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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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Amalgamation of South China into Rodinia during the Grenvillian accretionary orogeny: Geochemical evidence from Early Neoproterozoic igneous rocks in the northern margin of the South China Block

TL;DR: In this article, a combined study of whole-rock geochemistry, zircon U-Pb ages and Hf-O isotopes was carried out for igneous rocks from the Mianlue ophiolite in the northern margin of the South China Block.
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Zircon U-Pb ages for Wulian granites in northwest Sulu and their tectonic implications

TL;DR: The Wulian complex as mentioned in this paper is a Neoproterozoic intrusion in the northern margin of the Yangtze plate, and correspond to the magmatic complex at Luzhenguan in the eastern part of the Beihuaiyang belt in the Dabie orogen.
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Multiphase solid inclusions in zoisite-bearing eclogite: evidence for partial melting of ultrahigh-pressure metamorphic rocks during continental collision

TL;DR: In this article, multiphase solid (MS) inclusions in both garnet and omphacite were investigated for zoisite-bearing eclogite from the ultrahigh pressure (UHP) metamorphic zone in the Sulu orogen.
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Geochemical constraints on the source nature and melting conditions of Triassic granites from South Qinling in central China

TL;DR: In this article, a combined study of petrology, geochronology and geochemistry was carried out for them from outcrops at Guangtoushan (GTS) and Huayang (HY) in South Qinling.
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Geochemical constraints on the protoliths of eclogites and blueschists from North Qilian, northern Tibet

TL;DR: In this article, an integrated study of whole-rock geochemistry, mineral O isotope geochemistry and zirconology was carried out for low-temperature eclogites and blueschists from the North Qilian orogen in northern Tibet.