Optimized rejection sampling for estimating facies probabilities from seismic data

Patrick Connolly, B. Dutton
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Abstract

Seismic inversion for facies has nonunique solutions. There are invariably many vertical facies arrays that are consistent with both a data trace and the prior information. Stochastic sampling algorithms set within a Bayesian framework can provide an estimate of the posterior probability distribution of facies arrays by finding the arrays with relatively high posterior probabilities for each data trace. Sample-by-sample facies probabilities can be estimated by measuring the proportions of each facies type at each sample location from the set of posterior facies arrays. To enable the estimation of probabilities of facies mixtures and to obtain high-quality images of facies probability curves, facies must be modeled at high resolution. The facies arrays, or vectors, on which the sampling algorithm operates, must also be long enough to allow for vertical coupling caused by the wavelet. This results in very large sample spaces. The posterior probability distribution is highly nonconvex, which, combined with the large sample space, severely challenges conventional stochastic sampling methods in obtaining convergence of the estimated posterior distribution. The posterior sets of vectors from conventional methods tend to be either correlated or have low predictabilities, resulting in biased or noisy facies probability estimates, respectively. However, accurate estimates of facies probabilities can be obtained from a relatively small number of posterior facies vectors (about 100), provided that they are uncorrelated and have high predictabilities. Full convergence of the posterior distribution is not required. A hybrid algorithm optimized rejection sampling can be designed specifically for the seismic facies probability inversion problem by combining independent sampling of the prior, which ensures posterior vectors are uncorrelated, with an optimization step to obtain high predictabilities. Tests on both real and synthetic data demonstrate better results than conventional rejection sampling and Markov chain Monte Carlo methods.
优化剔除采样,从地震数据中估算岩相概率
地震反演的面阵具有非唯一性。总有许多垂直剖面阵列与数据轨迹和先验信息一致。在贝叶斯框架内设置的随机取样算法,可以为每个数据轨迹找到后验概率相对较高的面阵列,从而估算出面阵列的后验概率分布。通过测量后验面阵列集合中每个样本位置上每种面类型的比例,可以估算出每个样本的面概率。为了估算岩相混合物的概率并获得高质量的岩相概率曲线图像,必须对岩相进行高分辨率建模。采样算法所依据的面阵列或向量也必须足够长,以考虑到小波引起的垂直耦合。这就导致了非常大的样本空间。后验概率分布是高度非凸的,再加上样本空间大,对传统随机抽样方法获得估计后验分布的收敛性提出了严峻挑战。传统方法得出的后验向量集往往要么相互关联,要么预测率很低,从而分别导致有偏差或有噪声的面概率估计。然而,只要不相关且具有较高的预测能力,就可以从数量相对较少的后验面向量(约 100 个)中获得准确的面概率估计值。后验分布不需要完全收敛。针对地震剖面概率反演问题,可以专门设计一种优化剔除采样的混合算法,将先验独立采样(确保后验向量不相关)与优化步骤相结合,以获得高预测率。对真实数据和合成数据的测试表明,该方法比传统的拒绝采样和马尔科夫链蒙特卡罗方法取得了更好的结果。
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