It is one of the main reasons that induced strike-slip movement of main fault zone.
它是引起主断裂发生走滑的重要原因之一。
The average of its sinistral strike-slip movement since the late part of the late Pleistocene is up to 10.
晚更新世晚期以来的平均左旋走滑运动速率达10。
It shows sinistral strike-slip movement in western and middle segment, sinistral strike-slip and thrust in eastern segment.
西段和中段表现为左旋走滑，东段表现为左旋走滑逆冲运动。
In the overlap part of the right side of two main faults, the left-lateral strike-slip movement of them in Quaternary has formed the embryonic rhombochasm.
在两条主要左行走滑断裂的右侧叠覆区，两条主断裂第四纪的左行走滑运动产生一个胚胎期的菱形断陷。
The left-lateral strike-slip movement of the Zhongwei fault zone since late Pleistocene caused the differentiation of preexisting overthrust faults in the zone.
青藏高原东北缘的中卫断裂带在晚更新世以来的左旋走滑运动中，先存的挤压逆掩、逆冲断裂带发生了分化。
The left-lateral strike-slip movement is the main horizontal deformation, the rate of the vertical deformation is less than horizontal deformation, and showed the…
菱形块体的现今水平形变以左旋走滑运动为主 ，垂直形变速率较低 ，且呈上盘抬升与下降交替出现的运动特征 ；
The vertical movement strength and deformation status evolve with time. The horizontal movement and deformation show obvious compressional strike slip character.
垂直差异运动强度和变形态势随时间演变，水平运动与变形呈明显的挤压走滑特征。
Tanlu strike-slip fault zone had experienced several phases of movement, exerting strong influence and control upon the hydrocarbon pooling within the zone.
郯庐走滑断裂带经历了多期活动，影响和控制走滑断裂带内的油气成藏。
Based on the negative flower shaped structure and its relative structural movement track in Fangzheng area, this paper suggests that Fangzheng rift is a rifted basin formed by strike slip pull apart.
本文通过对方正地区所发现的负花状构造及其有关构造运动形迹分析的基础上，进一步提出方正断陷是走滑—拉分形成的断陷盆地。
If the relative movement of hanging wall and footwall is parallel to the strike of fault plane it is a strike slip fault.
如果断层上盘和下盘的岩石相对位移运动是平行断层面走向的，这种断层称为走滑断层。
The secular GPS crustal deformation image has reflected the relatively complete left lateral strike slip movement of this active fault zone.
长趋势GPS地壳形变图像反映了这条活动断裂带相对完整的左旋走滑活动。
If the relative movement of hanging wall and footwall is parallel to the strike of fault plane, it is a strike slip fault.
如果断层走向与区域构造的总体走向相平行，就称之为纵向断层；
If the relative movement of hanging wall and footwall is parallel to the strike of fault plane, it is a strike slip fault.
如果断层走向与区域构造的总体走向相平行，就称之为纵向断层；
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