Figure 6. TiO2 vs. FeO*/MgOdiagram of Miyashiro [40] showing calc-alkaline and tholeiitic characters of meta-igneous rocks from Edéa and Eséka areas


Origin and Evolution of the Formation of the Nyong Series in the Western Border of the Craton

Ndema Mbongue J. L., Ngnotue T., Ngo Nlend C. D., Nzenti J. P., Cheo Suh E.

Journal of Geosciences and Geomatics. 2014, 2(2), 62-75 doi:10.12691/jgg-2-2-4