喜马拉雅夏如淡色花岗岩⁃伟晶岩的矿物学特征

程飞越, 谢磊, 陈小明

Mineralogical characteristics of the Xiaru leucogranite⁃pegmatite in the Himalayan oregen

Feiyue Cheng, Lei Xie, Xiaoming Chen

图1 （a）喜马拉雅淡色花岗岩带地质简图（据文献[1]修改）；（b）夏如岩体地质简图（据文献[14]修改）； （c）夏如淡色花岗岩；（d）伟晶岩脉切穿白云母花岗岩

Fig.1 Simplified geological maps of (a) Himalayan leucogranite belt (modified after ref.[1]) and (b) the Xiaru leucogranite (modified after ref.[14]),(c) the outcrop of the Xiaru leucogranite, (d) the pegmatite dike cut through the muscovite granite