Fig. 10From: 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 plateDistribution of first-motion polarizations from observations and MT results. First-motion polarization is shown as black (up) and white (down) circles. Dashed lines are the isodistance lines with an interval of 50 km from the epicenter. Stations, which show different polarity compared to observations, are enhanced by purple circlesBack to article page