Tao Wang
Earth sciences
School of Earth Sciences and Engineering
Jiangsu
Language: English, Chinese
Contact
Seismic Structure Earth Planetary Interiors Body Waves Seismic Interferometry Ai Geophysical Research Data Analysis Signal Processing Earthquake
Areas of Focus
  • Studying seismic structure of the Earth and planetary interiors
  • Extracting body waves by seismic interferometry
  • Applying AI techniques for geophysical researches
Work Experience
  • 2022 - Professor, School of Earth Sciences and Engineering, Nanjing University, China
  • Oct.2016 - 2022 Associate professor, School of Earth Sciences and Engineering, Nanjing University, China
  • Sep.2013 - Oct.2016 Post-doc, School of Earth Sciences and Engineering, Nanjing University, China
Academic Background & Achievements
  • 2008-2013 PhD., Geophysics: University of Minnesota, USA
  • 2005-2008 MSc., Geophysics: Institute of Geology and Geophysics, Chinese Academy of Sciences
  • 2000-2004 BSc., Geophysics: Department of Earth & Space Science, University of Science and Technology of China
Publications
  • Martian Seismic Anisotropy underneath Elysium Planitia Revealed by Direct S Wave Splitting, Shi, J., Han, C.R., Wang, T.*, Qi, C.*, Chen, H., Yu, Z.H., Geng, J.Q., Yang, M.H., Wang, X., Chen, L., Hui, H.J., 2024
  • Differences in Scattering Properties of the Shallow Crusts of Earth, Mars, and the Moon Revealed by P-Wave Receiver Functions, Shi, J., Wang, T.*, Chen, H., Yang, M.H., Chen, L., Hui, H.J., Xu, Z.B., Lognonné, P. and Kawamura, T., 2023
  • Active source seismic first-arrival pickup method based on small sample convolutional neural network, Yu, Z.H., Wang, T.*, Sun, P.Y., Wang, W.C. and Guo, Z.B., 2022
  • Repeating infrasound from an earthquake doublet in Alaska, Yang, M.H., Wang, T.* and Shi, J., 2021
  • Receiver function velocity analysis technique and its application to remove multiples, Shi, J., Wang, T.* and Chen, L., 2020
  • Active source seismic identification and automatic picking of P-wave first arrival using convolutional neural network, Xu, Z., Wang, T.*, Xu, S.H., Wang, B.S., Feng, X.P., Shi, J. and Yang, M.H., 2019
  • Mantle transition zone structure beneath Northeast Asia from 2D triplicated waveform modeling: Implication for a segmented stagnant slab, Lai, Y.J., Chen, L.*, Wang, T.* and Zhan, Z.W., 2019
  • Influence of source factors on extracting empirical Green's functions by coda interferometry, Feng, X.P. and Wang, T.*, 2019
  • Simulation of core phases from coda interferometry, Wu, B.J., Xia, H., Wang, T.* and Shi, X.Q., 2018
  • Support for equatorial anisotropy of Earth’s inner-inner core from seismic interferometry at low latitudes, Wang, T. and Song, X.D., 2018
  • Equatorial anisotropy in the inner part of Earth’s inner core from autocorrelation of earthquake coda, Wang, T., Song, X.D. and Xia, H., 2015
  • Two-dimensional/three-dimensional waveform modeling of subducting slab and transition zone beneath Northeast Asia, Wang, T., J. Revenaugh and Song, X.D., 2014
  • Distinct velocity variations around the base of the upper mantle beneath northeast Asia, Wang, T. and Chen, L., 2009
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