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What is Granitoid Geochemistry in Congo Craton about?
This article presents new geochemical and geochronological data on granitoids from the Chaillu massif in the Congo Craton, revealing four distinct plutonic suites and their evolution related to crustal growth. The study identifies significant periods of magmatism, including TTG-type and sanukitoid-TTG-biotite granite associations, with zircon U-Pb dating indicating ages between 3012 ± 16 Ma and 2840 ± 9 Ma. The findings contribute to understanding the geodynamic evolution of the Congo Craton during the Arch
- Author
- L'Amoriate JC
- Language
- EN