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 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 forming age of maximum sinistral strike-slip occurred in Middle-Late Triassic.
最大左行走滑活动时期当在中晚三叠世。
The focal mechanism is mainly left-lateral strike-slip, with a small thrust component.
震源机制主要是左旋走滑，带有很小的逆冲倾滑分量。
The two boundaries of the Yili Block have been reworked by the Permian strike-slip faulting.
伊犁地块的南、北缘边界在二叠纪期间经受了走滑作用的强烈改造。
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。
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。
Jiaolai basin is a strike-slip and pull-apart basin controlled by the Yishu Fault Belt and Wulian -jimo-muping Fault.
胶莱盆地是中生代走滑拉分盆地，其形成与发育受到沂沭断裂和五莲-即墨-牟平断裂的控制。
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。
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。
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。
There have four kind of basins in the South China Sea area: rifting basin, strike-slip rifting basin, fore-land basin and fore-arc basin.
南海地区新生代沉积盆地有四类：张裂盆地、走滑拉张盆地、前陆盆地和前弧盆地。
Microstructure and ultramicrostructure of the strike-slip thrust belt in eastern Jiaodong have been studied using both microscopy and TEM.
应用偏光显微镜和透射电子显微镜方法，进行了胶东东部走滑逆冲构造带显微构造及超微构造研究。
"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。”
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。
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。
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。
Wan 'an basin is one of the most important Cenozoic oil and gas basins in the South China Sea, and it is also a typical Cenozoic strike-slip extensional basin.
万安盆地是南海重要的新生代含油气盆地之一，是较为典型的新生代走滑拉张盆地。
The left-lateral strike-slip movement of the Zhongwei fault zone since late Pleistocene caused the differentiation of preexisting overthrust faults in the zone.
青藏高原东北缘的中卫断裂带在晚更新世以来的左旋走滑运动中，先存的挤压逆掩、逆冲断裂带发生了分化。
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。
ETM data reveal that the Yuanmou fault is mainly characterized by horizontal left-lateral and shear strike-slip, including ringent shear and pressed shear in part.
ETM影像揭示了元谋断裂以左行剪切走滑为主，局部张剪或压剪的性质。
The ratio of poloidal to toroidal component of mantle convection determined the proportion of seismic energy released in the thrust, normal, or strike-slip earthquakes.
地幔对流的垂直运动与水平运动分量的比率，决定了逆冲、引张与走滑型强震的能量释放份额。
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。
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。
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。
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