Alkaline basalts encrust enclaves of peridotites, most of which are spinel lherzolites. They have been discovered on the Adamaoua plateaux and in the Liri region (south of the Kapsiki plateau). The basalts have a porphyritic microlitic texture and the enclaves have a protogranular texture, consisting of olivine, orthopyroxene, clinopyroxene and spinel crystals. The forsterite (Fo89-91) and NiO (0.30-0.44) contents in olivine crystals, the Mg# (≈ 94) number of orthopyroxene and the low titanium contents in clinopyroxene (TiO2
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