贵州省烂泥沟金矿深部水文地质特征初探——以磺厂沟矿段为例  

Preliminary study on the deep part hydrogeological characteristics of Lannigou gold mine Guizhou Province:taking the Huangchanggou ore section as an example

作　　者：陈川[1] 杨秀德[1] 王伟[1] 侯江勇[1] CHEN Chuan;YANG Xiude;WANG Wei;HOU Jiangyong(117 Geological Brigade,Bureau of Geology and Mineral Resources of Guizhou Province,Guiyang 550018,Guizhou,China)

机构地区：[1]贵州省地矿局117地质大队,贵州贵阳550018

出　　处：《吉林地质》2023年第3期73-78,共6页Jilin Geology

摘　　要：由于烂泥沟金矿区磺厂沟矿段水文地质条件是最初的以基岩裂隙潜水直接充水为主的简单类型,逐渐向碳酸盐岩溶水和构造裂隙承压温热水直接充水为主的复杂类型发生变化。因此在以往勘查工作成果的基础上,通过对磺厂沟矿段37号矿体11~31勘探线深部进行水文地质研究工作,初探烂泥沟金矿深部水文地质特征,对今后矿山勘查及防治水措施工作有一定的指导意义。The hydrogeological conditions of the Huangchanggou section in the Lannigou gold mining area have changed gradually from the initial simple type of direct water-filling mainly in the bedrock fissure phreatic water to the complex type of direct water-filling mainly in the carbonate karst water and the pressure-bearing warm water in the structural fissure.Based on the achievement of previous exploration work,the hydrogeological research of Lannigou gold deposit in the depth of the Exploration Line 1131 of No.37 ore body in the Huangchanggou mine section are studied.It has certain guiding significance for the future mine exploration and water prevention and control measures.

关 键 词：磺厂沟 金矿体 断裂 深部水文地质 

分 类 号：P618.51[天文地球—矿床学] P641.4[天文地球—地质学]