on tho proparty of
22
S2G16NWei68 52GtSNW**81 SIXMILE LAKE 010 l I J L CUWF.Y on tho proparty of AKAX ot -jL Sturgeon Luke Aren, Ontnrio by SHlilLO iUtLTnYiiJC:; Tirnmina, Qntario, March 26, 1970. R. T. e*lAPSHA^, P- n. O , Hrarjnhnu, ' \ tng. f Cunnultlnt) S •-.i
Transcript of on tho proparty of
S2G16NWei68 52GtSNW**81 SIXMILE LAKE 010
l I J L CUWF.Y
on tho proparty of
AKAX
ot -jLSturgeon Luke Aren, Ontnrio
by
SHlilLO iUtLTnYiiJC:;
Tirnmina, Qntario,
March 26, 1970.
R. T. e*lAPSHA^, P-n. O , Hrarjnhnu, '\ tng. f
Cunnultlnt) S
•-.i
2.157-INTRODUCTION
A mogn8tametar~alactromagnetic survey hns benn completed
on the Sprucacona Group of Amax Exploration Inn. in tha Sturgeon
Lakn arcs of northuoatern Ontario. The llnncutting uaa r.ompjoted
during the period January 15 to February 10, 1970 and the geophysical
survey work wan carried nut during thi* period February 19 tn
March 5, 1970.
Tha Sprucecone Group in nituotRrl B FRUI nilnn north nf thn
MBttagaml Lake eilver-baoe metal discovery on the Abitibi HJnr;k 7
property. The object of tho survey Is to locnte minornlizntion
aimilar to the Mattogami-Abitlbi ornbnriy.
PROPERTY. LOCfiTIClN AND AGCt.SS
The Sprucficnne Group la R contiguoua block nf 66 unnntentnd
cloima daaignated Pn 211720 to Pa 211737 inclunivn; Pa 2117'.fi tn
Pa 211757 inclusive and Pn 211760 to i 'n 2 117B1 inclusive.
In relation to i the dnttngami ornbody on Abitibi Hl.nck No. 7
the Bprucec'jna Group in situnteri 3 milon nnrthnant on tho nouth
shore-of Sturgeon Lnke. from iUtuix Lookout, on the C.N.H., the
property is located ^6 milea east-nouthpn^t.
To ths idoat of the property hiyhi.my 599 ponies i.ii'hln
10 milea of the property. A timber rond from hicjhuny 599 provldP?
OCC8BB to the proporty. Al to^n^ti^'8ly, flout or flki-eo,uJ ppptl
aircraft from Sioux Lookout to Sturgeon LnkR mny be utili?nn.
PRCVIOU3 UORK
The uriter is not nuaro of any prnvious work which hns
been carried out on tho property.
. 2 -
GECLOGY
Mapa by tho Ontario Department of HJnf!3 have been publishedM4F rio. l i M HW rio. P- 148
on tha area. These Includo t'-np Nn.2169 tint.) r.ap Nn. C. 1^0, the
moat detailed, nt a scale of one Inch to tfhp h.ilf mlln.iHDitfcfJ^ R,e*X
Map No, P,1'*fl ihi'lcntca ruck nxpunurnB on thn ntmi pSECTOR *^tir
Sturgeon Lake in the northeast at-ctnr nnti t'"1 nxtiRmn umnt nNadrHC^ST- M6TAOrAe6flj3
of thn proparty. In thn northenst, nclagnnhrn IntruriRB,Acc^Urfl^TH"
conformably, felsic agyloriarato nnii tuff IntnrhPtJdHd with rt'yullte
and dacite f louis ant] orgillite luhirh ntrikp Hlii^htly nnuth of Piint
and dip steeply north. In the unnt nector tif thp prnpnrty nmlnnitic
riouio and pilluus ore oxpnsod i.ihlch nrp shcvm'H fru! ptr
The pillouia TBCB north,
Thu regional genloqy of thn aroo la qhoun on Fiqurot^bubo-JHACf
after the O, O, M,, and tho following iBQRncJ applinn:
1, n Mafic metavolcanic rocks ond dorlvnri schistn anrl b Metnvolcanic rocks with a nmo f"
2. a Felsic metovolcnnlc tuTTa, no/jlnmnrntR, nndITeej^gD -SC
3. a Ketaaedimentnry rocko nnd rterivRd ac
**. a Gabbroic, mRtngabbrbic and mctarlinrltir.
5. a GneiBBRB to nchlntnnn fnlnic intnmlvn b Maaalv/a felsic intrusive rocks
6. Syenitlc intruaiva ronkaC^E^PHXiicAt-
Aa uill ba IndlcotRd by thu • J enphyrilnnl survoy rF.aultt), the intfj r-^PRvx.c"^iJ^ ^Ko^ft
pretntlon of the ynnlogy in the nrun of tho 'JpmcncoriR Gr u[i un
Figure 1 la moat quontiunoblo,
M.'*GrETUMCTCR SURVEY nCGULT'j rtN'JAT- t
The macinetomntBr onrvRy data Jn plnttrcf on R m*ip nt nAco^romuy.^i- TV* R.6R.P.1T
of ona ihch to fnur hundrntt TpRt aRcrn"pHnylni; thin repprt..
