Fig. 6From: An analysis of a moderate earthquake, eastern flank of the Red Sea, Saudi ArabiaComparison between the observed (black lines) and the synthetic velocity waveforms for the optimum solutions obtained from the regional waveform inversion a the deviatoric moment-tensor solution using the velocity model of Rodgers et al. (1999) and b the full moment-tensor solution using the velocity model of Rodgers et al. (1999)Back to article page