SUPERVISION GEO-X INC. - Ontario

l l l l l l l l l l l l l l l l l l l

42G04SW0ai1 2.12448 WALLS 010

GEOPHYSICAL REPORT

OF THE

WALLS TOWNSHIP PROPERTY

ONTARIO, CANADA

Val d'Gr, Quebec

December, 1988

Super vi si on 6eo--X I ne ,

Jean-Claude Parish, B. St:,

SUPERVISION GEO-X INC.(96, !9C Rut, VAL o'OK, QC. J9P 2X5 TEu.: (BI9) S2S-SD23 FAX (BI9) B3S-I1B1


42G04swe2ii 2.12443 WALLS TABLE OF

TABLE GF CONTENTS.. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

SUMMARY....................... . . . . . . . . . . . . . . . . . . . . . 3

CERTIFIGATE. . . . . . . . . . .... .. . . . . . . . . . . . . . . . . . .... . . . 4

INTRGDUCTION. ... . . . .. ... . . . . . . .. . . . .. . . . . . . . . . . . . . . 5

LOCATION, DESCRIPTION AND ACCESS. . . . . . . . . . . . . . . . . . . 5

CLAIM LIST......................................... 6..7

PREVIOUS WORK......... . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8

REGIONAL. GEOLOGY. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8. . 9

ECONOMIC GEOLOGY................................... 9

GEOPHYSICAL TECHNIQUES............................. 10.14

GEOPHYSICAL RESULTS..... ... . . . . . . . . . . .. ... . . . . . . . . . 14.15

CONCLUSION......................................... 16

RECOMMENDATIONS.. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17

Fj:i3yRESj

1. Lo c: at i on map.

2. Claim map

IN POCKET

E l e c t. r o m a g n e t i c map (V. L. F. )

Magnetic: map.

Max Min map.

SUPERVISION GEO-X INC.


SUMMARY

A m a g n e t. i c:, el e c: t r o ft) a g n e t i c: (V. L. F. ) a n d Ma x M i ri s LI r v e y s w e? r e

p e? r-f o r m e d on Mont, val Resources Ltd p) roper t y located i ri Walls

Townr.h i p , On tar i o.

Good correlation exist between each survey. 7'he magnetic: survey

was able to delineate the location o-f a mineralize horizon within

a sedimentary unit, (-felsic tu-f-f ?) , also it was able to pick up

the contact, between a sedimentary unit (-felsic tu-f-f ?) and the

basaltic flow located on the? south west part o-f the grid.

The V.L.F". survey delineates possible fractures within the

sedimentary unit (-felsic tu-f-f ?) and also it was able to

determine possible shear zones at the contact between the

sedimentary -formation and the basaltic unit located on the south

west part of the grid.

The Max Min anomalies correspond very well with the V.L.F.

anomaly B, which could be the indication of a possible mineralize

-fractured zone within the sedimentary -formation (-felsic tuff).

A drilling program is recommended in order to determine the

possible economic potenti el on the Montval Resources Ltd

propertyM A total of 6000 feet will be required to verify the

p oss i b l e g o l ci m i n er a l i z e st r uc t ur es.

SUPERVISION GED-X INC.


CERT IF-" I GATE OF QUALIFICATION

I Jean-Claude Parish, of Val d'Or, in the province of Quebec, C a n a da, d o hi e r e b y c e r t i f y that:

l reside at 121 Place Vanier, apartment 6, Val d'Or, Quebec.

I am a qualified geologist having received my academic training at University of New-E-irunswick in Fredericton, New-Brunswick graduated in 1976, B.Bc. honors.

I have been continuously engaged in my profession for the past 13 years. I have examined the assessment work files covering the subject property and the immediate area.

This report is based on the author's experience in exploration on a comprehensive study of all the work records and on geological maps and reports published for the area.

I have not, direct, l y or indirectly received or expect to receive any interest, direct or indirect, in the property of Montval Resources Ltd. or beneficially own, directly or indirectly, any s e c u r i i. i G s o f t li a t c o m p a n y.

Jean-Claude Parish, B.Bc.



Supervision Geo- X was asked on behalf of Gestion Edward Ingham

I n c:: . t. o w i"- i t. e; a g e o p h y s i c a l r t? p a rt a ri M o n t. v a l R e s o u r c e s Ltd.

p r o p f r- 1 y l a c a t. e d i n Wall s T' o w n s h i p .

B . M . E x p l o r a i. i on c u t a d e tail grid t o t a 1 1 i n g 35.62 miles o -f cross

lines, 2.63 miles of tie lines and 4.93 miles of base lines. An

electromagnetic survey (V.L.F.) arid a magnetic survey were

performed on the grid. The V.L.F. survey was performed with a

Beanies EM 16 instrument while the magnetic survey was executed

with a Scintrex mp-2 apparatus. Readings were taken at 100 ft

intervals along lines spaced at 600 ft. A total of 1874 readings

of V.L.F. and mag were taken during the surveys.

