A strong earthquake of magnitude Mw=7.9 occurred in eastern Sichuan region of China on 12
May 2008 (06:27 GMT). The focal mechanism solution showed
thrust type faulting. The ruptured fault has a SW-NE direction.
Thousands of people killed because of the earthquake.
The teleseismic Stations whose data were used in the inversion
and the focal mechanism of the earthquake
Teleseismic Modeling of P and SH waves for slip
Source Parameters determination using teleseismic recordings
Slip Distribution
Synthetic PGV map + EMSC seismicity
The earthquake modeled by Agalos A. email: aagalos@geol.uoa.gr
Earthquake modeled by Moshou Alexandra email: amoshou@geol.uoa.gr
References
Agalos A., Papadimitriou P., Makropoulos K., 2008. Rupture Histories of Strong Earthquakes.
31st General Assembly of the European Seismological Commission, held at the Creta Maris
Conference Center, Hersonissos, Crete Greece, Book of Short papers, p 9-16.
Bouchon Michel, (1981). A simple method to calculate Green's functions for elastic layered media. BSSA, 71, 4, 959-971.
Hartzell S. H., and Heaton T. H., 1983. Inversion of strong ground motion and teleseismic waveform
data for the fault rupture history of the 1979 Imperial Valley, California, earthquake. BSSA, 73, 1553_1583.
Moshou A., Papadimitriou P., Makropoulos K., 2008. Waveform Inversion using Teleseismic and
Regional Data for Earthquakes that Occurred in Greece. 31st General Assembly of the European
Seismological Commission, held at the Creta Maris Conference Center, Hersonissos, Crete Greece,
Book of abstracts, p 95.
Wessel, P. and W. H. F. Smith., 1991. Free software helps map and display data, EOS Trans. AGU, 72, 441.