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
by ground geophysical methods
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*
Conductor Designation
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
by ground geophysical methods
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
Ground Follow-up Undertaken
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
by ground geophysical methods
Geological Description
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.
Conclusions or Recommendations
' '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 ?^*;^;
Conductor Designation
Dlghe* - Anomaly Character
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.
Conclusions or Recommendations
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.
Explained as graphite. No further work.
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
by ground geophysical methods
Geological Description
Geochemical Analyses: S-Soll
(Max. values In ppm) BT-Basal Till
Composition
True Width In FeetRock Assays
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.
,
Unfavorable geology. No work.
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^ ' \
Conductor Designation
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.
Unfavorable geology. No work.
.
*
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. . .,
Dlghe* - Anomaly Character
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
Geological Description
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
Explained as barren graphite. No further work.
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
Conductor Designation
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
Geochemical Analyses: S-Soll
(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.
.
Unfavorable geology. No work.
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
Conductor Designation
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
No. of tests for conductor width
* 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
Results of Follow-uo
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
True Width In FeetRock Assays
A -normal assays .
Spct'semlquantltitlve spoclrographlc
Distance from OOH or Trench to man. O'.Win r esponse In feet.
Conclusions or Recommendations
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.
-
Unfavorable geology. No work.
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
Results of Follow-up
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
by ground geophysical methods
. 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.
Conclusions or Recommendations
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
Conductor Designation
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
Geological Description
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.
.
Unfavorable geology. No further work.
.....- . ..-;.: ; 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
AREA J J -ANOMALY 39 A
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
AREA J J -ANOMALY 39 A
GEOLOGYDATE Jl/NE.1976. 984
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liA'? - 5•* , ' f~
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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
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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
Ground Follow-up Undertaken
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
by ground geophysical methods
Geological Description
Geochemical Analyses: 5-Soll
(Max. values in ppm) BT*Basal Till
Compos 1 1 Ion
True Width 1n FeetRock Assays
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.
Conclusions or Recommendations
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.
Conductor Designation
Dlghe* - Anomaly Character
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
Geochemical Analyses: S-Soll
(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.
Conclusions or Recommendations
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
in5
127
2 A
12 5 1
6
NULL-CUTLS T I Sil WHALE
WAD KUADPPM ppw
0 -1 -11 4 1
-1 -1
0 0 2
0
2 0 37 4 2
2 3
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
IIA118
106
36A36B36C
23
- 5
1233
0-1
0
100
37ft 370 37C 37D
6 9
16 11
6 9 9 6
0 -1 2 1
*
5 7 3 3
7 fl
18 15
129 . 115 . 78 .
100 .
2 3 5 4
359 311 269 319
1007 267
11
0 217 205 211
178
75
-l
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2912
39 Hi
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3 161
7 6 6
0 2 0
0 2 0
2 31 1
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1 f) 1
213 303 275
1007 3
1007
0 219
0
79
125
113
50lin
215
331
1007
1007
151
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
25 Q39 'i
3 0
14 o4 1
4 -l10 -114 o
7 010 115 i|
13 n3n 2
5 i*13 l
17 o11 2
5 23 - G
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
*
DEPTH*.,PEF.T .
*25 .'
180 ..*
25 . 0 .
207 ..
''0 I192 .
*
14H |••2 .73 .
.
43 ,"30 .B .
.
60 !1 .0 .
21 ..
39 ;26 .
' 0 .133 ,
t
tt
0 .24 . 22 .12 .41 .76 .
4
19 .'19 .
126 ."7 .
HORIZONTAL SHEET-.
COMDWHOS
t
81
9 92
122
3182
3302
61211
1 1011
167111
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
10071007
•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
-10300
810330
4698191
32
72
7107
***** -
Jl?2518
135115230
0206
117
10073
9991m
0152
53A53353C53f)53E53F53G53M531
- 0274348n1
3Db2
6121716145
1274
nn2
. 00ii00
245352222
12036lil41
3642
' 0462356382734
117111
179
1211911
0213177196199161196344337
1007321
681007
210071007
0161135159730
15000
54A54054C
329
85
57
22
40
-2
206
. 1309
on60 .
110 .7 .
183
20
250328122
1251
22022897
55A55D55C55055E55F55G5DH
732
1015
11742
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21503033
32
1027442
2436354
1010102
186 .59 .11 .
117 .92 .
120 .215 .09 .
6- 9913331
452218116331294365512401
100722
100720
100710P71007
0172820
204000
56A56056C56056L
190
2623
92
1464
00022
31212
t
4
4
4
4
241
2213
70 .0 .
54 .0 .0 .
61611
2550
210119226
51007
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
-20nl23
3221?4
21319
119
702012068
118129
w
131332
251476
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134100734222
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9800
15800
. VERTICAL .
. CIKE .
. CONC
. KHOS
.
