42c12nwm95 42c12nwtos6 molson lake diamond … · 42c12nwm95 42c12nwtos6 molson lake 010 diamond...
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42C12NWM95 42C12NWTOS6 MOLSON LAKE 010
DIAMOND DRILLING
i
TOV.'NSHIP! Molson Lake REPORT No,: 27
WORK PERFORMED BY: Lac Minerals Ltd.
CLAIM No.
SSM 607779 SSM 607779 SSM 607751 SSM 607757 SSM 625564 SSM 607755 SSM 607754
SSM 607755 SSM 607762
fi
SSM 625569 SSM 607760 SSM 607759 SSM 607775 SSM 607777 SSM 607800 SSM 607782 SSM 607783 SSM 607806
HOLE No.
J-7-3 K-7-1 1-9-1 1-7-1 1-6-2 1-8-4 1-8-1 1-8-2 1-8-3 1-8-5 J-8-1 J-8-2 J-6-1 J-8-5 J-7-1 J-8-3 J-8-4 K-7-2 K-8-1 K-8-2 L-8-1
FOOTAGE DATE NOTE
ISOm150m153m279m225m159m177m163m150m162m121m249m150m210m141m249m735m144m156m735m321m
Aug/83Aug/83Aug/83Sept/83Aug/83July/83July/83July/83July/83July/83July/83July/83Aug/83Sept/83Aug/83Aug/83Sept/83Aug/83Aug/83Aug/83Sept/83
(l)(l)(l)(D(D(l)(D(D(D(l)(D(D(l)(l)(D(D(D(l)(D(D(D
Tor:
NOTES! (l) #134-84SSM. S, #221-84TB
LAST REVISION NOV 1 1. 1 983
PAGE 01 OF 05
EXPLANATION OF GEOLOG CODES.
***t (Cx " COLUMN no. x )
KEYS
/ Upper Tier of Data Entrv L Lower Tier of Data Entrv
(CI)
R Remark A Assav
K Kev Mor i 2 on S Survev
FLAGS X L ( C 2 - 4 ) (Preceded bv appropiate kev)
KOOi Ore Horizon TopK002 Ore Horizon BottomTOP TopSUR Survev AdditionsVGD Visible Gold
HED Header RemarksSUM Summarv RemarksSAM Sample TakenDBT Di abase TopAZM Azimuth Estimation
LOC GRD LucationSTR StructureMAG Magnetic UnitDBB Diabase Bottom
A Anhedral
CRYSTAL MORPHOLOGY L(C19)
E Euhedral S Subhedral
ROCKS /(C24-27)
BR/D Breccia DvkeCADI Carbonate DiopsideFLIN Felsic IntrusiveGOUG GouaeININ Intermediate
Intrusive LAMP Lamorophvre MFVL Ma-fic Volcanic PELT Pelite .sediment
with prains *ClX16m not visible to the CASG
naked eve.
FXPP Felsic Porphvrv BRECCHER Chert DI/DFLVL Felsic Volcanic GFSCGRPH Graphite INASINVL Intermediate
Volcanic IRFM LOST Lost Core MFIN SCHS Schist PEGM QZVN Quarz Vein SAND
Casi no
Breccia Di abase Dvke Graphitic Schist Intermediate Ash- now Tuf-f Iron Formation Ma-fic Intrusive Pepmati te Sandstone, sediment with orns MX16mrK2fl
PAGE 02TYPIFYING MINERALS
QUALIFYING MATERIALS/(C2Q-29). /L(C30-31) /LCC32-34). L(C30-31)
AC ActinoliteBI BiotiteCL ChloriteFL plagioclaseGA GarnetKF K-FdsMG MaonetitePX pvroxeneQX Quartz CrystalsST StauroliteCD ChloritoidTR TremoliteDI Diopsidr
AS ArsenopvriteBO BorniteCP ChalcopyriteFP Fds. PhencicrvstsGR GraphiteKY KvaniteMU MuscovitePY PvriteQZ QuartzTO TourmalinePB LeadAH AshFT Fluorite
AX AmphiboleCB CarbonateEP EpidoteFX Fds. generalHE HematiteLP LapilliPO PyrrhotiteQE Quartz EveRF Rock FragmentKA KayolinAP ApatiteFT FluoriteAH Ash
BI BiotiteMS Muscovite-sericiteQ2 QuartzBA Barite
ALTERATION MINERALS /L(C57-66)
CB Carbonate KYOE Ba-rich muscovite GAST Staurolite TO
Kvanite Garnet Tourmali ne
AS Arsenopvrite PY Pvrite
ORE MINERALS /L{69-74)
GD RG
Gold Real oar
MO Molybdenite SB Stibnite
AC ActinoliteEP EpidoteMG MagnetiteCD Chloritoid
ADDITIONAL MINERALS XX /L(C67.6B)YY /l
CL ChloriteGA GarnetPO pyrrhotiteSP Sphalerite
CP ChalcopyriteHE HematiteOR Orpiment
TEXTURES C Z 5 ~
ttF FlowBD BeddedEQ EquiGranularLM LaminatedMY Mylonitic
CL BN FO LP PP
Cleavaoe Banded Foli ated Lapi11 i Porphvritic
SS So-ft Sediment De-formation
8
BR G: MS SC XB
Breccia Graded Bedded Massive Shistose Cross Beddino
m
PAGE 03OPEN/CLOSED STRUCTURE 0/C L(C42)
O Open implies -framework is matrix supported.
C Closed implies -fragments of any sise are clast supported.
CL CleavageBD BeddinqFO FoliationQV Quartz Vein
STRUCTURE FEATURE IDS /HC49-50)
F/ FaultBN BandinqLM LaminationSC Schistosity
/D DvkeC/ ContactLN LineationVN Vein. General
HOW SCALE /LCC57.59.....) (Most Dominant Mode)
tt Breccia Filling< Micro VeinB BlebsE EnvelopesI Eves. AuqenL LaminatedO SpotsR Rosettesx'l ClustersV Vein
U
* Sheeti no> Macro VeinC CoatinqsF Framework CrvstalsJ InterstitialM MassiveP PervasiveS Selvage
Eu-hedral CrvstalsY Dalmationite
* ClastA AmvgdaloidsD DisseminatedG GougeK StockworkN NodulesO Quilts/PatchesT Staininos. as in
Tarni sh Z Fresh. Primarv Rock
Extrmlv Poorlv Sorted Verv Poorlv Sorted Poorlv Sorted
DEGREE OF SORTING L(C39)
4 Mod. Poorlv Sorted 75 Moderatelv Sorted 86 Mod. Well Sorted 9
Well Sorted Verv Well Sorted Extrmlv Well Sorted
l Extremelv Angular "2 Verv Anqular3 Anoular
DEGREE OF ROUNDNESS L(40)
4 Moderately Angular 75 Intermediate 86 Moderatelv Rounded 9
Rounded Verv Rounded Extremely Rounded
SHAPE OR SPHERICITY L(C41) (N-Scale)
O Nil1 Extremelv Low2 Verv Low3 Low
4 Fairlv Low5 Moderate6 Fairlv High7 Verv Hioh
8 Extremelv High9 Exceptional lv High X
PAGE 04G - S C A L E (PERCENTAGE)
? O Possiblv Present: Identitv Questionable7 .07 Present But No Estimate PossibleO nil *
Ol, O3.1.3
l
1234
3510203040
506070
8 809 90 X 100
67
1 Darkest2 Verv DarkZ Dark4 Medium Dark5 Medium6 Medium Lioht7 Lioht
LIGHTNESS AND COLOUR
L C SCALES L(C28-29)
B Pale9 PalestN Noir (black)W WhiteA GravB BlueG Green
S - S C A L E (in milimeters)
P PurpleR RedT Tan (khaki)U UmberY Yellowt Suffix "ish*
O123
. 003
. 008. 03. 12
D
67
28
3.2
89 X
13l/2m
2m
COMBINATION MODES
O Fresh. Primarv Rock (Z) ( Z -for Zero )
Amvqdaloids (A), minor Macroveins O) and/or scattered crvstals
2 Macroveins O) and Veins (V) Veins (V)and Dalmationite (Y)
:Spots (S) or :Patches (D) (as : in Quilts)
4 Veins (V) and/or occasional Envelopes (E)
6 Pervasive (P) or
8 Pervasive (P) or
: Veins (V)LESS: Microveins (OTHAN: Selvaoes (S)
: Envelopes (E)
i Veins (V)GREATER: Microveins (OTHAN : Selvaqes (S)
: Envelopes (E)
X Massive (M) and/or Laminated Bedded (L)
Veins (V) and/or abundant Envelopes (E)
Pervasive : : Veins (V)(P) or :EQUAL: Microveins (O
: TO : Selvages (S)i : Envelopes (E)
Pervasive (P) or Disseminations (D).Veins (V). Microveins (O. Selvages (S), and Envelopes (E), with much Breccia -filling (tt), Stockwork (K), and/or Sheeting
i
UNITS AND S U B - U N I TS
(C 47)
P -Principal Geological Unit (PGI)A -PGI Same As Previous PGI Exept As Noted.R -Repeat Unit (replacing PGI over specified interval)D -Ditto (same as PGI exept as noted)
(C 23) -Percent Mix(percentage of PGI effected bv qualifying entry in col. 47)
T - SCALE
The thickness ofenteredin (F 48)corresponding structure
l i tho-f eatures such as dvkes. veins, sills, etc. can be using the T-Scale and entering the ID of the feature in the
ID field.
RANGE ASSIGNED VALUE
MODE THICKNESS
SCALE VALUE
DESCRIPTION TEXTURAL TERM
2mm 5mm 2cm 5cm
< 2m C 5m
1mm 3mm lcm 3cm 10cm 30cm 1m 3m 10m 30m
O123456789
thinlv laminarlaminatedverv thinthinmed. thinmediummed. thickthickverv thickextremlv thick
fissile fi ssile fiaggy siabbv blocky blocky blockv massive massive massive
F* F* FY SB BK BK BK MX MX MX
LAC MINERALS LTD.
LEGEND FOR GEOLOGICAL ENCODING FORM
FLAGS: used for highlighting information and specific horizons
KEY HORIZONS;
X001 visible top of mineralized zone synonamous with ore zoneK002 visible bottom of mineralized zone synonamous with ore zoneH001 top of mineralized zone within hanging wall rocksH002 bottom of mineralized zone within hanging wall rocksF001 top of mineralized zone within footwall rocksF002 bottom of mineralized zone within footwall rocks
*NOTE: other mineralized zones within hanging wall orfootwall rocks are designated as H003, B004, F003, F004, etc. with uneven numbers representing the top of the mineralized zone and even numbers representing the bottom.
