Paper Publications

• [16] 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.
• [17] 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.
• [18] 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.
• [19] 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.
• [20] Qiong-Xia Xia.Formation of metamorphic and metamorphosed garnets in the low-T/UHP metagranite during continental collision in the Dabie orogen.Lithos.2012,136-139:73-92
• [21] 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.
• [22] 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.
• [23] 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.
• [24] 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.
• [25] 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.
• [26] 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
• [27] 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.