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富士火山の地震活動
https://doi.org/10.15083/0000033030
https://doi.org/10.15083/00000330306b430218-4012-4b14-a362-ed30b0e79623
名前 / ファイル | ライセンス | アクション |
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ji0562005.pdf (1.8 MB)
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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 | 富士火山の地震活動 | |||||
言語 | ja | |||||
言語 | ||||||
言語 | jpn | |||||
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 | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15083/0000033030 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | The Seismic Activity of Mt. Fuji Volcano | |||||
著者 |
宮崎, 務
× 宮崎, 務× 行田, 紀也× 平賀, 士郎 |
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著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 128780 | |||||
姓名 | Miyazaki, Tsutomu | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 128781 | |||||
姓名 | Gyoda, Noriya | |||||
著者別名 | ||||||
識別子Scheme | WEKO | |||||
識別子 | 128782 | |||||
姓名 | Hiraga, Shiro | |||||
著者所属 | ||||||
値 | 東京大学地震研究所 | |||||
著者所属 | ||||||
値 | 神奈川県温泉地学研究所 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Mt. Fuji, the highest peak in Japan, is one of the largest and most famous volcanoes which have displayed violent volcanic eruptions in historic times. It may easily be supposed that Mt. Fuji has the potential of erupting in the future. Therefore, in terms of its social impact, Mt. Fuji is one of the most dangerous volcanoes in Japan. In order to accurately predict volcanic eruptions from seismological observations, it is very important to clarify the detailed seismic activity of the volcano. We carried out temporal seismometrical observations of Mt. Fuji in 1969, 1970 and 1972. From the analysis of the temporal observational data combined with the data obtained by the routine observations of other observatories, the seismicity of Mt. Fuji may be summarized as follows: 1) Seismic activity identifiable as directly related to the volcanic activity was not found by the temporal observations carried out on and around Mt. Fuji. 2) Only three earthquakes with a magnitude over 3.0 occurred beneath the body of Mt. Fuji proper during the past 18 years, from Jan. 1961 to Dec. 1978. The seismic activity inside Mt. Fuji seems rather low compared to that in the area around Mt. Fuji. 3) The analysis of the distribution of P-wave initial motions of the earthquakes which occurred inside Mt. Fuji indicates the existence of horizontal compressional stresses in the direction NW-SE. | |||||
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 56, 号 2, p. 391-414, 発行日 1981-09-30 |
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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Scheme | NDC | |||||
主題 | 453 | |||||
出版者 | ||||||
出版者 | 東京大学地震研究所 | |||||
出版者別名 | ||||||
値 | Earthquake Research Institute, University of Tokyo |