Glacial isostasy and long-term crustal movements in Fennoscandia with respect to lithospheric and asthenospheric processes and properties : comment

Recently, Mörner discussed his model of glacio-isostatic compensation in the light of new seismological models of the upper mantle below Fennoscandia. He concluded that the P-wave velocity distribution is in "full agreement" with his estimate of the viscosity distribution as inferred from...

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Main Author: Wolf, Detlef
Format: Article in Journal/Newspaper
Language:English
Published: 1991
Subjects:
Online Access:https://doi.org/10.18419/opus-7135
http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50905
http://elib.uni-stuttgart.de/handle/11682/7152
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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 Recently, Mörner discussed his model of glacio-isostatic compensation in the light of new seismological models of the upper mantle below Fennoscandia. He concluded that the P-wave velocity distribution is in "full agreement" with his estimate of the viscosity distribution as inferred from glacio-isostatic relaxation. Whereas the consistency of seismological and geodynamical earth models is a necessary condition for their soundness, the particular type of agreement sought by Mörner is not required or expected, nor can his method of attaining such agreement be approved. For easier understanding of my criticism, I briefly recall the type of information provided by the seismological and by the glacio-isostatic evidence.
format Article in Journal/Newspaper
genre Fennoscandia
genre_facet Fennoscandia
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institution Open Polar
language English
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op_doi https://doi.org/10.18419/opus-7135
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spelling ftunivstutt:oai:elib.uni-stuttgart.de:11682/7152 2025-04-13T14:18:31+00:00 Glacial isostasy and long-term crustal movements in Fennoscandia with respect to lithospheric and asthenospheric processes and properties : comment Wolf, Detlef 1991 application/pdf https://doi.org/10.18419/opus-7135 http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50905 http://elib.uni-stuttgart.de/handle/11682/7152 en eng 321601483 info:eu-repo/semantics/openAccess Isostasie Lithosphäre Asthenosphäre Fennoskandia 550 article 1991 ftunivstutt https://doi.org/10.18419/opus-7135 2025-03-18T06:41:26Z Recently, Mörner discussed his model of glacio-isostatic compensation in the light of new seismological models of the upper mantle below Fennoscandia. He concluded that the P-wave velocity distribution is in "full agreement" with his estimate of the viscosity distribution as inferred from glacio-isostatic relaxation. Whereas the consistency of seismological and geodynamical earth models is a necessary condition for their soundness, the particular type of agreement sought by Mörner is not required or expected, nor can his method of attaining such agreement be approved. For easier understanding of my criticism, I briefly recall the type of information provided by the seismological and by the glacio-isostatic evidence. Article in Journal/Newspaper Fennoscandia OPUS - Publication Server of the University of Stuttgart
spellingShingle Isostasie
Lithosphäre
Asthenosphäre
Fennoskandia
550
Wolf, Detlef
Glacial isostasy and long-term crustal movements in Fennoscandia with respect to lithospheric and asthenospheric processes and properties : comment
title Glacial isostasy and long-term crustal movements in Fennoscandia with respect to lithospheric and asthenospheric processes and properties : comment
title_full Glacial isostasy and long-term crustal movements in Fennoscandia with respect to lithospheric and asthenospheric processes and properties : comment
title_fullStr Glacial isostasy and long-term crustal movements in Fennoscandia with respect to lithospheric and asthenospheric processes and properties : comment
title_full_unstemmed Glacial isostasy and long-term crustal movements in Fennoscandia with respect to lithospheric and asthenospheric processes and properties : comment
title_short Glacial isostasy and long-term crustal movements in Fennoscandia with respect to lithospheric and asthenospheric processes and properties : comment
title_sort glacial isostasy and long-term crustal movements in fennoscandia with respect to lithospheric and asthenospheric processes and properties : comment
topic Isostasie
Lithosphäre
Asthenosphäre
Fennoskandia
550
topic_facet Isostasie
Lithosphäre
Asthenosphäre
Fennoskandia
550
url https://doi.org/10.18419/opus-7135
http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50905
http://elib.uni-stuttgart.de/handle/11682/7152