geohpys surv rpt - ontario
TRANSCRIPT
42AISSWTO29 63.1588 MANN 010
this r o port deals with 54 ttinin# olniine oorapos*
ing the oatit jwrt of thw Joiumith Kino** property in Mann Town**
whip. Thu pro pa rt y la oowposod of a ulngl* block of 94 claim*.
A report was previously submitted by the writer covoritvj th*
wt*st 40 claim group surveyed in t ho fall of 1964* Both survey*!
have includfltl gooniAftnotic anct oleotromajjnetic work. The' i ' '' ^ -' ' -
recent *urvoy was carried out in the aprinc of 1965* -v
A program of diamond drilling with the ufia of
two drilln i* proceeding on the K OB t part of t ho Joimmith
pt*rty at tlm time of writing.
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Tho cluiwtf oro in a Mirveyod Xownthi p divided
into lot" and coMcesftiona *nd tho clftima aro recorded in the
1'oroupin** Mining Wivieion AM follow* i ,,
Kos, f. 68494 - P.6B511 Inol. **.* 18P.68524 - I*.68S47 Inwl. ..., 24l*. 7164 3 - J', 71654 Inol. .... 12 Cl*iw*
Total 54
Tho ground o over od in this* report i* composed
of 54 deltas or 2,160 acron in the couth part of Hann Towtv-
ship, dimming Aroa, Ontario. The aooea* road to the
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II" """" 1111 """"""" III 42AI5SW0029 63.1588 MANN 010 ...
This rop,wt. deals wj,th S4 .tirJing ol.1m.oo"po.... '
inu tho naust. purt of' th~ JonaJ{4:lt.h MlnC!JM pf'operty in Mann fow~ ...
shir). 1.'h{, l,roi»trt)' i8 OO}t4posod of • "illg18 block of 94 ala! ...
A rtlport was proviouJily Hul)Jllitt.ed by tho writer COytJl'.tng the
west .$\1 olAiJal group blurv"ycd in U • ., full of 1964. (loth .urvCt,,8
ht'lVtfI inoluded «uomaanet.ic and oleotro"e"netio work. Th.
r8cent Burvoy waG carri(1d (mt ttl the .prins.! of 1965.
A fn'og.'.I1, of d i •• ond drit ling with the u •• or, two drill. t. prooeed,ill« on thu ..,ast part of the JOIl~ft\tth pro.'"
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Tho 01 ,d .• e , aro ir, a ~urv.Y',d 'folta.hip ~U.v.tcl.d,: r,'
into lot a Anfl C.H)UCOJitlidon,. .,ut, tho c1 ....... 0 reoorded in t". '
~08. f.68494 - P,68$11 lnol. P.6B524 - p.68547 Inul. J'.11643 - ",11654 blOl.
Total
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18 'Clai", " ,', 24 Clai_ 12 C~.:i ..
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Tho ground coverod :In thilil roport ,. oOfllH).ed
of S4 elL\ :tm~ or 2.160 Aor"a :1n the. eouth part orManD 'I'own.- .' " i
property is by vay of lli&hway 11 to a point 3 mi l os north
of Nellie Lake* Station. A buwh road from thi* point l o Ada
8 lutles weist to the property, During wet weather A ftwatsp
buggy i* required for transportation over thi* r i** d,
The ci ft i ins described in thit* report ara largely
pverburdened but aotae of tho geology may be clod weed from
mapping carried out on adjoining Jonswith ground to tho woat*
A gooloffical wnrvey ii^ currently in proems* during which it
i 6 h op*} d to locate any isolated rock outcropping^,
An u xit ra ino t ion of thu rook outcropping* near
bouuct/iry of thiv ulain group ion Lot 4 f C once&dion II,
tho prortouoo of poridotito tt IK! gabbro rockn intruding:
volcnnios compoiiod chiofjy of rhyolite* and rhyolite
Tha&e rook** firo part of tho general eaat~vo0t
' striking formation in thi* locality and the batt io and ultra
basic gabbro Ami peridotite are i*ill-lik** forfMtion* with a dip
to the north. While no uranite rook outcropping have been
found to date on th* 54 olttitna, it ie believed that A l a rue
granite aroa exists near tVie north boundary of the map area,
us evidanoett by gr&nita occurrence* in the northwest part
of the Jonsmlt h
• prOr)()rt)' 1. \», li.1 of Ulghway 11 to ••• oint 3 .dl"e north.
of Nolli. L.lw :.t,ltt j t?n. A bUHh road frolll th1_ point lOAd.
