Q Q SAUM-ALOOHA. HP. l PftOJMT (A. C. R.)

REPORT ON VJDRK DONE DuVJHC AUGUST - O. A. CHECKUH (PART l

BATCHEHAMl AREA. TWK3HI? PH

Mapping

Moore, in hie 1926 nap of the Batchevana area, groups certain interbanded sedimentary and volcanic rocke into the Batchewana Series, aa they could not be separated from one another* During the rail tra verse, those rocks along the track froa Rand to approx. 2 adles E of Batchewana were mapped aa sedimentary material, mainly on aecoxint of both fine and coarse banding which is well exposed in the railway rock cuts. A s this was all shown by Moore under one colour, green, but in continuation with an area of sedinentaries in yellow on the adjoining nap sheet (Kississagi Reserve and Ooulais River sheet) it was thought that some traverses should be run over the Batchewana area in order to attest to separate the larger lenses of sedimentary rocks at least, as had been dono by Moore in this other map sheet*

It was expected that approximately 2-3 days (excluding rainy weather) would suffice to cortplete any of these traverses except perhaps one to the S of Batchcwana. It was necessary to pack all requirements along, and the party of 2 r,et off on the first traverse N. froa near Rand towaidc Rig Pike like with a light tent, an axe, one blanket each, air photographs , mnpc, cook pots, and onouch rations to cover 3 days, as sonic rain conic \ *c expected to delay progress. It wac found, however, that much of the bush was difficult to got through, that excessive tiae was spent in divine r:w;iy ^i snooth, partly-liidc'.en outcrops and that the food carried (mainly rice find c-attac&l and other concentrates, to cave weight) wae really inadequate for tho energy-loss involved, so that the UJTI this traverse took wae extended by a full ("ay. In addition the rocks in many places arc weathered or altered and difficult to recognize a type. Koct of tho rockc wtre thought to be sedimentary material be cause of a clastic appearance or t clewi Gneissic character attributed to partial granitization of fi nely-bodded cedinento.

These rocks which wore thought to be sedimentary paragneisses are now thought to be metamorphosed lavas mostly of an acid nature. To wards the end of the northward log :nany intrusives of a granitic nature were observed, though quarts ittolf was not common and when seen was in small lences. Further N. a band of fine-grained basic (lib) gneiss was picked up, interbedded with light-coloured material (?bauic and acidic lavas), then a coarse basic gneiss. Near the lake ft very definite granite- gneiss was observed.

continued to the E. C1 r. tho southward leg of this traverse the rocks had much the fnme appearance as those found during the northward lop.. IVo bands of iron formation, each a few inches thick, were discovered, separated by about 9 ft. of overburden. These may represent a band of tho sane material 10 ft. wide. It was of apparently poor quality and no specimen was brought in.

*r':V ' f-'"

^?;, C*S ,T.

* "N

H , ' : ; - About ;thii period the- full report on thV Batchewana area \. beoaas available to sxs, and daring our reading of it ve oasis across ; . inforaation which causdd us to wonder whether tba x*)cks described above were, not in f act acid volcanics* Moore describe* these volcanic* as tending locally to have a definite banding' ecrtraoely like that of ; soae sedimentary rocks, and the constituent minerals are. sigllar to : arenaceous sediments such as arkose, fine-grained sanditone, quartaite, etc.' '-- - * " ' .. - ' ' - * ; . '' .

With this in ndnd, a second traverse was run to the H. from a point on the Batchewana River about one idle JB. of Batchewana station, From the start the topography was so rough and the bush so thick that by the end of the 2nd day very little progress had been aade, and out- . crops seen had been rather poor to map froau An old bush road was reached, along which a lot of outcrops had been cleared so that they were now washed clean. It was decided to follow the road while it went in our general direction and this road was surveyed in by pace and compass to the end, a* part of our traverse. Iron there the party struck across country to the tf.K., to a e l rone lineanent marked by a auch-beaverod waterway.

Air photographs ssemod to show a road which crossed the next ridge to a send -circular syetea of lakes just over the granite contact to the M., but no road could be found on the ground, the lino visible on tho air pnotograph bel ne tho end-to-ond channels of two streans draining opposite aides of the sane swasnp on the top of tho ridge. As wo at this tiao hod little food loft and could not have undertaken a further log to the N. without help fret* a road or track, wo returned to tha road and followed it all the way to the Batchewana River.

On this tmYteree the rocks roscabled thoec oocn on the first such trip, but with our new knowledge they were classified as acid vol- c&ttics. They continued all tho way to the end of the traverse which did not cross the granite contact. Two quartz veins were sewn and those were both sanplod. Other lonsoc and stringer*) of quarts were few and too small to be of value. The volcanics themselves chow local patches and spots of rust which are cauowj liy pyrite ppccke '.n tho rock when weathered, with chalcopyrite seen occasionally. One aone of very rusty rhyolite was sampled, as it showed much pyrite locally.

Tho cystem of olxJ locci"C roads in Twp. 26, Range Ib (PH) is quite extensive and it seened bet1*r to utilize these, recording all loc ations by pace and compass, than to try straight traverses through the bush. One of those roftcle wae used to get us quickly into tho aj^ea of mapped sediments in the H.V. part of Tvp. 25, Range lli (PI). Fron the end of this road ve were able to rfo traverse*? to chock the rocks in the area nnd alone the contact. The oedinente at this point arc quite well marked where exposed and eee.n to be slightly nore predominant than the lavas. The eranite contact ip fairly sharp with odgnatite formation Just to the S. No significant td ne rail cation was seen on this traverse although the lavas as before had specks of pyrite locally and there were a few

J

which were w*** **?,...; . . -t-,*; '~ 'V ' ''l^y-'--^^^M'V^:

, The -traversing party had cohsisted sp fair of O* Cnfroklin and J. Hough, but wben the .latter vat imobilited by continued poison-ivy v" ',; trouble it became necessity to utiliee B. Tyrrell*- 0. Ch4cklii, there^ '; f ore, walked the line. fro* 3atchcwaaa to Pangis on Angus\,2d^ partly to effectTyrrell withdrawal frcn the Pangis prospecting party, partly ;* ' to check the rooks along the truck, and also to visit the Hochefort brothera already, seen by Gr&hea and Ty/rell. These are two former pro spectors who live near the track at {Spruce Lake (A,C.R. Mile 71)*' The information gained from this latter conversation'will be incorporated . in later reports on both the Rochette and Roohefort properties, - .

, ~- " t' . - - ' *

From this track work SOUP modification of the rock type for 2 miles K of Batchewana was made. Also a small specimen of a rather at tractive porphyritic syenite dike was brought in. This nay have a matrix too soft for facing purposes, but if not it could be a highly decorative stone (also nay be useful for inside facing).

A long traverse vao j*ado to the S. of Batchewana, again util izing a lofting rood for some of the way* This took us to the S. of McColloufch and McOarry Lakes, and apparently across the contact between Moore's Batohowana Series, end lil s Kauain&e Series* There is, however, much low ground and swamp iu thic area, And while there is certainly plenty of diabasic material, f. characteristic of the Mamainse, the con tact is more likely to be a gradational one which we were not able to reeognLee. In tho Area of a long lake (running NK-SW) which is thought to be well within the Hamainse, chloritic schists and acidic lavas are found near each other.

At this point it uao intruded to carry the traverse through to the W about h miles to the granite contact N Si W of Dick Lake, but there was too much water and swamp intervening, and this leg would have served no useful purpone and mny havu wactod A lot of time. We therefore re turned alone 0 dua H* bearing and by the sane logging road as used earlier* This traverse use finished on September let which 6ny is included in this August report for convenience.

One eanple was taken during this traverse, from a large knob of white quarts, the boundaries of which on 3 tfides vere obscured by over burden. This was on the rldjje at the SK corner of MoCollough Lake.

The rocks seen so far in this Batchewana serlos area are, there fore nearly all acid volcanics which bfelonj to several different types* There are certainly a fow interbedded sediments, to bo distinguished by extremely fine banding In a horaojonoous mass, but many of the volcanics are gneissic and have tx-en injected by thin bands of mobile siliceous material which also gives euch rocks the appearance of having been finely banded. The injected Silica in such coaoe scon is not pyritiferous and these rocks generally show no rust colour whatsoever. It could be expected

y- ' \

night be. nor* easily eroded a**yVolcanics,, and there tay be relatively f ev band* of sediJBent* outcropping 'r !''- ;;'' in this region of the Batchewana Series became 6f this.' Also, b&aus* " of the difflfcult^.of distinction between thVaeiel Jayis anfc.^'iwaijiente, other1 roclrt than volcanics may have been wrongly typed* i^- , , .-

, Towards the NW part of the area mbch of the acid ikva tends' to : ; be finely gneissic, with mica foradng along the planes and often giving a brovnlBh colour to the rock as a whole. Some of thi* gneisaio naterial is stre&iqr where the biotite ie locally veil developed, but mineralisat ion is uncommon. Towards the SK the rocks seen to become progressively less gneiesic and nore massive, and the main type is a bluish, granular, even-grained (almost sacoharoidal) rock. which is very hard, '

' - .'' - " , . p - ' ' . Given Tjelow are soae of the different types of acid lava which

hare been seen in the field* - '' . --

(a) Dark, greyish, locally granular, micaceous^ vith adoaflattened along planes of gneissosity. '

(b) Pine-grained, siliceous, with cherty "squared" appear- anoo on the weathered surface*

(c) Greyish, micaceous, nodular} the nodules being snail portions of the rock vhich apparently have been hardened and have become more resistant to shearing* The nodules stand out on the weathered surface.

(d) Finely-gnoisBio, bluiah (but often with whitish weather ing), Granular, fine-grained, hard rock which on surface may show cross-cutting ribs of harder material which stand out.

(e) Maestve, bluish, very tough rock, mainly of quart* but with some feldspar, also a few specks of nica and with a microgranitic texture,

(f) Oreyish or dark, cryptocrystalline, rhyolitic, with almost a waxy lustre, very hard and breaking into splinters and sharp-edged fragments.

(g) Felsltes, slightly coarser, often pink or brown, and not RO splintery. (Seen particularly approx. l mile W alonf track from the A. C. R. bridge over the Batchewana River).

intruplvea are once af;aln fairly cowaon in this aroa, and are often extensive. In particular they are soon to font sharp outcrops, along the tops of many of tho ridges, and seen to be responsible for the resistance to erosion which causes the topography to be so rugged*

^

3js!i^

^fe:"

x^tfyi ^equate c^^ ',l-,'" iwli'-ftcwrad;.by^traviBrTlea,:-noi aiuch--haa--bjifn','added tO'thft'ca^|^pal: ^'^":: :^'i -;;^;':' , v '*:V 5-aappiUifi:pibture. The area has bften.aeen/howev^r^and it.is OQt felt; /;vi^;j1*; ;-

that in general it has Much proaiee froaiiA'proapeotpr'A pQint of vieW ,. ; V;*i V ' ; iher* l* little evidence of eheiring or' otixer structures' UfcUhi li* t ik k ' ' ; provide pasajigos for mineralizing fluids, The pyrite ia present

" amounta in wich of the rock,is evidently of ^riaary origin*

Prospecting' . . - * - !

Qrabam and Tyrrell spent 9 days prospecting in the Datchevana. area, from August 6 * 16th, During this tind the following work was dona t

(1) They prospected along the track both ways, paying particular attention to sections noted during,the railway traverse. .Several sanplea were taken*

(2) Several strong lin&anents which intersected therailway or ran close by were prospected* The strong lineament in which the Batchewana River runs was examined for 2\ olie s or so, but is too much filled with aanda and gravels in this area to be usefully prospected,

(3) They looked for iron foraation approx* \ mile X and ^ mile B of Batchewana, using thb dip needle, but they found no evidence of any iron in this area*

. (li) they prospected f root the power line SW to the granite contact.

They probpocUd in Lho general vicinity of the roads and the tr&neaiasion line.

,

:V:"'

SAULT-ALGCMA NO, l PROJECT '(A.C.RQ

REPORT ON WORK DONE DURING NOVEMBER I960 - O, A. CHECKLINE (PART 2)

QUINTET IAKES AREA. (Twp, 2^ and 26, Ranges 13 and 3J|) (QH, QI, PHf PI)

Prospecting was continued in this area until November ?th when the party (A. and P. Graham) portaged over,to Spruce Lake and caught the train to Sault Ste. Marie from there. Eight sanples were taken altogether in this area (SA 10h7 - ID^li) but these showed only "NIL" or "TRACE" values in gold. No other information on this area is available at this time as the prospectors are working in another area.

