Figure 11. a) Molar diagram CaO/(MgO+FeOt) vs Al2O3/(MgO+FeOt) for the Bamenda granites. b) La/Yb vs Gd/Yb showing the trend of the residual garnet in the source and the positions of Bamenda granitoids and Himalayan leucogranites (HHL & THL).

From

Contrasting Ba-Sr Granitoids from Bamenda Area, NW Cameroon: Sources Characteristics and Implications for the Evolution of the Pan African Fold Belt

Gus Djibril KOUANKAP NONO, Pierre WOTCHOKO, Alice MAGHA, Sylvestre GANNO, Ndam NJOYA, Aloysius AFAHNWIE NGAMBU, Jean Paul NZENTI, Veronique KAMGANG KABEYENE

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