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ISSUE 86 June 2007 Regional geochemical study paves way for national survey Regional geochemical study paves way for national survey Geochemistry of near-surface regolith points to new resources Megan Lech and Patrice de Caritat e omson Regional Geochemical Survey covered an area of approximately 155 000 square kilometres in northwestern New South Wales (figure 1), encompassing parts of the omson Orogen and the adjacent Lachlan and Delamerian Orogens (Greenfield et al 2006a). e project aimed to boost greenfield mineral exploration in the region by providing an internally consistent, background geochemical dataset for the southern omson Orogen region. It also aimed to refine sampling protocols developed in other regions to ensure their suitability to a range of environments across Australia. e region is covered by substantial transported regolith, including sediments from the Cainozoic Lake Eyre, Bulloo–Bancannia and Murray–Darling river basins and Cainozoic sand dunes and sand plains. Outcropping crystalline basement includes various mineral occurrences in the Broken Hill (lead, zinc, tin), Tibooburra (gold) and Cobar (lead, copper, gold) regions. Interest in conducting a geochemical survey in the omson region arose from a similar survey in the Riverina region of New South Wales and Victoria (Caritat et al 2004), and the preliminary interpretations that resulted (Caritat et al 2005). e Riverina survey identified geochemical patterns in the near-surface regolith that relate to geological and mineralisation features below the cover. ese included elevated regolith gold concentrations in catchments containing known gold deposits or occurrences, dispersion trains of arsenic and antimony from the Victorian goldfields, and anomalous silver, lead and zinc in the eastern part of the study area which borders the base metal-rich Lachlan Fold Belt. e Riverina and omson results show how regional geochemical surveys can provide fundamental datasets for mineral exploration and resource potential evaluation, environmental monitoring and policy development, and geomedical studies into the health of humans, animals and plants. e omson Regional Geochemical Survey was a collaborative project between Geoscience Australia, the Cooperative Research Centre for Landscape Environments and Mineral Exploration (CRC LEME), and the NSW Department of Primary Industries (Greenfield et al 2006b). Figure 1. Sample locations over image of the first vertical derivative of the total magnetic intensity (courtesy of NSW Department of Primary Industries). Project boundary Catchment boundary Drainage Outlet sediment sample 07-1670-1 SA QLD SA NSW 28 29 30 31 32 141 142 143 144 145 146 147 148 0 100 km Tibooburra Cobar Broken Hill Nyngan Bourke Lightning Ridge Wilcannia WA NT SA QLD NSW VIC TAS Bourke

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Page 1: Regional geochemical study paves way for national survey

issue 86 June 2007

Regional geochemical study paves way for national survey �

Regional geochemical study paves way for national surveyGeochemistry of near-surface regolith points to new resources

Megan Lech and Patrice de Caritat

TheThomsonRegionalGeochemicalSurveycoveredanareaofapproximately155000squarekilometresinnorthwesternNewSouthWales(figure1),encompassingpartsoftheThomsonOrogenandtheadjacentLachlanandDelamerianOrogens(Greenfieldetal2006a).

Theprojectaimedtoboostgreenfieldmineralexplorationintheregionbyprovidinganinternallyconsistent,backgroundgeochemicaldatasetforthesouthernThomsonOrogenregion.ItalsoaimedtorefinesamplingprotocolsdevelopedinotherregionstoensuretheirsuitabilitytoarangeofenvironmentsacrossAustralia.

Theregioniscoveredbysubstantialtransportedregolith,includingsedimentsfromtheCainozoicLakeEyre,Bulloo–BancanniaandMurray–DarlingriverbasinsandCainozoicsanddunesandsandplains.OutcroppingcrystallinebasementincludesvariousmineraloccurrencesintheBrokenHill(lead,zinc,tin),Tibooburra(gold)andCobar(lead,copper,gold)regions.

InterestinconductingageochemicalsurveyintheThomsonregionarosefromasimilarsurveyintheRiverinaregionofNewSouthWalesandVictoria(Caritatetal2004),andthepreliminaryinterpretationsthatresulted(Caritatetal2005).

TheRiverinasurveyidentifiedgeochemicalpatternsinthenear-surfaceregoliththatrelatetogeologicalandmineralisationfeaturesbelowthecover.Theseincludedelevatedregolithgoldconcentrationsincatchmentscontainingknowngolddepositsoroccurrences,dispersiontrainsofarsenicandantimonyfromtheVictoriangoldfields,andanomaloussilver,leadandzincintheeasternpartofthestudyareawhichbordersthebasemetal-richLachlanFoldBelt.

TheRiverinaandThomsonresultsshowhowregionalgeochemicalsurveyscanprovidefundamentaldatasetsformineralexplorationandresourcepotentialevaluation,environmentalmonitoringandpolicydevelopment,andgeomedicalstudiesintothehealthofhumans,animalsandplants.

