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    夏琼霞

    办公电话:
    0551-63601567
    邮箱:
    qxxia@ustc.edu.cn
    个人简介

    夏琼霞:特任教授、博士生导师。

    1979年出生于湖北监利。2001年6月毕业于中国地质大学(武汉)并获得学士学位,2005年1月和2009年12月分别获得中国科学技术大学硕士和博士学位。2009年12月至2012年3月在中国科技大学地球和空间科学学院从事博士后研究,2012年4月起任中国科学技术大学特任副研究员,2019年1月被聘为特任教授。2011年获中科院优秀博士学位论文奖,2012年获全国优秀博士学位论文提名奖,2018年获侯德封矿物岩石地球化学青年科学家奖。2018年获国家自然科学基金委优秀青年基金资助。

    在大陆俯冲带超高压岩石变质分异、变质脱水和部分熔融等方面取得多项成果。在Journal of Petrology, Chemical Geology、Lithos、American Mineralogist, Gondwana Research等国内外学术刊物发表SCI论文20余篇,其中第一作者和通讯作者论文SCI他引200多次。

    学习经历

    1997.9-2001.7, 中国地质大学(武汉), 地质学, 学士

    2001.9-2004.8, 中国科学技术大学, 地球化学, 硕士

    2005.9-2009.12, 中国科学技术大学, 地球化学, 博士

    科研项目

    国家自然科学基金优秀青年基金:俯冲带变质岩石学,2019/01-2021/12;主持

    国家自然科学基金面上项目:地壳深熔岩石中转熔矿物研究及其对混合岩和S型花岗岩成因的制约,2018/01-2021/12;主持

    国家自然科学基金面上项目大别造山带超高压变质岩石中部分熔融和变质分异的区分,2013/01-2016/12;主持

    国家自然科学基金青年项目:大别造山带超高压片麻岩中的石榴石成因研究,2010/01-2013/12;主持

    中国博士后科学基金第四批特别资助:大别造山带超高压变质岩中石榴石的成因研究,2011/09-2013/09;主持

    国家973计划项目子课题:大陆俯冲带壳幔相互作用,2015/01-2019/12;参与

    主要论文

    Luo, X., Xia, Q.-X.*, Zheng, Y.-F.,  Li, W.-C., 2022. An experimental study of partial melting of metafelsic rocks: Constraints on the feature of anatectic melts and the origin of garnets in collisional orogens. Journal of Earth Science 33, 753-769.

    Xia, Q.-X.*, Chen, Y.-X., Chen, R.-X., Zheng, Y.-F., 2022.  Elevation of zircon Hf isotope ratios during crustal anatexis: Evidence from
    migmatites close to the eastern Himalayan syntaxis in southeastern Tibet. Lithos 412-413, 106592.

    Yu, M., Xia, Q.-X.*, Zheng, Y.-F., Zhao, Z.-F., Chen, Y.-X., Chen, R.-X., Luo, X., Li, W.-C., Xu, H., 2021. The composition of garnet in granite and pegmatite from the Gangdese orogen in southeastern Tibet: constraints on pegmatite petrogenesis. American Mineralogist 106, 265-281.

    Xia, Q.-X.*, Gao, P., Yang, G., Zheng, Y.-F., Zhao, Z.-F., Li, W.-C., Luo, X., 2019. The Origin of garnets in Anatectic Rocks from the Eastern Himalayan Syntaxis, Southeastern Tibet: Constraints from Major and Trace Element Zoning and Phase Equilibrium Relationships. Journal of Petrology, 60, 2241-2280.

    Xia, Q.-X.*, Zhou, L.-G., 2017. Different origins of garnet in high pressure to ultrahigh pressure metamorphic rocks. Journal of Asian Earth Sciences 145, 130-148.

    Xia, Q.-X.*, Wang, H.-Z., Zhou, L.-G., Gao, X.-Y., Zheng, Y.-F., Van Orman, A. J., Xu, H.J., Hu, Z.C., 2016. Growth of metamorphic and peritectic garnets in ultrahigh-pressure metagranite during continental subduction and exhumation in the Dabie orogen. Lithos 266-267, 158-181.

    Xia, Q.-X.*, Zheng, Y.-F., Chen, Y.-X., 2013. Protolith control on fluid availability for zircon growth during continental subduction-zone metamorphism in the Dabie orogen. Journal of Asian Earth Sciences 67-68, 93-113.

    Xia, Q.-X.*, Zheng, Y.-F., Lu, X.-N., Hu, Z.C., Xu, H.J., 2012. Formation of metamorphic and metamorphosed garnets in the low-T/UHP metagranite during continental collision in the Dabie orogen. Lithos 136-139, 73-92.

    Xia, Q.-X.*, Zheng, Y.-F., Hu, Z.C., 2010. Trace elements in zircon and coexisting minerals from low-T/UHP metagranite in the Dabie orogen: Implications for action of supercritical fluid during continental subduction-zone metamorphism. Lithos 114, 385-412.

    Xia, Q.-X., Zheng, Y.-F.*, Yuan, H.L., Wu, F.-Y., 2009. Contrasting Lu-Hf and U-Th-Pb isotope systematics between metamorphic growth and recrystallization of zircon from eclogite-facies metagranites in the Dabie orogen, China , Lithos 112, 477-496.

    Xia, Q.-X., Zheng, Y.-F.*, Zhou, L.-G., 2008. Dehydration and melting during continental collision: Constraints from element and isotope geochemistry of low-T/UHP granitic gneiss in the Dabie orogen. Chemical Geology 247, 36-65.

    Xia, Q.-X., Zhi X.C.*, Li J.H., Huang X.N., 2004. Chondritic osmium isotopic composition of late Archean convecting upper mantle: Evidence from Zunhua podiform chromitites, Hebei, North China. Chinese Science Bulletin 49, 2515-2520.

    Zhou, L.-G., Xia, Q.-X.*, Zheng, Y.-F., Chen, R.-X., Hu, Z.C. Yang, Y.H., 2015. Tectonic evolution from oceanic subduction to continental collision during the closure of Paleotethys: Geochronological and geochemical constraints from metamorphic rocks in the Hong’an orogen. Gondwana Research 28, 348-370.

    Zhou, L.-G., Xia, Q.-X.*, Zheng, Y.-F., Hu, Z.C., 2014. Polyphase growth of garnet in eclogite from the Hong'an orogen: Constraints from garnet zoning and phase equilibrium. Lithos 206-207, 79-99.

    Zhou, L.-G., Xia, Q.-X.*, Zheng, Y.-F., Chen, R.-X., 2011. Multistage growth of garnet in ultrahigh-pressure eclogite during continental collision in the Dabie orogen: constrained by trace elements and U-Pb ages. Lithos 127, 101-127.

    He Q., Zhang S.-B., Zheng Y.-F., Xia Q.-X., Rubatto D., 2019. Geochemical evidence for hydration and dehydration of crustal rocks during continental rifting. Journal of Geophysical Research: Solid Earth 124, 12593-12619.

    Zheng, Y.-F., Xia, Q.-X., Chen, R.-X., Gao, X.-Y., 2011. Partial melting, fluid supercriticality and element mobility in ultrahigh-pressure metamorphic rocks during continental collision. Earth-Sci. Rev. 107, 342-374.

    Zhao, Z.-F., Zheng, Y.-F., Chen, R.-X., Xia, Q.-X., Wu, Y.-B., 2007. Element mobility in mafic and felsic ultrahigh-pressure metamorphic rocks during continental collision. Geochim. Cosmochim. Acta 71, 5244-5266.

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