博士生指导教师简介
贺振宇 男，中国地质科学院地质研究所研究员
北京市西城区百万庄大街26号，邮编：100037
E-mail: hzy@cags.ac.cn
主要研究领域：
一般：
花岗岩成因与岩浆作用过程；火山岩石学与火山岩浆演化；地壳形成与演化；岩石地球化学；锆石年代学；变质岩岩石学
具体研究：
中国东南沿海白垩纪火山-侵入杂岩成因；华南中生代构造演化；西藏冈底斯带花岗岩成因与岩浆混合作用；东天山-北山古老微陆块的地壳物质组成与花岗岩成因；塔里木克拉通前寒武纪地壳形成与演化

一、个人简历
2016年1月　中国地质科学院地质研究所，研究员
2013年1月—2015年12月 中国地质科学院地质研究所，副研究员
2012年9月—2012年12月 中国地质科学院地质研究所，助理研究员
2010年7月—2012年9月 中国地质科学院地质研究所，博士后
1997年7月—2005年9月 安徽煤田地质局第三勘探队，工程师
期间：2016年12月—2017年11月 德国埃尔朗根-纽伦堡大学，访问****
二、科研项目情况：
1、中国地质调查局地质调查项目，DD**，北方山系西拉木伦与贺根山基础地质调查，2019.01—2021.12， 120万元，项目骨干
2、国家自然科学基金面上项目，** ，东疆星星峡地区淡色花岗岩的成因及其蕴含的古老地壳组成信息，2018.01—2021.12，72万元，主持
3、中国地质调查局地质调查子项目，DD**-03，东天山星星峡1：5 万变质基底专题地质填图试点，2016.01—2018.12， 269万元，主持
4、中国地质调查局工作项目，401，冈底斯俯冲-碰撞岩浆带中段的岩浆演化及构造背景，2014.01—2014.12，140万元，主持
5、国家自然科学基金重点项目，**，喜马拉雅造山带东段的变质作用与构造演化，2013.01-2017.12，300万元，参加
6、国家自然科学基金青年基金项目，**，浙闽沿海大规模火山-侵入杂岩成因——典型案例剖析，2012.01-2014.12，24万元，主持
7、中国地质科学院地质研究所基本科研业务费重点项目，J1311，中国东南沿海火山-侵入杂岩的成因与岩浆作用过程，2013-2015，50万，主持
8、中国博士后科学基金面上资助项目“塔里木克拉通东北缘高压麻粒岩相变质作用及其构造意义”2011/01-2012/12 编号： （负责）

三、学术成果情况：
第一和通讯作者（28篇）
[1] Wen, D.-J., He, Z.-Y, Zhang, Z.-M., 2019. Geochemistry and tectonic implications of Early Permian granitic rocks in the Xingxingxia area of Chinese Central Tianshan Arc Terrane. Geological Journal, 54, 1578-1590.
[2] He, Z.-Y., Klemd, R., Yan, L.-L, Zhang, Z.-M., 2018. The origin and crustal evolution of microcontinents in the Beishan orogen of the southern Central Asian Orogenic Belt. Earth-Science Reviews, 185, 1–14.
[3] He, Z.-Y., Klemd, R., Yan, L.-L, Lu, T.-Y., Zhang, Z.-M., 2018. Mesoproterozoic juvenile crust in microcontinents of the Central Asian Orogenic Belt: evidence from oxygen and hafnium isotopes in zircon. Scientific Reports, 8, 5054.
[4] Yan Lili, He Zhenyu, Beier Christoph, Klemd Reiner., 2018. Geochemical constraints on the link between volcanism and plutonism at the Yunshan caldera complex, SE China. Contributions to Mineralogy and Petrology, 173: 4.
[5] Yan, L.-L., He, Z.-Y., Beier, C., Klemd, R., 2018. Zircon trace element constrains on the link between volcanism and plutonism in SE China. Lithos 320-321, 28-34.
[6] Shui, X., He, Z., Klemd, R., Zhang, Z., Lu, T., Yan, L., 2018. Early Jurassic adakitic rocks in the southern Lhasa sub-terrane, southern Tibet: Petrogenesis and geodynamic implications. Geological Magazine, 155, 132–148.
[7] Yan, L.-L., He, Z.-Y., Jahn, B.-m., Zhao Z.-D., 2016. Formation of the Yandangshan volcanic–plutonic complex (SE China) by melt extraction and crystal accumulation. Lithos 266–267, 287–308.
[8] He, Z.-Y., Klemd, R., Zhang, Z.-M., Zong, K.-Q., Sun, L.-X., Tian, Z.-L., Huang, B.-T., 2015. Mesoproterozoic continental arc magmatism and crustal growth in the eastern Central Tianshan Arc Terrane of the southern Central Asian Orogenic Belt: Geochronological and geochemical evidence. Lithos, 236-237, 74-89.
