Wang Qiong(Q. Wang)

Email:wangqiong@ief.ac.cn

Education: 

B. Sc. Geoinformation Science and Technology, Ocean University of China, Shandong (2009)

M. Sc. Geophysics, Institute of Earthquake Forecastting China Earthquake Administration, Beijing (2012)

Ph. D. Geophysics, Institute of Geophysics China Earthquake Administration, Beijing (2015)

Employment：

2015.07-Present     Institute of Earthquake Forecasting, China Earthquake

Administration, Research Associate

Research Experitise:  

1.Seismic anisotropy through the shear-wave splitting      

2.Crustal structure through ambient noise tomography

Selected of Publisments:

1.Wang Q, Gao Y. Rayleigh wave phase velocity and azimuthal anisotropy in the northeastern margin of the Tibetan plateau derived from seismic ambient noise. Chinese J. Geophys. (in Chinese),61(7):2760-2775.

2. Wang Q, Niu F L, Gao Y, Chen Y T. Crustal structure and deformation beneath the NE margin of the Tibetan plateau revealed by receiver function data. Geophys. J. Int., 2016, 204(1): 167-179. 

3. Wang Q, Gao Y, Shi Y T, et al. Rayleigh wave azimuthal anisotropy on the southeastern front of the Tibetan Plateau from seismic ambient noise. Chinese J. Geophys. (in Chinese), 58(11): 4068-4078. 

4. Wang Q, Gao Y.  Rayleigh wave phase velocity tomography and strong earthquake activity on the southeastern front of the Tibetan Plateau. Science China: Earth Sciences, 2014, 57: 2532–2542, doi: 10.1007/s11430-014-4908-2. 

5. Wang Q., Gao Y., Shi Y. T., et al. Seismic anisotropy in the uppermost mantle beneath the northeastern margin of Qinghai-Tibet plateau: evidence from shear wave splitting of SKS, PKS and SKKS. Chinese J. Geophys. (in Chinese), 2013, 56(3): 892-905, doi: 10.6038/cjg20130318.