Fig. 4
From: Sensor orientation of the TMD seismic network (Thailand) from P-wave particle motions
The RMT solution of Laos earthquake after (a, b, c) and before (d, e, f) realignment using waveform data from 3 stations (NANS, CRMM and CRMJ) with azimuth from source of 225°, 295° and 289°, respectively. a and d A comparison of observed (red traces) and predicted (blue traces) vertical, radial, and transverse waveforms. b and e A representative of best fitting focal mechanism versus depth curve indicating the best fitting focal mechanism of 66% at 7.0 km depth and 67% at 6.0 km depth before and after alignments, respectively. c and f Estimate of source location error and time shifts for the inversion