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首页> 外文期刊>Journal of Seismic Exploration >QUANTITATIVE CALCULATION OF ACQUISITION FOOTPRINTS FOR 3D LAND SEISMIC ACQUISITION GEOMETRIES
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QUANTITATIVE CALCULATION OF ACQUISITION FOOTPRINTS FOR 3D LAND SEISMIC ACQUISITION GEOMETRIES

机译:3D陆地地震采集几何图形的采集脚量的定量计算

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摘要

An inappropriate acquisition geometry can leave a strong footprint on the stack of 3D seismic data, which would reduce the accuracy of seismic processing and interpretation. However, it is difficult to completely eliminate acquisition footprints using processing methods. In this paper, we propose a quantitative method to calculate the acquisition footprints for given 3D land seismic acquisition geometries, which improves on the usually qualitative methods used in classical seismic geometry design. Our method can obtain the acquisition footprints at any target depth based on the seismic wave propagation (WRW) model in terms of matrix operators in the frequency domain. The footprint is expressed as. relative amplitudes of a stacked image of primaries for every source-receiver pair. With the proposed approach, we could quantitatively evaluate the acquisition footprints of different seismic acquisition schemes for any target depth and ultimately choose the optimal acquisition parameters that would yield the minimal possible footprint before initiating fieldwork. Through two theoretical examples, we investigate the influence two key acquisition parameters, the shot traverse spacing DS and the number of receiver lines repeated in a crossline roll-along K, have on acquisition footprints. Herein, a case study in an oilfield in China is presented by computing the footprint at different depths for different acquisition geometries. The results show that the qualities of the seismic migrations can be greatly improved by choosing the optimal geometry, which has the smallest possible acquisition footprint.
机译:不合适的采集几何结构可能会在3D地震数据的堆栈上留下较大的足迹,这会降低地震处理和解释的准确性。但是,使用处理方法很难完全消除采集足迹。在本文中,我们提出了一种定量方法来计算给定3D陆地地震采集几何图形的采集足迹,它改进了经典地震几何设计中通常使用的定性方法。根据频域中的矩阵算子,我们的方法可以基于地震波传播(WRW)模型获得任何目标深度的采集足迹。足迹表示为。每个源-接收器对的原始图像堆叠图像的相对幅度。使用提出的方法,我们可以针对任何目标深度定量评估不同地震采集方案的采集足迹,并最终选择最佳的采集参数,以便在开始野外作业之前产生最小的可能足迹。通过两个理论示例,我们研究了两个关键的采集参数,炮弹横移间距DS和沿交叉线滚动K重复的接收器行数对采集足迹的影响。本文中,通过计算不同采集几何形状在不同深度的足迹,对中国某油田进行了案例研究。结果表明,通过选择具有最小采集足迹的最佳几何形状,可以极大地改善地震迁移的质量。

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