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dc.contributor.authorMathison, IJen_US
dc.contributor.authorPoltock, Ren_US
dc.date.accessioned2013-10-23T07:50:17Z-
dc.date.issued1993en_US
dc.identifier.govdocCR1993-0221en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/63205en_US
dc.description.abstract4 percussion drill holes were completed in the south of the licence. The drill holes confirmed the presence of carbonate rich dolomite, which correlated with the Karns Dolomite. The source of the gravity high is yet to be determined. It may be due to local thickening of the Karns Dolomite or a basement high consisting of basic volcanics of the Tawallah Group.en_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationDrillingen_US
dc.subject.classificationPercussion drillingen_US
dc.subject.classificationGeochemistryen_US
dc.subject.classificationLithologyen_US
dc.subject.classificationMagnetic propertiesen_US
dc.subject.classificationMagnetic susceptibilityen_US
dc.titleReport for EL 7312 Wearyn year ending February 1993.en_US
dc.relation.isatmap100Wearyan 6265en_US
dc.relation.isatmap100Robinson 6365en_US
dc.relation.isatmap250Robinson River SE5304en_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.relation.isatgeolprovinceWearyan Shelfen_US
dc.description.stratnameMcArthur Groupen_US
dc.description.stratnameKarns Dolomiteen_US
dc.description.stratnameMasterton Sandstoneen_US
dc.description.stratnameTawallah Groupen_US
dc.description.drilling4 percussion drill holes totalling 306.2men_US
dc.description.drillingPercussion drill holes WMA-S-1 to S-4en_US
dc.identifier.tenureEL7312en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory24/10/2006en_US
dc.description.modifyhistory18/08/2014en_US
dc.description.modifyhistory03/12/2015en_US
dc.contributor.holderPeko-Wallsend Operationsen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1993en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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