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The study investigates the Medina batholith and associated granitic migmatites in the Araçuaí orogen of SE Brazil, revealing a complex history of granite production spanning from 630 to 480 Ma. The Medina batholith is characterized by high alkali and halogen contents, low CaO, and high FeOt/(FeOt + MgO) ratios, indicating it as a typical ferroan A-type granite formed during post-collisional anatexis. U-Pb dating suggests a significant thermal event around 500 Ma, likely linked to a mantle plume that trigger

Author

Beatriz Da Silva Lima

Language

EN