Glacial and post-glacial sedimentary processes in the Irish Rockall Trough from an integrated acoustic analysis of near-seabed sediments (original) (raw)
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Deep towed sidescan sonar data from the Rockall Trough, west of Ireland, provides an example of how shallow sedimentary facies architecture and slope morphology, related to major submarine canyons, evolve in a deep-water basin straddling the transition from a glaciated to a non-glaciated basin margin. In the north (54° to 56° N), glacial influences were overwhelming and a stacked sequence
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