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dc.contributor.authorKettlewell, DCen_US
dc.date.accessioned2013-10-23T18:56:59Z-
dc.date.issued1993en_US
dc.identifier.govdocCR1993-0150en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/71765en_US
dc.description.abstract352 samples were collected in a helicopter supported lag survey. Numerous weak anomalies were outlined. The majority of anomalies from sediments of the Barney Creek Formation occurred near fault traces. Interpretation Sirotem readings from 1991 indicate that the Barney Creek Formation is present beneath a thin cover of Bukalara Sandstone. During 1992 three areas of interest-the Splinter Fault, loop 72 anomaly and loop 73 anomaly were followed by Sirotem soundings. Interpretation suggests that in the area of the Splinter Fault there exists an uplifted block of Barney Creek Formation.en_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationLag samplingen_US
dc.subject.classificationEM surveysen_US
dc.subject.classificationSirotem surveysen_US
dc.titleSecond Annual Report EL 7218 Lancewood year ending 10 Janaury 1993.en_US
dc.relation.isatmap100Lancewood 6163en_US
dc.relation.isatmap250Walhallow SE5307en_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.relation.isatgeolprovinceBatten Troughen_US
dc.description.stratnameMcArthur Groupen_US
dc.description.stratnameBarney Creek Formationen_US
dc.description.stratnameBukalara Sandstoneen_US
dc.description.geochemicalsampling352 lag samplesen_US
dc.description.mineprospectnameM12 Anomalyen_US
dc.description.mineprospectnameGR2 Anomalyen_US
dc.identifier.tenureEL7218en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory23/02/2005en_US
dc.description.modifyhistory01/03/2005en_US
dc.description.modifyhistory24/10/2006en_US
dc.description.modifyhistory18/08/2014en_US
dc.contributor.holderMount Isa Minesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1993en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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