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dc.contributor.authorEsser, Den_US
dc.date.accessioned2013-10-28T07:54:47Z-
dc.date.issued2012en_US
dc.identifier.govdocCR2012-0181en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/76831en_US
dc.description.abstractThis annual report describes the work carried out on EL 24694 to 27 February 2012. EL 24694, which is located in the Southern McArthur Basin, on the northern edge of the Murphy Inlier, Northern Territory, is held by Murphy Uranium Pty Ltd; a wholly owned subsidiary of Bondi Mining Ltd. This exploration license was acquired because it is considered to have good potential for hosting unconformity type uranium deposits, similar to those located in the Alligator Rivers Uranium Field at the northern end of the McArthur Basin and sandstone hosted uranium mineralisation, similar to the Westmoreland deposit located to the east in Queensland. Concealed southern extensions of the highly prospective Emu Fault Zone are also interpreted to transect the area. Bondi Mining has been carrying exploration on this tenement since acquiring the licence from Buffalo Gold in 2007. This work has included geological and geophysical interpretations with targeting, alpha track sampling over major faults zones, Ionic leach soil sampling, close spaced RAB drilling over alpha track anomalies and wide spaced RAB drilling targeting phosphate deposits in the Georgina Basin limestone. In 2009 several three RC holes were drilled on anomalous uranium in soils targets. In 2010 part of a GEOTEM survey designed to locate conductive hosts for uranium mineralisation in the Proterozoic basement, was flown over part of the EL. Exploration activity during the 2011 field season included an environmental audit and drill hole rehabilitation. No significant uranium mineralisation was located on EL 24694 during the period of tenure and the geophysical and geochemical techniques used are not considered effective in locating uranium mineralisation under cover in the Proterozoic basement. However, much of this lease, particularly to the south-east appears to be 'floored' by the Nicholson Granite and therefore is not an attractive target. Due to the low prospectivity of the granite and the high cost of exploration under cover the decision was taken to let the EL lapse. There are a number of geological targets defined by Haynes that have not been tested (Esser, 2010).en_US
dc.subject.classificationUranium explorationen_US
dc.subject.classificationCopper explorationen_US
dc.subject.classificationDrillingen_US
dc.subject.classificationGeophysical surveysen_US
dc.titleAnnual final report, EL 24694 Murphy Projecten_US
dc.relation.isatmap100Paradise Bore 6161en_US
dc.relation.isatmap100Coanjula 6262en_US
dc.relation.isatmap100Puzzle 6162en_US
dc.relation.isatmap250Walhallow SE5307en_US
dc.relation.isatmap250Calvert Hills SE5308en_US
dc.relation.isatmap250Brunette Downs SE5311en_US
dc.relation.isatgeolprovinceSouth Nicholson Basinen_US
dc.relation.isatgeolprovinceGeorgina Basinen_US
dc.relation.isatgeolprovinceCarpentaria Basinen_US
dc.description.stratnameNicholson Graniteen_US
dc.identifier.tenureEL24694en_US
dc.description.modifyhistory01/05/2012en_US
dc.description.modifyhistory06/06/2013en_US
dc.contributor.holderMurphy Uraniumen_US
dc.contributor.holderBondi Miningen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2012en_US
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Appears in Collections:Minerals Exploration Reports (MEX)

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