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内蒙古赤峰莲花山金矿床成矿物理化学条件及成矿机理
引用本文:姜能,张文淮.内蒙古赤峰莲花山金矿床成矿物理化学条件及成矿机理[J].地球化学,1996,25(1):73-83.
作者姓名:姜能  张文淮
作者单位:中国科学院地质研究所,中国地质大学
摘    要:在对莲花山金矿床Au的成矿阶段划分的基础上,对与Au的主要成矿阶段密切相关的石英进行了流体包裹体的显微测温和气液相成分分析,结合其他分析结果和资料,确定出成矿流体的性质、盐度和密度;成矿过程的温度、压力、氧逸度和硫逸度以及成矿环境和pH、Eh值等Au的成矿物理化学条件。最后探讨了Au的活化、迁移和沉淀机理,认为导致本矿床Au的沉淀有两种机制,即沸腾去气机制和流体混合机制。

关 键 词:金矿床  物理化学条件  液包体

PHYSICO-CHEMICAL CONDITIONS AND MECHANISM OF MINERALIZATION OF LIANHUASHAN GOLD DEPOSIT, CHIFENG, INNER MONGOLIA
Jiang Neng.PHYSICO-CHEMICAL CONDITIONS AND MECHANISM OF MINERALIZATION OF LIANHUASHAN GOLD DEPOSIT, CHIFENG, INNER MONGOLIA[J].Geochimica,1996,25(1):73-83.
Authors:Jiang Neng
Abstract:Microthermometry and compositional analysis are carried out on fluid inclusions hosted in quartz which is intimately associated with gold mineralization. The composition, sality and density of mineralizing fluids, the p-T conditon of fluid entrapment and other physico-chemical parameters such as pH, Eh, fo2 and fs2 are calculated based on the theory of fluid inclusion geochemistry. Finally, two kinds of mechanism are sugessted for the precipitation of gold. They are boiling-degassing and mixing of fluid.
Keywords:gold deposit  fluid inclusion  physico-chemical condition  metallogenetic mechanism  Inner Mongolia  
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