世界有色金属Issue(6)：119-121,3.
冬瓜山铜矿大团山矿床深部水文地质特征及充水因素分析
Analysis of Deep Hydrogeological Characteristics and Water Filling Factors of the Datuanshan Deposit in Dongguashan Copper Mine
刘形林1
作者信息
- 1. 铜陵有色金属集团有限公司,安徽 铜陵 244000
- 折叠
摘要
Abstract
Through the analysis of the hydrogeological characteristics and genesis of the deep(-730m～-1000m)and 36A～43 lines of the Datuanshan copper deposit in Dongguashan,the study shows that the main ore body of this deposit is located below the local erosion benchmark,and the terrain is favorable for precipitation discharge.Surface water does not constitute the main water filling factor of the deposit.The underground water of the deposit mainly exists at a depth of-200 meters or more,with karst fissures containing water.The main aquifer is the Triassic carbonate rock,with a moderate to weak degree of water abundance.The groundwater in the ore deposit is replenished by precipitation,and the deep groundwater locally receives recharge from upper overflow and axial deep groundwater runoff.关键词
大团山矿床/地下水/岩溶裂隙Key words
Datuanshan deposit/Groundwater/Karst fissure分类
天文与地球科学引用本文复制引用
刘形林..冬瓜山铜矿大团山矿床深部水文地质特征及充水因素分析[J].世界有色金属,2024,(6):119-121,3.
