right lateral meaning in Chinese
右侧的,右外侧的
Examples
- 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。 - 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。 - The ne - strike compressional faults are not intersected with the ew ma in fault zone , but a kind of transform structure resulted from its right lateral strike slip , and one of the typical example is the mesozoic thrust systerm in the northeast side of the main fault in western liaoning
在青龙断裂带两侧,分布有许多北东向压性断层,它们与东西向主断裂带不是简单的切割关系,而是东西向主断裂带右行走滑活动中的分支断裂,位于青龙断裂带北东侧的辽西地区中生代逆冲推覆构造,也是青龙断裂带在右行走滑作用下,因构造方向的改变发生构造转换的结果。