41N0INW92I0 63A.500E TRONSEN 020 FBASC"

'?-^/.' IsrSV.V' '' "- . ' .Nr "*' -'* VSfeiS* "iV/i'^'Vv'f'i V-'.jSi'Pl'*^,,},^ ••i " - '-- * t -** "'- -'5'.' ' '..'iX.jRHj: J •Jn/^Jtek^'Vf -|--t--r"-.--'*JJf*- ^m^tm^iJA^ R*40rai^ A ASsociAiya;: - ' / ; lv-^'v ','"iX,-'v.r.^-^ * ' ' - ' -l . J . ' J^k^ * *' ' -* v ' ; "*

- "w- .-'.;'-- --,? 1 "^

ASOMALT L * 7

(Also known aa A.O.P.'a AoauQy #12)

GEOLOGICAL REPORT

..Airbora* Bagnwtometer surrey, carried out a few years ago, a Magnetic anooalous are* 1.8 miles louth of Batohevana

St*tion on A.C.R,

' . This report oorers that area.

york Done ,

,, ! Line 12 * 00' S on anomaly L - 8 was extended UOOO* to the s^uth* Froa 36 *00' SandliO*00' S two lines, both E-W going and *ach 2000' long, were cut. These two lines were surveyed with E. M. and magnetometer.

The anomaly was also geologically mapped.

Geology

Only three outcrops were seen in the entire area, one on and two north of line 36 * 00' S. At 600' W outcrop of basic dyke was seen 50* north of the line and of acid lava about 30', also north of the line.

At 1030' west on a bush road, outcrop of acid lava was found.

Overburden

Heavy overburden covers the area underlain by anomaly L - 7.

The central part of the western portion is mainly covered by swamp and beaver ponds. The southeast corner is flat and swampy. The remaining area is covered by large boulders.

All attempts to reach bedrock by digging were in vain.

Recoaaendation

No conclusion concerning deposits of economical interest in this area can be given due to lack of outcrops.

The results from the ground survey with magnetometer and E. M* are therefore the only sources for geological information on Area L - 7*

Batchewana Station - A.O.K. October 29, 1?62, Bakon 0. Lien.

Xnoauly VJ2^ 1.8" of- BalchawaotSUtlon)-

Work

Vl;?v '' ' .',V, Oround folloiJr :up with .Mgnetoneter (Model Sharpe X-2) and eleetro- ai^netoatetVr (Model 31^-200), vas carried out on a magnetic - anonaljr l, Q ~ south of JJalohavana Station qn the J.C.H.! ' \ - : '

area vat^ also geologically Mapped. ' * ;, , '\

Line 1200 feet east on nooaly i-8 vaa extended UXX) feet to the - south* Frcw 3600 feet south and 1*000' feet eouth on that line two east-wfflt trending linea, *ach 2000 '/eat long were cut; Iheae two linea were iuryayed ;, vi.th K.M, and GAgnetometer. For the K.N., survey a Sharpe SB-200 unit vaa uaed - and for the wag survey a Sharpe A-2 magnetoneter.

'- " V . '"" ' '' ' ' V .- - . " ' ' --v - - * .

Qeology ; ' ,-

Only three outcrops wero aeen in the entire area, one on and two north ' of line 3600 feet -south. At 600 feet vent, outcrop of basic dyke wa0 aeen 50 feet north of the line and of acid lava about 30 feet, alao north of the line.' At 1030 feet voet, on a bush. road, outcrop of acid lava waa found.

Over burden ' *

Keavy overDurden covers the areii underlain by Anomaly I/-7* The central part of the western portion is mainly covwred by swamp and beaver ponds. The southeast corner is .flat and swampy. The rwwirdnf eraa i e covered by large bould ers.

All attempts to reach bedrock by

Recommendation

were in vain.

iJo conclusion concerning deposits of economical interest in this area dan be given du* to lock of outcrops.

The results from the ground ourvey with magnetometer and JS.ft. are, therefore, the only source for geological information on area I/-7.

Batohawana Station A.C.K., November 2,

Hakon 0. lien.

^M^! .'';^'^:^^-^^•^j^/^r^v:/*;:,;

FRAHC. R. JOUBIN 6 ASSOCIATES

QROUHD INVESTIQAnON REPORT

ABEA

SUMMARY and COKOUJSIORSt

Two linea, UOO* apart, were cut due E-W to cross the site of an aerooagnetio anomaly known ae A.O.P. #12* The anonaly vas located on each line and gave a UOOO ganaae peak indication on the northerly line* It is still open, both to the north and south.

No apparent conduction has been revealed by the electrcmftcnetio survey.

The source of the magnetic ancnaly is either a basic intrusive or weak iron formation. The geophysical data does not foster further interest in this area.

Respectfully submitted,

(signed) Harold 0. Seigel, P. Eng,,

'^*;,W -v*- i-V . j.:. j*, v -.. -

Toronto, Ontario, November 15, 1962,

OCT 21 M65

RE8IDEMT GEOLOOISt8AUIT BTE. MAWf

NOT TO BE REMOVED FROM

THE OFFICE OF THE RESIDENT

GEOLOGIST. ONT. DEPT. OF MINES

SAULT STE. MARIE. ONT.

RECEIVED .FROM AIGOWA C?iiTRAL R.MLWAy

, ..— j , . .... . . r-4*t^i W. i *: :.-jSs.kA

*t-A'fi'ii'ri 1 -. v •'*' : V1 , '•''••"' ;

HAROLD 0. SEIGEL ft ASSOCIATES, LIMITED

^ROJECT

' SEIGEL ft ASSOCIATES. LIMITED;

PROJECT:

CONDUCTOR:

: ftA*t.TluT5O^l *tiB: •**.;.'*.**v:k

HAROLD 0. SEIGEL a ASSOCIATES, LIMITEDf

f t2", CONDUCTOR: Z. - 7

WOIK BY. , f n. f"LcT ft-ir!

': : •W'-'SW'.TfF.'/E ?. FJWf&fmsV&rK

Franf f. 3 'nnkm i l .'; '.^^ l d f C S

ic c.-

JNO.HALY...LI.Z-

' '...'V* Y&f-' '{t''' ,- /Y,.'1 ' '-'""

r'- -.^-l^ '^''^-'ty*'^^''''

PHAJKJ. R, JOUBIB 6 ASSOCIATE?

AMOHAU L-8

(Also Known As A.O.P. Anorialy 113)

OEOLOOICAL R&PQHT

ii located one nlle south of Batchwan* Station on the A.C,R. in Township 2(^, Range H, District of Algcwi.

Work DoneOna baseline and six crosslinks (liOO 1 apart) ware out and

chained. The grid covers approximately (1800 x 2000) square feet. Magnetometer and eleptronagnetoaeter surveys wer* oarrlod out along all crosslincs. The area was also geologically napped.

The E.K. and nagnetonetcr curveye were Xiret carried out along an old grid, cut by A.O.P. in 1#0, with the baseline running toward 30^. Due to lack of confirMation of A.O.P. 's conductors and the fact that the general strike direction of the rocks in the area is east-west, it was decided to cut a new grid with the boaelio * going east- west.

Geology

Anonaly L-8 is, generally opealdng, underlain by acid Itva with alternating bands of sediments, mainly quartzite and iron format ion. The bedding is in the northern and central part striking; east- west and dipping steeply to the north. In the southern part,, the etrike is northwesterly. A lineanwnt in the western portion of tha orra le striking ricrthwsterly and is believed to bo a fault. Ihe rocks along the lineament are sheared at a few locations.

Outcrops of the iron formation wore seon just emt yf the crt*J; in the central part of the area. It is banded and of a lc*n typo (I5jj to 20JC Fe), and can be slightly folded.

A large percentage of all outcrops observed were basic intrus ive*, particularly in the eastern half of the area.

FRABO. R. JOUBIN ft ASSOCIATES

AHOMAU

^^:wrm^m''. ' ( ' ' ' - . ', . M'- V " :',U - V -jf v.

e/t/fT ANrtfa ', ' ' ,: ' V 11 ^ '•'-•',*i ;."*. : '^

(Also Known As A. O, P. Anoaaly

.:t*K-:--y?'-^- . 4,. ••'i ;'A

j', x ^ -.:•*,/- r '.' ;^••*, ' "i \

-

GEOLOGICAL 1U5PORT

Location -.

Anomaly L*8 is located one rdle south of Batchewana Station on the A.C.R. in Township 26, Range Ut, District of Alcona.

Work DonaOne baseline, and six erosslinea (UOO* apart) were cut and

chained. The grid covers approximately (IdOO x 2000) 'square feet. Magnetometer and eleotromagnetometer surveys were carried out along all crosslines. The area was also geologically mapped.

The K.K. and magnetometer surveys were i'ii'et carried out along an old arid, cut by A.C.P. in 1959, with the baseline running toward 30^c . Due to l&ck of confirmation of A.O.P,'s conductors and the fact that the general strike direction of the rocks in the area is east-west, it was decided to cut a new grid with the baseline going east- west.

Geology

Auootaly L-8 is, generally speaking, underlain by acid lava with alternating bands of sediments, mainly quartzite and ii*on format ion. The bedding is in ih^ northern and central part striking east- vbjit and dipping steeply to the north. In the southern port, the strike is norvhweBtcrly. A iinea.tent in the western portion of the area lestriking northwesterly and is believed to bo a fault. the lineament are sheared at a few locations.

1 he rocks along

Outcrops of the iron formation were seen just 6*01 of the creek in the central part of the area. It is banded and of a lean type

to 2C# Fe), and can be elightly folded.

A large percentage of all outcrops observed were basic intrus- i vos, particularly in the eastern half of the area.

:' "^;'^tv^v:#v^'-.:.--', : ' ' ,' x-'. ' j ' . . 'f '''-'^ t-' vv'.-;v.;.. r .".' ' * li ' ; J *'- ' V i '. ' V. - Vi ,'.a; :,. \ --.v-*^j-1 ;.., ;ti .-... - -,- -,.,^ r 1 -;*,^ •^'.-/^A4f; -

8othU4'bi econortLcAl .interest WAS f^Jj'ii uiii' are*., Jth^'S^ ,\;': ffi&tj?-, too lean for

: - : me nortiwert portion of. Inoaaly L*8 is flatij, low ground' covered by svsjqp end scattered boulders. The retaining pert Coaaists

" " of hardwood ridges covered by boulders. v - ;,,.\These types of overburden Are very difficult to penetrate by

digging with'shovel And grub hoe. It WAS therefore inpossibjle to CArry out farther work to explore bedrock At locAtions 6f interest.,

Batchewana Station at A.C. October 27 t

Hakon 0. IAen, Geologist.

t.

;- ;- S^;^i!U;o#(*irtlib*ft^^^ * '

wan -first -prijj -but eiong W old grid, r toward 30*??* s jJvVto, lack of con-':

Mot-veot, it va* decided to o\lt 4 nev firt,d with the bMe* 'l'.

V t \ i *.

•:vfvc f- i - M.i 1: i 1. -

underlain fcgr.acid lava with aftedJ*e7itir,-Hal^ end irorrformation* ' ih*'beddin^l* .in the

~: ajqirthern''a^d central part striking eaeWeut, and dipping atteepty .to the'north. la . ; vthe; southern part -the; dtejLke le sonthwosterly. A iinflamont in the western portion : . oJr.jthe-'areale striidhg nort^iweaterly and is believed to be a fault. The rocks along .the iZlhennant aro sheared in a fev locations. .

' ' .outcrops of ^he iron formAtion,.woro seen Juot eaot of A creek in the central part of the aorea. It,is banded and of'a lean typo (15^ to 20# Fa) and can be slightly

''

. .

' , A large percentate o all outcrops observed was basio intrusive, particularly in the eaetern half of the area*

(frophyaica,Bce Dr. Seigel'o report for this

. 'Nothing Of econotnlcal interest WAB found in this area. Eia iron formation aeen, ia too lean for connefr'.al use.

Overburden

The northwest portion of Anomaly L-8 lo flat, low ground covered by swsap and Bcattered boulders. The remaj ning part conaiste mainly of hardwood ildgee covered by bouldera.

, - . Thece types *L overburden aro very difficult to penetrate by digging uJ.th hovel and grub hod. It was therefore impossible to carry 'out further work to expose bedrock at location* of interest.

