日本列島における地震発生メカニズムに関する研究 Earthquake Occurrence Mechanism in the Japanese Islands

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At present, a slow earthquake is continuing in the Tokai area. Then, the energy of approximately magnitude of 7.2 is estimated to have released. However, it doesn't find whether or not this slow earthquake develops into the big earthquake. This slow earthquake is supposed to have occurred because a part of the Philippin sea plate comes off. As the result, the extraordinary crustal movement in the Tokai district has been clarified from the GPS observation result. Moreover, recently, the extraordinary crustal movement has occurred in the wide area including Kanto and the central area. In this research, An analysis to clarify the occurrence mechanism of the earthquake in the Japanese Islands was progressed and the movement of the tectonic line in the Japanese Islands was clarified.

収録刊行物

  • 前橋工科大学研究紀要

    前橋工科大学研究紀要 6, 1-6, 2003-03-27

    前橋工科大学

各種コード

  • NII論文ID(NAID)
    110000033764
  • NII書誌ID(NCID)
    AA11225201
  • 本文言語コード
    JPN
  • 雑誌種別
    大学紀要
  • ISSN
    13438867
  • NDL 記事登録ID
    6605158
  • NDL 雑誌分類
    ZM2(科学技術--科学技術一般--大学・研究所・学会紀要)
  • NDL 請求記号
    Z74-B225
  • データ提供元
    NDL  NII-ELS 
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