王军鹏

基本信息Personal Information

教授 博士生导师 硕士生导师

性别 : 男

毕业院校 : 中国地质大学(武汉)

学历 : 博士研究生毕业

学位 : 博士学位

在职信息 : 在职

所在单位 : 地球科学学院

学科 : 地质学 构造地质学

办公地点 : 地勘楼

联系方式 : wangjp@cug.edu.cn

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个人简介Personal Profile

研究兴趣和方向:

[1] 前寒武纪地质学

[2] 造山带演化和构造解析

[3] 蛇绿岩、构造混杂岩

[4] 早前寒武纪铁矿

讲授课程:

《构造地质学》《解析构造地质学》《周口店野外实践教学》《秭归野外实践教学》

教育和工作经历:

2015.07- 至今   中国地质大学(武汉)地球科学学院 讲师、副教授、教授

2010.09-2015.06  中国地质大学(武汉)构造地质学专业 理学博士

2006.09-2010.07  中国地质大学(武汉)地质学(基地班)专业 理学学士

期刊任职:

《Geological Society of America Bulletin》副编辑

《Earth-Science Reviews》客座编辑

《Journal of Earth Science》《地球科学》青年编委

负责实验室仪器:

电子探针仪(JEOL JXA-8230) http://dxy.cug.edu.cn/info/1045/2015.htm

牛津能谱仪(OXFORD Aztec X-MAX80) http://dxy.cug.edu.cn/info/1045/2852.htm

莱卡喷镀仪(LEICA EM ACE200) http://dxy.cug.edu.cn/info/1045/2851.htm

科研项目:

2024-2027:主持自然科学基金面上项目

2021-2024:主持自然科学基金面上项目

2018-2022:主要参加国家自然科学基金重点项目

2016-2020:主持国家自然科学基金青年基金

       主持中国博士后科学基金特别资助和面上项目

       主持中央高校新青年教师计划、摇篮计划

       主要参加国家自然科学基金重点项目、地学长江计划核心项目群

发表文章:

ORCID ID: https://orcid.org/0000-0003-2174-2428               

ResearchGate: https://www.researchgate.net/profile/Junpeng_Wang12


教学文章

军鹏*,李福鹏,2020.地质学教学中普及大型仪器相关知识的探索和思考——以电子探针显微分析技术为例.中国地质教育,29(4):107-110.


2024

[44]Jiang, K., Wang J.P.*, Kusky, T., Ali Polat, Bo Huang, Wang, L., Shengli Li, Deng, H., Yaying Peng, 2024. Genesis of Archean to Paleoproterozoic banded iron formations in the North China craton: Geological and paleoenvironment implications. Earth-Science Reviews 250, 104710.

2023

[43]Wang, J.P., Jiao, Y.Z., Jiang, K., Kusky, T., Wang, L., Deng, H., 2023. Two Paleoproterozoic tectono-thermal events in the Central Orogenic belt, North China craton, determined from EPMA Th-U-Pb monazite geochronology of the Zanhuang massif. Terra Nova 35, 552–569.

[42]Wang, J.P., Gong, Y.C., Hu, X.Y., Shi, H.F., Jiang, K., 2023. Petrogenesis of granitoids in the southern Anhui Province, China: Implications for the Neoproterozoic tectonic evolution of the eastern Jiangnan orogenic belt. Precambrian Research 397, 107194.

[41]Ning, W.B., Kusky, T., Wang, L., Wang, J.P., Deng, H., Huang, B., Meng, J.N., Wang, R.Z., Hu, D., Peng, Y.Y., Chen, Z.Y., Wang, W.K., 2023. Neoarchean SSZ and MOR ultra-/high-pressure ophiolitic m´elanges of the Eastern Hebei Complex, North China Craton: Dynamics of an Archean paleo-subduction zone. Earth-Science Reviews, 240: 104403.

2022

[40]Wang, J.P., Jiang, K., Xiao, D., Li, F.F., Li, F.P., Li, X.F., Jin, S., Tao, G.H., 2022. Mineral Chemistry of Biotite and Its Petrogenesis Implications in ca. 2.5 Ga Wangjiazhuang Granitic Pluton, North China Craton. Journal of Earth Science, 33(2): 1-14.

