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.
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 strata form and quasi strata form ore bodies are controlled by strike slip faults.
矿体受层滑断层控制呈层状、似层状。
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 wedged rotating basins develop along the strike-slip faults with regional block rotation.
楔状旋转盆地是伴随区域块体旋转作用在走滑断裂上发育的构造盆地。
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 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。
Strike-slip faults widely developed and had certain control role on reform of carbonate reservoir, volcanic action and formation of traps.
走滑断裂广泛发育，对碳酸盐岩储层改造、火山活动及圈闭形成具有一定的控制作用。
The said fracture zone is composed of a series of ductile and brittle thrust faults, strike-slip faults and blocks as well as tectonic slices.
该带由韧性又脆性冲断层、平移断层，以及各种岩块、构造岩片等组合而成。
Faults which move along the direction of the dip plane are dip-slip faults and described as either normal or reverse, depending on their motion.
沿倾角方向移动的断层称为倾滑断层，并按他们的运动方向分别描述为正向或逆向。
Based on the above characteristics, it is believed that the Shigang, Chajian and Wubao fault systems are of discrete-type right lateral strike-slip faults.
这些特征反映石港、汊涧、吴堡断层体系应属离散型右行走滑断层。
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。
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。
Volcanic activities were the response to the neotectonic activities and were controlled by strike-slip faults produced during the uplift of the Qinghai-Tibet Plateau.
火山活动为新构造活动的响应，受控于青藏高原隆升过程中产生的走滑断裂。
Some large strike slip faults, such as the Xianshuihe fault, consist of main fault and several sub-faults, which are commonly arranged as en echelon (or parallel) pattern.
大的走滑断裂带，如鲜水河断裂，是由主干断裂及与其相伴的若干阶式（或平行）断裂组成。
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;
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；
In Bozhong depression, there were four types faults which were early extensional faults, middle strike-slip extensional faults, late strike-slip faults and long-term active faults.
渤中坳陷发育四种类型的断裂：即早期伸展断裂、中期走滑伸展断裂、晚期走滑断裂和长期活动的断裂。
In Bozhong depression, there were four types faults which were early extensional faults, middle strike-slip extensional faults, late strike-slip faults and long-term active faults.
渤中坳陷发育四种类型的断裂：即早期伸展断裂、中期走滑伸展断裂、晚期走滑断裂和长期活动的断裂。
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