dd rpt 46 madoc twp - ontario › mndmfiles › afri › ... · grained, f o lia ted j s heared...

31C12SEea09 46 MADOC 010

DIAMOND DRILLING

TOWNS]]]]': MADOC REPORT NO:46

WORK PERFORMED FOR: Noranda Explorations

RKCORDKD HOLDER: Same as Above [ xx ]: Other [ ]

Q] a j m No .

F,O 950293

EO 950290

Hole No.

I)] 87-1

1)187-2

Footage

256'

453'

" JOT

Date Note

July/87 (1)

July-Aug/87 (1)

NOTl'.S: (]) #87-63, filed i n A pr j 3/88.

. .,.,-r. ,~r- UUU.yb N 0 R AN 0 A EXPLOR ATIO N CO M PAN Y LI M ITE D ,. 1 6

*7,, SF DIAMOND DRILL CORE LOG i n?D P PARTI JR^

Tes*r, * 10lMest.)

Proi PT* No Hn!f* Mn -'AW/

Magnetic CorrectedBearing Bearing DinQTian M 3 Prnnprtv

125' -47* 0 VA VAnip AT rn\ \ A R

256'TOTA' f ~PT*-i

Tirrvni

" RFARI\T, ^^ I U60 256' -a/" X/A VA N TS

rnR^ S!7~ Oaf

MS

^ Madoc Two. n . ^ E Q 950293.. ........ TWP rip?m No

, er . ff .H July 25/87 r nmntawrf July 27/87

McKnight Drilling

B. KinoRCVAR^^ ! nnnprl hv J

^

Deoth S Lithology

0-5.0Ga s i ng

5.0-19.3AlteredG rani t e

19.3-30.9Al t e redGranite

|30.9-70.4 r

S

Q.

O.

AlteredGrani te

Description (colour, grain size, texture, structure, etc.)

Pink-red, mediumgrained, f o lia ted j s heared feldspar,quartz, chl, ser. carbonate, probableG2 type alteration, groundwater effectsincluding deterioration of pyrite andhem staining to 19.3'l-3cm qtz segregations white 9.5-10.5'(barren), cross cutting @ 60 O ' c. a.shear foliation @ 50 O

Medium-coarse granularbut diffuse, pale grey/pink, roundedqtz eyes, feldspar have faint heinatiticdusting only to 28.0 (same feldspar andtexture does continue)core angle 50 O @ 29 .0 ' (foliation)very competant unit, min 55 O fractures orjointing with 20cm spacing

15.8'-19.3': deep red, hematitic, wellfractured 20-60 , felkspar, yellow-redmicos, minor carbonate, appearssomewhat annealed

Medium grained, pale grey-green quartz-se rici te /chlo ri te , altered granite,rare quartz stringers up to 1 cm

Alteration

sub zone of G2-G3type alteration

G2-G3 or G3 type

Mineralization

<l% p y

up to 15% pylocally

<l% pyrite

Remarks

NORANDA EXPLORATION COMPANY LIMITED

DIAMOND DRILL CORE LOG

Sheet No.

Project No.

Property _

102Hole No.

DI87-1

.OF.

Dingman

Depth &L Lithology

Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

70.4-86.1 Alte red Granite

34.7: 35 fracture/joint with quartz and granular sulphides

40.1-40.7: minor 3cm qtz-carbonate segregation

48.0 50.0: increased quartz content as segregations

50.8-51.4: sheared, pink, groundwater altered, vuggy band of G2-G3 granite- good elongate felkspar crystals

54.0: c.a. 47 O

65.9-66.6: felsic segregation with single 5cm grey, coarse, essentially barren quartz vein @ 60 (opposing shear foliation)

Essentially grey-green, medium grained (avg.) pale feldspar, quartz, sericite/ chlorite, feldspar grains visible, unit lacks hem staining almost completely; feldspar weakly stretched

75.0-83.3: zone of increased quartz- numerous stringers and irregular quartz sweats with minor carbonate; quartz is generally grey, well strained with trace sulphides; zone coincides with general increase in grain size overall

G1-G2 to G2 type discrete feldspars stil . visible but are considerably altered to to sericite/chlorite few quartic segregation

blebs chalcopyrite in 5mm seam of fine granular py on margin of quartz barren

minn specks pyrite

minor blebs pyrrhotite, trace chalcopyrite, minor disseminated euhedral py; trace mf, possible telluride? py (altered) films on

fractures in qtz.


