陆地数据三维表面相关多重消除的最小二乘多重成像

Brandon Li, M. Miorali, K. Mills, G. Poole
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引用次数: 0

摘要

浅层反射镜会产生与表面相关的倍数,会降低图像质量,妨碍振幅分析。通常,在陆地地震数据中,严重的噪声水平和近地表的复杂性使得地表多次波难以识别和去除。本文提出了一种以短周期和中期表面倍数为目标的最小二乘多重成像(LSMI)驱动去多重成像方法。该过程包括对产生反射率的浅层多次进行反演,然后将其用于驱动多次建模。该方法允许真实振幅建模,因此在减法阶段需要最小的自适应。我们在阿尔及利亚获得的高密度土地数据集上演示了这种方法。结果表明,与传统的一次成像方法相比,多发生器成像具有更好的近地表照度和连续性。在近角存在的强多重能量在很大程度上被抑制,导致较少的振铃和更可解释的地震图像。与表面一致反褶积相比,所提出的去倍数方法扩展了被衰减的混响量,这对低频倍数尤其有效。
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Least-Squares Multiple Imaging for 3D Surface-Related Multiple Elimination on Land Data
Shallow reflectors which generate surface related multiples, can deteriorate image quality and hamper amplitude analysis. Typically, in land seismic data, the severe noise level and near-surface complexity make surface multiples difficult to identify and remove. In this paper, we present a least-squares multiple imaging (LSMI) driven de-multiple method which targets short and medium period surface multiples. The process involves inversion for a shallow multiple generating reflectivity, which is then used to drive the multiple modeling. The method allows true amplitude modeling, so minimal adaption is required at the subtraction stage. We demonstrate this method on a high-density land dataset acquired in Algeria. The results show that the multiple generator image gives better near-surface illumination and continuity compared to the conventional primary imaging approach. The strong multiple energy present in the near angle is largely suppressed, leading to less ringing and a more interpretable seismic image. Compared with surface-consistent deconvolution, the proposed de-multiple approach extends the amount of reverberation being attenuated, this is particularly effective on low-frequency multiples.
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