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Lie-Wen Xie
Researcher at Chinese Academy of Sciences
Publications - 115
Citations - 9471
Lie-Wen Xie is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Zircon & Inductively coupled plasma mass spectrometry. The author has an hindex of 36, co-authored 100 publications receiving 7849 citations.
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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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In situ simultaneous determination of trace elements, U-Pb and Lu-Hf isotopes in zircon and baddeleyite
TL;DR: In this paper, a combined method of simultaneously measuring U-Pb and Lu-Hf isotopes as well as trace elements in Phalaborwa baddeleyite and 91500, GJ-1, TEMORA-1 and SK10-2 zircons was described.
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Constraints on the timing of uplift of the Yanshan Fold and Thrust Belt, North China
TL;DR: In this paper, the authors report in situ U-Pb ages and Hf isotopic data on detrital zircons from Paleozoic to Late Mesozoic strata in the Xishan area near Beijing that provide important constraints on the evolution and paleogeography of the northern part of the North China Craton.
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Tracing magma mixing in granite genesis: in situ U–Pb dating and Hf-isotope analysis of zircons
TL;DR: In situ zircon U-Pb and Hf-isotopic data have been determined for mafic microgranular enclaves and host granitoids from the Early Cretaceous Gudaoling batholith in the Liaodong Peninsula, NE China, in order to constrain the sources and petrogenesis of granites.
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Combined chemical separation of Lu, Hf, Rb, Sr, Sm and Nd from a single rock digest and precise and accurate isotope determinations of Lu–Hf, Rb–Sr and Sm–Nd isotope systems using Multi-Collector ICP-MS and TIMS
TL;DR: In this article, a combined procedure for separating Lu, Hf, Rb, Sr, Sm and Nd from a single sample digestion is presented, and the results show good agreement with previously reported values by isotope dilution methods.