strike slip meaning in Chinese
走向位移
Examples
- Some controversy has been put on aheqi fault , our data shows it is a ne trending left lateral strike slip fault , but its activity is weak
阿合奇断裂是一条引起争议的断裂，我们收集的资料表明它是一条走向北东东的左行走滑断裂，但它的活动性不是很强烈。 - A right lateral strike slip , which is shown by mapview distribution of the whole fault zone , displacement of the strata , drag folding , s - c fabric and association of subsidiary faults , forms the mainly deformational mechanism
右行走滑活动的主要标志包括断裂带的平面展布、地层错动、牵引褶皱、 s - c组构、次级破裂组合等。 - Based on analysis of geology and geomorphology of the region and study on structure and revolution of the two faults , a strain partition model is built to adjust the strike slipping and compressional deformation of the area
通过区域地质、地貌分析和二条断裂带的结构、活动历史的对比研究，建立了该区走滑和挤压活动的应变分配模型。 - Analyzing collected dada , the conclusion is : northwestern trending right lateral strike slip faults are predominant , other active structures include northeastern trending left lateral strike slip faults and west - east trending folds
对上述资料分析认为：天山山间主要以北西向的右行走滑活动断裂为主，另有一些北东向的左行走滑活动断裂和东西向的活动褶皱。 - Yanqi basin is an intermont basin of tian shan , there is a nww trending right lateral strike slip active fault in southwestern basin , its maximum slip distance is 210m , and slip rate is about 10mm / yr , moreover , there is a west - east trending active anticline along northern basin
焉耆盆地是一个天山山间盆地，盆地西南缘发育一条走向北西西的右行走滑活动断层，最大走滑距离为210m ，走滑速率约10mm / yr ，盆地西北缘发育走向近东西的活动褶皱。