Deglacial land emergence and lateral upper-mantle heterogeneity in the Svalbard Archipelago-I. First results for simple load models
The glacial-isostatic adjustment following the removal of the Pleistocene ice sheets furnishes basic information on the thickness of the Earth’s lithosphere and the viscosity of the subjacent mantle. Paper I is concerned with an elementary interpretation of the post-glacial land emergence observed a...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1032.6005 2023-05-15T15:38:40+02:00 Deglacial land emergence and lateral upper-mantle heterogeneity in the Svalbard Archipelago-I. First results for simple load models Doris Breuer Detlef Wolf The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1032.6005 http://gji.oxfordjournals.org/content/121/3/775.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1032.6005 http://gji.oxfordjournals.org/content/121/3/775.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://gji.oxfordjournals.org/content/121/3/775.full.pdf Key words asthenosphere viscosity Barents Sea glacial isostasy lateral heteroge- neity lithosphere thickness. Maxwell viscoelasticity Svalbard Archipelago text ftciteseerx 2016-10-30T00:15:14Z The glacial-isostatic adjustment following the removal of the Pleistocene ice sheets furnishes basic information on the thickness of the Earth’s lithosphere and the viscosity of the subjacent mantle. Paper I is concerned with an elementary interpretation of the post-glacial land emergence observed at a restricted set of six locations in the Svalbard Archipelago. The interpretation is based on a three-layer, incompressible Maxwell-viscoelastic earth model, which is forced by a time-dependent load distribution simulating the deglaciation history of the Svalbard Archipelago and the Barents Sea. In view of inconclusive geomorphological evidence suggesting either totul or partial glaciation of the area at glacial maximum. two simple load models, BARENTS-TI and BARENTS-PI, are considered in the first instance. A comparison between the calculated and observed values of land emergence suggests increases in lithosphere thickness and asthenosphere viscosity with increas-ing distance of the location from the continental margin. The trends are qualitatively insensitive to the load model, load thickness or load cross-section used. For load Text Barents Sea Svalbard Unknown Barents Sea Svalbard Svalbard Archipelago |
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ftciteseerx |
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English |
topic |
Key words asthenosphere viscosity Barents Sea glacial isostasy lateral heteroge- neity lithosphere thickness. Maxwell viscoelasticity Svalbard Archipelago |
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Key words asthenosphere viscosity Barents Sea glacial isostasy lateral heteroge- neity lithosphere thickness. Maxwell viscoelasticity Svalbard Archipelago Doris Breuer Detlef Wolf Deglacial land emergence and lateral upper-mantle heterogeneity in the Svalbard Archipelago-I. First results for simple load models |
topic_facet |
Key words asthenosphere viscosity Barents Sea glacial isostasy lateral heteroge- neity lithosphere thickness. Maxwell viscoelasticity Svalbard Archipelago |
description |
The glacial-isostatic adjustment following the removal of the Pleistocene ice sheets furnishes basic information on the thickness of the Earth’s lithosphere and the viscosity of the subjacent mantle. Paper I is concerned with an elementary interpretation of the post-glacial land emergence observed at a restricted set of six locations in the Svalbard Archipelago. The interpretation is based on a three-layer, incompressible Maxwell-viscoelastic earth model, which is forced by a time-dependent load distribution simulating the deglaciation history of the Svalbard Archipelago and the Barents Sea. In view of inconclusive geomorphological evidence suggesting either totul or partial glaciation of the area at glacial maximum. two simple load models, BARENTS-TI and BARENTS-PI, are considered in the first instance. A comparison between the calculated and observed values of land emergence suggests increases in lithosphere thickness and asthenosphere viscosity with increas-ing distance of the location from the continental margin. The trends are qualitatively insensitive to the load model, load thickness or load cross-section used. For load |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Doris Breuer Detlef Wolf |
author_facet |
Doris Breuer Detlef Wolf |
author_sort |
Doris Breuer |
title |
Deglacial land emergence and lateral upper-mantle heterogeneity in the Svalbard Archipelago-I. First results for simple load models |
title_short |
Deglacial land emergence and lateral upper-mantle heterogeneity in the Svalbard Archipelago-I. First results for simple load models |
title_full |
Deglacial land emergence and lateral upper-mantle heterogeneity in the Svalbard Archipelago-I. First results for simple load models |
title_fullStr |
Deglacial land emergence and lateral upper-mantle heterogeneity in the Svalbard Archipelago-I. First results for simple load models |
title_full_unstemmed |
Deglacial land emergence and lateral upper-mantle heterogeneity in the Svalbard Archipelago-I. First results for simple load models |
title_sort |
deglacial land emergence and lateral upper-mantle heterogeneity in the svalbard archipelago-i. first results for simple load models |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1032.6005 http://gji.oxfordjournals.org/content/121/3/775.full.pdf |
geographic |
Barents Sea Svalbard Svalbard Archipelago |
geographic_facet |
Barents Sea Svalbard Svalbard Archipelago |
genre |
Barents Sea Svalbard |
genre_facet |
Barents Sea Svalbard |
op_source |
http://gji.oxfordjournals.org/content/121/3/775.full.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1032.6005 http://gji.oxfordjournals.org/content/121/3/775.full.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766369898951344128 |