Xingcheng Liu
liuxingcheng@gig.ac.cn
Chinese, English
Guangdong
University of Chinese Academy of Sciences
Earth sciences
  • 2009-09--2015-01 PhD: Guangzhou Institute of Geochemistry, Chinese Academy of Sciences
  • 2005-09--2009-07 Bachelor of Engineering: Chang'an University
  • 2019-01~present, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Researcher
  • 2017-07~2018-12, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Associate Researcher
  • 2015-08~2016-07, Tokyo Institute of Technology, Special Assistant Professor
  • 2015-01~2017-06, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Assistant Researcher
  • 2014-09~2014-12, Tokyo Institute of Technology, Visiting Scholar
  • 2012-04~2012-10, University of Bayreuth, Germany, Visiting Scholar
  • Zhu Li Yuehua Excellent Doctoral Student Scholarship, Academy Level, 2015
  • Representative Achievement of the Year 2014, Guangzhou Institute of Geochemistry, 2015
High-temperature high-pressure experiments
Magma-hydrothermal ore deposit deep processes
Subduction zone magmatic processes elemental differentiation
  • Oxidation state of Cu in silicate melts at upper mantle conditions, Xingcheng Liu, 2024
  • Experimental study on copper solubility in hydrated silicate melts, Xingcheng Liu, 2022
  • Sulfur dissolution capacity of highly hydrated and fluid-saturated dacitic magmas at the lower crust and implications for porphyry deposit formation, Xingcheng Liu, 2022
  • Gold solubility in silicate melts and fluids: Advances from high-pressure and high-temperature experiments, Xingcheng Liu, 2021
  • The partitioning behavior of trace elements in subduction zones: Advances and prospects, Xingcheng Liu, 2020
  • Sulfur abundance and heterogeneity in the MORB mantle estimated by copper partitioning and sulfur solubility modelling, Xingcheng Liu, 2020
  • Element Migration of Supercritical Fluids in Subduction Zones: Progress and Problems of Experimental Researches, Xingcheng Liu, 2020
  • Oxidation State of Arc Mantle Revealed by Partitioning of V, Sc, and Ti Between Mantle Minerals and Basaltic Melts, Xingcheng Liu, 2019
  • Stability of the hydrous phases of Al-rich phase D and Al-rich phase H in deep subducted oceanic crust, Xingcheng Liu, 2019
  • Aqueous Fluid Connectivity in Subducting Oceanic Crust at the Mantle Transition Zone Conditions, Xingcheng Liu, 2018
  • TiO2 Solubility and Nb and Ta Partitioning in Rutile-Silica-Rich Supercritical Fluid Systems: Implications for Subduction Zone Processes, Xingcheng Liu, 2018
  • Nb/Ta Fractionation by Amphibole in Hydrous Basaltic Systems: Implications for Arc Magma Evolution and Continental Crust Formation, Xingcheng Liu, 2017
  • Partitioning of Cu between mafic minerals, Fe-Ti oxides and intermediate to felsic melts, Xingcheng Liu, 2015
  • Partitioning of copper between olivine, orthopyroxene, clinopyroxene, spinel, garnet and silicate melts at upper mantle conditions, Xingcheng Liu, 2014
  • Adakitic rocks and destruction of the North China Craton: Evidence from experimental petrology and geochemistry, Xingcheng Liu, 2011
High-Pressure High-Temperature Experimental Magma Hydrothermal Ore Deposits Subduction Elemental Differentiation Geochemistry Experimental Petrology

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