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日光・足尾地域の地震活動 : 1993年11月~1997年1月
https://doi.org/10.15083/00032280
https://doi.org/10.15083/00032280c640594e-5909-4673-9934-3488e939f889
名前 / ファイル | ライセンス | アクション |
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02_043-072.pdf (45.8MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2017-05-15 | |||||
タイトル | ||||||
タイトル | 日光・足尾地域の地震活動 : 1993年11月~1997年1月 | |||||
言語 | ja | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題 | Nikko-Ashio | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | microearthquake | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | earthquαke swarm | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | Uchinokomori-fault | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | law frequency earthquake | |||||
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 | 10.15083/00032280 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | Seismic Activities in the Nikko-Ashio Area : November 1993~January 1997 | |||||
著者 |
萩原, 弘子
× 萩原, 弘子 |
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著者別名 | ||||||
識別子 | 72142 | |||||
識別子Scheme | WEKO | |||||
姓名 | HAGIWARA, Hiroko | |||||
著者所属 | ||||||
著者所属 | 地震地殻変動観測センター, (東京大学地震研究所) | |||||
著者所属 | ||||||
著者所属 | Earthquake Observation Centεr, (Earthquake Research Institute, University of Tokyo) | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Nikko-Ashio area, the northwestern part of Tochigi prefecture, is one of the most seismically active regions in Japan. We detected many earthquake swarms by routine observation of Earthquake Observation Center, Earthquake Research Institute. This paper reports those seismic activities in the area during the period from November 1993 to January 1997. This area is divided into four active regions. The Ashio region, lying along the Uchinokomori-fault, had the remarkable activity in the period. The earthquake swarm occurred at the bending part of the fault at first on February 1994. In the following three years, the swarms gradually migrated from the north to the south along the lineament of the fault, accompanying many microearthquakes, and then spread toward the east and the west. Finally, those microearthquakes filled up the area of 10x3 km along the Uchinokomori-fault. | |||||
内容記述 | ||||||
内容記述タイプ | Other | |||||
内容記述 | <論説> | |||||
書誌情報 |
技術研究報告 巻 2, p. 43-72, 発行日 1997 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 13426486 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA11286807 | |||||
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 |