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幔游课题组

"Rocking Mantle" Group





曾罡  副教授
江西宜春人,岩石学博士,副教授,硕士生导师。
教育经历

2006.09~2011.06   南京大学地球科学与工程学院,获岩石学博士学位

2002.09~2006.06   南京大学地球科学系,获地球化学学士学位

工作经历

2015.07~               南京大学地球科学与工程学院,副教授

2011.07~2015.06  南京大学地球科学与工程学院,专职科研

学术任职

中国地质学会岩石专业委员会委员

中国矿物岩石地球化学学会岩浆岩专业委员会委员 中国矿物岩石地球化学学会火山及地球内部化学专业委员会委员
研究方向

火成岩岩石学与地幔地球化学

重点关注地幔物质组成、壳幔相互作用机制及幔源岩浆作用过程(如玄武岩成因、幔源岩浆的深部演化过程等)。近年来,以中国东部玄武岩及其蕴含的橄榄石斑晶、熔体包裹体等为主要研究对象,通过元素地球化学、Sr-Nd-Pb-Hf-Mg-Fe同位素和橄榄石矿物化学等联合示踪的方法,深入探讨了玄武岩的地幔源区岩性特征与深部过程。尤其关注在地球物质的深部循环过程中,碳、氟、氯等挥发分对物质循环、元素配分、金属迁移-富集等过程的潜在影响。

个人荣誉
2022-2026:江苏省“333高层次人才培养工程”第三层次
获2016年度江苏省科学技术奖一等奖(排名第3)

获“第19届侯德封矿物岩石地球化学青年科学家奖”

项目与经费

2024–2026   国家自然科学基金优秀青年基金(主持)   地幔中氟-氯的熔体包裹体示踪”

2022–2027   国家重点研发计划项目(骨干)   “东亚陆缘古太平洋板块俯冲的构造-岩浆活动及浅部效应” 2022–2026   国家自然科学基金重点基金(骨干)   “从大陆火山岩视角了解深部地幔化学储库的属性” 2017–2020   国家自然科学基金面上基金(主持)   “中国东南部新生代小规模溢流玄武岩成因研究” 2015–2019   国家自然科学基金重点基金(骨干)   “华夏地块古生代-早中生代花岗岩及相关岩石成因与陆
                     壳再造”
2014–2017   国家自然科学基金面上基金(骨干)   “南太平洋Louisville海山玄武岩的成因与源区特征” 2013–2015   国家自然科学基金青年基金(主持)   “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”
电子邮箱
论文发表

51. Yu, H.-Y., Zhang, H.-L., ZhangX.-Y., Jiang J.-X., Liang, Y.-K., Chen, L.-H., Zeng, G.*, 2024. Characteristicsand potential origin of carbonate components in the Louisville seamounts. J.Earth Sci., accepted.

50. Zhang, H.-L., Zeng, G.*,Chen, L.-H., Liu, J.-Q., Yu, J.-H., Xu, X.-S., 2024. Evaluation of CO2concentration in a carbonated eclogite mantle source: A new attempt based onthe compositions of olivine phenocrysts. Lithos, 107669.

49. Dai, C.-C., Wang, X.-J.*, Chen, L.-H., Hanyu, T., Zhang, X.-Y., Zeng,G., Xie, L.-W., 2024. Iron isotopic compositions of HIMU Ocean islandbasalts: Implications for the mantle source lithology. Lithos 470-471,107531.

48. Wang, X.-J.*, Chen, L.-H., Hanyu, T., Zhou, Z.-B., Liu, J.-Q., Zeng,G., Zou, Z.-Q., Bai, J.-H., 2024. Calcium isotopic variability in hotspotlavas controlled by partial melting and source lithological heterogeneity.Chem. Geol. 644, 121857.

47. 曾罡*, 张慧丽, 刘建强, 陈立辉. 2023. 海南岛玄武岩橄榄石斑晶中熔体包裹体示踪氟、氯深部循环. 矿物岩石地球化学通报, 42, 20232.

46. Zhang, H.-L., Zeng, G.*,Liu, J.-Q., Chen, L.-H., Yu, J.-H., Wu, B., Wang, X.-J., Xu, X.-S., Liu, X.-W.,2023. Carbonated eclogitic component beneath eastern China revealed by olivinephenocrysts in nephelinites. Chem. Geol. 640, 121744.

45. 郑志翀, 曾罡*, 张慧丽, 刘建强, 陈立辉, 周中彪. 2023. 中国东北鸡西新生代玄武岩源区岩性制约. 高校地质学报, 29: 186-200.

