Time-advanced occurrence of moderate-size earthquakes in a stable intraplate region after a megathrust earthquake and their seismic properties. [PDF]
Sci Rep, 2018 Hong TK, Lee J, Park S, Kim W.
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Coseismic seafloor deformation in the trench region during the Mw8.8 Maule megathrust earthquake. [PDF]
Sci Rep, 2017 Maksymowicz A +9 more
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Activity of Significant Earthquakes before and after Megathrust Earthquakes in the World
Zisin (Journal of the Seismological Society of Japan. 2nd ser.), 2014 KOYAMA, Junji, TSUZUKI, Motohiro
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Ultralow-angle faults produce giant earthquakes. [PDF]
Sci AdvIde S, Furuichi M, Sato DSK.
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Strain accumulation associated with locked subduction megathrusts revealed by deep-ocean borehole observations. [PDF]
Sci AdvSun T, Davis EE.
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Large megathrust earthquakes in cold mantle wedge corners under lawsonite blueschist facies. [PDF]
Nat CommunZhang H +5 more
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Effects of plate interface frictional heterogeneities on earthquake cycle dynamics in subduction zones. [PDF]
Sci RepRay S, Ghosh A, Kundu B, Senapati B.
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Observation of Earth's free oscillation by dense GPS array: after the 2011 Tohoku megathrust earthquake. [PDF]
Sci Rep, 2012 Mitsui Y, Heki K.
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Active protothrusts and fluid highways: Seismic noise reveals hidden subduction dynamics in Cascadia. [PDF]
Sci AdvKidiwela M +3 more
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Variability of megathrust earthquakes in the world revealed by the 2011 Tohoku-oki Earthquake
Variability of megathrust earthquakes in the world revealed by the 2011 Tohoku-oki EarthquakeThe seismicity of the Pacific coast of Tohoku, Japan has been investigated in detail and characterized into regional seismic segments. The 2011 megathrust earthquake of Mw9.0 on 11 March ruptured almost all of the segments in that area, causing devastating tsunami.
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