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dc.contributor.authorNorris, MSen_US
dc.date.accessioned2013-10-23T19:09:22Z-
dc.date.issued1990en_US
dc.identifier.govdocCR1990-0417en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/71959en_US
dc.description.abstractThe majority of the EL consists of granite of the Coomarie Dome which is considered unprospective areas are restricted to the areas of aeromagnetic. Anomalism in the southwest and northeast. The aeromagnetic anomaly in the southwest of the EL is related to ultramafic rocks.en_US
dc.description.abstractLag sampling results are not available.en_US
dc.titleAnnual report EL 6459 for year ending 22-05-1990en_US
dc.relation.isatmap100Pargee 4758en_US
dc.relation.isatmap250Tanami SE5215en_US
dc.relation.isatgeolprovinceTanami Regionen_US
dc.identifier.tenureEL6459en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory15/04/2005en_US
dc.description.modifyhistory24/10/2006en_US
dc.description.modifyhistory09/02/2015en_US
dc.contributor.holderWestern Miningen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1990en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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