DIAMOND DRILL CORE LOG Project No.

Property

102

Sheet N o.

Hole No. -

.OF.

DI87-1

DI\GMA\

Deotn St Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

86. 1-94.9Alte red Grani te

4.9-104.5 Alte red Grani t e

f-

Pale pink. /grey, coarsely crystalline with distinct feldspar crystalls, very weak hematitic staining; very weak foliation, unit appears reerys tallized with pronounced interstitial chloritic material-but fabric is weak (ie. slight qtz elongation)

88.0: 24 0 quartz filled fracture, rusty due to groundwater action

Pale grey-green, well foliated,generally fine grained, roundedqtz, in a largely chl/sericitematrix with relic feldspar, hintof hematitic stainingcore angle 50 O @ 96'(foliation)quartz segregations @ 97.2-97.7;irregular, grey, coarsequartz segregations @ 98.44-98.7

98.1: 3cm carbonate-quartz-fluorite open cavity filling; purple fluorite minor sulphide

G1-G2 type; interstitical chloritic material

py specks

G2-G3 type py specks

possible alteration of py to hem showing on crystal margins

locally 1 -27. p yrite with small blebs pyrrhotite, trace cpy , trace mt

several 1mm pyrite euhed ral


DIAMOND DRILL CORE LOG102

Project No.

Property -

Sheet No.

Hole No.

.OF.

DI87-1

Dingman

Depth Si Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

104.5-127.5 Al te red Granite

127.5-137.1AlteredGranite

f

Pale grey/pink to buff, medium coarse diffuse qtz, feldspar with varying amounts chloritic sericitic material- has appearance of porphyry; generally increased sulphides; few minor qtz segregationsvery weak fabric approx. 45 @ 107' persistent jointing @ 70 - 10-20 cm spaci ngsCoarse but diffuse qtz, moderate to intensely altered felkspar, lacks well defined foliation, qtz has blue tint; generally pale green with minor pink (hematitic) staining

128.8: 5mm, 40 O calcite-quart z filled fracture with blebs granular pyrite

132.7-132.9: irregular, coarse, grey quartz segregation, essentially barren, minor cc 133.7-134.1: irregular, coarse grey qtz segregation, wandering, minor cc 134.4-137.1: definite increase in kspar content, gradationally becoming more coarse and well defined although the pale green chloritic/ sericitic matrix is still prevalent

G1-G2 to G2 type locally Gl

1-37. subhedral pyrite specks pyrrhotite, all well disseminated

G2-G3 type does not fit classifi cation scheme well seems to lack fabric of of the generally more advanced alteration

1-27. f inely disseminated euhedral pyrite

locally S-10% py

increase in kspar locally corresponds to increase in pyrite to 3—57. m ore coarsely disseminated



Sheet No. .OF.

Project No.

Property _

102Hole No.

DI87-1

Dingman

Depth 81 Lithology



152.0-154.7 Transi tional Zone(Contact Zone)

Generally coarse, pink to red, kspar-qtz with chloritic/se ri ci tic interstitial material, kspar crystals (distinct); very ninor fabricthroughout, jointing regular @ 80-85 with 10~30cm spacing

140.9: 5cm qtz stringer or segregation @ 20'; grey-blue, essentially barren, associated with minor brecciation with increasing depth, quartz becomes more blue

144.5-152.0: unit becomes "equigranular" with rather diffuse crystals of qtz and buff coloured kspar; virtually no fabric, small clots of biotite

Very fine, schistose, chloritic and ;ericitic zone; minor banding with biotite, finely granular calcite- quartz segregations-possible epidote, several -Clmm seams of granular pyrite may be mylonitic?

