a^^^^^e^ :^r -' -; . v:• ; .' i ... · tivo winter r^ ' uio ... circulating tho ca...
TRANSCRIPT
a^^^^^e^ :^r -'yt*i 'ii- 1 ' ' . • ; .'.... :--.;-'.'--: •••' :- ' -mm- ? - ; v: i; ': - . •-- ; -ppi".- IpF
a,^*: '-j-..Xf-.'. ;...-. -
PROJECTS UNIl
HYMAN
RECEIVEDMAR l - W 7
MINING UNDS SECTION
010
K.-:R:* ADD] SUM MlNrii? l.JM3T.-:i)
A.SBK.'jr^.-L'IT I/OIIK KKl'tHCI'
-.rOMTKR JO'IMT VKTITUK!-: - ! KO.lXOT "0.0.2"
. J. !linr-o, J. P. ^'o^lor iv.bru:-!-y ?.977
••it :
Combined radon gus and scintillometer surveyo wore conducted by.
Kerr Addison Minos Limited over a group oi' 9 clpjirj hold jointly with
Max Exploration Incorporated in Hyman Town::hlj^ District or i'u-.'.bury.
The purpose of those surveys won to locate urnii.uim hunrJnj oJ ! ;;'-niotic
con glomerate-r. similar tt; those in thy otxh-vly o^'jr.tJ,
production at Aynow Lake Mine which lacy tm nbncumd by
Hight anal], radon cu3 unJ three rn-inl: l..loritttor . uoni.l; . :-.
encountered. There v.?.c no correlation but'.;')'jn tliu tuo : :u:-vi.y;:. Th,,
r:uion f '}tis ttnoir.yll en :-;ro l ikely due to ovfU'bui'dc:: i .-/Toe: t, G jv.tJi-,. t!,.- n \ )i:^~
rock c or.cc;:trat.iyi:r. o l" r r. d i o;, c 1 to v^j n^nor.-.l::.
'•:
-y oP
.. . ' . .Kerr Addison Mines Limited and A'nsx ^xploraUon Incorporated
jointly, hold a total of 9 claims in Hyinnn Township, adjoining tho
boundary botvoon Hyman end Porter Townships, iM.strict of JJiidbuvy. Tho
urtiniiur. iTiinoraliaation ])Ot(?ntJal of the property w. r. .'!:-.:je.?:-:od by X (j r r
Addison Nines Limited in' tho fall of 1976 with n p ro[;rw::no of I.inu-
cuttins, radon cos tind ocintJ llometor .-survey r? . Thi.'j work
oi^ht distinct radon sas nnd thrco .-u;Jj U.L:...,iui/-. /tno:!i;-J ^ -;r:.
The :;ubcliv'i:uon for thin pnrt of !:y.-!ij,n T(v,;nr'lii;: \:!uro
clainr. 1:1 o Jiua boon urmullod. Tlv.; projKM-l.y i;-'!::;: ;jt.;
'r;; r roximatcly
to
'ii/.TJC!; A:;. i AI;-:.-;;."
1'ov.iirhip, 3//, r. i l -.5
: r: o . lir; to
tivo winter r^
' Uio juiict-- :; Mf ,'nr,;* r ir hi( t. -r '?
r c L' til j l'-""; vty.
' : 5 pi'fjv'. 1 '. - ' * i." : t! i rt yfvi ' -'-;'' - ;. u'.lr '.v '. '.'r-' t
jjo.'i-jiVd'.j by vr;i.n; td) i';;rv! i-r/ r"--: ;":-: ; : M - ; 1
^^ttftig^'K-^Y': y-.'.-Y- 'Y' -;Y -'Y.'--. ' ."
2..
.,. ....^.^..^V:.-^.
' '17-'bridges; the Spanish Kiver. This road onds at
jy snowmachjno to reach the property.
Y'V '•..'.
l
; ;/ V" ; " Hy^an Township has been extensively prospected for uranium' ', . ; - -. ;. - - . - , . .' ^ '' - ' :. . . - :
^','Y-Y ' during tho uraniuio rushes of tho oarly 1950's and lato 1960's, especially,- '- '' ' ' - '
following the discovery of tho Agnew Lake Kino dcpon.it. Tho property li.v.s
been drj.llod at least oneo in an attorapt to locate additional uraniiua
boai'ing eonglcmerates. In 1969, Bronlan Reef Hine^ J.imiied put down four
holes totalling 1880 foot in tho area presently covered by clam no.