ADDITIONAL INFORMATION;
VG visible goldSAM sample takenSTR structural remarkMAG magnetic zone
GEOLOGICAL "DATA ENTRIES
FROM - TO; defines the interval over which a particular rock type or characteristic occurs
REC%; * recovery of core
MIX *: * of a subunit or a modified unit within a primary rock unit
ROCK: indicates rock type
-2-
ROCK TYPE ABBREVIATIONS
BREC Breccia LAMP CADI Carbonate Diopside Unit - LOST CASG Casing MFIN CHER Chert MFSH UIAB Diabase Dyke MFVL FLIN Felsic Intrusive' MSSH FLVL Felsic Volcanic ' PEGM FPFV Felsic Volcanic Rock with PELT
Feldspar Crystals as dominan- fragment type
FXPP Feldspar Porphyry QEFV GFSC Graphite Schist GOUG GougeINAS Intermediate Ashflow QZVNININ Intermediate Intrusive SANDINVL Intermediate VolcanicIRFM Iron Formation SCHS
LamprophyreLost CoreMafic IntrusiveMafic SchistMafic VolcanicMuscovite SchistPegmatitePelite (grains predominantly
1/16 mm - not visible to the naked eye) Felsic volcanic rock with quartz-eyes as dominant frag ment type Quartz VeinSandstone (grains 1/16 mm to 2 mm) Schist
ROCK TYPES CHARACTERISTIC OF MAIN ORE BODY:
BART Barite RockMSSB Muscovite SchistSASH Stibnite/Realgar bearing Muscovite SchistSIRX Siliceous Rock
ET: Entry Type: Categorizes rock types using abbreviations D,M,S
U - Main Rock Type - forms majority of a specified interval
M - modification of main rock type over specified interval (all data is identical to tihe description of the main rock type except where specified).
S - sub-rock type contained entirely within a main rock type (eg. a FXPP within PELT)
T: average thickness in metres of a sub-rock type or of bedding or "~ banding in the main rock type
R-F MINERALS; indicates the main rock-forming minerals of the specified rock type
-3-
MINERAL ABBREVIATIONS
METALLIC MINERALS
As ArsenopyriteAu GoldBo BorniteTp ChalcopyriteHm HematiteMg MagnetiteMo MolybdeniteOr OrpimentPb GalenaPo PyrrhotitePy PyriteRg RealgarSb StibniteSp Sphalerite
NON-METALLIC MINERALS
Ac ActinoliteAp ApatiteAx Amphiboleba BariteBi BiotiteCb CarbonateCd ChloritoidCI ChloriteDi DiopsideEp EpidoteFt FluoriteFx Feldspar (composition
unspecified) Ga Garnet Gr Graphite Ka Kaolinite Ky Kyanite Ms Sericite Mu Muscovite Oe Oellacherite Pi Plagioclase Px Pyroxene Qz Quartz St Staurolite To Tourmaline Tr Tremolite
TYPIFYING MATERIAL: material(s) (with percentage) which typify specified rock type
ABBREVIATIONS
ASH AshAXB Amphibole BandsFP Feldspar PhenocrystsLAP Lapilli-size fragmentsQE Quartz Eyes
-4-
COL: shade and colour of rock
1 Darkest2 Very Dark3 Dark
SHADE AND COLOUR ABBREVIATIONS
4 Medium Dark 7 Light5 Medium B Pale6 Medium Light 9 Palest
A Grey B Blue G Green
Black
P PurpleR RedSP Salt and PepperT Tan
U UmberW WhiteY Yellow$ Suffix "ish"
CRN SIZE: grain size of rock described using the size scale
ABBREVIATIONS
FF - average size of fine fraction CF - average size of coarse fraction *C - * coarse fraction MP - maximum particle size
-5-
PARTICI.E DIAMETER SYMBOL RANGE (mm)
SIZE SCALE
EQUIVALENT GRAIN SIZE
o
l
2
3
4
5
6
7
C .004 mm
.004-.016
.016-.0^
.06-.25
.25-1
1-4
4-16
16-64
64-250
250-1000
> 1000
SEDIMENT
clay size
fine silt
medium-coarse silt
:ine sand
medium-coarse sand
grit/granule
small pebble*
medium-large pebble
cobbles
small-medium boulder
large boulder
OLCANOCLASTICS
fine ash
coarse -ash
small lapilli*
large lapilli*
cobble-size blocks
boulder size blocks
extra large blocks
-7-
TEXTURES:
TEXTURAL ABBREVIATIONS
BD Bedded BN Banded BR BrecciatedCL Cleavage EQ Equigranular FL Flow StructuresFO Foliated GB Graded Bedding LM LaminatedMS Massive . MY Mylonitic PP PorphyriticSC Schistose SS Soft Sediment XB Cross Bedding
XLMP; crystal or phenocryst morphology
ABBREVIATIONS
XL - phenocryst type (eg. FP) M - mode of occurrence
E Euhedral Crystals S Subhedral Crystals A Anhedral Crystals
P - maximum particle size (use size scale)
FC: fracture count; defined as the average number of fractures in l m of core for specified rock type
CO: competence scale; rock competency described using a scale from l to 5 with l being the most competent and 5 being the least competent
S1DP S2DP; Description and dip angle of 2 structural features in a unit. ' ~~~" Dip is measured from a plane'perpendicular to the core axis
(core normal angle).
-6-
CST MOR: clast morphology
ABBREVIATIONS
^p - sorting? described using degree of sorting scaleS - roundness, described using degree of roundness scalefp - sphericity, described using sphericity scaleO - open or matrix supportedC - closed or clast supported
1 Extremely Poorly Sorted
2 " Very Poorly-Sorted3 poorly Sorted
1 Extremely Angular2 Very Angular3 Angular
DEGREE OF SORTING
4 Moderately Poorly Sorted
5 Moderately Sorted6 Moderetely Well
Sorted
DEGREE OF ROUNDNESS
4 Moderately Angular5 Intermediate6 Moderately Rounded
7 Well Sorted
8 Very Well Sorted9 Extremely Well Sorted
7 Rounded8 Very Rounded9 Extremely Rounded
O Nil1 Extremely2 Very low
SPHERICITY
4 Fairly low5 Moderate6 Fairly High7 Very High
8 Extremely High9 Exceptionally High
-8-
STRUCTURAL ABBREVIATIONS
BD BeddingBN BandingCL CleavageCT ^.ontactDY DykeFO FoliationFT FeultGO GougeLM LaminationLN LineationQV Quartz VeinSC SchistositySP SlipVN Vein (General)
MINERALOGY; Observed minerals described by mode of occurrence and percentage of the total rock.
MODE OF OCCURENCE ABBREVIATIONS
A Anhedral CrystalsB BlebsC Envelopes or CoatingsD DisseminatedE Euhedral CrystalsJ Eyes, AugenJ InterstitialK StockworkL LaminatedN NodulesO SpotsP PervasiveQ PatchesR RosettesS Subhedral Crystals
T Tarnish or StainV VeinW BooksY Amygdaloidal or SpheruliticZ Selvagel Breccia Filling^ Micro Vein$ Sheeting1 Amount Dir.seminated ̂ Amount
in Veins2 Amount Disseminated Amount
in Veins3 Amount Disseminated^ Amount
in Veins
mli?
p lo
lo
lo
p
ppp lo
po
o 'o
o
to
p lo
o
L FUS
X Q^i3pK.O.Q^.j) IDEN6B0202MAINPRI^6DW02TUBQ830810CJB IPRJ LAC MINERALS LTD. SOOO O 50 MT 225 . 180. -45. XSCL MT.2MT.1
V O AB- OP V(*VcB V J* J J J
0813STLAMBTB308010B09 RBGRD 0, -j WHITE RIUER PROPERTY -
sLsLRRSTRS
Lt
RKAG/Lxi*RSTRRRR/rJL*
RSO 01RAZMRxLRSTRRKAGxLRSTRRRxLxLRRRRRRRSTRRRSTR
.' " '0 *'
-W^'RSTR--" ' r"'R
RRRSTRxL
, f-, s ' --fc- ; -'L- V ,;
0
288
256425642564
25643234
3978
39783978397839784813
48135050506592
659265926874
6874687468747513
8022
80228022802280228022802280228022919422
.-.p.- . .942294229647
. 9647S6479647
9647
280 OVER . P
2564 PELTQZAX BNF02314 7 P BN 25 gpo-AGBI FO 25U) K*
3978V. LEAN FACIES IRFM, UHICH IS WELL AND THINLY BANDED.3978BN AND FO VARIES FROM 10 TO 20DEG TO CXN.4813 IRFMQZAXPO*BNFO2334 8 P - L( - -MG -- .
AGPOFX* V) t - D? X-N4813FAIR TO STONG MAGNETISM. /~"( \3523 XFXPPQZFX PP. 2515 R D( ( A \)-^'
6ABI ^-S '4813 X PO- 2313 D BN 35 L*
SC FO 35 L(4813LOCALLY HIGHLY CRENULATED.4813PO MOSTLY IN DISITNCT LAMINATIONS (LOCALLY MASSIVE) UP TO 3MM4813THICK AND INTERGROUN UITH PY. U CONTACT OF THIS D INTERVAL IS4813MARKED BY 10CM OF CRUMBLED CHLORITIC CORE.6874 PELTQZFXAX*BNF02313 5 P BN IS
PABI FO 156874AX IN DISTINCT BANDS INTERGROUN UITH QZ.100 MT . 180. -45. .100 AZIMUTH AND INCLINATION ASSUMED, SINCE ACID TEST UITH UNLIKELY100 RESULT OF -46DEG.6974 X AX) D BN 25 GRD-
FO 25 Q. D- L- L)6874BN AND FO VARIES BETWEEN 15 AND 30DEG TO CXN.6874MAGNATIC INTERVAL.8022 CADIDIGAAX1BNSC3436 SP D*
7GCB V* D.8022BN AND SC VARY BETWEEN 0 AND 70DEG TO CXN.8022GA IDENTIFIED BY OGS - G. SARAGUSI (PER*. COMH) AS BROUN TO8022PINKISH BROUN VITREOUS MINERAL.8022 X D MG
D(9422 MFVLAXFX BNF02323 9 P BN 15 DID* PO
SG FO 15V+L* L) L- L*9422DI IN BANDS OF CADI UNIT UP TO 10 CM THICK WHICH ALSO CONTAIN9422DISS. LAMINATIONS (UP TO 1\) OF GA. INTERVAL ALSO INCLUDES LOCAL9422BLACK BANDS^UP'TO 10CM THICK CONTAINING UP TO 10* PY AND PO.9422THE BANDS ARE V.FINE GRAINED AND HAVE A HARDNESS OF ABOUT 7, SO9422ARE PROBABLY QZ RICH; THE BLACK COLOUR MAY BE DUE TO DISS.9422GRAPHITE.9422LOCAL KINK BAND WITH AXIS AT 40DEG TO CXN. BN AND FO VARIES9422BETUEEN 10 AND 50DEG TO CxN.9422HIGHLY FRACTURED -AND BROKEN UP CORE.9647 SCHSGR SCBR11 IP L+
20 Vi V29647HIGKLY FRACTURED CORE. ANGLE BETWEEN SC AND CxN IS HIGHLY9647VARIABLE. .10045ROCK IS MUCH SOFTER AND LOCALLY A LIGHT-GREEN COLOUR -UHAT10045MINERAL IS CAUSING THIS? (CL?) .10045FRACTURE COUNT IS APPROX 14.16286 PELTQZFXBI*BNF02334 5 P BN 25 D- PO
GAAX FO 25V* ^ D.10045 : X v -' D L*
; ;' : - '- ' ' i;-'-: ;l-i^" - ' ' .- - ;- . . .. L -J.... V* ' , .,.. . :
R R R5002 RAZM IR sL R R R R R s L R5003 RAZM
964796479647
10010010010114
101141011410853138451384513845
1384515015016286
16286
19214
16286PINK TO BROUNISH-PINK MINERAL IS COMMON ADJACENT TO QZ VEINS,162B6AND IS LOCALLY PRISMATIC OR HAS A RHOMBIC OUTLINE -COULD THIS I16286ANDALUSITE OR IS IT GARNET?150 MT , 180. -44, ,150 AZIMUTH fi. ACID TEST ASSUMED. TEST RESULT OF -45DEG CHANGED IN150 UIEU THAT ACID TESTS ARE CONSISTANTLY l TO 2DEG TOO STEEP.1017 XFXPPQZFXFP2PP 2525 R
BABI1017 ZONED FP-ROCK LOOXS SIMILAR TO THE SO-CALLED POPCORN UNIT OF T 1017 WILLIAMS PROPERTY.10864POSSIBLY REDDISH BROUN ANDALUSITE IN QZ UEIN.13853GREY METttLIC MINERAL UITH A HARDNESS OF 2-3 IN PEGM -COULD BE 138'.'3, BUT NOT REALLY IN A FORM ONE UOULD EXPECT. 15406 1PEGMQZFX 2525 R SPD( PO
UU D- DC D( 15406LOCAL CRYSTAL OF CHALCOPYRITE AND MAGNETITE IN PEGM. 200 MT , 180. -43. . .- .
