巨厚砂岩下厚煤层采动覆岩离层形成机理与探测

    Formation Mechanism and Detection Method of Overburden Abscission Layer in Mining Coal Seam Under Thick Sandstone

    • 摘要: 为了研究巨厚砂岩下厚煤层采动覆岩发育特征及形成位置,以大同某矿2301工作面厚煤层采动引发的覆岩运动为例,采用理论计算公式、超声成像和彩色钻孔电视系统分别对巨厚砂岩下厚煤层采动覆岩离层的发育位置进行理论计算和定量探测。结果表明:煤层上覆岩层中存在多层亚关键层,但主关键层只有1层,离层主要产生于各关键层下,其向上发育高度终止于主关键层;得到巨厚砂岩下离层发育深度为343、346.5、328.61 m;证实了巨厚砂岩下厚煤层采动会形成离层。

       

      Abstract: In order to study the development characteristics and formation location of mining overburden in thick coal seam under thick sandstone, the overburden movement caused by mining of thick coal seam at 2301 working face in a Datong mine is taken as an example. Theoretical calculation formula ultrasonic imaging and color drilling television system are used to calculate and quantitatively detect the development position of overburden strata in mining thick coal seam under thick sandstone. The results show that there are several sub-key layers in the overlying strata of coal seam, but there is only one main key layer, the abscission layer is mainly generated under each key layer, and the upward development height ends at the main key layer. the development depth of the abscission layer under the giant thick sandstone is respectively 343, 346.5, 328.61 m. It is proved that the stratum separation will be formed in the mining of the thick coal seam under the huge thick sandstone.

       

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