Il•4I003SE0001 MARTEL 10A1 MARTEL 010

r

REPORT OF

t

MISSBIAIBI MAGNETITE FORJ-IATIOII

by V. R. Venn

November lith, 1959

** ^-"rf*-WRf 15

A J. d os* A

KTSSINAIRI MAGNETITE

Location and Accessibility

; The Missinaibi magnetite formation consists of 39 claims,

No's S109133-152, S109657-659, S109671-673, located in the northwest corner of

the township of Lang.

The property is more accessible by air, however it may be

approached by boat or canoe from Missinaibi through Dog Lake and Crooked Lake

into Baltic Bay on Missinaibi Lake.

Topography

The general terrain is very rough, consisting of hills rising

300' 500' above Missinaibi Lake. This is typical of the topography on the

property itself, as the iron formation is located on the top of a high hill.

The overburden on the property is not deep except in one

location at D.D.H. #2; here the overburden consisted of high hills of sand which

'( form gullies and ravines. Drilling proved the sand to be about 65' thick.

The topography in this area probably represents glacial outwash.

History of.. Work

The Missinaibi iron formation is not an original discovery by

Algoma Ore Properties. The property was originally staked 15 - 20 years previously,

as old staking was seen on the property.

Algoraa Ore Properties, while Hying an airborne magnetometer

over a block of ground in the Missinaibi Lake area during the fall of 1958,

discovered the anomaly.

On January 15th, 1959? a survey party headed by M. Carter entered

upon the ground, intent or. performing a reconnaissance dip needle survey and

staking if necessary.

While doing the dip needle survey, two iron formations were found.

One was a typical Lake Supei ior type banded iron formation, the other was a high

gradv? rnagnet.ite~illTS3ni.te ore. It was to the latter that the company's interest

j; - was attracted and the following work done.

S SI-o rfC-

iV

A system of base lines and x-3.incs vrere cut as shown on the

accompanying maps 0 A magnetometer and partial electro-magnetic survey were

"conducted on the property.

The result outlined a magnetic body 9000' long and 250' wide

-at its widest point.

V Later in the winter of 1959 four diamond drill holes were

drilled on the property. . ".-,. - In the spring of 1959 a party headed by V. R. Venn again

^entered the property to complete the geology and re-run the magnetometer survey

at 25' intervals using 28,600 gamma magnet. The claims were alro tagged at this

/time.

Regional Ggolojy

-; : The ore formation itself appears to consist of a gabbroic ore

bearing rock (Hornblend gneiss) lying concordantly between a series of schists

gneisses. The formation is approximately 9000" long, strikes N.30 VI. and dips

:80~850H.

It i s bounded on the east by schisted greenstones and on the

west by granite gneiss (meta-sedimentary). Further to the west the granite

.gneiss is again boused by a formation similar to the ore formation. Some

anomalous magnetics are associated with it.

The local? is cut by a systam of diabase end granite dikes.

Detail, Goolor-y

Hornblende gneiss - (Gabbro, hornblende gneiss)

This rock is the host rock of the magnetite ore. The rock is

essentially dark green in colour, containing large euhedral crystals of hornblende,

surrounding in an augen type structure, elliptical pods of felsitic tutorial

believed to consist of plagi.-xan feldspar and some quartz. The hornblende crystals

vary in length from 1/8 to l /r inches.

In many places where the silica and the feldspar in the

.hornblende gneiss are more plentiful the rock tpkes on a dioritic appearance.

This was also mapped as hornblende gneiss as re was thought to be a phase of it,

SSM- 586-

- 3 --

If:

m

There arc places where the horj':b.lenc'e bcconcf. very fine (;ra ined

.and highly ru-h'ud.cd, excluding trie quart//. ':r;d fej.cL-r-fia-, In ;?uch Jnr.terj'V::-; the

ro: i.ra:-:

. The hornVO.c.-nde gneiGts bcco:.';-:; very imvrov.- to the north arid

south t, few outer opt.- j n^s arc to be neon but at 5? ovJdent th-.it the forrriLio.'.

becomes 'j.ni-crk^idoJ with the r;r:-:.:nto {;ncJiT nad hor;:Vu er.de t;r:hi::l..j or. t':ie ve.;t

and east a c- you prccoou nort':'.:t:ol- or r.outl'iec.r. b. This diifc;rj;.-.,l:'o;i j. r- r,;;b:'t-.-.*!t1..:.toi

by 'D.D.H. j'O .