A total of 8.39 miles of a Max M in survey was performed on the

property. Readings were taken at. 100 ft intervals with a cable

separation of 500 ft. A total of 443 readings were taken during

the B u r ve y.

The walls property is made f o 142 contiguous unpatented mining

claims for a total of approximately 2,300 hectares. It is

located in the central part, of walls township.

The walls claim group is accessible from a forest access road

going south from Hearst and -from another access road located a

few kilometers further west. A few logging roads off the main

access rout, cos; extend near and os' e r parts of the walls claim

group. Logging took place over large sections of the property.

Many of the secondary roads are unused and vegetation infringes

a l o n g t h e r o a d s i d e s .

SUPERVISION GEO-X INC.-

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UP

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CLAIM LIST

The war-

proper t

The hi

1 isted

CLAIMS

923356

923330

923322

923373

923204

923236

916724

916730

The bal

CLfilMS

923320

923379

923301

923377

923326

923362

923352

923371

923202

9232 1O

k was per -formed

y "ac k o -f ci a i nts

bel o w::

-- 923361 inclusi

- 923351 inclusi

-- 923325 inclusi

-- 923376 inclusi

-- 923209 inclusi

- 923242 inclusi

- 916727 inclusi

- 916736 inclusi

a ne e of the clai

- inclusi

i ne 1 us i

-- 923321 inclusi

- 923378 inclusi

- 923329 inclusi

-- 923370 inclusi

-- 923355 inclusi

-- 923372 inclusi

-- 923203 inclusi

-- 923234 inclusi

. . . . . . . . C2 1 in i- 1

on part of

at which

vel y

vel y

vel y

vel y

ve?l y

vel y

ve?l y

vel y

m group is

ve?! y

vel y

vel y

vel y

vel y

vel y

vel y

vel y

vel y

VE;! y

n\ /ir?in K.I f"2

the Mont val Resources Ltd.

the surveys were executed, are

CLAIMS AREA (Hec.)

6 96

22 352

4 64

4 64

6 96

7 112

4 64

7 1 1 2.

60 claims 960(hec. )

listed below :

CLAIjvis ARE A (Hec. )

1 16

i 162 1 336

2 32

4 64

9 144

4 64

2 32

2 32

25 400

trn.V iKir" .. ........ . .... , ...... ,..,, ........,. ,...

l l l

^ L.JST

( SU I TE )

9 2 3 3 B O - 9 2 3 3 8 3 i rt c l u s i v e l y 4 64

1 916728 - 916729 inclusively 2 32

9J.6723 -- inclusively l 16

923387 - 923390 inclusively 4 64

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l - BUPERVIBIDN GED-X INC.

82 claims 1312(Hec

ft—jsL-.\s\s

PROPERTY BOUNDARY

Total of 142 claimsApprox. 2,300 hectares ( 5680 acres)

Scale H*0,000

MONT VAL RESOURCES LTD.Walls PropertyCLAIM MAP

FIGURE 3


.....O,

A m a x Hi n e r a l s E. x p l o r a t. i o n I.. t d conducted an a e r o m a g n e t i c survey in

1980 over parts o -f Walls and Minnipuka Township (1-1961). This

survey was -followed in 1981 by diamond drilling, -four holes being

o n 1 1' \ e s u b .j e c: t W a 1 1 s p r o p e r t y .

l' h e l a t e s, t. w o r- k r e g i s t e r e d on t h e assessment -files was p e r -f o r m e d

in early 1978 -for Golden Trio Minerals Ltd. It consisted of an

airborne magnetic and electromagnetic survey (V.L.F.) which

covered large area, including the subject property (T-3127) . The

survey was per -formed using a Cessna 172 equiped with a Proton

Precession Magnetometer and a Totem V.L.F. electromagnetic

system. The average line spacing was one third o-f a mile.

Several conductors were detected by the airborne geophysical

survey published in 1986 by the Ontario Geological Survey. A

wide anomalous zone of electromagnetic anomalies runs across the

W a 1 1 B p r o p e r t. y a t a p p r o x i m a t e l y l O 5 degrees.

The area is underlain by rocks o-f Precambrian age o-f the Superior

Province of the Canadian Shield. A large belt is composed mainly

o-f sedimentary rocks and with less abundant volcanics rocks and

their i n t r u s i. v e e equivalent. T h i s bel t i s p a rt t:) f t h e Q u e t i c o

S u b p r o v i n c e .

