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煤炭是我国的基本能源,煤系地层的区域地质是决定采矿方法的重要依据。现采用普查与翻阅资料结合的方法,得到邯西矿区区域地质概况,认为该区域地层由老到新依次为:奥陶系、石炭系、二叠系、三叠系、第四系构成,构造形态以NE向的断裂构造为主,伴有向东南倾伏的褶曲构造,本区域还有零星岩浆岩。经研究,为安全采矿做好基础性研究。
Coal is the basic energy of our country. The regional geology of the coal measure strata is an important basis for determining the mining method. By using the combination of census and flipping through the data, the regional geology of the Hanxi mining area is obtained. The strata of the area from Ordos to Carbonate are: Ordovician, Carboniferous, Permian, Triassic and Quaternary The morphology is dominated by the NE-trending fault structure, with a convoluted to the southeast fold structure and scattered magmatic rocks in this area. After research, make basic research for safe mining.