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Runaway slip to the trench due to rupture of highly pressurized megathrust beneath the middle trench slope: The tsunamigenesis of the 2011 Tohoku earthquake off the east coast of northern Japan

Marine GeologyTsunami ScienceEngineeringInduced SeismicitySeismologyEarthquake SourceCivil EngineeringMiddle Trench SlopeNorthern JapanEarthquake RuptureSeismic HazardEarth ScienceRunaway SlipTectonics