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Time-varying wavelet estimation and its applications in deconvolution and seismic inversion

机译:时变小波估计及其在反卷积和地震反演中的应用

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Wavelet holds an essential role in seismic data processing and characterization, for examples deconvolution and seismic inversion. Unfortunately, wavelet is an unknown data. Several existing methods attempt to estimate and extract the wavelet fromseismic data. However, the methods give only a single wavelet from one seismic trace. When seismic data are non-stationer,single wavelet usage will cause a problem, that is raising the error. This paper proposes a time-varying wavelet estimationmethod to accommodate this problem. It uses matrix diagonalization to estimate a set of wavelets. Next, the time-varyingwavelet is applied to deconvolution and seismic inversion. The experiment shows that time-varying wavelet improves theresults in both deconvolution and seismic inversion. The errors decreased and spectrum bandwidth broadened.
机译:小波在地震数据处理和表征中起着至关重要的作用,例如反卷积和地震反演。不幸的是,小波是未知数据。现有的几种方法试图从地震数据中估计和提取小波。但是,这些方法仅从一条地震道中给出单个小波。当地震数据不平稳时,单个小波的使用会引起问题,从而增加了误差。本文提出了一种时变的小波估计方法来解决这个问题。它使用矩阵对角化来估计一组小波。接下来,将时变小波应用于反卷积和地震反演。实验表明,时变小波改善了反褶积和地震反演的结果。误差减少,频谱带宽扩大。

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