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Delor, C., Siméon, Y., Vidal, M., Zeade, Z., Koné, Y., Adou, M., Dibouahi, J., Bi Irié, D., Yao, B.D., N’Da, D., Pouclet, A., Konan, G., Diaby, I., Chiron, J.C., Dommanget, A., Kouamelan, A.N., Peucat, J.J., Cocherie, A. and Cautru, J.P. (1995) Notice explicative de la carte géologique de la Cote d’Ivoire à 1/200,000, feuille de Nassian. Ministère des Mines et de l’Energie, DMG, Abidjan.

has been cited by the following article:

• TITLE: The Geological Formations of Koun Fao (East of Côte d’Ivoire): Petrographic Characterization and Associated Deformations

  AUTHORS: Tokpa Kakeu Lionel-Dimitri Boya, Fossou Jean-Luc Hervé Kouadio, Allou Gnanzou, Martial Pohn Koffi Adingra, Odrouro Ablan Anne Marie Kouame, Marc Ephrem Allialy

  KEYWORDS: Petro-Structural, Geological Formations, Comoé Basin, Koun Fao, Côte d’Ivoire

  JOURNAL NAME: Open Journal of Geology, Vol.12 No.10, October 28, 2022

  ABSTRACT: This study aims to contribute to improve knowledge on geological formations of Comoé basin. The petrographic study of the geological formations of Koun Fao has highlighted two major lithological families: magmatic rocks consisting of monzonites, monzogranites, diorites, biotite granodiorites, syenites, porphyritic micromonzonites and porphyritic dacite and metamorphic rocks from sedimentary origin (quartz schists, meta-greywackes, schists, andalusite chloritoschist and paragneiss). These formations are affected by amphibolite to greenschist facies metamorphism and hydrothermal alteration (pervasive and vein) marked by the presence of quartz, epidotes, chlorites and sericite. Minerals such as andalusite, muscovite and chlorite characterize a local low pressure contact metamorphism in the andalusite chloritoschist. Remote sensing data (Landsat 8 image) coupled with field data allowed the production of a geological map of the area. The study of the structures and microstructures highlighted two deformation mechanisms. These are flattening and simple shear (ductile and brittle). The study area is affected by four deformation phases: D1 marked by a N-S to NNE-SSW elongation, D2 marked by a NW-SE to NNW-SSE compression phase, D3 which is a NE-SW to NNE-SSW transpression phase and D4, responsible for late structures, marked by a NW-SE to NNW-SSE transpression phase.