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Conditioning of levy-stable fractal reservoir models to seismic data

机译:分形稳定储层模型对地震资料的处理

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We have developed methods of conditioning non-stationary Levy-stable geostatistical models to 3D seismic data. The technique involves adapting the sequential Levy simulation method such that the convolutional response of the realisations acceptably "matches" the seismic amplitude map. A rejection scheme is used, which requires fast repetitive simulation of gridblock columns and generation of convolutional responses. The non-stationarity of the model means that this cannot be achieved using the conventional large kriging system. We use a different, but comparably rapid method, based on storing the relevant parts of a sequential simulation calculation for the column. Working directly with the amplitude traces also has the advantage of avoiding the ambiguties and non-uniqueness involved in inverting the traces to acoustic impedance. The most difficult part of the problem is estimation of the seismic wavelet, and this is often done non-optimally. We describe a sophisticated method of estimating the wavelet, and show that this can yield better than expected results. Suitable rejection criteria are proposed, based on reasonable probabilistic models. The application of the technique is demonstrated with a field example.
机译:我们已经开发了将非平稳Levy稳定地统计模型调整为3D地震数据的方法。该技术涉及适应顺序Levy模拟方法,以使实现的卷积响应可接受地“匹配”地震振幅图。使用了拒绝方案,该方案要求网格块列的快速重复仿真和卷积响应的生成。该模型的非平稳性意味着使用常规的大型克里格系统无法实现这一点。基于存储列的顺序模拟计算的相关部分,我们使用了一种不同但相对较快的方法。直接使用幅度迹线工作还具有避免将迹线反转为声阻抗所涉及的模糊性和非唯一性的优势。问题中最困难的部分是地震子波的估计,而这通常是非最优的。我们描述了一种估计小波的复杂方法,并表明它可以产生比预期结果更好的结果。根据合理的概率模型,提出了合适的拒绝标准。通过现场实例演示了该技术的应用。

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