GEOPHYSICAL ENGINEERING LIMITED€¦ · TEL; 416-3(2-1571 TELEX: 02-39087 March 4, 1977 Mr. L. Oliphant, Algoma Central Railways, P.O. Box 7000, Sault Ste. Marie, P6A 5P6 Dear Len,

41N81NE0001 DAVIEAUX29 RUNNALLS 300

GEOPHYSICAL ENGINEERING LIMITEDSUITE 4900 TORONTO-DOMINION CENTRE P.O. BOX No.49 TORONTO, CANADA MSK 1E8

TEL; 416-3(2-1571 TELEX: 02-39087

March 4, 1977

Mr. L. Oliphant, Algoma Central Railways, P.O. Box 7000, Sault Ste. Marie, P6A 5P6

Dear Len,

Enclosed is our report no. 578MB, dated November 22, 1976 for ACB lands which were held under our agreement with you dated November 15, 1974 as amended.

Please accept my apologies for our oversight in not sending this to you at the time.

Yours sincerely,,GEbPHYSIGAL ENGINEERING LIMITED,

/'

John L. May, President.

JLM/cs encU

rt.

41 Ma 1NEaeei DAVIEAUXSS RUNNALLS 010

INTERIM REPORT

ON

-

EXPLORATION OF A.C.R. PROPERTY

FOR THE

DIGHEM SYNDICATE

N.T.S. 41 N/l

Geophysical Engineering Limited

North Bay, July 23, 1976

•r,

SUMMARY

Follow-up was undertaken 1n the period May 1st to July '

10th, 1976. Many conductors which looked poor on the Dlghem map

were slated for follow-up because of their presumed relation to

long horizons of felsic volcanics reported by the 0.D.N.R. and con

firmed at several locations by our reconnaissance. Further work by

the O.D.N.R. and our preliminary reconnaissance of many of them

now Indicate that the felsic volcanics are located 1n three areas

while the long conductors can be correlated with quartzltes. This

change 1n the geological Interpretation makes the exploration of

these long conductors no longer justified. However, two short con

ductors near areas of known felsic volcanics, still remain unexplained

and are recommended for drilling.

(D

LINE MILES FLOWN OVER A.C.R. GROUND

GROUND INVESTIGATIONS UNDERTAKEN

CONDUCTORS LOCATED BY SYNDICATE ACTIVITY

Explained on Surface

9C-11D, 14A, 31B-33A, 31CDE, 55E

55GH-56E, 62DE-64E, 79A, 84C

Unexplained but rejected due to geology

14B, 17BC-19C, 70A-71A, 82B,

85A-87AB, 90A .

Unexplained but further work necessary* . t

39A, 40B . .t

CONDUCTORS NOT LOCATED

37AB, 84A, 84B-85B

CONDUCTORS EXPLAINED BY OTHER COMPANIES

9CD-11D, 10AB-11AB, 52E-56C,

72C-77C, 75A-78A

CONDUCTORS RECOMMENDED FOR ADDITIONAL EXPLORATION

Diamond drilling

39A, 40B

335

17

;: m^MMSL

^ ;

v .r ; ..;; i-yivf^yi." w

' . .-..- . ' " ; 'V)i-il^^

DlGNOt SYNDKATC ' \ .- ;..' :^';^|^j|i

- TABULATION Of CONDUCJOM : . "- Y' ^Aii'0;#'V;{^^^^ ML Job MJJJ - KTJ 1MH/1., . IWttW Jul* M/7*," HIM. ;' v ̂ V s V^^

Conductor Designation

Dlghem - Anomaly Character

Kax. mho valueNo. of linesDepth tsttmated

Q - Open , X - Staked by others S - No. of claims staled by syndicate

cM

Z

ssi i13

V.I .f. ReconnaissanceV.I. M. ReconnaissanceV.I. F. Profiles

S v.C.H. DetaTlv Horltontal Shootback f .M.n Other Surveys.S Do, of tests for oaral)el conductor

Ho, of tests for conductor widthP**i o f H iwi af l^trtAAf ft^ftff

k Ifffl) feolo^v maooed (checked)

"e Conductor axistL ai rnfulnrtnr mil

nrrxruwtxl

trenchedri r 111 .1*

{ No. of geochemical soil samplest No. of rock samples analysedc No. of basal till samples

Previous Activity

Results of Follow-up

Conductive Material

Anomaly located: Yes*T; No- Mlength of Anomaly in feetConductivity Rating by .

ground C. M. or S. P. responseHagnetU Response In gaimas (g)estimated Depth to Source

by ground geophysical methods

geological Description

Ceochenlcal Analyses: S'Sotl

(Max. values in ppi) BT-Basal Till

Composition

True Width in Feet

Rock Assays

Abnormal assays

Spct-ieniquantitatlve spectrograph^

Distance from DON or Trench to max. e in feet.

Conclusions or Recoomendations

JA-M

It2

W to 149'

IA.11Cf4

49* ta IK*

tco-no -?M

J

40* tn ISO'

;:..v !OAMMr^

141

ti* tn U1*

A.C.H. option . Vibert loxnshlf ^•f^'-^S^"^ 1̂.

*

' -

Strongly Mttaorphg George Slrlug* - M

-

.

Geology, tM, mag, gravity-1964-6S- Rlocanex.

sed sediments (verb* p to be published ne

Unfavorable geology No work.

I

I

*

1t

10

I

Oology, {M. M* 19M-C*n*x.

1BOO open

Strong

W

\ report from O.O.N. it year).

Metamorphic quart- ilte, conglomerate, graphitic shale.

Graphite.

fxplalned as barren graphite. No further work.

. . .. .. -

-i .

...S.1i

Ceolony, Ol, Mf.) gravity 1M4-CS- ; Rtxanea.

-

-

SMlogist ; ,, :

1

Unfavorable geology. No work.

/K * ,,,,. . .-.r.'-.

' :i;: r ' ' ' . "' ' . :'.'-'-;.^^ . .'."'' " . ,, - - - -if- '••MC4tt"n

: ' : ; OIGHCH SWOKMC . v ' ' ,: ; ; :'v; -. .; V'-^^MT ABUIAT 10* of CONDUCTORS "•" - -'"' ^" f iK' .- -: -S'^^^^-s

6ft Job 98* JJ HIS It H/f - mill* .^1* M/Jf flllW. 1 ^X^' 4'^*^

Conductor Oti Ignition

Dlghe* - Anomaly Character

Has. mho valueNo. of linesDepth estimated

9 * OP*" . , . * - suled by e ther*S - No. of cUlM (Uked by syndlcttt

SW **

Ck

Ie

hk

U

V. l. F. RKonnilitanctV.C.H. ReconniltttnctV.I. F. Profiles

u V.C.H. DettllS llorltontil Shootback t. M.^ Other Surveysu No, of tetti for oiralle) conductor

No, of tem for conductor widthNo. of Hr.frt Bf rvignf tnvtf r

t. locil oeoloov MDDCd (checked)e TiflndUf ' nf* **^ pirAcn*rt*il"c Conductor .ax li trenchedU rnfuliirrnr xlt rfrlllMl

f No. of geochemical soil soviett No. of rock samples analysedu No. ot basal till samples

Prtvious Activity

Si

*O

u.*-oM**

D

1

Conductive HjterU'l

Anomaly located: Yei-Y; No-Ntenqth of Anomaly 1n feetConductivity Rating by

ground t .H. or S. t . responseMagnetic Response In ganMS (g)Estimated -Depth to Source


Geological Ascription

*

Ceochemtcal Analyses: S- Soil

(Hax. values 1n ppo) IT-Basal Till

Composition

True Width In FeetRock Assays

A*normal aiiays

Spct-seolquantltatlve spectrographlc

Distance from OOH or Trench to max. DIGHFM response in fcft.

Cone luj Ions or ftccomifendttloni

I4A"'W

.HI

M

1n 1

WC-JJC* vM

1W to 154'

-:-;:cvW Xii^

1 -.:. -,.-.. ,,

- -:-- W -- -A.C.*. optlo* - flbtrt tww5M* ; ?i .v . j.^j^^;^

.

d)-

t

Graphite shale.

Graphite.

(ip)ilned as barren graphite. Mo further work

i

ii

.1 X ,* .

ii

pt

-

T1500 Men south

Strong

Partial ISOg

*yStrongly metamori

Quar tt Ile and thai* (a* weak possibility that the rocks may b* a metamorphosed felsic to Inter mediate lapilli tuff).

',-

x

t1M

.

t '

I

,

311

T?600 ooen

Strong

SackgromwJ

W

^hosed sediments.

o outcrop on the conductor axis. HetaquartlUes nearby.

*

The conductors not explained however the 9*0 logy unfavorable. Ho further work.

-. \,

* , '

:^, ' - . ' t :

9

. t

*

.

.

Unfavorable geology. NO work.

cri Job w

OICHCH SVNOICATI ^ ' . . :, - ' [ ' ' . ;; : ' -:.;V^M

TAOUUTION Of CONDUCTORS ' - - , .- ' ". :' : ;, ,"'.', , ^^4-^^ IJJ NTS 41 N/1 . INKllft .Jyly tVJtu r iNAL ' s-i v.'"fSWA*


DlghM - Anomaly Character

Max, mho valueNo. of linesDepth estimated

0 - Open X - Staked by others S - No? of claims staked by syndicate

Ground Follow-up Undertaken

V.I. F. ReconnaissanceV. C. H. ReconnaissanceV.I. F. Profiles

" Y, f. M. DetailS Horizontal Shoplback t. H.^ Other Surveysu No, of tests for ojrallel conductor

No. of tests for conduct of width

* local otoloov manned (checked)

*f Conductor ail j trenched0 Conductor axil drilled

[ No. of geochemical soil samples{ No. of rock samples analysedu No. of basal till samples

* Previous

9

j*oU.

O

w*

* Of

Activity

Anomaly located: fes-T; No-Nlength of Anomaly in feetConductivity Rating by

ground [.H. or S. P. responseMagnetic Response In gammas (g)estimated Depth to Source


Geological Description

*

teoc helical Analyses: S-Soil

(Max. values 1n ppn) BT-Basal Till

Composition

True Width in FeetRock Assays

A-normal assays .

Spct'senlqujntltattve spectrographlc

Distance fron 00)1 or Trench to max. OIONfM response In /ret.

Conclusions or Recommendations

31I-3JA*J3

34' to 193*

31COC

17

63' to 1?0*

. 31*1.,,. . ....-'

h-^nv w iw

^:,37e.-,;^

H1It*

A.C.X. option . Vibert Township. - ; ; ^,.v-r^.i^

xx*xx

4x

11

Y1200 open

Strong

(OOOo. negative2S'

Felsic to inter- metiate lapilli tuff, graphitic shale with some pyrite, diabase dike.

-

Graphite.

explained as graphite with barren sulphides. No further work.

i

t

.

x

Serlclte-schtst (altered quartt- IteJ). graphitic shale.

Graphite.

Explained as graphite. No further work.

