CAJ | 학술논문

重庆市渝东南渝东北碳酸盐岩地区岩溶发育程度以灰岩类最发育，白云岩类次之，泥质灰岩类发育最弱；灰岩中的岩溶大泉、暗河数量多于白云岩类，白云岩中的岩溶大泉和暗河数量远远大于泥质、硅质岩类；而钻井成井率大小为白云岩类>灰岩类>泥质、硅质类。在岩溶找水工作中，不同地区应因地制宜，选择不同的找水方式。
중경시투동남투동북탄산염암지구암용발육정도이회암류최발육，백운암류차지，니질회암류발육최약；회암중적암용대천、암하수량다우백운암류，백운암중적암용대천화암하수량원원대우니질、규질암류；이찬정성정솔대소위백운암류>회암류>니질、규질류。재암용조수공작중，불동지구응인지제의，선택불동적조수방식。
There is the most development degree of karst development in the limestone, the dolomite second, the argilla-ceous, siliceous limestone is weakest development in the Chongqing southeast and Chongqing northeast carbonate area; In the number of the karst springs and underground rivers, the limestone's number is more than the dolomite's, the dolomite's number of far more than the argillaceous, siliceous limestone's; In the number of the well completion, the dolomite>the limestone>the argillaceous, siliceous limestone. So, the different regions should adjust measures to local conditions, and choose the dif-ferent ways in the work of looking for the karst groundwater water.