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The possibilities of compressed-sensing-based Kirchhoff prestack migration

机译:基于压缩感知的Kirchhoff叠前迁移的可能性

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摘要

An approximate subsurface reflectivity distribution of the earth is usually obtained through the migration process. However, conventional migration algorithms, including those based on the least-squares approach, yield structure descriptions that are slightly smeared and of low resolution caused by the common migration artifacts due to limited aperture, coarse sampling, band-limited source, and low subsurface illumination. To alleviate this problem, we use the fact that minimizing the L1-norm of a signal promotes its sparsity. Thus, we formulated the Kirchhoff migration problem as a compressed-sensing (CS) basis pursuit denoise problem to solve for highly focused migrated images compared with those obtained by standard and least-squares migration algorithms. The results of various subsurface reflectivity models revealed that solutions computed using the CS based migration provide a more accurate subsurface reflectivity location and amplitude. We applied the CS algorithm to image synthetic data from a fault model using dense and sparse acquisition geometries. Our results suggest that the proposed approach may still provide highly resolved images with a relatively small number of measurements. We also evaluated the robustness of the basis pursuit denoise algorithm in the presence of Gaussian random observational noise and in the case of imaging the recorded data with inaccurate migration velocities.
机译:通常通过迁移过程获得地球的近似地下反射率分布。但是,常规的迁移算法(包括基于最小二乘法的算法)会产生结构描述,这些描述由于孔径受限,采样粗糙,带限光源和低表面照度等原因,由常见的迁移伪影引起,略有拖尾且分辨率较低。 。为了缓解此问题,我们使用一个事实,即最小化信号的L1范数会促进其稀疏性。因此,我们将Kirchhoff迁移问题公式化为基于压缩感知(CS)的追踪消噪问题,以解决与标准和最小二乘迁移算法获得的图像相比高度聚焦的迁移图像。各种地下反射率模型的结果表明,使用基于CS的偏移计算的解提供了更准确的地下反射率位置和幅度。我们使用密集稀疏的采集几何将CS算法应用于来自故障模型的合成数据图像。我们的结果表明,所提出的方法可能仍会以相对较少的测量值提供高度分辨的图像。我们还评估了在存在高斯随机观测噪声的情况下以及在以不准确的偏移速度对记录的数据进行成像的情况下,基本追踪去噪算法的鲁棒性。

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