S auU(tl'li WCH~t to tJ)6 property. DLirintt 'Wet. weathor _ 8wallp
bu,ggy i" ro(~uJred for trflnaport.atlon over thia r')Ad,
'J'he 01 (l :hnw tlfu;ccribed in th:l~ report are largel y
Qvo"t1urdenecl but SOMe oj' tho f.le()lo~y may be ded\l.oed fro",
AI&I,ptn\~C)ifrricd (tut ()l\ adj oining JOfllJud,th ""(JluK! to the woat.
A &;ooloai(.:.al Imrvoy i,~ vurrent1.y in progre8" c1urin" whioh it
i. hupud to locot6 any iscllated rock outoroppin~la,
An axnrn1nt\tiou of thn rook ou~crop,')b,4C. no" .. tho
WtUtlt bound/lr)' ()f thit; u1a1 ... group isl Lot 4, .CQnoe ... io,.ll,
.. h",,,. ttw 1.)1"1:\1:1(,,:.00 of' l-'Oridot!to 4Ind g~bbro rocka.t'ltruclin,
Keewatin volcn.nio8 o()mpo~o.d chjetl.)' of rhyolite ant;! rh)'olite
a"~lo.eratu. 1·h<~l.e rocJ1< .. ANI p~J't of the «en.,. .. l •• et"",wo .. t "
I IJtrik.t.n~ ftlJ'Nation in tht. local it)' and the b •• to .Ad ultr.
ba.tc tl.bbl"o And rterittotito lire .. tIl-like tOI'lMt.tone ""tt.h • dip
t.o the north. Whi1., no Atrantte rook outcroppinit' haw b •• n
found to dftttl on tha 54 olIA1 .. , it .1. believed that. largo
"rEmite aroa exists nE:st" the nopth boundary of t.h •• Ip area, ...
lA_ ev.1dono.d by g'r", ... U,o OOCHll'roncoa in tho ,..ortlaw •• t part.
of the Jonsmit.h holclingft.
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drilling carried out during the pa B t few months In the w t? e t part of Joiwnith has a h own th* proaanco of feldspar porphyry dikott intruding the basic intrueivws and the *Kjftw*tin. The diaiaond drilling ha* nleo indicated that the widespread gabbro outcropping* on thfl woet part of tho property wwy be a flat capping over the underlying
Diamond drilling to date by Jojvfcmith on the wu*t of tho area described in this report h*u
concentrations of pyrrhotite, pyrite And graphite in rhyolite, rhyolite *jt(jlo*aor*te Amt rhyolite tuff*
Hinor amounts of chalcopyrite and aph*Xerito may be observed with thin anl phide minor*! iftfttioot
On iiurfaoe in the naiffhborhood of the drilling* outcrop*) fthow sulphide occurrence over widths up to 75 f**t trending owwi-wokt in rhyolite formation* The rhyolite show* three sotfc of jointinj;, one northo6ist-*outhwoiit^-one noutheaet* northwost, And one ny^ten of flat Jointing. The mtrfftoe *ul- phidea upp&ar to bo follo^vlnjf one or wore of theft* eye t on* of joint w, but (hoy are *il o included in a broad naohnnioal breooia in tha rhyolite, vrhioh arft outlined ae atrong electrokinetic oonduotora Atrikina eart-woftt for distanoos of approxiwately
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Month. in the W('Jo&;t part of "lon~ud . .th has fl,hc>wn the ),.0881100 of
feldlJpAr ~ ... orphfry dj.ko~ intruding tho ha8ic 1ntru • .tVCl8 And
tho j.~..,w .. t·in. 'J'b6 di81111)nd drill hIll has aloo imUoat..od thBt
t.ho "".td08()~oad gabl)ro outcroppinU8 (m th~ WGat part of t.ho
Ju~operty Ill"), be & flat. clippina over thf:t und.,.lying l(eowAtin
voloaniclt.
).!tU?/,Al.. p,C f'O;.', ,n'Ji
HiAlfl()ncl drilling t.o date by J'onl/mith on t·bo grc>ulld
.im:'tte:Uotely w".t of tht) arOB de61CJribed :in thts rftport .h.~
.holtn {.loooentrat1ona of pyrrhotite, pyrtto and nraphtt .. .in
fr~cttu--ed rh)'01 ite,rhyolft.o .,U(loaorate and rh),oltt. tuft~
~u..nor .IDOltuts or chRlcu(lyrite and .ph.l.rite, ."" be qb •• r".d
"tth th!" .. ttl f,hide PlinoN,l. .i •• tton.
