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- W1569542902 abstract "Abstract : An analysis of 418 small-event (m sub b or = 5.8) seismograms recorded at 17 world-wide stations, and of 148 large-event (m sub b, M sub s (NOS), or m sub b from Pasadena or Berkeley or = 7.0) seismograms recorded at 8 worldwide stations and TFO indicates that coda shape is primarily a function of the arrival times and relative amplitudes of significant secondary arrivals. However, for times greater than 10 to 20 seconds into the coda, large-event codas are approximately 0.14 m sub b units greater in amplitude at any given time relative to their maxima, than the corresponding relative amplitude for small-event codas. This suggests that large events are, in fact, multiple events, with the nominal period of source activity for a given sequence estimated to be on the order of 1 to 2 minutes. Correspondingly, large events also tend to be emergent, displaying a 0.2 to 0.3 m sub b increase in amplitude between 5 and 30 seconds into the P-wave arrival over that observed in the first 5 seconds of the arrival. Because of their differences, large-event and small- event coda observations cannot be combined." @default.
- W1569542902 created "2016-06-24" @default.
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- W1569542902 date "1973-11-12" @default.
- W1569542902 modified "2023-09-26" @default.
- W1569542902 title "Average P and PKP Codas for Earthquakes" @default.
- W1569542902 doi "https://doi.org/10.21236/ada004960" @default.
- W1569542902 hasPublicationYear "1973" @default.
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