPE MINSH H H K H ANY H H H ANY

ID STK DIP A A A A A MIN A A A MINAZM RT QZ B! CY CB MG XX PY CP GL YY SUMMARY

ROCK FOR EN RT TM OM2 TX TX S R S O DIP FQUAL MEM VQLC-3 3 4 O N H X SML IDES1G AGE COL R D P C


STRUCTUR-2 AAAAAAAA

VERSION OF ABOVE; THIN PYRITIC, CHLORITIC QUARTZ VEIN AT 58.40 WITH BLEBS OF TOURMALINE SEVERAL cm UP HOLE.

TRON QZ FX MA DA MU

PROGRESSIVELY MORE IN A QUARTZ VEINED

FM FO 34PA FR

ALTERED (SERICITE) ZONE (SHEAR?) WITH

P U/ 55 V1 F? VQ 62 F2

DOWN SECTION CULMINATING SULPHIDES; SEVERAL

MAFIC VOLCANIC XENOLITHS WITHIN THIS GREYISH QUARTZ VEINED ZONE; TRACE SILVERISH MINERAL, GALENA?

MFVL AX FX FG WF P S) E*DC BI LB GV

TYPICAL; LOWER CONTACT WEAKLY BRECCIATED.X TRON QZ FX MG MX N U/ 44

MA 81 BRBLEACHED, SIL'D TRONJ WITH ALTERED, B IOTl T I C , STRONGLY CARBONATIZED MAFIC VOLCANICS AT UPPER AND LOWER CONTACTS WITH t1X PYRITE; FOLIATION MEASUREMENT FROM SHEARED HALOES.

X TRON QZ FX FR FM N FO 40 P1 EIAL WH BI FO 52

COARSER AND FOLIATED; BIOTITE ALTERATION AT LOWER CONTACT WITH TRONJ.

TRON QZ FX HO WP P PW F2 WA MA BI MX L/ 64 ^

TYPICAL HOMO OTZ FELDS BIOTITE TRON WITH LOCAL BLUE QUARTZ EYES AND RARE THIN QUARTZ VEIN; WEAKLY SHEARED AT LOWER CONTACT AND IN LOCAL AREAS WITHIN UNIT.

34 S* E'MFVL AX FX AX6 FG WF DG CL FX2 LB HO

HOMOGENEOUS, FINE GRAINED, MAFIC VOLCANIC; LOCALLY ABUNDANT CARB STRINGERS/GASHES; OFTEN SHORT SILICIFIED, EP1D+-CARB. LIGHT GREEN SECTIONS WITH SHEARED B10TITIC HALOES; LOCAL PILLOW SELVAGES, ESPECIALLY AFTER 116.0

X TRON QZ FX WP FM N U/ DA BI MX L/

GROUND CORE WITH 20X CORE LOSS; LOCAL WEAK SERICITE X TRON 02 FX WP BK N L/

DA BI MXDISCRETE SHEARED SULPHID1C MAFIC VOLCANIC; ROCK ON EITHER SIDE IS BARREN MAFIC VOLCANIC WITH NUMEROUS THIN CARBONATE STRINGERS.

X MFVL BI QZ FG SH N FO 65 X2

4227

46

D) PY

AX D)

S) DT

F2 P1 D) DT +T

LYMX GEOLOG

F - I N T E R V A K L (UNITS s METERS) E A Y G F R O M - T O

K FE LY G

LRRRRRNLRRRRRNLRRRRRNLRRRRRRRRNL

PLRR

PLRRRR

*

105.40105.40105.4010.1010.1010.10

10.5310.5312.4412.44

112.44112.44

113.54113.54113.54113.54113.54113.54

114.17114.17114.17114.17123.50123.50123.50123.50123.50

130.66

130.66130.66

133.07

133.07133.07133.07133.07

"

106.37106.37106.3710.5310.5310.53

11.1511.1513. 5413.5413.5413.54

14.1714.17

114.17114.17114.17114.17

115.71115.71115.71115.71127.00127.00127.00127.00127.00

133.07

133.07133.07

188.88

188.88188.88188.88188.88

UMEX INC. BAMAJI


PAGE: 4 DATE: 88/MOV/25

CORE RECOV ERY

( X )

