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Water transport to the core–mantle boundary
Water is transported to Earth's interior in lithospheric slabs at subduction zones. Shallow dehydration fuels hydrous island arc magmatism but some water is transported deeper in cool slab mantle. Further dehydration at ∼700 km may limit deeper transport but hydrated phases in slab crust have c...
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| Publicado no: | Natl Sci Rev |
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| Autor principal: | |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Oxford University Press
2021
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8288335/ https://ncbi.nlm.nih.gov/pubmed/34691622 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1093/nsr/nwab007 |
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