G n e i s s i c r c:) c: k s i n t r- u d e d b y d o m a l -f e l s i c pi u t a n s a r- e c l a s s i -f i e d as

p a r t. o f t. h B W a w a S u b ~ p r o v i ri c e . Finally, a n a r r o w belt o-f

volcanic rocks, also part o-f the Wawa Sub-province trends

t. h r o u g h t. W a 1 1 s a n d M i n n i p u k a t o w n s h i p s .



R e g i a n a .1 m a t a m o r p h i s m i n t h e a r e a u s u ally r a n g e s f r o m m i d d l e t. o

L.I p p e r g r e e n c: h i s t -f a c i e s b u t. i t l c:) c: a l l y r c? a c h e s t. h e granulite--

a m p h i b o l i i. e i" a n g e o r- h i g h e i"- . A -f e w r e g i o n a l -fa u 1 1 s , m o st o -f them

striking north-east were mapped. Diabase dykes, most of them

B t. r i k i n g n o r t h - w e s t a n d n o r t. h - e a s t. , a r e r e l a t i v e l y v e r y n u m e r o u s .

There are very -few outcrops on the Walls claim group. Greywacke,

metamorphosed to schist, was encountered in the western part o-f

the Walls claim group. In the eastern part o-f the property, the

major rock units are, from north to south, tonalite, m a -f i c to

intermediate volcanic -flows, -felsic tuff and mafic. to

i n t fs r m e d i a t. e i" o c k s ( m o s 1. 1 y b r e c c: i a , t u f f and m i n o r g r e y w a c k e ) .

Sulphide mineralization was intersected i ri most o-f the holes

drilled in the general area. On the Walls property, -five of the

seven holes drilled in the past intersected graphite with pyrite

and\or pyrrhotite?. The other two contained pyrite and

p y r r hot i te.

Gold mineralization was discovered a few decades ago in Hawkins

and Walls townships, a few kilometers west of the walls property.

The gold occurs in quartz veins and is associated with sulphides.

T' h e h o s; t r o c k s a r s highly m e t a m o r p h o s e d volcanic roc k s .



l. Magnet i cs

T o t a l F i e l ci I n t e ri s i t y

The Earth's, magnetic -field generally ressembles that, of a bar-

magnet. This -field is distorted by several factors but through

the use of sensitive magnetometers the variations attributable to

l o c a l e f -f e c:: i. s c: a n b e m e s u r e d . T h e B e l o c a l e f f e c t s; generally

reflect the changes in magnetic susceptibility of the lithology

i n t h e s u r- v e y a r e a. G e o l c:) g i c: u n i t s o f d i. f f e r e n t m a g ri e t i c field

a t. t h e f:) o in t w h K r e t h e t w o u n i t s m e e t. T his distortion o r

a n o m a l y w i 11 h a v e a c h a r a c t e r i s t i c: s h a p B and amp l i t u d e s dependent

on the variation in the magnetic susceptibility of the rock

types, depth to the contact and the orientation of the magnetic

field with respect to the geometry of the contact.

M a g n e? t. i c: a n o m a l i e s m a y t h e r- e f o r e , be at t r i b u t e d to f a LA 11 s and

s h e B. r z o n e s , c h an g e s i n g e c:) l c:) g i c facies within a unit and to

concent rat i oris f or mi neral i 7. at i on havi ng magnet i c: mi neral s in

t h e i r- a s s e m b l a g e.

The magnetic field is affected by several factors, most notably

diurnal variations within the field and magnetic storms which are

attributed to solar activity. The variations can be corrected

from the magnetic measurements using a base station magnetometer

o f b y r e p e a t i n g t h e m a g n e t i c m e a s u r e m e n t at s p e c i f i c i n t e r v a l s at

a s e 3. e c: t e d t) a s e e; t a t i o n .

In cases where magnetic: storm activity is severe, measurement of

the total magnetic field should not be conducted as corrections

become impractical due to the number of high frequency variations

of the? f i el d .



- j j .

It is well known that, rocks types vary in conductivity arid that a

p r i di a r y e l e c: t. r- o m a g n e t i c f i e l d will gene r a t e se c o ri d a r y -f i e l d s

within the rocks. The more conductive geologic: units will have

h i g h e r a m p l i t u ci e a n o m a l i e s , t. hi u s an e x p r- e s s i. o n of t h e c o n d u c: t a n c. e

o f v a r- i o u s l i t h o l o g i e s o r c h E* n g e s within l i t h o l o g i e s can b e

acqui red .