On III.u'f~o. in the R(Ji,ghbol'hood of tho dril1I.n",·.
outo..,op. ah("" aulphid. (l()our.renoe over widths up to 1S t •• t ;
t..",end Lng ua~t~"'Wtu.t ill ,."y01 ite l'orIll4tton. tho rh,oltt. alun ... ' ',:
throe .ott.; of jointing, on". ftorthoatrJt .... ou thW •• tj·l one .otltb ••• t.
northwftst, And on~ aYli<toJ'J of '1 at jOinting. . Th,,:. surt_co .ttl
ptddea appeal" to he foIl 0\-.' JI1M one or NON or tho ••• ,..t.lI. of
joint 1;, hut thl'Y lU~" fllliO included in 4 broad -olunttoal b.-.oot.
in tht. rhyol1.to, whioh art! out.lifltld lUI .trOll" eleot"OJManet:l.o
o()ndl1otora "trikin({ ear-.t-wut.t. (01" d.f...,tano04 of appr()lftut.l,
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3,000 foot* A sulphide a one referred to as the "North Zone"
east into the wont boundary of the olaim yroup her* in
must i Vft eulphides ras y not bo obuerved on
surface, not** of l hw d lomond drill hole** such a* Ko* 2 have: " ; i 1
Bhown tnnfiftive mtlphide occurrence over core length* of SO foot
and this material haa aloo carried the most proiol*insc values
in ccppor, xinc ami w J Ivor*
Short **s!-ei*toi* fibre it abundantly developed
in sotno po ri dot i to outcrops near the west bounUary of the claim*
herein reported* Thu fibre /trade in unknown* The preaenv*
of a large draff fold i a indicated by the geophyftic* in the
northeast part of the Jom*mith holdinir* a* ahown by the geo*
mugnatio ftiap aOoot0p*nyih*! thint report* Thia condition could
he favorable to Miubeitto* fibre developtvent and the property
should be oonttiderttd an Aftbf**to* proftp^ot an *ell ae a baa* ; .
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a) Geomagnetic Survey
The gtfoMBrnotio survey ** aa oonduoted with a
A2 avtiMnetumoter uaint: a sensitivity of 20 gawwa* per1 , . '' ' ' r .
ttc&lo d ivision. This lino cutting grid ^ae laid out from
A base line extending oo*it*w at near the centre lin* of .
Conoecmion II f Hantt Township, and oroeeinjr tot* 4* 3y * *nd 1.
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3,000 teot. A ault.hide .one refer,...d to a. the "~orth lone"
.trike. eAst. into t,he ",oat hlHtnd.I'Y or tho olai .• g .. oup herein
.... ported.
ThOtlllh ""'8£d,ve .sulphides fIIay Dot be otjlJfu·yed on
8urtaoo, BOlj~ of t,lt ... dia.mond ('11'111 hole~ lI&uo"· a. No. 2 hove
"hown Jl'U'.IlIt.w ~\tlphi(10 ocourronoe ovor co,-. 10fl1Jth8 of' SO f.et
DPel ihis mat.orial haa Alo", cllrri.d t"$ .. oat prOidatns; valu~.
in o(Jppor, ~inc and aflver. , ,
ShOf't .l;Ihesto8 (JohN i. ahundantl, dev.loped
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.tn 80l.e f\0J'idotito oll"'oropa neor the weat houncJary ot t.b. ct.! ...
hereJ.n I'ftported. Tht, i'1.bre nrade i.a unknown. The pre,.noe
or II 1 •• "«6 drag told is indicatod b)' the' geophya:S.c. in t.he
ftot'thtUUlt purt of t.ho JOJUudth bold!,,"_ ••• howil byth. ,eo-. , ','
."gnatic ",AI' aOcuatl,),myihp. thJ.,. reptt .. t.. 1'hi. cond it-to" oo-.ld ,i
1,. t"Yofa'blo t.(J IwhodltQ& fibr. devolop_nt. and the prop.r')'
ah,ould he oon,.iiJerftd 8n Alsb"sto. pro".Hot. .IS ,.elt. ••• b ••• "
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a) Goomagnetio Suryey
"be gt:lt;Mlwnet.io .urvo), w .... oonduoted "ith • • :r _,~, ",
fU ..... po A2 .. ,unerto",,,",er lud.n£~ a •• najti".lty of 20 ,_.a. pt .. 1
.0410 divis.ion. The 11n~ cutting «rid ., •• 1.td out fro.
