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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Joint inversion of marine seismic AVA and CSEM data using statistical rock-physics models and Markov random fields
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Joint inversion of marine seismic AVA and CSEM data using statistical rock-physics models and Markov random fields

机译:使用统计岩石物理模型和马尔可夫随机场对海洋地震AVA和CSEM数据进行联合反演

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摘要

Joint inversion of seismic AVA and CSEM data requires rock-physics relationships to link seismic attributes to electric properties. Ideally, we can connect them through reservoir parameters (e.g., porosity and water saturation) by developing physical-based models, such as Gassmann's equations and Archie's taw, using nearby borehole logs. This could be difficult in the exploration stage because information available is typi-cally insufficient for choosing suitable rock-physics models and for subsequently obtaining reliable estimates of the associated parameters. The use of improper rock-physics models and the inaccuracy of the estimates of model parameters may cause mis-leading inversion results. Conversely, it is easy to derive statis-tical relationships among seismic and electric attributes and reservoir parameters from distant borehole logs. In this study, we developed a Bayesian model to jointly invert seismic AVA and CSEM data for reservoir parameters using statistical rock-physics models; the spatial dependence of geophysical and reservoir parameters were carried out by lithotypes through Markov random fields. We applied the developed model to a synthetic case that simulates a CO_2 monitoring application. We derived statistical rock-physics relations from borehole logs at one location and estimated seismic P- and S-wave velocity ratio, acoustic impedance, density, electric resistivity, lithotypes, porosity, and water saturation at three different locations by conditioning to seismic AVA and CSEM data. Comparison of the inversion results with their corresponding true values showed that the correlation-based statistical rock-physics models provide significant information for improving the joint inversion results.
机译:地震AVA和CSEM数据的联合反演需要岩石物理关系才能将地震属性与电学性质联系起来。理想情况下,我们可以通过使用附近的井眼测井开发基于物理的模型(例如Gassmann方程和Archie的拖船)来通过储层参数(例如孔隙度和水饱和度)将它们连接起来。在勘探阶段这可能很困难,因为可用的信息通常不足以选择合适的岩石物理模型并随后获得相关参数的可靠估计。使用不正确的岩石物理学模型以及模型参数估计值的不准确性可能会导致误导性的反演结果。相反,很容易从远处的井眼测井推导出地震和电学属性与储层参数之间的统计关系。在这项研究中,我们开发了一种贝叶斯模型,可以使用统计岩石物理模型联合反演地震AVA和CSEM数据以获得储层参数。地球物理参数和储层参数的空间相关性是通过马尔可夫随机场通过岩性来实现的。我们将开发的模型应用于模拟CO_2监视应用程序的合成案例。我们从一个位置的井眼测井推导出统计岩石物理关系,并根据地震AVA和CSEM数据。将反演结果与其对应的真实值进行比较表明,基于相关的统计岩石物理模型为改善联合反演结果提供了重要信息。

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