P o we r -f u l military communication transmitters i ri the 15 to 2. 5

kilocycle range have been applied to geophysical exploration;

electromagnetic receivers tuned to a specific transmitter can

measure the tilt and field strength of the secondary magnetic

f i e l d g en er at eel w i t h i ri t h e Earth. A s i mp l e math emat i c

relationship ex i sits to convert the tilt and field strength

measurements into the in-phase axncl cut-phase of phase components

(i terms of percent) which are presented by many instruments.

T h e s e m e a s u r- e m e n t s c a n t. h e n b e plotted and inspected to d e? t e r m i n e

the presence and orientation of conductive features.

V . L . F' , E M s u r v e y s m u s t b e c o n d u t:: t e d u n d e r c e r tain c r i t. e r i a f o r

the information to tie valid. These? criteria at r e easily met and

are as f o l l o w.

a) The orientation of the survey l i ri e s must parallel the

t r a n s m i 1 1 e d e l e c: t r o m a g n e t i c fie l d , t h a t is, be at 9 O d g r t o t h e

primary field direction w hi i eh is the direction to the location of

t hi e s e J. e c:: t e d t K 1 - a n s m i 1 1 e r .

Measurements of the secondary field can then be made in the

presence of a uniform primary field arid the variations of the

s e c o n ci a r y f i e l d w i 3 l r e f l e c:: t c h a n g e E, in c o n d u c t i v i t y with m i n i m a l

f i el d di start:!, on .



•f ''l i jf.

b) The measurements must. also be made with the instrument

facing in the same direction otherwise anomalies of opposite

p o l a r i t y w i 11 r e s u 11. a n d t h e d a t a c a n b e m i s i n t e r p r e t. e d.

In complex structural regions it. is often good practice to

m e a i:; u i" e res p an B e s u s i n g a s e c o n d 1.1" a r i s m i 11 e r- with a p r i m a r- y field

d i r e c t i o n a t a p p r o x i m a t e l y 9 O d g r to the direction of the f i r- s t

t r a n s m i 11 e r . T h e d e t e c: t i o n o f t h o se? an o m a l i e s a 11 r i b u t a b l e t o

f e a t. u r e s f.:) e r p e n d i c u l ax r t o t he general geologic strike will t hi e n

be enhanced. In normal practice these measurements are made

along the same lines as the first measurement to maintain a cost

efficient. program. However, in complex regions of unknown

geology, a B en: on d set of lines, perpendicular to the first, may

have t o b e p r ep ar ed an d sur veyed w i t h this second t r an sm i 11 er.

Presentation of V-L.F. -- EM data is as profiles of the in-p h as e

a n d o u t - p h a s e c o m p o n e n t s - H o w e v e r , m a ri y anomalies are gen e r a t e d

b y t h e h i g h f r e q u e n c y of t h e V. L.. Fr . t r a n s m i 11 e r w fi i c h a r- e d u e t o

variations in overburden conductivity, swamps and t op o g rap) h y as

well as geologic: conductors. A data processing techniques,

called the "Fraser Filter" can be applied to the data which

allows it to be contoured. This filter converts crossovers and

inflections to positive peaks and minimises station to station

random noise allowing an easier understanding of the data.

T h e V, L.. F. p r o f i l e s a r e i n t e r p i"- e t e d a s f o 11 o w s: a c r o s s o v e r i s

taken at every 2 K difference?. This method is utilised to

cj e t e r m i n e w e a k a n o m a l y p r- o b ably c: a u s e d by e x c e s s i v e o v e r b u r- c J (? n .

11 d e t e r m i n e t. h e o r i e n t a t i o n o f f r- a c t u r e s and possible f a u 11.

Major anomaly will be picked up as well as their weak

continuation. Anomalies which demonstrate continuation are

probably caused by major faults while the non continuous

anomalies are probably due to a small fracture system in the

area.



13-

t H. E. M.

The horizontal loop el ectromagneti c system is the most popular EM

system in use today. The transmitter and receiver are

i n t e r t:: o n n e c: t e d b y a r- e f e r e n c e c: a b le permitting the m e s u r e m e n t of

the EM -field at. the receiver. Frequenci e s which could be

utilized are 111, 222, 888 and 3555 hz . Interconnecting cables

are available several lengths, 25, 50, 100, 150 and 250 meters.

The components measured are; the in -phase and out phase in

p e r- c e n t a g e o -f t h e p r i m a r y -f i e l d .

Depth penetration is in most situations not more than 50-60

percent, o -f the coils separation. To ensure sufficient data for

proper interpretation, one must make measurements at stations not

more than half of the coil separation apart i ri non-anomalous

areas.

