Masurel Q. auteur aut IRD Eglinger A. auteur aut IRD Thebaud N. auteur aut IRD Allibone A. auteur aut IRD Andre-Mayer A. S. auteur aut IRD McFarlane H. auteur aut IRD Miller J. auteur aut IRD Jessell M. auteur aut IRD Ailleres L. auteur aut IRD Vanderhaeghe O. auteur aut IRD Salvi S. auteur aut IRD Baratoux Lenka auteur aut IRD Perrouty S. auteur aut IRD Begg G. auteur aut IRD Fougerouse D. auteur aut IRD Hayman P. auteur aut IRD Wane O. auteur aut IRD Tshibubudze A. auteur aut IRD Parra-Avila L. auteur aut IRD Kouamelan A. auteur aut IRD Amponsah P. O. auteur aut IRD text journalArticle eng text/pdf born digital access The southern part of the West African Craton includes the Baoule-Mossi Domain, the world's premier Paleoproterozoic gold province (similar to 10,000 metric ton gold endowment). Structural, metamorphic, and geochronological data suggest gold mineralisation occurred during three episodes that span much of the Eoeburnean and Eburnean orogenic cycles. Eoeburnean orogenic and rare skarn-hosted gold deposits formed between ca. 2200 and 2135 Ma during repeated episodes of volcanism, plutonism, and shortening, which thickened the Paleoproterozoic crust. Early Eburnean orogenic and placer gold deposits formed between ca. 2110 and 2095 Ma during inversion, metamorphism, and subsequent oblique shortening of intra-orogenic basins filled after ca. 2135 Ma. This episode of mineralisation terminated when the Baoule-Mossi Domain docked with the Archean Kenema-Man Domain at ca. 2095 Ma. Late Eburnean orogenic and less common intrusion-related gold deposits formed between ca. 2095 and 2060 Ma during strike-slip to oblique-slip tectonics, post-collisional high-K plutonism and crustal reworking across the western and southern Baoule-Mossi Domain. Eoeburnean gold deposits include ca. 10 % of the gold endowment of the Baoule-Mossi Domain, whereas the Early Eburnean and Late Eburnean deposits include ca. 50-70% and 20-40%, respectively. Here, we highlight the favourable confluence of accretion-collision tectonics, involving juvenile crust formation as well as protracted magmatic, metamorphic, and deformation histories that resulted in diachronous gold events spread over at least 100 myr throughout the Baoule-Mossi Domain. specialized West African Craton Paleoproterozoic Gold Eburnean orogeny AFRIQUE DE L'OUEST MALI BURKINA FASO GHANA GUINEE COTE D'IVOIRE SENEGAL 064 066 57 4 513-537 2022 0026-4598 https://www.documentation.ird.fr/hor/fdi:010081470 10.1007/s00126-021-01052-5 0026-4598 [F B010081470] https://www.documentation.ird.fr/hor/fdi:010081470 https://www.documentation.ird.fr/intranet/publi/2021-06/010081470.pdf Accès réservé (Intranet de l'IRD) IRD - Base Horizon / Pleins textes 2021-06-15 2025-02-24 fdi:010081470 fre