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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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Syn-exhumation magmatism during continental collision: Geochemical evidence from the early Paleozoic Fushui mafic rocks in the Qinling orogen, Central China
TL;DR: Zhang et al. as discussed by the authors carried out an integrated study of geochronology and geochemistry to find mafic igneous rocks in the Fushui complex in the Qinling orogen, central China.
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On the use of a three-dimensional method in solving the U-Pb two-stage model
TL;DR: In this paper, the U-Pb discordia plane model and the Pb-pb isochron plane model are developed respectively, to eliminate the effect of the unknown common lead correction.
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Origin of syn-collisional granitoids in the Gangdese orogen: Reworking of the juvenile arc crust and the ancient continental crust
Yu-Wei Tang,Long Chen,Long Chen,Long Chen,Zi-Fu Zhao,Zi-Fu Zhao,Yong-Fei Zheng,Yong-Fei Zheng +7 more
TL;DR: In this article, the authors investigated the role of syn-collisional granitoids in the growth of the continental crust in the Gangdese orogen and found that they do not contribute to continental growth in southern Tibet.
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The Meyer-Neldel compensation law for electrical conductivity in olivine
Xiaoping Wu,Yong-Fei Zheng +1 more
TL;DR: In this paper, a linear correlation exists between the logarithm of prefactor and activation energy in olivine, and it is shown that the electrical conductivities due to different conduction mechanisms or conducting species converge to a constant at a characteristic temperature.
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Interplay between oceanic subduction and continental collision in building continental crust
Di-Cheng Zhu,Qing Wang,Roberto F. Weinberg,Peter A. Cawood,Sun-Lin Chung,Yong-Fei Zheng,Zhidan Zhao,Zengqian Hou,Xuanxue Mo +8 more
TL;DR: In this article , the Gangdese continental arc magmatism started with fractional crystallization to form cumulates and associated medium-K calc-alkaline suites, followed by a period commencing at ~70 Ma dominated by remelting of pre-existing lower crust, producing more potassic compositions.