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Non-minimum-phase wavelet estimation using second- and third-order moments

机译:使用二阶和三阶矩的非最小相位小波估计

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摘要

This paper presents a new algorithm for estimating non-minimum-phase seismic wavelets by using the second- and higher-order statistics (HOS) of the wavelets. In contrast to many, if not most, of the HOS-based methods, the proposed method does not need to assume that subsurface seismic reflectivity is a non-Gaussian, statistically independent and identically distributed random process. The amplitude and phase spectra of the wavelets are estimated, respectively, using the second-order statistics (SOS) and third-order moment (TOM) of the wavelets, which will, in turn, be derived from the HOS of the seismic traces. In our approach, the wavelets can be 'calculated' from seismic traces efficiently; no optimization or inversion is necessarily required. Very good results have been obtained by applying this method to both synthetic and real-field data sets.
机译:本文提出了一种利用小波的二阶和高阶统计量(HOS)估计非最小相位地震子波的新算法。与许多(如果不是大多数)基于HOS的方法相反,所提出的方法不需要假设地下地震反射率是非高斯的,统计独立的且分布均匀的随机过程。利用小波的二阶统计量(SOS)和三阶矩(TOM)分别估计小波的振幅谱和相位谱,这将反过来从地震道的HOS中得出。在我们的方法中,可以有效地从地震道“计算”出小波。无需优化或反转。通过将此方法应用于合成数据集和实际数据集都获得了非常好的结果。

著录项

  • 来源
    《Geophysical Prospecting》 |2005年第1期|p.149-158|共10页
  • 作者

    Wenkai Lu;

  • 作者单位

    Institute of Information Processing, Department of Automation, Tsinghua University, Beijing 100084, P. R. China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

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