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Denoising of pre-stack seismic data using subspace estimation methods

机译:使用子空间估计方法对叠前地震数据进行去噪

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Denoising is one of the core steps in seismic data processing flow. The seismic gather consists of multiple traces captured at different receivers. A set of receivers observe waves which are reflected from the same reflection point. Those traces need to be grouped together as they contain the same information about the earth subsurface layers. This is done by finding a common mid-point (CMP) between the source and geophones. The time delay between CMP gathered traces are corrected by the normal move out correction method but the individual traces are corrupted by noise. In this paper we, propose a method for denoising individual traces. The set of traces can be modelled as belonging to a low-dimensional subspace of an ambient signal space. This allows for construction of sparse representations of each trace in terms of other traces in the CMP gather. The resulting sparse representations are subsequently utilised to construct approximations of individual traces and thus, noise is suppressed. We constructed, the approximations using orthogonal matching pursuit. We applied proposed method to synthetic and field seismic data, the proposed technique performs better on established benchmarks while capturing the true locations of weak reflections and effectively attenuating the random noise.
机译:去噪是地震数据处理流程中的核心步骤之一。地震道集由在不同接收器处捕获的多条迹线组成。一组接收器观察从同一反射点反射的波。这些迹线需要归类在一起,因为它们包含有关地下地下层的相同信息。这是通过在源和检波器之间找到一个公共中点(CMP)来完成的。 CMP收集的迹线之间的时间延迟可以通过常规移出校正方法进行校正,但是个别迹线会被噪声破坏。在本文中,我们提出了一种对单个迹线进行去噪的方法。可以将迹线集建模为属于环境信号空间的低维子空间。这样就可以根据CMP聚集中的其他迹线构造每个迹线的稀疏表示。随后将所得的稀疏表示形式用于构造单个迹线的近似值,从而抑制了噪声。我们使用正交匹配追踪构造近似值。我们将提出的方法应用于合成和野外地震数据,在捕获微反射的真实位置并有效衰减随机噪声的同时,提出的技术在已建立的基准上表现更好。

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