Cargando...
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...
Guardado en:
| Publicado en: | Nat Commun |
|---|---|
| Autores principales: | , , , , , , , , , , |
| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
Nature Publishing Group UK
2021
|
| Materias: | |
| Acceso en línea: | 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 |
| Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|