江西414矿床矿物包裹体研究  

THE STUDY ON FLUID INCLUSION IN MINERAL FROM No. 414 ORE DEPOSIT,JIANGXI

作　　者：谢世业[1] 林德松[1] 

机构地区：[1]中国有色金属工业总公司矿产地质研究院

出　　处：《矿产与地质》1994年第2期114-118,共5页Mineral Resources and Geology

摘　　要：重点研究了４１４矿床石英流体包裹体特征及成矿物理化学条件，其成矿温度４９０～５３０℃；成矿压力为１０８０×１０￣５Ｐａ；成矿溶液的ｐＨ值为４．８２～４．８３；Ｅｈ值为－０．４２５～－０．４３６伏特，ｆｏ＿２：为１０￣（－３０．４４）～１Ｏ￣（－３０．０９）。In this paper,the character and homogenization temperatuer of fluid inclusions in quartz from No.414 oredeposict,Jlangxi and their ore- forming physico-chemical condition were studied. The Mineralization occurred at490℃-530℃ with 1080×10￣5pa,pH 4.82～4.83,Eh-0.425～-0.436 V and fo_2 10￣(-30.44)～10￣-(30.09)in the oresolution.

关 键 词：金属矿床 钼 钨 矿物包体 矿化 

分 类 号：P618.204[天文地球—矿床学]