1·The formation time of NE strike slip faults is earlier than that of NW strike slip faults.
另一组为NW向走滑断层，形成时代较晚，破坏早期逆冲断层和NE向走滑断层。
2·The extensional structures developed in the central Bohai Bay basin are induced by strike slip.
这个走滑拉分盆地的中部发育伸展构造，这些伸展构造是由走滑作用派生而来的。
3·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。
4·The faults are mainly of reverse and strike slip faults, with a few synsedimentary normal, decollement and reversed faults.
断裂以逆断层和走滑断层为主，还有少量的同沉积正断层、滑脱断层、反转断层等。
5·In the after strike slip compressional stage, this lake was filled up with the clastic sediments of deltic and fluvial facies.
在随后的走滑挤压阶段，该湖泊为三角洲和河流相碎屑沉积物充填。
6·The distribution of slip displacement, slip velocity and friction force on the strike slip fault were obtained by numerical simulation.
通过数值计算得到了平移断层上滑移位移、速度及摩擦力的分布规律。
7·The lower-order faults were formed under the action of strike slip stress, extension stress, camber stress and traction of master faults.
低级序断层是在走滑应力、伸展应力以及受主断层的牵引或在局部地区的拱升应力等作用下形成的。
8·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。
9·According to the analysis of Mesozoic and Cenozoic tectonic evolution, Bohai Bay basin is a strike slip pull apart basin formed in the Cenozoic Eocene epoch.
从渤海湾盆地的中、新生代构造演化分析，渤海湾盆地是一个新生代早第三纪始新世形成的走滑拉分盆地。
10·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。