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Detrital and xenocrystic zircon ages from Neoproterozoic to Palaeozoic arc terranes of Mongolia: Significance for the origin of crustal fragments in the Central Asian Orogenic Belt
ArticleAbstract: The Central Asian Orogenic Belt contains many Precambrian crustal fragments whose origin is unknown,Palabras claves:Central Asian Orogenic Belt, Detrital age, Microcontinent, Mongolia, Probability plot, Tarim, zirconAutores:Alfred Kron̈er, Demoux A., Donskaya T.V., Liu D.Y., Sun M., Wang W., Xia X., Yamirka Rojas-AgramonteFuentes:scopusDevonian arc-related magmatism in the Tseel terrane of SW Mongolia: Chronological and geochemical evidence
ArticleAbstract: The Tseel terrane in the Gobi Desert of SW Mongolia consists of a composite crustal segment of imbriPalabras claves:Autores:Alfred Kron̈er, Badarch G., Demoux A., Hegner E.Fuentes:scopusLithostratigraphic and geochronological constraints on the evolution of the central Asian orogenic belt in SW Mongolia: Early paleozoic rifting followed by late paleozoic accretion
ArticleAbstract: New SHRIMP U-Pb and evaporation Pb-Pb zircon ages, together with a revision of the lithostratigraphyPalabras claves:Accretionary tectonics, Central Asian Orogenic Belt, Mongolia, Paleozoic, Tectono-stratigraphy, Zircon geochronologyAutores:Alfred Kron̈er, Demoux A., Lehmann J., Lexa O., Liu D.Y., Schulmann K., Štípská P., Tomurhuu D., Wingat M.T.D.Fuentes:scopusZircon ages from the baydrag block and the bayankhongor ophiolite zone: Time constraints on late neoproterozoic to cambrian subduction- and accretion-related magmatism in central Mongolia
ArticleAbstract: Central Mongolia represents a heterogeneous crustal domain of the Central Asian Orogenic Belt and isPalabras claves:Appendix, Color figureAutores:Alfred Kron̈er, Badarch G., Demoux A., Jian P., Tomurhuu D., Wingate M.T.D.Fuentes:scopus