首页> 外文期刊>Geophysical Prospecting >A model-based data-driven dictionary learning for seismic data representation
【24h】

A model-based data-driven dictionary learning for seismic data representation

机译:基于模型的地震数据表示的数据驱动字典学习

获取原文
获取原文并翻译 | 示例
           

摘要

Planar waves events recorded in a seismic array can be represented as lines in the Fourier domain. However, in the real world, seismic events usually have curvature or amplitude variability, which means that their Fourier transforms are no longer strictly linear but rather occupy conic regions of the Fourier domain that are narrow at low frequencies but broaden at high frequencies where the effect of curvature becomes more pronounced. One can consider these regions as localised signal cones. In this work, we consider a space-time variable signal cone to model the seismic data. The variability of the signal cone is obtained through scaling, slanting, and translation of the kernel for cone-limited (C-limited) functions (functions whose Fourier transform lives within a cone) or C-Gaussian function (a multivariate function whose Fourier transform decays exponentially with respect to slowness and frequency), which constitutes our dictionary. We find a discrete number of scaling, slanting, and translation parameters from a continuum by optimally matching the data. This is a non-linear optimisation problem, which we address by a fixed-point method that utilises a variable projection method with (1) constraints on the linear parameters and bound constraints on the non-linear parameters. We observe that slow decay and oscillatory behaviour of the kernel for C-limited functions constitute bottlenecks for the optimisation problem, which we partially overcome by the C-Gaussian function. We demonstrate our method through an interpolation example. We present the interpolation result using the estimated parameters obtained from the proposed method and compare it with those obtained using sparsity-promoting curvelet decomposition, matching pursuit Fourier interpolation, and sparsity-promoting plane-wave decomposition methods.
机译:地震阵列中记录的平面波事件可以表示为傅立叶域中的线。但是,在现实世界中,地震事件通常具有曲率或振幅可变性,这意味着它们的傅立叶变换不再严格地线性,而是占据了傅立叶域的圆锥区域,该圆锥区域在低频时较窄,而在高频时会变宽,的曲率变得更加明显。可以将这些区域视为局部信号锥。在这项工作中,我们考虑使用时空可变信号锥对地震数据进行建模。通过锥度限制(C限制)函数(傅里叶变换存在于圆锥内的函数)或C高斯函数(傅里叶变换的多元函数)的内核缩放,倾斜和平移来获得信号锥的可变性相对于慢度和频率呈指数衰减),这构成了我们的字典。通过最佳匹配数据,我们从连续体中找到离散数量的缩放,倾斜和转换参数。这是一个非线性优化问题,我们将通过定点方法解决该问题,该方法利用了具有(1)线性参数约束和非线性参数边界约束的可变投影方法。我们观察到,对于C受限函数,内核的缓慢衰减和振荡行为构成了优化问题的瓶颈,而C-Gaussian函数可以部分克服这一瓶颈。我们通过一个插值示例演示我们的方法。我们使用从所提出的方法获得的估计参数来呈现插值结果,并将其与使用稀疏度提高的curvelet分解,匹配追踪傅里叶插值和稀疏度提高的平面波分解方法获得的结果进行比较。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号