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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.)

Geodynamic evolution of the Minas Basin, southern Sao Francisco Craton (Brazil), during the early Paleoproterozoic: Climate or tectonic?

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Autor(es):
Rossignol, Camille [1, 2] ; Alkmim, Fernando [1]
Número total de Autores: 2
Afiliação do(s) autor(es):
[1] Univ Fed Ouro Preto, Appl Isotope Res Grp, Dept Geol, Rua Diogo Vasconcelos 122, BR-35400000 Ouro Preto, MG - Brazil
[2] Univ Sao Paulo IAG USP, Inst Astron Geofis & Ciencias Atmosfer, Dept Geofis, Rua Matao 1226, BR-05508090 Sao Paulo, SP - Brazil
Número total de Afiliações: 2
Tipo de documento: Artigo Científico
Fonte: Journal of South American Earth Sciences; v. 101, AUG 2020.
Citações Web of Science: 0
Resumo

Like many other cratons around the world, the Sao Francisco Craton is characterized by an early Paleoproterozoic (2.5-2.1 Ga) unconformity that is reported worldwide as the result of global glacial events leading to a major sea-level drop. To document the duration and the cause(s) of the stratigraphic hiatus in the Sao Francisco Craton, this study provides U-Pb dates obtained on detrital zircon grains from the Piracicaba Group, which directly overlies the unconformity. Our results show that this sedimentary unit is younger than 2333 +/- 11 Ma and consequently deposited during the late Siderian or the early Rhaycian. This maximum depositional age demonstrates that the early Paleoproterozoic stratigraphic gap lasted for at least 60 Ma. Based on quantitative analyses of the age distribution of the Piracicaba Group, we evidence a major shift in sedimentary provenance between the sedimentary units located below and above the unconformity. This change is interpreted to be directly related to the development of a subduction system along the southern and eastern margins of the Sao Francisco proto-craton. Our results indicate that regional geodynamic events, and not only global glacial events and their consequences, must be accounted for in Earth system models for the early Paleoproterozoic. (AU)

Processo FAPESP: 18/02645-2 - Cronestratigrafia e rastreamento isotópico do Supergrupo Minas, Paleoproterozóico
Beneficiário:Camille Yann Rossignol
Modalidade de apoio: Bolsas no Brasil - Pós-Doutorado
Processo FAPESP: 15/16235-2 - Evolução da vida e oxigenação da Terra primitiva: uma perspectiva a partir da América do Sul
Beneficiário:Pascal Andre Marie Philippot
Modalidade de apoio: Auxílio à Pesquisa - Programa SPEC