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dc.contributor.authorMackie, AWen_US
dc.date.accessioned2016-08-09T01:07:20Z-
dc.date.issued2013en_US
dc.identifier.govdocCR2013-0122en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/83189en_US
dc.description.abstractEL 28552 Cattlewater Pass comprising 36 reticular blocks is located between Cadney Fault zone, (north) and Mt Johnstone Fault zone, (south) two south east-trending, mantle-tapping structures traversing across eastern Arunta Inlier. The licence area is dominated by Ongeva granulite of lower Cadney metamorphics assigned to 1810 - 1790Ma Strangways Metamorphic Complex. The Ongeva granulite is overprinted by late stage potassic alteration which may possibly be a pathfinder to significant Cu-Au mineralisation within the licence area. A first year program of regional interpretation including TMI, Radiometrics, Gravity and Landsat datasets was undertaken.en_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationCopperen_US
dc.subject.classificationPrecious metalsen_US
dc.subject.classificationGolden_US
dc.subject.classificationGeophysical interpretationen_US
dc.subject.classificationExploration historyen_US
dc.subject.classificationGeologyen_US
dc.subject.classificationRegional geologyen_US
dc.subject.classificationGeneral geologyen_US
dc.titleEL 28852 Cattlewater Pass Annual technical report 6 February 2012 to 5 February 2013en_US
dc.relation.isatmap100Riddoch 5851en_US
dc.relation.isatmap100Laughlen 5751en_US
dc.relation.isatmap250Alice Springs SF5314en_US
dc.relation.isatgeolprovinceArunta Regionen_US
dc.relation.isatgeolprovinceAileron Provinceen_US
dc.description.stratnameOngeva Granuliteen_US
dc.identifier.tenureEL28852en_US
dc.description.modifyhistory26/04/2013en_US
dc.description.modifyhistory19/09/2017en_US
dc.contributor.holderGemparten_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2013en_US
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Appears in Collections:Minerals Exploration Reports (MEX)

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