Iron diapirs entrain silicates to the core and initiate thermochemical plumes

During planetary formation segregation of an iron core from rocky silicates takes place. Here, the authors use analogue fluid experiments show that iron diapirs entrain volatiles and silicates to the Earth’s core and initiate buoyant thermochemical plumes to reoxidize and hydrate the upper mantle an...

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Autores principales:	J. R. Fleck, C. L. Rains, D. S. Weeraratne, C. T. Nguyen, D. M. Brand, S. M. Klein, J. M. McGehee, J. M. Rincon, C. Martinez, P. L. Olson
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/89cf21a977f8406abb9f65f0373fa600
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spelling	oai:doaj.org-article:89cf21a977f8406abb9f65f0373fa6002021-12-02T17:31:12ZIron diapirs entrain silicates to the core and initiate thermochemical plumes10.1038/s41467-017-02503-22041-1723https://doaj.org/article/89cf21a977f8406abb9f65f0373fa6002018-01-01T00:00:00Zhttps://doi.org/10.1038/s41467-017-02503-2https://doaj.org/toc/2041-1723During planetary formation segregation of an iron core from rocky silicates takes place. Here, the authors use analogue fluid experiments show that iron diapirs entrain volatiles and silicates to the Earth’s core and initiate buoyant thermochemical plumes to reoxidize and hydrate the upper mantle and atmosphere.J. R. FleckC. L. RainsD. S. WeeraratneC. T. NguyenD. M. BrandS. M. KleinJ. M. McGeheeJ. M. RinconC. MartinezP. L. OlsonNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-12 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q J. R. Fleck C. L. Rains D. S. Weeraratne C. T. Nguyen D. M. Brand S. M. Klein J. M. McGehee J. M. Rincon C. Martinez P. L. Olson Iron diapirs entrain silicates to the core and initiate thermochemical plumes
description	During planetary formation segregation of an iron core from rocky silicates takes place. Here, the authors use analogue fluid experiments show that iron diapirs entrain volatiles and silicates to the Earth’s core and initiate buoyant thermochemical plumes to reoxidize and hydrate the upper mantle and atmosphere.
format	article
author	J. R. Fleck C. L. Rains D. S. Weeraratne C. T. Nguyen D. M. Brand S. M. Klein J. M. McGehee J. M. Rincon C. Martinez P. L. Olson
author_facet	J. R. Fleck C. L. Rains D. S. Weeraratne C. T. Nguyen D. M. Brand S. M. Klein J. M. McGehee J. M. Rincon C. Martinez P. L. Olson
author_sort	J. R. Fleck
title	Iron diapirs entrain silicates to the core and initiate thermochemical plumes
title_short	Iron diapirs entrain silicates to the core and initiate thermochemical plumes
title_full	Iron diapirs entrain silicates to the core and initiate thermochemical plumes
title_fullStr	Iron diapirs entrain silicates to the core and initiate thermochemical plumes
title_full_unstemmed	Iron diapirs entrain silicates to the core and initiate thermochemical plumes
title_sort	iron diapirs entrain silicates to the core and initiate thermochemical plumes
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/89cf21a977f8406abb9f65f0373fa600
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Iron diapirs entrain silicates to the core and initiate thermochemical plumes

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