“…The presence and disruption of graphite‐bearing conductors is one of the main exploration criteria for URU deposits in the Athabasca Basin, reflecting the presence of graphite‐rich fault zones within metasedimentary rocks (Hoeve & Sibbald, 1978; Jefferson et al., 2007; Kerr, 2010; Marlatt & Kyser, 2011; Potter & Wright, 2015). In addition to facilitating fault reactivation (Kyser et al., 1989; Song et al., 2022; Yeo & Potter, 2010), graphite within the metasedimentary rocks is a potential reductant to precipitate uranium from the oxidized basin brines (e.g., Alexandre et al., 2005; Dargent et al., 2015; Hoeve & Quirt, 1984; Hoeve & Sibbald, 1978; Kyser et al., 1989; Landais et al., 1993; Pascal, Ansdell, et al., 2016; Pascal, Boiron, et al., 2016; Potter & Wright, 2015; Martz et al., 2017, 2019; Yeo & Potter, 2010).…”