Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties

The authors here perform experiments to investigate the dihedral angle of olivine-H2O and olivine-H2O-NaCl systems. The observed effect of NaCl to decrease dihedral angles allows fluids to percolate through forearc mantle wedge and to accumulate in the overlying crust, accounting for the high electr...

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Auteurs principaux:	Yongsheng Huang, Takayuki Nakatani, Michihiko Nakamura, Catherine McCammon
Format:	article
Langue:	EN
Publié:	Nature Portfolio 2019
Sujets:	Science Q
Accès en ligne:	https://doaj.org/article/b22cc7d2a9ed4b008e02540cbfc80d36
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id	oai:doaj.org-article:b22cc7d2a9ed4b008e02540cbfc80d36
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spelling	oai:doaj.org-article:b22cc7d2a9ed4b008e02540cbfc80d362021-12-02T14:39:57ZSaline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties10.1038/s41467-019-13513-72041-1723https://doaj.org/article/b22cc7d2a9ed4b008e02540cbfc80d362019-12-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-13513-7https://doaj.org/toc/2041-1723The authors here perform experiments to investigate the dihedral angle of olivine-H2O and olivine-H2O-NaCl systems. The observed effect of NaCl to decrease dihedral angles allows fluids to percolate through forearc mantle wedge and to accumulate in the overlying crust, accounting for the high electrical conductivity anomalies in forearc regions.Yongsheng HuangTakayuki NakataniMichihiko NakamuraCatherine McCammonNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-10 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Yongsheng Huang Takayuki Nakatani Michihiko Nakamura Catherine McCammon Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties
description	The authors here perform experiments to investigate the dihedral angle of olivine-H2O and olivine-H2O-NaCl systems. The observed effect of NaCl to decrease dihedral angles allows fluids to percolate through forearc mantle wedge and to accumulate in the overlying crust, accounting for the high electrical conductivity anomalies in forearc regions.
format	article
author	Yongsheng Huang Takayuki Nakatani Michihiko Nakamura Catherine McCammon
author_facet	Yongsheng Huang Takayuki Nakatani Michihiko Nakamura Catherine McCammon
author_sort	Yongsheng Huang
title	Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties
title_short	Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties
title_full	Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties
title_fullStr	Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties
title_full_unstemmed	Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties
title_sort	saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/b22cc7d2a9ed4b008e02540cbfc80d36
work_keys_str_mv	AT yongshenghuang salineaqueousfluidcirculationinmantlewedgeinferredfromolivinewettingproperties AT takayukinakatani salineaqueousfluidcirculationinmantlewedgeinferredfromolivinewettingproperties AT michihikonakamura salineaqueousfluidcirculationinmantlewedgeinferredfromolivinewettingproperties AT catherinemccammon salineaqueousfluidcirculationinmantlewedgeinferredfromolivinewettingproperties
_version_	1718390494577295360

Saline aqueous fluid circulation in mantle wedge inferred from olivine wetting properties

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