No significant boron in the hydrated mantle of most subducting slabs

Boron is one of the main proxies for seawater-derived fluids in subduction zone volcanics and it is vital to characterise the location and concentration of boron in the oceanic lithosphere. Here the authors show that boron concentration in the mantle of downgoing slabs has been overestimated, becaus...

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Autores principales:	Andrew M. McCaig, Sofya S. Titarenko, Ivan P. Savov, Robert A. Cliff, David Banks, Adrian Boyce, Samuele Agostini
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/834b489c48254261ba5d88fa80916efd
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spelling	oai:doaj.org-article:834b489c48254261ba5d88fa80916efd2021-12-02T16:49:31ZNo significant boron in the hydrated mantle of most subducting slabs10.1038/s41467-018-07064-62041-1723https://doaj.org/article/834b489c48254261ba5d88fa80916efd2018-11-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-07064-6https://doaj.org/toc/2041-1723Boron is one of the main proxies for seawater-derived fluids in subduction zone volcanics and it is vital to characterise the location and concentration of boron in the oceanic lithosphere. Here the authors show that boron concentration in the mantle of downgoing slabs has been overestimated, because boron is strongly decoupled from water in the hydration process.Andrew M. McCaigSofya S. TitarenkoIvan P. SavovRobert A. CliffDavid BanksAdrian BoyceSamuele AgostiniNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-10 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Andrew M. McCaig Sofya S. Titarenko Ivan P. Savov Robert A. Cliff David Banks Adrian Boyce Samuele Agostini No significant boron in the hydrated mantle of most subducting slabs
description	Boron is one of the main proxies for seawater-derived fluids in subduction zone volcanics and it is vital to characterise the location and concentration of boron in the oceanic lithosphere. Here the authors show that boron concentration in the mantle of downgoing slabs has been overestimated, because boron is strongly decoupled from water in the hydration process.
format	article
author	Andrew M. McCaig Sofya S. Titarenko Ivan P. Savov Robert A. Cliff David Banks Adrian Boyce Samuele Agostini
author_facet	Andrew M. McCaig Sofya S. Titarenko Ivan P. Savov Robert A. Cliff David Banks Adrian Boyce Samuele Agostini
author_sort	Andrew M. McCaig
title	No significant boron in the hydrated mantle of most subducting slabs
title_short	No significant boron in the hydrated mantle of most subducting slabs
title_full	No significant boron in the hydrated mantle of most subducting slabs
title_fullStr	No significant boron in the hydrated mantle of most subducting slabs
title_full_unstemmed	No significant boron in the hydrated mantle of most subducting slabs
title_sort	no significant boron in the hydrated mantle of most subducting slabs
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/834b489c48254261ba5d88fa80916efd
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No significant boron in the hydrated mantle of most subducting slabs

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