-3-
An Appendix attached to this report descrihes the survey method and
instruments utilized for the survey. The nngnntomnter aurvny plan
has bean contoured at 100 gurrma intcrvnlsi with thn oxcnntlnn nf thnt
area underlain by rcngnntie suscBptlhili tint? bntunnn 2I1U nml5o
gammos which has benn contoured nt 5H
There nrn tun nr?ms of diffnrlng i^'KjnpTin hnckqrnuml, nnn
to the east and nne tn the usnt nf nn infnrrerj fnult dHniqn:i',Rd
V &fl&T on the accompanying plnn. To thR r?;jat thR mpqnstic background
ranges from about 1UO to 3UU tj-romnn while trj thn west t.he nMtjnntic
background rangen frnm 3DD tn 500 yjmmus.
Along the north boundary nn liturgeon Lake in ti brnnrl
magnetic high, ranging from 7UI! tn 17UCJ q-imn--B, rtnslgnatRd A on
tha, plan. The IsomaQnBtics trend qenernlly nnnt-nnrtMeaBt.
Aa based on the magnetic suocoptltiilltlpn and the regionnl tjenloqy
this magnetic high la thought to represent n gnbbro or syenite
intrusive.
An inferred enst-northeast trending fnult zone just off
the south shore nf Sturgeon Lake, termed 1 on thR accompanyingAc BA?CD
plan, tsrminatBQ the gabbro or Byenlts mass. t\s l naed on tho feu
rock nxposurea on the nhtirn of Bturgnnn L^ke, the fault
probably Includes sheared gabhro, volcanico nml sRdlmnntB.K^CCl-iorJ^L 4-^o/jXf/
rlong the fault na interprohud Tri'm tho reiji"nol unolnyy ip pnt'th
nida-eest, north nide-uioot.De^i^MftTEO Aft-S Cvi*wo
NorthRast trending faultn doRitjn-itnd 2 end 3 nrn nhouin
crossing and possibly of f sotting thn tjp.bbrn nr syertite intruniva.c.H^f^-^
Thaae faults ore bnasrl on the chan jQ in trnndn of the toAa la apparent on thn magnetic plnn thurs la leas avldencn for
existence of fault 3 than fault 2.
- l* -CorraBponding to thn outcrop arBn on th-' shore of Sturgeon
EXvr-MofcnUttSr Laks batwaan Lines O to BE la an BBat-northPBMb trending magnetic
^NDj^it-ic high up to **DO gammas above background. rtnilmJUc f louis nnd pi Hou
CurcRop lava, showing east-west ahunring, form the outcrop end apparently
account* for the magnetic high.,
The aaat outcrop area in thB vicinity of Linn MM. , nnA,
the shore of Sturgeon Lake corresponds t.n n nnrl^s of generally
BBst-uBst striking local magnetic hlyhs nnd Im-i*. Thn mntfjn/ibbrn
corretiponda closely to a magnBtic hlrjh lucatptl on Linn 1DHC,
Stcition 2BN. The nnomaly la only snvnral hiindrnd fRRt Itmtj tretitlinq
east-uaat. The argillite nnd falnic ngijln'-inrntf nricl tuTf
are in areas of generally lower marjrmtlc aiincnptibillty.Po(Z.Tiori
Tha major part of thf? land pnrtlo'- nf tho B
Group axhibits tuo distinctly dirfnront ar*?n!3 (jf mngnRtic nusr:Bp-tA*l4rfJgTIC
tibility. To the uaat the nia^jnutic hackijrnund rongBO From nb ut
300 to 5DO gemnaa with vary few magnotii: tilghn nntJ o poorly tlofinnd
eaat-UBst trend of the iBomaynatics. Tt) the nnst thn magnetic-- tO fei f
background ranges frnm about 100 to li'[] qonmao find the efi3t-unntBX
trend of the isomagnBtics la uell dofinrul dy mngnntic highs.
These diffaring nagnntic chnrncteriBticn account fnr thn northeast
trending fault, dogiynated Tnult U, which crosses the propwrty.t^SiCy/^M^Og e.
Uost and east of the fault the nrenn nre URsignntBd L) und HL AT^c. A/, \Jt tn ff\ L
reapectivaly on the nccnmpanying plan. l.ntRrnl ant! vertlnnJ.
movement is poatulatud for thn fault with thn nnat block (nrnn C)uiisrsr Sux-K (/XPLCI^ B)
moving north and up with rsopect tn the i.mwt block (area U),
CompoBita movement, in tha order of aovarol thouBiind feet
likely.