- ../ .Dalchavana .Station :Jovewbar 2, 1962

Hakon O. Lien*

-\'

' ' .;* ..*i"* * -i ,.-S'V. '*H?-- :. -j. . -;.;'t f,';'.i ^ftn,'

. .. '/.-A ^•'-'r '\"-f'V.-';':iAi'i..'.vv ^- :":^^\v^ :^- : - •: ':*-tf \**'i*;A^'

FRANC. R. JOUBIN 4 ASSOOUTE3

QBOUHD ZRTESTIOAnOIf-REPORT

AREA L-8

. - . -'.^vv-W.•-y (^- ^v/.-;. 1 -- .'*

"'-^y^-i:1^

SUMMARY AND CONCIJUSIOKSt ?,

The source of interest in tide area waa aa aeronagnetio known as A.O.P. j?13. Ground EJl.aid aagnetcneter surveye wero carried out initially on six linea froa an old A.O.P, base line oriented 3Q50,- and later from six lines at iiOO' intervols from a new base line oriented 2?00*

The change in lino direction was baaed on the discovery that tba fcmational strike vas almost due fc-W. .

The magnetoraerter survey has revealed several narrow bands of what is undoubtedly magnetite iron formation* Two of these bands each have poeoible continuity over at least 1200' of strike length and are still open to the west. The indicated widths are generally ^0* or less, which is too narrow to be of likely economic interest.

Aside froa 'reverse 1 type tilt angles associated with iron formation, one true conductor is observed. This lies within 50' 'south of the nev base line, between lines 16B and 21*2, and about IfX) 1 south of and parallel to one of the iron formation bands. It is of weak electrical anplltttde and has no consistent magnetic correlation* Its source is poesibly cd nor oulphldes or praphlte in a shear tone. There Is no outcrop napped on the trace of the conductor.

No r*coBT(wndationc can bc made for further work in this area on the basis oi the present geophysical data.

Respectfully outwitted,

1)01*014 0. Seigel, P. Eng,,

Toronto, Ontario, November 16, 1962.

KH

Hovember 19, 1962.i P l . ' l - - L.' W .- ' , . .

f-V

^f?;;^.:^y'^^'.H'?'^'"' i3jf.'-**\:': ' Vvv; ./^••iv'-* y -- ".:... :v.;^^::^V- - •••-,v. ^'V-v''* ' - - ' - jW^r^;A -' -. ; '- - -^!';-'; ^: ; ; -;-.V' .' . xWVt- l 'v" : '-'''-"-'•*w:.- :'..'- .- .... .'.'if?/o r ; - - -- '

y* K 81 "S C *

r O z S-is * siQU

fe o

S

i B

O f-8 g

A. K

w

*" ft ~

S S 3 z f SO

0)

Donald Smith, Esq., \ Frano. fl* Joubin 6 Associates,

Leo Avenue, -- Sault Stf. Karie, Ontario*

Enolosed herewith ia a copy of the results and reports on Areas 1^7 and J/-8. I regret that there IB little of interest to be seen, based on the present geological and geophysical data.

Halcon Lien has kindly cent a copy of hi* geological reports on each area, which I find very helpful in tying things together* I trust that he will continue to send these with the geophysical results*

I h&Ye Bone incomplete data and notes from Hubbard on L-13* I gather the crew moved off this to t ankle another area, and is probably back on it nov.

The E.M. reconnaissance results, which are the nore complete, confira a zone of multiple conduction of moderate amplitude over a strike length of 2000 ! and still open, particularly to the south. We have really only three lines of magnetometer coverage, and this over the li grid where no detail E.M. has yet been received, so that precise correlation is not yet pos Bible. There is, however, a significant positive-negative magnetic pattern, often indicative of pyrrhotite^ which lies in rather close association with the general conductor locations on these lines. A sulphide origin, including pyrrhotite, appears likely for this conductor system.

Assuming that the sulphide mine rail cation in either of the Rowings in this area carries values of economic interest in base or precious aetals, then the present grid should be continued, both to the north and ooutl to delimit the conductors preparatory to laying out a drilling program.

Sincerely yours,

(signed) Harold 0. Seigel, P. Eng.,

cot Toronto Office.

RECEIVED FROM ALGOMA CENTRAL RAILWAY

OCT 21 1965

RESIDENT GCOLOGIST

HAROLD O. SEIGEL a ASSOCIATES .LIMITED/e.

HAROLD O. SEIGEL a ASSOCIATES. UML ^.D.

PROJECT-.

CONDUCTOR: L.. Q

Conductor

SSOCIATESAssoc/ATe-S

-•^i^ •.-i.-t-i-v-.-- — .-- *?-v,,.-'. i-'..** ,*- - - -•"E * 1 ^- ***~*,-.rr * --*3**w"~ -''

^^ki j^js^^*?-^^;

HAROLD O. SEIGEL ft ASSOCIATES, LI MITKD

-. L O CAT/CM

^S^S4^-4^---^^M-:k^;*^f

,V''r .* r": '- ' •'"" t-'••\\'\ -'-' ~" , -' - ' ';' v.;/- •..-.''- - ' '-':.' '- :- ! ^.;'"V'V -'' ,-:/';;-;;,,, v^"/' ,/ :A.c.R* TOWSSHIP 26 RAypg Hi (PH) X'''')':-'*.*',''." '*' v ,.'''. ' -" ' ' .- . ' ' ' ' " - ' " - ' . ' - ; : ' ' "'i : ' '". ' ' ' ' '' ;*''^ntroduoticm ,. . '. ^' , v . : - - '•'- v - ' " . ' : :-\ •••'.'''f^'-'.',

- . ' ' , - ' '. . ' - ' '.'"~ * - " '.'' i, General goolocic&l mappine vas carried out in the eastern half and thil southwest corner of this Jownship during tne period of October. The main target v&s to locate th* greonstouo contacts. ., . ,

Geology ,

Frofft a fcaall horthwest-southaust trending Jake-one and one-half tdlea eouth of Batcljt&ysna Sta'ica, the contact between greenstone and diorite (the latter on the eouthc*Bt side of tho contact) strikes northeasterly and hits Batchayana River about two tdles northeast of Uetchw:ar.a Station. On ^he north bide of the river it ie 'found four ndloe northeast of the station. A rafcjor fault alonfi the river is beliovod to hove caused the 2 *nile displacement,of the contact.

Cn the ficarpnent down to tho river on the south side a slightly Mineral ized (pyrite only was often) quartz-breccia was found. A swaple for Au was taken (&A-32?

dykes).The rocks on both sides of the contact are cut by baeio intrueives (mainly

In t-he area 3 nilas southweet of Batohawana Station, ecid or intermediate intrusives WGJ-O not observed on the south clde of Batcliawana /Uvor, only besio and ooid lava. Tho contact between the greenstone and the granite-gneiss complex to the northwest is therefore assumed to follow the river.

Pee-In.?/

()n tho napplnc traverse in the area about 3 miles southwest of Batohawana Station, a heiiv^y .mineralized sulphide sone was discovered about 900 feet west of a half mile 10:4 lake (east-west trending) in the southvoet corner of the Township. The zone was undtr Investigation at the end of October and will be further detailed in the Monthly I.eport for fio^enbar. (Samples 3A-329 and iiA-330 w*re tkken).

Samples

iJA-321'. Locaticn: From couth cide of Batchuwano Mver npproxira&tely 2 adles northehtt of Batchauana Station A.C.Ti, .Mot selected ..rab aanplo fron quartz breccia with son© ruot (SIK( pyrite), Dat-e; October l/, I?o2. Sampled for Au.

From top of ocarpraent on south side of Batchawana River 3 miles southwest of ratchawana C t At ion (Area I/-13). ii 1 wide chip sample frow rusty cone (onlj' h 1 exposed) striking about north-south and poesibJy 2000' lon^;. Dote: October 20, 1962. Sanpled for Au.

3A-330. From 1DOO' west of a half mile long lake (east-woat trending) in the southwort cornor of tho township. Kot selected grab o*mple from 15' wide rustyand raineralircd zone (only pyrite seen). 26, 1^62. Sampled for Au.

Zoiw striking toward 10 . -'atei October

BatcoAvana Station A.C. November 2, 1962.

Hakon 0. lien*

QKOLOOICAL'REPORT

' ^*,,•f.' " ~'."'S'jf- -'

-IKTRODUCTIOHi

Two showlnga klneralited b-' pyrite, fcpprtaimtely 1^00 feet apart, were diecovered last a*onth by a geoloetet from this Coapatij, onv * across-*, untry traverae* . *, V-

;. ' " " ' ' '' *J - ^ '. . ' *- ': '

It was decided to carry out E*M. and Magnetometer ground surrey in the area. The geology in the vicinity of the ehowing, vaa Also napped*

* ' ' ' - ' ' f - '

Some 36,000 feet of line were cut, covering an are* about . (^600' x. 2000') feet, arranged into three grids along a north-southerly direction* : . . '/,

- ^i , , '

LOCATIQll

'.\e BuTToyed area le located Just woat of a 3/2 Bile long, east- west trending lake in the southwest corner of A.C.R. Township 26, Range Hi, approxinAtely 3 milfis south-west of Batchewana Station, A. C* R* Tho area 10 accessible via bush-roads from Batchewann Station*

The general rock type in the surveyed area le altered basic lava* In the southern and central grid, the strike of the foliation le northerly. In the northern portion, it is northwesterly. The dip is generally to the east, variatinc between UO0 and 800,

A xdneralited *hear zone cuts across the area from the north to the south and follows the east contact of a bed of acid lava which, In places, can be porphyritic. This bed is in the northern portion of the area, at least 300 feet wide, and forms a scarpnent along the west contact. The acid lava appears to narrow down in the central port of the area and is not seen to the south.

A shear eone was also found In the eastern portion of grid 13*

Stringers and veins of blue quartz, (up to 1/2 foot wide) are canon in the sheared rock*

The greenstone is at many locations coarse grained*

The big hills along the west border of the surveyed area are underlain by coarzd grained basic dikes.

Jtf ^m i i o l'*1* 1 * '. p -' '" .t' - ' '*''"' -' * *'* "" ^''"^ j'^ EOOKMIO'"

...' ,V-N'^,?'.'i "'•X':.

, , The north-southrunning ehear zone along which the surveyed grids were out, can at several places' be well-nineraiiaed by pyrite. Grab sampleiB ware taken, but the result of the assays is at the preeent time not known. ' ; . ' -- - -- - r ' .' -. ; "" --

The cause of tha magnetic activity alone the ehear tone vaa not discovered, as no oagnetio minerals have been found in the area up to this date. Trenching or diamond drilling would be necessary to detercdno whether pyrrhotite or magnetite is causing thece high magnetic intensities.

OVgRBURDEgi '

The northern dnd of the surveyed aroa is covered by oand, gravel and boulders, and the southern end by swamp. Except for .those areas, the overburden is believed to be very shall*.* and a relatively large part of tho bedrock lo exposed.

Hakon 0. lien, Geologist,

Batcliewana Station, A.C.H., November 30, 1962.

r:-v

V ^-X^'OV ....^ .im*, ../-J

|^^^;^M^?-'^^: ;V:' ;^^:: ''---^^'*Af**-v-;V'J'i ..-' '".-'V " *-; ' 1.,"' -. '- - - '-- - " - Y.. "\ -- ' . .J^^V;;-':;,-. - x--^".^:^ ., -. -;.: -- ' . . -;l :;|).v ;,: .. '.Saj^/VV ^ ' ---L./ •••.•V. v ^"' '- BaROtp O. SEICBl ft A——".P^MV^;r ?-' - ;; :7- ' - ' ' ' ' ^ - *-r- itb *

SQOBV& ASSOCIATES

FRANd. R. JOUBXH it ASSOCIATES, LIMITED- - - - -- , .

GROUHD I OTESTIGATION REPORT '

' ARKA L-13 '^I^

IHTIflDDCTIONt

. Rather extensive geological mapping and geophysical surveys vere carried out over an area about 2000' x 5600 ', including two pyritised outcrops.

A geological report, and nap, by Mr. Hakon 0. lien are appended.

Three base lines were cut. The farthest north, ((fi) was oriented N250E, the middle (#2) was oriented 1160^, and the farthest south (#3) was oriented N25OE. Approodittately seven miles of cross line were cut from theeo baselines. The Geophysical work, under the super vision of Mr. lien, was carried out at various tines by J. F. Hubbard, D. Leaper, H. Lien, and 0. Theriault.

