“…Synrift rocks from the Scotian Shelf and Grand Banks region, directly south and north of the eastern Orpheus rift basin (Figs. 1a, 3), respectively, include red sandstones and shales of Late Triassic age which underlie and/or interfinger with synrift salt of Late Triassic to Early Jurassic age (Tankard et al, 1989;Wade and MacLean, 1990;MacLean and Wade, 1992;Welsink and Tankard, 2012;Weston et al, 2012). Similarly, synrift strata on the conjugate margin of Morocco consist of Late Triassic redbeds and Late Triassic-Early Jurassic synrift salt (Hafid, 2000;Hafid et al, 2006;Tari and Jabour, 2013;Saura et al, 2014;Martin-Martin et al, 2017).…”