地质构造对宿南矿区72煤层厚度变化的控制作用

Controlling effect of geological structure on the thickness variation of 72 coal seam in Sunan mining area

  • 摘要: 宿南矿区为淮北煤田重要矿区,其中72煤层为矿区主要可采之一。地质勘探资料表明,该煤层的厚度变化较大,变化特征明显。在矿井地质调查及矿区地质构造研究的基础上,发现该煤层煤体结构破碎,煤层厚度变化与区内地质构造具有密切的联系。在煤厚区域分布特征方面呈现NW-SE向厚薄相间分布,其方向与研究区总体褶皱方向一致。局部厚度变化特征方面与断层走向及褶皱轴向关系密切。因此,排除该煤层原生沉积影响因素,断裂构造与褶皱构造以及褶皱作用伴生的层滑构造为区内煤层厚度变化的主要控制因素。

     

    Abstract: Sunan mining area plays an important role in Huaibei coalfield and coal seam 72 is one of the minable coal seams in the mining area. Geological exploration data show that the change of coal seam is large and it's thickness variation is obvious. Based on the research of mine geological survey and geological structure, it is found that the coal structure is broken, and the thickness variation of coal seam is closely related to the geological structure in the area. The distribution of coal thickness shows NW-SE alternative thickening and thining, the direction is the same as the overall fold direction. The local thickness variation is closely related to the trend of the fault strike and the axial direction of the fold. Therefore, excluding the impact of the coal seam of primary sedimentary factors, the faults, the folds and the layer slip structure associated with fold action mainly control the thickness variation of coal seam.

     

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