A tectonic model for the juxtaposition of granulite- and amphibolite-facies rocks in the Eburnean orogenic belt (Sassandra-Cavally domain, Cote d'Ivoire) Koffi, A. Y. /Baratoux, Lenka Pitra, P. Kouamelan, A. N. Vanderhaeghe, O. Thebaud, N. Bruguier, O. Block, S. Kouadio, Hjlf Kone, J. exhumation Archean Paleoproterozoic monazite geochronology West African Craton Cote d'Ivoire The Sassandra-Cavally (SASCA) domain (SW Cote d'Ivoire) marks the transition between the Archean Kenema-Man craton and the Paleoproterozoic (Rhyacian) Baoule-Mossi domain. It is characterized by the tectonic juxtaposition of granulite-facies and amphibolite-facies rocks. Migmatitic grey gneisses, garnet-cordierite-sillimanite migmatitic paragneisses and garnet-staurolite-bearing micaschists reached peak pressure conditions ranging from 2023 text https://www.documentation.ird.fr/hor/fdi:010090012 fdi:010090012 Koffi A. Y., Baratoux Lenka, Pitra P., Kouamelan A. N., Vanderhaeghe O., Thebaud N., Bruguier O., Block S., Kouadio Hjlf, Kone J.. A tectonic model for the juxtaposition of granulite- and amphibolite-facies rocks in the Eburnean orogenic belt (Sassandra-Cavally domain, Cote d'Ivoire). 2023, 194, 11 [33 p.] EN COTE D'IVOIRE