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

The oxidised nature of arc magmas is either attributed to recycling from the slab or magma differentiation. Here, the authors show that oxidised iron and sulfur, respectively in sub-arc mantle spinel and glass inclusions with elevated U/Th, Pb/Ce, Sr/Nd and δ34S, trace dehydration products of slab s...

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Autores principales:	Antoine Bénard, Kevin Klimm, Alan B. Woodland, Richard J. Arculus, Max Wilke, Roman E. Botcharnikov, Nobumichi Shimizu, Oliver Nebel, Camille Rivard, Dmitri A. Ionov
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/e25643cda77542dfb96a5b05450493ca
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spelling	oai:doaj.org-article:e25643cda77542dfb96a5b05450493ca2021-12-02T16:56:55ZOxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas10.1038/s41467-018-05804-22041-1723https://doaj.org/article/e25643cda77542dfb96a5b05450493ca2018-08-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-05804-2https://doaj.org/toc/2041-1723The oxidised nature of arc magmas is either attributed to recycling from the slab or magma differentiation. Here, the authors show that oxidised iron and sulfur, respectively in sub-arc mantle spinel and glass inclusions with elevated U/Th, Pb/Ce, Sr/Nd and δ34S, trace dehydration products of slab serpentinites.Antoine BénardKevin KlimmAlan B. WoodlandRichard J. ArculusMax WilkeRoman E. BotcharnikovNobumichi ShimizuOliver NebelCamille RivardDmitri A. IonovNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-10 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Antoine Bénard Kevin Klimm Alan B. Woodland Richard J. Arculus Max Wilke Roman E. Botcharnikov Nobumichi Shimizu Oliver Nebel Camille Rivard Dmitri A. Ionov Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas
description	The oxidised nature of arc magmas is either attributed to recycling from the slab or magma differentiation. Here, the authors show that oxidised iron and sulfur, respectively in sub-arc mantle spinel and glass inclusions with elevated U/Th, Pb/Ce, Sr/Nd and δ34S, trace dehydration products of slab serpentinites.
format	article
author	Antoine Bénard Kevin Klimm Alan B. Woodland Richard J. Arculus Max Wilke Roman E. Botcharnikov Nobumichi Shimizu Oliver Nebel Camille Rivard Dmitri A. Ionov
author_facet	Antoine Bénard Kevin Klimm Alan B. Woodland Richard J. Arculus Max Wilke Roman E. Botcharnikov Nobumichi Shimizu Oliver Nebel Camille Rivard Dmitri A. Ionov
author_sort	Antoine Bénard
title	Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas
title_short	Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas
title_full	Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas
title_fullStr	Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas
title_full_unstemmed	Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas
title_sort	oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/e25643cda77542dfb96a5b05450493ca
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Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas

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