Petrogenetic links between rare metal-bearing pegmatites and TTG gneisses in the West African Craton: The Mangodara district of SW Burkina Faso

•Mangodara forms a dome cored by tonalitic gneiss, mantled by granodioritic gneiss.•Gneiss-granitoids derive from partial melting of Birimian greenstones.•Residual melt from syntectonic gneiss genesis formed rare-metal pegmatites. We describe the geological context of rare metal-bearing pegmatites f...

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Veröffentlicht in:	Precambrian research 2021-09, Vol.364, p.106359, Article 106359
Hauptverfasser:	Bonzi, Wilédio Marc-Emile, Vanderhaeghe, Olivier, Van Lichtervelde, Marieke, Wenmenga, Urbain, André-Mayer, Anne-Sylvie, Salvi, Stefano, Poujol, Marc
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth Sciences Eburnean orogeny Geology Geosciences, Multidisciplinary Melt segregation Mineralogy Partial melting Petrography Physical Sciences Rare metal-bearing pegmatite Science & Technology Sciences of the Universe TTG gneiss West Africa Craton
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