ROCK QUA L DESIG

X M ROCK I X TYPE

FOR EN RT MEM V 0 AGE

TYPI- DAL FYING MIN TM TM MAT

1 2 OM1

TM OM2 LC- 3COL


1 2 F F C P # TK

TX TX S R 3 4 0 N

R D

S 0 DIP F H 1 SML I P C

T 1

T 2

STRUCTUR- 1

AZM RT

ID STK DIP AZM RT

STRUCTUR-2

ALTERATION MINS C H H H H H ANY

02 BI CY

KF MU CL H

CB MG XX

EP HE HA H H H

)RE-TYPE MINS H H H ANY

J A A A MIN PY CP GL YY

PR MO SL H H H

HA H

SUMMARY

AL LU CB QV BLEACHED SILICIFIED AND ;POOR SULPHIDE CONTENT; STAIN.BOTH UPPER AND LOWER CTC'S VOLCANIC HALOES, LONGER AT

X TRON OZ FX MGWA LA

CARBONATIZED MAFIC VOLCANICS; FRACTURED WEAK POSITIVE REACTION TO ANKERITE

FEATURE B10T1TIC CARBONATIZED MAFIC LOWER CONTACT.

N U/ 66 PW ES VQ 20

BIOTIT1C, CARBONATIZED SHEARED MAFIC VOLCANIC; 32 DEGREES TO CORE AXIS.50X OF SECTION IS BLEACHED (CREAMY WHITE/GREEN), SILICIFIED VARYINGLY CARBONATIZED MAFIC VOLCANIC; MINOR POSITIVE REACTION TO ANKERITE STAIN; POSSIBLE EPIDOTE COMPONENT AS WELL.

X MFVL AX FX AX6 FG WF 34 D OM E*BL CL FX2 LB HO

STRONGLY SULPH1D1C SHEARED, CARB'D, BIOT1TIC, LOCALLY BANDED MAFIC VOLCANIC; COULD CORRESPOND TO ONE OF SHEARED SULPHIDE RICH MAFIC VOLCANIC SECTIONS IN BAM-06 WHICH WAS ANOMALOUS IN AU; GRADUAL DECREASE IN ALTERATION INTENSITY TO LOWER CONTACT WITH FRESH MAFIC VOLCANIC.

X MFVL BI SX BI3 FG SH 2 3 N FO 63 X+ F3AL MU 0 2 S X1

SHORT SECTIONS OF SILICIFIED LIGHT GREEN POSSIBLY EP1DOT1ZED CARBONATIZED MAFIC VOLCANICS AS AT 112.44; AT LEAST ONE VERY SHORT BIOT1TIC/CARB SHEAR AS AT PREVIOUS ALTERED MV; MV IS FOLIATED THROUGH THIS SECTION AT 42 DEGREES TO CORE AXIS. LIGHTER IN COLOUR AND SI L ICEOUS--RELATIVELY HARD; ABUNDANT LOW ANGLE(20 DEGREES TO CORE AXIS) BIOTITE, QUARTZ AND CARB BANDS, PROBABLE PILLOW SELVAGES; TYPICALLY WAVY AND FEATURING SOME THIN CARB STRINGERS.

X MFVL AX FX AX6 FG WF 34 D PW E* MG CL FX2 LB HO

TRON QZ MA

TYPICAL WEAKLY CARB, BIOTITIC

MI OZ2 WP FM 2 5FX FX4 HO MXSILICIFIED, QUARTZ FELDSPARMAFIC VOLCANIC AT UPPER AND

2 4 67

* U / 57 PW F1 L/ 65 F1

PORPHYRITIC TRONJ; LOWER CONTACTS.

' QM EMFVL AX FX FG WF PI DG 81 LB HO

TYPICAL MV WITH LOCAL SIL'D, EPIDOTIZED, SLIGHTLY BLEACHED APPEARING SECTIONS; PILLOW SELVAGES COMMON, USUALLY IRREGULAR; OCCASIONAL TRONJ DIKE; CARB THREADS/STRINGERS/FRACTURE FILLS VERY COMMON; OCCASIONAL SPOTTED, VARIOLITIC OR HORNFELSIC

D)

S) QM

PM QZ D* DT +T PS D) **

S)

B*

S)Q +

DT

DT

CB DT Q +

LYNX GEOLOG

F K L ( E A Y G

K FE LY G

RNLRRRRRRRNLRRRRRRRRNLRR

PLRRRR

PLRRR

- I N T E UNITS s ME!

