Experiments on Cu-isotope fractionation between chlorine-bearing fluid and silicate magma: implications for fluid exsolution and porphyry Cu deposits

Hydrothermal fluid is essential for transporting metals in the crust and mantle. To explore the potential of Cu isotopes as a tracer of hydrothermal-fluid activity, Cu-isotope fractionation factors between Cl-bearing aqueous fluids and silicate magmas (andesite, dacite, rhyolite dacite, rhyolite and...

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Detalles Bibliográficos
Autores principales: Guo, Haihao, Xia, Ying, Bai, Ruixia, Zhang, Xingchao, Huang, Fang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Oxford University Press 2020
Materias:
Earth Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8288860/
https://www.ncbi.nlm.nih.gov/pubmed/34692160
http://dx.doi.org/10.1093/nsr/nwz221

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8288860/
https://www.ncbi.nlm.nih.gov/pubmed/34692160
http://dx.doi.org/10.1093/nsr/nwz221

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