- 5 -
Area B is characterized by a low magnetic intensity and
a general lack of prominent magnetic gradient suggesting thereby
the presence of a uniform rock type, possibly massive nndesitlc
or dacitic flown atriking about euot-wcnt.
Within area C ore two sub-nro^n tn the north am) tn Urn
south uiiiich exhibit a well defined oant-urot trend by a serins orftfcjEAS AI^ 2Soo
magnetic highs and lows. The anomalous prnnn firn loss than 25t'0CofcRCi.ATiN)(T-
feet long and average a feu hundred feet uldn. Correlating the]?cckl (T/^PoSoR^*
magnetic characteristics with the rock exposures on the shore nf
Sturgeon Lake suggests thtit the area in underlnin by an Bsneroblntjf?
of rhyolltic pyroclastics end flouis interbedded uith oome fine^ ^fQ-ALC*/ ^A*r-v*0g
grained eedimenta uhich Btrike rjenerctlly cnst-uiest.
CLCCTROMAGNCTIC SU'l'.'CY RUSULTa AfgH IfjrLfU'ntl T J
The olectromagriBtic survey dattj in plottnd ?it n nt:oTo
of one inch to four hundn-d fe-:t on the acrprnponylng planOescR.i^g9 ii^ -nte
survey method and Crone JEM unit la tloscrihoij in the Appendix tnC^l^AJM-^p'V-rz, "Jt " ifituUCI^
this report. Seven conductoro deaignntBd "r" tn "x" inclusiveTH&f (W& PgScR.*ft^P A.S Po
have been located by tho survey. Thnae are du'.cribed no follnua:
CONDUCTCH "r"
Thia one line anor-aly on Line 12iil is of vary wf?nk Intensity
but may be a valid bedrock conductor.
CINDUCTOR "a"looATT^c? Fj*a.-rrf BAS^S L HJ&
This conductor in locntec! r^orth of tho bnsa linn cronsing^Hfro^f J^JCLUXiV^ ) 2oofT^S
Linea ****E to 5GE inclusive for a length of nvnr 1200 fa^t.Acao r^rwipS, s*rt?s"v^'^*T Aftp
a multiple conductor aoma 200 fuot uiido, striking about unnt-went
- 6 -
la chown on ths plan, this affect may be council by 8 variable depthTo. k^ PRtf^j^Nic/ :tNJp\cA.rF
of ovarburdin. The ratios of high to low frequnncy indicateCopOOe.rio.ry CloO&R.gP Q/ M *R.^ f*fA^ So ^f&CC o f2
gBnerally good conductivity covered by n.nre thnn 5H Tent of OVPT-8*Roe*i. "TR^Ke Ate: Vbo*k ITAOi CACHES oF A^PlP TO T-*ytf. burden. There ara poor indication* of a dip to the north.
Conductor "B" pornllelfi and nlrrost coinciden with southVM^TOR. ^^^(t^a. to^E iKk sTvjn.c^O \J\v.Z- T^f
edge of on inferrari major ohanr zona in Gturyaun Loke. Ttm mnoo^oocrtia. A^ces K ^BOMT- -^Hao ^
intensity of the cnnductor axR3 is nbnut i* '.JO gnrnmna
CONDUCTOn "t""OPFoff thn southThie one Una conductor creasing Line
of i Bhore of Sturgeon Lake la rf ueok intensity uilthin UIR lnf*?rrfid
~TH^ APP^^-JTo^efl^M^j OP THE: Sturgeon Lake oheer znna. The apparont mnnknces of thn cnnductor
may be due to deep overburden.
CONDUCTOR "u"UrJZ. THIi tlortOJCTZiP-
North of the base linn this conductor nroaooa LinenFt* R. A-
to 1QOE, striking nsnt-ueat, for u length of 16IHJ feet. Hatioa nfCr-CXiC' C-0^ OOcTI^ *iy- f*-**^ it-tf S" UfS
high to low frequency indicate gr. od conductivity. Profilp nnnpen~*s ftf -r
indicate an overburden thicknRsa of 75 feet nr tjroatrr uith
esaentially a vertical dip.-n5R.rni^*cr^ AT A,
The west end of the conductor tnrminotRn at o prominent
northeust trending fnult Inferred from thR mngnRtc'mRtnr Burvny.Co^pOoTO**- MrJ^uJV i ^ x:Nn-e:^sitv
Magnetic faatjres along ths conrJuctor rnnging in intensity fromAifP^A*. Tt* Bfc Cfe-vscpr By
36** to ov!?r 600 gammas epptmr td 'n1 crosscut by thn conductorCPKiOucToft. KElPR.es i'trS A rAOU-r:
BXBB suggesting thot the conductor rcprnnentn n fnult.
cr-NDUCTonMAX
Thin conductor, crossing Linnrj 10'*E nnd 10BF. mey bs
- 7 -**JP s M Ape or
the extension of Conductor Hu". Tha Intensity and ahnpa nf tha
profiles indicate conductivity characteristics .'ilmilar to ConUuntor
"u".
