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由震源机制解资料研究川滇地区构造应力场

Research on Structural Stress Field Basing on Focal Mechanism Solutions Data in Sichuan-Yunan Area

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【作者】 曹颖吴小平沈娅宏李兆隆

【Author】 CAO Ying 1 ,WU Xiao-ping 2 ,SHEN Ya-hong 1 ,LI Zhao-long 1 ( 1. Earthquake Administration of Yunnan Province,Kunming 650224,Yunnan,China) ( 2. School of Resource Environment and Earth Sciences,Yunnan University,Kunming 650091,Yunnan,China)

【机构】 云南省地震局云南大学资源环境与地球科学学院

【摘要】 利用1978~2009年川滇地区的124个地震震源机制解资料,采用对震源机制参数统计的方法,详细分析了地震断层类型和川滇地区的现代构造应力场特征。结果表明,云南地区(21°~28°N,97°~108.8°E)主要受近N-S向的水平挤压力影响,区域应力场背景以水平作用力为主;四川地区(28°~34.5°N,97°~108.8°E)由于平均P,T轴的仰角接近水平,构造应力场接近水平,主要受近E-W向挤压力作用,断层面较陡,受水平剪切力作用。川滇地区走滑型地震较多,主要分布于云南地区,四川地区内发生的地震类型较为分散且每种类型都有。

【Abstract】 Basing on 124 focal mechanisms data from 1978 to 2009 in Sichuan-Yunan area,we analyzed the fault type of earthquake and the characteristic of modern tectonic stress field in Yunnan-Sichuan area by the statistic method of focal mechanisms parameters. The results show ed that it was influenced by horizontal compression in nearly NS direction in Yunnan area ( 21° ~ 28°N,97° ~ 108. 8°E) ,and the main characteristic of regional stress field background is characterized by horizontal compression. Because of the average plunges of P-axis and T-axis were close to horizontal,the tectonic stress field which is close to horizontal mainly influenced by compression in nearly EW direction in Sichuan area ( 28° ~ 34. 5°N,97° ~ 108. 8°E) . The fault plane which was influenced by horizontal shear tress is stepper. The main type of fault is strike-slipe in Sichuan-Yunnan area,and mainly dis- tributed in Yunnan. The earthquake occurred in Sichuan area had many types and scattering distribution.

【基金】 国家自然科学基金项目(41074044)资助
  • 【文献出处】 地震研究 ,Journal of Seismological Research , 编辑部邮箱 ,2013年02期
  • 【分类号】P315.33
  • 【被引频次】10
  • 【下载频次】192
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