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Le premier stratotype continental de quatre stades isotopiques successifs du Pléistocène moyen pour le bassin méditerranéen septentrional : le Vallo di Diano (Campanie, Italie)
Russo Ermoli, Elda; Juvigné, Etienne; Bernasconi, Stefano et al.
1995 • In Comptes Rendus de l'Académie des Sciences. Série 2a, Sciences de la Terre et des Planètes, 321 (10), p. 877-884

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Comptes_rendus_de_l'Académie_des_[...]Académie_des_bpt6k6410227s(1).pdf

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