全部

1·For the sake of stress relaxation, the tectonic boundary between these two different terrains (i. e. the Lingshan structure zone) expressed as a dextral fault in late period.

由于应力弛张作用，使两地体间的构造分界线（灵山构造带）后期表现为左旋断层性质。

2·Since the Tertiary period, the Red River Fault Zone suffered both of the sinistral movement and dextral movement, but the activities of the north and the south segment were different.

断裂带自第三纪以来，经历了左旋运动、右旋运动，南北两段的活动性有一定的差异。

3·The main shock occurred on the dextral obduction-type fault zone and the hypocenter depth was about 15km .

汶川地震的主震发生在具有右旋性质的仰冲型断层带上，震源深度为15公里左右。

4·This study shows that the formation of antithetic normal fault is controlled by NE WS strike tensile stress and dextral shear stress and the strike is nearly vertical to the tensile stress.

研究认为，北北东向反向正断层的形成受北东—南西向张应力及右旋剪切力控制，反向正断层的走向与张应力方向基本垂直；

5·The early fault zone was reconstructed and became dextral right - step Z - type fault during dextral - slip stage.

在右行走滑改造阶段，早期左行右阶断裂带被改造为“Z”型右行右阶断裂带。

6·The main fracture of the western margin fault zone of the South China Sea is originated from the Mesozoic basement fault, continuously developed into dextral strike-slip fault zone in Cenozoic.

南海西缘断裂带的主断裂是一条形成于中生代的基底断裂，在新生代持续活动扩展为右行走滑活动断裂带。

7·The geometry and inner structures as well as the kinematics of the east-west dextral strike-slip fault system in the middle segment of the intraplate Yanshan orogenic belt are described.

阐述了分布于燕山板内造山带中段的近东西向中生代右行走滑构造系统的几何学与运动学特征。

8·Karayulgun dextral strike-slip fault, which is a thin-skinned structure, adjusted the deformation difference located at frontal range of Quele area.

喀拉玉尔滚右旋走滑断层为薄皮构造，调节了却勒地区东、西段前缘的变形差异。

9·The origin of the Jiyang movement is closely related to the transformation of the Tanlu Fault Belt from sinistral to dextral movements.

济阳运动的成因，与郯庐断裂从左旋转向右旋的活动密切相关。