sekciswotm whipper lake · !'m'r^'?..the berry claim group is situated in the...

SEKCISWOTM WHIPPER LAKE-, -,. . ,". ,, ;,-.,-v-v'^ ". •-;.- : '-7';-.'- ; -- -' 'rW;^'

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MAGNETOMETER AND ELECTROMAGNETIC

SURVEYS ON THE BERRY, HIGHWAY

AND GOODIE CREEK GROUPS, - . .w . -•--.:.--*t*' ' -- i -? fei, ..•..^.v-t-.-i .:.-'': i-i.'

PREPARED FOR

NAHANNI MINES LIMITED

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\ -' • '-••- 1 ' ' ' v"-'' 'i^'^'l i'*'1 ''? ' " ' ' ' ' " '- .iv.i^.i-isj I.M-'-'" DERRY, MICHENER, BOOTH A WAHL

^" ;: -^t32fe^^?D. G. Wahl, P.Eng.Consulting Engineer

Toronto, Canada -.'.: . - : . ^, . - .- -,.' -•.^;'\'-Uv '^-' - ':-' r': ; .' -' •-•/••r-xv:-'".'- - .".'October. .14, 1983,' ' ' . ; ,;,^\6'^^, -.'. '.' •''•^;-^S'li'':;': .' ; ..^..',V^r-^-: :;r,^\'''V,v;s;i: ;': . , ; : ' : ;'' ''' , ' •.• ; -\ . : .'J:v^^^'.vi.'^'^5:' : : s f'H^' ;:?:^SSi:^:^^ ;^' - "' - " "' : ' : : ; ?- y'fel^:- -t{This report may not be reproduced, in whole or in part, v/ithout the written consentof Derry, Michener, Booth 5c Wahl. ; , y

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f- ^ TABLE (JJ CONTENTS

•SUMMARY:;,. 52Je4sweeie s2Keiswe034 WHIPPER LAKE 010C•SfkX/^^J^'^'^^'y'i'fîf^ 'i, ." '

1^ ^ ?' Tabledl;|âgnetbirie.terând .Electromagnetic Surveys'•'••.'.•/••''' " ' "'. i i: .-.' .. i" 'V.'^'-J'."".;"i-'. ;: : -'. ; V-•••'•'•• ; .'..' "S.'l-l? :Vi'^--'^-ii't:'v* ; 'i ) '.•s/;-.-.- . - ; .;,v.-,' . ' - 'V', - ', : :-. . .'- A -•'•- !'- •',.'-' :; *' :-'p *-:'" !'-^-''-''-^ fi^^?-'"..-''' v " •''•'- ' :-- ' ' .

Table 2:; Proposed Diamond Drill Holes

1.0 INTRODUCTION

Figure 1: Property Location Sketch, Sioux Lookout Area

.2.0 ' BERRY' GROUP- !l^ "

Figure 2: Claim Location S tetch

2.2 LINE CUTTING

2.3 GEOPHYSICAL SURVEYS

2.3.1 Magnetometer Survey

2.3.2 Geonics VLF Electromagnetic Survey

2.3.3 MaxmSn H Horizontal Loop Electromagnetic Survey

2.4 CONCLUSIONS

2.5 RECOMMENDATIONS

Figure 3: Proposed Diamond Drill Hole, Berry Group

3.0 HIGHWAY GROUP

3.1 INTRODUCTION

3.2 LINE CUTTING

Figure 4: Claim Location Sketch

(i)

(ii)

(iii)

1

2

3

3

4

5

5

5

6

7

8

8

9

10

10

10

11

.'.'i:\-fi.- - ' * .:.-i.-\...---.S., -.#.' \-'-',-'-*'-'f'^. DERRY.i' M ICHENER, f .BOOTH^ft

3.4 'CONCLUSIONS

9L1^!'-i,JftW.V.!ifr;A^y,':.: f .- :, ,. ' •.. irv:y.," 1 , j '*', ' X -;." •'.. /./^./if^^v^&^xVi'ily.tiajyV^vi-v^^^

TABLE OP CONTENTS v? (Continued) j v g.


Page

12

I& ^s&l*:3.3.1 Magnetometer Survey ;. . L *. ' '. . . v ; . - . ,.;:... J H-. | '.j",^ . ••-,',.-.,/. '.' i ^

3.3.2 Geonics VLF Electromagnetic Survey ;;

3.3.3 Maxmin n Horizontal Loop Electromagnetic Survey 13

13

t Figures: Proposed Diamond Drill Hole, Highway GroupV ! 16

Figure 6: Proposed Diamond Drill Hole, Highway Group 17

4.0 GOODIE CREEK GROUP ;.; ( ^ '^•^'^••^•^

;,'; ."-4.1 INTRODUCTION-., ^f^.'., . //V-' . ' : '^-\ ^^-j'S-^-' :' ;^-- : '-\ ':',18

4.2 LINE CUTTING ,, Vi 18

Figure 7: Claim Location Sketch y 19

4.3 GEOPHYSICAL SURVEYS ' y 20

4.3.1 Magnetometer Survey i. . 20

4.3.2 Geonics VLF Electromagnetic Survey 21

4.3.3 Maxmin n Horizontal Loop Electromagnetic Survey 21

4.4 CONCLUSIONS. l' f 4 23

4.5 RECOMMENDATIONS ; J; i 23

FigureS: Proposed Diamond Drill Hole,Goodie Creek Group . 24

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: r - - -,'- ••- ' y:' l. v ''. v y, ;^r:j; : ,:,; : v ;-;-: ;^vi.•,';i.i;, '^f;^#*i^^fe^ 'iieLSimYBY;^^^^^^

103 ELECTROMAGNETIC SURVET:444 Hz

104 . ELECTROMAGNETIC

GOODIE CREEK GROUP

201 MAGNETOMETER SURVEY

202 VLF-EM 16 SURVEY - ' ,J,j(l..-i

203 ELECTROMAGNETIC SURVEY 444 Hz

204 ELECTROMAGNETIC SURVEY 1777 Hz

BERRY GROUP

301

302

303

304

MAGNETOMETER SURVEY

VLF-EM 16 SURVEY

ELECTROMAGNETIC SURVEY 444 Hz

ELECTROMAGNETIC SURVEY 1777 Hz

. ••••'••^'^tl^'fe^V"' '. •••'^•':.''^WMK&^^^^'^W'^':^^?!''

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^K^f^l'iMagnetbmeterTahd electromagnetic surveys were carried out on behalf of^^^^^^^^•^'^'•:--- -.''' :- ' '- - • ^"'•'•••''•'.'••• ; '' ; ' y ' l?:;^hanni^Mines Limited by Derry, Michener, Booth 3c Wahl (DMBW) on three claim

^; groaipViil'the! Sioux Lookout area, designated as the Berry Group, Highway Group

and Goodie Creek Group, during the period from August 25 through September 3,

' '

Toronto, Canada October 14, 1983

Table l, on the following page, summarizes the results of the geophysical

y y i it is recommended that the conductors listed in Table 2, Page (iii), be tested

by diamond drilling. . V ^ ^

Respectfully submitted, '

DERRY, MICHENER, BOOTH A WAHL

D. G. Wahl, P.Eng. Consulting Engineer

e.*c.iTD.

e

Hifhvty

Croup Conductor strike Dip Length Kidth Depth Conductivity Mjg. Mtoe. Inferred Causative Body

BC-1 Eatterly near 1.2 kB variable 12 * 224 Khos f 177? H*. direct up to Sulphides (pyrrhotite)vertical up to to 900 chos l 444 V : 5800 r.T Volcanoclastic metasediment

li it 4 8 B Lapilli tuff

HC-l Easterly

HG-^ 4 28 Satterly

near vertical

nearvertical to 80 N

300 o

TOO*

variable up to 10 n

variable up to 35 n

27 ato

30 B

IS ato

24 st

74 nhos * 1777 Kx 90 the t * 444 Hz

2S mhos * 1777 Kt ISO nhos * 444 Ms

flank* weaktug

direct up to1600 nT

Sulphides, graphite 7 Clastic Mtattd.jsnt

Sulphides (pyrrhotite) Clastic aetasedinent

OCG"1

GCO-2

E*ittrly flat 400 B narrow indettrminatt

Eatterly rita r vertical

TX) o ?0 * 10 B to

low

)7 nhot t 1777 Hi ISO nhot l 444 Hi

no cay assoc.

flanking nag assoc.

overburden

Culphid* facies Iron fornatlon

H- H-

l^^^^m^^y^' - '"'•'' ' ' . - ' ' ' : : ' . •'J&tiffi'&ti

O *C.UO

'Berry

Table 2

PROPOSED DIAMOND DRILL HOLES

Location

Conductor

BG-1

Drill Hole

No. l

Line

1-fOOW

Station

1+OON

Azimuth

Southeast along line

Dij2. Length

-60V 125 m

Overburden

10 m

Highway

HG-1

HG-2a S 2b

No. 2

No. 3

3+OOW

1+OOW

3+35S South along line

0+50S south along line

-60 150 m

150 m

25 - 30 m

25 m

^GoodieGCGr2 No. 4 3^-OOW 1-fOON South along

line

-60" 150 m 18 - 27 m

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•XV'

1.0 INTRODUCTION

The following report details the results of the magnetometer and

electromagnetic surveys carried out on behalf of Nahanni Mines Limited by Derry, V^" '.'. -'.' .' . , ' : --i -- .' -., ;I;' - r i-'' •••-'' l "-.r : /?.^-^Michener, Booth A: Wahl (DMBW) on three claim blocks designated as the Berry 1:

Group, Highway Group and the Goodie Creek Group (Figure 1).; ji S -: ' ' ' ' v.. -' : " ' - ' '''; ;"- • ; ' ^ -'': - --^ '^

The magnetometer survey was carried out using a Scintrex MP-2 total field j |

proton precession magnetometer. The total magnetic field intensity data was

recorded at 25 m stations at an observed elevation of 2m above-ground level, with '

a sensitivity of +1 nT. Diurnal fluctuations were monitored and all data was adjusted

accordingly. The magnetic data is presented as corrected station values, above the

local background of 59,000 nT, and as a contoured interpretation of these data.

The electromagnetic surveys were carried out using a Geonics, VLF, EM-16

and a Maxmin n horizontal loop survey unit in the maximum coupled mode. The

VLF in-phase and quadrature response parameters were recorded with an accuracy

of ^l**), at 25 m stations. The transmitting station used during the survey is located

in Cutler, Maine and broadcasts at an assigned frequency of 17.8 Hz. All data was

plotted as line profiles at a vertical scale of l cm to 1096. The in-phase and

quadrature response parameters for the Maxmin D were recorded with an accuracy

of +196, at 25 m stations on two frequencies 444 Hz and 1777 Hz, utilizing a 100 m

Tx-Rx coil separation. All data was corrected for topography and plotted as line ,: v •v' ''V •'•j-:-v : '- ' -'' ^ ;v " ..'--h ' • •"/'^''/' '"' ' : - ' : ' ' ': 'fl profiles at a vertical scale of l .cm.;'.to.;i096.;

- DERRY,"'MICHENEa^ BOOfHk'a!' WAHlS'';/':^!^*^^

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LOOKOUT

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NAHANNI MINEft LIMITED

Properly Location 'Sketch

SIOUX LOOKOUT AREA

DMBW - (985

SCALE l inch ' 4miles (opprox

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- 3 -

2.0 BERRY GROUP

-l^ie*l!

Pii^i^-V

m^K't.SfA*W; ;V''. d '

; INTRODUCTION

!'M'r^'?..The Berry claim group is situated in the Whipper Lake area, Patricia Mining

Division, District of Kenora and consists of the following twelve unpatented,

contiguous mining claims (Figure 2).

Pa-590158* Pa-590159* Pa-590160 Pa-590161*

Pa-590162* Pa-590163* Pa-590164* Pa-590165

Pa-59.0166 Pa-705961* Pa-705962* Pa-705963*

The recently completed ground geophysical surveys^ however, only covered

nine of the aforementioned claims so designated with an asterisk.

The property is readily accessible by car southwest;from Sioux Lookout via

Highway 72 to Highway 664, which is then followed westerly past the CNR station1 ' : ' .- . . . r s .'" , " ' "' '"-' "- :-""\- -•"•.'"'C- ' :;' A V'*\^' : '"' : * '. :'' : " r ' f ~-'- - '

at Hudson, to a point approximately 3 km northeast of Goodie Lake, at which point

the road crosses the southeast corner of the property on claim Pa-590160.

xW^yty&'l'yfalr, 'Zte\?faf**Sl

\r

Claim Location^^~^ ' -' ' ,"" . , . " . "- ••- V . ' :..'-.-' to l nni^-vr: ';'^^i:iV'c; - \\ ^.-^\. y i: -: - •^*'frte*Z:^38^^gg^^

B^&W'rj-itJ.î.;.' - •--••-•-.'8Steige#tIi^^W-'V^ m^^K^m:

Ipfm Itpif ̂-i ifc^t^^K M?Sr4fc*rff ''Nfci C*' WH^^teiV^.-SS* ^Xk-' f-';, i.,v .•.•-.-•".

