Interbed demultiple using Marchenko redatuming on 3D field data of the Santos basin

M. Staring, C. Wapenaar
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引用次数: 7

Abstract

We apply Marchenko redatuming using an adaptive double-focusing method to 3D field data of the Santos basin, Brazil. This method was already successfully applied to 2D field data and we now study the acquisition geometry and preprocessing requirements in 3D. We start from 3D synthetic data modeled on a dense grid of colocated sources and receivers and decimate down to a realistic NAZ streamer acquisition. The synthetic tests show that the sail line spacing and the missing outer cables are the acquisition parameters with the strongest effect on Marchenko redatuming. We can interpolate for the sail line spacing and the near offsets, but the missing outer cables are unfortunately a limitation of the acquisition. After applying the proposed interpolation to 3D field data, interbed multiples are successfully predicted and subtracted from the target area, resulting in a significant improvement in the geological interpretation. Naturally, the pre-processing requirements and challenges strongly depend on the acquisition geometry and the geology of the area under investigation (e.g. water depth, shape of the overburden, maximum dip). Hence, these tests only give a general idea about the limitations of 3D Marchenko redatuming
利用Marchenko重新数据对Santos盆地的三维现场数据进行互层分解
采用自适应双聚焦方法对巴西Santos盆地的三维野外数据进行了Marchenko重拾。该方法已成功应用于二维现场数据,现在我们研究三维的采集几何形状和预处理要求。我们从三维合成数据开始建模在一个密集的网格上的并置源和接收器,并减少到一个现实的NAZ拖缆采集。综合试验表明,帆线间距和漏缆是对马尔琴科重测影响最大的采集参数。我们可以对帆线间距和近偏移进行插值,但不幸的是,缺失的外电缆是采集的限制。将所提出的插值方法应用于三维野外数据后,成功地预测并减去了目标区域的互层倍数,从而显著提高了地质解释水平。当然,预处理的要求和挑战很大程度上取决于所调查区域的采集几何形状和地质情况(例如水深、覆盖层形状、最大倾角)。因此,这些测试只给出了关于3D马尔琴科重定的局限性的一般概念
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