Fig. 12From: Moment tensor inversion of the 2016 southeast offshore Mie earthquake in the Tonankai region using a three-dimensional velocity structure model: effects of the accretionary prism and subducting oceanic plateComparison of three-component velocity seismograms for periods of 5–100 s. Black and red traces are the observed and synthetic velocity waveforms at F-net stations, respectivelyBack to article page