- 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
MARGIN: 0cm 0cm 0pt" class=MsoNormal> mary name="EnDivSummary">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 (56.5man’; mso-hansi-font-family: ’Times New Roman’">～45.0 Ma)→strike-slip pull-apart basin stage (45.0man’; mso-hansi-font-family: ’Times New Roman’">～30.0 Ma)→overall uplift and intermountain residual basin stage (23.5man’; mso-hansi-font-family: ’Times New Roman’">～16.0 Ma)→foreland basin-confined basin-intermountain residual basin stage (16man’; mso-hansi-font-family: ’Times New Roman’">～2.6 Ma).mas-microsoft-com:office:office" />