En-echelon faults are a basic characteristic of fault combination in a shear zone.
断层呈雁列式是剪切带的构造组合特点。
The "multiple-order en echelon" pattern is one of the important geometric characteristics of the fault zone.
该断裂带主要的几何特征之一是具有“多重羽列”性质。
It serves not only as a geographic boundary but also as pre-tertiary en-echelon drapes and a Cenozoic tectonic conversion zone controlled by the basement fault zone.
该带不仅是一个地理界线，而且是一个由基底断裂带控制的前第三系雁列褶皱带和第三系构造转换带。
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