A reanalysis and reinterpretation of geodetic and geological evidence of glacial-isostatic adjustment in the Churchill region, Hudson Bay
We review the historical, geological, tide-gauge, GPS and gravimetric evidence advanced in favour of or against continuing land uplift around Hudson Bay, Canada. After this, we reanalyse the tide-gauge and GPS data for Churchill using longer time series than those available to previous investigators...
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Geoforschungszentrum
2004
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ftgbv:oai:gbv.de:opac-de-7:ppn:474730700 2023-05-15T16:35:21+02:00 A reanalysis and reinterpretation of geodetic and geological evidence of glacial-isostatic adjustment in the Churchill region, Hudson Bay Wolf, Detlef [2004] electronic Elektronische Ressource electronic resource remote Online-Ressource (PDF-Datei: 49 S., 2 MB) http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0411.pdf http://www.gfz-potsdam.de/bib/pub/str0411/0411.htm http://deposit.ddb.de/cgi-bin/dokserv?idn=972813977 http://nbn-resolving.de/urn/resolver.pl?urn=urn:nbn:de:kobv:b103-04111 eng eng Geoforschungszentrum Niedersächsische Staats- und Universitätsbibliothek 550 520 16,13 ggo geo 2004 ftgbv 2016-01-30T09:01:37Z We review the historical, geological, tide-gauge, GPS and gravimetric evidence advanced in favour of or against continuing land uplift around Hudson Bay, Canada. After this, we reanalyse the tide-gauge and GPS data for Churchill using longer time series than those available to previous investigators. The dependence of the mean rate of relative sea-level change obtained on the length and mid-epoch of the observation interval considered is investigated by means of the newly developed linear-trend analysis diagram. For studying the shorter-period variability of the tide-gauge record, the continuous-wavelet transform is used. The mean rate of land uplift obtained from GPS is based on a new analysis using IGS solutions of GFZ. Furthermore, sea-level indicators from the Churchill region representing the relative sea-level history during the past 8000 a are included. Finally, the four types of observable are jointly inverted in terms of mantle viscosity. The optimum values are 3×10^20 Pa s and 1.6 × 10^22 Pa s for the upper- and lower-mantle viscosities, respectively. Other/Unknown Material Hudson Bay Georg-August-Universität Göttingen: GOEDOC Canada Hudson Hudson Bay |
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Open Polar |
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Georg-August-Universität Göttingen: GOEDOC |
op_collection_id |
ftgbv |
language |
English |
topic |
550 520 16,13 ggo geo |
spellingShingle |
550 520 16,13 ggo geo A reanalysis and reinterpretation of geodetic and geological evidence of glacial-isostatic adjustment in the Churchill region, Hudson Bay |
topic_facet |
550 520 16,13 ggo geo |
description |
We review the historical, geological, tide-gauge, GPS and gravimetric evidence advanced in favour of or against continuing land uplift around Hudson Bay, Canada. After this, we reanalyse the tide-gauge and GPS data for Churchill using longer time series than those available to previous investigators. The dependence of the mean rate of relative sea-level change obtained on the length and mid-epoch of the observation interval considered is investigated by means of the newly developed linear-trend analysis diagram. For studying the shorter-period variability of the tide-gauge record, the continuous-wavelet transform is used. The mean rate of land uplift obtained from GPS is based on a new analysis using IGS solutions of GFZ. Furthermore, sea-level indicators from the Churchill region representing the relative sea-level history during the past 8000 a are included. Finally, the four types of observable are jointly inverted in terms of mantle viscosity. The optimum values are 3×10^20 Pa s and 1.6 × 10^22 Pa s for the upper- and lower-mantle viscosities, respectively. |
author2 |
Wolf, Detlef |
title |
A reanalysis and reinterpretation of geodetic and geological evidence of glacial-isostatic adjustment in the Churchill region, Hudson Bay |
title_short |
A reanalysis and reinterpretation of geodetic and geological evidence of glacial-isostatic adjustment in the Churchill region, Hudson Bay |
title_full |
A reanalysis and reinterpretation of geodetic and geological evidence of glacial-isostatic adjustment in the Churchill region, Hudson Bay |
title_fullStr |
A reanalysis and reinterpretation of geodetic and geological evidence of glacial-isostatic adjustment in the Churchill region, Hudson Bay |
title_full_unstemmed |
A reanalysis and reinterpretation of geodetic and geological evidence of glacial-isostatic adjustment in the Churchill region, Hudson Bay |
title_sort |
reanalysis and reinterpretation of geodetic and geological evidence of glacial-isostatic adjustment in the churchill region, hudson bay |
publisher |
Geoforschungszentrum |
publishDate |
2004 |
url |
http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0411.pdf http://www.gfz-potsdam.de/bib/pub/str0411/0411.htm http://deposit.ddb.de/cgi-bin/dokserv?idn=972813977 http://nbn-resolving.de/urn/resolver.pl?urn=urn:nbn:de:kobv:b103-04111 |
geographic |
Canada Hudson Hudson Bay |
geographic_facet |
Canada Hudson Hudson Bay |
genre |
Hudson Bay |
genre_facet |
Hudson Bay |
_version_ |
1766025572381622272 |