Geochemical signatures and magmatic processes of Bindiba granitoids: Neoproterozoic crustal evolution of the central domain of the Pan-African fold belt

Key Points

• Bindiba granitoids show distinct geochemical signatures, revealing insights into magmatic processes.
• Geochemical analysis highlights Neoproterozoic crustal evolution, indicating its significance in the Pan-African fold belt.
• This observational analysis involves detailed geochemical profiling of granitoid samples across the region.
• Findings underscore the importance of these processes for understanding crustal development and tectonic history.