基于层序地层学和地震沉积学的高精度三维沉积体系:以渤中凹陷西斜坡BZ3-1区块东营组为例
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摘要
基于层序地层学、地震沉积学理论及三维可视化技术,结合3D高分辨率地震资料,对渤中凹陷西斜坡BZ3-1区块东营组层序进行高精度三维沉积体系分析.研究将东营组古沟谷分为V型、U型、W型及复合型4种类型,并详细刻画不同类型、不同期次的古沟谷从上游-下游的分叉、汇合的充填特征及其从发育-消亡的不同时期演化特征.研究区地震多属性异常区域在平面上多紧靠断层的下降盘,呈规模不一的扇状展布.结合测井曲线、岩心、地震相、地震多属性特征等分析可知,东营组层序沉积相类型分为扇三角洲、辫状河三角洲、滨浅湖,同时对不同相带边界进行了定量厘定.高精度三维沉积体系分析结果表明,由于三级层序发育于二级层序的不同体系域,会导致三级层序的体系域沉积体发育特征产生不同.SQd3层序发育于二级层序的低位体系域,其低位体系域的扇体规模要远远大于高位体系域的扇体;SQd2L层序发育于二级层序的水进体系域,其低位体系域三角洲朵体规模与高位体系域的三角洲朵体相当;SQd2u层序发育于二级层序的高位体系域,其高位体系域三角洲朵体规模远远大于低位体系域的三角洲朵体.
Based on sequence stratigraphy,seismic sedimentology theory and 3D visualization technology,High resolution three-dimensional facies architecture was described in detail using the recent 3D seismic data of Dongying Formation of BZ3-1 Block,western slope of Bozhong sag.The paleo-channels of Dongying formation could be subdivided into four types including type V,U,W and Compound,and were delineated the branching and converging infilling characteristics from up-stream to down-stream and the evolution stage from occurrence to extinction.Normally,Fan-shaped abnormal areas of seismic multi-attributes were located in the footwall of faults.On the basis of an integrated analysis of well log and core data,seismic facies,seismic multi-attribute,the sedimentary facies of sequences of Dongying formation were found to include fan-delta,braided river delta and coast-shallow lake,and the boundaries of these facies were crystallized quantitatively.The results of high resolution three-dimensional sedimentary systems analysis show that the third-order sequence located in different system tracts of second-order sequence could be lead to their system tracts with the different sedimentary types and scale.Because sequence SQd3 belong to the lowstand system tracts of second-order sequence,and the fan scale of lowstand system tracts of sequence SQd3 was larger than that of its highstand system tracts';Sequence SQdL2 is located in the transgressve system tracts of second-order sequence,and the delta scale of lowstand system tracts of sequence SQdL2 was equal to that of its highstand system tracts';Sequence SQdu2 developed in the highstand system tracts of second-order sequence,and the delta scale of lowstand system tracts of sequence SQdL2 was less than that its highstand system tracts'.
Based on sequence stratigraphy,seismic sedimentology theory and 3D visualization technology,High resolution three-dimensional facies architecture was described in detail using the recent 3D seismic data of Dongying Formation of BZ3-1 Block,western slope of Bozhong sag.The paleo-channels of Dongying formation could be subdivided into four types including type V,U,W and Compound,and were delineated the branching and converging infilling characteristics from up-stream to down-stream and the evolution stage from occurrence to extinction.Normally,Fan-shaped abnormal areas of seismic multi-attributes were located in the footwall of faults.On the basis of an integrated analysis of well log and core data,seismic facies,seismic multi-attribute,the sedimentary facies of sequences of Dongying formation were found to include fan-delta,braided river delta and coast-shallow lake,and the boundaries of these facies were crystallized quantitatively.The results of high resolution three-dimensional sedimentary systems analysis show that the third-order sequence located in different system tracts of second-order sequence could be lead to their system tracts with the different sedimentary types and scale.Because sequence SQd3 belong to the lowstand system tracts of second-order sequence,and the fan scale of lowstand system tracts of sequence SQd3 was larger than that of its highstand system tracts';Sequence SQdL2 is located in the transgressve system tracts of second-order sequence,and the delta scale of lowstand system tracts of sequence SQdL2 was equal to that of its highstand system tracts';Sequence SQdu2 developed in the highstand system tracts of second-order sequence,and the delta scale of lowstand system tracts of sequence SQdL2 was less than that its highstand system tracts'.
引文
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Fan,T.L.,Li,W.D.,1999.A successful case on sequence stratigraphy applied to the prediction of non-marine oil reservoir.Acta Petrolei Sinica,20(2):12-17(in Chinese with English abstract).
Feng,Y.L.,Xu,X.S.,2006.Syndepositional structural slope-break zone controls on lithologic reservoirs—a case from Paleogene Bohai Bay basin.Petroleum Exploration and Development,33(1):22-25(in Chinese with English abstract).
Gu,J.Y.,Zhang,X.Y.,2005.Sedimentary characteristics and sequence framework of intracontinental foreland ba-sin in the western China.Acta Sedimentologica Sinica,23(2):187-193(in Chinese with English abstract).
Hao,F.,Zhou,X.H.,Zhu,Y.M.,et al.,2009a.Charging of the Neogene Penglai 19-3field,Bohai Bay basin,China:oil accumulation in a young trap in an active fault zone.AAPG Bulletin,93(2):155-179.doi:10.1306/09080808092
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