“…These approaches are often conducted in the frequency-space domain, where the multidimensional signal is embedded in Hankel/Toeplitz matrices for each fixed temporal frequency (Gao et al, 2013;Sternfels et al, 2015;Chen et al, 2016;Zhang et al, 2016Zhang et al, , 2017Carozzi and Sacchi, 2021;Oboué et al, 2021). Reduced-rank tensor completion has also been used for multidimensional seismic data recovery (Kreimer and Sacchi, 2012;Kreimer et al, 2013;Gao et al, 2015;Carozzi and Sacchi, 2019;Cavalcante and Porsani, 2021). All the aforementioned applications are deeply rooted in the following assumption: Clean and complete seismic data can be represented as low-rank matrices or tensors.…”