53
52BMSEeei3 2.4256 WEAVER RECEIVED NOV - 61981 MINING LANDS SECTION 010 GEOLOGICAL REPORT LAZAW PROPERiy CROOKED PINE LAKE AREA 52 B/14 B(/: Randy Ciou)te.y iyhx.-Ca.nada LimJittd AM THUNDER BAY MINING DIVIOION E C E l V E HOV 3 1981 i

GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

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Page 1: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

52BMSEeei3 2.4256 WEAVER

RECEIVEDNOV - 61981

MINING LANDS SECTION

010

GEOLOGICAL REPORT

LAZAW PROPERiy

CROOKED PINE LAKE AREA

52 B/14

B(/: Randy Ciou)te.y iyhx.-Ca.nada LimJittd

AM

THUNDER BAYMINING DIVIOION

E C E l V EHOV 3 1981

i

Page 2: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

LAZAW PROJECT

NTS 52 B/M

fie.pofit A ummoA-czei -the /leAot-ti o (J a geo-tog-ccat completed o n -the pfiopeAty in Jane. 19B1.

JWTROPUCTIOM

The pfiopeAty con*i*t* 0 (J It contignoa*, unparented mining claim* numbered ai

TB 519657T8 5 57S36~B41 inclusive.TB 557*72-876 inclusive.T6 S"SfeoS"Z- oars' f*e.

The ge.ological *uAve.y m* completed oveA all on pafit o^ the, following S claim*.:

TB 5/9657TB 557S37-S40 -cnc-doA-cveTB 557*74-876 inclusive.

LOCATION AW ACCESS

The pfiopeAty i* ce,ntAe.d on a Amall lake.- The, Pothole.-. 6 km nonth of, C/toofeed Rcne Lafee -en -the Townih-cp o^ WeaveA (M-2066). The ptiopeAty -ci within the. Viit/iict of. Rainy RiveA and the. claim* aAe. fie.cofide.d in the, TkandeA Bay M-cn^.ng P-cu-ci-con.

AcceiA to the, pfiopeAty -ci by bain -toad ^fiom Kawene (On H-ooat/ 633) to a landing on the, tooth A ho/ie o f, Cfiooke.d Pine. Lake, at 91" 0 5 'W 4 t 0 46' H. Then, by boat to a point on the, noith Ahone. o^ Crooked P^.ne Lafee . i km tooth 0)5 the. Pothole,.

PREl/IOUS WORK.

Wo ptie.vioa* wo/ife -ci /tecoided -tn the. oiieiiment ^ei o (J the MinibtAy o^ NatuAal ReiouAcei -en ThandeA Bay. Howeuet, -en 1963 Wo/ianda Exploration* Co. Lcm-cted caMie,d oat limite.d tAe.nching with one. tample. tie.potite.dly fietoAning . 3 oz./ton/ 9 ' (W. Moo^iehoaie peA*onal communication). NumeAoui o^.d g-^td ^cneA and claim poA-ti weAe locate.d in the. ^ieJLd, TheAe, i* no ev-cdence o (5 drilling on the. pfiopeAty.

The. pfiopeAty ha* been ovetjf-Cown by -two e-t'ec-tAomagnextcc/mao.net-tc AUAvet/A. keAodat completed a Au/ivey ({o^i R-co T-cnto and QueAtoi SuAve.y* completed a * ative.y tot the. Mini*tny ol WatuAaC ReAouAceA OA paA^; o^ -the laAgeA ktikikan MAbofine. AuAvet/ in 1 9 80 (Map 30521).

Wo EM conductor we/ie detected on -the pfiopeAty howeve*, bo-th AuAvet/A detected a b^oad EaAt-WeA-t frimching magnetic anomaly nea/i South end 0({ -the pfiopeAty.

Page 3: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

A * hort description of, the property occur* in the OGS Report 179; Geology o^ -the Crooked Pine. Lake. M.ea, by J. Pirie..

REGIONAL GEOLOGY

The property occur* within the Wabigoon Subprovince o^ the Superior Province, approximately .Bkm North ofi the Quetico fault which mark* the boundry O jJ -the Wab-ujoon and Quetico Subprovinces .

The Wabigoon Subprovince. i* an E -W trending belt O fj mafiic to felsic volcanic rock* with lesser *edimentary rock*. These rock* have been intruded by mafiic to ultramatic dyke* and *ill and granitic pluton*. Metamorphism range* firom the. greenschist to granulite facies.

The Quetico Subprovince. i* dominantly comprised ofi meta-turbidites . These turbidite* are now re.prese.nted a* interlayered pelitic (o^ten garnetiferous) band* and coar*er grained p*armitic band*. The Quetico Subprovince no* also been int*ade.d by mafiic to ultramafic *iH* and by ^eJUic pluton*.

The. Quetico fault farm* a narrow, highly de.farme.d, and mylonize.d zone, along the. Month *hore. o^ Crooke.d Pine Lake (Pirie 1 97 K ]

PROPERTY GEOLOGY

GENERAL

The property i* undertain-: by a *eries o^ ma^ic to felsicvolcanic* with interbe.dded e.xhatitive *ediment*. These, rock* have *ub*e.que.ntly been intruded by concordant to *ubconcordant diaba*e and gabbro *WL* and dyke*.

The economic interest in the property occur* in a quartz invaded shear zone, which trend* East-West accros* the property.

MAFIC 1/OLCANfICS ( MAP (WIT 1)

The mafcc volcanic rock* occur South o tf -the Pothole. Shear lone, only two exposures have, been recognized north O j( the shear zone.

The maffic volcanic rock* u*uaULy host a strong slaty cleavage which JU^ defined by ever present chlorite. Other alteration mineral* are calcite and minor sericite. Minor disseminated pyrite occurs locally. The mafiic volcanic rocks occur in homogeneous band* and interbedded with chlorite schist and felsic volcanic rocks in the shear zone.

Page 4: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

CHLORITE SCHIST ( MAP MIT 2 )

unit occurs mostly along the, East-West tAe.ndU.ng shear zone on the. south 4 hole o fi the. Pothole, but it albo occurs in thin conformable band* at some distance North and South o 6 the. shear zone.. This unit is the. host of, the. aurifierous quantz veins, however the. quartz veins are restricted to subunit 26; the, chiolite. sericite schist.

Subunit 2a consits entirely o fi chlorite and calcite, with the. penetrative fiabric defiined by chiolite..

Subunit 2b consits o^ chiolite., teAicite., calcite. ~ pyrite, and chalcopyrite.. ThiA Aubunit i6 much mole. ^i^&He. than 2a and ha* a orange. iA.on

Thib unit uAuatty i* interbedded with teJltic volcanic OjJ unit 4 and voith cheAt and ch&it bn.tc.cia. oft unit 5 .

I^ERMEPJATE t/OLCAMIC ROCKS ( MAP UN/IT 3)

InteAmediate, volcanic AockA oAe, D J{ limited extent on the pAopenty. The unit i* nepfie&ented a* moA&ive to ^otiated slightly chloritic lock* 0& portable ande&itic' composition. Calcite ib al&o ptie&ent OA an alteration mineral.

FELSIC WLCAMIC ROCKS ( MAP MIT 4 )

Thi* unit i* represented by a wide variety of, ^el^ic ^low, minor pyroclastic rocks, sericite schist and breccia. These rocks occurs in narrow to wide bands and are ofiten interbedded with chlorite schist and chert.

Porphyritic felsic volcanic rocks t quartz porphyritic, fields porphyritic and quartz- feldspar porphyritic rocks are the dominant felsic phases. They occur North and South ofi the shear zone, are usually pale green in color, f,ine grained^with various amounts o fi sericite, chlorite and biotiteon cleavage planes. Between L- O .and L- 12 there -C6 a well defined zone in which the porphyritic fielsic rocks are interbedded with chlorite schist.

Pyroclastic fielsic volcanic rocks were observed on the North shore o fi the Pothole between L- B and L-12. The pyroclastic rocks are lapWU. tufifis with lithic firagments - 5mm in diameter.

Sericite schist is restricted to a zone between L-42 and L- 50 along the baseline. There the sericite schists are interbedded with chlorite schist*, Individual schist bands can be 5 J Ocm.