•^^[t^^-v^-i' i;v--'.EjB^^f^W'^v8ipifioi-(

pte^v'f•UIH& ^'•^'•'V' '••' i • ; ;" '*-Hpp^.^-'t" ;-! "-' - .- "' P^^v.;.:, v,.,. ; - ;,/ -fer : -o|fe- :,v- "'--. . •vPA:'''.'vV ' .v '- , ' I.--.K-, .-- ,*:^v.v.. '™, .^V-;".''. ' t" :Y.-.-.- '-. -s"- ''. v - -. "

1 MY ' . P - ,-^:ffc. "' ' * si fe"f ; ', r . . * 'K-y':.':,:te^-v / : ' :- ' '."'.^^•V/-.'"1 ,"'' 1 . -' ' 'l- : - :fe4 'P:- 'pi*,, v .P"-'fei- :ll^;,:,,.-:|p,5r\'' r^^^'fev-.'.-r. '

HfcBiSvS'-BB^^f t^'SvJv ;'?' :f: i;::'-

I^^pt^^'^vi'

fPf-^P:f;te:^:--; y: -gSf^'i;:^1 ' ^;,\ ' . '. ' . . . .

IIIKI^^

^^^^RffSP^':iI!':-^"'--^•^^^^^^^•'^"-^•'•/'••••'•••^''•'••'i'- -.': ' v". ^ , : "' .'.- ' .. . ' ;.,'..' .-'.•- ."' - ' ' : •'; '^'- : :i; : '3;'--; : ; ;iV"

•//S-'C' 1*!:;*"' 1^'' iiii'c 11-':- 1-'-.., '.'./',.'-v. s e - l p , : .:..:^*-.-,-ir:'.,v^vi#,'-- •-.;--; ;,-, . - - 5 - . .:': - ; .i';U-'-;S'i'^''^'-^: V;-. -' - ' ..^ 2.2f LINE CUTTINGi^Sli^flvîri;!'::^;-^;/;-''^ - -t t-f;f.!f-','iiffM'A''-;.f.'-'-f'' - :- 'i:.--. :'^'', y ' \' ••••. i ' . ^SMfeV^V-'^,-.-'.-'"': . ..y?iyy';;^'.-:-:,;A*?,.." v ' :,' ^:-;.. '::-;S .^ J J;- 'l;;The line cutting was carried out by Ken Bernier of Sioux Lookout during

|fth^fpwiodifroni ̂ JVugust 15th through August 19th, 1983, inclusive. The survey grid,

"^consisting '^'of 9.675 -km of line, was oriented such that the baseline trends S700 W

twittiîd lines trending N200 W at 100 m intervals along the baseline. Twenty-fiveV^V'^-^Â^y^l'"''" 1 . - ' '"'''" •*'~* -'i" i '"' ' •'•""f\ : .'" ' ,- '' '

inietref stations were established on all lines.''w;A'";tY': ''-v.Y'fl''^-' ' - " '. ' '- ". . .

,' - fi ~, -~ "i - ' - '" ' ' " - ' ''.•*i - - ' ' '- - ! Vii -.' ' ' v "- 1 ' ' '" . ' i ;.-''?;''-;''V-'V;7' -; - ''. '' ' - ' -••: ; - . .

'^'••^:-: ^:''t': ; v ,- ' ; ;^. ; ; - - •'.;; - ' . •^;:4v:v-:' ;v: .;.- 1 v'V'y.v,:;.--- 1 ,: '-;- . '- - ;- .-- ; ' : \

2.3 GEOPHYSICAL SURVEYSy.. v-;'.." .'',:'. -.. .' - ' . ; . ' ' . '. . . '

' . : - :. ' . ' ' .'

The ground "geophysical surveys were carried out during the period from

'August 25th through August 27th, inclusive, under the direct supervision of R.E.

Routledge, M. Se."i. ' '- "' S , . .

•.y ' •'.•.y - - - ,;t . . :. . : y .

;-- ' .' ' ' . . . .' .' .;. V-' 1 . ,'i'. ., /,


The magnetometer survey (Ref. Map 301) was able to further define the

regional magnetic trends mapped on the property by the Geological Survey of Canada

and published in Geophysical Paper 1147G.

The results of the magnetometer survey indicate the property to be underlain

by a metavolcanic-metasedimentary sequence, which has been intruded by a younger:.V" 'v"' ''.' ' ' ; : ' ' : ' ' - ' ".''V ;'. : "'^-'"' 'l-^ 1 ;yi;. ; "' : ' -'.•;k granite. ;. : . - .-••- '-'. . . \;..- ^"•...••••-'•'•^'•^••^^•'^4^'.'''.^•^'^•• : '--:'-: - • ••••'•••- : ', .-- - ' - ' ;.' ' ' '•^•'••^^z^jgfcj&^t:: ^••^,"s-;^ ' - - ' ••'^^•^'^rT^

- ~ . - t

K;::,',/;.,;.',;/,.','-'' . -. .-. '.: .' -':.. : ' ,/ . . •.-•,''. •..; '/'^'-,-; '. , ,' : : -- ..: ^-^^^kf^:. • ••" •••'•' 'J '*' i:". ii ••''.'.• ; :'; ' :"-.-';;- ••'••- -. - : ' ; 'DFRRY, MICHENER^ BOOTH- a; WA^L';:;;- ;;.^'^ ;^t^^^^^.f^f;^'.i"y; v '

' aBw B^SaWr ̂ ̂Tr1^^^^^fM*?

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IVtv - : ^- vV;..-- ' ', :"-',t-?.fr; . ^/. ' '.•.'••• : .||:T.: ; ,' S& ' '"i;- ::m ' .. '. ' ,

{|S; . ..ifevvr . -' .":r:^x.|*jjfe.-..V. -- ||; :Vfo:.^--l ;| vi;.".V.cS,:. -

•'.•'''7-' tf '.

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t|fc"' :If^'i'''-'^--''.'.-'.'-; - ' '

IP;-^^•'•V--..'.',;.--"-'' '- : ;W1 '--- : " ' .'f'-ppi "' ' '^"^B ' ' '. " - 'IP'r : : ; ';; ' '-•^ 1'

|lf ; ;^; .tfW; r -111.- ' V---wî''^- '.y . .;•K' H-Sife-K'S1 ^'-'-"' '.' ; ffiBî'-f^jv:'' : .-C'..-lillfe'Jii^tit^x ' ^'v '4p-gjji^?^?-- .^''.;tllliif-?^^fflp^'i'H''if'fc'^.".;,'. ;-. ; .!''i-lispr'^^'vj*'' j' '. '": A'5;,': 11. - i vV ." ' .'.

HP'B.^'îi^'H^-'. "':^?t B '^tfeS'Wi ' ' ' . ' ' :feS*ii;'''!v,;'. ;v,';t:'i ''" '•••,- ' . '.' 'Ss&Kfi'^'''' *^'' ^ •'''-'•'"'•'•'V' ' ' ' r'

;^^^^^''* ~ ' " - V ' ' ' '' ' ' - ' V' - -- ". ., ," '"..•'•- H-.H -" rt - - -. - " ' ' j ,- .'-,, j ; v .-. V '/i ' ' .'-i':'i--"--' VVl ' j/ 'i- 1*:'*^;,,-. v--,". ..,--, -,-''-

' . '- ' , --p ; . -. v -' , v . '-' ' • 1 ' '- ' '--- - '- - ' 0 ' '. ' ' '' ' ' ' ' i ' "' '-' - ' •''."•- *' v~ ^ ' '-•'-"' i ~ ' -' ' t ; - '-.' '-''-v - ; " .' - ' . - ' r ' ' '' L , - . - . - ,, - -". ' - ' :' •••.'j ; i?-. - ; '/' /-- ' - ' ' ' ' - - - 1 i* 1 : -•••- .v *'- K .i". ",'J ." l lh ' "-'-V'/ - ' VS - '-.-'^ - * i "'-"

The metavolcanic unit has been magnetically inferred to underlie the southern

one-third and northeastern one-quarter of the survey area ' ' ^li!!^^-, . . ^ ' , ; . . ; ' - . t - ' ' ; - . - . ' ' '' '' - : , i\ , , f (''-'; : f-\rffctf7!'^'?,^ • -'•^^•-- '.'' : '-'ii ;''VP"' ^.^ -7-.':^ '; ^'.'•'.''. - 'V 1 '.' ' - •'•" - ' ' '' ' :-'-.- :.\''.."''--'.-'-'' '. ' " '' - •...-.; .. : ' : ' ; . ^c-.^ '/'^ ' ' - '^'••fy^^S^f^^'^'^^^^f^':^:'!'^^^/^-

broad, uniform regions of moderate magnetic relief, upltov 3,obo^[in.TJ;abbve local- ' ' . ' '. ' ' -' - -*1 - . - .''-"p.' - ""t.'., '' -s - p.,.; ,' ! - ' - ^.'i/'-V H. j -,, "' ' r,v''"' - ,- . ..' '•- -v

background. This unit has been interpreted to be an easterly striking, ; iiel^vertically '-;;i'^.^^^^ dipping '.intermediate 'to. mafic flow. ; : ' ; v.. : - . ;̂ ̂ vs^^l '-^^^"M^^^y^ ,; v •••. '•-.•..'•.'••••'- • •.•.-•-•.'- . -. :. ' ;;.'' v - .' -' - : \ ' : . .•-'^V^'^^^^^^f^.y^^••' '.' ^' -' ' : ;:- ,! ;.7. ; ^ : ' - ', • v;;'-. , :; :-/;^'". ;.'. ''.;; :;.:'. ^^|^;:;'f;:'|^

: ' i - r . ' ••'V '' -'". /' r ''i'-.'iV -'.•••:-'^-: ,X' : "'."--v" '"' /^'^v''1!''.-;^'^"';''.

The metasedimentary unit has been magnetically inferred D tdiuificlerlie i.l the. '- ' - --r , ' . . . w - . ' . ' - ^ - 4', ,\-','4r"" ' • .'-iS."''--' f • "-•" --j • ',''- 1-j:^-.L'" v*'' : ••'•' !"V"t ' : *' ' " J ' r

'. ' '-' -- ' '' '' ' - .'••'•- :- ' ' '' ; '•'•••'. '' - : ^.'^•^^(^^^'^•'^^^^•'•^^^^central portion of the survey area and is characterized by; a narrq^glenticular

magnetic anomaly up to 5,800 nTalDove local ;backgroiin^^^

interpreted to be either an easterly striking, near vertical dipping ̂ *clasticr sediment^ . ' ; ' ; - ; "' '•-•- - 1 ' ' '- .' '.' V. !.-..!:.,î..y. •-••'.. -.'- '•,-.-;Vv - S.-.-;! - .ft-".'" -.^

' - ' i - ' " '-•'.••'•'•.- . -, 1 '' ;' . - ,! ''' - -,- -; -.V-,-'.' VsJ^'.i^Vj'r.' .'•.••V'-''''''' l ; '' ; '' ' 'i-'--' ' "'':or a lean " iron formation. . :' ' -v'^'/- ; ;.;- : . '••;- - - ;'- ;- ;- ' :f; '^l' v' ^v.;; ''.'^^1-!:;-.,' '" 1^ : :';; ;"/' ;" ' ''' ' .- .

The remaining northwestern one-quarter of the survey area has been. ' ' . . , i . , ** \ "? '. -' . - ' . . .. . :

magnetically inferred to be underlain by a granitic intrusive and is characterized by' ' ' - ' - , ' . -- .'j r-..- - --' .-i v. ' - :'!.' p'. :. :V'i\* ' " - -- --^ ^ v;.; -v,-.'.;-, p-"''..- . ', i.''

a broad region of low uniform magnetic relief in the range of 300 to 800 nT above

local background. '. \ ''- '' ' ''- - ••;,. '' . :- : ":';.V,: ; : "-' -' . .'•/. •••r.i^^f- ,- ;;v : :--- ' •;; -- ' ':' ! '•'••; ; . y 0 -' ' ' - - • '.'.•'•.^'••..^':.^ ••^'•- '--î^f :-.^ ''^ ^ . : -.,

•: ' . - ; - -.,. :,V'. - ; .-.'."' ''. - ' ' ; ':-l-^-;:' : - ' --^ ' v '.—' ' ' ' ' ' ' ' ' - ' ' ' ' ' ' '\"n,'-' - ' 1 ,'" . , " ' . ' ' .

