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• W2019473932 abstract "Incipient granulite facies conditions and charnockitization affected metasedimentary formations of northern Nigeria during the early stage of the Late Neoproterozoic (Pan-African) orogeny. This domain is characterized by recumbent foliations consistent with crustal thickening. Far from the Pan-African plutons, initial Barrovian-type metamorphism (medium temperature) evidenced by kyanite and staurolite inclusions is documented only from garnet cores. This early stage was followed by a temperature increase up to ≧700°C, with decompression coeval with the generation of garnet-cordierite melts and emplacement of garnet granitoid sheets. Hectometric-wide layers of non-retrograded granulites survived conformably within anatexites and S-type garnet-bearing anatectic granites from the Toro area. Temperatures of ≧800°C required for the crystallization of granulites facies rocks at c. 0.7 GPa pressure and coeval dry anatexis, were reached regionally as a result of heat supply from abundant anhydrous monzo-dioritic to noritic magmas injected as metre-wide veins and as stocks and plutons (charnockites, monzodiorites). The available geochronological results suggest a long-lived thermal perturbation (638–585 Ma) in this former continental domain of northern Nigeria rooted by Archaean crust that was later the site of the Jurassic anorogenic magmatism." @default.
• W2019473932 created "2016-06-24" @default.
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• W2019473932 date "2007-01-01" @default.
• W2019473932 modified "2023-09-27" @default.
• W2019473932 title "Granulite facies metamorphism and charnockite plutonism: examples from the Neoproterozoic Belt of northern Nigeria" @default.
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• W2019473932 doi "https://doi.org/10.1016/s0016-7878(07)80046-0" @default.
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