Figure 10. Zr vs (Nb/Zr)N diagram of Thiéblemont and Tegyey (1994) for the Pitoa granitoids: (A) subduction-zone magmatic rocks, (B) collision zone rocks; (C) alkaline intra-plate zone rocks; (D) Field of peraluminous leucogranites related to collision zones. Normalization values from Sun and McDonough (1989)


Contribution to the Petrogenesis of Pan-Africain Granitoids from East Pitoa in the Northern Cameroon Domain of the Central Africain Fold Belt: Implications for Their Sources and Geological Setting

Cedric Roth Happi Djofna, Merlain Houketchang Bouyo, Daouda Dawai, Rigobert Tchameni, Landry Kouedjou, Martial Periclex Tchunte Fosso, Hervé Brice Fotso Kengne

Journal of Geosciences and Geomatics. 2022, 10(3), 112-125 doi:10.12691/jgg-10-3-1