[39]Lü T., Wang J.P.*, Jiang K., Jiao Y.Z., 2022. 39Ar-40Ar geochronology and EBSD analysis of mylonite in Zanhuang Massif: Implications for Paleoproterozoic tectonothermal evolution of the North China Craton. Earth Science, (in Chinese with English abstract). https://kns.cnki.net/kcms/detail/42.1874.P.20220914.0843.002.html

[38]Deng, H., Jia, N., Kusky, T., Polat, A., Peng, G., Huang, B., Wang, L., Wang, J.P., 2022. From subduction initiation to hot subduction: Life of a Neoarchean subduction zone from the Dengfeng Greenstone Belt, North China Craton. GSA Bulletin 134, 1277-1300.

2021

[37]Xiao, D., Ning, W.B., Wang, J.P.*, Kusky, T., Wang, L., Deng, H., Zhong, Y.T., Jiang, K., 2021. Neoarchean to Paleoproterozoic tectonothermal evolution of the North China Craton: Constraints from geological mapping and Th-U-Pb geochronology of zircon, titanite and monazite in Zanhuang Massif. Precambrian Research, 359(12): 106214.

[36]邵航,军鹏*,肖登,2021.北京房山岩体黑云母矿物化学特征及其对岩石成因的指示意义.地球科学https://kns.cnki.net/kcms/detail/42.1874.20210429.1338.004.html.

[35]Wang J.P.*, Jiang K., 2021. Kinematic analysis of mélange fabrics : Exemplified by the Neoarchaean Zanhuang and Zunhua mélange, North China Craton. Scientia geologica Sinica, 56(02): 449-470 (in Chinese with English abstract).

[34]Huang, Y., Wang, L., Robinson, P.T., Ning, W.B., Zhong, Y.T., Wang, J.P., Hu, W., Polat, A., Kusky, T., 2021. Podiform chromitite genesis in an Archean juvenile forearc setting: The 2.55 Ga Zunhua chromitites, North China Craton. Lithos, 394-395, 106194.

[33]Zhao, R.Z., Wang, M. F., Li, H., Shang, X.Y., Ullah, Z., Wang, J.P., 2021. Texture and Geochemistry ofScheelites in the Tongshankou Deposit in Daye, Hubei, China: Implication for REE Substitution Mechanism and Multistage W Mineralization Processes. Minerals, 11: 984.

[32]Zhong, Y.T., Kusky, T.M., Wang, L., Polat, A., Liu, X.Y., Peng, Y.Y., Luan, Z.K., Wang, C.H., Wang, J.P., Deng, H., 2021. Alpine-style nappes thrust over ancient North China continental margin demonstrate large Archean horizontal plate motions. Nat. Commun. 12, 6172.

2020

[31]Jiang, K., Wang, J.P.*, Kusky, T., Polat, A., Deng, H., Wang, L., 2020. Neoarchean seafloor hydrothermal metamorphism of basalts in the Zanhuang ophiolitic mélange, North China Craton. Precambrian Research, 347: 105832.

[30]Shi H.F., Wang J.P.*, Yao Y., et al., 2020. Geochemistry and geochronology of diorite in Pengshan area of Jiangxi Province: Implications for magmatic source and tectonic evolution of Jiangnan Orogenic Belt. Journal of Earth Science 31 (1), 23-34.

[29]Kusky, T.*, Wang, J.P.*, Wang, L., Huang, B., Ning, W., Fu, D., Peng, H., Deng, H., Polat, A., Zhong, Y., Shi, G., 2020. Mélanges through time: Life cycle of the world's largest Archean mélange compared with Mesozoic and Paleozoic subduction-accretion-collision mélanges. Earth-Science Reviews, 103303.

[28]陶光活,李晓峰,王军鹏*,蒋康,2020.冀北崇礼红旗营子岩群中镁铁质岩石地球化学和年代学研究:对华北克拉通新太古代晚期-古元古代早期大地构造演化的启示.地球科学,45(9):3436-3450.

[27]Ning W.B., Kusky T.M., Wang J.P., Wang L., Deng H., Polat A., Huang B., Peng H.T., Feng P., 2020. From subduction initiation to arc-polarity reversal: Life cycle of an Archean subduction zone from the Zunhua ophiolitic melange, North China Craton. Precambrian Research 350: 105868.