DISCUSSION OF RESULTS t

Threo conducting zones have been detected by the electromagnetic survey and are shown on the electromagnetic plan*

Conductor l - hao a possible extension from Line UN (B.L.I) to line 2 N (B.L.2), and is strongest on Line U S (B.L.I). At this point, it is within 200' of an outcrop carrying pyritic mineralization and is apparent ly on strike with it. There is very strong magnetic activity on or near this conductor, with a range from off-scale positive to 1*000 gammas negative, in the immediate vicinity of Line US. Obviously , there must be some magnetite associated with this conductor as well ae sulphides.

Conductor 2 - has been confirmed on Lines O, 28 and hS of B.L.2. It lies, apparently, in basic lavas about 50' to 100' east of gossanous outcrops on each of these three lines) although subsidiary, weaker conductive indications do reflect these pyritic occurrences. Magnetic correlation is present, but variable, on the main conductor. It varies from 1500 gammas positive on Line O to only 200 gammas on Lines 2S and IjS. There is also a negative trough flanking the conductor on its west side, indicating strong reversed polarization.

Conductor 3 -is strong on line US (Grid 3) only, but possibly carries through to line O of that grid. It lies in a small valley between diabase to the east and sheared basic laval to the west, and is directly correlated by an 600 gammas magnetic anomaly.

Mbtfthly Report for December 1?62*

'1/^13 (A mineralised shear aphe southwest of Batchewana Station A.C.R.)^ ,, ^ MMWMPB-W T ™. - - -—— - - - -- - - — - ^^w*-^-i^^^-- —( r ^ i—,. *- ^ -L - - -n. r ^ " ' \ T ~^- .7 ^^^^^ C ' " . -t , ,

- -. j. Introduotion "'. ' ; ' --' ' '" ''"-, •'•""' '.'- v .-, ' ••'•'•'- ' - Ay'i'', ; : ' * - "' -, ' ;PI " ' - ' ' - . - ^ -.

Two showings mineralized by pyrite^ approximately 1,500* feet ap'art,- ' :were discovered in October 1962 by a geologist from

country traverse.

, - It was decided to carry out E. H. and magnetometer survey in the area, flfce geology in the vicinity of the showings was also napped.

Some 36,000 feet of line were cut, covering an area about (5,600 x 2,000) square feet, arranged into throe grids along a north-southerly direction.

Location- *

.The surveyed area ie located just west of a half mile long east-west trending lake in the eouthvect corner of A.C.3. Township 26, Range Ib, approximately three miles southwest of Batchewana Station A.C.R. The area is accessible via bush- roads from Batchewana Station.

Geology

The general rock type in the surveyed area is altered basic lava. In the'southern and central grid the strike of the foliation is northerly. In tho northern portion it is northwesterly. The dip is generally to the east variating between ItO0 and 80O .

A mineralized shear zone cuts across the area from the north to the soi-th and follows the east contact of a bed of acid lava which in places can be porphyrit ic. This bed is in the northern portion of tho area at least 300 feet wide and forms a scarpment along the weeu contact. The acid lava appears to narrow down in the central part of the area and is not seen to the south,

A shear eone was also found in the eastern portion of grid /f'3.

Stringers arid veins of blue quartz (up to one-half foot wide) are common in the sheared rock.

The greenstone is, at many locations, coarse grained.

The bic hills alon?; the west border of the nurveyed area are underlain by coarse grained basic dykes.

M--

running shear sons slijhg wuicty ^he; Mir^^vere cut, dm/ aV'MVer'al places, be veil sdneralieed by pyrite* ,'wab simples - .- l 'X'

;*: i:a'' 4 vert taken but^the results of the assays are, at the present itiaa/jnot Jfnown*;/.^o'-^-

lj! ' ? ' i , vthe causeof the magnetic activity alcmg.Uje shear wtoe-iras' not ^'' '/, discovered aa no :raagnetio minerals have been found in the ares uj

It is reccnnended to carry out trenching or diaaond drilling to ' ' ' detemine vhe'ther pyrrhotite or magnetite are causing the high nagnatic Inten* f sities in the area* \ ,\llftt fct, r **,y fit-*-. D-p H rt /^ \ '"'••'- '.-"-.

JPverburden - -. -" i ,;1 ' , - - ' ' ' ;. -. '- '

The northern end of the surveyed ariba is covered by sand, gravel and ' boulders, and the southern end by svaiop. Except for those areas, the overburden ' is believed to be very shallow and a relatively large part of the,bedrockis ex-,' posed.

Batchewana Station A.C*R., December H,

llakon D* lien*.

.,'V.

^m^^Wm^Jm^^-^'^--, rv^'V^--V^!r: ?^V*^^^ ^, V ; ''^;:;. -; \ \ -- - :\ :-^/k^i^^^''^'*''-, *' .- ''j'"' " '-^ '- *SMtoO. 8EKB5L i ASSdCUtlsl lUMtTKD ' * ^V*f *ii^* ^** V "V--"' ' -t ^T/.O:* '/"A* ''.•-."i ' '"j ' V "*- * *, . ' * '—A—. ' . n -V: *i?t^V-.^.''i'i ;V^: .'- .•'•'••' '' ' -" " "" '""' 9*!3*, . "' ; -""'

PRAHC. R. JOUBIN i XSSOCIATBS

QROUJID mVESTICiATION RKPOET

AREA

: ^;;:,i^-;.^' -?'. -*--i - H ' -' * r ' - .''.' j- ' -

" '"' V*. ' -/'., .J-'

.Vv^-''-.iV.- ;i.-

\.-

So

c.. i-j

tt

S

ti:D

aU!

IUKU QO*~v-oz

Ou ot0ux

H

W

0oob1U0

uuiH

t t!

.JD•iw

IHTRODUCTlom

The basis of interest in this area was an aeromagnetic anomaly, designated A.O.P. #1)*, which was revealed by an earlier airborne magnetometer survey.

A ground magnetometer survey had previously been carried 'out by A.O.P. and confirmed the existence of * narrow band of iron formation. The present magnetometer and electromagnetic surveys vere performed on the same grid.

The grid base line strikes 1080 astronomic. Cross lines vere cut at UOO' intervals over a 5,200* strike length and all extend 1000' north of the base line. Pour lines extend **00' south as well.

A geological report and plan by Hakon O* Lien covering the gridarea IB attached hereto.

DISCUSSION OF RESULlSt

A relatively narrow band of iron formation strikes almost due east- west across the full ^200* length of the grid and is still open at either end. Judging by the order of the magnetic relief, the widths and percentages of magnetite are too small to be of economic interest.

Rather persistent low-order reverse or magrjtite-type tilt angle curves are to be seen on the electromagnetic survey results* These coincide with the iron formation band and are, no doubt, caused by it. They are of no significance ao far as conduction is concerned.

A possible weak conductive indication on line 20W, north of the iron formation, was not confinaed by detail suiveying.

The present geophysical results do not foster further interest in this area, so far ae possible base metal deposits are concerned.

Reepootfully submitted,

(signed) Harold 0. Seigel, Phd, P.Eng.,

SAULT STE. MAH1L

Hbs/r. Enolosure.

EO FROM ALGO.VA C^.'THAl tJ"'

•'S'•/;.'' ^.U

December 17,

Donald fi. Smith, Esq.,franc. R. Joubin 4c Associates, limited,3JiU Leo Avenue,Sault Ste, Marie, Ontario.

Dear DomI enclose herewith the following!

1. Tvro copies of Lien*s geological report and report as well, covering L-13.

2. Lien's original geological plan.

Very sincerely youro,

HAROLD 0. SEIGEL tt ASSOCIATES, UMITED

(signed) Harold 0. Seigel, P. Kng., President,

HOS/r.

Enclosures.G

SAULT fiTL. ,v./.;.::., ON r

-i, RECEIVED FROMCENTRAL RAILY/AY

DOCT 2 1 1965

RESIDENT C LCLDDIBTBAUL* fifV.- MARIE

Bwi(^•X^'&Vi' --' ' vi'te CONCUraONS AHD RECCMMENDATIOSSj .v - * \

..••V ., - , ,The geophysical and geological pictures air*' corisl*tienVwJLth/ . ^vv-'

lenses of sulphide mineralization, undoubtedly Mainly pyritf^but" probably /;. with some jarrrbotlte aa well, together with magnettte^rtctfixw lying ^r within one or more chear tones, mainly in basic lavas* Accidentally^ or ; otherwise, the strongest conduction does i not occur in the vicinity of ,th* *V pyritic outcrops, thereby leaving a^nething to the imagination.: Th*k;tili ^ angle curves suggest a dip to the east on the conductors^ which agrees with' ' Uen'e geologic dips* - - ' ^, . ^ v^-

' . ' - : ' '- - ',', , ' i i-',' ' 'r- ' ,' - v\ : '.

At the present tine the writer is not; as yet aware of the assay results of the san^ling of the pyritio outcrops* If these are encouraging then, of course, further work is required* Even if these assays are negative, it can be argued that a ccnplete section cannot be seen, on any one of the three conductors. The JC*ologloal enviroment appears .quite favourable. According to Lion 1 a tosnents, trenching nay be possible on ; conductor 2, and this is therefore /^.oramended, either on 'Line O or 23 , (B.L.2).

Trenching should also be attempted on Conduotor l, on Line US (B.L.I), and on Conduotor 3 on Line US (B.L.3)* If this does not appear feasible, then action on these two conductors should be delayed, pending results of the trenching on Conductor 2* .

Respectfully submitted,

(signed) Harold O* Seigel, P. Eng.,

HOS/r.

f-. - -, fi 'v*' :i'

Toronto, Ontario, December lh, 1962*

.•C.R. TOWHSIgP 26. lUHQg -Ut (PH) , \ [

- . - . - - . - .. - ...- -- - - . 1,,.-- *- , ..-, '- vv. -- .' -- - ' ,. . -- v". - -.:,i,. -"' 1'-.'.-r:;? -: ''''-t. : Tho ; ooly' tloyje,carried out in thi'd TwrnsMp during the

'0f Wcftaber 1^62 was ground-Bagnetoneter eurvey on anomaly- - ---' ; "'" "'.. ' . ' " ' ' V - . . - '

rjree'banda of magnetic B were found and nore work la required to explain the anomaly and will be carried out during the coming period. , '

PT - ' l'-X*'.

Sault Ste* Marie, Ontario, December 31, 19&2.

Hakon 0. Lien*

JM*--'kvV*^';; v.-v*-- .

l i

'A geophysical and geological survt^ vere cpbduct^d on an areascne 1DOO x SOOO foat and it IB underlain by a magnetic anonaly

discovered by an airborne aacnetoneter survey carried out by A.O.P. a few years ago. . ' ;^., -. '. -.... v.' . . ,

Only a few outcrops were soon due to two feet bf anew*

Location ,

. .The surveyed area is located in A.c.R. Township 26, Range 1U, • District of Angora, about l mil* north of Batdhowana Station on the A.C*fl.

Geology

The napped area appears to be cut by numerous baoio dykes along a trend 500 to 400 feet wide which strikes in a northwesterly direction. Ihe touthern border of the trend enters the surveyed area at 900* li on L 32 W and cuts the base line at about L 20 W, The northern border cute the base line at about IJLne 0.

To the northeast of the trend, outcrops of dark, blue quartait* wore seen, striking about 1000 and dipping steeply to the northeast.

Outcropo of what is believed to bo altered, acid and intermediate lava were oeen to the southwest of the trend.

Overburden

Due to snow tho naturo of tiio overburden could not be determined.

Sumcdt Station on the A.C.H., llakon 0. Lion. February l, 1963.

. i ^ V

-u .'

__________A.O.P.

Introduction . . ''v ' . r ' ;V ,

The source for.Anooaly I/-10 is a magnetic oooaaly found by an airborne raaguetoaeter survey carried out a f eV yoars aco by A.O.P. That coiipaay followed tht anomaly up on the ground vitn * macn*tt*neteri but ' .-' appear to have ndssed the main magnetic bands due to too ahorv cross lines* I^r ext*ndlnc the lines 3XXX) feet to the west,' a series of magnetic bands W9re revealed. ^ . :

The BurveyecJ arett Measures approxinwtoly eoae 3000 # 2000 feet.

Only a portion of all outcrops believed, to be present ia iha area could be seen due to one and. one-half feet of snow*

Location

Anomaly L~K3 is located in the aouthvx-stcrn portion of township 26, Rflnp.e Hi (Ph), Diatrir-l of Algc:aa, about 2 idles oouta-iect of h&tchawana Station on the A.C.it. and can be ruashccl via buth ro&ds i'rom. the otation.

