发育于地壳浅层中的脆性断层常常由一系列次级小断层所构成。
In lower crust, faults often consist of a series of secondary fractures.
该带由韧性又脆性冲断层、平移断层，以及各种岩块、构造岩片等组合而成。
The said fracture zone is composed of a series of ductile and brittle thrust faults, strike-slip faults and blocks as well as tectonic slices.
在吉南样子哨坳陷北缘石道河镇一带，于元古代新老盖层间存在韧—脆性滑覆断层。
There occurs ductile-brittle gliding-nappe faults in the Proterozoic, new and old cap rocks on the north margin of the depression in the Shidaohe area, Yangzhishao, southern part of Jilin Province.
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