One outcrop o fi breccia was mapped at SOON 1-22. The breccia consi&ts o fi pale green siliceous, angular firagments in a blackish fiine grained siticeous matrix. It -ci not known ifi this breccia ifi ofi 'tectonic, or volcanic origin.

Page 5: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

CHERT ( MAP UNIT 5)

The. chert unit i* ie.pme.nttd by well banded and brecciated chert* that generally occur a* thin dibcontiJnuouA band* that are o^ten ApatiaMty oAAoc-tated with ^el*ic volcanic*. However, the chert* do occur interbedded with chlorite Achi*t.

Chert breccioA occur at l-U on the. Aouth Ahora o tf -the Pothole and on LtneA H and 3 0 on the tooth *hore o rf the Pothole. At both the cheAt biecc-uii ate oAAoc^ted wctn cWo-'Uxte A C-hiAt and fie.p'te^e.nt

to ihea'u.ng. Tne bA.ecCxca4 oA.e no-t

Banded and moAA-tue cheAt OCCUA to tne ^outh o fi the. ?othote. and eue/u/wheAe oAiocuated wttn ^ eJi&ic. votc.ani.cA. The. banding -t* de^-tned

by

A bed 0(5 weJUL banded. cheAt OC.CUA& interbedded with chiolite. at the. Ea&t end o fi the. showing between 1-30 and L-32.

o fi di*6ej)u.nate.d pyrite, and aMe.nopytiite..

PIABASE ( MAP UMIT 6 )

Concordant to ^ enttconco^dant diabase. bWUb are. very on the. property. The. unit ib 4.epte6ented at fiine. graine.d diabase., porphyritic diabase, and quartz diabase., ktt pKa6e6 a^.e moA&ive. and ioJum tieAibtant ridge*. Contact* with ho&t rock* are. not o^ttn exposed but chitte.d contact* have, b een ob^etved.

Tne diaba&e. only tocalty dibptaub a magnetic attraction wfu.cn a poon and erratic magnetic signature.. Pytute. and pyrrhotite,

06

GABBRO ( MAP UN/IT 7)

TTu-6 unit it, re*tricte.d to the. northeast corner o 6 the. grid. The. gabbro -06 coarse. gnaine.d, black, moA&ive. and Atrongty magnetic, from the. magnetic pattern the. gabbno occur* a* EaAt-Weit tre.nding AiW. or dyke*.

MONZOWITE ( MAP UNIT S )

Thi* unit i* very limited in distribution. It occur* a* a medium graine.d, e.quigranutar maA&ive. rock with minor alteration o 6

gUARTZ l/EINS ( MAP UNIT 1 0 )

Tne quartz vein* o^ economic intere*t occur along a zone, which trend* along the Aouth Ahore ofi the Pothole. The quartz vein* invade a very ^ii,*4Jie chlorite- sericite tchibt. There are three area* Oj{ expo^uAe; L -22 on South .ihoie 0(( the Pothole, L-24 on the South thore ol the Pothole and in a Aerie* o jj trenche* between L-2B and L-32. The*e eKpoAureA Apan a ] 050 foot Atrike length. Similar material ha* been located in ((-Coat at L - 1 2 on Aouth Ahore o^ lake, and b etween l- 1 0 and L -12 /ait

Page 6: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

1-22

The quantz vein it, 5 ' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin seams O fJ cht.orite. and clots o6 calcite,. The. quartz i* mineralized with disseminated pyrite, and chalcopyrite. - 1 1 by volumne. The. vein is concordant and trend* 062*7*5* N-verticdl.

kssay result*: Au A^ Width.005 oz/ton 5 '

.01 oz/ton

L-24

An B . 5 ' wide. .shear zone, with several injection* ofi quartz up to 2 .5' wii.de. The quartz i6 concordant with a very fiibsile chlorite sericite schist trending 065 c fBO cN - vertical. The quartz varies ^rom white to black depending on the amount o 6 included chlorite. Mineralization

diA&em pyrite and chalcopyrite - I I by volumne.

r.e*uJUU: Au A Width.01 02/ion X. 5'

.03 oz/ton

L-2S-to L-32

Trench " J: Tn^ Juk, the mo&t easterly expoiuAe, it conAidtb o^ a whitequartz vein - J ' thick with almost moA&ive band* O fJ arsenopyrite with minor, pyrite and chalcopyrite. The quartz i* concordant with the chlorite- sericite schist. Assay results indicate that the arsenopyrite is carrying the gold.

kssay results:

l Cu. Au. oz/ton Ag. oz/ton Width Remarks

.27 J 3 Grab Massive arsenopyrite

.005 W/P G^uib Quartz no sulphide,3/ .005 .03 Grab Quartz 1 -21 chalcopyrite

Trench " 2: A 9.5' wtcde quartz vein in contact with chlorite-sericiteschist on the north side. The south contact i* no-C exposed - The vein is concordant and trends 065 C J70 C N. The quartz carries no visable sulphides.

hssay results; Au Ag^ Width Remarks.005 oz/ton 9 .5' Sawien' quartz

W/P

Page 7: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

TAench #3; The quartz vein ho4 aw exposed width of, H (Jeet. HoweveA, watt rock ib not exposed on eitheA A-tde. The quaAtz it, white, with chiolite team and veAy iittie Auiphide. A Await incision ( ?) o f, greyish cheAt occurs at the. north end 0(( -the trench.

Assay resuits: Au oz/ton Ag oz/ton Width RemarksTrace . 03 IS' BaAAen quartz

.02 .OS Grab CheAt incision

T tench #4: The. vein spiits into two se.peAate. vein*, theAe. i* no expoAuAe between the. vein*. The. tooth vein i* concordant with chiorite-

tchibt which tAe.ndA 055 0 fveAtic.at. The. chiolite. i6 mineAatize.d with pynite. and chatcopyiite..

tieAuttA: Aa oz/ton Ag oz/ton Width

cite. Achi&t .06 .28 Grab Sch-t6t with pynite. S Chatcopynite.

WoAth Vein .005 W/P 5' QuaAtz with minox. chatcopynitt

South Vein Tw.ce. . 03 4 ' Qaahtz with - H chatcopyiite.

TAench #5; A 4 ' wide, quantz vein inje.cte.d confionmabty into chiolite, tchibttAe.nding O 55" J 60- 1 5 C W . AttnoA dib&eminated pyrite, and chatcopynite..

tieAuttt*: Au oz/ton Ag oz/ton Width RemaAfe-6

.02 .41 4' White, quantz and quaAtz tiich jjauttgouge with minox. pyrite S chalcopyrite..

A gAab tampte taken between -trench "I and tAe.nch *2 a -tAace oX, gotd dnom a Q*ie.y cheAt with dibt,eminate.d pyrite, and chatcopyiite..

The Ahowing* ex-tend oueA a t tAike. ttngth ofi 1050' with an ageAage tAend O jJ 0 65 0 f65 c -S0 0 N. The vein it o ^Aet between tAtncheA " 2 and *3 by a NoAih-Soitth trending ^autt. Hotiizontai dibpiaceme.nt being approximately 10'. Between -fienchw #1 and "2 the. ttAu.ctu.'ie. appeau to be. totde.d) it to the fatd witt piunge 45'f270 c .

QuaAtz

TheAe are two AepeAote occuAancei o X. QuaAtz fiioat on the. i ou-th -4-cde oj{ the. Phothote.

L-12: The quartz ib white and boM.en with minor chiorite.. HoweveA, viAabte. goid wa* (Jound by R . M-tddaugh at thit, tocation, fuAtheA investigation hoi not Aeuea^ed moAe (jAee goid.

Page 8: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Au oz/ton Ag oz/ton Width

.005 W/P G/iab Btwien quantz

L-10 to L-12: QuaAtz ^loat showing contact with chiolite.The. quantz it, conformable. and the. oiie.ntation 0 (J the. jtloat it, conformable. with the. AtMuUgnaphy. the. vein in ^loat ill cLppfioximateJty 6" wide. Wo

Gzophy&icaJt

A ^fjuKgate. magnztornzteA AuAve.y f,aHe.d to heZp deJUneate. the. tsie-nding AheaA zone.. HoweucA, it doe* outline, the. tsie.nd S width

Ae.veAal diabase, and gabbro

A ^na&eA-6ilteAe.d VLf-EM A tfivew wo* Aucce^&^uUt in tracing the. thlotiite.-AeAidte. AheaA zone, thich it* me. ho&t o^ the. ouAifieAouA quaAtz vein*. Two otkeA anomalies in the. Pothole, ale. unexplained. Ml otheA "land" anomalies aAe. in low twampy ground and aAe. probably coxtied by conductive. oveA bu/iden.

