北京科技大学主页平台管理系统贺振宇--中文主页--论文成果

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论文成果

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[1] 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. [The genesis of middle Jurassic Syenite-gabbro in Southern Jiangxi Province and their geological significance].
[2] 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. [Geochronology and geochemistry of shoshonitic volcanics in southern Jiangxi Province].
[3] 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..
[4] 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..
[5] 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..
[6] 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. [Zircon geochronology of Xingxingxia quartz dioritic gneisses: Implications for the tectonic evolution and Precambrian basement affinity of Chinese Tianshan orogenic belt].
[7] He Zhen-Yu, Xu Xi-Sheng, 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..
[8] 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..
[9] 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. [Zircon U–Pb dating and Hf isotopic studies on the Beishan complex in the southern Beishan orogenic belt].
[10] 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..

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