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dc.contributor.authorFleming, AWen_US
dc.date.accessioned2013-10-23T18:20:56Z-
dc.date.issued1980en_US
dc.identifier.govdocCR1980-0052en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/71365en_US
dc.description.abstractTest geophysical surveys using the Rapid Reconnaissance magnetic Induced Polarisation technique over copper sulphide mineralisation at Sandy Flat revealed additional anomalies similar to that for the Sandy Flat mineralisation. Follow-up geophysics indicated a number of targets which wre subsequently tested by shallow percussion drilling. No additional copper-bearing breccia pipes similar to Sandy Flat were found. The geophysical anomalies are thought to be due to disseminated sulphides. One of the targets requires further testing. The geophysical data for Sandy Flat and results from one shallow drillhole indicate significant untested potential for additonal mineralisation both near surface and at depth.en_US
dc.subject.classificationCopperen_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationMagnetic surveysen_US
dc.subject.classificationPercussion drillingen_US
dc.title1980 Annual Report for Redbank (Sandy Flat) Titlesen_US
dc.relation.isatmap100Wollogorang 6463en_US
dc.relation.isatmap250Calvert Hills SE5308en_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.description.stratnameTawallah Groupen_US
dc.description.stratnameGold Creek Volcanicsen_US
dc.description.geochemicalsampling177 drillhole samplesen_US
dc.description.drilling21 percussion drillholes for 1014 metresen_US
dc.description.mineprospectnameSandy Flat Prospecten_US
dc.description.mineprospectnameRedbank Depositsen_US
dc.identifier.tenureSMLA66en_US
dc.identifier.tenureSMLA67en_US
dc.description.modifyhistory01/02/2016en_US
dc.description.modifyhistory05/10/2023en_US
dc.contributor.holderTriako Minesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1980en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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