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Fine structure beneath the Tohoku district, northeastern Japan arc, as derived by an inversion of P-wave arrival times from local earthquakes

GeophysicsMarine GeologyEngineeringSeismic WaveSeismologySeismic Reflection ProfilingLocal EarthquakesEarthquake SourceGeographyNortheastern Japan ArcFine StructureSeismic HazardEarth ScienceTectonics