' ' ' ' " ' ' ' -~' '"li" '; ' ' ' r j ,'

2.3.2 Gconics VLF Electromagnetic Survey. : ; . ' ' ' ' -' ' -' ' . - -' . - ,- ••.'- .' r- ' "" .'

' '' " - . . ' -- : ' ' ' ' '

The VLF electromagnetic survey (Ref. Map 302) identified a major anomalous

conductive zone, designated as BG-1, striking easterly across the central portion of' ' ' ' ' " " ''"" ; ' '

the survey area. Bî-1 exhibits strong uniform conductivity along the entire 1.2 km' ' ' . .' '' . ' ',

strike length and is characterized by a sharp, large amplitude in-phase cross-over,

,.' up to 120% (+60 to -60), over a horizontal distance of 100 m. /Associated with ; this' ; :":' i: ; '' tV',^-'"K^:^^:^^y.t^;^ ;^^^'; v ; y /^l '^r'^;#^sV!;.^vvanomaious in-phase : response is an equally anomalous /reverse sehse^ qiiadra ture'

1 ' ' .' - '' ' "' - , ' - . ' ' - ,r'' " 1 . ' ' '" ' " , J ' - . ' ' ' -' ' " :' '' , '- ' ' "' . ' ' ' ' ' '•"" - '. .' .-' r !lr 1 '-' -^ - -' ! ;**'-. : " i, ' '- V ' ' "'

' ' ' ' . ' ' .' ;' -. .' ' ' i ' ' \ ' . *. " ' ' " ' ' . . ' ' '' , ' ' ' ' ' - -i* 1" ' ' ' ' ! ^ .'- ' ' '-r, ' ' ' ' . J-' ' - ' .^ ' -- , . ' ' ' ' ' ' i ' " ' - - ~", - . t . - ' \' ,' ' i ' . ' . ' ' - r ."'p , ' ';iV* '" ,.f ' - ,', '', '

" ' l1 ' 1 ' 1 ' ' "" . ' ' " - ' '' "- "- . - ' ' . ' '~ ' - ,,'" n . - '- ''' -.•'•'V''f l vf {''"' '^-' 'p-'-'v '' ' : -' ' i 1 !* ;'. '- ; •••" :-' '•'''.': : ;^ ' ;' : ' ; '- ;- : ' ''•'•••' ''- -' ; •"-'"'•- -' ;' .-.' •'•' : '\' ' •:' ; ;-..' ; -':'S;K : ' v ' ; '^ ; :''/'' •'•^^..• ;:^'l^.1^^ ;-*' : ''.^vv:^1 ' ' .' '" ' . ' ' -' "' . "- , . ' . -' ,. --. " ' :^ ,! p-'" 1 ," ': - ' •'••~ " !: . - '. - . - - - . ' . , . ' - - - - - ;; i ^- . -T:.---- , , ^' ;:" - - - '

1 , ..'' ' - ' ' ' " i ' ' ~ ", . i " '.'H' '"' . - ' '. , ; '. ' - .: - :' ••••' -: ' ' -'•••.:\, :-:'\"--.^ . '" "' '' ' - ' •,'-"' ; .'. ;"v ; , v "-'.: . ' - - : "' ' : '•^l^2?:^.;.vr'^y- ; .;--,' '--.-. •-V.. .; .'••.v., ^^.f.;-'. : ;. ; •:. , -. '-\ ,-...: ; - 'v' .' .- •'^•'rf^-''^ : '^'^ " . ':^ ^^•v^.,'-k-.^v. :^^.s^:^;.-^v:-.;i^,V'- , - . 'v.-o.;v' -' v,:;,. v,;.-:;;:,-..,..'..-^. ^:V•^•:^^"•:i' 1•^;^!',%v^,i ,^•: ; ^f l^lf W^^^^^9 :̂ " DERRY': ' MICHENEaf 'B(..^^WA^|*f|^|^^^^^^^f

m

luVl^V*',VL*L*: "-' -' ":'.r - ...'itV*iM;ifeS i&v.!..S"*.v''

WP' 0S^

mtfsv

^iiPiii^^|;;;: ;; :;'||l|*|:^:;l^^^'; ' ;'. " '--'vi"".,- ''V''1 - '••y^1 '^-*V;' ':r,- ' '. - .-'•••' '•V''''; V: * '; - i "-'?'",-'/*":''? ' ' "' :,.- ' "' .' -

response/of up f to 6096 ("30 ito+30),^ over a horizontal distance of 200 m. BG-1''^^'':'::i^^'^^^ : '. . : ' ,appears to^ bo open ? along strike to the east and to the west,

••'••' ' •,''.y. ;-':"- 'f" ' '.v i j ''l';'-'-V''-'fitf?t'-!!S '••i.-"'. 'S' - V,''-' 111 '-'-.' '"- t'"'"" - - '' r ; ;" • •.''••' ;i- ;'. ; ?:V:(; ,*-'..('v- ''-.'- (''-'." S;;-'' ••;-.' : '' -.V " ; '^:?i :,..- ",;., ' . ' - . 'O- v "•••'.v.;-.-.- •-.: -V^' •.•.'••.s-' '.V '- : ' '^- .y-vvSP-.to !':''^vW ,it'. ; 'V^ ..y,:'.:-H,-

inferred

*fe';i .

'i ''f, ii v,^Conductor^:BQ7l^^;lies^:, coincident, with the magneticallyW*^^^ . . '- : :.metasedimehtary ̂ ^nit; ̂ striking; easterly across the central portion of the property.

2.3.3 Maxmin H Horizontal Loop Electromagnetic Survey

f /The Maxmin II horizontal loop electromagnetic survey (Ref. Maps 303 and

304) was able to further define the easterly striking anomaly BG-1 identified on

the property as a result of the VLF electromagnetic survey.

The electromagnetic response parameters indicate that conductor BG-1 is a

near vertical conductor sheet, up to 18 m wide, exhibiting a conductivity thickness

of up to 224 mhos at 1777 Hz and 900 mhos at 444 Hz. This four-fold increase in

the conductivity, with a decrease in frequency, indicates that BG-1 is an excellent

bedrock conductor. The response parameters also suggest that the conductor appears

to weaken to the east. Depth to top calculations indicate that from 12 to 48 m

of glacial till lie atop the conductor.

As was the case with the VLF data the horizontal loop defined the conductor

lying coincident with the magnetically inferred metasedimentary unit.

:^

'•^^^^^^

••' - : ' ' '' '. -. ' '-' ' -"'' '' '-" r '.'"T''""--; 'i'. - .v-;i-. ' v. " -,. -' ' ' • •'.''.•:. ~ ••.-••.".''/.•k.- 1 -:-'•;- •.'::.. ";'.'.v:;v;-. - 8-. •.•••; i :c- ::^.^v' : -i v'-. 0 - 1' v :.-V : ::- v-^v : :

bw-r?-^;mm

ja|y "'lil";

2.4 CONCLUSIONS

Conductor BG-1 is an excellent near-surface, easterly trending conductor^ i \' ' ' -.'" -' • :-. : • '.•^•':; ••' ; .'.'.. ; '. ' ^".••."../••^ivV'X'v. ''^'••./'•' \' ;-"' ,".'-''/'.' ''^;M''^';":^ -exhibiting u near ' vertical' dip/ .t'' '- -'V ?*'; 'v-'-'- fri':: :':- v : 'TSf ;C-^'^ "'j' ̂ v- '." .^'^r:1 ' ''.'':;;^';i;f feHlr i

" • - • ' v 1 : ' - -'- '''" - ' ; '- '- ' ' '* -

• ' . - . •. . . ,. . .The causative body of conductor BG-1 is thought to be a highly conductive!

- .' ' :''"'.. . - '•.-'•' " -- . '.'.'" '-. ; '-. . '' i" : '"'', :, ; .; '-; :'--- •V'^^l.'^g&'^Si volcanoclastic metasediment or lapilli tuff containing a high percentage of sulphides H?

• i . f , 1 ''. 1 .,' 1 . ~; . ' ' ; ' -. . ; 'M** , '' ., , j ' '.-, '. - 1[ " i - . - ' ' . L p ., r •V.'( "V. ''-i- '"'-^ ' r ~*;'' ' " '•'.•' ' V''. ''" 'V :il ! Y. v :^ '' . '- ' '''''-^ " "'' '•'•'' :- : ' ' v '''•••:'-- '..•/: - '-'''' '•'.'•"'-.'••y' .''•^•'.•;fy^i^'"^'-^\(mainly pyrrhotite) with minor amounts of graphite. ( r ^ "^1^ ic^ - ' ' ' •••• •• - - - ' " ' ••

2.5 RECOMMENDATIONS

•"",,: -:, V'-' v""•"- - - . •.••'••••'•!'..\ f: - r-.:"1 -#*A^'^^^'A? J(jj.i*-V''^^ ^-:^cA^,^^'^s|^|ii^|;-. ' .-' - .;-- ••-i;-' '.. ;- '.- •-•'. • v..,;-.v' 1 .^j-it-'-i Vfesn

'•. ' " :-' r ; ' W*:-. : - :.-":' 'i'" ".''•A'-^:'.1*-^ ,Vf .-/iv-:?,.; ;:-..' .:;) .:'.-:^;v.; ;.:v..-, t-, r . /.f;:-;;;v|*f ;;;^\*

It is recommended that anomaly BG-1 be tested by diamond drilling. '

Figure 3 presents the location of the proposed diamond drill hole and

illustrates the geophysically inferred orientation of the causative body. :

:'-K,. ;^

•fev' ''"fi'f,-''.--'p;:ifcli^.*'

;^.

l

i^.*'.'V-' -m?"-.-i^-;

.1 lfi':l

,f|fe

P.-j.' '-

ft|l;i.,-

ife**''

litef"W;-':.IT&v . 11-;:'

TOTAL FIELDPROTON MAGNETOMETER(bockgrsund 59,000 nT)

*

B.L. 2N

MAXMIN E HORIZONTAL LOOP 444 Hz.

B.L.

Lin* Ui Station UOONl

2NOy*rburtf*n s 10 m

tooo

1000

1000

. o .

•10

- 80

eo

MAXMIN E HORIZONTAL LOOP 1777 Hi.

- ;o

- 90

40

-90

•O

PROPOSEDDIAMOND DRILL HOLE

BERRY OROUP 112500

FIGURE 3"••'•^^;^^v--: ; M-v;#^

. - . •. ;^.,;: 'v ..'., ^ - - v'..' --,. i^v•••; ;i:^--;s^-"-^:'''-••"•'V: ' ;" J'' v ''•--'^-v : -:-..;

PPliS'i

LiSjSiM&^lf.Jti 1 :11 " 11 --. 1 '-", .

3.1 INTRODUCTION

.' v--' ; v~ 10 rv.... Vf

3.0 HIGHWAY GROUP

The Highway Group is situated in Drayton Township, Patricia Mining Division,

District of Kenora and consists of the following four unpatented, contiguous mining

claims (Figure 4).

•J- Pa-590156 Pa-646329

Pa-590157 Pa-646330

The property is conveniently accessible by car southwest from Sioux Lookout

via highway 72, to highway 664, which is then followed westerly for a distance of

1.2 km, at which point the highway crosses the northern half of the property.

.ft*-ilfefe4.™^' -- ^•••:

* lp®,v:V". 'm^^--^.

3.2 LINE CUTTING

The line cutting was carried out by Ken Bernier of Sioux Lookout during

the period from August 20 through August 23, 1983, inclusive. The survey grid,

consisting of 6.325 line km, was oriented east-west with grid lines trending north-

south at 100 m intervals along the baseline. Twenty-five metre stations were

established on all lines.

DERRY,' MICHENER

piMMiifHi^l^f^^.; :''-- : :cv#?

^vx^CLAIM LOCATION SKETCH

lo ImlU iJ-.'•••••ri f

p^ffv-'x,^^*.,'*?™;p:3|fp^-.^

^•©^f^fe'v'-'

fellS^-v

KpS^feitetiisl

|"' : ,; : ' ;'':,s,::p-

m^

^5*w;;,tjiim


};: ; ?, The ground geophyscial surveys were carried out during the period from

August 28 through August 29, 1983, inclusive, under the direct supervision of R. E.

Routledge, M.Se.


The magnetometer survey (Ref. Map 101) was able to further define the

regional magnetic trends mapped on the property by the Geological Survey of Canada

and published in Geophysical Papers 1138G and 1147G.

The results of the magnetometer survey indicate the property to be underlain

by a metasedimentar'y sequence consisting predominately of clastic metasediments

interbedded with arkose.

The clastic metasediments have been magnetically inferred to occupy the

southern half and northern quarter of the survey area and are characterized by

somewhat erratic magnetic relief in the range of 1,000 nT to 3,000 nT above local

background.

