摘要
本文简述了兴海县某银多金属矿区水文地质概况,分析了含水岩组特征,查明了矿区水文地质条件,总结了矿床充水因素。研究表明:矿区主要充水含水层为基岩风化带和构造裂隙带,富水性弱至中等,水文地质类型为第二类,勘探复杂程度为第一型。
In this paper, the hydrogeological Survey of a silver polymetallic mining area in Xinghai County is described, the hydrogeological conditions in the mining area are ascertained, and the water filling factors are summarized. The study shows that the main aquifer is the bedrock weathering zone and the tectonic fissure zone, the hydrogeological type is the second type and the exploration complexity is the first type.
作者
杨延林
漆颖超
高荣辉
YANG Yan-lin, QI Ying-chao, GAO Rong-hui(Tibetan institute of Nuclear Geology, Chengdu 610052,Chin)
出处
《世界有色金属》
2018年第2期200-200,202,共2页
World Nonferrous Metals
关键词
银多金属矿
矿床充水因素
水文地质条件
Silver polymetallic deposit
water filling factor
hydrogeological condition
