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15 DecLAMBOOABN 27 09
ASX: LM
CORPOLevel 6, 3Brisbane
OPERATUnit 2, 7 JoondaluTelephon
CONTAC Richard TChief Exerichard@0412 307 Tony CorHead of Otony@lam0427 349
Ken BankInvestor Rkbanks@0402 079
cember 20O RESOURCE99 098 192
MB
RATE OFFIC344 Queen St QLD 4000
TIONS OFFIPackard Stree
up WA 6027 ne: +61 8 930
CT
Trevillion ecutive Officer
@lambooresour7 087
rmack Operations mbooresource 451
ks Relations
@bigpond.net.a 999
014 ES Limited
CE treet
CE et
01 1047
r rces.com
es.com
au
OUEXCTARAN
Lamfinal McInWes
HIGH
The survRussinteranomgrapwith
Lam"ThedelivMcInthis signi
TSTANDCEEDS RGET 4 D NICKE
boo Resouresults o
ntosh Flakstern Austra
HLIGHTS:
3-Dimeover 3
Deliverhighly be attri
final 3 diey data forsell Mortimrpretation omaly with ephitic schis
high poten
boo Resoe interpretaver exceptntosh is rapalong withifies an exc
DING TAEXPEC IMMINEEL POT
urces (ASXof the 3 dke Graphitalia.
:
ensional ikilometre
ry of theconductivibutable t
imensionar Target 3
mer at Soutof the VTEextremely
st. Target 3ntial for thic
ources Heaation of ttional resupidly taking
h the coppciting futur
ARGET TATION
ENT, WITENTIAL
X:LMB or Ldimensionate Project
interpretaes of folde
e Target ve bodieso a coppe
l interpretahas been thern Geos
EM supermhigh cond3 is interpckening of
ad of Opehe VTEMults for thg shape aser / nickel re for the c
3 VTEMNS. INTETH SIGN
L.
Lamboo) ial interpre in the E
ation of Ted graphit
4 interps defined er / nickel
ation of thcompletedscience Co
max data huctivity bereted as athe graph
rations, Tosuperma
he compas a world cpotential
company".
M RESULERPRETNIFICAN
is pleasedetation of East Kimb
Target 3 tic schist
retation by VTEM l mineralis
he VTEM d by geophonsultants has identifielieved to ba large synitic schist i
ony Cormax survey any and iclass flakeat Target
LTS TATIONNT COP
to announTarget 3
berley Reg
completeidentified
imminentare belie
sation.
supermaxhysical con
(SGC). Thed a largebe a responformal stin the fold
ack, commis continuts shareh graphite p4 - Melon
N OF PPER
nce the at the
gion of
e with d.
t. The ved to
x aerial nsultant he final e target onse to ructure hinge.
mented uing to holders. project, Patch,
Lamcomgrafoldmodthe
TheFiguanoelecmap
mboo Resompleted by phitic schi
ded, large delled at Tthickening
Figure 1: F
e Septembure 1) coomalies. Fictromagnepping, petr
ources is p Russell Mst is interpregional
Target 3 ang of the gra
Final processe
ber 2014 Vvered a tive of thes
etic (EM) terographic a
pleased toMortimer, hpreted to bantiforms
nother signaphitic schi
ed VTEM sup
VTEM supetotal of 64se were prechniques analysis, ro
o announceas identifiebe in exce
(convex nificant deist unit alon
permax image
East Kimber
ermax surv42 line kilreviously idand confi
ock chip sa
e the final ed a large ess of threup), with
evelopmentng the fold
ery (channel
rley, Western
rvey over tlometres adentified brmed to bampling an
3 dimenssynformal
ee kilometrthe synfo
t for the cod hinge.
