长江下游皖中南地区块状硫化物矿床成因及找矿探讨  

Discussion on the genesis and prospecting of massive sulphide deposits in the central and southern parts of the Yangtze River

作　　者：程超杰 CHENG Chao-jie(East-China Metallurgical Institute of Geology and Exploration,Hefei 230088,China)

机构地区：[1]华东冶金地质勘查研究院

出　　处：《世界有色金属》2019年第15期234-235,共2页World Nonferrous Metals

摘　　要：通过地质勘测和同位素检测,对安徽铜陵矿区内硫化物的成因进行分析,硫化物矿床的成因主要在于石炭纪海底热水活动,硫化物矿的主要矿源是来自于海水硫酸盐。本文对安徽铜陵矿区内的块状硫化物的成矿原因以及对矿物的寻找标志进行讨论。Through Geological Survey and isotopic detection,the cause of sulphide in tongling mining area of Anhui province was analyzed.The main cause of sulphide deposit was the activity of seabed hot water in carboniferous period.The main source of sulphide deposit was seawater sulfate.This paper discusses the metallogenic causes of massive sulfides in Tongling area of Anhui Province and the finding marks of minerals.

关 键 词：铜陵矿区 成矿原因 找矿标志 

分 类 号：P618.2[天文地球—矿床学]