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.
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