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The Genesis of the Damiao Granodiorite in Siziwangqi and Its Constraint on the Crust Evolution of Inner Mongolia

The Genesis of the Damiao Granodiorite in Siziwangqi and Its Constraint on the Crust Evolution of Inner Mongolia
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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
关键词 MAFIC microgranular ENCLAVE granodiorite MAGMA mixing Siziwangqi INNER Mongolia mafic microgranular enclave granodiorite magma mixing Siziwangqi Inner Mongolia
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