Controlling factor of incoming plate hydration at the north-western Pacific margin
Bend faulting prior to subduction is considered to promote hydration, yet the relationship remains ambiguous. Here, via analysis of seismic surveys from the Japan and Kuril trenches junction, the authors show that pre-subduction bend faulting and post-subduction plate hydration are strongly correlat...
Guardado en:
Autores principales: | Gou Fujie, Shuichi Kodaira, Yuka Kaiho, Yojiro Yamamoto, Tsutomu Takahashi, Seiichi Miura, Tomoaki Yamada |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2018
|
Materias: | |
Acceso en línea: | https://doaj.org/article/9821e0fa564d4cbc889dfc3fab80cbb2 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench
por: Ryuta Arai, et al.
Publicado: (2016) -
Methane hydrates in the Chilean continental margin
por: Morales G.,Esteban
Publicado: (2003) -
THE TIME FACTOR IN THE MODEL OF MARGINAL INCOME
por: A. K. Solodov
Publicado: (2014) -
Gas hydrate versus seabed morphology offshore Lebu (Chilean margin)
por: Iván Vargas-Cordero, et al.
Publicado: (2020) -
Detection of hydroacoustic signals on a fiber-optic submarine cable
por: Hiroyuki Matsumoto, et al.
Publicado: (2021)