2017
DOI: 10.1111/1365-2478.12567
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Joint PP‐ and PSV‐wave amplitudes versus offset and azimuth inversion for fracture compliances in horizontal transversely isotropic media

Abstract: We propose a robust approach for the joint inversion of PP‐ and PSV‐wave angle gathers along different azimuths for the elastic properties of the homogeneous isotropic host rock and excess compliances due to the presence of fractures. Motivated by the expression of fluid content indicator in fractured reservoirs and the sensitivity of Lamé impedances to fluid type, we derive PP‐ and PSV‐wave reflection coefficients in terms of Lamé impedances, density, and fracture compliances for an interface separating two h… Show more

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Cited by 12 publications
(2 citation statements)
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References 44 publications
(65 reference statements)
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“…The physical property parameter prediction method based on linearized rock physics inversion applies to linear or slightly nonlinear rock physical models (Zhang et al, 2020b;Pan et al, 2021). For the highly nonlinear rock physical model, the empirical formula method is used to predict the porosity (Zong and Yin, 2017;Chen et al, 2017;Pan et al, 2017;. It is to obtain a statistical empirical relationship between porosity and rock elastic parameters (such as P-wave velocity, S-wave velocity, density, and elastic impedance) by using rock physics test data and logging data and then use this statistical empirical relationship to convert the elastic parameters obtained by seismic inversion into porosity parameters.…”
Section: Porosity Inversionmentioning
confidence: 99%
“…The physical property parameter prediction method based on linearized rock physics inversion applies to linear or slightly nonlinear rock physical models (Zhang et al, 2020b;Pan et al, 2021). For the highly nonlinear rock physical model, the empirical formula method is used to predict the porosity (Zong and Yin, 2017;Chen et al, 2017;Pan et al, 2017;. It is to obtain a statistical empirical relationship between porosity and rock elastic parameters (such as P-wave velocity, S-wave velocity, density, and elastic impedance) by using rock physics test data and logging data and then use this statistical empirical relationship to convert the elastic parameters obtained by seismic inversion into porosity parameters.…”
Section: Porosity Inversionmentioning
confidence: 99%
“…Rocks located in areas with high values of strain energy density are more prone to produce ruptures. Therefore, this parameter can be used to determine the probability of internal ruptures in rocks [68]- [70].…”
Section: Sweet Spot Prediction a Strain Energy Density Distributionmentioning
confidence: 99%