Bulletin of the Seismological Society of America; October 2001; v. 91; no. 5;
p. 1158-1166; DOI: 10.1785/0120000708
© 2001 Seismological Society of America
Estimates of Stress Drop of the Chi-Chi, Taiwan, Earthquake of 20 September 1999 from Near-Field Seismograms
Ruey-Der Hwang*,
Jeen-Hwa Wang,
Bor-Shouh Huang,
Kou-Cheng Chen,
Win-Gee Huang,
Tao-Ming Chang,
Hung-Chie Chiu and
Chu-Chuan Peter Tsai
Institute of Earth Sciences, Academia Sinica
P.O. Box 1-55, Nankang
Taipei, 115 Taiwan
Manuscript received 31 July 2000.
The apparent stress and stress drop of the Chi-Chi, Taiwan, earthquake are estimated from near-field seismograms. The estimated apparent stress and stress drop for the southern part of the fault are about 100 bars lower than those for the northern part. The estimated ratio Es/M0 also suggests that there is a higher dynamic stress drop in the northern part than in the southern one. This indicates the transformation of a higher percentage of strain energy into the seismic-wave energy in the northern part than in the southern part. Based on a parameter proposed by Ramón Zúñiga (1993), we propose that the stress model of frictional overshoot can interpret the rupture of the Chelungpu fault, on which the Chi-Chi, Taiwan, earthquake occurred.
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