township of ashmore work performed by: hollinger mines ltd ... · work performed by: hollinger...
TRANSCRIPT
42EieNWei45 16 ASHMORE 010
Diamond Drilling
Township OF ASHMORE Report NQ: 16
Work performed by: HOLLINGER MINES LTD. (WILSON s KALSON OPTIONS)
Claim NQ
TB 229617
TB 229616
TB 10971
TB 139353
Hole NO Footage Date
A-14-73- 790' June 11 3
NoteA-l-70 'A-2-70 -A-3-72 :A-4-72 -A-5-72 -A-8-72 :A-10-73 -A-12-73 '
A-6-72- 'A-7-72 '.
A-9-73A-ll-73 -
642'323.3'443'494'448'301'402'491'
492'302'
302'301'
Aug/70Nov/70Jan/72Jan/72Jan/72Feb/7219731973
Jan/72Jan/72
19731973
(D(D(D(D(D(D(D(D
(D(D
(D(D
(2)(3)(4)(4)(5)(5)(6)(6)
(5)(5)
(6)(6)
(l) (6) (7)
Notes:
( . .. ) date placed on file(1) (May/74)(2) 145/70(3) 228/70
(4) 6/72(5) 22/72(6) MEAP GB #33 (cross-sections only)(7) 102/73
AWL.004(r-69Jrev.9-7-2
iyxii'iiiit
. A 3 /S rt Q&jZ
Location of
A"
t
c PA,W2? from w,*p * on West Side of Claim TB 22961? ,^LO t,o. M^——.f ̂ ?'D|AIVIOND DRILL REpORTEAST. -*.ELEV. —— AZIM. DIP -
HOLE NO. COMMENCED.
/ -l
. ,. -, .100 'C' PURPOSE OF-
HOLE ———-—-.
Claim TB 22951?'
FROM
0
A3
1U
137
\*^
kX*
TO
Ae
115
-137
331
DESCRIPTION
CaoinK
Clroy r,ro(in n^iiuivo non na^nntic
Amiocito uniforn app. to coro
i'cldspar Tor. ('roy to ^-Toen
v.ith incr. in chlorito riuriorous plwnocrytv
of feldspar 2/10 of mi inch in ciia.
throughout aoBtioa.
Cwtfjcto (-round 23' C'ol of I'orphry.
Harvlod chloritic "uff or !"od. brov;nioh
b-rJ!icio rica? nml ^.roon chloritic b'lndn
ioc-'.Ily rdn \-'ith Pyrr Ty -*- chalco
bnruiin..- ' ' rtOO to 60 to i". A.
2 f l^icitic band at 157.
162* sn. blebs 1'yr. oba.
170 am blobs of pyrr. oba.
190 - 261 nottled
Lt. col. D-icitic Tui'f?
it 264' chorty section ninor pyrr. and
c lin le o
FROM
f '
3
170
192
2A2
261
ccTO
170.5
193
2AA-5
26A
)RE SAMPI
RECOV.
.5
1.0
2.5
3.
-ES
WIDTH
B
1.0
2.5
3.
ASSAY
50'
9(1 '
157*
215'
315
DESCRIPTION OF SAMPLE
l* f r.r'd Amesite
n-,)!j r. ij'netic
rattled fins fr'a nd ;;.-,i;.e
non n 'f n otic
I acite It. col. bracci ted
I'oitlftci ^nd or d-ic.tte?
! 1, cherty section '~yrr.
-
c: hi b -md :'yrr -*- c ha le o.
Vr?ry n.-ii -K-tic
/i" r.ass Tyrr * Py minor :'nalc
, ; tz. ;;trs. 30 to .A
bleached section yollow
" ^ricitic
Chl. band I'yrr * chalco
11
FORM S22
NORTH ——. EAST. —-. ELEV. —— AZIM. -—— DIP ____-
DIAMOND DRILL REPORTPROPERTY __ i.IL. : /; orVIO'I - I'iOh
HOLE NO. COMMENCED. FINISHED--— PURPOSE OK- HOLE-
r.Vp.
FROM
Wfn1970
ilL^iiilii.
367
402,
TO
W
404.5
442
DESCRIPTION
rosaivo speckled AncJeaito fine (;r'do
c intict ?it 70 to RA
Dk. fra..'Roritfil Andesite nun niifnotio
iiO niu.
I'aoo. elk. t', f* Anclnnite opockled app.
t.j core n-jn ni'i 4 notic.
.FROM
264.5
269.5
?79.5
2;!4.5
2^7.5
2?t9
315
323
!,64
ccTO
269.5
274.5
279.5
2^4.5
2^7.5
2*59
293.5
urt
32fl
465
)RE SAMPl
RECOV.
5.0
5.0 '
5.0
5.0
3.0
1.5
4.5
1.0
5.0
1.0
.ES
WIDTH
5.0
5.0
5.0
5.0
3.0
1.5
4.5
3.0
5.0
1.0
ASSAY
i
f DESCRIPTION OF SAMPLE
r.liwrty chl. ection
1 inar pyrr. V.L. chaico
''inor pyrr. V,.,. c.v'dc^
rinor i*yrr. C. L. c::ilc3
Very little riner.il
band of Pyrr ririor ch-ilco
1" nearly mss Pyrr. * i y
r.iinor chaico
vftry little nin.
ciil. section
f T ir .uruunt o!' Fyrr ch'ilco
in cectijn Udert y
l,ao:.'l streaks of lyrr rinar
chalco.
fdss. ryrr * r^alco
/l.
NORTH.— EAST. —— E LEV. -—— AZIM. —— DIP ____
DIAMOND DRILL REPORT*'I'--'-OH U''TI )H - /isl-j-i
HOLE NO. COMMENCED.————..FINISHED---—^——. PURPOSE OF—————. HOLE___________
-
THUNDER BAY"" ni.'iirjo ,-Jivir.iOfi
iJflhCHf fc TTSEP 10 1970
WA PM
7j8!9|10|l!jl2| 1^3^5,6
i
FROM
U2
Ufl.5
t "-7.5
501. J
607
TO
.M. 5
4*7.5
501.5
6;;?
620.5
DESCRIPTION
6.5* Cherty Tuff
Dk. sp. ftndcnito
Fine f,r'd reta-Tuff-.".ed
bnr.ilinr -? 60O to C. A.
f-' ne, a highly Alt. Ant'i-site
r'in with pyrr ninor
chalet)
572' cherty bands tf 500 to C. A.
Bluish c bort: fractured
and brecciated minor min.
01';. 5 - 619.9 Breccia
"radation to amygdaloidal
,'iii. Andesite wall rein
highly nartifttic pyrr.
arid chalet) ffttn
FROM
497
502
517
522
5*7
532
537
572
575
577
579
587
592
597602
607
612
617
619
622
ccTO
502
507
522
527
532
537
5L2
575
577
579
582
592
597
602
607
612
617619
622
624
)RE SAMPL
RECOV.
5
5
5
5."
5.0
5.0
5.0
3.0
2.0
2.0
3.0
5.0
5.0
5.05.0
5.0
5.02.0
3.02.0
-ES
WIDTH
5
5
5. c
5. c
5. f
5. t
5. C
3.'
2.(
2.(
3.t
5.t
5.1
5.'
5.'
5. C
5. t2.(
3
2
ASSAY
0
0
DESCRIPTION OF SAMPLE
V.L. vin.
Highly Alt. dies r-yrr.
: ;ias. ! yrr. Mt. .lection
2 en qtz. strs. r yrr in
section
3 arc qtz. stra. n.n
sections
Hin. .net. cherty V.L. min
fair ar-.^unt of i yrr. in Ut.
.'flction ninor chnlc'J
2 1 chort bines
Disa. Vyrr. fin. chart b.mus
."in. with ! yrr * c.Tilco
i^iss. 1'yrr minor ciialco
iyrr. tain., vdth chalco
i;iss. I'yrr. minor ci.alco
r " qta. i;tr. win sect.
i'iss, iyrr in 'ect.
Thirty b^ncJa V.L. min.
.1 ii ' ,. ft
Very little nin.
V.ell nin action i yrr -tchslco
Tin. diss Tyrr some chalco
FORM S22
EAST. DIAMOND DRILL REPORT* ELEV. -^
AZIM. — DIP ——— PROPERTY-
,.;-j;i OPTI r; - ,\.;-.v. s
HOLE NO.COMMENCED-FINISHEDPURPOSE OF— HOLE_______
FROM
620.5
TO
Gl,2
DESCRIPTION
U-k f;roon silicified amygdaloidalotuiosito well ciin with
!'yrr. -m. clmlc;) pyrite
6jJ**6it2 micaceous section rum rricnotic
.-6^2 r!il) OP IDLE
x' '^'^ yna^fo^+jf^
HOlUNfiER-M!NES-i!MHfl ———————————Tiiiiiitip nuTADin.TIMMINS, DNIARIU
-
CORE SAMPLES
FROM
)2n
\?.7
•29>32
^4
TO
627
629632
632
RECOV.
'1.0
2.03.0
2.0
WIDTH
3.0
2.0
3.02.0
ASSAYDESCRIPTION OF SAMPLE
i pll f)i!! T VlflRt ?:-fCt-i^1
spjts pyrr * chslcov^ry n .. rv- tic
i-.all nin not so rmch chi.icoViri. vith pyrr * ch.-iicoVery li'.tl^ n-.in.
THUMDER'bAY" .
iEeeiifiHpSEP 10 1970
7|8|9|10;1!|12|I|2|3|4|5|S|
i
*^SiSK
^:i ̂
^^.feiiA
l^rf^fcf^asM
ate
s- WA ^
•,', f. t//''M'? v Q i t.'/,,,-. - *j i -- ' a- tt Y -' - i ' i -'
f/'-^l'' //6\'//;1U^ ' V-i—,-
7
r
9 P Z Z
MjUwWM
DDH f Al, A2, 1^3 ft. M -Wave previously
DDH # A5 coaaenqed Jan. 22/72 Finished " 24/7^
A6 Commencd Jan Pinishe
DDH ^ A7 Comcaenc Finis]
nee* Feb. 2/72 Ishedl " 3/72
- Bradley Bros. Ltd. Timmins, Ontario.
Dia. of Core :- 3/16*
-a--74
VS.-'
yz-t;
NORTH EAST. —— E LEV. —— AZIM.. DIP
00 -i- HOLE NO.i "j *n " '
IAMOND DRILL REPORTPURPOSE OF
loo*; PROPERTY-
TS- 2. Z tt'7 !. t."facle'v~!Trj'3.
FROM
0
20
30.5
49.7
TO
20
30.5
49.7
71.6
DESCRIPTION
(!ua ing
nilicifted andesite fra/oaentul . The
fragments are very snull-lesn than J"
and cenorally obscure the franmonts are
siliceous. The andesite is dork preen
to. grey,.. siliceous, chloritic cut by quart
carbonate stringers* No ninornlisfition.
Amygdaloidal andesite - amygdalos are
locally well defined - rounded to elliptic
in shape and either siliceous or filled
with chalcopyrite and pyrrhotite.
There are also strin^ero of pyrrhotite
and chalcopyrite in this section.
The andesite is weoniah to ere y withchlorite and silica and cut by
quarta-CO.j stringers.
Aniieaite i'rafTaontal-probably a tuff
ainco the f rapnonts are very snail i"
in size. It is separated fron the
ipiypdaloidal andenite wainly on the
basis that the framents ere very
anr.ular and siliceous in nature* Also
them does not appear to be any roplnccner
or fillinr of the frafjient structure by
pyrrhotite and
chalcopyrite. Instead the mineral
CORE SAMPLES
FROM
i
al
45
i. j
70
TO
50
72
RECOV. WIDTH
5
2
ASSAYDESCRIPTION OF SAMPLE
-
Anyfdaloidal andesite Cp t Po
for Cu, Hi, Au,Ag
l,^K^.^y-,M^^L[/^^'
\,H r'?r:i4'MQ ^iUlOjSiJ;:,/!.!-;, i., ."^-Jii-JiL?l''J'*i5j5/
A
Lower part of fragmental Vv.
Po-Cp section
FORM E22 NORTH——. EAST, -—— ELEV. —— A2IM. —— DIP ____
DIAMOND DRILL REPORT
PROPERTY- lv TO'.:HSHIP
HOLE NO. COMMENCED. FINISHED——. PURPOSE OF- HOLE————.
FROM
71.6
79.4
90.7
TO
79.4
90.7
L05.4
DESCRIPTION
j ci sinply oissoninated and localized
o stringers. From 49. 7 to 55
.radational contact uith the frumontal.
71-71.5 near maoaive (section of
jyrrhotite and chalcopyrito-noatly
pyrrhotite.
'ono of nixed chort und amygdaloidal
"aterial. The amygdaloidal sections
aliow abundant po and aono cp completely
filling; tho amygdales.
such are: 75-76.3 77.3-79.2
Tho chort is vory d-irk and hard
j.t is brownish in colour, no mineral or
very ninor py along shears. Of ton
fractured and filled with chlorite.
