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东升庙矿区应力场以及矿岩层形成变化规律分析
Analysis of the stress of mining area and the rules that formed and changed of rock mass in Dongshengmiao
【摘要】 地应力产生的原因十分复杂,但其在研究区域和采场稳定性问题方面,是必不可少的考量因素。通过对东升庙区域应力场及其演化分析,得到了矿区局部应力场的几个分布特征,掌握了矿岩层的形成与变化规律,探讨了同生断裂活动对矿岩体稳定性的影响。
【Abstract】 The causing of in-situ stress is very complex,but it is the essential factor in the research of stability of region and stope.Through the analysis of regional stress field’s evolvement,several distribution characteristics of local stress in mining area is advanced,the rule of formation and change of strata is mastered,the influence that caused by the synchronous fault to the stability of rock mass is researched.
【关键词】 区域应力场;
局部应力场;
同生断裂;
东升庙矿;
【Key words】 regional stress; local stress; synchronous fault; Dongshengmiao mine;
【Key words】 regional stress; local stress; synchronous fault; Dongshengmiao mine;
- 【文献出处】 中国矿业 ,China Mining Magazine , 编辑部邮箱 ,2011年04期
- 【分类号】TD31
- 【被引频次】1
- 【下载频次】56