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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/64836
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dc.contributor.authorYpma, PJen_US
dc.date.accessioned2013-10-23T09:47:10Z-
dc.date.issued1986en_US
dc.identifier.govdocCR1986-0235en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/64836en_US
dc.description.abstractHost rock geochemistry identified stromatolitic dolomite as the most likely host to mineralisation. Sulphides and barite are found as stratiform and stratabound cavity fillings. The mineralisation is disperse and of wide lateral extent but low in grade. Ore grade material is confined to faults that breach shallow anticlinal structures. Here localised values of up to 10% lead and 1% zinc occur.en_US
dc.subject.classificationLeaden_US
dc.subject.classificationZincen_US
dc.subject.classificationSulphidesen_US
dc.subject.classificationBariteen_US
dc.subject.classificationGalenaen_US
dc.title1986 Final Report on exploration activities over EL 3166 and 3214en_US
dc.relation.isatmap100Arapunga 6053en_US
dc.relation.isatmap250Huckitta SF5311en_US
dc.relation.isatgeolprovinceGeorgina Basinen_US
dc.description.stratnameArthur Creek Formationen_US
dc.description.stratnameDulcie Sandstoneen_US
dc.description.stratnameElkera Formationen_US
dc.description.stratnameArrinthrunga Formationen_US
dc.description.mineprospectnameBox Hole Bore Prospecten_US
dc.identifier.tenureEL3166en_US
dc.identifier.tenureEL3214en_US
dc.description.modifyhistory06/09/2004en_US
dc.description.modifyhistory05/05/2015en_US
dc.description.modifyhistory19/08/2015en_US
dc.description.modifyhistory09/09/2021en_US
dc.contributor.holderPlenty River Mining Companyen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1986en_US
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Appears in Collections:Minerals Exploration Reports (MEX)

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