Azimuthal Attenuation Elastic Impedance Inversion for Fluid and Fracture Characterization Based on Modified Linear-Slip Theory

Abstract

The seismic attenuation should be considered while accounting for the effect of anisotropy on the seismic wave propagating through a saturated fractured porous medium. Based on the modified linear-slip theory and anisotropic Gassmann’s equation, we derive an analytical expression for a linearized PP-wave reflection coefficient and an azimuthal attenuation elastic impedance (AAEI) equation in terms of fluid/porosity term, shear modulus, density, dry normal and tangential fracture weaknesses, and compressional (P-wave) and shear (S-wave) attenuation parameters in a weak-attenuation isotropic background rock containing one single set of vertical aligned fractures. We then propose an AAEI inversion method to characterize the characteristics of fluids and fractures using two kinds of constrained regularizations in such a fractured porous medium. The proposed approach is finally confirmed by both the synthetic and real data sets acquired over a saturated fractured porous reservoir.

Characterization and analysis of attenuation anisotropy in viscoelastic vertical transverse isotropic media

“…However, multiple seismic attenuation inversion approaches are only developed in an isotropic medium. Q inversion in anisotropic media is mostly used to predict fracture (Chen & Innanen, 2018; Pan et al., 2019, 2020, 2021). In addition, the approximate form of the reflection coefficient in a viscoelastic anisotropic medium is complex, and there are many parameters to be inverted (Yang et al., 2021; Zong et al., 2021).…”