简  介：

1982年生，博士，副研究员，硕士生导师。目前主持中国地震局地质研究所基本科研业务专项等项目共2项。迄今为止已在Quaternary Science Reviews、Geomorphology 等杂志上发表论文19篇，其中以第一作者发表SCI论文10篇。主要研究方向：光释光测年、河流地貌、冰川地貌、古灾害、环境考古。目前探索研究：1、三门古湖演化与黄河贯通；2、藏东南冰湖堰塞-溃决灾害过程；3、加查峡谷河流下切与南北裂谷发育；4、金沙江石鼓段堰塞-溃决洪水过程及其对古人类影响；4、从青藏高原到孟加拉扇：沉积物释光信号指示物质循环；5、冰碛物侵蚀指示青藏高原长期构造作用。

https://www.researchgate.net/profile/Gang_Hu19

教育背景：

2010-2014年   中国科学院青藏高原研究所，自然地理专业，博士

2006-2009年   北京大学城市环境学院，第四纪地质学专业，硕士

2000-2004年   中国地质大学（北京），宝石与材料工艺专业，本科

工作经历：

2017.7-至今     中国地震局地质研究所，副研究员

2014-2017年：  中国科学院青藏高原研究所博士后流动站，博士后，合作

导师：丁林研究员

研究方向：

光释光测年、河流地貌、冰川地貌、古灾害、环境考古

国际合作与交流：

2016.02-04月：香港大学地球科学系，助理研究员，光释光年代学，合作导师：李盛华教授

2014.01-03月：香港大学地球科学系，助理研究员，光释光年代学，合作导师：李盛华教授

承担科研项目：

1. 三门峡盆地演化对黄河贯通的控制作用，中央级公益性科研院所基本科研业务专项(编号: IGCEA2008)，2020.01-2023.12，项目负责人

2. 青藏高原冰碛物侵蚀机制研究，中央级公益性科研院所基本科研业务专项(编号: IGCEA1813)，2019.12-2021.12，项目负责人

3. 雅鲁藏布江中段加查地区河流阶地年代学研究，中央级公益性科研院所基本科研业务专项(编号: IGCEA1720)，2017.12-2018.12，项目负责人

4. 喜马拉雅东构造结内朗峰末次冰期以来冰进序列年代学研究，国家自然科学基金青年基金(编号: 41501061)， 2016.01-2018.12，项目负责人

代表论著（*表示通讯作者）：

[1] Hu Gang, Wang Ping*, Sufi Mostafizur Rahman, et al. Vicissitudes experienced by the oldest urban center in Bangladesh in relation to the migration of the Brahmaputra River. Journal of Quaternary Science accepted.

[2] Huiying Wang, Hu Gang*, Wang Ping*, et al. Dam and megafloods at the First Bend of the Yangtze River since the Last Glacial Maximum. Geomorphology accepted.

[3] Hu G.*, Yi Chao-lu, Liu Jin-hua et al. Glacial advances and stability of the moraine dam on Mount Namcha Barwa since the Last Glacial Maximum, eastern Himalayan syntaxis. Geomorphology 2020, 365, 107246.

[4] Hu G., Wang, P., Li, D.H., Huang, J.W., Wang, H.Y., Yang, X.Y., Zhang, J.F., Chen, J., Qiu, M.H., Zhang, A.M., Shi, L.F., 2020. Landscape change and its influence on human activities in Lhasa Basin of central Tibetan Plateau since the last deglacial. Quaternary International 536, 1-12.

[5] Hu G., Yi, C.L., Hou, J.Z., Zhang, J.F., He, Y., Pan, B.L., Liu, J.H., Jiang, T., Yi, S.W., 2018. Luminescence dating of lacustrine sediments from Linggo Co, central Tibetan Plateau. Boreas 47, 656-670.

