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。
Strike-slip faults occurring in the converging crust, or transpression, rocks are faulted upward in a positive flower structure.
正断层、逆断层和走滑断层。
研究了走滑断层的成因；
判读走滑断层的变位方向及变位量，需注意地貌面上的线性地物。
We must pay attention to the linear landforms when we determine direction and displacement amount of strike-slip fault.
断裂的类型主要有拉张或张扭断层、拉压或压扭断层、走滑断层。
The main type of fracture are tensional fault, compressional fault and strike slip fault.
大部分活动断层属左旋斜滑断层，部分活动断层为左旋走滑断层。
Most of the active faults are left-lateral oblique-slip ones and part of them are left-lateral strike-slip ones.
不同时期徐中断层生长指数图和断裂落差图分析，得出徐中断裂为走滑断层。
Xuzhong fracture is strike-slip faults can be obtained from different periods fault growth index chart and fracture throw figure of Xuzhong fracture.
传统的理论解析方法和已经开展的数值模拟方法主要是基于走滑断层进行的。
Traditional analytic methods and numerical simulation methods which have been done are mainly to study the response resulted from the 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。
In each model, fault was classified into three types: all-fault, dip-slip fault and strike-slip fault.
喀拉玉尔滚右旋走滑断层为薄皮构造，调节了却勒地区东、西段前缘的变形差异。
Karayulgun dextral strike-slip fault, which is a thin-skinned structure, adjusted the deformation difference located at frontal range of Quele area.
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 formation time of NE strike slip faults is earlier than that of NW strike slip 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。
The faults are mainly of reverse and strike slip faults, with a few synsedimentary normal, decollement and reversed faults.
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。
If the relative movement of hanging wall and footwall is parallel to the strike of fault plane it is a strike slip fault.
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。
In areas where strike-slip faults occur in converging crust, or transpression, rocks are faulted upward in a positive flower structure.
第三篇概述了震源机制与海啸警报的关系，指出：地震海啸同逆断层或正断层有关，而和走滑断层无关；
The third one has reviewed relation between focal mechanisms and tsunami warnings. The article pointed out that earthquake-tsunami is related with overthrust or nomal fault but strike-slip fault.
准噶尔盆地西北缘前陆冲断带构造样式复杂多样，除规模较大的逆断层外，还发育一系列北西向的走滑断层。
The foreland thrust belt has complex and various structural styles. Besides the large-scale reverse faults, there are a series of north-west strike-slip faults.
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。
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.
胶莱走滑拉分盆地层序特征表现为：（1）靠近走滑断层的区域发育浅水型层序，而远离走滑断层的区域发育深水型层序；
The Jiaolai strike-slip pull-apart basin is characterized by: 1 shallow-water sequences along the strike-slip faults and deep-water sequences far from the strike-slip faults;
区域地质构造解析结果表明，连云山花岗岩与晚三叠世—侏罗纪nne向会聚走滑断层动热变质—剪切重熔型岩浆作用有关。
The analyses of regional structures show that Lianyunshan granite is associated with dynamic metamorphism shear remelt magmatism of NNE trending convergent strike slip faulting during t 3-j.
渤中34 - 1浅层复杂断块区处于郯庐走滑断裂带内，受其影响和控制该区断层较发育。
Bozhong 34-1 complex fault-blocks zone is located in Yanlu strike-slip fault zone. Affected and controlled by the strike-slip fault zone, faults are developed.
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”。
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.
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 lower-order faults were formed under the action of strike slip stress, extension stress, camber stress and traction of master faults.
研究结果表明，区域盖层、走滑性质、断层的活动强度、油源的充足程度是油气纵向分布的主要控制因素；
These factors include district cap rock, strike slip properties, the intensities of fault activity and the distance from oil source.
该断裂带北段的木吉河断层运动特征以逆冲为主，兼有右旋走滑分量。
Mujihe fault lies on the northern segment and its main motion characteristics is thrusting, and have dextrorotation slip component.
从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在，指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。
The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.
从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在，指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。
The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.
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