Ixt1I

SP.

3l

T

Intermediate ash. lapilli and block tuffs

-

Surveys at greater than ?00 loot coil separation Imp ossible due to topography. Mo further Inter est unless en couraging results obtained In 39A.

j

f

J

9 " '

'

.

Not surveyed. The ftology not very encouraging. No work unless favorable result) obtained in ne l r b/ anomalies.

m *

t

ea Job

1 - * - - . . .. . . - . .... ...* . . ,.

' OlOlCM JYNOICAU , j'^-:

TAWiAT 10H OF CONDUCTORS - ' '"^' HTS . 1OTK1M ^ fllW

Conductor Designation'

Dlghco - Anomaly Character

Hax. mho valu*No. of linesDepth estimated

0 - Open X - Slaked by othen S - Ho. of da IMS staked by syndicate


V. l. F. ReconnaissanceV.t.H. ReconnaissanceV.I. F. Profiles

5 v.C.H. Detailx Horizontal Shoptback E. H.^ Other Surveyso No. of tests for naralle] conductor

No. of ttits for conductor widthMo^of line* nf Gaanctoflieter

* ^MM aeoloov maooed (checked)S fendurlnr tillc Conductor aiis

p-ntpoMnt

trenchedu fnnrinrtnr nit rfrlllrrf

{ No. of geochemical soil samplest No. of rock samples analysed* No. of haul till samples

devious Activity

Results of Follow-uo

Conductive Material

Anomaly located: Yes-Y; No*Nlength of Anomaly In feetConductivity Rating by

ground C. H. or S. P. responseMagnetic Response In gammas (g)Estimated Depth to Source



Geochemical Analyses: S-Soll

' (Max. values In ppn) BT-Basal Till

Composition

True Width 1n feetRock Assays

Abnormal assays Spct'semtqutnt Hi live spectrographk

Distance from OOH or Trench to NX. DICHfH response 1n feet.


' 'J9A

191

J9*

' 4M

M1

iorA.C.X. option - Vibert Township

x

ix

4xx

S

Y1200

StrongSOOg direct

zs- - .Interacdlatc lapilli and ash luff.

. -

-

An excellent conductor In fair geology. One Winkle drill hole.

x

tIx

1

4

xx

S

yTOO

StrongUOg flanking

IS*

Felsic Upllll tuff, diabase. Rusty sections in the tuffs.

-

A-Cu, 23ppm Cu, lOppn Pb, Slppa In, 0 .4ppd Ag. 71. St S10;.

An excellent . conductor In good qeology. One Winkle drill hole,

, *KM4l'^,

SIn

0 ta 19?'

..-M o.-,^4-

.

r

t

Sediments.

o

-

A long anomaly in unfavorable geology. No work.

jj.'^. W-lli'-/^

. ^

- ' l -' ''O la iT'

^^.?.v*^i

"

4

f

-

' A weak anomaly in sediments. Ho work.

* .

^ DICItlH STNOICATt ' ' - V^f;

' JAWtATION Of CONDUCTORS . ' ' : ' ; -^} -Ul^V^'*' ea Job w JJ - MS 41 Wl . IMTW1H .OulxZVJ* riNAL ?^*;^;



Hat. mho valueMo. of linesDepth Estimated

0 - Open X - Staked by other* S - ho. of ci l 1*1 staled by syndicate

Ground Follow-vp Und-rtaVfB

V.I. f. ReconnaissanceV. C. M. ReconnaissanceV.I. f. Profiles

5 V.C.M. DetailV lloriiontal Shootbjck E. H.p Other Surveysu No. of tests fo f parallel conductor

No, of tests for conductor widthNo.. of lin** nf

, local woloav w,

r j n n^ t fu|^ \f f

*o Conductor axis trenchedtnr^Auftnr m il trl\\fA

r Ho. of geochemical toll samples

f No. of rock samples analysed

e Ho. of basal till sanples

Previous Activity

8iSoVI

V* 1 M

Conductive Material

Anomaly located: *es*Y; No-Nlength of Anomaly In feetConductivity Rating by

ground E. H. or S. P. responseMagnetic Response in gamnas (g)

EstlMated Depth to Source by ground geophysical Methods

6eoloo.ictl Description

Ceochealcal Analyses: S-Soll

-(Hax. values in ppm) ' BT'Basal Till

Composition

True Width In Feet. Hock Assays

A -normal assays

Spct-seffllquintitatlve spectrograph^ AA - atonic obsorptlon.

Distance fron DON or Trench to nax. DICHtM response in feet.


S2C-S6C

MS

ji |A ^,A.C.R. option- Tibert Township.

*

Geophysical . surveys, two j drill holes- ' Canex. '

Sedlnents (T). Pyrite, Minor chalcopyrite.

Explained as barren sulphides. No work.

ssc10

1w

SSGH-StC

10

b to tWA.C.K. option - Davieaux Township n

Cx)

,

Slaty seiilnenls, graphitic shale, diabase.


i

x

ii

x

20TO

y600 DBMI

StrongZSOg

f

Mafic volcanics Intermediate tuff, graphitic shale.

S-Hax 297 Cu, 42 Pb, 877 In.

Graphite.

M S CMS.

AA - nax Miff* Cu, MPPIH M.,eaopp* in.

Explained as barren graphite. No further work.

STO-NIC inli

w tom1A.C.R. optlo*- Desbiens TownsMp.

" ' "- 1 - '-' v-

' ' . - . - ; : ".

,.v; - . : .

" )

A long anwaly probably in sedlotnts. No work.

DICIICH SYNDICATE

- TADUIAT10K OF CONDUCTOKS V'S/^'M Ml Job WJ -NTS *1 H/l INTERIM Jnly M/M FINAL "-^W''!^

- Conductor Designation

Dtghca - AnoMly Character

Max. who valueNo. of linesDepth Estimated

. 0 - Open X - Staked by others S - Mo. of claims staked by syndicate

c fM

1. t'

O

i

13

V.I. F. ReconnaissanceV.C.M. ReconnaissanceV.I. f. Profiles

S V.E.H. Detail" Horizontal Shootback E. H.tj Other Surveys5 No.^ of tests for oarallel ^on^u^ter

No. of tests for conductor wldfhNo. df Unfit K l r ionctrw.t.1-

s. Local aeoloov cvaoocd (checked)

"c Conductor ails trenchede fftnrtiiftnr jiill drilled

f No. of geochemical soil samples"t No. of rock samples analysede No. of basal till samples

Previous Activity

Results of Follov-uj

Conductive Material

Anomaly located: US-IT; No-Nlength of Anomaly in feetConductivity Rating by

ground E. M. or S. P. responseHagnetic Response In gammas (g)Estimated Depth to Source




(Max. values In ppm) BT-Basal Till

Composition


A-norma) assays

Spct-ienit quantitative spectrographtc

Distance fron DDK or Trench to max. DIGHF.H response In feet.

Conclusions or Kecoflmendatlons

WDE-64E

41S3

.t 1 to?;'

ME-73EF

7?5

38' to 83' '

70A-7U , v ,

M

113' to Htt'

v-^.nw'*.^ji

M1 M US' i

A.C.R. option - Desbiens Township , , ,,., . ;,-i 1^;.^'

xxx

3x

t'

t1000 open

Very Strong

IS.SOOg directC2S' -

Mafic volcanics, Iron formation.

Iron formation.

*

Although not , detected the conductor strength suggests the presence of graphite or massive sulphides. Ho further work.

The aeromagnetic data Indicates that this anomaly is on the same iron formation horlton ' as anomaly C?OE- 63E.

,


4

(x)t

-

Miflc pillow lava, tops south.

-

Unfavorable geology. No further wrl.

.

,

.

t

4

- \

. j-' t

A weak anomaly unfavorable geology to the northwest and southeast. No work.

DIGMM StNOICAH ' '.''^^^

'- ' tAKKATlON OF CONDUCTORS .V " ".i"''- ;' S;N;' ,x'^|fM^ ' \


Dlghcn - AnoMly Character

Ma*, tiho valueHo. of linesDepth Estimated

0 - Open , , J - SlakeJ by others l - lio. of clal*s staked by syndicate

y. L. F. Reconnaissancey. t. M. ReconnaissanceV. l. F. Profiles

t C y. t. H. Detail1 S, horiiontal Shootback. E. M.t fe Other SurveysT- u No.i of tests for oarallel conductora No, of tests for conductor width F Ha. Df linrt n{ fMgnMAmttfkf

6 , l pf|l ofolnnv gunnod (thtcktdl"" " CnndM" B' J*i* Brntl*rl*il

^ *| Conductor axis^ c Conductor **t*

trenchedrirlI1.il

u | No. of qeocheakal soil samplesf No. of rock sai pics analysedc Ho. of basal till samples

Previous Activity

Anomaly located: Ves-T; No- Hlength of Anomaly 1n feetConductivity Rating by

ground I. M. or S. P. responseMagnetic Response 1n gannas (g)Csltidted Depth to Source

by ground geophysical Methods

t, Geological

I

U.

oy

a

1

Description

Geochealcal Analyses: S- So H

(Max. values In ppn) ' BT'Basal Till

Composition

- -^ True Uidlh In Feet4, . Dock Assays3

^ A -normal assays . j Spct-scnlquantltative spectrographlci.

Distance from DDK or Trench to NX. DIGHEM response in feet.

Conclusions or teconr.endattons

728-79*

10s

?V '9 "J*

7K-77C

mr to isv

. ^730.77C^-^

10S

8 1 to 109*

^"4*** '" 24 " ' 1 . '

4 1-s*' to m* ,

A.C.*. option - Desbiens Townifctp.,,;., , /.r.j.-'^vi^-i^i^^.'-

*

On strike of t known iron format i on.


.

*

On* diamond drill holt.

Iron f or m t lo*, graphite.

Graphite

Cxp'tafncd as barren graphite. No work.

*

-

-

*

-

Unfavorable oafic volcanics and sediments on strike. tto work.

; :\

. "- - - . i- ... . . . ,. -j.,.^.

W, Mg. jrwlt* surveys, one drll hoi*.

-

Iron for*a t lo*. , [ sediments, graph- Ut. seat isulphides. j

-

eraphite, sulphides.

14.0

Ciplalned as graphite and ". barren sulphide Ho work. -

IMUUtMM Of CONDUCTORen jot. w jj .mi 4i a/i imiim ^ijf^m^riiiAL ' ' r iw: : '^vf-!

Conductor Designation. . .,


Max. Kho valveNo. of linesDept* estimated

Q - Open I - Staked by others S - lio. of claim stated by syndicate

Ground Follov-uB Undertaken 1

y. l. F. Reconnaissancey. C. H. ReconnaissanceV. l. F. Profiles

u V.f.H. DetailC Horizontal Shootback f. H^ Other SurveysS No. of tests for oaralle^ conductor

No of tests for conductor widthNo. of H ne t af

f r.r^tor ,,U

*s Conductor axis trenched

f No. of qexhemlcal soil samples

u No. of basal till samples

Previous

Results of Follow-uo !

