Geochronology of Precambrian basement rocks from Ibadan, Southwestern Nigeria

Physics

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Scientific paper

A Sb-Sr isochron age of 2205 ± 70 my given by a granite gneiss demonstrates that Eburnean granitic and older metamorphic rocks are widespread in southwestern Nigeria. In the Ibadan area the reactivation due to the Pan-African thermo-tectonic event (600 ± 150 my) appears to have been largely thermal in character. Its termination some 480 my ago is dated by K-Ar ages on separated minerals and on one member of an unmetamorphosed basalt dyke suite. The host rocks to the Eburnean granite gneiss may have crystallized during the 2800 ± 200 my Liberian cycle.

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