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Super-resolution least-squares prestack Kirchhoff depth migration using the L0-norm

机译:使用L0范数的超分辨率最小二乘叠前Kirchhoff深度偏移

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摘要

Least-squares migration (LSM) is applied to image subsurface structures and lithology by minimizing the objective function of the observed seismic and reverse-time migration residual data of various underground reflectivity models.LSM reduces the migration artifacts,enhances the spatial resolution of the migrated images,and yields a more accurate subsurface reflectivity distribution than that of standard migration.The introduction of regularization constraints effectively improves the stability of the least-squares offset.The commonly used regularization terms are based on the L2-norm,which smooths the migration results,e.g.,by smearing the reflectivities,while providing stability.However,in exploration geophysics,reflection structures based on velocity and density are generally observed to be discontinuous in depth,illustrating sparse reflectance.To obtain a sparse migration profile,we propose the super-resolution least-squares Kirchhoff prestack depth migration by solving the L0-norm-constrained optimization problem.Additionally,we introduce a two-stage iterative soft and hard thresholding algorithm to retrieve the super-resolution reflectivity distribution.Further,the proposed algorithm is applied to complex synthetic data.Furthermore,the sensitivity of the proposed algorithm to noise and the dominant frequency of the source wavelet was evaluated.Finally,we conclude that the proposed method improves the spatial resolution and achieves impulse-like reflectivity distribution and can be applied to structural interpretations and complex subsurface imaging.
机译:通过最小化各种地下反射率模型的观测地震和逆时偏移残余数据的目标函数,将最小二乘偏移(LSM)应用于图像的地下结构和岩性.LSM减少了偏移伪影,增强了偏移的空间分辨率图像,并产生比标准偏移更为精确的地下反射率分布。正则化约束的引入有效地提高了最小二乘偏移的稳定性。常用的正则化项基于L2-范数,从而平滑了偏移结果例如,通过涂抹反射率,同时提供稳定性。但是,在勘探地球物理学中,通常观察到基于速度和密度的反射结构在深度上是不连续的,说明了稀疏的反射率。为了获得稀疏的迁移剖面,我们提出了通过求解L0范数来解决分辨率最小二乘Kirchhoff叠前深度偏移此外,我们引入了两步迭代的软硬阈值算法来检索超分辨率反射率分布。此外,该算法还适用于复杂的合成数据。此外,该算法对噪声的敏感性最后,我们得出结论,该方法提高了空间分辨率,实现了脉冲状的反射率分布,可用于结构解释和复杂的地下成像。

著录项

  • 来源
    《应用地球物理(英文版)》 |2018年第1期|69-77|共9页
  • 作者单位

    Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing, 100029, China;

    University of the Chinese Academy of Sciences Beijing, 100049, China;

    Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing, 100029, China;

    Beijing Research Center, Aramco China, Beijing 100102, China;

    University of the Chinese Academy of Sciences Beijing, 100049, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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