同时稀疏反褶积

E. Talarico, A. Gomes, M. Sobreira, C. Cunha
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引用次数: 0

摘要

提高地震分辨率是地球物理学界长期追求的目标,在其他应用中,为更详细地解释地震斜形、更好的地震反演和定量解释服务。稀疏反褶积方法在这一过程中起着核心作用。然而,尽管稀疏方法在单地震叠加或声波反演任务中表现良好,但其在多地震叠加体中的应用及其在弹性反演中的应用仍然是一个具有挑战性和正在进行的研究课题。难点在于如何获得反射率体积之间的高度相关性。在这项研究中,我们提出了一种新的方法,在一组具有不同反射角的地震体中进行同时稀疏反褶积(SSD)。提出的算法在估计的反射率轨迹上强制峰值的共定位,另外允许用户通过超参数控制稀疏性。与独立稀疏反褶积(ISD)相比,该方法在合成数据集和实际数据集上都得到了验证,证明了其共定位能力,并且反射率体积之间的相关性更高。由此产生的反射率体积更适合下游任务,如高分辨率振幅与角度(AVA)分析,或高分辨率弹性反演的输入。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Simultaneous Sparse Deconvolution
Increasing seismic resolution has been long pursued by the geophysical community, serving, among other applications, for more detailed interpretation of seismic clinoforms, better seismic inversion and quantitative interpretation. Sparse deconvolution methods play central role in this pursuit. However, although sparse methods have performed well for single seismic stack or acoustic inversion tasks, their application for multi-stack seismic volumes and consequent use in elastic inversion is still a challenging and ongoing research topic. The challenge is to obtain reflectivity volumes with high correlation between them. In this study, we present a new method to perform simultaneous sparse deconvolution (SSD) in a group of seismic volumes associated with different reflection angles. The proposed algorithm enforces co-localization of the spikes on the estimated reflectivity traces and additionally allows user control of the sparsity via hyperparameters. The method is validated in both synthetic and real datasets proving its co-localization capability and resulting in higher correlations between the reflectivity volumes, when compared to independent sparse deconvolution (ISD) of the seismic stacks. The resulting reflectivity volumes are, henceforth, better suited for downstream tasks such as high resolution amplitude versus angle (AVA) analysis, or input for high resolution elastic inversions.
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