Andesite fra^nontsl - tho fra^raonto
iro Ip.rncr hore |" size and only
Locally were defined. Thoy nay be either
:hftrty or chloritic. The andenito is
rreen in colour, fine frained with
ibund'int chlorite - cut by snail quartzcarbonate stringers.
Another aone of brownish chort-
fractured with chlorite, epidote and
quart z -c arb onate .
FROM
75
ccTO
77
1
IRE SAMPl
RECOV.
-ES
WIDTH
'
2
ASSAYDESCRIPTION OF SAMPLE
Some chert and amyfdaloidal
rnterial Cp To in anygdalticlal
.
j'^J.-v'^i-S^Tfj i/ij' ' f^ if, li W [c ii j)( "f r t si- / '•i/ci1 A\l ' '-J l - I"'U
^ii^^i^ipffj—————————— t ——————————
FORM SC2 NORTH —— EAST. —— ELEV. —— AZIM. . DIP ————.
DIAMOND DRILL REPORTPROPERTY- ASHMORE
HOLE NO.COMMENCED,FINISHED-—.PURPOSE OF- HOI F
A-2-70 3.
FROM
105. t
U9.t
23S./,
TO
UQ.i,
233.1
r
248.7
DESCRIPTION
Ant! e site fra&tvmtal - fra/jRanta are
around ^" size and vory numerous.
'i'hcro are chorty, chloritic, epidote and
sillc80U3 typos* Vho clvirty snf* sillcooustypes of frafmanto may bo separated
uinco tho corty typos ixro i^ttyioli ^^ fcrownand nearly clear while the siliceousfrnrrionto are a bleached white colour
and noticeably different. Thore are
numerous small chert bands cutting thecore as v/ell (i rt acrosa) 113-125 asilicified zone where t hore are not asnany fra/unents aa surrounding. Theandesite is Kreenioh (dark) in colour.:!o nin.
Zone of weakly anyjTdaloidal andesito119.4 152.3 eradutional contact with
above. Generally the andesite looks
ascive to a medium grained variety with
occasional anyfidaloa filled with po and
py. i'he andesite is {'roon, contains chloi
cut by qunrtz-COj otrinKcra.197.6 - 200 - anall chnrt breccia
Zone of chert as before - brownish incolour.
FROM
'
LtA, ——
GC
TO
)RE SAMP1
RECOV.
-ES
WIDTH ASSAY DESCRIPTION OF SAMPLE
1 i ' -' r T:;-;-' 'pXv"
iW^^v'i^L n;:r H HO ".
•httfii-W^wij^firfli
FORM S22
NORTH— EAST. —— ELEV. —— AZIM. ——— DIP ————
DIAMOND DRILL REPORT
PROPERTY- ASiiMOltE TOWilSHIP
HOLE NO. COMMENCED- FINISHED- PURPOSE; OF—HOLE————-
A-2-70
FROM
?;rt 7
2i'0
2fl2.
300.4
30^.1
TO
?ftn
2*2.9
9 300.4
304.1
323.3
DESCRIPTION
y.ono o.'" coarae {'.rained andesitehornoblendo -carbonute-chlorito Schist.
Schistosity at 55 to Core Axis
^roen in colour, cut by quartz carbonate
chlorite stringers.I'one of brownish chort a&ain.
Andefjito fr-ncnontal-fragmnts aro
J" in s J ae and often obscure, occurring
'j s siliceous or chloritic p^tehnsrinned by chalcopyrite nnd pyrrhotite*Chero io uune Cp and To dissjeninntcd
throughout and some ciineraliaation in
the quartz-carbonate etrin^ora. There isabundant chlorite und oome epidote.
('one of chert - crean coloured and locally
;)rocciated-gradea into lowor eone- no
lino ra li nation.
Anyfdaloidal anriesite-very
ainilar to tho pievioua horiaon witht
C p and Po in tho anygdalna and ala o in
lenses and disseminated throughout.
/Vr.yrdales locally woll defined-anall 1/fJ"
sise aone pyrite may be found in strinfiors:ir. well.
AT/, /C5 attMHtLusHOlll^OER KiJiS LIMITED
FROM
2^5
315
ccTO
2<X)
320.
)RE SAMP1
RECOV.
-ES
WIDTH
5
5
ASSAY DESCRIPTION OF SAMPLE
Andesite fr-ipaental cp, Po
Anygdaloidil andes, Cp, Po
!
L Jp^'-vK^'lIfiJ''.- 1.!.'' 1 '™ .-.J
————— i ——— ,,^.,.,,, , ,,.... .,..r/MM/NS, ONTARIO
N\
-v.
LEGEND
ALGOMAN
Ng — Feldspar (Albite ) Porphyry
Ki r- Gabbro ( Hornblende)
KEEWATIN
A2 SP Andesite
bx -breccia
Shearing
Topographic Feature
TR. - Trench
JTS. - Joints
; \ Esker
, JTS
HAS ELI AZi DIP
xl 2K LHAIVIUNUv ?yrfac*M ..80"
CO Tar © 4" PBOPFBTV VJTTi3)*300 — L.5 o "Aij
FROM
0
60
-
TO
60
342.:
.DESCRIPTION
Casing
Andesite - dark green - fairly haichloritic and siliceous - locally carlsections which are slightly more browr
in colour. Locally there are small
quartz-carbonate stringers. @ 62 and@ 67.5 there are a few chlorite blebs
in the core, which is somewhat leachecin these two sections. Mineralization
at the first is practically negligibl*only rare splashes of py.
186.1-204 Much more siliceous bamIt is not a chert band though - fairly
hard, black. Sulphides are very minorbut there is some cp.
190-200 apparently there is some
lost core - it is broken up here butno evidence of a fault is indicated.
At 204 the rock is less siliceousand mor* andesitic in appearance. Aft 1
a short zone of carbonatization, the
mineral consent increases, around208.2. The reck here is identical to
the rock @ 2 50 in DDH A-4-72, except
that the mineralization here is mainl
disseminated, flhal ropyrit* pnnt-.*nt. i n
UK ILL MtKUKI FINISPUR! HOU
SON — OPTION #1 ———— ——Ashmore Twp.
•M™ TanuarJ ZG/^STftsr. F-yr.ftnsion of
rnnn^r 7.on(* and ma?.
Drilled by: Bradley BrothersCORE SAMPLES
FROM
donatizish
-
r
208210
TO
ed
210213
RECOV. WIDTH
2
3
ASSAYDESCRIPTION OF SAMPLE
A2C03 - 10^ sulph. Tr.cp" - 7fi sulph. Tr.cp
FORM B22 NORTH —- EAST. -— ELEV. —— AZIM, -—— DIP ____
DIAMOND DRILL REPORTPBQPFPTV WILSON OPTION #1 ———————————
Ashmore TWP.
HOLE NO. A-3-72COMMENCED——-——-———— FINISHED——————.-——————PURPOSE OF- HOLE______
FROM TO DESCRIPTION
very minor - The main mineral is
pyrrohotite and some pyrite. Totalmineral - 7-10# Even with 5-7# po
the rock is only slightly magnetic.
This above rock gradually gradesback to a carbonatized andesite. fh~e
pyrrohotite also becomes more magnet^
around 230. The mineralization graduitends to change to a more throughgoirstringer type of mineralization, Thei
is also a gradual increase in copper
content, although pyrrohotite andpyrite are the major minerals present
Where there is a larger amount ofsulphides, the pyrrohotite is genera!
much more strongly magnetic.The rock changes gradually from
silicified to carbonatized zones
throughout this entire section.Around 283 the mineralization
is in the form of both stringers anddisseminations, and increases to
approximately 7# sulphides overall.
The sulphide content remains highuntil around 321, where the mineral
content decreases rapidly. As previo
CORE SAMPLES
FROM
215
220
225
234240
c 249
ryS 255e
4
ly285290
295300
305
310
315
*,
TO
220
225
230
235
245
250
260
290
295
300
305
310
315
320
,
RECOV. WIDTH
555
.151
5
55555
5
5
ASSAYDESCRIPTION OF SAMPLE
Cu,Zn,AgA2C03 - 7J6 Sulph. minor c p
n .556" it cp
" - 5# " " cp" - 756 " " cpn . 5*j H n Cp
" - 5jJ " some cp
n - minor Sulph. vis cp
.
" -105S Sulph 1^ cpn - 3jJ Sulph. smell cp
" - 5j5 " minor cpn . 5^ " " cp
11 - minor Sulph. no
visible cp" - 7-10J& po py very
minor cp" - 7-lOjJ po py neg. c p
FORM 122 NORTH EAST. — ELEV. —— AZIM. —— DIP ____
DIAMOND DRILL REPORT
PROPERTY- WIESON OPTJ.QN j lAshmore Twn-
HOLE NO. A-3-72 ...3COMMENCED-—————————————————FINISHED——————————.————————.PURPOSE OF————..^-——.———.—.——— HCil F -——-—-.———.-...-—....————
FROM
3.42.2
TO
443
DESCRIPTION
most of the mineralization is pyrite
and pyrrohotite, with only local splaof chalcopyrite. This zone is the mos
strongly magnetic. There is also some
biotization developed.Around 321, the rock grades to a
dark green, unmineraliaed andesite -it is chloritized and carbonatized.
Diorite - grey in colour, with
numerous feldspar phenocrysts (ormetacrysts) developed - often feldspa
shows minor epidote alteration. Silic
Weakly magnetic in the presence of sp
- being po and py After 360^ theredoes not appear to be any pyrrohotite- only very minor pyrite. Here the.
rock gradually becomes more massive awell.
387-394 strongly carbonatized zor
only vestiges of feldspar crystalsremain.
394-405 massive as 360-3^7
@ 405 the diorite becomes more hi
altered with a much higher epidote coSome of the feldspar crystals are sta
reddish by iron, while others ara
CORE SAMPLES
FROM
she s•'
n
Lfied
irse s
j
! -
'
Shly
itent.Lned
TO
alphid
RECOV.
es
WIDTH ASSAYDESCRIPTION OF SAMPLE
FORM SSl
NORTH EAST. —— ELEV. ——- AZIM. -—DIP ____
DIAMOND DRILL REPORT
PROPERTY WILSON OPTION
HOLE NO. COMMENCED. FINISHED—-- PURPOSE OF- HOLE-—————
A-3-72 * . .4
Tvm.
FROM TO
443
DESCRIPTION
completely altered to epidote. The
rock now is a limey grey-green asopposed to the original grey colourof the earlier intersection. As befo:
some sparse pyrite.
End of Hole
HGIHTa ft&S LiDEi)JIMKINS ONTARIO
-
*
CORE SAMPLES
FROM
e
TO RECOV. WIDTH ASSAY DESCRIPTION OF SAMPLE
FORM M2 NORTH EAST. —— ELEV. —— A2IM. —— DIP ————
DIAMOND DRILL REPORT
WILSON OPTION #11———— Ashmore
HOLE NO. A-3-72 ...5COMMENCED-——.^—...—-—™—.————. FINISHED^-—————.^.-————.-——.— PURPOSE OF__________________.——— HOLE___________________________
FROM TO
62
100
150200
250
300350
393438
DESCRIPTION
SAMPLES FOR THIN SECTION
Andesite - a few chlorite blebs in a
zone which is cut by a short quartz-carbonate stringer with wall rock lea
Andesite - dark, chloritic, siliceoue
Silicified and carbonatized andesitezone of dark silicified andesite
Carbonatized andesite with po and py
Carbonatized andesite, po, magneticGrey silicified diorite
Carbonatized dioriteAltered diorite - some epidote
* .
CORE SAMPLES
FROM
:hing
TO RECOV. WIDTH ASSAY DESCRIPTION OP SAMPLE
O/yts. P.Ct/t^tf/itk^pii?!RFR r;:;^ OED
NllUKIHS, ONTARIO
f--T3 t3 fD
FORM O2
AZIM. .
. '.r
1 0,-.-i /T
— 5-rr-t-rc-f: di la r
r ~ /, i *
3'i?'f -ice." IrV"
Lt-L-Li, 0
DIAMOND DRILL REPORT
PROPERTY- /JOlJ GFTIiJ!- ..''l
HOLE NO. COMMENCED- FINISHED___ PURPOSE OF- HOLE————
_____ , A s h" o r r: Tovnphi
FROM
r,l'l
TO
-V337
DESCRIPTION
C n ^ i n c*The rock is best described as or
andrsitic flow, although there are a
vide variety of charges in the rockitself. For thn r.ost pr.rt the ar.d^sitf
io dark groen end fairley "*ssivf;. It
is chloritic tind ^enorally highly
C 9rborinti aecl. Thor-'; a re a few s." -fell
qxiartz-carbonnte Gtrin^ors v.'hich
locally show loachin^ and silicifcr-t
into tho surrotu.dinr rock. Locallythe andesite ^rc'.dcs into n member
vhich is corrpo.sr.d of nunr-ronr. blebs
of chlorite. Ac theso bleb? brcon'O
larger thoy appear to bc altered fr.^
Th?ro is n S':."'ll a: ount of epidot.f;
"iRsocifted with thir unit P. s veil.
This rrprrbf-r ir- pro^ir^nt fror^ ICO-l?
