Fig. 11
From: Discriminating non-seismic long-period pulses and noise to improve earthquake source inversion
Source amplitudes calculated from synthetic seismograms for a the Philippines network and b F-net and corresponding source amplitude ratios for c the Philippines network and d F-net. Strike, dip, and rake angles were systematically changed, and source locations were assumed to be near the center of each network (stars in Figs. 1a, 8a)