CONDUCTOR "u*.
South of tho base line, crossing Lines 8*4^ to 9fil, forC-o^CXiCrt*. STtUklSS
a dlatanca of 1200 feet this conductor strikes enst-uiost. IT weak
to moderata strongth t^la cunductur IP cuuerKtJ by Bpproxl^ot'?ly"mtT f^^^Tl^ 'rtTErOl!^ ^U>^i^
75 feet of overburden. Tho 'naghBtlc Intensity ninny tho rOR.DeC.or l^a
axes la of the ortlor tif 13 r )
CL'NDUCTDR "x"CoirV.iCa?i.
This one linn conductor on Line 60F. coincides closnly tot^oo r^tfr Loio^-. Oup^&ufcDC'J ij"
the centre of a magnntic llnHfir 15HO f* et Inng. Ovarburdnn Is
Indicated to be at lannt 5f1 fn*.'t (fripfi rind thn n'.ndiictlvl ty InTD "TVs: J?iP
weak according to thn dip nnglo
, The maynBtlc llnaor atrlken nnrthii-snt nnd In terminatedNoKTIWSs-r TRe^PCoH- FAOLT P^5TUW
to tha wast by a prominent northwest truntllnij fnult puatulntetl
from the rnagnntometor survey.
CONCLUSIDNS————————— blS-DA^T f^K&^'A^ t**-*- KSe^&
At least threo distinct firuas riT rock nnnsmblagi? r.ppnrntnd
by faulting H. o indlcntnd by the ToaijnatnmntRr nurvBy and rngiunslS-ntt^^ty^ t-Ajte A rAwu.yooiroR.vv
geology. To tha north belom Stur;jetin Luke n fairly uniform "Tg
high la poatulateri tn reprcnant gnbhro nr synnltR. The south edgeBoyrJ^e^ 4X A MATDiLjrAsr-WoCTHfVr Jrxrlc
of this intrusive is bounded by ri major I'ont-nnrthnout atriklrigrctr- byjipWj ALoO^TW/f Soortf SHo*i.
shear zone, aevrral hundred feet wide, nlontj thw noiith shnrR nffRoiiAfrue SMCA.Z. 3o^cr pbe^s A B
Sturgeon Lake. This probable sheor zone forr-n n brnnrJ boundnryTo TH-/5" A*O HJ-rf Aiwo f^&qet
betuenn tha gobhro or syenite to the north nnd probably mns
-To TUlc Seurtt SHUfcl^ A&xJT andasitic and dacltlc rocks to thn south striking about sast-uest.
APPEAR T* The maoalvB volcanics In turn nppnnr t.n '-e tnrmlnatnd
to the BBot by a prominent northonst tipnrllnij fnult approxlmntnly WJopecrX. JEM r oP +H'* pWucr 15
through tha cantre of tho jiropsrty. Tn'tt nT tti5i Tgult in
postulated tho presence of rhyolitir. pyroclastics tirtd flou'pC^HicAf SrJUr*? W^A*. Z*6.
intnrbBdded sadlments uKich ntriko nunr rn-'t-uiRHt.tooAr^o ot\j ruz
Df several conductors lonotRfJ on thp property thrme~TO BF- TH/ Mojr
"s", "u", "v", and "x" appnnr to he thn mint siynlficnnt. In eachSvKjev &Y eN/^ee^fl/?^ AT ^ijSXJ
case, houisver, tha conductors ara hurind tiy nwfrhurc'on nt 1p;mtCoiODOcr^^. "IA.;^ "V, A -OO
50 feat deep and parhnps much nroatcr. Cornluctnrn "u , "v",
"x" ore locatBd within ths^ rock iinsrmblnyo inr.luMlng rhyullLin'Zjf&iroe.'i-rsi. ^urMoo^-ri -fH^s^ coMDa
pyroclasticB and flouo, and uodl""Bnts. M thmitjh thi nn cotnlur. torn
should ultimately IIB investiyntad by diamond drilling It isttgcA\lsZ o 1- TH& f os. iltL^. **J iPtf"
difficult to BSHign priorities tTscHuaB of the
deep ovarburdsn on tho property and tha lock nf i]R"lo.)tcol dnla,
nECI-IMMENDATIONSA Dfi.ii.L- Trtisfsn^rt** tr~ /*,
Qafora proceeding with B drill investigation it IB, thera-
fore, racommsnded that tha property ba i]o;".)otiic.illy surveyed in
detail, Ths geological survey may indicate the riBod fur qennrnlFX .
or local coveraga of the propRrty hy ri vnrt.inii Innp BlnctrnnngnRtlc
aurvBy, prior to drilling.
