姓名:孙习林

职称、职务：副教授

电子邮箱：sunxi-lin@163.com

通信地址：武汉市武昌区友谊大道368号威廉希尔官方网站

主要研究方向

沉积物物源、地貌演化、低温热年代学

教育背景

2013 - 2017，阿姆斯特丹自由大学， 理学，博士

2008 - 2011,中国地质大学（武汉），第四纪地质学， 硕士

2004 - 2008,中国地质大学（武汉），资源环境与城乡规划管理，学士

经历:

2020 - 2021，苏黎世联邦理工学院，博士后研究

2018 - 2020，中山大学 博士后研究

主要社会兼职

荣誉和获奖情况

承担（主持）的主要科研项目

1.国家自然科学基金面上项目(59万)：青藏高原东南缘新生代沉积物再循环约束对金沙江演化的启示（2022-2025），主持

2.主持国家自然科学基金青年基金项目(25万)：剑川盆地新生代沉积物碎屑矿物Ar-Ar定年对金沙江上游水系演化的启示（2019-2021），主持

3.主持高校基本科研业务费-青年教师培育项目（12万）:元谋盆地碎屑白云母年龄对雅砻江-大渡河演化的约束（2019-2021），主持

4.参与国家自然科学基金面上项目：江汉盆地宜昌冲积扇物源解析与区域地貌演化（2016-2020），参与

5.参与国家自然科学基金面上项目：长江上游水系拓展过程的地貌与碎屑锆石年龄双重约束研究

（2009-2012），参与

代表作（*通讯作者）

⑴Sun, X.L.,Tian, Y.T., Kuiper, K. F., Li, C. A., Zhang, Z., & Wijbrans, J. R. (2021). No Yangtze River prior to the late Miocene: Evidence from detrital muscovite and K‐feldspar⁴⁰Ar/³⁹Ar geochronology. Geophysical Research Letters, 48(5), e2020GL089903.

⑵Sun, X.L.; Kuiper, K.F.; Tian, Y.T.; Li, C.A.; Zhang, Z.J.; Gemignani, L.; Guo, R.J.; de Breij, V.H.L.; Wijbrans, J.R.⁴⁰Ar/³⁹Ar mica dating of late cenozoic sediments in se tibet: Implications for sediment recycling and drainage evolution.Journal of the Geological Society. 2020, 177, 843–854.

⑶Sun, X.L., Kuiper, K.F., Tian, Y.T., Li, C.A., Zhang, Z.J., Wijbrans, J.R., Comparison of Detrital Zircon U-Pb and Muscovite⁴⁰Ar/³⁹Ar Ages in the Yangtze Sediment: Implications for Provenance Studies.Minerals. 2020; 10(7):643.

⑷Sun, X.L., Kuiper, K.F., Tian, Y.T., Li, C.A., Gemignani, L., Zhang, Z.J., Wijbrans, J.R., 2020. Impact of hydraulic sorting and weathering on mica provenance studies: An example from the Yangtze River.Chemical Geology.2020; 532, 119359.

⑸Sun, X.L., Li, C.A., Kuiper, K., Zhang, Z.J., Gao, J.H., Wijbrans, J., 2016. Human impact on erosion patterns and sediment transport in the Yangtze River.Global and Planetary Change143,88-99.

⑹Sun, X.L., Li, C.A., Kuiper, K., Wang J.L., Pieter Vermeeschd., Zhang Z.J., Zhao J.X., Wijbrans, J., 2017. Detrital geochronology and geochemistry of the Jianghan Basin: implications for the Cenozoic evolution of the Yangtze River.Basin Research. (2017) 1–14, doi: 10.1111/bre.12268.

⑺Guo R.J,Sun X.L*, Li C.A*, Li Y.W, et al. Cenozoic evolution of the Yangtze River: Constraints from detrital zircon U-Pb ages[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2021, 579: 110586.

⑻Gemignani, L.,Sun, X.L.,van Gerve, T.D.,Braun, J., andWijbrans, J.R.A new detrital mica⁴⁰Ar/³⁹Ar dating approach for provenance and exhumation of the Eastern Alps.Tectonics,36, doi: 10.1002/ 2017TC004483.

⑼Zhang, Z.J., Daly, J.S., Li, C.A., Tyrrell, S.,Sun, X.L., Yan Y., 2017. Sedimentary provenance constraints on drainage evolution models for SE Tibet: evidence from detrital K-feldspar.Geophysical Research Letters,10.1002/2017GL073185.

⑽Sun, X.L., 2016. Human impact on erosion patterns and sediment transport in the Yangtze River.Geo.brief 5, 12-14.

⑾Zhang, Z.J., Tyrrell, S., Li, C.A., Daly, J.S.,Sun, X.L., Blowick, A., Lin, X., 2016. Provenance of detrital K-feldspar in Jianghan Basin sheds new light on the Pliocene − Pleistocene evolution of the Yangtze River.Geological Society of America Bulletin, B31445. 31441.

⑿Zhang, Z.J., Tyrrell, S., Li, C.A., Daly, J.S.,Sun, X.L., Li, Q.W., 2014. Pb isotope compositions of detrital K-feldspar grains in the upper-middle Yangtze River system: Implications for sediment provenance and drainage evolution.Geochemistry, Geophysics, Geosystems15, 2765-2779.

⒀Qi, M., Xiang, H., Zhong, Z. Q., Qiu, H. N., Wang, H.,Sun, X.L., & Xu, B. (2013).⁴⁰Ar/³⁹Ar geochronology constraints on the formation age of Myanmar jadeitite.Lithos, 162, 107-114.

⒁Gemignani, L., Kuiper, K.F., Wijbrans, J.R.,Sun, X.L, Santato, A., 2019. Improving the precision of single grain mica⁴⁰Ar/³⁹Ar-dating on smaller and younger muscovite grains: Application to provenance studies.Chemical Geology511, 100-111.