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dc.contributor.authorGole, Men_US
dc.date.accessioned2013-10-23T20:59:21Z-
dc.date.issued2005en_US
dc.identifier.govdocCR2005-0630en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/73554en_US
dc.description.abstractThe Wave Hill tenement, E22812, formed part of AusQuest Limited's broader WANT Antrim Project which involved exploration for Noril'sk-style Ni-Cu-PGE sulphide deposits. Geochemical evidence from whole rock analyses of Antrim basalts show that they are markedly depleted in Ni, Cu, and PGE throughout the province and throughout the stratigraphic section. Analytical data also show that the basalts are strongly contaminated by crustal material. Basalts associated with the giant Noril'sk Ni-Cu-PGE sulphide deposits also show these geochemical features which are intimately tied to the magmatic ore forming processes. As at Noril'sk, the Antrim basalts were extruded through flat lying epicontinental sedimentary sequences that include some sulphur-bearing mudrocks and other highly reactive sedimentary lithologies. Contamination of the magma by these rocks may have been the trigger for sulphur saturation and sulphide formation within the basaltic melt. As at Noril'sk such sulphides may be concentrated in trap sites within the magma plumbing system within the sedimentary successions immediately below the Antrim basalt sequence. Interpretation of available geological and geophysical data over the Antrim Province identified a NNW trending gravity/structural corridor to the west of the Wave Hill tenement as a potential feeder zone as well as ENE trending structures such as the Neave Fault as potential fissure eruption sites. Deeper magnetic anomalies located close to these structures potentially reflect intrusions near the base of the basalts related to the outpouring of the Antrim basalts. The Wave Hill tenement (EL 22812) covers one such target along the Neave Fault that is modelled on the basis of magnetic data as a sill-like mafic intrusive at depth of ~500m. Sixteen line km of in-loop transient electromagnetic surveying on 4 traverses were completed over the interpreted sill. No sub-surface conductors were identified and the decision was made to surrender the tenement.en_US
dc.subject.classificationNickelen_US
dc.subject.classificationCobalten_US
dc.subject.classificationPrecious metal depositsen_US
dc.subject.classificationGeophysical surveysen_US
dc.subject.classificationGeophysical dataen_US
dc.subject.classificationGeophysical interpretationen_US
dc.subject.classificationTransient EM surveysen_US
dc.subject.classificationModelsen_US
dc.subject.classificationGeochemical explorationen_US
dc.subject.classificationGeochemical samplingen_US
dc.subject.classificationGeologyen_US
dc.subject.classificationRegional geologyen_US
dc.subject.classificationGeneral geologyen_US
dc.subject.classificationExploration historyen_US
dc.titleWave Hill EL 22812 Final Feport for the period October 2001 to September 2005en_US
dc.relation.isatmap100Watson 5062en_US
dc.relation.isatmap250Wave Hill SE5208en_US
dc.relation.isatgeolprovinceVictoria-Birrindudu Basinen_US
dc.description.stratnameAnuma Schisten_US
dc.description.stratnameWattie Groupen_US
dc.description.stratnameBullita Groupen_US
dc.description.geochemicalsampling4 Geochemical samplesen_US
dc.identifier.tenureEL22812en_US
dc.description.modifyhistory07/02/2014en_US
dc.description.modifyhistory18/08/2020en_US
dc.contributor.holderAusquesten_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2005en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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