Sub-bottom profilers are used across shallow and deep oceanic waters with several applications, such as sea-level studies (e.g., Bastos et al., 2010; Ko?a, 2015; Aquino da Silva et al., 2016; Yoo et al., 2016), sedimentation process (e.g., Miller et al., 2013; Alves and de Mahiques, 2019), gas seeps (e.g., Benites et al., 2015; Michel et al., 2017), geomorphology (e.g., Jobe et al., 2011; Gomes et al., 2016), and others. Marine magnetometer data have also been used for most various studies, as archeological (Boyce et al., 2004), environmental (Boyce et al., 2001), engineering (Yu et al., 2007), and geological, mainly for mineral exploration (Dehler and Potter, 2002) and academic purposes (Müller et al., 1997). Combining both techniques enhances considerably the possibilities of geological and oceanographic interpretation, as multi-data surveys in marine environments allow complementary studies (e.g., Kadima et al., 2011; Demir et al., 2012).
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