Fig. 4From: Inversion of Love waves in earthquake ground motion records for two-dimensional S-wave velocity model of deep sedimentary layersResults of principal component analyses for records along Line-1. a Horizontal particle motions and principal axis directions, indicated by the black and red lines, respectively. The horizontal axis indicates a basin-edge distance. b E values for the observatories at individual periods. The waveforms at stations located within the distances indicated by the arrows are used in the 2D inversion analysis. c Relationship between periods of ground motions and basin-edge distances for confirmation of the two-dimensionality in 2D inversionBack to article page