id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
amq-277	Loiacono, Francesco	Growth process of a long-lived Late Pleistocene spit along the Adriatic coast (Brindisi, southern Italy)	2010	11	.pdf	application/pdf	6768	317	55	The sedimentary body is composed of bioclastic grainstones and rudstones arranged in well bedded succession made up of about 30° SE dipping beds and bed sets in a cyclic alternation of coarse-grained planar units (Facies A), small- to medium-scale trough cross-bedded units (Facies B), and Bichordites-bearing beds (Facies C). From the bottom: Facies B in a thick bed (trough cross bedding, locally hummocky, foreset migrating landward, on the right) interpreted a rip channel or a large swale cut at the top by a flat erosional surface (middle part of the photo); Facies A (very coarse sand, plane bedding), evolving to thin beds of Facies B (low angle cross bed- ding, locally bioturbated) referred to a new elementary sequence.	cache/amq-277.pdf	txt/amq-277.txt