冯鹏简历
导师简介：
冯鹏，男，1991年5月出生，湖北宜昌人，博士，副教授。2013年毕业于中国地质大学（武汉）地质学专业，2019年获中国地质大学（武汉）构造地质学博士学位，2021年于中国地质大学（武汉）地质资源与地质工程博士后流动站出站，随后进入南华大学教学科研岗位工作。主要从事造山带演化、板块碰撞边界变质作用和岩浆活动等方面的研究，主持国家自然科学基金青年基金、博士后面上基金、湖南省自然科学基金项目、国家重点实验室自主研究课题各1项，参与国家自然科学基金面上项目2项。累计发表SCI论文16篇，其中以第一或通讯作者6篇，主讲《大地测量学》、《变质岩石学》和《旅游地质学》等课程。
研究方向：
造山带演化、板块碰撞边界变质作用和岩浆活动、地质年代学
E-mail: fengpeng@usc.edu.cn
主持和参加的主要项目：
[1] 国家自然科学基金青年科学基金项目—深俯冲陆壳的P-T-t-熔流体演化轨迹:来自苏鲁超高压榴辉岩中多相固体包裹体的约束（主持；2022.01至2024.12）
[2] 湖南省自然科学基金青年科学基金项目—苏鲁造山带内同碰撞安山岩成因研究：对大陆俯冲带壳幔相互作用的启示（主持；2023.01至2025.12）
[3] 中国博士后科学基金面上资助—苏鲁超高压榴辉岩中多类型多相固体包裹体研究：对深俯冲陆壳P-T-t-熔流体演化轨迹的约束（主持；2021.03至2022.12）
[4] 地质过程与矿产资源国家重点实验室自主研究课题（主持；2020.04至2022.04）
[5] 国家自然科学基金面上项目—超高压榴辉岩的P-T-t-变形-熔融演化过程及其流变学意义（参与；2016.01至2019.12）
[6] 国家自然科学基金面上项目—北苏鲁造山带变基性岩的部分熔融：构造，P-T-t轨迹和熔流体演化之间的联系（参与，2021.01至2024.12）
发表论文：
[1] Feng P., Wang L.*, Brown M., Johnson, T.E., Kylander-Clark, A., and Piccoli, P.M., 2021. Partial melting of ultrahigh-pressure eclogite by omphacite-breakdown facilitates exhumation of deeply-subducted crust, Earth and Planetary Science Letters, 554.
[2] Feng P., Wang L.*, Wang S.J., Brown M. and Li X.W., 2019. Separating multiple episodes of partial melting in polyorogenic crust: An example from the Haiyangsuo complex, northern Sulu belt, eastern China. Geological Society of America Bulletin, 132, 1235-1256.
[3] Feng, P., Deng, H., Zhang, Y., Sui, Q.L., He, H.Y., Xie, Y.S., Chen, L., Duan, X.Z., Xiao, W.Z., Li, X.W., and Li, N., 2023, Pressure–temperature–time path of ultrahigh-pressure metamorphic terrane constrained by zircon petrochronology: a case study of orthogneisses from the northern Sulu belt, China: Journal of Asian Earth Sciences, p. 105877.
[4] Feng P., Wang L.*, Kusky Timothy, Chen Z., Hu W., Yang X.D., 2023, Slab breakoff diorite porphyries derived from two cratons in a continental subduction zone, Sulu orogen, China. Geological Society of America Bulletin.
[5] Feng P., Wang L.*, Li X.W., Ding W.J., Chen Z., 2023. SS-LASS Zircon Dating Deciphering Multiple Episodes of Anatexis in A Deeply-Subducted Continental Crust: An Example from Sulu Orogen, China. Journal of Earth Science.
[6] Duan, X. Z., Shen, H. J., Li, N., Xiao, W. Z., Sui, Q. L., He, H. Y., Feng, P.*, and Tang, Z. P.*, 2022, Transformation of the Sub-Continental Lithospheric Mantle Beneath the North China Craton (NCC): Constraints from the Geochemical Characteristics of Olivine Websterite Xenoliths and Their Minerals in the Cenozoic Basalts from Hannuoba: Minerals, v. 12, no. 4, p. 401.
[7] Wang, S.J., Wang, L., Brown, M., Piccoli, P.M., Johnson, T.E., Feng, P., Deng, H., Kitajima, K.and Huang, Y., 2017. Fluid generation and evolution during exhumation of deeplysubducted UHP continental crust: Petrogenesis of composite granite–quartz veins in the Sulubelt, China. Journal of Metamorphic Geology, 35(6): 601-629.
[8] Wang, L.*, Wang, S.J., Brown, M., Zhang, J.F., Feng, P., Jin, Z.M., 2018. On the survival of intergranular coesite in UHP eclogite. Journal of Metamorphic Geology, 36(2), 173-194.
[9] Wang, S.J., Wang, L.*, Brown, M, Feng P., 2016, Multi-stage barite crystallization in partially melted UHP eclogite from the Sulu belt, China. American Mineralogist, 101, 564–579.
[10] Ishwar-Kumar, C., Sajeev, K.*, Windley, B.F., Kusky, T.M., Feng, P., Ratheesh-Kumar, R.T., Huang, Y., Zhang, Y., Jiang, X.F. and Razakamanana, T., 2015. Evolution of high-pressuremafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications. Tectonophysics, 662(2): 219-242.
[11] Ning, W. B., Kusky, T.*, Wang, J. P., Wang, L., …. Feng, P. 2020. From subduction initiation to arc–polarity reversal: Life cycle of an Archean subduction zone from the Zunhua ophiolitic mélange, North China Craton. Precambrian Research, 105868.
[12] Wang, S.J., Wang, L.*, Brown, M.*, Johnson, T.E., Piccoli, P.M., Feng, P. and Wang, Z.L., 2020. Petrogenesis of leucosome sheets in migmatitic UHP eclogites—Evolution from silicate-rich supercritical fluid to hydrous melt. Lithos, 360-361.
[13] Zhang, Y. J., Kusky, T.*, Wang, L., Li, J.W., Feng, P., Huang, Y., Giddens, R., 2016. Occurrence of gold in hydrothermal pyrite, western Taupo Volcanic Zone, New Zealand. Geodinamica Acta, 28(3), 185-198.
