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1970年MS 7.7云南通海大地震强地面运动模拟

  • 谭黎中 ,
  • 孟令媛 ,
  • 史保平
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  • 1. 中国科学院研究生院地球科学院, 北京 100049;
    2. 中国地震台网中心, 北京 100036

收稿日期: 2011-04-15

  修回日期: 2011-05-05

  网络出版日期: 2012-07-15

基金资助

中国科学院知识创新工程(KZCX2-YW-Q08-2)资助

Strong ground motion simulation of the 1970 MS 7.7 Tonghai earthquake, Yunnan, China

  • TAN Li-Zhong ,
  • MENG Ling-Yuan ,
  • SHI Bao-Ping
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  • 1. Earth Science College, Graduate University, Chinese Academy of Sciences, Beijing 100049, China;
    2. China Earthquake Networks Center, Beijing 100045, China

Received date: 2011-04-15

  Revised date: 2011-05-05

  Online published: 2012-07-15

摘要

对1970年云南通海大地震(MS7.7)进行了强地面运动模拟.采用复合震源模型和有限断层随机振动模型,针对包括昆明在内的4个特征城市的地表运动进行模拟计算.结果表明,在0.5~10 Hz频带范围内,2个模型的结果在波形、振幅、频率含量及持续时间上均具备较好的相似性.进一步采用复合震源模型模拟了通海地震的烈度分布图,与实际观测的烈度分布一致程度较高.

本文引用格式

谭黎中 , 孟令媛 , 史保平 . 1970年MS 7.7云南通海大地震强地面运动模拟[J]. 中国科学院大学学报, 2012 , 29(4) : 476 -484 . DOI: 10.7523/j.issn.2095-6134.2012.4.007

Abstract

Using a composite source model, we simulate the strong ground motion from the 1970 Tonghai earthquake (MS 7.7). Due to the lack of strong ground motion recordings and for verifying the reliability of simulated results,a finite fault model, developed based on the stochastic theory with the same input source parameters including fault slip distribution pattern and size, is additionally used to generate synthetic strong motion seismograms for comparison purpose. The acceleration time histories at four selected sites or cities, simulated by the two models, show good agreements in the amplitude, waveform, frequency content, and time duration within the 0.5-10 Hz frequency domain.

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