id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
amq-82	Giraudi, Carlo	QUATERNARY EVOLUTION OF THE PLAIN BETWEEN CASALE MONFERRATO AND VALENZA: IMPLICATIONS FOR THE TECTONICS OF THE MONFERRATO THRUST FRONT (PIEDMONT, NW ITALY)	2015	22	.pdf	application/pdf	17712	680	60	For this reason, the geological structure of the terti- ary bedrock lying below the Quaternary cover and some peculiar geomorphological and geological features of the Eastern Monferrato Hills are presented and discussed before the data on Quaternary sediments. 7. CONCLUSIONS The plain between the Po river and the Eastern Monferrato Hills consists of fluvial sediments lying on the Tertiary marine bedrock.	cache/amq-82.pdf	txt/amq-82.txt