晚期自生粘土矿物的形成和早期粘土矿物的重结晶作用。
Formation of late authigenic clay minerals and recrystallization of early clay minerals.
依据形成机制和过程可以划分为动态重结晶和静态重结晶作用。
According to origin mechanism and process, recrystallization in mylonite can be divided into dynamic recrystallization and static recrystallization.
晚期韧性剪切变形与区域D_3变形幕有关，伴随有绿泥石、冻蓝闪石等的出现和石英、方解石的动态重结晶作用。
The late ductile shearing(DF_2) formed in D_3 deformation phase is accompanied by the appearance of chlorite and barroisite etc. and dynamic recrystallization of albite, quartz and calcite.
晚期阶段以稳态重结晶为特征，仅在韧性滑脱剪切带主界面形成了低压型低角闪岩相的变质作用。
The late stage is characterized by recrystallization in a stable enviroument. The metamorphism of low pressure type of low amphibolite facies only occurs on the main boundary planes of the zone.
岩石中橄榄石和辉石的变形都是由粗变细重结晶过程，尖晶石则有较明显的溶解、迁移和再沉淀作用。
The deformation of olivine and pyroxene in the rock is the recrystallized process from coarse to fine grain, the spinel has obvious dissolution, migration and reprecipitation.
岩石中橄榄石和辉石的变形都是由粗变细重结晶过程，尖晶石则有较明显的溶解、迁移和再沉淀作用。
The deformation of olivine and pyroxene in the rock is the recrystallized process from coarse to fine grain, the spinel has obvious dissolution, migration and reprecipitation.
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