刘伟

中国科学院地质与地球物理研究所

浏览次数

444

收藏次数

0

接洽次数

0

  • 刘伟
  • 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:

刘伟,研究员,稳定同位素地球化学实验室主任。从事花岗岩类和流体-岩石相互作用研究。提出中国阿尔泰花岗岩类主要是由从蒙古西部湖区、萨彦-阿尔泰以及蒙古-图瓦新元古代微陆块先后剥蚀搬运而来的碎屑物质重熔形成,中国阿尔泰花岗岩类的高正εNd(t)和高正εHf(t)是上述地体文德纪-寒武纪和新元古代地壳生长的同位素记忆,并不代表中国阿尔泰显生宙巨量的地壳生长。首次提出东准噶尔A-型和I-型花岗岩类是由来自上、下洋壳的岩浆与地幔岩浆混合形成。内蒙古林西二叠纪-中侏罗世花岗岩类主要是由洋壳熔融形成。发现了新疆镁铁-超镁铁侵入岩和蛇绿橄榄岩中的富CH4原生包裹体。在国内率先开展了矿物-水氧同位素交换反应动力学研究,模拟了花岗岩类共生矿物-水的18O/16O交换反应动力学。从厘米尺度的元素双向扩散交代质量平衡,论证了层状矽卡岩及其铅-锌矿床的成因。以第一作者在SCI刊物上发表论文三十多篇,主持过多项国家自然科学基金项目、973项目二级课题、中科院知识创新工程重要方向性项目。教育经历1995.10-1998.10:中国科学院广州地球化学研究所地球化学专业,博士研究生(在职),获理学博士学位1982.08-1985.05:中国科学院长沙大地构造研究所大地构造与成矿学专业,硕士研究生,获理学硕士学位1978.01-1982.02:中南工业大学地质系矿产普查与勘探专业,本科生,获学士学位工作经历2005.11-2006.02:日本秋田大学资源与工程学院资源与物质科学研究所,客座教授2003.04-2003.07:德国图宾根大学矿物岩石地球化学研究所,访问研究1999.06-现在:中国科学院地质与地球物理研究所,研究员,稳定同位素地球化学实验室主任1998.08-1999.06:中国科学院地球物理研究所,研究员1997.01-1997.08:日本地质调查所地壳流体部,访问研究。1995.03-1998.08:中国科学院矿物资源探查研究中心,研究员1992.04-1995.03:中国科学院长沙大地构造研究所,副研究员,研究室副主任1991.03-1992.04:日本理化学研究所地球化学研究室,合作研究1985.06-1991.02:中国科学院长沙大地构造研究所,助理研究员1982.02-1982.07:安徽省冶勘815地质队,地质技术员

学科类别:
花岗岩类岩石学和地球化学,稳定同位素地球化学
研究方向:

