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dc.contributor.authorEupene, GSen_US
dc.date.accessioned2013-10-23T16:18:27Z-
dc.date.issued2002en_US
dc.identifier.govdocCR2002-0313en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/69797en_US
dc.description.abstractAll geophysical data has been reviewed and the source of the prominent magnetic feature has been analyzed. It appears that most likely source of the feature is a basis intrusive of post Properozoic age, possibly related to the Antrim Plateau Volcanics, though this is probably not an extrusive centre. This target could be a layered mafic intrusive, with potential for accumulations of metal sulfides deposits of Ni, Co, Cu etc. Follow up work would involve magnetic traverses, gravity, mobile ion geochemistry and subsequent drilling in year 3.en_US
dc.subject.classificationRegional geologyen_US
dc.subject.classificationStratigraphyen_US
dc.subject.classificationLiterature reviewsen_US
dc.subject.classificationMagnetic interpretationen_US
dc.subject.classificationCopperen_US
dc.subject.classificationPlatinum group elementsen_US
dc.subject.classificationNickelen_US
dc.titleFirst annual report for EL 9856 'Gregory's Depot'en_US
dc.relation.isatmap100Gregory's Depot 4963en_US
dc.relation.isatmap100Mount Barton 4962en_US
dc.relation.isatmap250Limbunya SE5207en_US
dc.relation.isatgeolprovinceTanami Regionen_US
dc.relation.isatgeolprovinceVictoria-Birrindudu Basinen_US
dc.description.stratnameInverway Metamorphicsen_US
dc.description.stratnameBirrindudu Groupen_US
dc.description.stratnameAntrim Plateau Volcanicsen_US
dc.identifier.tenureEL9856en_US
dc.description.modifyhistory16/03/2006en_US
dc.description.modifyhistory17/12/2013en_US
dc.contributor.holderEupene Exploration Enterprisesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2002en_US
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Appears in Collections:Minerals Exploration Reports (MEX)

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EL9856_2002_A_02_Variation_of_Expenditure_Covenant.pdf105.5 kBPDF Add
EL9856_2002_A_03_Table1.pdf130.09 kBPDF Add
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