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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/63209
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dc.contributor.authorKettlewell, DCen_US
dc.date.accessioned2013-10-23T07:50:33Z-
dc.date.issued1992en_US
dc.identifier.govdocCR1992-0643en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/63209en_US
dc.description.abstractA further 15 anomalous zones were defined by geophysics. The majority of the PROTEM conductors were probably caused by near surface ferruginous clay and laterite with a minor ground water component. Conductors in holes LD10-11 and LP14-15 were caused by abundant disseminated pyrite in black-grey dololutite. Lead isotope work suggests that the majority of samples tested have undergone in situ radioactive decay of U and Pb. The isochron age of the samples points to a younger source for the lead than for the HYC deposit. An epigenetic origin for the lead has been inferred. Stockdale Prospecting have downgraded 2 of the 3 aeromagnetic anomalies.en_US
dc.subject.classificationDiamondsen_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationDrillingen_US
dc.subject.classificationDiamond drillingen_US
dc.subject.classificationPercussion drillingen_US
dc.subject.classificationGeophysicsen_US
dc.subject.classificationAerial surveysen_US
dc.subject.classificationGround EM surveysen_US
dc.subject.classificationGravity surveysen_US
dc.subject.classificationGeochemistryen_US
dc.subject.classificationSoil samplingen_US
dc.subject.classificationGeochemical anomaliesen_US
dc.subject.classificationGeological mappingen_US
dc.subject.classificationPetrologyen_US
dc.subject.classificationDown hole geophysicsen_US
dc.subject.classificationAerial EM surveysen_US
dc.subject.classificationCross sectionsen_US
dc.subject.classificationBouguer anomaly mapsen_US
dc.subject.classificationGravity anomaliesen_US
dc.subject.classificationLiterature reviewsen_US
dc.subject.classificationLead isotopesen_US
dc.subject.classificationLead isotope datingen_US
dc.subject.classificationRC drillingen_US
dc.titleSecond annual report EL 6808 Lorella year ending 2 November 1992.en_US
dc.relation.isatmap100Tawallah Range 6066en_US
dc.relation.isatmap250Mount Young SD5315en_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.relation.isatgeolprovinceBatten Troughen_US
dc.description.stratnameTawallah Groupen_US
dc.description.stratnameMcArthur Groupen_US
dc.description.stratnameLynott Formationen_US
dc.description.stratnameYalco Formationen_US
dc.description.stratnameHot Spring Memberen_US
dc.description.stratnameWollogorang Formationen_US
dc.description.stratnameCaranbirini Memberen_US
dc.description.stratnameWarramana Sandstoneen_US
dc.description.stratnameWununmantyala Sandstoneen_US
dc.description.drilling8 NQ diamond and 6 RC percussion totalling 2337.40men_US
dc.identifier.tenureEL6808en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory23/02/2005en_US
dc.description.modifyhistory01/03/2005en_US
dc.description.modifyhistory31/03/2005en_US
dc.description.modifyhistory24/10/2006en_US
dc.description.modifyhistory03/10/2014en_US
dc.contributor.holderMount Isa Minesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1992en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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