Fission track and U–Pb in situ dating applied to detrital zircon from the Vale do Rio do Peixe Formation, Bauru Group, Brazil
Combined methods of fission track (FTM) and U–Pb in situ zircon dating were applied to sedimentary samples from the Vale do Rio do Peixe Formation, Bauru Basin, Brazil. Detrital zircons of nine samples were determined by the FTM, and the obtained ages varied from 239 Ma–825 Ma, which can be grouped...
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Published in: | Journal of South American earth sciences Vol. 31; no. 2; pp. 298 - 305 |
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Abstract | Combined methods of fission track (FTM) and U–Pb
in situ zircon dating were applied to sedimentary samples from the Vale do Rio do Peixe Formation, Bauru Basin, Brazil. Detrital zircons of nine samples were determined by the FTM, and the obtained ages varied from 239 Ma–825 Ma, which can be grouped into four main populations as the 230–300 Ma, 460–490 Ma, 500–650 Ma and 696–825 Ma groups. The U–Pb data show two clear source areas: the Early Paleozoic to Neoproterozoic zircons, ranging from 445 ± 14 to 708 ± 18 Ma, and the Paleoproterozoic zircons, ranging from 1879 ± 23 to 2085 ± 27 Ma. Subordinate occurrences of Early Neoproterozoic to Mesoproterozoic zircons (836 ± 15 and 1780 ± 38 Ma) were identified. The combined information allows us to characterize Early Brazilian, Brazilian and Rhyacian material as the main source for the zircons, which are areas situated to west of the Bauru Basin (e.g., Goiás Massif) that have been incorporated into the sedimentary cycles in the Phanerozoic (mainly in the Paraná Basin). FT zircon ages reflect the main denudation processes of the South American Plate from Neoproterozoic to Early Triassic as those related to orogenic cycles of Early Brazilian, Brazilian, Famatinian/Cuyanian and Gondwanide.
► Detrital zircon of Bauru Basin, Brazil, dated by combined FT and U-Pb analyses. ► FT zircon ages reflect the main denudation processes of the South American Plate. ► U-Pb data shows two tectonic events: the Early Paleozoic and Neoproterozoic. ► The combined information allows characterizing main source for the zircons. |
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AbstractList | Combined methods of fission track (FTM) and U–Pb
in situ zircon dating were applied to sedimentary samples from the Vale do Rio do Peixe Formation, Bauru Basin, Brazil. Detrital zircons of nine samples were determined by the FTM, and the obtained ages varied from 239 Ma–825 Ma, which can be grouped into four main populations as the 230–300 Ma, 460–490 Ma, 500–650 Ma and 696–825 Ma groups. The U–Pb data show two clear source areas: the Early Paleozoic to Neoproterozoic zircons, ranging from 445 ± 14 to 708 ± 18 Ma, and the Paleoproterozoic zircons, ranging from 1879 ± 23 to 2085 ± 27 Ma. Subordinate occurrences of Early Neoproterozoic to Mesoproterozoic zircons (836 ± 15 and 1780 ± 38 Ma) were identified. The combined information allows us to characterize Early Brazilian, Brazilian and Rhyacian material as the main source for the zircons, which are areas situated to west of the Bauru Basin (e.g., Goiás Massif) that have been incorporated into the sedimentary cycles in the Phanerozoic (mainly in the Paraná Basin). FT zircon ages reflect the main denudation processes of the South American Plate from Neoproterozoic to Early Triassic as those related to orogenic cycles of Early Brazilian, Brazilian, Famatinian/Cuyanian and Gondwanide.
► Detrital zircon of Bauru Basin, Brazil, dated by combined FT and U-Pb analyses. ► FT zircon ages reflect the main denudation processes of the South American Plate. ► U-Pb data shows two tectonic events: the Early Paleozoic and Neoproterozoic. ► The combined information allows characterizing main source for the zircons. |
Author | de Godoy, M.C.T.F. Dias, A.N.C. Soares, C.J. Chemale, F. Tello, C.A.S. Iunes, P.J. Osório, A.M.A. Bruckmann, M.P. Guadagnin, F. |
Author_xml | – sequence: 1 givenname: A.N.C. surname: Dias fullname: Dias, A.N.C. organization: Dep. de Física, Química e Biologia – FCT/UNESP, 19060-900 Presidente Prudente-SP, Brazil – sequence: 2 givenname: C.A.S. surname: Tello fullname: Tello, C.A.S. email: tello@fct.unesp.br organization: Dep. de Física, Química e Biologia – FCT/UNESP, 19060-900 Presidente Prudente-SP, Brazil – sequence: 3 givenname: F. surname: Chemale fullname: Chemale, F. organization: Laboratório de Geocronologia,IG-UnB, 70904-970 Brasilia-DF, Brazil – sequence: 4 givenname: M.C.T.F. surname: de Godoy fullname: de Godoy, M.C.T.F. organization: Dep. de Física, Química e Biologia – FCT/UNESP, 19060-900 Presidente Prudente-SP, Brazil – sequence: 5 givenname: F. surname: Guadagnin fullname: Guadagnin, F. organization: Laboratório de Geocronologia,IG-UnB, 70904-970 Brasilia-DF, Brazil – sequence: 6 givenname: P.J. surname: Iunes fullname: Iunes, P.J. organization: Instituto de Física Gleb Wataghin – DRCC/UNICAMP, 13083-970 Campinas-SP, Brazil – sequence: 7 givenname: C.J. surname: Soares fullname: Soares, C.J. organization: Instituto de Geociências e Ciências Exatas – IGCE/UNESP, 13506-900 Rio Claro-SP, Brazil – sequence: 8 givenname: A.M.A. surname: Osório fullname: Osório, A.M.A. organization: Dep. de Física, Química e Biologia – FCT/UNESP, 19060-900 Presidente Prudente-SP, Brazil – sequence: 9 givenname: M.P. surname: Bruckmann fullname: Bruckmann, M.P. organization: Laboratório de Geocronologia,IG-UnB, 70904-970 Brasilia-DF, Brazil |
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in situ zircon dating were applied to sedimentary samples from the Vale do Rio do Peixe Formation, Bauru... |
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Title | Fission track and U–Pb in situ dating applied to detrital zircon from the Vale do Rio do Peixe Formation, Bauru Group, Brazil |
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