S461102. Ho radioactivity or assayo were roportod i!i the euro Jo;;;; (on
f i lo Pt tho Resident Geologist'.'; Kilos, District of I'udbury). i,.n (-;rt,:-
pebbli'3 wore only noted :In one hole, in n ;?A foot ui'.ie bod of .-,mjrt-.-..i t,c-.
Ile other work hss bo-an rccorciod at tho Kesidojit fJeolo^lBt 1 :; offico ir.
::'-udbu:-y on this property.
..^ r.! p t ".on
Tlio oldest roc]:s in tho area ,-jro mcLr-vo •lc.Miic:;. Thv.1 :; r:'.
iutnided by granitic rooks of lato l.roho:.;n •."•/.'•. i:vor!;'in;- thr: ...r 'i ; :-
iiuroninn
in fcju.lt or Mr)^
rcclu? (
(pt J;,r
rocks nuiKo up thiu pt.rt of tho sequence. V-.) Li:;u..: n :: o i'
or :r;f;y not tie jm-JAiok;'.! anJ arc ua;i;]y CCII['U'::.M.'. w ; .i; nv;
g/ibbroic intruDlour that v/ore -jr/^ac^d ;J.on;; b-u: :'. 1:5; v
ir.ionto. All of tho abovu ;a-o cut by at l.?,-i.'ji, n::-: :...-t
dykes.
hi r. L fj^:', .-j:..; . ..-.;;
h- t , •.•A \r:-.--: \} : ^-- ; : ---' : ••.- •
:: ' ; M;-
t-.-i- ci r.!i?-:-.:.-
-.r -- - - .
Pleistocene tills and glaciofluvial
plains in tho claim group. Tlu-sc
fluvial sando end
sFbi
Fk
;-V': ; ,:-.hs^:d';b!ceh partially reworked by ;;treams to form J
i; ; ; ;vV'. . ; Tirae-stratigraphic nomenclature used for Huronian sediments :n
: : ; :':;^; - -the-Blind^River-lClliot LaJco uranium camp i B difficult to apply to tho
Hyman .Township area, duo to incomplete mapping between tho two area.0, and
; : - the"stmetural-'complexity of tho huronian .'sequence in and around Hyman-V .' •'•' -- '. : " ' '' ;'-''' ' :" '"' - '
Township. Nevortholesu, porno correlations have boon attempted
and Lalonde (1973) placed the Agnow Lako hine deposit in the 5-'.
Formation, while Robertson (1976) puto it in the Katinenda
fxlnce tho fniartxltes of the project appear to overlie ar^'.llacooiu1. ;:
. (KcK.1jn For:nfttion'?) and a polymictic confjloireraLo with a nuarUitc J-.atriy.*
(ftav.roy L".!:o Fonnotion?), it nay be that tiny are part of the l--A.-^j :-.:MJ^'
Formation (ace Card, 1965, Kt^n
LL
Th.e I'.Hrr-yjiiajc-rortor elcin ^roup .Hor; • ••:\ t lio {-.outh. l:::-;) o;' i -
northoast trending tinticlinu that cut? ai'ro.-j.; tb.o con'.rc nj' hiyn.-.r. 7r-.:n:;h.1;
Cs?o Card, 1965, Map 2055). Tin J!ur-o)i:ian !:'-;trf.:-. d:!r.^ntri:-; r roc!';- d'::
eply t-o the :?outh, and arc cut by n nv^ho- i..f r.cTll:o,-i:-.t t! 1 '-'--•.::;:; i';-u:;j ,
r fouitr. a r o oriented in a northv.-unt •Ji.-oc-i/.'-.n.*
CJ J'^JinniQ. (ViolQfry ',
Uranium ani thorium mjuoraliiv.l'n--i! ocf-u:-:: ^n ci:' f;::r.:; ' L.': c ".-.-r.-
and arkose s rioar1 tho bam of tho lin r o: r'1 (jr. :v,;ra;r;v:o. At /."r.oi:
J.lne, thons havo fcrnod a doporsit c:::,i:^L--i l r ' \;f i jl-O'/,.: 1 tc;:r
2.10 Ibtr/tcn UjjOg p.lun an additicin.vJ /;.,X.OC),(H)G t.-.m:; -ivcr; i;' v ;^
1,53 Ibs/ton U^Og (tho Northern I'-nor, Oct. .If,, 1975). -noth-r 1,.'00,C.'^
tons with an avsra^o ^rado of ^./f7 Ibr/ton U-^V, 3 i or; o r. aOjoi nir^ ;.;x^er'.
