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Adding geologic prior knowledge to Bayesian lithofluid facies estimation from seismic data

机译:将地质先验知识添加到地震数据的贝叶斯岩石流相估计中

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Using inverted seismic data from a turbidite depositional environment, we have determined that accounting only for rock types sampled at the wells can lead to biased predictions of the reservoir fluids. The seismic data consisted of two volumes resulting from a (multi-incidence angle) sparse-spike amplitude variation with offset inversion. Information from a single well (well logs and petrological analysis) was used to define an initial set of lithofluid facies that characterized rock type and porefill fluid to emulate a typical exploration setting. Based on our geologic understanding of the study area, we have augmented this initial model with lithofluid facies expected in the given depositional environment, yet not sampled by the well. Specifically, the new lithofluid facies accounted for variations in the mixture type and proportions of shales and sands. The elastic property distributions of the new lithofluid facies were modeled using appropriate rock-physics models. Finally, a geologically consistent, spatially variant, prior probability of lithofluid facies occurrence was combined with the data likelihood to yield a Bayesian estimation of the lithofluid facies probability at every sample of the inverted seismic data. Applying the augmented geologic prior probabilities, we were able to generate a scenario consistent with all available data, which supports further development of the field. In contrast, using the initial, purely data- driven lithofluid facies model based on a single well, the Bayesian classification would lead to prospectivity downgrade or suboptimal development of the field. We found that limited well control in quantitative interpretation needs to be counterweighted by geologic prior information based on detailed stratigraphic interpretation, to derisk geologic scenarios without bias.
机译:使用来自浊积岩沉积环境的倒置地震数据,我们已经确定仅考虑在井中采样的岩石类型会导致储层流体的预测有偏差。地震数据由两个体积组成,这两个体积是由(多入射角)稀疏峰值幅度变化和偏移量反演所产生的。来自单个井的信息(测井和岩石学分析)用于定义岩石流体相的初始集合,这些岩石相以岩石类型和孔隙填充流体为特征,以模拟典型的勘探环境。基于我们对研究区域的地质了解,我们在给定的沉积环境中用岩石流体相扩展了该初始模型,但该井尚未进行采样。具体而言,新的岩石流体相解释了页岩和砂岩的混合类型和比例的变化。使用适当的岩石物理模型对新的岩石流体相的弹性性质分布进行了建模。最后,将岩石流体相出现的地质上一致的,空间变化的先验概率与数据似然性相结合,以在每个反演地震数据样本上得出岩石流体相概率的贝叶斯估计。应用增强的地质先验概率,我们能够生成与所有可用数据一致的方案,从而支持该领域的进一步发展。相比之下,使用基于单个井的,纯数据驱动的初始岩石流体相模型,贝叶斯分类将导致该油田的前瞻性降级或欠佳的开发。我们发现,在定量解释中有限的井控需要通过基于详细地层解释的地质先验信息来抵消,以便无偏见地跟踪地质情况。

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