1) tortuously non-connected fault
拐折非连通断层
1.
To study the infrared anomaly features of tectonic activity and process of instability,the tortuously non-connected fault is selected as a physical simulation model,and the thermal infrared radiation(TIR) variation features of fault models are experimentally studied in the process of loading and instability by means of uniaxial loading system and TIR imaging system.
为研究构造活动及其失稳过程的红外异常特征,选择拐折非连通断层作为模拟对象,利用单轴加载试验系统和红外热像仪,对模型受力及失稳过程的热辐射时空演化特征进行试验研究。
2) bend fault
拐折断层
1.
A similar example is observed when the sample with tensile en echelon faults changes into that with a bend fault after two segments of the en echelon fault linking up.
第一个实验通过改变加载方向使构造活动模式从挤压型雁列变为拉张型雁列,得出前一阶段b值比后一阶段要高;第二个实验通过持续加载使拉张型雁列变为拐折断层,与第一个实验类似,前一阶段b值比后一阶段要高。
3) discontinuous jointed faults
非连续组合断层
1.
The fracturing of discontinuous jointed faults is a mechanism of tectonic earthquake.
以构造地震孕震机制之一即非连续组合断层破裂发震为模拟对象,利用双轴加载实验系统和红外热像仪,对雁列和同线非连通这两种非连续组合断层在双轴加载破裂失稳过程中的红外辐射特征进行了模拟实验研究。
5) expediting of a call in progress
通话折断
6) slope break fault
坡折断层
1.
Dynamic analysis of sand body controlled by slope break faults in Bonan Subsag;
渤南洼陷坡折断层控砂动态分析
补充资料：层层加码
1.谓逐级增加任务和逐级提出各种要求等。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条