"."isll ci..- t of pyrite : 137
A zone of strong c.-rbonitiaetion sta
'•:' 14^, rock is d i rk 2r0(?n in colourand prfdop to a much li^htrr 2rr""in
'vith increased, car'ionate ccntfnt.Around 15? start to 2 Qt a ruinor airou
of dir-sernirct^l riyr.it o witli about 3;'- disseriinated pyrite -: Ifi/,-]/)?. Here
CORE SAMPLES
FROM
i. on
y - ftiits
-t p
\t
TO RECOV, WIDTH ASSAYDESCRIPTION OF SAMPLE
'
FORM (22 NORTH EAST. —- ELEV. —— AZIM. —— DIP ————
DIAMOND DRILL REPORTHOLE NO. * COMMENCED—— FINlSHFO PURPOSE OF— HOLE—————.
PROPERTY-Ashi or'H T.-: r -,
FROM TO DESCRIPTION
there are occasional splash??, of cp
with the py, hut or.ly a ve rv minor an164-173 Short chert band - con
are diffuse pince th^ andesite is silat the contacts. F.inor py in first
chert bc,nd(or flow top) at the contacotherwise barren. Colour is nark grey
black.After the chert band the andesi
again highly carbonatized; the firstoccurrence, of po is noted h(-;re - only
weakly ra^netic though.
Around 200 the alteration is qu
strong and lc.t"r around ? 25 thn rockcrudely ba-'d^d in layers of alterati
at 6C 0 to the core axis.- nairlybrownish carbonate a::d chlorite.
After 175 there is j'-rerplly ssulphide tninfirali nation throughout.
ov fi r,?ll py-3/^ - in Isr^e clots,
in stringer fillir^s, disseminations
and alon^; s hoar planes,po - ninor - usually associated
with small clots or blobs of py.
cp-ninor may bo disseminated in srnal
splasher, - m rely alonr ;-ir, a 1 z.r?cr
CORE SAMPLES
FROM
Mint.•-acts
cifie
' ito
.e is
164
.tee
)n
llliS
TO
16?
'
RECOV. WIDTH
.
3 '
ASSAYDESCRIPTION OF SAMPLE
3^ dipi-CBiin.-trd r-, :-.ir.rcp in cc-r'horati W'-T! A?
NORTH EAST. — ELEV. —— AIIM. ——DIP ———
DIAMOND DRILL REPORTOPTIC,;; '
HOLE NO. COMMENCED FINISHED-— PURPOSE OF HOLE——
FROM TO DESCRIPTION
bleb, since usually found with py
either vith or without po.213. 5-214. 5 ~ sreill white chert '
Around 230 the cp content begins to
increase - still in the. cfrbonati^odandesite .
cp is the ne in mineral here - upto approximately 254.
- 239-23/4. isolated stringers andblobs of cp. I ~2fo o verall
- 234-~49 very rinor cp
- 249-25C chert, white250-254 numerous small stringers
of cp w/w'out po approximately 5;a cp
254-265 brownish, carbonatised,andesite - blobs calcite, numerous
blebs cp, po, some py locally along
shoars especially pfter ?57*5
some biotite? small xls. tfiay be Zn.
265-271 mainly stringers of cpa^sin, FOP. e po - rock grades back to
more ^rey green cftrbonatized andesite
2?l-274 srey green carbonati?,edandesite. Only one small stringer of
275-276 sorne brownish carbonate' 4^ cp
CORE SAMPLES
FROM
2200and
230
250
252254
258
25926C
265
270
275
cp.
TO
235252
. 25425?
259
260265
27C
275
276
RECOV. WIDTH
52
24
1
15551
ASSAYDESCRIPTION OF SAMPLE
s:r:?ll c]ot of vty ir.calcite - Groche*1". f. au
Cu,"n,AsA2-C03 -2;'- cp
" -5?5 cp 3^ TO
" -2-3JJ cp 2,1 po" -minor cp, po, py
" -4; J cp, 4;^ T O py" -].5/' cp rilnor po pyI! -2-3;1 c p 4;' py po" -l-2;4 cp 5;: po py
" -;::' nor c p
" -4!?. CP
rORM Ut NORTH—™ EAST. —- ELEV. —— AZIM. ——. DIP ————
DIAMOND DRILL REPORT
PROPERTY- OPTION
HOLE NO. A-4-72 COMMENCED—————————.FINISHED——————————PURPOSE OF————————HOLE——^—-—————-———
...A
FROM TO
1
DESCRIPTION
276-291 mostly grey green carbonatize
andesite, local blotches of cp with pysome brown carbonate with cp @ 278.5-
280 and 290-291.5
291-294 3 short bands of chert, breccwith minor py po
294-302 some stringers of py, a few s
of cp, very minor po302-303 small chert band
303-314 strongly silicified zone,brecciated with substantial blobs of
dark grey - local patches of chloritevery massive
314-320.5 more of a transition zone t
an actual change in rock type. Locall
silicified and local patches ofcarbonate alteration, minor cp locall
320.5-337 a short unit .of tuff -
would appear to be more of a dacite tandesite. - paler green - fragments
are generally small and leached whiti
Mineralization - negligible - onlyoccasional py. Both contacts are
gradational into 5 feet of heavilycarbonatized rock.
CORE SAMPLES
FROM
afc PO
Lated
iringe
2?6280285
:p 29C295
300
lan 303,305307
r 316
lan an
ih in
TO
'S
280285
290
295300
303
305307310318
:olour
RECOV. WIDTH
4
55
55
322
32
ASSAYDESCRIPTION OF SAMPLE
A2-C03 - IJf cp # 3# py po" -1 small blob cp" - very minor cp
11 - minor cp" - minor cp
" - minor cp
w - 456 cp blobs" - minor cp" - 1J& cp very minor" - minor cp po
FORM S22
NORTH ———
EAST. —— EUEV. —— AZIM. —— DIP —~—
DIAMOND DRILL REPORT
OptionAshmore Twp.
HOLE NO. A-4-72 COMMENCED-—————— FINISHED___________ PURPOSE OF—^————— HOLE—————.——————
...5
FROM
337
357.7
456
TO
357.7
458
494
494
DESCRIPTION
Diorite? - this zone is siliceous, gr
in colour, with a general developemerof feldspar phenocrysts throughout.
fairly massive unit, unmineralized -
some epidote near contacts. Sugarytexture - strongly carbonatized.
Andesite - darker green and more chic
contacts, while the central portion itlighter in colour and more siliceous.
There are a few splashes of cp in thefirst 20 feet but afterwards the
mineralization is negligible. Some smj
quartz carbonate stringers with local
iron stainings. Minor epidote.
Diorite - Pale grey to dark grey i)
colour. Darker than previous intersecNumerous small blotches of epidote
alteration, rock is silicified and ea:Feldspar phenocrysts (or metacrysts) ,,
common as before. No mineralization
non-magnetic.End of hole.
CASING LEFT IN HOLE.
miumm m^ LI?MED
CORE SAMPLES
FROM
3y'f
ritic
11
ion.
bonatire
TO
at the
zed.
*
RECOV. WIDTH
*
'
ASSAYDESCRIPTION OF SAMPLE
TJMMIHS, UNTARIU
FOHM (22 NORTH EAST. —- ELEV. -—— AZIM. ___ DIP ————
DIAMOND DRILL REPORTWILSON OPTION #1
Ashmore Twn.
HOLE NO. COMMENCED FINISHED—— PURPOSE OF HOLE.-——
* * * ^J
FROM TO
117.;150
200249.
300
350
400
450479
DESCRIPTION
SAMPLES FOR THIN SECTION
Andesite (tuff?) with chloritic frag)Carbonatized andesite with minor
disseminated pyCarbonatized andesite minor py, cp
i Just previous to the copper zone ~Carbonatized andesitePale grey green Carbonatized andesiti
(dacite?) py fc cpCarbonatized diorite
Silicified andesite
Altered andesiteCarbonatized diorite with epidote
Check collar @ 42 0 Azimuth @ 1800
CORE SAMPLES
FROM
ents
TO RECOV. WIDTH
*
ASSAYDESCRIPTION OF SAMPLE
DtHU- K. UC6'sYtfsvtt4f "
I'.-X J"|-:-p II'*'fN ["'JTCJl- hUl.Ui- u .ii L;rt:i Lii.uitJ
OHTARiO
A^i-7241 6*1-005
00
OV b 53'
,
scale i*-ioo'
FORM S22
NORTHEAST
I-H____ ______1S-•. —— xI-J DIAMOND DRILL REPORTHOLE NO. A-5-72 COMMENCED
AZI DIP
M IgC' 0
— Collar @ 4-5-? — ©JOO-^-5— PROPERTY __ WU,uiaira Ttf **ye
FROM
0
76
TO
76235.6
DESCRIPTION
CasingAndesite - massive with tuffaceous
sections. The andesite is generally da
green in colour but is often lighter ituffaceous sections.
The first part is unmineralized,non-magnetic , and chloritic
The tuffs have a very fine fragmesize - usually less than 1/1)6". In sonsections there is a predominance of
chlorite blebs throughout the rock :Tuff : 95-97, 103-106, 108-112. Q 117.and 122-122.5.
@ 112 a crude chicken track structureis developed with numerous blebs ofchlorite and some lath-like crystals
which appear to be altered to chloriteThere are also some quartz-carbon
stringers with hematite staining in thzone.
Some contacts between different
units are readily visible and areconsistently @ 60" to the core axis.Some other contacts are either irregulor gradational.
OAV nomTrtxt Jl*oUft UriiUfi ffi17* Aflhmora— SWD On.
HOLI
t. r-
CORE SAMPLES
FROM
•k
1
It
1
J
it e.6
ir
TO RECOV. WIDTH
t
ASSAY
: —— Te 8 t~*xt* rtsi en-of ——— copper-zone ————————H*illftri W i Rririlf-x- Rrjvn
DESCRIPTION OF SAMPLE
FORM B2e
NORTH EAST. ELEV. AZIM. - DIP -
DIAMOND DRILL REPORT
PROPERTY WILSON—&PHON
HOLE NO. COMMENCED. FINISHED—— PURPOSE OF- HOLE——————
A-5-72 ...2
FROM
'
TO DESCRIPTION
around 162, as pyrite in a short sill(
band 160.9-162
Small amount of tuff ? G 165 withchlorite blebs.
169.8-171.5 , Short zone of chert
bands (or flow tops). Same as materia]in holes A-l &A-2. A short stringer oipyrite @170.9. The rock is grey in coland leached whitish.
171. 5-177. L - Grey green andesitewith minor disseminated pyrite.
177.4-181 very dark chloritic andes- tiny white flecks of leucoxene - ma)be a diorite since there are vestigesof feldspar.
The rock now becomes strongly
carbonatized - brownish carbonate wit Jsome minor pyrite.
200.6-205 small chert bands also fe214.1-215.4, 217-218.8
Around these chert bands, the andesJappears to be tuffaceous, only occasi(
fragments though.
@ 2 21.5 start of a zone of carbonat
- brownish colour. Extends to 233 wher
it jrrfidofi into a V^T*V siiicflovifl DOHA
CORE SAMPLES
FROM
eous
our
ite
tenal
Lzatio
S
TO
n
RECOV. j WIDTH ASSAYDESCRIPTION OF SAMPLE
'
rOSM (22 NORTH EAST. —— ELEV. —— AZIM. —— DIP ————
DIAMOND DRILL REPORTPROPERTY———WfilS&N
HOLE NO. ^. COMMENCED FINISHED— PURPOSE OF HOLE——————
-.3
FROM
235.6
254.9
264.2
26?270.1
TO
254.9
264.;
26?
270.1279.5
DESCRIPTION
up to 235.6. First minor cp in thiszone - 2 small splashes - one @ 221.5and one @ 230. Minor py
Short dyke of hornblende gabbro -very dark green with numerous smallblocky crystals of hornblende 1/16 "size, carbonatized
Contacts with the andesite are ir;upper @ 90" to C, A. lower 3 45 0 t.n C.
@ 240.2 a large bibob of cp alonga quartz-carbonate stringer. No miner;
^ ft f*or^ t/h&tj- but afterwards there sorntcp and py all through the dyke. It isusually associated with small quartz-carbonate stringers but this is notalways the case.
' Silicified and carbonatized ancle;- very minor py po
Diorite (or albite porphyry) - gn
with numerous feldspar phenocrysts
(or metacrysts) . There is some epidoti
alteration - mrit.artjR irregular. Minoidisseminated pyrite throughout.
Andesite, Krey-green, unmineraliz*Diorite (or albite porphyry), as
previous SPCfclnn py^y folHfirtny* AP|t(
CORE SAMPLES
FROM
egulaiA,
1240
241
245250
ite
302
y
d.
OfjA
TO
241
245250255
303
RECOV. WIDTH
.
'
1
45
5
1
ASSAY
;'
DESCRIPTION OF SAMPLE
Cu, Zn, Ag
Kl - 23, Cu?
