Lithosphere deformation by continental ice sheets
In treating problems of mantle deformation, a common assumption of convenience is that deformation is viscous or viscoelastic. An important consequence of this assumption is the unproven prediction that the lithosphere is depressed far beyond the margins of steady-state continental ice sheets at the...
Published in: | Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences |
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Language: | English |
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The Royal Society
1981
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Online Access: | http://dx.doi.org/10.1098/rspa.1981.0165 https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.1981.0165 |
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crroyalsociety:10.1098/rspa.1981.0165 2024-06-02T08:08:14+00:00 Lithosphere deformation by continental ice sheets 1981 http://dx.doi.org/10.1098/rspa.1981.0165 https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.1981.0165 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences volume 378, issue 1775, page 507-527 ISSN 0080-4630 journal-article 1981 crroyalsociety https://doi.org/10.1098/rspa.1981.0165 2024-05-07T14:16:49Z In treating problems of mantle deformation, a common assumption of convenience is that deformation is viscous or viscoelastic. An important consequence of this assumption is the unproven prediction that the lithosphere is depressed far beyond the margins of steady-state continental ice sheets at the time of their maximum extent. Depression beyond the margins of shrinking ice sheets is proven by the formation of proglacial lakes along melting margins of retreating late Wisconsin-Weichselian ice sheets. No such lakes existed during the maximum extent of these ice sheets. An investigation of viscoplastic deformation in anisotropic polycrystalline rocks leads to the conclusion that transient creep in the lithosphere is predominantly time-dependent viscous flow, but that slow steady-state creep in the lithosphere is time-independent viscoplastic flow and begins at a viscoplastic yield stress. These results predict lithosphere depression beyond the margin of a growing or shrinking ice sheet, but not beyond the margin of a steady-state ice sheet at its maximum extent. Article in Journal/Newspaper Ice Sheet The Royal Society Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences 378 1775 507 527 |
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Open Polar |
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The Royal Society |
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crroyalsociety |
language |
English |
description |
In treating problems of mantle deformation, a common assumption of convenience is that deformation is viscous or viscoelastic. An important consequence of this assumption is the unproven prediction that the lithosphere is depressed far beyond the margins of steady-state continental ice sheets at the time of their maximum extent. Depression beyond the margins of shrinking ice sheets is proven by the formation of proglacial lakes along melting margins of retreating late Wisconsin-Weichselian ice sheets. No such lakes existed during the maximum extent of these ice sheets. An investigation of viscoplastic deformation in anisotropic polycrystalline rocks leads to the conclusion that transient creep in the lithosphere is predominantly time-dependent viscous flow, but that slow steady-state creep in the lithosphere is time-independent viscoplastic flow and begins at a viscoplastic yield stress. These results predict lithosphere depression beyond the margin of a growing or shrinking ice sheet, but not beyond the margin of a steady-state ice sheet at its maximum extent. |
format |
Article in Journal/Newspaper |
title |
Lithosphere deformation by continental ice sheets |
spellingShingle |
Lithosphere deformation by continental ice sheets |
title_short |
Lithosphere deformation by continental ice sheets |
title_full |
Lithosphere deformation by continental ice sheets |
title_fullStr |
Lithosphere deformation by continental ice sheets |
title_full_unstemmed |
Lithosphere deformation by continental ice sheets |
title_sort |
lithosphere deformation by continental ice sheets |
publisher |
The Royal Society |
publishDate |
1981 |
url |
http://dx.doi.org/10.1098/rspa.1981.0165 https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.1981.0165 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences volume 378, issue 1775, page 507-527 ISSN 0080-4630 |
op_rights |
https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ |
op_doi |
https://doi.org/10.1098/rspa.1981.0165 |
container_title |
Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences |
container_volume |
378 |
container_issue |
1775 |
container_start_page |
507 |
op_container_end_page |
527 |
_version_ |
1800753425988714496 |