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(gòu)造組合特點(diǎn)。
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(gè)地理界線，而且是一個(gè)由基底斷裂帶控制的前第三系雁列褶皺帶和第三系構(gòu)造轉(zhuǎn)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(guò)這些次級(jí)構(gòu)造和雁列類型的關(guān)系，來(lái)判斷斷層的運(yùn)動(dòng)和主應(yīng)力方向。