“…In addition to sandy mass-transport deposits and turbidites, sandy contourites and reworked turbidites constitute important petroleum reservoirs and are an important part of the spectrum of deep-water deposits (Shanmugam, 2008a(Shanmugam, , 2012(Shanmugam, , 2013aStow et al, 2011Stow et al, , 2013Gong et al, 2013). Sandy contourites and reworked turbidites have been recognized in the Gulf of Cadiz (e.g., Nelson et al, 1993Nelson et al, , 1999Hernández-Molina et al, 2006, 2013Stow et al, 2011Stow et al, , 2013Brackenridge et al, 2013), the Brazilian Marginal basins (Viana et al, 1998;Mutti and Carminatti, 2012), the Gulf of Mexico (Shanmugam et al, 1993a(Shanmugam et al, , 1993b, in the Mozambique Basin (Palermo et al, 2014), and on the northern South China Sea margin (e.g., Zhu et al, 2010;Li et al, 2012;He et al, 2013;Gong et al, 2013;. More than 80% of 2 million barrels of oil (boe) daily production in the Brazilian marginal basins come from the Cretaceous and Tertiary deep-water sandstones, a large proportion of which has been interpreted as reworked turbidite or sandy contourites by Mutti and Carminatti (2012).…”