代表论著: [1]Huang Xuemeng, Du Yi, He Zhongtai, Ma Baoqi, Xie Furen, (2015), Late Quaternary slip rate of the Batang Fault and its strain partitioning role in Yushu area, central Tibet, Tectonophysics, 653: 52-67. [2]Huang Xuemeng, Du Yi, He Zhongtai, Ma Baoqi, Xie Furen, (2015), Late Pleistocene-Holocene paleoseismology of the Batang fault (central Tibet plateau, China), Geomorphology, 239: 127-141. [3] Du Yi, Zhang Xiaoliang, Huang Xuemeng, Du Yuben, Xie Furen. Late Quaternary Activity and Strong Earthquake Recurrence Interval along the North Segment of the Longling-Ruili Fault. Earthquake Research in China, 27, 344-357 [4]杜义,张效亮,黄学猛,杜宇本,谢富仁,(2012), 龙陵-瑞丽断裂北段晚第四纪活动性特征及强震复发间隔.震灾防御技术,7(3):215-226. [5]黄学猛,杜义,何仲太,马保起,谢富仁,(2011), 乌兰乌拉湖-玉树断裂东段晚第四纪滑动速率, 地震地质,23(4): 889-900. [6]张井飞,谢富仁,荆振杰,杜义,黄学猛, (2011), 太原盆地地震潜势分析. 大地测量与地球动力学, 31(05):47-51. [7]黄学猛,杜义,舒赛兵,谢富仁,(2010), 龙陵- 瑞丽断裂(南支)北段晚第四纪活动性特征. 地震地质,32(2):222-232. [8]谢富仁,荆振杰,杜义,崔效锋,黄学猛,(2009),利用断层滑动矢量反演协庄矿区构造应力场. 煤炭学报, 34(02):193-197. [9]杜义, 谢富仁,张效亮,荆振杰 (2009),汶川Ms8.0级地震断层滑动机制研究. 地球物理学报, 52(2):464-473. |