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2012年10月31日三峡库区M_L3.8小震群研究

RESEARCH OF M_L3.8 SMALL EARTHQUAKE SWARM IN THREE GORGES RESERVOIR AREA ON OCTOBER 31,2012

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【作者】 陈俊华姚运生吴海波吴建超申学林魏贵春戴苗赵凌云

【Author】 Chen Junhua1,2),Yao Yunsheng1,2),Wu Haibo1,2),Wu Jianchao1,2,3), Shen Xuelin1,2),Wei Guichun1,2),Dai Miao1,2)and Zhao Lingyun1,2) (1)Key Laboratory of Earthquake Geodesy,Institute of Seismology,CEA,Wuhan 430071 2)Earthquake Administration of Hubei Province,Wuhan 430071 3)Wuhan Research Institute of Earthquake Engineering,Wuhan 430071)

【机构】 中国地震局地震研究所(地震大地测量重点实验室)湖北省地震局武汉地震工程研究院

【摘要】 对2012年10月31日三峡库区屈原镇ML3.8小震群活动的研究表明,是一次与三峡水库蓄水过程直接相关震群活动;地震主要聚集在仙女山断裂带北端,深约10 km,分布在结晶基底附近;震源体的线性尺度较小,主要限定在5 km的范围;主震和较大地震表现为较典型的构造型地震特征;震群活动为水库高水位蓄水引发仙女山断裂北端构造应力调整,其震群为水库触发型构造地震。

【Abstract】 The largest magnitude is ML3.8 small earthquake swarm which occurred on October 30,2012,Quyuan town of Zigui County in the Three Gorges reservoir region.The studies show that the small earthquake swarm are directly related to the Three Gorges Reservoir impounding;the earthquake swarm gathered in the northern end of Xiannvshan fault zone,earthquakes most located within 10 km near the crystalline basement;linear scale of hypocenter body is smaller,mainly limited radius of 5 km of range;mainshock and larger seismic performance typical stereotype earthquake characteristics;earthquake swarm triggered the fault structure Xiannvshan stress to adjust in the high water level of the reservoir impounding,small earthquake swarm are reservoir triggered tectonic earthquakes.

【基金】 中国长江三峡工程开发总公司专项基金(SXSN/2377);中国地震局地震研究所所长基金(IS201246114)
  • 【文献出处】 大地测量与地球动力学 ,Journal of Geodesy and Geodynamics , 编辑部邮箱 ,2013年02期
  • 【分类号】P315
  • 【被引频次】3
  • 【下载频次】120
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