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For the hypocenter relocation, we used the manually picked P and S arrival times, with P and S arrival time differences for 27,440 and 38,883 pairs, respectively.
The number of absolute P- and S-wave arrival times was 47,785 and 43,155, with the differential arrival times for manually picked P and S waves reaching 257,416 and 225,281, respectively.
We picked P and S arrival times from digital and analog seismograms recorded by 96 seismic stations in Morocco and Spain between 1989 and 1996 and combined them with arrivals carefully selected from local and global catalogs (1964-1998) to generate a starting data set containing over 100,000 arrival times.
We manually picked P - and S-wave first motions for the triggered events.
We manually picked P and S phases from the waveform data recorded by the local permanent network and our temporary station arrays.
The correlation measurements were conducted using the velocity waveform of a 0.75-s time window and a 3 20 Hz bandpass filter, including the manually picked P -or S-warrivalival times.
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The differential arrival times for the manually picked P- and S-waves were 548,454 and 494,403 pairs, respectively.
We picked P-wave, and S-wave, arrivals of 135 local earthquake events at 289 seismic stations.
Waveforms are band-passed from 2 to 16 Hz and then aligned with manually picked P-wave arrival times.
The numbers of differential arrival times for the manually picked P- and S-waves are 6697 and 4003, respectively.
The differential arrival times for the manually picked P- and S-waves were 79,026 and 68,408, respectively.
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