- [1] Wang, An.A Non-Critical Hillslope Model: Evidence and Topographic Implications.Geomorphology.2024,453 :109155
- [2] 王岸.青藏高原东南缘金沙江下游新生代构造与地貌演化.地质力学学报.2023,29 (4):453−464
- [3] Wei Jie.Tectonic segmentation by N-S-trending cona cross structure in the Eastern Himalaya: Evidence from thermochronology and thermokinematic modeling.Tectonophysics.2022,839
- [4] Wang An.Fast Valley Landscape Response to Climate Change in the Lower Jinsha River, Southeastern Tibetan Plateau: Field Investigations and Numerical Modeling.Geomorphology.2022,403
- [5] Wang An.Tectonically dominant surface denudation and topography in the Himalaya: Evidence from coupling between bedrock channel and valley hillslope topographies. Terra Nova, . h.Terra Nova.2021,33 :602-612
- [6] Shen Tianyi.Controls on Cenozoic exhumation of the Tethyan Himalaya from fission-track thermochronology and detrital zircon U-Pb geochronology in the Gyirong basin area, southern Tibet.Tectonics.2016,35 (7):1713–1734
- [7] Wang An.Slow exhumation of the Greater Himalaya in the Yadong region, the transition between the Central and Eastern Himalaya, during the Late Neogene.Journal of the Geological Society.2019,176 :1207-1217
- [8] Wang An.Quaternary channel-focused rapid incision in the Phung Chu-Arun River in Central Himalaya: Implications for a Quaternary capture event.Journal of Asian Earth Sciences.2009,129 :243-25
- [9] Jiang Ren.Late Cenozoic tectonic evolution of the southern segment of the Tan-Lu fault zone, Eastern China.Journal of Asian Earth Sciences.2019,182 :103932
- [10] Chen Yu.Evolution of the Barkol Basin, eastern Tian Shan, and its geodynamic background.International Journal of Earth Sciences.2019,108 (4):1253–1271
- [11] 张克信.青藏高原新生代隆升研究现状.地质通报.2013,32 (1):1–18
- [12] 张远泽.循化-化隆盆地晚白垩世以来盆山耦合过程：来自物源与磷灰石裂变径迹年代学分析的证据.地球科学—中国地质大学学报.2013,38 (4):725-744
- [13] 黄文星.雅鲁藏布江大拐弯地区河流形态特征及其意义.地质通报.2013,32 (1):130-140
- [14] 李明.西藏吉隆地区高喜马拉雅新近纪冷却剥露——裂变径迹年代学证据.地质通报,31 (1):86-92
- [15] Wang An.Episodic exhumation of the Greater Himalayan Sequence since the Miocene constrained by fission track thermochronology in Nyalam, central Himalaya.Tectonophysics.2010,495 (3-4):315-323
- [16] Wang An.Late Quaternary river terrace sequences in the eastern Kunlun Range, northern Tibet: A combined record of climatic change and surface uplift, Journal of Asian Earth Sciences.Journal of Asian Earth Sciences.2009,34 (4):532-543
- [17] Wang An.Late Neogene mountain building of the eastern Kunlun Orogen, as constrained by DEM analysis.Earth Science—Journal of China University of Geosciences.2009,20 (2):391-400
- [18] Wang An.Tectonic landform of Quaternary lakes and its implications for deformation in the northern Qinghai-Tibet Plateau.Acta Geologica Sinica.2009,83 (1):121-129
- [19] 王岸.东昆仑造山带新生代早期构造事件的碎屑裂变径迹年代学证据.地球科学.2010,35 (5)
- [20] Wang An.Fission Track Geochronology of the Xiaonanchuan Pluton and the Morphotectonic Evolution of Eastern Kunlun since Late Miocene.Earth Science—Journal of China University of Geosciences.2006,17 (4):302-309
王岸 (副教授)
副教授 硕士生导师
性别：男
出生年月：1980-05-08
毕业院校：中国地质大学（武汉）
学历：博士研究生
学位：理学博士学位
在职信息：在职
所在单位：地球科学学院
入职时间：2008-07-01
职务：副教授
学科：构造地质学
办公地点：主楼515
联系方式：Email：anwang@cug.edu.cn Tel：13971366156
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