It la axpBcted thnt the ijnolnqiniil aurvRy uculd nut oxcar.'d
a cost of ^2500.
RBspnctfully fjMJCLU lil
J'^-cori, Ontario, R. J, nrwiiRhpu, P,
March 26, 1970. Consulting Smilogiat.
^:: "J,0^
1-60 I, Ronald J. Bradahnu, roqldinij nt f* 00 HouinrtJ Straat,
' CoOJUVTirtfc ^oLOCfl^T* ^rW OPTX.^M~~ 3 t POntario, a consulting gublogiot ulth officB nt 25 f'lno Htrrnt
V& uet.4By c^tri South, Tlwmlnn, Dntnrlo, do hereby certlFy
I attandvd Uueon'a Unlvnrslty, Hinjnton, Pntnrio, nnti grnriiint"fJOJTH AkAO H*fJoJ(Lf 6.A. P^R*2 /fs) ^^OLo^i^ftf, ScJ/T-oce-^ 1^ IfJTB.ulth en Honours 13. A. de',TBn In nnolrglcnl ^rlpncun in VJ5IK
; AI Bm a Fellou of the (ionlorjicnl Aannclntion of Cannda, n
OF T~4^ ^lA.j/^Ojft'O^yJSTi-njr^ ^^ iwi^iiJGf A**O ^^t-ALLV^^Tof the Canadian InntitutB nf Mininy nnri f'etnllunjy nnd n
.of tha Association nf f'rofnBiilrnnl f-nglr.nnra rf the Prowincn nf cwor/xR^io. , Ontnrio.
t~ff
I hnva no intwrent sitMnr dirnctlv IT indirectly in thn Bhnrnu nr3f^ S^C.UR.'T7^5 OP^ A^Atf ^/"BBcuritlas of Amox Explorotlnn Inc.
of
Timmins, Ontario,
MarDh 26, 1970.
H. J. BrndBtinw, P.
C j insultiny o
P
SURVEY METHOD AND INSTRUMENTEX 'S\)SURVEY
AA Sharpe H.P.-1 fluxgntn 'nntjnatnwptnr wn^ used In
ixagnotic aurvay, Thia Inntrun-ont nniinuni'j thn uorticnlF -t-H^. ^AgTH'f f^t^N^nc. f^i^Lf / /O *f^*v^A/. tfAS
of tho earth's rangnntln field In nnmi.'nn. tinno ntn'.ir;nn Tt:r
tarmining tho mngnntir. diurnnl vnrlntirnn wnrr pntnhlinhtui TH^'*U'A3 & J&& Jj*f AT (oo F**r / /ors^vAis W/AJf A T~PJP^ thn wnin base line Rt 1UO font lntnrvnl 1 ; unlna M tripod m-
^cnVrxe> M-F -i-icx^ Fi.wyUr AT^" fAA *r w^ Ttxv^en?^ . Ai^/oer iicintrax h.F.-1-HJO flnx;intR m/CinDtimHtRr, ' nyimtlc rrnijl Ajcarr) AT -.TO poor !NTEtujFlULy AU^CT THE CR^i* lidCSS oov^^RE Trtf taken at 5f. foot IntnrvalB, olnnci tbn nrfin 1) lin n uhnrn t'm f-RADl^^T-l^ ^Refvr-^'^'^^A^ ^oti Q-A1 '^A^ i l^i loo fj?eT OT Qradiant la groatar thnn 20fl ^nrrfrinn in 1".') Fnn*.ftET^Di rJ^i v^&^T-AlCciO ^"r" to^ Foot"readings were token nt H'D font
ELECTnCHAGNCTIC\Kj rwii Sofvwif^ {s c^mf R.ii6C? d? f
The Cruna JLK unit u:iei1 in fiiii survey i in cuwprlnml ofco. u/M.rr CJHK.M fcoTrt -TiAOsrAtf" A.^0 fcjEcf^ OM A
two aimilnr coil unitn uhic" both trunnmit nnrj rucnivo on n o F Iftoci od * go Kt. "r-we pgofERry ^^ CoR^py^Q r^ of 1{JQQ or 'iflU Kz . Tho prnpRrty uns onrv^vnft M^plnyinq ttiR "nh--nt-
Jy^r^/^ ooiTH A co i L- yg:P**B-A-r*dr5 o/^ -2.00 F"ise"7~T back" ayntew with a coil i unparutlun :jf i'ii'J Ti'nt.
