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- 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。
- Lu, C.-Y.(1994) Neotectonics in the foreland thrust belt of Taiwan. Petroleum Geology of Taiwan, 29, 1-26. 卢佳遇(1994)台湾岛前陆冲撞带的新构造运动。台湾石油地质，第29号，第1-26页。
- The forward directivity velocity pulse generated by strike slip fault in full space is studied. 本文在均匀弹性全空间中对走滑断层附近方向性速度脉冲作了定性研究。
- The northern Qaidam Basin, located to the east of the Altyn Tagh sinistral strike-slip belt, has long been considered to be a foreland thrust belt. 摘要处于阿尔金左行走滑构造带东缘的柴北缘，过去一致认为是个前陆逆冲带，并对其逆冲构造特徵作了大量的研究。
- Wuxia fault belt in the eastern part of northwestern margin of Junggar basin is an important part in the thrust belt of the northwestern margin. 摘要乌夏断裂带位于准噶尔盆地西北缘的东部，是西北缘冲断带的一个重要组成部分。
- Strike slip fault is an important tectonic type in continental orogenic belts,and usually acts as a channel way of fluid flow. 走滑断裂是大陆造山带中一种非常重要的构造类型，并常常成为各种流体异常活动的场所。
- A second important consequence of the collision was major strike slip faulting, facilitating the tectonic "escape" of China like a squeezed melon seed. 碰撞的第二个重要结果是主要的平移断层，它促进了中国构造的逃离，就象一颗被挤出的西瓜籽。
- The foreland thrust belt in northwestern margin of Junggar basin is a large-scale imbricated thrust system developed since Late Carboniferous. 准噶尔盆地西北缘前陆冲断带是自石炭纪晚期发育起来的大型叠瓦冲断系统,哈拉阿拉特山冲断带为其冲断前锋构造带的东段。
- The Kalpin thrust belt, located at the NW margin of the Tarim basin, is a part of the southern South Tianshan marginal thrust system. 摘要柯坪冲断带位于塔里木盆地的西北缘，是南天山南缘冲断系统的一部分。
- The Paleogene tectonic framework in Bohai Bay was controlled by both Mesozoic sinistral strike slip and Paleogene extension resulted from diapiric intrusion of mantle. 中生代左行走滑和早第三纪伸展作用共同控制了渤海海域早第三纪的构造格局。
- Foreland basin is one type of the most prolific petroliferous basins in the world, where thrust belt is one of its most abundant plays. 摘要前陆盆地是世界上油气资源最为丰富的盆地类型之一，而前陆盆地冲断带又是前陆盆地中最主要的油气富集区带之一。
- Both reverse faulting and strike slip occurred on the segment to the north of Beichuan, and strike slip offsets are greater than the vertical ones in some places. 北川以北段为逆冲兼走滑，水平位移量与垂直位移量基本相当，或水平位移略大.
- Quilitake anticline in Kuqa thrust belt and Bapanshuime anticline in Keping thrust belt along the piedmonts of the southem Tianshan are such complex imbricate folds. 应用断层相关褶皱理论,依据地表倾角产状、二维地震剖面和钻测井数据,建立了南天山山前库车秋里塔克背斜和柯坪八盘水磨背斜的构造模型。
- Along strike slip fault,the degassing strengh is different.This is strictly related to seismicity.The degassing strength also changes with fault activity. 在走滑断层拉分区，地球排放气体活动的强度与地震活动有密切的关系；
- The reservoir of thrust belt was mainly of pore-fracture type, dissolved pore, fracture and a little primary pore are mainly interstice of the reservoir. 该区发育有4个构造带：前陆冲断带储层类型为孔隙-裂缝型，以溶蚀孔和裂缝为主，见少量原生残余孔；
- Fault-propagation fold is an important tectonic style developed in a foreland basin.It usually occurs in an area covered seclusively in the front of a thrust belt. 摘要断层传播褶皱是前陆盆地中发育的一种重要构造样式，往往出现在冲断构造带的前缘隐伏前锋带。
- The axial direction of Kulongshan anticline in the south thrust belt of Qingxi Sag in Jiuquan Basin is accordance with the regional structural trend of NWW. 摘要处于酒泉盆地青西凹陷南缘冲断带内的窟窿山背斜构造，轴向为北西西向，与区域构造走向相一致。
- The results have shown that Tangshan seismogenic fault is a NW dipping dextral strike slip Quaternary contemporaneous fault,which offsets the Holocene(Q 4),late Pleistocene (Q 3),middle Pleistocene(Q 2) and early Pleitocene(Q 1) strata. 结果表明：唐山地震断层是一条倾向NW的右旋走滑第四纪同生断裂，它错断了全新统（Q4）、晚更新统（Q3）、中更新统（Q2）和早更新统（Q1）地层。
- On the basis of the Scanning Electron Microscopy (SEM) experiments for 76 samples, this paper presents important proofs related to the dextral strike slip movement of the Liaohe Basin, China during the Dongying phase of Late Eogene. 依据 76块岩样显微扫描电镜实验结果 ;报道辽河盆地早第三系东营期右行走滑构造运动的重要地质证据 .
- From the Point of view of the focal mechanizm and behaviour of ground crack, the component of right-lateral shear strike slip was dominant and at the same time with dip slip during Tangshan earthquake. 震源机制结果与极震区地裂缝的力学性质,都说明唐山地震是以右旋剪切走向滑动为主且兼倾向滑动的主震型大地震。
