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dc.contributor.authorMelville, Pen_US
dc.contributor.authorSawyer, Len_US
dc.contributor.authorRosewall, Den_US
dc.contributor.authorBeckitt, Gen_US
dc.date.accessioned2016-10-09T23:41:41Z-
dc.date.issued2002en_US
dc.identifier.govdocCR2003-0173en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/83489en_US
dc.description.abstractExploration activities during the seventh year of tenure consisted solely of a RAB drilling program, which covered specific areas of the Myra Falls Metamorphics (MFM) stratigraphy. The aim of the program was to follow up prospective results from the previous years' drilling and to investigate pre-existing anomalies as well as adding further geological clarification in the process. A north west striking anomaly some 200 metres long is suggested from the position of the anomalous holes. The range of elements present is indicative of both mafi and nonmafic lithotypes. The NIM6 airborne anomaly originated from the initial regional airborne work carried out by PNC in 1996. During the current year, thirty-four holes were drilled, most of which are located immediately north of the originally drilled airborne anomaly. Chemistry from the NIM6 holes confirms multiple lithologic associations. KRR860 was the most interesting from this grid with anomalous uranium (69ppm), nickel (575ppm) and elevated levels of Al2O3, Co, Au, Fe2O3, Li, Pd and V. Eight other holes (KRR872, 873, 875, 876, 885, 886, 887 and 888) are located in the central and south western portion of the grid and all show varying levels of uranium anomalism. Holes 872, 875, 886 and 888 have elevated U with 882 and 888 at 39 ppm and 35 ppm respectively. Other anomalous elements include As, Co, Cu, Pb, Li, Ni, V and Zn. Given that holes in various locations on the grid contain some degree of uranium anomalism, no definite trend can be firmly established. However, there is a suggestion of a broad northerly strike through the centre of the grid with a branching to both the north and north east on the most northerly line.en_US
dc.subject.classificationUraniumen_US
dc.subject.classificationRegional geologyen_US
dc.subject.classificationExploration historyen_US
dc.subject.classificationExploration costsen_US
dc.subject.classificationDrillingen_US
dc.subject.classificationRAB drillingen_US
dc.subject.classificationDrill cuttings samplingen_US
dc.subject.classificationGeochemical methodsen_US
dc.subject.classificationGeochemical anomaliesen_US
dc.subject.classificationMajor element analysisen_US
dc.subject.classificationTrace analysisen_US
dc.subject.classificationPIMA analysisen_US
dc.subject.classificationGeophysical anomaliesen_US
dc.subject.classificationAssayingen_US
dc.subject.classificationAssay valueen_US
dc.titleKing River Project EL 734 Annual report 2002 Field Seasonen_US
dc.relation.isatmap100Oenpelli 5573en_US
dc.relation.isatmap250Alligator River SD5301en_US
dc.relation.isatgeolprovincePine Creek Orogenen_US
dc.description.stratnameNimbuwah Complex, Myra Falls Metamorphics, Kombolgie Formation, Oenpelli Doleriteen_US
dc.description.geochemicalsamplingRAB drill samplesen_US
dc.description.drilling53 RAB holes for 1,106 men_US
dc.description.mineprospectnameKing Riveren_US
dc.identifier.tenureEL734en_US
dc.description.modifyhistory20/06/2005en_US
dc.description.modifyhistory16/03/2006en_US
dc.description.modifyhistory29/08/2016en_US
dc.description.modifyhistory10/10/2016en_US
dc.description.modifyhistory11/01/2017en_US
dc.contributor.holderCameco Australiaen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2003en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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