TEST RESULT OF -44DEG (SEE 002).
192441924420020020841
21892218922189222483225225
BN FO
20 20U*
D-
R4
PO D(
MG D)
200 AZIMUTH AND INCL. ASSUMED. 21593 PELTQZFXAX*BNF02324
5ABI 19244 *FLULQZFXQE-
AU 19395 XPELTCLBICB1MS 24-5 P
2GCB19395HIGHLY FRACTURED, CRUMBLY CORE. 19395FAIRLY STRONGLY MAGNETIC. 225 MT . 180. -41. 225 AZM. 6. ACID TEST ASSUMED. 20859 XPEGMQZFX
AU FLULQZFXQE1FO
6ABIFP1 INULFXQZAX1FO
AGBIFP1MODERATELY MAGNETIC.AX INCREASES IN ABUNDANCE DOUN-HOLE AND FP DECREASES IN ABUNDANCE. SECTION OF PELT, MT . 108. -37. AZM, AND ACID TEST ASSUMED. TEST RESULT OF -38DEG (SEE S002)
TEST RESULT OF -42DEG (SEE SO02) R
2525 2 P FO
2425 4 P
25 D-
D. PO DC
'
l̂u oV
^ M**k *
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FROM TO
o
D
D
D
D
O
D
D
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O
O
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o
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RECOV. % ROCK 1MTM OM TX TXFCW* PC l 2CT 10 AZ* D** MS TO KY Bl ST XX PT SB GO YY
-H l l l l l mihlim l l l l l l i M M MT-
XLHPQMO 1C 7M OM2 TX TXSRSOSMLZ T O AZ*I WP QZ GA Ct C3 Bft ho AS MO RO ho
^EN6B0202MAINPR^(3'Dlf(nj2^) BQB30716CJB IPRJ LAcTllfrlERALS LTD. SOOO O 50 MT 163. 180. -45. /SCL MT.2MT.l ' O 728 OVER
0718STLAMBT8307130715 RB CRD 0. - WHITE RIVER PROJECT-f
-*- 2-z;728728
1318APPROX * FX WHICH MAY BE ALTERATION PRODUCT.10692
L S
L R s L R R SLRMAGRRRsLt
/
L
P. RS001 RAZM R s L R R s L R / L R R
. RSAM R SLRRRSAMSO 02^L
L R
PELTQZFXAX * BNF02 313PABI
1318 1691 X AX1 2425AGOOFF- '
1318 169lAPPARENTLY ALTERED PELT. 2021 2514 X
5 P flN FO
D BN FO
77
77
202120212514
25142514251425143655
4473
44734473447344735050505587
558755876135
61356691
69976997715171517812
781278128835100510692
D*
00 Q-
00
D- D7 D( 00
L* 00
FO L*
L-
D(CDD- 0(00
PO L) PO L-
SOME OF OFF- GA
2514PROBABLY CORRELATABLE WITH ROCKS IN TRENCH ON 1*OOW AT APPROX25142*75N.4473 X 000 D BN 5L* L) L*CDD( PO
FO 5V)D( D*00 L* 10692MAGNETIC PATCHES.10692CD IDENTIFIED AS GREEN OR BLUISH-GREEN OVOID AND RHOMBIC 10692PATCHES. THESE MAY BE LARGEr.Y TO CL AND MS, AND ARE PROBABLY 10692TKE SAME THING AS WHAT WAS IDENTIFIED AS CL BLEBS IN 1-8-1.3793 XFLVLQZFXQE1BNSC2314 R BN 7 L-
7AMU SC 7 10692 X BNSC D BN 5 V-L-
SC 5L*D*10692TABULAR MAGNETIC ILMENITE IN QZ VEIN WITH TO. 10692AX MED TO LIGHT GREEN, VARIABLY ALTERED TO CL. 10G92UHITE MINERAL CLASSIFIED AS KY COULD POSSIBLY BE AN AX. 10692LOCALLY WITH WELL DEVELOPED BLEACHED HALOES. 1005 . 183. -45. .1005 ACID TEST, AZIMUTH ESTIMATED. ALSO INCLINATION ESTIMATED SINCE 1005 TEST GAVE ANGLE OF 46DEG WHICH IS UNLIKELY.5884 XSCHSQZFXQX* R MGD- PO
3ABI D* D. L-5884PROBABLY HIGHLY ALTERED OR METAMORPHOSED PELT.5884AX MOSTLY 7G AND SOME ALTERED TO, CL. SOME AX IS LIGHT GA.6202 2SCHSFXAX SC 2324 R4SC 3
5G6202AX IS LIGHT GREEN IN.COLOUR (TREMOLITE?).6721 XMFINFXBICB1PP 24-5 R
GNCB7009LIGHT BLUISH GREY BAND WITH*ABUNDANT LIGHT COLOURED (GA) TO7009ALMOST COLOURLESS AX. .716 SAMPLE UM-19 TAKEN TO SEE IF ANY OF OFF-WHITE FIBROUS MINERAL7L6 IS AX AND NOT JUST KY. " '7951 XPELTQZFX. MS R D*
81 P2D*795lAPPARENTLY SILICIFIED PELT. GA (* LOCALLY ST) HAVE WELL7951DEVELOPED BLEACHED HALOES.8845UM-20 TAKEN FOR GENERAL PETROGRAPHY. 163 . 186.5 -43. . . .11113
11113 12018
11113111131111312018
IRFMQZFXMG-BNF025-5 6GABIAX-
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24653LOCAL BLUISH-GREY PATCH. THIS INTERVAL IS THE MOST SIMILAR TO 24653THE FOOTWALL OF THE WILLIAMS OREBODY, 25004 5FXPPQ2FXFP1PP 2575 R
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268
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2682739
246532465325004
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24653LOCAL BLUISH-GREY PATCH. THIS INTERVAL IS THE MOST SIMILAR TO 24653THE FOOTWALL OF THE WILLIAMS OREBODY.
25755FXPPQ2FXFP1PP7A
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0726STLAMBT8307190721 RB GRD 0.-- Q o WHITE RIVER PROJECT J7- o"" j
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2983451
PELTQZFXAX-BNF022 29 P BN 6L+ L( D- PO APBI FO 6V)D* O- D-
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GPBI Ql < ~ D C D-3451ALTERED PELT, PROBABLY CORRELATABLE WITH ALTERED PELT (IN 1-8-2 3451FLVL IN 1-8-4) AND PYRITE BEARING PELT (IN THE SAME K.'ISS) .3451 X AX l 2415
003451BANDING IS BETTER DEVELOPED,
i 1623 PELTQZBI BNF022 2 7 P BN LIV-
11623BANDING COMMONLY OBSCURED BY GROWTH OF KY PATCHES OF A LIGHT 11G23GREEN MINERAL WHICH COULD BE CL, 81, AS, OR A MIXTURE OF ALL 3. 11623SOKE OF WHAT IS THOUGH TO BE KY IS A LIGHT GREENISH BROWN AND 11623COULD BE AX INSTEAD.' LOCALLY COARSE (2-3MM). GA HAVE BLEACHED 11623HALOES. APPROX D+ AC AND LOCALLY BANDS OF A LIGHTER GREEN AX.
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126 . 185. -44.126 AZIMUTH ESTIMATED, SINCE TROPARI GAVE UNLIKELY READING OF 126 225.SDEG. 9558 XINVLQZFXFP-FO 25-5 R FO 15
RABIAX*9558COULO SO-CALLED INUL BE AN ALTERATION FEATURE? 10344 XO.ZVH R M4
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12001 12908
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13044 14964 X
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UABI17383 177 IRFM AX-BNF02315 P BN
PA MG* FO 17383 177 STRONGLY MAGNETIC,17383 177 VERY UELL BANDED. MUCH OF WHITE ANHEDRAL THROUGHOUT UNIT MAY 17383 177 BE KY, WHICH MAY THEREFORE BE PRESENT IN AMOUNTS UP TO 10V AX 17383 177 CRYSTALS MOSTLY ISOLATED IN GREY MORE SILICEOUS BANDS. 177 177 . 185. -42.177 177 ACID TEST, AZIMUTH ESTIMATED. ALSO 1DEG SUBTRACTED FROM ACID 177 177 TEST READING OF -43DEG SINCE ACID TESTS ARE CONSISTENTLY 1DEG 177 177 TOO HIGH.
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66 12249MS IS LIGHT GREEN AND IS INTERGROUN UITH CL. BOTH SEEM TO66 12249PSEUDOMORPH A PRISMATIC MINERAL (AX?). BANDING IS LESS UELL66 12249DEVELOPED IN THIS INTERVAL. POSSIBLY SOME REVERSE GRADING UITH65 122490RIGINALLY FINE GRAINED PELITIC TOPS NOU METAMORPHOSED TO THE66 12249COARSER GRAINED BANDS UITH KY, GA ETC. BASED ON THIS CRITERIA,66 12249HOUEVER, DEFINITIVE TOPS COULD NOT BE DETERMINED.675 100 . 182.5 -44. .8955 93 4INVLQZFXFP-FO 25-5 R5FO 12 D-
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. 182.5 -44. . 4INVLQZFXFP-FO 25-5 R5FO 12 D-
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1545 ACID TEST, AZIMUTH ESTIMATED. DIP ALSO ESTIMATED SINCE TEST 1545 RESULT OF 46DEG SEEMED UNLIKELY.
