Images of debris fans and other deep-sea sediments on the sea bed of the Faroe–Shetland Channel based on 3D seismic data
Authors:
- 1 April 2005
- journal article
- Published by Geological Society of London in Scottish Journal of Geology
- Vol. 41 (1) , 81-86
Abstract
Synopsis: The Faroe–Shetland Channel (FSC) is covered by 25 000 km 2 of 3D seismic data which have been used to image the morphology of the sea bed. Among many of the observed geological features, the image reveals a system of down-slope linear gullies and associated debris fans on the floor of the FSC. These gullies and fans are interpreted as the products of high-energy mass flow. These features are not observed elsewhere in the FSC and are localized t o this part of the West Shetland Margin. Their restricted geographical extent and episodic longevity implies that there must have been a significant difference in the nature of the ice margin here, possibly caused by the outflow of an ancient ice stream that fed the gully and fan systems with semi-liquid sediments on this part of the West Shetland Shelf.Keywords
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