Integrated analysis reveals lithium exploration potential in granitoids from the Pamsi area, suggesting future studies.
This study presents an integrated petrographic and geochemical investigation of granitoid and metamorphic rocks from the Pamsi locality in the North Cameroon Domain of the Pan-African Fold Belt. Field observations, microscopic analysis, and whole-rock geochemistry reveal five main lithological units: amphibole-biotite granite, leucogranite, granodiorite, orthogneiss, and amphibolite. These rocks form a calc-alkaline suite ranging from syeno-diorite to granite, classified as I-type, sub-alkaline, potassic to hyperpotassic, and predominantly peraluminous to metaluminous. Geochemical signatures include strong LREE enrichment, negative Eu anomalies in most samples, and multi-element patterns showing negative Ta-Nb, Sr, and Ti anomalies with positive Th, Zr, and U anomalies, characteristic of differentiated magmas from mixed crustal-mantle sources. Tectonic discrimination diagrams indicate volcanic arc to syn-collisional settings consistent with Pan-African orogenesis. Pathfinder element analyses reveal preliminary indications of lithium exploration potential, with samples N11 and N51 showing notable cesium enrichment (8.80–11.30 ppm) and elevated Cs/Rb ratios. Based on established geochemical correlations—and pending direct lithium measurements—estimated lithium contents of 200–800 ppm are proposed as preliminary targets for further investigation. These results highlight the Pamsi area as a promising prospect for lithium mineralization associated with evolved pegmatitic systems, warranting systematic follow-up studies.
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Kepnamou et al. (2026) studied this question.
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