XIRFMQZFXMG*BNF022 2 R L* 7-4ABIAX- D)
11503LEAN IRFM - HOWEVER IS SIMILAR TO IRFM INTERSECTED IN 1-8-1 ANDAX VARIES FROM LIGHT TO DARK GREEN.
HSnSPOSSIBLE LOAD FEATURES INDICATE TOPS UP-HOLE.
PELTQZFX 4ABI.
FO P FO 10 L* V*D)
DCAXD. V-
V POORLY DEVELOPED BANDING (REWORKED MFVL?).X AX1 D L? OOOODC
00 QC 00COULD MUCH OF WHAT APPEARS TO BE FX BE KY? MAGNETIC PATCHES. AX IN BANDS UP TO 15CM THICK.
-FXPPQZFXFP1PP 2575 R . MG
545'-"'"''159.*^' ' ; X'': 185.5 —43. '' . -~ ' ; ' ' " - ~ ' - :'-" •'•-"ifi.?''? .-''- 1 'v-'rri545Xi59XAZIMUTHCESTIMATED SINCE TROPARl'GAVE UNLIKELY READING OF 191DEG.
iRSTRxl586S;15868POSSIBLE SCOUR FEATURE INDICATES TOPS UP-HOLE. : '": ; X ̂ ;^- v 5883~'-' 159--..KG;CONTENT-APPROX:*(IN BANDS). PY CONTENT APPROX ^(^LONG-XX;
)
t
PROJECT: IMTE RIUER TARGET: EES LAKE l.PCORE SJZE:BO __ ^~~~DRILLED BY: ST. UVKKT SURVEYED BY: R. BARAN LOGGED BY: C. BRADBROOKDATE STARTED: 29/8/83 DATE OmJETED: 1/9/83 DATE LOGGED: H*'**} ^LINE GRID AZltWTH: LINE: 14*OOE STATION: 3*25N UNITS OF fCASURE: UT ^^SURVEY GRID AZIKJTH:0.0 NORTHING: 10333.536 EASTING: 113B8.058 ELEV. 19317.074 TOT DEPTH: 153
1 DRILL HOLE Nfc I9J PROPERTY: WITE RIVER
)
i
'
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,
1
1
1
9
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R
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0
13.97
23.07
46.12,.
59.44'
64.05
75.02
77.46
83.92
87.15
92.75
94.27
102.83
102.83
153
TO
13.97
64.05
24
.54.02
"62.05
75.02
77.46
83.92
87.15
92.75
102.83
98.47
153
116.4
153
DRILL HOLE *:
LOCATION
085.5 151.5
XR SI ROCKET T
CASGU
RF-niNS TYP-HATS
PELT U OZ FX BI AXB1 ROCK IS SiniLAR TO FQ.T ABOVE ORE ZONE ON
X FXPP S OZ FX BI FP10
x nx. it ;.-
IDENTITY OF THISavLUpaTuFLVLUFQ.TO
"^.. ^ ". •-,: . - - '
COFF CF ttfPSR RN SPOCTlT2T3XLflP FC
AP23103 BNFOSC 7 UILLIAT1S WC ALSO TO INTERSECTION fi 61.76 TO 71.
8A2 5 105
QZAXFXFP5 LAP! GA 2 4 ROCK IS DIFFICULT TO DETERMINE -IN OZFXnSFPl LAP1QE1 8A25
OZFXBI
QZFXnSFP3 OE3
OZFXBI
SCHS 0 OZ tG OE? nODERATaY nAGNETIC PATCHES.
X PELTS OZFXBI
4A2
8A2
5A2
8A2
3A2
2
4
3
3
3
,-
206 FOBN OTHER INTERSECTIONS THROGH IT -IT 56 FO
2
6 5
10 3
5 3
103
FQ.T U OZ FX BI 4ft 2 3 10 3 LOCAL a PATCHES -POSSIBLY SOTC PRYSmTIC tllNERAL (AX?). LOCAL
X H POSSIBLY IN THE HINGE OF A FOLD. COARSE-GRAINED KY CRYSTALS UP
191"SURVEYED BY:
AZinUTH DIP
180 184.5 180.5
t -45 * -44
-40
TOTAL DEPTH: K '
tCTHOO REMARKS
COLLAR T - T
5 "*
BNFOSC
FO
BNFOSC
SC
BNFOSC
FOSC nAGNETIC INTERVALS.
BNFOSC TO 3— LONG.
7HAS4
9
4
6
12
11
6
C S10IP S2D1P MSBITOKYGASTEPOZOECBBAaCDKFHHrePO ASPYSBRSrOAU
4
8N5 FTJ5 L10 LTr L.I OTr W 0.1 LTr L.3 . . .79- IN 1-8-5. . - -. -:- -
v. J ;,,. 01 -: L20 L3 ?^Si;V
L3 00 UO U Li' "\, ' '
F02 BK2 LTr ' 13 VARIOUSLY BEEN CALLED ALTERED PELT AND FLUL.
F02 LTr LI
BN2 L3 LTr DTr
TO L.I
BN3 FD3 L3 U DTr - D7 L.I L.I
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60
77
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PROJECT: WHITE RIVER TARGET: CADI ZONE CORE S1ZE:TUBODRILLED BY: ST. LAtBERT SURVEYED BY: R. BfiRAN LOGGED BY: C. BRAD8ROOKDATE STARTED: 9/8/83 DATE COMPLETED: 13/8/83 DATE LOGGED: 24/8/83LINE GRID AZIIVTH: LINE: 26'OOU STATION: 1*00N UNITS OF MEASURE: HTSURVEY GRID AZinUTH:fl.O NORTHING: 10117.038 EASTING: 7411.711 ELEV. 10335.615 TOT DEPTH: 15ft
DRILL HOLE NO: J6.1 PROPERTY: UHITE RIVER
f-HFLAGFROn
0
4
RSTR 4
26.31
29.14
RSTR 29.14
30.62
R 45.22
45.22
R 46.35
49.71
70.89
RSTR 69
73.47
75.27
76
RtlAG 76.17
76.85
R 78.78
RSTR 81.98
R 81.98
87.92
R 87.92
TO
4
29.14
49.71
29.14
30.62
49.71
32.25
46.35
46.35
48
70.89
81.98
96
74.38
76
76.85
76.85
78.13
81.98
87.92
97.92
90
97.92
VR Xrt ROCK ET T RF-tllNS TYP-tlATS
CASGU
flFVLU AXFX
COFFCFXCrPSRRNSP
AG 2 3 20 4
LOCALLY BANDS ARE VERY CRENULATED BY FOLDS UITH AXES BETWEEN 35 AND 80FXPPS OZFXBIFP5 6A2555
80 FXPP S 02 FX BI FP5
IRFH 0 AX 02 BI 061 BN 3-4M THICK. UELL DEV BM. V IEAN IRFtl
X FXPP S 02 FX BI FP20
6A2 5 5 5
OCTlT2T3XLttPFCC S1DIP' S20IP HSBITOKYGASTEPOZOECBBACLCDKFmnGPO AS PY SB RG MO AU
BNFO BK30 f030 L3 OTr
PP 0.1
PP 0.1
AG23204 BNFO 6BN18 lF018 U.I V3 VI D.I 01 PROBABLY RELATED TO IRFH FROH 25.64 TO 48.13 IN 16.2. B*N TO PNKI-BRN tllN UITH RHOTBIC OUTLINE -ANDALUSITE OR 6A?
5A 2 5 20 5 PP cTr
60 SCHS S .5 HS AX 86 2 5 10 5 AX IS LIGHT GREEN AND TRONSLUSCENT (TRETOLITE?). ROCK FEELS GREASY
40 aiN S .5 02 FX BI 5A 2 3 10 3
IRFtl IS HORE tWSSIVE AND CONTAINS APPROX PELT U 1 OZ FX BI AX5
CADI U DI CB GA AX10
VERY FRACTURED -POSSIBLE FAULT ZONE? X SOS S tSAX
X H OZ29 Tr DISS Sp.
X LATP S BI CB
STRONGLY HAGNETIC Iftf. X HFVLS FX AX
2.5k DISSEHINATED PO. 6A2 2 2
063 5 207
GA 2 3 10 3
NH
GA
X 000 LOCALLY COARSE GRAINED HO. AnOUNT OF CB AND GA IS LESS.
tFVLU AXnSCL 46 2 3 20 3 GR IS LW 4 .3* BN AND FO LOCALLY AS ttJCH AS 90Deg FROM C/N BECAUSE
EP ALTERATION IN BANDS AND VEINS.mn u FX BI a AX? 26 2 2 2
-' /.' '"- "' ." ' "' "
se(TALC?). LOCALLY VERY FRACTURED.
re
BNFO BN20 F020 C.I cTr WTr 2.1
BN 12 BK20 < .l C .I DTr
SC DTr c.3 Y
DI D.I
c.3
BNFO BN15 F015 V3 LI OF FOLDING. FOLD AXIS AT 50D*g TO C/N.
OS 15 D3 D.I* -fl/T *f*
. L/v rv7 *,*OJNIftCI.BETUEEN IPVL flft) (FIX IS HftRD TO, DISCERN BECAUSE OF SILICIFICATION AND CHLORITIZATION." ' ^'ife^fe^^^1^^.^^.--^ s.&g&tf^fx--
91.27 SCHS U GR QZ C8SCHS IS tCRY FRACTURED AND CRUHBLED.
R 91.2? 150 PELT O OZ FX BI fiXBJ 5A 2 3 3 JSP IS Tr V. HO AH) SP IN OZW 1 * UHICH ARE UP TO 10c* THICK
R 94.44 96 X GOUG S O. CB 36222CB IN VEINS AND PATCHES.
116.06 166.42 XFXPPS QZFXO.FP20 7A25206
10 BfCO FD20
RfWG 128.29 129.27HAGNETIC LAff.
128.29 129.27 X Lttf S BI CB
TOTAL DEPTH: R. BARAN
COLLARAZH ESTInATEO AZnESTinATEO AZH ESTIMATED
O o/t* 3[jr TxTT^" Z^/'^/^c^vt/J) D^'L*. 4.0C#TSO*s
x ' r\ iCA ': WHITE RIVER TARGET: flOBE LAKE ICORE SIZE:BQ
DRILLED BY: ST. LAtBERT SURVEYED BY: R. BARAN LOGGED BY: C. BRADBRQOK DATE STARTED: 15/8/83 DATE COTLETED: 18/8^3 DATE LOGGED: 26/8/83 LINE GRID AZinUTH: LINE: 5*OW STATION: O.OON UNITS OF MEASURE: UT rf
Q SURVEY GRID AZIMUTH:
DRILL HOLE NO:
FLAGFROn TO
9 3.08
1D R 3.08 33.78
4.23 12.2
22.71 30.11
^ RHAG 29.08 31.28
^ 33.78 37.86
RSTR 37.86 55.33
* 43.3 55.33
RSTR 48.42 51.43 ™
R 55.33 124.95
^ 55.33 83.3
^ 55.33 59.43
83.3 92.02
* 124.95 141
^ END 141 141
e^ DRILL HOLE *:
0.0 NORTHING: 9983.456 EASTING: 9496
J7.1 PROPERTY: WHITE RIVER
*R SI ROCK ET T RF-HINS TYP-MATS CO FF
CAS6U
tFVLU flxarx 322EP ALTERATION IK DISTINCT BANDS.
