Large fault slip peaking at trench in the 2011 Tohoku-oki earthquake
The 2011 Tohoku-oki earthquake slip occurred on the shallowest part of the megathrust, but the nature of the shallow slip has been poorly constrained. Here, the authors model bathymetry differences before and after the earthquake to determine that the slip exceeded 60 m increasing towards the trench...
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| Autores principales: | , , , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2017
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/9e5fc3eeae004c079d4560d6d15ce127 |
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