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An application of vector wavefield decomposition to 3D elastic reverse time migration and field data test

机译:矢量波场分解在3D弹性逆时偏移和现场数据测试中的应用

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摘要

Wavefield separation is a crucial step in suppressing crosstalk artifacts and improving imaging quality in elastic reverse time migration (ERTM). In isotropic elastic media, the most popular wavefield separation technique is the Helmholtz decomposition. However, the Helmholtz decomposition produces pure-mode wavefields with incorrect amplitudes, phases, and physical units. In addition, when we implement multi-shot ERTM using puremode wavefields, polarity changes in the converted wave can destroy reflection events because of incoherent stack. To remedy these problems, we theoretically analyze the characteristics of amplitude and phase distortion of wavefields in the decomposition of P- and S-waves based on the Helmholtz decomposition in time-space domain, and formulate accurate wavefield decomposition and recomposition equations. In this paper, we produce vector P- and S-wavefields through the following two steps. First, we correct the amplitudes and phases of the pure-mode wavefield during the Helmholtz decomposition. Second, we obtain vector P- and S-wavefields using a wavefield recomposition method. Using the separated vector wavefields, we adopt a scalar imaging condition for ERTM. These operations enable us to produce migrated images directly with the correct amplitudes, phase, and physical units. Through several 3D numerical examples and a 2D real data example, we demonstrate that the proposed ERTM provides high-quality migrated images. The method is also feasible and sufficiently robust for imaging complex subsurface structures.
机译:在弹性反向时间迁移(ERTM)中,波场分离是抑制串扰伪影和提高成像质量的关键步骤。在各向同性弹性介质中,最流行的波场分离技术是亥姆霍兹分解。但是,亥姆霍兹分解会产生振幅,相位和物理单位不正确的纯模式波场。此外,当我们使用纯模式波场实现多次发射ERTM时,由于堆叠不相干,转换后的波中的极性变化会破坏反射事件。为了解决这些问题,我们基于时空域的亥姆霍兹分解,从理论上分析了P波和S波分解中波场的振幅和相位失真的特征,并建立了精确的波场分解和重构方程。在本文中,我们通过以下两个步骤产生矢量P和S波场。首先,我们在亥姆霍兹分解过程中校正纯模波场的幅度和相位。其次,我们使用波场重组方法获得矢量P和S波场。使用分离的矢量波场,我们为ERTM采用了标量成像条件。这些操作使我们能够直接以正确的幅度,相位和物理单位生成迁移的图像。通过几个3D数值示例和2D实际数据示例,我们证明了所提出的ERTM提供了高质量的迁移图像。该方法对于成像复杂的地下结构也是可行的并且足够鲁棒。

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  • 来源
    《Computers & geosciences》 |2019年第10期|112-131|共20页
  • 作者单位

    China Univ Petr Sch Geosci Qingdao 266580 Shandong Peoples R China|Qingdao Natl Lab Marine Sci & Technol Lab Marine Mineral Resources Qingdao 266071 Shandong Peoples R China;

    Chinese Acad Geol Sci Beijing 100037 Peoples R China;

    China Univ Petr Sch Geosci Qingdao 266580 Shandong Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Geophysics; Seismology; Algorithms;

    机译:地球物理学;地震学演算法;

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