49BZL) of the
Australia.
the McIntoand identifby inducede flake gra
nd explorat
ional interstructure o
res. Targetormal strucompany du
e McIntosh F
osh Flake Gfied a tota
d polarisatiaphite schtion drilling
rpretation ooverall strits 5 and 6cture (conue to the l
lake Graphite
Graphite Pal of 12 ion (IP) an
hist by geog.
of Target 3ke length o6 are tightnvex downikelihood o
e Project
Project (sehigh-prioritnd historicaological fiel
3, of ly n) of
ee ty al ld
Tar
Theas highclosbou
rget 3
F
e strongestdefined b
hlights the ser spacinunding mod
Figure 2: Targ
t zone of inby the hig
presence ng in the delled cond
get 3 anomaly
nterest at gh amplitu
of a broadnorth-eastductive un
y (channel 49
the Targetude late cd conductivt sector. Pits are app
9BZL) with dr
t 3 prospecchannel Vve sequenPresence parent.
rill hole collar
ct area is tVTEM imagnce bounde
of additio
rs and VTEM
the centralgery. VTEed by sub-nal condu
flight lines.
l to north-eEM model-vertical couctors with
east sectioling overa
onductors ahin the tw
on all at
wo
ThekiloTar
Plaalonthicplat
e area of metre hav
rget 3 is in
nned drillinng the VTEck plate mtes and <3
Figure 3:
strong coving strong
excess of
ng at the EM flight liodels are
300S denot
Plan view of
onductancepotential tthree kilom
end of theine L1365 present. H
ted by the
the Target 3
e alone reto host flakmetres.
e wet seas(see Figur
High condred model
anomaly (ch
epresents ke graphite
son will focre 3) and tuctance o plates.
annel 49BZL
a strike lee schist. Th
cus in thethe surrouf >300S is
) with model
ength potehe total str
area withnding souts denoted
plates.
ential in erike length
h the stronth west seby the pu
excess of potential a
ngest centrction wherurple mode
a at
re re el
Thedeebe 400
Thisbeindrivthat
Figure 4
e synformaeper towardapproxima
0m below t
s large regng associaver of hight will be the
: South-west
al fold hingds the souately 150mhe surface
gional scalated with aer grade /e focus of
t looking obli
ge at Targeuth west of m below the in the sou
e folding aa large sca/ larger flaall future e
que view of t
et 3 has a the Targee surface
uth west of
at Target 3ale thrustinke graphite
exploration
the Target 3 a
south weset 3 area. T
in the norf the prosp
3 has also g event. Te mineralis activities.
anomaly (cha
sterly plungThe depth rth east, p
pect (see F
undergonThese strucsation, it is
annel 49BZL)
ge, meaninof the fold
plunging doigure 5).
e significactures are s these str
with model p
ng the fold hinge is eown to ap
ant faultingseen as aructural en
plates.
d hinge getestimated tpproximate
, potentialan importannvironment
ts to ly
ly nt ts
Fig
Fig
gure 5: North-
gure 6: South
-east view of
h-west view o
Target 3 mod
of Targets 1 a
del plates, gr
nd 3 model p
raphical drill
plates and gra
holes interce
aphical drill h
epts and folde
holes intercep
ed synform in
pts for Targe
nterpretation
ets 1, 2 and 3.
.
.
Tar
TheconGeobiotgab
rget 4 - Me
e VTEM sunductive boological Sutite bearingbbroic McIn
elon Patch
Fig
upermax imodies belieurvey of Wg olivine gntosh Sill in
h
ure 7: Target
magery of teved to b
Western Agabbronoritntrusion.
4 anomaly (c
the Target e associaustralia's 1te associa
channel 49BZ
4 - Melon ated with t1:100,000 ted with th
ZL) with VTEM
Patch prothe presenmapping
he Sally D
M flight lines
ospect has nce of cop(see Figur
Downs supe
.
identified pper and re 8) has ersuite of
large highnickel. Threcorded the layere
ly he a
ed
Figure 8: Target 4 ge
Figure
ology (GSWA
e 9: 2005 Thu
A 1:100,000) w
ndelarra stre
with 2005 Thu
eam / soil / ro
undelarra str
ck chip locat
eam / soil / ro
tions at Targe
ock chip loca
et 4.
ations.
TheThuprosamcorrvaluNic
e Target 4undelarra igram of th
mpling prorelates extues of >50kel values
4 - Melon Pn a 2005
he Melon Pgram identremely w00ppm weranging be
Figure 1
Patch areaopen file aPatch areantified a bell with th
ere recordeetween 80
10: 2005 Thun
a has beeannual repa are provroad zonee highly ced in soil to 250ppm
ndelarra stre
en the focuport. Graphvided in Fie of anomconductiveand 250 t
m were rec
am / soil / roc
us of previhical resultgures 9 aalous cop bodies idto 500ppmcorded in s
ck chip resul
ous explos of a strend 10 beloper and n
dentified bym in rock csoil sample
ts for copper
oration as eam / soilsow. The gnickel, thisy the VTEchip (see
es (see Fig
r at Target 4.
reported bs / rock chigeochemicas zone alsEM. CoppeFigure 10ure 11).
by ip al
so er
0).
