• 责任者：Yang Xin (Key Laboratory of Petroleum Resources ; Chinese Academy of Sciences ; Lanzhou 730000 ; China) ; Zheng Jianjing
• 刊名：Geoscience
• 出版年：2011
• 卷期：25(3)
• 关键词：盆山耦合 ; basin range coupling ; 前陆盆地 ; foreland basins ; 云南 ; Yunnan Province
• 页码：p.447-455
• 图表：7 illus., 40 refs.
• 分类号：0300
• issnNo：ISSN1000-8527
• isbnNo：CN11-2035/P

Accompanied with the orogenic belt evolution stage from collision to post-collision and intraplate stage, the coupled basins transform from foreland basin to extensional basin and strike-slip structural basin. The Mesozoic-Cenozoic basin-orogen coupling of Sanjiang region of western Yunnan is a typical example of this conceptual model. Based on strata and outcrops, the authors divide Mesozoic strata of Lanping-Simao basin into 3 second sequences and 11 third sequences. The 3 second sequences corresponded to the evolutional stage of foreland basin, extensional basin and strike-slip structural basin, on behalf of each single prototype of the sedimentary basin filling. The growth of 11 third sequences controlled by several times non-cyclical basin basement activities including repeatedly deflection response to thrust load, episodic faulting activity of basement, and strike-slip structural function.