• 责任者：Xi Yunfei (State Key Lab. of Oil-Gas Geology and Development ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Li Zhongquan
• 刊名：Yunnan Geology
• 出版年：2013
• 卷期：32(4)
• 关键词：构造演化 ; structural evolution ; 海拉尔盆地 ; Hailar Basin
• 页码：p.480-483
• 图表：4 illus., 5 refs.
• 分类号：0300
• issnNo：ISSN1004-1885
• isbnNo：CN53-1041/P

     According to the seismic section, we have divided Beier depression with the recovery method of balance section, ie 4 forming stages： fault depression stage （Tongbomiao Formation, sag stage （Damoguaihe Formation, Yimin Formation） ; sinking stage （ Qingyuangang stage （Cenozoic） 4 reforming stages： tension -torsion deformation stage of end period Nantun Formation） ; fault Formation） and shrinkage of Nantun Formation Mem- ber 1 and Member 2 Sedimentation ; tension - torsion deformation stage of end period of Yimin Formation sedimen- tation and reversal deformation stage of end period of Qingyuangang Formation sedimentation.