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Finite-offset common reflection surface stack using global optimisation for parameter estimation: a land data example

机译:使用全局优化进行参数估计的有限偏移共反射面堆栈:陆地数据示例

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In recent years, several research works dealing with velocity model independent seismic imaging have been published. These methods are capable of simulating arbitrary offset seismic sections by stacking a set of measured prestack seismic data along paraxial travel-time surfaces. Hyperbolic common-reflection-surface travel-time approximation is one of the most robust descriptions, which simulates not only zero-offset but also finite-offset sections with high accuracy from noisy multi-coverage seismic data. In order to reconstruct seismic reflection events in common-offset sections, the common-reflection-surface travel-time approximation depends on five kinematic attributes (or parameters) for each selected point of the common-offset seismic section. The main challenge of this method is to provide a computationally efficient data-driven strategy for accurately determining the best set of parameters. Here, we introduce an approach for simultaneously estimating the five parameters from prestack seismic data by a very fast simulated annealing optimisation algorithm. For each sample point of the common-offset section to be simulated, we determine only one set of common reflection surface attributes corresponding to the global maximum or the event with highest coherency. We applied our method of simultaneous global optimisation on synthetic and real data examples and showed the potential of the proposed strategy to enhance the reflection events in noisy data, even with very low signal-to-noise ratio. Finally, we demonstrate the regularisation capability of our method in a land seismic data example with missing traces for near, middle, and far offsets. In order to better appreciate the field data results, we present the time-migrated sections with and without application of the proposed regularisation strategy.
机译:近年来,已经发表了一些与速度模型无关的地震成像的研究工作。这些方法能够通过沿近轴行进时间面堆叠一组测得的叠前地震数据来模拟任意偏移的地震剖面。双曲共反射面传播时间近似是最鲁棒的描述之一,它不仅可以从嘈杂的多覆盖地震数据中高精度地模拟零偏移量,而且可以模拟有限偏移量部分。为了重建共同偏移段中的地震反射事件,共同反射面行进时间近似值取决于共同偏移段的每个选定点的五个运动学属性(或参数)。该方法的主要挑战是提供一种计算有效的数据驱动策略,以准确确定最佳参数集。在这里,我们介绍了一种通过非常快速的模拟退火优化算法同时从叠前地震数据中估算五个参数的方法。对于要模拟的公共偏移部分的每个采样点,我们仅确定一组与全局最大值或具有最高相干性的事件相对应的公共反射面属性。我们在合成和真实数据示例中应用了同时全局优化的方法,并展示了所提出策略的潜力,即使在信噪比非常低的情况下,也可以增强噪声数据中的反射事件。最后,我们在陆地地震数据示例中证明了我们的方法的正则化能力,该示例缺少了近,中和远偏移的迹线。为了更好地了解现场数据结果,我们介绍了使用或不使用建议的正则化策略时的时间迁移部分。

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