Conductive Material

Activity

Anomaly located: Yes**; Ho-Nlength of Anomaly 1n feetConductivity Rating by

ground C.N. or S. P. responseMagnetic Response In gaimas (g)CstlMted Depth to Source

by around geophysical methods


Geochemlcal Analyses: S-Soll

(Max. values In pro) BT-Ba:aI Till

Composition

True Width 1n FeetRock Assays

Abnormal assays

Spct'tealquantUatlve spectrographlc

Distance from DDII or Trench to nan. D!GH[H response In feel.

Conclusions or Decomendatlons

7SI-78C

M3

0 to S8'A. C. R. option* Desbiens Township.

.

-

-

The aeromagnetic data Indicates that this anomaly Is on the extension of Iron formation Identified to the northwest.

-

Unfavorable geology, tlo work.

7M-iSC i

1W tt W

.

-

The aeromagnetic dot a Indicates that this anomaly Is on the exten sion of the iron formation and graphite causing anomaly 72C-77C.

Unfavorable geology on strike Ho work. '

. ' '-.m-^-l

" i 'T?'-'' 1-

^'liwoii^

,: t "' '- -

W t. t*'

- A.C.*. option - DeibtMt Toms*)*;

,

xx

251

y

400

Strong

UOOa direct^S'

Mafic pillow lava and tuff, graphitic schist, SI pyrite.

5-31 Cu. IS Pb, 113 In, 11 Co, 27 HI, 0.9 Ag. 2Sppb Au.

Graphite;

13.0

A-0.01S Cu, 0.02* Pb, 0.061 In, 0.20ozi. Ag, Trace Au.

400


1J

i

t

Sediments and ' i r M faraatlon M * strike to the northwest.

\

Unfavorable geology. ' No work.

l ll

-i'**"

D1GIICM SYNDICATE . '-- ,:; ' 'ffify

Ctt Job *M-M .ms 41 H/1 WEMM-WyJVM riML^ ; ' V M!ff


Olohem - Anomaly Character

Hal. ffho valueNo. of linesDepth Estimated

" 0 - Open . . I - Staked by others J - No. of claims staked by syndicate

j* k

Ground fei low-

y. l .F. Reconnaissancey.E.M. ReconnaissanceV.I. f. Profiles

S y.E.M. Detailt Horljontal Shootbick t.M.a Other SurveysS Wo. of tests for urallel conductor

No. of tests for conductor width

v local aeoloov raoocd (checked)E rnnrfurtnr i. Itj Conductor axis

jirntpM-ttrftrenched

{ No. of oeocheoteal soil samplesv No. of rock sanples analysede No. of basal till samples

Previous

Conductive Material

Activity

Anomaly Located: YeS'V; No-Hlength of Anomaly in feetConductivity Dating by

ground E. M. or S. P. responseMagnetic Response In ganrnas (g)Estimated Depth to Source

by ground geophysical method!

geological Description


(Max. values in ppn) 8T*Basal Till

Composition

True Width in feetDock Assays

A-normal assays

Spct-semlquanUtaUve spectrograph le

Distance from DDK DIGHfM rcsr-or.

or Trench to max. .e in feet.

Conclusions or Recomjndatlons

7W.UOM4

*i- to m-

-

The aeromagnetic data indicates that this anomaly Is part of the mafic volcan ic- sedlments-lron formation series Identified to the northwest.

.


au ui i

H1

41'

'i :"-.-wm,*teJ- V ,-

" - l ' - 'ty to to*

- A. C. t. option - Ocsblent TowijM* v,^ ; tv ^

*

*

The aeromagnetic data Indicates that this anomaly Is part of the Iron formation horizon Identified to the northwest.

Unfavorable geology. Ho work.

,

,(

.

1

x*

11

4

y

500

Strong

!4ta direct

W

Mafic flows, pillow lava, ash tuff, lapilli tuff, slate.

5-26 Cu. 172 Pb. SI In, 14 Co. 17 Ni. 0.9 Ag. lOppb Au.

A- Tr. Cu. Tr. Pb. 0.011 In. 4 7.61 SiO;.

The source of the conductor not identified. On strike of the graphite tone caustni) W. Unfavorable geology. The soil sample results low.

.No further work.

. - - . -- *

. ____________ '-;

t

-

i

1

On strike of sedlunts and Iron formatlo* to the northwed

Probable unfav orable geology. A weak anomaly. No work.

CO. Job M4JJ -OTS. 41 N/l

OICIKM SYNDICAU .

Of CONOUCTOUINTUIH July WU F 1NAX


Dlghc* - Anomaly t hi r ic ter

Hit. mho vilu*No. of linesDepth tstlMited

0 - Ope* , . 1 - SlJkcd by olhcn i - to. of claim j Hit J by syndicate

Ground Follow-up UM*'tl***i

V.I. F. Reconnalssjnc*V.C.H. ReconnaltSJKCtV.I. F. Profllei

v y . [.n. Detailt Horizontal ShootbJCk t. H.o .other SurveysS No of tests for parallel conductor


* Local oeoloov p

"e Conductor oilu fnndurtflT Axil

aD!teJ (rhe4;t|fdl

trencheddrlllnl

f No. of geochemical toll samplest No. of rock samples analysedc no. of basal till samples

Previous


Conductive Material

Activity

Anomaly located: Tes'Y; lio'Nlength of Anomaly In feetConductivity Rating by

ground t .H. or S. t . responseMagnetic Response In gannas (9)ttttnated Depth to Source

by (ground geophysical methods

teoleqlcal Description

Geochemical Analyses: S'Soll

(tox. values In ppn} BT-Basal Till

Composition


A -normal assays .

Spct'semlquantltitlve spoclrographlc

Distance from OOH or Trench to man. O'.Win r esponse In feet.


8X-85F 6tf

18 Kf l

80' to W 80'

8X-*Ot

tt'

*' to 117'

84A W8-8S8

w ?: .*

7S' 34* to 112'

4C M

'lW1 1

A.C.*. option . DestlfM Towirtl^

-

-

.

Probable unfav- onble geology. No work.

,

Tht aeromagnetic data Indicates that this anomaly Is on the Mfie volcanic* Iron formation horizon checked to the northwest.

-


1 na1tt

1 '-

i

1

i

M

Haflc flows, felsic flows. Mont tic gabbro or diabase.

A-mppm Cu, ISppm Pb, 13?ppm In, l.lppm Ag, 8ppbAu.

The conductors not located and possibly due to noise'. The geology unfavor able. No further work.

l -

lX 'i

-

i

-

Ht !

;

T700* i

HetflM

ea Job 9M-JJ .NTS 41 K/!

DICHIM SVNDICAK

TABUIAIION OF CONOUCTMSriML

Conductor Designation.

Dlghra - Anomaly Character

Max. mho valveNo. of linesDepth Estimated

0 . Open . X - Staked by others I - No. of claims staked by syndicate

{

V.I. F. ReconnaissanceV. E. M. Reconnaissancey.l.F. Profiles

5 i.E.M. Detailt Horl rental Shoo t back E. M.p Other SurveysX (lo, of tests for mrallel conductor

1)9. of tests for conductor widthMo ofJinss 3f rjoiwtOTPtrr

> Local Qeolflov f^ ConJuclor **i*"{ Conductor aits

aroed (checked)nratiwrlMl

trenched43 Cfiftdlif* ftr **it J*rl11l*ft

| Ho. of geochenlcal soli samplest No. of rock samples analysedc No. of basal till sanples

rrevlovs Activity


Conductive Material

Anomaly located: rei'f; Mo-Hlength of Anomaly in feetConductivity Rating bjr

ground E. H. or S. P. responseMagnetic Response In gatmas (g)Estimated Depth to Source


. geological Description

Geochemical Anal)ses: S'Sotl

(Man. values In ppm) BT'Basa) Till

Composition

True Width tn feetRock Assays

A-nomal assays

Spct-semlquantitattve spectrographlc

Distance from ODH or Trench to man. DIGIIEM rc5Bon',e In feet.


MH141

714*

SA-87AI

w3

K' to W

KO-901

)S1

0 U IDS'

KH-MO

1)5

39' to WA.C.X. option - Desbiens Township . - '

'

.

Associated with the Kaflc volcanics -Iron formation horlton checked to th* west.

' '

Unfavorable geology.

.No M)rk.

x

.

M

- '

Y

Mafic flows, diabase dikes.

Unfavorable geology. No further work.

'

Sediments on strike to the northwest.

'

Probable unfavor able geology. No work.

*

Mafic volcanics, sediments and Iron formation on t strike to the northwest. - '

1

Probable unfavor able geology. No vork.

t '

' ' ' DIGWN iweicAU . * , ,. , '..'-' ' ;:- . .'' :'!.'..^'^j*;1 . TAWUTION Or COMUCTMS '•'••••'. ;. '•'•.'•'•••'.''•^•"^^:^}^

GCl Job 9B4MJ JflS 41 N/l - M INTUM 'Ally \ 3f1t - - FIML ' - ' v, : - V:.'38f


Dlghcfl - AMwaly Character

tin. mho valueNo. of linesDepth (stlmatH

' 0 - Open X - Staked by others i - Mo. of claim staked by syndicate

Ground Follow-wp Undertaken

V.I. F. krconnalssanceV.C.N. ReconiulssanceV.I. F. Profiles

S V.t.H. Detailx Hgrliontal Shootbick f .H.|f Other Surveysu No r of tests for uraljfl conductor

No. of tests for conductor widthNO. of iini-i of tugaetot&ttr

^ tocal oeoloov maoocd fcheckedl

"j Conductor ails trenchedK FnnAurtrtr lvl* 4rl\\eA

l No. of geochemical soil samplesf No. of rock samples analysedu No. of basal till samples

Previous Activity

J

o

M f

OC

1

u

c0

Anomaly located: Yes-T; No*Nlength of Anomaly In feetinnductlvlty Rating by

ground t. M. or S. P. responseMagnetic Response In gamas (g)

' (st lau ted Depth ta Source by ground geophysical methods


Ceochmlca) Analyses: 5-Soll

(Max. values In ppa) BT'Basal Till

Compotltlon

True Width In FeetRock Assiys

A-nonul assays

Spct'sealquantltatlve spectrographlc

Distance I ron DON or Trench to wx. OICHfK reipons* In feet.

Conclusions or tccomendatlons

MA

(gi

46'A.C.k. option* Desbiens Township.

x

M

1.

Y

Mafic flows.

.


.....- . ..-;.: ; V^Vi^-^jjfjfe

"//^iSl

j f

lo9

8

7

6

GEOLOGICAL LEGEND

AREA *JJ* BATCHAH/WA EAST, ONTARIO*

.f , -

PLEISTOCENE -- sand, gravel, clayr

DIABASE DYKE* * '

•"DIABASE SHEET : .

