福建省双旗山浅成脉型金矿地质及其意义  

The Geological Characteristics and Its Significance of Shuangqishan Gold Deposit of Epithermal and Vein Type in Fujian Province

作　　者：刘连登[1] 陈国华[1] 刘允良 许锦雄[2] 谢文清[2] 宋开族[2] 

机构地区：[1]长春科技大学 [2]福建省双旗山金矿

出　　处：《福建地质》1999年第2期51-58,共8页Geology of Fujian

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.Its 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 deposits natural characteristics in this paper,It is identified that its 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.

关 键 词：浅成脉型金矿 成矿环境 矿床本质特征 金矿床 

分 类 号：P618.510.2[天文地球—矿床学] P618.510.5[天文地球—地质学]