Shule river fault zone is a buried deep basement fault zone, it locates in the Southof Beishan area in Gansu Province.
疏勒河断裂带位于甘肃省北山地区南缘，为隐伏基底深断裂。
After late Cretaceous, structural deformation shows a series of movable basement fault again and new's fault. The fold structure is very simple.
晚白垩纪后，构造变形表现为一系列重新活动的基底断裂和新生断裂，褶皱构造简单。
It serves not only as a geographic boundary but also as pre-tertiary en-echelon drapes and a Cenozoic tectonic conversion zone controlled by the basement fault zone.
该带不仅是一个地理界线，而且是一个由基底断裂带控制的前第三系雁列褶皱带和第三系构造转换带。
Basement fault is an associated structure with the basin. The deposition in a basin and the tectonic style as well as the distribution of resources are determined by basement faults.
基底断裂与盆地是一对相互影响的伴生构造，断裂活动控制盆地内沉积填充和构造样式以及后期资源的分布。
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。
Hailar basin is a fault-depressed basin formed on Variscan folded basement.
海拉尔盆地是在华力西褶皱基底上形成的中生代断陷盆地。
The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement.
伊通地堑是一个主体在海西期褶皱基底上发育起来的第三纪含油气走滑断陷盆地。
The late stages tectonic organize related to intracontinental convergence forms the fault block system of basement.
晚阶段构造组合与陆内会聚有关，形成基底断块系统。
Regional exploration has revealed that the basin basement is divided into southern and northern parts, and this plays a strictly controlling role in the fault distribution and structure development.
区域勘探确定了盆地基底南北分区特征，它对盆地的断裂展布、构造发育具有严格的控制作用。
The NNE-striking Qikou coastal zone is located along the northern extension of Liaolan fault separating Taihang Mountain from Luxi basement.
大港歧口沿岸带位于太行山基底和鲁西基底接触的断裂带上——聊兰断裂北延段，沿海岸线呈NNE向展布。
The NNE-striking Qikou coastal zone is located along the northern extension of Liaolan fault separating Taihang Mountain from Luxi basement.
大港歧口沿岸带位于太行山基底和鲁西基底接触的断裂带上——聊兰断裂北延段，沿海岸线呈NNE向展布。
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