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Caby, R., Delor, C. and Agoh, O. (2000) Lithology, Structure and Metamorphism of the Birimian Formations in the Odienne Area [Ivory Coast]: The Major Role Played by Plutonic Diapirism and Strike-Slip Faulting at the Border of the Man Craton. Journal of African Earth Sciences, 30, 351-374.
https://doi.org/10.1016/S0899-5362(00)00024-5

has been cited by the following article:

• TITLE: Petrochemical Studies of Fouimba and Goma Mounts, Central-West of Cote d’Ivoire: Implication on Petrogenesis Tectonic Setting

  AUTHORS: Allialy Marc Ephrem, Siogbo Davy Bedel, Kouadio Fossou Jean Luc, Houssou N’guessan Nestor, Kouassi Brice Rolland, Konan Félix Oufouet, Diakité Sekou

  KEYWORDS: Petrography, Geochemistry, Mount Fouimba and Goma, Seguela, Côte d’Ivoire

  JOURNAL NAME: Open Journal of Geology, Vol.13 No.2, February 9, 2023

  ABSTRACT: Petrogeochemical analysis of mafic rocks of Fouimba and Goma Mount in the Séguéla region (central-western Côte d’Ivoire) is the subject of this study. This analysis combines remote sensing, geophysics, petrography and geochemistry, in order to determine the major characteristics of the mafic formations in the said area, and above all to participate in the detailed mapping of all the Ivorian terrains. The mafic formations encountered in this region are essentially metatonalites to metadiorites, amphibolites, amphibole bearing pyroxenites and porphyry basalts. Chemical analysis indicates that these mafic formations are tonalitic to monzonitic. They are thought to have derived from mantle depleted magmas.