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| Episodic slow slip events in the Japan subduction zone before the 2011 Tohoku-Oki earthquake Y Ito, R Hino, M Kido, H Fujimoto, Y Osada, D Inazu, Y Ohta, T Iinuma, ... Tectonophysics 600, 14-26, 2013 | 356 | 2013 |
| Coseismic slip distribution of the 2011 off the Pacific Coast of Tohoku Earthquake (M9. 0) refined by means of seafloor geodetic data T Iinuma, R Hino, M Kido, D Inazu, Y Osada, Y Ito, M Ohzono, H Tsushima, ... Journal of Geophysical Research 117 (B7), B07409, 2012 | 340 | 2012 |
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| Slow slip near the trench at the Hikurangi subduction zone, New Zealand LM Wallace, SC Webb, Y Ito, K Mochizuki, R Hino, S Henrys, SY Schwartz, ... Science 352 (6286), 701-704, 2016 | 305 | 2016 |
| Spatial distribution and focal mechanisms of aftershocks of the 2011 off the Pacific coast of Tohoku Earthquake Y Asano, T Saito, Y Ito, K Shiomi, H Hirose, T Matsumoto, S Aoi, S Hori, ... Earth, planets and space 63, 669-673, 2011 | 272 | 2011 |
| Trench-normal variation in observed seafloor displacements associated with the 2011 Tohoku-Oki earthquake M Kido, Y Osada, H Fujimoto, R Hino, Y Ito Geophysical Research Letters 38 (24), L24303, 2011 | 212 | 2011 |
| Very low frequency earthquakes within accretionary prisms are very low stress‐drop earthquakes Y Ito, K Obara Geophysical Research Letters 33 (9), 2006 | 193 | 2006 |
| Tsunami source of the 2011 Tohoku-Oki earthquake, Japan: Inversion analysis based on dispersive tsunami simulations T Saito, Y Ito, D Inazu, R Hino Geophysical Research Letters, 2011 | 185 | 2011 |
| Very low frequency earthquakes excited by the 2004 off the Kii peninsula earthquakes: A dynamic deformation process in the large accretionary prism K Obara, Y Ito Earth, Planets and Space 57 (4), 321-326, 2005 | 183 | 2005 |
| Dynamic deformation of the accretionary prism excites very low frequency earthquakes Y Ito, K Obara Geophysical Research Letters 33 (2), 2006 | 179 | 2006 |
| Change in stress field after the 2011 great Tohoku-Oki earthquake A Hasegawa, K Yoshida, Y Asano, T Okada, T Iinuma, Y Ito Earth and Planetary Science Letters 355, 231-243, 2012 | 172 | 2012 |
| Stress before and after the 2011 great Tohoku‐oki earthquake and induced earthquakes in inland areas of eastern Japan K Yoshida, A Hasegawa, T Okada, T Iinuma, Y Ito, Y Asano Geophysical Research Letters 39 (3), 2012 | 157 | 2012 |
| Tsunami-generated turbidity current of the 2011 Tohoku-Oki earthquake K Arai, H Naruse, R Miura, K Kawamura, R Hino, Y Ito, D Inazu, ... Geology 41 (11), 1195-1198, 2013 | 125 | 2013 |
| Slow slip source characterized by lithological and geometric heterogeneity PM Barnes, LM Wallace, DM Saffer, RE Bell, MB Underwood, A Fagereng, ... Science Advances 6 (13), eaay3314, 2020 | 113 | 2020 |
| Extension of continental crust by anelastic deformation during the 2011 Tohoku-oki earthquake: The role of extensional faulting in the generation of a great tsunami T Tsuji, K Kawamura, T Kanamatsu, T Kasaya, K Fujikura, Y Ito, T Tsuru, ... Earth and planetary science letters 364, 44-58, 2013 | 103 | 2013 |
| A discrete episode of seismic and aseismic deformation of the Nankai trough subduction zone accretionary prism and incoming Philippine Sea plate EE Davis, K Becker, K Wang, K Obara, Y Ito, M Kinoshita Earth and Planetary Science Letters 242 (1-2), 73-84, 2006 | 97 | 2006 |
| Earthquakes and tremor linked to seamount subduction during shallow slow slip at the Hikurangi margin, New Zealand EK Todd, SY Schwartz, K Mochizuki, LM Wallace, AF Sheehan, SC Webb, ... Journal of Geophysical Research: Solid Earth 123 (8), 6769-6783, 2018 | 95 | 2018 |
| Simple relationship between seismic activity along Philippine Sea slab and geometry of oceanic Moho beneath southwest Japan K Shiomi, M Matsubara, Y Ito, K Obara Geophysical Journal International 173 (3), 1018-1029, 2008 | 92 | 2008 |
| Potential tsunamigenic faults of the 2011 off the Pacific coast of Tohoku Earthquake T Tsuji, Y Ito, M Kido, Y Osada, H Fujimoto, J Ashi, M Kinoshita, ... Earth, planets and space 63, 831-834, 2011 | 89 | 2011 |
Ryota HinoTohokku Uniersity在 tohoku.ac.jp 的电子邮件经过验证
