赵英萍, 韦士忠, 陈绍明. 用频谱研究小金地震震源参数[J]. 华北地震科学, 1994, 12(4): 68-75.
引用本文: 赵英萍, 韦士忠, 陈绍明. 用频谱研究小金地震震源参数[J]. 华北地震科学, 1994, 12(4): 68-75.
Zhao Yingping, Wei shizhong, Chen Shaoming. A STUDY OF THE SOURCE PARAMETERS OFTHE XIAOJIN EARTHQUAKE BY SPECTRUM ANALYSIS[J]. North China Earthquake Sciences, 1994, 12(4): 68-75.
Citation: Zhao Yingping, Wei shizhong, Chen Shaoming. A STUDY OF THE SOURCE PARAMETERS OFTHE XIAOJIN EARTHQUAKE BY SPECTRUM ANALYSIS[J]. North China Earthquake Sciences, 1994, 12(4): 68-75.

用频谱研究小金地震震源参数

A STUDY OF THE SOURCE PARAMETERS OFTHE XIAOJIN EARTHQUAKE BY SPECTRUM ANALYSIS

  • 摘要: 本文用CDSN宽频带数字记录,计算了不对称双侧破裂模式的P波远场位移谱,用频谱方法研究中强地震的震源参数,并将它应用于1989年9月22日四川小金MS=6.6级地震的震源参数研究中。研究结果表明,断层长度为8.4km;宽度为2.9km;动力学参数:地震矩为4.7×1017N·m;平均位错64.6cm;应力降18.9×1015Pa.并用余震震源深度分布的空间图象证明了:地震断层为走向NW33°的走滑断层,断层面倾向为北东,倾角约为20°。

     

    Abstract: In this paper, using the CDSN broad-band digital recordings, we calculated the spectrum of thedisplacements of P waves in the far-field radiated from a fault whose mode of rupture is bilateral andasymmetrical. The source parameters of moderately strong eaarthquakes are studied by the spectralmethod, and are applied to the Xiaojin earthquake with M=6.6 in Sichuan Province which occurred onSeptember 22, 1989. The results show that the fault is 8.4km long; 2.9km wide. The dynamic parameters are estemated as fallows:the seismic moment, 4.7×1017N. m F the average dislocation, 64.6cm, stress drop, 18.9×1015Pa. We also used the three-dimensional image of the focal depth distribution ofthe after shocks to prove that the earthquake malt is a strike-slip one, striking NW33°, dipping NEwith dip angle being 20°.

     

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