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The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data
https://nipr.repo.nii.ac.jp/records/15629
https://nipr.repo.nii.ac.jp/records/15629c193c2bd-0336-4969-b7cc-54a4c1df77e0
Item type | 学術雑誌論文 / Journal Article(1) | |||||||||||
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公開日 | 2019-06-30 | |||||||||||
タイトル | ||||||||||||
タイトル | The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data | |||||||||||
タイトル | ||||||||||||
言語 | en | |||||||||||
タイトル | The October 14, 1908 MW 6.6 earthquake in the Barents and Kara sea region of the Arctic: Relocation based on instrumental data | |||||||||||
言語 | ||||||||||||
言語 | eng | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | 1908 earthquake | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | Relocation procedure | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | Barents sea region | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | Kara sea region | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | Instrumental seismicity | |||||||||||
資源タイプ | ||||||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||||
資源タイプ | journal article | |||||||||||
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アクセス権 | metadata only access | |||||||||||
アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||||||||
著者 |
Morozov, Alexey N.
× Morozov, Alexey N.
× Vaganova, Natalya V.
× Konechnaya, Yana V.
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抄録 | ||||||||||||
内容記述タイプ | Abstract | |||||||||||
内容記述 | 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. | |||||||||||
書誌情報 |
en : Polar Science 巻 20P2, p. 160-166, 発行日 2019-06 |
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ISSN | ||||||||||||
収録物識別子タイプ | ISSN | |||||||||||
収録物識別子 | 18739652 | |||||||||||
DOI | ||||||||||||
識別子タイプ | DOI | |||||||||||
関連識別子 | https://doi.org/10.1016/j.polar.2019.05.001 | |||||||||||
関連名称 | 10.1016/j.polar.2019.05.001 |