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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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Detalhes bibliográficos
Publicado no:Nat Commun
Main Authors: 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: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2018
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Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC6115406/
https://ncbi.nlm.nih.gov/pubmed/30158630
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-05804-2
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