“…East of the Boltana Anticline, the sequences are dominated by submarine channel-fill turbidite bodies (Mutti et al, 1988), which are separated predominantly by upper slope-derived MTDs Pickering and Corregidor, 2005). Westwards from the Boltana Anticline, the succession is characterised by non-channelised sandstone lobes (Mutti and Ricci Lucchi, 1972;Mutti, 1977;Remacha et al, 2005). Cronin, 1994), showing upwards thinning from 1.3 m (base of channel) to 14.2 m, through Units A (0-8.6 m) and B (8.6-13.7 m).…”