“…The study of DWMS became the focus of emerging research over the last two decades and the concept is readily applicable to several deep‐marine sandstone deposits across the globe including North Sea, United Kingdom (Argent et al, 2000; Duranti & Hurst, 2004), Gulf of Lions, Mediterranean Sea (Gaudin et al, 2006), Gulf of Corinth, Greece (Rubi et al, 2018), Italian Apennines (Wynn et al, 2005), Peira Cava Basin, SE France (Cunha et al, 2017), Eocene Corel Field, offshore Mozambique (Fonnesu et al, 2020), Ordos Basin, central China (X. Li et al, 2016), and Numidian Flysch, Sicily (Thomas & Bodin, 2013). Earlier, these deep‐marine sediments with diverse and heterogeneous characteristics were mainly termed as turbidites (Al‐Mufti & Arnott, 2020; Sajid et al, 2020; Sinclair & Tomasso, 2002; Stow & Smillie, 2020; L. Zhang et al, 2017). However, detailed investigations of deep‐water facies have revealed some new terminologies applicable for deep‐marine deposits for example, DWMS.…”