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Mechanism of subsidence of the Northeast Japan forearc during the late period of a gigantic earthquake cycle

The forearc in Northeast Japan subsided (3–4 mm/year) in the interseismic ~100 years before the 2011 Tohoku earthquake (M(W)9.1) just like it did during this event. This study attempts to understand the mechanism of the vertical displacement of the forearc during gigantic earthquake cycles via numer...

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Detalles Bibliográficos
Autores principales: Sasajima, Ryohei, Shibazaki, Bunichiro, Iwamori, Hikaru, Nishimura, Takuya, Nakai, Yoshihiko
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6451026/
https://www.ncbi.nlm.nih.gov/pubmed/30952917
http://dx.doi.org/10.1038/s41598-019-42169-y