en-echelon fault

基本解釋

En-echelon faults are a basic characteristic of fault combination in a shear zone.
斷層呈雁列式是剪切帶的構造組合特點。
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.
該帶不僅是一個地理界線，而且是一個由基底斷裂帶控制的前第三系雁列褶皺帶和第三系構造轉換帶。
The fault movement and the direction of principal stresses may be determined by considering the relationship between the different secondary structures and en-echelon patterns.
因此可以通過這些次級構造和雁列類型的關系，來判斷斷層的運動和主應力方向。