Complex spherical-wave seismic inversion in anelastic media for the P-wave minimum quality factor

Author:

Cheng Guangsen1ORCID,He Chuanlin2ORCID,Zong Zhaoyun3ORCID,Liang Zhanyuan2ORCID,Yin Xingyao3ORCID,Zhang Xiaoyu2ORCID

Affiliation:

1. Qilu University of Technology (Shandong Academy of Sciences), Institute of Oceanographic Instrumentation, Qingdao, China. (corresponding author)

2. Qilu University of Technology (Shandong Academy of Sciences), Institute of Oceanographic Instrumentation, Qingdao, China.

3. China University of Petroleum (East China), School of Geosciences, Qingdao, China.

Abstract

Attenuation always exists when seismic waves propagate in underground anelastic media, especially in hydrocarbon-bearing reservoirs. Quality factor Q or attenuation factor 1/ Q can be used to quantify the seismic wave attenuation and has become an important hydrocarbon indicator. The relationship between the plane-wave reflection coefficient ([Formula: see text]) in anelastic media and P- and S-wave quality factors has been widely used in the plane-wave seismic inversion to estimate the quality factors. The [Formula: see text] provides an adequate approximation for the deeper subsurface. However, for the shallow subsurface and anelastic wavefields excited by point sources, the [Formula: see text] is inaccurate and its meaning involves some fundamental difficulties. In view of this, a Q-dependent P-P spherical-wave reflection coefficient ([Formula: see text]) in anelastic media is used here. Considering that having too many parameters to be inverted will lead to unstable and inaccurate inversion results, we further derive an approximate anelastic [Formula: see text] and anelastic spherical-wave impedance ([Formula: see text]), which are frequency dependent and are the functions of P- and S-wave velocities, density, and P-wave minimum quality factor ([Formula: see text]). Finally, a complex spherical-wave seismic inversion approach in anelastic media for the P-wave minimum quality factor is developed. Using the Bayesian inversion approach and complex convolution model, we first estimate the multilayer [Formula: see text] from the complex seismic traces with different frequencies and incidence angles. Based on the inverted angle- and frequency-dependent [Formula: see text], the P- and S-wave velocities, density, and P-wave minimum quality factor are further estimated using a nonlinear inversion tool. Synthetic examples verify the feasibility and robustness of the complex spherical-wave seismic inversion approach in anelastic media. In the shallow subsurface, the spherical-wave inversion is superior to plane-wave inversion. A field example further demonstrates the accuracy and great potential of our approach in hydrocarbon-bearing reservoir prediction.

Funder

National Natural Science Foundation of China

Natural Science Foundation of Shandong Province

the Basic Research Projects of Science, Education and Industry Integration Pilot Project of Qilu University of Technology

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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