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Abstract Diopside-rich, skarn-hosted, coppergold ore derived primarily from carbonaceous metapelites at Mount Elliott forms a distinctive member of the spectrum of CuAu(Fe oxide) deposit styles in the Cloncurry district of the Paleoproterozoic to Mesoproterozoic Mount Isa Block. The mine sequence is a package of carbonaceous metapelites and metagreywackes containing amphibolites derived from tholeiitic...
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