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The Costeiro domain integrates the Oriental terrane of the Ribeira belt, which encompasses arc-related orthogneisses of the Rio Negro complex (ca.790–605 Ma), with a well-documented subduction signature, and the high-grade metasedimentary rocks of the Sao Fidelis group. The arc-related rocks intruded the lower unit of the Sao Fidelis group, while both units are crosscut by syn-to late collision granitoids related to the development of different stages of the Brasiliano Orogeny (ca. 605–480 Ma). New U–Pb (LA-ICP-MS) data of detrital zircon grains from quartzites of the top unit of the Sao Fidelis group yielded a large spectrum of Mesoproterozoic and Paleoproterozoic ages, with subordinated Archean and Neoproterozoic ones. The largest age peaks occur at ca. 1.2 Ga and 2.2 Ga. The youngest detrital zircon of ca. 613 Ma, and metamorphic overprints, with ages varying from ca. 602 to 570 Ma bracket the age of sedimentation of the top unit. Two orthogneisses of the Rio Negro complex intruded within the basal unit of the Sao Fidelis Group rendered similar ages of ca.620 Ma. These orthogneisses and the basal unit of the Sao Fidelis group are interpreted as possible sources of the upper unit. The provenance pattern of the Sao Fidelis Group is similar to that of the Kaoko Belt, suggesting that the Angolan basement, where Mesoproterozoic ages are common, constitutes another important source area. |
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