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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Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15629
http://id.nii.ac.jp/1291/00015524/
id ftnipr:oai:nipr.repo.nii.ac.jp:00015629
record_format openpolar
spelling 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
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