1.南海洋陆转换模式的洋壳岩石原位地球化学研究（22120210525），2021.11-2023.10，10万，同济大学自主原创基础研究项目，负责人；

2.南海扩张初期洋壳增生的岩石地球化学研究（IODP-U1500站）（41906051），2020.01-2022.12，27万，国家自然科学基金青年课题，负责人；

3.国际大洋钻探计划合作研究（20590780200），2020.10-2023.09，270万，上海市科技创新行动计划国际科技合作项目，参与；

4.南海南部巽他陆架沉积古环境演变（2018YFE0202402），2019.08-2022.07，210万，国家重点研发计划战略性国际科技创新合作重点专项课题，参与；

5.南海中新世洋中脊玄武岩的镁和铁同位素组成（MG20190301），2019.01-12，15万，海洋地质国家重点实验室自主课题，负责人；

6.南海洋中脊玄武岩成因研究（17YF1420300），2017-2020，20万，上海市青年科技英才扬帆计划，负责人；

7.南海西南次海盆中新世洋中脊玄武岩成因研究与构造意义（2017M621525），2017-2018，5万，中国博士后科学基金面上资助，负责人；

8.南海中新世火山碎屑岩的成因与源区特征（MG20160408），2016-2017，10万，海洋地质国家重点实验室自主课题，负责人；

9.东北新生代高镁安山岩的成因（41672049），2017-2020，80万，国家自然科学基金面上课题，参与；

10.南太平洋Louisville海山玄武岩的成因与源区特征（41372064），2014-2017，99万，国家自然科学基金面上课题，参与；

11.中国东部新生代玄武岩的成因-以苏皖地区玄武岩典型剖析（41202039），2013-2015，25万，国家自然科学基金青年课题，参与；

12.山东蓬莱新生代玄武岩的源区组成（41172060），2012-2015，74万，国家自然科学基金面上课题，参与。

(1)   Tian,J., Ma, Z., Lin, J., Xu, M., Yu, X., Le, B.M., Zhang, X., Zhang,F., Guo, L., 2023, Mantle heterogeneity caused by trapped water in theSouthwest Basin of the South China Sea, Nature Communications, 14:2710.

(2)   Li,Y., Yu, X., Liu, H., Huang, X., Yue, W., Lian, E., Yang, S.,2023, Tectonic and magmatic evolution of NE Cathaysia Block controls sedimentgeochemical heterogeneity of rivers in SE China, Catena, 223, 106910.

(3)   Yu,X., Liu, Z., Wu, J., An, Y.-J., Shi, J.-H., 2022, Ironisotopic variations in basalts from oceanic crust due to low-temperatureseawater alteration, Marine Geology, 454, 106949.

(4)   Yu,X., Liu, Z., Zeng, G., Cao, W., Meas, R., Hoang, L.V.,Sang, P.N., 2022, Mantle plume-stagnant slab interaction controls thegeneration of a mixed mantle source for continental intraplate basalts, Lithos,426-427, 106795.

(5)   Lyu,X., Liu, Z., Wu, Q., Colin, C., Yu, X., Liu, C., Li, Q., 2022, Quantifyingiron oxide mineral contents in Miocene Oceanic Red Beds for the deep-seaoxidation evolution in the South China Sea, Frontiers in Earth Science,10:875292.

(6)   Wu,J., Liu, Z., Yu, X., 2021.Plagioclase-regulated hydrothermal alteration of basaltic rocks withimplications for the South China Sea rifting, Chemical Geology, 585, 120569.

(7)   Zeng,G., Chen, L.-H., Hofmann, A.W., Wang, X.-J., Liu, J.-Q., Yu, X., Xie, L.-W., 2021, Nephelinites in eastern Chinaoriginating from the mantle transition zone, Chemical Geology, 576, 120276.