G.1-G2 type, only slightly altered kspar, hematite dusting of kspar

av. 2-5 7, p yrite, locally 5 -77, a s euhedral pyrite minor pyrrhotite

chloritic/sericitic alteration may be prograding to biotite

Z-3% euhedral pyrite

few specks pyrite



Property _

102

Sheet No.

Hole No.

.OF.

DI87-1

Dingman

Depth St Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

v .-'

154.7-256.0CalcareousMud s t one jBandedSiliceousMarble

256.0

Fine grained/c rv stalline, banded marble, blue-greybroken layering defined by more pelitic bands, possible drag folding? core angle 52 @ 200' ,

214.4-226.0: unit becomes finely banded

239.0-246.5: increased grain size, increased pelitic material (ie. biotite content increases)

End of Hole

minor calc-silicate bands, up to 15 cm with pale ferrugenous calcit chlo rite, epidote

minor specks ( pyrite; few mt

euhedral ( < l rnrn '

LATITUDE 0+59. &M NORANDA EXPLORATION COMPANY LIMITED QK DD, M^ 1 n r 7

DIAMOND DRILL CORE LOG 1 02 Di8 7 - 2nFPARTllRF .J-IOO.UL Prnippf Mn ,. . Hnlf Mn

10Um D^th D ipF! FVATION 6 Pt

Magnetic Corrected Bearing BearingN/A N/A P ro'

Dingman mrty

-4}" HZ.IM. iuu , n , X7io Y/A Y/A Madnr L U yMlvyil niPATrniiAR . RFARINH W ? -J'z V M l N ' H NTS TWP l d uuu r,., ;mVo - u ^u^/u

y, -,,^ j D ij/ Julv 27/87 Aua. 1/87TDTAI DFDTH CORF SI7F Dprp sTarrprf ' rnmn!p-ori

nrni p .q McKnoaht DrillinarORF STORAHr Tnntrai-tnr ......

B. KingRFMARKS . -- - .. ... ...... - - I nrjnerl hv . . . ..

Depth S Litho'ogv

20-5.0Casi ng

5.0-63.5CalcareousMe t a sed i me n t s(Marbles)

Tc

o.

o.


-variable blue to pink, fine-mediumgrained siliceous-very impure marblesand calcareous mudstones-moderately band ed 1 f olia ted with someevidence of drag folding-groundwa ter : weathering effects onfractures to approx. 21' (badly brokencore)-portions are somewhat dolomitic?, butotherwise uniform-17.0', 6cm qtz segregation, vugs with corrod*pyrite; vein margins very irregular - may bedisco rd an t?-26.2-37.4; minor calc-si lici te alteration,banded ferrugeneous dolorai te f c alci te ,epidote; minor qtz segregations; 28.7 severalcoarse blebs po with minor cpy-40.0-50.0, dolorai tic/ siliceous zone; finergrained, buff coloured-50.0; return to grey-blue impure marbles-55.9-59.0; siliceous zone; essentially acoarse quartz vein with zones of granularqtz S sericite, + " residual biotite; @ 57.5, 4 cm vug of cc S very coarse biotite S marcasite?-23-0; core angle 45 (foliation)

Alteration

id

Mineralization

up to 10% subhedralpy (4- marcosite)locally - average S-4% sulphide

Remarks

Depth a Lithology

63.5-74.5 Al t e red Grani te

74.5-76.2 MassiveSulphide




Property

102

Sheet No.

Hole No.

.OF.