' HLSIC INTRUSIVESgranitegranodioritequartz feldspar porphyryfeldspar porphyry

.MAFIC INTRUSIVES(a) diorite(b) gabbro -

SEDIMENTS

rv v

#

. ' . *

Qt

cQex

gh

Iron Formation, chertlimestone-dolomiteshale (mudstone)-slate . 'siltstonesandstone-quartzltegreywacke'schistgneiss

3 . MAFIC VOLCANICS

2 'JELSIC A INTERMEDIATE VOLCANICS

1 ", fELSIC VOLCANICS: (a

- lcrhyolite ( 70* SiOjrhyodacite (64-69* SiO,)dacite 59-64* SiO^)

d) andesite 52-59* SiOf)(e) basalt 52* SiOS)(fi'-

t -hiJk0

tuff 'crystal tufflapilli tuffagglomeratefragments, breccia.flows•pillows

(m) porphyritic (n) amygdaloidal

GEOPHYSICAL SURVEY STANDARD LEGENDSMAGNETOMETER SURVEY (MAPI SELF-POTENTIAL SURVEY

M *Mr*nr**M

MSTMMtNTi , .

WSTMWCNTi

ELECTROMAGNETIC SURVEY

VERTICAL LOOP (V.EJH.I

*r M/ Mn/M.

S11 —****r.XAf.-*w*i

son MI.

"Hf/11*1

t

*MwiMir^*H*M ArwriUMf Innnt

*tn* K"*1' MSTIIUMCMT 1

VERY LOW FREQUENCY (V.L.F.E.M.)

Shoetbaek (Horiionlal or Ceailol)

INSTRUMrNTi

li.-Slttltn i

H.E.M.

Piltitll•- ' ' O-', ; \.-?f'?^gwg:

. ,-:;a-iift1 -:-..^'; -:;::;W.^^^

T*~* Jv '* ..

ttriu

.(0*

^^^^p^•^^M^M'i&ji ••••:'^ijeg*^\mfcga

VIBERT TWR (T.25.R.I4)

-—— LOGSINS ROAD

INSTRUMENT! CRONE C.E.*). UNITCRONE V.L.F. UNIT

OPERATOR i KIELCY-GRANT Tx.STATIONi CUTLER, PAINE

DiGHEM SYNDICATE

AREA J J -ANOMALY 39A

E.M. SURVEY

.976

.VIBERT TWP. (Twp.25-Rge.l4)

iNSTRUMtKT: FLUXGATE flF-1 fUG.OPERATOR t GRANT

utm* o so noft t r e

DIGHEM SYNDICATE

AREA J J -ANOMALY 39 A

MAG. SURVEY

DATE JUNt.1976. X)B 984

vi'

VIBERT TWR (T.25,R.I4)

y ;

r

— LoseINS ROAD

INSTRUMENT: CRONE C.E.*!, UNIT CRONE V.L.F. UNIT

OPERATOR i KIELEY-GRANT IX.STATIONI CUTLER, fAiNE

•mn

MIT toef

DIGHEM SYNDICATE

AREA J J -ANOMALY 39A

E.M. SURVEYDATE JUNE 1976 JOB 984

1 -.. LJJIililiijLJjlilillilililil liiliifliiiliijliiiliifhiilililiiiliifliiil 1,1,1? liiiliiiinfH

• VIBERT TWP. (Twp.25-Rge.l4)

UtTRU

hmr o lotf

INSTRUMENT: FLUXDATE.HF-I fUo. OPERATOR j GRANT DI6HEM SYNDICATE


MAG. SURVEY

DATE JONt.1976. JOB 984

ISiiiik^

m.

s —— LocciKc ROAD

rGEOLOGY DONE BY KRANZ/PORRITT

VIBERT TWP. (Twp.25-Rge.K )

o •o toorciT 6

DIGHEM SYNDICATE


GEOLOGYDATE Jl/NE.1976. 984

!llilllll.ljLlllllllllllll?!lllllllll|j||lMl|||||jl!lli|j6

/f'?"

liA'? - 5•* , ' f~

ss?

w:Wl__ VIBERT TWP. (Twp.25-Rge.l4)

llt Stnltltl100' cm $l^.

INSTRUMENT: CRONE C.E.M. UNIT CRONE V.L.F. UNIT

OPERATOR : KIELEY-GRANT Tx.STATION: CUTLER,

*fe

M

•mn * fur o loo-

DIGHEM SYNDICATEAREA JJ - ANOMALY 40B

E.M. SURVEYPATE MAY 1970 '- JOB 984

iliiuliliiililjJilflilililjlilihlS•i

V

I..

"'00

VIBERT T-W P.(Twp. 25-Rge.l4)

INSTRUMENT: FLUXGATE MF-1 MAG, OPERATOR : GRANT,

METRES

FEET

100200'

DIGHEM SYNDICATEAREA JJ - ANOMALY .408

. MAG. SURVEY

DATE MAY 1976 JOB 984

^ itflllllllllllllll5 .6

"/••f;

•n

•r.

•s.

"'O.

VIBERT TWP. (Twp.25-Rgc.l4)

GEOLOGY DONE BY J.PORRITT

DIGHEM SYNDICATE AREA J J - ANOMALY 40 B

GEOLOGY

DATC MAY (976 JOB BM

llllllllllllllllMlllllllllllllfhlllllllllllllMlllllllllllllflllllllllllllllj

l

DJGIIEH SYNDICATE

TABULATION OF CONDUCTORS GEL Job "HA NTS -1 IN/1. J INTERIM NOV, M. I97S FINAL

Conductor Dei i gnat i on

Dighc* - Anomaly Character

Max. mho valueHo. of linesDepth estimated

0 - Open X - Staked by others S - No. of claims staked by syndicate


V.L.F. ReconnaissanceY. E. M. ReconnaissanceV.I. F. Profiles

5 V.E.H. DetailS Horizontal Shootback E. H.o Other Surveysa No, of tests for parallel conductor

No. of tests for conductor widthHo i of li ni*? o T Ri3ofl**tonv*|(*T

r. Local flcoloov mapped (checked)c CondYC.tor **Js. prosper''*'*"S Conductor axis trenched0 .Cnnductni- "li IrlMfd

J No. of geochemical soil samplesu No. of rock samples analysedu No. of basal till samples

Previous Activity

Results of follow-up

Conductive Material

Anomaly Located: Yes* Vi tto-NLength of Anomaly in feetConductivity Rating by

ground t. H. or S. P. responseMagnetic Response In gammas (g)Estimated Depth lo Source



Geochemical Analyses: 5-Soll

(Max. values in ppm) BT*Basal Till

Compos 1 1 Ion


A*norma) assays Spc t* semi quant i tat i ve spectrograph t c

Distance from DDH or Trench to max. OIGHFK response 1n feet.


322A

271

216*

A.C.R.XX

2X

1

N

Ureywacke-lype amphibolite intruded by granite, porphyry and pegmatite dikes. 250 feel east on utrlke a 2cm horizon with 10ft pyrite.

2 cmS pet. - no significant values. A. A - l.Sppm Ag, 25ppb Au.

2SO

The anomaly not loca'rd oiul prubobly Is coii.sc'i] by noise os OK; topography i.s

Unfnv.nira''lc geology. No fiirllicr work.

329A

101

156*

Option ' . A.-X

x -f -

: t-'-

X r-'x -.x

' 1

Y200 otxin

Strong

DIGIIEH SYNDICATE

TACUIAIION OF COMDUCTORSGEL Job 9RIA JlfTCRIH Mo*.M. 197V THIN.



Max. mho valueNo. of linesDepth Estimated

0 - Open J. - Staked by others S - Ho. of c laims staked by syndicate

Ground FoTlcw-up Undertaken

V. l. F. ReconnaissanceV.E.K. ReconnaissanceV.I. F. Profiles

v V .E.H. Detail5 Horizontal Shootback E. H.S Other SurveysS No. of tests for parallel conductor

No. of tests for conductor widthNo. nf Hnnt nf nunpptravvtpr

•, Local Qcolcxw Hooped (checked!o Cnndurtnr ailt Drntiwvti-d"c Conductor axis trenchede Cnndurtnr a* Is drillrd

j No. of geochemical soil samplesL No. of rock samples analysede No. of basal till samples

Previous Activity

D

i*o l*.

o4-*

3

W

V i.

stl

*f tj•oc o o

Anomaly located: Yes**; lto*Mlength of Anomaly in feetConductivity Rating by

ground E. H, or S. P. responseMagnetic Response in gamas (g)Estimated Depth to Source

by ground geophysical methodsGeological Description


(Max. values In pprn) BT-Basal Till

Composition

Iru? Width in FeetRock Assays

A-nornu] assays Spct'semiquanti tative spectrograph^

Distance from ODH DIGHfM respon:

or Trench to max. e in feet.


22^227D

104

62' to 199'

0

Geopliynlra) surveys 1963 -Joubin for A. C. R.

MciaActliinents. A pyrliu showing 700* north of (bc comkicotr axis (OPM map P998).

Unfnvourohlc gcolojry. No work.

J31A

131

110*

OX

2

1Xx

2

Y100 open

I300(i di reel

•eSO'

MulartuUlmunt* (greywacke quartzite) and mafic flows.

Disseminated pyrite. Iron oxide staining In sediments

Spot. -no significant values. A, A. - 0. 7 ppm Ag,

100

Unfavourable gcolopy. Exposed In outcrop. No further work.

24IB-24-IR

124

19' la 131'

X

1X

-

2XX

1

Y300 open

Strong

MOOg direct

41N01NE08I01 DAVIEAUX29 RUNNALLS

Report No. D60J "^ 0S0 N.T.S. Nos. 40-N-l, 40-0-4

DIGHEM SURVEY

OP

AREA "JJ", BATCHAWANA AREA, ONTARIO

FOR

GEOPHYSICAL ENGINEERING LIMITED

BY

DIGHEM LIMITED

Toronto, Ontario March 15, 1976 D. C. Fraser

President

S. Greinwald Geophysicist

SUMMARY

A. DIGHEM survey of 497 line-miles was flown

at a l/8th mile line-spacing for Geophysical Engineering

Limited on behalf of the Dighem Syndicate. The survey

was flown from February 8th to February 25th, 1976, in

the Batchawana area of Ontario (Figure 1). A total of

334 anomalous EM responses were recorded, 136 of which

are of the first (or lowest) conductance grade. Many of

the latter probably are surface effects, as indicated by

the interpretation on the EM map. Many bedrock conductors

were located, with conductances up to the sixth grade.

Some are of medium to short length.

,

aqj,'t

dVW NOI1V301t

CONDUCTORS IN THE SURVEY AREA

The DIGHEM map provides an interpretation of

conductors as to their length, strike direction/ depth,

and conductance quality or conductivity-thickness

product in mhos, ^hese conductors should be correlated

with the known geology to assess their relative importance

prior to ground followup.

When studying the EM map for followup planning,*

consult the anomaly listings appended to this report.

to ensure that none of the conductors are overlooked.

The original map may be printed with topography burned

out, so that only the anomalies remain clearly visible,

assuring that all conductors are clearly identified.

