翁爱华,教授,博士生导师,“唐敖庆学者领军教授B岗”。2001年博士毕业于吉林大学,留校任教。2004年-2006年在浙江大学博士后科研流动站工作;2010年在美国俄勒冈州立大学访问研究。获2005年度中国地球物理学会傅承义青年科技奖;2008年度中国地质学会第十一届“青年地质科技奖”(银锤奖)。先后主持国家自然科学基金、国家重大仪器研发专项、深地专项等科研项目。主要从事地球电磁理论、方法技术与应用研究,取得的重要成果包括:建立勘探电磁格林函数的通用框架;开发出三维可控源地球电磁勘探反演技术;获得了中国东北地区软流圈电阻率图像,发现广泛的地幔水化现象;揭示了板内火山的跨岩石圈传输体系及其在地壳中的演化分异过程的地球物理证据;利用地磁测深技术,获得转换带的精细电导率图像,给出了板块滞留、水进入地幔转换带及下地幔的地球物理约束。近年来,在Nature Communications、Earth and Planetary Science Letters、Geology、Geophysical Research Letters、中国科学:地球科学等地学TOP期刊先后发表科研论文100余篇。
近年主要论文目录:
[1] Li, S., Li, Y., Zhang, Y., Zhou, Z., Guo, J., & Weng, A. (2023). Remnant of the late Permian superplume that generated the Siberian Traps inferred from geomagnetic data. Nature Communications, 14(1). https://doi.org/10.1038/s41467-023-37053-3
[2] Li, Y., Weng, A., Zhou, Z., Guo, J., Li, S., Ventura, G., & Xu, W. (2024). Crustal root shapes the plumbing system of a monogenetic volcanic field as revealed by magnetotelluric data. Earth and Planetary Science Letters, 626(November 2023). https://doi.org/10.1016/j.epsl.2023.118523
[3] Li, S., Li, Y., Guo, J., Zhou, Z., & Weng, A. (2023). A water transport system across the mantle transition zone beneath western North America as imaged by electrical conductivity data. Geology, 51(5), 505–509. https://doi.org/10.1130/G51005.1
[4] Li, Y., Weng, A., Xu, W., Zou, Z., Tang, Y., Zhou, Z., et al. (2021). Translithospheric magma plumbing system of intraplate volcanoes as revealed by electrical resistivity imaging. Geology, 49(11), 1337–1342. https://doi.org/10.1130/G49032.1
[5] Li, S., Guo, J., Zhang, Y., Li, Y., Zhou, Z., Xu, W., et al. (2025). Water Reservoirs in the Lower Mantle Beneath Northeastern Asia. Geophysical Research Letters, 52(8). https://doi.org/10.1029/2024GL114180
[6] Li, S., Weng, A., Li, J., Shan, X., Han, J., Tang, Y., et al. (2020). Deep origin of Cenozoic volcanoes in Northeast China revealed by 3-D electrical structure. Science China Earth Sciences, 63(4), 533–547. https://doi.org/10.1007/s11430-018-9537-2
[7] Li, S., Weng, A., Zhang, Y., Schultz, A., Li, Y., Tang, Y., et al. (2020). Evidence of Bermuda Hot and Wet Upwelling From Novel Three-Dimensional Global Mantle Electrical Conductivity Image. Geochemistry, Geophysics, Geosystems, 21(6), 1–24. https://doi.org/10.1029/2020GC009016
[8] Li, S., Li, Y., Guo, J., Hong, D., Wang, Z., & Weng, A. (2023). Mantle Plume Reconstruction by Three-Dimensional Electromagnetic Induction. IEEE Transactions on Geoscience and Remote Sensing, 61, 1–17. https://doi.org/10.1109/TGRS.2023.3303642
[9] Xu, W. L., Chen, J. H., Weng, A. H., Tang, J., Wang, F., Wang, C. G., et al. (2021). Stagnant slab front within the mantle transition zone controls the formation of Cenozoic intracontinental high-Mg andesites in northeast Asia. Geology, 49(1), 19–24. https://doi.org/10.1130/G47917.1
[10] Zhang, Y., Weng, A., Li, S., Yang, Y., Tang, Y., & Liu, Y. (2020). Electrical conductivity in the mantle transition zone beneath Eastern China derived from L1-Norm C-responses. Geophysical Journal International, 221(2), 1110–1124. https://doi.org/10.1093/gji/ggaa059
[11] Guo, J., Li, S., Wang, X., Zhou, Z., & Weng, A. (2025). A water-rich zone crossing the 660 km discontinuity beneath the SE Tibetan Plateau revealed by one-dimensional electrical conductivity modelling. Earth, Planets and Space, 77(1). https://doi.org/10.1186/s40623-025-02162-4
吉林大学  其他
西安地质学院  其他
长春地质学院  其他
吉林大学 地球探测科学与技术学院