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。
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
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
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 toultrahigh 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 andperitectic garnets in ultrahigh-pressure metagranite during continentalsubduction 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 forzircon growth during continental subduction-zone metamorphism in the Dabieorogen. 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 metagraniteduring continental collision in the Dabie orogen. Lithos 136-139, 73-92.
Xia, Q.-X.*, Zheng, Y.-F., Hu, Z.C., 2010. Trace elementsin zircon and coexisting minerals from low-T/UHP metagranite in the Dabieorogen: Implications for action of supercritical fluid during continental subduction-zonemetamorphism. 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. Dehydrationand melting during continental collision: Constraints from element and isotopegeochemistry of low-T/UHP granitic gneiss in the Dabie orogen. Chemical Geology247, 36-65.
Xia, Q.-X., Zhi X.C.*, Li J.H., Huang X.N., 2004. Chondritic osmium isotopiccomposition of late Archean convecting upper mantle: Evidence from Zunhuapodiform 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 tocontinental collision during the closure of Paleotethys: Geochronological andgeochemical constraints from metamorphic rocks in the Hong’an orogen. GondwanaResearch 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 duringcontinental collision in the Dabie orogen: constrained by trace elements andU-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.