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This paper reviews the geochronology of the São Luís Craton and Gurupi Belt in Brazil, highlighting the complex geological evolution of these regions through various isotopic analyses. Key findings include distinct ages for different lithostratigraphic units, with implications for understanding the Paleoproterozoic history and subsequent Brasiliano reworking. The study emphasizes the integration of Rb-Sr and Sm-Nd isotopic data to elucidate the geological framework and evolution of these cratonic areas.

Author

Eduardo Breda

Language

EN