Fig. 6.
From: Analysis of the rupture process of the 1995 Kobe earthquake using a 3D velocity structure
Comparisons of the observed (black) and synthetic waveforms from inversion using 1D (blue) or 3D (red) Green’s functions at stations KOB, KPI and OSA. The maximum amplitude is given in cm s−1 above each trace. Because the sensor orientation of the borehole seismometer at station KPI has been corrected, the maximum amplitudes for the EW and NS components are different between the blue and red traces.