DI87-2

Dingman

l 14.0-120.5 Calcareousptetasediraents (Irapu re

^•larble )


-very sillceous-p otassi c granitoid rock; very coarse with distinct crystals, but not well defined (diffuse appearance); pale grey-essentially without foliation

-minor jointing @ 50 and 55 , average 30cm spacing-well mineralized; disseminated py S cpy prevalent euhedral-subhedral py throughout

-fine-medium grained massive py, minor cpy and possible sp.; siliceous martix

-similar to 63.5-74.5-very coarse; s i liceous-potass i c granitoid rock-minor felsic; generaly diffuse crystal bound a ri e s-minor jointing @ 80 O t* 5 0 O average 25-35cm spacing-well mineralized with disseminated py S cpy

-112.7-114.0; contact zone 4 minor breccia with shearing (augen-like or "proto mylonitic"

-grey blue, fine-medium grained, well banded, calcareous mudstone with minor siliceous segregations-core angle 45 O 2 120'

Alteration

Gl; seems unaltered other than silicifi cation and silphide enri c hnent

very minor hem dusting of feldspar trace sericite

Gl; silicified withsignificant sulphideenrichment; veryminor hem. dustingof kspartrace sericite, tracecc-several ^ram seams ofbio with trace hem

-minor calc-silicite alt. with sulphide in narrow bands

Mineralization Remarks

63.5-66.4; 2-32 pyri te66.4-74.5; 2 -17. pyrite, 3 -107, c py

-SO-85% py-5-17. c py-trace sp.?

-76.2-86.4; 3 -157. p y 1-107. cpy86.4-111.5; 1-52 py tr - 2 7. c py decreasing with depth

-seams or narrow pockets granular py S sp 118.0-118.6 semi-massive py in 3 narrow bands generally sediment has 1 -27. p yrite



Sheet No.

Project No.

Property _

102Hole No..

DI87-2

.OF.

Dingman

Depth St Lithology


120.5-141.7 Altered Gani te

141.7-158.9 Altered Granite - Sheared Zone


-essentially a coarse, qtz-sericite rock with chaotic fabrics; numerous coarse qtz segregations or veins; minor cc; approx. 15% qtz stringers or segregations-this unit may be transitional from an altered calcareous sediment to an altered granite in the contact zone-upper contact has lcm seam of granular po-t-py + ga parallel to compositional foliation-122.6-123.3, qtz vein of sorts, very irregular margins, coarse, well strained (grey-white) with numerous fractures; seams of po, py and very coarse brown sphale ri te; also minor cpy

-126.7, l cm seam of fluoride (purple) with several py euhedral -- may be folded? also t race hem @ 40

-fine grained, moderately foliated, pale grey-green unit very minor cc or dol., micaceious partings, especially sericite-snail, rounded, pale blue qtz eyes-most surfaces have slickensides of sorts-155; core angle 48-essentially a mylonite-157.2-158.8; well banded

-medium grained, well foliated rock consisting of generally rounded pale blue quartz grains and pale green sericite altered kspar?; very little kspar, recognizable, very uniform throughout

G2-G3? type altered granite; silicified with minor calc- silicate alteration (ie. contamination from calcareous wall rocks ?)

-does not confirm to "G" system of classification (mechanically altered)

G2-G3 type -conforms to G2-G3 type with severely altered kspars; lacks significant hem

-other than qtz veins orsegregations Z-4% py, 1 -27. c py S minor po, especially in <l cm se ams qtz vein material carries locally serai- massive sp. po+py St minor cpy

^17. anhedral py - very finely disseminated

generall <l% euhedral subhedral pyrite, locally 3%, minor po, trace cpy


DIAMOND DRILL CORE LOGSheet No. .OF.

Project No.