TheThomsonRegionalGeochemicalSurveywasacollaborativeprojectbetweenGeoscienceAustralia,theCooperativeResearchCentreforLandscapeEnvironmentsandMineralExploration(CRCLEME),andtheNSWDepartmentofPrimaryIndustries(Greenfieldetal2006b).

Figure 1. Samplelocationsoverimageofthefirstverticalderivativeofthetotalmagneticintensity(courtesyofNSWDepartmentofPrimaryIndustries).

Project boundary

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Regional geochemical study paves way for national survey �

Floodplain sediments provide evidence

Themainsamplingmediumtargetedforthesurveywasoverbanksedimentsinfloodplains.Thisismorelikelythanothermediatorepresentanaveragecompositionofentirecatchments,enablinglow-costsamplingoflargeareas(Ottesenetal1989,Bølvikenetal2004).Targetsamplesiteswereselectedbyconductinghydrologicalanalysistodeterminethelowestpointineachcatchment.Sampleswerecollectedatbackgroundlocations,awayfromareasofobviousdisturbanceorcontamination.

Ateachsite,twointervalsapproximately10centimetresthickweresampled:oneat0to10centimetresbelowtherootlayer,ifpresent(topoutletsediment,TOS),andanotherusuallyatadepthof60to90centimetres(bottomoutletsediment,BOS).Atotalof99catchmentoutletsitesweresampledoverthearea,givinganaveragesampledensityof1per1540squarekilometres.Todate,geochemicalresultsareavailableforthefirst76sites.

Samplesweredriedandsievedat<75µmand<180µmfractionsbeforegeochemicalanalysis.Theconcentrationsofover60majorandtraceelementsweredeterminedbyX-rayfluorescenceandinductivelycoupledplasma–massspectrometry(ICPMS).SamplepreparationforICPMSinvolved4-acid‘near-total’digestionformulti-elementanalysisandmulti-aciddigestionforseleniumanalysis.Ionselectiveelectrodeanalysiswasundertakentomeasurefluorine,andgraphitefurnace–atomicadsorptionspectrometryforgold.

High concentrations at several sitesFigures2atocand3provideinformationontheconcentrationsofcopper,leadandantimonywiththeircorrespondinggeochemicaldistributions.

AcopperanomalyispresentintheBOS<75µmand<180µmfractions(32milligramsperkilogram(mg/kg)and24mg/kg,respectively)neartheBarrierRangesnorthofBrokenHilland50kilometressoutheastofBrewarrina(29mg/kgand27mg/kg).SeventykilometressoutheastofTibooburrathereisasamplewithanotablyhighcopperconcentration(25mg/kg)inthe<180µmfraction.Higherconcentrationsofcopperinthecentralwestareonlyafewkilometresawayfromarecentexplorationcompanydrillholethatintersectedbeddedpyritemineralisation(figure2a).

Elevatedleadconcentrations(21.7mg/kg)arevisibleinthesoutheast,presumablyreflectingproximitytotheBarrierRanges,andnortheastofCobarnearoutcropoftheLachlanFoldBelt.Bothregionshaveknownleadmineraloccurrences.Elevatedleadvalues(19.48mg/kgand19.22mg/kginthe<180µmfraction)alsooccurinthecentralwest,coincidentwithelevatedcoppervalues(figure2b).

Antimonyshowssimilargeochemicalpatternstoleadandcopper.AntimonyisnotablyhighernortheastofCobarandinthecentralwest(0.70mg/kg)inthe<180µmfraction.Valuesof0.86mg/kgand0.79mg/kgforthe<180µmfractionwererecordedinsamplescollected40kilometresnorthofCobaronYandaCreek(figure2c).

Anomalousconcentrationsoflead,copperandantimonymostlyoccurproximalto

“TheRiverinaandThomsonresultsshowhowregionalgeochemicalsurveyscanprovidefundamentaldatasetsformineralexplorationandresourcepotentialevaluation,environmentalmonitoringandpolicydevelopment,andgeomedicalstudiesintothehealthofhumans,animalsandplants.”

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Regional geochemical study paves way for national survey �

outcroppingcrystallinebasement.Threemainareashavebeenidentified:

southwestregion,correspondingtotheCurnamonaCratonwhichhoststheBrokenHillorebody

centraltosouthwestregionatthejunctionoftheKoonenberry,ThomsonandLachlancrustalelements

easternandsouthernregion,wheretheeastandwestLachlancrustalelementsadjoinbeneaththeCobarBasin.

Lessons for explorationLowerelementconcentrationsgenerallycoincidewithareasofthickerGreatAustralianSuperBasincover.Thresholdsinthisareamayneedtobeloweredtocorrectlyassesstheprospectivityoftheseterrains.

