摘要
金牛山金矿床的石英包裹体划分为纯液相包裹体、气液相包裹体和ＣＯ２三相包裹体三种类型，均一温度在１５０～３００℃，主成矿温度在１９０～２１０℃之间。研究表明成矿热液由南向北运移。
Three types of fluid inclusions have been found in quartz of the Jin Niushan gold deposit, they are liquid inclusions, gasliquid inclusions or gasliquid and CO2 gas inclusions. Their homogeneity temperatures vary from 150℃ to 300℃. The main oreforming temperature is 190℃￣210℃. It is shown by this paper that the oreforming fluids moved from south to north.
出处
《矿产与地质》
1998年第4期246-249,共4页
Mineral Resources and Geology
关键词
金矿床
均一温度
金牛山
液包体
类型
Jin Niushan, Gold deposit, Inclusions, Homogeneity temperature
