赣西微细浸染型金矿床成矿流体特征及成因探讨  

Characteristics and genesis of ore-forming fluids in micro-disseminated gold deposits in Western Jiangxi

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)

机构地区：[1]江西省地质矿产勘查开发局赣西地质调查大队,江西南昌330030

出　　处：《世界有色金属》2018年第23期79-80,共2页World Nonferrous Metals

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.

关 键 词：赣西 赣西微细浸染型金矿 成矿流体特征 成矿成因 

分 类 号：P618.51[天文地球—矿床学]