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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/65349
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dc.contributor.authorFarlabolini, Wen_US
dc.contributor.authorOmnes, Gen_US
dc.date.accessioned2013-10-23T10:19:43Z-
dc.date.issued1971en_US
dc.identifier.govdocCR1971-0155en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/65349en_US
dc.description.abstractSeismic refraction yielded less satisfactory results than the resistivity technique. 9 conductive anomalies were delineated. It is suggested that these conductive anomalies represent wide buried channels filled with conductive material. Provenance of sediments from the north. The edges of these channels may be favourable sites for mineralisation.en_US
dc.subject.classificationGeophysicsen_US
dc.subject.classificationResistivity surveysen_US
dc.subject.classificationSeismic refraction surveysen_US
dc.subject.classificationEquipmenten_US
dc.subject.classificationPersonnelen_US
dc.subject.classificationCopperen_US
dc.subject.classificationMalachiteen_US
dc.subject.classificationAzuriteen_US
dc.title1971 Geophysical survey at EL 786 Mount Skinneren_US
dc.relation.isatmap100Woodgreen 5753en_US
dc.relation.isatmap250Alcoota SF5310en_US
dc.relation.isatgeolprovinceGeorgina Basinen_US
dc.relation.isatgeolprovinceAileron Provinceen_US
dc.description.stratnameCentral Mount Stuart Formationen_US
dc.description.stratnameArunta Complexen_US
dc.description.mineprospectnameMount Skinneren_US
dc.identifier.tenureEL786en_US
dc.description.modifyhistory21/04/2005en_US
dc.description.modifyhistory12/09/2016en_US
dc.description.modifyhistory25/10/2021en_US
dc.contributor.holderCentaminen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1971en_US
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