FROM -

133.07133.80

H5.00145.00153.00156.20156.20156.20167.13167.13

168.48168.48168.48168.48168.48168.48168.48168.48168.48

175.75175.75

188.88

188.88188.88188.88188.88

194.56

194.56194.56194.56

R V A L fERS)

' T 0

188.88135.20

152.50152.50154.50161.80161.80161.80167.53167.53

169.85169.85169.85169.85169.85169.85169.85169.85169.85

185.50185.50

194.56

194.56194.56194.56194.56

200.25

200.25200.25200.25

UHEX INC. BAMAJI

DRILLHOLE/TRAVERSE : BAM88^13 (CONTINUED)

PAGE: 5 DATE: 88/MOV/Z5

CORE RECOV ERY

( X )

ROCK QUAL DESIG

X M ROCK I X TYPE


TYPI FYING TM TM

1 2

TM LC- 3 COL

CAL TEX- GRAIN FRAC- MIN TURES CHARACS TURE MAT TX TX F C X M OM1 1 2 F F C P # TK

QM2 TX 3

TX S R S 0 4 0 N H X

R D P C

DIP F SML 1

T 1

T 2

STRUCTUR-1 ALTERATION MINS ORE H H H H H ANY H

AZM RT QZ BI

ID STK DIP KF MU AZM RT

STRUCTUR-2

CY CB

CL EP H H

MG XX PY

HE HA PR H H H


CP GL YY

HO SL HA H H H

SUMMARY

LOOKING TEXTURE CAUSED BY PERVASIVE CARBONATIZATION.X TRON QZ MI OZ2 WP FM 2 5 N U/ 60

MA FX FX4 HO MXPATCHY VARIOLITIC, SPOTTED TEXTURE (ALTERATION?), USUALLY ACCOMPANIED BY STRONG CARBONIZATION AND FINE DISSEMINATED PY. BLOCKY GROUND CORE.NUMEROUS SECTIONS OF LIGHT GREEN BLEACHED AND SPOTTED (VARIOLITIC?) MV; SIL'N, EPIDOTE AND CARB ALTERATION; ALSO PATCHES/MASSES QTZ AND IRREGULAR THIN QTZ VEINS; POOR SULPHIDE TYPICAL SIL'D TRONJ WITH BIOTITE, CARB'D SHEARED MV MARGINS

X TRON QZ FX WP FM N PH E1UA DA BI

SECTION IS COMPOSED OF DOMINANTLY VEIN QTZ WITH UPPER AND LOWER MARGINS OF SHEARED PYRITIC, BIOTITIC, CARB'D MV; THE QTZ IS MILKY WHITE TO LOCALLY GREY WITH PO AND PY IN FRACTURES AND PARTINGS AS WELL AS SOME LOCALIZED DISSEMINATIONS; THE PO IS NOT MAGNETIC; SOME CARB WITHIN QTZ VEIN ITSELF BUT MORE OFTEN AS FRACTURE FILLINGS; THE LAST 38 CM APPEARS TO BE INTENSELY SIL'D AND PYR1TIZED MV WITH SOME BRECCIATON EVIDENT; RESEMBLES QZ-BR-SHEAR ZONE WITH MINOR CARB(CALC I T E )

X QZVS QZ SX QZ7 FG FO N VO 30 *:*LA BI BM FO 51

HOMO F.G., MUCH FEWER CARB VEINLETS; OCCASIONAL THIN QTZ VEINLET AND WEAKLY SIL'D WALLROCK.

TRON QZ SE QZ2 FG PO 3 5 P FO 48 PW F1AL LA FX SE3 SH MY U/ 53

INITIAL 1.5m WEAKLY ALTERED, FOLIATED; SERICITE STRONGEST BETWEEN 189.60-192.50m; ALTERATION INTENSITY WEAKENS AT LOWER CONTACT AS WELL; CENTRAL SECTION INTENSELY ALTERED; TYPICAL ALTERED/SHEARED TRONJ; MINOR THIN QUARTZ VEINS.

MFVL AX FX FG WF PPI DG BI LB HO

PATCHY, VARIOLITIC, LIGHT GREEN SIL'D, EPIDOTE, CARB SECTIONS; THIN TRONJ DIKES/SILLS; 200.25 m EOH; CASING LEFT IN HOLE; CORE STORED AT UMEX MINE.

