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Xiaoming Liu

Researcher at Northwest University (China)

Publications -  152
Citations -  17332

Xiaoming Liu is an academic researcher from Northwest University (China). The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 62, co-authored 141 publications receiving 14780 citations. Previous affiliations of Xiaoming Liu include China University of Geosciences (Wuhan).

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Recycling lower continental crust in the North China craton

TL;DR: It is suggested that lower crustal foundering occurred within the North China craton during the Late Jurassic, and thus provides constraints on the timing of lithosphere removal beneath the NorthChina craton.
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Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry

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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Tectonic evolution of the Qinling orogen, China: Review and synthesis

TL;DR: In this paper, the authors present new distribution maps of the Early Paleozoic ophiolites and associated volcanics in the Shangdan suture zone and the Middle Devonian-Middle Triassic Ophiolitic melange in the Mianlue suture zones, as well as the maps of granitoid and metamorphic belts displaying various ages.
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Simultaneous determinations of U-Pb age, Hf isotopes and trace element compositions of zircon by excimer laser-ablation quadrupole and multiple-collector ICP-MS

TL;DR: In this article, an in situ method for simultaneous measurement of U-Pb-Hf isotopes and trace element compositions of zircons using a quadrupole and multiple-collector inductively-coupledplasma mass spectrometer (Q-ICP-MS and MC-ICP-MS, respectively) connected to a single excimer laser-ablation system was described.
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Detrital zircon geochronology of Precambrian basement sequences in the Jiangnan orogen : dating the assembly of the Yangtze and Cathaysia Blocks

TL;DR: In this article, LA-ICP-MS U-Pb dating of detrital zircons suggests that the maximum depositional age of the basement sedimentary rocks in the western part of the Jiangnan orogen is ca. 860-800 ǫ.