Evolution of the early Proterozoic Boundiali-Bagoe Supracrustal Belt and associated granitic rocks, northern Cote d'Ivoire, West Africa
The ca. 2.1 Ga Boundiali-Bagoo Supracrustal Belt is situated in the BaouM-Mossi domain of the West African craton. The belt is composed of greenschist facies metavolcanics and metasediments which comprise the Bagoo River Supergroup (BRS). It occurs in sheared contact with syn-tectonic granitic gneis...
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University of Portsmouth
1995
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.261540 |