Tarthe on dimweenea
rget 4, or MMcIntosh the deve
mensional Vek, Lamboar future.
Figure
Melon PatcProject an
elopment VTEM inteo looks for
11: 2005 Thu
ch as refernd whilst of the Mrpretation rward to pr
undelarra stre
rred to in tit is a we
McIntosh Fof the Tar
roviding fur
eam / soil / ro
the GSWAelcome adFlake Grarget 4 - Merther upda
ock chip resu
A mapping,ddition, the
phite Proelon Patchtes for Tar
lts for nickel
is a signife companoject into h prospect rget's 4, 10
at Target 4.
ficant deveny is firmly
productiot is due in 0, 11, 7, 8 a
elopment ay focusseon. Final the cominand 9 in th
at ed
3 ng he
Tony C
Head o
Compet
InformatiinformatiMining aexperienin the 20this repo
Cormack
of Operatio
ent Persons
ion in this repion previouslyand Metallurgnce which is r012 edition of ort of the matt
ons
s Statement
port relating ty compiled angy and a fullrelevant to thef the Australaters reviewed
to explorationnd / or reviewl-time employe activity prevsian Code of
d by him in the
n results and wed by Mr. Toyee of Lambviously underf Reporting ofe form and co
d geological dony Cormackboo Resourcertaken to qualf Exploration ontext in whic
data at the Mck, Member of es Limited. Mlify as a "ComResults and
ch they appea
cIntosh Projethe Australas
Mr. Cormackmpetent Persoconsents to t
ar.
ect is based osian Institute k has sufficieon", as definethe inclusion
on of
ent ed in
App
Sa
Q
V
pendix 1 –
Sectio
Crite
Sampling te
Drilling tec
Drill sample
Logg
Sub‐samplingand sample p
Quality of asslaborato
Verification oand ass
Location of d
Data spacdistrib
Orientationrelation to
struct
Sample s
Audits or
– JORC 20
on 1 eria
echniques
chniques
e recovery
ging
g techniquespreparation
say data andory tests
of sampling saying
data points
cing and ution n of data in geological ture
security
reviews
012 Criteri
Reverse samples splitter dRC using RC split sto the drAll RC chi
1m sampLaboratorpulverisedTotal Sulp
The RC sablank andduplicateprocess aVerificatiadjustmeDrill holedifferentiGarmin 7accuracy.RC drill htraversesRC drill hhorizons.with α anSamples self sealithen tranpulps desample seSamplingmanagem
ia
Circulation which repreuring the dria 5.5 inch hasamples havill rig. The saips were geoples from tries in Perthd and analyphur (TS) usinamples that d certified s and standand the dataon was basents to assaye collars wal GPS. Preli76c Global P The map prholes at the s 80 to 250 moles were dr. Diamond dnd β angles mwere collectng plastic bansported by respatched toecurity is cong techniquesment service
(RC) drillingesent 1m splilling processammer. Holeve been recoample recoveologically logthe RC drill. The samplesed for Totang a Leco Fu were submtandard at aard samples and was foused on use y data has bewere surveyeiminary RC cPositioning rojection useTarget 1 Ex
m apart. rilled at neardrill core hasmeasured anted from thags prior to road to Actlao Actlabs Lansidered to bs and data s in Perth, W
Commenta
g was empits. The sams. es ranged upovered from ery and physged in the fiing were ses were riffleal Graphitic rnace, and t
mitted to theapproximatewere statist
und to be satof duplicat
een made. ed by Whecollars were System (“Ged is the Ausxtension and
r perpendicus been oriennd positionede cone splitbeing put iabs in Perth.aboratories be adequatehave been
WA – Rock So
ary
loyed to geples are take
to a maximua cyclone anical state weeld by qualifubmitted toe split on a 5Carbon (TGChe other spl laboratory ely every 20t
tically analysisfactory. tes, standar
lans Surveylocated by hPS”) units wstralian Geod Targets 2, 3
ular to the stnted using ad using a Kenter in caliconto bulka ba The samplein Canada
e. n handled bolid Data Pty
enerate 2 ten directly f
um depth ofnd cone spliere recordedfied geologiso either Ac50:50 basis, C), Total Carit held as in include a duth sample sused as part
rds and blan
yors, Kununhand‐held Gawith a typicdetic MGA 943, 5 and 6 a
rike of the ga Reflex ACEnometer. o bags and tags. The bules were procor ALS in B
by an indepLtd.
