Time-reverse location of microseismic sources in viscoelastic orthotropic anisotropic medium based on attenuation compensation

Time reversal is a key component of time-reverse migration and source location using wavefield extrapolation. The implementation of time reversal depends on the time symmetry of wave equations in acoustic and elastic media. This symmetry in time is no longer valid in attenuative medium. Not only the...

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Bibliographic Details
Published inApplied geophysics Vol. 17; no. 4; pp. 544 - 560
Main Authors Jie, Tang, Ying-Chang, Liu, Lei, Wen, Cong, Li
Format Journal Article
LanguageEnglish
Published Beijing Chinese Geophysical Society 01.12.2020
Springer Nature B.V
School of Geosciences,China University of Petroleum,Qingdao 266580,China
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Summary:Time reversal is a key component of time-reverse migration and source location using wavefield extrapolation. The implementation of time reversal depends on the time symmetry of wave equations in acoustic and elastic media. This symmetry in time is no longer valid in attenuative medium. Not only the velocity is anisotropic in shale oil and gas reservoirs, but also the attenuation is usually anisotropic, which can be characterized by viscoelastic orthotropic media. In this paper, the fractional order viscoelastic anisotropic wave equation is used to decouple the energy dissipation and the velocity dispersion. By changing the sign of the dissipation term during backpropagation, the anisotropic attenuation is compensated and the time symmetry is restored. The attenuation compensation time-reverse location algorithm can effectively locate the source in viscoelastic orthotropic media. Compared to cases without attenuation compensation or using isotropic attenuation compensation, this method can remove location error caused by anisotropic attenuation and improve the imaging effect of the source. This paper verifies the effectiveness of the method through theoretical analysis and model testing.
ISSN:1672-7975
1993-0658
DOI:10.1007/s11770-020-0833-7