Hornble

To t?!o c'.r;i. of the ^

.vide formation of r-c:dn.c'.J i- r c JM;-'!,;.!!!^

essentially of hornblcr-:-; ,TI.O'':' .'.r. Lul-

schists also exist.

The gi-rr.c-i. }-...;r:i-0.r..':-l;

body in that they were i,o ! .'-d '-. Tc.-.^v

gneiss schist contact.

.vd j.':cc: ( i. to .It ir,

Tin.: roc!;;- o t- 1. i:-, fo: . . i.' -;i covl/

;v ' ID b,-; r.-; ]- : '.cO t:i t ; .-- ; o:

Granite Gneiss

To the west of t;:;; r.-d./:..-;-. '.- v fer,

These rocks appeared to have been c:""f,': 1 ; .;. ; . '

' novr comprise various types of gneissv:. \ -:^j': , . ':. :

Pink orthoclase feldspar is prevalent, h. :."!^f;.- ,:

schist interbanded with the granite gneJ -',

There is, at a point whtro ':;: d;.-

#8109144} exposed a band of eliptically shrpc/. .^ r :v

banded with the granite gneiss. These structure, -,::

about 300' west of the midcD.e of the east boundc - f.

an old conglomerate bed.

ior^j v-rosses Claiti

material inter-

; .-.on on Claim S109150,

ray possibly reprec-ent

C

Dikes

There have been at least two and possibly three periods of

diabase intrusion:-

SSM-580-

a. On the property vt+s found a pyston of dikes that strike at O t-i*{ 7v ^I'v-, S

-' JI.H, and if projected indicate a rhombic block or faiOt patt :^aV^t';':S'^l \^ !

: The diaboi-e is fro- 10 ! - 50' thick and dip? vertically. ; ; , ;:'^' '' ^^''^ :

b. One of the dikes in the net j UT. t rv:ir;ti or.od co.t:u'.inP JAS.:~J ' phenocrysts J; '-; ;'.'- '. .'" .-- - -' .'.'v '-' ""';""--"'',::::":-^' ;' of plagioclase feldspar. This was thought to he a second pellet, of .,'." .

c. One othor d:'Ik e -/as noted on the property w;.-, oh might best.be . , :

classified as Iw.iprophyr. It occj;-s on line 32+00 S-30' west. The /i i

dike cut:; through the gaUo-"~ 6..oiss but does not appear to be cutting

through the high ^rudr r-^-e zone* This outcrop was not revisited . .

and tiie i K-.cr.'i^'.f-;' of '- -3 structure ai'e still unknown.

In the- e-;;u,r?jL section of the ore body i.e. 0*00-20+00 N. the ore is

badly cut by vride diabase dikes. The dikes make the ore literally

iiiij/or - ,.r,io for future work.

Granite dikes -' -

On the property are various granite and granite pegmatite dikes.

These appear to be later than the ore formation. Many of these dikes seemed to be -

lacking .in quartz but not enough so to be classified as syenite. ' !

- Syenite

-On the southern boundary of Claim //S109675 there is interbedded

with the greenstone, outcrops of bands of syenite. The rock was noted in mapping,

but was not intensely explored. The syenite is pink to buff in colour and is medium

to fine grained. -- . ' . . . : . .r " * . - - '*

- - . -Ore zone .. . . . '.

'- - - The tiain ore zone is situated between lines Z&0?:. and z'-"~'y:t 5

and is located along the footwall, of the gabbro. It is 250' wide at its widest

point, dipping 85O to the southwest (see geology map).

There are three bands of high grade ore located within the main

zone. Between these high grade bands are zones of ore which consist of magnetite

disseminated with the gabbro. As1 one proceeds further west magnetite mineralization

in the gabbro is non-existent.

SSM- 586-

'''

C

i '.: ' . The zone of ore along the footwall is about 40' wide and the

second band to the vest of this is about 80' wide. Both bands run about 35#

.sol. iron (see drill section 23+00 S.). . .. - . . .:.

i

Faulting

::: No Taulting vras seen on the property. However, there is a fault indicated in the magnetics in the area between 16+00 S. and 20+00 S. The

displacement would be about 350' - 400'. l ." " ' ".

Folding - - :. - . ~

E..' - .One largo fold is to be seen on the property. This is located

in the main ore zone and causes the ore to be thickened in this area (see geology

map). A small drag fold shows that there is some W - SE movement. This also

correlates with the rhombic pattern of the dikes on the property (see sketch on Page 5b following).

