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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:scopusZircon U-Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic
ArticleAbstract: Gneissic rocks in the Chinese Altai Mountains have been interpreted as either Paleozoic metasedimentPalabras claves:Altaids, Gneiss, Hf isotope, U-Pb age, zirconAutores:Alfred Kron̈er, Lin S., Long X., Sun M., Wu F.Y., Xia X., Xiao W., Yuan C., Zhao G.C.Fuentes:scopus