id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
amq-95	Giraudi, Carlo	THE EVOLUTION OF THE NORTHERNMOST APENNINE FRONT (PIEDMONT, ITALY): PLIO-PLEISTOCENE SEDIMENTATION AND DEFORMATION IN THE PO BASIN AND MONFERRATO HILLS	2016	22	.pdf	application/pdf	14950	641	57	Also the main defor- mation phases of the Cerrina valley syncline are coeval with the activity of the Lucedio and Cavourrina faults, that correspond to two differ- ent buried thrust fronts. Behind the Monferrato thrust fronts, active also in Plio-Quaternary times (Fig. 1B), deep piggyback basins are present: the subsidence in the basins was contemporary with the compressional tectonic (Dela Pierre et al., 1995; Irace et al., 2009).	cache/amq-95.pdf	txt/amq-95.txt