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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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Zircon U-Pb ages, Hf and O isotopes constrain the crustal architecture of the ultrahigh-pressure Dabie orogen in China
TL;DR: In this article, the crustal structure of the Dabie orogen was reconstructed by a combined study of U-Pb ages, Hf and O isotope compositions of zircons from granitic gneiss.
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Deep Fluids in Subducted Continental Crust
TL;DR: In this article, the authors provided a framework for understanding fluid-mediated mass transfer in deeply subducted continental crust at temperatures below 650 °C, aqueous fluids derived from dehydration reactions involving hydrous phases contain limited amounts of solutes.
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Estimation of oxygen diffusivity from anion porosity in minerals
Yong-Fei Zheng,Bin Fu +1 more
TL;DR: In this paper, an empirical model for predicting oxygen diffusivity from anion porosity is presented for a wide range of minerals, based on the examination of experimental diffusion data under anhydrous and hydrothermal conditions.
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Zircon U-Pb age, element and C-O isotope geochemistry of post-collisional mafic-ultramafic rocks from the Dabie orogen in east-central China
TL;DR: In this paper, the origin and genesis of post-collisional mafic-ultramafic rocks in the Dabie orogen of China are investigated with respect to Mesozoic transport of mass and energy between mantle and crust.
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Syn-exhumation magmatism during continental collision: Evidence from alkaline intrusives of Triassic age in the Sulu orogen
TL;DR: In this article, a combined study of zircon U-Pb ages, Lu-Hf isotope, mineral O isotopes, whole-rock elements and Sr-Nd isotopes was carried out for alkaline intrusive rocks (including gabbro, syenite and granite) in the Sulu orogen.