If the axial plane of a fold is essentially horizontal. Then we call it recumbent fold.
如果褶皱构造的轴面基本上是水平的，那么我们称它为平卧褶皱。
Like overturned fold, the rock sequence of one limb of the recumbent fold is overturned.
如同倒转褶皱一样，平卧褶皱构造其中一翼的岩层层序是倒转的。
Without late tectonic deformation, the features of recumbent fold on the geological map would be the same as those of horizontal strata.
平卧褶皱若未经后来构造变动，其图面特征与水平地层区完全一样，除了褶皱转折端以外，只是一系列平行等高线的地质界线。
Without late tectonic deformation, the features of recumbent fold on the geological map would be the same as those of horizontal strata.
平卧褶皱若未经后来构造变动，其图面特征与水平地层区完全一样，除了褶皱转折端以外，只是一系列平行等高线的地质界线。
应用推荐