1) interlayer gliding fault
层滑断层
1.
Broken interlayer gliding faults, rumpled interlayer gliding faults, composite interlayer gliding fault, high angle downthrown faults, and associated drag-folds were established by about NE-SW stretching stress, which caused a large scale of extensional sliding movement in Yan’an Formation in the late period of early Cretaceous.
破裂型层滑断层、揉皱型层滑断层、复合型层滑断层、高角度正断层及其伴生的牵引褶皱,是延安组在早白垩世晚期NE-SW向近水平拉伸应力作用下发生大规模的伸展滑脱运动形成的。
2) strike-slip fault
走滑断层
1.
Discovery of strike-slip fault and its origin analysis in Biyang depression of Xinzhuang oilfield;
泌阳凹陷新庄油田走滑断层的发现及成因分析
2.
Relationship between strike-slip faults and petroleum in the central segment of the eastern subbasin of the Liaohe oilfield,China;
辽河油田东部凹陷中段走滑断层与油气的关系
3.
Relation between features of strike-slip faults and hydrocarbon accumulation in Subei basin;
苏北盆地走滑断层特征与油气聚集关系
4) detachment fault
滑脱断层
1.
Genetic mechanism and geological significance of Mazhai detachment fault in Dongpu depression;
东濮凹陷马寨滑脱断层的形成机制及地质意义
2.
A geometrical model,which utilizes an assemblage of parameters of propagation anticline to constraint the depth and geometry of the blind detachment fault,is figured in this paper based on both balanced geosection principles and previous studies.
滑脱断层断坡倾角为29°~45,°属于中等倾角。
6) dip-slip fault
倾滑断层
1.
A coherency model of ground motion on base-rock corresponding to dip-slip fault;
基岩地震动的一个相干函数模型——倾滑断层情形
补充资料:逋走
1.逃走,逃亡。
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