U-Pb dating of detrital zircon and its implications for provenance of the sediments of Penedo Formation, Basin of Sergipe-Alagoas, NE Brazil
DOI:
https://doi.org/10.11606/issn.2316-9095.v18-126934Keywords:
Provenance Analysis, U-Pb Dating, Penedo Formation, Sergipe-Alagoas Basin.Abstract
The Penedo Formation represents a river-delta system of braided pattern that belongs to the rift stage of the Sergipe-Alagoas Basin. This work was executed on the classical outcrop section in the city of Penedo, state of Alagoas, Brazil, and named here as PDO-01. The methodology consisted of paleocurrent analysis allied to U-Pb dating of detrital zircon by laser ablation mass spectrometry. The sedimentary record of paleocurrents indicate a contribution coming from north, as the analyzed crystals yielded ages ranging from Mesoarchean (3098 ± 33 Ma) to Paleozoic (530 ± 12 Ma), that can be gathered in five groups (G1 to G5). From this analysis, the following sources were proposed: for the first group (G1), Neoproterozoic granites (~670 Ma) from the Pernambuco-Alagoas Domain; for the second group (G2), the rocks of the Cabrobó Complex (~0.9 – 1.2 Ga); for the third group (G3), the rocks of the Arapiraca Complex with Paleoproterozoic ages (~1.6 – 2.2 Ga); and for the fourth and fifth groups (G4 and G5), the rocks of the Nicolau Campo Grande Complex, with Neoarquean ages (~2.4 – 3.0 Ga).
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