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首页> 外文期刊>Bulletin of the Seismological Society of America >Estimates of stress drop of the Chi-Chi, Taiwan, earthquake of 20 September 1999 from near-field seismograms
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Estimates of stress drop of the Chi-Chi, Taiwan, earthquake of 20 September 1999 from near-field seismograms

机译:利用近场地震谱估算1999年9月20日台湾集集地震的应力降。

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摘要

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 E-s/M-0 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 Ramon Zuniga (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. [References: 30]
机译:台湾Chi-Chi地震的表观应力和应力降是根据近场地震图估算的。断层南部的估计表观应力和应力降比北部低约100巴。估计比率E-s / M-0也表明,北部的动应力下降比南部的动应力下降大。这表明北部的应变能转换为地震波能的比例要高于南部。根据Ramon Zuniga(1993)提出的参数,我们提出摩擦超调的应力模型可以解释发生在台湾集集地震上的Chelungpu断裂的破裂。 [参考:30]

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