Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga

Most known porphyry Cu deposits formed in the Phanerozoic and are exclusively associated with moderately oxidized, sulfur-rich, hydrous arc-related magmas derived from partial melting of the asthenospheric mantle metasomatized by slab-derived fluids. Yet, whether similar metallogenic processes also...

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Detalles Bibliográficos
Autores principales: Meng, Xuyang, Kleinsasser, Jackie M., Richards, Jeremy P., Tapster, Simon R., Jugo, Pedro J., Simon, Adam C., Kontak, Daniel J., Robb, Laurence, Bybee, Grant M., Marsh, Jeffrey H., Stern, Richard A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8044198/
https://www.ncbi.nlm.nih.gov/pubmed/33850122
http://dx.doi.org/10.1038/s41467-021-22349-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8044198/
https://www.ncbi.nlm.nih.gov/pubmed/33850122
http://dx.doi.org/10.1038/s41467-021-22349-z

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