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Geochemical evidence for mélange melting in global arcs
In subduction zones, sediments and hydrothermally altered oceanic crust, which together form part of the subducting slab, contribute to the chemical composition of lavas erupted at the surface to form volcanic arcs. Transport of this material from the slab to the overlying mantle wedge is thought to...
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| Publicado no: | Sci Adv |
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| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
American Association for the Advancement of Science
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5384804/ https://ncbi.nlm.nih.gov/pubmed/28435882 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1602402 |
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