CONCLUSIOM

Ge-ophy&ical AuAve.yA and ge.ological mapping have. delineate.d a Ahe.aA zone, which tA.e.ndt* Ea&t-WeAt faom L- 32, along the, touth thoie. ofi the. Pothole, to L-16 and hence, through the. centre. O jJ the. Pothole, to 1-4.

Sampling o^ all exposed showing ha* been complzte.d and aA&ay neAvJttA ate. not 6u^icie.ntly e.ncou*aging to continue. e.xploMLtion at thib time..

Page 9: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

PH36

\

5

J 5

* 5̂

^ *

^- *^ chert ^"" ^

*lr -" '-1-PH 33 5

qtz.v.^ - " ̂ ̂ ^ ^ qtz.vein

^ ^- ^ ' Py-cpy ^^"5 ^^-^ PH35 ^^ __ ,^^

6 •^"c'hl.schist ^""PH^ -^ X PI H H 3 1

Pit 5 32

*

A- - , ^ PH 37 x" mf - ^ x N^' VOlC - "--- -N\ \ ^

j^r --•' j ' qt?-vfodw -- - - - -^: - chert *- q^L ^ Pyqtz.vein ^ - ~~ c hl. schV — ̂ CPV

^ - " Pit1 ospy"Jl o PH 27^^ 28

PH 30 2 9

" .-*SCALE s 20.

M60N

M60N

MAON

M20N

L100N

L-32

Page 10: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

QUEBEC: 183 RUE GAMBLE O., C.P. 665 - ROUYN, J9X 2RB -TEL: 1819) 762-3010

ONTARIO: 20 VICTORIA STREET. SUITE 606 - TORONTO. M5C 2NB- TEL: (416)366-3100

CERTIFICATE OF ANALYSIS

FOR Mr. Mac WatsonLynx Canada Exploration Ltd. 520 - 25 Adelaide Street East Toronto, Ontario M5H 1S3

LAB NO.

33,450

1

2

3

K

5

6

7

8

9

33.1160

33.462

^,Jl6l

33,463

4

5

6

7

8

33,469

SAMPLE NO.

26

7

8

9

30

1

2

3

H

5

6

7

8

9

40

1

2

3

4

45

GOLD OZ. PEN TON

0.01

0.005

0.005

0.005

Trace

0.01

0.02

Trace

0.10

0.0050.02

Trace

0.005

0.005

0.06

0.27

Trace

0.005

Trace

Trace

ILVEM OZ. PER TON

0.01

0.01

N.D.

N.D.

N.D.

0.03

0.41

0.03

0.10

N*D.

0.08

0.03

0.03

0.06

0.28

0.13

N.D.

N.D.

0.03

COPPERk

0.063

0.20

0.31 ,g

ZINC11

eUl l0 bU\O\|U

?tf-33

1-n J-S*'

t-** *\9-,Jtrf\USA4-2*

WHP Qt - ̂3

W 3W "3

di- scl.

?/^

ft-Urz^ A^W 2

^s, c \J{,

CM SeU,

r *c c i *K *-~

-(r v/tlt

9rU

/.*.fc* cafzi

z*k.?#--56

^-35-

cU.sci.

o^t t*^-11.'Ptf-'Sl

iv^lU C.12- (

cU. J.-ns^-% t-^c*-

at l**s'

c. IV*

\- L-2.

/t J- A,, i-u ck""'Se^'

- CdCo uci-

*s'

4-'

4-'

V*h-i

11 *\ Aa

*\t-*.Tk.O18'

/xCo- U * T*\ ,

Wlf.

.*l.

sw* J\i

Ir*.

/..t-

t.

i. -\**00-o

•e .

L- (t, J i.

^b-

Ct*O-i

a.

DATE

July 14, 1981CERTIFIED CORRECT •Wvil

vi JOT EtN ADJUSTED TO COMPIN-UNLf SS IT IS SPECIFICALLY STATED OTHERWISE COLD AND SILVER VALUES REPORTED ON THESE SHEETS H A VI.SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE ASSAY PROCESS.SAUF MENTION CONTRAIRE. LES ESSAIS POUR I'D R ET L'ARGENT, NE SONT PAS CORRIGES PUUR LES PERTES ET CAINS OUI SONT INHERENTS AUPROCEDED'ANALYSE.

Page 11: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

l HV/IITFF"}

QUEBEC: 1 83 R UE GAMBLE O.. C.P. 665 - ROUYN, J9X 2RB - TEL: (819) 762-3010

ONTARIO: 20 VICTORIA STREET, SUITE 506 - TORONTO, M5C 2NB- TEL: (416) 366-3100

CERTIFICATE OF ANALYSISFOR Mr. Mac Watson

Lynx Canr.da Exploration. Ltd. 520 - 2 5 Adelaide Street East Toronto, Ontario M5H IS3

LAB NO.

33,^70

1

33.172

(AMPLE NO.

i|6

U7

48

OOLD OZ. PCPI TON

0.005

Trace

Trace

SILVER OZ. PER TON

N.D.

0.01

N.D.

COPPER'K ZINC*

frl-W

loftw^-*/^ f̂

n-^-j

VUU-i-v

Lrl L-l

clt^ O-el

Tst./ie.U.tL

0.47 . ^tftl1 o -f .4J**t\

i ~Mz .

DATE

July 1*1, 1981CERTIFIED CORRECT

f^JL^f

UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BKN ADJUSTED TO COMPEN SATE FOR LOSSES AND CAINS INHERENT IN THE HRE ASSAY PROCESS. *""^-~-*^—XSAUF MENTION CON1RAIRE, LtS ESSAIS POUR L'OR ET L'AROCNT. NE SONT PAS CORRICES POUR LES PERTESET~GXlNS OUI SONT INHERENTS AU PROCEDED'ANALYSE

Page 12: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

52B14SE8813 2.4256 WEAVER

RECEIVEDNOV - 61981

MINING LANDS SECTION

GEOPHYSICAL REPORT

LAZAN PROJECT

CR00KEP PINE LAKE AREA

THUNDER BAYWININO DIVISION

E Q E NNOV 31981

AU

By. Randy Ciowte.y

Fo/t: Lynx Canada Ex.ptoMLtLon* LJunvUttd

Page 13: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

LAZAN PROJECT NTS 52B/M

Ae.poAt AammoAizeA the, AeAottA 0 (5 a magnetic and l/LF-EM AuAve.y completed on the pAopeAty in MaAch 1981.

INTRODUCTION;

Tne pAopeAty conAi&tA o (5 16 cont^gnoaA, unpatented mining claim* numbered OA

T8 519657TB 557*36 - 8 41 inclusive. TB 557*72 - *76 inclusive. TB 536052 - 055 inclative.

The. ge.oiogic.at AuAve.y wa6 completed oveA ait OA poAt 0 (5 the. following S claims.

TB 5 19657TB 557*37 - 8 40 inclusive.TB 557874 - 876 incla&ive.

LOCATION ANP ACCESS;

Tne pAopeAty itt censed on a AmatC take. - The. Pothole. - .8 fern noAth ofi CAooke.d Pine. Lake, in the. Toumhip 0 (5 WeaueA (M-2066). Tne pAopeAty ib within the. Vi&tAict o (5 Rainy R-tveA and the. cJtaimb oAe, Ae.c.oAde.d in the. ThandeA Bay Mining Division,

Acce6A to the. pAopeAty it, by ba&h Aoad ^Aom Kawene (On Hyway 6 33) to a landing on the, Aoath AhoAe. ofi CAooke.d Pine. Lake, at 9 1" 05'W 4 t c 46 'W. Then, by boat to a point on the. noAth AhoAe. 0 (5 CAooke.d Pine. Lake., ,8 km tooth 06 the. Pothole..

