The Cameroon Volcanic Line revisited: Petrogenesis of continental basaltic magmas from lithospheric and asthenospheric mantle sources

The volcanic activity of Mts Bambouto and Oku (Western Highlands) and of the Ngaoundere Plateau, in the continental sector of the Cameroon Volcanic Line, Equatorial West Africa, ranges in age from Oligocene to Recent. It is characterized by basaltic, alkali basaltic mid transitional basaltic series. Mineral chemistry, major and trace element bulk-rock compositions, and geochemical modelling suggest that the magmatic series evolved mainly at lore, pressure (2-4 kbar) through fractional crystallization of clinopyroxene and olivine +/- magnetite, at moderately hydrated (H2O = 0.5-1 wt %) and QFM (quartz-fayalite-magnetite) to QFM + 1 fO(2) conditions. Basalts from Ngaoundere (Miocene to Quaternary) and from the early activity (31-14 Ma) of the Western Highlands have incompatible trace element and Sr-Nd isotopic compositions similar to those of oceanic Cameroon Line basalts, pointing to a similar asthenospheric mantle source. By contrast, the late (15-4 Ma) Western Highlands basanites and alkali basalts have anomalously high concentrations of Sr, Ba and P, and low concentrations of Zr; which are exclusive features of continental Cameroon basalts.;The genesis of these latter magmas is consistent with derivation from an incompatible element enriched, amphibole-bearing lithosheric mantle source. Western Highlands basalts show a continuous spectrum from high to low Sr-Ba-P compositions, and may result from variable amounts of mixing between melts derived from an anhydrous lherzolite source (asthenospheric component) and melts from an amphibole-bearing peridotite source (lithospheric HSr component). New 40Ar/39Ar ages for Mts Oku and Bambouto basalts, combined with previous 40Ar/39Ar and K/Ar ages of basaltic and silicic volcanics and with volcanics, and with volcanic stratigraphy, suggest a NE-SW younging of the Peak magmatic activity in the Western Highlands. This SW younging trend extending from the Oligocene volcanism in northern Cameroon (e.g, Mt Oku) to the still active Mt Cameroon, suggests that the African plate is moving above a deep-seated mantle thermal anomaly. However the age and location of the Ngaoundere volcanism does not conform to the NE-SW younging trend, implying that the continental sector of the Cameroon Volcanic Line cannot be easily interpreted as the surface expression of a single hotspot system.