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  1. 131 地震研究所
  2. 東京大学地震研究所研究速報
  3. 14
  1. 0 資料タイプ別
  2. 30 紀要・部局刊行物
  3. 東京大学地震研究所研究速報
  4. 14

1974年伊豆半島沖地震、本震直後の余震活動

https://doi.org/10.15083/00032028
4efe3fb3-8a96-45c6-abe1-2374f89d231d
名前 / ファイル ライセンス アクション
jis0140006.pdf jis0140006.pdf (595.8 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-12-22
タイトル
タイトル 1974年伊豆半島沖地震、本震直後の余震活動
言語
言語 jpn
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 10.15083/00032028
ID登録タイプ JaLC
その他のタイトル
その他のタイトル Aftershock Activity Immediately after the Main Shock, the Izu-Hanto-oki Earthquake of 1974
著者 南雲, 昭三郎

× 南雲, 昭三郎

WEKO 71022

南雲, 昭三郎

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大内, 徹

× 大内, 徹

WEKO 71023

大内, 徹

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笠原, 順三

× 笠原, 順三

WEKO 71024

笠原, 順三

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是澤, 定之

× 是澤, 定之

WEKO 71025

是澤, 定之

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著者別名
識別子
識別子 71026
識別子Scheme WEKO
姓名
姓名 Nagumo, Shozaburo
著者別名
識別子
識別子 71027
識別子Scheme WEKO
姓名
姓名 Ouchi, Toru
著者別名
識別子
識別子 71028
識別子Scheme WEKO
姓名
姓名 Kasahara, Junzo
著者別名
識別子
識別子 71029
識別子Scheme WEKO
姓名
姓名 Koresawa, Sadayuki
著者所属
著者所属 地震研究所
抄録
内容記述タイプ Abstract
内容記述 Intense aftershock activity immediately after the main shock has been revealed by the playback of a magnetic tape recorded at the HATA station, epicentral distance being about 100km. Many large aftershocks (M>4) occurred during a 70 minute period after the main shock. These aftershock activities would be caused by violent crustal activation, produced by the main shock faulting.
内容記述
内容記述タイプ Other
内容記述 1974年伊豆半島沖地震調査概報
書誌情報 地震研究所研究速報

巻 14, p. 45-53, 発行日 1974-09
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN10165194
日本十進分類法
主題 051.1
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
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