The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data
A magnitude Mw (ISC) = 6.6 earthquake on October 14, 1908 in the Barents-Kara Sea region was the strongest in this region for the entire observation period. We performed earthquake relocation based on our compilation of all available seismological bulletins of the time that included data from the IS...
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ftnipr:oai:nipr.repo.nii.ac.jp:00015629 2023-05-15T15:03:07+02:00 The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data 2019-06 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15629 http://id.nii.ac.jp/1291/00015524/ en eng https://doi.org/10.1016/j.polar.2019.05.001 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15629 http://id.nii.ac.jp/1291/00015524/ Polar Science, 20P2, 160-166(2019-06) 18739652 1908 earthquake Relocation procedure Barents sea region Kara sea region Instrumental seismicity Journal Article 2019 ftnipr https://doi.org/10.1016/j.polar.2019.05.001 2022-12-03T19:43:10Z A magnitude Mw (ISC) = 6.6 earthquake on October 14, 1908 in the Barents-Kara Sea region was the strongest in this region for the entire observation period. We performed earthquake relocation based on our compilation of all available seismological bulletins of the time that included data from the ISC-GEM (International Seismological Centre–Global Earthquake Model) project, the EuroSeismos project, the Geophysical Survey of the Russian Academy of Sciences and the Russian State Library. The relocation was performed using a modified generalized beamforming method based on the BARENTS travel time model. The epicenter was located in the estuarial part of the Franz Victoria Graben at the continent-ocean transition zone. According to our justification, an earthquake of such magnitude could well have occurred in the area of Franz Victoria Graben. Article in Journal/Newspaper Arctic Barents Sea Kara Sea Polar Science Polar Science National Institute of Polar Research Repository, Japan Arctic Barents Sea Kara Sea Polar Science 20 160 166 |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
1908 earthquake Relocation procedure Barents sea region Kara sea region Instrumental seismicity |
spellingShingle |
1908 earthquake Relocation procedure Barents sea region Kara sea region Instrumental seismicity The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data |
topic_facet |
1908 earthquake Relocation procedure Barents sea region Kara sea region Instrumental seismicity |
description |
A magnitude Mw (ISC) = 6.6 earthquake on October 14, 1908 in the Barents-Kara Sea region was the strongest in this region for the entire observation period. We performed earthquake relocation based on our compilation of all available seismological bulletins of the time that included data from the ISC-GEM (International Seismological Centre–Global Earthquake Model) project, the EuroSeismos project, the Geophysical Survey of the Russian Academy of Sciences and the Russian State Library. The relocation was performed using a modified generalized beamforming method based on the BARENTS travel time model. The epicenter was located in the estuarial part of the Franz Victoria Graben at the continent-ocean transition zone. According to our justification, an earthquake of such magnitude could well have occurred in the area of Franz Victoria Graben. |
format |
Article in Journal/Newspaper |
title |
The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data |
title_short |
The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data |
title_full |
The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data |
title_fullStr |
The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data |
title_full_unstemmed |
The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data |
title_sort |
october 14, 1908 mw 6.6 earthquake in the barents and kara sea region of the arctic: relocation based on instrumental data |
publishDate |
2019 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15629 http://id.nii.ac.jp/1291/00015524/ |
geographic |
Arctic Barents Sea Kara Sea |
geographic_facet |
Arctic Barents Sea Kara Sea |
genre |
Arctic Barents Sea Kara Sea Polar Science Polar Science |
genre_facet |
Arctic Barents Sea Kara Sea Polar Science Polar Science |
op_relation |
https://doi.org/10.1016/j.polar.2019.05.001 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15629 http://id.nii.ac.jp/1291/00015524/ Polar Science, 20P2, 160-166(2019-06) 18739652 |
op_doi |
https://doi.org/10.1016/j.polar.2019.05.001 |
container_title |
Polar Science |
container_volume |
20 |
container_start_page |
160 |
op_container_end_page |
166 |
_version_ |
1766335018040295424 |