Glacio‐dynamic structures from the Blackwater Formation, Co. Wexford, Ireland
A series of large‐scale glacio‐dynamic structures exposed in 10 km of coastal cliff cut through the Screen Hills kame‐morainc, Co. Wexford. Ireland, is descrihed. The structures range from simple ovcrfolds to complex multiple thrusts, have a consistent structural trend, and result from marginal defo...
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crwiley:10.1111/j.1502-3885.1984.tb00053.x 2024-06-02T08:08:14+00:00 Glacio‐dynamic structures from the Blackwater Formation, Co. Wexford, Ireland THOMAS, GEOFFREY S. P. SUMMERS, A. JOHN 1984 http://dx.doi.org/10.1111/j.1502-3885.1984.tb00053.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1984.tb00053.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1984.tb00053.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 13, issue 1, page 5-12 ISSN 0300-9483 1502-3885 journal-article 1984 crwiley https://doi.org/10.1111/j.1502-3885.1984.tb00053.x 2024-05-03T11:08:22Z A series of large‐scale glacio‐dynamic structures exposed in 10 km of coastal cliff cut through the Screen Hills kame‐morainc, Co. Wexford. Ireland, is descrihed. The structures range from simple ovcrfolds to complex multiple thrusts, have a consistent structural trend, and result from marginal deformation by an ice‐sheet moving from the NE. The relationship between the structures and other, gcomorphic and stratigraphic components is resolved into a simple model of repeated ice‐marginal oscillation during a phase of overall glacial retreat. Article in Journal/Newspaper Ice Sheet Wiley Online Library Boreas 13 1 5 12 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
A series of large‐scale glacio‐dynamic structures exposed in 10 km of coastal cliff cut through the Screen Hills kame‐morainc, Co. Wexford. Ireland, is descrihed. The structures range from simple ovcrfolds to complex multiple thrusts, have a consistent structural trend, and result from marginal deformation by an ice‐sheet moving from the NE. The relationship between the structures and other, gcomorphic and stratigraphic components is resolved into a simple model of repeated ice‐marginal oscillation during a phase of overall glacial retreat. |
format |
Article in Journal/Newspaper |
author |
THOMAS, GEOFFREY S. P. SUMMERS, A. JOHN |
spellingShingle |
THOMAS, GEOFFREY S. P. SUMMERS, A. JOHN Glacio‐dynamic structures from the Blackwater Formation, Co. Wexford, Ireland |
author_facet |
THOMAS, GEOFFREY S. P. SUMMERS, A. JOHN |
author_sort |
THOMAS, GEOFFREY S. P. |
title |
Glacio‐dynamic structures from the Blackwater Formation, Co. Wexford, Ireland |
title_short |
Glacio‐dynamic structures from the Blackwater Formation, Co. Wexford, Ireland |
title_full |
Glacio‐dynamic structures from the Blackwater Formation, Co. Wexford, Ireland |
title_fullStr |
Glacio‐dynamic structures from the Blackwater Formation, Co. Wexford, Ireland |
title_full_unstemmed |
Glacio‐dynamic structures from the Blackwater Formation, Co. Wexford, Ireland |
title_sort |
glacio‐dynamic structures from the blackwater formation, co. wexford, ireland |
publisher |
Wiley |
publishDate |
1984 |
url |
http://dx.doi.org/10.1111/j.1502-3885.1984.tb00053.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1984.tb00053.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1984.tb00053.x |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Boreas volume 13, issue 1, page 5-12 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1502-3885.1984.tb00053.x |
container_title |
Boreas |
container_volume |
13 |
container_issue |
1 |
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5 |
op_container_end_page |
12 |
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1800753440161267712 |