id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
amq-325	Mantovani, E.; Viti, M.; Babbucci, D.; Ferrini, M.; D’Intinosante, V.; Cenni, N.	Quaternary geodynamics of the Apennine belt	2009	12	.pdf	application/pdf	9424	567	57	One sugge- sts that crustal uplift has occurred in response to the break of the underlying slab (e.g., CINQUE et al., 1993; WESTAWAY, 1993). In the northern sector of the Southern Apennines, from the Matese to Irpinia zones (Fig.1), normal faults trending from NW-SE to E-W, have deve- loped along the inner side of the Molise-Sannio wedge (e.g., ORTOLANI & TORRE, 1981; CINQUE et al., 2000; BROZ- ZETTI & SALVATORE, 2005; ASCIONE et al., 2007), forming several troughs, such as the Middle Volturno, Calore and Boiano.	cache/amq-325.pdf	txt/amq-325.txt