"*' Mn.'
:r '- - .
od 1 o:: '•sr.i.r'.'.V^
r.-. ):-ur.v To-.Ticln p lo liio
'..;.^®f
t
}-.vv
^
I
Jt) l.i'v.' out t.; M;; :srv.! oh't.i n..i ".^
b) "adon ^ c purv-r;
c) o!j,! Tit:ii:ion.'t:r uurvv/
V'..' 1 :' ;; -.-:-;
6. f ni ' .j;;
A brro .!.i;K^ i.-.-i,'; o o t."i)J. ; ::lv:'l J s .-i r. -;- 1 .- •••:;. l. : ' ;---- ' MV , b.-;;ii". '
-.t li; : !u:::.b:.:- tiirco f*-- - :l ( .:':\:l\i\i'.-"-t o o.-\'-. -'*) - r' .-i: -r ::,:. :'. '6'. !.' ;: . :i -y
iii;^:;' ,.-.?f(-; J-:t ;-'jr;.:-:;,v' '-i:):*; 1 ',o t!io !;:.y.'.: '.''". v'. .'.O! f l 'r,^ : j, 1. ..-v-. : .-. :!
::.;:.;.3 .•.••-•."•.•: V:t-.:l'! by '.: .v i; -.:'.r'.". i rj; ^.n-.: ohaj ;i.i v :. i''.? M -- r:: 1 fl'n.: "-' -v \ V" :
r. t 1C'' i'.vr'
:v ' "v^
"ho radon
v.r5 th r;., ion ij; i:n\''.
and r. a:. v\-r ;-V h'? :-- ; :.' .-r.'' :.
-r, i: -:- /,-:'.;:-(.' : i y •'.-.\. - 1 ' ; :
1 - : " -.:'-: "': '' .;..." t:. :-: - \ 'r.Th: toc
.!',!? o d inl? Ohiv.drj In \ ')d", by Ih-; '.V^i.1 :. ;' • •••, ; u:-v-;'
as -K! on tn - r'' ;;' ; : - ! ,'..-,-
::'.norc,v ^i' Canada loj::Hed, in (.•c.-civova^:: 1 : 1. '.' : Lrs t. 1 : J,;.,'..
Radon -^an consist:; nuiuly or l"o i ::ot-:, .:; : : H
lUidon ;^?0, The former i c tho :;i.-:th m^-nbcr or ^ivj '
of Uraniim ?38. With a half lifo o?: 3-8,? days, -It,
"h
emission to Polonium ?,18. Radon .'i 20 iy l.ho flfLh n-;:-'b;:r o:' tin-
.'^v -.vi
-i^-v. ::- :
by nJj.ha
'-
•'. -- :-
JVA -- s.'^-v';, .!. v. - . . . ' ' 5..
'-j 1'
^f . : ' disintegration series of Thorium 232, which decays wjth a half Ljfo of
54-5 seconds by alpha emission to I'o Ionium 2.16.
. . The RU200 ia a scintillometer that detects ;nid counts nlphu
: ' particles over n pre-set period of ono minute ;;o that it j B possible to
detect radiation .source:; obscured by overburden. The operation of the
11U200 is rapid and easy, requiring that overburden bc present to t r tip•.
soil jar? at or bolow the humus cover. 'Die method involves au^orh:^ u
hole into the noil, inserting a ho!3ov/ probe, and by moans of a. bulb
pump, circulating tho ca " hack into an alph?'.-r.-::n:.;ltivo :dno suJrhaU-
coll. Th!i; ce3J. 1,-v coupled vtith tho scintillometer that counts the
alpha pur t; c] co detected in ono ir.inuto.