" - neg. sulphides
" - I fi sulph, 1-5^ cp11 - minor sulph. vis. cp
A2 - ty aulph. 2* ftp
FORM SZ2 NORTH__ EAST. ___ ELEV. —— AZIM. ——. DIP ————
DIAMOND DRILL REPORTHOLE NO. COMMENCED. FINISHED——— PURPOSE OF- HOLE______
A-5-7?
PROPERTY
FROM
279.5
306.5
326
330.9
336.8
TO
306.5
326
330.9
336.8
437
DESCRIPTION
and disseminated pyrite.
Andesite - grey-green, locallycarbonatized or silicified, minor ser
in streaks. Mineralization is minor,disseminated pyrite, very minor cp.
There are two blots of cp between 302with some po,- just cutting the core.
Diorite (or albite porphyry),contact 3 SO0 to the core axis. Spars'
mineralized with py cp -only one tin;
splash of cp seen, carbonatized.The rock is similar to before ex
that from 317-322 it becomes more mas
and finer grained.
Carbonatized andesite - unminera:
Diorite (or albite porphyry), ve:dark here, with feldspar as before, t!is a lot of epidote alteration in thijOnly one small splash of cp seen @ 33;
Andesite - grey-green to the var:that is carbonatized and brownish, Verj
sparsely mineralized - cp is very mintMineralization is usually with quartz*
carbonate stringers. Around 402 the
andesite becomes darker in colour and
weakly amygdaloidal in pla^As, ^^w*
CORE SAMPLES
FROM
cite
3.03
ly
e pt
ive
ized
yerezone.
ety
r.
is
TO RECOV. WIDTH
*
ASSAYDESCRIPTION OF SAMPLE
.
FOKM XI NORTH EAST. —— ELEV. —— AZIM. ——— DIP ————
DIAMOND DRILL REPORT
WILSON -OPTION
HOLE NO. A -5-72 ...JCOMMENCED———^——.^———-..^.-^.^ FINISHED————-.———————————PURPOSE OF——^————————-———.^ HOLE_________________,_______
FROM
437
TO
448
448
DESCRIPTION
iron staining in the quartz-carbonatestringers. Minor epidote and/or seric
Diorite (or albite porphyry), asbefore - a bit coarser grained, minordisseminated pyrite, epidote alteraticarbonatized.
End Of Hole
CORE SAMPLES
FROM
Lte.
m,
TO RECOV. WIDTH
*
ASSAYDESCRIPTION OF SAMPLE
FORM *22 NORTH— EAST. —- ELEV. —— AZIM. ——— DIP ————
DIAMOND DRILL REPORTHOLE NO. A-5-72COMMENCED——————————FINISHED————-———————. PURPOSE OF—-—-—-———. HOLE————.————————
.. .6
FROM TO
76112
150200
250300350
400440
DESCRIPTION
SAKPLES FOR THIN SECTION
Grey green andesite - chloriticChicken track structure in tuff 7 -
chloriticGrey green andesiteCarbonatized andesite
Hornblende gabbroAndesite - grey greenAndesite - dark green - weakly carbona
Andesite - few quartz-carbonate stringDiorite (or albite porphyry) - pyrite
CORE SAMPLES
FROM
tized
srs
TO
1
RECOV. WIDTH
,
ASSAYDESCRIPTION OF SAMPLE
HOLLINGER KiKS IWITED4 IKHiS, ONTARIODdU. /f. QjtMO*ebA
A .
A/
scole '"-100
NORTH EAST. . ELEV. . AZIM. —--
S7-5-N-
DIP —^heok—
-xi-l-2-E———- Surface————-OSO*———-——
DIAMOND DRILL REPORT
jSON OPTION
HOLE NO. A-6-72COMMENCED
PURPOSE OF-HOLE—check— E,V-a no ir,aly-
a ,w-.**. . Claim TB 229616 Ashmore Twp. Ont. Rr
FROM
0
4
37.4
TO
437.4
40.8
DESCRIPTION
Casing(AX)
Hornblende Gabbro - medium to dark
green in colour with numerous blockycrystals of hornblende. The rock ie
quite highly altered with carbonate a
talc, local specks of leucoxene.Some shearing with talc and chlori
13.5 - 14 @ 45 0 to Core axis and @ 18.
20 also® 45 0 to core axis There aresome very fine hairline stringers of
quartz-carbonate which usually carry asmell of po and cp.
23.5-23.9 blob of chert very irreg
in shajpeThe lower contact of the hornblend
gabbro is finer grained @ 45* to theCore Axis along a quartz-carbonatestringer with po, cp
Chert - grey to whitish in colourrather milky. The first inch is filled
with numerous laths of amphibole - verblack. The remainder of the zone is
weakly banded in darker and lighter
patches, massive. There are some blobs
of po with some cp. The po is quitestrongly magnetic, locally, very fine
CORE SAMPLES
FROM
id
e -
.
ilar
r
37
TO
41
'
RECOV. WIDTH
.
4
ASSAY
JLX&d by * Brsdl^v Bros
DESCRIPTION OF SAMPLE
Chert - 5# po minor cp
NORTH EAST. — ELEV. — AZIM. — DIP ———
DIAMOND DRILL REPORTPROPERTY—WJiSQiJ—OPTION
Ashmore Twp.
HOLE NO. ^..fc..72COMMENCED—————,—— FINISHED^-———^—^-— PURPOSE OF————————HOLE——————————-—.
...2
FROM
40.8
46.3
4 7.9
TO
46.3
47.9
63.2
DESCRIPTION
disseminated mineral.Zone of carbonatized andesite -?-
Kost of the rock is carbonate and therare local patches of dark grey chert -gradational - and irregular in shape.
It is also gradational from the moremassive cherty material. There is a lo
of blue-grey chert as interstitial witthe carbonate. Mineralization is mostl
po - very minor cp. (5# po)Short zone of cherty material, ban
blue-grey and darker grey @ 45 C to theCore Axis. Numerous quart z- carbonatestringers. The upper contact is more oless gradational - lower @ 45 C to the iSome shearing and some biotite along
single planes of shearing @ 45" Thereare some small stringers of po usually
with quartz-carbonate often minor cp.@ 47.8 small bit od cp with a po
bearing stringer.
Andesite - and carbonatized andes:The first 2 feet is massive andesite w:numerous quartz-carbonate stringers © ito the Core Axis, bearing some po and
Mineralization is erratic though.
CORE SAMPLES
FROM
41
47
ed
ore A:
teth5"y.
TO
4649
is
RECOV, WIDTH
52
ASSAY
,j"
DESCRIPTION OF SAMPLE
A2? - minor po,py,cp
" - 5# po cp
FORM ta
NORTHEAST. -EUEV. _ AZIM. - DIP -
DIAMOND DRILL REPORT
PROPERTY —— WILSON OPTION #1 ——— —Ashmore Twp.
HOLE NO, . A-6-72 COMMENCED———.^———. FINISHED—-^-™.——-—-. PURPOSE OF———.—^-.^—. HOLE________________
...3
FROM
63.2
76.4
84.8
TO
76.4
84.8
128.4
'
DESCRIPTION
After that the andesite is generallymassive with carbonatized sections.Very minor disseminated py,cp onlylocally. Lower contact slightly irreg
d 60" to the Core Axis.
Albite porphyry (logged in previholes as diorite), There are numerousfeldspar phenocrysts or metacrysts,some epidote alteration, and some biotMineralization is minor with some very
finely disseminated po,py4 The lowercontact of the dyke is nearly normal t
the Core Axis.Andesite - brownish, carbonatiz
with very minor mineral (some py visib!Contact with dyke @ 84.fi is at 450
Albite porphyry with numerousfeldspars as before, locally finer
grained. There is some biotite developthroughout. Epidote alteration is comnxThere is approximately 3# pyrite dissei
throughout. A quartz-carbonate stringe@ 103.5 has the only po cp seen in thizone - only a minor amount -
The pyrite commonly shows a cubic habilLower contact @ A.5 0 .
CORE SAMPLES
K ROM
lar
us
te.
d ,
e)
dn.inatec
*
TO RECOV. WIDTH ASSAYDESCRIPTION OF SAMPLE
FOAM .22
NORTH EAST. —— ELEV. —— AZIM. __ DIP ————
DIAMOND DRILL REPORT
WILSON OPTION #1———— Ashmore Twp.
HOLE NO. COMMENCED- FINISHED-.— PURPOSE OF- HOLE——————
A-6-72 ...
FROM
128.4
187.2
195.6
TO
187.2
195.6
492
DESCRIPTION
Andesite - the first few feet are
massive and chloritic but it grades ina darker carbonatized lava. Mineralizeis very minor - usually pyrite but a fspecks of cp are seen (rare). Around 1
you start to get some epidote alteratiin the andesite, some talc ? in thesections that are strongly chloritic.
Around 183 the andesite becomesbrecciated with infillings of calciteand numerous bands of alteration. Theebands show no consistent strike. Q 185the andesite becomes quite siliceous
and hard with a few of the brecciafractures filled with py,po,and cp. Itappears to grade into a chert horizon
A short blue-grey chert band,
locally layering @ 80 to 85 0 to theCore Axis. The chert is brecciated asthe surrounding andesite with mainlypo filling stringers - very minor cp.
The EM-17 conductor plots here. Thepo is magnetic but not strongly so.
Andesite - banded @ 90" to the
Core Axis in alteration layers of
FROM
0
ionw0
n
round
185
190
ccTO
187.2
190
195
)RE SAMPL
RECOV.
.ES
WIDTH
55
ASSAY DESCRIPTION OF SAMPLE
5# po minor cp5/6 po minor cp
'
FORM S22 NORTH EAST. .,— ELCV. - AZIM. — DIP ————
DIAMOND DRILL REPORT
PROPERTY—WILSON—OPWON—#4-
HOLE NO. A.Q.. 72 COMMENCED-————... FINISHED———————— PURPOSE OF———————HOLE^—————————.
...5
Ashmore Twp.
FROM TO DESCRIPTION
There is some biotite developed. Therock grades to a more uniform carbonat
andesite around 202.- it is nore greerthan the ordinary brownish carbonatize
andesite. Generally unmineralized but
there is a small stringer @ 212.7 witlsome po,cp and py.
- 253-255 blue-Grey chert band wittsome py and minor cp in stringers*
Contacts normal to the Core Axis,After 255 we return to a carbonatiz
andesite with a speckled type ofcarbonate alteration.
@ 286 and @ 299.8 quartz stringer
with some tourmaline.328-329 short black siliceous band
with strong alteration at both contactContacts are gradational - 7/6 dissemir
After that there is. minor dissemirpo,py and cp in a zone that has patchy
alteration - mainly local zones ofof silicification and carbonatization.
@ 346.5-348.5 gradational contactson a paler green tuff unit. The fragmeare small - leached white - locally
feldspar metacrysts T After t.h* *.iiff
CORE SAMPLES
FROM
.zedishd
254
3d
328j fited p
ited335340
its
TO
255
329
r
340
345
RECOV. WIDTH
1
1
5
5
ASSAY DESCRIPTION OF SAMPLE
Chert - minor py cp
10# di BS. py
minor diss. sulph, py po c p
w " " py po cp
-
TORM S22
NORTH EAST. —— EUEV. ..— A1IM. ——— DIP —————
DIAMOND DRILL REPORTHOLE NO. COMMENCED. FINISHED- PURPOSE OF. HOLE______
A-6-72 ...6
PROPERTY #1Ashrcore TWP.
FROM TO DESCRIPTION
there are a few bands of the brownish
carbonatized andesite.
Around 350 there is some silicificand another tuff unit. -(352. 3-353)
353-360 zone of strong leaching,chloritization and carbonatizationno mineral.
After 360 a return to the dark grecarbonatized andesite - only rare spec
of mineralization - some biotite devel389.2-369.6 Short altered band
containing 15# po 3# cp (EK-16 ?)Around 415, the rock starts to bee
strongly silicified and greyer in colo
It is not a chert unit., unroineralizedaround 424 this zone ends in a shortaltered, breccia zone.
After 424 - brownish carbonatized
andesite, leaching around quartz-carbostringers. @435 and @438 chert.
440.8-444 short tuff band as befo444-463.8 andesite carbonatized463.8-465 a highly contorted zone
of mixed andesite and blue-grey chert.465-467 silicified andesite
The remainder of the hole is
CORE SAMPLES
FROM
tion
ncs
389imeir.
late
•e
TO
390
RECOV. WIDTH
V
1
ASSAYDESCRIPTION OF SAMPLE
A2 alt. - 10# po 2# cp
FORM 6 22 NORTH EAST. —— EUEV. —— AZIM. ——— DIP ————
DIAMOND DRILL REPORT
WILSON OPTION #1———— Ashmore Twp.
HOUC NO. A-6-72 COMMENCED———————- FINISHED___________
...7
PURPOSE OF- HOLE—____
FROM
-
TO
492
551100
15020025C
254300350356399450492
DESCRIPTION
andesite with short zones ofcarbonatization.
END OF HOLE
SAMPLES FOR THIN SECTION
Hornblende Gabbro
Massive andesiteAlbite porphyry - with epidoteChloritic and carbonatized andesite miDark green strongly chloritized andesiVery dark silicified andesiteChert bandCarbonatized andesite - unmineralizedCarbonatized band in the andesiteStrongly altered zone - chlorite carboDark groen andesite with biotiteAltered andesite with carbonate chlorimassive andesite.
