2019
DOI: 10.1111/1365-2478.12842
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Seismic amplitude inversion for the transversely isotropic media with vertical axis of symmetry

Abstract: Transverse isotropy with a vertical axis of symmetry is a common form of anisotropy in sedimentary basins, and it has a significant influence on the seismic amplitude variation with offset. Although exact solutions and approximations of the PP‐wave reflection coefficient for the transversely isotropic media with vertical axis of symmetry have been explicitly studied, it is difficult to apply these equations to amplitude inversion, because more than three parameters need to be estimated, and such an inverse pro… Show more

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Cited by 30 publications
(3 citation statements)
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References 51 publications
(85 reference statements)
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“…To estimate effective properties of clays as well as shales, a mixture of different rock physics models and workflows have been used. Differential effective medium (DEM), self‐consistent approximation (SCA) and Backus averaging are the main combined models for these purposes (Zhang et al., 2019). However, the model presented here can handle all at once.…”
Section: Rock Physics Modelmentioning
confidence: 99%
“…To estimate effective properties of clays as well as shales, a mixture of different rock physics models and workflows have been used. Differential effective medium (DEM), self‐consistent approximation (SCA) and Backus averaging are the main combined models for these purposes (Zhang et al., 2019). However, the model presented here can handle all at once.…”
Section: Rock Physics Modelmentioning
confidence: 99%
“…Elastic parameters can be recovered by using pre-stack amplitude variation with offset (AVO) inversion in oil and gas exploration (Minato and Ghose, 2016;Xu et al, 2016;Zhang et al, 2019). Due to the strongly non-linear inverse problems based on the exact Zoeppritz equation, several approximate Zoeppritz equations have been proposed and used in practice.…”
Section: Introductionmentioning
confidence: 99%
“…Then, under the assumption of weak anisotropy, Rüger [25,26] derived a simplified expression for the reflection coefficient as a function of the three Thomsen's parameters. Due to the simple and linear forms, the Rüger approximation and its modified forms have become the widely used reflection coefficient expressions for AVO/AVA inversion of VTI media [27][28][29][30][31]. However, these approximations have lower accuracy at large incidence angles and are restricted to the assumptions of weak anisotropy and weak impedance contrasts, which limit the accuracy and applicability of the corresponding inversions [32,33].…”
Section: Introductionmentioning
confidence: 99%