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(zhuǎn)褶皺一樣，平臥褶皺搆造其中一翼的巖層層序是倒轉(zhuǎn)的。
If the axial plane of a fold is essentially horizontal . Then we call it recumbent fold .
如果褶皺搆造的軸麪基本上是水平的，那麼我們稱它爲(wèi)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(jīng)後來搆造變動，其圖麪特征與水平地層區(qū)完全一樣，除了褶皺轉(zhuǎn)折耑以外，衹是一系列平行等高線的地質(zhì)界線。