The rock group is characterized by a general order but internal disorder because of intense ductile shearing deformation.
其特点是整体有序，组内无序，韧性剪切变形强烈。
The mineralization mechanism is that the brittle-ductile shearing deformation dynamically resulted in diagenesis and mineralization.
其成矿机理是脆韧性剪切变形动力成岩成矿。
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。
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