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Field relationships and age of supracrustal Beit Bridge Complex and associated granitoid gneisses in the Central Zone of the Limpopo Belt, South Africa
ArticleAbstract: Field relationships in the Sand River in the Central Zone of the Limpopo Belt show that the supracruPalabras claves:geochronology, Gneiss, Granite, Metamorphism, Proterozoic, South AfricaAutores:Alfred Kron̈er, Brandl G., Hofmann A., Jaeckel P., Nemchin A.A.Fuentes:scopusField relationships of mid- to late Archaean high-grade gneisses of igneous and sedimentary parentage in the Sand River, Central Zone of the Limpopo Belt, South Africa
ArticleAbstract: Mid- to late Archaean supracrustal and granitoid gneisses exposed south of Messina in the central LiPalabras claves:Archaean, Deformation, Gneiss, Metamorphism, South AfricaAutores:Alfred Kron̈er, Brandl G., Hofmann A.Fuentes:scopusSource composition, fractional crystallization and magma mixing processes in the 3.48-3.43 Ga Tsawela tonalite suite (Ancient Gneiss Complex, Swaziland) - Implications for Palaeoarchaean geodynamics
ArticleAbstract: The ca. 3480-3430 Ma Tsawela Gneiss (TG) is a well-preserved coarse-grained diorite to tonalite suitPalabras claves:Continental crust, Hf-Nd, Magma mixing, Swaziland, Tonalite, TTGAutores:Alfred Kron̈er, Geng H.Y., Hegner E., Hoffmann J.E., Hofmann A., Iaccheri L.M., Schneider K.P., Viehmann S., Wong J., Xie H., Yang J.H.Fuentes:scopusThe Chirwa dome: Granite emplacement during late Archaean thrusting along the northeastern margin of the Zimbabwe craton
ArticleAbstract: The Chirwa dome in northeast Zimbabwe is situated at the boundary between the Zimbabwe craton and ArPalabras claves:Autores:Alfred Kron̈er, Dirks P.H.G.M., Hofmann A., Jagoutz O., Jelsma H.A.Fuentes:scopus