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Direct Geostatistical Seismic Amplitude Versus Angle Inversion for Shale Rock Properties

机译:直接地统计地震振幅与页岩岩石特性的角度反转

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The purpose of seismic reservoir characterization is to predict the spatial distribution of the subsurface rock properties from a set of direct and indirect measurements. Commonly, rock property volumes are obtained in a two-steps approach. First, the elastic properties are inverted from seismic reflection data and then used to compute rock properties volumes by applying a calibrated rock physics models. Such an approach is not only time consuming but may also lead to biased results as the uncertainties related to seismic inversion may not be propagated through the entire geomodeling workflow. Here, we propose an iterative geostatistical shale rock physics seismic AVA inversion method to invert seismic reflection data directly for shale rock properties. The workflow consists of three main steps starting from shale properties model generation of brittleness, total organic carbon (TOC), and porosity using stochastic sequential simulation and cosimulation and calculation of a volume of shale. In the following step, elastic property volumes are calculated based on a calibrated shale rock physics model using the self-consistent approximation. The elastic models are then used for the calculation of the synthetic seismic data. In the final step, the misfit between synthetic and real data is calculated and used as part of the stochastic update of the model parameter space. The whole process is repeated until a minimum misfit between the observed and synthetic seismic is achieved. The proposed method is successfully tested on an onshore Lower Paleozoic shale gas reservoir in Northern Poland, and the predicted shale rock properties agree with those observed at a blind-well location.
机译:地震储层表征的目的是预测来自一组直接和间接测量的地下岩石性能的空间分布。通常,在两步方法中获得岩石性能。首先,弹性特性从地震反射数据反转,然后通过应用校准的岩石物理模型来计算岩石属性卷。这种方法不仅耗时,而且还可能导致偏置结果,因为与地震反转相关的不确定性可能不会通过整个地理模区工作流程传播。在这里,我们提出了一种迭代的地统计页岩岩石物理地震AVA反转方法,可直接转向地震反射数据,用于页岩岩石特性。工作流程由三个主要步骤组成,从页岩属性模型产生脆性,总有机碳(TOC)和使用随机顺序模拟的孔隙度和孔隙率和计算的孔隙率。在下一步骤中,使用自一致近似基于校准的页岩岩石物理模型计算弹性物质体积。然后将弹性模型用于计算合成地震数据。在最后一步中,计算合成和实际数据之间的错入并用作模型参数空间的随机更新的一部分。重复整个过程,直到达到观察到和合成地震之间的最小不足。该方法在波兰北部的陆上下古生代页岩气藏成功测试,预测的页岩岩石属性同意在盲目井位置观察的人。

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