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The Monte Sporno limely marly Flysch type sediments outcropping in Po Valley side of Northern Appenninies, are 1,800 metres thick and are on micropalaenthological basis, Paleocene to Middle Eocene age.

The Monte Sporno limely marly Flysch type sediments outcropping in Po Valley side of Northern Appenninies, are 1,800 metres thick and are on micropalaenthological basis, Paleocene to Middle Eocene age.