P M r (x' C O O Ol'*-' O kM

ICO

0

0

.' ' - - Genesis - -

||^; . There has net been enough work done to determine the exact

ffv -origin of the ore. However, enough criteria have been seen in the field to

?1r suggest some possibilities.ySsfv,"''^jjv; Listed below are some criteria indicating magmatic origin

'-" and either intrusion or extrusion:-"^'\ '' ~*

x " Intrusion

^: . (a) Large textural changes in the gabbro indicate magmatic origin,

' i * (b) Other than its slight gneissic appearance the rock is essentially

; massive, lacking any stratification that would indicate sedimentary

origin.

(c) Some small sills of gabbro were found in the granite indicating

possible intrusive origin.

Extrusion

(a) There is no evidence of cross-cutting relationships. If the gabbro

had been intruded, there should be more material from the gabbro

(C in the surrounding formations in the form of small dikes and sills.

(b) The fact that the ore is situated against the footuall of the

gabbro formation would possibly indicate that the gabbro was

extruded as a sill and the magnetite segregated out as a residual

liquid. This would account for the ore being located within the

formation as it is. It would also give it a syngenetic origi.n.

The granite would be deposited as a sediment and would necessarily

be younger than the ore. Tilting of the beds would occur later,

(see sketch next page).

Geophysics

Magnetics

A dip needle survey was conducted, previous to a magnetometer

survey. The dip need]e outlined the magnetics very well, however, because of lack

of expression along the contacts of the ore aone, a magnetometer survey was run

at 50" intervals and later at 25' intervals.

IDEALIZED SECTIONS

'm

GADBRO

SRJL

~ SEDIMENTS ~ ~" T-, L5TER-ALTERED TO GTRAFTlTE GNEISS.

GA9DRO

f * ' : - ,. . . - , *' ^

t '.' \ '',- - ' *,.' v* '. /r,. - t

* ""-7 V "-V-. 'l-

. , t * - v - -. .1 t J-~.

xs. .y-..v..

.; . tv - . v1 v' ' ,- K .'.. \ llk-' v *. ^^^T"^^)! SS E.M l NAT E p

ORE

GARNET HORNOnLENO GNEISS

IDEALIZED VERTICAL SECTION SHOWING GABBRO AS A SILL DEPOSITED ON

NOnNDLEMD SCHIST SEDIMENT IS THEN DEPOSITED ON TOP OF 6ADBRO.

c;

GRAfJIIlZED SEDIMEUTS

DISSEMINATED__ORE

DlSSEUINATEi' ORE ORE^

" QBE,GARf.'Et

VERTICAL SECTION SHO.VING TILTIHG O? DEDS

'it. f. -4'.-SSM-5bo-

SCALE l" ' ICO'

Electromagnetics

A partial electromagnetic survey vas started on the northern

section of the ore zone (20+OON - 444OON) . A conductive body is shown by the

crossovers on the map. . , . ,. . . . .' " '

It would appear that the crossovers indicate the contact

between tho gabbro host rock (ore bearing) and the country rock.- - ' - '

Correlation of Magnetics and

The geology along the strike of the ore zone correlates very well with the magnetometer results. On the southv;est side of the southern

section of the ore zone •' he ore is disseminated and there is no definite contact between the Hbd gneiss and the disseminated magnetite. Here the 20,000 gamma

line appears to represent the boundary of the ore on the west side.

^ In the section of the ore zone between 0*00 and 20+0011, the

magnetic trend is very badly broken. The geology shows that these breaks are

caused for the most part by diabase dikes, some of which were found to be at least Jy

'f 40 ' wide. 'The area between 20^003. and 16-) OOS, has no high magnetic

expression. It is thought that this might well be another diabase dike or a fault

zone. The broken topography in the area indicates some disturbance . (see

following sketch). :

C

600 CO0

— TOO ELEV.

COO CLfV.

ALGOMA ORE PROPERTPS LIMITED

MISSINAIDI MAGNETITE

DRILL SECTION

CHAI M AGE 12 -J- 00 a ^SSM

SCALE l" * 60* MARCH 23, TOO- 5W

li&f'* B?-.- --

C

o --—....

600

CO"

CO0

40*

l&.oo3. BO

i®r^ BO. IG*S. GO -2.30

CLEV.

* j^ wy\rÔ3 4i.T

COO' ELEV.

