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scopus(11)
Geochronological evidence for Archaean and Palaeoproterozoic polymetamorphism in the Central Zone of the Limpopo Belt, South Africa
ArticleAbstract: The Central Zone of Limpopo Belt is a polymetamorphic and complexly deformed Precambrian terrane whoPalabras claves:Autores:Alfred Kron̈er, Brandl G., Brandt S., Klemd R., Xie H.Fuentes:scopusField 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:scopusEvolution of the northeastern Kaapvaal craton and the central Limpopo belt, South Africa, based on single-zircon ages (extended abstract)
ArticleAbstract:Palabras claves:Autores:Alfred Kron̈er, Brandl G., Jaeckel P., Nemchin A.A., Pidgeon R.T.Fuentes:scopusPressure-temperature evolution during two granulite-facies metamorphic events (2.62 and 2.02 Ga) in rocks from the Central Zone of the Limpopo Belt, South Africa
ArticleAbstract: The Central Zone of the Limpopo Belt in southern Africa is a classical example of a polymetamorphicPalabras claves:Delamination, granulite, Limpopo Belt, Neoarchean, P-T path, PseudosectionAutores:Alfred Kron̈er, Bobek P., Brandl G., Brandt S., Fischer A., Klemd R., Li Q., Zhou T.Fuentes:scopusLate Archaean to early Proterozoic granitoid magmatism and high-grade metamorphism in the central Limpopo belt, South Africa
ArticleAbstract: The Central Zone of the Limpopo belt in southern Africa has previously been interpreted as a segmentPalabras claves:Absolute age, Granulites, Limpopo Belt, Metamorphism, orogenyAutores:Alfred Kron̈er, Brandl G., Jaeckel P., Kamo S.L., Wendt J.I.Fuentes:scopusSingle zircon age for the felsic rubbervale formation, Murchison Greenstone Belt, South Africa
ArticleAbstract: Age data for the various greenstone belts of the northern Kaapvaal Craton are generally scarce and iPalabras claves:Autores:Alfred Kron̈er, Brandl G., Jaeckel R.Fuentes:scopusSingle zircon ages for felsic to intermediate rocks from the Pietersburg and Giyani greenstone belts and bordering granitoid orthogneisses, northern Kaapvaal Craton, South Africa
ArticleAbstract: Previous models for the temporal evolution of greenstone belts and surrounding granitoid gneisses inPalabras claves:Autores:Alfred Kron̈er, Brandl G., Jaeckel P.Fuentes:scopusSingle zircon ages for granitoid gneisses in the Central Zone of the Limpopo Belt, Southern Africa and geodynamic significance
ArticleAbstract: Ion microprobe, evaporation and vapour digestion single zircon emplacement ages for granitoid rocksPalabras claves:Archaean, geochronology, Granitoid gneisses, Granulite metamorphism, Limpopo Belt, zirconAutores:Alfred Kron̈er, Brandl G., Jaeckel P., Nemchin A.A., Pidgeon R.T.Fuentes:scopusTwo orogenic events separated by 2.6 Ga mafic dykes in the Central Zone, Limpopo Belt, southern Africa
ArticleAbstract: The Limpopo Belt of southern Africa is a typical early Precambrian orogen that experienced two high-Palabras claves:Limpopo Belt, Mafic dyke, Orogenic event, SHRIMP, zircon datingAutores:Alfred Kron̈er, Brandl G., Xie H., Yusheng W.Fuentes:scopus