“…Synthesis of the plate tectonic history of the North Atlantic Ocean, based on these data, has demonstrated that three distinct phases of spreading structurally isolated the Rockall Plateau (Vogt et al, 1971;Le Pichon et al, 1972;Laughton, Berggren et al, 1971;Olivet et al, 1973;Roberts, 1975). The first phase, in Early-Middle Cretaceous time, may have contemporaneously opened the Rockall Trough and Bay of Biscay and was preceded by a rifting phase perhaps represented by the Cimmerian epeirogeny of northwest Europe (Roberts, 1971(Roberts, , 1975Roberts et al, 1973;Jones and Roberts, 1975).…”