调和地质与地球物理:估计地震振幅反演的先验相概率。第一部分,理论

K. Epov
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引用次数: 0

摘要

提出了一种将地质知识定量地结合到地震反演过程中的方法。沉积盆地的沉积环境和地质演化信息以及测井解释和石油弹性建模数据不仅可以用于背景模型建立和反演正则化,还可以用于反演结果解释和储层物性预测。该方法基于使用所谓的“广义地质变量”或g因子对地质模型进行参数化。这些变量提供了观察到的或预期的相范围的定量描述。模型的拓扑和度量性质由一组参考沉积环境和相转换概率的估计来定义。该方法旨在解决在贝叶斯框架内所需的先验相概率估计的一个众所周知的问题。它可以应用于涉及确定性或随机反转算法的工作流中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reconciling Geology with Geophysics: Estimating A-Priori Facies Probabilities for Seismic Amplitudes Inversion. Part 1, Theory
An approach to quantitative incorporation of geological knowledge into the seismic inversion process is presented. Information about depositional environments and geological evolution of the sedimentary basin along with well logs interpretation and petro-elastic modeling data are used not only for background model building and inversion regularization, but also for inversion results interpretation and reservoir properties prediction. The method is based on the parameterization of the geological model using so-called “generalized geological variables” or G-Factors. These variables provide a quantitative description of the range of observed or expected facies. Topological and metric properties of the model are defined by a set of reference sedimentary environments and estimates of facies transitions probabilities. The method aims at solving a well-known problem of a-priori facies probabilities estimation required within the Bayesian framework. It can be applied in workflows involving either deterministic or stochastic inversion algorithms.
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