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(Referência obtida automaticamente do Web of Science, por meio da informação sobre o financiamento pela FAPESP e o número do processo correspondente, incluída na publicação pelos autores.)

Sedimentation of the Cretaceous Bauru Group in Sao Paulo, Parana Basin, Brazil

Texto completo
Autor(es):
de Paula e Silva, Flavio [1] ; Kiang, Chang Hung [1] ; Caetano-Chang, Maria Rita [1]
Número total de Autores: 3
Afiliação do(s) autor(es):
[1] UNESP, LEBAC, Inst Geociencias & Ciencias Exatas, BR-13506900 Rio Claro, SP - Brazil
Número total de Afiliações: 1
Tipo de documento: Artigo Científico
Fonte: Journal of South American Earth Sciences; v. 28, n. 1, p. 25-39, JUL 2009.
Citações Web of Science: 14
Resumo

The post-basaltic sediments of the Cretaceous Bauru Group in the Parana Basin cover an area of 117,000 km(2) in Sao Paulo State, and are subdivided into the Caiua, Pirapozinho, Santo Anastacio, Birigui, Aracatuba, Adamantina and Marilia formations. The sedimentation of Bauru Group was controlled by a combination of post-basaltic tectonism (responsible for the migration of the depocenters), erosion and climatic changes. Three main depositional phases are separated by two erosive/non-depositional phases defining depositional sequences. The fluvial-lacustrine deposition represented by the Caiua/Pirapozinho formations (first sequence), initially filled the basaltic substratum troughs. After an erosional interval, the Santo Anastacio Formation was deposited and overlapped (eastward) underlying beds (second sequence). Renewed erosion and tectonism initiated the last depositional sequence, with the migration of the depocenter to the Queiroz depression. High topographic gradients initially favored the accumulation of fluvial deposits of braided systems of the Birigui Formation. With the enlarging of the depositional area, a lacustrine system was formed (Aracatuba Formation) and overlapped by a fluvial system with progradation of lacustrine deltas (Adamantina Formation). The sedimentation of the Bauru Group ceased with deposition of marginal fans of Marilia Formation. (C) 2009 Elsevier Ltd. All rights reserved. (AU)

Processo FAPESP: 04/06296-0 - Estudos geológicos de superfície aplicados à prospecção de água subterrânea em área de ocorrência do Grupo Bauru (K), região Sudoeste do Estado de São Paulo
Beneficiário:Chang Hung Kiang
Modalidade de apoio: Auxílio à Pesquisa - Regular