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So close and yet so far: U–Pb geochronological constraints of the Jaibaras Rift Basin and the intracratonic Parnaíba Basin in SW Gondwana

Published online by Cambridge University Press:  06 April 2021

Rodrigo I. Cerri*
Affiliation:
Departamento de Geologia, Instituto de Geociências e Ciências Exatas, Universidade Estadual Paulista - Unesp, Avenida 24-A, Bela Vista, 178, 13506-900, Rio Claro, SP, Brazil
Lucas V. Warren
Affiliation:
Departamento de Geologia, Instituto de Geociências e Ciências Exatas, Universidade Estadual Paulista - Unesp, Avenida 24-A, Bela Vista, 178, 13506-900, Rio Claro, SP, Brazil
Filipe G. Varejão
Affiliation:
Departamento de Geologia, Universidade Federal de Ouro Preto, Campus Morro do Cruzeiro s/n, 35430-000, Ouro Preto, MG, Brazil
Alex J. Choupina A. Silva
Affiliation:
Instituto de Engenharia, Ciência e Tecnologia, Universidade Federal dos Vales do Jequitinhonha e Mucuri (UFVJM), Janaúba, MG, Brazil
Cristiano Lana
Affiliation:
Departamento de Geologia, Universidade Federal de Ouro Preto, Campus Morro do Cruzeiro s/n, 35430-000, Ouro Preto, MG, Brazil
Mario L. Assine
Affiliation:
Departamento de Geologia, Instituto de Geociências e Ciências Exatas, Universidade Estadual Paulista - Unesp, Avenida 24-A, Bela Vista, 178, 13506-900, Rio Claro, SP, Brazil
*
Author for correspondence: Rodrigo I. Cerri, Email: roocerri@gmail.com

Abstract

Several sag-type basins apparently developed from rift systems, but there is no consensus about how and if these grabens influenced the sedimentation of the post-rift thermal subsidence phase. The Ediacaran Jaibaras Rift Basin is one of the best-exposed sedimentary records among the NE Brazil late Precambrian – early Cambrian rift system, cropping out at the eastern margin of the intracratonic Parnaíba Basin and extending below it towards the west. Here we present detrital zircon U–Pb ages of rocks from the Jaibaras (Aprazível Formation) and Parnaíba (Ipu Formation) basins, in order to understand the provenance patterns, maximum depositional ages (MDA) and age relationship between these units. The MDA for the Aprazível Formation (c. 499 ± 5 Ma) indicates a Cambrian age for the upper part of the Jaibaras Basin. The bulk U–Pb data indicate that the Ipu Formation started to deposit during late Cambrian and/or Early Ordovician time, despite its MDA (c. 528 ± 11 Ma) being older than that of the Aprazível Formation. Detrital zircon provenance suggests that the primary source areas for the early deposits of the Parnaíba Basin were mountains related to the Brasiliano Orogeny to the south and SE (e.g. Rio Preto and Riacho do Pontal metamorphic belts). Finally, our data emphasize the key change in source areas from the rift to the initial deposition of the intracratonic phase, indicating major depositional style changes between both basins after the Gondwana assembly.

Type
Original Article
Copyright
© The Author(s), 2021. Published by Cambridge University Press

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So close and yet so far: U–Pb geochronological constraints of the Jaibaras Rift Basin and the intracratonic Parnaíba Basin in SW Gondwana
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So close and yet so far: U–Pb geochronological constraints of the Jaibaras Rift Basin and the intracratonic Parnaíba Basin in SW Gondwana
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