o 3 kilografrom the con
f 198m. itter mounted. ts. ctlabs or ALwith one sprbon (TC) anstorage. uplicate, sanubmitted. Thof the QAQ
nks used. N
urra using armin 62S ancal ±5 metre4 Zone 52. are spaced o
raphitic schiE tool (Act I
hen placed lka bags weressed and thBrisbane. Th
pendent dat
m ne
ed
LS lit nd
nd he QC
No
a nd es
on
st I),
in re he he
ta
Section 2
Cri
Mineral teland ten
Exploratiother
Geo
Drill hole
Data agmet
Relationshmineralisaand interc
Diag
Balanced
Other suexplora
Furth
2 iteria
enement andnure status
on done by r parties
ology
Information
ggregation thods
hip betweenation widths cept lengths
grams
d reporting
ubstantive ation data
er work
d
Lamboothe Mctotal arethere arsubject The Easno activduring Ruglessof the exploraThundeLamboooccur inthe Eastas the Twesterngranulitpressurelargely sillimanLambooanomalwith poapplicatinclude 5 have and 6. A total o5 and 6 All dataSolid Pt
There iGraphitin bothclearly Refer toAll RC reporteAll explholes thRC and and 6. A
o Resources Intosh Projeea of 665.3 re no encumto a mill gatest Kimberley ve previous eregional mas mapping anGreat North
ation by Auserlarra Resouo Resources n the high grt Kimberley oTickalara Men side of the metamorpe although tupper amphite and evideo has identiies over a stotential for tions. Thefive (5) idenbeen drilled
of 165 RC an at McIntosha is handled ty Ltd. s a very clotic Carbon TGh the RC chirelated to tho the figuressamples froed on. oration datahat have resudiamond drAdditional dr
Limited holdect area in tkm2. All gra
mbrances, roye net royaltyhas been laexploration fapping in thnd RAB drillinhern Highwastralian Angurces Ltd oveLtd recognirade metamof Western Aetamorphicshe major Haphic facies uthe metamohibolite facience of origified graphittrike length ir another 2e McIntosh ntified target to date wit
nd diamond dh Graphite foby an indep
ose relationsGC% assays. ips and diamhe geologicals in the text oom drilling a
a has been rulted in a JOrilling prograrilling at Targ
Comment
ds eight (8) gthe East Kimnted miningyalties or impy of 1%. rgely explorefor graphite.he Mabel Dong in the vicay in 1993 lo Americaner the last 20sed the pot
morphic terraAustralia. Ths extending alls Creek Funder condiorphic gradeies with thenal cordieritte schist hoin excess of 25 km striktarget areast areas – Tarh additional
drill holes haor a total of 1pendent dat
ship betweeThe presenc
mond drill co logs. of this documat Targets 1
eported on RC 2012 comms are planget 1 is plann
tary
granted ELs mberley, WAtenements
pediments ex
ed for base m. Graphite haowns area finity of Meloand has ben Ltd, Panor0 years. ential for grain of the Hahe host stratifor approximFault. The mtions of higin the McIn
e presence e. rizons and 10 km withike length os contains trgets 1, 2, 3, drilling plan
ve been com17,985.5 metabase mana
n the graphce of graphitore so that
ment 1, 5 and 6
and include mpliant resouned for grapned to increa
and three (3A. The tenemare in goodxcept for E8
metals and dad been notfor the BMRon Patch boreen located ramic Resou
raphite schisalls Creek Migraphy has mately 130 metamorphicgh‐temperatuntosh area aof key min
accompanyiin the granteof graphite typical flake 5 & 6. Targnned for Tar
mpleted at Taetres. ager in Perth
hitic schist utic schist is cthe assay w
have been
165 RC and urce at Targephitic schist Tase the grap
3) ELAs withments cover standing an0/4733 that
diamonds wited by GemuR in 1967, bre, to the eaduring nickurces Ltd an
st horizons tMobile Zone been mappekm along thc rocks reacure and highappears to berals such a
ng aerial EMed tenemenschist in Egraphite an
gets 1,2, 3 angets 1, 3, 4,
argets 1, 2, 3
h, WA ‐ Roc
unit and Totclearly evidenwidths can b
analysed an
diamond dret 1. Targets 1, 2, hite resource
in a
nd is
th tz by st el nd
to in ed he ch h‐be as
M ts EL nd nd 5
3,
ck
tal nt be
nd
rill
5 e.
