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1974年伊豆半島沖地震の余震のP波スペクトル
https://doi.org/10.15083/00032033
c1a13b92-417e-4d71-82fb-b6c7c37a7b65
名前 / ファイル | ライセンス | Actions | |
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item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2010-12-22 | |||||
タイトル | ||||||
タイトル | 1974年伊豆半島沖地震の余震のP波スペクトル | |||||
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 | 10.15083/00032033 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | P Wave Spectra from Aftershocks of the Izu-Hanto-oki Earthquake of 1974 | |||||
著者 |
中村, 功
× 中村, 功 |
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著者別名 | ||||||
姓名 | ||||||
姓名 | Nakamura, Isao | |||||
著者所属 | ||||||
地震研究所 | ||||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | An earthquake of magnitude 6.9 occurred off the Izu Peninsula on May 9, 1974. Many aftershocks were recorded at the Dodaira Micro-earthquake Observatory Network, and power spectra of P and S waves were analyzed. The magnitude of the analyzed event was in the range of 2.0-3.0. The power spectra of P waves are classified into four types according to peak frequency. The power spectra of S wave agree well with these four types. The power spctra of the P waves of the fault zone and the Amagi region are different by a low frequency ingredient. The Amagi region has a lower frequency ingredient than fault zone. | |||||
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. 93-98, 発行日 1974-09 |
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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Scheme | NDC | |||||
主題 | 051.1 | |||||
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 |