While the survey is executed, great care has to be taken to keep

the distance between the coil constant from station to station

a n d t. o h o l d t h e c o i l s i n o n c o m m o n plane?. A d e s c: r e p a n c y of l

percent. in the coil separation causes an in -phase error of 3

percent which can be important when looking for very weak

conductors in the 5 percent peak to peak amplitude range. A

k n o w l e d g e o f t hi e e s t i m a t e ci o v e r burden t hi i c k' n e s s is i m p o r t a n t when

c o n d u c: t i n g a n H E. M s u r v e y .

The two components measured, in phase and on t --phase are plotted

a n d s i m p 3. e i n t e r p r e t a t i o n s s c:: h e m e s a r e u s e d t o c a l c u l a t e d i p and

depth. The width of the conductor is calculated by subtracting

the coil separation from the distance between the ;-:ero value

points of the i rv -phase and out--phase curves. The widths

c a l c u l a t e d u s i n g t h e i n - p h a s e o u r- o u t ~- p h a s e p r o f i l e s m i g h i. d i f f e r

somewhat. Only the val LIE? o b t a i net-:, from the cleanest cur VE? should

be considered correct. A week conductive halo around a very good

SUPERVISION GED-X INC.-

l -14-

I conductor often causes a wider out--p h a se than i ri-p h a se profile.

An estimate o-f the clip o-f the conductor is determined by using a

l dip monogram,, The highest positive peak of in--phase component

tells you the direction of the dip.

m In areas where conductive overburden or host rock is present or

w h e r e t. h e c: o n d u c:: t o r i s e l e c t r- i c a 11 y sat u r a t e d at. higher

l -frequencies these calculated values will often differ-

considerably. In such situations it is imperative to use a

l multi frequency approach to obtained using data collected with the

lowest frequency (that. is, the lowest frequency that produced

l data of suf f i c i ent ampl i t ud e t o be interpreted.

BEDPHYSICAL RESULTS

ll. El*- c t r o m a g n e t i c: s u r v e j/

An electromagnetic survey (V.L.Fr .) was conducted on Montval

l R e s o u r c e s L. t d prop e r t y in Wall s township.

The survey was performed with Geonics E'M 16 instrument. The data

:.i b t a i n e d f r o m t h e s u i"- v e y d e

and D see accompanying map.)

obtained from the survey delineate four major anomalies (A,EI,C,

lThe possible shear zones determined from the survey seem to trend

l in the north-west and south-east direction.

mjjnet i c survey

l The magnetic survey was able to delineate the contact bet we? en

different qeologi cal formation.

l

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..., i 5...

High magnetic:: responses occur between l i ne '54 W and 12 E at 60 M

and 50 N, line IB E and line 48 E at 36 N and 22 N , line 54 W and

48 E at 24 M and 5 M, line 12 W and line O at 26 N and 22 N, line

72 E and line 78 E at 8 N and 5 N, line 96 E and line 156 E at

BLO and 12 N, line 90 E line 138 E at 9 N and 16 N.

3. Ma K Min sur ye y

A Max Min survey was executed on selected lines on Montval

p r o p e r t y. T h e p u r p o s e s o -f t h e s u r v e y w e r- e to confirm V. L. F.

a n o m a l i e s a ri d t o d e t e r m i n e b e 11 e r d r- i 11 i n g t a r g e t s.

A total of 8.39 miles o-f Max Min was per-f armed on the property.

Max Min anomalies are located along line 24 W and 18 W at 51 N

and 48 N, line 24 W and 18 W at 35 N and 33 N, line O and 6 E at

40 M, line o and 6 E at 24 M and 21 N, line 24 E and line 36 E at

20 N and 16 N, and finally line 126 at 6 B.



CQNCLUBigN

"l" h e m a g n e t i c s u r- v e y w a s a h le t o d e? l i n e a t. e a h i g hi m a g n G t i c

response probably cause by a pyrrhotite horizon located in a

sedimentary -formation (felsic tuff ?) . Possible mineralise

horizon o cur r ing at the south west, of the grid was pick up by the

magnetic survey. This horizon seems to be present at the contact

b e? t ween a basaltic: and a sedimentary unit. A high magnetic

response occurs at the eastern part of the grid. This anomaly

could be the result, of a mafic plug.

The el ectromacjnet i c survey was able to locate four major possible

shear zones. Anomaly A correlate with the magnetic responses

which could be due to a pyrrhotite horizon within the sedimentary

u n i t.,,

Anomaly B corresponds very well with the Max Min anomalies. This

g e o l o g i c: a l f e a t. u r- e c o u l d b e t h e r e s u 11. s o f a m i n e r ali z e f r a c t u r e

l c:) c a t e d w i t h i n t h e s e d i m e n t a r- y (f e l s i c t u f f ) u n i t.