PREVIOUS WORK;

Wo pAevioa* woAk ib Ae.c.oAded in the. awe6Ament (J^deA ojj the. Mini&tAy 0 (5 \iatuAat Re*ouA.ceA in ThundeA Bay, Howeve/i, ^n 1963 WoAanda EzploAotionA Co. Limite.d caAAie.d oat UjniteJd tAe.nc.hing with one, Aampie Ae.poAte.dly A&tuAning . 3 oz/ton/9' ( W. Mo-tenooAe peMonat communication). WuweAoaA o-dd g/i^d ^cneA and c^um poAtA wcAe located ^n the fiieJtd, TheAe. i6 no ev/cdence 0(5 dAifJU.ng on the. pAopeAty.

The, pAopeAty had been oueAjJ-town by two eJ.e.ctAomagnzticfmagnztic 4aAve.y4, keAodat completed a AuAvey ^o/i R^.o T-cn-to and QaeAtoA SaAve.y* completed a AuAvei/ (Jo/i the Mini&tny o j{ NatuAol Reioa^ceA OA pa^t otf the laAgeA Att.fa.fean MAboAne, 6uAve.y in 7 9*0 (Map *052J)

Page 14: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Wo EM conductor weAe detected on the. pAopeAty howeveA, both AuAveyA detected a bAoad EoAt-WeAt frLe.nc.h4.ng magnetic, anomaly neoA the South end o fi the. pAopeAty.

A .AhoAt description o 6 the. pAopeAty OCCUAA in the OGS RepoAt J79; Geology otf the. CAoofeed Rote Lafee AAea, By J. PiAx.e.

REGIONAL GEOLOGY;

The pAopeAty OCCUAA within the, Wabigoon SubpAov-oice Of( the SupeA/toA PAov-tnce appAox^mate^y . Bkm NoAth 0(J ^fie Quetico Faatt

boundhy oft the. Wabigoon and Que-tcco

Tne Wabigoon Subp/tou^nce -ci an E-W -fiencnxng beW 0({ volcanic locfe* w^t^i leA&eA Ae.dUme.ntaAy /locfe^. Theae

nave been -cniwided by wa^c ^:o a^iamaicc dt/fee^ and kWL and ptutonA. Me-tamoApfo/cdm Aange4 ((Aom ^he ghe.e.nAc.hiAt to

Tne (Jaeitco Subp4.ov4.nce ^CA dominantty comp-^cded 0({ meta-TheAe. tusibltiteA oAe now Aep^e^en^ed a* A,nttAtayeAe.d peJiitic.

[o^te.n QOfimti^eAou^} bandi and cooAiCA gAax.ned pAomm^tcc band*. T/ie Qae^tLc.o Subpiovince. no* a-tio been -cniAuded by ma^c -to uttAomafcc and by ^eJUic. pluton*.

The. Qu.ztLc.0 fautt (Jo^mA a noAAow, highly defJoAmed, andzone a&wg the. NoAtn AnoAe otf CAoofzed P4.ne Lafee (P-c/ute J97S).

PROCEDURE AW THEORY OF OPERATION;

Tne EM AaAvet/ WOA completed t^ttttzing a CAone Radem ULF-EMn^xt Jut* a one. man portable. EM unit utilizing low ^e.que,nc.y

wave6 emitted j{Aom miUtaAy iAanAm-ttieAA A-tAxated aAoand -tne g-Cobe. The. A ouAce (JoA ike pAesenX -AuAvet/ WOA SeaitCe Washington, utilizing a frequency 0(( /S. 6 KHz. Thib ' jjAequency -CA ^ow w. A. -t. Aad-co A tationA but veAy high w . A. -t. o-tneA EM- g e.ophy4ical

The. Radem meo4uAe4 ^:ne ang^e jjAom the. vertical 0 (J -t^ie iecon- fiietd ge.neAate.d by conduc-ttve bodies that oAe Aub/ec^ted -to -the

piimatiy fiieZd, The. "cAoAAoveA" OA zeAo po-tnt ^A diwctly oveA ^ne cuAAen-t ax-cA o fi the. conductor. The. angle, ib meoAaAed by a clinomtteA at the. minimum ^ieJtd Atsie.ngth.

BecaaAe otf geologic no^Ae component wfutcfi -CA caaAed by, -t/ie /u.g^i f^Aenquency employed, i^ie data naA been AilteAtd. Known OA tne FAOACA F^tteA method, the. data manipulation tnanAfotim noiby date -cnto -CeAA no-6Ay contoAab^e data. The. fiilteAing alto

o anomalies.

The. magnetic. ^uAvey WOA completed utilizing a Scu.ntAex MF- 2 iJ&ugate magnetometeA. Thib type. 0 (( magnetometeA emp^oyA a SatuAab^e coAe 4enAoA ne^d -tn a yeAt-cca^ dine.ction to meaAuAe veAttca^ -tntenA-tty wctfc an elective * e.nAitivity O jJ AeveAo^ gammoA. Tne /tnAtAument g-tveA a Aeadtng diAectXy -tn gamma*.

Page 15: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Von ^ieJtd Aunve.ying the. needle on the. mcteA ib Act at a heading at a chosen boAe. 4 tot*.on in a. "non-anomotout" anea (fan th-iA *unve.y the 6o6e station wo* located at L28/00) . At AucceiA-tve the <LnAtnu.me.nt -i* le.velle.d and the. incneoAe. on dccneaAe. in the. magnetic ^ieJid w.n.t.. The. bate. Atation iA nead. Magnetic contAol wo* maintaine.d by the. tune. aveAaging method. A boAeJtine. Aiitive.y wtti completed and the. di^eAe-nce. betuie.e.n the. two leading* at the. Ataiting point u, u*e.d to adjust the. value* at each check in point. Magnetic, variation i* -taken to be. constant oveA time..

Magnetic, variation* ate caaied by di^eAe.nc.e* in the. magnetic AULAe-ptabitity o 6 the. lock* faom one. point to anotheA b ecaafie o (J variation* in the. quantity ofi magnetic mineAotb in the. nock. The. con/touied data a&Aibt in determining the. location, e.x.te.nt, ge.omeJxy and geology ofi an anomalous anea.

RESULTS;

The EM AuAvzy dtte,cted numeAouA conductor. \tl conductor, except the ma-tn concfuctoA. thnough the. centre o ^ the. "Pothole." one. in low Auxunpy gnound and one, pnobably caaAed by conductive oueAbu-tden.

The ma^n conductor through the. cenfie o (f the Pothole, 1-4 to L-22 i* the. extention o ^ the. weak conductor awoc-tated with the iheoA zone wh-cch hoAti, the ouni^eAouA quantz vein* at L 30/IN. Th-c5 anomaly ik the. undeAwateA extent^on 0({ the AheaA zone exposed at L-30, L -18 and L-22.

The. magnetic Aunve.y wai not helpfaM. in ^untheA delineating the. main EM anomaly. The/te /66 no coi/ie-Cat-ton between the magnetic* and the. mapped A hean zone, on between the ma-tn EM anomoly and the.

The. magnetos, *unve.y deJU,neate.d many "buWte,ue." magnetic anomotieA which one. coincide.nt with motive, diabase, which contain* minon dib*minate.d pynnhotite.. The 4t^.ong magnetic high* in the. nonthea*t conneA o (J the gnid one. coincident with n\a**i\ie. coanAe. gnaine.d gabbno.

RECQMMEWATIM;

Go-Cd value* one. a**ociate.d with Aulfiide, mineralization*, e.*pe.cialJty aA*e.nopynite.. An induced po^o-'u.zatx.on *unve.y would deteAmine. ifi theAe. i* *ul^ide. mineAalization a**ociate.d with the. Ahean zone. coincide.nt with the. EM anomoly between L-4 and L-22 ..

/J ! A

Randy

Page 16: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

52BMSEeen3 2.4256 WEAVER 030

TIE POTHOLE GOLD OCCIRISIXS

NTS 52 3 1ii

Phantom L:xlcration Services Ltd.

