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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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Water contents and hydrogen isotopes in nominally anhydrous minerals from UHP metamorphic rocks in the Dabie-Sulu orogenic belt

TL;DR: In this paper, a continuous flow method, by a combination of thermal conversion elemental analyzer (TC/EA) with isotope ratio mass spectrometry (MS), was developed to determine both H isotope composition and H2O concentration of ultrahigh pressure (UHP) metamorphic rocks in the Dabie-Sulu orogenic belt.
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The effect of Rayleigh degassing of magma on sulphur isotope composition: a quantitative evaluation

TL;DR: In this paper, the effect of Rayleigh distillation by outgassing of SO2 and H2O on the isotopic composition of sulphur remaining in silicate melts is quantitatively modelled.
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Miocene high-temperature leucogranite magmatism in the Himalayan orogen

TL;DR: In this article, the authors used the Ti-in-zircon thermometry in combination with the thermodynamically calibrated relationships of T-aSiO2-aTiO2 to retrieve crystallization temperatures of Miocene (ca. 17 Ma) two-mica granites from Yalaxiangbo, in the eastern Himalaya, SE Tibet.
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An experimental calibration of oxygen isotope fractionation between calcite and forsterite in the presence of a CO2H2O fluid

TL;DR: In this article, the isotope fractionation between calcite and forsterite has been experimentally calibrated in the presence of small amounts of a supercritical CO2-H2O fluid at temperatures from 600° to 900°C and pressures from 3 to 12 kbar.
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Paleoproterozoic tectonic evolution of the northern Yangtze craton from oceanic subduction through continental collision to continental rifting: Geochronological and geochemical records of metabasites from the Tongbai orogen in central China

TL;DR: In this article, the existence of multistage collision-and rift-related tectonothermal events in the northern margin of the Yangtze craton was reported through an integrated study of geochronology and geochemistry for Phanerozoic metabasites from the Tongbai orogen in central China.