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新島・式根島・神津島の変動はなぜ時間変化するのか? : 2000年三宅島噴火に伴う地殻活動
https://doi.org/10.15083/0000032597
https://doi.org/10.15083/00000325973850d3d7-42b2-4edc-b216-2f8abe25d794
名前 / ファイル | ライセンス | アクション |
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ji0771006.pdf (1.6 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 | 新島・式根島・神津島の変動はなぜ時間変化するのか? : 2000年三宅島噴火に伴う地殻活動 | |||||
言語 | ja | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題 | Niijima | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | Shikinejima | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | GPS | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | dyke | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | and magma chamber | |||||
主題Scheme | Other | |||||
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 | 10.15083/0000032597 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | Why do displacement velocities of the Niijima, Shikinejima, and Koudushima islands vary over time? : Crustal activity accompanied by the 2000 Eruption of Miyakejima Volcano | |||||
著者 |
飯尾, 能久
× 飯尾, 能久 |
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著者別名 | ||||||
識別子 | 126115 | |||||
識別子Scheme | WEKO | |||||
姓名 | Iio, Yoshihisa | |||||
著者所属 | ||||||
著者所属 | 東京大学地震研究所 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Displacement velocities of the Niijima, Shikinejima, and Koudushima islands to Minamiizu from June to August in 2000 measured by the GEONET vary over time. It seems that the displacement velocities of the Shikinejima and Niijima islands show a reverse correlation. This can be explained by two pairs of dyke and fault plane, the northern and southern pairs. It is inferred from seismic activity that these pairs alternately became active. The displacement velocity of the Shikinejima was large when the southern pair was active, while that of the Niijima was large when the northern pair was active. Further, all of the displacement velocities became small for a few days after a large earthquake (M>6) occurred. This might be explained by a decrease in volumetric strain in and around the magma chambers in the lower crust. | |||||
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 77, 号 1, p. 77-85, 発行日 2002-07-30 |
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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 | 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 |