44. 熊巧, 曾罡, 郑志翀, 张慧丽, 周中彪, 王小均, 刘建强, 陈立辉*. 2023. 东北牡丹江地区古近纪高镁安山岩的发现及其岩石学特征. 高校地质学报, 29: 161-173.

43. Shi, J. H., Zeng G.*,L. H. Chen, X. J. Wang, J. Q. Liu, L. W. Xie, Y. H. Yang, and H. L. Zhang.2023. Lithology of EM1 Reservoir Revealed by Fe Isotopes of ContinentalPotassic Basalts. J. Geophys. Res.: Solid Earth, 128(1).https://doi.org/10.1029/2022jb025133.

42. Shen,J.*, Zuo, Z., He, Y., Li, S., Huang, J., Zeng, G., Qin,L.,2023. Chromium isotope system of intraplate basaltic lavas: Implication forrecycling materials into mantle. Lithos 454-455, 107264.

41. Wen,D.-J., Hu, X.*, Chapman, T., Zeng, G., Ma, A.-L., Wang, R.-Q.,2023. Late Cretaceous bimodal volcanic rocks in Shuanghu induced bylithospheric delamination beneath the Southern Qiangtang, Tibet. Lithos460-461, 107368.

40. 陈立辉, 曾罡, 刘建强, 王小均, 张超. 2022. 从大陆火山岩视角了解深部地幔化学储库的属性. 岩石学报, 38(12): 3703-3711. doi: 10.18654/1000-0569/2022.12.10.

39. Liu, J.Q.*, Chen, L.H., Wang,X.J., Zhang, H.L., Zeng, G., Saskia, E., Zhang, L., Ren, Z.Y. 2022.Olivine and melt inclusion chemical constraints on the nature and origin of thecommon mantle component beneath eastern Asia.Contributions to Mineralogy and Petrology, 177. https://doi.org/10.1007/s00410-022-01981-y.

38. Sheng S. Z., Wang S. J., Yang X.M., Chen L. H., Zeng G., Xiao Y., Shen J., Dong X. H & Lv Y.W. (2022) Sulfide dissolution on the nickel isotopic composition of basalticrocks. Journal of Geophysical Research: Solid Earth. https://doi.org/10.1029/2022JB024555.

37. Liu, J.-Q.*, Chen, L.-H.,Wang, X.-J., Zhang,X.-Y., Zeng, G., Saskia, E., Murphy, D.-T.,Collerson, K.-D., Komiya,T., Krmicek, L.(2022) Magnesium and zinc isotopic evidence forthe involvement of recycled carbonates in thepetrogenesis of Gaussberglamproites,Antarctica. Chemical Geology.https://doi.org/10.1016/j.chemgeo.2022.121067.

36. Zhang, H.-L., Zeng, G.*,Zhang, C., Zhang, W.-L., Chen, L.-H., Yu, J.-H., 2022. Electron ProbeMicroanalysis measurement of F-Cl-Nb-P for Geological Glasses. Geostandards andGeoanalytical Research, 46, 851-864. https://doi.org/10.1111/ggr.12454.

35. Zhang, X.Y., Chen, L.H., Wang,X.J., Hanyu, T., Hofmann, A.W., Komiya, T., Nakamura, K., Kato, Y., Zeng,G., Gou, W.X., Li, W.Q., 2022. Zinc isotopic evidence for recycledcarbonate in the deep mantle. Nature Communications, 13, 6085.

34. Shi, J.-H., Zeng, G.*,Chen, L.-H., Hanyu, T., Wang, X.-J., Zhong, Y., Xie, L.-W., Xie, W.-L., 2022.An eclogitic component in the Pitcairn mantle plume: evidence from olivinecompositions and Fe isotopes of basalts. Geochimica et CosmochimicaActa, 318, 415-427.   https://doi.org/10.1016/j.gca.2021.12.017.

33. Zeng, G.*,   Chen,L.-H.*, Hofmann, A.W.*, Wang, X.-J., Liu, J.-Q., Yu, X., Xie, L.-W., 2021.Nephelinites in eastern China originating from the mantle transition zone.Chem. Geol., https://doi.org/10.1016/j.chemgeo.2021.120276.

