Focal mechanism of 22 June 2002 Changoreh- AvajEarthquake using strong ground motion data
Category | Tectonic & Seismotectonic |
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Group | GSI.IR |
Location | 21th symposium on geosciences |
Holding Date | 24 May 2008 |
Abstract:
The causative fault parameters of Changoreh- Avaj earthquake has been estimated using the strong ground motion data recorded by Iranian strong ground motion network. To estimate these parameters SH- waves has been analyzed. Strike, dip and rake for the causative fault have been estimated by compression of observed and calculated amplitude of SH- waves as, 118, 52 and 82 respectively. The focal mechanism of this earthquake is reverse similar to the 1962 Buin- Zahra earthquake.
General:
The catsative fault parameters of Changoreh- Avaj earthquake has been estimated using the strong ground motion data recorded by Iranian strong ground motion network. To estimate these parameters SH- waves has been analyzed. Strike, dip and rake for the causative fault have been estimated by compression of observed and calculated amplitude of SH-waves as, 118, 52 and 82 respectively. The focal mechanism of this earthquake is reverse similar to the 1962 Buin-Zahra earthquake