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韦州煤田位于鄂尔多斯盆地西缘中段,属石炭—二叠纪煤田,煤炭资源丰富。运用地质力学观点,依据近年来本区研究成果及最新的地震、钻探等地质资料,分析认为:韦州煤田主体构造为一不对称向斜构造,轴向北北西,北端延至区外,南端在下马关附近翘起而收敛,轴部地层由石炭—三叠系组成,向北轴部地层逐渐变新;西翼倾角陡,东翼较缓,向斜内次级断层较发育,造成煤层的重复或断失。
Weizhou Coalfield is located in the middle of the western Ordos Basin, is a Carboniferous - Permian coalfield, rich in coal resources. Based on the geomechanical view, based on the research results of the area in recent years and the latest geological data such as earthquakes, drilling and so on, the author thinks that the main structure of Weizhou Coalfield is an asymmetrical syncline structure with north-west axis and north-to-north extension, The lower part of the Guanzhang warped and converged. The shaft formation was composed of Carboniferous-Triassic and gradually changed into a northward-axial formation. The west wing had a steep dip with a slow east wing and a more developed secondary fault in the syncline, resulting in a Repeat or lost.