J-'ost of the area of ^.nor.uly L-10 is underlain ay sodijients which strike i:; -i northarl;' nirectio::. in t;n.- :*or-ru*eu'vom portion o! the surveyed trid, outci'ops of dai^ l^rut* quartzite w?re tccn i'o^nin^ a nortli-so'ith runiiing escarpment. The dip of the new] In-/ lo a bc ut 600 to tho erst, .'ir'fosc was obfcer\'ed in 'he souvtoraotor" part of ^f.c area. A fcv outcrops of vhat is believed to l* a l4 tree?, acid and intemiecllate lava wortj also observed.

'ilus nor v I.vi.iU;rTi corr.cr of the *ri^. i c '.inderlclr. b/ g b.isic dykeng northwests:* l;/.

Overburden

Due to snow, it was jjopooeiblc -o :w;* .ne ovcrciuruw: completely.

A.-: arec rr.c.iB .rirtj :-o:io ^00 x lO'O feet, located ir; the central part of the southern hall' of the ,;ric, iu covered by tua;ip.

Sminiit Station on the .'..C.?(., Hakon 0. lien. Tcbruary l, 1963.

OEOLOOICAL REPORT

/:;^.:--;t#'-

'^r* i vv - ,

fife:^?Jfe,..' A•1jiy?V .'-o •v'-"•'iS'V :'. '* .'iv' (r ' H * . " vfm-: fe .vhf/'.,' . ' -•s;V*. :^V-'^-,-v •.^•.'•: ."

/ J ' A geophysical and ecological aurvey was conducted on an area sowa 1000 X 5000 square feet large, underlain by a magnetic anomaly discovered by an airborne nagnetomoter survey carried out a few yews ago;.by A.O.P. -;. ' f ^W;

Only a fow outcrops vere seen, due to 2 feet of snow*

LOCATIOHt

- The surveyed area is located in Township 26 - Range li* ~ District of Algona, about l mile north of Batchewana Station A.C.R,

CEOLOOYi : r ~

The mapped area ceemo to be cut by numerous basic dikes along a trend JJOO to 600 feet vd.de, striking northwester3y. The southern border of the trend enters the surveyed area at 900* N. on I32W and cuts the baseline at about L20W. The northern border cuts the baseline at about LtO.

To the northeast of Die trend out-cropr of dwk, blue quartaite vere seen, striking about 1000 and dipping otceply to the northeast.

Outcrops of vhat ie believed to be elttred, acid and intermediate lava were epcm to the southwest of the trend.

OVERBURDEN!

Duo to snow, the nature of the overburden could not be determined.

Hakon 0. Lien*

i?-

\*

Datchowtma Station, A.C.R., January Ui,

^^^M^T-7^-v,-~,~ * s^'^'^u'.. -r *v

' HAROLD/O. SEIGEL ^A^SOCJ^ES,JL^Mr[EDPROJECT i^ww R. JOUBIN a ASSOCIATES, LTD.

CNDUGTOR :

'HAROLD O. SEiiQEL a ASSOCIATES. LI MITtD

: FRANC R. JOUBIN a ASSOClArES.LTD.

' ~J~*l*.*iLf ** " LiQfnd

XV^ 0 -; ;--* v -, *

•8tWr *"'fy&L . -' , ;

.** if--

^tfC,?" ;' 'v

VV J*''.:, -v;,v '''•^•; - ' - V-*.- ., "f ' 't ,v* f: *! -' ' *'r'. -

FRANC. R. JOUB1V AM) ASSOCIATESf'

AHOHAPf IrlO (A.O.P.'s Anomaly

QEOIOQICAL REPORT

INTRODUCTION}

The source for Anooaly L-10 is a magnetic anomaly found by an airborne magnetometer survey carried out a few years ago by A.O.P. That company followed the anomaly up on grovnd with a magnetometer, but appear to have missed the main aagnetio bands due to too short crorslinea; Ey extending the lines an extra 1000 feet to the west a series of aagnetio bands were revealed*

in width.The surveyed area is approximately 3000 feet long by 2000 feet

Only a small part of all outcrops could be seen due to 1-1/2 feet of snov cover.

LOCATION!

Anomaly L-10 is located in tho southwestern portion of A.C,R* Twp. 26 - Range lU, District of Algoma, about 2 miles southwest of Batchewana Station, on the A.C.R., and it can be reached via bushroads from the station.

OEOLDOTi

Most of area L-10 is underlain by sedimentary rocks, striking in a northern to northeastern direction. In the northwest portion of the surveyed grid, outcrops of dark, bluish quartzite were seen, forming a north-south trending escarpment. The dip of the bedding is about 600 to tho east. Arkose was seen in the southeastern part of the area. A few outcrops of what is believed to be altered, acid and intermediate lava were also observed.

Tho northeastern corner of the grid is underlain by a basic dike striking northwesterly.

OVERBURDEN

Due to snow it was impossible to map tho ovorburdau completely.

An area of come ^00 by 1000 feet is covered by swamp in the central part of tho southern half of the yrid.

Hakon 0. Hen*

Batchewana Station, A.C.R., January 25, 1963.

.'' bordar of the 1000-entera the surveyed area at 900.' 0 on.Una, }2 W and,:" "" ' "" " ' "" ' ~ ' L20W., : . ' - ' " ' ' ' '--V- "' " " '

•To the northeast of the tone outcrops of d^trk blue'quartzite' seen striking about 1000 and dipping steeply; to, the northeast. ,;'

'. . . ," ' - ' - . t T ' ' ' " ''' i ' .. of what iaf believed to be altered acid and -1 -''' - '

lava vert aeen t**^ the southwest of the zone., . - ' , ', ,,'V

L-10 (A.O.P.'a Anomaly 11, the Poverline Anomaly) . . - ;.; ; \

^T^," r . - : The source for Anomaly Ji-10 la a wagnetic anomaly found by an ;ih , airborne magnetometer survey carried out a fev yoara ago by A.O.P. That"•,/: . coapany followed up.the anomaly on the ground with a magnetometer, but ,.. ,'i\''!'~ thffy appear to have nieaed the main magnetic bands dee to too abort cross*^rc-v r lines. Ey extending the lines 1000 feet to tha vest a aeriaa of magnetiq :•v-'v*:'.-, . bands vara encounterad. The autrayad area neasurea aome 3000 ac 2000 -~^"

Moat of arau of I*-10 ia underlain by aediaantary rocka, atriking northerly. In the northwest portion of the grid outcrops of dark, blue quartzite were seen, forming a north-south trending escarpment. The dip Of the bedding ia about 600 to the east. Arkoee was seen in the aouth- veetem part of the area. A few outcrops of i;hat ia believed to be altered acid and intermediate lava were also observe*!. The norlheaetern corner of the grid la underlain by e basic dyke striking northwesterly.

An *rsa, aeacurlng approxiwatoly ^00 x 1000 foet, located in the central part of th* southern bftlf of the #*l(J, is covered by ewanp*

Summit Station on the A.c.H., H&kon 0. Lien. February l, 1?63.

SAMJMIflOa KO, l PROJECT (A,C.

MOKTHLT REPORT - JAKUART 196*3

The ground geophysical eurvey, atArted in 1?62, eoatinotd . during the period of .January. The writer had on* week'0 holiday this month (January 20 to 27 th). The rest of the nontb vaa spent with the geophysical field crew on field work.

Investigation of the following three area* was terminated during tho periodt

W-3 in tho northwestern corner of Crown Township 26, Range 13 (QH)L*? in the northern portion of A. O.K. Tovaehip 26. Range Ut (PH) .V10 in tho southwestern part of A. c. R. Township 26, Range. 1J) (Hi)

The geological napping was oxtre.iely difficult due to threo to four feot of snow.

For the geophysical work in tho areas see Dr. Seigel 's reports.

(y,agncr*s E.M. conductor of sane na^)

Thic area eeeuns to contain two conductive cones revealed by an airborne E.M. survey carried out for the A. C. R* about A year ago* One of tho zones is underlain by graphitic schist, striking nore or less in on oapt-veot direction and dipping vertically. Uo mineralization vaa observed. The other zono woo located by the ground survey, but no out crops of the conductor were soen due to overburden and enow.

ATtorod b&oic If ve IE bolicvod to bo the main rock type in thearea, with graphitic schists in the southern part. The lava lo cut bybasic dykeo in the 6outhwostt-ii and northeastern portions of the grid.

(A. P.P.* 'B Anomaly U t , Carpenter Lake)

A ground geophysical and ecological survey was conducted on a rectangular area monnurlng cone 1000 x 5'OQO feet, Iho area is largely underlain by a magnotic anomaly discovered by au airborne magnetometer survey carried out. a fcv; yearn BCO by A.O.P.

The napped area 3s bolievod to bo cut by riuworcus basic dykes along a tone- ^00 to 6DO feet wic'e cti-ikinc northwwfitci-ly. *liO southern

(A. C. R.)

Reporl for January Ma,p

o r omaliefi W-"3

- Areasla. - A.J.R. Twp.

v

BAROID 0. SEIGEL t ASSOCIATES, UMItED

. .i* : . ' FRANC* R. JOUBTH 6 ASSOCIATES, LTD.•V- GROUND INVESTIGATION REPORT

The basis of interest in this area was an aeromagnetic indication, known as A.O.P. 011, revealed by an earlier airborne aagnetoneter survey*

A base line 3200* long was cut, oriented due north-south. East- vest cross lines were cut at 200* intervals, extending 1500* V and 500' E of the base line. Every second line was covered by a magnetometer survey at 100' station intervals, olosing down to 25* intervals in areas of interest* After repeats of some of the A,O.P. aagnetoneter stations revealed good agreement. the earlier results were incorporated and used, with a suitable base correction*

The electromagnetic reconnaissance survey was carried out on all lines, except 223 to 28S, inclusive, east of the base line* An interccil spacing of only 200' was employed, due to the proximity of a power 1**** which generated considerable magnetic noise*

A geological report and plan by H&kon O* Lien is appended* Due to 1-1/2' of snow the outcrops in the area were largely hidden*

DISCUSSION OF RESULTS!

The magnetometer survey indicates the presence of several bands of. magnetic iron formation, striking almost due north-south across the entire 9rid Grea* "^ 8ti11 o?0* to the north and south* These bands are all narrow

tt w S J- (100* or less) and do not appear to be of economic interest, at least fork S u. o -V*tl**-o y ou K . w Tilt angles exceeding y are observable only in the northern portion Q w a 5 of the area, particularly on lines O and 23. With the exception of a possible, Q ** vft&k conductor on line O at about ^hO 1 W, the tilts are attributable rather tou . s the magnetite (susceptibility effects) than to true conduction.* O h ulil l t) Q *- The present results offer no encouragement from a base metal atand-D u w point. No further investigation can be recommended.O '- h k0 2 J

oIU O <i J "l Iteopoctfully submitted,H w

e*

(signed) Harold 0. Seigel, P*Etg,

Toronto, Ontario February 19th, 1?63.

y RECEIVED FROM 'ALGOMA CCNTRAl RAJIV/AV RESIDENT C^'-

SAULT 6Ti. M ARIE,

•5

5p

-'^^P

^a

.^::'

";'^

'^??

^s'.-.

••

-.-',-

' -

'•-.

.•f-

' --"'.-•.^

f:'^

".

SJ

•^^ ^

o V c r-

-r ~r ( V

x G K JV,

C,

r,

^

I'-ntm

imrv

-^-:;

-;-t^

: --;.

"'" .

:-:;:.;

'i!"":'

;rf'

' '"

;";v

.' * -

'-'f v

1* .--

-'•"•"'

^

;®lfa

.cv?;'

-;:^

.'st::?.

'v.:-

;S^;

^S

•n N ^ ^

s: ^. ^ w i

Ss

t.^••

fci

•S&'-v

SAULT-ALGOMA NO. l PROJECT (A.C.R.)

MONTHLY REPORT ~ FEBRUARY 1963

The period from February l to February 17 was spent in the Sault Ste. Marie office performing general office work, while the remainder of the month was spent supervising diamond drilling in A.C.R. Township 26, Range 14. The drilling program was ter minated at the month end, and the crew left the area on February 28. H. 0. Lien supervised the drilling during the first portion of the month, but the following report is a summary of drilling results for the month as a whole.