Anomaly C located at. the eastern part of the grid correlates with

a Max Min r e s p o n s e s, again this g e o l o g i c: a l s t r u c t u re c o u Id be

c a u s e b y a m :i. n e i"- a l i z e f r a c t LA r- e s p r e s e n t w i t. h i n t. h e s e d i m e n t. a r y

un i t *

A n o m a l y D c: o u l d i n d i c: a t e a m i n e r a l i z e f r a c:: t u r- e d h o r i z o n l o c: a t: e d

w i t h i n t IT e b a s a 11 i c f l o w.



RECOMMANDATlON

The magnet, i c: responses; correlate very well with the

e l e c:: t r o m a g n e t i c: a n o m a l i e s.

F LI r t lie r w o r k s h o u l d b e e x e c u t e d t o d e t. e r m i n e t h e e c o n o m i c:

importance which could occur along a pyrrhotite horizon within a

s e dim e n t a r y u n i t (f e l s i c: t. u -f -f '?) t h e p o s s; i b l e mineralize h o r i z o ri

a l o n g t. h e c o n t a c: t ta e t w e e n a s e d i m e n t a r y -f o r m a t i o n a rt d a basaltic

unit located at the south west. part of the grid, and finally

a 11 e n t i o n s h o u l d b e given t o t h e p o s s i b le mineralize -f r a c t u r e

occurring within the sedimentary unit (determine from the V.L.F.

and Max lvlin anomaly B).

A drilling program is recommended to be executed i ri order to

determine the economic importance of those geological structures

mention above. A total of 6000 ft will be required to verify the

p o s s i b l e g o l d m j. n e i"' a l i. z e s t. r u c t u res.

R e s p e? c t f u 1 1 y s u b m i 1 1 e d ,

, s . -C J4fL**^t-\ 4 si i**

J e a n -- C l a u d e P a r i B

Chi e f Geo l oqi s


Ministry ofNaturalResources

Ontario

Report of Work(Geophysical, Geological, Geochemical and Expenditures)

DOCUMEN' U ;890S

Mining ,...2.12448 WALLS 900

uu nut use snaoeo areas Deiow,

Type of Survey(s)

Max Min, ElectromagneticClaim Holder(s)

Golden Trio Minerals Ltd.

Townihip or

T-720Address

Suite 402-27 Queen Street East, Toronto. OntarioSurvey Company

B.M. Exploration Inc.Date of Survey (from ft to)

05 V 12 .88 l 22 12 88bay j Mo. J Yr. j Day | Mo. [ Yr.

Total Miles of tine Cut

43.18Name and Address of Author (of Geo-Technical report)

Jean-Claude Parise, 121 Place Vanier, Apt. #16, Val d'Or, Quebec J9P 2R1

• .r-MS

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

•Other (MaX

Mi n)Geological l ""/

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Expenditures (excludes power stripping)Typ* of Work Performed

Days per Claim

Atfldflf{

S^-\Jjf

]r\ i O

Day* per Claim

Da y t per Claim

—————— p-Clv I

Performed on Ciaim(s) ;\

MiiiiMCaic uianon of Expenditure Days Credits

Total Expenditures

S •s- 15

Total Davs Credits

s

Instructions Total Days Credits may be apportioned at the claim holders cÔ'ce. Enter number of days credits per claim selected in columns at right.

Date , Recordcd Holder or Agent (Signaiure)

CV.1

L

L

Certification Verifying Report of Work ty~ vCl— O.-^LtA ,

Mining ClaimPrefix

"- :.. - . V' ,\

fi--

t

EtV^ IS

^NDS 'i

Number

SEE

-ATTACHED-

SHEET

flfiXIMUM 2.

fiGfypMSlC.

^r^TJ^KI "i

THIS S6C

EDi——....89 j ivy

ECTIONf l-jit

Expend. Days C'.

QJZQA i.

i^flfijvr)ZZ"/o*^

P

L,. /.' v \~

S

'

t

i t•' i

4

For Office UwOnlyTotal Days Cr. Dale Recorded . Recorded 1 1 V/ L/ /P Q

rtL/ Date Approvecfas Recorded

Mining ClaimPrefix

m1909

Number

SECORD

MAY 6 4 i!

•i it --

Expend. Days Cr.

—— ...—

P"" '

89

— j ''c;, tlotfll number o* mining claims covered by this 60 report of work.

MnnlÛdffiBranch Director

( } Z^f i^vJ-thereby certify that 1 have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work

or witnessed same during and/or after its completion and t'lc annexed report is true.

