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  1. 131 地震研究所
  2. 東京大学地震研究所彙報
  3. 78
  4. 2
  1. 0 資料タイプ別
  2. 30 紀要・部局刊行物
  3. 東京大学地震研究所彙報
  4. 78
  5. 2

What Control Segmentations of Mega-Thrust Earthquakes in the Nankai Seismogenic Zone : a Review of High-Resolution Wide-Angle Seismic Surveys

https://doi.org/10.15083/0000032561
eb6ae190-9dff-4a2b-9e95-f8f4aba41893
名前 / ファイル ライセンス アクション
IHO78205.pdf IHO78205.pdf (15.6MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2007-04-23
タイトル
タイトル What Control Segmentations of Mega-Thrust Earthquakes in the Nankai Seismogenic Zone : a Review of High-Resolution Wide-Angle Seismic Surveys
言語 en
言語
言語 eng
キーワード
主題 Nankai trough
主題Scheme Other
キーワード
主題 seismic survey
主題Scheme Other
キーワード
主題 seismogenic zone
主題Scheme Other
キーワード
主題 seismogenic zone,
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 10.15083/0000032561
ID登録タイプ JaLC
その他のタイトル
その他のタイトル 南海トラフ地震発生帯において巨大地震破壊域セグメント化を規定する地下構造: レビュー
著者 Kodaira, Shuichi

× Kodaira, Shuichi

WEKO 125710

Kodaira, Shuichi

Search repository
Nakanishi, Ayako

× Nakanishi, Ayako

WEKO 125711

Nakanishi, Ayako

Search repository
Park, Jin-Oh

× Park, Jin-Oh

WEKO 125712

Park, Jin-Oh

Search repository
Takahashi, Narumi

× Takahashi, Narumi

WEKO 125713

Takahashi, Narumi

Search repository
Kaneda, Yoshiyuki

× Kaneda, Yoshiyuki

WEKO 125714

Kaneda, Yoshiyuki

Search repository
著者別名
識別子
識別子 125715
識別子Scheme WEKO
姓名
姓名 小平, 秀一
著者別名
識別子
識別子 125716
識別子Scheme WEKO
姓名
姓名 仲西, 理子
著者別名
識別子
識別子 125717
識別子Scheme WEKO
姓名
姓名 朴, 進午
著者別名
識別子
識別子 125718
識別子Scheme WEKO
姓名
姓名 高橋, 成実
著者別名
識別子
識別子 125719
識別子Scheme WEKO
姓名
姓名 金田, 義行
著者所属
著者所属 Institute for Frontier Research on Earth Evolution, Japan Marine Science and Technology Center
著者所属
著者所属 Deep Sea Research Department, Japan Marine Science and Technology Center
抄録
内容記述タイプ Abstract
内容記述 A series of wide-angle seismic surveys has been carried out in recent years of the entire Nankai seismogenic zone under the working hypothesis, ""structure of subducted plate might control segmentation of rupture zones"". In this paper we summarize the key results of these surveys. Along a profile crossing the rupture zone of the 1946 Nankaido earthquake we successfully imaged a large-scale subducted seamount, which is 50km wide and 3km high. The seamount is interpreted to be one member of the Kinan seamount chain, which is recognized on the incoming plate. Comparing the location of the subducted seamount and a detailed rupture distribution of the 1946 event shows that the rupture starting off Cape Shiono turned around the landward foot of the seamount. Another structure preventing rupture propagation was also found along a profile looking at the eastern edge of the 1944 Tonankai earthquake. High-resolution wide-angle seismic data clearly imaged two lines of subducted ridges, which are interpreted to be a subducted ridge parallel to the present day ridge system on the incoming plate. One of the subducted ridges is situated immediately outside the rupture zone where GPS data indicate strong coupling at present. We propose, from these results, that a subducted convex, which underlays a back stop structure, played the role of a barrier preventing earthquake rupture propagation.
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 78, 号 2, p. 175-183, 発行日 2003
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 51.1
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
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