摘要
通过对辽河群岩石中主要变质矿物的观察和研究,以岩石的变形历史作为变质结晶作用的相对时标,确定了矿物生长的时序特征及其演化过程。发现变质与变形既是有密切联系的又是各自独立的地质作用,辽河期的变形作用存在明显的3个变形幕,而辽河期的变质作用是个连续的完整的过程,无明显的热波动。变质作用高峰和变形作用高峰存在时间差。
Based on the studies on the major metamorphic minerals from Liaohe Group,the chrono-genesis characteristics and evolution process of the minerals growth are ascertained while thedeformation history of the rocks is regarded as the relative timemark of metamorphic crystal-lization. Then the metamorphism and deformation are discovered to be closely related and al-so independent.The deformation occuring in Liaohe period has undergone obvious 3episodes,but the metamorphism in Liaohe period has undergone a complete and continousprocess without obvious thermal fluctuation,and there is time difference between the peaksof metamorphism and deformatijon.
关键词
变质岩
变质序列
包体径迹
Liaohe Group Metamorphic succession Deformation succession Struc-ture analysis method Inclusion track