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相山铀矿田邹家山矿床成矿流体特征
引用本文:郭建,李子颖,李秀珍,聂江涛,王健. 相山铀矿田邹家山矿床成矿流体特征[J]. 铀矿地质, 2014, 0(5): 263-270
作者姓名:郭建  李子颖  李秀珍  聂江涛  王健
作者单位:核工业北京地质研究院中核集团铀资源勘查与评价技术重点实验室,北京100029
摘    要:通过流体包裹体的岩相学研究、显微测温和激光拉曼探针测试,探讨了邹家山铀矿床成矿流体特征、演化及矿质沉淀方式。研究结果表明,该矿床的成矿流体为中低温热液,碳氢化合物对铀的富集具有不可忽视的作用,流体持续的沸腾作用是矿质沉淀的主要因素。

关 键 词:邹家山铀矿床  流体包裹体  流体沸腾  成矿机制  相山

Mineralization Fluid Features of Zouj iashan Uranium Deposit in Xiangshan Ore field,Jiangxi
GUO Jian,LI Zi ying,LI Xiu zhen,NIE Jiang tao,WANG Jian. Mineralization Fluid Features of Zouj iashan Uranium Deposit in Xiangshan Ore field,Jiangxi[J]. Uranium Geology, 2014, 0(5): 263-270
Authors:GUO Jian  LI Zi ying  LI Xiu zhen  NIE Jiang tao  WANG Jian
Affiliation:( CNNC Key Laboratory of Uranium Resource Exploration and Evaluation Technology, Beijing Research Institute of Uranium Geology, Beijing 100029, China)
Abstract:Based on the petrographic analysis,temperature measurement,laser Raman study of fluid inclusion,this paper discussed the features, evolution and precipitation forms of mineralization fluids. According to the research,the fluid belong to middle low temperature and uranium was transported by carbon dioxide and organic matter,fluid boiling is suggested to be the main mechanism for metal precipi-tations in this deposit.
Keywords:Zoujiashan uranium deposit fluid inclusions fluid boiling mineralization mechanism Xiangshan
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