Radon gar. roridir.^ voro spaced 100 foot ic.-r.rt :J.on^
-1. ;no3. V/her-; a rending er.eeeyed 100 count:; nor -..liinrte over
o second reci-linrj \ i;i:- taken at n. y.i foot jntorvul, Tor onomall or. L,r-.-r)V;r-
tLan 250 q .'M over background, three conr.ee\itivo ono riAnuto rn.vlin^s e f
'ho rr:-? ;;--;"jO.'j v;oro t?.i!:en, and tho v^te of decay of the radioactive
r: our c c rotc^i. In this manner, a uranricr.i ;;ourcc CPU "ne d! f f crerar tod
fron u thoriun r.ource, on the b;u:is of tho.lr rer:poctivo .1 oncer and rhortcr
h::J f lives.*
Tho advantage of the radon ;--.a teahniouo over ]ir:-vio-J::ly'u-o'-*
^'kd hotter raovn ^p^rna-ray f;e?^nr and ;;irint.i.llo.T;eter rurveya i.7 that
rayr, aaccciatod with the decay of Uranium, Thorium and )'otc:r;r;.u' n.
are or.i si.].y Masketl l-,y overburden, and thor-oforu only c-.ffoc-t.lve
en bos'rGC'k o:pc;nireo. Thor o are alro n p.ur.ber o-' d:; r ulva-ita^":- to tho
method. !v?adin^s earnot be tyken v;hcro rro'.l ir; thin (lens than six
.Inchon) or when the raider is unable to pen-.-Uvite into th-j crounri (for
, Vuldor-rick tills, talus r.lopcs). Alr;o, if the soil is v/ot,
- '
tho wet earth likely indicates
'vhieh establishes reducing conditions in tho coil.
Uran^x , 'which';J.s:;Vfater soluble under oxidising conditions, is then able^.'W''}:,;:'-':/' l:'''.^-' ;.\S. : '.' - ' -tb'p'roOjlpJtsy very closs to tho snrfr.ce. A sample taken in this situation. r'''"-'-.''": 1 , ;v '.v'"; -' ' ,': '. : 'i - ' -
would fdvo'jni'ctriom; lour, high reading, which would not at all reflect bod-
rock aeeu-nuUi.vions'-of radioactive ninoruls. Thr- type and thickness of
ir '
P- 11 'by.
:;oll etui nlso; Influence tho strength of tho radon ^as rcsj;on,'jo.
Tioabla c'lay layers will tond to mask bedrock effects, us the soil- .. . ' ; '-'".'. - .' ''' ~-ci-nnot ceoarjp into hj (;hor •lc.val:; :hi the ovorlv.M-d'..-n, Housings In area:; of
lacustrine cloys vill bo low. Anotlvji- po:j::ibii! ity oxists whereby f;
hole .13 moored throne^ n c loy or hrrdpun l.-iyc-r \ :)i:-.ro rndc'ii r :".; h^r;
causing a higii ro."dlr.j volntivo lo l,hor--c; re;;d1n?,;f; t.".'--..n ;n
not nocen:i!; rily rc-present-itive of th.-: i;n;:erly'i!v- Ivdroch.
radon c-3 'inonrJjcs wore ej!:y.:uiit":-c:-.1. y*.1.1 but or:e of t);onc
!;V,e over :,CO fo-:t betv-on r.r.rvy 'Ino;- ( Lh-: •.••xcifr-Lio:: ;: i,::-:
.on,-3 John Creek m Ihi; s;vL r.!r-rn L'.'.nJvy -i' •:'l-:':: ;v. .''.'/..' 'J' : ,";
tho h- -;!i roc-Uivjs here ;-.;-j likely ti fri:;ci:io:: i-f \.v.-l .M!.:/! -r s.v ,. r:/" ly
the. crock rather than r-:.-io:.ictrve ;n.lnvral:^ in t!ri corj-o.LMi'.' d iA\l-; :v.!::t:.
