地质构造上的断层表现为一个碎裂面，其断裂作用发生在地层形成之后。
In geology tectonics, the faultage is a cataclasm face formed after when the stratum had shaped.
这类岩石缺乏面理构造，是由于矿物颗粒的脆性碎裂，旋转以及颗粒边界的磨擦滑动和扩展而造成的。
These rocks are lack of foliation and resulted from the brittle fragmentation of mineral grains with rotation of grain fragments accompanied by fractional grain boundary sliding and dilatancy.
宁镇，茅山山脉褶皱逆冲一推覆构造带的构造岩类型主要为碎裂岩系列，其次为糜棱岩系列。
The main type of tectonites in the belts of fold thrust - nappes in Ningzhen, Maoshan mountains is the cataclasite series, and then mylonite series.
宏观碎裂结构与微观糜棱状结构是断层构造岩的主要特点。
The tectonites are characterized by macroscopic cataclastic and microscopic mylonitic structures.
川西北地区金矿矿田构造规律的研究表明，金矿化局部富集主要发生在断裂产状变化部位、两组断裂的交汇部位以及碎裂岩与构造透镜的接合部位。
It showed that the concentration of gold occurred in the variation position of attitude of faults, at the intersection position of two sets of faults and at the intersection of STR...
川西北地区金矿矿田构造规律的研究表明，金矿化局部富集主要发生在断裂产状变化部位、两组断裂的交汇部位以及碎裂岩与构造透镜的接合部位。
It showed that the concentration of gold occurred in the variation position of attitude of faults, at the intersection position of two sets of faults and at the intersection of STR...
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