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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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Geochemical constraints on the nature of Late Archean basaltic-andesitic magmatism in the North China Craton
Xi Wang,Wenju Zhu,Yong-Fei Zheng +2 more
TL;DR: In this paper , an integrated study of whole-rock major and trace elements as well as zircon Hf and wholerock Nd isotopes in late Archean basaltic-andesitic rocks from the North China Craton (NCC) was conducted.
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Enhanced weathering as a trigger for the rise of atmospheric O 2 level from the late Ediacaran to the early Cambrian
TL;DR: The distribution pattern of rare earth elements and the concentrations of water-insoluble elements in the carbonates indicate a sudden enhancement in chemical weathering of the continental crust during the early Cambrian, which may be a trigger for the rise of atmospheric O2 level.
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Isotopic disequilibrium in ultrahigh-pressure and retrograde metamorphism of eclogite and gneiss from the Chinese Continental Scientific Drilling in the Sulu orogen, China: evidence from mineral Nd–Sr–O isotopic composition
TL;DR: In this paper, a combination of investigation on Sm-Nd, Rb-Sr, and O isotopic compositions of minerals separated from ultrahigh-pressure eclogite and gneiss that were collected from the main hole of the Chinese Continental Scientific Drilling project located in the Sulu orogen, eastern China.
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Whole-rock geochemical and zircon Hf-O isotopic constraints on the origin of granitoids and their mafic enclaves from the Triassic Mishuling pluton in West Qinling, central China
TL;DR: In this article, an integrated study including petrology, mineralogy and geochemistry was carried out for monzogranites and the hosted mafic microgranular enclaves (MMEs) as well as biotite granites from the Mishuling pluton in the West Qinling, central China.