花岗岩成因地球化学成矿流体

职务:
社会任职:
承担科研项目情况:
国家自然科学基金项目《中国阿尔泰花岗岩类源岩组分的氮同位素分辨》(编号:41273019),起止年月:2013年1月--2016年12月。课题负责人。中国科学院知识创新工程重要方向项目《矿物和岩石中固定氮的同位素分析》(项目编号:KZCX2-YW-JS109),起止年月:2010年1月--2012年12月。项目负责人。国家自然科学基金项目《东准噶尔北部哈旦逊辉长岩-碳酸岩杂岩的成岩机制和源区示踪》(编号:40972053),起止年月:2010年1月--2012年12月。课题负责人。国家自然科学基金项目《甘肃北山印支期典型金矿床含金流体渗透的压力-深度-温度体制及其起源》(编号:40472056),起止年月:2005年1月--2007年12月。课题负责人。国家重点基础研究发展规划项目《中国西部中亚型造山与成矿》,03课题“古生代地壳双向增生过程中的流体作用”。起止年月:2002年4月-2006年6月。第二负责人。中国科学院知识创新工程重大项目《大陆盆山系统与战略资源预测》04课题“大区域构造过程对华北东部盆-山系统的控制”。起止年月:2000年6月-2003年6月。课题负责人。
获奖及荣誉:
代表论著:
Liu, X.J., Liu, W., 2014. Source characteristics and tectonic setting of the Early and Middle Devonian volcanic rocks in the North Junggar, Northwest China: Insights from Nd–Sr isotopes and geochemistry. Lithos, 184–187: 27–41Liu, W., Liu, X.J., Liu, L.J., 2013. Underplating generated A- and I-type granitoids of the East Junggar from the lower and the upper oceanic crust with mixing of mafic magma: Insights from integrated zircon U–Pb ages, petrography, geochemistry and Nd–Sr–Hf isotopes. Lithos, 179: 293–319Liu, X.J., Liu, Wei., 2013. Re-Os dating of the Suoerkuduke Cu (Mo) deposit, Fuyun County, Xinjiang, and its geodynamic implications. Journal of Earth Science, 24 (2): 188–202.Liu, W., Liu, X.J., Xiao, W.J., 2012. Massive granitoid production without massive continental-crust growth in the Chinese Altay―Insight into the source rock of granitoids using integrated zircon U-Pb age, Hf-Nd-Sr isotopes and geochemistry. American Journal of Science. 312: 629–684Liu, X.-J., Liu, W.(corresponding author), Liu, L.-J., 2012. The generation of a stratiform skarn and volcanic exhalative Pb-Zn deposit (Sawusi) in the southern Chinese Altay Mountains: The constraints from petrography, mineral assemblage and chemistry. Gondwana Research, 22: 597–614Liu, W., Pan, X.-F., Liu, D.-Y., Chen, Z.-Y., 2009. Three-step continental-crust growth from subduction accretion and underplating, through intermediary differentiation, to granitoid production. International Journal of Earth Sciences, 98 (6): 1413–1439 doi:10.1007/s00531-008-0299-yLiu, W., Pan, X.-F., 2006. Methane-rich fluid inclusions from ophiolitic dunite and post-collisional mafic-ultramafic intrusion: the mantle dynamics underneath the Palaeo-Asian Ocean through to the post-collisional period. Earth Planet. Sci. Lett., 242: 286–301Liu, W., Siebel, W., Li, X.-J., Pan, X.-F., 2005. Petrogenesis of the Linxi granitoids, northern Inner Mongolia of China: constraints on basaltic underplating. Chemical Geology, 219: 5–35Liu, W., 2002. Fluid-rock interaction during subsolidus microtextural development of alkali granite as exemplified by the Saertielieke pluton, Ulungur of the northern Xinjiang, China. Chemical Geology, 182: 473–482Liu, W., Li, X-J and Tan, J., 2001. Petrogenetic and metallogenetic background of the Dajing Cu-Sn-Ag-Pb-Zn ore deposit, Inner Mongolia, and characteristics of the mineralizing fluid. Resource Geology, 51(4): 321–331Liu, W., 2000. Two disequilibrium quartz-feldspar 18O/16O fractionations within the Aral granite batholith, Altay mountains of China: Evidence for occurrence of two stages of O and H isotopic exchange of a heterogeneous granite system with aqueous fluids. Journal of Petrology, 41(9): 1455–1466.Liu, W., Liu, C.Q., and Masuda, A., 1997. Complex trace-element effects of mixing-fractional crystallization composite processes: applications to the Alaer granite pluton, Altay Mountains, Xinjiang, northwestern China. Chemical Geology, 135: 103–124.刘秀金,刘伟(通讯作者),刘丽娟,尚海军,周刚,2011. 阿尔泰南缘麦兹火山-沉积盆地东部萨吾斯铅锌矿床成因探讨. 岩石学报, 27(6): 1810–1828 Liu, X.J., Liu, W. (corresponding author), Liu, L.J., Shang, H.J., Liu G.R, 2011. Genesis of the Sawusi lead-zinc deposit in the eastern Maizi volcanic-sedimentary basin, southern Altay Mountains. Acta Petrologica Sinica, 27(6): 1810–1828.