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1)  fracture transformation
断裂转换
2)  fault rotation
断裂旋转
1.
When calculating the discontinuous fault strain,we should consider three factors that affect the establishment of equations: fault geometry,fault rotation,and fault size or fault displacement.
已经提出三种断裂旋转机制:刚性旋转,垂直剪切和斜向剪切。
3)  torsional fracture
扭转断裂
1.
The results show that the fracture was caused by the banded structure which decreased the permitted rotational moment and resulted in the torsional fracture of the bolts during installation process.
结果表明:螺栓断裂是由于其制造时产生了严重的带状组织,降低了螺栓的许可扭转力矩,导致螺栓在安装过程中发生扭转断裂。
4)  trans-rift
转换裂谷
5)  transform fault
转换断层
1.
TRANSFORM FAULT AND ITS GEOLOGICAL SIGNIFICANCE ——A study on the Altyn Tagh transform fault;
转换断层及其地质意义——以阿尔金转换断层为例
2.
The strike slip fault can be divided into three different levels corresponding to the different scales of petroleum exploration targets, such as transform fault dominated the basin forming, transfer fault controlled the play, and tear fault charged the trap.
走滑构造体系盆山耦合常由于走滑断层弯曲所产生 ,结合油气勘探中盆地—区带—圈闭 3个层次 ,相应地划分为 3类走滑断层 :(1)转换断层为控盆断层 ;(2 )转移断层为控带断层 ;(3)撕裂断层为控藏断层。
3.
In mid-late Paleozoic, it was a great intracontinental transform fault of right-lateral slip, and in Mesozoic and Neozoic it was revived in different parts.
在卫星遥感图像宏观解译和野外调查基础上,充分参考了近年来的区域地质调查和前人研究成果,分析了阿尔金山各边界断裂特征,结果表明南缘断裂形成于元古宙,早古生代中晚期是一条具有右行走滑性质的巨型陆内转换断层,中新生代分段差异复活;西北缘断裂系形成较晚,中新生代以来发生强烈的左行走滑,应属于亚洲共轭滑移系的组成部分;红柳沟-拉配泉断裂属于塔里木地块中央构造带系统,是一条蛇绿构造混杂带,早古生代属于陆缘或陆间裂谷。
6)  Varied cross-sections
断面转换
补充资料:可转换证券的转换价值

可转换证券的转换价值——
       如果一种可转换证券可以立即转让,它可转换的普通股票的市场价格与转换比率的乘积就是可转换证券的转换价值,即转换价值等于普通股票的市价乘以转换比率。


说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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