[6] Hu, G., Yi, C.L., Zhang, J.F., Dong, G.C., Liu, J.H., Xu, X.K., Jiang, T., 2017. Extensive glacier advances during the Last Glacial Maximum near the eastern Himalayan syntaxis. Quaternary International 10, 1-12.

[8] Hu, G., Yi, C.L., Zhang, J.F., Liu, J.H., Tao, J., Li, S.H., 2016. Late Quaternary glacial advances in the eastern Qilianshan, north-eastern Tibet, as inferred from luminescence dating of fluvioglacial sediments. Journal of Quaternary Science 31, 587-597.

[8] Hu, G., Yi, C.L., Zhang, J.F., Liu, J.H., Tao, J., 2015. Luminescence dating of glacial deposits near the eastern Himalayan syntaxis using different grain-size fractions. Quaternary Science Reviews 124,124-144.

[9] Hu, G., Yi, C.L., Zhang, J.F., Liu, J.H., Jiang, T., Qin, X., 2014. Optically stimulated luminescence dating of a moraine and a terrace in Laohugou valley, western Qilian Shan, northeastern Tibet. Quaternary International 321, 37-49.

[10] Hu，G., Zhang，J.F., Qiu, W.L., Zhou, L.P., 2010. Residual OSL signals in modern fluvial sediments from the Yellow River (HuangHe) and the implications for dating young sediments. Quaternary Geochronology 5(2), 187-193.

[11] Zhang, J.F., Qiu, W.L., Hu, G., Zhou, L.P., 2020. Determining the age of terrace formation using luminescence dating—a case of the Yellow River terraces in the Baode area, China. Methods and Protocols 3 (1), 17.

[12] Xu, X.K., Dong, G.C., Pan, B.L., Hu, G., Bi, W.L., Liu, J.H., et al. 2017. Late glacial glacier-climate modeling in two valleys on the eastern slope of Samdainkangsang Peak, Nyaiqentanggulha Mountains. SCIENCE CHINA-EARTH SCIENCES, 60(1), 135-142.

[13] Liu, J., Yi, C., Li, Y., Bi, W., Zhang, Q., Hu, G., 2017. Glacial fluctuations around the karola pass, eastern Lhagoi Kangri range, since the Last Glacial Maximum. Journal of Quaternary Science, 32(4), 516-527.

[14] Zhang, J., Feng, J.L., Hu, G., Wang, J., Yang, Y., Lin, Y., et al. 2015. Holocene proglacial loess in the Ranwu valley, southeastern Tibet, and its paleoclimatic implications. Quaternary International, 372, 9-22.

[15] Xu, X., Hu, G., Qiao, B., 2013. Last glacial maximum climate based on cosmogenic 10Be exposure ages and glacier modeling for the head of Tashkurgan Valley, northwest Tibetan Plateau. Quaternary Science Reviews 80, 91-101.

[16] Guo, Y.J., Zhang, J.F., Qiu, W.L., Hu, G., Zhuang, M.G., Zhou, L.P., 2012. Luminescence dating of the Yellow River terraces in the Hukou area, China. Quaternary Geochronology 10, 129-135.

[17] Pan, B., Yi, C., Jiang, T., Dong, G., Hu, G., Jin, Y., 2012. Holocene lake-level changes of Linggo Co in central Tibet. Quaternary Geochronology 10, 117-122.

[18] Zhang, J.F., Wang, X.Q., Qiu, W.L., Shelach, G., Hu, G., Fu, X., Zhou, L.P., 2011. The paleolithic site of Longwangchan in the middle Yellow River, China: chronology, paleoenvironment and implications. Journal of Archaeological Science 38(7), 1537-1550.

[19] Zhang, J.F., Qiu, W.L., Wang, X.Q., Hu, G., Li, R.Q., Zhou, L.P., 2010. Optical dating of a hyperconcentrated flow deposit on a Yellow River terrace in Hukou, Shaanxi, China. Quaternary Geochronology 5(2), 194-199.