Time Functions Appropriate for Deep Earthquakes
نویسندگان
چکیده
The seismic signatures of isolated body phases from many: deep-fo~cus earthquakes were analyzed in the time domain. Most shocks were found to be multiple events when examined in detail. The time history derived from P waves for single events predict synthetic S-wave shapes that match the observations, indicating compatibility with shear dislocation theory. Several other features of source functions in the time domain have been brought to light.
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تاریخ انتشار 2005