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翁辉辉
  • 职称: 职称: 准聘副教授
  • 岗位: 仅研究系列选择
  • 联系电话: +86-02589681885
  • 办公地址: 地科楼A456
  • 电子邮件: weng@nju.edu.cn
  • 课题组链接: https://huihuiweng.github.io

个人简介

翁辉辉博士,副教授(PI,特聘研究员),博士生导师,主要从事震源物理的理论和数值模拟研究,入选2021年国家青年人才(海外)计划。2015年取得中国科学技术大学博士学位,先后在香港中文大学、法国UCA和法国国家科学研究中心从事博士后工作,2022年9月加入南京大学。研究兴趣包括但不限于:震源物理的理论和数值模拟研究、估算油田诱发地震的最大震级、大地震动态破裂过程反演等,在Nature Geoscience, Nature Communications, JGR, GRL等国内外刊物发表论文十余篇。


研究方向

地震破裂理论

数值模拟  

断裂带变形机制

评估大地震震级



教学情况

自2025  深部构造与地球动力学(联合授课)

自2022  地震学(独立授课)

2019   International summer schools    海报

 2019 Advanced Workshop on Earthquake Fault Mechanics: Theory, Simulation and Observations at ICTP. Trieste, Italy


科研情况

在研项目:

1、国家自然科学基金委优秀青年(海外)科学基金,主持,在研

2、国家自然科学基金委面上项目,主持,在研

3、主持国家重点研发计划专题,主持,在研


学术兼职

基金评审人:国家自然科学基金(NSFC)、美国自然科学基金(NSF)、新西兰马斯登基金Marsden fund

期刊评审人:Nature CommunicationsJGRGRL,  GJITectonophysicsBSSASRLTerra NovaPure and Applied Geophysic 





详情欢迎访问个人主页:https://huihuiweng.github.io/


课题组长期招收硕士、博士研究生、博士后/专职科研岗,欢迎对地震震源物理、断层活动等感兴趣的你加入!


Diving into the Unknown!

教育经历

工作经历

学术兼职

研究方向

开授课程

科研项目

学术成果

(* corresponding author)

Submitted / in preparation:

[S5]  Dezheng Zhao#, Huihui Weng*, Qin Wang, Yijian Zhou, Han Chen (2024). Multiscale fault-zone structures governed by earthquake rupture dynamics. Submitted.    

[https://doi.org/10.21203/rs.3.rs-5432823/v1]

[S4] Huihui Weng*, Loes Buijze, Jean-Paul Ampuero (2024). Theoretical model for physics-based estimation of maximum earthquake sizes. Submitted.

[S3]  Loes Buijze, Huihui Weng, Jean-Paul Ampuero (2023). Physics-based estimates of the maximum magnitude of induced earthquakes in the Groningen gas field (application part). In manuscript.

[S2]  Huihui Weng*, Jean-Paul Ampuero (2023). Toward assessing seismic hazard from laboratory observations of rate-and-state frictional parameters. In manuscript.

[S1]  Huihui Weng*, Jean-Paul Ampuero (2023). The theoretical energy release rate of in-plane elongated ruptures. In manuscript.


Published: 

[17]  H. Weng*, The dynamics of fast and slow earthquake ruptures in viscoelastic  materials” Journal of Geophysical Research: Solid Earth, 2025.

[pdf] [https://doi.org/10.1029/2024JB030663]

[16]  Diao, F.*, H. Weng*, J. P. Ampuero, Z. Shao, R. Wang, F. Long and X. Xiong, “Physics-based  assessment of earthquake potential on the Anninghe-Zemuhe fault system  in southwestern China.”Nature Communications, 2024.

[pdf] [https://doi.org/10.1038/s41467-024-51313-w]

[15]  D. Zhao, C. Qu, X. Shan, W. Gong, H. Weng,  H. Chen, D. Wu, “An updated fault coupling model along major  block-bounding faults on the eastern and northeastern Tibetan Plateau  from a stress-constrained inversion of GPS and InSAR data.” Journal of Geophysical Research: Solid Earth, 2024.

