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《Geoscience》 2005-04
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Formation Mechanism of Carboniferous Central Paleouplift of Ordos Basin

WANG Qing-fei~(1,2),DENG Jun~(1,2),~()HUANG Ding-hua~(3),GAO Bang-fei~(1,2),XU Hao~(1,2)(1.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China;2.Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education,China University of Geosciences,Beijing 100083,China;3.Faculty of Earth Sciences,China University of Geosciences,Wuhan,Hubei 430074,China)  
To reveal the formation mechanism of the Carboniferous slender-waist-shaped central paleouplift in Ordos Basin,a series of stress-strain simulations were carried out,in which the basin was simplified into an isopachic,isotropic and elastic shell model and loaded with the NS trending extrusion.The positive strain along Z axis(ε_(z)) corresponded to the uplift,and the shape of positive ε_(z) isoline_()represented that of the uplift.Repeated simulations showed that the outline of positive ε_(z) isoline always appeared slender-waist shape along the maximum stress axis,which approved that the central uplift resulted from stress transfer in the Ordos Basin under the NS trending extrusion.(More-)(over),the shape of the positive ε_(z) isoline caused by the point force was narrow,while that by the linear pressure was relatively wide in the simulations.Since the shapes of ε_(z) isoline induced by the linear pressure was less analogical to the geological uplift in the Ordos Basin,the linear pressure was less reasonable than the point force,which may represented the point collision between microplates or arc-continent collision during Carboniferous.
【Fund】: 国家重点基础研究规划项目(2003CB214600);; 教育部科学技术研究重点项目(03178);; 教育部跨世纪人才基金项目
【CateGory Index】: P554
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