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dc.contributor.authorButler, IKen_US
dc.date.accessioned2013-10-23T06:20:44Z-
dc.date.issued1994en_US
dc.identifier.govdocCR1994-0293en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/62155en_US
dc.description.abstractInterpretation of the gravity data suggests that the gravity high is associated with the presence of Coomalie Dolomite in the core of a NW trending antiform. Weak elevated Pb values are associated with the gravity high.en_US
dc.subject.classificationGeophysicsen_US
dc.subject.classificationGravity surveysen_US
dc.subject.classificationGeochemical anomaliesen_US
dc.titleAnnual report for year two EL 7670 13-04-1993 to 12-04-1994.en_US
dc.relation.isatmap250Darwin SD5204en_US
dc.relation.isatgeolprovincePine Creek Orogenen_US
dc.description.stratnameCoomalie Dolomiteen_US
dc.identifier.tenureEL7670en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory20/04/2005en_US
dc.description.modifyhistory11/06/2014en_US
dc.contributor.holderAztec Mining Companyen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1994en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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