Generally,catchmentswithknownmineraloccurrencesrelatingtolead,copperorantimonyhaveanomalousconcentrationsofthatelementintheoutletsample.Dispersionofelementsappearstobeatthecatchmentscale.

Severalanomalousconcentrationsoccurawayfromknownmineralisationandwarrantfurtherinvestigation.TheseincluderesultsfromrecentcompanydrillingnorthoftheKoonenberryBeltandnortheastofCobar.

ThesuccessoftheThomsonandotherpilotgeochemicalsurveysledtotherecentannouncementofthecontinent-wideNationalGeochemical

Project boundary

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Major commodity (Cu)

Thomson Catchment(ANUDEM)

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Cu (mg/kg)(<180 m) BOSµ

Exploration drill hole

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Exploration drill hole

Project boundary

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Thomson Catchment(ANUDEM)

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0.29 - 0.350.36 - 0.380.39 - 0.500.51 - 0.86

Mineral commodities(NSW)

AgCuAuZn

SnPtPb

Figure 2. (a)GeochemicalmapofcopperconcentrationsintheBOS<180µmfractionwithknowncopperoccurrences;(b)GeochemicalmapofleadconcentrationsintheBOS<180µmfractionwithknownleadoccurrences;(c)GeochemicalmapofantimonyconcentrationsintheBOS<180µmfractionwithknownmineraloccurrences

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Regional geochemical study paves way for national survey �

SurveyofAustraliaproject(Baldwin2007).ThatprojectispartoftheAustralianGovernment’sOnshoreEnergySecurityInitiative(Johnson2006)andwillgathergeochemicaldatathatwillprincipallybeusedtosupportexplorationforAustralia’senergy-relatedresources.

ReferencesBaldwinB(ParliamentarySecretaryforIndustry,TourismandResources).2007.ZeroinginonAustralia’sonshoreenergyandminerals.Mediarelease,2March2007,DepartmentofIndustryTourismandResources.Availableat:minister.industry.gov.au/index.cfm?event=object.showContent&objectID=0F26ADF9-C2A0–4C89-FC1574CD3883BEAA

BølvikenB,BogenJ,JartunM,LangedalM,OttesenRT&VoldenT.2004.Overbanksediments:anaturalbedblendingsamplingmediumforlarge-scalegeochemicalmapping.ChemometricsandIntelligentLaboratorySystems74:183–199.

CaritatPde,JairethS,LechM&PykeJ.2004.Regionalgeochemicalsurveys:RiverinaPilotproject—methodologyandpreliminaryresults.CooperativeResearchCentreforLandscapeEnvironmentsandMineralExplorationOpenFileReport160.Availableat:www.crcleme.org.au/Pubs/OFR160/CRCLEME_OFR160.pdf

CaritatPde,LechM,JairethS,PykeJ&LambertI.2005.Riverinageochemicalsurvey—ANationalFirst.AusGeo News 78.Availableat:www.ga.gov.au/image_cache/GA6632.pdf

GreenfieldJ,ReidW,GilmoreP,CaritatdeP,LechM,HillS,HulmeK,WatkinsJ&WorrallL.2006a.TheThomsonOrogenProject—aworkinprogress.In:FitzpatrickRW&ShandP(eds),Regolith2006—Consolidationanddispersionofideas.ProceedingsoftheCRCLEMERegolithSymposium,Hahndorf,SouthAustralia,6–9November2006.Availableat:crcleme.org.au/Pubs/Monographs/regolith2006/Greenfield_J.pdf

GreenfieldJ,CaritatdeP,HillP&ReidW.2006b.TheNSWThomsonOrogenProject:newfrontiersinexploration,In:NSWDPIMinesandWinesConference,Cessnock,25–26May2006,Cessnock.Availableat:www.smedg.org.au/Greeab.pdf

JohnsonJ.2006.OnshoreEnergySecurityProgramunderway.Webpage:www.ga.gov.au/ausgeonews/ausgeonews200612/onshore.jsp(accessed29February2007).

OttesenRT,BogenJ,BølvikenB&VoldenT.1989.Overbanksediment:arepresentativesamplemediumforregionalgeochemicalsampling.JournalofGeochemicalExploration32:257–277.

Related websites/articlesAusGeo News 78:Riverinageochemicalsurveyanationalfirst

www.ga.gov.au/ausgeonews/ausgeonews200506/geochem.jsp

For more informationphone MeganLechon+61262499459email [email protected] PatricedeCaritaton+61262499378email [email protected]

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Figure 3. Boxplotsofcopper,leadandantimonyconcentrationsintheTOSandBOS<75and<180µmfractions.