a baae IJ..u, extefld1n,; .""t.-W8at noar the aentre 1 iN 0'
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picket limK wer^ spacod 400 feet Apart and wtsr* cut
th from tho bane lino, with station* established every
100 feet* Throe thousand three hundred and t wen t y- a oven mag
netic stations* w tiro road njvl recorded* Accompanying this ro-
port iti a ^ ofijflunot io contour map on a *oale of 400 feet to
l inch*
Tho tivii'ence of Mi underlying rock etruoturo on
the tsa&t part of the Jontmith property htsrein reported, is bosciU
on a proJeotJion of the known rooks striking into thin
from the Wfjot, ami the t*osult4 of tho poomofinetio survey*
IU!Corii*i of diamond drilling and surface work on
the ground to th^ vent tihow an eft&t-wtt^t striking structure of'V ! :i
Keewatin formjotion, ohlwfly volcanics of rhyolite compofcition,
intruded by 3, a r f; e feill**like whoff-tif of peridotite ami gabbro t
Ihift fterieb of rocks dips to the north with evidence that ^
Hi* flip may be telite flat ot eomo looationn* '
' 1'he {?Gt}0iM."neticj survey over thi* known rook true*
tur* bthoHft tho j!ori*loiite to be highly faaKnetie outlinml by
A tti/if'iicMc Intensity oxcftodinj: 3*000 gammas. The gabbro i*
only mod or at el y lu^netio and is included in thw range of
1500 to ,3000 {Tnnuaue wharft it outcropn on surface, The ^Sie watin
rookft vhere they do not include tho wngnotic pyrrhotite
sulphide wineraliration, show o background reading of 1,000 to
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'l'he p:J,cket 1 in~;l6C we.ra 5JHlC6d 400 feet apAri And WtU"O cut
nColrtb"IH>llth from tho bal~G litH), with .tati(,M ost.bliahod every
100 feot. T'hroe tlH'Hlaand t.hroe hundr~d and l.wont)'-eovon Iuog
not,ie ttlt.aticmEl Wdro road 4uv1 rocordsd. Aocoltflflnyj.n{t thts " ....
port, is a. tta()Jnt\(!n~t.ic) cont.our Ina" on .. ~oMl. of' 40() teet to
1 inch.
''j'h(\ l."Ivic'ence oi' th~ nnd6rlyinf.! rock fltruot"I"" on .'.
the fH'~t pa.'t of the Jon.-.dt.h pr'c;;p0rty hllre:l.n r.vol't.~, ia ba ... d'
larl~~l)' on 3 p,"ojeoot.ltm of t.ho known ro(:ka atr:!lcing int.o this' ,
l,}·rNu).d frol!.l th~ 'iHWt. and the result. of thft Roomagnetiq aUI've)'." ,
nCU,lO,',:aa of dialVlOud dr.il 1 inu And 6urfllc. work on .'
. the PN)I.U)rl t<J U.~, WtH~t •• how all tU\6t-Wft4t et.riktJl{l 8t.ruciu.,.· 0' , . '. K6!ewlltill fm'mation, ohiotl y volcanics. of rhyol.1t.~ cCfmJu»,d.tioft,
. intruded by l.argo ,.tll ... like Qho«"t . ., of peridotite .BI)d.JabbI'O •.
'ht& aorie .. of rook. dip,. to th" nflrth with ."iclenQ. 'that
th~ dip ~a, h~ Quito flat at .umo looationa • ':,'. :,
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1'h(~ IlOtHtlarnot,icl hurvey over. tht6 known rock .t.rlI0';"·
t.uro t4i~ow* thu p" rtf'fntH.& to be hi·RhI, .. aunetiC) oHtl:lnMl by
A U14 f{rlet.iQ in(.onsity ox(.'(.~dinf.:' 3,000 g.lA""... The ,.bbro ,_
opl), modorat.ely JII..ug,netio l)rtt1 is inoludad tf' thft "An". ot
1500 to ,3000 nanulJl1S NhtJrf') it, out.or()p. on surfaoe, The AeewatiJi
rO(l.k~ \<d:wre the)' do not ind.ude tho mognot1c) p)Trhotlt.$
sulphide .>line-ral i~ation, .h~ .. a hackgrounrl reading 0' 1,000 to
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1*5^0 gammas. Tho^e areeft bo low 1500 ffamKftS are probftbly under**
lain by f; ran i to.
