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11 (a)康巴淡色花岗岩Sr含量与87Sr/86Sr比值相关关系；(b)康巴淡色花岗岩Rb含量与87Sr/86Sr比值相关关系 |
| Fig.11 Correlation between Sr concentraion and 87Sr/86Sr ratio (a) and correlation between Rb concentraion and 87Sr/86Sr for Kamba leucogranites (b) |
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