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Precambrian Research(3)
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Journal of Asian Earth Sciences(1)
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Geochemistry, zircon U-Pb ages and Lu-Hf isotopes of early Paleozoic plutons in the northwestern Chinese Tianshan: Petrogenesis and geological implications
ArticleAbstract: The northwestern Chinese Tianshan is a key part of the southern Central Asian Orogenic Belt. VoluminPalabras claves:Central Asian Orogenic Belt, Crustal growth, Junggar Ocean, subduction zone, TianshanAutores:Alfred Kron̈er, Huang Z., Long X., Sun M., Wang Q., Wang Y., Yuan C., Zhao G.C.Fuentes:scopusEvolution 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 granitic gneisses in the Chinese Central Tianshan Block: Implications for tectonic affinity and Precambrian crustal evolution
ArticleAbstract: The Chinese Tianshan is the southernmost orogenic terrane located in the long-lived accretionary CenPalabras claves:Central Asian Orogenic Belt, Chinese Tianshan, Crustal growth, Precambrian basement, Tectonic affinityAutores:Alfred Kron̈er, Chen B., Huang Z., Long X., Wang Y., Yuan C., Zhang Y.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:scopusZircon REE patterns and geochemical characteristics of Paleoproterozoic anatectic granite in the northern Tarim Craton, NW China: Implications for the reconstruction of the Columbia supercontinent
ArticleAbstract: Because Archean basement rocks are sparsely distributed around the Tarim Basin, little is known of tPalabras claves:A-type granite, Columbia supercontinent, Hf isotope, Tarim craton, Zircon REE patternsAutores:Alfred Kron̈er, Hu A., Long X., Sun M., Yuan C.Fuentes: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:scopusReworking of the Tarim Craton by underplating of mantle plume-derived magmas: Evidence from Neoproterozoic granitoids in the Kuluketage area, NW China
ArticleAbstract: Most Neoproterozoic granitoids in the Kuluketage area, northern Tarim Craton are characterized by stPalabras claves:Adakitic rocks, Craton reworking, mantle plume, Tarim, UnderplatingAutores:Alfred Kron̈er, Hu A., Long X., Sun M., WILDE S.A., Yuan C., Zhao G.C.Fuentes:scopusThe high-grade Tseel Terrane in SW Mongolia: An Early Paleozoic arc system or a Precambrian sliver?
ArticleAbstract: The high-grade metamorphic Tseel Terrane in southwestern Mongolia is dominated by a strongly deformePalabras claves:Arc system, Early Paleozoic, High-grade gneiss, Tseel Terrane, zircon datingAutores:Alfred Kron̈er, Jiang Y.D., Long X., Sun M., Tumurkhuu D., Xiao W., Yuan C., Zhao G.C.Fuentes:scopus