The magnetically inferred arkosic unit occupies a 150 m wide zone,

interbedded with the clastic metasediments, lying parallel to and immediately north

of the baseline and is characterized by a region of moderately/low uniform magnetic;-::: V;:'.,; • : ,':""": . . - " ' ' •••''''••^'^^^^^.^•(.:'; . ^ '.f.'A" relief in the range of 900 to 1,000 nT above local background.' ^

~ - - ' ' - ' - - - - - - - 1DERRY. MICHENER. BOOTH 'ft WAHL

i

i

Sv-.

T f ' . :

l

fpW#-T-t" • sSfei:,'^

Mm

3.3.2 Georira VLF Electromagnetic Survey ' .:'p:^--:^-±.-: .. : i.''

The VLF electromagnetic survey {Ref. Map 102) identified two anomalous

conductive zones, designated as HG-1 and HG-2a and 2b, onUhe/property^ V ^

Conductor HG-1 is located in the southwest corner of the property on claim

Pa-590157 and is identified by a very weak, low angle, in-phase response accompanied

by much more diagnostic reverse sense quadrature response. The poor in-phase

response could be an indication of varved clay in the underlying glacial tuff." ' ''- 1 ' ' ' : ' - ' '. ' ''..'''"'. ;V :''" i '. .- . J ; 'V ' ' ,,'.' J . '••'''•' : ' ''•I'.'v.''-/'.''-."' '- ' \- ' '

Conductors HG-2a and 2b are centrally located within the survey area and

will be discussed together because it is felt that they are part of the same easterly

trending anomalous conductive horizon. Both conductors exhibit moderately strong

conductivity along the entire 700 m composite strike length. The zone is

characterized by a moderate in-phase response accompanied by a much more

diagnostic reverse sense quadrature response. As was the case with HG-1, the in-

phase respoase for HG-2a and 2b is thought to be distorted, to some extent, by the

presence of varved clays in the glacial till. Both conductors are open along strike

to the east and west.

3.3.3 Maxmin II Horizontal Loop Electromagnetic Survey

The Maxmin n horizontal loop electromagnetic survey {Ref. Maps 103 and.

104) was able to further define the VLF anomalies identified on the property.

'DERRY. MICHENER. BOOTH a ;WAHL

î^'tr1^1^?^^ f'^^^-'-v'^-T^'* '^':' :- """'':'-"'J'''

JIB*: ;-^ The electromagnetic response parameters indicate that conductor HG-1 is a. -. - -'^. ^ .-'- '~ \-,., ^ ',-V' '.. 'V'- 1 "';/. - \ 'i, ;: - .' - V ' - '" ~ ; ••'- -'

neâr^yerticalj'possibly southerly dipping conductive sheet, up to 10 m wide and

exhibitsfa; conductivity thickness of up to 74 mhos at 1777 Hz and 90 mhos at 444

Hz.f "The m iestjincrease in the conductivity with a decrease in frequency indicates

^;tlwt;%^:iL^'.ii5'Ja^Va.ii'd''' (b'e^ro'ck conductor.' The response parameters also suggest that

ihe'.''conductor; weakens to the east and strengthens to the west. HG-1 is open along

strike to the; west. ;; Depth to top calculations indicate that from 27 to 30 m of

glacial till, with varved clay interbeds, lie atop the conductor.

Conductor HG-1 appears to lie on the southern flank of a weak, 25-30 nT,

magnetic anomaly.

The electromagnetic response parameters indicate that conductors HG-2a

and 2b are both part of the same easterly trending zone, up to 35 m wide exhibit

a conductivity thickness on line 1+OOW of up to 25 mhos at l*7 ?? Hz and 150 mhos

at 444 Hz.

This increase in conductivity with a decrease in frequency indicates that

HG-2a and 2b are excellent bedrock conductors. The response parameters also

suggest that this conductive zone appears to weaken along strike in both directions.

Depth to top calculations indicate that from 15 to 24 m of glacial till lie atop the

zone.

Conductors HG-2a and 2b were found to be directly associated with a region

of above background magnetic relief in the range of 1200-1600 nT. ; .î, ; ' ;.

DERRY. MICHENER.

• JV tt- - v . :*m^":

- 15 -

3.4 CONCLUSIONS

" ; : ' :''v-' • •'•',.l::' : - ' - ' 'U' ' ;--' • ''^'••'^t' r/V^?^^i^s^^^^f^ Conductor HG-1 is a good, easterly trending, bedrock conductor: lying; with W

a clastic metasedimentary unit exhibiting a near-vertical to southerly dip;^tl||^ft^v,

Conductors HG-2a and 2b are both part of the same anomalous||;easteriy is-

trending, conductive zone inferred to lie within a magneticaUy''defihabie^TO^;.--withiri'^.:

the clastic metasediments, at or near the contact with the arkosic unit^ ;Trie;'v

causative body of conductors HG-2a and 2b is thought to be sulphide mineralizatioiiji

associated with the stratigraphic unit within the clastic metasediments. |,S- ^ ^ s

3.5 RECOMMENDATIONS

It is recommended that three claims be staked adjacent to Pa-590157 to

cover the possible western continuation of conductors HG-1 and HG-2o.

It is also recommended that anomaly HG-1 and anomalous zone HG-2a and

2b be tested by diamond drilling.

Figures 5 and 6 present the locations of the proposed diamond drill holes

and illustrate the geophysically inferred orientation of the causative bodies.

w**

MAXMIN H

HORIZONTAL LOOP1777 Hz

O.R X- — h-^-^ ——— wfr*^--* — A, .rr^ — y-ii.p.

MAXMIN X

HORIZONTAL LOOP Hz

Line l KX) W Stolion 0(503

O -

- - lo -

-•20 -

- -so -

150 mPROPOSED

DIAMOND DRILL HOLE HIGHWAY GROUP

h 2500, ,

FIGURE 3

':^; ; Vv?v ^i-%; - ;4:S^'i :'^C*'^??^i(fi

.*i '^'5'ii1 ; 1 '.iS L- k' '• 1 /' 1'.' '- ' *'-~ ' " ' " .'

?;? ' ?

w'a^'i •••"'"-'*j' i- - :- '"'

TOTAL FIELD PROTON MAGNETOMETER

(bockground 59,000 nT)

4S

O.P. x..-

MAXMIN H HORIZONTAL LOOP 1777 Hi.

i.r.

ss

1900 i

{*00

1100

M looo

N O

-10

•to

•M

MAXMIN H HORIZONTAL LOOP 444 Hi. •'•*

-10

•to

10

58

Lin* 3 * 00W Station 3115 S

4S

•l No. 2

Overburdenft 25 to 30m

ISO M

N

PROPOSED DIAMOND DRILL HOLE

HIGHWAY GROUP

. lw . l : 2500 l———H. FIGURE 6

4.0 GOODIE CREEK GROUP

4.1 INTRODUCTION ' , . , ;- v" /^' ' ''-^ • '^M'^VVi:''' v— ' - .,-

The Goodie Creek claim group is situated in Lamond Township, Patricia

Mining Division, District of Kenora and consists of the following six unpatented, • contiguous mining claims' (Figure 7). :: "'^'.^.W'fc'Yv^'"-" : ' ! '.'^^•''•f^^S^lvf '-' ; "'; -"

v Pa-590160

Pa-590167 Pa-590170

Pa-590171

Pa-590172

The property is readily accessible by truck southwest from Sioux Lookout,

via Highway 72 to Highway 664, which is then followed westerly to Goodie Creek,

a distance of approximately 30 km; at which point an old bush road trends

southeasterly to the H.E.P.C. transmission line which crosses the northwest corner

of the property. -

4.2 LINE CUTTING

The line cutting was carried out by Ken Bernier of Sioux Lookout during

the period from August 24 through August 30, 1983, inclusive. The survey grid,

consisting of 5.425 line km, was oriented east-west with grid lines trending north-

south at 100 m intervals along the baseline. Twenty-five metre stations were

-'established on all lines. .' •...•'•. ' .. - .- ' •••:.\^^i ' v -v ,r;' : yX^'- 1 .;!-' --- - ' - -. : '. ^'^'vvyV:^^,^'1 -

^'•i'-j'i^'v-.-'v' V;.,; iv .' ; - ' ' -' • .-••. , - - ,- , .,-,,t ... ; ',-,- t--:, . ... ^r.. ' ,- - - -.- - - ,..?-.-' - .- 1 - ,'... -.-' \, r.-*-# - -, -•'^'t&'^r,,.^-',:.' t v.* ••. i,- vv'.'-.! -v-u"-, iix[ iW'^..-i 't'V.^^^;-v-vv': . lii' ^ " ^''f^'v.^O': 1 ^-"-: /'"'-.•^/•^•^v;- "' 'DERRY,: MICHENER BOOTH?* •'W^HL;: :C : : : :' v: :' ; ': ; ?^'^''^'

W"^Kt^i^v WHIPPER LAKE AREA

e?-

wf /? /J/ X i l O N

O* ^

CLAIM LOCATION SKETCH ZlnchM tp l wilt . l" t.

5CG670

GOODIE CREEK

GROUP

* 86

Figur* 7

|'"I^-V •'•'•- •-.' ^^^M '; . - r^v*. --' - - "" '-' ^^^V ' ;

*V,* '" ' . . - -

'*fv~ *"' ' -

,g|.j.iir - ; ;P; :

i; ; :II fl ;f' !i "ti1f;IjVv

ifefBtfp. 1 .

Ip.;

®^pf^w;^;f^??^-#;^#'; :^^

';-- ; -'- v - '.- . : :. : '-"."" . '-' " ' ' : - ; ' - 20 - . ,-. r .v '•; , '•^, : ; ••••:." : - .-;. . , : . : ; ; --; -'- "-. \ ^•.••- :;' : -:-4.3 GEOPHYSICAL SURVEYS

• ' . " . , - - ' ". ." ' '- ' ' ' . . ' - '' -J

. ' -. "' -:*-:-;- . ^ - *- ' "i ;- - '-'- •' i .', ''''.'^•I'l/^'i^ii.'si*!'' 1**.*'^''^'*-' A'; '"*v*-;*

^l^^^^p^f; . ' - - . . ^•••ii'-Vr '':'. - l: 1-'-'.'.'"'".1 ' . - . . • •,- '-.f-f^-i- - "-. • ••.-..-•-.

- ' /',-. " - '- - ,- - ' viv'-7 J'.,-;'.: - -'"i : ',':.~

;. , - . ' : .•^.''.•.'•••'•,1 - " f'' :f''-. :V i "-

The ground geophysical surveys were carried out during the period from. . ; ' . .. . . . - - . ; ; ; ' : ; ,- - --- ..•'/•: .- .'-, .;,v ' -.'V ,- . '- • -

'•" August 30 through September 3, 1 983, inclusive, under

E. Routledge, M.Sc.


The magnetometer survey (Ref. Map 201) was

regional magnetic trends mapped on the property by the

and published in Geophysical Paper 1157G.

The results of the magnetometer survey indicate

by metavolcanic-metasedimentary sequence.

the direct Supsrvisipn of .R.- ' '- .'':'':;: : ' •''.• :r;K.^yy^:f'i^'.lr ::

. , . --i " ! ,* --.- j ' '-j'- -if. ,.- '\'i'. -" - ' ' '- . ' -' ' .' ' ' . ' . . .* - . ' ,-. .-- . r . -*- ,. , ; . 1i -^t;. T- 1- . '-.* - -; - - -- 'i , ,: -' -

. . ' . ..•'•.'..^:'.i'' ".l^^:^-:^'^''^'^^^,^^:

- ' ••..' - ''~',i : ' • •'•. - ••- ; ; '-' -'.. -. . :

able to further define the

Geological Survey of Canada

•' - ,- ' '

the property to be underlain

; - ' . -' - ' '. i .' '

The metavolcanic unit has been magnetically inferred to underlie almost

8096 of the survey area and is characterized by broad uniform regions of low toi

moderate magnetic relief, in the range of 900 to 1,450 nT above local background.

