摘要
保山市金厂矿区铜、铅锌均为隐伏矿体,埋藏于高中山斜坡之下,属于一个完整的斜坡径流-埋藏水文地质单元区。区内构造断裂控水、裂隙网络系统赋水、较强地下水径流带和高水头承压水等,对该矿床今后的斜坑采矿来讲,坑内充水因素复杂,水文地质条件类型比较特殊。
The blind ore body of Jinchang Cu,Pb-Zn orefield in Baoshan is buried under the slope of highmiddle mountain,belonging to a complete slope run-off buried hydrogeological unit area. In this area,water control of fault,water-bearing of fissure network system,intense underground water run-off zone and high water head pressure water,etc,for the oblique shaft mining of this deposit in the future,water filling factor is complicated and geohydrological condition is particular.
出处
《云南地质》
2017年第2期292-295,共4页
Yunnan Geology
关键词
金厂矿区
矿坑充水因素
Jinchang Orefield
Water Filling Factor
