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小湾库区水库诱发地震的地质环境分析
引用本文:毛玉平,王洋龙,李朝才.小湾库区水库诱发地震的地质环境分析[J].地震研究,2004,27(4):339-343.
作者姓名:毛玉平  王洋龙  李朝才
作者单位:云南省地震局,昆明,650041;云南省地震局,昆明,650041;云南省地震局,昆明,650041
摘    要:在文献1]的基础上,通过对小湾库区岩石介质、地质构造、构造应力场、库区及周围地震活动特点的分析,认为小湾库区水库诱发地震的地质环境比较复杂,存在发生岩溶型、裂隙型、构造型等三种成因类型的水库诱发地震的基本条件,而沿通过库区的澜沧江断裂带及其次级断层,和无量山断裂带发生构造型水库诱发地震,是小湾库区水库地震活动的主要诱发因素:

关 键 词:水库地震  地质构造  应力场  小震活动  小湾库区
文章编号:1000-0666(2004)04-0339-05
修稿时间:2003年11月4日

Seismo-geological Ambiance Analyses of Reservoir-Induced Earthquake in Xiaowan Area
MAO Yu-ping,WANG Yang-long,LI Chao-cai.Seismo-geological Ambiance Analyses of Reservoir-Induced Earthquake in Xiaowan Area[J].Journal of Seismological Research,2004,27(4):339-343.
Authors:MAO Yu-ping  WANG Yang-long  LI Chao-cai
Abstract:On the basis of reference 1], through the analyses of rock media, geological structures, tectonic stress field and seismic active characteristics in the reservoir area and nearby, it is considered that the geological ambiance of reservoir-induced earthquake in Xiaowan area is complicated. There exist three types of geneses for conditions of reservoir-induced earthquake, such as karst type, fissure type and structure type. However, the structural reservoir-induced earthquake along the Lancangjiang Fault and its sub-faults, as well as the Wuliangshan Fault Zone which crosses the reservoir areas, is the major inducing factors.
Keywords:reservoir-induced earthquake  geological structure  stress field  activities of small earthquake  Xiaowan reservoir area
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