Figure 5
From: A study on the predominant period of long-period ground motions in the Kanto Basin, Japan
Seismic velocity structure of the sediment and the amplitude response of different surface wave modes. (a) Seismic velocity structure model of the SITH01 at Iwatsuki from Yoshimoto and Takemura (2014). (b) Depth variation of the normalized amplitude of the fundamental Love wave at a period of 7 s for Iwatsuki's model (calculated by a computer program by Herrmann (2013)). (c) Amplitude response of the Love and Rayleigh waves calculated from Iwatsuki's model.