“…Conventional seismic reflection methods can also be used for object detection by imaging PD hyperbolas in 2D and 3D seismic data sets (Bull et al., 2005; Carbon Trust, 2020; Gutowski et al., 2008; Vardy et al., 2008). As diffractions are up to two orders of magnitude weaker than reflections (Khaidukov et al., 2004), and thus difficult to detect within high‐amplitude reflection energy, a number of dedicated diffraction imaging techniques utilize reflection‐suppression methods such as Radon transforms (Bansal & Imhof, 2016), eigenvector filters (Bansal & Imhof, 2016; Guigné et al., 2014), plane‐wave deconstruction filters (Fomel et al., 2007; Ford et al., 2021), or adaptive subtraction (Khaidukov et al., 2004; Preine et al., 2020; Schwarz, 2019; Schwarz & Gajewski, 2017; Schwarz & Krawczyk, 2020). After suppression, the diffractions can be imaged via migration (Bachrach & Reshef, 2016; Ford et al., 2021; Preine et al., 2020), Radon transforms (Karimpouli et al., 2015; Nowak & Imhof, 2004), or beamforming (Guigné et al., 2014).…”