中文
Qiongxia Xia

Specially Appointed Professor

Email: qxxia@ustc.edu.cn

Xia Qiongxia 

Postdoctor of Geochmistry

Department of Geochmistry
School of Earth and Space Sciences
University of Science and Technology of China
Hefei, Anhui 230026, P. R. China
Tel: 86-551-3601567
E-mail:
qxxia@ustc.edu.cn


RESEARCH INTERESTS: Metamorphic geochemistry

PUBLICATIONS:

(1) Xia, Q.-X., Zheng Y.-F., Lu, X.N., Hu, Z.C., Xu, H.J., 2011.Multistage growth of garnet in low-T/UHP metagranite during continental collision in the Dabie orogen. Lithos (In revision).

(2) 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.

(3) 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.

(4) 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.

(5) 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.