Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/71893
Export to Endnote
Full metadata record
DC FieldValueLanguage
dc.contributor.authorPietsch, BAen_US
dc.date.accessioned2013-10-23T19:05:09Z-
dc.date.issued1973en_US
dc.identifier.govdocCR1973-0216en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/71893en_US
dc.description.abstractFluorite mineralisation occurring as quartz-fluorite-barite veins, was found as hydrothermal fissure veins within granite. Three fluorite occurrences contain veins large enough for mineral resources calculations. Geochemical and geophysical surveys failed to locate anomalous base metal mineralisation.en_US
dc.subject.classificationFluoriteen_US
dc.subject.classificationCopperen_US
dc.subject.classificationLeaden_US
dc.subject.classificationZincen_US
dc.subject.classificationHeavy mineral samplingen_US
dc.subject.classificationStream sediment samplingen_US
dc.subject.classificationBariteen_US
dc.title1973 Final report on EL 470 Oorabraen_US
dc.relation.isatmap100Jinka 6052en_US
dc.relation.isatmap250Huckitta SF5311en_US
dc.relation.isatgeolprovinceArunta Provinceen_US
dc.description.stratnameDulcie Sandstoneen_US
dc.description.stratnameNora Formationen_US
dc.description.stratnameTomahawk bedsen_US
dc.description.stratnameArrinthrunga Formationen_US
dc.description.stratnameJinka Graniteen_US
dc.description.mineprospectnameOorabra Fluorite Prospecten_US
dc.identifier.tenureEL470en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory08/03/2004en_US
dc.description.modifyhistory08/07/2016en_US
dc.description.modifyhistory13/09/2021en_US
dc.contributor.holderCentral Pacific Mineralsen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1973en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

Files in this Report:
File SizeFormat Add to
Download
CR19730216.pdf2.44 MBPDF Add


Items in GEMIS are protected by copyright unless otherwise indicated.

Get Adobe Reader