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首页> 外文期刊>Interpretation >Using instantaneous frequency and colored inversion attributes to distinguish and determine the sandstones facies of the Late Ordovician Mamuniyat reservoir, R-field in Murzuq Basin, Libya
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Using instantaneous frequency and colored inversion attributes to distinguish and determine the sandstones facies of the Late Ordovician Mamuniyat reservoir, R-field in Murzuq Basin, Libya

机译:使用瞬时频率和有色反演属性来区分和确定利比亚Murzuq盆地R油田晚奥陶世Mamuniyat油藏的砂岩相

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摘要

The Mamuniyat petroleum reservoir in southwestern Libya is comprised of clean sandstones and intercalated shale and sand facies that are characterized by spatial porosity variations. Seismic reflection data from the field exhibit relatively low vertical seismic resolution, side lobes of reflection wavelets, reflection interference, and low acoustic impedance contrast between the reservoir and the units underneath the reservoir, which make mapping those facies a difficult task. In the absence of broadband seismic data, optimizing frequency bands of bandlimited data can be used to suppress pseudoreflectors resulting from side-lobe effects and help to separate the clean sandstone facies of the reservoir. We have optimized the data based on our investigation of seismic frequency bands and used instantaneous frequency analysis to reveal the reflection discontinuity that is mainly associated with the reservoir boundary of the sandstone facies of the clean Mamuniyat reservoir. We also preformed rock-physics diagnostic modeling and inverted the seismic data using spectral-based colored inversion into relative acoustic impedance. The inverted impedance matches the up-scaled impedance from the well data and the inversion of relative acoustic impedance confirms the conclusion that was drawn from the instantaneous frequency results. The interpretation of facies distributions based on the instantaneous frequency was supported by the inversion results and the rock-physics models.
机译:利比亚西南部的Mamuniyat石油储层由洁净的砂岩和插层的页岩和砂岩相组成,其特征是空间孔隙度变化。来自现场的地震反射数据表现出相对较低的垂直地震分辨率,反射小波的旁瓣,反射干扰以及储层和储层下面单元之间的低声阻抗对比,这使得绘制这些相成为一项艰巨的任务。在没有宽带地震数据的情况下,可以使用优化带宽限制数据的频带来抑制由旁瓣效应引起的伪反射器,并有助于分离储层的干净砂岩相。我们根据对地震频带的调查对数据进行了优化,并使用瞬时频率分析来揭示反射不连续性,该不连续性主要与干净的Mamuniyat油藏砂岩相的油藏边界有关。我们还进行了岩石物理诊断建模,并使用基于频谱的彩色反演将地震数据反演为相对声阻抗。反向阻抗与来自井数据的放大阻抗相匹配,相对声阻抗的反向证实了从瞬时频率结果得出的结论。反演结果和岩石物理模型支持了基于瞬时频率的相分布解释。

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