Property _

102 DI87-2

Dingman

Depth S Lithology


233.4-352.l Altered G rani t e

-minor qtz stringers or segregations, generally in clusters,gene rally barren; 1-4 cm, concordant to foliation; overall S-10% qtz vein/segregations-lacks significant jointing, very corapetant-foliation - core angle; 52 @ 160'-185.5, broken core, minor fault?-193.0-196.3 zone of increased silica -

stringers -

qtz vein,

qtz vein,

vuggy with

coarse , grey

coarse grey

diffuse qtz sweats St decomposing pyrites-210.5; 5cm concordant qtz with trace py S cc-211.5, 5cm concordant qtz trace py S cc-216.4, 4cm qtz segregation with coarse pyrite subhedral-223.0, core angle 60 O (foliation)-230.6; marked textural change to a more coarse, more sheared appearing rock, otherwise mineralogy same

-pale grey green, medium grained, poor to moderately foliated with qtz "eyes", interstitial sericite and some sericitic replacement of kspar-very minor qtz segregations S stringers (generally barren)-generally, individual kspar crystals are noted but are in varying stages of decomposition-slight hem dusting of kspars 233.4-234.8'-233.4-234.4, qtz-kspar segregation, coarse, diffuse and essentially unaltered

-240', core angle 6Q O foliation

silicification S sulphide increase

-avg. 2-5% py, po, 1 -37. c py,

1-37,

-G2 to G2-G3 type with moderate to severely sericitized kspars

-<^^ f ine diss. pyrite

specks po (l-2%)



Property —

102

Sheet No.

Hole No. —

.OF.

DI87-2

Dingman

Deoth S Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks


4

-242.0-243.5; zone of kspar and qtz segregation similar to 233.4-234.4; essentially unaltered-281.5-290.0 (approx.) feldspars severely deteriorated but still recognizable-290.0-306.0 increased kspar content in coarse, diffuse segrations, minor qtz sweats-320.5-323.7; zone of more intensely sericitized kspars-322.0; core angle; 70 O-326.0-345.5 zone of increased qtz stringers and segregations; 343.8-345.5 coarse qtz segregations with diffuse boundaries, pale pink tint with minor sericite content, minor brown carbonate?, minor py

-coarse subhedral kspar crystals in a weak to moderately foliated pail green sericitic ma t rix-siliceous segregation/qtz veining throughout generally l-4cm-core angles variable; avg. 60 but changes rapidly from 40-80-minor joining @ 80 (weak)-373.8-374.5; blue-grey, coarse qtz vein, upper contact sharp S regular, lower contact wandering; qtz is well strained, minor cc

293.8-312.6; minorpervasive carbonatealterationmay better be definedas G2-G3 type

G2 - minor sericitic breakdown to kspar

no significant sulphides

minor increases in sulphides content; 1-27. locally 331.4 discontinues seam of coarse py along probable fracture; @ 15

generally 1 7, o r less py but with blebs py S po trace py generally

-365.0-366.5; 2 -37, blebs S disseminated

pyritic films on fractures; minor disseminated pyrite and single very coarse bleb of

granular/altered py



Property —

102

Sheet No.

Hole No. -

.OF.

DI87-2

Dingman

Depth 8t Lithology Description (colour, grain s ize, texture, structure, etc.) Alteration Mineralization Remarks


391.6-401.4 Calcareous Me tas edi men t s (Marble)

401.4-409.5 Alte redG rani te

fin

-pale green, medium grained, moderately foliated with majority of kspar crystals sericitized-ninor qtz stringers or segrations, l-3cm, and generally also foliated, avg. 15% qtz vei ni ng-minor hem dusting (faint) of same kspar-385.0, core angle 80 O (foliation)

-upper contact well banded and somewhat dolomitic-394.0-minor ferrugenous calcite (pink)-395.9-397.6 - qtz-carbonate vein, wandering with sharp contacts, dolomite or ankerite(?) on vein contacts coarse subhedral pyrite throughout vein; chalky/cataclastic texture, grey-397.6-398.8; sheared, biotitic marble-probable sheared band-398.8-400.0; pale green, siliceous, fine grained altered marble, 10% qtz segregation finely foliated-400.0-401.4; sheared zone, dark grey, banded "mylonitic" zone of fine, dark micas calcite, single l cm qtz vein or segregation

