スマトラ・アンダマン島地震の大きさと持続時間は,遠域静的オフセットによるものです
P Banerjee1, F F Pollitz, R Bürgmann
1Wadia Institute of Himalayan Geology, Dehra Dun, 248001, India.
まとめ
2004年のスマトラ地震は,世界中のGPSステーションによって検出された重要な地位移転を引き起こしました. 分析により,平均滑り幅が5メートルを超え,最終的な大きさはMW9.2を超えないことが明らかになった.
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
- プレート・テクトニクス (プレート・テクトニクス)
背景:
- 2004年のスマトラ地震は,広範囲に及ぶ影響を持つ大規模な地震でした.
- 静的偏移は,震源から4500kmまでのグローバルポジショニングシステム (GPS) ステーションによって測定されました.
研究 の 目的:
- 静的なGPSの移動を用いて,2004年のスマトラ地震をモデリングする.
- 地震モデルに地球の形状と深度変動の剛性を組み込むために.
主な方法:
- 継続的に動作するGPSステーションからの静的オフセットを利用した.
- 地球の地質学パラメータを考慮した地震モデルを開発した.
- 地質学的な情報源のパラメータを地震による推定値と比較した.
主要な成果:
- アンダマン海域を含む破裂地帯全体に沿って,平均5メートル以上の滑り込みが示唆されました.
- 合計モメントの25〜35%が1時間以上の時間帯で発生したと示した.
- 地震のマグニチュードは9.2MWを超えないと判断し,dip依存モメントの推定を考慮した.
結論:
- 地質学的データは,大規模な地震の破裂プロセスに関する重要な洞察を提供します.
- 2004年のスマトラ地震は,大きな滑り込みと,かなりの長期間モメントの放出を含んでいた.
- Mw 9.2は,地震のマグニチュードの推定上限である.
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