研究区域采区内裂隙水发育,分布变化较快,地下水变化较为复杂,并且采坑边坡已有多处滑塌破坏发生,增加了后期边坡治理的难度。利用高密度电法和地质雷达对9个断面进行勘探观察。所勘探区下部视电阻率较低存在地下裂隙水,且地下多板岩破碎带以及断层破碎带。 In the study area, the fissure water in the mining area is developed and distributed rapidly, and the groundwater changes more complicatedly. In addition, many landslides have occurred in the mining slope, which makes it more difficult for later slope treatment. 9 sections were surveyed by using high-density electric method and GPR. The lower apparent resistivity in the exploration area is lower with underground fissure water, underground multi-slate fracturing zone and fault fracture zone.