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1)  olistostrome
滑来层
2)  olistolite
滑来岩块
3)  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。
4)  extrastratal source
层外来源
5)  extrinsic stacking fault
外来层错
6)  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
补充资料:逋走
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