部分断裂到第四纪表现为右行走滑。
这些特征反映石港、汊涧、吴堡断层体系应属离散型右行走滑断层。
Based on the above characteristics, it is believed that the Shigang, Chajian and Wubao fault systems are of discrete-type right lateral strike-slip faults.
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。
The early fault zone was reconstructed and became dextral right - step Z - type fault during dextral - slip stage.
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。
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.
认为由北东向南西的掀斜隆升和右行走滑剪切作用是欧亚大陆阿尔泰山脉西南麓隆升的主要机制。
The uplifting, right-lateral strike-slip shearing, tilting and southward shearing of the Altai Mountains in Xinjiang have affected, since Oligocene, the drainage systems evolution and development.
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。
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。
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.
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