30 FXPP S .5 . : FX BI FP28 3A 2
10 PELT S .5 QZ AX 7A 2
90 SOS S 1 a AX BI AC 2 LOCALLY MAGNETIC.
trVLU CLAX 5G2
873 ELEV. 10345.414 TOT DEPTH: k 141 9
^••'^*i l *CFttHPSRRNSPaTl 12 13 M. M P FC C S1DIP S2DIP nSBITOKYGASTEPOZOECBBACLCDKFHnnGPO ASPYSBRGnOAU
f-jjjjj^ 'K - * 3 20 3 fD f: V'^pt? F010 OTr O V3 V3 . BTr DTr W
5 20 5 pp - - *^ DTr ^
2 2 BNFOBR BW5 f015 L5 L5
2 2 SC -. SC15 D.3 O
3 20 3 SC PY S 5 12 2-5 0
SCHSU a AX 662 2 2 SC 30 SC02 VI 23 D.3 DI LOCALLY CREULATED -FAIRLY STRONGLY MAGNETIC. A
X B 6.1
X SCHS S a AX TA? 7A 2 3 30 3 SC 7.3 D3 0.3 ^ SC NOT STRONG ENOUGH TO rftSURE IT's ORIENTATION. ROCK FEELS SOAPY (TALC?) AX IS LIGHT GREEN IN COLOUR.
INVLUQZFXAXFP5LAP3 GA243063350BNFO BN13 F013 c3V5cl D.I HE-STAINING ASSOCWTED UITH EPIDOTIZATION (*C BRECCIATION. A
30 PELT S QZ FX AX GA 2 3 10 3 BN FO BN13 TO13
X H
X PELTS QZFXBI AP 2 Tr GRflPHITE IN c.
PELT U QZ FX BI AX5 GA 2
t
J7.1 TOTAL DEPTH: SURVEYED BY:
u m3 10 4 BN FO 7 BH10 FD10 D.I DTr
3 10 3 BN FO 3 BW5 1=015 V3 ci DTr 9
1 9
- -'., . -* LOCATION AZinUTH DIP METHOD REMARKS . .
^ .8 180 Ti 58 180fg;i9r;,;/,; - m-'*X-,'- ut ' ; '; -V "" moj|k-,vV."* 'V w*
-45 COLLAS -42 A AZnESTimTED -45 ft AZH ESTIMATED
' -43 ,A AZH ESTIMATED
SKSSfe Sfe^v-^^ ;' ; ' ' ; -
., "•"•.
^r^iS^-:^ . - '. :- - - - : .:-- ^ 'i,^,t- - - ^-^-^ -1-- '^ ^-^
* /-Ar .-n ' \ \PROJECT: WITE RIVER TARGET: S. MOUSE LAKCORE SIZE:BO f /~\ , \^X DRILLED BY: ST. LAMBERT SURVEYED BY: R. BARAN LOGGED BY: C. BRADBROOK ( X 0 V DATE STARTED: 21/8/83 DATE COMPLETED: 23/8/83 DATE LOGGED: 29/8/83 ^-^ LINE GRID AZIMUTH: LINE: 10*OOU STATION: 2*50S UNITS OF MEASURE: HT SURVEY GRID AZIMUTH: 9.0 NORTHING: 9768.074 EASTING: 9018.128 ELEV. 10349.251 TOT DEPTH: 150.38
DRILL HOLE NO: J7.3 PROPERTY: UHITE RIVER . ;
FLAG FROrt TO *R W ROCK ET T RF-HINS TYP-HATS
0 3.42 CASS U
3.42 41.55 INVLU AX OZ FX FPIO LP3
RSTR9 15HIGHLY FRACTURED CORE.
41.55 71 PELT U OZ FX BI AX1
R 43.85 45.37 X n - :MGR (0 -.HSP (0 -.W6L (O.
41.55 56.07 50 FLVL S OZ FX BI FPIO OE5
R 41.55 110.84AX IN DISTINCT BANDS. ADJACENT TO QV's IS
56.07 57.59 X ININ S OZ FX AX
57.59 71 50 FLVL S OZ FX BI FPIO OE5
71 110.4 PELT U OZ FX BI AX3
R 71 110LOCAL a-RlCH BANDS UP TO 10c* THICK.
94.72 95.81 X FLIN S OZ FX BI FPIO OE1
R 102.96 103.17 X FXPP S OZ FX FP3POSSIBLY SILICIFIED.
105.89 106.83 50 FXPP S 5 OZ FX FP20 OE5
RSTR 108.27 110.84 X HHIGHLY FRACTURED CORE.
R 110.84 112.26 BRECU GR OZ CB .GR FORMS THE BRECCIA MATRIX AtO CB FORMS <
RSTR 112.26 122.4 FQ.T U OZ FX AXPROBABLY INTERMIXED PaT AND HFVL. LOCAL
R 122.4 158.38 MFUL U AXFX.
COFFCFJICHPSRRNSPOCT1T2T3XLHPFCC S1D1P S2DIP HSBITOKYGASTEPQZOECBBACLCOKFHM
562 4 2 6' - - S- . f- "
"- . *- . .'-. .PA 2 324' : . f
-' .
PA2 4 3 5
PINK VITREOUS MINERALGA2 4 2 5
PA2 4 3 5
6A2 2 2
4G2 4 1 5
GA
8A2 5 3 5
RN2 6 2 7 4 3
GA 2 3 1 4
BNFO-i- -"-.* v- ' -'.'BNFO
t
FO
CH4-5). RHOMBIC
FO
BNFO
PP
PP
PP
BR
5 OBR
BNFOW STAINING. EP (0 IN DISTINCT BANDS.AG2 3 3 4
LOCAL SILICEOUS BANDS. POSSIBLY AN ALTERATION FEATURE. PATCHESEND 150.38 150.38
BNFO
V 7 8N15 FD15 i. 3 V3 O
6 BN15 F015 ^1V3 '
F015
OR DIAMOND-SHAPED IN X-SECT10H AND A PRISMATIC LONG SECTION (ANDALUSITE?).
FD15
4 BN10 FD10 V3 D.I <.l
30 0 Tl
25 Tl
12 BK20 F020 U V3 OLOCAL HIGHLY FRACTURED CORE.
7 BN20 FTJ20 15 W . <Tr
3-1®
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D.I
D.It
D.I
D.I
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XUVPQM3 LCTMQM2 TXTXSRSOSMUZ T D AZM DIP OZ GA CC C8 BA ho AsWRG*ho'
IDEN6B0202MAINPRJ~8'DK001 BQ830727CJB 0728STLAMBTB3 072 10725 RBGRD 0.
SGOO/SOLsLR'
KS7RRS7RRS7RR 57 RRSTRs
0
0
2216
21621621621621b
1441
SS
S
19322797
322
322RSTR 322R 322R 322R 322/ 4568
RMAG 4568SCGl 50RAZM 50RAZM 50s 6 172
RTOP 8831.KDBT 8935/ 8935
R 8935 S002 975 KD8B 1059 S - 1 059
LAC MINERALS LTD. ' 50 MT 121.76180. -45. M7.2MT.1 . - 216 OVER
-T O 1-J O 1WHITE RIVER
D)216CORE FROM GRANITE BOULDER.1441 PELTQZFXAC3BNF02435 6 P BN 5
GAAX FO 51441BANDING ONLY POORLY DEVELOPED AND IS MANIFESTED BY GREY QZ-RICH 1441BANDS UP TO 3CM INTERBANDED UITK QZ-AC BANDS UP TO 10CM. THE 1441LAT7ER MAY UELL BE AN ALTERATION PRODUCT. BANDS ARE LOCALLY 14410FFSET 2-3MM BY SMALL SCALE FAULTS, AND CORE IS HIGHLY FRACTURED l44lLOCALLY -IS THERE A FAULT NEAR BY? 2797 PELTQZFX BNFO22 2 8 P BN 5L*
AP3I1932 2295
D-
D- L*
L1CDD- D7
2295LOCALLY QE IN MORE MS-RICH BANDS. 3220 PELTQZFXQE)BNF02313 7 P BN
89357AMUAX*
PELTQZFXAX* BNFO2313 APBI SC
FO 5V* L* P BN 4L-L-L- D(CD< CFO - 4 DC D?
89353ANDING IS NOT ALUAYS UELL DEVELOPED AND IS MANIFEST BY 3935INTER3ANDING OF BI, MS OR KY-RICH BANDS.8935SOME LAYERS UP TO 3MM THICK ARE ALMOST PURELY LIGHT BLUE KY, PY 6935PARTICULARLY COMMON IN NS-RICH BANDS, UHICH ALSO CONTAIN A FEU 8935QE. AX IN DISTINCT BANDS UP TO 20 CM THICK.48 XSCHS3ICL SC 22 2 R ' DC MG
5GFX <) D* 48 MAGNETIC SCHS, UHICH ALSO HAS COARSE C1CMLONG) PY CUBES. 975 . 181. -44. .975 ASSUMED AZIMUTH AND DIP SINCE ACID TEST UITH UNLIKELY 975 INCLINATION OF 47DEG.6403 22 2
PA6403 8935
6403640376438748
50000 5 DI 50000L1 5V*
LI 00D BN FO
D BN 50000L1 D-CLD-D?FO 5V* Q?
8935POSSIBLE CL IS LIGHT GREEN MICACEOUS MINERAL, AND MAY BE 8935INTERMIXED UITH MS. MAY BE PSEUDOMORPHING AX. 7647PROBABLY SB XTAL IN QZVN UHICH ALSO CONTAINS 1-2* ILMENITE.8896 R6 D-8FLVLQZFXFP- 25-S
SftBI8834POSSIBLE SCOUR OR LOAD STRUCTURE UHICH INDICATES TOPS UP-MOLE. 8935
1059 44 4DIxDFXPX3G
1059 UPPER AND LOUER CONTACTS CHILLED OVER 12176 . 181.5 -43. 1059 11627
10-15CM SAUSSURITIZED FX.
L* DC
10812 10969
1081211627
S003 12176RAZM. 12176"RAZM 12176
PELTQZFXAC-BNF022 25 PBN 5V* I APBI SC FO 5 LI
XININQZFXFP+FOPP23+4 R FO 5 D. 6ABI
10969IS THIS REALLY AN INTRUSIVE OR IS IT JUST ALTERED PELT?12176 PELTQZFX FOSC23*3 8 P FO 6 L- D.
APBI SC 6 DC12176 . V: 182. -43'. .12176ASSUMED AZIMUTH AND DIP SINCE ACID TEST UITH UNLIKELY12176INCLINATION OF 43DEG.