This unit has been interpreted to be an easterly striking, near-vertically dipping

intermediate to mafic flow. 1 -

The metasedimentary unit has been magnetically inferred to occupy the

remaining 2096 of the survey area, being confined to a band of approximately 100

m wide, striking easterly across the northern half ofVthe, survey area, and v is y

characterized by a narrow lenticular magnetic anomaly ; or up to 4,647 nT above ^

local background. This unit has been interpreted as aformation.

near-vertically dippi;ig iron

: ,' . ' ., .. ' ' ' ' . ' -V . . .- ','- f -- V ' 'H ' L ''-" . ' ' ^ '.J [ "' - "

!^g*'#^'-?V ̂ ' ^v : : . /. - ' ' ^K ••^DERR^" MICHENER. '' BOOTH ̂ WA&^t?^^ ;W--"i:'::.-:~:.--ti;P'*:''-. ' -' ' -' '." -. -': . ' -^,'- ' .•"..'••- ' ---; -^ ' - • •^'ify[S^'^:^/ . ;. •.- ..:."" . '-: "- .'^-"•.v.-

— -: .-•••- ' :^®'^wt-•^"••T'-. : \' ; :':-'.Y'";s ; :;'; v , v-;V.-;.-^ ; 'NH"V-'''-'V-'.'? ---- V^s 1-: ir 01 - .;" , - ' . '' . - --' ' '•--•^LV.:,-.-' r.- ', - -••.;--'..^-:...^.. , •*.l i..'"'V'i;'; .-fi v;'fe./- * A ' --' ' - . '- .vi"^^'; •^^/'•••:•^:>:^^•' ::^.-''?'^^ :H ; • ;I; ^''^''^•*-•^•Ji'^•••(;''^'•'''^'• ;'.^' .; '' - ' ' -- - ' - ' ; • i '"' :

:^;' r 4.3.2 ; Gebnics VLF Electromagnetic Survey

"lBlES^t:38^ -- - . " : ' : .'-.: -* ;;^ The VLF electromagnetic survey (Ref. Map 202) identified two anomalous

••"•y:c'6hductive^zone"s^''de'signat'6d'riMV'GGG-l and GCG-2 on the property.' ' T -v - - ' '" ' - : V^H'.

;,' j- iv^y concuctor^GCG^liis'located in the southwest corner of the property and is.' ! :r?^' : ^ I:'^:;^fe,^;^'v^-v^j^::?;-^-.:':^., ' '-' " - identified !by^ al j moderate,; 'low? angle, in-phase response accompanied by a very weakmuch less definitive similar sense quadrature response. The moderate, low angle,

-0'.:; • : : 1 ;:.-- i ...fr: v : -': ;" -'5 ' ':- v-' ' : ;:v" : '/\ ;i " ;-'.- : ;7 -: ' ' .--- -- ' ' .

in-phase .response coupled With the vweak similar sense quadrature response suggests

that GCG-1 is a poor conductor.\:-:-: ' V - :: , ; v;-; ' 1. 1 .; l;';' '. , .' :- 1 .; i-.-'' . .f.: : .'''~'.. ' - ' . ; . 'l'-: - " "'' . ' "'

•if. ". - ' : , : ''., .: ':"'" ; ' . •''••' ^'.".' '••••' ", ' ': ' ''- ' •;f-; •'''•"''VK'- . ' : --' . ."' ' : . ' ;:"' - '' '. ' ' . ' : " -V'

Conductor GCG-2 is located in the north central portion of the survey area

lying approximately parallel to, and 50 to TOO m north of the baseline and is

characterized by an erratic, low angle, in-phase response accompanied by a

moderately strong reverse sense quadrature response. The erratic, low angle, in-

phase response coupled with thi. moderately strong, reserve sense, quadrature1 - ' . ' ' - '

response, suggests that GCG-2 is a good conductor associated with a region of high

magnetic gradients. Conductor GCG-2 was found to lie along the southern flank of

a major magnetic anomaly inferred to be an easterly trending iron formation.

4.3.3 Maxmin II Hori7X)ntal Loop Electromagnetic Survey

The Maxmin II horizontal loop electromagnetic survey (Ref. Maps 203 and

204) washable to further define the VLF anomalies identified on the propety.•'•"'^ '''-' ; '' v ' ''. j " " ' ' '-''. ' '." -,- ' ' '. - '- ' , . -'- . : '.- '-.- -s - ' - ' . . '' - ' . . . ' . "' - - ' ' '. ' . . ' '' - -' ' , ',

'.' " '" . -' '"- 3 -- ' ' "' .' - ' - ' -' - "' - ' ' ' . ' - "i -' \ '- ~

"' • •' .'' ' '', ''' '' '' 'ri 1 ' ' " - ' ' ; ' '. ' - : ' ' ' ' ' - . ' -. . -. ' ' ' " ' s - ' ' ' " ' ' - ' . ' - ' '* ' ' '--, 1 . , ' '-' -,- " ' : :-

•' '.''•'•''•', "'' '--'- '' :'. •'•- y'j- ' ' ; : '-' ; - J ' ' ' - ''-'\ ' ' ' . '-' . ' ' -~ ' ' '- ' . --' V '" '-' : .' " -' - -. . -.,. - ' ' ; . -.. -; r; : ' ' - ' - :. - - -. ' - ' . "- . ; '' - ' ' , " . ;

•'. -Vvv;;v'^^-^?r;.' : "' '"'' ' ; ' '.' "' ' ' " :''"V.v' ;. /''••. ' * :- ', ' - . , - ' .•'••" . •••''•'•- • ,"'".,'-' -J'--'. • .',": -."- ; '.'. i •'.•''

;s|||g||:gif|iAf^

||Rl|Kft-':Y|pR?;:-'-';

1^F'I. C - ".fit??'- 1 ' ' '

III,;::;"fffe- VV -'

fife i| ;.pC.'-* '|||; 'IffliM'B'Y' .- .

• T&r ^H '

m

7^^^*:^

^^g^W^^ :;:v';;v ;.-,'' ; ' -•"•- -Y'- Y ' "Y;-;-;;;;, Y.; 1 - 22'- :;The electromagnetic response parameters indicate that conductor GCG-1 is

..' . Y.Y;\Y^'; Y:*;:;V'.'Yv, :-,'V .'-•..:' : :- .a very weak conductor up to, 25 m wide and exhibits little^ if ;ahy In-phase response

and only a very w :ak quadrature response. The response parameters suggest that

conductor GCG-1 is a very poor conductor and could reflect conductive overburden

or an extremely deep conductor.

The electromagnetic response parameters

1 :" - |T '- - .'.: -, ' -"'- " : .- ' ' ' ' '-- - ''- ...\:"

indicate that conductor GCG-2 is' : . '. Y Y ' - ".-.Y', '. .. "/. :.. : - - - ,. -. •-•' '••-. •.••.-.'•'•f.: . ' ' . '.-ia near-vertical conductive sheet of indeterminate width and exhibits a conductivity,

' - - - - ' : . ' . '••"-.•, ' Y- '. ' . ' ' - , ' . -' '.' -' '. ' ' '' " - •-' thickness of up to 37 mhos at 1777 Hz and 150 mhos at 444 Hz. This four-fold

increase in the conductivity with a decrease in frequency indicates that GCG-2 is

an excellent, near-surface bedrock conductor. The response parameters also suggest

that the conductivity is variable along its 700 m strike length. Sixty-cycle

interference from the power transmission lines, located north of the conductor, has

distorted the northern shoulder resulting in the somewhat inferred dip and width

extent of the conductor. Depth to top calculations indicate that from 10 to 27 mV ; . ' .- : '

of overburden lie atop the conductor.'

As defined by the VLF survey conductor GCG-2 lies along the southern flank

of an easterly trending magnetic anomaly.

' ; ' : : \ . . :i-'-\ :. ; ; ' ;;: '^ ?-'l^Y.IY Y.;,Y .YV.C^Y:',. •:^;.-i?^^i;:^. :;,i, ;Y.^ , j': ; '4- ; -.^ ̂ : "••^•••^ ̂ j , ^

. ' ' ' /''' ."v Y .' ''-,: 1 '.* ' '.' ' .''^ '"': ' j', 1 -, i.' ' '' -' . ' ' ''. ' -' - "' i ' .- - •'•"iiV''. "' ' -.,'

Y'^TY;: ;."." : r- : -:-V''-: -' i; ' r -- '^^ ' : : .Y-. V , ,- '.";',: V"'-YY;, :Y: ,Y.--.-'-;. • -..

' . ,

. ' ' ; . ' '-- ..' ' -' ' , ' ' : ' ' ' '- "' ~ - : ' • •'. ''.

' . "' . ' " ' ' ~ "' . ' ' '. ' ' ' ' '-

W^^-^^^^: -- DERRY^ Mlci^^^^^i;IS

m

4.4 CONCLUSIONS

Conductor GCG-2 is a poor conductor and is probably a reflection of

YYconductive overburden. '

; Y AiY4 Conductor GCG-2 is an excellent near-surfaca vertically:; dippjhgj^hductor;'

lying on the souther ri flank of a strong; regional magnetic anomaly interpreted tp be

an iron formation. Conductor GCG-2 could possibly be the sulphide facies of this

iron f or m ali on. Y' ;^ l \^;

4.5 RECOMMENDATIONS

It is recommended that conductor GCG-2 be tested by diamond drilling.

Figure 8 presents the location of the proposed diamond drill hole and

illustrates the geophysically inferred orientation of the causative body.X : v

S:iyYYY^YY;;'feyt ;"'''-''^Y: ;yY-:Y'-

li*,TOTALS .FIELD.:^.;;^^;:^ PROTON MAGNETOMETER

(bockground 59,000 nT)

^sim-/

MAXMIN H HORIZONTAL LOOP 1777 Hi.

8.L. -t

Lin* 3+OOW1

Stotion l*OONj~l

No.

Omburdtn16 to 27m

^i^l&K^J^t'^^; ^^^-sl^j^fe^i^fe.^'tiiliiitei

4000 *T

•ooo

tooo

1000

- so

- 40

IS,** H-

1 -. ' --^

-Hw -'i"

x^" "*V

3.L.

. ^-- — trntn — ' — '|N - r^'

'"*"/'"'^'• 10

-10

-40 .

PROPOSED DIAMOND DRILLS

GOODIE C REEK ^ GROUP'^ ?' If

liiiiliiifi

saKeiswee34 WHIPPER LAKE 900

atural Resources;DG1CAL - GEOCHEMICAL ATA STATEMENT

Pile.

wST.-,.

K•tfti--

li

I ffi'f fr

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(g} Magnetometer-Electromagnetic (VLF s Maxmin) Township or Area _ frfoipper Lake-pravton-Lamond_________ l Claim Holder(g) Nahannj Mines Ltd._________________ l

Suite 1107-3.30 Bav St.. Toronto.—.-——— Survey (Vimpany Dfirry, Michqrier f Bootfo S Wahl——^———-——-Author of Report n. a. wahl r lAddress of Author . Snit-.ft 23Q2-4Q1 Bay St.. Toronto

Covering Dates of Survey Aug. J 5/83 to Oct.(bncoittln{ to of/let)

Total Miles of Line Hm 21.425 kro

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes VLF line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic.—Magnetometer——Radiometric——

DAYS pec claim

40

20

(Maxmin II) 20

GeologicalGeochemical

MINING CLAIMS TRAVERSED Llit numerically ;: V

Fa 590158*^Pa 590

AIRBORNF^ CREDITS (SpecW provUlon aediti do not apply to airborne lurveyi)

Magnetometer .Electromagnetic.

nATR- Oct. 14/83

(enter (Uyi per clkim)

.:^/^Au

.Radiometric

V'^' '.'::

(mincer)

- Whipper Lake•4***|*tl**244**t****t|t*******'

..P.a..7.0596iV

..P.a..7.05Q63.

..p.a..5aoi56.'

..Pa-646329

S.uihoh bf Riport or A(tnt

..Ea..5aQ16Q.

P ^;fIP p

leIn

ii•5'''",Si:.': ';"w/

SC:' :i;t?'i'' ;

i

Res. Geol. Oiialifiratinnt lo^.^QO^

Previous SurveysFile No. Type Date Claim Holder

- .

..Ka..59Q169.V^...,R. Laoond.....................

..Ba..59Q120.^........................................,

..BB..S90121^\.........M.......................^....

