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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.)

Paleozoic Parana Basin transition from collisional retro-foreland to pericratonic syneclise: Implications on the geodynamic model of Gondwana proto-Andean margin

Texto completo
Autor(es):
Henrique-Pinto, R. [1] ; Basei, M. A. S. [1] ; Santos, P. R. [1] ; Saad, A. R. [1] ; Milani, E. J. [2] ; Cingolani, C. A. [3] ; Frugis, G. L. [1]
Número total de Autores: 7
Afiliação do(s) autor(es):
[1] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, SP - Brazil
[2] Tecton Grp, Petrobras Res Ctr, Explorat R&D, BR-21941915 Rio De Janeiro, RJ - Brazil
[3] Univ Nacl La Plata, Fac Ciencias Nat & Museo, La Plata, Buenos Aires - Argentina
Número total de Afiliações: 3
Tipo de documento: Artigo Científico
Fonte: Journal of South American Earth Sciences; v. 111, NOV 2021.
Citações Web of Science: 0
Resumo

Providing significant advancements in the knowledge and development of the global plate tectonic theory, the Paran ` a Basin records a long period of sedimentary accumulation with evidence of substantial climatic and biostratigraphic changes throughout most all of the Phanerozoic. Two cycles of sedimentation are identified in the lowermost sequences (Rio Ivai and Paran'a groups), followed by a similar to 50 Ma gap until the deposition of the early Gondwanic cycle (Itarare' Group). The literature suggests that some of those depositional cycles were influenced by episodes of terrane accretion during the amalgamation of the Gondwana Supercontinent. The paleotopography generated by the Ocloyic orogeny (460-430 Ma) likely resulted in flexural subsidence in the lowermost stratigraphic cycles of the Paran'a Basin. In response to dynamic topography, the forebulge probably shifted to a system dominated by long-wavelength propagation developed over a distance of more than 800 km, most likely due to the influence of the subducted oceanic lithosphere of Panthalassa. The presence of Ordovician sources in the pre-Carboniferous sequences supports a provenance of exhumed Famatinian magmatic arc and associated rocks given that Ordovician magmatic activity is not recorded anywhere else in the cratonic regions. Furthermore, important detrital zircon population yielding Cambrian ages, likely derived from Eastern Pampean Range. In additional, the gap between crystallization and depositional ages within the Paran'a Basin supports a model that transitions from a collisional retro-foreland basin to a pericratonic syneclise after the deposition of the Paran'a Group. (AU)

Processo FAPESP: 19/02320-9 - Investigação das áreas fontes da Bacia do Paraná á partir do estudo isotópico de zircões detríticos: implicações para os modelos geodinâmicos da margem sudoeste do Gondwana
Beneficiário:Renato Henrique Pinto
Linha de fomento: Bolsas no Brasil - Pós-Doutorado
Processo FAPESP: 15/03737-0 - O Cráton Rio de la Plata e o Gondwana Ocidental
Beneficiário:Miguel Angelo Stipp Basei
Linha de fomento: Auxílio à Pesquisa - Temático