Sedimentary Evidences of the Uplift of the hemas-microsoft-com:office:smarttags" />
详细信息
- 责任者：Chang Hong (State Key Laboratory of Loess and Quaternary Geology ; Institute of Earth Environment ; Chinese Academy of Sciences ; Xi’an 710075 ; China) ; Jin Zhangdong
- 刊名：Geological Review
- 出版年：2009
- 卷期：55(1)
- 关键词：角度不整合 ; angular unconformities ; 隆起 ; uplifts ; 青海 ; Qinghai Province
- 页码：p.49-57
- 图表：5 illus., 1 table, 42 refs.
- 分类号：0300
- issnNo：ISSN0371-5736
- isbnNo：CN11-1952/P
摘要
Combined deformation of sediments and regional information, it can be deduced that an existed thrust, Qaibeiyuan-Qinghai Nanshan northwest dipping thrust was reactivated along the region of the southward range-front of modern Qinghai Nanshan by Late Cenozoic right-lateral movement of Wenquan fault. The mountains range is thus a tectonic ramp that thrusted southward over the hemas-microsoft-com:office:smarttags" />Gonghe Basin Lake Qinghai and Gonghe Basin