Sucessão sedimentar do Grupo Bauru na região de Pirapozinho (SP)

• Autor(a) principal: De Paula E Silva, Flavio [UNESP]
• Data de Publicação: 2006
• Outros Autores: Chang, Hung Kiang [UNESP], Caetano-Chang, Maria Rita [UNESP], Stradioto, Márcia Regina [UNESP]
• Tipo de documento: Artigo
• Idioma: por
• Título da fonte: Repositório Institucional da UNESP
• Texto Completo: http://www.periodicos.rc.biblioteca.unesp.br/index.php/geociencias/article/view/118; http://hdl.handle.net/11449/69319
• topic: Bauru group; Depositional paleo-environment; Stratigraphy; climate conditions; Cretaceous; depositional environment; lacustrine environment; lithostratigraphy; paleoenvironment; sedimentary sequence; Brazil; Parana Basin; Pirapozinho; Sao Paulo [Brazil]; South America

There is yet enthusiastic debate in the literature about the environmental conditions that originated the Cretaceous deposits of the Bauru Group, despite many authors accept that arid climatic conditions widely dominant at the base, evolved to chiefly fluvial-lacustrine conditions at the intermediate portion, and to arid conditions again at the top of the unit. The Bauru Group covers an area of about 117.000 km 2 of the Paraná Basin in São Paulo State territory. Core samples of this lithostratigraphic unit collected from a drill hole at Pirapozinho (Southwest of the São Paulo State) are described and together with well log data brought new information that do not agree with the described model. It was identified in this well the Caiuá, Pirapozinho, Santo Anastácio, Araçatuba and Adamantina formations. The study of these core samples clearly showed the dominance of hydrodynamic sedimentary structures and high to medium intensity of bioturbation in whole profile. These characteristics observed in core samples and compared to patterns of geophysical logs testify the dominance of fluvial processes in the Bauru Group deposition at the studied area. These new data suggests that the paleo-environmental evolution of the unit was much more complex, showing strong lateral and vertical changes that diverges from the model more widely accepted in the literature.