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 two boundaries of the Yili Block have been reworked by the Permian strike-slip faulting.
这个走滑拉分盆地的中部发育伸展构造，这些伸展构造是由走滑作用派生而来的。
The extensional structures developed in the central Bohai Bay basin are induced by strike slip.
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。
In areas where strike-slip faults occur in converging crust, or transpression, rocks are faulted upward in a positive flower structure.
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。
Strike-slip faults widely developed and had certain control role on reform of carbonate reservoir, volcanic action and formation of traps.
低级序断层是在走滑应力、伸展应力以及受主断层的牵引或在局部地区的拱升应力等作用下形成的。
The lower-order faults were formed under the action of strike slip stress, extension stress, camber stress and traction of master faults.
断裂对渤海湾盆地的形成起着决定性的作用，总体上看既有拉张也有走滑。
Fracture plays a decisive role in the formation of Bohaiwan basin. Not only tension but also strike slide works in general.
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。
The wedged rotating basins develop along the strike-slip faults with regional block rotation.
花牛山—五峰山和黄尖丘—新场两地区形成正性的走滑隆升区，其相应中间地带则显示了负性拉分拗陷作用，发育了大奇山拉分盆地。
Huanushan - Wufenshan and Huangjianqiu -Xinchang formed positive strike -slip up-warping region, middle belt shown negative down warping, developed Daqishan pull -apart basin.
提出了地幔底辟和深断裂带右旋走滑位移两种动力机制联合作用主导了东濮凹陷的新生代应力场演化的构造动力学模式。
It indicates that two dynamical mechanisms of mantle diaper and right-lateral strike slip in deep faulted zone lead tectonic dynamics model evolved in Cenozoic stress field of Dongpu depression.
区域地质构造解析结果表明，连云山花岗岩与晚三叠世—侏罗纪nne向会聚走滑断层动热变质—剪切重熔型岩浆作用有关。
The analyses of regional structures show that Lianyunshan granite is associated with dynamic metamorphism shear remelt magmatism of NNE trending convergent strike slip faulting during t 3-j.
研究表明 ，相山火山盆地火山活动划分为两个旋回 ，其就位受制于区域深断裂的走滑拉分作用。
The study shows that volcanic activity in Xiangshan volcanic basin may be divided into two cycles, and its emplacement is controlled by strike slip pull apart process originated from the deep regiona.
研究表明 ，相山火山盆地火山活动划分为两个旋回 ，其就位受制于区域深断裂的走滑拉分作用。
The study shows that volcanic activity in Xiangshan volcanic basin may be divided into two cycles, and its emplacement is controlled by strike slip pull apart process originated from the deep regiona.
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