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《Journal of Jilin University(Earth Science Edition)》 2008-02
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Basin Filling Features and Evolution of Sequence Stratigraphy of Paleogene in Wushi Sag

SUN Wei1,FAN Tai-liang1,ZHAO Zhi-gang2,WANG Hong-yu1,GAO Zhi-qian1,DUAN Rui-hui11.School of Energy Resources,China University of Geosciences,Beijing 100083,China2.Beijing Research Center,China National Offshore Oil Corporation,Beijing 100010,China  
By means of sequence stratigraphy,sedimentology and with comprehensive study of core section,cuttings,well-logging,seismic informations,fossils and geochemistry data the authors recognized three kinds of unconformities and classified the Paleogene into seven seismic sequences of third grade,vertical section of which is transgression,regression and aggradation respectively.Tectonic subsidence play dominant role in their geometric shapes,basin fillings,sequence evolution and sediment distribution in the Wushi Sag.Outline of the sequences are in shape of box-wedge or sheet-wedge and boundaries of sequences are varied from bilateral fault to monoclinal fault overlap,so that the sequences show distinct semigrabens which overlay in different ways.Seven sequences were formed in different stage of tectonic evolution.The sequence of SQ1 formed in initial rift stage and deposited alluvial sequence.Sequences SQ2-SQ4 developed in intense rift stage and sediment lacustrine sequence.Sequences SQ5-SQ7 formed in late period of rift before thermal subsidence and deposit mere and delta sediment.The place adjacent to the synsedimentary fault is the subsidence center and depocenter;meanwhile,controlling fracture migrates in horizontal made subsidence and sedimentary center of the sag changed.
【Fund】: 中国海洋石油公司科技攻关项目(CNOOCLTD-2006-Kt-007)
【CateGory Index】: P539.2
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