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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/67432
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dc.date.accessioned2013-10-23T13:07:36Z-
dc.date.issued1998en_US
dc.identifier.govdocCR1999-0121en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/67432en_US
dc.description.abstractPhotogeoloical and purchased aeromagnetic data interpretation concluded that possible paleo channels that could be host to alluvial diamonds, are due to iron staining. Other gravel zones below the Cambrian were found to be part of the Moonlight Valley glacigenic section. The variation in magnetic intensity can be explained by the variable thickness of the Antrim Plateau Volcanics.en_US
dc.subject.classificationGeophysical surveysen_US
dc.subject.classificationAerial magnetic surveysen_US
dc.subject.classificationGeneral geologyen_US
dc.subject.classificationPhotogeologyen_US
dc.titleRelinquishment report EL9009 Newryen_US
dc.relation.isatmap100Newry 4765en_US
dc.relation.isatmap250Waterloo SE5203en_US
dc.relation.isatgeolprovinceVictoria-Birrindudu Basinen_US
dc.identifier.tenureEL9009en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory02/12/2004en_US
dc.description.modifyhistory07/06/2013en_US
dc.description.modifyhistory15/09/2020en_US
dc.contributor.holderExploration Technology Servicesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1999en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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