The geomagnetic survey has shown that the o ft ut part
of t ho Joniwith property le underlain by a large percentage of fairly highly Magnetic rocks, This would be an eastern ex tension of the peridotite And tfobbro will formations,
pcr-itlotitu lonow {ire indicated on thet onclosod
map* tin of t ho tt o is- located noar the? north rtd^ro of the ISM p ai i'*a oontlnninf ftorontJ Lote 4, 3 and 2 Jn an ** a w t* wu is t direction* In Lot l an abrupt 90 dogr*e turn in th^ mtrika of tho forwtvtion i*^ shown, remiltin^ in tho peridotite rook* showinji a north-south strike near tho oatiit boundary of tho ground at the Newmarket Townthlp boundary* Ina^naioh ae the peridotite
to be a will f orient ion it is nasuwed that a lar^* fold in tho Keewatin rooks at thin location with the axis of
tho fold striking nor t ho a o t at the northaafct cornet* of t hd map *r**a ih Lot l, Concos^ion III of Mann township* ' r/ r ^
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In addition to the Above peridotite lone 4 three other l o* w *)ttont:ivo highly sia^na tic areas in Lots 3, 3, and 4, Corvccasion II, arc intorproted as peridotite sill formation* Those Al*o w how aowe effect of the folding, adopting a trend to the sovitheott at their eantern extensions* Xhe peridotite
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tona* ara apparently eoparatod by' fairly extensive fabbro
occuiTonoo at surface bedrock,
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1,500 gaPUlleta. 'l'hOJi~f) area,. bolow 1 SOO g."'lIla. Are prob{\bly unclo~
la;l,n by 'fran! to.
th(~ C;ftC1m8(f,tHJt!C surv(t)' hAa shown th"t the .a~t Pll,-t
of t.hO' Jona6l!ttU. proJw.'rty 18 underl ain by a l.ar«o J'8J'centa r:_ of fair-I,. ht.«hly U18gnet1c ,·ock.. This 'Would be an 6 ... torn ea
t4.1Jlahm 01' the p~ridot1to f.nd gabbro tc111 formations. Thr ••
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jJ1'OmifU'Ult. pM'.htot.ito &OntlH are iodicI\t,ed on th" ftl101oIJod "eo
h1a«tl<~t1c awp. Ontlt of tJwliiio i& loo,at-ed noar t.lte' nt>l'th edB«' of
tho up 'AI l:,a J)ol1thminr. llioro,,"s Lot.s 4, 3 and 2 in an tttUi;t-W •• t
tHrootlul'. In Lot 1 An IAtlrupt 90 degree turn in t.hit _trike
of tho forr-u\tiQn it; a;hown, reattlttna :{,n tho peridotit.e rook. ".' !
ahow.tn~t a u1.)rth-ar)uth 8triko 116M" the oa.t boun(~nr)' ot tho ,round:"
at t.hl) NewAlfu-ket 'J'ownsh1.p bOlllldar)", Inatnmach ae the peridotite
ilia IUll1lUIIKtO to be It eill fo.·."t.ion Jt 18 ""'lulled thAt f\ 1.,. •• , told " "
,,>:tl$t8 tn thft K08k'Qtin "ol,ka at th1R loc.tion with t,h.,,fnrS.'ot
thCl fold etrUdug north~'a.,t At the Il(U~the.lVt oorner Or th~ '''P'
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In add Jt.f.on to t.he I1bo~. pertdot.lto .0"0, thr.',
ot,h." 16au .ktont:tvft h1"hly IIA&(nfttio .. roil • .tn Lot. a, J, .nd 4. Cooo6aa.i.on 1 r, aro J nt,orprtlted 48 Pfjrtdot.ite atl1for •• ttOQ. ,
ThuBo al~o ... how 801M') ttffQct or t.h~ folding, adopt.tng • t ... ad .'j
to th(l sout:.he£ut:;t at their eaJilt.ern ext,oMione. tho 'portdot.it.
&one$ arB aPl)llrBntly aopilratad by' fairly oxtone! •• gabbro
OCCUf'ronoe At 6urf ace bedt·ock.
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Probably ^ewstin volcanic* aleo ocriir at bedrock
conformably with tho peridotite, l;ue to the largo
e howovor of highly magnetic rock formation, thctae
voloanioe are not outlin&d by OK* Magnetic Intejiuitioe* Jt
ie vory likely that the peridotite and gabbro are Kill-like
intrusive* into the keewatin volcanic area aa found (o tho west.
b) Eleoi roinaunotic Survey
Tho electromagnetic biirvoy wna conduotod ovor th*
*awe piokot lino ijrrid is f; tho nia#netonmt**r work using the Konka
l!ori?onl si Loop Method with ft frequency of 7&Q ops. Anfi a
c/tMrt separation of 200 fo^t* Two thousand four hundred and
ninety-two eloctrowa^juHic stations wore r#ad and rec&rdod
awl ehow on th; aooowpAnying: nloot-romasnetie ***fl on o *oalo ,
of 400 foot to l inch* Tho deeper negative in-pho*e romdin^s,
te long ae they are not exceeded by the out-of-phftwe, are,- ' r', .' '"' \.
