摘要
浙江武义萤石矿田中金（银）－萤石矿床，是中国首次发现并厘定的元素地球化学性质迥异，但物源、力源又相同，受同构造控制，形成于同一成矿期不同成矿阶段的金（银）－萤石矿床新类型。矿床严格受控于盆地构造格局的时空演化规律和帚状控矿构造型式，对中国东部中生代火山岩带萤石矿田（床）中金（银）矿的寻找具有极为重要的实践和理论价值。
The Au(Ag) fluorite ore deposit, a new type of gold deposits, is hosted in the Wuyi fluorite ore field, Zhejiang Province. Studies show that the electrum and the fluorite in the ore deposit were formed by the same origin and controlled by the same fault. Further studies show that the metallization of this deposit is closely related to the tectonic evolution of the Wuyi Basin, especially to the broom structural type. There are significant effects for predicting this kind of ore deposit in the fluorite ore field located in the Mesozoic volcanic rock belt of the eastern China.
出处
《成都理工学院学报》
CSCD
1999年第2期107-112,共6页
Journal of Chengdu University of Technology
关键词
武义盆地
控矿构造型式
金矿
银矿
萤石矿田
Wuyi Basin
Au(Ag) fluorite ore deposit
ore controlling structural type
