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DC Field | Value | Language |
---|---|---|
dc.contributor.author | Benger, JW | en_US |
dc.date.accessioned | 2013-10-24T04:32:35Z | - |
dc.date.issued | 2008 | en_US |
dc.identifier.govdoc | CR2008-0784 | en_US |
dc.identifier.uri | https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/74835 | en_US |
dc.description.abstract | Elevated iron results came from a narrow (max. 1 metre wide) discontinuous vein with no apparent potential. Other assay results were all of a low order. Mafic rock samples contained only normal background results for nickel, copper,etc. One high order magnetic anomaly (sample taken several years previously by the EL holder before the grant of the title) proved to be barren of any elevated mineral content. | en_US |
dc.subject.classification | Iron | en_US |
dc.subject.classification | Base metal exploration | en_US |
dc.subject.classification | Nickel | en_US |
dc.subject.classification | Rock chip sampling | en_US |
dc.title | Second annual and final report for EL 24535 Hamilton Creek year ending 5 October 2008 | en_US |
dc.relation.isatmap100 | Kulgera 5546 | en_US |
dc.relation.isatmap100 | Umbeara 5646 | en_US |
dc.relation.isatmap250 | Finke SG5306 | en_US |
dc.relation.isatmap250 | Kulgera SG5305 | en_US |
dc.relation.isatgeolprovince | Musgrave Block | en_US |
dc.description.geochemicalsampling | 11 Rock chip samples. | en_US |
dc.identifier.tenure | EL24535 | en_US |
dc.description.modifyhistory | 22/12/2008 | en_US |
dc.description.modifyhistory | 07/06/2013 | en_US |
dc.description.modifyhistory | 21/11/2013 | en_US |
dc.contributor.holder | Imperial Granite and Minerals | en_US |
dc.identifier.collectionname | Minerals Exploration Reports (MEX) | en_US |
dc.identifier.govdocprefix | CR2008 | en_US |
local.flag.notified | 1 | |
Appears in Collections: | Minerals Exploration Reports (MEX) |
Files in this Report:
File | Size | Format | Add to Download |
---|---|---|---|
EL24535_2008_AS_01.pdf | 1.24 MB | Add | |
EL24535_2008_AS_02_Rockchip_Samples.xls | 17 kB | Microsoft Excel | Add |
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