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《Oil & Gas Geology》 2010-05
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Provenance systems and their control over sandbodies in the upper Es~4 of the Shengtuo area in the Dongying Sag,the Bohai Bay Basin

Liu Hui1 and Wang Shenglan2(1.School of Energy Resource,China University of Geosciences,Beijing 100083,China;2.CNOOC Petroleum Research Center,Beijing 100027,China)  
An analysis of the provenances and sandbody types of the upper 4th member of Eogene Shahejie Formation(Es4)in the Shengtuo area of the Dongying Sag,the Bohai Bay Basin was carried out based on an integration of seismic,logging and geochemical data,a paleogeomorphologic analysis,and a study of lithic fragment assemblage,ratio of characteristic elements and net-to-gross ratio.The results indicate that there were two different provenance systems during the deposition of the upper Es4:one on the upthrow of the Tuo-94 fault and the other on the upthrow of the Shengbei fault.Controlled by these two systems,various types of sandbodies were developed in the area,including nearshore subaqueous fan,sublacustrine fan and channel turbidite.The nearshore subaqueous fans mainly occur on the downthrow of the Chennan fault,the sublacustrine fans mainly occur on the downthrows of the Tuo-94 fault and the Shengbei Fault,while the channel turbidites occur in the trough along the Shengbei fault.It is suggested that the braided channel sandbodies and channel turbidite have the best poroperm characteristics,and their reservoir space is composed of fractures and dissolved pores.Therefore,the braided channel is a favorable facies belt for oil and gas accumulation.
【Fund】: 国家科技重大专项(2009ZX05009-002);; 教育部油气沉积地质创新团队(IRT0864)
【CateGory Index】: P618.13
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