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The Tectonic Evolution of the São Gabriel Terrane, Dom Feliciano Belt, Southern Brazil: The Closure of the Charrua Ocean

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Geology of Southwest Gondwana

Part of the book series: Regional Geology Reviews ((RGR))

Abstract

The Dom Feliciano Belt (DFB) is an important Neoproterozoic to Cambrian orogenic complex, extending from eastern Uruguay to southern Brazil. It comprises a collage of oceanic domains and continental fragments developed between 0.9 and 0.54 Ga between the Rio de La Plata Craton (RLPC), Nico Perez Terrane (NPT) and Kalahari Craton. In southern Brazil, the DFB comprises two metamorphic-granitic terranes, a batholith and a foreland basin that cover all units. The São Gabriel Terrane (SGT) consists of two Neoproterozoic (Tonian and Cryogenian) juvenile arcs and a late-collisional basin, interleaving with relicts of ophiolitic complexes. A review of the geologic and geochronological data of the SGT is presented. Sm–Nd TDM model ages between 1.2 and 0.8 Ga and positive ɛNd(t) values between +1 and +5 characterize the SGT units. Plate tectonic evolution started with the opening of the Charrua Ocean to the east of the RLPC and west of NPT, between 0.93 and 0.90 Ga. An intraoceanic island arc (Passinho Arc), between 0.89 and 0.86 Ga, and a continental margin arc (São Gabriel Arc), between 0.77 and 0.72 Ga, was generated by eastward and westward subduction and was subsequently accreted to the western margin of the NPT, between 0.71 and 0.70 Ga. The post-collisional stage is marked by the emplacement of late orogenic granites (0.70–0.68 Ga). The late orogenic Pontas do Salso basin presents zircon provenance between 0.86 and 0.68 Ga and represents the collapse of the SGT.

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Acknowledgements

We would like to acknowledge the Brazilian National Council for Scientific and Technological Development (CNPq) for the research grants, the Geoscience Institute of Rio Grande do Sul Federal University (UFRGS) for field work support and laboratories, and the Geochronology Research Center of São Paulo University (USP), for the access to LA-MC-ICP-MS laboratories. We are grateful to reviewers for the helpful comments and suggestions and to the editors for comments and editorial handling of the manuscript.

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Authors and Affiliations

  1. Geosciences Institute, Federal University of Rio Grande do Sul (UFRGS), Av. Bento Gonçalves, 9500, Porto Alegre, RS, CEP: 91501-970, Brazil

    Ruy Paulo Philipp

  2. Geosciences Institute, Federal Unversity of Brasília (UnB), Campus Universitário Darcy Ribeiro ICC—Ala Central, Brasilia, DF, CEP: 70.910-900, Brazil

    Marcio Martins Pimentel

  3. Geosciences Institute, Geochronological Research Center (CEPEGEO), São Paulo University (USP), R. do Lago, 562—Vila Universitaria, São Paulo, SP, CEP: 05508-080, Brazil

    Miguel Angelo Stipp Basei

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  1. GZG—Structural Geology and Geodynamics University of Göttingen, Göttingen, Germany

    Siegfried Siegesmund

  2. Geosciences Institute, University of São Paulo, São Paulo, Brazil

    Miguel A. S. Basei

  3. Departamento de Geodinámica Interna, Universidad de la República, Montevideo, Uruguay

    Pedro Oyhantçabal

  4. GZG—Structural Geology and Geodynamics University of Göttingen, Göttingen, Germany

    Sebastian Oriolo

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Philipp, R.P., Pimentel, M.M., Basei, M.A.S. (2018). The Tectonic Evolution of the São Gabriel Terrane, Dom Feliciano Belt, Southern Brazil: The Closure of the Charrua Ocean. In: Siegesmund, S., Basei, M., Oyhantçabal, P., Oriolo, S. (eds) Geology of Southwest Gondwana. Regional Geology Reviews. Springer, Cham. https://doi.org/10.1007/978-3-319-68920-3_10

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