Section 3
Cri
Databas
Site
Geological I
Dime
Estimation atech
Mo
Cut‐off p
3 Estimaiteria
se integrity
e visits
nterpretatio
ensions
and modellinniques
isture
parameters
ation and R
The datmetadachecks coveredRock SocertifieddatabasThe Comfamiliarincludin
on
The graplanar stratigraboth alobe anyextensioconsisteestimataerial EMThe facthicknesmetamohave affand thuincludedThe grastrike lediamontested bportion
ng
Block mhigh graIMS comwas comBlock mheight. The tonA 2% Tnatural isolatedresourcblocks fbulk mi
Reporting
a as provideta administeand balanced by in – houolid Pty Ltd pd standards se. mpetent Perr with all theng the RC andaphite schistbody that aphy. Thereong strike anunforeseen
ons to the ment with the e. The extenM anomaly tctors affectinss of the grorphic terraifected the gs cannot be d in the resophitic schist ength of 580 d drilling. Thby RC drillingof the resou
modelling usade outliers mputer softwmpleted. All modelling use No sub‐blocnnages were TGC cut‐off wcut‐off exh
d single resoce although from the resning method
g of Minera
ed by the labered by the es in place se checks. rovides a ful and duplic
rson has unde Lamboo pd Diamond dt host at Tais concord
e is very goodnd at depth,n complicatmineralised zgeological insion of thethat defines ng the contraphite unit n. A small nurade due to reasonably
ource and havhost coveredm and exten
he north‐eastg during 2013urce at depthsing an ellipand no uppeware was usdrill assays wed a standarcking was usestimated owas adoptehibited by thource blocksmarginally source was d.
al ResourcComment
boratory is adatabase mto ensure d
ll QA/QC repcates prior
dertaken extpersonnel andrilling contrarget 1 essedant with td correlation and there itions in thezone that fonterpretatioe Target 1 rethe mineraliinuity of grwhich is toumber of feldilution. Sumodelled. Cve resulted id by the currnds to a depttern end of t3 thus limitinh. soidal ID2 seer cut was apsed. A standwere used tord block sizesed. Downhoon a dry basisd based on he mineraliss aggregatingless than tconsidered t
ces tary
dded directlanager, Rocdata reliabilit
port based onto incorpor
ensive work d the outsidactors used entially reprthe host hn between RCs no reason e geologicalrm part of tn used for tesource alsosed zone. ade are limo be expectsic intrusivech intrusionsonsequentlyn a minor dirent JORC reth of about 2the graphiticng the tonna
earch. Statispplied to the ard cross seo interpolate of 10 m (N‐ole sample les as per the aa simple st
sed lenses. Ng 1,088 tonnhe 2% TGC to be unrea
y to the Mcck Solid Pty ty. Field dat
n the statistiration into
k on the projde contractofor the drilliresents a sthigh grade C and diamoto believe tl and assaythis resourcehe original Jo correlates
mited to varited in such es were inters are likely ty the intrusivlution in graesource exten200 m in arec schist has oge in the no
stical analysie assay data. ection flitch ie the block ce‐S), 2 m (E‐Wengths were assay data utatistical anaNote that fones were incut‐off. Exlistic in view
Intosh ProjeLtd who havta is similar
cal analysis othe resourc
ect site and ors employeng. eeply dippinmetamorph
ond drill holethat there wy data. The upgrade arORC resourcwell with th
iability of tha high gradrsected. Thesto be irregulaves have beede. nds over a as tested by only been rthern
is indicate n interpretatioentroid valueW) and 5 m 1 m intervalssed. alysis and thour individucluded in thcluding thesw of the like
ct ve rly
of ce
is d,
ng hic es, will he re ce he
he de se ar en
no
on e. in s.