[9] Mao, L.-J., He, Z.-Y., Zhang, Z.-M., Klemd, R., Tian, Z.-L., Zong, K.-Q., 2015. Origin and geodynamic significance of the early Mesozoic Weiya LP and HT granulites from the Chinese Eastern Tianshan. Lithos, 239, 142-156.
[10] Huang, B.T., He, Z.Y., Zhang, Z.M., Klemd, R., Zong, K.Q., Zhao, Z.D., 2015. Early Neoproterozoic granitic gneisses in the Chinese Eastern Tianshan: Petrogenesis and tectonic implications. Journal of Asian Earth Sciences, 113, 339–352.
[11] He, Z.Y., Zhang, Z.M., Zong, K.Q., Xiang, H., Chen, X.J., Xia, M.J., 2014. Zircon U–Pb and Hf isotopic studies of the Xingxingxia Complex from Eastern Tianshan (NW China): Significance to the reconstruction and tectonics of the southern Central Asian Orogenic Belt. Lithos, 190–191, 485–499.
[12] He, Z.Y., Zhang, Z.M., Zong, K.Q., Xiang, H., Klemd, R., 2014. Metamorphic P–T–t evolution of mafic HP granulites in the northeastern segment of the Tarim Craton (Dunhuang block): Evidence for early Paleozoic continental subduction. Lithos, 196–197, 1–13.
[13] Huang, B.T., He, Z.Y, Zong, K.Q., Zhang, Z.M., 2014. Zircon U–Pb and Hf isotopic study of Neoproterozoic granitic gneisses from the Alatage area, Xinjiang: constraints on the Precambrian crustal evolution in the Central Tianshan Block. Chinese Science Bulletin, 59 (1), 100-112.
[14] He, Z.Y., Zhang, Z.M., Zong, K.Q., Dong, X., 2013. Paleoproterozoic crustal evolution of the Tarim Craton: constrained by zircon U-Pb and Hf isotopes of meta-igneous rocks from Korla and Dunhuang. Journal of Asian Earth Sciences, 78, 54–70.
[15] He Zhen-Yu, Zhang Ze-Ming, Zong Ke-Qing, Wang Wei, Santosh M., 2012. Neoproterozoic granulites from the northeastern margin of the Tarim Craton: Petrology, zircon U–Pb ages and implications for the Rodinia assembly. Precambrian Research, 212–213, 21–33.
[16] He, Z.Y., Xu, X.S., 2012. Petrogenesis of the Late Yanshanian mantle-derived intrusions in southeastern China: Response to the geodynamics of paleo-Pacific plate subduction. Chemical Geology, 328, 208-221.
[17] He Zhen-Yu, Xu Xi-Sheng, Niu Yao-Ling, 2010. Petrogenesis and tectonic significance of a Mesozoic granite-syenite-gabbro association from inland South China. Lithos, 119, 621–641.
[18] He Zhen-Yu, Xu Xi-Sheng, Zou Hai-Bo, Wang Xu-Dong, Yu Yao, 2010. Geochronology, petrogenesis and metallogeny of Piaotang granites in the tungsten deposit region of South China. Geochemical Journal, 44, 299–313.
[19] He Zhen-Yu, Xu Xi-Sheng, Yu Yao, Zou Hai-Bo, 2009. Origin of the Late Cretaceous syenite from Yandangshan, SE China, constrained by zircon U-Pb and Hf isotopes and geochemical data. International Geology Review, 51(6), 556–582.
[20] 陆天宇，贺振宇，张泽明，水新芳，颜丽丽, 2016. 西藏冈底斯尼木后碰撞花岗岩的岩浆混合作用：显微结构证据. 岩石学报, 32(12), 3613-3623.
[21] 水新芳，贺振宇，张泽明，陆天宇, 2016. 西藏冈底斯带东段早侏罗世英云闪长岩的岩浆起源及其对拉萨地体地壳演化的意义. 地质学报, 90(11): 3129-3152.
[22] 颜丽丽，贺振宇，刘磊，赵志丹, 2015. 浙江雁荡山火山-侵入杂岩的岩浆混合作用：暗色包体中长石环带的证据. 地质通报, 34(2-3), 466–473.
[23] 贺振宇, 孙立新, 毛玲娟, 宗克清, 张泽明, 2015. 北山造山带南部片麻岩和花岗闪长岩的锆石U-Pb定年和Hf同位素: 中元古代的岩浆作用与地壳生长. 科学通报, 60(4), 389-399.
[24] 贺振宇, 宗克清, 姜洪颖, 向华, 张泽明, 2014. 北山造山带南部早古生代构造演化：来自花岗岩的约束. 岩石学报, 30(8), 3949-3967.
