Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic
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 ob...
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ftunivstirling:oai:dspace.stir.ac.uk:1893/27900 2023-05-15T16:40:14+02:00 Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic Stewart, Heather A Long, David British Geological Survey 2016-12-31 application/pdf http://hdl.handle.net/1893/27900 https://doi.org/10.1144/m46.94 http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf en eng Geological Society of London 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 http://hdl.handle.net/1893/27900 doi:10.1144/m46.94 956283 http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf 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 http://creativecommons.org/licenses/by/3.0/ CC-BY Journal Article VoR - Version of Record 2016 ftunivstirling https://doi.org/10.1144/m46.94 2022-06-13T18:43:41Z 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). Article in Journal/Newspaper Ice Sheet University of Stirling: Stirling Digital Research Repository Laberg ENVELOPE(17.820,17.820,68.862,68.862) Rona ENVELOPE(13.943,13.943,66.985,66.985) Geological Society, London, Memoirs 46 1 361 362 |
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Open Polar |
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University of Stirling: Stirling Digital Research Repository |
op_collection_id |
ftunivstirling |
language |
English |
description |
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). |
author2 |
British Geological Survey |
format |
Article in Journal/Newspaper |
author |
Stewart, Heather A Long, David |
spellingShingle |
Stewart, Heather A Long, David Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic |
author_facet |
Stewart, Heather A Long, David |
author_sort |
Stewart, Heather A |
title |
Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic |
title_short |
Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic |
title_full |
Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic |
title_fullStr |
Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic |
title_full_unstemmed |
Glacigenic debris-flows observed in 3D seismic high-resolution seafloor imagery, Faroe–Shetland Channel, NE Atlantic |
title_sort |
glacigenic debris-flows observed in 3d seismic high-resolution seafloor imagery, faroe–shetland channel, ne atlantic |
publisher |
Geological Society of London |
publishDate |
2016 |
url |
http://hdl.handle.net/1893/27900 https://doi.org/10.1144/m46.94 http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf |
long_lat |
ENVELOPE(17.820,17.820,68.862,68.862) ENVELOPE(13.943,13.943,66.985,66.985) |
geographic |
Laberg Rona |
geographic_facet |
Laberg Rona |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
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 http://hdl.handle.net/1893/27900 doi:10.1144/m46.94 956283 http://dspace.stir.ac.uk/bitstream/1893/27900/1/361.full.pdf |
op_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 http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1144/m46.94 |
container_title |
Geological Society, London, Memoirs |
container_volume |
46 |
container_issue |
1 |
container_start_page |
361 |
op_container_end_page |
362 |
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1766030616161157120 |