摘要
南翁丢铅锌矿位于扬子准地台与华南褶皱带的接触带部位,其矿体分布受区域构造控制,主要矿化物为闪锌矿、方铅矿。该文结合区域地质背景,分析该铅锌矿地质特征,地球化学特征,对其成矿机制进行探讨。
Nanwengdiu lead-zinc deposit is located in the contact zone between Yangtze quasi-platform and South China fold belt.Its orebody distribution is controlled by regional structure.The main minerals are sphalerite and galena.Based on the regional geological background,this paper analyzes the geological characteristics and geochemical characteristics of the lead-zinc deposit,and discusses its metallogenic mechanism.
作者
罗强
Luo qiang(Institute of Geophysical and Geochemical Survey,Guizhou Geology and Mineral Exploration and Development Bureau,Guiyang 550000,China)
出处
《有色金属设计》
2019年第3期82-84,87,共4页
Nonferrous Metals Design
关键词
铅锌矿
地球化学
矿产成因
地质特征
Lead-zinc deposit
Geochemistry
Deposit genesis
Geological characteristics
