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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Bibliographic Details
Main Authors: Panuntun, Hidayat, Miyazaki, Shinichi
Format: Conference or Workshop Item NonPeerReviewed
Language:English
Published: 2015
Subjects:
Online Access:https://repository.ugm.ac.id/276581/1/JPGU%202015%20Hidayat.pdf
https://repository.ugm.ac.id/276581/
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Institution: Universitas Gadjah Mada
Language: English