The last 40 ka evolution of the Central Po Plain between the Adda and Serio rivers

We reconstructed the geological evolution and the history of the fluvial network in the central part of the Po Plain in Lombardy, northern Italy, since the Middle Würm. We focused on evidences of dissection and incision of former rivers into the large outwash fans originating from piedmont glaciers...

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Xehetasun bibliografikoak

Egile Nagusiak:	Ravazzi, Cesare, Deaddis, Massimiliano, Amicis, Mattia De, Marchetti, Mauro, Vezzoli, Giovanni, Zanchi, Andrea
Formatua:	Artigo
Hizkuntza:	Inglês
Argitaratua:	Groupe français de géomorphologie 2012
Gaiak:	Dernier Maximum Glaciaire géomorphologie fluviale plaine alluviale réseau fluvial stratigraphie événementielle plaine du Pô Last Glacial Maximum alluvial geomorphology alluvial plain fluvial network event stratigraphy Po Plain
Sarrera elektronikoa:	https://doi.org/10.4000/geomorphologie.9794 https://hdl.handle.net/20.500.13089/gipk https://journals.openedition.org/geomorphologie/9794
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