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Yong-Fei Zheng
Researcher at University of Science and Technology of China
Publications - 396
Citations - 29325
Yong-Fei Zheng is an academic researcher from University of Science and Technology of China. The author has contributed to research in topics: Zircon & Metamorphism. The author has an hindex of 86, co-authored 354 publications receiving 25033 citations. Previous affiliations of Yong-Fei Zheng include University of Göttingen & Center for Excellence in Education.
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Journal ArticleDOI
Zircon U-Pb ages and Hf isotope compositions of migmatite from the North Dabie terrane in China: constraints on partial melting
Yuan-Bao Wu,Yuan-Bao Wu,Yuan-Bao Wu,Yong-Fei Zheng,Yong-Fei Zheng,Shao-Bing Zhang,Zi-Fu Zhao,Fu-Yuan Wu,Xiaoming Liu +8 more
TL;DR: In this article, the ages of migmatite gneisses are constrained using U-Pb dating and Hf isotope analysis, showing that they are Neoproterozoic in age.
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Post-collisional granitoids from the Dabie orogen in China: Zircon U–Pb age, element and O isotope evidence for recycling of subducted continental crust
TL;DR: In this paper, a combined study of zircon U-Pb dating, major and minor element geochemistry, and O isotopes in Early Cretaceous post-collisional granitoids from the Dabie orogen in China demonstrates that they may have been generated by partial melting of subducted continental crust.
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Fluid flow during exhumation of deeply subducted continental crust: zircon U-Pb age and O-isotope studies of a quartz vein within ultrahigh-pressure eclogite
TL;DR: In this paper, SHRIMP U-Pb dating of zircon from a kyanite-quartz vein within ultra-high pressure eclogite in the Dabie continental collision orogen yields two age groups at 212±−7 and 181±−13.
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Neoproterozoic continental accretion in South China: Geochemical evidence from the Fuchuan ophiolite in the Jiangnan orogen
TL;DR: In this paper, a combined study of geochronology and geochemistry was carried out for the Fuchuan ophiolite in the eastern Jiangnan orogen, South China.
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Melting of subducted continent: Element and isotopic evidence for a genetic relationship between Neoproterozoic and Mesozoic granitoids in the Sulu orogen
TL;DR: Zhang et al. as mentioned in this paper showed that postcollisional granitoids were generated by Early Cretaceous melting of subduction-thickened continental crust that has geochemical affinities to Neoproterozoic protolith of ultrahigh pressure metaigneous rocks that were derived from the Yangtze Block.