A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt

The study proposes an inversion method applicable to observations of deglacial land uplift and tilt near the margin of a major Pleistocene ice-sheet. This information allows the determination of the cross-section of the ice-sheet and the calculation of the thickness of the lithosphere. The method is...

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Bibliographic Details
Main Author: Wolf, Detlef
Format: Article in Journal/Newspaper
Language:English
Published: 1986
Subjects:
Online Access:https://doi.org/10.18419/opus-7132
http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50867
http://elib.uni-stuttgart.de/handle/11682/7149
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author Wolf, Detlef
author_facet Wolf, Detlef
author_sort Wolf, Detlef
collection OPUS - Publication Server of the University of Stuttgart
description The study proposes an inversion method applicable to observations of deglacial land uplift and tilt near the margin of a major Pleistocene ice-sheet. This information allows the determination of the cross-section of the ice-sheet and the calculation of the thickness of the lithosphere. The method is applied to the Pleistocene glaciations in Fennoscandia and Laurentia and yields similar lithosphere thicknesses of 110 ± 30 km and 130 ± 35 km, respectively. Since the method is based on a static theoretical model, the thicknesses must be interpreted as upper bounds.
format Article in Journal/Newspaper
genre Fennoscandia
Ice Sheet
genre_facet Fennoscandia
Ice Sheet
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institution Open Polar
language English
op_collection_id ftunivstutt
op_doi https://doi.org/10.18419/opus-7132
op_relation 321600290
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publishDate 1986
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spelling ftunivstutt:oai:elib.uni-stuttgart.de:11682/7149 2025-04-13T14:18:32+00:00 A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt Wolf, Detlef 1986 application/pdf https://doi.org/10.18419/opus-7132 http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50867 http://elib.uni-stuttgart.de/handle/11682/7149 en eng 321600290 info:eu-repo/semantics/openAccess Lithosphäre Isostasie Fennoskandia Platte <Geologie> 550 article 1986 ftunivstutt https://doi.org/10.18419/opus-7132 2025-03-18T06:41:26Z The study proposes an inversion method applicable to observations of deglacial land uplift and tilt near the margin of a major Pleistocene ice-sheet. This information allows the determination of the cross-section of the ice-sheet and the calculation of the thickness of the lithosphere. The method is applied to the Pleistocene glaciations in Fennoscandia and Laurentia and yields similar lithosphere thicknesses of 110 ± 30 km and 130 ± 35 km, respectively. Since the method is based on a static theoretical model, the thicknesses must be interpreted as upper bounds. Article in Journal/Newspaper Fennoscandia Ice Sheet OPUS - Publication Server of the University of Stuttgart
spellingShingle Lithosphäre
Isostasie
Fennoskandia
Platte <Geologie>
550
Wolf, Detlef
A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt
title A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt
title_full A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt
title_fullStr A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt
title_full_unstemmed A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt
title_short A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt
title_sort method of calculating lithosphere thickness from observations of deglacial land uplift and tilt
topic Lithosphäre
Isostasie
Fennoskandia
Platte <Geologie>
550
topic_facet Lithosphäre
Isostasie
Fennoskandia
Platte <Geologie>
550
url https://doi.org/10.18419/opus-7132
http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50867
http://elib.uni-stuttgart.de/handle/11682/7149