he al he se ely
Mining assum
Environmenassum
Bulk
Classi
Audit o
Discussionaccuracy o
factors or mptions
ntal factors omptions
density
ification
or reviews
n of relative of confidence
The stywith oncut minschist oat leastunweatangles tMining althougsome into be mlogging
or
Dry seaevidencwith thThese csome pMeasurair/weiglimited oxide zoThe resdefineddata alo“indicathole asassay dCompetonly qudrilling The resprincipa
e
The Combased onature and ActThe geoby comgeologi
le of mineranly a very smning of the gof up to 40 mt 200 m. Ththered and to be safely umethods wo
gh continuounternal dilutminimal at Tof the drill hason fauna ce of endange presence ocreeks will hotential for orements werght in wateto graphite sone and 2.72source is a d geometricaong the lengted” to a massay data. Foata the resotent Person uestionable ais under‐repource modeal of MineMampetent Peron the densof the assaytlab Laboratological datampetent senical data has
alisation and mall poorly mgraphite schism ensure thate steep dip competent used in an oould be by cus surface mtion due to cTarget 1 baseholes. and flora s
gered speciesof some croshave no signoxidising sulre made by er method oschist zones 2 for the primsingle tabulally, has beegth of the reaximum depor primary rource has bealso reflect
aspect in theporting the %el and calculaap Pty Ltd anrson considesity of RC any data providtories and vea collected isior geologistbeen review
the presencmineralised cst lens. The t open cut mof the minecrystalline
pen cut mineconventionamining methcross‐cuttinged on surfac
surveys haves in the areass‐cutting crenificant impaphides in watwo indepe
on selected included in mary (unweaar body in fn classified aesource. Thepth of 50 m resource bloeen classifieds confidencee resource es%TGC grade. ations have bnd a Members that this Jnd diamondded by indeperified by das deemed tots, Mr Simowed by Mr. T
ce of the mincap of abouttrue widths
mining could beralised lensrocks will e. l truck and lhods will beg dykes althoce geologica
e been alre. The area aeeks that areact on a manaste rock dumendent labordiamond cothe resourceathered) zonform. The oas “inferred”e primary zoin the verti
ocks below td as “inferree in the usestimation is tSee note on been reviewer of the AusIORC resourc drilling empendent labotabase mano be accuratn Attwell anony Cormack
neralisation t 1 m lends iexhibited bybe extendeds that occurenable max
loaded opene assessed. Tough these wal mapping a
ady carried at Target 1 ise dry for monaged mine mps and tailiratories by tore. Measure. Densities oe were applioxide zone, a” due to theone has beencal dimensiothe 50 m bod”. The knowe of these cathe possibilittwin holes. ed by Mr SeIMM. ce estimate tmployed, andoratories ALSnagers, Rock te and has bnd Dr Craig k.
