Broadband finite-difference Q-compensated reverse time migration algorithm for tilted transverse isotropic media

Author:

Zhou Tong1ORCID,Hu Wenyi2ORCID,Ning Jieyuan3

Affiliation:

1. Formerly Peking University, Beijing 100871, China; presently Michigan State University, East Lansing, Michigan 48824, USA.(corresponding author).

2. Advanced Geophysical Technology, Inc., Sugar Land, Texas 77478, USA..

3. Peking University, School of Earth and Space Sciences, Beijing 100871, China..

Abstract

[Formula: see text]-compensated reverse time migration (Q-RTM) is effective for improving the seismic imaging quality degraded by low-[Formula: see text] anomalies. However, it is difficult to apply existing pseudospectral-based Q-RTM methods to large-scale problems due to the obstacles to high-efficient parallelization posed by the global pseudospectral operators. On the other hand, finite-difference Q-RTM is intrinsically appropriate for domain decomposition and parallel computation, thus being suitable for industrial-sized problems but facing a twofold challenge: (1) to effectively compensate the phase in a broad-bandwidth sense during the wave back-propagation process and (2) to accurately handle the tilted transverse isotropic (TTI) medium with attenuation. We have developed a new framework of finite-difference Q-RTM algorithm by expanding the linear viscoacoustic constitutive relation to a series of integer-order differential terms and a unique integral term that can decouple the amplitude and the phase to allow accurate compensation in a broader frequency range. This framework has two typical implementations: (1) optimizing the frequency-dependent phase velocity (while fixing the negative constant [Formula: see text]) and (2) optimizing the [Formula: see text] value (while fixing the frequency-dependent phase velocity). We generalize this broadband finite-difference Q-RTM algorithm to TTI media, where an artificial [Formula: see text] is applied to suppress the shear-wave artifacts induced by the acoustic TTI approximation. Numerical examples demonstrate that this Q-RTM method accurately compensates the phase and amplitude in a broad frequency range of 5–70 Hz and produces high-quality images. Due to the local nature of finite-difference operators, this algorithm is expected to outperform the existing pseudospectral-based Q-RTM methods in terms of computational efficiency and implementation convenience for real-world Q-RTM projects.

Funder

National Natural Science Foundation of China

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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