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Separation of supercritical slab-fluids to form aqueous fluid and melt components in subduction zone magmatism
Subduction-zone magmatism is triggered by the addition of H(2)O-rich slab-derived components: aqueous fluid, hydrous partial melts, or supercritical fluids from the subducting slab. Geochemical analyses of island arc basalts suggest two slab-derived signatures of a melt and a fluid. These two liquid...
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| Main Authors: | , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2012
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3503209/ https://ncbi.nlm.nih.gov/pubmed/23112158 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1207687109 |
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