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Subducting serpentinites release reduced, not oxidized, aqueous fluids
The observation that primitive arc magmas are more oxidized than mid-ocean-ridge basalts has led to the paradigm that slab-derived fluids carry SO(2) and CO(2) that metasomatize and oxidize the sub-arc mantle wedge. We combine petrography and thermodynamic modelling to quantify the oxygen fugacity (...
Guardat en:
| Publicat a: | Sci Rep |
|---|---|
| Autors principals: | , , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2019
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6925189/ https://ncbi.nlm.nih.gov/pubmed/31862932 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-55944-8 |
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