bslow). ,'Jj.ricc these r'.ricin^lier; ;.rj In ?.,'Vx-l ;:-.!'"'.. ;;r,uri:uv in ; ri ;\v :-. o/
thick can.' aecv;::ulat,U;::, !,::ey ai'o pvobr.bly ir i .h;.: t^ u:':::..!v:". ':: 1"..•*
bedrock.
n?t
A
Ur;.'ni'im, .I'iior'u"; r.nd l o!.-:::' '.'i- i .
a visutl roadr'it of radiooct' v; .i n'. :r
count:! per ncjcond. '^risr-ion '••f.o;v;.y (
volts, :'ov.) for unstable o'l.-::n-:ntR of
-r' ?.v:;;..r----.
.v;-.-'Mi r r n
;- :r-'. -.r; :'
f./:'i '.: ; :,h '.':, -!:r--
,; t.l-.ir v/i.:-.---.:,
.Ir: .Mr;.'.,;-...: , : -
,-,i'r •'."'.••t" ; " f' 1.' "V-'."'
fc ".
f'V. :- ^ :",:;/:;{ r-:Votass3iini '/;0 (daughter product of Fotaormin: ^0) 1.46 Kev.
fh^; : L: ;: 'V ;' Bisrmith 2H (daughter product of Uranhim W S) 0 .608-2.44 Mev.
'a V Thaliun; ;?2;? (daughter product of Thorium W ) 0 .277-2.62 Kov.
r---.
•••••
,^: ;
Enerjjy roiiponso of the Kxj).loraniui:i GllS-101 pcrtnblo
scintillonoter uaod in thin survey in to totaJ. countu (aJ..I. o.nor'n.or.: .--bove
0.05 Kev.). Tho cryrUd detector of the GHS-101 lo 1.25" dl.onotor by l".
The {ic.int3lloir.ot.cr survey war, dono at tho samo timo o:-, the
radon gus survey. Tho instalment way held lit waist hoicht for ocich
reading, and Jcept on continually during each day's work.
Advantages of a pcinti Homo-tor ::urvuy .-TO: a;; y od tavl o.vso of
operation; and it i s ideal for uoo an urea;.; ci' btu'o rot:l: or vor;- Mi i ri
overburden. It is not. ur.oful where th.ieh oviu-burdon conc'\-xl:; i) -d-rci-,*
an this; masks ga'ruria-ray radiation from tho radioactive; souivror.. /'J::o,
It doer, not difi'erontu-.tf the sources it dotoctn.
Only fo\ir reudinyo rosa 3i{jnifjcant'iy nliovo tin; bivn^rourv.l of
25 cps on the project (a reading was oon:;:id.-rcd iii^li if /..t Iwusi. t-.'Jco
tho background count; the: highest reading cncountorod w.-;.u 6;-: ci-.:;;. A3.i
of tho highs occurod north of the base linu, on Lino 3.6i 1) (Si') .-oicl L.i sn
202 (3.6N, 1?N, 2^1)). Thi3 in an aroa of outcro]), mr.npcd by K. J). Card
of tho Ontfii'io Department of Kinos aa ••iuart-i.to;;, ni-horjo and f;roy\;;ic'-o*
(see Card, 1965, Hap 2055). '-'Such rolatJvoBy vie.ik rending JndJcute ;j l ow
radioactive? mineral content for theno rocko, which in likely true nlnoi '
for tho bedrock concealed by unconsolidated sediment;;. Since no radon
gas'readings vero possible) on tho outcrop, thoro in no correlation with'.
the 3c;.ntillonioter survey.
" : """•'"^" -" " : : :; v -' --JVv^x.'';:- '.•.-.'.'•; '.'••"•- ' - ' - ' .---
±m
-
.:
:\ - ."5; .-u-'ve;- o;:-:-.''.:* x si--::- - - . .- -
:;: \: either thlc5: d of ;:.v.:r. 1 or in w::', -rounit: f.r.-in-.y 1 v , -
. -' not ncccaijarjly jood ttu'^ot:-. for -Juv*.:'
:
. ' no .-correlation betu'.;o;i tho n \;u.ir. . ;: i; - w i -.i-: i .? f J .1 /.o,'..-:-Uir survey;:, :
; 'tho Kcintillonioter Ir^hr .-c:-\!V(^:! ovy bfd'^'t.']'. ;(!-.:tM roll vrr; non-
oxj strii'.t.. A dot: : J.lcui .•"•colo^ic.''.'. survey i;; ••o^fir""nv.! f i-iii ' 'o? tJi.^ ;'-J.;-'.
