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Geochemical Characterization of Pegmatites in the Alabata Area, Sheet 260 SE Abeokuta Nigeria: Implications for Petrogenesis and Sustainable Rare Metal Exploitation

Enwerem Chima Kingslay, Ahmed Isah Haruna, Abubakar Sadiq Maigari, Adamu Hassan Muktar, Abdulmuhyi Yahaya Yaro

Abstract

The Alabata pegmatites plot within the continental field on a K?O–TiO?–P?O? discrimination diagram, affirming a crustal origin linked to granitic magmatism in continental settings. TiO? versus SiO? data suggest a metasedimentary source with igneous contributions, implying a mixed continental margin environment with both volcanic and sedimentary processes. Depth-related Rb– Sr ratio variations reveal source heterogeneity from multiple magmatic, metamorphic, and recycling events. Major?element trends, Harker plots, and peraluminous indices confirm highly evolved, S-type granitic affinities formed by fractional crystallization and crustal melting under collisional regimes. Trace?element spider patterns indicate LILE enrichment and HFSE depletion typical of crustal or subduction?related melts, highlighting their potential for Li, REE, and Cs mineralization.

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