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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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| Vydáno v: | Nat Commun |
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| Hlavní autoři: | , , , , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2021
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8044198/ https://ncbi.nlm.nih.gov/pubmed/33850122 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-021-22349-z |
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