摘要
近年来,鉴于微细浸染型金矿的特殊成因及巨大矿藏潜力,国家以及相关的地质工作者加大了对该类矿床类型的研究和勘探,并将它分离为一种相对独立的矿床种类。本文通过研究赣西萍乐地区微细浸染型金矿成矿地质条件以及矿床特征,探讨了细浸染型金矿床的成矿原因,以供相关地质工作者参考和研究。
In recent years, in view of the special genesis and huge potential of micro-disseminated gold deposits, the state and relevant geologists have intensified the research and exploration of this type of deposits, and separated it into a relatively independent type of deposits. By studying the metallogenic geological conditions and characteristics of fine disseminated gold deposits in Pingle area, western Jiangxi Province, the metallogenic causes of fine disseminated gold deposits are discussed for reference and study by relevant geologists.
作者
李凡顺
裴阳
LI Fan-shun;PEI Yang(Jiangxi Geological Survey Brigade of Jiangxi Provincial Bureau of Geological and Mineral Exploration and Development,Nanchang 330030,China)
出处
《世界有色金属》
2018年第23期79-80,共2页
World Nonferrous Metals
关键词
赣西
赣西微细浸染型金矿
成矿流体特征
成矿成因
western Jiangxi
fine disseminated gold deposits in Western Jiangxi
characteristics of ore-forming fluids
metallogenic genesis