首页> 外文期刊>Marine and Petroleum Geology >Three-dimensional facies architecture analysis using sequence stratigraphy and seismic sedimentology: Example from the Paleogene Dongying Formation in the BZ3-1 block of the Bozhong Sag, Bohai Bay Basin, China
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Three-dimensional facies architecture analysis using sequence stratigraphy and seismic sedimentology: Example from the Paleogene Dongying Formation in the BZ3-1 block of the Bozhong Sag, Bohai Bay Basin, China

机译:基于层序地层学和地震沉积学的三维相构造分析-以渤海湾盆地渤中凹陷BZ3-1区块古近纪东营组为例

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摘要

The Bohai Bay Basin is a classic non-marine rift basin in eastern China. The Paleogene Dongying sequences are the main hydrocarbon-bearing stratigraphic unit in the basin. Using three-dimensional (3-D) seismic data and one well control in the BZ3-1 Block in the western slope of the Bozhong Sag, we analyzed 3-D facies architectures of the Dongying sequences. The Dongying Formation, a second-order sequence, can be subdivided into four third-order sequences (from base to top: SQ1, SQ2, SQ3, and SQ4). The facies architecture was analyzed by using the seismic sedimentology approach based on 3-D seismic data. Sediment of the Dongying sequences was derived from the northern Shijiutuo Uplift via four major configurations of incised valleys, namely "V", "U", "W", and composite shaped incised valleys. Seismic stratal slices reveal branching and converging characteristics of the channels from upstream to downstream. On the basis of an integrated analysis of well log, core data, seismic facies based on multi-seismic attributes, three sedimentary facies (e.g., "delta", "fan-delta", and "shore" or "shallow lacustrine" facies) have been recognized. The four types of incised valleys and their evolution control the sedimentary systems in the sedimentation area. The numbers and sizes of the fans are controlled by the sedimentary systems at various scales. Incised valley-fill and deltaic sand bodies are excellent hydrocarbon reservoirs and potentially good exploration targets for the study area. The reservoir quality of sequences SQ1, SQ2, and SQ3 become better gradually from base to top. The proposed sediment dispersal patterns may aid in the prediction of potential reservoir distribution. This study also demonstrates that facies architecture analysis using sequence stratigraphy and seismic sedimentology may serve as an effective approach for constructing 3D facies models for petroleum exploration in areas lacking of well or outcrop data.
机译:渤海湾盆地是中国东部经典的非海洋裂谷盆地。古近纪东营层序是盆地中主要的含烃地层单元。利用渤中凹陷西斜坡BZ3-1区块的三维(3-D)地震资料和一口井控制,我们分析了东营层序的3-D相构造。东营组是一个二阶序列,可以细分为四个三阶序列(从底到上:SQ1,SQ2,SQ3和SQ4)。通过基于3-D地震数据的地震沉积学方法分析了相结构。东营层序的沉积物是从北石臼托隆起通过四个主要构造的切谷形成的,即“ V”,“ U”,“ W”和复合形状的切谷。地震地层切片揭示了从上游到下游通道的分支和收敛特征。在对测井,核心数据,基于多地震属性的地震相,三个沉积相(例如“三角洲”,“扇三角洲”和“海岸”或“浅湖相”相)进行综合分析的基础上已经被认可。四种类型的切谷及其演化控制着沉积区的沉积系统。风扇的数量和大小由各种规模的沉积系统控制。切开的河谷填充物和三角洲砂体是优良的碳氢化合物储层,并且是研究区域的潜在良好勘探目标。序列SQ1,SQ2和SQ3的储层质量从底部到顶部逐渐变好。提出的沉积物扩散模式可能有助于预测潜在的储层分布。这项研究还表明,使用层序地层学和地震沉积学进行相结构分析可能是在缺乏井眼或露头数据的地区构建石油勘探3D相模型的有效方法。

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