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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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Two styles of plate tectonics in Earth’s history
TL;DR: In this paper, the authors studied how the dynamic regime and thermal state of subduction zones have affected the style of plate tectonics in Earth's history, which resulted in two styles of plate-tectonics.
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Fluid inclusions in granulites, granulitized eclogites and garnet clinopyroxenites from the Dabie–Sulu terranes, eastern China
TL;DR: In this paper, it is suggested that the primary fluid in the HP granulites was high-density CO2, mixed with a significant quantity of water, which was consumed by retrograde metamorphic mineral reactions and may also have been responsible for metasomatic reactions occurring at quartz-feldspar boundaries.
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Metamorphic zirconology of continental subduction zones
Ren-Xu Chen,Yong-Fei Zheng +1 more
TL;DR: In this article, an integrated study of zircon mineragraphy (internal structure and external morphology), U-Pb ages, mineral inclusions, trace elements, and Lu-Hf and O isotope compositions is presented.
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Tectonic development from oceanic subduction to continental collision: Geochemical evidence from postcollisional mafic rocks in the Hong'an–Dabie orogens
TL;DR: In this article, an integrated study of major trace elements and stable-radiogenic isotopes in post-collisional mafic igneous rocks from the Hong'an-Dabie orogen, east-central China was performed.
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Sm-Nd and Rb-Sr dating of pyroxene-garnetite from North Dabie in east-central China: problem of isotope disequilibrium due to retrograde metamorphism
Zhi Xie,Zhi Xie,Yong-Fei Zheng,Bor-ming Jahn,Michel Ballèvre,Jiangfeng Chen,Pierre Gautier,Tianshan Gao,Bing Gong,Jian-Bo Zhou +9 more
TL;DR: In this paper, the authors show that the oxygen isotopes in metamorphic minerals can be used to evaluate the validity of Sm-Nd mineral isochrons in dating peak metamorphism events.