[25] 姜洪颖, 贺振宇, 宗克清, 张泽明, 赵志丹, 2013. 北山造山带南缘北山杂岩的锆石U-Pb定年和Hf同位素研究. 岩石学报, 29(11), 3949-3967.
[26] 贺振宇, 张泽明, 宗克清, 于飞, 王伟, 2012. 星星峡石英闪长质片麻岩的锆石年代学：对天山造山带构造演化及基底归属的意义. 岩石学报, 28(6), 1857-1874.
[27] 贺振宇, 徐夕生, 王孝磊, 陈荣, 2008. 赣南橄榄安粗质火山岩的年代学与地球化学. 岩石学报, 24(11), 2524-2536.
[28] 贺振宇, 徐夕生, 陈荣, 邢光福, 2007. 赣南中侏罗世正长岩-辉长岩的起源及其地质意义. 岩石学报, 23(6), 1457-1469.

合作者（约30篇）
[1] Dong, X., Zhang, Z.-m., Klemd, R., He, Z.-y., Tian, Z.-l., 2018. Late Cretaceous tectonothermal evolution of the southern Lhasa terrane, South Tibet: Consequence of a Mesozoic Andean-type orogeny. Tectonophysics 730, 100-113.
[2] Yuan, Y., Zong, K., He, Z., Klemd, R., Jiang, H., Zhang, W., Liu, Y., Hu, Z., Zhang, Z., 2018. Geochemical evidence for Paleozoic crustal growth and tectonic conversion in the Northern Beishan Orogenic Belt, southern Central Asian Orogenic Belt. Lithos 302, 189-202.
[3] Zong, K., Klemd, R., Yuan, Y., He, Z., Guo, J., Shi, X., Liu, Y., Hu, Z., Zhang, Z., 2017. The assembly of Rodinia: The correlation of early Neoproterozoic (ca. 900 Ma) high-grade metamorphism and continental arc formation in the southern Beishan Orogen, southern Central Asian Orogenic Belt (CAOB). Precambrian Research 290, 32-48.
[4] Ma, X., Xu, Z., Chen, X., Meert, J.G., He, Z., Liang, F., Meng, Y., Ma, S., 2017. The origin and tectonic significance of the volcanic rocks of the Yeba Formation in the Gangdese magmatic belt, South Tibet. Journal of Earth Science 28, 265-282.
[5] Zeng, G., He Z.-Y., Li Z., Xu X.-S., Chen L.-H., 2016. Geodynamics of paleo-Paci?c plate subduction constrained by the source lithologies of Late Mesozoic basalts in southeastern China. Geophysical Research Letters, 43, 10189-10197.
[6] Yuan, Y., Zong, K., He, Z., Klemd, R., Liu, Y., Hu, Z., Guo, J., Zhang, Z., 2015. Geochemical and geochronological evidence for a former early Neoproterozoic microcontinent in the South Beishan Orogenic Belt, southernmost Central Asian Orogenic Belt. Precambrian Research 266, 409-424.
[7] Zhang, Z., Xiang, H., Dong, X., Ding, H., He, Z., 2015. Long-lived high-temperature granulite-facies metamorphism in the Eastern Himalayan orogen, south Tibet. Lithos 212, 1-15.
[8] Zhang, Z., Dong, X., Xiang, H., Ding, H., He, Z., Liou, J., 2015. Reworking of the Gangdese magmatic arc, southeastern Tibet: post-collisional metamorphism and anatexis. Journal of Metamorphic Geology 33, 1-21.
[9] Dong, X., Zhang, Z.M., Liu, F., He, Z.Y., Lin, Y., 2014. Late Paleozoic intrusive rocks from the southeastern Lhasa terrane, Tibetan Plateau, and their Late Mesozoic metamorphism and tectonic implications. Lithos 198-199, 249-262.
[10] Zhang, Z.M., Dong, X., Xiang, H., He, Z.Y., Liou, J. G., 2014. Metagabbros of the Gangdese arc root, south Tibet: Implications for the growth of continental crust. Geochimica et Cosmochimica Acta 143, 268-284.
[11] Zong, K.Q., Liu, Y., Zhang, Z.M., He, Z.Y., Hu, Z., Guo, J., Chen, K., 2013. The generation and evolution of Archean continental crust in the Dunhuang block, northeastern Tarim craton, northwestern China. Precambrian Research, 235, 251–263.
[12] Zhang, Z.M., Dong, X., Liu, F., Lin, Y., Yan, R., He, Z.Y., Santosh, M., 2012. The making of Gondwana: Discovery of 650 Ma HP granulites from the North Lhasa, Tibet. Precambrian Research, 212-213, 107-116.
