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6 (a)康巴淡色花岗岩稀土元素蛛网图；(b)康巴淡色花岗岩稀土元素配分图.原始地幔和球粒陨石标准值来自文献[ |
| Fig.6 (a) Trace element distribution patterns for the Kamba leucogranite，(b) rare element distribution patterns for the Kamaba leuocgranite,primitive mantle and Chondrite data are from ref.[ |
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