柳畅 - 同济大学 - 海洋与地球科学学院

个人简介

教育背景 04/2008-02/2013 ，固体地球物理学，博士(联合培养) Ecole Normale Superieure Paris法国巴黎高等师范学院(01/2010-02/2013) 中国科学院大学，中科院计算地球动力学重点实验室(04/2008-12/2009) 09/2002-09/2005, 中国地质大学(北京), 地球物理学，硕士 09/1998-09/2002, 江汉石油学院(现名长江大学), 地球物理学，学士工作经历 03/2019-08/2019：悉尼大学，地球科学学院，访问学者 03/2017-：同济大学，海洋与地球科学学院，副教授 11/2015-03/2017：中山大学，地球科学与地质工程学院，特聘副研究员 09/2013-10/2015：华中科技大学，地球物理研究所，博士后 02/2013-08/2013：加拿大卡尔加里大学，地球科学学院，助理研究员 09/2005-12/2007：北京市康科瑞公司雇员科研项目基于精细断层结构的鲜水河-小江-龙门山断裂带系应力演化与地震危险性的三维数值模拟研究(No. 41974102)，2020-2023，80万，国家自然科学面上基金，主持鲜水河-安宁河-龙门山断裂带系断层相互作用与地震活动性的数值模拟(No. 9ZR145960，2019-2022，20万，上海市自然科学面上基金，主持西太平洋边缘海深部结构及海域地震发生机理(MG20180205)，2018.01-2019.12，40万，海洋地质国家重点实验室自主探索基金，主持康定地震引起的龙门山断裂带地震空区的应力变化及对其地震危险性的影响(No. 16GPY10)，2016.01-2016.12，15万，中山大学青年教师培育项目，主持青藏高原东北缘新生代构造演化与深部动力学过程(No. 41590865)，2015.01-2020.12，4000万，国家自然科学基金重大专项，参与龙门山断裂带西南段地震空区地震危险性的三维数值模拟研究 (No. 41404075)，2015.01-2017.12，国家自然科学青年基金，主持地震分析预测若干实用技术研究 (No. 2012BAK19B03-5), 2012.01-2015.12，800万，科技部国家科技支撑计划，参与岩石圈三维结构与动力学数值模拟(SinoProbe-07)，2008.01-2013.12，2000万，国土资源部深部探测项目第七专题，参与华北克拉通破坏 (No. 90814014), 2008.01-2012.12, 400万，国家自然科学基金重大研究计划，参与荣誉与奖励 2013　加拿大卡尔加里大学“Eyes High” fellowship 2011　中国科学院“科教结合与创新”学生一等奖

研究领域

通过数值模拟的方法分析地球动力学若干问题(侧重于岩石圈动力学、地震成因机理、地震力学与地震活动性分析）： 1. 建立断裂带区域的力学模型，分析构造应力场与地壳形变特征以探讨地震孕震成因机理 2. 断层之间的相互作用过程、地震触发 3. 地幔-岩石圈相互作用过程，及其在地震孕震成因中的作用 4. 岩石圈变形过程，包括：造山带、张裂大陆及洋盆演化，探讨区域岩石圈流变结构在构造动力学中的控制作用