project to doi(?rnJno tho vo;; 1-'. t,;:'o;- v.n!t;u:it ;.uJ 1C oo:;.".) i,1 ! ' ••:;.'.i ;T:
t!ieri to foi"jn."J. tino-strut.i. ;.-;:;-}jic ur.it::. '
-. v -,
J. ir
/1/tS (^ Mlt^t*
' " .' :'. ''/-•'.•.,- : -;. - : :--:-'' : '''-.-^ •;:;'...- :- . ••••.'-:--.'-;-.v. .', \-!i--.^-:-v ' •../•..••;i:;.'•••'-.••;--..: -,^;;.-,J ;,;-':-.. . ../v , : V.'-v; ::;', ^.-;.,
-•'' i".".t
... ...•' ' - •'••'' ! ' •'-"-'-'- ••' *'-'
*mmm^*mm^^'^ •w^-w- :^:' : - •^.^•^^•^^w'x--:.;.''Si"';'.'•yv-\C • -•f''.''.'.": ' : ' ..'•;' . ' •-' ."'' •''••"- .- " -'•••••'••' ,' ' -. - '- - ' - -. . '- "' ." ' . .'••-.'
'•7.-y'-/';'. f-".\V •*'-'.'; : '- ''-iri.'-'1. ; : - : . "' '.., ' " ' ' '
'own R hip,
d Drury Tovnisblpy, iH.;tr.:ot of i-'u''il)HT7, . Mines Cool. Hopt. Ho. 3/,, 3^. Accf.wwtdod bv
...ihc:^ iKr^r, Tag ; ' '.- ' .'.
i-'..-
lK;-
: Otto IK-.- A 6,
r!." ^.••,•. J. A. ' ''I0 ';6: The Blind r-iveiv nrzuiiv.n dwoivilri: ^.:io oro:; nrvl the'.f
vl o Di.Y. i:i!v-r^ l-TC'j, /: ^).
.'i''-
K.':- A,'...'. '--
'•.'•'•\ A-'-'-V ?Vy/. - '' t/" A i ""^. ';:^v V "••'••'. ' ' ' '' - ' ' " " "- - ; '. -' ":'" -- ' '- ' * ' - - ' ' ' ' - ;- - ' ' ' ~ ' -.' - 1 ";."' -M- ; ; - ; ;"-r' -V':..V:~ '"V^U'"'*-'ff"^^^^i;; -; -. -; AJ^TRACT i -- :-. ••-.;^;,.-;:-'. .-••^s^-pr-.^;^•^•^^^S&lS'-v^"'''.'-''" D isintegration Sc'h* vj Tkoriifiu ~ /.-^ : ' '•"'^vS"•'"' /A- ''X ;-.,"•".-^"' -. '.•''''""••'-; :-'J : v..-v;"'. -" - ' ' ' ; . : - .- ' - ' * . ' '- ' . .' " '"-..."••.mmmm^ ••••a*-r,**~*- , : . ^^^•••^j -,, : " -. - -. ' -. -j' . ..'. .'. ' ., "- -'i - ' - . ' -
i' ' '. - . ' '^ "' - - . . . ,- - -.•".." ' ' . . - ' ' - '
\ "
Kniliuni 2.!S !0.7yj
;:.j ' ~.•^":"
l::' ~*
^
ft-
fe.v:^••" -'-
n
x
IV.!i.i;io'n l'l'J !:U! X Id V;
•r \
A. H. J,:;),-, J. lv. c; l . i .. :-j o ;
•v
1 ,". ' *. ^ ' -- ' ' - ' -^ '"' , '-'' -'- 4. ..-'' -' : '.'. ', • -* :' ' -..'' -
' ' "•'-!.''.
