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Ptygmatic: Folds are chaotic, random and disconnected. Typical of sedimentary slump folding, migmatites and decollement detachment zones. Piercing fold: A fold which develops by the forcible upward movement of mud or salt diapirs. Suprataneous fold: A fold in which the beds are thinner at the crest and thicker at the trough. Typically forms when folding and sedimentation are contemporaneous. Reclined fold: Axial plane dip direction and hinge line plunge direction is same.