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Accepted Version For Publication Post Print The Original Or

Accepted Version For Publication Post Print The Original Or

2016-6-16During the post-Calabrian and early Holocene period the Subapennine clays were eroded by the sea to form platforms above which calcarenite and sandy deposits transgressively accumulated forming coastal terraces sloping towards the present shoreline Ricchetti 1970. There is little coastal topography except the gently incised stream systems

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