Formation of large low shear velocity provinces through the decomposition of oxidized mantle

Dense Fe3+-rich bridgmanite can explain the seismic features of Large Low Shear Velocity Provinces, as it can form large-scale thermochemical piles in the deep mantle that remain stable throughout Earth’s history.

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Autores principales:	Wenzhong Wang, Jiachao Liu, Feng Zhu, Mingming Li, Susannah M. Dorfman, Jie Li, Zhongqing Wu
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/6cdcd89a8faf48eb92592205180f8a9b
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spelling	oai:doaj.org-article:6cdcd89a8faf48eb92592205180f8a9b2021-12-02T17:04:01ZFormation of large low shear velocity provinces through the decomposition of oxidized mantle10.1038/s41467-021-22185-12041-1723https://doaj.org/article/6cdcd89a8faf48eb92592205180f8a9b2021-03-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-22185-1https://doaj.org/toc/2041-1723Dense Fe3+-rich bridgmanite can explain the seismic features of Large Low Shear Velocity Provinces, as it can form large-scale thermochemical piles in the deep mantle that remain stable throughout Earth’s history.Wenzhong WangJiachao LiuFeng ZhuMingming LiSusannah M. DorfmanJie LiZhongqing WuNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-10 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Wenzhong Wang Jiachao Liu Feng Zhu Mingming Li Susannah M. Dorfman Jie Li Zhongqing Wu Formation of large low shear velocity provinces through the decomposition of oxidized mantle
description	Dense Fe3+-rich bridgmanite can explain the seismic features of Large Low Shear Velocity Provinces, as it can form large-scale thermochemical piles in the deep mantle that remain stable throughout Earth’s history.
format	article
author	Wenzhong Wang Jiachao Liu Feng Zhu Mingming Li Susannah M. Dorfman Jie Li Zhongqing Wu
author_facet	Wenzhong Wang Jiachao Liu Feng Zhu Mingming Li Susannah M. Dorfman Jie Li Zhongqing Wu
author_sort	Wenzhong Wang
title	Formation of large low shear velocity provinces through the decomposition of oxidized mantle
title_short	Formation of large low shear velocity provinces through the decomposition of oxidized mantle
title_full	Formation of large low shear velocity provinces through the decomposition of oxidized mantle
title_fullStr	Formation of large low shear velocity provinces through the decomposition of oxidized mantle
title_full_unstemmed	Formation of large low shear velocity provinces through the decomposition of oxidized mantle
title_sort	formation of large low shear velocity provinces through the decomposition of oxidized mantle
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/6cdcd89a8faf48eb92592205180f8a9b
work_keys_str_mv	AT wenzhongwang formationoflargelowshearvelocityprovincesthroughthedecompositionofoxidizedmantle AT jiachaoliu formationoflargelowshearvelocityprovincesthroughthedecompositionofoxidizedmantle AT fengzhu formationoflargelowshearvelocityprovincesthroughthedecompositionofoxidizedmantle AT mingmingli formationoflargelowshearvelocityprovincesthroughthedecompositionofoxidizedmantle AT susannahmdorfman formationoflargelowshearvelocityprovincesthroughthedecompositionofoxidizedmantle AT jieli formationoflargelowshearvelocityprovincesthroughthedecompositionofoxidizedmantle AT zhongqingwu formationoflargelowshearvelocityprovincesthroughthedecompositionofoxidizedmantle
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Formation of large low shear velocity provinces through the decomposition of oxidized mantle

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