Article ID Journal Published Year Pages File Type
5782852 Chemical Geology 2017 39 Pages PDF
Abstract
Overall, these results suggest that the presence of S of mixed oxidation state (sulfide S2 −, sulfite S4 + and sulfate S6 +) limits transport of Cu in porphyry and epithermal systems and may even trigger Cu precipitation. Furthermore, these experiments provide evidence that the presence of the S3− ion does not increase Cu solubility in fluids. Thus, if present in such environments, S3− ion could fractionate Cu from Au in porphyry-epithermal environments.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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