The formation of porphyry copper deposits
Abstract
Copper is a moderately incompatible chalcophile element. Its behavior is strongly controlled by sulfides. The speciation of sulfur is controlled by oxygen fugacity. Therefore, porphyry Cu deposits are usually oxidized (with oxygen fugacities > ΔFMQ +2) (Mungall 2002; Sun et al. 2015). The problem is that while most of the magmas at convergent margins are highly oxidized, porphyry Cu deposits are very rare, suggesting that high oxygen fugacity...
Paper Details
Title
The formation of porphyry copper deposits
Published Date
Nov 5, 2016
Journal
Volume
36
Issue
1
Pages
9 - 15
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