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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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Formation and evolution of Precambrian continental lithosphere in South China
Shao-Bing Zhang,Yong-Fei Zheng +1 more
TL;DR: In this paper, an overview of the formation and evolution of the Precambrian continental lithosphere in South China is presented based on an integrated study of zircon U-Pb ages and Lu-Hf isotopes in crustal rocks, with additional constraints from Re-Os isotope data on mantle derived rocks.
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Partial melting, fluid supercriticality and element mobility in ultrahigh-pressure metamorphic rocks during continental collision
TL;DR: In this paper, a review on available results from experimental petrology concerning the possibility of partial melting under conditions of continental subduction-zone metamorphism, and petrological evidence for the occurrence of dehydration-driven in-situ partial melting in natural UHP rocks during the continental collision is presented.
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Chemical geodynamics of continental subduction-zone metamorphism: Insights from studies of the Chinese Continental Scientific Drilling (CCSD) core samples
TL;DR: In this article, a series of combined studies were carried out for UHP metamorphic rocks from the main hole (MH) at continuous depths of 100 to 5000 m. The results provided new insights into the chemical geodynamics of continental subduction-zone metamorphism, especially on the issues that are not able to be resolved from the surface outcrops.
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Low-Grade Metamorphic Rocks in the Dabie-Sulu Orogenic Belt: A Passive-Margin Accretionary Wedge Deformed during Continent Subduction
TL;DR: In this paper, an integrated study of geochronological, petrological, and paleontological observations demonstrates that precursors of flysch-facies metasedimentary rocks were deposited along the northern, passive continental margin of the Yangtze plate prior to the Triassic.
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U Pb, Hf and O isotope evidence for two episodes of fluid-assisted zircon growth in marble-hosted eclogites from the Dabie orogen
Yuan-Bao Wu,Yuan-Bao Wu,Yong-Fei Zheng,Yong-Fei Zheng,Zi-Fu Zhao,Zi-Fu Zhao,Bing Gong,Xiaoming Liu,Fu-Yuan Wu +8 more
TL;DR: In this paper, a combined study of internal structure, U-Pb age, and Hf and O isotopes was carried out for metamorphic zircons from ultrahigh-pressure eclogite boudins enclosed in marbles from the Dabie orogen in China.