摘要
辛置煤矿位于郭庄泉域东南角,临汾断陷盆地水文地质单元的东北部,地处两个水文地质单元的交接带。东有近南、北向的霍山大断裂,西为赤峪断层,北为李曹断层,将辛置煤矿区切割成具有相对独立水文地质特征的地段。本文对该矿井地质构造特征和陷落柱发育规律进行研究,分析了F28和F34组成的地堑构造对井田内地下水径流方向的影响,并对矿井主要含水层水化学特征进行对比分析,得出了辛置矿区地下水运移规律。
Xinzhi coal mine is located in the southeast corner of the Guozhuangquan domain, the northeast of the hydrogeological unit of Linfen fault basin and the junction region of the two hydrogeological units. East has near south, north to the Huoshan fault, Chiyu fault is in the west, there is Licao fault in the north, the Xinzhi coal mine areas are cut into the sections of which has relatively independent hydrogeological characteristics. In this paper the mine geological structure characteristics and subsided column development laws were studied. The f28 and F34 graben structure influence on groundwater flow direction in mine field are analyzed and the mine mainly containing aquifer water chemical characteristics are contrasted and analyzed. The migration law of groundwater flow direction in Xinzhi mining area is obtained.
出处
《山西焦煤科技》
2016年第1期43-45,共3页
Shanxi Coking Coal Science & Technology
关键词
地下水
断层
控水
陷落柱
化学特征
Groundwater
Fault
Controlling water
Collapse column
Chemistry characteristics
