Figure 8From: Velocity increase in the uppermost oceanic crust of subducting Philippine Sea plate beneath the Kanto region due to dehydration inferred from high-frequency trapped P waves Simulated vertical velocity seismograms derived from the 2D and 3D simulations. (a) Model A1. (b) Model A2. The dashed and solid lines in each trace are the onsets of the P and trapped P waves, respectively. The location of the stations in the 2D and 3D models is shown in Figure 7b,c.Back to article page