基于三维地震勘探的巴拉素煤矿22盘区地质构造研究

Geological structure of 22-panel area of Balasu Coal Mine based on three-dimensional seismic exploration

  • 摘要: 【目的及方法】为解决巴拉素煤矿22盘区地质构造复杂、原有勘探成果精度不足的问题,采用三维地震勘探技术系统研究区域地质构造特征。【结果】结果发现,区域共解释5条小型正断层(落差<;5 m),以EW/N-S走向为主,最大延伸长度150 m,对煤层开采的影响有限;2号、3号、8号煤层底板起伏平缓(倾角0°~5°),东西部呈相反倾斜方向,与相邻煤层形态高度一致;2号煤层厚4.4~5.3m(西厚东薄),3号煤层厚4.3~6.5 m (厚—薄—厚变化),8号煤层厚1.4~1.7 m (北厚南薄);未发现陷落柱、岩浆岩等灾害性地质体。【结论】研究为巴拉素煤矿22盘区开采和设计提供了重要地质依据。

     

    Abstract: Aiming at the problems of complex geological structure and insufficient accuracy of previous exploration results in the 22-panel area of Balasu Coal Mine, this study adopts 3D seismic exploration technology to systematically study regional geological structure characteristics.The results show that there are five small normal faults(drop <5 m) in the region, mainly EW/N-S strike, with a maximum extension length of 150 m, which has limited influence on coal seam mining.The floor of coal seam No.2, 3 and 8 has gentle fluctuation(dip Angle 0°~5°), and the east and west are opposite inclined direction, which is consistent with the shape of adjacent coal seams.The thickness of No.2 coal seam is 4.4~5.3 m(thick in the west and thin in the east), No.3 coal seam is 4.3~6.5 m(thick-thin-thickness change), and No.8 coal seam is 1.4~1.7 m(thick in the north and thin in the south).No catastrophic geological bodies such as collapse columns and magmatic rocks were found.The study provides important geological basis for the mining and design of the 22-panel of Balasu Coal Mine.

     

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