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Chaohui Liu

Researcher at University of Hong Kong

Publications -  39
Citations -  2535

Chaohui Liu is an academic researcher from University of Hong Kong. The author has contributed to research in topics: Craton & Zircon. The author has an hindex of 26, co-authored 39 publications receiving 2128 citations. Previous affiliations of Chaohui Liu include Peking University.

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U–Pb and Hf isotopic study of zircons of the Helanshan Complex: Constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton

TL;DR: In this paper, the authors used cathodoluminescence (CL) images of zircons combined with isotopic data of zirons to enable the resolution of magmatic and metamorphic events that can be directed towards understanding the formation and evolution of the Khondalite Belt in the Western Block of the North China Craton.
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The growth, reworking and metamorphism of early Precambrian crust in the Jiaobei terrane, the North China Craton: Constraints from U-Th-Pb and Lu-Hf isotopic systematics, and REE concentrations of zircon from Archean granitoid gneisses

TL;DR: Zircon cathodoluminescence (CL) images have assisted in obtaining U-Th-Pb and Lu-Hf isotopic systematics, and rare earth element (REE) concentrations from distinct zircon domains of complex zircons, and the results have been integrated in order to unravel the growth, reworking and metamorphism of the early Precambrian crust in the Jiaobei terrane.
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Petrogenesis and tectonic significance of Paleoproterozoic meta-mafic rocks from central Liaodong Peninsula, northeast China: Evidence from zircon U–Pb dating and in situ Lu–Hf isotopes, and whole-rock geochemistry

TL;DR: In this paper, the authors present zircon cathodoluminescence images, U-Pb dates, and Lu-Hf isotope data for these rocks, in order to constrain the tectonic nature and evolution of the Jiao-Liao-Ji Belt.
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U-Pb and Hf isotopic study of detrital zircons from the Hutuo group in the Trans-North China Orogen and tectonic implications

TL;DR: In this paper, detrital zircons from the Hutuo Group in the Wutai Complex in the middle sector of the Trans-North China Orogen were analyzed and concordant 207 Pb/ 206 Pb ages of 2.88, 2.11, 3.5, and 2.65 were obtained with Neoarchean to Paleoproterozoic ages.
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U-Pb and Hf isotopic study of detrital zircons from the Yejishan Group of the Lüliang Complex: Constraints on the timing of collision between the Eastern and Western Blocks, North China Craton

TL;DR: In this paper, detrital zircons from foreland basins in the Trans-North China Orogen have been used to provide rigorous constraints on the timing of the collision between the two blocks.