| 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 S2 â, 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 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
												
											Related Topics
												
													Physical Sciences and Engineering
													Earth and Planetary Sciences
													Geochemistry and Petrology
												
											Authors
												M. Louvel, A. Bordage, B. Tripoli, D. Testemale, J.-L. Hazemann, J. Mavrogenes, 
											