地震学:スマトラ地震の速度と大きさ
1Department of Geological Sciences, Northwestern University, Evanston, Illinois 60208, USA. seth@earth.northwestern.edu
Nature
|April 1, 2005
まとめ
2004年のスマトラ・アンダマン地震は,以前考えられていたのより2.5倍大きめで,1,200kmの断層に沿ってストレスを放出しました. 記録された地震で2番目に大きいこの大きな地震は,蓄積されたストレスを放出し,この特定の地域で即時の津波のリスクを軽減しました.
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:
- 2004年のスマトラ・アンダマン地震は,広範囲にわたる破壊と大規模な津波を引き起こしました.
- 初期の大小の推定は,イベントの規模を完全に捉えていない可能性があります.
研究 の 目的:
- 2004年のスマトラ・アンダマン地震の規模と断裂の特徴を再評価する.
- 地震性ストレンの放出と関連する津波発生の可能性を評価する.
主な方法:
- 地震学データの分析により,地震の規模と断層の滑り方を決定する.
- 断層破裂の拡散とエネルギー放出のモデリング.
主要な成果:
- 地震のマグニチュードは,当初報告されたの2.5倍で,記録された地震の中で2番目に大きい地震となった.
- 1,200kmの断層滑りが発生し,長い破裂期間と大きなエネルギー放出を示しています.
- 破裂地帯全体が滑り落ち,インド・ビルマプレート沈下からの累積した圧力が放出されました.
結論:
- 2004年のスマトラ・アンダマン地震は,以前よりもかなり大きく,以前よりも長い断裂がありました.
- プレート境界のこのセグメントに沿ったストレスの完全な解放は,同様の津波の即時のリスクを軽減します.
- 将来の地震と津波の脅威は,南のプレート境界の他のセグメントから可能である.
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