ALGOMA OH2 PROf-'irnVKiO LIMITKD

DRILL SECVION

CHAI WAGE S2-5-OON- A' ^}5 S 6

SCALE l" * 00* ODD

-e-

. Magnetic Zones

Zones l and 2 have been accounted for in the main body of

this report (see claim map with zones marked).

Zone 3 ~ This zone consists of a highly folded formation of banded magnetite.

|A - . Dip needle work and some geological mapping were done on this zone.l*- : ' : -'|r . . The only magnetite of significance is a band 2' wide of about Iffy material. - ^ . Zone 4- - This zone is unaccounted for.f S; -" - -W( Zone 5 - This zone is unaccounted for. It occurs close to a granite greenstonelv contact. .

Zone 6 - This zone is unaccounted for. It occurs on a very high hill in the

hornblende schist. : ~

Zone 7 - This zone is located in a hornblende gneiss formation similar to the

main zones l and 2, It is caused by disseminated magnetite and is about

5' - 10' wide. ' - '

Sampling

A^,-' A. bulk sample weighing 350 pounds was removed from the property for assaying and mill tests. The sample was taken from lino 32-K)OS-20'U.

Conclusions

The oaly section of ore having a minable width lies between

20+003. and 34+OOS. The ore, located as it is on a high hill, gives rise to an

excellent setting for open pit operations. However, the limited tonnage does

not lend itself to this type of operation and an underground operation would probably be more fear.ible.

A. rough estimate is given below. The final figure is a composite one, in that it is derived from averaging the ore limits as bounded by the 30,000

gamma and 20,000 gar::na magnetic survey lines. A more definite figure could be derived if more drilling had been done. -

r

;V SSM-

- 9 -

,i"^l .f-*f ; -'

r using 30,000 line as the ore limitx length , ~, .

ffytont foot

10

b . 79.0 xiflK) x i s 12j^5 tonsAert , foot .

25,373 E 12,687 tonsAert. foot

- using 20,000 line as ore limit a. 2025 x 99.6 x l .

b. 2025 x 96. A x l - T^Q J-

.??:???.. t . s 19,895.0 tons/vert, footavc.

X.Averaging the 20,000 and 30,000 are limits -

19,895 x 12,687 - , , ^ , , , ~ , -^——p——'—— - 16,291 tons/vert, foot

If mined to a depth of 3000' the approxiuate total tonnage v/ould be 16,000,000

tons of ore assaying approximately 35^ sol. iron.

V. R. Venn.

OFF SCALE

3000

8000 If

looo ^f

ZERO

w.——

oKea o ^ o

ALGOMA ORE PROPERTIES LIMITED

MISSINAIBI MAGNETITE DRILL SECTION

CHAIN AGE 26 * 00 S.SHOWING RELATION Or MAC-.\'liT!CS (GAMMAS) TO DniLL SSCTIOMS

SCALE l" s DO" L f"* /CO'

eo0 — -

60 0

20'

1 SOL F E

2 SOL. FE

3 SOL. FE.

3581

3? 48

35.62

ALGOMA ORE PROPERTIES LIMITED

MISSINAIBI MAGNETITE

DRILL SECTION

CHAI WAGE 26 + 00 SSSM-586 -

SCALE l" ' CO' MARCH w, isr.9

ALGOMA ORE PROPERTIES LIMITEDuxpLon.vnon DEPARTMENT

DIAMOND. DRILL HOLE KO. l PROPERTY

LOCATION OF COLLAR ChtlilClgO 32 +00 K. B.L. "B"

AZIMUTH AT coLL/vn. 9QO Eiot of HasD Linoon0

DIP AT COLLAR. 30

VERTICAL OECTION NO. 32 *00 li. LENGTH

l.'lg.

262 COKU CIZE-

IJGC. IN WIN. ZONE. LOGGED DY.A.ll.G.OOduirjAr.TKD. JlTT.9/59 15lT.il/59

^'•t rOOTAO!!

li'- o - 66-12.5

12,5-15

15-2121-22.5

22.5 - 23,:23.5-24

V ,H - 2525 - 50

50 - 6S65 - 71 71-74.5

74.5-7575 - 100

100 - 120

120 - 125

355 - 127

' "M5 - 150

MKKimcKI

Overburden :'coai'oo toxturod grcon-vhito nottlod JfJ-ilo euoloa - sees 1/2 - 2 jjachon lj

i

vhito i:cd. gr. granitoj not riuch qti eyccitichorribloiulo gnoiso

pxLo pin?: to Miiito pyetiitic gran.

