Abstract
The paper describes two methods, suitable for routine application to teleseismic recordings that characterize the time history of seismic events. Stacking short-period signals from large regional arrays provides stable estimates of high-frequency radiation from the source, and an empirical Green's function deconvolution procedure extracts reliable, broadband time functions suitable for analysis of faulting complexity and the spatio-temporal extent of rupture. Combined, these procedures characterize the source radiation of large events (Ms > 7) between 200- and 0.5-sec periods. -Authors
Original language | English (US) |
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Pages (from-to) | 1266-1271 |
Number of pages | 6 |
Journal | Bulletin - Seismological Society of America |
Volume | 84 |
Issue number | 4 |
State | Published - 1994 |
All Science Journal Classification (ASJC) codes
- Geophysics
- Geochemistry and Petrology