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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Pubblicato in:Nat Commun
Autori principali: Bénard, Antoine, Klimm, Kevin, Woodland, Alan B., Arculus, Richard J., Wilke, Max, Botcharnikov, Roman E., Shimizu, Nobumichi, Nebel, Oliver, Rivard, Camille, Ionov, Dmitri A.
Natura: Artigo
Lingua:Inglês
Pubblicazione: Nature Publishing Group UK 2018
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Article
Accesso online: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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