Narrte end Postal Address of

Jean-Claude PPers

ajiOn Certi

i se,Tying

121. Place Van i LÂpJL.J fi Val rj'Or Quebec J9P 2R1Date Certified ' Certified by (Signature) /J?

K iffj&a-n^ cÔf*--**-*- r**A*"'*

CLAIMS

923356

923357

92335B

923359

923360

923361

'923330

923331

923332

923333

923334

923335

923336

923337

923338

923339

923340

923341

923342

923343

923344

923345

923346

923347

LIST OF MINING CLAIMS TRAVERSED ON MONTVAL RESOURCES LTD

PROPERTY IN WALLS TOWNSHIP.

CLAIMS

923348

923349

923350

.923351

^ 923322

723323

923324

.923325*

-923373

923374

923375

x-923376

-9232O4

923205

923206

7232O7j

92320C !

v 721209 .'

- 923236

923237

923238

9"2:323'-7

923240

723241 y

CLAIMS*

923242

916724 l

916725

916726

.916727

.916730

916731

916732

916733

916734

916735

916736

o T A L. - O

MAY 4 ]P3,0

Ministry ofNorthern Developmentand Mines

Ontario

Geophysical-Geologlcal-Geochemical Technical Data Statement

File..

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

I

Type of Survey(s) Magnometer, Max-MJn, Electromagnetic (U.L.F.)

Township or Area Walls Township-^—————ClaimHolder(s) Golden Trio Minerals Ltd.

c/o 27 Queen Street East, Suite #402 Toronto, Ontario MbC 'dm———————Survey Company B.M. Explorations Inc.________________Author of Report Jean-Claude Parise______^^____

Address of Author 121 Place Vanier, Apt. #6. Val d'Or. Que Covering Dates of Survey 5/12/88 - 22/12/88____________

(linecutting to office)

Total Miles of Line Cut 43.18_______________________

SPECIAL PROVISIONSCREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

Geophysical

-Electromagnetic— Mapnefnmeter...,, .

— Rnî^nr'f'c-Othpr( Max-Mi n)Gpnlngiral

Hcnrhpmiral.

DAYS per claim

4020

20

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer Electromagnetic Radiometric(enter days per claim)

HATR- 10/FEB/89 SIGNATURE:—r

rt iAuthor of Report or Agent

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)

SEE

.ATTACHED.

SHEET

TOTAL CLAIMS-

837 (85/12)

IND

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SURVEYS If

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SELF POTENTIAL

Instrument———————————————————————————————————————— Range.Survey Method -————————^^—————.^——-————-——^^——.——————.-—

Corrections made.

RADIOMETRICInstrument.

Values measuredEnergy windows (levels)———————.—^-————^—.—————.—-—..—.^—^^—.—.

Height of instrument___________________________Background Count. Size of detector-———————————.-——^^———-^^———.—————.——..Ôverburden -————————.—————-——^^——.—.—-^——...^——————.^—————

(type, depth - include outcrop map)

OTHERS {SEISMIC, DRILL WELL LOGGING ETC.) Type of survey____————————————————————Instrument ——————————————^—^—^——Accuracy_______________^____________

Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS

Type of survey(s)———

Instrument(s) —————(specify for each type of survey)

Accuracy——————^—————————.(specify for each type of survey)

Aircraft used——————^————-——.——^^—-..-—————————

Sensor altitude-Navigation and flight path recovery method.

Aircraft altitude______________________________Line Sparing Miles flown over total area________________________Over claims only.

i •"•s

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.

Total Number of Samples. Type of Sample.

(Nature of Material)

Average Sample Weight——————— Method of Collection————————

Soil Horizon Sampled. Horizon Development. Sample Depth———— Terrain————————

Drainage Development——————————— Estimated Range of Overburden Thickness.

ANALYTICAL METHODSValues expressed in: per cent D

p. p. m. Dp. p. b. D

Cu, Pb, Zn, Ni, Co, Ag, Mo, As.-(circle)

Others ___________________——————Field Analysis

Extraction Method. Analytical Method- Reagents Used——

Field Laboratory AnalysisNo. ___________

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

Mesh size of fraction used for analysis ————

Extraction Method. Analytical Method - Reagents Used——

Commercial Laboratory (- Name of Laboratory— Extraction Method-— Analytical Method —— Reagents Used —^———

.tests)

.tests)

-tests)

GeneraL General.

C L. A I M G

923356

923358

923359

923360

923361. 923330"

92333:1. -

923332

923333

923334

923335

923336

923337 '

92333;:;

923339

923340

923341 -

923342

923343

923344

923345

923346

923347

NING CLAIMS'VAL RESOURCES LTD

(ALLS TOWNSHIP.

CJ-AJMJ3

923348 '

923349,

923350 .

923351 .

923322 .

923323 -

923324 -

O ' ;.t 'i/ ' :x '2 i:r -

923373 -

923374

923375

923376 -

9232O4

923205

923206.

