2011年のMW 9.0の東北大震災で,浅いダイナミックオーバーショットとエネルギー深い破裂が発生した
Satoshi Ide1, Annemarie Baltay, Gregory C Beroza
1Department of Earth and Planetary Science, University of Tokyo, Hongo 7-3-1, Bunkyo-ku, Tokyo 113-0033, Japan. ide@eps.s.u-tokyo.ac.jp
まとめ
2011年,東北大震災が起こりました.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
- テクトニクス (地質学) とは
背景:
- 2011年の東北大震災 (マグニチュード9.0) は,大規模な被害をもたらしました.
- 破裂の特徴を理解することは,地震の危険性評価に不可欠です.
研究 の 目的:
- 東北大震災の空間と時間の断裂の特徴を分析するために.
- 破裂行動,地震,津波発生の関係について調査する.
主な方法:
- 限られたソースの画像技術が採用されました.
- 地震波形と余震分布の分析.
主要な成果:
- 断裂は,明確な深層と浅層の相を持つ,重要な空間的変化を示した.
- 溝の近くで大きな浅い滑りが発生し,それはおそらく断層の幾何学と吊り壁の適合によるものです.
- 通常の故障後の余震は,滑りやすい地域ではダイナミックなオーバーショットを示した.
- 高周波放射線は,より浅いものよりも,より深い破裂地帯からより強いものでした.
結論:
- 破裂の特徴の空間的変動は,震動の強さと津波の大きさに直接影響した.
- 断層の幾何学と吊り壁の性質は,大きな浅い滑り方を可能にする役割を果たしました.
- 地震の断裂のダイナミクスは,メガスラスト地震の行動と地震波放射線の洞察を提供します.
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