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A refreshing 3D view of an ancient sediment collapse and slope failure
Author(s) -
Huvenne Veerle A. I.,
Croker Peter F.,
Henriet JeanPierre
Publication year - 2002
Publication title -
terra nova
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.353
H-Index - 89
eISSN - 1365-3121
pISSN - 0954-4879
DOI - 10.1046/j.1365-3121.2002.00386.x
Subject(s) - geology , sediment , submarine pipeline , structural basin , horizon , geomorphology , geotechnical engineering , seismology , physics , astronomy
The combined analysis of high‐resolution 2D seismics and an industrial 3D seismic data volume from the western Porcupine Basin, offshore SW Ireland, revealed an unusual picture of a buried sediment collapse and slope failure. A proportionally thin (≤ 85 m) but vast (> 750 km 2 ) slab of consolidated sediments started to slide downslope, in the meantime breaking into hundreds of vertically undisturbed blocks, up to 500 m in diameter. The most probably overpressured underlying horizon seems to have liquefied and acted as a slide plane until the excess pore pressure had dissipated. Then – still very early in the slide development – the process stopped, freezing the failure at its initial stage.

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