PROJECT: WITE RIVER TARGET: EEC LAKE I.PCORE SIZE:BOA DRILLED BY: ST. LftTBERT SURVEYED BY: K. BHKHH LUbbtD BT: C. BWDBKOW -""l C/ V * K" W DATE STARTED: 28/7/83 DATE COMPLETED: 1/8/83 DATE LOGGED: 10/8/83 i J —Y ~L~~s W
LINE GRID AZIMUTH: LINE: 7'OOE STATION: 2*50N UNITS OF MEASURE: HT j V If ^ SURVEY GRID AZIMUTH:0.0 NORTHING: 10253.12 EASTING: 10696.238 ELEV. 10323.786 TOT DEPTH: 24f Q K
DRILL HOLE NO: 38.2 PROPERTY: UNITE RIVER \ P
9
9
9
9
9
FLAGFROH
0
R 2.27
2.27
RSAM 13.03
RSTR29.2
TO
2.7
29.2
29.2
13.13
38.28
*R W ROCK ET T RF-MINS TYP-MATS
CASGU
PELTUAC IN BANDS UP
18 FLVLS
REPRESENTATIVEPELTU
OZ FXBI AC5TO 5ca THICK INTERGROUN UITH
OZ FX BI FP5 OE5
CO
(f
FF
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i 9 1
1
K-'-
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SAMPLE TAKEN. ^ K'OZ FX AC AD 8110 AG 2 4 30 5 BNFO 7 BN4 P04 D.I DI W fe
POORLY DEVELOPED BANDING. VERY ALTERED PELT. g
^
*
*
^^
-
*
4*
*
*
^
.9
38.28
45.48
57.53
61.75
75
76.98
RSTR 76.98
183.71
105.2
130.36
RSAtl 123.38
149.73
152.63
159.05
159.05
164.94
Z 165.92
45.48
57.53
61.75
149.73
76.98
193.71
149.73
105.2
149.73
133.32
123.57
152.63
159.05
236.05
160.85
165.92
168.25
avLu
PELTU
PELTU
PELTU
70 FLVLS
X H
ORIENTATION OFx n
x n
OZ
OZ
OZ
OZ
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FXMSOE3 AX3
FXBI
FXMS
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4A
8A
PA
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2
2
2
2
2
435
353
535
2 2
3 10 4
SC VARIES FROM PARALLEL TO BN TO 400eg TO C/H.
n FLVL S .5 OZ
REPRESENTATIVEIRFHU
PELTU
PELTU
20 avt sX INIHS
FXPPS
FXBI FP5
5A
BNFO 6
BNFO 5
BNFO 6
BNFOSC 6
SC
KY GENERALLY FINER-GRAINED
FO
SAMPLE TAKEN.MG
OZ
02
OZ
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OZ-^ RED COLOUR COULD BE
AXOZ
FXBI
FXBI
MS
FXBIFP3
FXCLFP19
AG
GA
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GRDUE TO K-ALTERATIDN RATHER
- -..-^-, . . - ..
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354
4 10 5
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BN3 F03 LI L3 K
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BN3 80 L5 D5 LTr Ql D.I 9
THAH INMOST OF THE UNIT. *BN3 00 L5 010 L20 00
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R 168.25 172.16 58 WIN S .5 QZFXBIFP3 4A24105 FO ^ (\ ^IN1N USUAaY HAS SHARP CONTACT WITH PELT -THE UPPER AND LOUER ONE LOCALLY BEING OBLIQUE TO EACH OTHER.
A 191.41 191.45^ QZUN WITH 2-3* PY AND 2 CRYSTALS OF A GREY nETAUIC HINERAL (H-4). ftT
206.39 236.85 X H . BN FO BWO fOll LI 00 00 DTr LI
R 228.66 228.68QZUN UITH AC ALTERING TO PROBABLE ASBESTOS. I .
R 206.39 236.05 30 INUL S QZ FX BI AX3 AG 2 4 10 4 FO F012 L3 '- 1 D- 3 uHINOR EP IN K.
R 214.5 220BOX 37 HAS JUWLED CORE.
RrtAC 206.39 249WEAKLY TO STRONGLY HAGNETIC INTERVAL.
RSAM 224.87 224.9SAWLE Un-23 TAKEN FOR IDENTIFICATION OF LIGHT GREEN FIBROUS TO BLADED MNERAL (ALTERED AX?).
R 236.85 245.68 IRFH U QZ HG BI HG3 AG 2 2 2 BM FO 18 BN12 F012 03 uLEAN IRFIt. FIBROUS WHITE RINERAL (AX ALTERED TO CHRYSOTILE?) ALONG FRACTURES. LOACAL HE-STAIN1MC.
RSTR 245.68 249 IRFH QZ BI AX HG5 RA 2 2 2 BN FO 6 BN5 f05 VI KTr T5 WSTWl SCALE FAULTING (UHICH OFFSETS QZVNs) TRENDS ALONG CORE LENGTH. AX IS BLACK -PROBABLY HORNBLENDE.
END 249 249
DRILL HOLE *: J8 2 TOTAL DEPTH:SURVEYED BY:
LOCATION AZtnUTH DIP tCTHOD REHARKS
0 188 -45 COLLAR58 180 -45 T108 179 -44 A AZIt ESTItWTeP151.5 178 -48 T208 178 -42 A AZHESTimTS'O249 178 -42 A AZtl ESTimTED
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DRILL HOLE NO: 08.3 PROPERTY: WHITE RIVER -' . j•-' i-.*. .
FLAG FROM TO W HI ROCK ET T RF-HINS TYP-MATS COFFCF*CMPSRRNSPOCflT2T3XLMPFCC S1DIP S2D1P MSBITOKYGASTEPOZOECB
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RMAG 9.17 11.59 X IRFM S OZFXBIMC5AX5 AG23195 --. - ' BN FO BN15 F015STRONGLY MAGNETIC. - :- - - .-y. - - ' ? *- * r-.-jn
11.59 13 X k M v. . -" ...- ^ vx- *;-*. ---"V^l mtRMAG 27 46.39 IRFH 0 QZ BI HG3 AX1 5*2*2 '2
V. FINE GRAINED -MASSIVE SILICEOUS IRFH. AX INTERGROUN UITH OZ IN BANDS 2-3e. THICK. MODERATE TO STRONGLY MAGNETIC.33.13 34.26 X IRFH S QZ BI HE5 AX3 A6 2 2 .2 BN FO BN15 F015 DI
24.41 25 X H L19 99
R 45.39 46.39AMOUNT OF MG DECREASES AND PY CONTENT INCREASES.
RHAG 46.39 53.5 FXPP U OZ FX BI FP28 RA25285 PP 7LOCAL WEAK MAGNETISM.
46.39 53.5 29 PELT S OZ FX BI AX19 SA 2 3 19 3 BN FO BN19 F019
R 53.5 57.69 PELT U OZ FX BI AX19 GA 2 3 19 3 BN FO 8M19 F019AX INTERGROUN UITH OZ IN DISTINCT BANDS WHICH ARE LOCALLY TARNISHED RED BY HE.
RHAG 57.69 127.81 MFVL U AX FX 36 3 3 3 BN FO BN12 F012 V5 MMAGNETIC PATCHES.
R 79.84 127.81 X H BI3 D.IHFVL ALTERED IN BANDS UP TO 5c* THICK -MOSTLY SILICAS UITH UP TO m PO AH) Tr CP; LOCALLY LIGHT GREEN PX (DI?).
R 126.9 126.95VEIN OF GREENISH-BROWN MINERAL LOCALLY UITH GOOD PRISMATIC CRYSTALS (US or EP7).
RHAG 93.96 97 89 FXPP S 1 OZ FX BI FP28 4A25295 PP VIICAKLY MAGNETIC FXPP.
197.45 198.1 X IRFtlS QZAX P019 2 3 19 3 BN FO
RSTR 127.81 149.44 SCHSO BICLAX NG23293 SCFDf^E515F029SC29SC AND FO 5 TO 28feg TO C/N. AX IS LIGHT GREEN (TR?).
R 139.99 133 X GOUG t 910. NG BR V5 K5MOSTLY GOUGED SCHS BUT FROM ? .4 TO 133 !S FXPP. GOUG POST-DATES OZ VEININE PS THIS IS BRECCIATED.
133 149.44 X H 03
RMAG 136.13 149.18 X FXPP S OZ FX BI FP29 5A 2 5 29 5 PPMAGNETIC CRYSTALS MOSTLY UITHIN FP.
R 149.44 146.22 . MFVL U AX FX . 3A 3 3 3 BN FO 9 BN19 F019 L19 EP AlTERATION IN DISTINa BANDS PARALLEL TO BN AN) FO OF MFVL. DISSEMINATED PY IS COMMON IN THE BANDS. t
RHAG 142.72 146.22 X HMODERATELY MAGNETIC.
R 146.22 249 PELT U QZ FX AC BI19 GA 2 3 18 3 BN FO 9 BM29 F029 DTr KTr V.IPROBABLY (MOSTLY) REWORKED MFVL.
R 179.25 176.74 89 LAMP S BI FX CB19 NH 4 4 4CLOTS OF BI HAY BE PSEUDOHORPHS OF AX.
197.31 199.54 X H 03
EM) 249 249
DRILL HOLE *: J8 3 ; TOTAL DEPTH: 249'SURVEYED BY: R. BARAN
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TO RECOV. K ROCK TM TM QMI TX TX FC*M FC 1 2ET ID ATM OlP MS TO KY Bl ST XX PY SB GO YY 53W?S——— l —— r-M —— MH — M 1 1 H 1 1 1 1 1 1 1 1 — l — 1 1 l 1 i 1 1 j l l l ^^XLMPOM3 LCTMOM2 TX TXSRSOSMLZ TIOAZM DIP OZGAOECBBAhq AS MO RG ho
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735 M7 154.38180. -45. . 9887.88 9899.6 10343.8213 FO IS AT 29DEG TO C/NOVER TOP 10M.13 )UGHLY FRACTURED CORE (FRACTURE COUNT UP TO 30).13 MFUL ALSO BANDS OF SILICEOUS ALTERATION UP TO 3CM THICK.3981 MFULAXFX FO 3414 P FO 15 EPLC PO
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SG DC DC5109COARSE EUHEDRAL CUBES OF PY.5109 SCHSCLBI SC 22 230 A DC 00
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100 . 182.5 -43. .100 ASSUMED AZIMUTH SINCE TROPARY READING OF 186.5 CONSIDERED100 ULIKELY.9255 X 000 D
D*1435 . 183. -43. .1435 ASSUMED AZIMUTH AND INCLINATION SINCE ACID TEST UITH UNLIKELY1435 RESULT OF -44DEG.14169 X D CP
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GA3IAX) D* D(9287NUMBER OF F. GRAINED SILICEOUS BANDS GRADUALLY DECREASES.7640POSSIBLE LOAD OR SCOUR STRUCTURE INDICATING TOPS UP-HOLE.87 PHENOCRYSTS NOU BI-POSSIBLY PSEUDOMORHING AX.875 SUWPBIrX y? 2S1S ^
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4aCtaNW0895 4aCiaNW0056 MOLSON LAKE 900
Ministry ofNaturalResources
Report of Work
Ontario
Inttujctlonil/ ' fl/
Supply required del* on t separate form Tor etch lyp* ol W0fk l o b* f*e0f{)*d *'M t*1 * below). For Oeo-technlcel work use form no. 1362 "Report of Work (Geologic*!, Geophysical, Geochemical and
W IV-./f.r L08J7GName and PostaPAdpreti 6T Recorded Holder
LAC MINERLAS '.TD.