,:.-.:'- ;;,':: :;:'.* ''' -
V~t..S.tfV:--;:;.,-;* ,,'-,. .. - omitUM) . .;-r ' i'-;- ---f - , . ' - ' --'' - - -1^#-P ; ;: ::K: -' v '----:v:--: :-'-\^.•i',;.yV:- ; ••"••'"',' : ' ••• : - :.
•??:.-.' '1 ^-
.?v' l,,.;J;/- - .'
* *."
Series P/Wriir.ium 238.: c'jiislitDlmr, K'.is llmii 0.^ per cent of the decay jirodii .s W:
Uiunuiiii'!:)!'1' 1-1-11 X lO'.v]
! fti " ii ni i
i
i.'uuiimii v:ji l:, is x I'l'y! l ! al
Thojiii'ii '.'.(O 1S.O X Id'' ,t i x
ll u l
.!i v..-..! ! ii "'i
I'c
i l
'.M i I
l .i f 1
I 1.!-:;,'*',!. VH
li*
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|p;-5 Ontario
atural Resources 900
. __OGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT RECEIVED
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION,
AUG O - 1977
LANDS SECTION
gw
8Flu.
Type of Survcy(s). Township or Area. Claim Holdcr(s)—
gas surveyHmnn Tovnahi
-Inax Exploration Ino.1302-7 King St. East, Toronto, Ont. M5C 1A2
Survey Company_____Korr ArlrHson Mlnqn Mmitod———-——,
Author of Report. G. J. Hinsa
of Author Boy 1788, Espanola, Ontario POP 1COCovering Dates of Survcy-
Total Miles of Line Cut —.
Nov. 7. 1976 * Jan. A. 1977.(Incoming to office)
_______8.4__________
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.
ENTER 20 days for each additional survey using same grid.
DAYS, per claim
lysical
--Electromagnetic—————-Magnetometer———.——
-Radiometric————————-Oih,-r Radon Gas ZO
AIRBORNE CREDITS (Special provision credit! do not apply to airborne lurveyi)
.Electromagnetic. .Radiometric
^
(enter dayi per daim)
Author of Report or Agent
u. o . Hinse
Of '
Previous Surveys File No. Type Date Claim IJolder
MINING CLAIMS TRAVERSED List numerically
(prefix)s
(number)
S 461102
461103
461104
46112Q
461121
461122
TOTAL CLAIMS.
GEOPHYSICAL TECHNICAL DATA
— If more than one survey, specify data for i-.tch type of suwy
.Number of Readings
.Line spacing
Contour interval L ff) eonnta par admit*
376
u*M
fc ^C
Instrument.Accuracy ~ Scale constant, Diurnal cone c t ion method.Base Station check-in interval (hours). Base Station location and value ~——.
Hk
Instrument .—-— Coil configuration Coil separation m Accuracy .——— Method: Q Fixed iransmiltcr CD Shoot back D In line
'•4, Frequency.(iptcify V.L.f. union)
Parameters measured.
D Parallel line
Instrument,Scale constantCorrections made.
Base station value and location ..
Elevation accuracy.
Instrument2",^v *s
H
Q u;
Method D Time Domain Parameters - On time ——,;; : 1 -i; H -Off time,——
if.l~i, v 'fy{'5'. — Integration time. ir PftWM-V''.' ——————————
Electrode array.
^v- :Type ttf Electrode
D Frequency Domain _ Frequency ____ _ Range_______
milpm**^® S&^w^^m® ^^^•^;ii?j:^^^:\V'--:-^--%^'v';;:-^:^:- . ; V^.-:- : :;:;:
••,-A^v
l ES?^-,; -S/:;
POTENTIAL
•Instrument. Range.Survey Method.'
Corrections made.
RADIOMETRIC
Instrument.Values measured.Energy windows (levels). Height of instrument__ Size of detector_____
.Background Count.
Overburden.{type, depth - include outcrop map)
OTHKRS (SEISMIC, DRILL WELL LOGGING ETC.)
Type of survey_______________Radon Gas Survey——-——
Instrument ____ Portable radon detector. Modal RD-20QAccuracy.Parameters Decay products of UrArdiim gffi and
220 regpectivoly) .
Additional information (for understanding results) — Radon gas maasurad in counts par mi'iite.
