· 学习经历

吉林大学, 地质学理学学士学位，中国长春，2012.06
吉林大学, 构造地质学理学博士学位，中国长春，2017.06

· 工作简历

2017.07-2019.09，中国海洋大学, 海洋科学博士后流动站博士后，中国青岛
2019.09-至今，中国海洋大学, 海底科学与探测技术教育部重点实验室副教授，中国青岛

· 承担的重大重点项目

1.国家自然科学基金青年基金项目，“青藏高原八宿地区寒武纪片麻状花岗岩：对冈瓦纳大陆北缘早古生代构造演化的制约”（41802232，2019-2021），项目负责人。
2.中国博士后科学基金面上项目，“青藏高原中部尼则地区晚白垩世构造岩浆事件”（2017M622273，2017-2019），项目负责人。
3.中国博士后科学基金“博士后创新人才支持计划”项目，“藏北羌塘中部奥陶系海相地层的沉积环境及成因机制探讨”（BX201700216，2017-2019），项目负责人。

· 学科方向

特提斯洋构造演化，岩石大地构造

· 应用研究

运用多学科技术手段对青藏高原内各时期特提斯洋演化记录进行详细的岩石学、年代学、地球化学、沉积演化序列以及构造解析等工作。针对特提斯洋演化历程与地球动力系统和岩石圈深浅耦合机制等热点问题，取得一系列研究成果。

· 近期研究兴趣

（1）洋陆过渡带岩浆-沉积-构造作用时空耦合与动力学机制
（2）印度洋扩张与青藏高原隆升耦合机制

[1]Liu, Y.M., Wang, Y.H., Li, S.Z., Santosh, M., Guo, R.H., Yu, S.Y., 2020. Neoproterozoic Amdo and Jiayuqiao microblocks in the Tibetan Plateau: Implications for Rodinia reconstruction. Geological Society of America Bulletin, DOI:10.1130/B35632.1
[2]Liu, Y.M., Li, S.Z., Xie, C.M., Santosh, M., Liu, Y.J., Dong, Y.C., Wang, B., Guo, R.H., Cao, X.Z., 2020. Subduction–collision and exhumation of eclogites in the Lhasa terrane, Tibet Plateau. Gondwana Research, https://doi.org/10.1016/j.gr.2020.01.019
[3] Liu, Y.M., Li, S.Z., Santosh, M., Cao, H.H., Yu, S.Y., Wang, Y.H., Guo, R.H., Xu, L.S., Zhou, J., Zhou, Z.Z., 2020. The passive margin of northern Gondwana during Early Paleozoic: Evidence from the central Tibet Plateau. Gondwana Research, 78, 126-140.
[4] Liu, Y.M., Li, S.Z., Santosh, M., Cao, H.H., Yu, S.Y., Wang, Y.H., Zhou, J., Zhou, Z.Z., 2019. The generation and reworking of continental crust during early Paleozoic in Gondwanan affinity terranes from the Tibet Plateau. Earth–Science Reviews, 190, 486–497.
[5] Liu, Y.M., Xie, C.M., Li, C., Li, S.Z., Santosh M, Wang, M., Fan, J.J., 2019. Breakup of the northern margin of Gondwana through lithospheric delamination: Evidence from the Tibetan Plateau. Geological Society of America Bulletin, 131, 675–697.
[6] Liu, Y.M., Wang, M., Li, C., Li, S.Z., Xie, C.M., Zeng, X.W., Liu, J.H., 2019. Late Cretaceous tectono-magmatic activity in the Nize region, central Tibet: evidence for lithospheric delamination beneath the Qiangtang–Lhasa collision zone. International Geology Review, 61, 562–583.
[7] Liu, Y.M., Li, C., Xie, C.M., Fan, J.J., Wu, H., 2017. Detrital zircon U–Pb ages and Hf isotopic composition of the Ordovician Duguer quartz schist, central Tibetan Plateau: constraints on tectonic affinity and sedimentary source regions. Geological Magazine, 154, 558–570.
[8] Liu, Y.M., Li, C., Xie, C.M., Wang, M.,Fan, J.J., 2017. Geochronology of the Duguer range metamorphic rocks, Central Tibet: implications for thechanging tectonic setting of the South Qiangtang subterrane. International Geology Review, 59, 29–44.
[9] Liu, Y.M., Li, C., Xie, C.M., Li X., 2017. Structure and development of the Changliangshan ductile shear zone, North Tibet: implications for the initial closure of the Paleo-Tethys Ocean at central Qiangtang. International Journal of Earth Sciences, 106, 2945–2962.
[10] Liu, Y.M., Li, C., Wang, M.,Xie, C.M., Chen, H.Q., Li, Y.B., Fan, J.J., Li, X.K., Sun, Z.M., 2017. Cretaceous structures in the Duolong region of central Tibet: Evidence for an accretionary wedge and closure of the Bangong–Nujiang Neo-Tethys Ocean. Gondwana Research, 48, 110–123.
[11] Liu, Y.M., Li, C., Xie, C.M., Fan, J.J., Wu H., Jiang, Q.Y., Li X., 2016. Cambrian granitic gneiss within the Central Qiangtang terrane, Tibetan Plateau: implications for the early Paleozoic tectonic evolution of the Gondwanan margin. International Geology Review, 58, 1043–1063.
[12]刘一鸣，李三忠，于胜尧，曹现志，周洁，李阳，王誉桦，徐林山，郭润华，周在征，2019. 青藏高原班公湖-怒江缝合带及周缘燕山期微地块聚合与增生造山过程 大地构造与成矿学，43（4）：824-838．
[13]刘一鸣，李才，李三忠，解超明，王明，范建军，刘金恒，郭润华，2018．青藏高原羌南-保山板块都古尔地区早白垩世变质辉长岩：对班公湖-怒江洋俯冲闭合的制约．地质通报，37（8）：1450-1463．
[14]刘一鸣，李才，王明，吴彦旺，解超明，胡培远，2014．藏北羌塘盆地望湖岭流纹岩地球化学特征及其构造意义．地质通报，33（11）：1769-1767．