Publicação: Tectonic and stratigraphic evolution of the Punta del Este and Pelotas basins (offshore Uruguay)
dc.contributor.author | Morales, Ethel | |
dc.contributor.author | Chang, Hung Kiang [UNESP] | |
dc.contributor.author | Soto, Matias | |
dc.contributor.author | Correa, Fernando Santos [UNESP] | |
dc.contributor.author | Veroslavsky, Gerardo | |
dc.contributor.author | Ana, Hector de Santa | |
dc.contributor.author | Conti, Bruno | |
dc.contributor.author | Daners, Gloria | |
dc.contributor.institution | Fac Ciencias | |
dc.contributor.institution | Universidade Estadual Paulista (Unesp) | |
dc.contributor.institution | ANCAP | |
dc.date.accessioned | 2018-11-29T01:34:34Z | |
dc.date.available | 2018-11-29T01:34:34Z | |
dc.date.issued | 2017-11-01 | |
dc.description.abstract | Regional 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. | en |
dc.description.affiliation | Fac Ciencias, Inst Ciencias Geol, Igua 4225, Montevideo 11400, Uruguay | |
dc.description.affiliation | Univ Estadual Paulista, Inst Geociencias & Ciencias Exatas, Campus Rio Claro, Sao Paulo, Brazil | |
dc.description.affiliation | ANCAP, Explorac & Prod, Paysandu S-N & Av Libertador, Montevideo 11100, Uruguay | |
dc.description.affiliationUnesp | Univ Estadual Paulista, Inst Geociencias & Ciencias Exatas, Campus Rio Claro, Sao Paulo, Brazil | |
dc.format.extent | 415-426 | |
dc.identifier | http://dx.doi.org/10.1144/petgeo2016-059 | |
dc.identifier.citation | Petroleum Geoscience. Bath: Geological Soc Publ House, v. 23, n. 4, p. 415-426, 2017. | |
dc.identifier.doi | 10.1144/petgeo2016-059 | |
dc.identifier.issn | 1354-0793 | |
dc.identifier.lattes | 1989662459244838 | |
dc.identifier.uri | http://hdl.handle.net/11449/165863 | |
dc.identifier.wos | WOS:000414247600003 | |
dc.language.iso | eng | |
dc.publisher | Geological Soc Publ House | |
dc.relation.ispartof | Petroleum Geoscience | |
dc.relation.ispartofsjr | 0,530 | |
dc.rights.accessRights | Acesso restrito | |
dc.source | Web of Science | |
dc.title | Tectonic and stratigraphic evolution of the Punta del Este and Pelotas basins (offshore Uruguay) | en |
dc.type | Artigo | |
dcterms.rightsHolder | Geological Soc Publ House | |
dspace.entity.type | Publication | |
unesp.author.lattes | 1989662459244838[2] | |
unesp.campus | Universidade Estadual Paulista (UNESP), Instituto de Geociências e Ciências Exatas, Rio Claro | pt |
unesp.department | Geologia Aplicada - IGCE | pt |