刘小驰

中国科学院地质与地球物理研究所

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  • 刘小驰
  • 副研究员
  • 北京朝阳区北土城西路19号,中科院地质与地球物理研究所
简历:
2004.09-2008.06,中国地质大学(武汉),地球科学学院,地球化学专业,获学士学位2008.09-2013.06,中国地质大学(武汉),地球科学学院,地球化学专业,获博士学位2011.10-2012.10,加拿大纽芬兰纪念大学,博士研究生联合培养2013.07-2016.12,中国科学院地质与地球物理研究所,岩石圈演化研究室,博士后2017.01-今,中国科学院地质与地球物理研究所,副研究员
研究方向:
花岗岩成因与地壳演化喜马拉雅造山带岩浆作用
学科类别:
地质学
职务:
社会任职:
获奖及荣誉:
承担科研项目情况:
国家自然科学基金面上项目(41772058) 在研国家自然科学基金青年项目(41402055) 已结题中国博士后科学基金面上项目(2014M550086) 已结题
代表论著:
Liu, X.-C., Li, X.-H., Liu, Y., Yang, L., Li, Q.-L., Wu, F.-Y., Yu, H-M. and Huang, F., 2018. Insights into the origin of purely sediment-derived Himalayan leucogranites: Si–O isotopic constraints. Science Bulletin, 63(19): 1243-1245.Liu, X.-C., Wu, Y.-B., Fisher, C.M., Hanchar, J.M., Beranek, L., Gao, S. and Wang, H. (2017) Tracing crustal evolution by U-Th-Pb, Sm-Nd, and Lu-Hf isotopes in detrital monazite and zircon from modern rivers. Geology 45, 103-106.Liu, X.-C., Wu, F.-Y., Yu, L.-J., Liu, Z.-C., Ji, W.-Q. and Wang, J.-G. (2016) Emplacement age of leucogranite in the Kampa Dome, southern Tibet. Tectonophysics 667, 163-175.Liu, X.C., Wu, Y.B., Gao, S., Wang, H., Zheng, J.P., Hu, Z.C., Zhou, L. and Yang, S.H. (2014) Record of multiple stage channelized fluid and melt activities in deeply subducted slab from zircon U–Pb age and Hf–O isotope compositions. Geochimica et Cosmochimica Acta 144, 1-24.Liu, X.C., Wu, Y.B., Gao, S., Liu, Q., Wang, H., Qin, Z.W., Li, Q.L., Li, X.H. and Gong, H.J. (2012) First record and timing of UHP metamorphism from zircon in the Xitieshan terrane: Implications for the evolution of the entire North Qaidam metamorphic belt. American Mineralogist 97, 1083-1093.Liu, X.C., Wu, Y.B., Gao, S., Peng, M., Wang, J., Wang, H., Gong, H.J. and Yuan, H.L. (2012) Triassic high-pressure metamorphism in the Huwan shear zone: Tracking the initial subduction of continental crust in the whole Dabie orogen. Lithos 136–139, 60-72.Liu, X.C., Wu, Y.B., Gao, S., Wang, J., Peng, M., Gong, H.J., Liu, Y.S. and Yuan, H.L. (2011) Zircon U-Pb and Hf evidence for coupled subduction of oceanic and continental crust during the Carboniferous in the Huwan shear zone, western Dabie orogen, central China. Journal of Metamorphic Geology 29, 233-249.