利用稀疏层反射率反演和径向基函数神经网络进行综合薄层分类和储层表征:案例研究

IF 1.6 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
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引用次数: 0

摘要

摘要 了解地下储层、地质特征、流体成分和油气潜力在很大程度上依赖于精确的储层特征描述。地震反演是储层特征描述中的一种关键方法,可利用地震和井记录数据近似计算下伏岩层的声阻抗和孔隙度。本研究采用了稀疏层反射率(SLR)叠后反演方法,使薄层更加明显。为了生成阻抗卷,它使用了一个预定的小波库、一个目标函数和一个正则化参数,正则化参数是一个可调参数,用于控制紧密拟合数据(最小化误拟合)与确保平滑稳定的模型和稀疏计算系数之间的平衡。本研究使用 Blackfoot 数据,利用 SLR 和径向基函数神经网络(RBFNN)估算特定区域的密度、速度、阻抗和孔隙度。根据对阻抗剖面的解释,在(1040-1065)毫秒时存在一个阻抗范围为(8500-9000)米/秒*克/立方厘米的低阻抗异常区。根据地震数据和钻孔数据之间的相关性,低阻抗区被归类为碎屑釉质砂道(储层区)。此外,还将径向基函数神经网络(RBFNN)应用到数据中,以估算孔隙度体积,并对储层带进行更彻底的检查和交叉验证反演结果。研究表明,RBFNN 技术发现的高孔隙度区、低速度区和密度区与反演结果解释的低阻抗区是相关的,这证实了釉质砂道的存在。这项研究对于了解 SLR、RBFNN 和多属性分析如何有效界定砂道至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Integrated thin layer classification and reservoir characterization using sparse layer reflectivity inversion and radial basis function neural network: a case study

Abstract

Understanding subterranean reservoirs, geological characteristics, fluid composition, and hydrocarbon potential strongly relies on precise reservoir characterization. Seismic inversion is a key method in reservoir characterization to approximate the acoustic impedance and porosity of underlying rock formations using seismic and well-log data. A sparse layer reflectivity (SLR) post-stack inversion method approach is used in this study to make thin layers more visible. To generate an impedance volume, it uses a predetermined wavelet library, an objective function, and a regularization parameter, the regularization parameter is a tunable parameter used to control the balance between fitting the data closely (minimizing the misfit) and ensuring a smooth and stable model for and sparseness computed coefficients. This study uses Blackfoot data to estimate the density, velocity, impedance, and porosity of a particular region using the SLR and Radial Basis Function Neural Network (RBFNN). According to the interpretation of the impedance section, a low impedance anomaly zone with an impedance range of (8500–9000) m/s*g/cc is present at a time of (1040–1065) ms. The low impedance zone is classified as a clastic glauconitic sand channel (reservoir zone) based on the correlation between seismic and borehole data. Further, a Radial Basis Function Neural Network (RBFNN) has been applied to the data to estimate porosity volume and to conduct a more thorough examination of the reservoir zone and cross-validate inverted results. The research demonstrates that the high porosity zone, low velocity, and density zone are discovered by the RBFNN technique, and the low impedance zone interpreted in inversion findings are correlating, which confirms the existence of the glauconitic sand channel. This research is crucial for understanding how well SLR, RBFNN, and multi-attribute analysis work to define sand channels.

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来源期刊
Marine Geophysical Research
Marine Geophysical Research 地学-地球化学与地球物理
CiteScore
2.80
自引率
14.30%
发文量
41
审稿时长
>12 weeks
期刊介绍: Well-established international journal presenting marine geophysical experiments on the geology of continental margins, deep ocean basins and the global mid-ocean ridge system. The journal publishes the state-of-the-art in marine geophysical research including innovative geophysical data analysis, new deep sea floor imaging techniques and tools for measuring rock and sediment properties. Marine Geophysical Research reaches a large and growing community of readers worldwide. Rooted on early international interests in researching the global mid-ocean ridge system, its focus has expanded to include studies of continental margin tectonics, sediment deposition processes and resulting geohazards as well as their structure and stratigraphic record. The editors of MGR predict a rising rate of advances and development in this sphere in coming years, reflecting the diversity and complexity of marine geological processes.
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