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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/63571
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dc.contributor.authorTham, GHen_US
dc.contributor.authorO'Sullivan, KNen_US
dc.date.accessioned2013-10-23T08:18:47Z-
dc.date.issued1972en_US
dc.identifier.govdocCR1972-0067en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/63571en_US
dc.description.abstractThe area of Burt Plain was examined for its uranium potential. Seismic traverses were conducted to indicate depth to basement. These indicated the possible presence of Mesozoic sediments with a propagation velocity of 3600 m/sec beneath the Tertiary at 1500 m/sec. Precambrian rocks were assumed to 6000 m/sec. Radiometric traverses were conducted and water bores gamma logged. Apart from weak uranium anomalies associated with travertine, no indications were found.en_US
dc.subject.classificationUraniumen_US
dc.subject.classificationSeismic profilesen_US
dc.subject.classificationSeismic refraction methodsen_US
dc.subject.classificationWater wellsen_US
dc.subject.classificationRadiometric surveyen_US
dc.titleFinal Report, Burt Plain AP 3382 and EL 441en_US
dc.relation.isatmap100Burt 5651en_US
dc.relation.isatmap100Anburla 5551en_US
dc.relation.isatmap250Hermannsburg SF5313en_US
dc.relation.isatgeolprovinceArunta Regionen_US
dc.relation.isatgeolprovinceCenozoic sedimentsen_US
dc.relation.isatgeolprovinceAmadeus Basinen_US
dc.description.geochemicalsamplingWater bore sampling carried out.en_US
dc.identifier.tenureAP3382en_US
dc.identifier.tenureEL441en_US
dc.description.modifyhistory19/04/2007en_US
dc.description.modifyhistory07/08/2009en_US
dc.description.modifyhistory31/08/2016en_US
dc.description.modifyhistory11/01/2021en_US
dc.contributor.holderCRA Explorationen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1972en_US
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Appears in Collections:Minerals Exploration Reports (MEX)

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