-apparently a block or raft of altered granite within marble-pale grey/pink with discrete altered kspars, moderate to poorly foliated; pale blue rounded qtz-ID-15% qtz veining or segregations, all diffuse and irregular

G2-G3/G3 type minor carbonate S calc-silicate zones

minor cal-silicate alteration (skarn)

silicified or similar sediment

marble meta

or

G1/G2 with strong hem staining @ 403.4

17, well disseminated subhedral py

generallly < lI pyrite, locally 5% coarsely disseminated pyrite

-locally 2 Q7, p y in qtz vein

1-37, c oarse subhedral pyrite-l% ve ry finely disseminated pyrite

-17, c oarse euhedral (recrystallized ?)pyrite

1-27, d isseminated pyrite (finely), euhed ral



Sheet No. .OF.

102Project No.

Property —

Hole No. ,DI87-2

Dingman

Depth b Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

409.5-453 Calcareous Me ta sed imen (Marble)

ts

4530

-406.2, 30 , 7cm qtz-carbonate vein, with sharp contacts, chalky-cataclastic texture, coarse pyrite, minor tourmaline-409.3; similar t o 4 06.2, 4 cm, marks lower contact

-grey-blue, well banded carbonate-calcareous toadstone or very impure marble; fine biotite minor chlorite qtz-418' core angle 68 O (foliation)

-427.0-433.6; altered marble; dark green mafic appearing rock of chlorite, biotite S tourmaline and very coarse calcite

-443.0; core angle 60 (foliation)-impure marble to E.G.H.

End of Hole

-minor silicification S calc-silicate alteration (skarn)

apparent skarn type zone

426.0-427.5 minor calc-silicatealteration

107, euhedral pyrite

-minor pyritic films on fractures only

-2% finely disseminatedpy ri te

-1-27, d isseminated S banded pyrite

Ministry ofNorthern Developmentand Mines

Report 4 r,-, of Work 6 ' "

Onlarioort md

31C12SE8I009 46 MADOC 300Name and Postal TWdress of Recorded Holder j

Noranda fxploration Company, LimitedProspector's Licence No. i

A-34387 ^

Suite 1300 - 4 K j rig Street. West, Toronto, Ontario M3H 1B6 S

Summary of Work Performance and Distribution of CreditsTotal Work Days Cr, claimed

709for Performance of the following work. (Check one only)

[ j Manual Work

Qshaft Sinking Drifting or other Lateral Work.

[ [Compressed Air, other Power driven or mechanical equip.

Q Power Stripping

f^j Diamond or other Core drilling

[ j Land Survey

\"Prefix

to

A 1 ,^. r : ;

••"-I ' •'"'"'

- ' - ' ' ^ "Pr 1 ' K : '-'

, ' "'. 'V

V .X .'^'"l. -f"-' V ;, L . ' .

/lining ClaimNumber

930274

93027 b

930276

930277

930278

930279

Work Days Cr.

71

7]

7J

7J

7]

70

Mining ClaimPrefix

FO

-/-' i; \ -

'k'l *:T'J "C*:'vC.w, : .'rj•('•' •v"...''-Vf|

sW+x- :- '-\f̂ ',,'-. -,V.j

S':fcK

'•'ff'-'j'-.t

Number

930290

930291

930292

930293

..j.

!

j

Work Days Cr.

71

71'71 ' ' 71

... - .^;.:

f •

Mining ClaimPrefix

^-•""i-vt.'t-V '-'i.- ''* .

' - ' V -V. .1: V.-,;:i. '-•:

e^r^wi.-**^r'""*"'^

Number

i ' '"" 1 i

•'•'''i '\-——-|-\r^v~~"~V"

Work Days Cr.