hoynblondo 'gnoica

horablciiclo gn'^icohorijblondo gnoisn - \rcoyii?3 v-opD/iCo: by \i3iito foldn;:?!' ixi tliiji brjido, loi

27.5 - l"iT 3-ncl). ground qtz.

boivblor.do gnoir-fi ~ eor.vr.ov gi*.boi';:blcrdo gur-lcs - 50/1 folclopntMo

hor^blondo g^oiriO

hwiiblciido gnolus \ritli i.iu*o^ulc.r D.oi cor.D cpic'oto - rich Icycrs 96-93 - raiuly vlxito rycVfltoilm grated hon\blcj3Ao - opJO.r/oo ocpoaailxly rojxrcneMt.o altered dylic-rxLi f oD.da j-iit! lie Iryc.ir n .v'lito tyc^d-fcio Hiro.vi-fco - r-lr.jv frcodir;n:cjln^ttd ryj-.ltO| cry 2-5,^.

R

hovi:"?3,i":;!;a t; r^c;j, ivUior folds". a? -

pjii': r-yctiito voljilotfj

'

MIIMJNO

*

9C3,

brr.io c; liorrC;

cy fold

hiit.or

qt::. J

cVlroc.'

TO

-

LCiKlO

ipatldc

:::i'

- f Ir.o 1 gair.0

Ree.

soar-i

. t,, i - re

AMALYOC3

asd

b ' , -' "*'

'

l T.

."ALGOMA; ORE PROPERTIES LIMITEDOEPAHTMtNT

DIAMOND DrtILL HOLE NO.yti'-l

PROPERTY

CONTINUED

Kxg.

,fSv*r

Sfe '^ - ' '|: 150- 151fe ; 151 - 156~i-'-\-

|;:i56 ~ 158'j: 158 - 159 f 159 - 160: 160 - 161

161 - 175

175 - 187187 - 193

193 - 197.197.5-20C

V-, 200-215. 5

215.5-219.219.5-221221 - 225

225 - 250 ^;f

- ' l *, V

/? - 262

ft526

S "^

DSCCHIPT1OH

syc^jito

hornblondo gnoiso - 10^ pgt. diosenl

grey hornbleudo - feldspar gnoics

dark green hornblondo gneiss

magnetite oro

nagnetito oro

hornblende gnoiss tind schist - varyi

CAMPLINO

rnoM

oations

33 tsxtbands at 161 - 162.5 j 166. 5-167. 5) lf/0.5 -

hornblondo gnoios

Kagt. oro - uniforn corapos. and text2-5/5 disson. py. - groanish hbd3. irgranito oj\d qt?,. stringers

5 hornblende gnoir.s

grey to piiik eye: \itic granite

dark groen to blp.cV. hornblende gnsis200 - 201.5 - gran.

5 mgt. ore

horiiblcndo gnoiss

iigt. oro - lover grade - 20;' feldspr.

laixcd g-ranitcj end hornblende gneiss.240-249 - donccr f . gr. hbdo schistsnalJ. rod gevnots2.^9-250 ~ hornblondo schist vith 5/-'slightly 3r.:iS5t laagiiatic

f. gr. hbdo sch. - scnttored garnets

Oro Ssctions -

145-150 oro151-156 10^ Kgt.159-161 oro107-193 oro215.5-219.5 oro 221 - 225 oro lovor gro.da - 20J5 fc

D.lf.&J^ .Uv *

. - blr.ouritie:

3 - non

bhic ro

rlth abi

-,gt. -

- sligi

.dspat-k

to

- foldiL71.5; J

sk, ned,} - tiinc

lal 2-45

)lnccc:.ci

yidp.nt

it3y nr

c zoaor

MIC.

path!-4# p

gn.r

P7.

t.

notic

-

S

i

ANALYSED

j

r.

.

*,

SM-~5o.

i

i

i

i

ii

i

it

ij

i

1

i |1

s

i

i

i\J

;

i

;

-

!

l1

11iii

i i

86i 31t ^ l- l

ii

l

1 l

^^P5 ;v "- ALGOMA ORE PROPERTIES LIMITED ;'J?fSlili|?r ''V:--'; . . ' : CXPLOBAYION DSPAHTMENT ' .. :. ."V/^fH^tf^S'

DIAMOND DJ5ILL HOLE NO. 2 PROPERTY MiOSinaibi Lako J ^.