[26]Deng, H., Kusky, T.M., Polat, A., Fu, H.Q., Wang, L., Wang, J.P., Wang, S.J., Zhai, W.J., 2020. A Neoarchean Arc-Backarc Pair in the Linshan Massif, Southern, North China Craton. Precambrian Research, 341: 105649.

[25]Peng, H.T., Kusky, T., Deng, H., Wang, L., Wang, J.P., Huang, Y., Huang, B., Ning, W., 2020. Identification of the Neoarchean Jianping pyroxenite-mélange in the Central Orogenic Belt, North China Craton: A fore-arc accretional assemblage. Precambrian Research, 336, 105495.

2019

[24]Ning W.B., Wang J.P.*, Xiao D., Li F.F., Huang B., Fu D., 2019. Electron Probe Microanalysis of Monazite and Its Appilications to U-Th-Pb Dating of Geological Samples. Journal of Earth Science30 (5): 952-963. DOI: 10.1007/s12583-019-1020-8. https://rdcu.be/bT5eZ

[23]Huang, B., Kusky, T.M., Wang, L., Polat, A., Fu, D., Windley, B., Deng, H., Wang, J.P., 2019, Structural relationships and kinematics of the Neoarchean Dengfeng forearc and accretionary complexes, southern North China craton, Geological Society of America Bulletin https://doi.org/10.1130/B31938.1.

[22]Huang, B., Kusky, T.M.* Wang, L., Deng, H., Wang, J.P., Fu, D., et al., 2019. Age and genesis of the Neoarchean Algoma-type banded iron formations from the Dengfeng greenstone belt, southern North China Craton: Geochronological, geochemical and Sm–Nd isotopic constraints. Precambrian Research, 333, 105437.

[21]Deng, H., Kusky, T.M., Polat, A, Lan, B.Y., Huang, B., Peng, H.T., Wang, J.P., Wang, S.J., 2019. Magmatic record of Neoarchean arc-polarity reversal from the Dengfeng segment of the Central Orogenic Belt, North China Craton. Precambrian Research, 326, 105-123.

2018

[20]Wang J.P., Deng H., Kusky T.M., A. Polat, 2018. Comments on “Paleoproterozoic arc-continent collision in the North China Craton: Evidence from the Zanhuang Complex” by Li et al. (2016), Precambrian Research 286: 281–305, Precambrian Research, 304: 171-173.

[19]Deng, H., Kusky, T.M., Polat, A, Lan, B.Y., Huang, B., Peng, H.T., Wang, J.P., Wang, S.J., 2018. Magmatic record of Neoarchean arc-polarity reversal from the Dengfeng segment of the Central Orogenic Belt, North China Craton. Precambrian Researchhttps://doi.org/10.1016/j.precamres.2018.01.020.

2017

[18]Wang J.P., Kusky T.M., Wang L., Polat A., Deng H., Wang C., Wang S.J., 2017a. Structural relationship along a Neoarchean arc-continental collision zone, North China Craton. Geological Society of America Bulletin, 129: 59-75.

[17]Wang J.P., Kusky T.M., Wang L., Polat A., Wang S.J., Deng H., Fu J.M., Fu D., 2017b. Petrogenesis and geochemistry of circa 2.5 Ga granitoids in the Zanhuang Massif: Implications for magmatic source and Neoarchean metamorphism of the North China Craton. Lithos, 268-271: 149-162.

[16]Wang J.P., Deng H., Kusky T.M., Polat A., 2017c. Comments to “Paleoproterozoic meta-carbonates from the central segment of the Trans-North China Orogen: Zircon U-Pb geochronology, geochemistry, and carbon and oxygen isotopes” by Tang et al., 2016, Precambrian Research 284:4-29. Precambrian Research, 294: 344-349.

[15]Deng, H., Peng, S.B., Polat, A., Kusky, T.M., Jiang, X.F., Han, Q.S., Wang, L., Huang, Y.,Wang, J.P., Zeng, W., Hu, Z.X., 2017. Neoproterozoic IAT intrusion into Mesoproterozoic MOR Miaowan Ophiolite, Yangtze Craton: Evidence for evolving tectonic settings. Precambrian Research 289: 75-94.

[14]Jiang X.F., Peng S.B., Kusky T.M., Wang L., Deng H., Wang J.P., 2017. Formation Time of the Northeastern Jiangxi Ophiolite in the Eastern Jiangnan Orogenic Belt: Evidence from LA-ICP-MS Zircon U-Pb Dating of the Gabbro. Geoscience, 31(4), 697-704 (in Chinese with English abstract).

