Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/60044
Export to Endnote
Full metadata record
DC FieldValueLanguage
dc.contributor.authorJohnston, Len_US
dc.date.accessioned2013-10-23T04:05:04Z-
dc.date.issued1994en_US
dc.identifier.govdocCR1994-0273en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/60044en_US
dc.description.abstract60 BLEG silt samples were collected along the length of a poorly defined channel as follow up to anomalous values returned Year 1. This sampling failed to verify the original anomaly. 7 RAB holes totalling 177m were completed in the north of the licence to determine the thickness of outcropping Pedestal Beds. In the east of the drill section the Pedestal Beds are interpreted to be thicker than 39m. In the west drill holes encountered biotite granite and gneiss. The drill results and geochemistry results have downgraded the prospectivity of the EL.en_US
dc.subject.classificationGolden_US
dc.subject.classificationBLEG samplingen_US
dc.subject.classificationRAB drillingen_US
dc.titleEL 6449, Cornish Downs, Tanami Region, NT second and final reporten_US
dc.relation.isatmap100McFarlane 4757en_US
dc.relation.isatmap250The Granites SF5203en_US
dc.relation.isatgeolprovinceTanami Regionen_US
dc.description.stratnamePedestal bedsen_US
dc.description.stratnameTanami Complexen_US
dc.description.geochemicalsampling60 BLEG silt samplesen_US
dc.description.drilling7 RAB holes totalling 177men_US
dc.identifier.tenureEL6449en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory16/02/2005en_US
dc.description.modifyhistory18/04/2005en_US
dc.description.modifyhistory11/06/2014en_US
dc.contributor.holderZapopanen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1994en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

Files in this Report:
File SizeFormat Add to
Download
CR19940273.pdf1.04 MBPDF Add


Items in GEMIS are protected by copyright unless otherwise indicated.

Get Adobe Reader