LOCATION OF COLLAR 50' W. of Baso Line "D", o

AZIMUTH AT CCLLAH. 67 '

m- '. -*^iv- - -'

f?!--

1?S ! i e.r.'i04io-9i

CLEV. 775.9

DIP VO

VERTICAL SECTION NO. 12 +00 S. LENGTH 301 CORE SIZE. Ax

REC. IN M1N. 7.0NE. LO3GED DY. M.Carter CTAR7ED. 16/3/59 FINICHED. 19/3/59 j

;r.: -':5*;,'

/"~

W-

rooTAon

- 0 - 89

. 89 - 124

194-161.5

-

161.5-182

182 - 186

386-lS?i-

167& - 196

196 - 203

203 - 242.

242.5-301

DOXMIPTIKi

casing fine red sand

coarce textured hornblende gneiss

96-2" band fin3 textured hornblende g 97-3'i MB n H99-101"" " w ' n

ll8-n9!!IJ nun

nedixa textxired horjiblcnde gneiss

1^7-128 lOg Fe134.5-135:5 granite 136-139.5 1555 Fo 142 2" band fino textxivo diabase 3/1-150 15JS Fo 150-161.5 lOg Fo 157 3" band 35g Fo

lu'cnotite 35g

CAMM.WO

mott

QCiSSnnR

169 5" brjtid barren fino torctwcd bori^leiwO

finD tcxbxu'od licri\blo::do gneifjs cnall granite atrluserp at 183 end 1C4

j.-!agnotito 35g Fo

garnotifcroxyj hornblondo gixoies

fino tortured horiibloi'jio gnoico

^ diabaao 5g Fo

gnri!Dtiforoxm horjiblcudo gnoir-o

DIP TEST - 100' read 52O 200' rcr.d 53O

SSM-586-1

TO

(^'.rvxfi j

KCC.

i 1

AHALYuCU

lOg F(

lOg Fc5g F(

15g Fe

ii

*

t

1

i i

i

i

i1

1

1 ii

;

t

1 |

1

ALGOMA PROPERTIES LIMITEDEXPLORATION DEPARTMENT

C.P.-IMtO-tl

DIAMOND DRILL HOLE NO. 3 PROPERTY

LOCATION OF COLLAR 26 +00 S. on Baso Lino "B n CLEV.

AZIMUTH AT COLLAR. 9QO East of B.L. "B" ' .

DIP AT COLLAR. 30

VERTICAL SECTION NO. 26 +00 S LENGTH 231 CORE D!ZE. lx

REC. IN WIN. ZONE. LOGGED DY. STARTED. J.V H. FINIOHED.

J; rooTAcn

,.

0- 3.53.5 -3.73.7 - 8,58.5 - 1010 - 2S.5

26,5 - 32

32- 33f 33 - 40.:(^40.3-42

42-42.442,4-43.'

43.7 - 5858 - 58.558.5 - 7373-8787 r 89

89 - 91.591.5-93.593.5-95.595.5-9797 ~ 100100-104104 - 103103 ~ 122

( '22 - 1^0'S JO-150. 5

150.5-153153-153.5

DttCH^ON

casing

hornblende-chlorite schist

icagnetite

fino grained hornblende schist

garnetiferous hornblende gneiss -some nni'row bands of nassive itagnotitmagnetite

hornblends-chlorite schist

nagnotito

gi'anlte

uagnetito

granite

nagnotito

oj-iphlbolitc

tiagiiotito

gfiTDxirlferoiiD ouphibolito

hornblendo-chlorito schitit

garnotifcroxxs anpMbolito

fino gi*ainod hornblende schist

anpMbolito

fino grained hornblende schist

avipMbollto

chlorite- hornblende schist

gai-Aotiforo'.'.s gneiss .hornblende schist

gavnntlferous schist and gneiss

giirnotiferoxiD gnoics

ciLloritc-hornblendo tcJiint v '-'igai'notjfciroxio gnoisn

*A,. ?L,MO

mott

e

-51

TO

}Q w

,tc.

ANAUYCnO

352 F

152 F.

352 F

352 F,

)

-

1

i

)

135* fi

352 F.

352 F*

)

115,, 1 j

152 F!1

152 FJ

1

152 F(

102 F(

10," F(152 ^

152 K:

.

i

li

!

t l

ALGOMA ORE PROPERTIES LIMITEDo * . .. , . . EXPLOHATIOM DEPARTMENT

DIAMOND DRILL HOLE NO. 3 (continued) PROPERTY

LOCATION OF COLLAR '

AZIMUTH AT COLLAR.

