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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/73183
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dc.contributor.authorBurton, PEen_US
dc.date.accessioned2013-10-23T20:29:34Z-
dc.date.issued1993en_US
dc.identifier.govdocCR1993-0131en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/73183en_US
dc.description.abstractSites of anomalous Pb-Zn geochemistry outlined in 1991 were followed up in the 1992 field season. 651 samples were collected. This work has shown the Limmen Sandstone to be lead rich (maximum lead assay 3.13% Pb) and the Mountain Valley Limestone to elevated in zinc (maximum zinc assay 653000m Zn). It is thought that the mineralisation is due to circulating hydrothermal fluids (probably due to the predominance of lead).en_US
dc.subject.classificationDiamondsen_US
dc.subject.classificationBase metalsen_US
dc.titleCommon report ELs 6287 and 6288 Roper River area to 31 December 1992en_US
dc.relation.isatmap100Marumba 5770en_US
dc.relation.isatmap100Mainoru 5670en_US
dc.relation.isatmap100Throsby 5769en_US
dc.relation.isatmap100Flying Fox 5669en_US
dc.relation.isatmap250Mount Marumba SD5306en_US
dc.relation.isatmap250Urapunga SD5310en_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.description.stratnameLimmen Sandstoneen_US
dc.description.stratnameMountain Valley Limestone Memberen_US
dc.description.stratnameMainoru Formationen_US
dc.description.stratnameGundi Greywackeen_US
dc.description.stratnameMount Rigg Groupen_US
dc.description.stratnameDook Creek Formationen_US
dc.description.geochemicalsampling651 samplesen_US
dc.identifier.tenureEL6287en_US
dc.identifier.tenureEL6288en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory20/04/2005en_US
dc.description.modifyhistory24/10/2006en_US
dc.description.modifyhistory18/08/2014en_US
dc.contributor.holderStockdale Prospectingen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1993en_US
local.flag.notified1
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