Removal of frequency notches in marine seismic data acquired by a deeply towed source

H. Ozasa, J. Takekawa, H. Mikada
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Abstract

Summary We developed a processing method to separate and utilize long-period sea surface reflected waves by applying wavefield extrapolation processing. It would be possible to separate the sea surface reflection waves from the survey data with high accuracy using the pseudo sea surface reflection generated by downward wavefield extrapolation. In addition, it would also be possible to use the separated multiple to enhance the signal-to-noise ratio of the survey result by applying the upward wavefield extrapolation. We applied our method to the survey data obtained by the deep-towable marine seismic vibrator towed at 225 m depth to verify the effectiveness of our method. Our processing method could remove the effect of a long-period sea surface reflection, which has been a problem to realize a seismic survey with a deep-towed seismic source. In addition, our proposed method could use the decoupled reflection waves to enhance the signal strength by considering it as survey data from a mirrored source.
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深拖曳震源采集的海洋地震数据中频率缺口的去除
提出了一种利用波场外推法分离和利用长周期海面反射波的处理方法。利用波场向下外推产生的拟海面反射波,可以较高精度地从测量数据中分离出海面反射波。此外,还可以利用分离倍数进行波场向上外推,提高测量结果的信噪比。将该方法应用于225 m深拖曳海洋地震振动器的测量数据,验证了该方法的有效性。我们的处理方法可以消除长周期海面反射的影响,这一直是实现深拖曳震源地震调查的一个问题。此外,我们提出的方法可以将解耦反射波视为来自镜像源的测量数据,从而增强信号强度。
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