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dc.contributor.authorSawyer, Len_US
dc.date.accessioned2015-10-30T01:16:37Z-
dc.date.issued2013en_US
dc.identifier.govdocCR2013-0484en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/80744en_US
dc.description.abstractRock chip sampling carried out on EL 25931 in 2012-2013 indicated that low level anomalous zinc an lead within the fault breccia at the base of the Limmen Sandstone bluff is repeatable. The fault breccia is a wedge of sheared laminated limestone or stromatolite of the Dook Creek Formation between overlying Limmen Sandstone and the intruding Derim Derim Dolerite. The extent of the anomalism is limitied. In addition the occurrence lies beneathe or near to a communications tower and on the edge of the tenement with a zone which was excluded from the tenement. These factors severely down grade the tenement for lead - zinc or gold mineralisation.en_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationLeaden_US
dc.subject.classificationZincen_US
dc.subject.classificationGeochemical explorationen_US
dc.subject.classificationGeochemical samplingen_US
dc.subject.classificationRock chip samplingen_US
dc.subject.classificationAssayingen_US
dc.subject.classificationAssay valueen_US
dc.titleAnnual report 2013 year ending 3 June 2013 EL 25931 Bulman Projecten_US
dc.relation.isatmap100Marumba 5770en_US
dc.relation.isatmap250Mount Marumba SD5306en_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.description.stratnameMount Rigg Group, Derim Derim Dolerite Suite, Bone Creek Sandstone, Dook Creek Formationen_US
dc.description.geochemicalsampling7 Rock chip samplesen_US
dc.identifier.tenureEL25931en_US
dc.description.modifyhistory19/08/2013en_US
dc.description.modifyhistory23/09/2013en_US
dc.description.modifyhistory19/09/2017en_US
dc.contributor.holderBulman Resourcesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2013en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

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