| New titanite U–Pb and molybdenite Re–Os ages for a hydrothermal vein-type Cu deposit in the Lanping Basin, Yunnan, SW China: constraints on regional metallogeny and implications for exploration | |
Juan Li; Lei-Luo Xu ; Xian-Wu Bi; Yong-Yong Tang; Xiang-Yuan Sheng; Hai-Jun Yu; Gong Liu; Rui Ma
| |
| 2021 | |
| Source Publication | Mineralium Deposita (IF:3.396[JCR-2016],3.563[5-Year]) |
| Volume | 56Issue:3Pages:441-456 |
| DOI | 10.1007/s00126-020-00973-x |
| URL | 查看原文 |
| Indexed By | SCI |
| Language | 英语 |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.gyig.ac.cn/handle/42920512-1/12447 |
| Collection | 矿床地球化学国家重点实验室 |
| Affiliation | 1.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China 2.University of Chinese Academy of Sciences, Beijing 100049, China 3.MLR Key Laboratory of Sanjiang Metallogeny and Resources Exploration and Utilization, Yunnan Geological Survey, Kunming 650051, China |
| Recommended Citation GB/T 7714 | Juan Li,Lei-Luo Xu,Xian-Wu Bi,等. New titanite U–Pb and molybdenite Re–Os ages for a hydrothermal vein-type Cu deposit in the Lanping Basin, Yunnan, SW China: constraints on regional metallogeny and implications for exploration[J]. Mineralium Deposita,2021,56(3):441-456. |
| APA | Juan Li.,Lei-Luo Xu.,Xian-Wu Bi.,Yong-Yong Tang.,Xiang-Yuan Sheng.,...&Rui Ma.(2021).New titanite U–Pb and molybdenite Re–Os ages for a hydrothermal vein-type Cu deposit in the Lanping Basin, Yunnan, SW China: constraints on regional metallogeny and implications for exploration.Mineralium Deposita,56(3),441-456. |
| MLA | Juan Li,et al."New titanite U–Pb and molybdenite Re–Os ages for a hydrothermal vein-type Cu deposit in the Lanping Basin, Yunnan, SW China: constraints on regional metallogeny and implications for exploration".Mineralium Deposita 56.3(2021):441-456. |
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| File Name/Size | DocType | Version | Access | License | ||
| New titanite U–Pb an（1456KB） | 期刊论文 | 作者接受稿 | 开放获取 | CC BY-NC-SA | View Download | |
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