まとめ
1906年のサンフランシスコ地震と1989年のロマ・プリエタ地震からの水平の移転は,明確な断層の振る舞いを明らかにします. 1906年の地震は右横のストライクスライドの動きを示したが,1989年の地震はストライクスライドと逆欠陥の両方を有していた.
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
- ジオデシ (Geodesy) とは
背景:
- 1906年のサンフランシスコ地震と1989年のロマ・プリエタ地震は,この地域に大きな影響を与えた.
- これらの主要な地震の故障メカニズムを理解することは,地震の危険性評価に不可欠です.
研究 の 目的:
- 1906年と1989年のカリフォルニア地震の水平移動フィールドを計算し比較する.
- 地検データに基づいて,各地震に関連する断層メカニズムを分析する.
主な方法:
- 地質調査による測量の分析により,水平地位移転を決定する.
- 観測された移転パターンを理論的な故障モデルと比較.
主要な成果:
- 1906年の地震の移転フィールドは,サンアンドレアス断層に沿って右側ストライクスリップ運動と一致しています.
- 1989年のロマ・プリエタ地震は,ストライクスリップと逆断層の両方の重要な構成要素を示した.
結論:
- 明確な断層の特徴は,1906年と1989年の地震は,異なる断層平面が破裂した可能性があることを示唆しています.
- 地質学的データは,地震破裂の複雑な行動に関する重要な洞察を提供します.
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