Pa 590172*^ : ^ '

TnrA' n r AiMCf 19

tar ivivii^it'' ' • ; 'fe^ : - !5'9-- i^'^ ̂ - '•••• : : -:. ' - ^ ;r ' \ { i^ffifc:^-'^??-:.^ '"-"^ ^•:^;^^*ri?i;^- ; - i '^; ^;; *" ̂ •• ;'- ;:,-v^^x;;J ; :'!-^^"-;

V^S/:;^^'•': ^y : - : """' ;; - " J GEOPHYSICAI^f ECHNICAiyDATA^' ; .'v'"'",- 'P^T**'-'-- - '•'"'•.••"•'i-'-''':'-''-' " ' ' •'.'.•/y./"'"'.; y: : : yy ''y.//-:---/ -yy--' '". .'ffi;:'i;." GROUND SURVEYS,— If more loan one survey, specify data for each type of survey

Number of S tai i . .s 857 each Mag-VLF-Maxmin' i-, 1 '- : . ' ' ' ' '^'•'•• ;J '-''' .!:'.'-.^'': 'i -' .Station mterva, -... —:——25 ^i—————";-- 'y :'- : "y' ''—

Profile yc3 !^. j.'.cm.to 10% fofrfcoth VfiF and Maxroin

.Number of Readings 657 each Mag-VLF-Maxmin

.Line spacing_____100-ro____________

ife;. Contour interval., 200 nT, s 10QO nT-as required .f or structural dafirtition-:.IKt.".^.-.: -. . . . , *

i^'ru f^-^PW?'; :' w r^K--' 'Z•;" .? . Tc

Instrument gci.nt-.rex MP-2. Total Proton

•Accuracy — Scale constant — :-~..Diurnal correction method r Closed Innp - Hmo

Base Station check-in interval (hours)Base Station location and value -Ai/uppgellne " 5r:M____as basa

b?on

Instrument G9onice VLF Ma•vm^n TT

Coil configuration —CopliCoil separation ___Mqyn|iln..Tx-jt.y TOO ro.Accuracy . -l* Tn-phasft

Method: 6D Fixed transmitter (vlf) D Shoot back Ci.it-.Tgr. Main 17.R RH^1 - Maynin II 444 \\z - ft^1777 Hz.

(ipcdfy V.L.F. ttition)Parameters m,....,,rf m-phase and quadrature____________

In linc(Maxmin)Q Parallel line

Instrument,

Ol

Scale constant,Corrections made.

Base station value and location

Elevation accuracy.

Instrument ————————— Method D Time Domain Parameters — On time ———

-Off time ^^,

[~1 Frequency Domain _ Frequency_____ Range ____'..:

— Delay time.— Integration time.

Power.Electrode array — Electrode spacing.

of electrode

'" " ^''Vi^ .- r''1 '""Tff'&l' ''•^f r v ^'- ' **;*LT' -" ' ' -" "' ' ' " " -' ' i'- 1 *" - -" ''

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1288'280-

k28T

The Mining Act

, ,.'; v Instruction) 1, r*- PlcaioiV-.-'rA^Vr'V&^ir'jiu.p

- !: fxcefdsspace on this form, aiischii lit i.'•Note:,— Only, day* creditsfr.celcuiaiccfih.l 1 '!-

"Expenditures" secilon may be 'entered . , i: in ; the "Expend. Days Cr," column*

• ••n-:.':. ^f- : '*" .Oo not use ihadedireas below.-:' - ":

r (VLF and MaxMin)

film HoldorU) •.^-.-..••' - -.r,;, 1 : 1*:, -;;- - 'Naharini' Mines Limited

jT

1. -J

Towuhip or Ar ea

No.T-951;;^Suite•fii07'3C)lfiay' Street, Toronto, Ontario, M5H:.2S8—'-•~—---^^ ' ' - " - ' --

Suryey Company f.,. ,,Wahl

bate oi'suwiy (from ft tol tdtti Mliii of linti Cut"""; 5.425 km

Name end Addross of Author (of Gao-Technlcal report) . ' ' : - f•'•'•('ffi;.'*-,: '^','\' '-^^f1 ,W^~ • -"•-'-'•; -'--"--^-^K Suite 2302,-'4Q1 Bay Street, 1 ' Toronto, Ontario' • 'tASH^^^^.^^^-Jliredit? Requested per Each Claim in Columiis at fight Mining CJaims Tfaverteci (List in numerical sequence) 'iftff^ ^ ; ' :-v'-Ji

;... ..-....--. ! -..J..;. For;fint lurveys'-: A '^'^^

/Enter 40 dav^'iThiiH:'!; &j.xln.cludt! line cuttino)^;^-

(For each additibnal turvey)'; Ruling the *arne grid; -.' ;.v',V : '' I^J1 Enter 20 deyi (for each)?''' '' '••

.',Complete reverie side /i v j ^and enter totel(s) here ',ty 5

Gaophyilcal

Li1- E lectromejnjtlc

: :- - Radiometric

Geological

Gaochamlcal

Gtophytlccl

- Elcctromagnttlc

- Magn*t6meter

- Radiometric

Uayl par Claim

20

Oayt ptr Claim

Mining CliilmPrafix

PaNumber

590168 ^590167

; 590169590170590171

.590172

'.Note: Special provisions 'jgj: i' crediti'do not apply ;'

ji'-f- t o Airborne Surveyi.

Electromagnetic

Magnetometer

Radiometric

xpenditures (excludes power stripping)pe of Work Performed .'.i :' ' ' ! " •

clatipn t Expenditure Oayt Crtditi

. . .pt*l Otyl Ocdti m*y b* *pport!on*d *t th* cltlm hold*r'(

Enter,number of diyi credlti per cl*lm i*!*ct*d - *t rljht, -'~'-^ : c '.

October 14/83iCertifjcation Verifying Report of Work

certify that l have* pertonai and intimate knowledge of the (ecu tei forth in the Report of Work annexed heref., having performed the work ing end/or after its completion end the annexed repon it true.

•od Pottal Addren pf Pereon Certifying'nl;: P.Eng;, Derry, Michener, Booth t. Wahl, Suite 2302, 401 Bay Street.

' "DatfOct. 14,' 1983

ri) "^ 7 7iToronto;- Ontario^ M5H 2V4*p .V'V:'- ' ••''i /-" ' ' -- 1- ' -- '.' ' . ' .- '.' ' ' 1

Expend. Days Cr.

Mining ClaimPrufix Number

Expand. Day* Cr,'

Note: - Only days crctfiu" calculated *ih the ;'; "Expenditures" tociion rrviy bc in the "Expend, Days Cr." columns,

- Do not use fhadod areas btlow,I ho Mining Actc,r A raa

Drayton'tElectromagnetic (VLF and MaxMin)

Street. Toronto, Ontario M5H 2S8uryay Company ;, . ; : ! —

- Booth Wahime and Address Of Author (of Oeo-Tachnical report)

ptG•;KWahl;y'P: .1 Erig.y Suite 2302, 401 Bay Street, Toronto, Ontario M5H 2Y4.Credits Requested per Each Claim in Columns at ri

Special Pfpvllioni,.,:-,^^-.; J;.,;i^^^:^^;:, 1:'^^;^;:l&Fbf flnt lurvey:' X'^W

Iff o?, each additional survey:-. fe' iijlnji the iarna prid; v:;; '^ ;

^'Complete reverse side, ffiffi'. """-'-1'enter/total (s)' '-'•'"••'}

Wi'Vs'W'f-".',:/. ?ii-''.: ' . . ' ;-.-.-.'.'f.^- j ^^s'f&.ffe"!'''''--"-'..;;^'

Airborne Credits

^Npta; Special provislonrf';j|^|'.':crediti do not apply;? ^•'^4 to'Alrporne Surveyiv''^^^r?;4:; .'' -i'^-; A' i&fe^i-.jnft.'i-:'-,-,. •:.:-'ft.^'

Geophysical

/LP Electromagnetic

- Magnetometer

' - Radiometric

'•s - Other

Geological

Geochemical

Geophysical

, ;: - Electromagnetic

; - Magnetometer

, ! ; ; - Radiometric

;. - Other

Geological

Geochemical

Elactromagnatlc

Magnetometer

Radiometric

Expenditures (excludes power stripping)

Di vi par Claim

40

20

20

Diyi par Claim

Da yi par Claim

Mining Claims Traversed (List In numerical sequence)

ypa Of.Work Porlormed t/'^":••'•••',--felite V',-'aSi:' :

Clalm(s). •

Cculatlon o xpenditure D*ys Creditsi-';--:'-'. ' - ' '... ': v ' ,-/ Tptal expenditures . ,'sXp- ,

Total Days C'adlii

fTplaf Day* Credits may be apportioned at the claim holder's Kc^iblce, Enter, number of days credits par claim selected ,'ln columns at fight, ' v,,'' .

Mining ClaimPrefix

PaNumber

590156590157646329646330

AECElVEl

.PATRICIA M INING DIV.

i ^H A- f-

Expand Days C

80

808080

m

P.M.

:rtt)?;

Pr.fixMining Claim

NumberExpand. Days Cr.

Total nurnbar ol mining claims covered by this report of work, c

f leat ion Verifying Report ofWork

For Office Use Only

'Wjftby ceaify that l have a penonal and intimate knowledge of the fecu set forth in the Report of Work annexed hereto, having performed the work 4or witneited tame during and/or after its completion and the annexed report ii true.amt and Poiltl Address Of Person Ctrllfylng

feo y'; Wahl , ; P jEng . , Derry , Michener. Booth f. Wahl, Suite 2302. 401 Bay^tree.t.W^:X) v :-".-'." ' ; ^ :i ri"'. ; L"; ' "'"'"V^ "v r' . , P . , n ~. . ' " DneCeriilied Certip*8 by (Sijn*turi),'

Octt 1 4| 1 983 ^7* W,

Sn^jvC^) 1' /Ylt'^Geochenfiical 8 ntj Expenditures)

The Mining Art

Nota: -' : Ooly . days: . ,, . .. , . , ,,... - .' l"Ex|X)ncJituiesv..s*cti6n riCiy .l)n-*-ri)iMi\'), ; ';

-.—:0o not Ose shaded areoi bMoW. ' \ :' ; i

!jagnetotter--Electromagiietic ( VLF and MaxMin II)Towmhip or Area

•-v-: ,-

Ii;Nahanni Mines LimitedAddrei* . -.

Whipper Lake Pi -j Pr 01 p* c t o rTT. l cen ce bio.

l T-951

Su/vey Company ,".V^--,;X••(f. 'X';'-, V u - ' i*: , ' '•••'' .'V:'; 'y

Street, Toronto, Ontario M5H 2S8l Date of Survey (Troml

lDerryi(Michener, Booth ft WahlName and Address of Author (of Geo-Tezhnical report)

I'D^'G"j Wahl^PÊng., Suite 2302, 401 Bay Street, Toronto, Ontario M5H 2Y4

Total Milei of tine Cut9.675 km

Credits Requested per Each Claim in Columns at rightSpecl'il Provision* . . , i-.vi :, •v- ;" ,; -'':'- C"' 1 '.: ;- - "; ;;; :!-S ;'

fc " '"' first survey: , " ;', : V*:' ::;' .

S,iV-,V'.:: Enter ilO days. (This C/J, ;'s^ --'..Includes line cutting) jT.Ws'i' ,5 ''-V/ v;-/--- - : --'"-îrf •••. '- . .'' '•'•-,'.-' - , - : : ;-S- •W For each additional survey: :-"?f usina the same orid: ; '..-.j','-"- ,' * - --- -. - . - :' -;;'-~??.'.*'.-

^f; .1 Enter 20 days (for each) :

ilii'^silir^?*y^^"'''V^^:^M'® Complete'reverse side'iK?lt lêndenter'totaKs) hepe^^S";

|fel: -^fefe^:5^r; ;-: : ';:;tf|;: i^te^±--'-\ --r* w®-*?f;V r/'."1,;"^.' 1-" ' -'' •-•' - ; '.^-'/-'-US'? -'f'.''--: '•'-•'.W: pHv-'.'"-./'-".;' -- •--.'•:.'?vW,TM-; :,". -.--.'.. •,-. i .: - ' ' i'-.-''-'*, ;^,|;;-,.';.;::. ; :'.--;v .--.•' •,--'^:-?--:

^'f'y' -.- V". .; "^ '. '--.--V'-"Airborne Credit* . ••,. V 'j,VJ., v ,.';..; . ' ' . .. , - 1 - .' ; . • •~.:' j?.;-5l; : ;,'-. !';.''-V' ,.:- ,; ,-- .' ," ••':.'-'i! ^'••'"••'•f..;.-. ' ! - : . '- .i ;. :-v;, i/i" Note: Special provisions ji'j'itS^f ̂ - credits do not apply;-; JJ'*y:?iv to Airborne Surwysv

JHff-V- ,'; .'. ";;; - . -'-, • '.•.••••f.ftS

Geophyiice!

^LP Electromagnetic

'';- - Maenetomster

' - Radiometric

, '/other MaxMinGeological

Geochemical

.Geophyilcal '

•V'. :.*, Glactromapnatlc

i!; ' Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

40

20

20

l?.*y* P*r Claim

——————

De y J per Claim

Mining Claims Traversed (List in numerical sequence)

Typ* O* Work Performed ' ;.;V'

Performed on Galm(s)'it:.:

lculation of Expenditure Payi Credit*' -' '-"-.' ' , , :;.L ", . - -Expendli jr*i;j,:-;âK-- :: -!v ',

Totil Day* Crrdit*

,l Day* Credit* may be apportioned at the claim holder'*

i choice.'Enter number of.day* credit* per claim (elected column* et right, iO),.:

Mining ClaimPrefix

PaNumber

590158590159590161590162590163,590164705961705962705963

PATRICIA MININ(5DIV.

