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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 mafic
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 mafic