U-Pb ages of detrital zircon grains for the Canastra Group and Passos Nappe units and U-Pb and Lu-Hf isotope analyses from orthogneisses: Provenance and tectonic implications, southern Brasilia Belt, Brazil

The age and tectonic setting of Mesoproterozoic to Neoproterozoic covers that occur along the southwestern margins of the Sao Francisco Craton (SFC) are still uncertain. This study reports new Pb-207/Pb-206 LA-ICPMS ages of detrital zircon grains from metasedimentary rocks of the Passos Nappe units and Canastra Group, and combined U-Pb and Lu-Hf analyses on igneous zircon from orthogneisses within the metasedimentary units. The U-Pb age spectra of detrital zircon grains of the Canastra Group comprises a wide range from (similar to)1.30-2.71 Ga with a significant Rhyacian component source ((similar to)2.1 Ga). The second major source is represented by Statherian grains ((similar to)1.6-1.7 Ga), and are similar to the Statherian interval at Espinhaco Basin. The youngest ages fall around (similar to)1.30 Ga. This peak age is compatible with the initial extension and sedimentation of the Carandai and Middle Espinhaco basins, which mark the second intracratonic rifting of the Sao Francisco Craton. Zircon grains from the metasedimentary rocks the Passos Nappe yielded a very prominent Rhyacian peak at ca. 2.10 Ga with some Statherian and Neoarchean contributions. All samples from the metasedimentary units show a prominent peaks at ca. 2.10 Ga, suggesting that most sedimentary sources derived from a Rhyacian substratum similar to the Mineiro belt, Natividade-Cavalcanti block, Campinorte Complex and Juiz de Fora Complex. Rhyacian age is compatible with U-Pb crystallization ages of felsic orthogneisses (2122 +/- 67 and 2117 +/- 23), enclosed as tectonic lenses in the Passos Nappe and the Canastra Group. These rocks show initial EHf(t) values between + 2.1 to -13.0 and + 10.0 and -1.8, indicating that these orthogneisses are derived from Rhyacian granitic rocks, which were formed either by fractionation or re-melting of juvenile magmas, and by the reworking of more ancient, mainly Archean crust. The new data and regional geologic correlations suggest evidence of Paleoproterozoic terrain in the southwestern margin of the SFC.