U-Pb zircon and (40)Ar-(39)Ar K-feldspar dating of syn-sedimentary volcanism of the Neoproterozoic Marica Formation: constraining the age of foreland basin inception and inversion in the Camaqua Basin of southern Brazil


Autoria(s): BORBA, Andre W.; MARIA, Ana; MIZUSAKI, P.; SANTOS, Joao Orestes S.; MCNAUGHTON, Neal J.; Onoe, Artur Takashi; HARTMANN, Leo A.
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

20/10/2012

20/10/2012

2008

Resumo

New U-Pb zircon and (40)Ar-(39)Ar K-feldspar data are presented for syn-sedimentary volcanogenic rocks from the Neoproterozoic Marica Formation, located in the southern Brazilian shield. Seven (of nine) U-Pb sensitive high-resolution ion microprobe analyses of zircons from pyroclastic cobbles yield an age of 630.2 +/- 3.4 Ma (2 sigma), interpreted as the age of syn-sedimentary volcanism, and thus of the deposition itself. This result indicates that the Marica Formation was deposited during the main collisional phase (640-620 Ma) of the Brasiliano II orogenic system, probably as a forebulge or back-bulge, craton-derived foreland succession. Thus, this unit is possibly correlative of younger portions of the Porongos, Brusque, Passo Feio, Abapa (Itaiacoca) and Lavalleja (Fuente del Puma) metamorphic complexes. Well-defined, step-heating (40)Ar-(39)Ar K-feldspar plateau ages obtained from volcanogenic beds and pyroclastic cobbles of the lower and upper successions of the Marica Formation yielded 507.3 +/- 1.8 Ma and 506.7 +/- 1.4 Ma (2 sigma), respectively. These data are interpreted to reflect total isotopic resetting during deep burial and thermal effects related to magmatic events. Late Middle Cambrian cooling below ca. 200 degrees C, probably related to uplift, is tentatively associated with intraplate effects of the Rio Doce and/or Pampean orogenies (Brasiliano III system). In the southern Brazilian shield, these intraplate stresses are possibly related to the dominantly extensional opening of a rift or a pull-apart basin, where sedimentary rocks of the Camaqua Group (Santa Barbara and Guaritas Formations) accumulated.

PRONEX-FAPERGS/CNPq

PRONEX-FAPERGS/CNPq

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil)

Identificador

BASIN RESEARCH, v.20, n.3, p.359-375, 2008

0950-091X

http://producao.usp.br/handle/BDPI/30351

10.1111/j.1365-2117.2007.00349.x

http://dx.doi.org/10.1111/j.1365-2117.2007.00349.x

Idioma(s)

eng

Publicador

WILEY-BLACKWELL

Relação

Basin Research

Direitos

restrictedAccess

Copyright WILEY-BLACKWELL

Palavras-Chave #LA-PLATA CRATON #GEOCHRONOLOGY #MAGMATISM #JUVENILE #PROVENANCE #ARGENTINA #ACCRETION #EVOLUTION #CORDOBA #SIERRAS #Geosciences, Multidisciplinary
Tipo

article

original article

publishedVersion