Figure 1: a) Geological map of Cameroon with the three main domains of the Pan-African North-Equatorial fold belt (modified from [5]: (1) southern domain corresponding to the Yaoundé series thrust on the Congo Craton, (2) central domain, (3) northern domain. TBF, Tibati-Banyo Fault; CCSZ, Central Cameroon Shear Zone; SF, Sanaga Fault; ASZ, Adamaoua Shear Zone; NT, Ntem complex; DS, Dja series; NS, Nyong series. Bamenda area is marked by a white rectangle b) Geological map of the Akum-Bamenda Massif [5] showing the location of Bamenda town (Black filled square) : Contrasting Ba-Sr Granitoids from Bamenda Area, NW Cameroon: Sources Characteristics and Implications for the Evolution of the Pan African Fold Belt : Science and Education Publishing

Figure 1: a) Geological map of Cameroon with the three main domains of the Pan-African North-Equatorial fold belt (modified from [5]: (1) southern domain corresponding to the Yaoundé series thrust on the Congo Craton, (2) central domain, (3) northern domain. TBF, Tibati-Banyo Fault; CCSZ, Central Cameroon Shear Zone; SF, Sanaga Fault; ASZ, Adamaoua Shear Zone; NT, Ntem complex; DS, Dja series; NS, Nyong series. Bamenda area is marked by a white rectangle b) Geological map of the Akum-Bamenda Massif [5] showing the location of Bamenda town (Black filled square)

Journal of Geosciences and Geomatics. 2018, 6(2), 65-76 doi:10.12691/jgg-6-2-4