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The 1999 Chi-Chi, Taiwan Earthquake : A Subduction Zone Earthquake on Land
https://doi.org/10.15083/0000032654
https://doi.org/10.15083/000003265485aa5459-6e46-4b05-8278-eea2951c622e
名前 / ファイル | ライセンス | アクション |
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ji0751005.pdf (2.6 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 | The 1999 Chi-Chi, Taiwan Earthquake : A Subduction Zone Earthquake on Land | |||||
言語 | en | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題 | Chi-Chi earthquake | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | Taiwan | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | accretion | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | tsunami 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 | 10.15083/0000032654 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | 1999年台湾集集地震 : 陸上にのりあげた海溝系地震 | |||||
著者 |
Seno, Tetsuzo
× Seno, Tetsuzo× Otsuki, Kenshiro× Yang, Chao-Nan |
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著者別名 | ||||||
識別子 | 126569 | |||||
識別子Scheme | WEKO | |||||
姓名 | 瀬野, 徹三 | |||||
著者別名 | ||||||
識別子 | 126570 | |||||
識別子Scheme | WEKO | |||||
姓名 | 大槻, 憲四郎 | |||||
著者別名 | ||||||
識別子 | 126571 | |||||
識別子Scheme | WEKO | |||||
姓名 | 楊, 昭雄 | |||||
著者所属 | ||||||
著者所属 | Graduate school of Earth Sciences, Tohoku University | |||||
著者所属 | ||||||
著者所属 | Department of Geology, National Taiwan University | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Chi-Chi earthquake occurred at the thrust-decollement in the accretionary prism of a young collision zone in central Taiwan. This event is thus not different from a subduction zone earthquake if Taiwan were covered by the sea water. The surface ruptures were accompanied by little damage except for the collapse of buildings standing across the surface faults. The slip directions of the surface faults were mostly NW, which is consistent with the earthquake slip vector, but there were also many W-SW and N directed slips. At the northwest corner of the earthquake fault, significant uplifts and multiple thrusts in the river bed occurred. These might all be related to the fact that the shallow portion of the earthquake fault cut the weak accretionary prism and the sediment on it. The uplifts at the northwestern corner imply an abnormal tsunami if the area were under the sea, thus suggesting a new factor for the mechanism of tsunami earthquakes: deformation of the sediment or weak accretionary prism at the lowest trench slope (Seno, 2000). The Chi-Chi earthquake might provide a unique chance to observe a subduction earthquake on land. | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 1999年9月21日台湾中央部で起きた集集地震は,ルソン弧と中国大陸縁との間の衝突でできた付加体を切る逆断層(スラスト)で起きた.ここはユーラシアプレートとフィリピン海プレートとのプレート力学境界にあたり,通常の沈み込み帯でおきる地震と地学的には変わらない.地表で車寵埔断層として知られていた活断層に沿って地表断層が現れたが,その付近では,地表断層をまたいだ建物が壊れているのが特徴で,それ以外の被害は小さかった.地表断層のすべり方向は,かなりのものは北西方向であったが,一方西,南西,北方向のすべりもかなりの数がみられた.地表断層の北端では,大甲渓という河川の中の滝,桃畑の砂利断層崖,ダムの破損地などにおいて,弾性理論から期待できる隆起よりも3mほど大きい隆起が起きた. | |||||
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 75, 号 1, p. 57-77, 発行日 2000-09-22 |
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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 |