indications of mi1^wuri\ice conduotoref stioh a* grra phi to, pyrite,
pyrrhotite ami othor oouductive sulishide wlneralw. Maat*ive
will ifive much wore significant reading* than *i|l*
of the diwaemJmued type whiuh aro only oohduotor* in
appreciable amount c, :' - 1 * ' i" '- -' ; '
The roQitltH of the el^otrciina^netle au r ve y chow no
fttronft oonduotor aroau* this oould be duo to lack of penttra*
tion in a deup overburdened area such aa may exiet over mioh
of the ground surveyed* Under such conditions aone plotted
readings though low, muy be ai^nificunt and it ia recownended
t-li a t t he tie be tentod hy a vortioal loop method*
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Probabl y Koawltt i.n voloE\uic .. ,aleC) Oell'lll' at berlrook
.t.rJldnu (lfmformal;ly ldth the; p.U'.idotite. lJue to the la"ae
p01"Cf.tnt •. ·~c) IU)w(:lvor of II ip,;hly' .nagnetic r(\(~k fo),,,,,,t.tcm, t.oo •• voloanios :41'6 u~.,t outllJ\($d by ttlat' Mugn.tio tnt.emiitios. l,t
is very 1.ik61y th<~t. the poridotite arId gftbbro Aro .. il1 .... 1iko
b) Eleot.roma.gnetio Surv~y
1'ho olectrNua":netto ,""urve)' wna conductod over t.he
$al1.l$ ,)10 k6 t. 11n(t 4trJd 11(0 Ulii nlagnet()Jtjot.~r work using tho RC>l,ka.
llori;r,ont.al Loop Not.hod with 1\ froquency of 760 cpa. awl ft
9lttllt'\ $opi.'U'at:i<"l of 200 fo.!~t. 1'wo tholllland four hundred and
n1nety-t.wo f.ltluotroUltl&!IK"tic &tationEi wore r~ftd and recorded
&l'\d $how on th,.' ,,"00Qmpl'lOyin~ "l.och~fima~net . .ic mAp on a IIea1t) ',' ,;
of 400 ftict to 1 inch. 1ho deoper nel-tative in-phawo .rolldtnll., '
•• lc:;nn as U.uy aro not ft~cef'.::dod by tho out-ot-phatlle, Are
.;-
I
J.rldieationa of 8UI>-IIU,'l\')c(t oonduct.orB, .\lcb a. ,r.phito, ",.rite,~. . ,
pyrrhotit& lind oUlOr oouduc ti. Vft sulphide ruin",rAle. M __ sJ,ve
atJll)hidufl \<ill give rtlw:h moru "igl'l:l.fioBnt re~(U.nl'. th.~ '.,,1 ...
pht(toa of tho di88CUld ',utod typo wh.luh .1"0 (>nl), CO'lC'not«>t. t.
*ppr~c;d,ftblu "'I'amntc. . ,
The rmJIIlts of' tho elttot,rt'I'IIAlln8t10 eurvoy ahOw DO.
atrcmg oonduoto,. lal"0IUI. thUs owld be duet t,o laok of pelMftra.
tj,QJ\ in .. deu" ov(,..burll.n~d aroa such It. ~ay e.kiet over , .... oh
of t.he ground flUrV8)'6d. Under such oonditttH18 .0" plotted"
rf;adinrJ8 though lo~Y, muy btt sJgnj,fici.\nt and it 1a recC)ll¥,fUldH
'JkQVulijKj;Qn2Jt.Q* ~ B ~
In addition to low conductor Indications gained by
tho Ronka orthod during tho survey, *ix conductor* are known
to v xint In the northeast part of tho property AU l oca t ml by
mi Airborne electromagnetic survey. In this area the Ronko
orthod did not gain any conductor indications* Four aroas
X H holed 'A 1 , 'fi 1 , 'C 1 and 'D' on tho accompanying electromagnetic
shout Ara out l i nod for Additional work by a vertical loop mot-hod*
Tho ^ooroaijrKttl.o survey carried out recently on
54 ci e i we oompoftinf; tho o of. t part of tho Jonsmith property
ali en -s thy proeenoo of peridotite and gabbro rock types intrud
ing iHiow&tin volcania. 'i h IB formation strikes o*0t-weot ucros*
wost of thtt property but is folded abruptly) resulting in a
north-south striking formation At the eafit proporty boundary*
Iho rock formationu Arc on oxtenfdon eaet of thoftft presently
beinn dintvanii tlrjllod by Jonmaitti to the vront of t h i* map area*.
