Strike-slip faults occurring in the converging crust, or transpression, rocks are faulted upward in a positive flower structure.
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。
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 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。
Thrust- faults and strike-slip faults are the major structures in the studied area.
逆冲断层及边界走精断层是区内主要控矿构造。
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 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 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。
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。
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。
"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。”
In the overlap part of the right side of two main faults, the left-lateral strike-slip movement of them in Quaternary has formed the embryonic rhombochasm.
在两条主要左行走滑断裂的右侧叠覆区，两条主断裂第四纪的左行走滑运动产生一个胚胎期的菱形断陷。
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。
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。
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。
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。
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。
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