Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake

The deformation transient following large subduction zone earthquakes is thought to originate from the interaction of viscoelastic flow in the asthenospheric mantle and slip on the megathrust that are both accelerated by the sudden coseismic stress change. Here, we show that combining insight from l...

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Detalles Bibliográficos
Autores principales: Agata, Ryoichiro, Barbot, Sylvain D., Fujita, Kohei, Hyodo, Mamoru, Iinuma, Takeshi, Nakata, Ryoko, Ichimura, Tsuyoshi, Hori, Takane
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6435688/
https://www.ncbi.nlm.nih.gov/pubmed/30914636
http://dx.doi.org/10.1038/s41467-019-08984-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6435688/
https://www.ncbi.nlm.nih.gov/pubmed/30914636
http://dx.doi.org/10.1038/s41467-019-08984-7

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