山西朔州东坡煤矿构造关系及成因分析  

Structure relationship and cause analysis of Dongpo coal mine in Shuozhou

作　　者：王恩营[1] 马军超[1] 汪师逵[1] 杜琳玮[1] 邢鹏飞[1] 张飞[1] 

机构地区：[1]河南理工大学资源环境学院,河南焦作454000

出　　处：《中国矿业》2014年第1期74-76,共3页China Mining Magazine

基　　金：中国煤炭协会科学技术研究指导性计划项目资助(编号:MTKJ2009-295;MTKJ2009-296);河南省教育厅自然科学研究计划项目资助(编号:2009B62002);河南理工大学博士基金资助(编号:B2011-063)

摘　　要：东坡煤矿构造研究对矿井防治水具有重要意义。根据区域构造应力场分析和矿井构造统计,研究了褶皱和断层的发育规律、构造之间的关系及应力作用。研究结果表明:井田内主要发育近东西向褶皱、断层和NE-NNE向断层。其中,井田南部边界担水沟断层为第一序次构造,井田内断层和褶皱为第二序次构造,担水沟断层对井田内构造的形成具有控制作用。The research on the structure of Dongpo coal mine is of great importance to the prevention and control of mine water. The study is focus on the development rules of fold and fault, the relationship between the structure and the effect of stress according to the stress field analysis of regional structure and the mine construction statistics. The results show that the main structure inside the field are nearly East- Westward folds, faults and NE - NNE faults. Among them, the Danshuigou fault located the southern boundary of field was the first order structure, the fault and fold in the field were the second order tectonics. Danshuigou fault has a control effect on the structure formation in the field. K

关 键 词：山西省 东坡煤矿 褶皱 断层 

分 类 号：P542.2[天文地球—构造地质学]