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。
The main type of fracture are tensional fault, compressional fault and 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。
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。
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。
If the relative movement of hanging wall and footwall is parallel to the strike of fault plane, it is a strike slip fault.
如果断层走向与区域构造的总体走向相平行，就称之为纵向断层；
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 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。
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 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。
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。
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。
Through the analysis on stress field, palaeogeomorphology and spatial distribution of faults, Kendong region is considered to be 'concealed' strike - slip fault.
通过对区域应力场、古地貌和断裂空间展布等分析，认为垦东地区发育“隐伏型”走滑断裂。
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 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。
The main thrust-slip fault belts and the nappe structure zones, thrust sheets and low strain regions lying in between the main thrust-slip fault belts are described in detail.
对主干逆冲断裂带及其间的逆冲推覆体带、逆冲席带和低应变区的特征进行了详细描述。
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。
From this, it has been inferred that the strike of the dislocating fault plane of the main shock is NWW. It seems to be a left lateral horizontal slip fault with high dipping Angle.
由此推测，主震的错动面为北西西走向，可能是高倾角的左旋平移断层的滑动结果。
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。
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。
应用推荐