[13] Xu Xi-Sheng, Zhang Ming, Zhu Kong-Yang, Chen Xiao-Ming, He Zhen-Yu, 2012. Reverse age zonation of zircon formed by metamictisation and hydrothermal leaching. Lithos, 150, 256-267.
[14] Zong, K.Q., Zhang, Z.M., He, Z.Y., Hu, Z.C., Santosh, M., Liu, Y.S., Wang, W., 2012. Early Palaeozoic high-pressure granulites from the Dunhuang block, northeastern Tarim Craton: Constraints on continental collision in the southern Central Asian Orogenic Belt. Journal of Metamorphic Geology, 30, 753-768.
[15] Zhang, Z.M., Dong, X., Santosh, M., Liu, F., Wang, W., Yiu, F., He, Z.Y, Shen, K, 2012. Petrology and geochronology of the Namche Barwa Complex in the eastern Himalayan syntaxis, Tibet: Constraints on the origin and evolution of the north-eastern margin of the Indian Craton. Gondwana Research, 21, 123-137.
[16] Xu X.S., Griffin W.L., Ma X., O’Reilly S.Y., He Z.Y., Zhang C.L., 2009. The Taihua group on the southern margin of the North China craton: further insights from U-Pb ages and Hf isotope compositions of zircons. Mineralogy and Petrology, 97, 43-59.
[17] Xu X.S., Lu W.M., He Z.Y., 2007. Age and generation of Fogang granite batholith and Wushi diorite-hornblende gabbro body. Science in China (Series D), 50 (2), 209-220
[18] Xu X.S., O’Reilly S.Y., Griffin W.L., Wang X.L., Pearson N.J., He Z.Y., 2007. The Crust of Cathaysia : age, assembly and reworking of two Terranes. Precambrian Research, 158, 51-78.
[19] 孟元库, 许志琴, 陈希节, 马绪宣, 贺振宇, 张雪松, 2015. 藏南冈底斯中段谢通门始新世复式岩体锆石 U-Pb 年代学, Hf 同位素特征及其地质意义. 大地构造与成矿学, 39 (5), 933-948
[20] 陈希节, 许志琴, 孟元库, 贺振宇, 2014. 冈底斯带中段中新世埃达克质岩浆作用的年代学, 地球化学及 Sr-Nd-Hf 同位素制约. 岩石学报, 30 (8), 2253-2268
[21] 张泽明, 董昕, 贺振宇, 向华, 2013. 喜马拉雅造山带的高压超高压变质作用与印度-亚洲大陆碰撞. 岩石学报, 29, 1713-1726.
[22] 叶晓峰, 宗克清, 张泽明, 贺振宇, 刘勇胜, 胡兆初, 王伟, 2013. 北山造山带南缘柳园地区新元古代花岗岩的地球化学特征及其地质意义. 地质通报, 32(2), 307–317.
[23] 董昕, 张泽明, 向华, 贺振宇, 2013. 青藏高原南部拉萨地体的变质作用与动力学. 地球学报 34, 257-262.
[24] 徐夕生, 贺振宇, 2012. 花岗岩研究进展. 矿物岩石地球化学通报, 31(3), 205–209. [Progress in Granite studies]
[25] 董昕, 张泽明, 刘峰, 王伟, 于飞, 林彦蒿, 姜洪颖, 贺振宇, 2012. 拉萨地体东南部变质岩的成因与中-新生代造山作用. 岩石学报, 28(6): 1765–1784.
[26] 林彦蒿, 张泽明, 贺振宇, 董昕, 于飞, 2011. 中天山北缘华力西期造山作用——变质岩锆石U-Pb年代学限定. 中国地质, 38(4), 820–828.
[27] 陈志洪，邢光福，郭坤一，曾勇，匡福祥，贺振宇，柯学，余明刚，赵希林，张勇, 2011. 长江中下游成矿带九瑞矿集区(北部)含矿岩体的锆石U-Pb定年及其地质意义. 地质学报，85(7), 1146-1158.
[28] 刘峰, 张泽明, 董昕, 于飞, 王伟, 贺振宇, 林彦蒿, 严溶, 2011. 青藏高原冈底斯带东南部新生代多期岩浆作用及其构造意义. 岩石学报, 27(11): 3295–3307.
[29] 洪文涛, 徐夕生, 贺振宇, 闫峻, 2010. 南京蒋庙岩体的年代学、地球化学及其地质意义. 岩石学报, 26 (5), 1577-1588.
[30] 陈志洪, 邢光福, 郭坤一, 董永观, 陈荣, 曾勇, 李龙明, 贺振宇, 赵玲, 2009. 浙江平水群角斑岩的成因: 锆石U-Pb 年龄和 Hf 同位素制约. 科学通报 54(5), 610-617.