at the surfactself to openy the graphitd to a depth os in relativeximum batte
n cut methodThere will bwould appeaand geologic
out with ns relatively flast of the yeasite. There ings dams. the weight rements werof 2.38 for thied. although we limited assan classified aon below droundary frowledge of thategories. Thty that the R
ldon Mart th
to be accuratd the rigorouS LaboratorieSolid Pty Lt
been overseeRugless. Th
ce n‐te of ely er
ds be ar cal
no at ar. is
in re he
ell ay as rill m he he RC
he
te us es d. en he
Appen
Sample ID
TK300652TK300653TK300654TK300655TK300656TK300657TK300658TK300659TK300660TK300661TK300662TK300663TK300664TK300665TK300666TK300667TK300668TK300669TK300670TK300671TK300672TK300673TK300674TK300675TK300676TK300677TK300678TK300679TK300680TK300681TK300682TK300683TK300684TK300685TK300686TK300687TK300688TK300689TK300690TK300691TK300692TK300693TK300694
dix 2 - Thu
AMG North
2 8053400 3 8053400 4 8053400 5 8053400 6 8053400 7 8053400 8 8053400 9 8053400 0 8053400
8053400 2 8053400 3 8053400 4 8053400 5 8053400 6 8053400 7 8053400 8 8053400 9 8053800 0 8053800
8053800 2 8053800 3 8053800 4 8053800 5 8053800 6 8053800 7 8053800 8 8053800 9 8053800 0 8053800
8053800 2 8053800 3 8053800 4 8053800 5 8053800 6 8053800 7 8053800 8 8053800 9 8053800 0 8053800
8053800 2 8053800 3 8053800 4 8054200
undelarra s
AMG East
Au ppb
386000 0.5 386050 0.5 386100 2 386150 0.5 386200 2 386250 0.5 386300 0.5 386350 0.5 386400 0.5 386450 0.5 386500 0.5 386550 0.5 386600 0.5 386650 0.5 386700 0.5 386750 0.5 386800 0.5 385600 0.5 385650 2 385700 0.5 385750 2 385800 0.5 385850 0.5 385900 0.5 385950 3 386000 2 386050 3 386100 2 386150 3 386200 0.5 386250 2 386300 0.5 386350 0.5 386400 2 386450 2 386500 0.5 386550 0.5 386600 2 386650 0.5 386700 0.5 386750 0.5 386800 3 385600 0.5
soil / rock
Pd ppb
Pt ppb
0.5 3 6 2 3 2 2 1 3 2 1 0.5 2 1
0.5 0.5 0.5 0.5 2 0.5
0.5 0.5 1 1
0.5 2 0.5 0.5 0.5 1 0.5 0.5 0.5 0.5 3 3 2 10 5 5 4 0.5 2 0.5 3 3
0.5 1 2 1 2 2 3 1 3 4 4 65 2 2 2 3
0.5 2 0.5 3 1 1 3 0.5 2 1 2 1 1 0.5 1 0.5
0.5 1 1 1
0.5 1 1 0.5
geochemi
As ppm
Cu ppm
5 99 15 164 10 96 2.5 63 5 78
2.5 35 10 54 2.5 34 2.5 35 10 67 2.5 47 5 44
2.5 45 2.5 33 10 51 2.5 30 2.5 41 2.5 73 2.5 178 2.5 97 2.5 207 2.5 94 2.5 102 5 88
2.5 153 2.5 152 5 157
2.5 159 10 312 5 128
2.5 141 2.5 128 2.5 105 2.5 103 15 100 15 173 5 85
2.5 119 2.5 29 2.5 40 2.5 46 2.5 565 10 78
istry (annu
Ni ppm
Co ppm
46 18 41 18 46 20 44 22 50 16 25 12 47 18 24 16 40 16 40 16 34 14 49 22 49 18 30 16 39 20 24 18 44 26 50 22 49 24 44 26 46 26 48 22 55 22 55 20 96 36 78 30 97 40 89 28 97 38 51 28 65 36 52 26 47 26 31 20 37 16 40 22 41 30 30 16 29 18 43 18 18 16 93 28 29 18
ual report T
Cr ppm
Fe %
180 3.8 115 4.2 110 4.5 80 4.6
125 4.3 60 3 95 4.1 75 4.1 90 3.1 95 4.3 90 3.7
110 4.5 100 4.1 75 3.7
110 4 75 4.8
130 5.5 110 5.4 115 9.6 160 6.8 85 8.2
115 6.4 130 6.1 145 5.3 235 7.1 255 7.8 220 7.6 205 8 160 9.3 105 6.8 110 7.3 110 5.7 145 6.4 55 3.9 40 4.2 60 5
150 5.7 55 5.1 85 4.4
125 4.6 35 3.7
210 5.8 55 5.2
TOG006,20
Zn ppm
Mn ppm