T^) -m, t -jy?g et- 5vW2YT*\B ^eioLrA^^^c^CH/^ is AIn t' in typo of Biirvny th-i rpnultr^'t rnt*Jlny in n
fA^^r-,^ bfc^RC^ AoD Aw AMoA^AJ.y li USuDJ-vy A KjUuu- mvnt in dsgreus nnd an snunuly is ununliy n rnHultnnt rB :Mjln;j
graottr than plua or minus thren cmjronD. Inltlnlly thw r.urwov C^ODocTtO Oil/^r- Trt^. f//^^/ fS-p^QxviH'Ocy O^rf ^^ t^ |5 conductod uoinq tho ^igh f f rsquoncy i.nlt uhlrh Is
Any anomoloua cunditinns i arn nheckorl liy t.hf? Irju frnijuency p'j' Of e^esr t^Tt0^1^'^ "^^^ c-4tAn*c*'eWT*cs Or co^i^xru/'rv A thaiaby determining, thn cnnr.ictnrinticn i;f conijijr:tivl ty ;is -'{nt 1
T'Sbr^ T^e I^Arto w^A *CVH- -H) UXA) P^KiS^P^cX P-^^irX,^ A ^ATio from the ratio of ' iyh tn lou frntiuuncy ro.vJinys, ^ rntlti nf unityIS Tfft iP^Ai- Co^DJCTt^ /^L-T/yoU^-// OTHgA, PE*m,xtfC".S f+VSTQg ia tha idtiel conductor nlthnucjh uthor fpnturn" ntmt be cnntildnrstl. TW^ ABrt./rXTC' T-fcA^/^rr-ArOO Kec-ev^cr o^ JSoTrw c.0i^ a. Ur'M^^itt The ability to trnnamlt end recelvn on h fi c')lls RlimSn.itni th:ttK.^e tevt-ni^fr Ffe/v^ j^^/toP^^CaiL o^i6NrAt**4 ou^t^c^uAt. 7-j rror rBBuItlng fro" iwpropor coll nrlBi'tntii.'n nvnr irrnqulnr tRrrnln.
CRONE GEOPHYSICS LIMITED
979 LAKESHORE ROAD E. PORT CREDIT. ONTARIO CANADA
Phono: 274-3704
Since this method was developed 10 years ago hy Duncan Crone it lias heroine one of the mosi extensively used ground EM methods in Canada and the United States In this period (he J KM h;is been the basic grour .M equipment that in conjunction with other exploration methods has discovered over 110,000,000 tons of ore.
v
accurate dip and conduc tivity analysis
deptli penetration in the order of 150'
simple, reliable instru mental ion and operation
can he used with the Crone method or as a vei (ieal loop unit
This is a two man operation each carrying a unit capable of transmitting and receiving. They are spaced 200' or 300' apart and travel along the same line. Doth transmit and receive, the two dip angles thus obtained are then added together. If (he resultant is "O" no conductors arc present, otherwise a pattern is obtained dependant on the depth, dip and strike of the conductor.
•Canadian Patent #631,506 end U.S. #309,911
Example of a JEM traverse over a dipping conductor located in Denbigh, Ontario.
^)li^, y i
SPECIFICATIONS
1) Standard Unit2) High Frequency Unit
— Massive Sulphide Exploration— Disseminated Sulphide Exploration
480/1800 CPS 1800/3000 CI'S
READOUT
NULL INDICATOR
WEIGHT
RANGE
BATTERY POWER
— Dip angle from inclinometer r*. V'a 0
— Audio through crystal earphones
— Per man each transceiver unit — 15 Ib.Shipping weight including 2 spare batteries — 55 Ib.
— non-conductive overburden l" wide null at 300' non-conductive overburden 15 0 wide null at 500'
— Normal 12 volt -- TW-2 Murgcss; 732 Kvcready. M-!)19 Mallory Hi Power IP volt — 3 of G volt F'lBP Burgess and Adaptor BATTFHY LIFK — 2 weeks to l montli RECKIVKM — 1.4 volt mercury KM l H — life l year
PRICE S2.000.00 including method rights RENTAL S110.00 per month
-IS:;'Type of Survey™
SPECIAL PROVISI S2Gi6Nwai68 saciSNweesi SIXMILE LAKE
ASSESSMENT WORK DETAILS
ELECTROMAGNETIC
900
A M para t* form l* required (or each lyp* ci currcy
Chief Line Cutter or Contractor—Jll^:________________________________Norn* Address
26 Pine Street Bnuth, Timmins, CntnrioParty Chief A* Grotton *Noih* Address
Consultant Shield Garjphynica Limited, 26 Pine Street linut'i. Tlmmlnn, t'nt^rioMama Address
COVERING DATES Line Cutting January 15 - February 1u, 197D _____________
Field Geology or Geophysics omce Harch 12 -
February 19 - Mnrch 5. 19711
26, 1970
INSTRUMENT DATA Make, Model and Type Crona 3EH unit
Scale Constant or Sensitivity ______________________ Or provide copy of instrument data from Manufacturer1-* brochure.
