Cj. Ammon et al., ROUTINE ESTIMATION OF EARTHQUAKE SOURCE COMPLEXITY - THE 18 OCTOBER 1992 COLOMBIAN EARTHQUAKE, Bulletin of the Seismological Society of America, 84(4), 1994, pp. 1266-1271
We describe two methods, suitable for routine application to teleseism
ic recordings, that characterize the time history of seismic events. S
tacking short-period signals from large regional arrays provides stabl
e estimates of high-frequency radiation from the source, and an empiri
cal Green's function deconvolution procedure extracts reliable, broadb
and time functions suitable for analysis of faulting complexity and th
e spatio-temporal extent of rupture. Combined, these procedures charac
terize the source radiation of large events (M(S) > 7) between 200- an
d 0.5-sec periods.