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龙门山中段中生代前陆盆地的构造演化史
引用本文:王道永.龙门山中段中生代前陆盆地的构造演化史[J].成都理工大学学报(自然科学版),1994(3).
作者姓名:王道永
作者单位:成都理工学院地质学系
摘    要:依据龙门山中段中生代盆地的基底性质、沉积构造组合和构造变形,论证了川西拗陷是在印支期发育于扬子板块活动大陆边缘的弧背(前陆)盆地,前陆盆地的构造变形是经印支期构造变动和喜马拉雅期叠加改造形成的推覆构造;并讨论了龙门山中段中生代前陆盆地的构造演化历史。

关 键 词:龙门山,前陆盆地,构造演化,推覆构造,中生代,喜马拉雅运动

STRUCTURAL EVOLUTION OF MESOZOIC FORELAND BASIN IN THE MIDDLE LONGMEN MOUNTAINS
Wang Daoyong.STRUCTURAL EVOLUTION OF MESOZOIC FORELAND BASIN IN THE MIDDLE LONGMEN MOUNTAINS[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1994(3).
Authors:Wang Daoyong
Institution:Wang Daoyong
Abstract:Based on the characteristics of basement, sedimentary tectonics and tectonic deformation of the basin in the middle Longmen Mountains,this paper proves that the western Sichuan depression is the retroarc(foreland)basin developing in the active continent margin of Yangtze plate during indo Chinese epoch and that its tectonic deformation is the nappe formed by tectonization in Indosinian and superposition in Himalayanian. The paper also discusses the structural evolution history of the foreland basin in Mesozoic.
Keywords:Longmen Mountains  foreland basin  structural evolution  nappe  Mesozoic  Himalayan movement
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