Jn ml (Ut. i on to kuowti ooppor and Kino boarlnir aulphid* odoiirreno*
afcKocifttod with tho rock t. y pow, it i* believed that economic
oooitrrenoe of at. be t; tow fibre might bo found* Jn thi* regard. . i . . .'
tho peridot i toft in t bo folded aroa in the northttant corner of
the* magnetic shoot might be regarded a* favorable to asbestos
fibro occurrcjMoe which ia frequently loooted in area* of
dynaiaie motamorphlKw incJuding; faulting; and folding*
•
I;.'
; ,
In addition t.o lo\t cOllduotor indicationa ItllJ.n.d by
thu itonka m(.,t.hQd dl1l'inr. tho I.tUJ·vo)', .1x conduot.ore aro known
to (I)(iat itl th(~ nor·thoalft J',u't of th~ prop(t.-ty •• looat6d by
an IlJr\)O)~Il(' "'l(Jct.ro,"I4~UlOt,.ic s"rvo),,_ In thi" .rea the Ronka
rllUthod did not gaiu any cuucJuotOI' indJ.oationo. {'our aro ••
luboled 'A', 'n', 'e' lmd 'D' on ttl(' aCCOQI)Dl.yJ.ng oleotrolQagnet1o'
6hcot Aro oHtl inod l'or IHJdltional \"ork by • vertioal loop Not.hod.
6M"·iHA!i"i f~ '}UCPW'l,H)lI)!\1JONS
1'ho htOOmagrlQt:l.o Inwvoy carriod out reoently on
54 cla1.m$ (WDlpOl!dnf! t.ho 041ft· ~tllrt or tho Jonaratth property
at",vB tho prtnt:;enCG of J)('ridotit.,j) and gabbro rook type. intrud ..
.lnl~ i\.u8W/Jt.in vole.nis. l'iai8 formation at.rik •• o •• t ... " •• t ooro ••
Rlost· of the PJ"Ol-~J·t)" but. is fol.t1od abruptly, roaulting tn a
north ... south at.rlk.ir't~ t'Ot"Diltion ct the ealilt proptl.rt, bou",l.r,.
"ho rock formut.iorul ar~" un (txt.en"ton ••• t of tho ... pr .... "tl,.
beJ.I1R d inl1lvnc{ dt-J 11ctd by JOl'l.8rd.t.l;I to th~ WCUlt of thi. fliP ." •••
1" llddJ.t!or, to kllO\(tt (30PI)Ul' land .iuo boar,it", .ulphtd. of;)cnu" ... no •
•• "-;OUiAtud 'd.th tlw rock t.ypes, it t. believe.! tha., eoo .. o.l.o
OO(llU'rence of a.""et:toli t':lht'o mic.t'ht bo round. I" tht ... e,ard
thu pcu"!c.h',ti t~(Joh in t.ho foldod •• 'ea in the northtt •• t.. corD.r ot,.
th(~ mllt.:rmt.ic 8ht~.)t mil!bt. bo I"tlglJrdod •• favorab18 to .•• be.to.
fibro O(~CUl"J'OUCO \'ihJoh j~ frequontJy loc#.\ted 1n ar ••• Or dynrudc In4) tam orp htHr.I inc .JudJ us: r,ml t. 1.",-: and f old in,«.
- 9 -
Tho electromagnetic survey showed only very low
conductor evidence which tal'thi or nai&ht not- bo indicative of
underlying fiiilphide mineralisation in aoveral flroafi. Tho Jonsmith
North Conductor for instance, which was traced oartt to t ho ve* t
boundary of thiw in* p aroa, doe .i not chow poraitior.ee by tho
aioctrowoirntstic survey on tho accompanying ni4p* It i* likely
that, ovftrbnriion depth prevented locfitinf? of thia largo graphite
arxi fvulphi'lQ txicurrenco in rhyolite to the oa&t*
It if' recommended t luit four areas be fi u r ve y ad by a
vortical loop ol^utroitta^notlc wotliod 60 f ol Iowan
D*
It i*? recomwenrJod that tho aouth half of Lot* l,
2 and 3 in Concession 131 be surveyed by ft vertical
loop el rjctroitta,{not.io method to include the area
of dix indicated airborne* conductor** The
overburden horo la lx*lievod to be ISO to 400 feet
deep,
Xhjt JJ.Hi, ^rjia lit the overburdened e a* tern extension
of tho Jonamith North Conductor* Kxietin^ picket
linen horw should bo raimrveyed by the vertical
loop tH0thocl for a dititance of epproxinately
2,000 feet
•
" .
- 9 ...
