摘要
福建省双旗山金矿，主要由１３、１４、２１和２２号等金矿脉组成。尽管为一小型金矿床，但目前其黄金产量仅次于福建省紫金山铜金矿，而居全省第二位。双旗山金矿的成矿地质环境和矿床本质特征，表明其为形成于晚白垩世的浅成脉型金矿，是福建省重要的金矿类型之一，有良好的找矿前景。
The Shuangqishan gold deposit consists of many lodes,such as No.13、14,21 and 22 lode,etc.Its a small scale one,and its output of gold is just less than the Zijishan Cu Au deposit,but takes the second place in the whole province up to now.Studying of the mineralization and geological envirionment and the deposits natural characteristics in this paper,It is identified that its an epithermal and vein type gold deposit which formed in the early Cretoceous Era.It is the most important type of gold in Fujian Province,and has the good prospects of looking for this type of mineral deposit.The Shuangqishan gold deposit is a typical one.
出处
《福建地质》
1999年第2期51-58,共8页
Geology of Fujian
关键词
浅成脉型金矿
成矿环境
矿床本质特征
金矿床
epithermal and vein type of gold deposit,mineralization and geological envirionment,the deposits natural characteristics Shuangqishan,Fujian Province
