Syn-thrusting polygonal normal faults exposed in the hinge of the Cingoli anticline, northern Apennines, Italy
The Cingoli arcuate anticline is part of the Apennines fold-thrust belt in Italy.The anticline involves sedimentary carbonate strata generally affected by syn-thrusting contractional structures such as bed-normal pressure solution seams, folds, and reverse faults.An exception is constituted by an outcrop in the anticline hinge, where sub-horizontal