Dabrio, Cristino JoséPolo, María Dolores2016-04-082016-04-081996http://hdl.handle.net/10272/11814Eustatic movements generate intricate patterns of coastal units. The resulting stratigraphyc architecture depends on eustasy, sediment supply and local tectonics. Tri-dimensional relations due to sea-level changes are interesting because they allow to reconstruct the existence and magnitude of eustatic changes, to understand the role of coastal deposits during the evolution of a basin margin, and to correlate depositional eventsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/EustasyStratigraphic architectureCoastal depositsLittoralPleistoceneHoloceneIberian Peninsulajournal articleopen access