The area is characterized by a thin/ generally

non-conductive cover. A total of 334 conductive anomalies

were detected, as shown in Table I, of which 136 are of

the first (or lowest) conductance grade. Many of the

latter are likely to be surface effects.

- 2 -

TABLE 1. Distribution of EM Anomalies

AnomalyGrade

654321

Total

Number ofAnomalies

821535759

136.

334

The following anomalies may be of interest. Refer

to the Reference map for the conductor locations.

GROUP l Conductance grades: 1-4magnetic correlation: up to DO gammas Northwest end: 2A; Southeast end: 5A

Anomalies 3A and 3B occur on a relatively local 90 gamma magnetic peak, and might not be a oart of the anomalies to the southeast.

GROUP 2 Conductance grades: 1-4magnetic correlation: up to 400 gammas Northwest end: 1A; Southeast end: 19C

Many of the conductors in this area follow morphological features. However, the majority of the anomalies are believed to reflect bedrock conductors. 11A occurs on a lakeshore but is a definite bedrock conductor.

GROUP 3 Conductance grades: l, 2, 3, 5 magnetic correlation: 40 gammas Northwest end: 76A; Southeast end: 90A

These single-, two- and three-line conductors occur on the southern flanks of magnetic anomalies which might have a common geological source. 87A and 87B have a direct magnetic correlation.

- 3 -

GROUP 4 Conductance grades: l, 4magnetic correlation: 60 gammas - anomalies: 84A, 84B-85B

The grade l conductor 84B-85B coincides with an isolated magnetic high. The grade 4 anomaly 84A is located on the northern flank of this same high. These conductors may represent interesting targets.

GROUP 5 Conductance grades: 1-3magnetic correlation: 40 gammas anomalies: 79A, 82A, 82B, 8-iC

This grouping consists of three definite single-line bedrock anomalies, none of which has a meaningful magnetic correlation.

GROUP 6 Conductance grades: 1-5magnetic correlation: 40 gammas Northwest end: 45A; Southeast end: 73A

The conductors follow the magnetic trend in the southeast half of this grouping, but diverge from the trend in the northwest half. Consequently, the conductors in the northwest half may occur in different formations than those to the southeast.

GROUP 7 Conductance grades: 1-6magnetic correlation: up to 70 gammas Northwest end: 31B; Southeast end: 79B

The conductive band probably reflects graphite and iron formation. However, there are a few relatively isolated and short conductors which may warrant followup,

GROUP 8 Conductance grades: 2-4magnetic correlation: non-magnetic Northwest end: 37A; Southeast end: 40B

The grade 2 anomalies 37A and 37B have a direct magnetic correlation of 20 gammas, while the single-line grade 4 anomaly 40B is non-magnetic. These conductors may represent interesting targets.

- 4 -

GROUP 9 Conductance grades: l, 2, 3, 5 magnetic correlation: 20 gammas Northwest end: 44B; Southeast end: 58E

The conductors are closely related to a magnetic feature which covers the same area. There is, however, only a spotty magnetic correlation. .57E-58E appears to be an isolated grade 3 conductor, but may be an extension of 44B-54B.

GROUP 10 Conductance grades: 1-6magnetic correlation: up to 20 gammas Northwest end: 72C; Southeast end: 90S

The complex of anomalies of grades 1-6 may reflect iron formation. The non-magnetic conductor 83A-86C, of conductance gradet l to 2, appears to be outside the main conductive area.

GROUP 11 Conductance grades: 1-6magnetic correlation: up to 500 gammas Northwest end: 52F; Southeast end: 90E

The conductive complex, consisting of many conductors of short to medium strike length, probably belongs to one geological environment such as iron formation. Many of the conductors have a direct magnetic correlation, varying from 20 to 500 gammas.

GROUP 12 Conductance grades: 1-2magnetic correlation: rion-magnetic anomalies: 30B, 31C, 31D, 31E

These anomalies are believed to represent bedrock conductors, with the possible exception of 30P.

K?

- 5 -

GROUP 13 Conductance grades: 1-3

of a magnetic high.

Respectfully submitted/

Toronto, Ontario March 15, 1976 D . C. Fraser

President

S. Greinwald Geophysicist

following maps accompany this report:

5274a

5274b

5274c

5274d

Electromagnetic

Magnetic

Enhanced magnetic

Reference map

l map sheet

l map sheet

l map sheet

l map sheet

STANDARD COIL

L TNE K REAL UUADWNOf ALY PPM pPM

1Ain1C

2A i 213i ' 2C

3A 3B 3C

4 Aun4C

t

' 5A: 50j

66 0

15 2 2

17 20 4

65 5

126

164 2

6 47

24 12 8

127"5

74

WJLL-( FISH V

OUAQ PPM

-3-1 0

-2 -3 -3

23

-1

-10

-1

0 0

:CTLS'HALE

CHAD PPM

4 0 2

2 3 3

6 6 2

53 2

3 0

VERTICAL DIKE

CONC DEPTHwios FEET

2 91

27 3 ' 1

6 173

3 4 6

15 11

65 146

0

97ISO

0

52 81 20

69 85

133

1-3694

HORIZONTAL SHEET

coMD DFPTH KHOS FEET

i31

611

2 5 1

1 1 2

43

.199 402

0

315 11193

187 260 211

225 282 378

345347

COMDUCTIVE EARTH

RES IS DEPTH OHM-M FEET

111 10071007

5 10071007

33 8

1007

89 1007 1007

101007

76 00 ,

251 00

99 197

0m

970 0

2720

6A

7A50 .

134

250

378

1007

1007

OAno

9A9n9C 9D

10AIDD ICC 10D 10E 10F

. * r o

6 1

69a

31

1427 9 1

14 17

T TU . Ir-.

11

2

4n5 4

14?\ 10 2 4

10

3 1

1 2 2 2

-4 -5 3 0 0 1

3 4

0 3 2 2

7 9 5 4 3 4

9

4 1

4

*

9 9

12 . 234*

*

9 14 6 1

39 17

49 '

149 .*

^

161 . 105 . 121 . 40 .

t

74 ;48 . 00 . 23 .

130 ..U *\B 2 .

1 1

3 3 3

39

3 4 2 1 95

222 399

417 310 356 214

247 199 273 '278 344271

80 1007

1007 24 16 1

2210 39

1007 38

95 0

0 221 271 199

162 139 170

0 293206

OK o,

jLINF x"NOf/ALI

11Ann ne lin

13A

i

11Alin

ISA

16A160

i

17A 17H 17C

18Aien - . lac

19A 19B 19C 190

27A270

3QAson

1 , ,~,

"ST" ^^ ; viHm* .

r "SS u n̂ "ISS CSS i Kg D^'i

" *f -j " -' e ' o : 5 J ", j - ' ts" :" S 'i S : .! ,S:

' .0 * o l .' l o '* * u *

' ' 1c - * t

21 10 "J J n 209 . ^ 1 2 0 1 . 23 71 .

* .

1 6 o 3*i0 * 1 1 .* .

. ' 0 " 1 3*15 9 .9 o * a 0 * 9 " 2 2 . 1 60 .

* .

13 1 0 f) 3^2 5n *

S - -'S ? : !! Si*

•.^ li l 5 ^5 05 .'o 1 i 35 - i; s; -3 * i o .*

! i 1 ' -: i -i - S '? S : J ^:

* ."f ? J 1 * 2 193 '

7 10 0 2 . 1 ,3 ;

' .

2 4 1 0 ! 2 15.4 *2 ^ . I. 13 '4. D "1 0. 1 AR" * -1 J D ,

HORIZONTAL SHEET

cowo DEPTHWHOS FEET

3 205 2 119 1 283

20 271

1 3

t

3 187 6 . 212

1 117

1 01 215

1 197 8 191 3 192

2 260 5 1521 53

1 0 1 332 2 107 1 111

1 16fl2 262

1 3*01 220

CONDUCTIVE EARTH,; -:

nrsisOHK-H '

221007 78 1

.

1007

1007 5

1007

100776

210 3

18

17 6

251

1007 1007 1007 1007

100759

10071007

'.•./y:;,-'. '••?.

PEPTHFEET

126 0

151 211

0

0 187

0f

.0117

51 150 116

155 103

0

0 0 0 0

0115

00:*

PR o,

L I Mr *ANOMALY

31A 3]0 31C310 31E

j 31F

32A 32B

33A 33R 33C

31A

StAhiDAxD COIL

REAL uij/voPPM PPM

6 9a9 6 3

3 33

53 1 H

,

2

n7

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2 A

12 5 1

6

NULL-CUTLS T I Sil WHALE

WAD KUADPPM ppw

0 -1 -11 4 1

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0 0 2

0

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4 21

1

^

VERTICAL DIKE

CONC DEPTH* WIGS FEET

4 96

17 3 2

6 69

93 1

16

t

90 9991

120 63 76

193 59

31 81

131

tt A

HORIZONTAL SHEET

COHO DEPTH MHOS FEET

1 32 4 1 1

215

20 1 4

288 311281 393 231 2S7

492 219

169 264 401

CONCUCTXVE EARTH '

RESIS DEPTH OHM -M FEET

1007 2444 11 86

1007

1007 1

1 1007

12

0 213174 315 103

0

0 185

113 0

321

35A

38A

39A 390

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106

36A36B36C

23

- 5

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0-1

0

100

37ft 370 37C 37D

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100 .

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359 311 269 319

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11

0 217 205 211

178

75

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1 f) 1

213 303 275

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79

125

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215

331

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0 ,211 .100 .

111

92198167

23810071007

000

63

380

270379

1007

516

l 1

216 3C2

7613

210291

92301

LINE S

42B

43A 43H 43C

1'IA 440

ISA 45B 45C

46A 46H 4f,C

47A 470 47C 470

4Bf? 4 OC 400

49A 49M 49C 491) 49E 49F

50Ason50C 500

SIAfJuAItU NULL-COILS COIL FISH WHALE

REAL PPM

402

5478

4

444

64511

9b912

2594

0ft

952

02

04041

345

4645

73

WAD OIJADPPM ppv

19 23 1

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14 o4 1

4 -l10 -114 o

7 010 115 i|

13 n3n 2

5 i*13 l

17 o11 2

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1 025 3?1 510 312 0

6 0

?fl l29 ?

5 26 3

CUAO PPM

32

012

4

41

226

353

611

31

3422

228352

9S33

VEHTIC/ILCIKE

CONOXHOS

302

33 356

538

9816

10147

6

225013

4 4212

121 27224

222193

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DEPTH*.,PEF.T .

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180 ..*

25 . 0 .

207 ..

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.

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4

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126 ."7 .

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COMDWHOS

t

81

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122

3182

3302

61211

1 1011

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6631

DEPTHFEET

171455

157 113489

184440

394186237

262157173

226111

0174

101 190

0400

0163 166165IflO262

151151356300

CONDUCTIVE EARTH -V

ESTIVAILU DEPTH OE THE CONDUCTOR LIMLt UK IJf.CAUSE

.RESTS OHP-P

3too?

