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Changqing Yin

Researcher at Sun Yat-sen University

Publications -  88
Citations -  4552

Changqing Yin is an academic researcher from Sun Yat-sen University. The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 27, co-authored 66 publications receiving 3665 citations. Previous affiliations of Changqing Yin include University of Waterloo & University of Hong Kong.

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Amalgamation of the North China Craton: Key issues and discussion

TL;DR: In this article, a model for assembly and stabilization of the various Archean blocks of the NCC in the Paleoproterozoic has been proposed, based on the analysis of available stratigraphic, structural, geochemical, metamorphic and geochronologic data.
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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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LA-ICP-MS U-Pb zircon ages of the Qianlishan Complex: Constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton

TL;DR: The Qianlishan Complex as mentioned in this paper is located in the westernmost part of the Khondalite Belt, a continent-continent collisional belt along which the Yinshan and Ordos blocks in the north and the Ordos Block in the south amalgamated to form the Western Block, which then collided with the Eastern Block along the Trans-North China Orogen to forming the North China Craton.
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Polyphase deformation of the Fuping Complex, Trans-North China Orogen : Structures, SHRIMP U-Pb zircon ages and tectonic implications

TL;DR: The Fuping Complex is located in the central part of the Trans-North China Orogen (TNCO), a Paleoproterozoic collisional belt along which the Eastern and Western Blocks were assembled to form the North China Craton.