Article citationsMore>>
Egal, E., Thiéblemont, D., Lahondère, D., Guerrot, C., Costea, C. A., Iliescu, D., Delor, C., Goujou, J.-C., Lafon, J. M., Tegyey, M., Diaby, S., & Kolié, P. (2002). Late Eburnean Granitization and Tectonics along the Western and Northwestern Margin of the Archean Kénéma-Man Domain (Guinea, West African Craton). Precambrian Research, 117, 57-84.
https://doi.org/10.1016/S0301-9268(02)00060-8
has been cited by the following article:
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TITLE:
Petro-Geochemistry Contraints of Côte d’Ivoire North-East Plutonites: Implications for Eoeburnean Magmatism of Baoulé-Mossi Domain (Southern of West African Craton)
AUTHORS:
Brice Roland Kouassi, Marc Ephrem Allialy, N’Guessan Houssou Nestor, Kouadio David Koffi
KEYWORDS:
Plutonites, Contraints, Magmatism, Source, Geotectonics, Côte d’Ivoire, West African Craton
JOURNAL NAME:
Journal of Geoscience and Environment Protection,
Vol.10 No.9,
September
29,
2022
ABSTRACT: Plutonites are part of the set of crystallines compose the Precambrian
basement. Their study is capital because it allows participating in the debates
on the geodynamic evolution of the West African craton. This study concerns
granitoids and dioritoids of the North-East of Côte d’Ivoire located in the
Man-Leo ridge structured by Eoeburnean magmatism. The petrographic and
geochemistry constraints make it possible to say that these rock formations
have evolved by the process of fractional crystallization. They have a hybrid
origin (mantle and crust), metaluminous to peraluminous highlighted by geochemistry. Concerning the geotectonic context,
these plutonites of the Baoulé-Mossi domain are emplacement in a context
of subduction more precisely in a context of volcanic arc.
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