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Dispersion curves obtained from the record at Miyagi-Enoshima coincide pretty well with the calculation for the case of a continental shelf with a width of 40km and mean depth 500m, bordering an ocean 5000m deep. An appreciable phase change was observed at Miyagi-Enoshima 31 h 34m after the occurrence of the main shock. However, a cause for this phase change could not be defined. 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25. On the Alaska Tsunami of March 28, 1964, as Observed along the Coast of Japan
https://doi.org/10.15083/0000033639
https://doi.org/10.15083/00000336391fec0ce6-2b5d-49b0-a20c-29f80f4412e7
名前 / ファイル | ライセンス | アクション |
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ji0432009.pdf (552.5 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-05-30 | |||||
タイトル | ||||||
タイトル | 25. On the Alaska Tsunami of March 28, 1964, as Observed along the Coast of Japan | |||||
言語 | en | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15083/0000033639 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | 25. 日本における1964年3月のアラスカ津波について | |||||
著者 |
HATORI, Tokutaro
× HATORI, Tokutaro |
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著者別名 | ||||||
識別子 | 131457 | |||||
識別子Scheme | WEKO | |||||
姓名 | 羽鳥, 徳太郎 | |||||
著者所属 | ||||||
著者所属 | Earthquake Research Institute | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Some features of the tsunami generated off the south coast of Alaska, USA, at 3h 36m(GMT), March 28, 1964 are investigated on the basis of tsunami records taken along the coast of Japan. Dispersion curves obtained from the record at Miyagi-Enoshima coincide pretty well with the calculation for the case of a continental shelf with a width of 40km and mean depth 500m, bordering an ocean 5000m deep. An appreciable phase change was observed at Miyagi-Enoshima 31 h 34m after the occurrence of the main shock. However, a cause for this phase change could not be defined. Making use of records taken at Miyagi-Enoshima, the decay coefficient of the tsunami waves is estimated to be approximately 0.010 per hour. | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 1964年3月28日3時36分(GMT)ころ,米国アラスカ南部近海に大地震が起り,アンカレヂに多大の被害が生じた.この地震に伴ない津波が発生し,全太平洋に伝搬した.日本でも地震より約6.5時間後から太平洋沿岸で津波を感じ,数日間観測された.U.S.C.G.S.の観測報告によれば,本震は61.1゜N,147.6°W,深さ20Kmに発生し,マグニチュードは8.5で,3月28,29,30日の3日間に起きたマグニチュード6.1以上の余震はFig.1に示すように,500~600kmの広範囲に分布している. | |||||
書誌情報 |
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 巻 43, 号 2, p. 399-408, 発行日 1965-09-20 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00408972 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00162258 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
日本十進分類法 | ||||||
主題 | 453 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | 東京大学地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute, University of Tokyo |