D.D.H. No,

12

DEPTH (Feet)

401.0

Drilling Time(Hours)

67

MoveDistance (Feet)

#2-R.R. 24,000

Moving fe Setting-up Time___(Days)

Location of Drill Holes

12 Anomaly L-13 O -f 50 N A.C.R. Township 26, Range 14 l 4- 70 E

(B.L.#2) (P.L.J2)

Not staked

On anomaly L-13 in A.C.R. Township 26, Range 14, DDH 12 intersected sulphide mineralization in agreement with surface outcrops and the E.M. conductor. Greenstone occurs from O to 131.2 and 236.0 to 401.0 feet. The intervening width from 131.2 to 236.0 consists of a fine-grained gray schist of probable sedimentary origin, containing zones of tiny pyrite lenses in amounts up to 5*. Semi-massive pyrite and lesser pyrrhotite occurs from 136.7 to 13#.S feet and a trace of chalcopyrite was observed from 131.2 to 136.7 feet. Assays for this hole have returned only low values in copper and nickel with nil results for gold and silver. The best sample, Number SA 3-490, returned 0.049b copper, a faint trace of nickel and nil values for both gold and silver.

Sault Ste. Marie, Ontario, March 5, 1963. T. N. Macauley.

ft---'-.

?P ,*

THE OFFICE c;-- r:-,1 E ne::-GEOLOGIST, O^T. DEPT. OF MINES

SAULT CTZ. MARIE. ONT.

iru APR l 1036

RESIDENT GEOLOGISTSAULT STE. MARIE

PH DIAMOND D RILL RECORD*PROPERTY.Av^!k,?.^..2 /,.^ .............,..........:..:'.,,V,.,,,,................HOLE No..,,,......,...l2...

S'iEET NUMBH.......,...,,,........ . . ..., SECT.ON FOOM .

DEPARTURE.! . 70 ii (O, L. #2) . MAIING . . . .N.55.0 W.

ELEVATION................... ....... ........................DIP...... ....... . ."...M?.......... .

.COMHETEO

UIT|MATE DEPTH

.PROPOSED D fPTH... ...............UOO..f.Q,f

DEPTH FEET

0 - 13. *

13.5-62.!?'

YJ . i-lt^".t(j2. (;^o

w

FOR MATION

O.;;iii ; - J'r.olucting a 3' ...iTidto boulder

u:t ,.':;,' j'i( v. r .J - i(1 ln :-;^'''i.ncfl, ..-c j -l.ch-i'irecji

Oocv-.' ' :1. Li li/ ','iilto CIM. . ;alcHo

sti'.in^ors at all rubles c.-- rising veiy

rare speck of pyrite, V.V'.'cly sclitstoso

at } l. at W Q to r - :s, /.f tor 3h more pa

f-TOi. a "'.oration •'•; "t;; and spreading

outvor" '- i "•••••••i , 'i'l.foo i" quart:

strin-ors .;.;U;.^ ; 7^0 -. ~ '5'.0',

scj.:r;'j' - ; ' ' . . ' ' ' ; -and v.'!: i: i ' .'.ci i 1 . CL. ' -.l ) .o0 i, o - tf .

SAMPLENO.

1.

Le

FROM TO WIDTH AuASSAY

Ag

VALUES

Cu Ni

f no 7 ''"! i* '

DIAMOND . .DRILL RECORD.. *

6,,J^^^^

SHEET NUMBER........... ...i?.,........ ...........................SECTION FROM , ..^ P...,.......... . ..TO , .,..*?"*.7.L,,...,

..12..

.............STARTIO...................

LATITUDl.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, DATUM,,,,,,,,,.,., ,,..,,,,,,,,,,. ,,.,.,,.,,,,,,,,,.,,,,,,,,,,,,,COMPUTED,,,,,,,

DEPARTURE,,,, ,,,,,,,,,,,,,,,,,, ,,,,,,,,,,..,,, BEARING.,,,,,.,,,.. ,,,,,,,, ,,,, ,. ,, ,, , ,,, .................................UITIMATB DEPTH,

EtEVATION ,, ,,, ,,,,,. ,,,, ,,,, ,,,, ,. ,. ,,,,,,DIP.,,,.,,,,,,,,,,,,,,,,,, ,,,,,,,,, ,,,,, ,,,,,,,,,,,,,,,,,,,,MOPOSID DEPTH,

tDEPTH FEET

f

8^.0-109.6

'

109.6-D7.5

117.9-131-

^

J31. 2-336.7

FORMATION

ORE:i:-3TOMK - S?;ao as above. Dark groen

to grcyi;;h-crocn, Canie pale stringers

and alteration at fractures. A 2" quar

vein at 88,9' at 1#0 . A 5" scixistose

chloritc-bjotitc j;one at 103. h 1 at 700

to core.

G!?'-: ,::SiOKn - Co:.plotoly altered. Pale

erocr., '..'o.-v 5o0 .ociilstosity.

G,lv' f '..0;,r .' - :,r '; im-ous will to Gtiliifiors,

Weak . ' 0 .' ' -^'xijilty.

SCillul1 - i''j\.--i;raincd j /-jroyisli-yi-eun,

SAMPLE MO.

'Z

FROM

,,

TO WIDTH

1

Au

ASSAY

Ag

VALUE*

Cu Ni

HQKIHlKH H INtH 301 HCV lit

Canadian

c.)DIAMOND DRILL RECORD

^C.J, T^ No

SHEET NUMBER....... .... ,..,3....... . ,,....,...,.. .. .........SECTION fROM ,,13,6t 7. 1 ..

LATITUDE.,,,,,,,,, ..,............. .....................................DATUM................................ ,....

DEPARTURE.,,,,,.,,,,,, , . . ,, ,,, ,,,, ,, ,,,,BEARINO.,,,,,,,.,,,,,,,,, .

..STARTED.,,,,,,,,

.COMPLETED,, ,,,

ULTIMATE DEPTH,

ELEVATION ,..,.....,,.,,.....,., ,., ,,.,,,.,,,,,,, .......DIP..,......,.......,,,,,,,,....,,,..,,.,..,.,., ,,, ,,,,.,,,,,.,,,,,,,, ........PROPOSED DEPTH,

iDEPTH FEET

j

'

uy-woo1 ri

NONTHCftN

FORMATION

hard and soft zones, few quartz blobs.

About 5,* sulphides (pyrite ft pyrrhotite]

as s:r.all seojns and ve.ino up to 1" mostl)

parallel to schistosity at Ii5o-700 to c(

Pyrite in these veins occurs as euhedral

crystals surrounded by pyrrhotite, Few

tiny spC'-ks of chalcopyrite separate

from other sulphides, SAMPLM)

131.2-136.7 S/'lii'fai 30 31cm. seid. -quan titative'

Slia-1'J'.SSTVi'; SUI- :'- ' ,S - About 50^ sul

phides in r.chl^t -r, v-l.ns and lenses at

70-OQo ^ 0 C or0t atio pyrite; pyrrhotiMINCK FOAM 191 DCV./I4 3*1

Canadian Ion rri,rcnr

SAMPLE NO.

re.

SA3-1490

0 a

*.t',\

FROM

131.2

. f.

TO

136.7

H. Mac*

WIDTH

i

5.5'

wloy

Au

nil

ASSAY

Ag

nil

VALUES

Cu

o.ol*

Ni

.DBAMOND D RILL R ECORD^ No..,.,,,,,,,

SHEET NUM8E*.,,, . ,,,,,5,,,. , , , , ...,. , ...... .SECTION f*OM 152.5 ' ................TO. . ,..,r!:7?.*P..!......,...............8TAITIO.......................,.....

LATITUDE,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,.,,, DATUM.............. ,.,,,, . ,,,,,.,,,.,,,,,,,,,,,,,, ,,,,,,,,,,,,, .........COMWITIO........................

DEPARTURE.,,,,,,,,,..,,,,,,,,.,. ,,., ,,,,,,,,,,.BEA*INO,,,,,,,,,,,,,,,,,,,.,,,,,,,,,,,,,,,,,,, . , ................ULTIMATE DEPTH.,..,,.,,

EIEVATION ,, ,,,,. ,.,,,.,.,,,. , , ,,,.,,, . ,,,,,,. DIP,,,,.,,,,,,,,,,,,. ,,,, ,,,,,,,,, ,,,,,,,,,,. ,.,,.,,,.,, .........PROPOSED DEPTH .........

1 '' - t - ' v *Ci " ,"'' '"'*kVs'

DEPTH FEET

152.5 - 159.0

/2^o•.o -

179.0

FOR MATION

at 600 to ?00 to core, y/, sulphides.

1" quarts vein at 151.0 1 . S/d-IFLfcJ)

I)j7.8 -.152.5' t-JiPM!

SCIfCST - Fino-^-raincd,, ci'ey, uitLfonn

schistoaity at 6o0 to core. Tiny con

formable sulphide lonses, both pyrite 4

pyrrhotite. 3;5 sulpha. S-J-IPIJ-D

i,' rt r- , -^ ^ 30 Element scml- 11)2.5 - 1^.0' SAMPLE quantitative

SCHIST - Grey, hard, fine-drained, miif

650 Bchistosity. This rock is ^-obably

SAMPLE NO.

SA 3-1423

SA3~h2i

)rm

FROM

11*7.8

152.5

TO

152.5

1?9.0

-

WIDTH

14.7'

6.5'

ASSAY VALUE*

Au

nil

nil

1

Ag

nil

Cu Ni

HQHtHtHlt P INCH rOnU tot KCV./I4

m,,,, tr Ctuwdiftn Lwuaroar t ie. rft T. N. Macauley

JSf *-,V'."i''"l'W: v

1 t

DBAMOND D RILL R ECORD

26j...Range...lit,.,;Anomaly...L-rl3,,,,,,,,,,.,,,,,,,,, HOLE No

138.8' T0SHEET NUMBER,,,,,,,,,,,.,,,,,.,,,,, .SECTION fROM ,...

LATITUDE................................................ .....,.............. ...DATUM . ...........,,.,....,......, ...............,.............., ,....... .,.. ................,.. .COMPUTW.............

DEPARTURE........................ . ,.......... ,. . ,. . ..., ... . . . . BEARING. .... .............. ... ,. ,. . . .....,.... .......,...,....,.....,,.. .......... ,. .....ULTIMATE DEPTH...

ELEVATION ....,,,,,, ,,,.,,,,, ,... ,,,.,.. . ,,,,. ..DIP,.. ,..,,.,,,,,,,,,,,,,,, ,,,,...,,,,,.,,..,,,.,.,,,,,,,,,,, .......PROPOSED DEPTH.

DEPTH FEET

136.8 - Hl2.5

Ui2.^ - Ull,.8

^

UiV.6 - 152.5

FO R MATION

136.7 - 133.8 S/O-IPLS 30 Klcm. somi-quajititativo

l!tf'2';i\ST01-,rX .- i'Jujuerjpus zones and stringer;)f pale [j.rcen alteration (silicification'

Trace of pyrrhotite.

vSCiiTST -^l^.no-arainid, grcyiahrfiraen.Massive pyrite vo.lns up to 1" vrido andalso dicsc-Minated lenses at 600 to core,

Trace of pyrrhotite. 1#J sulphides. SAM]5 !

Ui2.5 - .T.7.0" S/d^i'LS 30 blew, sonil-quantitativo

SCJiTST - ',;lflo]y scattered pyrite lonsos

SAMPLE NO.

SA >U51

).

tS

S\3-U92

FROM

136.7

Hi2.5

TO

138.8

JliT.Q

WIDTH

2.1'

i

5.3'

ASSAY VALUES

Au

nil

nil

Ag

nil

nil

Cu

0.02

Ni

NOHTHCHN MIH(* fOKU 1 01 DCVVI4

,. ,,,,. ,, rv- n ".r H P n T^n-yo^r ,. T, N. M-ncnuloy

t) -DIAMOND DRILL R ECORD

'^i:...^^.?,,^,,*^?^,.?^.^ ,,,,.,,,,,,,,,,HOLE No.,,,,

SHEET NUM8ER ,,,,,,,,,,^,,,,,,,,,,,.,.,,,.,,,....SECTION FROM , M?,..P' , ,, .TO ,, 221.91,, . ....STARTED,,,,,,,,,,

lATITUDE,,,,,,,,,,,,,,,,,,, ,,,,,,,,,,,,,,,,,,, DATUM ,,,,, ,,,,,,,,,,,,.,,.,, ,,,,,,,, ,,,, , ,,,,,,,,,,,,,, ..COMPUTED,, ,,,..

