Cambios eustáticos y arquitectura estratigráfica de unidades costeras

Abstract

Eustatic 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.