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] 岩石大地构造

[5] 电子探针方法开发

讲授课程:

[1]《构造地质学》

[2]《普通地质学》

[3]《解析构造地质学》

[4]《周口店野外实践教学》

教育经历：

2010.09-2015.06  中国地质大学（武汉）构造地质学博士

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

工作经历：

2015.07-至今     中国地质大学（武汉）地球科学学院

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：

2018-2021：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

王军鹏*，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.

2021

[28]邵航，王军鹏*，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.

2020

[27]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.

[26]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.

[25]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.

[24]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.

[23]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

[22]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 Science, 30 (5): 952-963. DOI: 10.1007/s12583-019-1020-8. https://rdcu.be/bT5eZ

[21]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.

[20]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.

2018

[19]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.

[18]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 Research, https://doi.org/10.1016/j.precamres.2018.01.020.

2017

[17]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.

[16]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.

[15]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.

[14]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.

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.