DEPARTURE.,,,,,,,,,,,,, ,,,,,,,,. ,,,,,,,,,,,,,,BEARING,,,,,,, ,,.,,,,,,. , ,,,,,,, ,,.,,,, ,,,,..,,,,,,,,.,,,,.,:UITI*UI( DEPTH.,

ELEVATION ,,,,,,,,,,, ,.,,,,,,,,,, ,.,,, ,,, ,,,,OIP.,,, -,,,. ,,,.. ,,,,, ,,,,,..,,,,,,, . ,,, ,,,,,,,,,,,,,,, , ,,PROPOSED DEPTH,

iDEPTH FEET

*

179.0 - 187,0

107.0 - 212.0

212.0 - 221.9

-•—i

FORMATION

a metamorphosed sediment. Trace sulph

ides.

SCHIST - Same as above. About "# pyriteas fine -conformable lenses. SAMPLED

179.0 - 107.0' S/jMPIfi

SCHIST - Same as 'above. Occasional zoneup to l' Ion;] of similar pyrite mineral-

ization.

SCHIST - Sa;,io as above. Untfonn lenses

of pyrite up to 1/16" vddo (1#) parallel

to t ho 650 cclnstosity. S^-IPLi-D

SAMPueNO.

SA 3-li2

s

FROM

179.0

TO

187.0

WIDTH

8.0'

ASSAY VALUES

Au

nil

Ag

nil

Cu'

NL

NOHTHCKN MlNCH rONM SO* X IV II.

DXU.ICO 9 1.Canadian T. N. Macauley

D DRILL RECORD

" :

PROPERTY.,,,,, A.rC.vH...To:wns)i^ ,,,,,,,,,,,,,,, HOLE No.............. A?.,

,, L.,,, ,. ,,,,,,,,. . ,, .SECTION FROM ,,,?2^. 9' IO , 26.6,0 ' . .STARTED ,,,, ,,,,,,,,,,,.

,,.,,,,,,,,. , .,,,,,,,,,..,,,, DATUM ,,,,,,.. ,,, , . ,, ,,,,, , ......, ,,,, ,,,, ,,,,,.,.,,,,, ...COMPLETED,,,,,,,,,............

SHEET NUMKER,

LA11TUDE,,,, ,,

DEPARTURE,,,,, .,, ,,,, ,,, ,,,,,,,,,,,,. ,,,,,,,. BEARING,

EUVATION ,,,,,,,,, ,,, ,,,,,,,,, ,,. ,,,,,, ,,, DIP.,,,..,

..ULTIMATE DEPTH.,

. PROPOSED DEPTH,

DEPTH FECT

t

i221.9 - 267.0

257.0 - 236.0

-•-

FORMATION

212.0 - 221.9' SAi-d'IlS

SCHIST - Sa:nu as above. Sulplucies veryrare, Cricn slips and alteration at 239

and 2iJ3'. Kaint wottling in places duo

to quartz or feldspar grains.

SCHIST - Gradually becoracs more finely

laminated and variable in colour. B"ino

black lar.tLnae are not magnetite or gx'ap

ite. Consistent 650 schistosity, Quito

.t few open fractures from 2?6 to 206',

Pyrite .'.•. pyrriiotite vcinlcts and specks

at 20^.0 to 206.0'.

SAMPLENO.

SA3-'i#

i-

FROM

212.0

TO

221.9

WIDTH

9.9*

t

ASSAY VALUES

Au

nil

1

Ag

nil

Cu ML

i

fi J HCKH M l'KH fOtM tOI mv./K

! Canadian Lonmrear T* N. Mcauley

DIAMOND D RILL RECORDPROPERTY ^*P*?* Township 26, llange lli f Anomaly L-13 HOLE No. ^

SHEET NUMRER,,, ,,,9,,,,, ,,, , , SECTION FROM . . , 286.0 |. t .IQ ., . 3.75.*.Q.' . ,, , ....STARTED,,,,,,,,,,,,,,,

LATITUDE,.,,,,.,.,.,.,,,,.,,,,,,,,,,,,,,,, ,,,,,,. DATUM,, . . ,, ,, . , ,,,,,,.,,,,.,,, ,,,, ,, . ,,,, . . , . . . .COMPLETED.,,,..,.,,..,,,

,,,,,,, . ,,,,,, . . ,,, , , , ,.,, . ..REARING,, ...,, . ,,. ,,,,, . ,, , . ,,, , ,, ,,,,,,,,,,. ,,,, , .....'.....ULTIMATE DEPTH.,,,,,,,DEPARTURE.

SAMPLE

NO.FNOM TO WIDTH

ELEVATION ,,,,,,, ,,,,, , . , , ,,,. ,,,, , ..DIP,, .., ,,,,, ,,,,,,,,,,. ,,,,,,,,,,,,,,,,,,,,,,,,,, ,,,, ......PROPOSED DEPTH.

DEPTH FEET FORMAT ION

^j .

-JPllP-- ^-'^•SYOff^ - Finc-^rainod, scldBtoso

___ sections at 700 core angle. Numerous

white stringers at all angles. A 2" qua

_____ vein at 320.0'. A -|" zone of pyrrhotite

veinlets at 32)j.2'. Schistose and li" cal

cite vein at 328.0'. Brecciated 4 trace

of pyrite and pyrrhotite at 33h.5'*

337. b ~

te72"--

- Grey, Feldspar pheno

crycts (v/hito) up to 1/8". Sl±cht3y

schistose.

f:-!',; .i['jYOiji - KJ no crainod. Scltistoso )a o v/ith some brown biotite throughout

ASSAY VALUES

l MINI* fOHM JO* HlV/14

Canndinn lowyear T. N. Macauley

t

ILL RECORDt .

PROPERTY.,.,,........Ar?.^.V..^^ No.,,..,,,,?:?..

SHEET NUMBER.......,,. ,,.,....?.,.,, ,,,, ,, ......SECTION fROM ,..,3.75*.P.!,.,.,..,,,.TO., ,...,,..flPJ!:*P.!,.,.,...,,. .STARTED,,.,......,..,....,,,....

LATITUDE.,,

DEPARTURE..

........DATUM ........... ,. ........,............................... ......,..,.,...,... ........ . ...... ..COMPUTED., ,,.,.

........BEARING.,.......,, ,... . ,......,.,,,.,.,,......,......,..,,..,...,.. , ,....,,. ,. ...:. ULTIMATE DEPTH.

EUVATION ,.,,.,.,,,.,,,,,.,,. , . , .....,, ,,,, ,,,.DIP, ....PROPOSED DEPTH,

DEPTH FEET

'

37S.O -

1401.0

,:*

i

FOR MATION

at 6o0- ?i) 0 to core. Numerous tiny whi

stringers, occasional quartz blobs.

G;t.v::3"ONh; SCJilST - Sane as abovo excep

for more scliistosity. A 2" shear with

red voinlets at 382.3'. V.liito stringcx'.

and altered patches coranon.

KilD OK HOT,'*:

Notes

1, Size of coro - AXT2. Casing pullod out.

3. Core recoveiY - excellent.li. Drilling i.vitcr v/as "lost" at about l 5, Core utorod at drill si to.6. Coro boxos used - 16,

SAMPLE NO.

.e

00'.

FROM TO WIDTH

ASSAY VALUES

NOKTHCftN WINCH fOKM td IKV./I4

1 o im ,, o, T Canadian Lon/xyoar t tlitttt) T . N. Macauley.

DLDH. No. IE

LEGEND

/- xG reen stone

, probably

Fft|d s p*r

ASSAYSSECTION OF D.DH. NO. 12

PHANOMALY L-13

13(2- I5C7 l 367 -

|4Z.5- (475

S A "3- 4905 A3-

- 492.ACfc TOWNSHIP 2.L R-ANGE 14-

OF ALCSOMA, ONTARIO

SCALE. l"- 40' MAR.C-H . 963

i\7ZO-1870 2.IZ.0-22I.9

Anomaly # 13*

Batchewana Area #13.

Location, See Batchewana, Area # 13.

Work - A base line was cut at an azimuth of 31#o for a distance of 2000' north and 800' south, the station 0+00 is 500'; east of the north west end of a small pond south of the : i anomaly. Cross lines were cut at 400' intervals.

Magnetics - The magnetometer survey indicates a band of magnetics about 40' wide lying generally south west of the base line. A small pocket of higher magnetics was encountered at 500' west on line 8+00 N. the highest reading was 68 , The high readings are thought to represent a small band of iron formation.

Electro~map;netic Survey - Two parallel conductors were encountered (see map) the angles of dip associated with the X-overs are rather good and would appear to represent something

- besides a contact relationship.

Geology. - Some rock exposures can be seen on the property, theseoccur for the most part along the south east side of line 8+OON on the south west side-of the base line (see map). The anomaly is composed mostly of diorite . A few outcrops on the 8+OON at the base line appear to be argillaceous. A diabase dike about 60' wide was discovered, it strikes generally north. On the line Si-OON, 500' west there is a cliff from which some samples running 8-10,3 magnetite were taken.

Conclusions * The anomaly definitely warrants further investigation.

U.R. Venn.

This anoroalv was examined the following spring by U.R.Venn As no outcrops were exposed close to the main magnetic band the true cause of the magnetics could not be ascertained.

U.R.V.

- • ••- '•'•''t.'J^ :-'-: : '^:^:.^: : '* f ,\"- '' '•'• :- '-^ ' r ' "•-'•' " r ' -^-;.!'.o : --'^^ v^ ' V: :' s ':

•?-'" -i;': "- ',' •.!-"'". *,'': ; "' ••'•".'•'"'ir Ji^.;Jil ii^^faft

m:'

ANOMALY f 1 2. BATCHEWANA AREA

Location - See Batchewana Area #13.~ ———

,-,v .*^"?wy^av'Sv^iySi^i

-- Work' -. t ' . -~ ~- n

- r ~ , :' " '

..V^;v''^;'':

;J:"i

.'. . .A base line was cut at an azimuth of 346O for of 2000'. Cross lines were cut at 400' intervals. (See

The Magnetometer survey does not reveal any magnetic ,: concentrations of interest. " - .• ;.---y- ; , :'

.-. .-- ., . . . .•.-,- Electro'•Magnet i c Survey - A conductor was encountered on the west ' -

* side of the base line, the cross-overs appear to be very weak, ,: ' except for the one located on line zero.

frt/^H ;'.. ; ".l Conclusions - The complete lack of any magnetics associated with*'.' the conductor axis causes this anomaly to be very

. disinteresting. It is not advisable that more work should be done.

V.R.Venn.

This anomaly was checked the following spring. No reason for the magnetics or the E.?-', conductor was found.

V.R.V.

HAROLD P SEIGEL ft ASSOCIATES. LJMITEDPROJ ECT *M*g A. JOUBIN a

MAOMETOMETgH

LIMIT* OF IRON FORMATION

^

HAROLD O. SEIGEL * ASSOCIATES, Li Ml TEDPROJECT : nwc *- -*3Mwa ASSOCIATES .LTD CONDUCTOR l ~ 9SURVEY jSCALES '

i"- loo'i"- jo* tifcr*ctu*

*ccttTW***I*|TT1* .-- — P - — * —— ^jf-—-

HUDMNtfTVBI LOCATION /JAPPROXIMATE L IMITS

OF IffOft FORMATION

20-1-63

J -J

OQ-4

T jO -J

j'V.'j.

B

au

V

e

r

o*

.*o

f/

'f

sS.'

CO -

Franc. R. Joubin l

ANOMALY L"

of i* r 1 .'f.

33 - ci

H O

..., -i...

V.

.1

i

L Z Z 3

rt*M ri

-II

TF*

A* F

1*1*

W*

l**

•73TM

-i**

rvf

r-**

Ut

r- .1

•\

A* s

tn

tit

. r**-

TTf

11,1'r** i***.

TJW

-rir

ITT

ri T

l ^ .

— * rr* .^

f

f* 9 *T**

lit*

r* k

TIMf

V

y yt***

J*-*

M?

t f Z

J" lJHt

9*3

i*t*IT'1

/i**

111 I

Mi10*

i*

J 7Vt

14 11

1**'

'•rf

Jt**

i; *"*

*H

M*.M7H

JTf

Z*.

tt ID

•l 7*

1*1*

10

t. HE f

Jtl^-

940

/JLJ"

.t reT**

: n

H -ft

"

i.

v

i-

A. C. R. TWP. 26, RANGE 14

Hj?LROL O- SEIGEL 5 ASSOCIATES, L IMITED

PROJECT : FRANC R. JOUBIN ^a^ASSOCIATES, LTDCONDUCTOR : "L^TO"^"^"IHLIT I ""IZT SURVEY ;'"MAGNETOMETERScot**l". 200' J"l" - (OOO 0*MMA3 l inch " l" *2000 ~"~ 2 ln*hM

Mag. SurveyLtVtt

fJEMOVEO MOM OBStH\rtDVALUfS

IfORK St0. T.