32. Liu J. Q.*, Erdmann, S., ChenL. H., Zhang H.L., Wu B., Zeng G., WangX. J., Lei Z. L., Yu X. (2021). Petrological evidence for magma rechargeand mixing beneath the Ma'anshan monogenetic volcano of Xiaogulihe in NortheastChina. Lithos, 382-383, https://doi.org/10.1016/j.lithos.2020.105928.

31. WangX. J., Chen L. H.,Hanyu T., Zhong Y., Shi J. H., Liu X. W., Kawabata H., Zeng G., XieL. W.(2021)Magnesium isotopicfractionation during basalt differentiation as recorded by evolvedmagmas. Earth andPlanetary Science Letters, 565,https://doi.org/10.1016/j.epsl.2021.116954.

30. Jiang, D.-S., Xu,X.-S., Wang, X.-J., Zeng, G., Chen, A.-X., Huang, B., Huang, F.,2021. Geochemical evidence for the Paleo-Pacific plate subduction at ~125 Ma inEastern China. Lithos 398-399.

29. Zhu-LiangLei, Zeng, G.*, Jian-Qiang Liu*, Xiao-Jun Wang, Li-Hui Chen, Xiao-YuZhang, Jin-Hua Shi (2021), Melt-lithosphere interaction controlledcompositional variations in mafic dikes from Fujian province, southeasternChina. Journal of Earth Science, 32, 1445-1453, https://doi.org/10.1007/s12583-020-1358-y.

28. 何叶, 陈立辉, 曾罡, 王小均 (2020), 浙江建德新生代玄武岩源区特征及其成因, 高校地质学报, 26, 241-254.

27. 雷祝梁, 曾罡*, 王小均, 陈立辉 (2019), 中国东南部晚中生代基性岩脉地幔源区的岩性演化历史, 地球科学, 44, 1159-1168.

26. Xun Yu, Zeng, G.*, Li-Hui Chen, Xiao-Jun Wang, Jian-Qiang Liu, Lie-Wen Xie,Tao Yang (2019), Evidence for rutile-bearing eclogite in the mantlesource of the Cenozoic Zhejiang basalts, eastern China, Lithos, 324-325,152-164, doi: 10.1016/j.lithos.2018.11.003.

25. Xun Yu, Zeng G.*, Li-HuiChen, Sen-Lin Hu & Zhi-Qiang Yu (2019): Magma–magma interaction in themantle recorded by megacrysts from Cenozoic basalts in eastern China,International Geology Review, 61, 675-691, doi:10.1080/00206814.2018.1446190.

24. Y. He, L.-H. Chen, J.-H. Shi, Zeng, G.,X.-J. Wang, X.-Q. Xue, Y. Zhong,S. Erdmann & L.-W. Xie (2019). Light Mg isotopic compositionin the mantle beyond the Big Mantle Wedge beneath eastern Asia. Journal ofGeophysical Research: Solid Earth, 124, 8043-8056,   doi:10.1029/2018jb016857.

23. 薛笑秋, 陈立辉, 刘建强, 何叶, 王小均, 曾罡, 钟源 (2019). 中国东北软流圈地幔中的原始橄榄岩质地幔:来自大兴安岭地区新生代玄武岩的地球化学证据. 地球科学, 44, 1143-1158.

22. Wang, Z.-Z., Liu, S.-A., Chen, L.-H., Li,S.-G.& Zeng, G.   (2018), Compositional transition innatural alkaline lavas through silica-undersaturated melt–lithosphereinteraction. Geology, 46, 771-774, doi: 10.1130/g45145.1.

21. 曾罡*, 郑丽波, 陈立辉, 刘建强, 张欢, 张甬江, 施金华 (2017), 南海洋脊抽吸作用对其周边新生代玄武质岩浆活动的影响, 高校地质学报, 23, 373-382.

20. Xu, W., X. Xu*, and ZengG. (2017), Crustal contamination versus an enriched mantle source forintracontinental mafic rocks: Insights from early Paleozoic mafic rocks of theSouth China Block, Lithos, 286, 388-395, doi: 10.1016/j.lithos.2017.06.023.

19. Zeng G., L.-H. Chen*,X. Yu, J.-Q. Liu, X.-S. Xu, and S. Erdmann (2017), Magma-magma interaction inthe mantle beneath eastern China, J. Geophys. Res.: Solid Earth, 122, doi:10.1002/2017jb014023.

18. Yu, X., Chen L.-H.*,and Zeng G. (2017), Magmatic recharge buffers the isotopiccompositions against crustal contamination in formation of continental floodbasalts, Lithos, 284-285, 1-10, doi: 10.1016/j.lithos.2017.03.027.

