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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/87327
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dc.contributor.authorPolito, PAen_US
dc.contributor.authorKyser, KTen_US
dc.contributor.authorJackson, Jen_US
dc.date.accessioned2018-07-05T01:15:29Z-
dc.date.issued2006en_US
dc.identifier.govdocCSR0208en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/87327en_US
dc.description.abstractThe results presented in this study show that clastic sediments dominated by poorly sorted sandstone and conglomerate facies evolved through burial diagenesis to become aquifer lithologic units that hosted basinal brines with chemical characteristics and ages similar to those that are reported from the Pb-Zn and U deposits of the southern McArthur basin.en_US
dc.subject.classificationZincen_US
dc.subject.classificationLeaden_US
dc.subject.classificationUraniumen_US
dc.titleThe Role of sandstone diagenesis and aquifer evolution in the formation of uranium and zinc-lead deposits, southern McArthur Basin, Northern Territory, Australiaen_US
dc.typeCore Analysisen_US
dc.relation.isatgeolprovinceMcArthur Basinen_US
dc.description.publicnotesArticle published in: Economic Geology, v. 101, pp. 1189-1209 [2006], Society of Economic Geologists, Inc.en_US
dc.description.modifyhistory22/03/2017en_US
dc.description.modifyhistory04/08/2017en_US
dc.description.modifyhistory02/07/2018en_US
dc.description.modifyhistory05/07/2018en_US
dc.description.modifyhistory22/07/2019en_US
dc.contributor.corpauthorDepartment of Geological Sciences and Geological Engineering, Queen's University, Ontario, Canadaen_US
dc.identifier.drillholenameMcA14en_US
dc.identifier.drillholename82/4en_US
dc.identifier.drillholenameWE1en_US
dc.identifier.drillholenameDD95GC001en_US
dc.identifier.drillholenameDD95GC007en_US
dc.identifier.drillholenameDD91DC1en_US
dc.identifier.collectionnameCore Sampling Reports
dc.identifier.coredatid29en_US
dc.identifier.coredatid87en_US
dc.identifier.coredatid262en_US
dc.identifier.coredatid302en_US
dc.identifier.coredatid303en_US
dc.identifier.coredatid317en_US
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Appears in Collections:Core Sampling Reports

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