Page 17: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Location

The Pothole Gold Occurrence is located on the eaot shore of

The Pothole lake appropriately 0,8 Ion. north of Crooked Pine

lake in the township of leaver in the Thunder Bay inining di

vision. This sho",7ing and the iMioediate surrounding area are

covered by ciirbeen unpatented irlning claims numbered 5l?op7,

53^052-55 inclusive, 557o36-l|1 inclusive and 5S7&72-76

inclusive s talced by 'J. D. Jorehouse, D. Galley, and D. hetrunka

of Thunder Bay and now owned by Laaan Explorations and

Develoornents Li:iited of Thunder Bay, Ontario

Access

The :.x)st economical and probably the siraplest access is

provided by highways #11 and #633 to Kawene, Ontario located

on the Canadian National Railway. Several roads lead fror.i

here to the south shore of Crooked Pine lake. Boat or snot;

iiiachine, depending on the season, provide access to the north

shore of "ihc ?.:J:c, 0.8 ion. south of the S.IO\F^YJ.

Tiie .-.utiior visited the shoT.;ing on October 27 this year with

./.D. i.orehouse. Lir.iited prospecting and r.iapping was carried out

in addition to exanining the showing in an at'tewpt to better

Page 18: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

assess the economic potential of the occurrence and surrounding

area.

Previous

;;oranda Exploration Limited of Thunder Bay, Ontario did sone

trenching and coupling of the showing in the fall of 19o3 and

although no written confirmation '-ras found it has been stated

that one channel sanple did assay 0.3 oz. per ton gold across

nine feet.

A grab sanple talcen by J. D, Ilorehouse in 1972 assayed by

the jinistry of natural Resources of Ontario contained 0.11; oz.

per ton and 1.U6 02. silver per ton.

daises pirie and assistants mapped, the area in 1975 and

iiientioned sampling a snail pit on the east shore of The Pothole

lake. Assayed by the Ministry of Xatural ?.esources of Ontario,

the sa:.:ple contained 0.11 oz. gold per ton, 0.2p oz. silver per

ton and C. 73,3 copper. The description cf the area does not con

cur exactly with what the author saw. Either the Most easterly

pit wes the origin of the grab sci-ple and the other trenches were

not seen or the grab was from a pit even nore easterly than what

the author saw.

Discussion

On the south east side of The pothole IrJce, five trenches,

located at various intervals along the quartz vein system were

Page 19: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

-3-

exav,iined. This vain system, which is easily traceable for a

distance of 2?0 feet strikes north CO0 east and dips vertic;:!

to steep north and is associated with a shear aone. This

shear zone is coincident with a thin (10-30 feet) discontinuous,

tuffaceous, felsic r.ietavolcanic horizon located between two, more

nafic metavolcanic sequences. This horizon probably represents

a quiescent period between two more active volcanic phases.

Subsequent faulting, probably contemporaneous with later

felsic intrusive emplacements, would be concentrated along this

felsic horizon due to its intervolcanic origin and its competent

nature.

Appro;dLmately 1900 feet west of the showing, on the south

shore of the lake, visible gold lias found in a seemly barren

quartz material. There is some doubt as to whether this material

was found in situ. If it is float, it did not cone far and is

definiately related to the east -.rest shear zone.

On the southwest shore of the lake, apyro:dmately 2300 feet

west of the showing, a gossam with associated quartz veins was

located.

Quartz stringers with r.iinor sulphide mineralization were

also noted at several locations along the south shore of the l^:o

between the showing and where the visible gold was found. The

nature and geological environment of these stringers suggest that

the south shore of the lake is fault controlled and that a large

portion of the quartz vein system is located just north of the

south snore in the lake.

Page 20: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

-U-

. aneraligation

The quartz veins in the trenches contain pyrite, up to

2/j chalcopyrite, frequently associated with malachite and snore

rarely azurite, and arsenopyrite. The amount of arsenopyrite

seeros to increase to the east as the most easterly pit contains

stringers and veins, up to 3 inches wide, of massive arsenopyrite,

Since limited prospecting revealed several areas of

interest located on what is probably the western e:ctention of

the favourable horizon, further detailed prospecting should be

carried out all along this structural trend.

Further trenching 'and careful sampling of both new and old

trenches in the siain showing area is warranted to establish a

clear picture of gold and silver values.

Detailed VL? and proton magnetometer surveys should be

carried out over the rineralized sheared horizon to accurately

locate it and to test it fer areas of greater conductivity.

These areas should indicate zones of greater sulphide con

centration and hence greater gold and silver values.

It is suggested that the grid be oriented such that the

baseline has a azr,iuth of 800 . The wing lines should extend at

least 100 rioters north and south of the baseline and be at

50 rater intervals along its one id-lor.ietsr length. Picket

Page 21: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

-p-

stations at 20 neter intervals are suggestod although initial

survey results i;iay indicate that tighter intervals are warranted.

Upon completion of the geophysical surveys, surface wo ri:

where feasible should be attempted to better assess any conductive

sones located.

If encouraging results are obtained fron the above :;ork,

diar.iond drilling should be undertaken to assess the economic

potential of the aones at depth. /J though :nininur. amount of

drilling should be done to test all targets outlined, the

Lota.! anount of drilling unaertt-lcen is dictated by constantly

reevaluating the economical feasibility of the project.

Costs

Belovj are estimates of the costs of the above work.

Trencnzng and sampling

Assaying

Linecutting

Geophysical surveys

Diamond drilling

Geological consulting

#100.00 per :.ian day plus

^6-7.00 per sar.i.le per elejoent

3200-2^0.00 per lei.

0^0.00 per iuu. per survey

^25.00 per ft.

v?1 50.00 per day

i;ove2nber, 1960 Hi D. :-iddaugh

Page 22: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

JEIEHE-JCES

pirie, Janes

1?7o: Geology of the Crooked Pine Lake Area, District of Rainy River; Ontario Geological Survey ftenort 73 p* Accompanied, by I-jap 2li05, scide 1: 31oCO (1 inch to -a

Page 23: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

3gM W

File.

Ontario 52BHSEeei3 2 .42SG WEAVER 900o

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey (s) Magn&t-cc and Elecfriomagne&.c Township or Area TOKMArUp 0 ^ WwveA_______^_Claim Holdcr(s) Lazan Exploration 6 Ve.vetopme.nt Ltd

136 Maplewood S . Thund&i Bat/____

Survey Company_________________;—————^^-—— Author of Report Rqndy Cxowlzy_______________ Address of Author 335 Ad&tcu-de. Apt 602 1 Tkund&i BayCovering Dates of Survey MaAch to OctobeA 1981

(linecutting to office)

Total Miles of Line Cut -. 10.7

SPECIAL PROVISIONS 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———Other——————

DAYS per claim

in

Geological.

Geochemical.

AIRBORNE CRE1DITS (Special provision credits do not apply to airborne surveyi)

Magnetometer. .Electromagnetic{enter days per claim) / j

JC. Radiometric

16 1 7 9*7 SIGNATURE:

Res. Geo!., .Qualifications.Previous Surveys

File No. Type Date Claim Holder

pa..-uu U

i•ft

l

MINING CLAIMS TRAVERSE^ List numerically

..IR.......(prefix)

IB

.519.657...?!(number)

557*37^

..T?.. JB

TB

J.?..

l.?..

TB

557*3*...

557

.557*75....

557*76 .'

THUNDW? BAYMINING DWIMON

TOTAL CI.AIMS.

837 (5/79)

Page 24: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

GEOPHYSICAL TECHNICAL DATA

Nl) SURVEYS^ If more than one survey, specify data for each type of survey

Nuber ofStation in,,™.!~ ' -

Profile scale __ MA

Mag. 54Q t/LF 5 4025' t/LF

Numbcr o f RcadingsT . in , .

r o

CoM our interval Mftft. 1 00 gamPA l/LF 10. 2 0, 40

yH W

Instrument Sc/uttfr&x MF2Accuracy — Scale constant 7 gamma

Diurnal correction method T-OK6.

Base Station check-in interval (hours)___2Base Station location and value L -2B/00 1550

u*—4

H Wy,o

O

H W W

Instrument Chone. Racfpjti l/ L F- EMM/A

MA

Coil configuration

Coil separation —

Accuracy——Method: Q Fixed transmitter

Frequency___U.6 Jff/7 .Sgfl/^/g-

C! Shoot back Q In line Q Parallel line

Parameters measured.{specify V.L.K station)

H

Instrument

Scale constant

Corrections made.

