The Himalayan leucograite, which is typical production of continent-continent collision orogenic belt, has become a research hotspot of the Tibetan Plateau. The research on the leucogranite would help to verify and im...The Himalayan leucograite, which is typical production of continent-continent collision orogenic belt, has become a research hotspot of the Tibetan Plateau. The research on the leucogranite would help to verify and improve the continent-continent collision orogenic theory. （Huang et al., 2017; Fig. la）. Previous studies show the Himalayan leucogranite was mainly melted from crust materials （Guo and Wilson, 2012）. But it remains controversial for the formation model as to whether it formed from gathering of dikes or diaper of deep magma chambers.展开更多
基金supported by the National Key Research and Development Project of China (project 2016YFC0600304)the National Key Project on Basic Research of China (project 2015CB452604)the Strategic Priority Re-search Program (B) of the Chinese Academy of Sciences (project XDB03010301)
文摘The Himalayan leucograite, which is typical production of continent-continent collision orogenic belt, has become a research hotspot of the Tibetan Plateau. The research on the leucogranite would help to verify and improve the continent-continent collision orogenic theory. （Huang et al., 2017; Fig. la）. Previous studies show the Himalayan leucogranite was mainly melted from crust materials （Guo and Wilson, 2012）. But it remains controversial for the formation model as to whether it formed from gathering of dikes or diaper of deep magma chambers.