PLOT a. T. Olff*J4N 2A f *3

l

i 11*)

ir;

. 4*nM L

oiti -A.l8) t -** f)

-fKOfd

-* ' 1

* f-pr . , ,,^.

* , j.. *.

? . 'r - ' .

0 ' ' ' , ?\c ^ j fT A" ^CR T^R 2*, RANGE 14

——— TT—— —— ' —— -—— -" ———— —— —— * ——————— ~*-. t*iv-.,t*i#yf*-~*~mfi*Vi-**.~*~.m~.'** - *y-. *- 1, .. ————— y'-.—. f** . - y** "••4w:i m'**^l ' ^. i -P* n^"'"- ' tx'"-**"**'^

HAROLD 0. SEIGEL ft ASSOCIATES, LIMITEDti r

•* '

PROJECT: FRANC it. ^ouwii a ASSOCIATES. LTDCOWDiX^TOR- L- 109URVEY - E . M

Scot**:I**( 2OO' ,

1* * 20* (C Ml

f i i '

E. H. S*rv*jr JWMUU-fL HtQCt " —— -* ——

COKVCPTTIOM Ptc^rH TILT* c^ -: ' Trtf t49T 3rt)t C

HOt 9V f MTt V-*- : J*M 29/ti

j i

'

i

. M

\

i -

ir?

"W

/

ftc

\Ml

A/tM IMtf 41& - -A ——~ --.——H*.--

n*m

•It

•1C

-4

•C*

*: * ' ' . '

'* "^ 4^'.;

tcv

-. i- ,'f^

K f v Tf'. - i \.. *"i —f-*' "

b

HAROLD O. SE1GPL L ASSOCIATES, LIMITED

z- /3

r rI** \* S

T l

O***

AMI *******M**

't

r i.* T

*?

^^4

^M

.•* V

..*--

Vw

?'-5

*:.flA

vWw

't-*^-'^:*

N

!T

S

5 S

-

* -

* ;

fi 6

^

*

© i r

t* 'x^~^ —

*~J~^ '-s:,

- *-^

-' ^^

^

' t

f1

*" j

^

S

*

T

-*| "3

x ^

^

^ :

^i

s *s

-fs a f

3^

' *

f ^

e?

—^

^^

^ —

— *

——

— I...

ir V

t

•— ' -.

1•4

V

*.

* 3

5 ^s

s !; S*

^ a

'-- s ^ 1

s/ve/ 7

, ——

^^ — —

— r- —

ii4 t

•™w

^•*

* x

^ 4

* 7

t 4

* Y

*

™

T? J

'

i^

3^

4

|,

i Wl

l*v ^

* w

* *

". ~

\ '

A^~X

ft ••-" """

" ^

^-^

-rf-"-*"*"

~"~1"'^

y J

. . ,. v: —

"-"'•*

- . '

* .

*-'

' -

. ' - "

. V?' -, -, -

*- ;

*- -

"-- --

' -* -.~.

-"'•"-- * '-""p1 -f -'~' . * " "" v."* V"

" '. "*

- "* -

v " '

. "

: '

. *

.

* t.

? t

"*"' 9 I-

* ? ?

v' S * S

3 --e*

j i\- 1

t ^i

^v i

^•*

•^^^ -

^ — "* .-

. ."^*^-^ .?

T

^

^

,

V

J f K

-

^J

^

-^

' -4

-

'

' "

' -

iV

,

^

.

-., ^'-••. -*-' :',;'-^-.-, - -. -

,,'u

^-;-

. . '

* "- \

*~ ;-

' *'- . ' ;

'. - - r- ^

.^'

"' -. , '

.'

- '

Oi~

*:*

- ''

"' -. -,

' '

^f-v

-'-r ,-"ir-.

' -

-' "

*' '

' -

' -

" -'

"' f .4

' t

J

' 3* '-

V *

"'

i i ? i i T i i i i

——

— : —

——

——

——

——

——

——

——

——

'^p

^^

*"^^

^^

^

——

——

LI— -e

i•*.

*- T — .^--

- ^^*--,

. -^^^

-* '

-"^ l1 1

' ' -- - -

* .

* .

* '

i !

l! lil

I'll

W v

N

.v^v^^jf^

st

*. ; ^y.i*t.A

*-V^is

r

-t-doQG

—

. Q.

.-Oc

Q

-?

"^ d

0^

" — ST ;?

i t

i j

*STi "CI

5'! ft .

tt-

\x•x

Q00

t

--—-•i—

r

i^t^ ^*ii" 2ST

* ^

c\ o

; i -jj

i

-f- L-f—

U

e. : 4 r-

n

oK (U

\

X^Lx^

\ s/1

^^-^.^\v

'^+

S

" -^~

' ,

"l-V

iv-

^5•^

— ~V; -

M , te.h e

ALGOMA CENTRAL RAILWAYGmo/oo/ca/ M a- f*

Mo. t, 5h**f 3r

: t "-ZOO"- -:' t

S -^''^y

41NB1NW9210 63A.500E TRONSEN

*W v* -- - f- *- - 5

J

l

2 4 35"* O l l l

-Z O -Z

1410

1*40

(340

IZftO

JOtt

M.

910

13 W) x-

0

UN t

1547

1447

J496

1 33 w -- **^,- — ""—— —— M 0^

'---"""x ^

l*?4 ^^^.x x^^ ** x

** ^, -^'*

rt'O ^Hono^", '-?/' " , ^^

S; \l^-:^ *?*#'' : ' '' "3087 ^ '~'^2,Z " '

3ft85 ^tJZ''~'*ff'' ~

ItS

Ifc4l

I&S)

ri92

(197

1493

- -" " -* — - ^^2LBB ~~ -* — — — — — — — —— __

*-

- ^ " ^.^ ^' ^'"'*w --^:^-5 s'''-'''4./ QjJ "*— "" t*"" s^ r "^f ^ -*^ ~ "1 ^ jr ^

90*3 s" r*^'^'4407^-^ jr**" S

JL.4'9**' ^ ^ S "^jSSJpf ^ ^402 ^ '

1575

It 68

1622 ^-^"*~" "7-x ^

--- — * "^ "^

1959 ^— -^- ^ - aooo -^ -""

(Alt

1900

U4t /X 1694s

ss

' ' 'j . , '

rzoc /' * X /ri f fe , /f

, S f ff 949, .' x x

( f ' '

'A \ 'O-v x s ^ ^ -1

^ V ^ "1^..

I4W \ ^ s '~ ~ ~^^ s ^\ \. f\ ^ v.

J4A9 "^ v S

^-^ "^ ^ ^-x.

*92 ^ "

"2589 -^

s.

^^— ^^-^

~~ -- xJX. k

r ZW3f

1541

i A li Q1^1*7

ISH"^ *p*

^W*7 " "^ - ^^^. *^*fc "" *~ *- — — 9^W)Q ,.

^"^^, "" *— s. AWW "~ — — -^.^ — .^,— — — —

""^--""^^•- 25*o — -^ -^1ZSB "* — — - *.-

5657 __ ^-"'5000-^ ~~ ^ - - '•P**** * . ~ -- ~~ — if^ ~*

— — 10OO — - - ^ "

' 1497

1569

I58Z

/vy*

JM9

1746

1 R2.O1 OAA^

17*

1756

~~aXjw — " ~" "" "- ~-3O52 ^i ^

2068 ^^^. - - '

1^0

J932

1732

1^9

I7U5

1 4*5 i r y r- 1 St.1*

)4^fi1 **

ISOy

155)

1533

! Slfc

w15^1

ISfcl

J 6 1?

15*

1547

B 43 LIME. 66 LIME, I2S LIMB It S

ALGOMA ORE PROPERTIESBATCHAWANA ANOMALY N*llDIP NEEDLE AND MAGNETOMETER SURVEYSCALE 1 - 100' t, A J?^^f" — " JAN - l 960

^^^^f&lSLtA

COPltD MAR. M. R DIOTTE

I4W

149*i *"*

1490

1452

CACf *9v

IXAJS

149ft

1499

J5SS

ISM

1522

^LIME20S LINE 34S LIME 70S

T'SPAMQrM AAIA * IA

41N0)NW92ie 63A.5S10E TRONSEN 230

/

\\

20+CXiN

A Aft fi LIME. AX.

/

R.EM. SURVEYBATCHAWANA AREA

ANOMALY N e 12———— I0OO C.RS. READINGS———— 500O C P S. READINGS tf* CON DOCTOR AXIS

SCALE T* 100* f"*IO*

JAM. Itt, I960

COWED MARCH '62. R. DlOTTE

AOP 34OZ p

\

r

\\x

s s

/'4

\\\

s

o too

41N01NW92I0 63A.5C8E TRONSEN 300

RASE L l M E.____A2. 3lg*

\\\\

p\\

ANOMALY * 19

R. E. ML SURVEY

JULY IV.

<

12+OON StOON

N

4+OOM

———— IOOO C. R f. ftCADINQf

--- 5OOO C-P.f- READING*

^* CONDUCTOR AKI t

SCALE r-wo* r- ID*COFIEO JAM. 62. R. DIOTTE.

A o P. -3405

0*00

/

(

\00 S 8*005

41N01NW9210 63A.590E TRONSEN 310

Kl

4 4

720

tsoo

t —

O 5

Z O

l

MA

GN

ETO

ME

TER

S

UR

VE

Y

BA

TCH

EW

AN

A A

NO

MAL

Y 13

E. M

. C

ON

DU

CT

OR

A

XIS

DIP

N

EE

DL

E

JA

N.

20,

CO

PIE

D

JAN

. 6

2.

A O

P

3 4

O 3

4120

74

00

14*0

0 H

R.

D10T

TE

GAB

BRO

- D

IKE

DIO

RIT

E

3~1

AR

GlL

trrE

f P

AK

AG

NE

ISS

)

3 O

tO

J/fe

O

Z52

0 3/

2O

2180

3

l SO

32

00

S3

20

3280

3380

3260

2440

3060

4^0

0

3060

2640

332O

3420

35

40

2 39

20o t

oo4 4 6 2

322O

•334

0 Z

920

31 6

0

J 820

26

90

Z?

60

2860

2.46

0

3040

3/

2O

304O

4 f 0

0 S

2960

- 3040

3060

- 32

40

5660

38

60

35

60

33

60

2620

32

6O

2760

3(

80

Z92

O

2860

298

^

2840

2.

680

• +

OO

*

4 O

BEA

VER

D

AM

-S-

41N0INW9210 e3A.500E TRONSEN

32

0

GEOLOGYCARPENTER LAKE

ANOMALY 14SCALE l" s 100*

COPIED MARCH'W* R.DIOTTE

AOP 34-O4-

z -43 s 1 GOODr^

a

Iotsl

P W

LEGENDGRANIT1Z&D SEDI M e NTS - GRftYWACKE, ARKOSE

SOME RYOLITCS

(ROM FORMATION

GABBRO

I.F-

Oo4- 00

oo

3Oo4- 01

.72'

l FT. WIDE

AZIM- l Oft"

o o•*-09

Oo•4-

Oc

41N01NW92I0 63A.500E TRONSEN 330

CA

RPE

NT

ER

LA

KEB

ATC

HA

WA

NA

A

RE

AA

NO

MA

LY

H*

14IO

OO

O

PS

R

EA

DIN

GS

90

00

C

P6

RE

AD

ING

SC

ON

DU

CT

OR

A

KI f

t

SC

ALE

i

DE

C-

15,

1759

CO

PIE

D

MA

RC

H t

2.

R.

DlO

TT

E

AO

P

34

O4

-41N01NW3210

63A.500E TRONSEN

o o * tf c*

-l

-l

-l

-Z

Oi

-8

-I

-3

CA

RP

EN

TER

LA

KE

BA

TCH

AW

AM

A

AR

EA

AN

OM

ALY

N

* 14

JAN

. 1*

60

M.

CA

RT

ER

CO

PIE

D

MA

RC

H

'fc2.

R

. D

IOT

TC

A O

P

41NaiNW9210

B3A.5e0E TRONSEN

350

206

24O

1921-

144- i-

120 "

72

48

O *

24 1"

46 ^

72 H

10

41N01NW92ie 63A.S00E TRONSEN

J-li

360

ANOMALY KJ*I2BATCHAWANA AR&A

JAN. 20. I960,

MARCM '42~. R.OIOTTTE

l IZ

j. Z

,00/0 *[1