Tectonic and stratigraphic evolution of the Punta del Este and Pelotas basins (offshore Uruguay)

dc.contributorFac Ciencias
dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorANCAP
dc.date.accessioned2018-11-29T01:34:34Z
dc.date.available2018-11-29T01:34:34Z
dc.date.created2018-11-29T01:34:34Z
dc.date.issued2017-11-01
dc.identifierPetroleum Geoscience. Bath: Geological Soc Publ House, v. 23, n. 4, p. 415-426, 2017.
dc.identifier1354-0793
dc.identifierhttp://hdl.handle.net/11449/165863
dc.identifier10.1144/petgeo2016-059
dc.identifierWOS:000414247600003
dc.identifier1989662459244838
dc.description.abstractRegional seismic reflection profiles and well data from the Uruguayan margin were integrated in order to analyse and illustrate its tectonic and stratigraphic evolution. The evolution of the Punta del Este and Pelotas basins is divided into four major phases: pre-rift (Palaeozoic); rift (Jurassic-Early Cretaceous); transition (Barremian-Aptian) and post-rift (AptianPresent). Each of these phases is characterized by a specific structural configuration and a stratigraphic architecture related to basin type, tectonic elements, sediment supply and base-level changes. During the geological evolution of the Uruguayan continental margin, a NE migration of depocentres occurred. The Cretaceous depocentre is located in the Punta del Este Basin, while the Cenozoic depocentre is located in the Pelotas Basin.
dc.languageeng
dc.publisherGeological Soc Publ House
dc.relationPetroleum Geoscience
dc.relation0,530
dc.rightsAcesso restrito
dc.sourceWeb of Science
dc.titleTectonic and stratigraphic evolution of the Punta del Este and Pelotas basins (offshore Uruguay)
dc.typeArtículos de revistas


Este ítem pertenece a la siguiente institución