“…The weak reflectivities, complex scattering, and noisy data are the main characteristics of the Larder Lake seismic data (Naghizadeh et al., 2021). The MF methods are capable of generating high‐resolution stack sections in this type of noisy environment and are better suited to model the moveout of diffracted waves (Belfer et al., 2008; Berkovitch et al., 2004, 2008, 2011, 2012; Borghi et al., 2017; Chang, Zhang, et al., 2019; Curia et al., 2017; Gurevich et al., 2002; Landa et al., 1999). However, the early implementations of MF methods did not consider cross‐dip effects and horizontal variation of source and receiver coordinates (or variations in the azimuth of each source–receiver pair) in 3D space (Jodeiri Akbari Fam et al., 2021a).…”