TotalNumber of Stations Within Claim Group 2610 Nnmr.* r of Miles of Line cut Within Clnim 57.06
ASSESSMENT WORK CREDITS REQUESTED, . -' . * i ' ' i
•' :i " .',
MINING CLAIMS TRAVERSED1 ,
Pa 21172Q to 211737 inclusive
Geological Survey. .Days per Claim
Geophysical Survey-/—-i— Days per Claim
W-:'.*.
DATE 26, 1970
PB 21171.0 to 211757 inclu-ive
Pa 21176U to 2117rJ9 incluaiva
-
rnTAi. 66
H. J. BradshawSpecial provision credits do not apply to Radiometric Surveys.
^:-.. -
SPECIAL PROVISION
ASSESSMENT WORK DETAILS
Typo of Survey.____________HAGNETCJHETEMA separate lorn U required lor each typ* of cunrey
Chief Line Cutter or fin,.,..,.- ^ Cybulekl, 26 Fine StfHut liruth, Tjr^ln.% OntarioNome Address
Party Chief R. Drapar, 26 Pina Gtreot Sputh, Timmins, Untnrio__________Nome Address
Consultant Shield GeophyalcB Limited, 26 Pine Btroct !3n.ith, Timmins, t'nName Address
COVERING DATES Line Cutting January 15 - Februnry 1U, 197(1--—--———-
P. ,. r . r u - February 19 - March 5, 197U r icld Ueology or Oeophysics —————————loffice March 12 - March 26, 197(1
INSTRUMENT DATA M,V,, M^i .^ Typ, Sclntrex M. F. -1-100 fluxgnt.n mngnntanRter
Scale Constant or Sensitivity * or 5, O r provide copy of instrument data from Manufacturer'-s brochure.
Total Number of Stations Within Claim Group ——2p9D Nnmk^r of Miles of Line cut Within Claim Group———*
,l'-.'l•:\ . A Y*.* : , -
ASSESSMENT WORK CREDITS REQUESTED Geological Survey______-Days per Claim: ::':-, . .,,.-.,, 1 ., f i ' - , ;-w.. 1,0
' ' i-f' " ' Geophysical Survey- ' ''
MINING CLAIMS TRAVERSED
pa 211720 tp 2 11 *7?7 inrluaivB——i——.———.--—-—.——.
P, 2117Ln ^ ?11757 innluaivB——^————....-...—.—,
Pa ?ii7fin tn 2117B9 incluoiys_____ ——^————.
66
PATE Harch 26. 1970R. J. Dradohau
Special provision credits do not apply to Rndiometric Surveys.
Claim Mo.
JS^HCDULE.
Pa 211720 f-0211721 6021172*, h!)211723 SI!
; 21 1724 W211723 fi'~211726 S:;211727 60211726 SD211729 6fJ211730 GO211731 6"211732 fi"211733 60211731* Si'211735 B"211736 fin211737 On
P* 2117liO 6U2117^1 W211742 fi"211743 BH 21174U . Gil21 1745 f'O211746 6tJ211747 fit)211746 W211749 fi')211750 fiH211731 fi"211752 fi"211753 fi"211754 fin-21 1753 J fi'1211756 &H211757 fiO
Pa 211760 [J!!2117ft1 f (J211762 ft[ ,211763 r,M211764 . f,u211765 6i,211766 211767211766 fi"211769 W
211770 #211771211772211773 211771* 211773211776211777211778211779211780 2117S1211782211783 211781* 211783211786211787211788211789
2 -
60 fat) 60 fyQGOGOf.O 60GOGO GO 60 6D GOfin60 60 GO GO 60
C
STURGEON GROUP
DARKWA7HRGROUP
^
LOCATIQ^ AAAP STURGEON LAKE AREA
Scale: l" s smites -4
ADO GROUP
t: JJ
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,p*.
i i l IV ' l '4 \^*^^ ' ' -' 'l j j l j f 213*** '2t3**O V2I343* (/f343B | 2(9*37 . l J J4.O3* ' 74*OOO j 7**QOt I?4*CI7 l /74*fi.3 f— — -J -}- — — _r"* 1*1 J'' I P* "T**~———T~*i———"tVJ———/^P*"——— ~ P*./"^ J *V7 i"Vs- 'i i '2272S7" 2272*3
l kr"! v V^" ~^r-i*r--fe--7p,-—J24*040 . 743*** J 24*004 Pu O, ' l . . , 7 jT. , XT l ' ' t ' .
2'4-*5 '21431* 214*93 '2140* 2W2* ' ;- -
.--J-- --——t.
AREA OF SIXMILE LAKE
M-2877
SCALE: l inch = 4 0 chains
•A' i V- , ' /—^^ItX^wwwj) |744^*7^ , ______ ^"~\^ ' J4*C34 74*04. IP*.
