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Seismic reservoir characterization of a class-1 amplitude variation with offset turbiditic system located offshore Cote d'Ivoire, West Africa

机译:地震储层对位于西非近海科特迪瓦的抵消浊浊系统的1级振幅变化的特征

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We have evaluated a case study, in which a class-1 amplitude variation with offset (AVO) turbiditic system located offshore Cote d'Ivoire, West Africa, is characterized in terms of rock properties (lithology, porosity, and fluid content) and stratigraphic elements using well-log and prestack seismic data. The methodology applied involves (1) the conditioning and modeling of well-log data to several plausible geologic scenarios at the prospect location, (2) the conditioning and inversion of prestack seismic data for P- and S-wave impedance estimation, and (3) the quantitative estimation of rock property volumes and their geologic interpretation. The approaches used for the quantitative interpretation of these rock properties were the multiattribute rotation scheme for lithology and porosity characterization and a Bayesian lithofluid facies classification (statistical rock physics) for a probabilistic evaluation of fluid content. The result indicates how the application and integration of these different AVO- and rock-physics-based reservoir characterization workflows help us to understand key geologic stratigraphic elements of the architecture of the turbidite system and its static petrophysical characteristics (e.g., lithology, porosity, and net sand thickness). Furthermore, we found out how to quantify and interpret the risk related to the probability of finding hydrocarbon in a class-1 AVO setting using seismically derived elastic attributes, which are characterized by having a small level of sensitivity to changes in fluid saturation.
机译:我们已经评估了一个案例研究,其中位于西非海上Cote D'Ivoire的偏移(AVO)浊标系统的1级振幅变化,其特征在于岩石性质(岩性,孔隙率和液体含量)和地层元素使用符合LOG和PRESTACK地震数据。应用方法涉及(1)井 - 日志数据的调节和建模到展望位置的几个合理的地质情景,(2)P - 和S波阻抗估计的PRESTACK地震数据的调理和反演(3 )岩石产量的定量估计及其地质解释。用于定量解释这些岩石性质的方法是用于岩性和孔隙率表征的多点旋转方案,以及贝叶松流体相分类(统计岩石物理),用于流体含量的概率评估。结果表明,这些不同的避鸟和岩石物理的储层特征工作流程的应用和整合有助于我们了解浊度系统结构的关键地质地层元素及其静态岩石物理特征(例如,岩性,孔隙率和净砂厚度)。此外,我们发现如何使用地震衍生的弹性属性来量化和解释与在-1类AVO设置中找到碳氢化合物的概率相关的风险,其特征在于对流体饱和度的变化具有较小的敏感性。

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