个人简介
1982年于合肥工业大学地质系地质专业本科毕业；
1984年于合肥工业大学地质系构造地质专业获硕士学位；
1984年9月-1990年2月在合肥工业大学资源与环境科学系任助教、讲师；
1990年3月-1992年7月赴英国威尔士大学攻读博士学位，获构造地质专业哲学博士；
1992年11月至今在合肥工业大学资源与环境工程学院任副教授、教授、博士生导师；
000年享受国家政府津沾。
教学工作
本科生课程：《区域大地构造》；
研究生课程：《显微构造学》、《构造变形分析》、《断裂构造学》。
科研工作
主持的在研项目：
（1）国家自然科学基金重点项目：“郯庐断裂带起源机制研究”（2019-2023年；编号：41830213；经费：307万）
（2）国家科技部重点研发计划深地项目二级课题：“华北东部中生代构造演化与控矿机制”（2016-2020年；编号：2016YFC0600102；经费：664万）
（3）国家自然科学基金面上项目：“郯庐断裂带北段的起源型式、时间与动力学背景研究”（2015-2018；编号：41472186；经费：106万）
近期论文
查看导师新发文章
（温馨提示：请注意重名现象，建议点开原文通过作者单位确认）
[1]Zhu, G*., Chen, Y., Jiang, D. Z., Lin, S. Z. 2015.Rapid change from compression to extension in the North China Craton during the Early Cretaceous: Evidence from the Yunmengshan metamorphic core complex. Tectonophysics, 656: 91-110.
[2]Zhu, G*., Hu, W., Song, L. H., Liu, B. 2015. Quaternary activity along the Tan-Lu fault zone in the Bohai Bay, East China: Evidence from seismic profiles. Journal of Asian Earth Sciences, 114：5-17.
[3] Liu, B., Zhu, G*., Zhai, M. J., Gu, C. C., Liu, S. 2015. Quaternary faulting of the Jiangsu part of the Tan-Lu Fault Zone, East China: Evidence from field investigations and OSL dating. Journal of Asian Earth Sciences, 114: 89-102.
[4]Zhao, T., Zhu, G*., Lin, S. Z., Wang, H.Q. 2016. Indentation-induced tearing of a subducting continent: Evidence from the Tan–Lu Fault Zone, East China. Earth-Science Reviews, 152: 14-36.
[5]Zhu, G*., Wang, Y. S., Wang, W., Zhang, S., Liu, C., Gu, C. C., Li, Y. J. 2017. An accreted micro-continent in the north of the Dabie Orogen, East China: Evidence from detrital zircon dating. Tectonophysics, 698: 47-64.
[6] Gu, C. C., Zhu, G*.,Zhang, S., Liu, C., Li, Y. J., Lin, S. Z., Wang, W.2017. Cenozoic evolution of the Yilan-Yitong Graben in NE China: An example of graben formation controlled by pre-existing structures. Journal of Asian Earth Sciences, 146:168-184.
[7]Liu, C., Zhu, G*., Zhang, S., Gu, C. C., Li, Y. J., Su, N., Xiao, S. Y. 2018. Mesozoic strike-slip movement of the Dunhua–Mishan Fault Zone in NE China: A response to oceanic plate subduction. Tectonophysics, 723: 201–222.
[8]Zhu G*, Liu C, Gu C C, Zhang S, Li Y J, Su N, Xiao S Y. 2018. Oceanic plate subduction history in the western Pacific Ocean: Constraint from late Mesozoic evolution of the Tan-Lu Fault Zone. Science China Earth Sciences, 61(4): 386-405.
[9] Gu, C. C., Zhu, G*., Li, Y. J., Su, N., Xiao, S. Y., Zhang, S., Liu, C.,.2018. Timing of deformation and location of the eastern Liaoyuan Terrane, NE China: Constraints on the final closure time of the Paleo-Asian Ocean. Gondwana Research, 60: 195-212.
[10]Zhang, S., Zhu, G*., Liu, C., Li, Y., Su, N., Xiao, S., & Gu, C. 2018. Strike-slip motion within the Yalu River Fault Zone, NE Asia: The development of a shear continental margin. Tectonics, 37, 1771-1796.
[11] Li, Y. J., Zhu, G*., Gu, C. C., Su, N., Xiao, S. Y., Zhang, S., Liu, C., Xie, C. L. 2018. Structural evolution of the Paleoproterozoic Trans-North China Orogen: Evidence from the Xiaoqinling region, central China. Precambrian Research, 316: 244-274.
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