用数值模拟方法研究了几何、力学条件不同的雁列构造模型的应力场,探讨了几何参数对应力场的影响。
The stress fields of en echelon faults with different geometry and mechanical conditions were considered by dynamically numerical simulation.
因此可以通过这些次级构造和雁列类型的关系,来判断断层的运动和主应力方向。
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.
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。
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.
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