22

1007

l 1007

1007l

35

22l

37

5 l

1007 91

692

10071007

100753

216169

1007

45

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•CEPTH FEET

125

11675O

148 O

O156 142

17413978

17179O

47

67147

OO

O1131192347O

104103

. CO

P. r UNRELIAULE WCAl'SE THE STRONGER PART fit DEEPER OR TO ONE SIDE OF TH C FLIGHT

A SHALLOW DIP OR QVEfUjUftDFN EFFECTS

i t

j s i ANDAKDCOIL

LINE *AKOVflLY

51 A•51051C51051ESIF

j 51G

HF.ALPPM

354157

1066

t.'UAOPPM

131914181956

NULL-CUTLSFISH

QUADPPK

2202312

WHALE

QUADPPK

b635712

VEHTJCALCIKE

CONCvnos

403123188

DEPTH*FEL'T

510309

2113299

HORIZUNTALSHEET

CO NOKHOS

108111.22

DEPTHFEET

16216116713T158370311

CONDUCTIVEEARTH, j

RESISOil*-*'

23

1319760

10071007

DEPTH ; -,FEET ̂

119 !13938 419 ;,500 l0 '

52A52H52C52052FT

6392280

17

24221746

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810330

4698191

32

72

7107

***** -

Jl?2518

135115230

0206

117

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53A53353C53f)53E53F53G53M531

- 0274348n1

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6121716145

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. 00ii00

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12036lil41

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329

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. 1309

on60 .

110 .7 .

183

20

250328122

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55A55D55C55055E55F55G5DH

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117 .92 .

120 .215 .09 .

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t

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70 .0 .

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61611

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510071007

1970

16400

ILI) llEPTll NAY Rf UNRELIABLE PCCAUSE THE STRONGER PARTOF TIT CONDUCTOR M A Y pt UfLPr.R OK TO ONfl SIDE OF THE FLIGHTLIME* OH BECAUSE 01- A SHALLOW HIP OR OVf.RnURDCM EFFECTS.

SIANOARD GUI L

LINF s ANOMALY

57A 57R

i 57C57057E57F

REAL PPM

13 122444

OUAD PPM

97

101595

NULL-COILS FISH WHALE

QUAD PPM

0 0df.3-3 '

CHAD PPP

7 42632

VERTICAL CIKE

CONC KHOS

12 14

1224

DEPTH*FEET

77 109

01540

102

HORIZONTAL SHEET

COIYQKHOS

3 11111

DEPTH FEET

269 3199fl

146212355

CONDUCTIVE EARTH

RESTS OHV-K

15 12

306202127

1007

DEPTH -^ FEET ̂ 1

194 249

023670 .i

SPA58Rsec50058E58F

362

1364

83

121243

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3221?4

21319

119

702012068

118129

w

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15800

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. CIKE .

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. KHOS

.

12. 14

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119

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ER PART OF THF FLIGHT

EFFECTS.

LINE iANOMALY

63A630 63C 630

i 63E 63F 63G

SlAftOAKO COIL

REAL I'HM

1129 27T

99ion

0

UUAD PPM

228 27 6

22 17 8


OUAOPHM

0 -2 -1

1J 0

-2

GlJAf) PPW

2 5

13 ?7 69f*

VEHTICAL DIKE

CONO MHOS

58 1110

120 1C9

1

DEPTH* FEET

136 27 21

110 5 20

HORIZONTAL SHEET

CONOMHOS

12 3 32

;6381

DEPTH FEET

361 162 159331 111 106

0

CONRUCTIVE EARTH

RESIS OHK-M

1 13 16

1007 1 1

222

CEPTH FEET

319 91 890

91 920

61A 61B 64C61061 E 61F

13 11 82

73 3

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10 2041

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260 270215110 117 111

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CONEr/HOS

101

232

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314

34

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125101

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20611919

1136763750

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115163102

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13996

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198110

110979

HORIZONTALSHEET

CONDMHOS

.

3161

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DEPTHFEET

2882462592084

493352209

38123fl222278

0

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364302411302

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,* ESTJMAfEU DEPTH f'AY BC UNRFILIAIJLE BECAUSE THE STRONGER PART .. OF THE CONDUCTOR f'AY Rt.- DEEPER OR TO 0^ SIDE OF THf FLIGHT .. LINK* on OKCAU.SE OF A SHALLOW DIP OR OVERBURDEN EFFECTS. .

LINE sAKOKALl

76A760 76C

i 760 j 76Ei

77A770 77C 770 77E 77F 77G

STANDARD COIL

MEAL OUAD ' PPM PPM

72942 t

21

1411 15 0 5

127 . 1

615 30 6 5

in9

13 5 9

35 2


yijAH CI.IADPPM PPM

0 0-n

-1-3

0 0

-3 0

-1 4 0

2 3 6 3 0

5 2 3 2 3

16 0

VERTICAL HORIZONTAL, DIKE SHEET

CONC DEPTH* corjO' CEPTH MHOS , FEET WHOS FEET

8 24 12 4

03

9 10 10 1 3

92 1

121 50 46 55 39

70 9780 0 .

67 0

172

2 , 6 4 1

16

3 3 3 11

?11

•. , : , .345 217 176 265 252

240 293 255

0 244 88

423

CONDUCTIVE)EARTH; v ;

RES IS " DEPTHOHK-M FEET' - t , ; . - ' - ' '

1007 4

12 1007

1

22 20 18

1007 92 1

1007

0 165 111

0' 2 18

154 203 173

0 108 66 0

78A 7Pn 7BC

5 8

15

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10

1 0 0

0 0 0

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3 87 .6 106 .

15 58 .

124

258301249 '

964311

122193180

79A 790 79C 790 79E 79F

6 4 6 7

89 5

8 4

11 17 29 4

0 •1 1 2 ?0

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* * * * *9

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553 3

66 6

77 179 68 43 20

126

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2211

162

272420229176134371

611007

86931

1007

1510

10157

1050

13 5B 23

18003

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76212

6937

237168214

281

13

0. U.C.USC OF O,

146136142

P1A 810 81C 810 81C

1 25 4

2 'l 176

7 24 8 8

39

1 ?0 01

2 7 2 **

11

*

*

*

t

*

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1 10 3

39 143

50 . "9 .

112 . 61 . 7 .

1 3 1 9

31

167 190 293 233 98

1007 15

1007 2 1

0 119

0 1^2 80

82A rt 2 (3 82C 820 82E

j. re

l21 6.1 11 5

8 16 2f\ 5 5

2 31 0 0

2 3 6 3 3

4

V

*

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K

*

1 131320 c

0 43 32

12'f 141

t

*

t

t

*

*

1 4 4 5 2

45 207 167 348 374

236 12 10 7

1007

0 135 103 278

0

t*"-

SIAMUAUO MULL-COILS . VERTICAL . COIL FISH WHALE . DIKE .

LINE s,ANOMALY

83A 03D 83C 8?. D83E

81A BIB flIC*1D 81E *1F81G Bill

85A P5B 85C 85085F. B5F 856

P6A •J6B86C 860 86E *6F06686H

87A 87B 07C 87087E 87F 876 87H

REAL PPM

10 6

inI)

13

131 56 1 0

19 5

5 2 6 0

14 7

160

8 91 3

23 B11

21 23 18 26 2

10 3

UUAD OllAD PPM PPM

28 18 11 3

16

1 5 88 36

13 2

8 3

13 3

11 1

61

871 6

11 1

12 .8

11 6

22 61 3 6 5

,* ESTIfAlLU UEPTH . OF THE CONDUCTOR . LIME, OR BECAUSE

-1 0 3

-12

-3 -300

-23 1 0

-3 0

-2 0

-2 2 3

3 30 1

-1-3 20

2 21 2

-1 0 0 0

f A Y B f A Y OK A

SUAO . CONC PPM . MHOS

**

8 5 3

t 3

*

16 ! 123 1 71 1 0

*

t

5 2 3

* 2 2 r'

*•'

33 P 23

. 35

^

4

1 2 2 33 0 25

E, UNRELInL DCEPESHALLOW

3 2

181b

16 11 5

101

16 11

1 231

11 13 59

a10

i3

25161 2

15 56 331

10 3

353

DEPTH*! FEF.T .

.

23 !11 . 80 .0 .

11 ..

75 ;31 .1 n '" *91..

192 .0 .

61 . 211 .

*

65 \ 132 . 61 .0 .

100 .159 .

6 .*

25 i11 .

106 . 80 . 61 .eo .0 .

78 .*

12 Ieo .38 .o n '0 *

153 . 157 . 87 .HO ,

HORIZONTAL SHEET

CO MD f'HOS

.

11 51 2

9 11 2 31 1 1

11 11 3 3

15

23 1 1 611 1

1 13 913 1 01

DEPTH FEET

131 167 268

1 .200

321 239273 287 189

0 235 501

266 359 211

1290 110 99

212271 312 207 21036121

259

212 250 175269 107 121 283358

ABLE BECAUSE THE STRONGER PART R OR TO OP^E SIDE OF Tllp FLIGHT DIP PR OVFRnURREM EFFfCTS.

CONDUCTIVE EARTH

RESIS OHV-H

77 109

810P7

36

3 100?

78 53

10071007

9 1007

71 1007

911007

17 1007

1

3122

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11007312

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32 19

205. /T- 0'.:' 107, "'•--

273 0

lil 172

00

172 0

110 0

830

205 0

72

139186

0 0

18500 0

119 220 132

0 0 0

2310

S'lANUARUCUIL

LIME SAKOMALY

IflAQ fi M1PCOBD

R9Afl9RageR9D

90A9on90C90R90E9oF

REALPPM

277

122

0191913

23H2

191614

OUAOPPM

1012123

320201

1374

1456

-,,-- — ,-.~.-^n fnr-svtpjjp* **r*R: J^TTJr^V'I*!

HULL-COILS VERTICAL HORIZONTALrtsnUUAnPPM

00tl0

0200

-100001

WHALE

CHADPPM

5230

oQ

42

21?.300

DIKE

CONCMHOS

"

35493

1B9

60

1932

133924

DEPTH*FEET

573966

C 102

.

03441

135

46105125567296

SHEET

CO NOfHOS

9v31

133

14

511496

DEPTHFEET -

227202255366

'.. ' * '."' '.; ' . '

Q132190352

215298352225274305

. . 1

CONDUCTIVEEARTH^ ''

RESIS DEPTHOHM-r

: -, ' 376

V 221007

i . - *' . '

100722211

610071007

1235

FEET

17978

166:'.'t'- 0

: ."- ". - *- - j

0102111315;

( 1

1570* 0

159224242

,* ESTICAltU REPTH fAY BF! UNRELIABLE BECAUSE THE STRONGER PART .OF THF COMHUCTOR f'AY Rt OEEPER OR TO ONE SIDE OF THE FLIGHT .

