Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas

Subduction zone magmas are more oxidised on eruption than those at mid-ocean ridges. This is attributed either to oxidising components, derived from subducted lithosphere (slab) and added to the mantle wedge, or to oxidation processes occurring during magma ascent via differentiation. Here we provid...

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Detalles Bibliográficos
Autores principales: Bénard, Antoine, Klimm, Kevin, Woodland, Alan B., Arculus, Richard J., Wilke, Max, Botcharnikov, Roman E., Shimizu, Nobumichi, Nebel, Oliver, Rivard, Camille, Ionov, Dmitri A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6115406/
https://www.ncbi.nlm.nih.gov/pubmed/30158630
http://dx.doi.org/10.1038/s41467-018-05804-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6115406/
https://www.ncbi.nlm.nih.gov/pubmed/30158630
http://dx.doi.org/10.1038/s41467-018-05804-2

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