Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5782852 | Chemical Geology | 2017 | 39 Pages |
Abstract
Overall, these results suggest that the presence of S of mixed oxidation state (sulfide S2Â â, sulfite S4Â + and sulfate S6Â +) 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 S3â ion does not increase Cu solubility in fluids. Thus, if present in such environments, S3â ion could fractionate Cu from Au in porphyry-epithermal environments.
Keywords
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Authors
M. Louvel, A. Bordage, B. Tripoli, D. Testemale, J.-L. Hazemann, J. Mavrogenes,