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Multi-Ricker Spectral Modeling in the S-transform Domain for Enhancing Vertical Resolution of Seismic Reflection Data

机译:S-Transform域中的多Ricker光谱建模,用于增强地震反射数据的垂直分辨率

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摘要

We present a relatively straightforward methodology for extending seismic bandwidth and hence enhancing the seismic resolution by performing time-variant deconvolution. We use the generalized S-transform (GST) approach in order to properly compute the time-frequency components of the seismic reflection trace. In estimating the time-variant wavelet, we propose a spectral modeling method named multi-Ricker spectral approximation (MRA). After obtaining the estimated wavelet spectrum at each time sample, a deconvolution filter can then be built and applied in the S-transform domain. This proposed time-variant seismic enhancement method needs neither information on the subsurface attenuation model nor the assumption that the subsurface reflectivity is random. It is a data-driven methodology that is based on the seismic data only. We validate this proposed method on a synthetic and apply it to field data. Results show that, after enhancement, overall seismic bandwidth can be extended resulting in higher vertical resolution. Correlation with VSP corridor stack at well location ensures that the generated reflection details after enhancement is geologically plausible.
机译:我们提出了一种相对简单的方法,用于延伸地震带宽,从而通过执行时变碎屑来增强地震分辨率。我们使用广义的S转换(GST)方法来正确计算地震反射轨迹的时频分量。在估计时变小波中,我们提出了一种名为Multi-Ricker光谱近似(MRA)的光谱建模方法。在每个时间样本获得估计的小波谱后,然后可以在S转换域中构建并施加解卷积滤波器。这提出的时变地震增强方法既不需要关于地下衰减模型的信息,也不需要假设地下反射率是随机的。它是一种基于地震数据的数据驱动方法。我们在合成的验证中验证了该方法并将其应用于现场数据。结果表明,在增强后,可以扩展整体地震带宽,从而导致更高的垂直分辨率。井位置与VSP走廊堆栈的相关性可确保增强后产生的反射细节是地质上可粘合的。

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