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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| Main Authors: | , |
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| 格式: | Conference or Workshop Item NonPeerReviewed |
| 語言: | English |
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2015
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| 在線閱讀: | https://repository.ugm.ac.id/276581/1/JPGU%202015%20Hidayat.pdf https://repository.ugm.ac.id/276581/ |
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