“…Although many Q-RTM applications are implemented to improve the resolution of seismic imaging Li et al, 2016;Wang et al, 2018;Wang et al, 2019;Chen et al, 2020), however, most of these implementations ignore the anisotropy of seismic velocity and attenuation, which will inevitably harm the imaging results. Recently, some anisotropic viscoacoustic and viscoelastic wave equations have been derived to simulate the effect of attenuation and anisotropy on wavefield propagations (Bai and Tsvankin, 2016;Da Silva et al, 2019;Hao and Alkhalifah, 2019;Qiao et al, 2019;Qiao et al, 2020;Zhu and Bai, 2019;Zhang et al, 2020). Considering the significant computational cost and the complexity of wave-mode decomposition in viscoelastic wavefield propagation, the viscoacoustic wave equation is probably a better choice for anisotropic Q-RTM (Mu et al, 2022;Qiao et al, 2022).…”