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