' L1MF. OU BECAUSE OF A SHALLOW DIP OR OVERBURDEN EFFECTS. .

r-

•HN01NE0001 DAVIEAUXSQ RUNNALLS030

REPORT NO 576HB

GEOPHYSICAL ENGINEERING LIMITED

NORTH BAY, ONTARIO

* FINAL REPORT

ON

AREA JJ - BATCHAHANA EAST

FOR

THE DIGHEM SYNDICATE

N.T.S. 41 N/l

November 22, 1976

m m.

W

AREA JJ

'LOCATION MAP• 4*1*1 M* 00'

14*15* •4*OO'

Scole : 1:250,000

BATCHAWANA,SOUTHEAST,ONTARIO

•,. Ill 111111111111 i"l 11111111111111?! 11111111111! i l?l 1111111 111111 M 111111111111

1c - .-- .SUMMARY

Follow-up of Dlghem anomalies was carried out•** *

during the period May l, 1976 to October 16, 1976.' * -

Geological reconnaissance revealed that the felsic

rocks are much less extensive than originally believed.

Thus, numerous anomalies which appeared to warrant*v*i

follow-up because of tpftire proximity to felslcs were

eliminated from further consideration.

* Eleven anomalies were adequately explained oni

surface, two by diamond drilling. Eleven others werei . ' . jT*1" rejected due to unfavorable geology.

*

RECOMMENDATIONS

NO further work.

0)

LINE MILES FLOWN 497

GROUND INVESTIGATIONS UNDERTAKEN 24

CONDUCTORS LOCATED BY SYNDICATE ACTIVITY

Explained on surface 9

9CD-11D. 14A, 31B-33A, 31 COE, 55E,

55GH-56E, 62DE-64E, 79A, 84C.

Explained by diamond drilling 2

39A, 40B.

Unexplained but rejected due to geology 11

148, 17BC-19C, 45A-46A, 48A-49A,

55A, 57A-59A, 70A-71A, 76A, 82B,

85A-87AB, 90A.

CONDUCTORS NOT LOCATED 3

37AB, 84A, 84B-85B

CONDUCTORS EXPLAINED BY OTHER COMPANIES 7

. 1A-5B, 2AB-5A, 10AB-11AB, 40A-70B,

52E-56C, 72C-77C, 7CA-78A.

b

ttl Job 984 JJ MTS N/1

DICHOt SYKOICATC

TABULATION Of CONDUCTORS.fttvifcd January/;?

1KTW1M July ?t/:^ FINAL Boy.

y Conductor DesignationDlghem - Anomaly Character Max. mho valueNo. of linesDepth Estimated

0 - Open . , X - Slaked by others S - No. of claim staked by syndicate

Ground- Follow-up ttodef taken

V. L. F. ReconnaissanceY. E. M. ReconnaissanceV.l.F. Profiles

C y. E. H. Oelall5 Horizontal Shootback E. H.^ Olher SurveysS No. of tests for OJiralle) conductor

No. of tests for conductor widthtfo. of 1ln*f nf fru{'niktnrt*t*r

d local oeoloov ("aooed (checked)

"f Conductor axis trenchede Jlonductnr axii- r1rMl.il

l No. of geochemical soil samplesi No. of rock samples analysede No. of basal till samples

Previous Activity


Conductive Material

Anomaly Located: Yes-Y; No-NLength of Anomaly 1n feetConductivity Rating by

ground E. H. or S. P. responseMagnetic Response in ganmas (g)1st lw ted Depth to Source


Geocheoical Analyses: S-Soil

(Max. value* in ppn) BT-Basal Till

Composition

True Width in feetRock Assays

Abnormal assays Spct'senlquantitative spectrograph i c

Distance from OOH OIQHfH respor.

or Trench to lux. t i n feet.

Conclusions or Recomnendatlons

1A-5B11 -4

28' to 133'0

Geology, geophysics !9M-65-R1ocanex.

Strongly netamorph George Slrluga - ei

Graphitic shale. IDS pyrite and pyrrhotite, some Mgnetlte.

Graphite.

[xplalned as graphite and barren sulphides. No work.

IBq1

148' '

0

1 - - . .

ZAB-SA91

- 4S?' to ISO'

0'

.

4B !; V-:'.

41K*

0

. .

Geology. Hag. VCH. Gravity 1964-65 ftlocanex.

-

osed sediments (veroal report fron O.D.M. oeologlst ap to b* published next year).

Unfavorable qeolooy. Ho work.

.

located and nroh- ibly explained by Rlocanex. Unfavorable

No work.

Unfavorable geology. tto work.

ea Job w JJ m w.

OlCMtN SYNDICATE

TAWWTIOH OF CONDUCTORSRtfUttf

INTUM July ?V7g HNAt


Olghea - Anonaly Character

Max. oho valueNo. of linesDepth Cstlnited

0 - Open X - Staked by others S ' no. of cla1*s naked by syndicate

l•1

1Si

w

t, l. F. ReconnaissanceV.I. M. ReconnaissanceV.I. F. Profiles

v v.E.n. DetailS Horltontal Shootback C. H.'S Other Surveys•3 No. of tests for oarallel conductor

"o. gf ^ests for conductor width

* local 0*0 1 0*1 v w

"f Conductor axis

aooed (ch-ckedl

trenened

f No. of oeochewleal soli s*molest No. of rock sanples analysedc No. of basal till samples

Previous Activity


Conductive Material

Anomaly located: Yes-V; No*Nlength of Anomaly 1n feetConductivity Rating by

ground E. H. or S. P. responseMagnetic Response 1n ganaas (g)[stlnated Depth to Source

by ground geophysical methodsgeological Description

CeocheMlcal Analyses: S-Soll

(Kax. values In ppa) BT-Basal Till

Composition

True Width In feetRock Assays

A'nonntl *;;.*ys

Spct'semlquantltatlve sprctrographlc

Distance from OOH or Trench to mjx. DIGHEM rfiponse In fret.

Conclusions or Reconnendatlons

7A-8811Z

134* to 149'

8A-11Cg4

49* to IK*

JCO-110J14

340' tft UT

10A8-11Mu-

i4* to 1*1*

A.C.R. option - Vlbtrt Township

Strongly netacorpho Ceorgt Slrluga - w

-

*

Geology. tH, nag. gravity- 1964-65 - Rlocanex.

sed sediments (verba p to be published nei

Unfavorable geolony No work.

1

x.

t

10

2

Geology. EM, Mg 1965-Canex.

y800 openStrong

2S*

1 report f rea O.D.M. it yeir).

Hetanorphlc quart* lite. conglomerate, graphitic shale.

Graphite.

800

tiplained as barren griphite. No further wort.

j

gravity* 1964-63- Itlocanu. ' .

geologist

located and protubly eiplali by Rlocanex. Unfavorablt gtolony. No work.

OICHCN SYNDICATE

TAWUTIOH Of CONDUCTORSJob Jfl4 JJ NTS H/l

M..INTERIM July 23/76 HNAl Nov. 22/76


Dlghen - Anomaly Character

Max. mho valueHo. of linesDepth EstlMted

? - Open X - Staked by others - No. of claim staked by syndicate

Ground Follow-up Undertaken !

V.I. F. ReconnaissanceV.E.H. ReconnaissanceV.L.F. Profiles

5 V.E.H. Detail

t Mor 1 rental Shootback E. H.p Other SurveysNo. of tests for conductor width

* liOiff \ Q^gfoQv maoDed fch*cked)

"j Conductor axisfnnrfnrfrftr jialt t

trenchedrirH1*H

f No. of geochemical soil samplest No. of rock sar.pl ei analysede No. of basal till samples

Previous Activity


mt. 4

2•i

1iL

Anomaly Located: fes-Y; No-HLength of Anomaly 1n feetConductivity Rating by

ground E. H. or S. P. responseMagnetic Response In gamius (g)EstlMted Depth to Source

by oround geoohyslcal methods


Ceocheaical Analyses: S-Soll

(Max. values 1n ppm) BT-Basal Till

Composition


Abnormal assays

Spct'sralquantitative spectroqraphlc

Distance f rom ODH or Trench to max. DIGHfH response In feet.

Conclusion) or Recom*endat1ons

14A11

1209'

MBM1

71'

178C-19Ctt

128' to 154'

184t1

85'

A.C.R. option - Vibert Township

tt)

2

CraphHe shale.

Graphite.

200

Explained as barren graphite. No further work

i

xi

lx

t *

2

Y1500 ooen south

StrongPartial ISOg

25'

Strongly netaaoriQuartzite and shale (a weak possibility that the rocks nay be a metamorphosed felsic to Inter ned late lapilli tuff).

x

2R -

I

t

X

31

Y?600 ooen

StrongBackground

25'

phosed sediments.No outcrop on the conductor axis. MetaquarUHes nearby.

-

The conductors not eiplalned however the geology unfavorable. No further work.

'

-


ea Job NTS 41

UlUHth &INUJIAU

TABULATION OF CONDUCTORSINTERIM July 23/78 fJW. Hiv.


Dlghea - Anomaly Character

Max. mho valueMo. of linesDepth Estimated

? - Open . X - Staked by othars - No. of claims staked by syndicate


V. L. f. ReconnaissanceV.E.H. ReconnaissanceV. l. F. Profiles

5 V .E.M. Detail5 Horliontal Shootback E. M.p Other SurveysS No. of tests for Baril lei conductor


* local aeo!o?v maosed (checked)

"c Conductor axisBrouuvtMltrenched

43 fftftrfurtnf arlt rirlllprf

f No. of geochemical soil samolest No. of rock samples analysedo No. of basal till samples

Previous Activity


Conductive Material

Anomaly Located: Yes*V; No-fllength of Anomaly 1n feetConductivity Rating by

ground E. M. or S. P. responseMagnetic Response In gammas (g)Estimated Depth to Source


Geochenical Analyses: S-Soil

(Kax. values 1n ppm) BT-Basal Till

Composition

True Width in feetRock Assays

Abnormal assays Spct*sen1quantUat1ve spectrographlc

Distance from DON or Trench to max. DIQHCH response In feet.

Conclusions or Rec emendations

31B-33A

933 -

34' to 193'

JlCne .171

63' to 120'

37A8

81

37C181

H*' to 129' 78-

A.C.R. option - Vibert Township. '

xx2xx

4

X

x

11

y1200 open

Strong

6000a negative25'

Felsic to Inter- Mt1*te lapilli tuff, graphitic Shale with some pyrite, diabase dike.

Graphite.

200

Explained as graphite with barren sulphides. No further work.

x

2

R

'

' V *

Serlclte-schlst (altered quartz ite?), graphitic shale.

Graphite.

100


xx2xx

SP

3x

>

?

Intenreelate ash. lapilli anl block tuffs

-

Surveys at greater than 200 foot coll separation Imp ossible due to topography. Nearby conductors caused by barren graphite. No further work.

li

;

•'

Not surveyed. The qeolooy no) very encouraqlr Conductors on itrlkc caused by barren qraphlte. No work.

