个人简介
一、基本情况
男，地质学博士，讲师。
二、教育背景
2006-2010年南京大学地球科学与工程学院本科，获地质学学士学位；2010-2015年南京 大学地球科学与工程学院硕博连读，获地质学博士学位；期间于2014年10-12月在澳大利亚 Macquarie University交流访问。
三、工作经历
2015年9月起在桂林理工大学地球科学学院任教至今。
近期论文
查看导师最新文章
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1. Liu Lei, Xu Xisheng, Xia Yan, 2016. Asynchronizing paleo-Pacific slab rollback beneath SE China: Insights from the episodic Late Mesozoic volcanism. Gondwana Research 37: 397-407.
2. Liu Lei, Xu Xisheng, Xia Yan, 2014. Cretaceous Pacific plate movement beneath SE China: Evidence from episodic volcanism and related intrusions. Tectonophysics 614: 170-184.
3. Liu Lei, Xu Xisheng, Zou Haibo, 2012. Episodic eruptions of the Late Mesozoic volcanic sequences in southeastern Zhejiang, SE China: Petrogenesis and implications for the geodynamics of paleo-Pacific subduction. Lithos 154: 166-180.
4. 刘磊, 徐夕生, 2011. 大别造山带天柱山中酸性岩起源及地质意义. 高校地质学报,
17: 136-150.
5. Xia Yan, Xu Xisheng, Liu Lei, 2016. Transition from adakitic to bimodal magmatism induced by the paleo-Pacific plate subduction and slab rollback beneath SE China: Evidence from petrogenesis and tectonic setting of the dike swarms. Lithos 244: 182-204.
6. Zhang Xisong, Xu Xisheng, Xia Yan, Liu Lei, 2016. Early Paleozoic intracontinental orogeny and post-orogenic extension in the South China Block: Insights from volcanic rocks. Journal of Asian Earth Sciences, in press.
7. Xia Yan, Xu Xisheng, Zhao Guochun, Liu Lei, 2015. Neoproterozoic active continental margin of the Cathaysia block:Evidence from geochronology, geochemistry, and Nd–Hf isotopes ofigneous complexes. Precambrian Research 269: 195-216.
8. Xia Yan, Xu Xisheng, Zou Haibo, Liu Lei, 2014. Early Paleozoic crust–mantle interaction and lithosphere delamination in South China Block: Evidence from geochronology, geochemistry, and Sr–Nd–Hf isotopes of granites. Lithos 184-187: 416-435.
9. Xu Xisheng, Suzuki Kazuhiro, Liu Lei, Wang Dezi, 2010. Petrogenesis and tectonic implications of Late Mesozoic granites in the NE Yangtze Block, China: further insights from the Jiuhuashan–Qingyang complex. Geological Magazine 147: 219-232.
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