F
Fu-Yuan Wu
Researcher at Chinese Academy of Sciences
Publications - 400
Citations - 50062
Fu-Yuan Wu is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 107, co-authored 367 publications receiving 42039 citations. Previous affiliations of Fu-Yuan Wu include Curtin University & University of Rennes.
Papers
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Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology
TL;DR: In this article, the mean β Yb value of the individual spot and newly published Yb isotopic abundance data, six standard zircons and two standard baddeleyites, have been investigated using a Neptune MC-ICPMS, with 193 mm laser.
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Geochronology of the Phanerozoic granitoids in northeastern China
TL;DR: Zhang et al. as mentioned in this paper used zircon U-Pb dating to constrain the spatial and temporal distribution of granitoids in the area. But the results showed that granitoid emplacement dates are not as widely distributed as previously thought.
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Nature and significance of the Early Cretaceous giant igneous event in eastern China
TL;DR: In this article, Zhang et al. used zircon U-Pb SHRIMP (5 samples), laser ablation (LA) ICP-MS (22 samples), and TIMS (5 sample) dating to establish that the Early Cretaceous was a significant period of igneous activity in the Liaodong Peninsula, with a duration of about 10 Ma.
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Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry
Honglin Yuan,Honglin Yuan,Shan Gao,Shan Gao,Xiaoming Liu,Huiming Li,Detlef Günther,Fu-Yuan Wu +7 more
TL;DR: In this paper, laser ablation-inductively coupled plasma-mass spectrometry was used for age determination of zircons of Proterozoic to Oligocene ages (1060-31 Ma).
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A-type granites in northeastern China: age and geochemical constraints on their petrogenesis
TL;DR: A-type granites are widely distributed in northeastern China (NE China). They were emplaced during three major episodes (the Permian, late Triassic to early Jurassic, and early Cretaceous) and evolved in different tectonic regimes.