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Evolution of the middle Paleozoic magmatism in the Chinese Altai: Constraints on the crustal differentiation at shallow depth in the accretionary orogen
ArticleAbstract: The Chinese Altai underwent intensive mafic and felsic magmatism in the middle Paleozoic, which wasPalabras claves:Accretionary orogen, Central Asian Orogenic Belt, Chinese Altai, Continental crust, DifferentiationAutores:Chen Q., Huang X.l., Sun M., Yamirka Rojas-Agramonte, Yu Y., Yuan C., Zhao G.C.Fuentes:scopusNew geochemical and combined zircon U-Pb and Lu-Hf isotopic data of orthogneisses in the northern Altyn Tagh, northern margin of the Tibetan plateau: Implication for Archean evolution of the Dunhuang Block and crust formation in NW China
ArticleAbstract: Dunhuang Block is previously considered to be an eastern part of the Tarim Craton, but now it is proPalabras claves:Archean, Crustal evolution, Dunhuang Block, Tarim craton, TTG rocksAutores:Alfred Kron̈er, Long X., Sun M., Yuan C., Zhao G.C.Fuentes:scopusWhole-rock Nd–Hf isotopic study of I-type and peraluminous granitic rocks from the Chinese Altai: Constraints on the nature of the lower crust and tectonic setting
ArticleAbstract: The nature of the lower crust and tectonic setting of the Chinese Altai in the early to middle PaleoPalabras claves:accretionary orogeny, Central Asian Orogenic Belt, Chinese Altai, Continental growth, Nd–Hf decouplingAutores:Alfred Kron̈er, Broussolle A., Li P., Long X., Sun M., Yang J.H., Yu Y., Zhao G.C.Fuentes:scopus