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。
Tanlu strike-slip fault zone had experienced several phases of movement, exerting strong influence and control upon the hydrocarbon pooling within the zone.
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。
The Hanling-Pianling strike-slip fault zone is an important fault zone of the east of Liaoning, and a secondary fault at the east wall of the Tan-Lu fault zone in China.
寒岭—偏岭平移断裂带位于辽宁东部,是中国东部郯庐断裂东盘的一个次级断裂。