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《JIANGSU GEOLOGY》 1994-01
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The Geological Structure of Deeper Lithosphere and the Main Meso-Cenozoic Basins In the Eastern China

Fan Xiaolin et al  
The resultant Profiles of deep seismic sounding and magnetotelluric sounding have been multidisciplinary analysed by the regional geological and geophysical data.The relations between geological structure of deeper lithosphere and Songliao, Huabei,Ordos,Sichuan and Subei Meso─Cenozoic basins have been discussed.The lithosphere has the characteristics of heterogeneous anisotropic layer aud block─like structure which occurred intraplate deformational many times where the orohenic belt and basins have been formed by isostatic adjustmented of the lithosphere of the sballow crustal relation,to born of a new ocean(Pacific) and the vanishment of an old ocean (Tethys) in the eastern.
【Fund】: 国家八·五重点科技攻关项目 地矿部八·五重点基础科研项目
【CateGory Index】: P31
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