O Base station value and location

Elevation accuracy.

H

Q w

Qy.

Instrument -——.—.—--——— Method Ell.Time^Domain

Parameters - On time ——.— — Off time ^^- Delay time- Integration time

Power.

Electrode array————— Electrode spacing ———

Type of electrode -——

Q Frequency Domain— Frequency ^—-^^

—. Range ________

Page 25: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Instrument____________________________________..______ Range _. —.—.-Suwcy Method ________..__________________..________.__.....__ ,.^...,..^

Corrections made.

RAD1OMKTR1C

Instrument.Values measured .

Energy windows (levels) ———-—-———^—.-—.—-.^.-.——..————————————.——

Height of instrument_____________________________Background Count

Size of detector_______________________.—————..———————-——————..

Overburden___________________________._______—,—...—.—.———--—(type, depth - include outcrop map)

QT1JKRS (SEISMIC, DRILL WELL LOGGING ETC.)Ty p c o f sur ve y ____________________.___._______-_— - __.—- -_-. ——— Instrument____________________________.——-——.-—^—————-——-——^—

Accuracy—^——--————-———-——-——————————-——-——-———----—-————-——Parameters measured ——--—————---—--—-——----—————-^——————————.——-^.

Additional information (for understanding results).

Type of survey(s) Instrument(s) ^

(specify for each type of survey) Accuracy__________________

(specify for each type of survey) Aircraft used _____________-,.__ ————.^-^————^-—^—~.

Sensor altitude.

Navigation and flight path recovery method _-,.______

Aircraft altitude___________________________.______Line Spacing.

Miles flown over total area___.___.________-.________Over claims only.

Page 26: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.

Total Number of Samples. Type of Sample.

(Nature of Material)

Average Sample Weight-—————— Method of Collection—————————

Soil Horizon Sampled — Horizon Developmenl-. Sample Depth.^————

Terrain-^————--——

Drainage Development———————————— Estimated Range of Overburden Thickness.

ANALYTICAL METHODS

Values expressed in: per cent p.p. m. p. p. b.

a aa

Cu, Pb, Zn, Ni, Co, Ag, Mo, As,-(circle)

Others —————————————————^^^^

Field Analysis (.Extraction Method.

Analytical Method-

Reagents Used-—-.Field Laboratory Analysis

No. —————————.

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

Mesh size of fraction used for'analysis^——

Extraction Method.

Analytical Method.

Reagents Used——

Commercial Laboratory (- Name of Laboratory-—

Extraction Method.——

Analytical

Reagents Used

.tests)

-tests)

-tests)

General- General

Page 27: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

DUJ

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survcy(s) -Ge.olog.aial

LUU LU C*

CO l3*. O XL O

Township c

Claim Hold

Survey Con

Author of ]

Address of

Covering D

Total Miles

SPECIAL CREDIT

ir Area . TcM\^lfU.p o^

cr(s)-.±a.za.n. ExploreWaaueALtLon t, Ve.veJtome.nt Ltd

736 Maplewood S. ThundeA Baynpany*cnort Randy Cnowlzy

I " "

Author 335 Acfe&ude Apt. 602, TkundeA Bayales of Survey June

of Line Cut JO

. PROVISIONS 5 REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

to October 7 987(linccutting to office)

7

DAYS,, i-i Per claim Geophysical

--Rlf'rtrnmagnrtir

— Macrnrtnmelrr

— R}iHirim''(rir

-Othf-r

Geological 40

nrorhrrniral

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetome

DATEi&Cii

Res. Geol.^ Previous Su

File No.

ter F,)rrtrnmapnetic Radinmrtrir(enter days per claim) l ] A AJ ir i-jbeA 16, 7 987 SIGNATURE: rfW/vwA A/w^^A . '

Author ofVReport or AgV^

\ 'J

Qualifications

rveysType Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

TB 579657(prefix) (number)

TB 557837

TB 557838

TB 557839

TB 557840

TB 557874

TB 557875

TB 557876

THUNDER BAYMlNINO DIVIOIOH

jfij E D E 1 V E p......... . KW.................................t.*i

•f^ftitftiltil^ili^ Si4'R)B

TOTAL CI .AIMS 8

Page 28: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

GEOPHYSICAL TECHNICAL DATA

J-'KPtlN]) SURVEYS^ K m ore lli.iii one survey, specify d;ila for each t ype of survey ^^

WNiimber of Stations __________________________Number of Readings —————-—-—-————

Station interval ______________________________Line spacing.

Profile scale__________________________________________Contour interval.

-j. Instrument

Wx,o

otfH(J M

Accuracy — Scale constant

Diurnal correction method.

Base Station check-in interval (hours).

Base Station location and value ———

^ Instrument H

Coil configurationd Coil separation -—--^^^——————-—-^——————-————-——--^^-—-.—^-——--———^^—..——.

Accuracy ^^^.^—-——————^^^^^^^^——^——————^-^^-^-^—^—^—^-.—^—^—^^.^—^^^^^^^Method: CD Fixed transmitter CH Shoot back EH In line CH Parallel line

Frequency _______________________________.. _____.^^^-^—^————————^—^^^—^———{specify V.I..F. station)

Parameters measured—^^^^^———-———-——.—.—-.——^—————^——-————.-————...-—————-——^^——

Instrument

Scale constant

Corrections made.

PP-l

Base station value and location

Elevation accuracy-

InstrumentMethod D Time Domain D Frequency Domain

i*"'

H Parameters - On time ___________________________ Frequency _____

N ^ - Off time _______________________' Range ^. H

— Delay timeL.j'

If)Power.

— Integration time.

WuElectrode array.

Electrode spacing ———

Type of electrode ___

Page 29: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

SKKI'J'OTKNTJAK

Instrument___________________________________________ Range.

Survey Method ______________________________..^——————————

Corrections made.

RADIOMK'J'RIC

Instrument ———-

Values measured .

Energy windows (levels)-——--—————^—————^—^^—^^-^^-.—-.—-^^————^——.

Height of instrument______________________________Background Count.

Size of detector^^^^___________^^___^^-^^^---^^^^^^^___^___^^_^^^.^__

Overburden ̂ ————-—————^—--^.^———-——————————-———-—-^-^-^^^^^^^—--——(type, depth — include outcrop map)

OTIIKRS (SKISMIC, J)R]KK\VKK1, LOGGING I'/J'C.)

Type of survey—-————^—.—^-—————————-

Instrument -———^—^^^—————^——^-^———

Accuracy____________________________

Parameters measured.

Additional information (for understanding results).

AlRBORNKSimVKYS

Type of survey(s)————

Instrument(s) ————-(specify for each type of survey)

Accuracy—————.—.——--..——^^^—(specify for each type of survey)

Aircraft used————^^^—^^-——-—-.-——-^————————.———..———

Sensor altitude-

Navigation and flight path recovery method.

Aircraft altitude__________________________________Line Sparing

Miles flown over total area___________________________Over claims only.

Page 30: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

GEOCHKMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.

Total Number of Samples. Type of Sample.

(Nature of Material) Average Sample Weight———^—-—

Method of Collection,—^——^-.——-

Soil Horizon Sampled- Horizon Development-

Sample Depth——-—— Terrain^————^^^

Drainage Development-.——-——————

Estimated Range of Overburden Thickness.

.ANALYTICAL METHODS

Values expressed in: per cent p. p. m. p. p. b.

DnD

Cu, Pb, Zn, Ni, Co, Ag, Mo, As,-(circle)

Others—————^-—.——^-——————————Field Analysis

Extraction Method.

Analytical Method- Reagents Used-——

- Field Laboratory Analysis

No. (-^^^-^——

SAMPLE PR EJ'AR ATJON(Includes drying, screening, crushing, ashing)

Mesh size of fraction used for analysis -———.

Extraction Method. Analytical Method -

Reagents Used——-

Commercial Laboratory (_ Name of Laboratory-— Extraction MpfhnH

Analytical Method ,——

Reagents Used —————.

.tests)

-tests)

-tests)

General- General .