2016

[13]Deng H., Kusky, T.M., Polat, A., Wang, C., Wang, L., Wang, J.P., 2016. A 2.5 Ga fore-arc subduction-accretion complex in the Dengfeng Granite-Greenstone Belt, Southern North China Craton. Precambrian Research 275: 241-264.

[12]Kusky, T.M., Polat, A., Windley, B.F., Burke, K.C., Dewey, J.F., Kidd, W.S.F., Maruyama, S., Wang, J.P., Deng, H., Wang, Z.S., Wang, C., Fu, D., Li, X.W., Peng, H.T., 2016. Insights into the Tectonic Evolution of the North China Craton Through Comparative Tectonic Analysis: A Record of Outward Growth of Precambrian Continents. Earth ScienceReviews, 162: 387-432. 

2015

[11]Wang J.P., Kusky T.M., Wang L., Polat A., Deng H., 2015. A Neoarchean subduction polarity reversal event in the North China Craton, Lithos, 220-223: 133-146.

2014

[10]Wang L., Kusky T.M., Polat A. Wang S.J., Jiang X.F., Zong K.Q.,Wang J.P., Deng H., Fu J.M., 2014. Partial Melting of deeply subducted eclogite from the Sulu orogen in China. Nature Communication, 5:5604.

[9]Deng H., Kusky T.M., Polat A., Wang, J.P., et al., 2014. Geochronology, mantle source composition and geodynamic constraints on the origin of Neoarchean mafic dikes in the Zanhuang Complex, Central Orogneic Belt, North China Craton.Lithos 205, 359-378.

2013

[8]Wang J.P., Kusky T.M., Polat A., Wang L., Deng H., Wang S.J., 2013. A late Archean tectonic mélange belt in the Central Orogenic Belt, North China Craton. Tectonophysics, 608: 929-946.

[7]Deng H., Kusky T.M., Polat A., Wang L., Wang J.P., Wang S.J., 2013. Geochemistry of Neoarchean mafic volcanic rocks and late mafic dikes in the Zanhuang Complex, Central Orogenic Belt, North China Craton: Implications for geodynamic setting. Lithos, 175-176:193-212.

2012

[6]Wang J.P., Kusky T.M., Polat A., Wang L., et al., 2012. Sea-floor Metamorphism Recorded in Epidosites from the ca.1.0 Ga Miaowan Ophiolite, Huangling Anticline, China. Journal of Earth Science, 23(5): 696-704.

[5]Peng S.B., Kusky T.M., Jiang X.F., Wang L., Wang J.P., Deng H., 2012. Geology, geochemistry, and geochronology of the Miaowan ophiolite, Yangtze craton: Implications forSouth China’s amalgamation history with the Rodinian supercontinent.Gondwana Research, 21: 577-594.

[4]Jiang X.F., Peng S.B, Kusky T.M., Wang L., Wang J.P., Deng H., 2012. Geological features and deformational ages of the basal thrust belt of the Miaowan ophiolite in the southern Huangling anticline and its tectonic implications.Journal of Earth Science, 23(5): 705-718.

[3]Deng H., Kusky T.M., Wang L., Peng S.B., Jiang X.F., Wang J.P., Wang S.J., 2012. Discovery of a Sheeted Dike Complex in the Northern Yangtze Craton and Its Implications for Craton Evolution. Journal of Earth Sciences, 23(5): 676-695.

2011

[2]Rao C.V.D., Santosh M., Purohit R., Wang J.P., Jiang X.F., Kusky T.M., 2011. LA-ICP-MS U-Pb zircon age constraints on the Paleoproterozoic and Neoarchean history of the Sandmata Complex in Rajasthan within the NW Indian Plate.Journal of Asian EarthSciences, 42(3): 286-305.

2010

[1]Kusky T.M., Ye M.H., Wang J.P., Wang L., 2010. Geological Evolution of Longhushan World Geopark in Relation to Global Tectonics. Journal of Earth Science, 21(1):1-18.

  • 教育经历Education Background
  • 工作经历Work Experience
  • 研究方向Research Focus
  • 社会兼职Social Affiliations
  • 前寒武纪地质学