12. 14
1224
.* '
21319
119
*
*
114
252S731
20*t
538348
t
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12284
74. 415
6
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*77 !109 .
0 .15 .40 .
102 .*
70 !201 .20 .68 .
118 .129 .
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0 .0 .
14 .93 .31 .63 .73 .29 .69 .
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112602114
00
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374
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00
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371
17712
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7311
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0134106108145
0
,* rSTIPAHU DLPTII CAT IT IJNRFLlAMLE RECAUSE THE. OF THE COWHUCTOft M/iY nL CCLPrn OR TO ONfT SIDE. LINE* OH MirCAUSE PH A SHALLOW'O IP OR
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
NULL-COILS FISH WHALE
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
li7
111225 3
2 2
-212 0
5 3 117 0
10 2041
55 4
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3 5'•21
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260 270215110 117 111
197
61332
1 1007
171 201100
0 111
0
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nl2?10
136512
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.*
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58
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66A66066C66066E
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13
i9g
15 60
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133 4
13
201166 170 251 226
100720 18 10 1
091 94
188 191
67A670 67C67067E 67F 676
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t
120
1 23 3712
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167 .
1 511 6 9 3
253 353157118 193 212 130
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1111007
4 ' 2 1007
0 282310
113 168
0
7O
71
2l
5 l
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2l
287 O
10071007
OR
Oo
7QA 7QO 70C
71A 71B 71C 7lD 71E
72A 72R 72C
74A74B74 C•74D
75A 750 75C 750 75E
549
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494
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9
9
9
9
9
9
9
9
9
9
9
9
9
9
9
9
9
VEHTJCALCIKE
CONEr/HOS
101
232
14K7
29e
10fl1
314
34
245
72464
24
1010
55
125101
DEPTH*FEET
6466fl3 .54
20611919
1136763750
682547
115163102
6H3fl
153
13996
15965
198110
110979
HORIZONTALSHEET
CONDMHOS
.
3161
422
62321
111
1162
16111
1143
12
Ifl31
DEPTHFEET
2882462592084
493352209
38123fl222278
0
246202200
3024133161391R617439fl
364302411302
4953302*232fl304
10071007
31
5271826
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72
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OO
111
315 148 142 180
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105o
81
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25145
156136
O
O O
335 O
O O
251240
O
,* 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
NULL-COILS FISH WHALE
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
10 9
10
1 0 0
0 0 0
OOB8QC
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
1 2 25 3 3
* * * * *9
*
553 3
66 6
77 179 68 43 20
126
* * *
. t * * *
2211
162
272420229176134371
611007
86931
1007
1510
10157
1050
13 5B 23
18003
H23
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
*
*
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
*
*
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
1007 1007
11007312
1007
10 1 2
1007 1007 1007
31007
* t t
DEPTHFEET
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
Results of Follow-uo
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
by ground geophysical methodsGeological Description
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
Conductor Designation
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
Results of Follow-up
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
Conductor Designation
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
Results of Follow-up
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
Geological Description
Ceocheaical Analyses: S-Soll
(Max. values 1n ppm) BT-Basal Till
Composition
True Width 1n FeetRock Assays
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.
'
-
Unfavorable geology. No work.
ea Job NTS 41
UlUHth &INUJIAU
TABULATION OF CONDUCTORSINTERIM July 23/78 fJW. Hiv.
Conductor Designation
Dlghea - Anomaly Character
Max. mho valueMo. of linesDepth Estimated
? - Open . X - Staked by othars - No. of claims staked by syndicate
Ground Follow-up Undertaken
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
No. of tests for conductor width
* 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
Results of Follow-up
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
by ground geophysical methodsGeological Description
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
Explained as graphite. No further work.
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*
Conductor Designation
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
No. of tests for conductor width
* 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
by ground geophysical methodsGeological Description
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.
Conclusions or Recommendations
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.
Conductor Designation
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
No. of tests for conductor width
} 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
by ground geophysical methodsGeological Description
Ceot.:.*ffl1cal Analyses: S'Sotl
(Hax. value* in ppm) BT-Basal Till
C cm position
True Width In FeetRock Assays
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
Conductor Designation
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
Ground Follow-up Undertaken
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
by ground geophysical methods
Geological Description
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.
Conclusions or Recommendations
S5A
241
186'
0
xx2x
IX)
N
Mafic pillow lavas, tops south. Diabase dike.
Unfavorable geology. No further work.
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
Explained as barren graphite. No further work.
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 -
Conductor Designation
Dljhem - Anomaly Character
Hi K. mho valueNo. of linesDepth Estimated
? - Open J - Staked by others . Mo. of Claims staked by syndicate
Ground Follow-up Undertaken
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
True Width in FeetRock Assays
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.
'
Unfavorable geology. No work.
'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
True Width in FeetRock Assays
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.