AIR BORN K SURVEYS
Type of survcy(s) ——— Inslrumcnt(s) ,—————
Accuracy,^—-————.
Aircraft used.Sensor altitude.
(ipccify for each type of survey)
(ipedfy for each type of survey)
p-PP::,.ki-Ate
Navigation and flight path recovery method.
Aircraft altitude.Miles flown over total area.
l An f Sparing,
.Over claims only.
OFFICE USE ONLY
Ministry of Natural Resources
GEOPHYSICAL - GEOLOGICAL -TECHNICAL DATA STATEMENT
RECEIVEDAUG 0 - 1977
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.UNDS SECTION
Type of Survcy(s). Township or Area. Claim Holdcr(s)_
ScintillometerHyman Township
.ftpax Exploration, Ino.13C2-7 King St, East. Toronto, Ont. M5C 1A2
Survey Company____Kerr Addlnon Mines Limited _____ _G.. J t Hinge—————-..^^———.-...Author of Report —
Address of Author. Box 1788. Espanola. Ontario POP 1COCovering Dates of Survey_Hny, 7, 1976 - Jan. L , 1 977
(linecutting to office)
Total Miles of Line Cut. 8.
SPECIAL PRO VISION'S CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.
Geophysical-- Electromagnetic—
-Magnetometer-—.-Radiometric—2Q.-Other.——————
DAYS per cliim
AIRBORNE CREDITS (Special provision crediti do not apply to airborne turveyi)
Magnetometer .Electromagnetic. . Radiometric(enter days per claim)
Author of Report or Agenl
Res. Gcol... .Qualifications.Previous Surveys
File No. Type Date
tt. J. tiinse
^. / (f 6 2
Claim Holder
MINING CI AIMS TRAVERSED List numerically
.S....,...............AfcUQQ,(prefix)
s(number)
461102
^61 103
461104
461120
TOTAL CLAIMS.
GEOPHYSICAL TECHNICAL DATA
STJ- If more than one survey, specify da'.a I'm rarh type o! sutu-y
463_____________Number of Readings .Line spacing,_____
385
.- Accuracy '^ Scale constant.Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ——™
'..J'
.3
InstrumentCoil confi^tiralion
Coil !,q,;iialioii —
Accuracy —————Method:Frcqu en cy ——.—
D Fixed transmitter D Shoot hack D In line Q I'aralH line
(ipetify V.I.. f . lUlion)
Parameters measured.
InstrumentScilc constant
!:;l Corrections nude.'•r
Base stalidn value and lodiion —— — ^__,
Elevation accuracy.
Instrument ———-Method (~1 Time Domain Parameters — On time ———
- Off time
C'l Frequency Domain _ Frequency ______ Range___.—--—-
— Delay time————————————,————
— Integration time .. ————————__.
Power-.Electrode array ———— - Electrode spacing ——— Type of electrode ——.
POTENTIAL- . . . . .
|: * Instrument ——————————————————————————————————————— Range.- ; Survey Method - ____________ !'
Corrections made.
RADIOMETRIC
Values measured Total COUTVtn (all ffflftrgy abOYOEnergy windows (irvrU) KADi 1 .A6 Mev? Bi2Ut .606 to 2.U Kev; Th208; .277 to 2.62 Mev Height of instrument_________WaJBt Level__________Background Count 30 cps Size of fin prior Crystal 1.25 inch X 1 inch_____________________________ Overburden Varying thickness and lithology__________________________
(type, depth - include outcrop map)
OTMKRS (SEISMIC, DRILL WELL LOGGING ETC.)
Type of survey___—————————————————————————————— —————————————————————Instrument. Accuracy_Parameters measured.
l Additional information (for understanding results).
S SURVEYS
Type of survcy(s) Instrumcnt(s)
(ipecify for each type of lurvey)
Accuracy—..—..———.—————-—..—{specify for each type of turvcy)
Aircraft used-——,-————.,--—^^.—.—-——--—-.--—™-—.—-Sensor altitude.Navigation and flight path recovery method.
Aircraft altitude——————————————————————————:——Line Spacing—— Miles flown over total area———————————————————————Over claims only.
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