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Eustatic changes and stratigraphie architecture of Coastal Units

dc.contributor.authorDabrio, Cristino José
dc.contributor.authorPolo, María Dolores
dc.date.accessioned2016-04-08T09:08:58Z
dc.date.available2016-04-08T09:08:58Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/11814
dc.description.abstractEustatic 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 eventsen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherEustasyen_US
dc.subject.otherStratigraphic architectureen_US
dc.subject.otherCoastal depositsen_US
dc.subject.otherLittoralen_US
dc.subject.otherPleistoceneen_US
dc.subject.otherHoloceneen_US
dc.subject.otherIberian Peninsulaen_US
dc.titleCambios eustáticos y arquitectura estratigráfica de unidades costerasen_US
dc.titleEustatic changes and stratigraphie architecture of Coastal Unitseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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