2020
DOI: 10.1111/1365-2478.13023
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2D and 3D amplitude‐preserving elastic reverse time migration based on the vector‐decomposed P‐ and S‐wave records

Abstract: The elastic reverse time migration approach based on the vector-wavefield decomposition generally uses the scalar product imaging condition to image the multicomponent seismic data. However, the resulting images contain the crosstalk artefacts and the polarity reversal problems, which are caused by the nonphysical wave modes and the angle-dependent reduction of image amplitudes, respectively. To overcome these two problems, we develop an amplitude-preserving elastic reverse time migration approach based on the… Show more

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Cited by 15 publications
(2 citation statements)
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References 53 publications
(90 reference statements)
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“…Therefore, the main idea of our proposed approach is that we utilize the contributions of reflected PP‐ and converted PS‐wave modes in the multicomponent recordings to construct the reflectivity images of P‐ and S‐wave velocity, respectively, which is widely used in the conventional elastic and viscoelastic reverse time migration (RTM) approaches to reconstruct the PP and PS reflection images with clear physical meanings (Yan & Sava 2008; Du et al . 2012; Zhang & Shi 2019; Zhang et al. 2 020).…”
Section: Wavefield‐separation‐based Least‐squares Reverse Time Migration In Viscoelastic Mediamentioning
confidence: 99%
“…Therefore, the main idea of our proposed approach is that we utilize the contributions of reflected PP‐ and converted PS‐wave modes in the multicomponent recordings to construct the reflectivity images of P‐ and S‐wave velocity, respectively, which is widely used in the conventional elastic and viscoelastic reverse time migration (RTM) approaches to reconstruct the PP and PS reflection images with clear physical meanings (Yan & Sava 2008; Du et al . 2012; Zhang & Shi 2019; Zhang et al. 2 020).…”
Section: Wavefield‐separation‐based Least‐squares Reverse Time Migration In Viscoelastic Mediamentioning
confidence: 99%
“…The third wavefield decomposition method, which with clear physical significance and higher accuracy, is the wavefields decomposition in the wavenumber domain (Zhang and McMechan, 2010;Du et al, 2014;Zhang et al, 2020), the output decomposed P-and S-wavefields have the same amplitude, phase, and physical units as the input wavefields even in the case of inaccurate migration velocity. However, methods in the wavenumber domain suffer from expensive computation.…”
mentioning
confidence: 99%