id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
amq-413	Coltorti, Mauro; Ravani, Silvia; Verrazzani, Federico	THE GROWTH OF THE CHIANTI RIDGE: PROGRESSIVE UNCONFORMITIES AND DEPOSITIONAL SEQUENCES IN THE S. BARBARA BASIN (UPPER VALDARNO, ITALY) 	2007	18	.pdf	application/pdf	12564	738	63	therein; BILLI et al., 1991; SAGRI, 1991; BOSSIO et al., 1995; SAGRI & MAGI, 1992; BENVENUTI, 1993; MARTINI & SAGRI, 1993; ALBIANELLI et al., 1995). However, our results shows that: 1. the Chianti Ridge, as the other ridges of the eastern sectors (CALAMITA et al., 1999), are not anticlines but antiforms; 2, they were modelled after the emplacement of the Ligurian Units that moved along a major detachment; 3, there are no synsedimen- tary Pliocene faults between the ridge and the basin but progressive unconformities as a result of deformations of the sedimentary cover; 4, there are no lacustrine deposits in these basins but they are mostly filled by meander and braided flood plain deposits, similar to what was recognised in the nearby East Tiber Valley (COLTORTI & PIERUCCINI, 1997A; 1997B) and, in the Barga Basin to the north (LANDI et al., 2003; COLTORTI et al., submitted).	cache/amq-413.pdf	txt/amq-413.txt