DIP AT COLLAR.

VERTICAL SECTION NO. LENGTH

REC. IN W IN. ZONE. LOGGED BY. STARTED.

ELEV.

CORE S IZE.

FINISHED.

^•'.'''r.'- rooTAOit

i|;;^... . -..'^•'''•: ;^-

^158.5-164

164 -' 186 '186-189.5

189.5-197197-208.5 208.5-220220-222.5

222.5-.^; 223.5^ ^23.^-231

~^~

-

•: -'(,

. otxcnn

garnetiferous gneiss bscoioirg chloritic and schistose

magnetite - a few small bands of sck

chlorite-hornblcnde schist

magnetite-narrow schist bands

garnetiferous gneiss and schist

massive chlorite schist

garnetiferous schist

Kassive chlorite schist

garnetiferous schist

pnd of hole

DIP TESTS -- 100' - 40^ (uncorrec 200' - 40 (uncorrcc

DIP TEST - D.D.n. #2

300' - 48 (uncorrectoc

d CI Wl *m Ojj iji"

SAMPLING

not*

ot

'

:ted)tod)

5

,0 me.

ANALVCEO

ioj6 y355S li

35/S F20# Y

40/j^* *- *

Avera

i

ii

'

j

3

3

1& - 1*

t i l

1l

1

1

(.7*1 'or 205 '

i i

,

i

t i

'fi*?. . '

ALGOMA ORE PROPERTIES . LIMITEDKXPLORAYION DEPARTMENT

DIAMOND. DniLL HOLE NO. ^ PROPERTY ' .

LOCATION OF COLLAR 50' East of B. Ling B. 0 Change CLEV. 26 too S.

AZIMUTH AT COLLAtl. 9QO Vest of B.L.B.

DIP AT COLLAR- 30

VERTICAL SECTION NO. 26 too S. LENGTH 211 CORK SIZE. AX

HEC. IN WIN. ZONE. LOGGED DY. J.Y.H, CTARTED. FINIOHED.

v "'. - ** * * f POT AO 3"'"t- .

,y. :.

/, -'-"

'T. 0 -1303 - 25.5

.25.5-37

:37 - 33

38 ^.5

*2,5-A8

^. A8 - 51.5

.51.5 - 52

52-53

53 ~ 55.5

55.5-5S

58 - 60,5

60.5-105

87 - C3.5

92 - 9A

105 - 108

103 ~ 131

X53. ~ 1/.P.

U2 ~ U3#

v l/^ ~ 152

152 - 153

DSxmtmoM

-

casirg

riagnotlto

hornblende gn-aiBS

cchlst

enaloii

magxxotito

hornblende gntdns

uasaetito

chlorite hornblcxvio giioiss

cchlct

chlorito hoi*nblc::do gr.oiss

d-anlto

homUo^Jo enoinB

lost covo

Kanoivo cblorito d3 sscuiiiatcd iingnoti

chlorite diko

hornblcjdo gnoica

giiolpa

(poioo

gnoisa "a W* * *S *~' 5^ ^*

lo.'it covo

BM.1PL1HO

rr.on -

to

10

!

tc.

1

ANALYCE3

-

3555 Fi

10p Fi

20/ F(

3555 F(

555 R

303 F.

lOjb Fi

1555 F*

15* K

10-15S

5* Fc

302 Fc

103 Fc

.

t

i

:

i

Fc

iii

,

1

l

i

t

m -t.,^-&I&- ? V^r"

**B;VVIP"'.:

raS'-vv;-" ' ^ -li-v -IP:8C^

ALGOMA OVKS PROPERTIES" EXPLORATION DEPARTMENT

"DIAMOND DHILL KOLK NO. 4 (continued) PROPEIITYLOCATION OF COLLAR CLKV.

AZIMUTH AT COLLAR.

DIP AT COLLAR.

VERTICAL DECnON r.'O. LUNOTH

REG. IM HIM. ZONE. LOGGED DV. OTAnTIiO.'

COKU OIZK.