P.O. Box 580, MANITOUWADGE, Ontario
The Mining Act txpenoituresr .Prospector's Licence No.
T-664
POT 2COSummary of Work Performance and Distribution of CreditsTolel Work Day* O. cltlmed Mining Oilm
140for Performance of the following work. (Check one only)
Q Manual Work
O Shaft Sinking Drifting or other Latertl Work.
[^Compressed Air, other Power driven or mechinlcil equip.
Q Power Stripping
IT] Diamond or other Core drilling
[j Land Survey
All the work was performed on Minlnq Clilm(s):
Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)
) ; 8 "
TriTft. 1984
St. Lambert's Drilling Co. Ltd. P.O. Box 473 Va'leyfield QUEBEC, Canada J5S 4V7
TYPE OF MACHINE: St. Lambert's Model 250
Certification Verifying Report of Workl hereby certify that l have a personal and Intimate knowledge of the fteti let forth In the Report of Work annexed hereto, having performed the woik or wltnnsed lime during end/or after In completion and the annexed report li true.
Name end Pot tt l Address of Person Certifying
V.R. Venn P. Eng.. P.O. Box 580. MANITOUWADGE, Ontario POT 2CODate Certified
April 18, 1984Certified tSw)V CSIgry(ture)
rvV j ^ ^ . ^Table of Information/Attachments Required by the Mining Recorder
Type of Work
Manual Work
Shaft Sinking, Drifting or other Lateral Work
Compretted air, other power driven or mechanical equip.
Power Stripping
Diamond or other core drilling
Lent* Survey
Specific Information per type
Nil
Type of equipment
Type of equipment end emount expended. Note: Proof of ectual cot t mutt be tubmltted within 30 dayi of recording.
Signed core log thowlng; footage, dlemeter of core, number and angtei of holei.
Nema and addreti of Ontario land turveyer.
Other Information (Common to 2 or more types)
Namet end addreiiei of men who performed manual work /operated equipment, together with dates and hours of employment.
Namet and eddresiet of owner or operetor together with d* let when drilling/stripping done.
Nil
Attachments
Work Sketch: these ere required to f how the location and extent of work In reletlon to the nearest clelm post.
Work Sketch (as above) In duplicate
Nil
768(81/3)
Ministry ofNaturalResources
Report of Work
On! a rio
gf J ?. jj ̂ fi (f- I nnroellom - Supply requited dati on i teparate form for each T / V f C/ f type of work to b* recorded Uee isble below).
The Mining Act
- For Geo-lechnie*l work uie form no. 1362 "Report of Work (Geological, Geophyiical,Geochcmic*t*nd Expenditure!)".
amt andPOtWi Adrtfnt of Recorded Holdtr
LAC MINERALS LTD. Iotntrtor't Lictnct No.
T-664
P.O. Box 580 MANITOUHADGE. Ontario POT 2COLummary of Work Performance and Distribution of CredittTotal Work Diyt Cr. claimed
11, 726. 3 'for Partormanca of tha following work. (Chtck ont only)
[J Manutl Work
QSriaft Sinking Dri'ting or othtr Lataral Work.
QJComprtiitd Air, othtr Powar drlvtn or mac^anical tqulp.
Qpower Stripping
0 Diamond or Othtr Cort drilling
[~]LandSurvtv
Mining ClaimPrtflx
YV.. '.'i, . '"•••''J'
.'••. ^''"'
Numbtr
'lease seeattachedH^j- -- ^1 lav
Work Bay C'.
—— -. ——
—————
Mining ClaimPrtflx
j'' -. .'1 ' -.:- . .
't i
Numbtr
-— ——c-Nuni
K: 1 '
f-
R l
Work Dtyl Cr.
GiOiO•[', ; i j^j"•AHOrl
AY-4f
C E
Mining CulmPttflx
***Um ..*^.
ICAL SUIT FILE OCrlC
.m.VE C'li'. :-V
Numbtr
R7EYo
-
1*-*t**l
————
Work Dayt C'.
—————
All the work was perlormed on Mining Clsim(t): , ., . . ,. , W/t ' rf f-^^f f f*')See attached list M/L^A, LAW
Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)
St. Lamberts Drilling Co. Ltd. P.O. Box 473 Valleyfield QUEBEC, Canada 05S 4V7
TYPE OF MACHINE: St. Lambert's Model 250
R̂ G C G l V E
APR ? 6 1334p, M.
Recorded Holdtr orXgtnt l&rgnaturti
Certification Verifying Report of Workt htrcby ctrilfy that 1 havt a ptrtonal and Intlmatt knowladea of tht facti ttt forth In tht Rtport of Work inntxtd htrtto, having ptrformtd tht work or wltntMtd li m* during and/or afttr In eomplttlon tnd tht tnntxtd rtpoM li trot.
Nt7.iRn:Tnnringr:r^o'.Vin8ox 580 MANITOUWADGE, Ontario POT 2CO
fiWW, 1984Table of Information/Attachment* Required by the Mining Recorder
Typt of Work
Manual Work
Shtft Sinking, Drifting or Othtr Lattral Work
Comprttitd tlr, othtr powor drlvtn or mtchanlcal tqulp.
Powtr Stripping
Diamond or othtr co't drilling
LandSurvay
Sptelflc Informitlon par typt
Nil
Typt of equipment
Typt of tqulpmtnt tnd amount txptndtd. Nott: Proof of actual coil mutt bt tubmltttd within 30 dayt of rtcordlng.
Slgntd cort log thowlng; foottgt, dltmtttr of cort, numbtr tnd tngltt of holt*.
Nama tnd tddrttt of Ontario land turytytr.
/^ ")CtrtH ltd by (Slgp/turt)
Othtr Information (Common to 2 or mort typtt)
Namtt tnd tddrttttt of mtn who ptrformtd manual work/optrattd tqutpmtnt, togtthtr with dttat tnd hour* of tmploymtnt
Namtt tnd tddrttttt of Owntr or optrttor togtthtr with dittt whan drllllng/ttrlpplngdont.
Nil
Atttchmtnti
Work Skttch: thttt t't rtqulrtd to ihow tht location tnd txttnt of work In rtlatlon to tht nta'tit claim pott.
Work Sktteh (al tbovt) In dupllcatl
Nil
181/31 f*. 77. ̂
DIAMOND DRILL HOLES
WHITE RIVER CLAIMS
DDH DEPTH CLAIM N c . WORK TOWNSHIP
1-6-2
1-7-1
1-8-1
1-8-2
1-8-3
1-8-4
1-8-5
1-9-1
J- 6-1
J-7-1
J-7-3
J-8-1
.J-8-2
J-8-3
J- 8- 4
J-8-5 '
K-7-1 ,
K-7-2
K- 8-1
K- 8- 2
L-8-1
.21 Holes
225m
279m
177m
163m
150m
. 159m
162m
153m
150m
141m
150.4m
121.7m
249m '
249m
.154.3m
210m
150m
144m
156m
124.8m
148.5m
3,616.70m x 3.281 ft
~-vl (1 fc. I, 1 I.U \Jll
SSM 625564
SSM 607757 '
SSM 607 i S5
SSM 607755
SSM 607754
SSM 607755
SSM 607753
SSM 607751
SSM 625569
SSM 607759
SSM 607779
SSM 607762
SSM 607762
SSM 607775 '
SSM 607777
SSM 607760
SSM 625582 ^
SSM 607800
SSM 607782 '
SSM 607783
SSM 607806 1
* 1 1,866.39 ft. C V I
BOMBY
BROTHERS
BROTHERS
BROTHERS
BROTHERS
' BROTHERS
BROTHERS
BROTHERS
BOMBY
BROTHERS
BROTHERS
BROTHERS
BROTHERS
BROTHERS
BROTHERS
BROTHERS
RQMBY
•BROTHERS
BROTHERS
BROTHERS
BROTHERScredit drilled
TOTAL CREDITS AVAILABLE: 11,866.3
Education History
Christopher James Bradbrook
Date WBirth - October 2 , 1 958
Period Place onEducatinn
970-1975 Colchester Royal Grammar(equivalent to School. Colchestergrades 7-11 incl.) England
Qualifications Obtained————--—
7 'O' levels (exams taken in Engilsh High schools at age 16.'O' 'O 1 - Ordinary) ***"'
1975-1977 •(equivalent to grades 12 4 13)
1977-1980
Colchester Institute of H'nh Education, Colchester Eric,'and
Southampton University Southampton, England
3'A' levels 'A 1 - AdvancedThese exams are necessary for entryinto Universities in England)
B. Se. 1st class Hons Degree in Geology
1980-1982 University of Western Ontario, London Ontario, Canada
M. Se. in Geology
ASSESSMENT CREDIT - DIAMOND DRILLING
BOMBY TOWNSHIP
SSM 625560SSM 625561SSM 625562SSM 625563SSM 625564SSM 625565SSM 625566SSM 625567SSM 625568SSM 625569SSM 625570SSM 625571
20202020.20^20/40'40/20'2CK2020
SSM 625573SSM 625574SSM 625575SSM 625576SSM 625577SSM 625579SSM 625580SSM 625581
x SSM 625583
SSM 386674SSM 386675SSM 386676SSM 386677SSM 386678
^ SSM 386681
40 -^20202020-20'20.20.6.3'
20-20202020^20^
TOTAL CLAIMS - 27BOMBYTOTAL CREDITS - 586. 3
i J
ASSESSMENT CREDIT - DIAMOND DRILLING
BROTHERS TOWNSHIP
SSM 607720SSH 607721SSM 607722SSM 607723SSM 607724SSM 607725SSM 6U7726SSM 607727SSM 607728SSM 607729 SSM '607730SSM 607731SSM 607732SSM 607733SSM 607734SSM 607735SSM 607736SSM 607 7 37SSM 607738SSM 607739SSM 607740SSM 607741SSM 607742SSM 607743SSM 607744SSM 607745SSM 607746SSM 607747SSM 607748SSM 607749
\ SSM 607750
Per this pageTOTAL CLAIMS -BROTHERS -TOTAL CREDlfS
202020.202020-20 N202020 s 20202020 ,
20 ^202020202020202020202020202020'^
-
*jas-
- 2,760
SSM 607751/SSM 607752 -'SSM 607753*/SSM 607754''SSM 607755'SSM 607756/SSM 607757'SSM 607765.-SSM 607768-SSM 607769 SSM 607 785-:SSM 607786*SSM 607790"SSM 607791-SSM 607802^SSM 607804'SSM 607812-SSM '607813-SSM 607816 -.SSM 607817-SSM "607867SSM 607868SSM 607869 'SSM 607870.SSM 607871SSM 607872SSM 607873SSM 607874SSM 607875SSM 607876SSM 607877SSM 607878SSM 607879SSM 607880SSM 607881-SSM 607764.x
* * *
y
2020.2020.!2020 .2020
-2020 2020202020.20' '20 -20202020202020202020202020202020202020 -
SSM 607900SSM 607901SSM. 607 902SSM 607903SSM 607904SSM 607905SSM 607906SSM 607907SSM 607908SSM 607909 SSM 607910SSM 607911'SSM 607912S'SM 607913SSM 607914SSM 607915SSM 607916SSM 607917SSM 607918SSM 607919 .SSM 607920SSM 607921SSM 607922SSM 607923SSM 607924SSM 607925SSM 607926SSM 607927SSM 607928SSM 607929SSM 607930SSM 607931SSM 607932SSM 607933
NSSM 607934
20202020.20.2020202020 20202020202020202020202020202020202020202020202020
SSM 607935 SSM 607936 SSM 607937 SSM 607938 SSM 607939 SSM 607940 SSM 607941 SSM 607942 SSM 607943 SSM 607944 SSM 607945 SSM 607946 SSM 607947 SSM 607948 SSM 607949 SSM 607950 SSM 607951 SSM 607952 SSM 607953 SSM 607954 SSM 607955 SSM 607956 SSM 607957 SSM 607958 SSM 607959 SSM 607960 SSM 607961 SSM 607962 SSM 607963 SSM 607964 SSM 607955 SSM 607966 SSM 607967 SSM 607968 SSM 607969
607970
2020202020202020202020202020202020202020202020202020202020202020202020
l BROTHERS TOWNSHIP (Continued ...)
