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Are Tennant Creek Style Ironstone-Related Gold-Copper-Bismuth Deposits Unique? A Review of Available Data and a Comparison with Possible Analogous Deposits
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Citation (Style = APA)
(1994). Are Tennant Creek Style Ironstone-Related Gold-Copper-Bismuth Deposits Unique? A Review of Available Data and a Comparison with Possible Analogous Deposits.
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SpreadSheed (CSV)
(1994). Are Tennant Creek Style Ironstone-Related Gold-Copper-Bismuth Deposits Unique? A Review of Available Data and a Comparison with Possible Analogous Deposits.
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Reference Manager (RIS)
SpreadSheed (CSV)
Organization: The Australasian Institute of Mining and Metallurgy
Pages: 0
Publication Date:
Jan 1, 1994
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Abstract
Abstract
| The Proterozoic iron oxide related Au-Cu-Bi ('Tenant Creek style') deposits at Tennant Creek can be classified as syntectonic polymetallic hydrothermal replacement type mineralisation. These deposits have characteristics in common with a number of other Proterozoic iron oxide (Cu-U-Au-REE) hosted deposits in regions which include Southeast Missouri, USA; the Kiruna district, Sweden; the Great Bear Magmatic Zone, Canada; the Stuart Shelf, South Australia; and the Wemecke Mountains, Canada. Similarities between these and Tennant Creek style deposits include: 1. Tectonic Setting: Formed at shallow crustal levels ( |
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