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个人简介

男,博士,特任副教授,1989年出生 ►2007年9月—2011年6月,中国地质大学(武汉)资源学院学习,获学士学位 ►2011年9月—2014年6月,中国地质大学(武汉)资源学院学习,获硕士学位 ►2014年9月—2019年2月,同济大学海洋与地球科学学院学习,获博士学位 ►2017年1月—2018月1月,荷兰乌特勒支大学地球科学学院学习,访问博士生 ►2019年5月—至今,中国地质大学(武汉)海洋学院任教,特任副教授 ☆科研项目 ★国家科技重大专项课题“南海北部深水区富生烃凹陷评价”子课题“南海西北部深水区裂后期沉积体系研究和海底扇评价”(2011-2014,项目编号:2011ZX05025-002-02,已结题,参加) ★中海油湛江分公司科研项目“乐东区水道成因演化及优质储层展布”(2013-2014,项目编号:CCL2013ZJFN0701,已结题,参加) ★国家自然科学基金面上项目“南海东部白垩-中新世构造演变及沉积响应”(2016-2019,项目编号:41576059,在研,参加) 联系方式 湖北省武汉市洪山区鲁磨路388号中国地质大学海洋学院(邮编:430074)

研究领域

目前主要从事海洋地质与沉积地球化学等方面的教学和科研工作 古地理重建 古河流演化 物源分析

近期论文

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国际学术论文(*通讯作者) [1] Cao, L., Jiang, T., Wang, Z., Zhang, Y. and Sun, H., 2015. Provenance of Upper Miocene sediments in the Yinggehai and Qiongdongnan basins, northwestern South China Sea: Evidence from REE, heavy minerals and zircon U–Pb ages. Marine Geology, 361: 136–146. [2] Jiang, T., Cao, L.*, Xie, X., Wang, Z., Li, X., Zhang, Y., Zhang, D. and Sun, H., 2015. Insights from heavy minerals and zircon U–Pb ages into the middle Miocene–Pliocene provenance evolution of the Yinggehai Basin, northwestern South China Sea. Sedimentary Geology, 327: 32–42. [3] Shao, L., Cao, L.*, Pang, X., Jiang, T., Qiao, P. and Zhao, M., 2016. Detrital zircon provenance of the Paleogene syn-rift sediments in the northern South China Sea. Geochemistry, Geophysics, Geosystems, 17: 255–269. [4] Cao, L.*, Shao, L., Qiao, P., Chen, S. and Wu, M., 2017. Geochemical evolution of Oligocene–Middle Miocene sediments in the deep-water area of the Pearl River Mouth Basin, northern South China Sea. Marine and Petroleum Geology, 80: 358–368. [5] Shao, L., Cao, L.*, Qiao, P., Zhang, X., Li, Q. and van Hinsbergen, D.J.J., 2017. Cretaceous–Eocene provenance connections between the Palawan Continental Terrane and the northern South China Sea margin. Earth and Planetary Science Letters, 477: 97–107. [6] Shao, L., Meng, A., Li, Q., Qiao, P., Cui, Y., Cao, L. and Chen, S., 2017. Detrital zircon ages and elemental characteristics of the Eocene sequence in IODP Hole U1435A: Implications for rifting and environmental changes before the opening of the South China Sea. Marine Geology, 394: 39–51. [7] Zhu, W., Xie, X., Wang, Z., Zhang, D., Zhang, C., Cao, L. and Shao, L., 2017. New insights on the origin of the basement of the Xisha Uplift, South China Sea. Science China Earth Sciences, 60: 1–9. [8] Cao, L., Shao, L., Qiao, P., Zhao, Z. and van Hinsbergen, D.J.J., 2018. Early Miocene birth of modern Pearl River recorded low-relief, high-elevation surface formation of SE Tibetan Plateau. Earth and Planetary Science Letters, 496: 120–131. [9] Zhang, G., Shao, L., Qiao, P., Cao, L.*, Pang, X., Zhao, Z., Xiang, X., Cui, Y. and Li, S., 2019. Cretaceous–Palaeogene sedimentary evolution of the South China Sea region: A preliminary synthesis. Geological Journal: 1–22. ★国际学术会议 [1] 2015/05, AAPG GTW-Tectonic Evolution and Sedimentation of South China Sea Region, Kota Kinabalu: Middle Miocene-Pliocene Provenance Evolution of the Yinggehai Basin, Northwestern South China Sea.(展板报告) [2] 2017/12, AGU Fall Meeting, New Orleans: No Separation of the Palawan Continental Terrane from the South China Margin during the Cretaceous-Eocene.(口头报告)

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