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有道
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维基
百科
斜层理
oblique bedding
- 滑覆系统由C-P构造层组成，发育有复式向斜、顺层掩卧褶皱、透入性拉伸线理和流劈理等滑动构造；
Its gliding nappe system, which was composed by C-P structure layer, developed gliding tectonics such as synclinorium, bedding rheed fold, penetrative stretching and flow cleavage, etc. - 这些斜层理可以划分为高达4组不同特征的组合，分别代表潮流沙脊发育的不同阶段，对应于冰后期海平面上升的不同时期。
These inclined beddings can be divided into 4 bedding assemblages to represent different development stages of tidal sand ridges and to correspond to different postglacial sea-level rise periods.
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