パークフィールドの震動は,同じ強度でゆっくりと速い断裂を明らかにします
Deepa Mele Veedu1, Sylvain Barbot1
1Earth Observatory of Singapore, Asian School of the Environment, Nanyang Technological University, 50 Nanyang Avenue, Singapore 639798, Singapore.
Nature
|April 5, 2016
まとめ
サンアンドレアス断層
科学分野:
- 地理学
- 地震学
- 構造学
背景:
- サンアンドレアス断層の深い部分は 複雑な変形を示しています
- 構造的震動は 異常なストレスの蓄積と放出メカニズムを明らかにします
- パークフィールドの近くの 孤立した震源は 周期的な振動を示した
研究 の 目的:
- 地震の繰り返し発生するメカニズムを 調べるため
- 振動の滑り方をモデル化するために
- 2004年のパークフィールド地震の 震動パターンの影響を説明するために
主な方法:
- 振動の振動の物理モデル化
- 低周波地震の分析
- 孔圧の変化のシミュレーション
主要な成果:
- ゆっくりと速い滑り方を表すことができます.
- 交代的な再発間隔 (3-6日) は,アスペリティのサイズが臨界の核のサイズに近いときに自然に発生します.
- 地震後の毛穴圧の変化は,再発パターンの観察された変化を説明します.
結論:
- 単一の断層は,ゆっくりと速い破裂の両方を通じて,構造的ストレスを放出することができます.
- クリティカルな核の大きさに相対するアスペリティの大きさは,スリップの行動と再発を制御する.
- 大きな地震の後の断層滑りパターンを調整する上で重要な役割を果たします.
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