Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/75840
Export to Endnote
Full metadata record
DC FieldValueLanguage
dc.contributor.authorFabray, Jen_US
dc.date.accessioned2013-10-28T04:32:14Z-
dc.date.issued2010en_US
dc.identifier.govdocCR2010-0385en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/75840en_US
dc.description.abstractWestern Desert Resources Ltd (WDR) acquired this exploration licence from Tennant Creek Gold Pty Ltd in July 2007. The EL was granted on 20th July 2001 to Imperial Granite and Minerals Pty Ltd who sold it to Tennant Creek Gold Pty Ltd in January 2004. The tenement is located about 100km east-north-east of Alice Springs in the southern part of the Northern Territory. The EL is situated on pastoral leasehold land subject to a land claim under the Aboriginal Land Rights (NT) Act. The project area is located within the White Range Nappe at the eastern end of the Arltunga Nappe Complex. The Arltunga Nappe Complex, formed during the Early Carboniferous Alice Springs Orogeny (300-400Ma), and includes rocks of the Arunta Block and Amadeus Basin. Exploration activities during the early part of the tenements history was directed at the silver-copper-lead mineralisation at the Blueys prospect. These activities did not lead to an economic discovery. WDR flew two airborne surveys in 2007-2008. The airborne magnetic-radiometric survey outlined two significant thorium anomalies. The airborne SkyTEM survey delineated a number of anomalous ground conductors. Two diamond drillholes were completed in June 2008 to test two conductive zones from the airborne EM survey. Both holes intersected a similar pyritic, carbonaceous shale interval within the Bitter Springs Formation overlying the Heavitree Quartzite. These zones explained the EM conductors. The shale intervals were assayed for base metals with no anomalous results. Two significant thorium anomalies were outlined by the airborne radiometric survey. Rock chip sampling of granite gneiss, which outcrops in the area, showed that the anomalies are associated with sub-economic thorium and rare earth mineralisation.en_US
dc.subject.classificationBase metalsen_US
dc.subject.classificationUraniumen_US
dc.subject.classificationThoriumen_US
dc.titleFinal report on EL 10228 for the period 20 July 2001 to 29 April 2010, Blueys Projecten_US
dc.relation.isatmap100Riddoch 5851en_US
dc.relation.isatmap100Fergusson Range 5850en_US
dc.relation.isatmap250Alice Springs SF5314en_US
dc.relation.isatgeolprovinceAileron Provinceen_US
dc.relation.isatgeolprovinceAmadeus Basinen_US
dc.description.mineprospectnameBlueysen_US
dc.identifier.tenureEL10228en_US
dc.description.modifyhistory21/07/2010en_US
dc.description.modifyhistory04/08/2010en_US
dc.description.modifyhistory07/06/2013en_US
dc.description.modifyhistory07/03/2014en_US
dc.description.modifyhistory18/03/2014en_US
dc.contributor.holderWestern Desert Resourcesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR2010en_US
local.flag.notified1
Appears in Collections:Minerals Exploration Reports (MEX)

Files in this Report:
File SizeFormat Add to
Download
EL10228_2009_A.pdf1.19 MBPDF Add
CR2010-0385_Appendices.zip1.09 MBUnknown Add


Items in GEMIS are protected by copyright unless otherwise indicated.

Get Adobe Reader