A facies-constrained geostatistical seismic inversion method based on multi-scale sparse representation

IF 1.8 3区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Qin Su, Xingrong Xu, Ting Chen, Jingjing Zong, Hua Wang
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引用次数: 0

Abstract

Geostatistical seismic inversion is an important method for establishing high-resolution reservoir parameter models. There is no accurate representation method for reservoir structural features, and prior information about structural features cannot be incorporated into geostatistical inversion. Based on the assumption of the sparsity of stratigraphic sedimentary features, the same type of structural feature is used to represent the sedimentary pattern of reservoirs within the same facies. Different sparse representation patterns are used to represent the differences in sedimentary patterns between facies. Although changes in depositional environment might result in the multi-scale characteristics of geological structures for varying sedimentary rhythms, this paper proposes a facies-constrained geostatistical inversion method based on multi-scale sparse representation to better accommodate such situation. Using the method of sparse representation combined with wavelet transform, the multi-scale sedimentary structural features of reservoirs are learned from well-logging data. Seismic facies and multi-scale features are used as prior information for geostatistical inversion. Further, the likelihood function is constructed using seismic data to obtain the posterior probability distribution of reservoir parameters. Finally, the accurate inversion result is obtained by using multi-scale sparse representation as a constraint in the posterior probability distribution of reservoir parameters. Compared with conventional geostatistical methods, this algorithm can better match the structural features of reservoir parameters with varying geological conditions. Field data tests have shown the effectiveness of this method in improving the accuracy and resolution of reservoir parameter structural features.

基于多尺度稀疏表示的面约束地质统计地震反演方法
地质统计地震反演是建立高分辨率储层参数模型的重要方法。储层构造特征没有准确的表示方法,构造特征的先验信息无法纳入地质统计反演。基于地层沉积特征稀疏性的假设,同一类型的构造特征用于表示同一层位内储层的沉积模式。不同的稀疏表示模式用于表示不同岩层面之间沉积模式的差异。虽然沉积环境的变化可能会导致地质构造的多尺度特征产生不同的沉积节奏,但本文提出了一种基于多尺度稀疏表示的面约束地质统计反演方法,以更好地适应这种情况。利用稀疏表示与小波变换相结合的方法,从测井数据中学习储层的多尺度沉积构造特征。地震剖面和多尺度特征被用作地质统计反演的先验信息。然后,利用地震数据构建似然函数,得到储层参数的后验概率分布。最后,利用多尺度稀疏表示作为储层参数后验概率分布的约束条件,获得精确的反演结果。与传统的地质统计方法相比,该算法能更好地匹配不同地质条件下储层参数的结构特征。现场数据测试表明,该方法能有效提高储层参数结构特征的精度和分辨率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geophysical Prospecting
Geophysical Prospecting 地学-地球化学与地球物理
CiteScore
4.90
自引率
11.50%
发文量
118
审稿时长
4.5 months
期刊介绍: Geophysical Prospecting publishes the best in primary research on the science of geophysics as it applies to the exploration, evaluation and extraction of earth resources. Drawing heavily on contributions from researchers in the oil and mineral exploration industries, the journal has a very practical slant. Although the journal provides a valuable forum for communication among workers in these fields, it is also ideally suited to researchers in academic geophysics.
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