摘要
Based on a detailed analysis of the metamorphic minerals in rock samples, the authors hold that the main minerals in lower sub-group of Laoling Group can be divided into two generations: M1 and M2, which represent two metamorphic stages. Researches on metamorphic assemblage, distribution characteristics and division of metamorphic facies show that M1 is characterized by low-to-moderate temperature regional dynamic heat flow metamorphism which can be divided into two metamorphic facies: lower greenschist facies and high greenschist facies. Comprehensive studies show that metamorphism of the sub-group of Laoling Group in southern Jilin Province is characterized by reduction of influencing area and decrease of intensity from early to late. This tendency suggests that the earth’s crust became stable in Proterozoic.