17. Zhong, Y., L.-H. Chen*, X.-J.Wang, G.-L. Zhang, L.-W. Xie, and Zeng, G. (2017), Magnesiumisotopic variation of oceanic island basalts generated by partial melting andcrustal recycling, Earth Planet. Sci. Lett., 463, 127-135.

16. Liu, J.-Q., Chen L.-H.*, Wang X.-J.,Zhong Y., Yu X., and Zeng G.(2017), The role of melt-rock interaction in the formation ofQuaternary high-MgO potassic basalt from the Greater Khingan Range, NortheastChina. J. Geophys. Res. Solid Earth, 122, doi: 10.1002/2016JB013605.

15. Chu, Z.*, Y. Yan, Zeng G.,W. Tian, C. Li, Y. Yang, and J. Guo (2017), Petrogenesis of Cenozoic basalts incentral-eastern China: Constraints from Re-Os and PGE geochemistry, Lithos,278-281, 72-83.

14. 林蔚涵, 刘建强, 陈立辉*, 刘建强, 王小均, 钟源, 曾罡 (2017), 大兴安岭新生代高镁安山岩的确认. 高校地质学报, 23, 16-25.

13. Zeng G.*, Z.-Y. He, Z. Li,X.-S. Xu, and L.-H. Chen (2016), Geodynamics of paleo-Pacific plate subductionconstrained by the source lithologies of Late Mesozoic basalts in southeasternChina, Geophys. Res. Lett., 43, 10189-10197, doi:10.1002/2016GL070346.

12. Zeng G.*, Huang X.-W., ZhouM.-F., Chen L.-H., Xu X.-S. (2016), Using chalcophile elements to constraincrustal contamination and xenolith-magma interaction in Cenozoic basalts ofeastern China, Lithos 258-259: 163-172.

11. Liu, J.-Q., Chen L.-H.*, ZengG., Wang X.-J., Zhong Y., and Yu X. (2016), Lithospheric thicknesscontrolled compositional variations in potassic basalts of Northeast China bymelt-rock interactions, Geophys. Res. Lett., 43, doi:10.1002/2016GL068332.

10. Yu, X., L.-H. Chen*, and ZengG.(2015), Growing magma chambers control the distribution of small-scaleflood basalts, Scientific Reports, 5, doi: 10.1038/srep16824.‍

9. 冒福根, 陈立辉*, 杨怀仁, 刘建强, 曾罡 (2015), 五大连池钾质火山岩中辉石斑晶的反环带结构研究及其对岩浆演化的约束. 高校地质学报, 21, 507-522. ‍

8. Yu, X.*, C.-T. A. Lee, L.-H. Chen,and Zeng G. (2015), Magmatic recharge incontinental flood basalts: Insights from the Chifeng igneous province in InnerMongolia, Geochem. Geophys. Geosyst., 16, 2082-2096.

7. 陈霞玉, 陈立辉*, 陈旸, 曾罡, 刘建强 (2014), 中国中东部地区新生代玄武岩的分布规律与面积汇总. 高校地质学报, 20, 507-519.

6. Zeng G.*, L.-H. Chen, S.-L.Hu, X.-S. Xu, and L.-F. Yang (2013), Genesis of Cenozoic low-Ca alkalinebasalts in the Nanjing basaltic field, eastern China: The case for mantlexenolith-magma interaction, Geochem. Geophys. Geosyst., 14, 1660-1677, doi:10.1002/ggge.20127.

5. 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.

4. Zeng G., L. H. Chen*, A. W.Hofmann, S. Y. Jiang, and X. S. Xu (2011), Crust recycling in the sources oftwo parallel volcanic chains in Shandong, North China, Earth Planet. Sci.Lett., 302, 359-368.

3. Zeng G., L. H. Chen*, X. S.Xu, S. Y. Jiang, and A. W. Hofmann (2010), Carbonated mantle sources forCenozoic intra-plate alkaline basalts in Shandong, North China, Chem. Geol.,273, 35-45.

2. Chen, L. H.*, Zeng G.,S. Y. Jiang, A. W. Hofmann, and X. S. Xu (2009), Sources of Anfengshan basalts:Subducted lower crust in the Sulu UHP belt, China, Earth Planet. Sci. Lett.,286, 426-435.

1. 罗丹, 陈立辉*, 曾罡 (2009), 陆内强碱性火山岩的成因:以山东无棣大山霞石岩为例. 岩石学报 25, 311-319.