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DC Field | Value | Language |
---|---|---|
dc.contributor.author | Carter, A | en_US |
dc.date.accessioned | 2013-10-23T21:30:30Z | - |
dc.date.issued | 2005 | en_US |
dc.identifier.govdoc | CR2005-0712 | en_US |
dc.identifier.uri | https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/73914 | en_US |
dc.description.abstract | These ELs are held to drill test the gold potential of the Amadeus Basin. The exploration model is based on an analogy with the Witwatersrand Basin in South Africa. The presence of deep-seated shear zones and thrust faults, high geothermal gradients, the presence of sulfide-bearing quartz veins and other sulfides are seen as conducive to the transport and deposition of hydrothermal gold. Particular interest is focused on the unconformity at the top of the Bitter Springs Formation. | en_US |
dc.subject.classification | Gold exploration | en_US |
dc.subject.classification | Work programmes | en_US |
dc.title | Annual report for EL 24282 and EL 24283 | en_US |
dc.relation.isatmap100 | Fergusson Range 5850 | en_US |
dc.relation.isatmap100 | Pellinore 5849 | en_US |
dc.relation.isatmap100 | Undoolya 5750 | en_US |
dc.relation.isatmap250 | Alice Springs SF5314 | en_US |
dc.relation.isatmap250 | Rodinga SG5302 | en_US |
dc.relation.isatgeolprovince | Amadeus Basin | en_US |
dc.description.stratname | Bitter Springs Formation | en_US |
dc.identifier.tenure | EL24282 | en_US |
dc.identifier.tenure | EL24283 | en_US |
dc.description.modifyhistory | 16/03/2007 | en_US |
dc.description.modifyhistory | 20/07/2010 | en_US |
dc.description.modifyhistory | 07/06/2013 | en_US |
dc.contributor.holder | Raxile | en_US |
dc.identifier.collectionname | Minerals Exploration Reports (MEX) | en_US |
dc.identifier.govdocprefix | CR2005 | en_US |
local.flag.notified | 1 | |
Appears in Collections: | Minerals Exploration Reports (MEX) |
Files in this Report:
File | Size | Format | Add to Download |
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CR20050712_2005_GA.pdf | 470.22 kB | Add |
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