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...

Descripció completa

Dades bibliogràfiques

Autors principals:	Ravazzi, Cesare, Deaddis, Massimiliano, Amicis, Mattia De, Marchetti, Mauro, Vezzoli, Giovanni, Zanchi, Andrea
Format:	Artigo
Idioma:	Inglês
Publicat:	Groupe français de géomorphologie 2012
Matèries:	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
Accés en línia:	https://doi.org/10.4000/geomorphologie.9794 https://hdl.handle.net/20.500.13089/gipk https://journals.openedition.org/geomorphologie/9794
Etiquetes:	Afegir etiqueta Sense etiquetes, Sigues el primer a etiquetar aquest registre!