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
FG=Fractionated I?, S?, and M?type granites, OGT=Unfractionated I? ,S?,a nd M?type granites
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 |
|
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9 花岗岩类型判别图[ FG=Fractionated I?, S?, and M?type granites, OGT=Unfractionated I? ,S?,a nd M?type granites |
| Fig.9 Discrimination diagrams of the granites after ref.[ |
|
|