Breccia mechanics as an explanation for extreme geochemical micro-gradients and fluid mixing in the genesis of iron-oxide-Cu-Au deposits
Oliver, N.H.S., Williams, P.J., Cleverley, J.S., Mark, G., Keys, D.L., and Blenkinsop, T.G. (2008) Breccia mechanics as an explanation for extreme geochemical micro-gradients and fluid mixing in the genesis of iron-oxide-Cu-Au deposits. In: Australian Earth Sciences Convention. p. 192. From: Australian Earth Sciences Convention 2008, 20-24 July 2008, Perth, WA, Australia.
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Abstract
[Extract] Geochemical zonation in the breccia-hosted Ernest Henry iron-oxide-Cu-Au deposit of the Proterozoic Mt Isa Block occurs in an oscillatory fashion at micro-scales and irregular to broadly concentric fashions at broader scales.
Item ID: | 27808 |
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Item Type: | Conference Item (Abstract / Summary) |
ISSN: | 0729-011X |
Date Deposited: | 17 Sep 2013 06:30 |
FoR Codes: | 04 EARTH SCIENCES > 0403 Geology > 040307 Ore Deposit Petrology @ 100% |
SEO Codes: | 84 MINERAL RESOURCES (excl. Energy Resources) > 8401 Mineral Exploration > 840102 Copper Ore Exploration @ 50% 84 MINERAL RESOURCES (excl. Energy Resources) > 8401 Mineral Exploration > 840105 Precious (Noble) Metal Ore Exploration @ 50% |
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