Reconciling metal–silicate partitioning and late accretion in the Earth

Through platinum metal-silicate partitioning coefficient measurements, the authors here show that platinum partitioning into metal is lowered at high pressure–temperature conditions. This finding implies that the Earth’s mantle was likely enriched in platinum immediately following the core-mantle di...

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Autores principales:	Terry-Ann Suer, Julien Siebert, Laurent Remusat, James M. D. Day, Stephan Borensztajn, Beatrice Doisneau, Guillaume Fiquet
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/fa4ad3a3f2db4238878372dcbd80aeb4
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spelling	oai:doaj.org-article:fa4ad3a3f2db4238878372dcbd80aeb42021-12-02T15:52:52ZReconciling metal–silicate partitioning and late accretion in the Earth10.1038/s41467-021-23137-52041-1723https://doaj.org/article/fa4ad3a3f2db4238878372dcbd80aeb42021-05-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-23137-5https://doaj.org/toc/2041-1723Through platinum metal-silicate partitioning coefficient measurements, the authors here show that platinum partitioning into metal is lowered at high pressure–temperature conditions. This finding implies that the Earth’s mantle was likely enriched in platinum immediately following the core-mantle differentiation.Terry-Ann SuerJulien SiebertLaurent RemusatJames M. D. DayStephan BorensztajnBeatrice DoisneauGuillaume FiquetNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-10 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Terry-Ann Suer Julien Siebert Laurent Remusat James M. D. Day Stephan Borensztajn Beatrice Doisneau Guillaume Fiquet Reconciling metal–silicate partitioning and late accretion in the Earth
description	Through platinum metal-silicate partitioning coefficient measurements, the authors here show that platinum partitioning into metal is lowered at high pressure–temperature conditions. This finding implies that the Earth’s mantle was likely enriched in platinum immediately following the core-mantle differentiation.
format	article
author	Terry-Ann Suer Julien Siebert Laurent Remusat James M. D. Day Stephan Borensztajn Beatrice Doisneau Guillaume Fiquet
author_facet	Terry-Ann Suer Julien Siebert Laurent Remusat James M. D. Day Stephan Borensztajn Beatrice Doisneau Guillaume Fiquet
author_sort	Terry-Ann Suer
title	Reconciling metal–silicate partitioning and late accretion in the Earth
title_short	Reconciling metal–silicate partitioning and late accretion in the Earth
title_full	Reconciling metal–silicate partitioning and late accretion in the Earth
title_fullStr	Reconciling metal–silicate partitioning and late accretion in the Earth
title_full_unstemmed	Reconciling metal–silicate partitioning and late accretion in the Earth
title_sort	reconciling metal–silicate partitioning and late accretion in the earth
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/fa4ad3a3f2db4238878372dcbd80aeb4
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Reconciling metal–silicate partitioning and late accretion in the Earth

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