喜马拉雅康巴淡色花岗岩的高分异成因及 岩浆⁃热液演化特征
Highly fractionated origin and magmtic⁃hydrothermal evolution of the Kampa leucogranites in the Tethyan Himalaya
喜马拉雅康巴淡色花岗岩的高分异成因及 岩浆⁃热液演化特征 |
| 刘志超, 刘小驰, 俞良军, 王建刚 |
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Highly fractionated origin and magmtic⁃hydrothermal evolution of the Kampa leucogranites in the Tethyan Himalaya |
| Zhichao Liu, Xiaochi Liu, Liangjun Yu, Jian'gang Wang |
| 图7 (a,b)康巴淡色花岗岩锆石CL图像；(c)康巴淡色花岗岩锆石HfO2与Zr/Hf成分相关图 |
| Fig.7 (a,b) Showing the Cathodoluminescence (CL) images of the zircons from the Kamba leucogranite,(c) plot of HfO2 vs. Zr/Hf in zircons from the Kamba leuocgranite |
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