近期论文

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Chen J.Q., Liu, C.*, Zhang, H., Shi, Y.L., 2022. Seismic activities and hazards of the seismic gaps in the Haiyuan fault in northeastern Tibet: Insights from numerical modelling earthquake interaction. Earth and Space Science, 9(11): 1-14. Liu, C.* and Shi, Y.L., 2022. The role of fault interaction on earthquake migration in central Sulawesi, Indonesia. Tectonophysics, 839(20):1-14. Liu, C.*, Zhang, H., Chen, JQ., Shi, Y., 2022. Stress evolution before and after the 2021 Mw 7.3 Maduo earthquake in northeastern Tibet and its influence on seismic hazard. Earth and Space Science, 9(6): 1-15. Liu, C.*, & Shi, Y. 2021. Space-time stress variations on the Palu-Koro fault impacting the 2018 Mw 7.5 Palu earthquake and its seismic hazards. Geochemistry, Geophysics, Geosystems, 22 (5), 1-11. https://doi.org/10.1029/2020GC009552 Liu, C.*, Zhu, B.J., Shi, Y.L., 2020. Do the two seismic gaps in the southwest Longmen Shan fault present the same seismic hazards? Journal of Geophysical Research (Solid Earth), 123, https://doi.org/10.1029/2019JB018160 Liu, C.*, Dong, P.Y., Zhu, B.j., Shi, Y.L., 2018. Stress shadow on the southwest portion of the Longmen Shan fault impacted the 2008 Wenchuan earthquake rupture. Journal of Geophysical Research (Solid Earth),123. https://doi.org/10.1029/2018JB015633 Liu, C.*, Dong, P.Y., Shi, Y.L., 2017. Recurrence interval of the 2008 Mw 7.9 Wenchuan earthquake inferred from geodynamic modelling stress buildup and release. Journal of Geodynamics, 110:1-11. Liu, C.*,Dong, P.Y.*, Shi, Y.L., 2017. Stress change from the 2015 Mw 7.8 Gorkhar earthquake and increased hazard in the southern Tibetan Plateau. Physics of the Earth and Planetary Interiors, 267: 1-8. Liu, C.*, Zhu, B.J., Shi, Y.L., 2016. Lithospheric rheology and Moho upheaval control the generation mechanism of the intraplate earthquakes in the North China Basin. Journal of Asian Earth Sciences, 121:153-164. Liu, C.*, Zhu, B.J., Yang, X.L., Shi, Y.L., 2016. Geodynamic background of the 2008 Wenchuan earthquake based on 3D visco-elastic numerical modelling. Physics of the Earth and Planetary Interiors, 252:23-36. Liu, C.*, Zhu, B.J., Yang, X.L., 2015. Crustal rheological strength heterogeneities control the formation of continental plateau margin. Journal of Asian Earth Sciences, 107: 62-71. Liu, C.*, Zhu, B.J., Yang, X.L., Shi, Y.L., 2015. Crustal rheology control on earthquake activity across the eastern margin of the Tibetan Plateau: insights from numerical modelling. Journal of Asian Earth Sciences, 100: 20-30. Liu, C.*, Zhu, B.J., Yang, X.L., 2015. How does crustal shortening contribute to the uplift of the eastern margin of the Tibetan Plateau? Journal of Asian Earth Sciences, 98: 18-25. 柳畅, 石耀霖, 朱伯靖, 程惠红, 杨小林, 2014. 地壳流变结构控制作用下的龙门山断裂带地震发生机理. 地球物理学报, 57(2): 404-418. 柳畅, 石耀霖, 郑亮, 朱伯靖, 2012. 三维黏弹性数值模拟华北盆地地震空间分布与构造应力积累关系. 地球物理学报, 55(12): 3942-3957. 柳畅, 朱伯靖, 石耀霖, 2012. 粘弹性数值模拟龙门山断裂带应力积累及大震复发周期. 地质学报, 86(1): 157-169. Zhu, B.J., Liu, C., Shi, Y.L., 2012. Saturated dislocations transient propagation-evolution in olivine structure under ultra high-coupled thermal-force fields. Theoretical and Applied Fracture Mechanics, 58(1): 9-20. Zhu, B.J., Cheng, H.H., Qiao, Y.C., Liu, C., Shi, Y.L., Zhang, K., Sun, D.S., Lin, W.R., 2012. Porosity and permeability evolution and evaluation in anisotropic porosity multiscale multiphase multicomponent structure. Chinese Science Bulletin, 57(4): 320-327. Cheng, H.H., Qiao, Y.C., Liu, C., Li, Y.B., Zhu, B.J., Shi, Y.L., Sun, D.S. Zhang, K., Lin, W.R., 2012. Extended hybrid pressure and velocity boundary conditions for D3Q27 Latice Boltzmann model. Applied Mathematical Modelling, 36(5): 2031-2055. Liu, C., Zhu, B.J., Shi, Y.L., 2011. Coseismic stress variation and numerical analysis of 2011 Japan–Honshu 9.0 earthquake. Theoretical and Applied Fracture Mechanics, 55(2):118-130. Zhu, B.J., Liu, C., Shi, Y.L., Sun, D.S. Zhang, K.,2011. Application of flow driven pore-network crack model to Zipingpu reservoir and Longmenshan slip. Science China (D), 54(8):1532-1540. 朱伯靖, 柳畅, 石耀霖, 2010. 汶川地震断层应力强度因子分析超奇异积分法. 科技导报, 28(05): 49-54.

学术兼职

期刊审稿:Earth and Planetary Science Letters, Geophysical Journal International, Physics of the Earth and Planetary Interiors, Journal of Asian Earth Sciences, Science China (D), Human and Ecological Risk Assessment, Tectonophysics