All the work was performed on Mining Claim(s): [0930290 and F0930293

Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)

Contractor: McKriight \ Rontl'Tc, iDate Drilled: July 23 - Aug. 1, 1987 ,/

H.ooo-

D. D. H. DI87-1

Bearing : Az 106 0Dip: -43 0Size of Core: BQLength: 236'On Claim NO: E 0930293

Footage: f 0930290 312' FQ930293 397'

2^i!ijL DIB7-2

Bearing: Az 106 0Dip: -A3 0Si?e of Core: BQLength: 433'On Claim No: F0930290

SOUTHERN ONTARIO MINING OIV.RECEIVED

NOV-3AM PH

Total Footage: 709 ' '

v Core Stored at Aunor Mine Site TimminsDate of ReportOct. 27/87

Recorded Holder or Agent (Signature)

^Certification Verifying Report of Work

.^-^

S

1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person Certifyind Postal Address of Person CertifyingR. C. Denommee P.O. Box 1203

Timmins, OntarioDate CertifiedOct. 27/87

Certified by (Signature),

Table of Information/Attachments F^equired by the Mining (Recorder

Type of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

Land Survey

Specific information per type

Ni!

Type of equipment

1 ype of equipment and amount expiended. Note: Proof of actual cost must be submitted within 30 days of recording.

Signed core log showing; footage, diameter of core, number and angles of holes.

Name and address of Ontario land surveyer.

Other information (Common to 2 or more types)

Names and addresses of men who performed manual work/operated equipment, together with dates and hours of employment.

Names and addresses of owner or operator together with dates when drilling/strippingdone.

Nil

Attachments

Work Sketch: these are required to show the location and extent of work in relation to the nearest claim post.

Work Sketch (as above) in duplicate

Nil

768 (85/1?)

GU2

C2

G2-3

GS

l/lea

GEOLOGY ALTERATION LEGEND

olltrtd ' mtl t- coartt Quant 9*0 ftkttftf groat*, buff toHiui (iinlt is no ftaifafitt train}

at to meatrat* ttrtrvna* ' *nt**et tiHttpof oro*** wit* mittar Inttrtttnoi cfor-tfr, ttHftpor* fto't t tot tt JL

oltmratloti ' "tat fthatia* f t ffi trraeefMff of ftWtfar attwttn want gfo/nt, moder vi t ttr ontt alteration of ftftttfon, pali grttti totovr

moatrart-ttrofto olttrtttoti' 00*0*0" itttitrt du* fm ttfrtmt ttrttc*H*Q ana moOtroit ttnettt alteration of fflOifvt, *vnM art tuff to grim* tot Itcotty r*tf

tt r e*o atttfottw f t Iff t f Of t torsi t y ottorml to fait or*** muttortit/ itr/ctft, trrwp Wonot; roc t appton at auofH porphyry "ffi eetn*, rou*d ttitt-ff*r quar t j oret*t in o gr**" mtta tcfu*', tocottr with tfrortg i**tttlt* *rtW*'*c 0*rf rf - J * ******i fy.

GEOLOGY LEGEND

, fixt f* tuff, tmn fM* iOH #**w//, minor *fcura*e* atrt

Grant H

Mor t'9

tt taert* m***, t9 ft *0* won*. 4O to rs W fmlftpor ^>cc *$ofr , pfrttt; atlfttrtm* f** re Irttt ft* tmnertt* grain, tttot rrf**f

of toMitaf* ft fttff- aata artt* mvmcaviftstanetrt; rtat atHfi+4 mr *f^**r*** M* ttrte in tt*

arai*t*rtvtfaet

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LOCATION PLAN

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332

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SECTION 1400ESCflLE 1 l 30'

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ra(SIrsi

1987

NORflNDn EXPLORnTION

dd rpt 46 madoc twp - ontario › mndmfiles › afri › ... · grained, f o lia ted j s heared...

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