摘要
A large number of granitoids constitutes a giant granitic belt trending EW in the Inner Mongolia.As a representative of those intrusions,the Damiao granitoid in Siziwangqi area may serve as a natural laboratory for the study of genesis of granite and evolution of crust.It is mainly composed of mid-coarse grained granodiorite with abundant
出处
《地学前缘》
EI
CAS
CSCD
北大核心
2009年第S1期213-214,共2页
Earth Science Frontiers