Déruelle, B., Bardintzeff, J. M., Cheminée, J. L., Ngounouno, I., Lissom, J., Nkoumbou, C., Etamé, J., Hell, J. V., Tanyileke, G., N’ni, J., Ateba, B., Ntepe, N., Nono, A., Wandji, P., Fosso, J., & Nkouathio, D. G. (2000). Simultaneous Eruptions of Alkaline Basalt and Hawaiite at Mount Cameroon (March 28-April 17, 1999). Comptes Rendus de l’Académie des Sciences, 331, 525-531.
https://doi.org/10.1016/S1251-8050(00)01454-3

has been cited by the following article:

• TITLE: Magmatism of the Beka Volcanic Massifs (Cameroon Volcanic Line, West-Central Africa): New Petrographical and Mineralogical Data

  AUTHORS: Jacques Dili-Rake, Sahabo Aboubakar Abdoulaye, Joseph Legrand Tchop, Merlin Isidore Teitchou, Christian Mana Bouba, Oumarou Faarouk Nkouandou, Daouda Dawaï, Eddy Ferdinand Mbossi

  KEYWORDS: Cameroon Volcanic Line, Adamawa Plateau, Beka Volcanic Massif, Fractional Crystallization, OIB-Type Mantle

  JOURNAL NAME: Journal of Geoscience and Environment Protection, Vol.10 No.7, July 26, 2022

  ABSTRACT: The Beka volcanic massifs are located northeast of Ngaoundere region, within the Adamawa plateau. It consists mainly of basanites, trachytes and phonolites. The petrographic study shows that all the basanite lavas have porphyritic microlitic textures with a more pronounced magmatic fluidity than the felsic lavas displaying trachytic textures. The lavas are composed of phenocrysts, microlites and microphenocrysts of olivine, clinopyroxene, plagioclase and iron-titanium oxides for the basanites and of greenish clinopyroxene, alkali feldspar, and titanomagnetite for the felsic lavas. Chemical microprobe analysis indicates that the olivine crystals are magnesian (Fo73-78). Clinopyroxene crystals have a composition of diopside (Wo47-) in the basaltic lavas and diopside near the hedenbergite pole in the trachytes phonoliths and titanomagnetite (TiO2: 21.13% - 22.36% and FeO: 68% - 68%). Chemical analyses on whole rocks show that all the lavas belong to the same series and the felsic lavas come from the differentiation of basanite lavas by fractional crystallization of the minerals therein. The basanites originate from a low rate of partial melting of an OIB-type mantle. Contamination and mixing processes are suspected. Lavas of similar composition are found in other volcanic centres of the Adamawa plateau and the continental and oceanic sectors of the Cameroon Volcanic Line, in particular the Kapsiki plateau, Mounts Cameroon and Bamenda.