1) thrust anticline belt
逆冲断裂背斜带
2) Active folding and faulting belt
活动背斜-逆断裂带
3) thrusting fault belt
逆冲断裂带
1.
Based on the interpretation of geophysical data in the western margin of Ordos Basin, it is suggested that the formation and evolution of tri-shaped rift formed by Qinling -Qilian -Helan mountains would be the main factor to form south and north large thrusting fault belts in the western edge of Ovdos Basin.
对鄂尔多斯盆地西缘物探资料解释研究认为:秦祁贺三叉裂谷的形成和演化,是鄂尔多斯盆地西缘形成南北两大不同逆冲断裂带的主要原因。
4) fault-anticline belt
断裂-背斜构造带
1.
Dongying sag is a secondary structure unit of Jiyang depression, its current structural framework could be regarded as two expanding fault-fold systems controlled by Chennan listric fault zone and Lijin listric fault zone respectively, with each system consisting of four fault-anticline belts.
东营凹陷作为济阳坳陷一次级构造单元,现今的构造格局由四条NWW向断裂-背斜构造带和四条NE向断裂-背斜构造带叠合而成,可以看作是二个大型的分别受陈南铲式断裂带和利津断裂带所控制的伸展断弯褶皱体系,先后经历了NNE-SSW向和NW-SE向区域引张作用的叠加及NE向的右旋走滑作用的改造,具有NW-SE向和NNE向的双向伸展及右旋走滑变形的基本特点,这种构造格局及其演变特征控制了油气的生成、运移、聚集成藏过程和油气藏的分布,构造类圈闭是主要的油气保存单元,两个方向的八条断褶构造带成藏条件较好,是油气藏主要聚集区带。
5) oblique thrust tectonics
斜向逆冲断裂
6) No.Ⅱ back thrusting fault zone
Ⅱ号背冲断裂带
1.
The Ordovician Strata,structures,karst reservoirs and structural traps are very complex in the No.
卡塔克隆起卡1南三维地震工区Ⅱ号背冲断裂带中的奥陶系岩溶储层和构造圈闭非常复杂,奥陶系岩溶是本区油气突破的关键因素。
补充资料：背逆
1.背叛忤逆。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条