摘要
江武义金（银）－萤石矿床，属燕山晚—末期成矿作用的产物。成矿期构造活动的多期次脉动特征，导致了成矿的多期、多阶段性的演变特征与规律。这一新类型金（银）矿的发现与研究，对指导金（银）－萤石矿床的找矿实践和矿产的综合开发利用具有重要的现实意义。
The characteristics of multistage metallization is decided by the multiperiodic activity of ore controling structure. Studies show that the Au(Ag) fluorite ore deposit, a new type of gold deposits, was formed in the late stage of Yanshan and has been hosted in the Wuyi fluorite ore field. There are three metallogenic epoches and eight mineralization (sub )stages for its ore forming process and evolution.
出处
《成都理工学院学报》
CSCD
1999年第2期113-118,共6页
Journal of Chengdu University of Technology
关键词
武义盆地
金(银)-萤石矿床
成矿期与成矿阶段
Wuyi Basin
Au(Ag) fluorite ore deposit
metallization epoches and mineralization stages
