Normal fault, reverse fault and strike-slip fault.
正断层、逆断层和走滑断层。
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。
The Altyn Tagh fault zone is an important strike-slip fault zone in northwestern China.
阿尔金断裂带是西北地区一条重要的走滑断裂带。
Altyn structural belt consists of collisional orogenic belt and thrusting strike-slip fault systems.
阿尔金构造带包括阿尔金碰撞造山带和阿尔金逆冲-走滑断裂系。
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。
The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement.
伊通地堑是一个主体在海西期褶皱基底上发育起来的第三纪含油气走滑断陷盆地。
The affection on main tensile stress and shear stress field was weakened from Cherchen-xingxingxia strike-slip fault.
主拉应力场和剪应力场受车尔臣—星星峡走滑断裂的影响明显减弱。
We must pay attention to the linear landforms when we determine direction and displacement amount of strike-slip fault.
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。
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 that basis, the paper discusses whether the Tanlu fault is a gigantic sinistral strike-slip fault or a transform fault.
在此基础上，讨论了郯庐断裂带是否为巨大的左行平移断层或转换断层。
The pull-apart basin formed around the steps of the strike-slip fault refers to a low terrain area due to tensile force from the fault.
拉分盆地指沿着走滑断裂带弯曲部位，由于拉张而产生的地形上的低洼处， 多形成于走滑断裂带次级断裂的间列部位。
Karayulgun dextral strike-slip fault, which is a thin-skinned structure, adjusted the deformation difference located at frontal range of Quele area.
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。
Traditional analytic methods and numerical simulation methods which have been done are mainly to study the response resulted from the strike-slip fault.
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。
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。
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。
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。
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.
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。
The Hanling-Pianling strike-slip fault zone is an important fault zone of the east of Liaoning, and a secondary fault at the east wall of the Tan-Lu fault zone in China.
寒岭—偏岭平移断裂带位于辽宁东部，是中国东部郯庐断裂东盘的一个次级断裂。
This study is a basis on revealing the tectonic evolution and active pattern, deducing the strike-slipping history and forecasting the future behavior of a strike-slip fault.
这一研究是揭示走滑断裂的构造演化与活动习性，反演断裂走滑活动历史并预测其未来行为的基础。
It is significant to study the characters of the strike-slip structures for trap prediction and prediction of rules of hydrocarbon accumulation along the strike-slip fault zone.
研究走滑构造发育特征，对于预测圈闭分布以和研究油气富集规律具有重要意义。
The Fangxian basin of Cenozoic era of south Qinling is a pull-apart basin at the southeastern end of the Ankang-Zhushan-Fangxian NW-trending left-lateral strike-slip fault zone.
南秦岭新生代房县盆地是北西向安康竹山房县左旋走滑断裂构造带东南端拉分盆地。
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。
This paper considers that Aerjin Mountain strike-slip fault structure is a huge tectonic zone with the property of left active anticlockwise and thrust nappes and ductile shear zone.
该文认为，阿尔金山走滑断裂构造是一巨型左行左列走滑断裂兼逆冲推覆和韧性剪切性质的断裂构造带。
The geometry and inner structures as well as the kinematics of the east-west dextral strike-slip fault system in the middle segment of the intraplate Yanshan orogenic belt are described.
阐述了分布于燕山板内造山带中段的近东西向中生代右行走滑构造系统的几何学与运动学特征。
The main fracture of the western margin fault zone of the South China Sea is originated from the Mesozoic basement fault, continuously developed into dextral strike-slip fault zone in Cenozoic.
南海西缘断裂带的主断裂是一条形成于中生代的基底断裂，在新生代持续活动扩展为右行走滑活动断裂带。
Using the Finite Element Method (FEM) and dislocation theory, we simulated the asymmetric earthquake displacement field of a vertical strike-slip fault caused by laterally inhomogeneous medium.
结合位错理论和有限单元法，对介质横向不均匀性引起的直立走滑断裂地震水平位移场不对称性进行了数值模拟研究。
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.
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 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。
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”。
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”。
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