Two large historical earthquakes in Fennoscandia still large
Recent studies have claimed that two of the largest earthquakes in Fennoscandia, in 1759 and 1819, should have their magnitudes reduced by 0.5 and approximately 1 Ms units, respectively. It is shown that there is no cause for these downgradings in the macroseismic data and the implications of reduce...
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_232498 2023-05-15T16:11:20+02:00 Two large historical earthquakes in Fennoscandia still large Wahlström, R. 2004 application/pdf https://gfzpublic.gfz-potsdam.de/pubman/item/item_232498 unknown info:eu-repo/semantics/altIdentifier/doi/10.1016/j.pepi.2004.03.012 https://gfzpublic.gfz-potsdam.de/pubman/item/item_232498 info:eu-repo/semantics/openAccess Physics of the Earth and Planetary Interiors 550 - Earth sciences info:eu-repo/semantics/article 2004 ftgfzpotsdam https://doi.org/10.1016/j.pepi.2004.03.012 2022-09-14T05:55:59Z Recent studies have claimed that two of the largest earthquakes in Fennoscandia, in 1759 and 1819, should have their magnitudes reduced by 0.5 and approximately 1 Ms units, respectively. It is shown that there is no cause for these downgradings in the macroseismic data and the implications of reduced seismic hazard and risk for Fennoscandia are unwarranted. <copyright> 2004 Elsevier B. V. All rights reserved. Article in Journal/Newspaper Fennoscandia GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Physics of the Earth and Planetary Interiors 145 1-4 253 258 |
institution |
Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
unknown |
topic |
550 - Earth sciences |
spellingShingle |
550 - Earth sciences Wahlström, R. Two large historical earthquakes in Fennoscandia still large |
topic_facet |
550 - Earth sciences |
description |
Recent studies have claimed that two of the largest earthquakes in Fennoscandia, in 1759 and 1819, should have their magnitudes reduced by 0.5 and approximately 1 Ms units, respectively. It is shown that there is no cause for these downgradings in the macroseismic data and the implications of reduced seismic hazard and risk for Fennoscandia are unwarranted. <copyright> 2004 Elsevier B. V. All rights reserved. |
format |
Article in Journal/Newspaper |
author |
Wahlström, R. |
author_facet |
Wahlström, R. |
author_sort |
Wahlström, R. |
title |
Two large historical earthquakes in Fennoscandia still large |
title_short |
Two large historical earthquakes in Fennoscandia still large |
title_full |
Two large historical earthquakes in Fennoscandia still large |
title_fullStr |
Two large historical earthquakes in Fennoscandia still large |
title_full_unstemmed |
Two large historical earthquakes in Fennoscandia still large |
title_sort |
two large historical earthquakes in fennoscandia still large |
publishDate |
2004 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_232498 |
genre |
Fennoscandia |
genre_facet |
Fennoscandia |
op_source |
Physics of the Earth and Planetary Interiors |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.pepi.2004.03.012 https://gfzpublic.gfz-potsdam.de/pubman/item/item_232498 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1016/j.pepi.2004.03.012 |
container_title |
Physics of the Earth and Planetary Interiors |
container_volume |
145 |
container_issue |
1-4 |
container_start_page |
253 |
op_container_end_page |
258 |
_version_ |
1765996475671642112 |