“…(2021). Several studies of the evolution of the South Atlantic Ocean interpreted SDR‐related magnetic anomalies as a continuation of the oceanic crust by disregarding their geometry or the origin of the magnetic anomalies close to the coast (e.g., Chauvet et al., 2021; Collier et al., 2017; Granot & Dyment, 2015; Hall et al., 2018; Koopmann et al., 2016; Moulin et al., 2010; Rabinowitz & LaBrecque, 1979; Stica et al., 2014), which occur due to the magnetic susceptibility contrast rather than remanent magnetism (Davis et al., 2018).…”