THE SOURCE PARAMETERS OF THE SAN FERNANDO EARTHQUAKE INFERRED FROM TELESEISMIC BODY WAVES BY MAX WYss AND THOMAS

نویسنده

  • C. HANKS
چکیده

The accuracy of teleseismic estimates of moment, fault area, dislocation and stress drop was tested for the case of a thrust fault: the San Fernando, California, earthquake of Feburary 9, 1971. On the basis of P-wave spectra of 25 stations and S-wave spectra of 9 stations, the respective values were found to be 0.7.1026 dyne-cm, 570 km 2, 45 cm, and 14 bars. They agree well with the same parameters obtained from field observations. It is concluded that Brune's (1970) seismic source model is valid for the area determination of thrust earthquakes. The energy radiated in the form of S waves is estimated to be 5.1021 ergs.

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تاریخ انتشار 2005