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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:scopusNeoproterozoic-Early Paleozoic Peri-Pacific Accretionary Evolution of the Mongolian Collage System: Insights From Geochemical and U-Pb Zircon Data From the Ordovician Sedimentary Wedge in the Mongolian Altai
ArticleAbstract: Neoproterozoic to early Paleozoic accretionary processes of the Central Asian Orogenic Belt have beePalabras claves:Active margin sediments, Mongolian Altai, Neoproterozoic-early Paleozoic, Peri-Pacific accretion, Turbidite basinAutores:Alfred Kron̈er, Buriánek D., Hanžl P., Janoušek V., Jiang Y.D., Lexa O., Schulmann K., Sun M., Yuan 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:scopus