• 责任者：Wang Yadong (Key Laboratory of Petroleum Resources Research ; Institute of Geology and Geophysics ; Chinese Academy of Sciences ; Lanzhou 730000 ; China) ; Zhang Tao
• 刊名：Earth Science Frontiers
• 出版年：2011
• 卷期：18(3)
• 关键词：构造演化 ; structural evolution ; 沉积演化 ; sedimentary evolution ; 隆起 ; uplifts ; 青藏高原 ; Qinghai-Tibetan Plateau
• 页码：p.141-150
• 图表：3 illus., 1 table, 64 refs.
• 分类号：0300
• issnNo：ISSN1005-2321
• isbnNo：CN11-3370/P

On the basis of the analysis of structure and sedimentary evolution of the seismic section in rn:schemas-microsoft-com:office:smarttags" />Western Qaidam Basin and combining the basement lithology, faults distribution and history of tectonic movement, the authors reconstructed the dynamical evolution framework of structure and sedimentation of Western Qaidam Basin during the Cenozoic. The results suggested that Western Qaidam Basin was under the compression tectonic background of the Tibetan Plateau uplift caused by the collision of India and Eurasia in the Cenozoic and underwent two violent periods of tectonic deformation.