摘要
阳山金矿区第四系残坡积物分布面积较广,厚度较大。地下水有孔隙潜水、基岩裂隙水和构造带脉状裂隙水三种类型。地下水在各种含水介质中运移时,在宏观与微观上具有不同的规律。借助计算机技术对矿区地下水等水头线进行了模拟,确定了区内地下水流的运移规律。
The Quaternary thick eluvium and sliderock are dispersed over the Yangshan Au ore belt. The groundwater is composed of pore water, bedrock fissure water and vein - like fissure water in structural zones. The equipotential lines of the groundwater in the ore zone are simulated on a computer. Laws of migration of the groundwater flow in the Anba ore block are defined.
出处
《四川地质学报》
2007年第1期37-39,共3页
Acta Geologica Sichuan
