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。
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。
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 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。
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。
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。
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。
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。
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。
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。
The tectonic boundary between the Yangtze Continent and Qinling orogenic belt is a thrust-strike slip tectonic zone rather than a intracontinental subduction zone.
扬子大陆与秦岭造山带之间的壳内构造边界不具陆内俯冲性质，而是逆冲推复一走滑构造带。
In this paper, a method, the uniform slip method, estimating average slip rate along surface trace of strike slip fault zone by historical earthquake data is offered.
本文介绍并完善了作者提出的一种根据历史地震资料估计走滑断裂带地表断层平均滑动速率的方法：“均一滑动法”。
The oblique strike slip structure is resulted from the closing of little Jingshajiang regeneration ocean basin and the oblique intercontinental collision in late Triassic.
滇西北拖顶地区斜向走滑构造是金沙江再生小洋盆关闭、陆-陆斜向碰撞构造转化的结果。
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。
Strike-slip faults occurring in the converging crust, or transpression, rocks are faulted upward in a positive flower structure.
在会聚的地壳或压转岩石中发生的走滑断层以正花构造向上断裂。
The earthquake occurred along the North Anatolian strike-slip fault that extends roughly east-west beneath the Gulf of Izmit.
地震发生的北安纳托尼亚平移断层带，大约沿伊兹·米特湾呈东西向分布。
On type, the fractures appear normal fault, strike-slip fault and so on.
类型上，断裂主要有正断层、逆断层和雁行断层等形式。
For vertical strike-slip faults, the rupture directivity effect causes as strong spatial variation in ground motions for a given closest distance to the fault.
对于垂直走滑断层，在给定的距断层最近的范围内，破裂方向效应使地震动产生强烈的空间变化。
"Besides it being the biggest strike-slip earthquake ever recorded, the aftershock is the second biggest as far as we can tell," said Sieh.
他说：“这是记录在册的最大的走滑型地震，其余震也是我们所知的第二大余震。”
In areas where strike-slip faults occur in converging crust, or transpression, rocks are faulted upward in a positive flower structure.
在一些走滑断层产生于聚敛地壳内或处于转换挤压作用下的地区内，岩石向上断裂成一种正向花状构造。
Bengge syenites has been always regarded as the product of alkaline magma activity controlled by the strike-slip structures caused by collision between Yindia and Euroasia.
长期以来，甭哥正长岩体被认为是印度—欧亚板块碰撞引起的走滑剪切构造所控制的碱性岩浆活动的产物。
Detailed analyses of satellite images and field investigation have revealed that the active Kaidu River fault zone on the southern margin of the basin is a strike-slip fault zone.
详细的卫星图像分析和野外调查表明活动断层(开都河断层带)主要分布在盆地的南缘，具典型的走滑断层特征。
In each model, fault was classified into three types: all-fault, dip-slip fault and strike-slip fault.
每种模型中，根据断层类型将断层分成三类：所有断层，倾滑断层和走滑断层。
This paper discusses some features of fractals and deformational decomposition of oblique strike-slip faults in the Jinshajiang plate junction, northwest Yunnan.
从分形和变形分解的角度讨论了滇西北金沙江结合带斜向走滑构造分形和变形分解的某些特征。
This paper discusses some features of fractals and deformational decomposition of oblique strike-slip faults in the Jinshajiang plate junction, northwest Yunnan.
从分形和变形分解的角度讨论了滇西北金沙江结合带斜向走滑构造分形和变形分解的某些特征。
应用推荐