• ISSN 2097-1893
  • CN 10-1855/P
史才旺,李正波,陈晓非. 2024. 地震波泄漏模式研究进展. 地球与行星物理论评(中英文),55(0):1-25. DOI: 10.19975/j.dqyxx.2024-005
引用本文: 史才旺,李正波,陈晓非. 2024. 地震波泄漏模式研究进展. 地球与行星物理论评(中英文),55(0):1-25. DOI: 10.19975/j.dqyxx.2024-005
Shi C W, Li Z B, Chen X F. 2024. Advances in the research of seismic-wave leaky modes. Reviews of Geophysics and Planetary Physics, 55(0): 1-25 (in Chinese). DOI: 10.19975/j.dqyxx.2024-005
Citation: Shi C W, Li Z B, Chen X F. 2024. Advances in the research of seismic-wave leaky modes. Reviews of Geophysics and Planetary Physics, 55(0): 1-25 (in Chinese). DOI: 10.19975/j.dqyxx.2024-005

地震波泄漏模式研究进展

Advances in the research of seismic-wave leaky modes

  • 摘要: 地震波在层状结构中传播时会产生频散现象,基于频散曲线特征可以反演地下速度结构. 利用从地震记录和背景噪声中提取的面波频散曲线进行反演已经成为研究近地表和岩石圈结构的重要方法. 除面波外,近年来学者们在泄漏模式及其频散的研究和应用方面取得了重要进展. 泄漏模式可以为速度结构反演提供包括纵波速度在内的约束信息,能够与面波频散反演优势互补,实现更准确、全面的速度建模. 但相比于面波,地震信号和背景噪声中的泄漏模式振幅通常较弱,因此提取泄漏模式信息对观测技术具有较高要求;另一方面,研究泄漏模式需要更复杂的理论基础和数值求解技术,所以在过去几十年间泄漏模式并未受到太多关注. 数十年来,泄漏模式理论已随着地震学、光学和声学的相关研究而日趋完善,并形成了有效的数值计算方法和工具,这为泄漏模式的实际应用奠定了重要基础. 而随着高质量、高密度观测数据的增多以及数据处理技术的进步,学者们已成功从各类型数据(天然及人工地震、背景噪声等)中提取到了泄漏模式信息,并发展了基于泄漏模式的速度结构成像方法. 目前该成像方法已成功应用于天然地震、背景噪声和勘探地震的速度建模,具有较好的应用前景. 本文首先介绍了泄漏模式的理论基础和数值计算方法,并从敏感性角度阐述了泄漏模式对速度建模的意义;随后本文通过回顾代表性的研究介绍了泄漏模式观测和应用方面的重要进展,并对已提出的几种反演手段进行了比较和分析;最后,本文还对泄漏模式在地震成像中的关键问题进行了分析和讨论.

     

    Abstract: When seismic waves propagate in layered structures, dispersion phenomena occur. Based on the characteristics of dispersion curves, underground velocity structures can be estimated. Using the surface-wave dispersion curves extracted from seismic records and ambient noise for inversion is an important method to constrain the structures of the near surface and lithosphere. In addition to surface waves, significant progress has been made in the research and application of leaky modes and their dispersion in recent years. Leaky modes can provide constraint information for velocity structure inversion, including P-wave velocity, and can compensate for the shortcomings of surface-wave dispersion inversion, which results in more accurate and comprehensive velocity modeling. However, in comparison to surface waves, the amplitude of leaky waves in seismic records and ambient noise is typically much weaker, which leads to significant challenges for the extraction of leaky modes. Furthermore, the study of leaky modes requires a more intricate theoretical framework and numerical solution techniques, which have historically limited their attention in the scientific community. Over the past decades, the theories of leaky modes have been increasingly improved with the relevant research in seismology, optics, and acoustics, which give rise to effective numerical computation tools. This has laid a solid foundation for the practical application of leaky modes. With the increase of high-quality, high-density observational data and advancements in data processing techniques, geoscientists have successfully extracted leaky mode information from various types of data, including natural and artificial earthquakes, as well as ambient noise. This has led to the development of velocity structure imaging methods based on leaky modes. Currently, this imaging approach has been successfully applied in velocity modeling for earthquakes, ambient noise, and exploration seismology, which indicates promising potential for further utilization. In this review, we begin by introducing the theories and numerical methods of leaky modes. We further elaborate on the significance of leaky modes in velocity modeling from a sensitivity perspective. Subsequently, we review several representative studies to highlight the significant advancements in observation and analyze several proposed inversion techniques. Finally, we delve into the critical issues surrounding the use of leaky modes in seismic imaging.

     

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