CORE SAMPLES
FROM
ior py;e
late
:e
TO RECOV. WIDTH ASSAYDESCRIPTION OF SAMPLE
flCUra HIKES LIFTED\IIMMIKS. OMIQ
^W- X? (Zfara^jb^
A-6-72
txl.
Az 1800
l 1.' . 3 Ve U t. , .Cd* i -S
scale 1*100'
NORTH EAST. -EUEV. ___D^-Tr-T——i0P
-@-300—U*—-
DIAMOND DRILL REPORT
PROPERTY——WJiSQN——OPTION——#1———
JLEtiniore Iwoj
A-7-72—January-29/72-- FINISHED——ja nua rv—31/72
PURPOSE OF— HOLE
Pytl 1 ort hvf Brfldlpy'
FROM
010
.
53
TO
10
53
76.3
DESCRIPTION
CasingHornblende Gabbro - after 39 the ga
is similar to the previous hole. -numerous blocky crystals of hornblende- some altered to chlorite, occasionalhairline stringers of quartz-carbonatenonmagnetic, unmineralized, carbonatiz
Previous to 39, the gabbro is muchmore highly altered - almost all of thhornblende crystals are altered to chlwith the pseudomorphic shapes best seeon the fresh surface. There are somelarge greenish feldspars developed andoccasionally you can see some amphiboland biotite. Kuch more carbonate in thzone - unmineralized.
The gabbro becomes finer grainednear the contact. Contact broken.
The first 2 feet here is massiveandesite, while after that there is a
whole zone of interbedded chert andandesite. Units are too small to be
logged individually.3 main types - grey-green carbona
andesite, blue-grey chert-, and a darkto black siliceous member, the latter
CORE SAMPLES
FROM
bro
d.
rite,
s
izedrey
TO RECOV. WIDTH ASSAYDESCRIPTION OF SAMPLE
FORM B22
ELEV. .AZIM. - DIP _
DIAMOND DRILL REPORTPROPERTY———WILSON—— OPTWN——#i~
HOLENO. COMMENCED FINISHED —— PURPOSE OF HOLE —
...2
Ashmore Twp.
FROM
-
76.3
131.1
150.6
TO
131.1
150.6
302
DESCRIPTION
is very massive. Banding is generallynormal to the Core Axis. There is somefinely disseminated py po locally, whimost of the mineralization i e in largeblobs and stringers as po fi cp.69.5-69.9 iron? very fine grained,black, strongly magnetic, with cp po.
Andesite - the first foot is thebrownish carbonatized variety, whileafter that there is approximately 10*of massive andesite. The rest of the ^is carbonatized andesite but it is daigreen in colour. Strong alteration @ Swith some epidote. There is usually sovery fine specks of cp throughout thethe zone although there is not much c;overall. Some tremolite ? locally.
Around 121 some silicification -core changes to a dark grey to black@ 123 After 128, brownish carbonatizat
Albite porphyry - asin previous hwith feldspar, minor epidote, somebiotite, and unmineralized. Upper cont@ 90 0 lower @ 45 0 .
Massive grey-green andesite, 2small pyritic bands S 187.5. The rock
CORE SAMPLES
FROM
ler 63
7073
mek
)
ne
Lon.)les
tct
TO
707375
RECOV. WIDTH
2' 3
2
ASSAYDESCRIPTION OF SAMPLE
minor cp ponegligible sulphidesminor sulphides
..
FORM 922
NORTH EAST. —— ELEV. —.. AZIM. ___ DIP ————
DIAMOND DRILL REPORTPROPERTY WILSON OPTION-
HOLE NO. A-7. 72COMMENCED——..————- FINISHED—————-^—— PURPOSE OF———-——HOLE——-—————————
Ashmore Twp.
FROM
-
TO
302
DESCRIPTION
becomes highly carbonatized and brown!around 194, then the rock grades intoone of the dark silicified zones arour
208-210.2 - Silicified but pale gr*andesite.
210.2-216.5 - Darker andesite grade
darker grey with cherty and carbonatissections. 5/5 py po cp
216.5-218 - banded altered andesite218-219.8 - silicified band - grey219.8-240.2 - banded altered andesi
- banding @ 90 0 , numerous stringers ofquartz-carbonate; Some bands are chloxsome carbonatized andesite with talc?le. biotite. @ 225,5 3 tiny bands carrjArsenopyrite ^" of core along quartz-carbonate stringers. Very minor minerssome core broken P 230.
240.2-250 - grey silicified andesitvery minor mineralization - isolated lof po cp. 250-302 - Massive andesite (
local splashes of mineralization.264-265 Quart z-c&rbonate stringer
along the core axis with minor po py c
END OP HOLS
CORE SAMPLES
FROM
sh
i 203.an
2108 2129d 215
217
be
i. t i zed
Ing225,
Lizati
9 -
Lebsnly
264P*
TO
212215217220
i
5on
'
265
RECOV. WIDTH
2
323
1
ASSAY DESCRIPTION OF SAMPLE
A2 silic - minor po py cp" - 5-7# po py cp" - 5-7/S po py cp
A2 alt. - neg. sulph.
*
grab sample - Aspy forGeochemistry de Au
mass, ando s. - minor po py
'
'
FORM S22 NORTH—-- EAST. —— ELEV. .AZIM. — — DIP ____
DIAMOND DRILL REPORTHOLE NO. ^.0^COMMENCED—— FINISHED-———— PURPOSE OF———HOLE
Ashrrore Twp.
FROM
-
TO
1050
ICO200250300235
'
DESCRIPTION
SAMPLES FOR THIN SECTION1
Hornblende Gabbro - alteredHornblende GabbroCarbonatized andesite - tremolite?Carbonatized andesite -brownish baneDark green silicified andesite.Massive andesiteBanded altered andesite with talc?
-
*
CORE SAMPLES
FROM TO
' f
RECOV. WIDTH ASSAY
'
DESCRIPTION OF SAMPLE
*
MllfJRW f"?'w invTtnTJF""i'l1 rv-sn-r,———— 11.0, tl.^, U i^nfliJ ——————
Zk/Jl fc. UJjtlaHC/f.'L^
A -7- 7 2
Az 180e
scale 1-100'
DIAMOND DRILL REPORT
PROPERTY- WILSOM OPTION ffi
HOLE NO. A-3-72
COMMENCED————FINISHED—PURPOSE OF .^——————HOLE____^T^st copper
Claim TB 229617,Ashnore Townahipj Qnt. —DriHed"'byT"Trradlgy~^rgg,'-
FROM
0
60
TO
69
160. L
DESCRIPTION
Casino.
The fire, t 1C f oat IB cnrbonatijsecl andesiti
brownish - minor biotite. Then the endesi
becop.p,c nore massive tmd frey ffrcon in
colour. First bit of riiroralizfition seen
around S2 . minor pyrite,,
Around 100 there aro u couple of elliptic)
lensoo of po py - nagnetio.
After that the andesite becorjoo wenkly
brecciated vdth chlorite and minor pyrite
along these fracturoo.
Locally the rock is carbonatized brownish
There are a few qta-C03 otringora cutting
the core - aopifl are stained brovmish.
Around 119 there is some dark green
silicified andesite which grades to the
brownish cnrhonatisted andesite around 12k
The intermediary (121-124) io a putty
colour* Only minor mineralization - a feit
specks cp seen.
129-133 grey ^reen nilicified andesite.
133-H3 brownish carbonatized andesite.
143-144. 2 intermediary.
144*2-145.3 dark p.roen oilicified andesit
Short band of py (i 145*1
FROM
.
te
1
.
ccTO
)RE SAMPL
RECOV.
-ES
WIDTH ASSAYDESCRIPTION OF SAMPLE
rORM 522
NORTH—- EAST. —— ELEV. ——- AZIM. —— DIP ———
DIAMOND DRILL REPORTPPOPP..TV W ILSON OPTION A_______,
Ashmore Tovmship
HOLE NO. COMMENCED- FINISHED-—— PURPOSE OF- HOLE______
FROM
160 A
183.8
TO
183.8
212
DESCRIPTION
145.3-H8 grey preen silicified andesite
grades to a tore chorty member Q 147
with 155* py.
148 dark prosn cnrbonntizod andoaito
grades to a trey #reen naasive andesite
around 150.
153*2 dark proen and carbonatized ondesiti
apain v;ith minor pyrite, grades to a
brownish carbonatizod rock a round 154.5
and then to a massive frey green andesite
with local carbonatized patches around 157
Albite porphyry - lipht grey to dark Krey
with numerous feldspar phenocryst!! (or
metacrystal. This dyke is a bit finer
grained than that usually encountered.
Minor biotite developed, epidote alterati
common. Upper contact broken. Lower ®
600 to the Cure Axis.
Up to 185 - short sone of highly cur-
bonatiaed andoaito, some very fine
disseminated Mineralization; 05 184.7 Rome
py cp.185-193 a whole Bone of nixed blue-r,rey
chert und andesite. A few quartz strirrer
and some cp, po.jpy throughout*193-200.9 weakly banded oarbonatized
FROM
5.
184
186
n
188
19?
196
ccTO
166
183
193
196
201
)RE SAMP1
RECOV.
-ES
WIDTH
t
2
2
5
3
5
ASSAYDESCRIPTION OF SAMPLE
-
Ag * chert minor sulph.
Cherty .6Cu.
Cherty neg. oulph.
Neg. sulph*
A? - minor py, po, c p.
rORM 922 NORTH—— EAST. —— ELEV, -— AZIM, —— DIP ————
DIAMOND DRILL REPORT
PROPERTY. WILSON OPTION /
HOLE NO. COMMENCED,FINISHED.-— PURPOSE OF HOLE——^^—
As'more Township
FROM
212
213.6
TO
213.6
301
,-i
301
DESCRIPTION
andnaitft, somft biotite - nilieoous zona
(clnrk) 19'v. 5-195 some dinnominatvad py po
cp. 200.9-212 zona of mostly blue-grey
chart fractured with cp nnd po. Mnor pySomft ondsfiite?
Albite porphyry - an previous with
foldopar, Clino? epidota, BOGIO biotite.
Andoaito - niXfld groyinh silicfjous ZOHflS
and frey graen maaaiva andeaitq zona s, in
general crud^ contacts *it ^5O *- n 1'-hft
Core Axis. .Only minor -.cp s e an in ntz-CQ*f . . t \ } strincers. ** 21*1* 2?6, 290 the rockitself is generally unmineralized. Somebiotite.
.EH!) OP HOLE.
-
CORE SAMPLES
FROM
201
202
201.
210
242
TO
202
204
23,0212
244
RECOV. WIDTH
1
2
6.2
2
ASSAYDESCRIPTION OF SAMPLE
Cherty - minor sulph*
Chorty - l^S Cu.
w - minor nulph.
A^ * chert - .5 Cu.
*2 - with qtz-CO^ atr.
Minor cp, py, po.
:., : .
. '^i '
.•- :
FORM 922
NORTH——
EAST. —— ELEV. ——- AZIM. ——— DIP ————
DIAMOND DRILL REPORTPROPERTY. WILSON OTTIOM if l
HOLE NO. COMMENCED FINISHED—— PURPOSE OF-HOLE——^-.
Ashmore Tovmship
FROM TO
69100
150
200
250
300
DESCRIPTION
3AMPW.S FOR THIN SECTION
Brownish cerbonatizsd andesite.Mannive andesite.
Park prenn carhonati^ed and-nita vith py
Massive andesite.
Silicified andesite . biotite.
Mafloive AndftnitOf
-
FROM
CC
TO
)RE SAMP1
RECOV.
-ES
WIDTH
t
ASSAYDESCRIPTION OF SAMPLE
bOJU Z. QJiiX(M-dL^Howra BSSS flwnto"" upSS. OIUWIO
(fi o
DDH A-3-72
Appendix III Sheet
SUMMARY OF ASSAY RESULTS
Average Values
Cu(ppn) Zn(pptn) Nl(ppra) AE(OZ) Pb(ppm) Au(oe)
203-213
215-230
234-235
240-245
249-250255-260235-320
1174
7791330
2940
3330
700
1026
64
7567
261
6100
126
67
165
254
326
133
222
,070
.059
.093
.128
.231
.073
.072
id209
2060
4321
Nil
Nil
Nil
Nil
Nil
.02
Nil
Best intersoctions: 240-245 .294^ Cu, .123 oz Ag,
249-250 .33#i Cu, ,61# Zn, .231 oz Ag.
DDH A-4-72
164-16?
@ 200 - py
230.235
250-307
307-310
316-313
34
173
4990
4700
1630
1370
60
1050
132
182
199
92
121
1410
119
139
51
171
.029
.032
.131
.14
.070
.073
12
35
10
13
10
13
Nil
Nil
.02
.006
Nil
Nil
best intersections: 250-252 1.56?; Cu, .43 OB Ag.