DICHtrl SYNDICATE

TABUUTION Of CONDUCTORSsn. Job .964 jj m 4i H/I INTERIM FINAL- Ha*


DI f. hem * Anomaly Character

Kax. mho valueWo. of linesDepth Estimated

0 - Open X - Staked by others S - No. of claims staked by syndicate

|

gi

V.I. F, ReconnaissanceV.f.H. ReconnaissanceV.I. F. Profiles

S V .E.H. DetailK Horizontal Shootback t. H.1 Other Surveysu No. gf tests for parallel conductor


* local aeolocv rao?*d (checked!Ij rnnrfwfnr H\\"f Conductor axis

prntt*rforftrenched

u fnnrf-irfnr jrlt Ar\\\rA

f No. of geochemical soil samples•- No. of rock samples analysede NO. of basal till samples

Previous Activity

1 Results of Follow-up

CowJuetlve Material

Anomaly Located: Yes*T; No-Nlenqth of Anonaly In feetConductivity Rating by

ground E.M. or S. P. resoonseMagnetic Response In c,anmas (g)Estimated Depth to Source


Geochemical Analyses: S'Soll

(Kax. values In ppm) ST-Basal Till

Composition

True Width In FtetRock Assays

Abnormal assaysSpct'tenlqujntUatlve spectrograph^ AA- atonic absorption.Distance from DDH or Trench to rax.

OICHfH response In feet.


39A29

139'

A.C.R. optlon- ViMrt Township.

X

xx

4

xi

•-nnH .Ml

" 13

40A-70814731

0 to 119'

0

. -. -- . .

T1200

StrongSOOg direct

25'

Intermediate lapilli and ash tuff. DON - felsic tuff,

graphitic shale with 1 OX-402

Graphite, pyrite

24.8*AA-nax ppm- SSCu,

4SNI. I.SAg, 3Sppb Au.

400

Explained MS graph itic shale and Mrren sulphides. No further work.

EM, Mg surveys, packsack drill holes, trenching.

Sediments, Iron formation, pyrite, pyrrhotite, graphite.

Graphite, pyrite, pyrrhotite.

CiDlalned by others as nraphite and barren sulphides. No work.

406341

101*A.C.R. option* Vibert Township.

x

txx

.4

Xi

i.nnti .1.1?

11

T700

StrongISOg flanking

25'

Felsic lapilli tuff, diabase. Dusty sections Jn the tuffs. DDH - felsic tuff

and breccia. Graphitic shear with pyrite

-

Graphite

10.9A-Cu. 23pom Cu.10 Dp* Pb, 51 ppm In, 0.4ppn Ao.

AA- max ppn SJCu. 101N1. l.lAg. li ppb Au.

100

explained as qrapnlte. The sulphide in the drill hole is barren. Ho further work.

'448*541

5111

0 to 19^'

0

i

Sediment*.

A lonq anomaly unfavorable

No work.

Oob 964 JJ HTS O H/1

DICHOt SYNDICATE

MBUUTIOB OF CONDUCTORSINTERIH July 33/1S Jtev.


Dlghem - Anomaly ' Character

Hax. mho valueNo. of linesDepth Estimated

0 - Open , , X - Staked by others S - No. of claims staked by syndicate

cm k

o

I

S

0

V.L.f. ReconnaissanceV.E.M. ReconnaissanceV. L. F. Profiles

u y.E.H. Detailv Horizontal Shootback E. H. " ""o Other Surveys


} Local oeoloov maooed (checkpdl

"j Conductor axis trencheddrilled

| No. of geochemical soil samplesy No. of rock samples analysed 1c No. of basal till samples

Previous Activity

Results of Follow-uu

Conductive Material

Anomaly Located: tes-Y; No-8Length of Anomaly in feetConductivity Rating by

ground E. H. or S. P. responseMagnetic Response in gammas (g)Estimated Depth to Source


Ceot.:.*ffl1cal Analyses: S'Sotl

(Hax. value* in ppm) BT-Basal Till

C cm position


Abnormal assays Spct*sea1quant1tat1ve spectrographtc

Distance from OOH or Trench to max. 01GHF.M response In feet.

Conclusions or Recommendations -

45A-46A 48A-49A10 4Z 2

3* to 148* D to 19'

00

r.)

2

Mafic pillow lavis, tops south.

Unfavorable geology. Ho further work.

47Azz1

so0

.

Sediments.

Subsidiary to and probable Part of a long anomaly lone .caused by graphite and barren sulphides In Iron formation and sediments. No work.

49E-HO44

0 ta ft?'

0

-

-

-

A weak anomaly In sediments. No work.

SJC-S6Cea -;

7' t6 M*A.C.R. option* Vibert Township

-

Geophysical ' surveys, two drill holts* ! Cane*.

Sediments (T). Pyrite, Minor chalcopyrite.

Explained by Caner. as barrer sulphides. No work.

DICHM SYNDICATE

TABULATION OF CONDUCTORSea Job 184 HTS 41 N/1 INTERIM July 23/76 HNAl


0*1L i -.i- 1 Max. mho valueCHirlrtcr ' "O. of ItneS

1 Depth Eslimated0 - 0P*n , , * - Staked by others S - No. of cUttis staked by syndicate


l Geophysics

>

1

I

1

-

Si zott

V K

i Conductive Material

V. l. F. ReconnaissanceV. E.M. ReconnaissanceV.L.f. ProfilesV.E.h. DetailHoriiontal Shootback E.M.Other SurveysNo. of tests for parallel conductorNo. of tests for conductor width

Local aeoloQv mapped (checkedl

Conductor axis trenchedConductors, li drilled

No. of geochemical soil samplesNo. of rock samples analysedNo. of basal till samples

Previous Activity

Anomaly located: Yes-Y; No-Nlength of Anomaly In feetConductivity Rating by

ground E.M. or S. P. responseMagnetic Response In gamjs (g)Estimated Depth to Source



Geochentcal Analyses: S-Soll

(Mix. values in ppm) BT-Basal Till

Composition•k

True Width in FeetBeck Assays

r.-nomvil assays

Spc t' jemt quantitative spectrograph t c AA - atomic absorption.

Distance from DOH or Trench to eux. DIGHfM response In feet.


S5A

241

186'

0

xx2x

IX)

N

Mafic pillow lavas, tops south. Diabase dike.


sst101

92'

SSGH-S6C

102

0 to 215'

A.C.R. option - Davieaux Township

(x)

Slaty sediments, graphitic shale, diabase.

100

Explained as graphit*. No further work.

X

1

tJt , - '

x

20•3

Y600 ooen

Strong2SOg

Mafic volcanics Intermediate tuff, graphitic shale.

S-Max 29? Cu, 42 Pb, 877 In.

Graphite.

Z2S cms.

AA - rax *65ppti Cu, 32ppm Pb, 680ppa In.

300


S7A-S9A

12 !3

O to 77*

o .~

M

\

}

l' l

i. i

1

- \

Mafic pillow lavas.

Unfavoraole geolsqy. Ho further worl

OlCHtM SYNDICATE

TWUT10N OF CONDUCTORSen. Job 984 JJ NTS 41 N/1 . ' IKTMIM Joly 23/75 flHAl Nov. MW -


Dljhem - Anomaly Character

Hi K. mho valueNo. of linesDepth Estimated

? - Open J - Staked by others . Mo. of Claims staked by syndicate


V.I. F. ReconnaissanceV.E.N. ReconnaissanceV.I. F. Profiles

5 V.f.H. DetailS Horizontal Shootback E. H."g Other Surveysu No. of tests for parallel conductor

No. of tests for conductor widthFlo. of linn nf

* loca] aeoloav freinetoeeter-

SDDed (checked)e . .

7 Conductor axis^ f H r tn si i

trenched[•rillixi

S No. of geochemical soil samolesCo. of rock samples analysedNo. of basal till samplesPrevious Activity

Results of Follow-wo '

Condvctlve Material

Anomaly located: fes*Y; No*Hlength of Anomaly 1n feetConductivity Rating by

;round E. H. or S. P. responseMagnetic Response in gaemas (g)estimated Depth to Source

by ground geophysical methodsGeological description

Ceochenlcal Analyses: S-Soll

{Ka*, value) 1n ppm) ST-Basal Till

Composition


Abnormal assays 'Spct'seffiiquantttative spectrograph le

Distance from OOH or Trench to max. DIGHfH respons* in feet.

Conclusions or Recontnendattons

57C-S8C112

0 to 118'0

On strike of a hortton of sed iments. Probable unfavorable geology. No work.

570-71BC2313

10' to 129'A.C.R. option- Desblens Township.

A long anomaly probably in sediments. No vork.

S88-S98 *1)2

0 to 201 '0

Kaflc pillow livts 400 feetto the north.

'


'S.'C.*1Ci4

20' to 78*.. , - o-- -

!

i

'

ii

'

Subsidiary to and probably wi a similar sourc is anomaly 40A-700. Unfavorable geology. No work.

v-" -V." '^^^^mm^^^m^^.^^^DlOHtn ilHUUAIt

ta Job M* JJ NTS 41 "/lTABULATION OF CONDUCTORS

INTERIM July 23/76 FINAL ,Nnv.

t Conductor Designation

Dlghem - Anomaly Character

Man. mho value(lo. of linesDepth Estimated

Q - Open I - Staked by others 1 - No. of claims staked by syndicate

Srwnd'Follow-tfo Undertaken

V.L.f. ReconnaissanceV.E.M. ReconnaissanceV.I. f. Profiles

" V.C.H. DetailS Horliontal Shootback l M

f Other SurvevsNo ( gf tests fgr conductor widthfta of llnpt nf

* Local oeoloov wrjnn?tn-~t-r

aooed (checked)

*f Conductor ails trenchedCnndiirtnr- *iiijrti-Ul.rf

f No. of geochemical soil samplesv No. of rock samples analysede No. of basal till sanoles

Previous Activity

Results of Folio*-1*

Conductive Material

Anomaly Located: res-t; Mo-HLength of Anomaly 1n feetConductivity Rating by

ground E. M. or S. P. responseMagnetic Response in gannas (g)Estimated Depth to Source

by ground geophysical methods(eoloqical Description

(technical Analyses: S-So1l

(Max. values 1n ppm) KT'Basal Till

Co" position


A -normal assays Spct'seolquantltatlve spectrograph^

Distance from DDH or Trench to MX. OKJMfrt response in feet.

Conclusions or Recornnendattoni

61A-63A

583

136' to 218'0

Mafic pillow lava.

Unfavorable •geology, a short distance on strike to the northwest and southeast. No work.

I2K-64C

4153

2* to 27 1A. C. R. option* Desbiens Township-.

KIR

3 '

X

*

T1000 open

Yery Strong)6,SOOg direct

W

Mafic volcanics. Iron formation.

Documents

GEOPHYSICAL ENGINEERING LIMITED€¦ · TEL; 416-3(2-1571 TELEX: 02-39087 March 4, 1977 Mr. L. Oliphant, Algoma Central Railways, P.O. Box 7000, Sault Ste. Marie, P6A 5P6 Dear Len,