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期刊论文 [7]
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2016 [1]
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postseismi... [2]
subduction... [2]
tohoku-oki... [2]
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earthquake... [7]
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Heterogeneous rheology controlled postseismic deformation of the 2011 Tohoku-Oki earthquake
[期刊论文]
Geophysical Research Letters, 2016-01-01, 43 (10
Muto J.
;
Shibazaki B.
;
Iinuma T.
;
Ito Y.
;
Ohta Y.
;
Miura S.
;
Nakai Y.
View/Download:42/0
Possible shallow slow slip events in Hyuga-nada, Nankai subduction zone, inferred from migration of very low frequency earthquakes
[期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (2
Asano Y.
;
Obara K.
;
Matsuzawa T.
;
Hirose H.
;
Ito Y.
View/Download:19/0
Changes in seismicity before and after the 2011 Tohoku earthquake around its southern limit revealed by dense ocean bottom seismic array data
[期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (5
Nakatani Y.
;
Mochizuki K.
;
Shinohara M.
;
Yamada T.
;
Hino R.
;
Ito Y.
;
Murai Y.
;
Sato T.
View/Download:39/0
Complicated rupture process of the Mw 7.0 intraslab strike-slip earthquake in the Tohoku region on 10 July 2011 revealed by near-field pressure records
[期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (22
Kubota T.
;
Hino R.
;
Inazu D.
;
Ito Y.
;
Iinuma T.
View/Download:19/0
Small-scale heterogeneities in the oceanic lithosphere inferred from guided waves
[期刊论文]
Geophysical Research Letters, 2013-01-01, 40 (9
Shito A.
;
Suetsugu D.
;
Furumura T.
;
Sugioka H.
;
Ito A.
View/Download:0/0
Two-dimensional viscosity structure of the northeastern Japan islands arc-trench system
[期刊论文]
Geophysical Research Letters, 2013-01-01, 40 (17
Muto J.
;
Shibazaki B.
;
Ito Y.
;
Iinuma T.
;
Ohzono M.
;
Matsumoto T.
;
Okada T.
View/Download:14/0
Along-strike structural changes controlled by dehydration-related fluids within the Philippine Sea plate around the segment boundary of a megathrust earthquake beneath the Kii peninsula, southwest Japan
[期刊论文]
Geophysical Research Letters, 2013-01-01, 40 (18
Kurashimo E.
;
Iwasaki T.
;
Iidaka T.
;
Kato A.
;
Yamazaki F.
;
Miyashita K.
;
Shibutani T.
;
Ito K.
;
Takeda T.
;
Obara K.
;
Hirata N.
View/Download:26/0
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