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Yue Qi

Researcher at Chinese Academy of Sciences

Publications -  26
Citations -  477

Yue Qi is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Zircon & Terrane. The author has an hindex of 10, co-authored 24 publications receiving 273 citations. Previous affiliations of Yue Qi include University of Bristol & Center for Excellence in Education.

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Zircon U–Pb ages and O–Nd isotopic composition of basement rocks in the North Qinling Terrain, central China: evidence for provenance and evolution

Bing-Xiang Liu, +9 more
- 02 Jun 2013 - 
TL;DR: The Qinling Group was previously interpreted as the oldest Precambrian basement unit of the North Qinling Terrain, recording its formation and early crustal evolution as mentioned in this paper, which consists predominantly of gneisses, amphibolites, and marbles, which underwent multi-phase deformation and metamorphism.
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Eocene adakitic porphyries in the central-northern Qiangtang Block, central Tibet: Partial melting of thickened lower crust and implications for initial surface uplifting of the plateau

Quan Ou, +10 more
- 01 Feb 2017 - 
TL;DR: In this article, the authors reported on zircon U-Pb age and mineral, element, and Sr-Nd isotope composition data for Eocene adakitic porphyries in the Laorite Co area of central-northern Qiangtang Block, central Tibet.
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Geochemistry and Sr–Nd–Pb–Hf isotopic composition of the Donggou Mo-bearing granite porphyry, Qinling orogenic belt, central China

Li Yang, +7 more
- 18 Jun 2013 - 
TL;DR: Based on geochemical results, Donggou granite porphyry is a silica-supersaturated, high-K metaluminous A-type granite showing enrichment in light REEs, depletion in middle REEs and significant negative Eu, Ba, Nb, Sr, P, and Ti anomalies as discussed by the authors.
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Late Permian Bimodal Volcanic Rocks in the Northern Qiangtang Terrane, Central Tibet: Evidence for Interaction Between the Emeishan Plume and the Paleo-Tethyan Subduction System

Jun Wang, +8 more
- 01 Aug 2018 - 
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Adakitic rocks at convergent plate boundaries: Compositions and petrogenesis

Qiang Wang, +12 more
- 05 Nov 2020 - 
TL;DR: In this article, the authors show that partial melting of mafic rocks can generate adakitic magmas under pressure, temperature, and hydrous conditions of 1.2-3.0 GPa, 800-1000°C, and 1.5-6.0 wt.% H2O.