Mantle hydration along outer-rise faults inferred from serpentinite permeability
Abstract Recent geophysical surveys indicate that hydration (serpentinization) of oceanic mantle is related to outer-rise faulting prior to subduction. The serpentinization of oceanic mantle influences the generation of intermediate-depth earthquakes and subduction water flux, thereby promoting arc...
Guardado en:
Autores principales: | Kohei Hatakeyama, Ikuo Katayama, Ken-ichi Hirauchi, Katsuyoshi Michibayashi |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2017
|
Materias: | |
Acceso en línea: | https://doaj.org/article/77a211d3415a4a918093fce86bb26889 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle
por: Ryosuke Oyanagi, et al.
Publicado: (2021) -
Frequency dispersion amplifies tsunamis caused by outer-rise normal faults
por: Toshitaka Baba, et al.
Publicado: (2021) -
Outer rise seismicity related to the Maule, Chile 2010 megathrust earthquake and hydration of the incoming oceanic lithosphere
por: Moscoso,Eduardo, et al.
Publicado: (2012) -
Multi-scale magnetic mapping of serpentinite carbonation
por: Masako Tominaga, et al.
Publicado: (2017) -
No significant boron in the hydrated mantle of most subducting slabs
por: Andrew M. McCaig, et al.
Publicado: (2018)