Ab'/> Applying a probabilistic seismic-petrophysical inversion and two different rock-physics models for reservoir characterization in offshore Nile Delta
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Applying a probabilistic seismic-petrophysical inversion and two different rock-physics models for reservoir characterization in offshore Nile Delta

机译:在海上尼罗河三角洲施加概率地震岩石物理反演及两种不同岩石物理模型在尼罗河三角洲

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AbstractWe apply a two-step probabilistic seismic-petrophysical inversion for the characterization of a clastic, gas-saturated, reservoir located in offshore Nile Delta. In particular, we discuss and compare the results obtained when two different rock-physics models (RPMs) are employed in the inversion. The first RPM is an empirical, linear model directly derived from the available well log data by means of an optimization procedure. The second RPM is a theoretical, non-linear model based on the Hertz-Mindlin contact theory. The first step of the inversion procedure is a Bayesian linearized amplitude versus angle (AVA) inversion in which the elastic properties, and the associated uncertainties, are inferred from pre-stack seismic data. The estimated elastic properties constitute the input to the second step that is a probabilistic petrophysical inversion in which we account for the noise contaminating the recorded seismic data and the uncertainties affecting both the derived rock-physics models and the estimated elastic parameters. In particular, a Gaussian mixture a-priori distribution is used to properly take into account the facies-dependent behavior of petrophysical properties, related to the different fluid and rock properties of the different litho-fluid classes. In the synthetic and in the field data tests, the very minor differences between the results obtained by employing the two RPMs, and the good match between the estimated properties and well log information, confirm the applicability of the inversion approach and the suitability of the two different RPMs for reservoir characterization in the investigated area.
机译:<![cdata [ 抽象 我们应用两步概率地震岩石物理反演,以表征碎屑,气体饱和水库的表征位于海上尼罗三角洲。特别是,我们讨论并比较在反转中使用两种不同的岩石物理模型(RPMS)时获得的结果。第一个RPM是一种经验,线性模型通过优化过程直接从可用井日志数据派生。第二个RPM是基于赫兹思路接触理论的理论,非线性模型。反转过程的第一步是贝叶斯线性化幅度与角度(AVA)反转,其中弹性特性和相关的不确定因素被从堆叠的叠层地震数据推断出来。估计的弹性特性构成了第二步的输入,这是一种概率岩石物理反演,其中我们考虑了污染记录的地震数据的噪声和影响衍生岩石物理模型的不确定性和估计的弹性参数。特别地,使用高斯混合物a-priori分布用于适当考虑到岩石物理性质的相依赖性行为,与不同的立体流体类别的不同流体和岩石性能有关。在合成和现场数据测试中,通过采用两个RPM而获得的结果之间的差异非常差异,以及估计的性能和井的日志信息之间的良好匹配,证实了反转方法的适用性和两者的适用性研究区域中的储层表征的不同RPMS。

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