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This study analyzes alkali basalts from the Dibi area in the Adamawa Plateau, Cameroon, focusing on their mineralogical, petrological, and geochemical characteristics. The findings reveal that the lavas consist of basanites and foidites with specific mineral compositions, indicating they are within-plate basalts with OIB-like features. The research contributes to understanding the petrogenetic processes and mantle source variability in the region, which has been underexplored compared to other areas of the

Author
Paterne
Language
EN

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