Crustal evolution and geodynamic setting of the Sefwi Greenstone Belt, WAC Helen McFaralane Robin Armit Laurent Ailleres Peter Betts Mark Jessell J Ganne L Baratoux N Thebaud L Parra-Avila 10.4225/03/5a0fec5c61d87 https://bridges.monash.edu/articles/poster/Crustal_evolution_and_geodynamic_setting_of_the_Sefwi_Greenstone_Belt_WAC/5615380 <div>Crustal evolution and geodynamic setting of the Sefwi Greenstone Belt, WAC. The Palaeoproterozoic West African Craton (2.25 - 2.07 Ga) represents one of the youngest, large provinces of juvenile crust on Earth. It displays lithological and architectural similarities to a number</div><div>of late Archean Provinces, including the Abitibi-Opatica terrane, Superior Province and Karelian and Kola cratons of the Fennoscandian Shield. Forming just after the Archean-Palaeoproterozoic transition, the magmatic evolution and geodynamic setting of juvenile crust formation of the WAC continues to stimulate scientific debate.</div> 2017-11-18 08:16:24 West Africa Craton Sefwi Greenstone Palaeoproterozoic Geochronology Geochemistry Geochronology Geology Structural Geology Tectonics