Page 31: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

1983 06 14 2.4256

Mrs. Audrey HayesMining RecorderMinistry of Natural ResourcesP.O. Box 5000Thunder Bay, OntarioP7C 5G6

Dear Madam:

RE: Geophysical (Electromagnetic 4 Magnetometer) and Geological Survey on Mining Claims TB 519657 et al In the Township of Weaver

The Geophysical (Electromagnetic 4 Magnetometer) and Geological Survey assessment work credits as listed with my Notice of Intent dated May 20, 1983 have been approved as of the above date.

Please Inform the recorded holder of these mining claims and so Indicate on your records.

Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: (416) 965-1380

D. K1nv1g:mc

cc: Lazan Exploration and Developments Ltd 136 South Maplewood Street Thunder Bay, Ontario P7E 262

cc: Resident Geologist Thunder Bay, Ontario

Page 32: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Ministry of"""^•"4 Y^JY N atural

Resources Ontario

1983 05 20

Your file:

Our file: 2 .4256

Mrs. Audrey HayesMining RecorderMinistry of Natural ResourcesP.O. Box 5000Thunder Bay, OntarioP7C 566

Enclosed are two copies of a Notice of Intent with state

ments listing a reduced rate of assessment work credits

to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain the

other. In approximately fifteen days from the above date,

a final letter of approval of these credits will be sent

to you. On receipt of the approval letter, you may then

change the work entries on the claim record sheets.

Yours very truly,

E.F. AndersonDirectorLands Administration Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM?A 1W3Phone: 416/965-1316

D. K1nv1gXmc

Encl:

cc: Lazan Exploration and Developments Ltd. Weaver Township

cc: Mr. 6.H. FergusonMining 4 Lands Commissioner Toronto, Ontario

For further Information, If required, please contact Mr. F.W. Matthews at 4167965-]380

845 (6/79)

Page 33: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Ministry ofNaturalResources

Ontario

Notice of Intent

for Technical Reports

1983 05 20

2.4256

An examination of your survey report indicates that the requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on his record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.

If you are of the opinion that these changes by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.

If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.

If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days" method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted direct to the Lands Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked will be issued.

816 (82Y5(

Page 34: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Ministry ofNaturalResources

Technical Assessment Work Credits

File

2.4256

1983 05 20Recorded Holder

LAZAN EXPLORATION i DEVELOPMENTS LTDTownship or Area

WEAVER TOWNSHIP

Type of survey and number of Assessment days credit per claim

Geophysical

Electromagnetic

Magnetometer

Radiometric

Induced polarization .

Section 86 (18)

40Geological

Geochemical

Man days Q Airborne

Special provision 1*3 Ground

Mining Claims Assessed

days TB. - 557838 557874 to 76 Inclusive

days

days

days

days

days

days

D

D

[K] Credits have been reduced because of partialcoverage of claims.

CD Credits have been reduced because of correctionsto work dates and figures of applicant.

77(lfi)Special credits under sect ion 3 for the following mining claims

30. .Days Geology

TB. - 559657 557837 557839 - 40

No credits have been allowed for the following mining claims

n not sufficiently covered by the survey L l Insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 86(181-60:

828

Page 35: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Ministry ofNaturalResources

Technical Assessment Work Credits

Ontar

File

2.4256

1983 05 20Recorded Holder

Township or Area.A7AN FXPLORATION b DEVELOPMENTS LTDWEAVER TOWNSHIP

Type of survey and number of Assessment days credit per claim

Geophysical

Electromagnetic

Magnetometer ^

Radiometric ——

Induced polarization ,

Section 86 (18) —

Geological ^———

Geochemical

.days

. days

.days

.days

.days

. days

. days

Man days LJ

Special provision Cjj

Airborne [j

Ground [}3

LXI Credits have been reduced because of partial coverage of claims.

d Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

TB.- 519657557837 - 38557874 to 76, Inclusive

Special credits under sectiona or the following mining claims

15 Days E.M& Mag.

TB. - 55/839 - 40

No credits have been allowed for the following mining claims

LI not sufficiently covered by the survey LJ Insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 86(181-60:

828

Page 36: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Ontario

Ministry ofNaturalResources

Notification of recording

of assessment work credits

Lands Administration Branch

Mining Lands Section

Ministry of Natural Resources

Room 161 7, Whitney Block

Queen's Park, Toronto

M7A 1W3

RECEIVEDOCt 2U981

MINING IANDS SECTION

Date of recording of work: ^ .... O ctp.be r 8., _ L9.8.

Recorded holder:, AazaJ\ E^ ^^———^

Address ' ?6 South Map l ewood Street, Thunder Bay, Ont. J5? E 2G2

Township or Area: , ,. Wea V er ̂ To W.QS i h ,LPL

20

20

Type of survey and number of Assessment days credit per claim

Geophysical

Electromagnetic__________________days

Magnetometer__.^^

Radiometric __.- ....

Induced polarization —

Section 86 (18)- —Linecutting St GeologicaL

Geochemical —-—

40

Man days L l

Special provision W

Airborne LI

Ground k i

Mining claims

TB5I9657 TB557837-40 incl TB557874-76 incl

Notice to recorded holder:

PI Survey reports and maps in duplicate be submitted to the Lands Administration Branch, Toronto with in 60 days from the date of recording of this work.

L l Reports and maps are being forwarded to the Lands Administration Branch with this letter.

(^ -c-t -X -^Ji+J

Mimng recorder

c.c. Lazan Exploration # Development; Ltd., l 36 S. Map lewood St. Thunder Bay, Ont.

Randy Crowley, 335 Adelaide St, #602, Thunder Bay, Ont.

Page 37: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Ministryoi GeotechnicalReTces Report

Ontario Approval

Mining Lands Comments

To: Geophysics

Comments

Approved f) Wish to see again with correctionsDate Signature)

To: Geology- Expenditures

Comments

.["J Approved j ] Wish to see again with corrections

Date Signature

To: Geochemistry

Comments

l j Approved [ ] Wish to see again with correctionsSignature

j [TO: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)

1593 (81/10)

Page 38: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

1983 03 17 2.4256

Lazan Exploration Development Limited 136 Haplewood Street South Thunder Bay, Ontario P7E 2G2

Dear Sirs:

RE: Geophysical (Electromagnetic 4 Magnetometer) and Geological Survey submitted on Mining Claims TB 519657 et al 1n the Township of Weaver.

Thank you for answering our letter dated February 21, 1983. However we already have all this data on file. We require a set of V.L.F. EM maps showing the raw data plotted at each station to accompany the Fraser filter maps previously submitted by March 21, 1983.

Enclosed 1s the material received In this office on March 2, 1983.

For further Information, please contact Mr. F.W. Matthews at 416/965-1380.

Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380

A. Barr:se

Ends:

cc: Mr. Randy Crowley Rexdale, Ontario

cc: Mining Recorder Thunder Bay, Ontario

Page 39: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Ministry ofNaturalResources

Your file:

c— RECEIVED

MINING LANDS SECTION

February 25,1983

MEMORANDUM TO:

Land ManagementRoom 6450 Whitney BlockQueen's ParkTORONTO , OntarioM7A 1W3

Attention: E. F. Anderson

SUBJECT; Geophysical s Geological Survey Mining claims TB519657

Please find enclosed information for the above survey as requested in your letter dated December 9,1982.

A.M. Hayes (Mrs.)Mining RecorderThunder Bay Mining Division

AH*ca

^l

*'-* Y/i"-'"

.r

Page 40: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

1983 02 21 2.4256

Lazan Exploration fi Development Limited 136 Maplewood Street South Thunder Bay, Ontario P7E 2G2

Dear Sirs:

RE: Geophysical (Electromagnetic and Magnetometer) fiGeological Survey submitted on Mining Claims TB 519657 et al 1n the Township of Weaver,

Enclosed 1s a copy of our letter dated December 9, 1982 requesting additional Information for the above mentioned survey.

Unless you can provide the required data by March 7, 1983 the mining recorder will be directed to cancel the work credits recorded on October 8 t 1981.

For further Information, please contact Mr. F.M. Matthews at #16/965-1380.

Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380

D1ane W1ce:sc

Ends:

cc: Mr. Randy Crowley Rexdale, Ontario

cc: Mining Recorder Thunder Bay, Ontario

Page 41: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

1982 12 09 2.4256

Mr. Randy Crowley 2777 Kipling Avenue #505 Rexdale, Ontario M9V 4M2

Dear Sir:

RE: Geophysical (Electromagnetic and Magnetometer) and Geological Survey submitted on Mining Claims TB 519657 et al 1n the Township of Weaver.

