Enigmatic 1146 ± 4 Ma old granite in the southeastern rim of the West African craton, now part of the Dahomeyan orogenic belt in Ghana
Author:
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geology
Reference42 articles.
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2. Le bassin des Volta (Afrique de l'Ouest): une Marge Passive, d’âge Protérozoïque Supérieur, Tectonisée au Panafrican (600±50 Ma);Affaton,1990
3. The tectono-stratigraphic relationships between the upper Precambrian and lower Paleozoic Volta basin and the pan- African dahomeyide orogenic belt (West Africa);Affaton;Am. J. Sci.,1980
4. The Dahomeyide orogen: tectonothermal evolution and relationships with the Volta basin;Affaton,1991
5. Pan-African granulite formation in the Kabye Massif of Northern Togo (West Africa): Pb–Pb zircon ages;Affaton;Int. J. Earth Sci.,2000
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1. Cryogenian-Ediacaran crustal growth and evolution of the active margin of the Dahomeyide belt, Ghana;Geological Magazine;2023-10
2. Provenance and depositional setting of the Buem structural unit (Ghana): Implications for the paleogeographic reconstruction of the West African and Amazonian cratons in Rodinia;Gondwana Research;2022-09
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