Geological Characteristics and Fluid Inclusion Studiesof the Baogutu Porphyry Copper Deposit in West Junggar of Xinjiangoft-com:office:office" />

• 责任者：Guan Weina (College of Geosciences and Resources Engineering ; Urümqi 830049 ; China) ; Dong Lianhui
• 刊名：Chinese Journal of Geology
• 出版年：2010
• 卷期：45(3)
• 关键词：斑岩铜矿床 ; porphyry copper deposit ; 斑岩钼矿床 ; porphyry molybdenum deposit ; 新疆 ; Xinjiang
• 页码：p.873-884
• 图表：7 illus., 1 table, 14 refs.
• 分类号：1001
• issnNo：ISSN0563-5020
• isbnNo：CN11-1937/P

The Baoguto porphyry copper deposit locates in south of the Darbut magmatic arc of the western Junggar. The north-east regional structure mainly composed by a series of major faults. The Baogutu intrusion is intermediate porphyry with several lithologies and lithofacies. Mineralization type is disseminated mineralization，veinlets and network mineralization. The ore-forming process can divided into three phases. Fluid inclusions data showed：homogenization temperatures from the first stage to the third stage gradually reduced, indicating that mineralization from early and late going through a cooling process.oft-com:office:office" />