安徽省贵池区银坑洞银多金属矿地质特征及控矿因素浅析  

Geological characteristics and ore controlling factors of Yinkengdong silver polymetallic deposit in Guichi District,Anhui Province

作　　者：秦立平 QIN Li-ping(Geological Team of Anhui Provincial Bureau of Geology and Mineral Exploration,Anqing 246003,China)

机构地区：[1]安徽省地质矿产勘查局311地质队,安徽安庆246003

出　　处：《世界有色金属》2022年第19期67-69,共3页World Nonferrous Metals

摘　　要：当前多金属矿产的地质找矿已经成为发掘矿产资源的重点,对地质经济问题有着直接的影响。因此对多金属矿的地质特征以及多金属矿的找矿前景进行深入分析与总结。工作区位于高坦断裂北侧,陈塘-灌口向斜南翼,该区经受了长期复杂的历史演变及多期次的构造活动,具有多期多次活动的特征。为配合项目地质工作的开展,在区内同时进行1:10000水系沉积物测量及高精度磁法测量工作,查明区内的地球物理和地球化学特征。At present, the geological prospecting of polymetallic minerals has become the focus of mining mineral resources,which has a direct impact on geological and economic problems. Therefore, the geological characteristics of polymetallic ores and the prospecting prospects of polymetallic ores are analyzed and summarized in depth. The working area is located at the north side of Gaotan fault and the south wing of Chentang Guankou syncline. The area has experienced a long and complex historical evolution and multiple tectonic activities, with the characteristics of multiple periods and multiple activities. In order to cooperate with the geological work of the project, 1:10000 river sediment survey and high-precision magnetic survey are carried out in the area at the same time to identify the geophysical and geochemical characteristics of the area.

关 键 词：中低温热液型矿床 铁帽型 地质特征 控矿因素 

分 类 号：P618.2[天文地球—矿床学]