刘伟,刘丽娟,刘秀金,尚海军,周刚,2010. 阿尔泰南缘早泥盆世康布铁堡组的SIMS锆石U-Pb年龄及其向东向北延伸的范围. 岩石学报, 26(2): 387–400Liu, W., Liu, L.J., Liu, X.J., Shang, H.J., Zhou, G., 2010. Age of the Early Devonian Kangbutiebao formation along the southern Altay Mountains and its northeastern extension. Acta Petrologica Sinica, 26(2): 387–400.刘伟,潘小菲,谢烈文,李禾,2007. 大兴安岭南段林西地区花岗岩类的源岩:地壳生长的时代和方式. 岩石学报,23(2): 441–460Liu, W., Pan, X.-F., Xie, L.-W., Li, H., 2007. Sources of material for the Linxi granitoids, the southern segment of the Great Xing’an Range: When and how continental crust grew? Acta Petrologica Sinica, 23(2): 441–460刘伟,潘小菲,2006. 新疆-甘肃北山金矿南带的成矿流体演化和成矿机制. 岩石学报,22(1): 171–188.Liu, W., Pan X.-F., 2006. Evolution of ore-forming fluids and formational mechanisms for gold deposits in the southern Bei Shan, Xinjiang-Gansu border area of China. Acta Petrologica Sinica, 22(1): 171–188.潘小菲,刘伟, 2006. 北山金窝子金矿床流体包裹体特征及成矿流体演化. 岩石学报,22(1):253–263潘小菲, 刘伟(通讯作者), 2005. 东天山香山镁铁-超镁铁岩中富CH4流体包裹体的特征及其意义. 岩石学报,21(01):211–218. Pan, X.-F., Liu, W. (corresponding author), 2005. Characteristics and significance of CH4-rich fluid inclusions from the mafic-ultramafic complex at the Xiangshan, eastern Tianshan Mountains, Xinjiang of China. Acta Petrologica Sinica, 21(01): 211–218.Liu Wei, Li X J, and Tan J, 2003. Fluid mixing as the mechanism of formation of the Dajing Cu-Sn-Ag-Pb-Zn ore deposit, Inner Mongolia. Science in China (Series D), 46(7):652–663 刘伟, 李新俊, 谭骏, 2002. 内蒙古大井铜-锡-银-铅-锌矿床的流体混合作用―流体包裹体和稳定同位素证据. 中国科学(D辑),32(5): 405–414Liu Wei, Li X J, and Deng J, 2003. Sources of ore-forming fluids and metallic materials in the Jinwozi lode gold deposit, eastern Tianshan Mountains of China. Science in China (Series D), 46(Supplemented): 135-153. 刘伟, 李新俊, 邓军, 2002. 东天山金窝子石英脉金矿床成矿流体和成矿物质的来源. 中国科学(D辑), 32(增刊): 105–119.刘伟,杨进辉,李潮峰,2003.内蒙赤峰地区若干主干断裂带的构造热年代学. 岩石学报,19(4): 717–728.Liu, W., Yang, J.-H., Li, C.-F., 2003. Thermochronology of three major faults in the Chifeng area, Inner Mongolia of China. Acta Petrologica Sinica, 19(4): 717–728.刘伟,李新俊,秦克章,2002. 碱性花岗岩的动力学氧同位素交换和流体流动几何学: 交换机制和平流冷却. 岩石学报, 18(3): 331–339Liu, W., Li, X.-J., Qin, K.-Z., 2002. Oxygen isotope exchange and flow geometry of meteoric-derived water within an alkali granite pluton: exchange mechanism and advective cooling. Acta Petrologica Sinica, 18(3): 331–339.LIU Wei, 2000. Two stages of isotopic exchanges experienced by the Ertaibei granite pluton, northern Xinjiang, China. Science in China (Series D), 43(6):605–616 刘伟,2000. 新疆北部二台北花岗岩体的两期同位素交换反应.中国科学(D辑), 30(3): 298–306.LIU Wei, Zhao Zhenhua, and Zhang Fuqin, 1999. Oxygen and hydrogen isotopic compositions of coexistent minerals of the Tasigake alkali granite pluton, northern Xinjiang: constraints upon the cause of 18O-D depletion and the 18O/16O exchange kinetics. Chinese Science Bulletin, 44(12): 1086–1092. 刘伟,赵振华,张福勤,1999. 新疆塔斯嘎克碱性花岗岩体矿物-大气水相互作用的氢、氧同位素制约.科学通报,44(7): 704–710.LIU Wei, Li Zhi’an, and Zhao Zhi’zhong, 1996. Oxygen isotope exchange kinetics between coexistent minerals and water in the Ertaibei granite pluton, northern Xinjiang. Science in China (Series D), 39(2): 173–183. 刘伟,李志安,赵志忠,1996. 新疆二台北花岗岩矿物-水氧同位素交换反应动力学.中国科学 (D辑),26(1): 33–40.LIU Wei, Masuda, A., 1995. Complex trace element effects of source mixing-fractional crystallization composite processes in the Kalaan granodiorite pluton along the Wulungu tectonic belt, northern Xinjiang. Science in China (Series B), 38(8): 987–995. 刘 伟,增田彰正,1995. 新疆乌仑古喀腊安花岗闪长岩源区混合-结晶分异复合过程的微量元素效应.中国科学 (B辑),25(4): 434–440.Liu Wei, He Baichu, Chen Zhensheng, 1996. Oxygen isotope exchange kinetics between coexisting minerals and water in the Aral granite pluton of the Altay Mountains, northern Xinjiang. Acta Geologica Sinica, 9(4): 366–379. 刘伟,贺伯初,陈振胜,1996. 新疆阿尔泰阿拉尔花岗岩多维矿物相-水氧同位素交换反应动力学.地质学报,70(2): 129–141.刘伟,刘建明,储雪蕾,孙世华,1998. 新疆北部花岗岩-水18O/16O交换反应动力学—对于造山带岩浆熔融与流体循环的意义.地球物理学报,41(增刊): 195–205.