275-276 ,69?i Cu, ,23 oa Ag.303-305 2.36# Cu, .15 OB Ag,
III Sheet flbf
Cu(ppm) Zn(ppn) Ni(ppm) AE(OZ)
DDH A- 5 -72
240-255
302-303
Best
DDH A-6-72
37-46
47-49
1*5-195
254-255
328-329
335-345389-390
Best
DDH A-7-72
53-83
207-232
5987
15200
intersections
176
720
393
1550
282
145
3010
intersection:
151
95
ft 225,5 Aspy 8
264-265 454
80
134
: 240-241
302-303
56
38
33108
137
56
71
389-390
55
75
3790
90
299
6.9^ Cu,
1.52# Cu,
106
78
9756
105
139
156
.3* Cu, .
82
193
264
93
176
789
1.578
.789
035
038
028
064
053
034
088
088 oz
024
046
096
094
Pb(ppm)
18
34
oz Ag.
oz Ag.
27
10
8.5
17
39
913
Aft.
12
14
27
10
Au(oa
Nil
.01
.005
.005
Nil
Nil
.005
.01?
Nil
.15
.05
- 56-75 .025 oa Au,
lv : -A
*
4
AppendJ^III Sheet Wbt 3
Cu(pDm) Zn(ppm) Ni(ppm) AK(OB) Pb(ppm) Avi(paJDDH A-g-72
184-212 1540 74 8^ .086 14 Nil
242-244 5490 60 110 .266 15 .005
Bent intersections: 201-204 .fl5# Cu, .199 oe Ag.
242-244 .55^ Cu, .266 OB Ag,
42E18NW0MS 16 ASHMORE020
HOUXNOER MINES LIMITED
REPORT
GOVERNMENT EXPLORATION ASSISTANCE PROORAMKB
WILSON and KALSON OPTIONS
ASHMORK TOWNSHIP
taE10NW0M5 16 ASHMORE
TABLE OF CONTENTS
020C
X - SUMMARY (F EXPLORATION
A - LOCATION
B * WORK DONE
II - OPTION TERMS
III - GENERAL OROLOGY
XV - RESULTS
A * DRILLINO
B - ASSAYING
V - CONCLUSIONS UtA RECOMMENDATIONS
l
JL
1
2
6
6
APPKNDIX I
APPKriDIX II
APPT.NDZX III
Al'Pt^UIX IV
APPENDICES
PLANS OF DRILLING
DRILL SECTICXiS
SUMMARY GP ASSAYS
MAP OF PROPERTY
OF EXPLORATION
A* Location
Ashmore Township ia located in the Thunder Bay Mining Division and comprises part of the Little Long Lac gold mining area*The property consists of 25 unpatented and two patented claims under option, and ia located approximately four miles east of Geraldton along Highway H*The unpatented claims included are t
TO 139350.353 inel.i TB 229616-61* inel| incl*l TB 23*726-72* inol*t 325351*359 incl.t and
)1*
The two patented claims under option are i TB 10164 and TB 10971*
B* Work DoneThe original 14 claim group waa acquired in March, 1970. and Hollinger Mines United performed geophysical (magnetic and electromagnetic) surveys over most of this group* On tha basis of tha geophysical data, two holes were drilled in 1970. with a total length of 1117 feet* Later in mid-1971 a geological survey was performed over thia original group* Both the drilling results and the geological eurvey were filed for assessment*
In the last quarter of 1971* Hollinger Mines United applied and received a subsidy to do further work on the property through the provisions of the Ontario Government's Exploration Assistance Programme* Under thia programme, geophyeloal (magnetic and electromagnetic) surveys were performed on nine claims that had been added in 1971* These claim (numbered TB 325351*359 inol.) were adjacent to the original group on the eastern boundary*
The assistance programme continued into the first quarter of 19721 when-a drilling programme waa initiated* Six holea, with a total footage of 24*3 feet, were drilled to check anomalous copper values obtained in the 1970 drilling and to teat a one of ground conductivity*
- 2 -
Since that programme expired on March 31. 1972, two patented claims, adjacent to ths west boundary of the original group, have boon added* In May 1972, a geological survey was completed over the nine claims to the east (TB 325351*359 inel*)i and in November 1972, Magnetic, electro* Magnetic and geological surveys were completed over the two patented claims*
In April 1973, a second Exploration Assistance Agreement was signed to cover a drilling programme designed to teett
(a) a coincident magnatic*slsetromagnstic anomaly on patented claim 1097l|
(b) the best interssctlon obtained in the 1972 drilling at depth) and
(c) a Magnetic anomaly assumed to be on or near ths contact between the Tsmiskaming ssdimsnts and Keewatin volcanics*
XI* OPTION TERMS
An option agreement, dated March 23, 1970i between Donald Wileon of P* O* Box 730, Geraldton, Ontario, of the first part and Hollinger Mines Limited of the second part, gave Hollinger the riant to explore the original 14 claims and any subsequent contiguous elaias staked by Wilson or Hollinger,
The payments, under which Hollinger may acquire the property, aret
A sum of 6 l j 500.00 upon signing the Option1 . upon gnng pon, ljooo.00 on or before March 23* l 1,000*00 on or before March 231 1 lJOOO.00 on or before March 23! 1
T 1^000.00 on or before March 23l 1 and a further sum of 9100,000*00 on or before March 23, 1
* #
Thua, total payaents of ^105, 500*00 are needed to acquire the property*
Also, for any ore mined and Billed from eaid mining lands in excess of the first million tons, Wilson shall receive a 25*eent**per~ton royalty*
A total of ^4,500*00 hae been paid to date ae set out by the above agreement*
-l *, t
By a similar agreement dated Oetobar 30, 1972. tha two patented claims (TB 10164 and TB 10971) were optioned to Hollinger by Mr* Herbert Kalson of Geraldton, Ontario*The payments by whioh Hollinger nay acquire this property aret
A sun of 6 1.000*00 on signing the Option. -i ljooo.00 on or before October 30* 197 f liOOO.OO on or before October 30J l"
and a further sura of 9135*000*00 on or before October 30, lf *
A total of ^1,000*00 has been paid to date, ae outlined in the above agreement.
Ill, GKNKRAL GEOLOGY l
The property ie largely underlain by a sequence of Keewatin lavas Intruded by younger hornblende gabbro*, hornblende** * . * * * * ̂ J A M. A t* A f̂ A. W m—. .diorites and albite (or just feldspar! porphyry* The southern portion of the property is underlain by Tewiekaraing sediments. The Teolskaraing sediments encountered were congloneratea and arkose which are similarly intruded by the gabbro, diorite and albite porphyry*The Keewatin lavas consist of andeeitic to daeitio flowe and tuffs whioh are highly metanorphosed. Biotite and chlorite are often found in these volcanics, with accessory carbonate and silica* Tho tuffe are characterised by nunxtrous, mall, subangular fragment e in a chloritic matrix. The tuff horisons generally have a gradational contact with the massive flowe*The nasslve flowe often contain narrow chert horisons. Initially these cherty B nee were thought to represent flow tope, but there are at least three different types of occurrencesil* Chert band*gradation*! with the andesite
(How top*?)2* Chert banda with abrupt contact**3* 2one s of nixed blue grey chert and andesite
(silicification?)Although intersections of chert were quite cosnon in the 1972 drilling, very few chert horlsons were encountered in the present program** Hence, no additional inter* pretatlons can be made about the** unit**
The hornblende gabbroa are easily distinguished by the numerous blocky crystals of hornblende in a dark green chloritic natrix* Often these blocky crystals ara altered to chlorite) however, the crystal habit usually remains* The gabbro*, as with ths diorite*, are presumed to be Early Algoman in age*
The only hornblende diorite encountered waa in hole A~14*73| on claim TB 139352* No surfaes exposure* of thie unit are noted on the property* Although the blocky crystal* of hornblende still persist, as in the
fabbro, they ore only locally developed and calcic eldspar is the predominant mineral. Unlike the gabbro, the diorite was weakly magnetic. although there is no expression of an anomaly from the geomagnetic survey performed in the area*
The albite porphyry dykes are presumed to be Late Algonan in age, since in a couple of surfac* exposures ths porpnyrie* are seen to intrude the hornblende gabbro* The high sodic feldspar content is diagnostic of all dykes encountered* This rook is usually pale grey in colour and quite hard, with the main alteration noted * ' alight amounts of epidote after feldspar*
taming sediments are encountered in surface exposures on the Kalson claim* and in drill hole A-14-73, on claim TB 139352* Moat of the Teadekaming aerie* her* is represented by conglomerates, with only a few sonss of arkosic material noted in the drill hole*
Tha conglomerate contain* a variety of pabbla typos that show a wide range of alse and snaps* 'Many of tha smaller pebble* (usually lass than i inch), tend to bs - quits angulari while the larger one* (l inch or greater), ara distinctly nora rounded in nature* Tha matrix of tha conglomerate is brownieh and moderately biotitio with small quarts 'eye*' scattered throughout* Local increase* in alteration create a much softer, mor* chloritic natrix*
Tha arkosic bands saan in tha drill hols ara relatively narrow and ara characterised by numerous Miall grains of quarts and feldspar, in a grayish to grey-green matrix, Contact* ara usually gradation*! with the conglomerate units*
f ~IV* RESULTS
A. Prilling
Fivo holes were drilled encountering tho rook types previously described under general geology, beingi Chert, Andesite. Hornblende Diorite, Hornblende Oabbro, Albite Porphyry, and Toniokaming sediments including arfcose and conglomerate,
AU of t ho drill logs will bo filed for assessment, hence only a plan of tho drilling plus a copy of tho drill sections accompany thio report. A total of 2)91 feat wore driilodj 1005 foot to test tho magnetic-electromagnetic anomaly on tho Kaloon clalmsi 996 foot to check tho wide ooppor bearing ono found in tho 1972 drilling, and 790 foot to tost tho magnetic anomaly in the Tomtofcaming oodimonto*
Tho n*gn*tic*cloctromagnotio anomaly on tho Kaloon elaino Mao attributed to a narrow (up to ono foot) band of aaooiva pyrrhotite carrying adnor pyrite and chalcopyrite, Tho excellent profile! obtained fron the geophysical eunreya fron ouoh a narrow tone oro probably related to tho rather shallow overburden depth* in tho area*
t
During tho 1972 drilling, an intersection of 17 foot assaying .47? ooppor. *X4 ounces/ton silver v was obtained in holo A**~7** Hole A-12-7J was set out to cross thio sons approximately 100 foot vertically below tho original intersection. Although a substantial -width of rook anomalous in ooppor was encountered, assays show tho sons to bo Manor at thio depth.
Drill hole A*H-7J was designed to cross section a magnetic anonaly prosunod to bo in tho Keewatin volcanics -~ tho additional footage allowing tho hole to out the voleanio^sediaentary contact, Unexpectedly, after 196 foot of overburdoni tho hole ooUarod in Tomiskaning conglomerate which extended to a dyke of hornblende diorite at 610*) foot, Tho magnetic anomaly was attributed to approximately 45 foot of conglomerate containing numerous dioaorn* inated blobs of pyrrhotite.
Previous to tho drilling of hole A-14-7J, two olaims wore added along our south boundary to protect any possible results obtained in that hole. Thus, tho
present number of claims Mentioned at the first of this report it two creator than the number indicated upon signing tho Exploration Assistance Agreement* No work was carried out on those two now claim (TB 37279s and TB 372799), to that nono of tht provisions of tht Agreement woro violated*
Bt AssayingAssaying of oora camples waa completed at Hollinger Mine* limited. Assay Department, by tho atomic absorption method* Samples woro asaayad for ' various elements, inducing i copper, sine, nickel, silver, lead and gold*Each smplo is nroparod by crushing and grinding the rock to a -100 nosh fraction than dacoamoslng tht product by tho addition of hot nitric and hydrochloric acids*A list of tho assay rosults acccajpanlta this report in suvsiary fora*
V, COHCUI3IOH3 and RECOMMENDATIONS
Exploration to data has rtvtalad two rtlativtljr strong tlactroraagnttic anonaUos with associated high nagnttlos, to bs related to narrow bands of massiyt or ntar smssivs pyrrhotite with minor acstssory pyritt and ohaloopyrlto* One of these anomalios waa outlinod and drilled in 1972, the seoond anomaly lying within tho Kalson claims and boing drilled during tha course of the present programs*
t
Further, a sons of dissoainatod sulphides haying economic implications WAS previously outlined by drilling, to the east of the geophysical anomalies more recently located on tho Kalson claims* Thus, the Kelson anomalies appeared to be ideal targets for drilling as suggested from the nearby pyrrhotlte-chalcopyrite sone* Unfortunately, the data now available indicate that this entire section is not viable for mineral exploitation*
r
However, due to the intimate relationship between pyrrhotite and chalcopyrite noted in this area, magnetic horisons would appear to be favourable drill targets, either with or without a coincident electromagnetic anomaly* Several untested magnetic anomalies, which do not appear to bo indicative of a change in rook type, remain on tho Wilton elaias* The most probable interpretation to be applied to this is that the anomalies suggest the presence of pyrrhotite - hopefully continuing its association with chalcopyrite*
.7 -
The presence of Timiskaming sediments on ths property may indicate an additional exploration opportunity, in anarch of gold* Although most of the Tinlskaning bslt here has boon extensively drilled, very little work has boon dona in ths Rides Lake area* Unfortunately, the results received to date in the sedlnsnts hairs been very poor and no major structural features, which ars often closely associated with gold ores, appear to be indicated* In ths absence of known stringer aonss, or structural controls, a couple of oross*sootional hoist nay bs warranted to test ths Keewatin-Timiskaming contact*
August l, 1973*
WHINGER MINES LIMITED MHHINS, ONTARIO
APPENDIX I
Sheet
l of 2
(j^j^^SBassgssgfcaSf
(t W
^
-s?
