塔什库尔干断裂带是由多条运动性质不同的次级断层组成。
Tashikurgan fault zone is composed of many secondary faults with different motion characteristics.
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.
确立了一种用于研究低能次级放射性束逆运动学核反应的实验方案。
An experimental scheme is established for the study of the inverse kinematics reactions induced by low energy secondary radioactive nuclear beams.
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