(8)   Liu,J.-Q., Erdmann, S., Chen, L.-H., Zhang, H.-L., Wu, B., Zeng, G., Wang, X.-J.,Lei, Z.-L., Yu, X., 2021.Petrological evidence for magma recharge and mixing beneath the Ma’anshanmonogenetic volcano of Xiaogulihe in Northeast China, Lithos, 382-383, 105928.

(9)   Wu,L., Wilson, D.J., Wang, R., Passchier, S., Krijgsman, W., Yu, X., Wen, T., Xiao, W., Liu, Z., 2020, Late Quaternarydynamics of the Lambert Glacier-Amery Ice Shelf system, East Antarctica, Quaternary Science Reviews,10.1016/j.quascirev. 2020.106738.

(10) 俞恂, 陈立辉, 2020, 弧后盆地玄武岩的成分变化及其成因, 岩石学报,36, 1953-1972.

(11) Yu, X.,Liu, Z., 2020, Non-mantle-plume process caused the initial spreading of theSouth China Sea, Scientific Reports,10:8500, 10.1038/s41598-020-65174-y.

(12) Li,Y., Yue, W., Yu, X., Huang,X., Yao, Z., Song, J., Shan, X., Yu, X., Yang, S., 2020, Tectonic evolution ofthe West Bogeda: Evidences from zircon U-Pb geochronology and geochemistryproxies, NW China, minerals, 10,341, 10.3390/min10040341.

(13) He,D., Lee, C.-T., Yu, X.,Farner, M., 2019, Ge/Si partitioning in igneous systems: Constraints from laserablation ICP-MS measurements on natural samples, Geochemistry, Geophysics, Geosystems, 20. 10.1029/2019GC008514.

(14) Yu, X.,Zeng, G., Chen, L.-H., Wang, X.-J., Liu, J.-Q., Xie, L.-W., Yang, T., 2019, Evidencefor rutile-bearing eclogite in the mantle sources of the Cenozoic Zhejiangbasalts, eastern China, Lithos,324-325, 152-164.

(15) Yu, X.,Zeng, G., Chen, L.-H., Hu, S.-L., Yu, Z.-Q., 2018, Magma-magma interaction inthe mantle recorded by megacrysts from Cenozoic basalts in eastern China, International Geology Review,doi:10.1080/00206814.2018.1446190.

(16) Zeng,G., Chen, L.-H., Yu, X., Liu,J.-Q., Xu, X.-S., Erdmann, S., 2017, Magma-magma interaction in the mantlebeneath eastern China, Journal ofGeophysical Research: Solid Earth, doi: 10.1002/2017JB014023.

(17) Yu, X.,Chen, L.-H., Zeng, G., 2017, Magmatic recharge buffers the isotopiccompositions against crustal contamination in formation of continental floodbasalts, Lithos, 284-285, 1-10.

(18) Liu,J.-Q., Chen, L.-H., Wang, X.-J., Zhong, Y., Yu, X., Zeng, G., Erdmann, S., 2017, The role of melt-rockinteraction in the formation of Quaternary high-MgO potassic basalt from theGreater Khingan Range, northeast China, Journalof Geophysical Research: Solid Earth, doi: 10.1002/2016JB013605.

(19) Yu, X.,Lee, C.-T., 2016, Critical porosity of melt segregation during crustal melting:constraints from zonation of peritectic garnets in a dacite volcano, Earth and Planetary Science Letters, doi:10.1016/j.epsl.2016.05.025.

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(24) 陈立辉, 曾罡, 胡森林, 俞恂, 陈霞玉, 2012, 地壳再循环与大陆碱性玄武岩的成因: 以山东新生代碱性玄武岩为例, 高校地质学报, 18: 16-27.

主讲和参与教学的课程：

《岩石学》、《自然灾害与宜居地球》、《蓝色海洋中的地球奥秘》(本科生)

《元素地球化学》、《大洋板块》、《Marine Geology》(硕士研究生)

《同位素地球化学》、《地球化学原理和应用》(博士研究生)