We have not received a set of V.L.F. EM maps with the raw data plotted to accompany the Fraser filter maps you submitted for the above mentioned survey. On receipt of these maps a statement of assessment credits will be Issued.

For further Information, please contact Mr. F.W. Matthews at 965-1380.

Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380

A. Barr:sc

cc: Mining Recorder Thunder Bay, Ontario

cc: Lazan Exploration A Development Limited 136 Maplewood St. South Thunder Bay Ontario P7E 262

Page 42: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

Ministryof GeotechnicalResources R eP0rt

Ontario Approval

File

Mining Lands Comments

f o: Geophysics

Comments

\SL r /WtX-Cx*-o

Approved Wish to see again with corrections

ITo: Geology - Expenditures

D

Comments

\J\ Approved | j Wish to see again with corrections

To: Geochemistry

Comments

Approved Wish to see again with corrections

To: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1:

1593 181/10)

Page 43: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

t.'/vM',,-.' Gcoiccimicaln ' lUir '1 ' Reportw.-sources '

Ontario Approval

V, ir. "" " J l^ y* s i J

Mining Lands Comments LQ.

To: Geophysics

Comment*

- U^^i- ~

LJ Approved Q Wish to see again with correctionsDUB- Signature

To: Geology - Expenditures

Comments

] Approved i to see again with correctionsDate Signature

To: Geochemistry

Comments

[ l Approved |~| Wish to see again with correctionsDate Signature

l ITo: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)

1003 itn/io)

Page 44: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

1982 07 82 2.4256

Mr. Randy Crovley2777 Kipling Avenue 1505Rexdale, Ontario

Dear Mr. Crowley,

RE: GEOPHYSICAL (ELECTROMAGNETIC fi MAGNETOMETER) AND GEOLOGICAL SURVEY SUBMITTED ON MINING CLAIMS TB 519657 ET AL IN THE TOWNSHIP OP WEAVER

Enclosed is an Electromagnetic and Magnetometer nap (In duplicate) for the above survey. Please provide a signature on two of the naps and claim lines and numbers on all four.

When completed please return them to this office.

Yours very truly

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380

J. Skura:sc

Encl:

Page 45: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

1982 03 12 2.4256

Mr. Randy CrowleyApt. 602 ~ 335 Adelaide StreetThunder Bay, OntarioP7A 7T8

Dear Sin

Ret Geophysical (Electromagnetic and Magnetometer) andGeological Survey submitted on Mining Claims TB 519657 at al in jthe Townihip of Weaver T ^ ^ ^-^.

Enclosed are the V.L.F. naps and the Magnetoneter sap (in duplicate) for the above mentioned survey. In order to complete your submission please provide the following information to this officet

a) V.L.F maps need Raw data. i/

b) All maps must be signed.

c) All claim lines and claim numbers must be shown.

d) A geological map (in duplicate) must accompany the geological survey.

For further information, please contact Mr. F.W. Matthews at 416/965-1380.

Tours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phonei 416/965-1316

A. Barr/amc

Encl.

ccl Mining RecorderThunder Bay, Ontario

Page 46: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

1981 11 10 2.4256

Mining Recorder's Office Ministry of Natuaal Resources 435 James Street South P.O. Box 5000 Thunder Bay, Ontario P7C 5G6

Dear Sir;

We have received reports and taps for a Geophysical (Electromagnetic and Magnetometer) survey submitted under Special Provisions (credit for Performance and Coverage) on mining claims TB 519657 et nl in the Township of Weaver.

This material will be examined and assessed and a statement of assessment work credits will be issued.

Yours very truly

E.F. AndersonDirectorLand Managaent Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone 416/965-1330

J. Skura

ccs Lazan Exploration 6 Development Ltd., Thunder Bay, Ontario

Randy Browley Thunder Bay, Ontario

Page 47: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

i l ' - t. i rr W . /lAt. h-

- .A

.c -^

c A. t? lA -e

1 A

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-

\

l

'Nci.^oA

^2-771

S,:

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,4 u-t

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RECEIVEDLand Management BranchCIRCULATE LUtOHKHIlS HUM Pi

L-JBY

JUN21I932E. F. ANDERSON

J. R . MORTONJ. C. SMITH

J. M . i- i i

RF.HIK.M T O rt. 64i30

*\ ^ftooc

V\-t. \oC^^ T • tt.

Page 48: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

z j 7 rt Ytt

vr;

C-' i/

l-'

l/

Page 49: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

00O) ro cvi

o: LU

o cr

CROOKED PINE LAKE M.2368 BEDIVERE LAKE M. 1647

557841 857836fa" ~~ TT6 " ~

78^0,..—L - — 4-5 3-6 -

ro T TP 'TO

153605 A760I242 l 601243 l 60121 ' 601282

'"V \ s \ s— a— ^^1 .* ^^ l ^^f l ^^^

VX|55xSlid38 i 55^76' 5SVB 7!

CROOKED PINE LAKE M.2368 BEDIVERE LAKE M.164752B148EM13 8.4856 WEAVER 200

THE TOWNSHIP OF

WEAVERDISTRICT OF RAINY RIVER

THUNDER BAY MINING DIVISION

SCALE:1-INC^4O CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINES

PATENTED S.R.O.

*c.e

NOTES400* surface rights reservation along the shores of all lakes and rivers.

DEC-itawMinistry of Natural Resources i

|Ml" TORONTO ——

PLAN NO.-M. 2066

ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

Page 50: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

QUARTZ VEIN 10a quartz vein 10b breccia 10c quartz-carbonate.C*. -

small outcrop

outcrop areamonzonite

bedding, incl.vert.

foliation incl. vert

g col. contact obser

geo l. contact inter,

fault

6a fine grained6b porphyritic 6c quartz diab

CHERT 5a brecciaCU

5c sericitic

pyrite

chalcopyrite

arsenopyrite

FELSIC VOLCANIC4a cherty rhyolite4b qtz porphyritic4c felds porphyritic4d qtz-felds porphyritic4e lapilli tuff4f sericite schist4g chloritic4h breccia

claim post

old claim post

swamp

lake shore

mag. attraction

biotite

chlorite

4chUbiotINTERMEDIATE VOLCANIC

3a massive3b foliated

CHLORITE SCHIST2a chlorite schist

BL AZ 090 -MAFIC VOLCANIC

la slaty 1b chloritic 1c massive

2S 2a

-2a-4OFLT

2^ 42- -

52B14SETO13 2 .42S6 WEAVBJ

Page 51: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

L 30 L32 L 34 L 36 L38 L 40 L 42 L 44 L 46 L 48 L SO

S2BMSE0al3 2.4356 WEAVER sso

1700

1700

11 TP

L52

-2200

2100-2200

2000-2100

1900-2000

1800-1900

1700-1800

1600-1700

1500-1600

-1500

Basestation- L28/00

SCINTREX MF-2 FLUXGATE MAGNETOMETER

LYNX CANADA EXPLORATIONS LTD

MAGNETOMETER SURVEY

Surveyed by Scaler s 200'

DateJune 1981

y,-

Page 52: GEOL RPT LAZAN PROP CROOKED PINE L AREA...1-22 The quantz vein it, 5' wide and injected into a veAy fissile chlorite. sericite schist. The. quartz vein HA brecciated with very thin

40

20-40

10-20

;i f

LO L2 L4 L6

l52BHSE88I3 2.4356 WEAVER 230

-fiIT

L 8 L 10 L

— — — — — — —

12 L 14 L 16 L 18 L

— i.

20 L 22 L 24 L

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52

LYNX CANADA EXPLORATIONS LTD

VLF-EM SURVEY

FRASER FILTER

Surveyed by

t)}awji tjV A jJuvA/N^ \Grtfvftey ^

Date ./Pi * 1*1/' 1CA^C. VV. Q * '

Scale V's 200'

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LEGEND

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^

-40

(N) (S)

LYNX CANADA EXPLORATIONS LTD.

VLF-EM SURVEY

PROFILE SCALE l"' 40"

DATE MAR. 1983 SCALE l"'200'