• 责任者：Liu Yanxue (Institute of Geology ; CAGS ; Beijing 100037 ; China) ; Wang Guanghui
• 刊名：Acta Petrologica et Mineralogica
• 出版年：2011
• 卷期：30(3)
• 关键词：盆地演化 ; basin evolution ; 沉积演化 ; sedimentary evolution ; 青藏高原 ; Qinghai-Tibetan Plateau
• 页码：p.381-390
• 图表：4 illus., 14 refs.
• 分类号：0803
• issnNo：ISSN1000-6524
• isbnNo：CN11-1966/P

 Based on an analysis of sedimentary sequence, regional unconformity, lithologic character and distribution of Paleogene-Neogene sediments, the authors hold that the Paleogene-Neogene sediments can be divided into four upward-shallowing sequences of Tuotuohe Formation, Yaxicuo Formation, Wudaoliang Formation and Quguo Formation, which constitute two complete continental orogenic molasses formation sequences. The analysis shows that the Paleogene-Neogene Tuotuohe Basin has experienced such evolutionary stages as foreland basin evolution stage (56.5～45.0 Ma)→strike-slip pull-apart basin stage (45.0～30.0 Ma)→overall uplift and intermountain residual basin stage (23.5～16.0 Ma)→foreland basin-confined basin-intermountain residual basin stage (16～2.6 Ma).