'rho electromu;j;:natio BtU"V(~Y ollowud tmly very low
conduct-or evidenco which mlf~ht. 01- might not. bo inclicat·J.veof
ur\lhu'lying' finlphide utinl!'f.'lllhr.at:ion .in lIJov(wol Af"O.". T.he Jon&mith
North COI~luctar for inKt~nca, whioh was traced &a~t to fh~ we*t
bO/lUUfU'" of thill Jnap ah'~, dot., .. not. ,:;·ho\ .. pcrsir;t.unce by tho
.... loctron'lu.fumt.ic: iiUr\u)' em t.h~ uccompunyit1tt. 1ll4p. It i .. likely
ttl .. "t. ovewhurdcm dopth pJ'owmted loclltinr. of thiB l(lrgo araphit.e
afld &ulphi,'o oocur'reneo ill rh)'011to to the Olle.t.
It J.6'i reooJlUflenlied Uwt f'ClIl.~ OM&8 he t!.urv_yed by a
vo,"t {cal 100» ,~lm:t .. rmila(~not 1c IOlttthod oS follow."
2) •
.il.r'f.-...
It i~ f'6(HHl111,Ondod that tho 80uth half ot: Lot. 1,
2 And 3 in Corwelltdon III l,g surveyed by A vortioal
loop ~l"ctrt)mHllat.io mr.tnod to include the aroa
of "ix intlic;'lted 1A:f.rboJ'lno oonduotor.. The
overhur'de$l hCH'C1 1s hol.tevod to he 1S0 to 200 t •• t
d00P,
Ih1l. ..!.h.!. ,Aru tu thli' overburdened ••• tern ~.ten.J.oQ.
of' t hu Jor~mith North Conduotor. e,,:lat.tng pickot
1 hH.~1I 11t:~1"(;1 ~ah()1l1rl bo rt~l;urve)"ed by t.he vort 10al
loop llt<-lthod fot' a dJ.I.t,anoe of 6,)proxiutel,.
2,000 feet eu~t.
~ 10 -
3)* Ar&fl.. 1 ]:;' * e tht* Kenora! strike location
of t ho South Couclnctor on tho woat part of the
JonaiyJth ground, tow conductor .-evidence la gained
here by t h** KonUn iwthod and tho location ahould
be surveyed by tho vertical loop method for An
OAot-'WOi.t distance of 4,200 feet*
4)* Ar.3*L. 'HZ. ** *he central part of tho napped
aroa whora AOMO low Ronka reading* have been
ohtnitttxj. 'Jfhii* uro* should aluo be surveyed
by vert leo! loop procedure. The location i*
nonr thw nxial. pi w ne of the indicated large
fold, - ' . . - .- , ' . ; ' ... '1; 'i 1
total of the above rocomuended vertical loop method mrveyinr, la approxinately 17,5 wile* of line* Theao Jinos ttfo a lroudy a^tablifihod but will require clean
ing out a* they wore out clurinu the vintor wont ha. Diamond drill rocojftfuomtatlons should wait the r^^ulta of the vertical
loop
Wny 10,1961. H. L. Ma c Vr, i p h U,A*, M.S, , Ontario.
I .'
I· ,
:1
, r ~'." t,i. \' /
, ,.
:'\1,
~. ",
... 10 -
of tho Bout,h Con.ductor I.m tho W('Iot part of the
.JoJUuuit h gJ"()t)nd. " Low OON.hlt'tt.orevJ,thmoo is gained
hore hy ti~ kc>nl(Q J.'If:lthod and th., looattonahottld
be surveyed by tho vertical loop lMthod for an
eAat~WQ~t dietanoe of 4,200 toet.
., '
4). Ar.sa_ Ill! i. U,e oent·ral part or tha Rapped
81"68 WOON. 80"0 10\. Ronlul Nadine. have been
ot;,tn il1t,d. :f·hi.... ItrtUl .honld also bo _ .... veyed
by vaf·tic;:nl loop pro,'odu .. ". 1'ha looAt.ion i.
no *' f' the lI,~ilt1. plpne of Hut JndiOlltcsd loJ'lIe
fold.
Tho total 0,' the abov • .r~onulonct.d yortto.l
loop _thod !Htrv~ylnn tIcS Allproxi .... t.ly 1,7.5 1II~1t). or lillo.
"ht~~O 1 ino. a"o alr(H4dy fH.ta.bli"hctd but 'Will reqtti,.. oloa,,'" .• . ~ " , .
inH out 1Ih1 UIQ)' .wore cut during' t.ho "'into .. JIl~ftth.. l-t.lIlond .•
1 ()f>P IHU·VO)'. . I - " . ,
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