Ice-sheet dynamics through the Quaternary on the mid-Norwegian continental margin inferred from 3D seismic data ...
Reconstructing the evolution of ice sheets is critical to our understanding of the global environmental system, but most detailed palaeo-glaciological reconstructions have hitherto focused on the very recent history of ice sheets. Here, we present a three-dimensional (3D) reconstruction of the chang...
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Online Access: | https://dx.doi.org/10.17863/cam.8147 https://www.repository.cam.ac.uk/handle/1810/262856 |
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ftdatacite:10.17863/cam.8147 2024-02-27T08:40:26+00:00 Ice-sheet dynamics through the Quaternary on the mid-Norwegian continental margin inferred from 3D seismic data ... Montelli, A Dowdeswell, JA Ottesen, D Johansen, SE 2017 https://dx.doi.org/10.17863/cam.8147 https://www.repository.cam.ac.uk/handle/1810/262856 en eng Elsevier open.access Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 Fennoscandian Ice Sheet glacial geomorphology ice stream marine geology palaeo-glaciology seismic stratigraphy article-journal ScholarlyArticle JournalArticle Article 2017 ftdatacite https://doi.org/10.17863/cam.8147 2024-02-01T14:55:16Z Reconstructing the evolution of ice sheets is critical to our understanding of the global environmental system, but most detailed palaeo-glaciological reconstructions have hitherto focused on the very recent history of ice sheets. Here, we present a three-dimensional (3D) reconstruction of the changing nature of ice-sheet derived sedimentary architecture through the Quaternary Ice Age of almost 3 Ma. An extensive geophysical record documents a marine-terminating, calving Fennoscandian Ice Sheet (FIS) margin present periodically on the mid-Norwegian shelf since the beginning of the Quaternary. Spatial and temporal variability of the FIS is illustrated by the gradual development of fast-flowing ice streams and associated intensification of focused glacial erosion and sedimentation since that time. Buried subglacial landforms reveal a complex and dynamic ice sheet, with converging palaeo-ice streams and several flow-switching events that may reflect major changes in topography and basal thermal regime. Lack of ... Article in Journal/Newspaper Fennoscandian Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Fennoscandian Ice Sheet glacial geomorphology ice stream marine geology palaeo-glaciology seismic stratigraphy |
spellingShingle |
Fennoscandian Ice Sheet glacial geomorphology ice stream marine geology palaeo-glaciology seismic stratigraphy Montelli, A Dowdeswell, JA Ottesen, D Johansen, SE Ice-sheet dynamics through the Quaternary on the mid-Norwegian continental margin inferred from 3D seismic data ... |
topic_facet |
Fennoscandian Ice Sheet glacial geomorphology ice stream marine geology palaeo-glaciology seismic stratigraphy |
description |
Reconstructing the evolution of ice sheets is critical to our understanding of the global environmental system, but most detailed palaeo-glaciological reconstructions have hitherto focused on the very recent history of ice sheets. Here, we present a three-dimensional (3D) reconstruction of the changing nature of ice-sheet derived sedimentary architecture through the Quaternary Ice Age of almost 3 Ma. An extensive geophysical record documents a marine-terminating, calving Fennoscandian Ice Sheet (FIS) margin present periodically on the mid-Norwegian shelf since the beginning of the Quaternary. Spatial and temporal variability of the FIS is illustrated by the gradual development of fast-flowing ice streams and associated intensification of focused glacial erosion and sedimentation since that time. Buried subglacial landforms reveal a complex and dynamic ice sheet, with converging palaeo-ice streams and several flow-switching events that may reflect major changes in topography and basal thermal regime. Lack of ... |
format |
Article in Journal/Newspaper |
author |
Montelli, A Dowdeswell, JA Ottesen, D Johansen, SE |
author_facet |
Montelli, A Dowdeswell, JA Ottesen, D Johansen, SE |
author_sort |
Montelli, A |
title |
Ice-sheet dynamics through the Quaternary on the mid-Norwegian continental margin inferred from 3D seismic data ... |
title_short |
Ice-sheet dynamics through the Quaternary on the mid-Norwegian continental margin inferred from 3D seismic data ... |
title_full |
Ice-sheet dynamics through the Quaternary on the mid-Norwegian continental margin inferred from 3D seismic data ... |
title_fullStr |
Ice-sheet dynamics through the Quaternary on the mid-Norwegian continental margin inferred from 3D seismic data ... |
title_full_unstemmed |
Ice-sheet dynamics through the Quaternary on the mid-Norwegian continental margin inferred from 3D seismic data ... |
title_sort |
ice-sheet dynamics through the quaternary on the mid-norwegian continental margin inferred from 3d seismic data ... |
publisher |
Elsevier |
publishDate |
2017 |
url |
https://dx.doi.org/10.17863/cam.8147 https://www.repository.cam.ac.uk/handle/1810/262856 |
genre |
Fennoscandian Ice Sheet |
genre_facet |
Fennoscandian Ice Sheet |
op_rights |
open.access Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.8147 |
_version_ |
1792047550883168256 |