Fig. 3From: Inversion of Love waves in earthquake ground motion records for two-dimensional S-wave velocity model of deep sedimentary layersObserved velocity waveforms in the transverse direction. These waveforms are bandpass filtered for periods of 1, 3, 5, and 9 s. Triangles and circles indicate the arrival times of the P-waves and S-waves, respectively. The vertical axes denote the basin-edge distances. Segments at the times indicated with crosses from 0 s were used in the calculations for horizontal particle motions in Fig. 4aBack to article page