Middle Pleistocene glacial and glaciomarine sedimentation in the west central North Sea
A sequence of Middle Pleistocene (approximately early ‘Cromerian Complex’) sediments has been subdivided into subglacial, proximal glaciomarine, distal glaciomarine and marine facies. The subglacial facies represents lodgement till deposited during the final stages of ice‐sheet advance. At the onset...
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crwiley:10.1111/j.1502-3885.1985.tb00920.x 2024-06-02T08:08:11+00:00 Middle Pleistocene glacial and glaciomarine sedimentation in the west central North Sea STOKER, MARTYN S. BENT, ALISTAIR 1985 http://dx.doi.org/10.1111/j.1502-3885.1985.tb00920.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1985.tb00920.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1985.tb00920.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 14, issue 4, page 325-332 ISSN 0300-9483 1502-3885 journal-article 1985 crwiley https://doi.org/10.1111/j.1502-3885.1985.tb00920.x 2024-05-03T12:00:00Z A sequence of Middle Pleistocene (approximately early ‘Cromerian Complex’) sediments has been subdivided into subglacial, proximal glaciomarine, distal glaciomarine and marine facies. The subglacial facies represents lodgement till deposited during the final stages of ice‐sheet advance. At the onset of ice‐sheet retreat, streams deposited their load into a shallow‐water; glaciomarine environment; gravelly sediments immediately in front of the ice‐grounding line and finer material, in suspension, to more distal areas. Ice‐rafting, slumping and traction currents were also active within the glaciomarine environment. The lithofacies characteristics of this sequence are consistent with deposition from a grounded tidewater ice‐sheet. The glacigenic succession is restricted to the Forth Approaches area, which implies that the ice‐sheet had a limited offshore extent. Article in Journal/Newspaper Ice Sheet Wiley Online Library Boreas 14 4 325 332 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
A sequence of Middle Pleistocene (approximately early ‘Cromerian Complex’) sediments has been subdivided into subglacial, proximal glaciomarine, distal glaciomarine and marine facies. The subglacial facies represents lodgement till deposited during the final stages of ice‐sheet advance. At the onset of ice‐sheet retreat, streams deposited their load into a shallow‐water; glaciomarine environment; gravelly sediments immediately in front of the ice‐grounding line and finer material, in suspension, to more distal areas. Ice‐rafting, slumping and traction currents were also active within the glaciomarine environment. The lithofacies characteristics of this sequence are consistent with deposition from a grounded tidewater ice‐sheet. The glacigenic succession is restricted to the Forth Approaches area, which implies that the ice‐sheet had a limited offshore extent. |
format |
Article in Journal/Newspaper |
author |
STOKER, MARTYN S. BENT, ALISTAIR |
spellingShingle |
STOKER, MARTYN S. BENT, ALISTAIR Middle Pleistocene glacial and glaciomarine sedimentation in the west central North Sea |
author_facet |
STOKER, MARTYN S. BENT, ALISTAIR |
author_sort |
STOKER, MARTYN S. |
title |
Middle Pleistocene glacial and glaciomarine sedimentation in the west central North Sea |
title_short |
Middle Pleistocene glacial and glaciomarine sedimentation in the west central North Sea |
title_full |
Middle Pleistocene glacial and glaciomarine sedimentation in the west central North Sea |
title_fullStr |
Middle Pleistocene glacial and glaciomarine sedimentation in the west central North Sea |
title_full_unstemmed |
Middle Pleistocene glacial and glaciomarine sedimentation in the west central North Sea |
title_sort |
middle pleistocene glacial and glaciomarine sedimentation in the west central north sea |
publisher |
Wiley |
publishDate |
1985 |
url |
http://dx.doi.org/10.1111/j.1502-3885.1985.tb00920.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1985.tb00920.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1985.tb00920.x |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Boreas volume 14, issue 4, page 325-332 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.1985.tb00920.x |
container_title |
Boreas |
container_volume |
14 |
container_issue |
4 |
container_start_page |
325 |
op_container_end_page |
332 |
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1800753363420184576 |