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Huayun Tang

Researcher at China University of Geosciences (Wuhan)

Publications -  27
Citations -  1438

Huayun Tang is an academic researcher from China University of Geosciences (Wuhan). The author has contributed to research in topics: Craton & Zircon. The author has an hindex of 17, co-authored 26 publications receiving 1204 citations. Previous affiliations of Huayun Tang include Okayama University.

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Triassic “adakitic” rocks in an extensional setting (North China): Melts from the cratonic lower crust

TL;DR: In this paper, the Shuiquangou volcanic rocks with high Sr/Y (>72) and (La/Yb)N (>24) also show enrichment in light rare-earth elements and large-ion lithophile elements (e.g., Rb, Ba and Pb), and depletion in high-field-strength elements.
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Zircon U-Pb age and Hf isotope of Quanyishang A-type granite in Yichang: signification for the Yangtze continental cratonization in Paleoproterozoic

TL;DR: Zircon U-Pb age and Hf isotope, and major and trace element compositions were reported for granite at Quanyishang which intruded into the Kongling complex in Yichang, Hubei Province as mentioned in this paper.
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Linking continental deep subduction with destruction of a cratonic margin: strongly reworked North China SCLM intruded in the Triassic Sulu UHP belt

TL;DR: In this article, the authors used peridotites along the southern margin of the Sulu UHP terrane to understand the evolution of continental cratons and their margins and showed that the deep lithosphere of the cratonic margin experienced Proterozoic metasomatic modification, followed by a strong Early Mesozoic (~470 Ma) tectonothermal event and the Early Mesogeneic collision and northward subduction of the Yangtze craton.
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Geochemistry and geochronology of Carboniferous volcanic rocks in the eastern Junggar terrane, NW China: Implication for a tectonic transition

TL;DR: In this article, the early and late Carboniferous tectonic setting of the Junggar terrane, northern Xinjiang, NW China, has long been a matter of debate.
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Accretion and reworking beneath the North China Craton

TL;DR: In this paper, the ages and compositions of lower crustal and upper mantle xenoliths from the North China Craton (NCC) are synthesized to constrain the accretion and reworking processes that have affected the deep lithosphere beneath the craton.