Crustal tectonic stress and poroelastic relaxation of the Mw 9.1 tohoku earthquake

The Mw 9.1, Tohoku-oki earthquake has been investigated by many scientists. This earthquake produces changes in the state of strain and stress in the surrounding rupture area. Postseismic deformation following large earthquake including afterslip, viscoelastic relaxation, and pore fluid flow, furt...

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Detalhes bibliográficos
Principais autores: Panuntun, Hidayat, Miyazaki, Shinichi
Formato: Conference or Workshop Item
Idioma:English
Publicado em: 2015
Assuntos:
Acesso em linha:https://repository.ugm.ac.id/276581/1/JPGU%202015%20Hidayat.pdf