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Guo-Ding Yi

Researcher at Chinese Academy of Sciences

Publications -  5
Citations -  262

Guo-Ding Yi is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Zircon & Subduction. The author has an hindex of 5, co-authored 5 publications receiving 212 citations.

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Early Jurassic high-pressure metamorphism of the Amdo terrane, Tibet: Constraints from zircon U-Pb geochronology of mafic granulites

TL;DR: In this article, the results from a combined study of Cathodoluminescence imaging, LA-ICPMS U-Pb dating, and trace element analysis of zircons from high pressure (HP) mafic granulites from the Amdo terrane were reported.
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Late Triassic island-arc--back-arc basin development along the Bangong-Nujiang suture zone (central Tibet): Geological, geochemical and chronological evidence from volcanic rocks

TL;DR: Zhang et al. as discussed by the authors presented new zircon U-Pb geochronology, rare earth elements (REEs) and bulk-rock geochemistry of these magmatic rocks in the Amdo area, the middle Bangong-Nujiang suture zone, central Tibet, to identify significant and new records of Mesozoic tectonomagmatic processes.
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A syn-collisional model for Early Cretaceous magmatism in the northern and central Lhasa subterranes

TL;DR: In this paper, the authors focus on the Lower Cretaceous volcanic rocks in the Nagqu area, northern Lhasa subterrane, and present their zircon LA-ICP-MS U-Pb ages, in situ Hf isotopic data, whole-rock major and trace element compositions, and Sr-Nd isotope data.
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Middle Triassic volcanic rocks in the Northern Qiangtang (Central Tibet): Geochronology, petrogenesis, and tectonic implications

TL;DR: In this paper, the age of primitive volcanic rocks from the Yanshiping area, Northern Qiangtang terrane was investigated using the whole-rock major-trace elemental, Sr-Nd isotopic data, and zircon U-Pb age.
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Middle Triassic ultrapotassic rhyolites from the Tanggula Pass, southern Qiangtang, China: A previously unrecognized stage of silicic magmatism

TL;DR: The Tanggula Pass rhyolites were derived by partial melting of mixed source rocks including older sedimentary rocks in the upper crust and juvenile materials, triggered by north-dipping subduction of the Bangong-Nujiang Tethyan oceanic lithosphere as mentioned in this paper.