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Structural Style and Character of Evolution for Central Uplift Belt in Qikou Depression

SHI Shuang-shuang,QI Peng,AI Neng-ping (Graduate School,China University of Geosciences,Wuhan 430074,China)  
This paper has reconsidered the secondary tectonic units of Qikou Depression and discussed its tectonic style for central uplift belt scientifically.It is pointed out that central uplift belt in this depression is a complex tectonic system and its mechanism of deformation is illuminated.On this basis,the process of information and evolution in Cenozoic is quantitatively studied with subsidence history analysis method.The conclusion is that the central uplift belt in Qikou depression developed through a multi-period and multi-episode evolvement process.It moved to the east of central uplift belt from Oligocene,characterised by consistent subsidence rate——it is quicker in the east than in the west.The basin is mainly controlled by an extensional regime during E s 2+3 period,when tilting horst block was formed in the west of the central uplift belt.Flat horst was formed in the middle with the influence of strike slipping of deep fault during E s 1,while in the east,large-scale compound rollover anticline shaped during E d,with tulip flower structure.The conclusions should be of great significance for the exploration of the central uplift belt in Qikou Depression.
【Fund】: 国家自然科学基金项目(40672089);; 教育部构造与油气资源重点实验室项目;; 教育部含油气盆地构造研究中心项目
【CateGory Index】: P618.13
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