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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/79847
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dc.contributor.authorCarthew, Sen_US
dc.date.accessioned2015-03-19T07:49:47Z-
dc.date.issued1996en_US
dc.identifier.govdocCR1996-0817en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/79847en_US
dc.description.abstractA reconnaissance of the Koolendong Valley south of the Fitzmaurice River examined three of the four low rises in the valley floor between the outcropping Meeway Volcanics and the Fitzmaurice River which are shown as Noltenius Formation on the PORT KEATS 1:250,000 geological map (SD52-11 ). All were found to be formed of sandstone of the Moyle River Formation Sandstone with no sign of veining or significant alteration.en_US
dc.subject.classificationGolden_US
dc.subject.classificationGold depositsen_US
dc.subject.classificationQuartz veinsen_US
dc.subject.classificationExploration historyen_US
dc.subject.classificationLiterature reviewsen_US
dc.titleEL 8040 Koolendong Relinquishment report for the period ending 9 July 1996en_US
dc.relation.isatmap100Fitzmaurice 4968en_US
dc.relation.isatmap250Port Keats SD5211en_US
dc.relation.isatgeolprovinceVictoria Basinen_US
dc.relation.isatgeolprovincePine Creek Orogenen_US
dc.description.stratnameMeeway Volcanicsen_US
dc.description.stratnameMoyle River Formationen_US
dc.identifier.tenureEL8040en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory02/02/2004en_US
dc.description.modifyhistory06/12/2004en_US
dc.description.modifyhistory16/02/2005en_US
dc.description.modifyhistory12/03/2015en_US
dc.description.modifyhistory19/03/2015en_US
dc.contributor.holderCorporate Developmentsen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1996en_US
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Appears in Collections:Minerals Exploration Reports (MEX)

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