CAJ | 학술논문

南桐煤矿在多年采动影响下，P3 c含水层地下水形成一个由离层裂隙导通的“地下水库”， T1 j含水层地下水形成一个有拉张裂隙导通的“统一含水体”。结合矿区实际情况，得出含水层破坏的三种破坏模式分别为：采动破坏、封闭不良钻孔破坏和导水断层破坏。T 1 j地层的“统一含水体”和P3 c地层中的“离层裂隙储水带”为中国南方丘陵山区采煤沉陷区寻找地下水资源的有利区域。
남동매광재다년채동영향하，P3 c함수층지하수형성일개유리층렬극도통적“지하수고”， T1 j함수층지하수형성일개유랍장렬극도통적“통일함수체”。결합광구실제정황，득출함수층파배적삼충파배모식분별위：채동파배、봉폐불량찬공파배화도수단층파배。T 1 j지층적“통일함수체”화P3 c지층중적“리층렬극저수대”위중국남방구릉산구채매침함구심조지하수자원적유리구역。
After mining over years ,P3 c aquifer groundwater formed an “underground reservoir”conducted by separated fissures and T 1 j aquifer groundwater formed an “unified aquifer” conducted by extensional fissures in Nantong coal mine .We conclude that aquifer destruction patterns are :mining destruction ,destruction of sealed adverse borehole destruction of water conductive fault .The “unified Aquifer” in T1 j and “underground reservoir” in P3 c are favorable area for searching groundwater in hilly mining subsidence area in Southern China .