R
Ryota Hino
Researcher at Tohoku University
Publications - 201
Citations - 5878
Ryota Hino is an academic researcher from Tohoku University. The author has contributed to research in topics: Subduction & Aftershock. The author has an hindex of 37, co-authored 192 publications receiving 4962 citations.
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Journal ArticleDOI
Continental Crust, Crustal Underplating, and Low- Q Upper Mantle Beneath an Oceanic Island Arc
Kiyoshi Suyehiro,Narumi Takahashi,Yoshiro Ariie,Yasutaka Yokoi,Ryota Hino,Masanao Shinohara,Toshihiko Kanazawa,Naoshi Hirata,Hidekazu Tokuyama,Asahiko Taira +9 more
TL;DR: A detailed structural model of the crust, subducting slab, and underlying upper mantle across the northern Izu-Ogasawara (Bonin) island arc system is derived from a marine seismic reflection and ocean bottom seismographic refraction survey and subsequent forward modeling combined with tomographic inversion.
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Episodic slow slip events in the Japan subduction zone before the 2011 Tohoku-Oki earthquake
Yoshihiro Ito,Ryota Hino,Motoyuki Kido,Hiromi Fujimoto,Yukihito Osada,Daisuke Inazu,Yusaku Ohta,Takeshi Iinuma,Mako Ohzono,Satoshi Miura,Masaaki Mishina,Kensuke Suzuki,Takeshi Tsuji,Juichiro Ashi +13 more
TL;DR: In this paper, the authors describe two transient slow slip events that occurred before the 2011 Tohoku-Oki earthquake, which induced increases in shear stress, which in turn triggered the interplate earthquakes.
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Frontal wedge deformation near the source region of the 2011 Tohoku-Oki earthquake
Yoshihiro Ito,Takeshi Tsuji,Yukihito Osada,Motoyuki Kido,Daisuke Inazu,Yutaka Hayashi,Hiroaki Tsushima,Ryota Hino,Hiromi Fujimoto +8 more
TL;DR: In this paper, an ocean-bottom pressure gauge was installed before the 2011 Tohoku-Oki earthquake on a frontal wedge, which formed an uplift system near the Japan Trench.
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Coseismic slip distribution of the 2011 off the Pacific Coast of Tohoku Earthquake (M9.0) refined by means of seafloor geodetic data
Takeshi Iinuma,Ryota Hino,Motoyuki Kido,Daisuke Inazu,Yukihito Osada,Yoshihiro Ito,Mako Ohzono,Hiroaki Tsushima,Syuichi Suzuki,Hiromi Fujimoto,Satoshi Miura +10 more
TL;DR: In this paper, the authors estimate the coseismic slip distribution based on terrestrial GPS observations and all available seafloor geodetic data that significantly improves the spatial resolution at the shallow portion of the plate interface, revealing that an extremely large (greater than 50 m) slip occurred in a small (about 40 km in width and 120 km in length) area near the Japan Trench and generated the huge tsunami.
Journal ArticleDOI
Slow slip near the trench at the Hikurangi subduction zone, New Zealand.
Laura M. Wallace,Spahr C. Webb,Yoshihiro Ito,Kimihiro Mochizuki,Ryota Hino,Stuart Henrys,Susan Y. Schwartz,Anne F. Sheehan +7 more
TL;DR: Detailed seafloor deformation observations made during an offshore slow-slip event (SSE) in September and October 2014 are presented, using a network of absolute pressure gauges deployed at the Hikurangi subduction margin offshore New Zealand.