Geological Characteristics of East Gobi Molybdenum Deposit in Xinjiang and Hydrothermal Mineralization Stages and Mineral Paragenesis in the Deposit
详细信息
- 责任者：Yang Zhiqiang (No.2 Geological Survey Institute ; Henan Geological Survey Bureau ; Xuchang 461000 ; China) ; Li Zhanming
- 刊名：Contributions to Geology and Mineral Resources Research
- 出版年：2013
- 卷期：28(4)
- 关键词：斑岩钼矿床 ; porphyry molybdenum deposit ; 天山 ; Tianshan Mountains
- 页码：p.514-523
- 图表：13 illus., 4 refs.
- 分类号：1001
- issnNo：ISSN1001-1412
- isbnNo：CN12-1131/P
摘要
libri" size="3">East Gobi molybdenum deposit in Xinjiang is the first super-large deposit discovered in north- west China. It is located near the Yamansu fault and occurrs in low grade metamorphic Lower Carbonifer- ous clastic rock intercalated with volcanic rocksl. According to cutting relation of ore veins hydrotrhermal mineralization in the deposit is divided into 4 stages and mineral paragenesus is determined on basis of cut- ting, replacement and edge share relation of the minerals.