结晶作用（crystallization）即形成晶体的作用，指物质在一定的物理化学条件下（温度、压力、组分浓度）转变为结晶质的作用。
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.
结构和组构分析表明，新组构的形成机制主要是再结晶作用。
Analysis of structure and fabric shows that the formation mechanism of new fabrics in these experiments is principally recrystallization.
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.
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