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dc.contributor.authorPalmer, DCen_US
dc.date.accessioned2013-10-23T18:57:53Z-
dc.date.issued1993en_US
dc.identifier.govdocCR1993-0270en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/71779en_US
dc.description.abstract20 -2mm and 17 -80# stream sediment samples were examined for kimberlitic indicators and base metal anomalism respectively. No microdiamonds-kimberlitic indicator minerals were noted in the former and no base metal anomalies were outlined in the latter.en_US
dc.description.abstractLow level airborne magnetic-radiometric survey completed by Kevron Geophysics May 1992 with a line spacing of 300m tie lines 500m and terrain clearance 60m.en_US
dc.subject.classificationDiamondsen_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationStream sediment samplingen_US
dc.subject.classificationIndicator mineralsen_US
dc.titlePartial Relinquishment Report EL 7175 Heifer Creek year ending 21 January 1993.en_US
dc.relation.isatmap100Calvert Hills 6363en_US
dc.relation.isatmap100Wollogorang 6463en_US
dc.relation.isatmap250Calvert Hills SE5308en_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.relation.isatgeolprovinceWearyan Shelfen_US
dc.description.stratnameWollogorang Formationen_US
dc.description.stratnameMasterton Sandstoneen_US
dc.description.stratnameTawallah Groupen_US
dc.description.stratnameHobblechain Rhyoliteen_US
dc.description.stratnameGold Creek Volcanicsen_US
dc.description.geochemicalsampling20 -2mm and 17 -80# stream sediment samplesen_US
dc.identifier.tenureEL7175en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory22/02/2005en_US
dc.description.modifyhistory23/02/2005en_US
dc.description.modifyhistory20/04/2005en_US
dc.description.modifyhistory24/10/2006en_US
dc.description.modifyhistory18/08/2014en_US
dc.contributor.holderCRA Explorationen_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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