V
^
* .^ 5
APPENDIX I Sheet 2 of 2
^ C'O '
APPEN
DIX
II
Sheet
l of 5
5o,VV,
(Vi
APPENDIX II
Sheet
2 of
5
xvj
APPEN
DIX
II
Sheet
4 of
5
\
H
Qtt -P M O P-. O) CL,^ •^ co
t*
3I: e
* **w\
55 3*1m
m I^f
o o
*"t
. .
Mb
d 3 ii^
* *
I*; ^*fi
tt tt
N
N *
N
N
*~O
O
O
~
"o
e
eaMaeW*
s fe•3m
o
a ^
..
** o o
ott
tt g
tt tt
* t0
-S R
li.a* *A
9399
00
00
*3|J^* **
Wt
^A
C*
XiA ^*
-^ nR 5*4 ia ^
i* ^ ;J
is*
iH
^1 O
M
M
^O
O
O S
O
ae g
- 0 0
A
tt tt
lsaS
w *rv
68**\
t*- IB
^
\*4
W
JS f-l
-PCoe e
4*
*o to *• 4*
B.O
^
5•S
^^S
*ft i-4 O
fi.h
a
o
5fci
O7
e
*4 vt
*4 *4
NO
*^ IA
i.P.^ s^sss ssS
H
loll
K\
O
O
CM O
S
O\ to
a••^ *^
*53S
J5 O w
** O
rf rf
APPENDIX Stott 2
A*10*73 (continued)
242*245 .19* Cu, .11 OB Ag 245*247 .10* Cu .05 OB Ag370*375 .34* Cu, .13 OB Ag 375*3*0 .135* Ctt, . OB Ag
All grab aamploB ahowod background valuta, All assays for gold woro Nil.
DDK A*U*73 Cu(pptj) Zn(ppn) Ni(ppei) Ag(os) Pb(pjpft) Au (on)
40*50 190 45 *7 .03 12 Nil 30-130 264, 02 64 .03 17 Nil
Highest aeeayai 100*105 .10* Ou, .05 OB Ag123*125 .W Cu, .09 OB Ag * l foot of
pyrrhotite.All assay* and grab aamplta in thia holo war* mie h pooror. AU asaaya for gold Vftra Nil.
DDK A*12*73 Cu(pjw) Zn(ppa) Ni(pjw) Ag(os) Pb(ppw) AU(OB)160*195(172*177)250*2652d5*360(350*360)
3341608201372510
37304749
302
*9121111919^
.02
.03•03.05.05
1212141110
NilNilNilNilNil
High*at aseayai 167*170 *04?S Cu, .03 OB Ag172-175 .222* Ou, .05 OB Ag175*177 .064* Ott, .02 OB Ag253*255 .077* Ou, .05 OB Ag292*294 .145* Cu, .05 OB Ag295*300 .069* Ou* .03 OB Ag
310*315 .06* Ott, .04 OB Ag320*323 .066* Ctt, .a OB Ag
330*335 .01* Ou, .07 OB Ag355*360 .09* Ott, .06 OB Ag
APPENDIX 111 Shoot 3
A-12-73 (continued)
Moat of tht grab aanplaa in thia hola yioldod background values, except for two aa follows t
275'300*
Cuppsi
573170
Znpym3460
d5
Hippei
35idd
Agos.3
2.6
PbPPM
id3d
AUosNilNil
In tha light of high aaaaya for split samplas shown above, it thua appaars that tha interval 275* to 360' is characterise! by valuta whleh ara high background or slightly abova.All aaaaya for gold values waro Nil*
DDH A.14-73 Cu(pjw) Zn(ppa) Ni(ppsi) Ag(oi) Pb(ppai) Au(oa)
200*360 10d d3 97 .02 19 Nil640-695 500 40 50 .04 10 Nil(640*655) 1240 5d 54 .07 U Nil720*745 450 4d 59 *04 11 Nil760*7dO 523 32 40 .03 12 Nil
liighaat aaaayat 315*320 .03^ Cu, .02 os Ag640*645 *W Cu, .10 os Ag645*650 .13* Cu, .06 os Ag650-655 .0#, Cu, .05 os Ag732-735 .0# Cu, .07 os Ag737*740 .13* Cu, .Od os Ag764*765 .32* Cu, .17 os Ag76d*770 .09* Cu, .04 os Ag770*771 .07* CU, .03 os Ag
All grab aanploa yioldod background valuaa.Although thia hola intoraaetad Taniskaning eongloaarata and arkoaa which onhaaood tha prospoot of finding gold, all aaaaya for gold waro Nil. Tha aadiaonts would appoar to bo barron unlaaa affootod by a aajor atructural foaturo and/or host to ona or mora atringar sonos.
'7.s f—/7
'SNIWW11 S3NIW M39NmOH
/.d S ST 7 ' 6rf z- 7*2
J
'•"/s'ff^'FORM 522 "
EAST. .
FI f",AZ'M. , . , ,, ,nip L/IKiC.C
31-i-OOSj 9-;-;; oy;29,^3
collar 'i - ^q - ,
rv?
:eTP^J-T
voftt
/v^/
. 300' .- '\ f L ^ '
DIAMOND DRILL REPORTHOLE NO. A-l/i-73
COMMENCED^ FINISHED-^——
PROPERTY- VIIQr: OPTIOl!PURPOSE OF______———HOLE_'fist ;ri;.::':;^
.Ashmore township .y'-iril?:'''
FROM
0
126
TO
1266 M). 3
DESCRIPTION
CAoino.Coneloi.ierate - /I'enisknr.inr in age. .
UD to ISO the conglomerate is slightly
frfienish fcrav to grev in colour. After
1^0 1",*i" rort^ 1'! n^Av^tf*' i -^ r "Ppy i ^ fnloUT1
with numerous fragments or pebbles. The
more sedimentary nature of the con'-lonera!
is not truly noted until further down the
hole where the pebbles are much more
rounded.
Aftor ISO we start to ret a few smoky
rmarts RVP.S and the conglomerate tends to
Ion],- ri ft ,o ri y i ri on t. i r, T 1 t-i thp niit.prop on
t.ViR T'alsori , i-,t.i nr,, '"^n t.evhiirp nlnn
changes s one v/h at ?fter ISO from the su&arj
nature over the first 60' to a more
inar.Kivfi groimdpi.iss \-nA;h t.hp ounrt,?, pyes.
Ahciiit. -i.hp 'inlv o-f-.hpr rii Rt.iprn-i shaVil P.
rdneral in the matrix is biotite which
occurs in vorv tiny brownish flecks. The
amount of biotite decreases after 1#0.
The pebble sif.e is f enerallv 'in the
^ to J" ranpe althouf'li some fra;-.nents are
greater than an inch. The larger pebbles
are usually e Ion rat e at approximately 4 5to the core axis. The smaller fragments
FROM
Q
t
CO
TO
RE SAMPL
RECOV.
ES
WIDTH ASSAYDESCRIPTION OF SAMPLE
FORM S22
NORTH EAST. - ELEV. - AZIM. — DIP___
DIAMOND DRILL REPORTHOLE NO. A -1A.-73
PROPERTY- Uilson Option :.-l
COMMENCED- FINISHED——— PURPOSE OP- HOLE——————
Ashr-'ore "i.p e
PROM TO DESCRIPTION
are fenerally more angular although this
tyne of occurrence is also seen in the
outcrop on t. h R iC.ilson property. The
pohhlor, nrp nf ssvnral types - the dominan
tvpe ceinff blue grey and cherty - in some
instances almost translucent; E**ey to buff
cherty pebbles; black siliceous pebbles -
fv?'ther dov;n the hole sorie of these look
r"i,!-jpr slaty; olus some dark brownish to
"T..pniRh pphblfis \;hj.ch often contain
r* 1 op -i t. A -h -i nt. -i t. A t
153.4-153 and 167-180 are nore massive
sf.'-itions - d -ir k ^rev rreen in colour -
ne n-i pt.i n^ii-i f?hahl A pjnftra^s. The pebble
sj v e and number .lust generally decreases
ir'jo these zonos - arkosic?
; After ISO the pebble size r.radually
increases over 2' and then we start to
r,et some better conglomerate and the
quartz eyes begin to occur.
rineralization is only minor with a
f AW tinv h .1 ab F. of Rijl-jhides in the early
p:^rt 'if t.bft hole - mostly pyrite - some
pyrrhotite and rarely chalcopyrite. The
pyrrhotite ip onlv iveakly ma^'iieti^c - and
the chalcopyrite is generally associated
FROM
CO
TO
-
RE SAMPL
RECOV.
ES
WIDTH
*
ASSAYDESCRIPTION OF SAMPLE
}'[.
'-.
('
NORTH. EAST. - ELEV. - AZIM. — DIP———
DIAMOND DRILL REPORT
PROPERTY- V/IL30I! OTTI01! -:?1
HOLE NO.
COMMENCED. FINISHED— PURPOSE OF- HOLE———————
•.-l!; -75
Ashmore Twp,
FROM TO DESCRIPTION
.••i t h it in tinv solashos. After 210 thereis a general increase in the amount of
sulphides - here vre have raostly dissemin
ated blebs of pyrrhotite and the rock is
more r-iarmfitie. fip ir, vsry m nor hfii*e t
Ar^un^ ?rt? i-.he p j 7," flnd r"mho^ nfpebbles gradually decreases into a short
zone of arkose from 30i..5 to 330. In the
G.ojTv lorip.r At.fi up t.o t, 'IR qrko.qe f.liA frapwrts
ir f- fi" in TV of t. h p Muiph frey t.ypo-
similarly at the lov/er contact after 330
althouc-'h the rradation here (330) is much
faster.
Ths arkose is rreener in colour than
the rrey conglomerate and contains a few
noticeable grains of ouartz and feldspar.
pTMct.i nnlly iinaJt.Ar'p.d - very I'n'nnr-
chlorite-sericite nearly the same as the
alteration in the conglomerate. Very
,-iinor pyrite in the arkose - solash of
chalcopyrite at 319.5. There arc a few
carbonate strinrers in the arkose unlike
the conglomerate r.u}d thore is some minor
brecciation and alteration with a few
narrov: carbonate. Rt.Hnr^rs f-rn^ ^n.^,^ t-n310.5.
CORE SAMPLES
FROM
200
205
210
215230225
230
235
240
2t5
250
255
260
26,5
270
275
22028-5
2902Q5
TO
205
JJ10
21^
220
225
230
23^
?;,n2L5
2^0
255
260
265
270
?7^2!sO
2^5
200
. 29.5300
RECOV. WIDTH
5t
5r,
5
5
*;*;
^5
5
s*5
S
•5
q
5
5
5
5
5
ASSAYDESCRIPTION Of SAMPLE
gl - very ninor sulnh.
ii ir it it
It It '.t IT tj, ^
" minor rjo i..y
tt Tt r^ ^ Tiy t, ̂ f ri
" ! t po py
II 11 r,,, y
" '' Tip ^V tv . C P1
" " no r'V tr. c*'
Tt It ^ 3 .-.y
If It T,,j r,y
" very •••I o ir f-,;;' -.'i.
TT It '1 If
It It !t If
" ninor mvrite
" " pyrite
vprv ,,inor ^
tt It tt ^y
" r^inor nv
FORM S22
NORTH— EAST. __ ELEV. —— AZIM. —— DIP____
DIAMOND DRILL REPORT
PROPERTY- \,'1LJO:J or'i'IOL? -'l
HOLE NO.
COMMENCED- FINISHED-—— PURPOSE OF- HOLE______
Ashriore 1'wn.
FROM TO DESCRIPTION
After the arkose v.re are into a eood
conglo.-r.erata before "tyO. There i? a
not.ahlfi iT'p-rpHRfi ^n py pn h^rp r - K i/oll
Schistosity due to frarincnt ,, elongation at
55 0 t o the core. Similar lithology aaprp.vi nnpl.y rlep.f.rihfiri nongl ni^erar.^ ,
^if^^r ^^0 "I'.li^ r, 3 A t. "p "i ir of1 t.hp ^ni"\c' i (ij'^y^p
becomes ,t;reeuer...and there are very numerouv/el.l rounded pebbles, llostlv blue prey
cherty, some white, some porphyry, some
black, none brown and some dark green.
Fvrit.fi -pyrrl-inr.il-.fi r.nnt.Pnt. rapirtly
rlonr'pnppp ft -f i-, o 37 ^Sn.
