动态重结晶（dynamic recrystallization）是和变形作用同时进行的重结晶作用。矿物在高于0.5Tm（Tm为熔点温度）下变形，或在达到一定临界应力和较慢应变速率的蠕变中，都有可能产生动态重结晶。
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.
韧性变形岩石中动态重结晶石英颗粒边界形态具有自相似性，表现出分形特征。
Grain shapes of dynamically recrystallized quartz in ductile deformed rocks, characterized by fractal dimension, are statistically self_similar.
载金矿物为沿糜棱面理分布的细粒黄铁矿、动态重结晶石英集合体及铁白云石。
Gold carrier minerals are fine-grained pyrite, recrystallized quartz aggregates, and ferrodolomite along foliations of mylonite.
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