科研人员

Scientist

基本信息

姓名:王玺
性别:女
出生年月:1987年4月
祖籍:山东济南
联系地址:山东省青岛市崂山区松岭路238号,邮编266100
电子邮箱:wangx@ouc.edu.cn

主页访问量:2398

简历

· 教育经历

2011.09-2014.12,南京大学,构造地质学,博士学位
2008.09-2011.06,中国石油大学(华东),构造地质学,硕士学位
2004.09-2008.06,中国石油大学(华东),资源勘查专业,学士学位

· 工作简历

2022.09至今:中国海洋大学,副教授
2020.01-2022.09:南京大学,特任助理研究员
2016.12-2019.12:中国石油大学(华东),讲师
2015.01-2016.12:南京大学,博士后

· 学术兼职

《Precambrian Research》《Global and Planetary Change》《中国科学:地球科学》《Journal of Asian Earth Sciences》《Journal of the Geological Society》等期刊审稿人

· 主持和参与的重要科研项目

(1) 国家自然科学基金-面上项目,阿拉善地块晚太古代岩浆作用与陆壳生长及其构造机制 (42472258, 2025.01-2028.12), 50万元, 主持, 在研;
(2) 山东省自然科学基金-省优青项目,早前寒武纪微陆块增生与聚散 (ZR2023YQ036, 2024.01-2026.12), 50万元, 主持, 在研;
(3) 国家自然科学基金-面上项目,华北中部新太古代-古元古代镁铁质火成岩地幔源区性质随时间变化的地球化学研究 (42072218, 2021.01-2024.12), 60万元, 主持, 在研;
(4) 国家自然科学基金-青年项目, 华北中部吕梁地区新太古代构造-岩浆作用与地壳演化 (41702198, 2018.01-2020.12), 23万元, 主持, 结题;
(5) 山东省自然科学基金-博士基金, 山西吕梁地区新太古代-早古元古代岩浆作用与构造意义 (ZR2017BD008, 2017.07-2019.07), 7万元, 主持, 结题;
(6) 中国博士后科学基金面上资助项目, 华北中部吕梁杂岩野鸡山群沉积时代与构造背景探讨 (2016M591816, 2016.03-2017.03), 5万元, 主持, 结题;
(7) 国家自然科学基金-重大研究计划, 基于三千米科学钻孔岩芯的川西甲基卡花岗伟晶岩型锂矿床成因与成矿构造背景探讨 (92162211, 2022.01-2025.12), 330万元, 参与, 在研;
(8) 中国石油大学(华东)自主创新科研计划项目,“华北中部吕梁地区新太古代岩浆作用、地壳演化与构造意义 (17CX02001A, 2017.01-2019.12), 10万元, 主持, 结题;
(9) 南京大学国家自然科学基金培育项目, 华北吕梁地区野鸡山群沉积时代约束与构造背景探讨 (2016.03-2016.12), 5万元, 主持, 结题;
(10) 国家科技重大专项 “煤层气预测与多学科综合评价技术——煤层构造演化及煤层气富集规律研究 (2011ZX05035-005-001, 2011.01-2015.12), 560万元, 项目骨干, 结题。

