华南地震2016，Vol.36Issue(2)：6-12,7.DOI:10.13512/j.hndz.2016.02.002
贵州剑河5.5级地震的地质构造背景
The Tectonic Background Introduction of Jianhe MS 5.5 Earthquake in Guizhou
杨光忠 1李吉春 1王志京1
作者信息
- 1. 贵州省地矿局101地质队，贵州 凯里 556000
- 折叠
摘要
Abstract
The Jianhe MS 5.5 earthquake has relatively serious threat to people's lives and property in earthquake region, and has certain influence to “the safe island of earthquake” southeast Gizhou. This paper briefly describes the tectonic background of Daxinan-taihang-wuling gravity gradient zone and its faults, and analyzes of the cause of the Jianhe MS 5.5 earthquake. The results show that the Tudong fault cutting through the reservoir joins the Jianhe (gedong) -taijiang fault in deep epicenter, which results in the concentration of local tectonic stress and earthquake preparation; under the influence of water percolation of fault and function of Sanbanxi reservoir's load, stress is unbalanced and earthquake is triggered. By the adjustment of reservoir, the greater earthquake may be prevented and avoided.关键词
地震/地质构造背景/贵州剑河Key words
Earthquake/Tectonic background/Jianhe分类
天文与地球科学引用本文复制引用
杨光忠,李吉春,王志京..贵州剑河5.5级地震的地质构造背景[J].华南地震,2016,36(2):6-12,7.
