Please use this identifier to cite or link to this item:
http://hdl.handle.net/1893/27900
Appears in Collections: | Biological and Environmental Sciences Journal Articles |
Peer Review Status: | Refereed |
Title: | Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic |
Author(s): | Stewart, Heather A Long, David |
Issue Date: | 31-Dec-2016 |
Date Deposited: | 4-Oct-2018 |
Citation: | Stewart HA & Long D (2016) Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic. Geological Society, London, Memoirs, 46 (1), pp. 361-362. https://doi.org/10.1144/m46.94 |
Abstract: | Glacigenic debris-flows represent successive mass-flow deposits that build out a prograding wedge of sediment beyond the grounding zone of an ice sheet (e.g. Laberg & Vorren 1995; King et al. 1998). A prograding sedimentary depocentre extending from the outer shelf to the upper slope has been observed in geophysical datasets from the West Shetland margin of the Faroe–Shetland Channel, NW of the UK in the NE Atlantic. Overlapping, glacigenic debris-flows comprise the Rona and Foula wedges and provide insight into the extent and stability of the northern sector of the British Ice Sheet during the last full-glacial period (Stoker & Varming 2011). |
DOI Link: | 10.1144/m46.94 |
Rights: | Copyright 2016 The Author(s). This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0/). Published by The Geological Society of London. Publishing disclaimer: www.geolsoc.org.uk/pub_ethics |
Licence URL(s): | http://creativecommons.org/licenses/by/3.0/ |
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File | Description | Size | Format | |
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361.full.pdf | Fulltext - Published Version | 5.87 MB | Adobe PDF | View/Open |
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