%P 2471-2493
%I Blackwell Publishing Ltd
%A A.A. Babasafari
%A D.P. Ghosh
%A A.M. Ahmed Salim
%A M. Kordi
%V 68
%T Lithology-dependent seismic anisotropic amplitude variation with offset correction in transversely isotropic media
%J Geophysical Prospecting
%L scholars12692
%O cited By 4
%N 8
%R 10.1111/1365-2478.13001
%D 2020
%K Elasticity; Lithology; Seismic prospecting; Seismic response; Seismic waves; Well logging, Amplitude variation with offsets; Anisotropic correction; Lithology identification; Pre-stack seismic data; Reflection boundaries; Reflection interfaces; Reservoir characterization; Transversely isotropic medias, Anisotropy, amplitude; AVO method; correction; lithology; prestack migration; seismic anisotropy; seismic data; seismic reflection; transverse isotropy; well logging
%X Analysis of amplitude variation with offset is an essential step for reservoir characterization. For an accurate reservoir characterization, the amplitude obtained with an isotropic assumption of the reservoir must be corrected for the anisotropic effects. The objective is seismic anisotropic amplitude correction in an effective medium, and, to this end, values and signs of anisotropic parameter differences (�δ and �ε) across the reflection interfaces are needed. These parameters can be identified by seismic and well log data. A new technique for anisotropic amplitude correction was developed to modify amplitude changes in seismic data in transversely isotropic media with a vertical axis of symmetry. The results show that characteristics of pre-stack seismic data, that is, amplitude variation with offset gradient, can be potentially related to the sign of anisotropic parameter differences (�δ and �ε) between two layers of the reflection boundary. The proposed methodology is designed to attain a proper fit between modelled and observed amplitude variation with offset responses, after anisotropic correction, for all possible lithofacies at the reservoir boundary. We first estimate anisotropic parameters, that is, δ and ε, away from the wells through Backus averaging of elastic properties resulted from the first pass of isotropic pre-stack seismic inversion, on input data with no amplitude correction. Next, we estimate the anisotropic parameter differences at reflection interfaces (values and signs of �δ and �ε). We then generate seismic angle gather data after anisotropic amplitude correction using Rüger's equation for the P-P reflection coefficient. The second pass of isotropic pre-stack seismic inversion is then performed on the amplitude-corrected data, and elastic properties are estimated. Final outcome demonstrates how introduced methodology helps to reduce the uncertainty of elastic property prediction. Pre-stack seismic inversion on amplitude-corrected seismic data results in more accurate elastic property prediction than what can be obtained from non-corrected data. Moreover, a new anisotropy attribute (ν) is presented for improvement of lithology identification. © 2020 European Association of Geoscientists & Engineers