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。
2
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。
3
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.