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。
Tanlu strike-slip fault zone had experienced several phases of movement, exerting strong influence and control upon the hydrocarbon pooling within the zone.
大的走滑断裂带，如鲜水河断裂，是由主干断裂及与其相伴的若干阶式（或平行）断裂组成。
Some large strike slip faults, such as the Xianshuihe fault, consist of main fault and several sub-faults, which are commonly arranged as en echelon (or parallel) pattern.
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。
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.
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”。
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.
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。
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.
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。
The left-lateral strike-slip movement of the Zhongwei fault zone since late Pleistocene caused the differentiation of preexisting overthrust faults in the zone.
长趋势GPS地壳形变图像反映了这条活动断裂带相对完整的左旋走滑活动。
The secular GPS crustal deformation image has reflected the relatively complete left lateral strike slip movement of this active fault zone.
龙陵断裂带及其以北的局部地区，最大主压应力方向为近南北或北北西，应力结构为走滑型。
In Longling fault zone and the area north to it, the direction of maximum compressional stress is near NS or NNW, the stress regime is of strike slip type.
该断裂带北段的木吉河断层运动特征以逆冲为主，兼有右旋走滑分量。
Mujihe fault lies on the northern segment and its main motion characteristics is thrusting, and have dextrorotation slip component.
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.
阿尔金断裂带最大累积走滑位移量——900km?。
The maximum cumulative strike-slip displacement of the Altyn Tagh Fault-900 km?
阿尔金断裂带最大累积走滑位移量——900km?。
The maximum cumulative strike-slip displacement of the Altyn Tagh Fault-900 km?
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