| REE geochemistry of primitive ore fluids in Ailaoshan gold belt, Southwest China | |
| Bi Xianwu;Hu Ruizhong | |
| 1998 | |
| Source Publication | Chinese Journal of Geochemistry
 |
| Volume | 17Issue:1Pages:91–96 |
| Abstract | The REE patterns of primitive ore solutions in the Ailaoshan gold belt are characterized by significant enrichment of LREE, a weak negative anomaly of Eu and a rather strong negative anomaly of Ce. In conjunction with the tension crust in the region, the ore solutions are thought to be originated from a CQ2-rich fluid as a result of mantle degassing. |
| Keyword | Ailaoshan Gold Belt Ore-forming Fluid Ree Geochemistry |
| Indexed By | EI |
| Language | 英语 |
| Document Type | 期刊论文 |
| Identifier | http://ir.gyig.ac.cn/handle/42920512-1/9441 |
| Collection | 矿床地球化学国家重点实验室 |
| Affiliation | Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 55000 |
| Recommended Citation GB/T 7714 | Bi Xianwu;Hu Ruizhong. REE geochemistry of primitive ore fluids in Ailaoshan gold belt, Southwest China[J]. Chinese Journal of Geochemistry,1998,17(1):91–96. |
| APA | Bi Xianwu;Hu Ruizhong.(1998).REE geochemistry of primitive ore fluids in Ailaoshan gold belt, Southwest China.Chinese Journal of Geochemistry,17(1),91–96. |
| MLA | Bi Xianwu;Hu Ruizhong."REE geochemistry of primitive ore fluids in Ailaoshan gold belt, Southwest China".Chinese Journal of Geochemistry 17.1(1998):91–96. |
| Files in This Item: | ||||||
| File Name/Size | DocType | Version | Access | License | ||
| REE geochemistry of （340KB） | 期刊论文 | 作者接受稿 | 开放获取 | CC BY-NC-SA | View Application Full Text | |
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