82 688 78 518 65 801 73 678 57 575 61 463 67 625 57 658 43 469 60 555 61 508 64 645 61 570 61 543 56 538 64 520 56 609 87 997 99 1310 91 10600 79 3170 87 2590 75 1010 64 834 87 1220 87 3940 96 1690 81 774 85 730
103 1040 109 1110 100 932 105 997 81 712 93 499
110 726 110 905 81 400 82 506 75 634 66 517 85 606 77 742
005)
Tenement
E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579
Sample ID
TK300695TK300696TK300697TK300698TK300699TK300705TK300706TK300707TK300708TK300709TK300710TK300711TK300712TK300713TK300714TK300715TK300716TK300717TK300718TK300719TK300720TK300721TK300722TK300723TK300724TK300725TK300726TK300727TK300728TK300729TK300730TK300731TK300732TK300733TK300734TK300735TK300736TK300737TK300738TK300739
AMG North
5 8054200 6 8054200 7 8054200 8 8054200 9 8054200 5 8054200 6 8054200 7 8054200 8 8054200 9 8054200 0 8054200
8054200 2 8054200 3 8054200 4 8054200 5 8054200 6 8054200 7 8054200 8 8054200 9 8054600 0 8054600
8054600 2 8054600 3 8054600 4 8054600 5 8054600 6 8054600 7 8054600 8 8054600 9 8054600 0 8054600
8054600 2 8054600 3 8054600 4 8054600 5 8054600 6 8054600 7 8054600 8 8054600 9 8054600
AMG East
Au ppb
385650 0.5 385700 2 385750 8 385800 0.5 385850 3 386150 2 386200 0.5 386250 0.5 386300 0.5 386350 0.5 386400 0.5 386450 0.5 386500 0.5 386550 2 386600 0.5 386650 0.5 386700 0.5 386750 0.5 386800 0.5 385800 0.5 385850 0.5 385900 0.5 385950 0.5 386000 0.5 386050 0.5 386100 0.5 386150 2 386200 2 386250 2 386300 2 386350 2 386400 0.5 386450 2 386500 0.5 386550 0.5 386600 0.5 386650 0.5 386700 0.5 386750 0.5 386800 0.5
Pd ppb
Pt ppb
2 2 2 175
36 21 4 2 6 133
0.5 2 3 1 1 60 4 6 1 2 2 1 8 7
0.5 1 1 2 4 2 2 2 2 2
0.5 3 6 8 2 2 4 5 2 1 2 3 1 1 1 2
0.5 1 0.5 1 2 2 3 3 3 4 1 0.5 1 0.5
0.5 1 0.5 1 2 1
0.5 0.5 3 3
0.5 0.5 0.5 0.5 0.5 0.5
As
ppm Cu
ppm 2.5 109 2.5 171 2.5 249 2.5 98 10 339 10 275 2.5 116 2.5 67 2.5 171 2.5 81 5 220
2.5 93 2.5 77 10 88 2.5 33 2.5 54 10 80 2.5 40 2.5 48 5 41
2.5 55 2.5 49 2.5 68 10 70 15 31 2.5 34 2.5 41 2.5 49 10 39 2.5 66 2.5 45 2.5 24 2.5 16 2.5 25 2.5 45 2.5 17 2.5 94 2.5 40 2.5 27 2.5 16
Ni
ppm Co
ppm 24 18 44 18
268 56 40 20 89 32 54 22 81 28 69 32 73 30 53 24 56 24 82 30 53 28 71 38
212 42 55 26 45 26 82 32
108 40 62 26
115 48 49 26 65 32 53 28 50 26 24 28 27 16 67 28 75 38 98 38 39 28 17 12 11 8 22 16 37 26 10 6 66 22 33 14 12 10 15 8
Cr
ppm Fe %
60 5.4 150 8.9 380 7.9 80 5.1
145 7.3 110 5.5 165 6.7 130 7.8 200 7.8 125 5.1 115 5.9 250 7.9 155 6.5 155 5.7 340 6.3 135 5.8 70 6.5
285 6 285 6.5 190 6.5 335 11 115 5.8 170 6.5 110 5.8 115 5.5 50 6.3 70 3.9
145 7.3 180 7.7 270 7.8 145 7.7 40 4.3 30 3 50 3.7
115 5.8 25 2.4
140 5.6 80 3.8 35 2.2 40 2.4
Zn
ppm Mn
ppm 63 763 69 1080 95 1540 77 523 71 588 82 554 93 845 92 1450
100 1350 73 660 77 756 61 740 75 793 52 718 55 692 40 718 86 947 89 923 74 1420 95 981
106 1830 82 897 86 877 75 889 71 924 87 1010 67 644 85 1120 68 1130 72 948 83 914 74 552 74 384 65 527 71 835 51 302 86 651 74 545 63 358 61 373
Tenement
E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579 E80/2579
