Discussion on Fluid Inclusions in Quartz Veins of Shazijiang Uranium State w:st="on">Ore Deposit, Northern Guangxi
详细信息
- 责任者：Shi Shaohua (State Key Laboratory of Ore Deposit Geochemistry ; Institute of Geochemistry ; Chinese Academy of Sciences ; Guiyang 550002 ; China) ; Hu Ruizhong
- 刊名：Mineral Deposits
- 出版年：2011
- 卷期：30(1)
- 关键词：铀矿 ; uranium ores ; 流体包裹体 ; fluid inclusions ; 广西 ; Guangxi Province
- 页码：p.33-44
- 图表：5 illus., 1 tanle, 49 refs.
- 分类号：1001
- issnNo：ISSN0258-7106
- isbnNo：CN11-1965/P
摘要
The Miaoershan uranium orefield, one of the five large-size uranium orefields in central South China, hosts the Chanziping uranium ore deposit, which is the largest carbonaceous-siliceous-pelitic rock type uranium ore deposit in China, and some granite uranium ore deposits. A series of petrographic,microthermetric and Laser Raman microspectroscopic studies of fluid inclusions (FI) in the quartz veins of the Shazijiang uranium ore deposit, one of the important granite-hosted uranium ore deposits in the orefield, were carried out by the authors. Meanwhile, hydrocarbon-rich host granite created favorable conditions for uranium ore body preservation. The hydrocarbon is composed of lots of saturated hydrocarbon, benzene, olefin and bitumen.