Fold 3
Fold 3 : Bending or curvature of a stack of originally flat and planar surfaces, such as sedimentary strata, that results in permanent deformation. Folds are commonly formed by shortening of existing layers, but may also form as a result of displacement on a non-planar fault (fault bend fold), at the tip of a propagating fault (fault propagation fold), or by differential compaction
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