1、Like overturned fold, the rock sequence of one limb of the recumbent fold is overturned.
2、If both limbs of overturned fold have same dip angle, we call this special overturned fold isoclinal fold.
3、We call it overturned fold because the bedding sequence of one limb is overturned due to folding.
4、(4)The synsedimentary deformation structures are common in eolian dunes, such as brecciated foresets, drag folds and overturned folds.
