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Li Sitian(China University Geosciences,Wuhan,430074)Lin Changsong(China University of Geosciences,Beijing,100083)Xie Xinong;Yang Shigong;Jiao Yangquan(China University of Geosciences,Wuhan,430074 )  
The Ordos basin is one of the most important coal-bearing and hydrocarbon-bearing basin in China. The Mesozoic stratigraphy can be divided into five tectonic se-quences (TS) which coincide with the evolution stages of Ordos basin.The Early to Mid-dle Triassic sequences(TS-1)were formed in intracratonic regime,whilethe Upper Triassic(TS-2)sequences were developed in flexural regime under the influenceof orogenic movement of Qinling belt.The Early-Middle Jurassic sequences(TS-3)wereformed in a successor basin under ralatively stable condition which permits the detailedstudy of sequence stratigraphy. A molasse wedge developed in Upper Jurassic time(TS-4)overlied by the Cretaceous red beds(TS-5).The Yanan Formation is a typical nonma-rine sequence in TS-3. which is confined by unconformities at the bottom and top and in-cised valley have been found at the sequence boundaries.8-11 parasequences have beensubdivided from Yanan Formation and the depositional system tracts have been recon-structed.
【CateGory Index】: P539
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