PINICHSD.

f|.V,rooTAOC

Hf: : '

.p-'l53 - 159

| 159-163

163 - 166

166-170.5

170.5-172

172 - 173

,~ 173 - 176 ^'176-179.5

179.5-102

182 - 1HA

1CA - 1C6

1C& - 190

190 - 192

192 - 19/v

19/f - 197

197 - 200

200 - 203

203 - 206

206 - 203

(. 2u3 ~ *̂

MBttHllKSI .

gnoics

(P31CO

gndipB

gnaiss

paoica

loot covo

ocblpt

t'AOlflS

{fAOlOD

fiUj.OO

gnolDD

gaoics

gi\3i03

CnQins

piair.o

enoioo

6113108

gnoios

gnoicE

Hol.Q Ricppsd

5 H v^

C/Jl^UtJO

raou

*

- TZ.

TO R3C.

'

MIALYCI81

102 F

202 r

102 F

152 r52 F

152 P

102 F

152 F

io;5 F

152 P

f (f V?/* *^

202 F

152 F(

52 Fc

152 Ft

52 Fc

102 Fc

)

j

3

il

)

)

)

1

)

l

l

)

,

j

i52 Fc, i

ii

C , ' '- i " i Q f* \

: C

j c.

lle

IDt-

*0-3.

1*

-?

enido*)

i oV'.

v/i \,

'- c :.o

-Q

(

r1

O

f:C T

S

TS

S?i,;

O

o

J O

C J3.

•^. --5

^

^f ? 5 fb

O

O

A

—y

f. i

O

-Cv/0

^ -±~ .J*

-3 J

) O

*

^

c^ 3" V

; O

-

—

, .-

*-' ''

To ^1

l ^7

0. ^

"7: -O

! -^ n

s*

-\- rJ

-5 r^

^A

-~ ^

M r-

o

11 i -O C

r-

;-J V.

1

8, M-(T.^• b z t* h7.ft ' ', 0

T ̂

1 ^i 7*"t- O.1

OfVOV

h t

•st•0|

-loc;

riL i -^L- . -

Vs

c, x1

xs'

S

"LI

oh

.rl

f*

^

^.

S

•H'cra

o

•s.-toe;

J"

//K"

S*/

os.

o?

.r//

.r.r

C?/'

fe'

t/

H -0-

ifew^te^'''^^^'''•?* jifrj? : \':'-'.'if''!,\:'ii:''..:'-"-. ' , "

SCALE 1 *2 MILES

T^'^% , :V\V'^1",1 •. '\v'.p;l

burtuct H iyhlb t\tl^^^fl;^::^ oround oil Lokes onditiiiif*ffi's*~

\)H.DSTBie

Scale 40 Cliaiiis

BRACKIN

t f

14

. ff n

410035E000I MARTEL 10A1

MARTEL

30

0-

OO

/O-A

)

fl LD

EN

UK

ffRQ

?

Scal

e; /

' -2

00'

UM

EX C

OR

POR

ATI

ON

LTD

.DR

AWN

BY-

B

Ea

iff16

r

H9 f

f 2

AK.E

^L

V

\~32

- W

-

41003S

ea00l

MA

RT

EL1

0AI

MA

RTE

L2

10

LAKE

PUP

R

Scal

e: /

" -

UM

EX C

OR

POR

ATI

ON

LTD

.DR

AWN

BY

DA

TE:

gY:

y M

it O

Sow

a H

a

l:;•c

&Jk

-:

i"V-*S

*^-

?fcr

?*V

32E

5**

ZO

N

I8JV

Iftf

LA

C

W

V—

I-'

^...

LJ^

", v *

- -

* *

. .

.'

j~~~

~ L —^^

^^ '

t *. -

t*

017*"

*t

. - -,

x-'-

- .

' '

' * J-

^**

-- r ^^y

-

..

J,,

-- -

-^Z

-^-j

** v

J-"A

v^p

*-**

*-z*

f :*J

^ ~

'z -V

://

** ~

- '

^ ~

*-^*

" ^

* i^

/.-v

V^'

-r -

V"*

- ~'9

L^'

•tf ^

LE G

EfVD

F

, ̂T

urf

; ^

~ IN

T.

o^ b. fi .

rtic^

**

w/*

k. r

t***

tt *

t

C?

) :

t T

I.r.

w rf

' ? i

4I003SE0001

MARTEL10A1

MARTEL

22

0

L/l If

E

i- -

'"S

*

Scal

e:

p r

UM

EX C

OR

POR

ATI

ON

LT

ttD

fWW

NB

Y;

6-X

* D

ATE

: S

**?

.' SU

RVE

YS)

8V:

DWG

. Mo,