/t06-407.5 - short arkosic band}
speckled nature of ot^-feldsoar.
419.4-445 r rat.hnr sharp. .upper contao.tnt. J|.0 O t,o dark ^rov fairly manK3Vf! ( vf)ry
Rlifht.1v nlt.PT-fid nrlfrtse,
;, J, *; -I|J, f* - v^^y rt&rk- {jr-ny pnncT opo-^at .c.
vr..ry nnn 1 1 Vii\io r r^y fmr.-nontp p nmo nyrit
- contacts Kradational.
Wj.S-^56.7 - Fradation to greenish
arkose, fairlv passive, Minor nyrite.
^A.y.^m , ? - ^rflriat.inr, t" a Cnnri
conglomerate - mostly bluish grey and
CORE SAMPLES
FROM
300
305
310315
320
.^325
^30•ns
Mfi
345350 .
- 355
TO
305310315320
325
330
335
™.n
31.5iw
355360
RECOV. WIDTH
?
5
55
5
5
5
5
^
H
55
ASSAYDESCRIPTION OF SAMPLE
Ofl - very ninor ^y ^o
irkose - vary ninor r'v n o
it it it n v ., 0
It II It r,y T^ o p,,
It . !t !1 r)V -: 0
If It ' It ,r . l Q
)r"l r. i nor ;v no
" " ny r,Q
" ^ ; pv no" ITT nor r'y ~n
11 *} j r.v nn
" 3 'j pv v)0
rORM S22
'NORTH EAST. - ELEV. - AZIM. — DIP———
DIAMOND DRILL REPORT
PROPERTY- soi: nmo:; --"i
HOLE NO.
COMMENCED, FINISHED- PURPOSE OF- HOLE——————
Ashnore Tv;p.
FROM TO DESCRIPTION
whitish cherty fragments, minor py po.
Lineation of frarr.ients at about 75 O to the
core.
501.2-509.1 - short shear (I'M at
401,2 at. 60 to core then conglomerate
vi t, h a more arkosic: matrix. Pra^ments are
ri f"1 li f^Wpr ^n PHt'ih^T* t'. ban ot.ViPT f*oriP"l divier.*
h:rizons. ......, -,, . — ..- . ,,-,...509.1-521 - short band of co&rse con
glomerate - more brov;nish chloritic alter
ation. Traces of sulphides.
521-5L.3.f3 - some arkose but mostly
n'.ru'l o- -IP. rat i n fra^t.-.fint. fi in a rioi'fi arkosic
rr.;',t.rix ^ s irniLir t,.n thp. unit 501r-5Q9 ^"t,
l"V : re there is some areas with no fragments
T! fit h contacts fjraclatipiial - lov;er is more
r fp 1'^' ^ lit.t.lR piorp. alteration here -
chlorite, sericite. Lineation at 60 to
cors.
54^ T f5-605.S - return to conglomerate
H-inoat.p.d at 60 flonf axis of frajJT'fintfi) .
l-'uch more highly altered than previous -
matrix is ouite brovmish. Larpe number
of nebbles as before - mostly blue Krey
chertv,. some white, Rprao buff chertv, sonit
brov/nish and aandv. At 554.9 trace of
FROM
hf^
.
CO
TO
'
RE SAMPL
RECOV.
ES
WIDTH
t
ASSAYDESCRIPTION OF SAMPLE
FORM 622
NORfH- EfcST. —
ELEV. - AZIM. — DIP___
DIAMOND DRILL REPORTHOLE NO.
COMMENCED-
A-l/i-73
PROPERTY- UILGOi; OPTIOI? :rPURPOSE OF- HOLE ———.——
FROM
.
'
~ ^^W^•' ! Sfk
TO DESCRIPTION
chalcopyrite - otherwise very little sul
phides. -\round 565 we "•rade into a less
r.ltarcd conglomerate and the colour ehangr
from brownish t.o r-rey. Vnrther a] nnn- t.hp
zone the conglomerate also becomes more
.605.3-609.8 - contacts at ^5 0 - con-
.vnr^'iiir- to a short Dyke of gabbro??
Yer^ 'fine groundiiass i/ith soine fairly lar'
i rrp^'iil ar blph^ of brov;n5 tCn b i ot.i t.i r.
m,*} t.pTM ^i 1 ^nr! ^OT!!P TarlA rr^^n pp^t-^ nf
chlorite. It appears to have no effect
on the arkosic material at either contact
although the rivke seems to be slightly
c.hillRd and brownish at its contacts.
i'T on-!"aLnetiCj carbonatized.
609.8-611.3 - arkosic, grey green as
before. *
611.3-623 - sharp contact at 1+5 0 to
band of conglomerate , grey, hard, numerous
pabble.q- T;-inn-r RnlphiripRj traofi of np ^
612.1. Lover contact is quite abrupt at
80O to core into the much finer conglomer*tfffot* **S."w i ?s'*- 6 23-6W.5 - gradation from the con-clonerate for the first 2' then quite a
CORE SAMPLES
FROM
ft
be.
TO RECOV. WIDTH ASSAYDESCRIPTION Of SAMPLE
FORM 522
NORTH EAST. - EL6V. — AZIM. -. DIP———
DIAMOND DRILL REPORT
PROPERTY- ^O;-:' OFTIOi! j,''
HOLE NO.
COMMENCED- FINISHED—— PURPOSE OF- HOLE——————
A-l/,-73 7.
Ashr:iore ri'v;p.
FROM
640.?
TO
7QO
DESCRIPTION
dark r.rey f;reen arkose, llassive. Very
minor sulphides. Lower contact al one a
fiuartz Btrinrer.
Hornblende diorite dvke, upper contac
along- a quart. K stringer. Rather high per-
rent.^c-o nf feldspar VIOVA ,inH 1 really the
feldspar content is extrene. The rock is
medium ;:reen in colour with fairly numerou
hlehs of psp.iidomorphie chlorite after horn
blende, The roi^k is v^ry slightly magnet. -i
Hp t.n A6? t-h^rp nrp onit.e a f^w quart- 7-
stringers - usually at a low angle to the
norfi - nftst.ly hlinsh in colour, Assoftiated
.-"ronnrl thfiSfi n1-.rin 0^r,c' are ftor\A Rnlphlrinn
py pii v/it-h 6 nn0 f; 0^"^ sized splashes ofchalcopyrite.
667.5-670.3 - few quartz-carbonate
stringers hore, making the diorite quite
altered. The diorite becomes finer grains
r.iora silicified, v;ith sortip. brink red
staining of the felriRpnr, Arr.pr.f.nry ^hT^r
vdth the stringers - less than normal
chlorite .vdthin the diorite.
Sone chalcopyrite around a quartz
stringer at 6S6.
Around 9??-1 t.hel rli nr-i ta hoflnme-R .1 hit
CORE SAMPLES
FROM
640
, 6L5
6506^5660
j 66S
. 670
:. 6756rtnArtc6 on
l, ———
It-0
TO
64-5
6-50
6^
660
665
670
6756rtn
6ft5
690^95
RECOV. WIDTH
^
^
555•5
*;i5
5
5
ASSAYDESCRIPTION OF SAMPLE
T,^ - vpry r^-innr rp p. -i r.y
' minor py j.io .cptf " en roy
" n pv cp
" " py np
" very riiinoT- py } t.r. r.^
" t. T A r A py
" np^li^ihTo piilph.
!1 ——— minor ".y c P ————————————•* ** *
-.'J
FORM S22
NORTH—. EAST. —— ELEV. —- AZIM. —— DIP————
DIAMOND DRILL REPORT
PROPERTY- VJLS01: OPTIOH j/
HOLE NO.
COMMENCED,. FINISHED——— PURPOSE OF- HOLf-————.—
A-14-73
Ashmore Tv/o.
FROM
-
TO
7QO
DESCRIPTION
finer trained and then -around 728.8 the
rock becomes very brownish and micaceous,.
After 728.8 to 741.3 the rock looks some.
vrtiat like the matrix of the brownish con
glomeratic. Thnrfi la so much bint.-it.P an ri
ouart.7. arminrf t. h i s 7.nnn t. hat. it. -j p v^ry
rii f. f iciilt, to inte7?pret. There is about30,3 bluish qtz strinp'ers here and some
sulohides associated v/ith them.
741.3-790 - p:rever diorite than
nrevious - contfict alpnr; stringer zone
v.dth above. Hathnr mottled apnearanon
vnt.h t.hfi hi ^ h fplr^npqr rnrit.^nt. , On'ly ^
pt."pj n^'^rs her^ — ^'Tiiitj© nu^rti?— c3.rbonntGi.^, - - .- j ^ ---,- ,. ^ -, - ,^ with very minor sulohides:- 764.8, 778.2
and 7o3.
ra TD OP TTOLT!
fifrk K . CWo/rtrft/HOLLINGER HIKES LIMITED
TIMMINS, ONTARIO
CORE SAMPLES
FROM
720
725
7^0
7^9.735
737
740742
745
760764
765
768
770771775
777779788
TO
7?-5
730732735.737
740
74274 fi7^n
764765
768770771775777779780789
HECOV. WIDTH
5
*5
•y
l
2
3
2
3
r.
41
32142
2
1
1
ASSAY jDESCRIPTION OF SAMPLE
LI - traces of py no CTJ
" ninor qt.K, n-inor -y po
tt it H n-i ^n-r -v rio r- r:
" SO 5, " t r . py C^
" 30 j ; t rr.ino:V-y no cri
" 20 .r " rrp nor -'V "'j c^
" minor !t " py oo c ~)
'.L nfiglSf- 'sulph or qtc
it tt it ir it
LI mass, (slightly magnetic)fl/L mass., 1" str. 1" 20O to C.A.-
bordered by heavy black tourma line with minor cp throughout.
Mass LI - minor py @ 300 to C. A. {magnetic).
Slightly min. - qtz Xi w. small tourmaline strs. -w. cp 6: py (ra^ndi
••lass. alt. LI with py fc cp (magnetic )
Coarse grained LI massive ̂
Coarse gr. LI - slightly min.1" green qtz str 200 to,.C.A.. cp * py, shear plain @ lo0 to fi. A.
3tz diorite - chloritic and pyritic (magnetic)
2n qtz calcite str. in an un- mineralized diorite.
NORTH EAST. — ELEV. - AZIM. — DIP.. .
DIAMOND DRILL REPORT
PROPERTY-
HOLE NO.
COMMENCED FINISHED PURPOSE OF- HOLE-——^
A -14 -73
Ashnore
FROM
r*U
G -r T3
Gr, * T.--i
G
G H- T3
G
G -i- T3
rt 4- V:"!
GG * T3
G
G -t- T3
G
G v T S
r.
G * T 3
G
G -i- T S
G
G i m ^ v i o
TO
126
150
.175
?nn225
250
2?5
. 300..,.
3?5•3.f.n
375400
425
450475500
r,2 r,
550
.57.5
600
60S
62?
650
DESCRIPTION
Geochemistry and Thin Section
"emiskar.iinf conr/loraerate - biotitic
Ijiotitic conglomerate
; 'OT'n n,Ts.RTVP. spriinipnt. - nrkosfi? .
it
11
li
" 'ara n rkpRir: pnrt of r.rr.ri.it.a on
Coarse, conglomerate
Finer conglomerate
Dark rrev arkose
^rkose vi t h a few dark f r arpent s
Gorij^lonerate, blue trey pebbles
f,.5r': r rny non^ lorisrptft
flrnv'T oi •-•.Pi'fll'.n - fpvj pphViTpR - avkoRT^ mnt.^ J
Conf lornerate - more hirhly altered --- py
Oonflornerate - e-revish
nnnf;1 nr^pr?it,p. - rinTp arko.oic nat.rix
To Dr. Koddle - rabbro?
Grev crfiRn arkoss
' :uite hlshly altered diorite, py cp
CORE SAMPLES
FROM
X
1
TO RECOV. WIDTH
*
ASSAYDESCRIPTION OF SAMPLC
FORM SZ2
NORTH EAST. — ELEV. - AZIM. — DIP———
DIAMOND DRILL REPORT
PROPERTY- •JILSOII OI-TIQi: :''
HOLE NO.COMMENCED. FINISHED- PURPOSE OF-HOLE——————
A-i;,-73
Ashnorc Twp
FROM
G
G H- TS
G
n v T3r.
G -i- T3
TO
675
700
72^
750
775
790
DESCRIPTION
Geochemistry and Thin Section
Diorite with hirh feldspar content
Diorite - RONR ny
^io'n'1'.p' ~ r ^ }-\p p'T^/^Tn^d v7 "*^"n ^u-'^rt-E
Greenish diorite - aoiiie po
Greyish biotitic dioriteH 11 H
.
CORE SAMPLES
FROM TO RECOV. WIDTH
*
ASSAYDESCRIPTION Of SAMPLE
KENOGAMISIS
LAKE
0 + 00 B.L
L
AST.
CL
I-
(T 10
~ l mi
iflUJNGER MINES LIMITED x 11WHS, ONTARIO
WILSON OPTION No l
ASHMORE TWP
Scale : l "s lOOO'
16 ASHMORE200