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...
Guardado en:
Autores principales: | Yongsheng Huang, Takayuki Nakatani, Michihiko Nakamura, Catherine McCammon |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2019
|
Materias: | |
Acceso en línea: | https://doaj.org/article/b22cc7d2a9ed4b008e02540cbfc80d36 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Rupture of wet mantle wedge by self-promoting carbonation
por: Atsushi Okamoto, et al.
Publicado: (2021) -
Olivine-rich achondrites from Vesta and the missing mantle problem
por: Zoltan Vaci, et al.
Publicado: (2021) -
Dislocation interactions in olivine control postseismic creep of the upper mantle
por: David Wallis, et al.
Publicado: (2021) -
Fossilized Melts in Mantle Wedge Peridotites
por: Kosuke Naemura, et al.
Publicado: (2018) -
Influence of Saline Fluids on the Electrical Conductivity of Olivine Aggregates at High Temperature and High Pressure and Its Geological Implications
por: Wenqing Sun, et al.
Publicado: (2021)