主要学术领域

· 学科方向

岩石大地构造,前寒武纪地质学,岩浆岩地球化学

· 近期研究兴趣

早期地球演化,包括:太古宙大陆地壳的形成与演化,板块构造启动与早期板块构造运行特点,以及早期微陆块在超大陆旋回中的聚散过程等。

主要论文与论著目录

第一作者/通讯作者文章:
(1) Wang X*., Ge R.F., Zheng Y.-F., Zhu W.B., Li S.Z., Tian R.S., Wang Y., Rong Y.W., 2024. Successful subduction of oceanic plate after failed attempts in the Late Archean: Petrological and geochemical constraints. Earth and Planetary Science Letters 644: 118944.
(2) Wang X*., 2023. Crustal growth and reworking at Archean plate margins. Science China: Earth Sciences 66: 2977-2982.
(3) Wang X*., Zhu W.B*., Zheng Y.-F., 2022. Geochemical constraints on the nature of Late Archean basaltic-andesitic magmatism in the North China Craton. Earth-Science Reviews 230, 104065.
(4) Wang X*., Zhu W.B*., Zheng Y.-F., Ge R.F., 2022. Tectonic switch from a lithospheric rift to an active continental margin in the Paleoproterozoic: evidence from low δ18O granites from the Trans-North China Orogen in the North China Craton. Precambrian Research 377, 106672.
(5) Wang X*., Liu Y., Cao J., Liu Y.D., Luo B., Wu K.Y., Shi Z., Kang H.B., 2021. Controls of deep-seated faults and folds and their effects on hydrocarbon fluid migration and accumulation in the sedimentary basin: a case study from the northwestern Sichuan Basin of China. Geofluids 5371021.
(6) Wang X*., Zheng Y.-F., Zhu W.B., 2019. Geochemical evidence for reworking of the juvenile crust in the Neoarchean for felsic magmatism in the Yunzhongshan area, the North China Craton. Precambrian Research 335, 105493.
(7) Wang X*., Zheng Y.-F., Zhu W.B., 2019. Geochemical constraints on the origin of Neoarchean magmatic rocks in the Lüliang Complex, North China Craton: tectonic implications. Precambrian Research 327, 212-231.
(8) Wang X*., Zhu W.B., Liu Y., Luo M., Ge R.F., Zhang H., Ren X.M., Cui X., 2017. Revisiting the Yejishan Group of the Lüliang Complex, North China: Implications for a Paleoproterozoic active continental marginal basin in the Trans-North China Orogen. Precambrian Research 292: 93-114.
(9) Wang X., Zhu W.B*., Luo M., Ren X.M., Cui X., 2014. Approximately 1.78 Ga mafic dykes in the Lüliang Complex, North China Craton: Zircon ages and Lu-Hf isotopes, geochemistry, and implications. Geochemistry, Geophysics, Geosystems 15(8): 3123-3144.
(10) Wang X., Zhu W.B*., Ge R.F., Luo M., Zhu X.Q., Zhang Q.L., Wang L.S., Ren X.M., 2014. Two episodes of Paleoproterozoic metamorphosed mafic dykes in the Lvliang Complex: Implications for the evolution of the Trans-North China Orogen. Precambrian Research 243: 133-148.
(11) 王玺, 陈清华, 朱文斌, 马婷婷, 王晓蕾, 刘寅, 2013. 苏北盆地高邮凹陷边界断裂带构造特征及成因,大地构造与成矿学 37, 20-28.

非第一作者/通讯作者文章:
(12) Tian R.S., Wang X., Ge R.F., Zhu W.B., Xie G.A., 2023. Early to Middle Paleozoic magmatism and metamorphism in the Alxa Block and its northern margin: Implications for the western extension of the Bainaimiao arc. Lithos 440-441: 107041.
(13) Cui X., Zhu W.B., Wang X., 2022. Neoproterozoic modification of heterogeneous continental lithosphere beneath the Yangtze interior: revealed from mafic dykes from the Huangling area, South China. International Journal of Earth Sciences 111:27-51.
(14) 朱文斌, 王玺, 葛荣峰, 2021. 地体的单向和多向聚合与离散, 地质学报, 95 (1): 124-138.
(15) Liu Y., John Suppe, Cao Y.C., Hao F., Liu Y.D., Wang X., Wu K.Y., Cao Z.C., Wei H.H., 2023. Linkage and formation of strike-slip faults in deep basins and the implications for petroleum accumulation: A case study from the Shunbei area of the Tarim Basin, China. AAPG Bulletin 107, 331–355.
(16) Liu Y., Wang X., Wu K.Y., Chen S.N., Shi Z., Yao W.J., 2019. Late Carboniferous seismic and volcanic record in the northwestern margin of the Junggar Basin: Implication for the tectonic setting of the West Junggar. Gondwana Research 71: 49-75.
(17) Liu Y., Chen Q.H., Wang X., Hu K., Cao S.L., Wu L., Gao F., 2017. Influence of normal fault growth and linkage on the evolution of a rift basin: A case from the Gaoyou depression of the Subei Basin, eastern China. AAPG Bulletin 101(2): 265-288.
(18) Liu Y., Wu K.Y., Wang X., Liu B., Guo J.X., Du Y.N., 2017. Architecture of buried reverse fault zone in the sedimentary basin: A case study from the Hong-Che Fault Zone of the Junggar Basin. Journal of Structural Geology, 105: 1-17.
(19) Cui X., Zhu W.B., Fitzsimons I.C.W., Wang X., Lu Y.Z., Wu X.H., 2017. A possible transition from island arc to continental arc magmatism in the eastern Jiangnan Orogen, South China: insights from a Neoproterozoic (870-860 Ma) gabbroic–dioritic complex near the Fuchuan ophiolite. Gondwana Research, 46: 1-16.
(20) Ge R.F., Zhu W.B., Wilde S.A., He J.W., Cui X., Wang X., Zheng BH., 2014. Neoproterozoic to Paleozoic long-lived accretionary orogen in the northern Tarim Craton. Tectonics 33, doi:10.1002/2013TC003501.