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Seismic Facies Analysis for Fracture Detection : a Powerful Technique

机译:裂缝检测的地震相分析:一项强大的技术。

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Fractured reservoir analysis requires an accurate delineation offracture corridors, as well as an estimate of the fracture density.Fracture corridors are often closely associated with faults, large andsmall. 3D seismic data is of great help for minor “sub-seismic” faultdetection and characterization, small faults being often expressed asvery subtle zones of deformation (discontinuities), with no obviousoffset of seismic reflections.A large number of seismic attributes are known to highlightdiscontinuities. They can be horizon-based, such as curvature, dip,edge, azimuth or based on the 3D seismic trace variability in a givenneighborhood such as “coherence-type” attributes or computed afterFourier or Hilbert transform as instantaneous phase or frequency.This paper proposes, in a large Upper Cretaceous carbonate reservoironshore UAE, to use jointly a set of selected “fracture relevant”attributes in a multi-variable statistical process called Seismic FaciesAnalysis (SFA). The resulting seismic facies map delineates areasspatially oriented towards two directions that are consistent with thegeneral structural knowledge of the field. Analyzing seismic attributedistributions within each seismic facies gives a preliminaryinterpretation of these seismic facies in terms of fracture density. Thevalidation of this interpretation with well data (BHI, core anddynamic data) delivers an accurate map of fracture occurrence. Thismap is then used to interpret structural lineaments and constrainstochastic realizations of the fracture model.
机译:裂缝性储层分析需要准确描述 裂缝通道,以及裂缝密度的估算值。 断裂走廊通常与断层,大断层和大断层密切相关。 小的。 3D地震数据对于较小的“亚地震”断层有很大帮助 检测和表征,小故障通常表示为 非常细微的变形区域(不连续),没有明显的变化 地震反射的偏移量。 众所周知,大量的地震属性可以突出显示 不连续性。它们可以基于地平线,例如曲率,倾角, 边缘,方位角或基于给定3D地震道的可变性 邻域(例如“相干类型”属性)或 傅里叶或希尔伯特变换为瞬时相位或频率。 本文提出在一个大型上白垩统碳酸盐岩储层中 陆上阿联酋,共同使用一组选定的“与裂缝相关的” 属性在称为地震相的多变量统计过程中 分析(SFA)。生成的地震相图勾勒出区域 在空间上朝向与 该领域的一般结构知识。分析地震属性 每个地震相内的分布给出了初步的 用裂缝密度解释这些地震相。这 用油井数据(BHI,岩心和 动态数据)提供准确的裂缝发生图。这 然后使用地图来解释结构轮廓和约束 断裂模型的随机实现。

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