Dabrio González, Cristino JoséPolo Camacho, Dolores2023-06-202023-06-2019960213-683Xhttps://hdl.handle.net/20.500.14352/56812Eustatic movements generate intricate patterns of coastal units. The resulting stratigraphyc architecture depends on eustasy sediment supply and local tectonics. Tri-dimensional relatians due to sea-level changes are interesting because they allow to reconstruct the existence and magnitude of eustatic changes, to undersland the rofe of coastal deposits during the evolution of a basin margin, and to correlate depositional events.spajournal articlehttp://www.sociedadgeologica.es/publicaciones_geogaceta.htmlopen access551.7EustasyStratigraphic architectureCoastal depositsLitoralPleistoceneHoloceneIberian PeninsulaGeología estratigráfica2506.19 Estratigrafía