9^3207'

923208 '

923209

923236

923237 -

923238

9"23239

923240', --t , -j /| ,,

/ ..: . -..' ..:, *-r .1.

.

CLAIMS*

923242 .

916724 '

9J.672S .

916726

9 1 6727 .

916730 .

916731 '

916732 '

916733-

916734 -

916735

916736 -

ntario

Ministry ofNorthern Developmentand Mines

Ministere du DeVeloppement du Nord et des MinesAugust 7, 1989

Mining Lands Section 880 Bay Street, 3rd Floor Toronto, Ontario M5S 1Z8

Telephone: (416) 965-4888

Your File: W8906-244 Our File: 2.12448

Mining RecorderMinistry of Northern Development and Mines60 Wilson AvenueTimmins, Ontario 'P4N 2S7

Dear Sir:

Re: Notice of Intent dated July 7, 1989 Geophysical (Electromagnetic, Magnetometer and HEM) Survey submitted on Mining Claims P 923357 et al in Walls Township.

The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.

Please inform the recorded holder of these mining claims and so indicate on your records.

Yours^since/ely,

J W/R. Cowbf Provincial Manager, Mining Landsl Mines l Minerals Division

W/A'^C; GEOLOGICAL SURVEYt * - i -. ,- '-1 i 1 * -' c? r* 11 r™ o[i Ait)ba.'.)l'v ; (;-.r.! l FILto

OFFICE

/J l IR 10 1989

RECEIVED

RM:eb Enclosure

cc: Mr. G.H. FergusonMining and Lands Commissioner Toronto, Ontario

Golden Trio Minerals Ltd. Suite-402-27 Queen Street E. Toronto, Ontario M5C 2M6

Jean-Claude Pan'se 121 Place Vanier Apt. #6Val D'or, Quebec J9P 2R1

Resident Geologist Timmins, Ontario

Ministry ofNorthern Developmentand Minos

Technical Assessment Work Credits

OntarioDate

July 7, 1989Mlnlni Work!

TO*

2.12448Recorded Report of

U6-244

Recorded Holder

GOLDEN TRIO MINERALS LIMITEDTownship or Area

WALLS TOWNSHIP.Type of turvey and number of

Assessment day* credit per claim Mining CUImt Assessed

Geophysical

Electromagnetic.

Magnetometer.

Radiometric

Induced polarization.

HEM 13

.dayi

.days

.days

.days

-days

Section 77 (19) See "Mining Claims Assessed" column

Geological ———————————————————days

Geochemical _________________days

P '923357 to 359 Incl. 923332 to 336 1ncl. 923339 to 343 1ncl. 923348 to 350 1ncl. 923323 to 325 incl. 923207-208 923236 923238-239

Mondays Q

Special provision Gfl

Airborne D

Ground

D Credits have been reduced because of partial coverage of claims.

f~l Credits have been reduced because of corrections l lo work dales and figures of applicant.

Special credits under section 77 (16) for the following mining claims

No credit! have been allowed for the following mining dalms

rio l sufficiently covered tay the turvey Q Insufficient technical data filed

The Mining Recorder may reduce (he above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical -60; Geologoe*! - 40; Geochemical - 40; Section 77(19) -60.

Ministry o)Northern Developmentend Mines

Technical Assessment Work Credits

Ontario Oil*

July 7, 1989

File

2.12448wJTrl00 "**0"'*'11 Report ot

foS9b'6-244

Recorded Holder

Township or AreaGOLDEN TRIO MINERALS LIMITED

WALLS TOWNSHIP.Type of survey and number of

Assessment days credit per claim Mining Claims AsMtxd

Geophysical

Electromagnetic.

Magnetometer.

Radiometric ._

Induced polarization .

Other———--———

-dayj

.days

.days

-days

.days

Section 77 (19) See "Mining Claims Assessed" column

P 923356 to 923330 to 923322 to 923373 to 923204 to 923236 to 916724 to

"916730 to

361 Incl.351 1ncl.325 1ncl.376 incl.209 1ncl.242 Incl.727 1ncl.736 1ncl.

Geochemical. .days

Man days [3

Special provision M

Airborne Q

Ground C3.

Q Credits have been reduced because of partialcoverage of claims,

i _j Q) Credits have been reduced because of corrections j to work dates and figures of applicant.

Special credits under section 77 (16) (or the following mining claims

No crediti have been allowed for the following mining claims

not sufficiently covered by the survey Q insufficient technical dal* filed

The Mining Recorder may reduce the above credits if necesury in order that ih* total number ot approved assessment tfoyt recorded on each claim does not exceed the maximum allowed as follows: Geophysical -80; Geologocal. 40; Geochemical - 40; Section 77(19}-GO.

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