A.M.nCT20.9fti

Expend. Day* Cr,

808080so80

80

80

80

80

vti

Mining ClaimPrefix

JING

NumberExpend. De y i Cr,

———Al

.' : ,',, v , Total number of ipining^••.f'iVV;.1' s" !"'i- '••'claims covered by'ihls'K*'report of

*

Pate;iOct. 14, 1983

s

For Office Use OnlyTotal Days Cr. Recorded

Date necoroeo

OcT-Ofte Approved ei Hecoroeo Brencn Director

Verifying Report of Workf*by certify that l have 8 personal and intimate knowledge of the facn set forth in the Report of Work annexed hereto, having performed the work

'.' O r witnessed same during and/or after it* completion and the annexed report it true.

x and Poital Addreii of Person Certifying' i- Wahl, P. En g. /Perry , M ichener . Booth fc Wahl, Suite 2302, 401 Bay^Strcet.r~'~~'"',',",r"r -. " '.' ,, ~̂ ~,~. " " ~ One Certified CeriLk*a by /Si*n*rti'el //I^Toronto, Ontario M5H 2Y4

'9rV.

One CertifiedOct. 14, 1983

,-.. Lands Comments ;

. 1 .Geophysics

Wlih to lee ageln with correction!

..To: Geology - Expenditures

••'•r* \:M-^.-:.. li'';-'? 1 '."^ 1 '.,^! ^-'-, i' 1-" 1 ' .'Appf0v*d'' :' i}'1 ' D Wlin to le* again with correctloni

"-'--'' ••' ' '••-'ToYGeocKemistry ' •-'/^•-

^rj Approved [j Wlih to i*e again with correction!

To; Mining Lands Section, Room 6462, Whitney Block,

.??^^

fmm''v.-v^.?v3D*ta .'i,;/. ;,.;.yjv

March 29 , 1984 ; '

ji-iejgjjssi^^wmrt1 . \ .': -'. ., - -- ' ' ' ' ' '-.' - - ' * - *

'MINES LIMITED. .

LAKE AREA ,

^|;;^' S;:. Type of turvey and number of fev'-^ ***t*sment day* credit per claim Mining Claim* Autmd

E jectrornagnitlc , -:MIN - '20 :""-' ;-

' d*yi ' PA 590157 to 59 inclusive 590161 to 64 inclusive 646330 705961 -62

^lSI;Wi"'S':;', : ''" :l*. .'- -f.: - -' j -- . '.r|j,t |on '•;:.:'" ;.

II^^Mji^daya.^lI];^!- 1 -; \ . Airborne S^'^^M^'i^V-':'^.;--;;-;.^'-^;'-:'

D

4 'Special provision Ground

;;C3;i: Credit!'have been'reduced because of partial

LJ,' Credits have been reduced because of corrections ^^ to'work dates and figures of applicant.fe:rS'l':''' '..'.i--'' 1 i:.-..''" - - t '"-^V '

•- '' i' -- '", v - ' • •'''\^:,:''J*'.' . .'.'- ' r ..' ^: . " -; -'A-^V'"'-

:-^S^^;^^;

;Ml:Pv ' : r'fil

^Special credits under lection 77 (16) for the following mining claimi

15:DAYS MAX MIN

'PAI 590167 y ;;i?590170 to 72 inclusive

10 DAYS MAX MIN

PA 590156 590168 - 69

di'creditt have been allowed for the following mining claimi

LJ lniu(fici*nt ttchnicil data filtd

]hft Mining Recorder max reduce the above credits if necessary In order that the total number o) approved assessment days recorded on ' aM'clalm'does pot exceed the maximum allowed as follows; Geophysical — 60; Geological — 40; Geochemical —40; Siction 77(19)—60;

ITeiphiplcaf Aseowmenf VHfc'*.^^ .''. - ''^'v: ;'lf:

Del*March 29, 1 984:

2.6093Minlno Recorder'! Report ofWork*0' 83-114,115,

LIMITED

r LAMOND. i-WHIPPER LAKE AREA;'

|^|f)ijypr o( *iirvey a nd number of; ' :|^ Assessment days credit per c laim Mining Clilmt AttMMd

* i EiKtrom* jnttle ••••"•''r'l1 '""'::: 1 -tttirti -^K*t:A;.##iK-:;:^' : ^

40

20

' k''~ ' ; " '•'' -'' ii' h| r

PA 590157 to 59 inclusive 590161 to 64 inclusive 646329 -30 705961 to 63 inclusive

. dtyt

Section 77 (18) 8*1 "Mining Clilmt AiiMted" c olumn

,f Geological —

|Ge.pcherriiC8l.——,

Special provision ua^-; r

Airborne CD

Qround S

(3 Credits have been "reduced because of partial^'coverageo'clalms;^ 1 ^ .wm^m^.-.'' -'

LJ,; Credits have been reduced because of corrections *P^ 'to work dates and figures of applicant.

^Special credit! under section 77 (16) for the following mining clairm

ffll 15 DAYS MAGNETOMETER20 DAYS VLF AND10 DAYS MAGNETOMETER

PA 590168

m^^-M:-:^:^:-.^y-^'-' inclusive4o credit! hive been allowed for the following mining claimi

B;|^3 -hotiyfflcienily covered by the lurvey; :

D Insufficient tKhnicil dau filed

i&vWWtM®*M*-\- Pf^-^^.vicJ'" • ••i' 1 . -v - - '.. ' ' ',

CThe Mining Recorder may reduce the above credits if necessary In order that the total number of approved assessment days recorded on ' h Valm does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 7709I—60;

jfflftiZff^

Hanson V Recorder.; \/i;;:

Natural ResourcesOntario

We have received reports and maps for a Geophysical;;^.E ^ ectroP5a ?' net '' c a n:1 I'agnctonetcr and V.L.F.) survey suU)1ttcd under Special Provisions {credit for Performance

on rnlnlna claims PA 590156 et al 1n tde :rbwn2iiips of Drayton ; and Lamond and the Area of Whipper''' ''

This material will be examined and assessed and a ;'statei:ient of assessment work credits will be Issued.

Yours very truly,

t^^ft*;V:-v; ^i.^'i E. F. r Anderson -. Director Land Management Branch

i t j : - . fc. f l f ,. f tf i t*

P^M^iV;^ Director B*.^^.-/^. 1 -;:;-?---.-::"^-'':

|SiS ^''l: ' ; ^;;rUhitnoy Block, Room 6643 iK'lii^'^Wcenf s Park' '.' ,: . - ; SP^/ilf^-S'^'^Joronto, 'OntarioSS.,r: fr- few.-' -i'' ; ^':VVf inn., "l no ' . . ' -. .

•1380

Limited•p j ' . . " ' ' ' . w "' ••••V. ,-,':

), Ontario

U.G, Wahl P.Eng. Suite 2302 401 (Jay Street Toronto, Ontario M5H 2Y4

iEj&j'-uV.;'.' ;,*mfr^:r-'^^:'V-vr ;*. ;^-v " -, --., -';.

^feMl

Your File: 83-114,115,116 , Our File: 2.6093

l bert Hanson Recorder,"y of Natural Resources v

).VBox 669 O - " . - . ,,jux lookout, Ontario

vV'îPpV^TO - ; - -.'- ' . '.:feiîfi--:.-,. ;. - -; ,.. -. '\, ..v,.,;,'-:,... . -.- - ,- :,^' ^ sllDearjSir:':' . ^ . .^.;v ;:..;;0 .'. ' ,, ^ • ;^r---. "- ,^'. ' :"-:': " :' ,";:: "':-"'

;;f; Ênclosed are two copies of a Notice of Intent with statements:v-;; :7. uî,-,-; :-, ' '. .- .- y r ,.-.. ,, ,-;^r, , ' .. ' . ,'' - - - . ' :....^^..it; ;:i?f 1,1 sting a reduced rate of assessment work credits to be allowedt?|5V

1 "; ; for a technical survey. Please forward one copy to the recordedjl* { : holder o f the claims and retain the other. Jn approximately '^tjjjUljty. v|fifteen days from the above dateVâ'final letter of approval;of^^; :-these credits will be sent to yoi/.t'On receipt of the appr

: .letter, you may then change the work entries on the claim ^'sheets. ' ' . -.'- . . : .-,'. ; '/,;.. .... ' . -. ' - , -.-^' ""*-jj' j i -

"further information, if required, please contact?'^' F- w - Matthews at 416/965-6918;" ' "

Yours very truly,

m-,W('-fr't-'-^YS}[.\';'V:-.

i. E/Yundtrector

Land Management Branch

Whitney Block, Room 6643Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1316

m^'^'M'vl&fytf^ '^!-i&fev-1/-'

&V&!

cc: Nehanni Mines LimitedC?0:v Suite 1107 -

:V;:: 330 Bay Street; Toronto, Ontario

- M5H 2S8

ccV7 Mr, G.H. Ferguson V Mining A Lands Commissioner 845s; Toronto, Ontario\-,'r '-.!x:d \ -'. '•

v'v'^y'-^K

9^

•ai^^.^w*?^^.!ÎgJl^Pînistryof . :,-,;.,; .;; :!, Vv ; Notice of Intent',-. ; - - . ^ - -:^

Natural ; :'for Technical Reports

1984 03 29 :

2.6093/83-114.115,116

of your survey report indicates that the requirements of The Ontario Mining been fully met to warrant maximum assessment.work credits. This notice is

;vi;.s) claims,'you may during the next fifteen days apply to the Mining and Lands Commissioner for extension of time. Abstracts should be sent with your application. '-i ;r ^f

tM" : v-i; If the reduced rate of credits does not jeopardize the status of the claims then you neecl notfrom the Mining and Lands Commissioner and this Notice of Intent may be

^survey was submitted and assessed.under the' "Special Provision-Performance and tH^ls^ Coverage^method and you are of the opinion that a re-appraisal under, the "Man-days" ,^^|;|;j|;-methdd would result in the approval of a greater number of days credit per claim, you may, ^|j!Jj|^,withinthe^said fifteen day period, submit assessment work breakdowns listing the employees |j0^'"|f|ârnes,:adc)resses and the dates and hours they worked. The new work breakdowns should be *^;ii|vH^ submitted direct to the Lands Management Branch, Toronto. The report will be re-assessed and Ifflrl^fsi new statement of credits based on actual days worked will be issued.

ftSO^t^'^-^:^^^mt&.^m.^îS^M:.-;..;r,.; Vtei;-^ 1 ;

'

P^V-v-,-P-/'ir-;,-

f&aw^-.'f-'•^-•'••'- - ..jfe^':-;-.'^-^'''- - :mim

Your Filei 83-114,115,116 Our Pilei 2.6093

Mr. Albert Hanson '. /. ;,". . ' '.;'r;" :---; Mining Recorder ; :: 'v'^v'^-'^ Ministry of Natural ResourcesP.O. BOX 669 ••; .-•.. ,- ;, ' /V-,;-Sioux Lookout, Ontario vPOV 2TO -- ' ; - - " . - ...- .;:: .;: ' ':v:

Dear,

REx Notice of Intent dated March 29, 1984. Geophysical (Electromagnetic 6 Magnetometer and V.L.P.) Survey on Mining Claims PA 590156 et al in the Townships of Drayton and Lnmond and the area of Whipper Lake.

The assessment work credits as listed with the above mentioned Notice of Intent, have beon approved as of the above date. :

Please inform the recorded holder of these mining claims and so indicate on your records.

Yours sincerely,

S.E. YundtDirectorLand Management Branch

Whitney Block, Room 6643Queen's ParkToronto, OntarioM7A 1W3Phono: (416) 965-6918

D. Kinyig:cc

cc: Nahanni Mines Limited Suite 1107 330 Bay Street Toronto, Ontario M5H 2S8

cci Mr; G.H. FergusonMining S Lands Commissioner

v;:.:.|'v;: ' jToi'dnt(5,'- ::'Ontario ̂ "̂ .•^•^"^•^•'•i

cci Resident GeologistSioux Lookout, Ontario

^'•"'^••^•^.^'^•"'-vS -'- ' '" -^f^^î^M^..'^; :S,:(- ^./;.sim^Bfes^t^

O - -tv\9/

- ..:-'.-;;-"*(4i"v - . .: - •••'•' . •vî'r^ ;' .";i ••"•;.' •••.••!.V-"..-:^M .^.;;'-.'^ ';-^;:;^"-îa| •- '":- ~'/ :.1"' --' Jv .'., ;. '.: x'v'yj^l

•'•j^:--:^:.-,.^'^^^.

SdVW!