[https://doi.org/10.1029/2023JB028483]

Numerical modelling of earthquake cycles based on Navier-Stokes equations with Viscoelastic-plasticity rheology. G-cube,2023.

[pdf] [https://doi.org/10.1029/2023GC010872]

[13]  H. Weng* and J.P. Ampuero, Integrated rupture mechanics for slow slip events and earthquakes. Nature Communications, 2022.

[pdf] [https://doi.org/10.1038/s41467-022-34927-w]

[12]  H. Weng* and J.P. Ampuero, Continuum of earthquake rupture speeds enabled by oblique slip. Nature Geoscience, 2020. 

[pdf] [https://doi.org/10.1038/s41561-020-00654-4]

[11]  Oral E., H. Weng, and J.P. Ampuero, Does a damaged fault zone mitigate the near-field impact of supershear earthquakes? Application to the 2018 Mw 7.5 Palu earthquake. Geophysical Research Letters, 47(1), 2020.

[pdf] [https://doi.org/10.1029/2019GL085649

[10]  H. Weng* and J.P. Ampuero, The dynamics of elongated earthquake ruptures. Journal of Geophysical Research: Solid Earth, 124, 2019.

[pdf[https://doi.org/10.1029/2019JB017684

[9]    H. Yang, S. Yao, B. He, A. Newman, and H. Weng, Deriving rupture scenarios from interseismic locking distributions along the subduction megathrust. Journal of Geophysical Research: Solid Earth, 2019.

[pdf[https://doi.org/10.1029/2019JB017541

[8]   H. Weng and H. Yang, Constraining frictional properties on fault by dynamic rupture simulations and near-field observations. Journal of Geophysical Research: Solid Earth, 123(8), 6658-6670, 2018. 

[pdf[https://doi.org/10.1029/2017JB015414

[7]   H. Weng and H. Yang, Seismogenic width controls aspect ratios of earthquake ruptures. Geophysical Research Letters, 44(6): 2725-2732, 2017.

[pdf[https://doi.org/10.1002/2016GL072168]

[6 H. Weng, H. Yang, Z. Zhang, and X. Chen,  Earthquake rupture extents and coseismic slips promoted by damaged fault zones. Journal of Geophysical Research: Solid Earth, 121(6): 4446-4457, 2016. 

[pdf[https://doi.org/10.1002/2015JB012713

[5]   J. Yin, H. Yang, H. Yao, and H. Weng,  Coseismic radiation and stress drop during the 2015 Mw8.3 Illapel, Chile megathrust earthquake. Geophysical Research Letters, 43: 1520-1528, 2016.

[pdf[https://doi.org/10.1002/2015GL067381]

[4]   H. Weng, J. Huang, and H. Yang,  Barrier-induced supershear ruptures on a slip-weakening fault. Geophysical Research Letters, 42(12): 4824-4832, 2015.

[pdf[https://doi.org/10.1002/2015GL064281]

[3]   H. Weng, and J. Huang, Numerical simulations about subduction earthquake cycles: The case of Japan Tohoku Mw9.0 earthquake. Journal of Geodesy and Geodynamics (in Chinese), 2015.

[2]   H. Weng, and J. Huang, Numerical simulations about the influence of stress disturbance on earthquake cycle and seismic moment. Acta Seismologica Sinica (in Chinese), 2015.

[1]   F. Diao, X. Xiong, R. Wang, Y. Zheng, T. R. Walter, H. Weng, and J. Li, Overlapping post-seismic deformation processes: afterslip and viscoelastic relaxation following the 2011 Mw 9.0 Tohoku (Japan) earthquake. Geophysical Journal International,  196(1): 218-229, 2014.

[pdf[https://doi.org/10.1093/gji/ggt376




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