平朔矿区井工矿井的充水水源有第四系孔隙水及地表水、石炭—二叠系砂岩裂隙水、奥陶系灰岩岩溶裂隙水。
Water filling sources of underground mine in Pingshuo mining area have Quaternary pore water, surface water, Permo-Carboniferous sandstone fissure water and Ordovician limestone karstic fissure water.
利用实例说明了该技术在识别断层及其它构造、解释煤层厚度变化、预测奥陶系灰岩岩溶裂隙等的具体应用情况。
Some application examples, including detecting faults, interpreting the thickness variation of coal seams, and predicting karst fractured zones in carbonate rocks were given.
寒武系、奥陶系地层主要为灰岩和白云岩，其问赋存有较丰富的岩溶裂隙水。
There is abundant karst fissure water in the limestone and dolomite of Cambrian and Ordovician.
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