-V-^-lIf'•: ;,-':IS^

B:^-^::,^:iiI

4 N

2 N

B. L

Z S

4 S

391

1000

j- 979 t- 995

Pa 646329

^^—P?T 590157

roi

OJi

O i

UJ LU CM

52J84SWTO10 52KaiS*0034 WHIPPER LAKE200

D

LJro

i

HWY 664

LEGEND

RELATIVE C ONDUCTIVITY

Poor

Excellent

ELECTROMAGNETIC SURVEY

SCALE

METRES

NAhANNl MINES LTDHIGHWAY GROUP

MAGNETOMETER SURVEY

( B ackground 59,000 nT

DERRY, MICHENER, BOOTH ft WAHL

SURVEY BY

D. R.

URAWN BY; J B.

APPROVED BY

D G. W.

N.T.S.

52 04 S.WDATE-

AUG. 1983

DWG. No

10

A V

X A

In Phase Quadrature

NAHANNIHIGHWAY GROUP

VLF - EM 16 SURVEY

NAA CUTLER, MAINE 17.8 kHz

DERRY, MICHENER, BOOTH E* WAHL

4 N

2 N

B. L.

2 S

4 S

ro CVJl

Oi

LU LJCJ

i

UJ ro

i

s2K®iswe834 WHIPPER LAKE 320

HWY 664

LEGEND

x -

x - \

25.

•X --

I.P OP

6 3

l O

\ -19 \ -9

-20 -10

M,

x-2

6 5

4 3

30 20 10 O 10 ZO 30 l l l l————l————l————l

4 ive - neg

l P (INPHASE)

- O.P (OUT OF PHASE)

25Conductivity

(mhos)

10Depth

( m etres)

Conductor axis

SCALE

ME TRES

NAhANiMl MINES LTD,HIGHWAY GROUP

ELECTROMAGNETIC

SURVEY

444 Hz.


SURVEY BY C. D.

DRAWN BY:

J. B.

APPROVED B'r D. 6. W.

N.T.S.

52 J 4 S.W.

DATE

AUG. 1963

DWG. No

103

4 N

2 N

B. L.

2 S

4 S

Pa 646330 , 8 /,x

ro i

(Mi

Oi

.J

L±J LU CO

LUro

52KeiswM34 WHIPPER LAKE S30 ^lk/0

HWY. 664

LEGEND

. K -

X -

25.

-x --

l.P OP

6 3

l O

___ E] ——— -20 -10. - L ' i i

-4 -2

8 5

6 5

4 3

30 20 10 O 10 20 30

- neg

---x-

l.P (INPHASE)

---x-- O.P (OUT OF PHASE)

25Conductivity

( mhos)

10Depth

C metres)

Conductor axis

100SCALE

METRES

200 300

NAHANN MINES LTDHIGHWAY GROUP

ELECTROMAGNETIC

SURVEY

I777 Hz.


SURVEY

C. D.

DRAWN BY:

J. B.

APPROVED BY D. 6. W.

N.T.S.

52 J4 S.W,

DATE:

AUG. 1983

DWG. No.

I04

B. L

4 S

52J04SW0dl0 52K01SW0e34 WHIPPER LAKE

iniro

ioo

l-l

ol

-l

UJ

l-I

UJCO

i-J

UJro

i-i

240

LEGEND

RELATIVE CONDUCTIVITY

Poor

Excellent


SCALE

100 200

METRES

300

NAHANNI MINES LTD.GOODIE C REEK G ROUP

MAGNETOMETER SURVEY

( Background 59,000 nT

DERRY, MICHENER, BOOTH a WAHL

SURVEY

D. R.

DRAWN BY:

J. B.

APPROVED BY

D. G! W.

N.T. S.

52 J4 S.W.

DATE '

SEPT. 1983

ffi Ne

201

LEGEND

O^ PoorIn Phase Quadrature

Excellent

\ \

HANNI MINESGOODIE C REEK G ROUP

VLF - EM 16 SURVEYD. G . WAHL

NAA CUTLER, MAINE 17.8 kHz

DWG. No

20252o04s*eeie 52K8iswee34 WHIPPER LAKEDERRY, MICHENER, BOOTH a WAHL

590167

2 N

B. L.

a590170

2 s

4 S

D

.—a a

-6

52K81SWM34 WHIPPER LAKE 260

(\- 2 -

- 3 -

- 14

-17 -

- 16

- 12 -

-10 -

- 7 -

-8 -

-9 -

-. 8 --

-7

- 7

- 8

-81-

. e -

- 8 -

- B -

- 5 -

y6

. 3

10 Ifv\\\i

1i

1 -4 , . -

1 \

A2 . .

-13 .

\ .\ i:: -3 ; — - — ' — ̂ i7 c

i- 1 / - 1;;i - 1i i\ - 2

\\f f

X ^

i ii

0

2 -

3 .

3 '

12 .

| 4

,l

;l/

I - 9 f

f

-4 -T .

1-\ - 3 .

-1 -7 .

l -j

. A"O -

-5 '

- e *

- B -

-1 - 9 -

p

-2 -9 C

0 - 9 -

- 8 -

"ft1

- 7 *.1 1 1

- 7 -1 1

-6 i1

- 3 .

f2

, - 1\ \

. - 1

C

\

i

}1

' 1^t

tr'-'

- 1

0

1,1* " 1 "i/* # "

\Jt

\

1 l

*

Vl l1l i

j-l - i1 lJ -ifi1

l

l,'i

4 -4 .

3 - .^

\o ;

-4 .

^. -7 . 5 .

\.j ::- 32

1 ™'-32 -

- 16

f- 4 .:

1

- 3

0 -7

- 10

l . ,1-M\

. 0 -5

i - 1 6

1,. - 1 -8f ——GCG-T

-7

J.2

l

. . - 'r/-\ 590168

-12 -/

•' 4

NL2,tv, ,:

fx ^V\ \\ X

-9* * * - 5 0 J21

-t JJJ-7- '-50-

r- 4 ^s^ - 40/\/^

• 2 4 - fc

fi V. '. - l - 4 .

!\\ 0 - 4 -

A ., .ir "J - - " - 1 5 90169 1

i . - 3 .

J l -T/-

(J 1.'.0 - 9 -It- -^

^ --

0 -8 -

. . - 5 -

- 7 -

-3 -

-3 ,i l 1

1 -6 *11

- 3 -|

1 - 4 .

J

J^

-10 -(I

- 1 0

, 12.5 ( : i

' i- 9 - -72 -

\ t , 1

-63 1

^ — ' ^

2 -2 .\

^. . -7 - 2 -

//-, .6 i-

| t

' 0 - 7 -

1 B '

; 1 1 1'i ~ 7 '

V , ., ii\ ..i

^^.0 ——. - 6 .

| il 2 e 'r i

-2. -7 .

•' /..1 ,y.

0\i.' :/'

i0

A^r\ 0\\ - 1

1

1

2

yyi \z

\

590171

/r*4

JT* —

- 9 -j

.e -

*

^^

-li

^^-20 -

- a35̂

^^*-*1*^ - 18 -

— -" 6C6 - 2 - 6 .

f 1.-z. -

l 1y i' - 2 \

^ -5 .

- 7 .

2 -B ,

1f

0

\f.

-

- 9 -

•^- 5

- 7 .

- 2 .

- 2 *

3e

- 2

2 - l *

-7. .LV

—

!

f

J,

J^ ^

0

{. . .4i\- -8 *. - -^ 60 f 10

\ "~" -*

.^r-. 2 5

-10 1 V -16 -1 Ji yQ ' s. 9 . * - 7 -

/;" rl -4

V.i.1 -,-.1l

X 590172', - 2 -

0*. - 6 HyQ - 4 ^

1 - 3 -

1 .2 -

1 - 4 -

- 2 -

- 3 -

- 3 -

9X .

l)

' Jt J

i ^^^^* , - 4

!\0 - -7 f

t 0 - 8 *

l ..i1

1 -7 '* - 1 - ' * -

1 1

-s!.i i.0 -ei

\. J,il.'-.

,: - 1 - 3 .\.Llf 0 . 5 .

i| /': ..11-2 -12 1

j!I - 2 -19 -

\.' i - 1 -20.1

-1 - 7 -

- 5 -

-

-

ini

— a

roi

D

CJl

5l

O i

UJ

i

UJCM

i

-t O *

1,1 J,\

l

,/

V

-2

- 2

i

\-2

UJro

i

a

•a

LEGEND

X -

x -

Oo

25 ,

X -

I.R OP

6 3

l O

-6

-19 \ -9

___ ei .__ -20 -10- - ' i i

' x'•15 -7

' f

-4 -2

8 5

6 5

30 2 0 1 0 O 10 20 30

ive -neg

—— "——— — l.P (INPHASE)

- O.P (OUT OF PHASE)

Depth , 0 ( metres)———— C —

25Conductivity

(mhos)

Conductor axis

SCALE

100 200

E5M EIRE S

300

NAHANNI MINES LTD.GOODIE CREEK GROUP

ELECTROMAGNETIC

SURVEY

444 Hz.

DERRY, MICHENER, BOOTH a WAHL

SURVEY BY'

c.o.DRAWN BY: J. B.

APPROVED BY D. G.W.

N.T.S.

52 J 4 S. W,

DATE '

SEPT. 1 983

DWG. No

203

D

590167

2 N

B L .

D

590170

2 S

4 S

S2JMSKW1* 52K9ISWee34 WHIPPER LAKE 270

ro i

CM i

Oi

LU

i

LUCM

l

UJ

rei

-J

LEGEND

I.P OP

x -

x -

o o

-x --

-li -6

-19 \ -9

——— g] .—— -20 -ID

25. J !

* r /

30 20 10 O 10 20 30

i ve -neg

— l P (INPHASE)

-- O.P (OUT OF PHASE)

c25

Conductivity { mhos)

Depth metres)

Conductor axis

SCALE

100 200

!55METRES

300

NAHANNI MINES LTD.GOODIE C REEK G ROUP

ELECTROMAGNETIC

SURVEY

1777 Hz.

DERRY, MICHENER, BOOTH S WAHL

SURVEY BY: C. D.

DRAWN BY' J. B.

APPROVED B Y D. G. W.

N.T.S.

52 J4 S.W.

DATE '

SEPT. 1983

DWG No

204

RELATIVE CONDUCTIVITY


MINES LTD.NAHANNIBERRY GROUP

APPROVED BY

D. S. W.MAGNETOMETER SURVEY

( Background 59,OOOnT)

^TDERRY, MICHENER, BOOTH a WAHL52J04SWW18 52K31SW0834 SHIPPER LAKE

In Phase Quadrature

52K81SWM34 WHIPPH? LAKE 230

NAHANNI MINES LTD.BERRY GROUP

SURVEY BY

C. B.

DRAWN BY;

J. B.

VLF - EM 16 SURVEY

NAA CUTLER, MAINE 1 7.8 k Hz.

________-26093DERRY, MICHENER, BOOTH a WAHL

APPROVED BV

D. G. W-

N.T.S.

52 J 4 S.W,

DATE AUG. 1983

DWG. No

302

l

6 N

4 N

Z N

A.

2 S

4 S

UJ 00

-l

5SKsiiswea34 WHIPPER LAKE 300

LEGEND

x -

x -

I.P OP

6 3

O O

25 " 4

•X -

•X -

-19 \ -9

5 '. V. —— -20 -10

8 5

6 5

4 3

30 20 10 O 10 20 30 l————l————t————l————' ' '

ive -neg

—— I.P (INPHASE)

---x---,*-- O.P (OUT OF PHASE)

Depth metres)

25Conductivity

{ mhos)

Conductor a xis

SCALE 100 200

^SdE

METRES

300


ELECTROMAGNETIC

SURVEY

444 Hz.

DERRY, MICHENER, BOOTH S WAHL

SURVEY BY- C. D.

DRAWN BY- J. B.

APPROVED BY' D. G. W.

N.T.S. 52 J 4 S.W

DATE - AUG. 1983

DWG. No

303

6 N

4 N

2 N

B. L

2 S

4 S

saxeisweea* WHIPPER LAKE 310

LEGEND

x ^

25

h-

•X4

l.R OP

4 l

6 3

S 3

-19 \ -9

'•15 -7,'V' -4 -2

8 5

6 5

4 3

30 20 10 O 10 20 30l____l____l____\____I....... .. l li l ve -neg

—— r——— —— IP (INPHASE)

-.^X--.^-- O.P (OUT O F PHASE)

Conductivity ! mhos)

10Depth

( metres)

Conductor axis

100

SCALE

METRES

200 300


ELECTROMAGNETIC

SURVEY

I777 Hz.

DERRY, MICHENER, BOOTH B WAHL

SURVEY C. 0.

DRAWN BY:

J. B.

APPROVED BY'

D. G. W.

N.T. S. 52 J 4 S.W.

DATE AUG. I983

DWG. No.

304

sekciswotm whipper lake · !'m'r^'?..the berry claim group is situated in the...

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