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APPLICATION OF IMPROVED GABOR DECONVOLUTION ON ZERO-OFFSET VSP DATA USING A NOVEL SMOOTHING METHOD IN LOGARITHMIC SPECTRUM

机译:改进的Gabor Deconvoluls在对数谱中使用新颖的平滑方法进行零偏移VSP数据的应用

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摘要

Absorption phenomenon attenuates seismic signal amplitudes, reduces the vertical resolution, and hassles the detection of thin layers. The key objective of this study is the vertical resolution enhancement of zero-offset vertical seismic profile data (ZVSP) by Gabor deconvolution. According to constant Q theory, it is reliable to apply a smoothing along hyperbolic trajectories in the time-frequency domain. In conventional hyperbolic smoothing, an empirical whitening factor is added to stabilize the process. Experiments on real seismic data show that the whitening factor can smear useful information or produce artifacts. To prevent these shortcomings, we apply a logarithmic magnitude spectrum (LMS) hyperbolic smoothing on ZVSP data. As a result, by replacing divisions with subtractions whitening factor is used. Smoothing the Gabor magnitude spectrum of seismic data along hyperbolic paths in the logarithmic spectrum can obtain the magnitude of the attenuation function, eliminate the effect of source wavelet, then, estimate the source wavelet amplitude spectrum. Applying different deconvolution methods on synthetic and real data we show that the performance of the Gabor deconvolution using the LMS is better than that of other methods including Wiener deconvolution and conventional hyperbolic smoothing method.
机译:吸收现象衰减地震信号幅度,降低了垂直分辨率,并麻烦了薄层的检测。本研究的关键目标是通过Gabor Deconvolulation垂直分辨率提高零偏移垂直地震剖面数据(ZVSP)。根据常数Q理论,在时频域中沿双曲轨迹施加平滑是可靠的。在传统的双曲线平滑中,加入经验美化因子以稳定该方法。真实地震数据的实验表明,美白因素可以涂抹有用的信息或产生伪影。为防止这些缺点,我们在ZVSP数据上应用对数幅度谱(LMS)双曲线平滑。结果,通过使用减法的划分使用增性因子。在对数频谱中平滑沿着双曲线路径的地震数据的Gabor幅度谱可以获得衰减函数的大小,消除源小波的效果,然后估计源小波幅度谱。在合成和实际数据上应用不同的折卷积方法,我们表明使用LMS的Gabor Deconvolules的性能优于其他方法,包括维纳解卷积和传统的双曲线平滑方法。

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