Abstract
The Nyos volcano located in the Oku Volcanic Group (OKVG) of the CVL is unique because it hosts basanite and alkaline basalts in association with tholeiitic basalts. The aim of this study is to constrain the petrogenesis of these rock types from their geochemical characteristics. Similarity in Zr/Hf and Nb/Ta ratios of both alkaline and tholeiitic basalts strongly indicated their derivation from the same mantle source.