recumbent fold

基本解釋

Like overturned fold, the rock sequence of one limb of the recumbent fold is overturned.
如同倒轉褶皺一樣，平臥褶皺構造其中一翼的巖層層序是倒轉的。
If the axial plane of a fold is essentially horizontal . Then we call it recumbent fold .
如果褶皺構造的軸面基本上是水平的，那么我們稱它為平臥褶皺。
Without late tectonic deformation, the features of recumbent fold on the geological map would be the same as those of horizontal strata.
平臥褶皺若未經后來構造變動，其圖面特征與水平地層區(qū)完全一樣，除了褶皺轉折端以外，只是一系列平行等高線的地質界線。