基于深度神经网络的地震小波提取

D. Lu, J. Gao, D. Chen, H. Chen, Q. Wang
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引用次数: 3

摘要

在反射地震学中,地震小波估计对高分辨率反射率反演具有重要意义。小波估计的方法可以分为两类。一个是确定性的,另一个是统计性的。对于后者,传统方法采用谱拟合方法估计地震小波。常用的方法有基于相关性的方法、对数谱平均法和谱整形法。这些方法都假定反射系数序列(RCS)为白色,源小波为零相,在某些条件下可能无效。本文提出了一种基于深度神经网络(DNN)的地震小波提取方法。将该方法得到的小波与常用的频谱建模方法得到的小波进行了比较。然后,将得到的小波应用于HPP算法对RCS进行反演。与传统方法相比,即使源小波不为零相位,深度神经网络也能获得更精确的小波。利用得到的小波,反射率反演的分辨率得到了显著提高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Extraction of the Seismic Wavelet Based on Deep Neural Networks
In reflection seismology, seismic wavelet estimation is of great significance for high resolution reflectivity inversion. The method for wavelet estimation can be classified into two categories. One is deterministic and the other is statistic. For the latter, a conventional method uses a spectrum fitting method to estimate the seismic wavelet. The commonly used methods are correlation-based method, the log-spectrum-averaging method and spectrum-shaping method. All of these methods assume that the reflection coefficient sequence (RCS) is white and the source wavelets are zero-phase which may not be valid under certain conditions. In this paper, we propose a new approach to obtain the seismic wavelet based on deep neural network (DNN). We compare the wavelet obtained by our method with the wavelet obtained by widely used spectrum modeling method. Then, the obtained wavelet is applied to perform the inversion of the RCS using the HPP algorithm. Compared with the conventional method, DNN can achieve a more accurate wavelet even if source wavelet is not zero-phase. The resolution of reflectivity inversion is significantly enhanced by using the obtained wavelet.
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