Fluid Inclusion and Carbon Oxygen Isotope Studies of Qiongbulake Copper Deposit in oft-com:office:smarttags" />Awulale Mountains
详细信息
- 责任者：Luo Yong (Guangzhou Institute of Geochemistry ; Chinese Academy of Sciences ; Guangzhou 510640 ; China) ; Liao Siping
- 刊名：Mineral Deposits
- 出版年：2011
- 卷期：30(3)
- 关键词：铜矿 ; copper ores ; 流体包裹体 ; fluid inclusions ; 新疆 ; Xinjiang
- 页码：p.547-556
- 图表：6 illus., 3 tables, 37 refs.
- 分类号：1001
- issnNo：ISSN0258-7106
- isbnNo：CN11-1965/P
摘要
Located in Yining County of Xinjiang, the Qiongbulake copper deposit was formed in relation to magmatic hydrothermal fluids. These fluids formed a stockwork of calcite veinlets. On the basis of the studies by means of inclusion petrography, microthermometry and carbon, oxygen stable isotope, the authors systematically studied characteristics of the ore-forming fluids and the origin of the Qiongbulake copper deposit. Three types of fluid inclusions in calcite were recognized. On the whole, the Qiongbulake copper deposit is a moderate-low hydrothermal ore deposit. oft-com:office:office" />