II"" l" l
' ' !itjaa*,-.! -*f?^ ' 24*OZ2 ' Z4to?3 24*03* [2^^! \T^~~4ii
!' j I2CTO73 J225OC2 '2Z9O6I ' 229O5o'z29O:! ^908522*074 S turgeon ' ' __ j..l f~ — —l — — — — -* . — — ——— — — -j — -~ — . J?- " '*~- l ""- -l l p" IP*.
22*307 J *,,r^lMT 3* '2.173*. ' 211737 2l l 73i ' 2.'. s* l Z i. 7^7 ! tll'77S l 2H77*.1 l
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*l 1227254^*272333 J ' 22*41* J
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27232, , 227230 l l•^2II7/*-!,
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l Pa l Pa. IPO IP* ID, P.- l Pa.
i l l l l l ' :Z29083.Z29C7*. 229O7I l 229O6* I229O39 l 2?9O3S : :29O*7
H2H7SI
l 2'..82 (2"T83(
. 22*.*04 .Z2*22* l
I*—— -^—•**™^ *W*b ffi *" l 4L,*,-"-" l t •U.^^^rf^V-v |4V*b7*lAJ7 * *C*C7U3*C '
!P. l Pa iTa. P. .p*. l Pa. ' Pa.ill l229O82t2Z9O77| 229O7O j 229O65 ' 229O58 ' 2Z9OS3 , 2-9 .i^-'T'* i** i"*" '"- i"" '^ i'* '"" r*"i i*'-29O*. '22907*' 229O69 1 229O*B Z29O57 122,03* ( 22*3.3 22*3.2 j 22*3C3 ;Z2*3OO.
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2"- '23
:""722
"X l 1.7 - TP. J2il S3 2)174.
l PA
J
w : 227230 . ^^x. 'A-' ' ' - : A\ ' ' '2233**;i7*3**7?2l3** -'MSOT*.j 22*3**^, 22*3*3 j 22^3** 22*3*7 L^Z**J••":u'W ' pi~ "~^~ ~ rv* ~^'"tpT ~ '"-p*\ ~T~~ ~ —*~ —~~^'~~ — —r- — ~ —^"Srf*|
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lot r 2 j* ...*. J| L,.,/, j; - -j-. J .
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,—— — -i- — ^-:- ——l—--: — --l —)-. L— —^.— — -*— — -t — ——Z/ ' :. '. ""/' i'*" • f*~ ; '*" JP* 5? 'P*- JP*- IP*- IP*- ' P*
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AREA CODE— /f 16- 365-6913
ON1AUIO
Dfc'PARTMONT OK MINHi; AND NOR! HI-HN AF TAIUSMiiiicr, i Ann 1 ; (•'lAticii
Febi-uary Itfth. 1971.
Mr. \}.A. Buchan, Mining Recorder, Court House, Sioux Lookout, Ontario.
He: Mining Claims PA. 211720 et al,Sixmile Lake Area._FileJ|o...2^1^7..
Dear Sir:
The Geophysical (Magnetometer and Klectromapnetic) assessment work credits an shown on the attached list have been approved as of the date above. Please inform the recorded holder and so indicate.1 on your records.
Yours very truly,
Fred W. Mn t the? v; R, Supervisor, Projects Section.
c,c. Aroax Exploration Inc., 1302 ~ ? Kin?, St., East, Toronto l, Ontario.
FV/M/mr
c.c* Mr. H.L. King,Resident Geologist, HOiJ Hobertson St., Kenora, Ontario.
PROJECTS SECTION
Recorder Holder
Township or Area
DEPARTMENT OF M INES AND NORTHERN AFFAIRS
TECHNICAL ASSESSMENT WORK CREDITS
Anax Exploration Incorporated
Sixmile
PUP 2.157
Type of Survey and number of Assessment Days Credits per claim
GEOPHYSICAL Airborned GroundQc]
Magnetometer ...............W?.................days
Electromagnetic............?.?......,.....,....days
Radiometric .......................................days
t.- ', - "GEOCHEMICAL........................................days*- ; ' ' SECTION 84 (14)......................................days'A j-.' •••••'
Jv. ' ' Special Provision! X j Man days |_j
NOTICE OF INTENT TO BE ISSUED
'j l Credits have been reduced because of partial coverage of claims.
|J Oedits have been reduced because of i; , Corrections to work oates and figures of
, applicant.
NO CREDITS have been allowed for the " following mining claims as they were not sufficiently covered by the survey:
Mining Claims
PA. 211720 to 37 Inclusive
2117AO to 57 Inclusive
211?60 to 69 Inclusive
Tht Mining Rtcorder may reduce the sbovt credits if necextry in order thjl tht total number of tpprovtd tfsessment days recorded on etch claim does not exceed the iiaximum allowed ts follows: Geophysical - 80; Geological - 40; GeocHemictl - 40;
•VSHSKftT
SEE ACCOMPANYING MAP® IDENTIFIED AS
-3
LOCATED IN THE MAP CHANNEL IN THEFOLLOWING SEQUENCE
(X)