D+ DT

GEOLOG DICTIONARY LEGEND

BAMAJI PROJECT

TABLE,FLAGALZOVB

ALTERATION ZONE Overburden

TABLE,ROCK AMPH - FETF = INFI ~ INFV = INVL = MFVL - MSC OVBQFPO = QZBS s* QZFP = QZVN - QZVS = TRON =

AmphiboliteFELSIC TUFFINTERNED TO FELSIC INTRUSIVEINT-FELSIC VOLCANICINTERMEDIATE VOLCANICMafic VolcanicMISSING CORECASING, OVERBURDENQUARTZ FELDSPAR PORPHYRYQUARTZ BRECCIA SHEAR ZONEQUARTZ FELDSPAR PORPHYRYQUARTZ VEINQTZ VEINED SHEARTRONDHJEMITE

TABLE,MINERALAX BI CB CL FX MF MI MU PF QX QZ SEsx

AMPHIBOLE BiotiteCarbonate, CALCITE ChloriteFeldspars, general Mafics, general Micas, general Muscovite PLAGIOCLASE Quartz, crystals Quartz, general SERICITE Sulphides, general

TABLE,TEXTUREAG = Augen structuredAU ~ AUGENBK = BlockyBN = BandedBR ^ BrecciatedCO ~ CONTORTEDCR = CrenulatedCV s CARBONATE VEINEDEQ = EquigranularFC ~ FINE TO COARSE GRAINEDFG ^ FINE GRAINEDFM * FINE TO MEDIUM GRAINEDFO = FoliatedFR = FRACTUREDGN = GneissicGR ~ GRANULARGV = GRANITIC VEININGHO - HomogeneousIH = INHOMOGENEOUSIQ = InequigranularIR = IRREGULARLB " LOCALLY BANDEDLE = LineatedLF - LOCALLY FOLIATEDLP = LOCALLY PORPHYRITICMF = MODERATELY FOLIATEDMG ~ MEDIUM GRAINEDMO ~ MOTTLEDMX = MassiveMY = MyloniticPA = PatchyPI ~ PILLOWEDPO = PORPHYRITICQV ^ QUARTZ VEINEDSF = STRONGLY FOLIATEDSH ~ SHEAREDSU = SUCROISICVA = VARIOLITICVU = VUGGYWF ** WEAKLY FOLIATEDWP = WEAKLY PORPHYRITICXE ~ XENOLITHIC

TABLE,QMINAX s Amphiboles, generalBI s BiotiteCL = ChloriteFX = Feldspars, generalPF = PlagioclaseQZ = Quartz, generalSE = SERICITESX ^ Sulphides, general

TABLE,HOW-SCALE11 ~ Clear Field# = Breccia fillingsS ~ BOTRYOIDAL) - CL/MG replaces MF* = Clasts4- ~ Within QTZ VN, DISS'D/PARTINGSO = Fresh,primary rock1 - DISSEMINATIONS, SCATTERED XLS2 ** DISSEMINATIONS AND AGGREGATES3 = DISS'NS, AGGS AND FRAC FILLS4 e IRR STRINGERS/BANDS PARA FOL5 = VEINLETS6 e GASHS7 - PARTINGS IN QUARTZ8 = SEMI-MASSIVE9 = PHENOCRYSTS< - fracture fillings, SMEARS

MS/CY replaces FX > = IRR PATCHS, VEINS A = A, cavity fillings B = BlebsC = Coatings S encrustationsD ~ FINE DISSEMINATIONSE = Envelopes/HALOS ADJ VNS/VNLTF = Framework crystalsG = GougeH = Replaced phenocrystsI = Eyes,augenJ = FLECKSK = StockworkL ^ Laminations/BANDSM = MassiveN = SELVAGESO ^ VEINS AND STRINGERSP = PervasiveQ = PATCHY, LOCAL DEVELOPMENTR = PATCHS AND BLEBSS s STRINGERST = StainingsU = Eu-hedral crystalsV = VeinsW = WISPSX = BANDSY = IRR ENDS/COMPLEX INTERLOC AGGSZ = Massive,Laminated/Bedded

TABLE,G-SCALE" = Clear Field) = .5 to < 2%* - < .5%-f ^ 2 to 31/ = Est. ImpossibleO = Nil, Absent1 7 to

TABLE,SIDBN ^ BandingFO - FOLIATIONGV = GRANITIC VEINL/ ~ LOWER CONTACTU/ = UPPER CONTACTVC = VEIN, CARBONATEVQ ^ VEIN, QUARTZ