Sm 607 971 SW 607 972SSH 607973,SSH 616424SSH 616425SSH 616426SSH 616427SSH 616428
^SSH 61 6429 1 -SSH 620464'.SSH 620465SSH 620466SSH 620467 , SSH 620468/
SSH 620470- SSH 620471
SSH 620472' SSH 620473
SSH 620474SSH 620475SSH 620476SSH 620477SSH 620478SSH 620479
. SSH 620480 .SSH 620481SSH 620482SSH 620484SSH 620485SSH 620486SSH 620487SSH 620488.SSM 620489SSH 620490SSH 620491SSH 620492
VSSM 620493^SSM 6255d5SSH 625586SSH 625587SSH 625588SSH 625589SSM 625590SSM 625591 SSM 625592SSH 625593SSH 625594SSK 625595SSM 625596SSM 625597
VSSH 625598
20 x 20202020 -2020202020.20.2020 2020"
2020202020202020202020202020 -20-20
. 2020202020202020202020202020 20202020202020 '
^SSM 625S99*7 SSM 625600SSM 625601SSM 625602SSM 625603SSM 625604SSM 625605 -SSM 625606SSM 625607SSM 625608SSM 625609SSM 625610 .SSM 625611 SSM 625612SSM 625613SSM 625614SSM 625615SSM 625616SSM 625617 -SSM 625618SSM 625619 .SSM 625620SSM 625621SSM 625622SSM 625623 -SSM 625624SSM 625625SSM 625626SSM 625627SSM 625628SSM 625629SSM 625630-'SSM-625631SSM 625632SSM 625633 ,
\SSM 6256341/"SSM 62578BSSM 625789SSM 6257 9DSSM 625791SSM 625792SSM 625793SSM 625794SSM 625795SSM 625795 SSM 625797
V SSM 625798
20- 202020202020202020202020 202020202020••2020202020202020202020202020202020202020202020202020 2020
SSM 625799 SSM 625800SSM 625801SSM 625802SSM 625803SSM 625804SSM 625805SSM 625806SSM 625807SSM 625808SSM 625809SSM 625810SSM 625811 SSM 625812SSM "625813SSM 625814SSM 625815SSM 625816SSM 625817SSM 625818SSM 625819SSM 625820SSM 625821SSM 625822SSM 625823SSM 625824 -SSM 625825 -SSM 625826SSM 625827
20 20202020 .;20.. .;-
. 20 .20 l-.-20 - '-2020 - ,;20 -, -i20. ; \.-:
.20 . :;2020 ,-2020 .20 .
. 20 .20 .20202020 . '20 -202020
SSM 625828 20\SSM 625829'' 20
SSM 625831SSM 625832SSM 625833
X SSM 625834^SSM 692695SSM 642696SSM 642697SSM 642698SSM 642699
^SSM 642700^'
^
As per this TOTAL CLAIMSAs oer this
20202020202020202020
page -139
paqeTOTAL CREDITS - 2,780*
LABERGE TOWNSHIP
C^Pto No.
SSM 607820SSM 607821SSM 607822SSM 607823SSM 607824 ;SSM 607825SSM 607826-SSM 607827SSM 607828SSM 607829SSM 607830SSM 607831SSM 607832 .SSM 607833
" SSM 607834 :SSM 607835 -SSM 607836
- SSM 607837- .SSM 607838 ---SSM 607839SSM 607840SSM 607841 'SSM 607842SSM 607843SSM 607844SSM 607845SSM 607846SSM 607847 -'SSM 607848SSM 607849 -
. SSM -607850--?::,SSM 607851'^SSM 607852SSM 607853SSM 607854SSM 607855SSM 607856SSM 607857SSM 607858SSM 607859SSM 607860SSM 607861SSM 607862
\ SSM 607863X SSM 607864^
Cr.
20.2020 .2020202020202020202020'
20202020
•202020202020.2020 '20202020.20.-.20' 20
2020202020202020202020-20
Claim No.
SSM 607882SSH 607883SSH 607884SSM 607885 'SSM 607886SSM 607887SSM 607888SSM 607889SSM 607890'
,
SSM 607980SSM 607981 .SSM 607982SSM 607983SSM 607984
. SSM 607985SSM 607986SSM 607987 -
-SSM .607 988.'^SSM 607989SSM 607990
' SSM 607991SSM 607992SSM 607993SSM 607994
v SSM 607995'NSSM 607996;
"
' SSH 625501
tCr.
2020 -20 .202020202020-.
20202020 -20.'202020 .20.20"2020202020.2020
20SSM. 625502-^,20SSH 625503-'*;
-SSM 625504^:-SSM 625505' "SSH 625506
, SSM 625507 -' SSM 625508 .SSM 625509SSH 625510SSM 625511SSM 625512SSM 625513SSM 625514SSM 625515SSM 625516 -
\SSM 625517,
"20-20 -20'
20202020202020.2020202020
Claim No.
SSM 625518 SSM 625519
- SSM 625520 SSM 625521-SSM 625522 SSM 625523 SSM 625524 SSM 625525 SSM 625526 SSM 625527 SSM 625528 SSM 625529 SSM 625530 SSM 625531 SSM 625532 SSM 625533 SSM 625534 SSM 625535 -
- SSM 625536 " ' SSM 625537 . SSM 625538 SSM 625539 SSM 625540 SSM 625541 SSM.625542'
- SSM 625543 SSM 625544 "SSM 625545*
- SSM 625546 : -SSM 625547-^-~ SSM 1625548-.-: SSM-625549"
SSM 625550 SSM 625551 SSM 625552 SSM 625553 SSM 625554 SSM 625555 SSM 625556 SSM 625557
v SSM 625558 \SSM 625559-
Cr. Claim No. Cr.20 20 20 20 20 20- 20. 20 20 .
"- 20 \ 20 '
"20: "20 '--20
202020
. 20.20
. 20. 20 20 20-
' 20
. 20 20 20 20
--. 20--'- 20:x 20 -
. 20' 20
202020
- 20 20
- 20 20 20. 20
SSM 625640SSM 625641
: . SSH 625642SSM 625643;SSH 625644 .SSM 625645'
i SSM 625646 : SSH 625647
SSH 625648' :. SSH 625649
SSH 625650-SSH 625651- SSH 625652 SSM 625653 SSH 625654. SSH 625655 SSH 625656
- SSM 625657- SSH 625658 SSH 625659' SSH 625660 SSM 625661 SSH 625662
' SSH 625663 SSH 625664. SSH 625665 SSH 625666 SSH 625667 SSH 625668
- SSH 62566?--•sSH-625670, ' SSH 625671"
SSM 625672 SSH 625673 SSH 625674 SSH 625675 SSH 625676 SSH 625677 SSH 625678 SSM 625679
\SSM 625680
.-- 20. .. v.. 20 vr20:c;' 20 " VV20./ i - 20 '
202020
.2020
. .20 ' 20
20.2020-20202020 -
' - 202020-20
' 2020
. 20202020.-•-20 20 20 20. 20 20 20 20 20
S 20 S 20
As per this page TOTAL CLAIMS - 171 As per this page TOTAL CREDITS - 3.420 J
LABERGE TOWNSHIP (Continued ...)
H 625681SSH 625682SSH 625683SSH 625684SSH 625685.-.SSH 625686 -SSH 625687SSH 625688SSH 625689SSH 62569*0SSH 625691SSH 625692 .SSH 625693SSH. 625694SSH 625695 'SSH 625696 :SSH 625697 'SSH 625698SSH 625699SSH 625700SSH 625701 '-SSH 625702 'SSH 625703SSH 625704SSH 625705SSH 625706SSH 625707SSH 625708SSH 625709SSH 625710 ~SSH 625711SSH 625712 -SSH 625713 ?SSH 625714 XSSH 625715SSH 625716SSH 625717 -SSH 625718SSH 625719SSH 625720^
2020202020".2020202020202020•20202020: 202020
. 20202020202020202020
, 20
-20"20"20
2020202020
SSH 625721SSH 625722
- SSH 625723SSH 625724SSH 625725
' - SSH 625726SSH 625727SSH 625728SSH 625729SSH 625730SSH 625731SSH 625732 ;SSH 625733 VSSH 625734 *SSH 625735 -SSH 625736
•r SSH 625737SSH 625738SSH 625739 .
- SSH 625740 'tSSH 625741-:-'SSH 6?5742SSH 625743SSH 625744SSH 625745SSH 625746SSH 625747 'SSH 625748 .SSH 625749SSH 625750 :SSH 625751..-.
r". SSH. 625752- SSH. 6257531-7
. SSH : 625754 '. SSH 625755
SSH 625756SSH 625757SSH 625758S^H 625759/
20202020
. 2020202020202020202020
. 20• 202020^20-20'20
2020202020202020
-20^20520- 2020•20202020
SSH 625760SSH 625761SSH 625762SSH 625763SSH 625764SSH 625765SSH 625766
. SSH 625767SSH 625768SSH 625769SSH 625770
' . 'SSH 625771. SSH 625772'
SSH 625773. SSH 625774 .
SSH 625775 .SSH 625776'SSH 625777 .SSH 625778
V SSH 625779 ~' ' SSH 625780
SSH 625781SSH 625782SSH 625783SSH 625784SSH 625785SSH 625786SSH 625787^... ..SSH 626737 '
. .N SSH 626738 .
. ^ -*- . .'- . . ••"- '
* * *
.. '
20202020202020202020202020202020"20
2020•202020202020202020
2020/.
'
As per this page TOTAL CLAIHS - 109 As per this page J TOTAL CREDITS - 2,180 y
TOTAL CLAIHS FOR LABERGE - 280 .
TOTAL CREDITS FOR LABERGE - 5.600