Application of an iterative least-squares waveform inversion of strong-motion and teleseismic records to the 1978 Tabas, Iran, earthquake
Bulletin of the Seismological Society of America
By: S. Hartzell and C. Mendoza
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Abstract
An iterative least-squares technique is used to simultaneously invert the strong-motion records and teleseismic P waveforms for the 1978 Tabas, Iran, earthquake to deduce the rupture history. The effects of using different data sets and different parametrizations of the problem (linear versus nonlinear) are considered. A consensus of all the inversion runs indicates a complex, multiple source for the Tabas earthquake, with four main source regions over a fault length of 90 km and an average rupture velocity of 2.5 km/sec.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Application of an iterative least-squares waveform inversion of strong-motion and teleseismic records to the 1978 Tabas, Iran, earthquake |
| Series title | Bulletin of the Seismological Society of America |
| DOI | 10.1785/BSSA0810020305 |
| Volume | 81 |
| Issue | 2 |
| Year Published | 1991 |
| Language | English |
| Publisher | Seismological Society of America |
| Description | 27 p. |
| First page | 305 |
| Last page | 331 |
| Country | Iran |
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