武汉大学主页平台管理系统潘雨迪--潘雨迪--论文成果

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[1]. Qin, T. , Bohlen, T. , Allroggen, N. , Klotzsche, A. 和 Pan, Y.. Application of subset full-waveform inversion to multi-offset surface ground-penetrating radar data. IEEE Transactions on Geoscience and Remote Sensing. 2024.
[2]. Qin, T. , Bohlen, T. 和 Pan, Y.. Indirect joint petrophysical inversion of shallow-seismic and multi-offset ground-penetrating radar field data. Geophysical Journal International. 237 (2). 974-988. 2024.
[3]. Pan, Y. 和 Gao, L.. Individual and Joint Inversions of Shallow-Seismic Rayleigh and Love Waves: Full-Waveform Inversion Versus Random-Objective Waveform Inversion. Surveys in Geophysics. 44. 983–1008. 2023.
[4]. Gao, L. , Pan, Y. , Rieder, A. , Bohlen, T. 和 Mao, W.. Multiparameter 2-D viscoelastic full-waveform inversion of Rayleigh waves: a field experiment at Krauthausen test site. Geophysical Journal International. 234. 297-312. 2023.
[5]. Irnaka, T.M. , Brossier, R. , Métivier, L. , Bohlen, T. 和 Pan, Y. 3D Multi-component Full Waveform Inversion for Shallow-Seismic Target: Ettlingen Line Case Study. Geophysical Journal International. 229. 1017-1040. 2022.
[6]. Hu, Y. , Pan, Y. 和 Xia, J.. Wavefield-separated full-waveform inversion of shallow-seismic Rayleigh waves. Pure and Applied Geophysics. 179. 1583-1596. 2022.
[7]. Pan, Y. , Gao, L. 和 Bohlen, T.. Random-objective waveform inversion of 3D-9C shallow-seismic field data. Journal of Geophysical Research: Solid Earth. e2021JB022036. 2021.
[8]. Gao, L. , Pan, Y. , Andreas, R 和 Bohlen, T.. Multiparameter viscoelastic full waveform inversion of shallow seismic surface waves with a preconditioned truncated-Newton method. Geophysical Journal International. 227. 2044–2057. 2021.
[9]. Gao, L. , Pan, Y. 和 Bohlen, T.. 2D multi-parameter viscoelastic shallow-seismic full waveform inversion: reconstruction tests and first field-data application. Geophysical Journal International. 222. 560-571. 2020.
[10]. Pan, Y. 和 Gao, L.. Random objective waveform inversion of surface waves. Geophysics. 85 (4). EN49-EN61. 2020.

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