TABLE,DIP10 = 10.0000 DEG.15 = 15.0000 DEG.18 ^ 18.0000 DEG.20 = 20.0000 DEG.22 - 2 2.0000 DEG.24 - 2 4.0000 DEG.25 ~ 25.0000 DEG.26 = 2 6.0000 DEG.27 *s 27.0000 DEG.28 = 2 8.0000 DEG.32 - 3 2.0000 DEG.33 ^ 33.0000 DEG.34 = 34.0000 DEG.35 e 35.0000 DEG.36 = 36.0000 DEG.37 = 37.0000 DEG.38 ^ 38.0000 DEG.39 = 39.0000 DEG.40 = 40.0000 DEG.41 s 41.0000 DEG.43 ~ 43.0000 DEG.45 = 45.0000 DEG.46 = 46.0000 DEG.47 = 47.0000 DEG.49 s 49.0000 DEG.50 = 50.0000 DEG.51 ^ 51.0000 DEG.52 = 52.0000 DEG.53 - 53.0000 DEG.54 = 54.0000 DEG.55 s 55.0000 DEG.56 = 56.0000 DEG.58 ^ 58.0000 DEG.60 = 60.0000 DEG.62 ^ 62.0000 DEG.63 ^ 63.0000 DEG.64 ^ 64.0000 DEG.65 ^ 65.0000 DEG.68 = 68.0000 DEG.70 = 70.0000 DEG.74 ~ 74.0000 DEG.75 = 75.0000 DEG.80 = 80.0000 DEG.? = UNKNOWN DEG.

BAMAJI LAKE PROPERTY 1988 DRILL PROGRAM SAMPLES

FROM

BAM88-07

19.5521.0521.8023.3024.8025.4426.0626.3630.1531.6532.2533.3834.3835.7837.0660.0061.5062.6364.1365.6367.1368.2268.9270.4271.9272.4590.08108.70109.78110.30115.46122.76125.12128.80130.30131.80132.80133.85135.35136.25136.65138.15138.85140.25146.95147.91

TO

21.0521.8023.3024.8025.4426.0626.3628.3931.6532.2533.3834.3835.7837.0638.4061.5062.6364.1365.6367.1368.2268.9270.4271.9272.4573.9590.78

109.78110.30111.30116.26123.56126.82130.30131.80132.80133.85135.35136.25136.65138.15138.85140.25141. 14147.91148.50

NUMBER

B84301B84302B84303B84304B84305B84306B84307B84308B84309B84310B84311B84312B84313B84314B84315B84316B84317B84318B84319B84320B84321B84322B84323B84324B84325B84326B84327B84328B84329B84330B84331B84332B84333B84334B84335B84336B84337B84338B84339B84340B84341B84342B84343B84344B84345B84346

ONTAWO GSOIOQICAL SURVEY ASSESSMENT FILES

omen DEC l G 1983

RECEIVED

FROM TO NUMBER

149.72166.29166.86168.15169.35169.77

BAM88-08

150.72166.86168.15169.35169.77170.87

B84347 B84349 B84350 B84351 B84352 B84353

10.0411.5413.0414.5415.5416.5418.0422.5726.3227.8230.9432.4433.9435.9737.4238.9240.4241.9247.4549.6263.6666.2067.7072.2473.7475.2482.4291.0092.6493.57102.45103.95105.45106.57107.71109.21110.86112.36114.40115.50116.53118.03119.10

11.5413.0414.5415.5416.5418.0419.7423.3727.8228.4532.4433.9435.9737.4238.9240.4241.9242.9849.2351.1564.5267.7069.2073.7475.2476.4582.7291.6293.5795.07103.95105.45106.57107.71109.21110.86112.36114.40115.50116.53118.03119.10120.00

B84354B84355B84356B84357B84358B84359B84360B83361B84362B84372B84363B84364B84365B84366B84367B84368B84369B84370B84371B84373B84374B84375B84376B84377B84378B84379B84380B84381B84382B84383B84384B84385B84386B84387B84388B84389B84390B84391B84392B84393B84394B84395B84396

FROM TO NUMBER

120.00120.98122.58123.50130.85135.11151.17157.92163.50164.50165.38165.68167.10167.35

120.98122.58123.50125.00132.35136.61151.67159.42164.50165.38165.68167.10167.35168.85

B84397 B84398 B84399 B84400 B84401 B84402 B84403 B84404 B84636 B84637 B84405 B84406 B84638 B84639

BAM88-09

3.284.786.287.789.599.88

11.4012.9013.9015.4016.6218.1219.6221.3222.8224.2324.9526.4727.9729.4730.9731.6733.1734.2135.7143.9544.5045.3046.1547.1149.0849.3854.5755.7356.57

4.786.287.789.599.8811.4012.9013.9015.4016.6218.1219.6221.3222.8224.2324.9

DD RPT 30 FRY LAKE€¦ · lykx geolog f -interval k l (units - m eters) e a y g from -to k f e l y g p l r r r p l r r r p l r r p l r p l r r r r r n l p l r r r p l r r 108.70

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