Three-dimensional variations of the slab geometry correlate with earthquake distributions at the Cascadia subduction system
Variations in seismicity are observed at subduction zones, but the oceanic sides remain poorly resolved. Here, the author presents tomographic results of the Cascadia subduction system demonstrating that there are significant variations of the oceanic lithosphere along the subduction zone.
Guardado en:
Autor principal: | Haiying Gao |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2018
|
Materias: | |
Acceso en línea: | https://doaj.org/article/fd0358b3ab214c9f8a26716966d8f9d1 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Cascadia low frequency earthquakes at the base of an overpressured subduction shear zone
por: Andrew J. Calvert, et al.
Publicado: (2020) -
An evacuation building project for Cascadia earthquakes and tsunamis
por: Raskin,Jay, et al.
Publicado: (2011) -
Dehydration-induced earthquakes identified in a subducted oceanic slab beneath Vrancea, Romania
por: Thomas P. Ferrand, et al.
Publicado: (2021) -
No significant boron in the hydrated mantle of most subducting slabs
por: Andrew M. McCaig, et al.
Publicado: (2018) -
Fault zone heterogeneities explain depth-dependent pattern and evolution of slow earthquakes in Cascadia
por: Yingdi Luo, et al.
Publicado: (2021)