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.
TEM亚微分析表明,细粒基质是由粗大碎屑经过亚颗粒旋转,并伴随着局部颗粒边界迁移形成的动态重结晶颗粒。
It is shown from TEM analysis that the fine grained matrix materials are mainly derived from the huge clasts by subgrain rotation and local grain boundary migration.
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.
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