贵州及邻省区与蒸发岩和油气有关的汞矿成矿物理化学条件  

Physicochemical Condition of the Hg Ore deposits Related to Evaporite Rocks and the Oil-gas in Guizhou and the Neighboring Areas

作　　者：刘平[1] 

机构地区：[1]贵州省地矿局106地质大队,贵州遵义563000

出　　处：《贵州地质》2002年第3期156-162,共7页Guizhou Geology

摘　　要：对区域汞矿床中辰砂及其共生的脉石矿物的同位素组成和矿物包裹体成分的研究 ,讨论了所论汞矿成矿的物理化学条件。结合四川、重庆等地现代卤水 (黄卤、黑卤 )的对比研究和分析 。The physicochemical condition of the Hg ore deposits is put forward for discussion by the cinnabarite study in the Hg ore deposits of Guizhou, its isotopic composition of intergrowth veinstone minerals and associated mineral inclusion composition. In association with the contrastive analysis and study on the modern bitterns from Sichuang province, Chongqing and the other places, it is believed that the yellow bittern and black bittern may belong to the connate thermal bitterns with ore-forming potential.

关 键 词：蒸发岩 油气 汞矿床 物理化学条件 贵州 矿物包裹体 硫同位系 成矿作用 

分 类 号：P618.68[天文地球—矿床学]