千秋煤矿新井煤柱区冲击地压频发地质原因

    Geological Causes of Frequent Rock Burst in New Shaft Coal Pillar Area of Qianqiu Coal Mine

    • 摘要: 为了理清千秋煤矿新井煤柱区域冲击地压频发的地质原因,从而对冲击地压防治工作提供启示,对顶板岩性、地层结构、地表沉降和断裂构造等地质因素进行了统计、对比和分析,阐述了各因素导致冲击地压发生的机理,研究了地表沉降与冲击地压之间的关系。指出煤层上覆巨厚砾岩和“两硬一软”的地层结构是新井煤柱区冲击地压发生的地质基础。煤柱南部采空区地表下沉系数仅为0.18,上覆岩层远未达到充分沉降,造成煤柱区应力高度集中,是该区域冲击地压频发的主要原因。

       

      Abstract: It is necessary to clarify the geological causes of rock burst in the new shaft coal pillar area of Qianqiu Coal Mine, which can provide the inspiration for rock burst control work. The geological factors are arranged, compared and analyzed such as roof lithology, stratum structure, surface subsidence and fault structure. The mechanisms of rock burst are elaborated caused by geological factors, and the relationship is studied between rock burst and surface subsidence. The research indicates that the geological bases of rock burst are the thick conglomerate overlying coal seam and the special stratum structure of “two hard one soft”. The surface sedimentation coefficient is only 0.18 in the southern goaf of coal pillar, and the overlying rock is far from adequate sedimentation, thus results in a high concentration of coal pillar stress, which is the main reason that the rock burst takes place frequently in this area.

       

    /

    返回文章
    返回