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 (...

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Detalles Bibliográficos
Autores principales: Piccoli, F., Hermann, J., Pettke, T., Connolly, J. A. D., Kempf, E. D., Vieira Duarte, J. F.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6925189/
https://www.ncbi.nlm.nih.gov/pubmed/31862932
http://dx.doi.org/10.1038/s41598-019-55944-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6925189/
https://www.ncbi.nlm.nih.gov/pubmed/31862932
http://dx.doi.org/10.1038/s41598-019-55944-8

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