利用(3S)谱蓝化、谱平衡和随机反演提高Fluvio三角洲环境地震反演分辨率

A. Maulana
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引用次数: 0

摘要

在油气田勘探开发中,地质建模阶段的准确性至关重要。地震反演是提高模拟精度的因素之一。地震反演作为估计协同克里格的辅助资料,具有重要的意义。地震反演的结果在分辨率方面往往是有限的。由于无法分离地下地质事件,如果仍将其用于岩石性质建模,将是不稳定的。因此,本研究提出了一种综合的地震反演增强方法,即3S方法。结合谱蓝化、谱平衡、随机反演等3S技术,有望解决薄层地震反演中存在的问题。光谱蓝化旨在通过分析井数据的斜率谱、带通和分析反褶积算子来增加蓝色光谱的优势。在该方法中,利用井资料的光谱来分析一般地震资料中不存在的蓝色光谱分量的斜率。这个过程将产生一个反卷积算子小波,增加了蓝色光谱区域的幅度谱。此外,谱平衡是一种可以平衡振幅谱的形状,使其类似于平台形状的特征。该方法的基础是在几个频率范围内进行带通,并结合每个频率的幅度归一化处理。该方法旨在使每个频谱区间的优势均衡。最终的结果将是一个体积合并频谱,将其重新统一为一个更平衡的地震频谱立方体。采用基于蓝谱优势较好的地震资料的地震反演模型。利用该方法的输出,可以在地震谱的上限处实现数据反演过程的最大化。采用随机反演方法进行基于地质统计学的地震反演,并将基于模型的反演结果作为输入数据的趋势指南来实现,进一步提高了分辨率。为了对反演结果提供各向异性约束,需要一个变异函数模型。他们使用确定性倒立方体作为初始横向变异函数模型,并将升级井数据作为实际的垂直变异函数模型。迄今为止,共完成了5个随机地震反演实现。对每次反演结果进行QC和QA,确保反演结果具有良好的可靠性。采用均方根误差法、决定系数法和性能差法进行可靠性分析。将正演模拟地震与实际地震进行对比,并与实际声阻抗进行反演。可以看出,地震增强方法可以显著提高健康度与地震活动性的相关性。此外,随机增强可以为地质统计不确定性输出提供选项,从而有效地提高井间的相关性。该方法具有通过最大化地震数据和进行地质统计实现来提高多重分辨率的优点。这样就可以将异常与地下地质事件进行最优的分离和描述。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seismic Inversion Resolution Enhancement With (3S) Spectral Blueing, Spectral Balancing, and Stochastic Inversion on Fluvio Deltaic Environment
The accuracy of the geomodelling stage is vital in the exploration and development of oil and gas fields. One of the many factors that can improve the precision of the modeling is seismic inversion. As secondary data in estimating collocated co-kriging, seismic inversion is notable. The results of seismic inversions are often limited in terms of resolution. It is precarious if it is still used for rock property modeling because of the inability to separate subsurface geological events. Therefore, this research offers an integrated seismic inversion enhancement method, namely the 3S method. Using a combination of 3S, namely Spectral Blueing, Spectral Balancing, and Stochastic Inversion, it is expected to give a solution in overcoming issues in thin-bed seismic inversion. Spectral Blueing aims to increase the dominance of Blue Spectrum by analyzing the slope spectrum of the well data, bandpassing, and analyzing the deconvolution operator. In this method, the spectrum of the well data is used to analyze the slope of the blue spectrum component, which is absent in seismic data in general. This process will produce a deconvolution operator wavelet that increases the amplitude spectrum in the blue spectrum area. In addition, spectral balancing is a feature that can balance the shape of the amplitude spectrum to resemble a plateau shape. This approach's base is bandpassing in a few frequency ranges combined with each frequency's amplitude normalization process. This approach aims to equalize the dominance in each spectrum interval. The final result will be a volume merging spectrum to re-unite it into a more balanced seismic spectral cube. The seismic inversion model is applied based on seismic data with better blue spectrum dominance. The data inversion process can be maximized at the upper limit of the seismic spectrum by using this method's output. The improved resolution was further improved using the Stochastic Inversion method by performing a geostatistics-based seismic inversion and realization with the results of a model-based inversion as a trend guide for input data. A variogram model is required to provide an anisotropic constraint on the inversion results. They are using a deterministic inverted cube as the initial lateral variogram model and upscaling well data as the actual vertical variogram model. A total of 5 stochastic seismic inversion realizations have been produced. QC and QA are performed on each inversion result to ensure the inversion results have good reliability. Reliability analysis was carried out using the Method of RMS error, coefficient of determination, and property difference. The forward modeled seismic is compared with the actual seismic, and the inverted acoustic impedance is performed with the actual acoustic impedance. It can be seen that the seismic enhancement method can significantly increase the wellness and seismicity correlation. In addition, stochastic enhancement can effectively improve the correlation of wells by providing options for geostatistical uncertainty outputs. This method provides the advantage of increasing multiple resolutions by maximizing seismic data and carrying out geostatistics realization. So that anomalies and subsurface geological events can be separated and described optimally.
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