地震の断裂の決定的な性質について
Erik L Olson1, Richard M Allen
1Department of Geology and Geophysics, University of Wisconsin Madison, 1215 W. Dayton Street, Madison, Wisconsin 53706, USA.
Nature
|November 11, 2005
まとめ
初期の地震エネルギー周波数量は,地震の大きさを予測する. これは,地震の破裂が以前考えられていたよりも決定的であることを示唆し,より早い規模推定を可能にします.
科学分野:
- 地球科学 地球科学 地球科学
- 地震学 地震学とは
- 地質物理学 地質物理学とは地質物理学です.
背景:
- 地震の破裂を理解することは,断層システムと地震の危険性を評価する上で重要なことです.
- 広く引用されているカスケードモデルは,地震は非決定的であり,破裂が止まった後にのみサイズが決定されると示唆しています.
- 現在,断層破裂プロセスを説明する統一理論はありません.
研究 の 目的:
- 地震破裂の決定的性質を調査する.
- 破裂過程の初期に地震の大きさを予測できるかどうかを判断する.
主な方法:
- 地震破裂の最初の最初の数秒で放射される地震エネルギーの周波数含有量の分析.
- 初期の地震エネルギーの特徴と最終的な地震の大きさの相関関係.
主要な成果:
- 破裂の最初の数秒間に放射される地震エネルギーの周波数量は,最終的な地震の大きさに比例する.
- このスケーリングにより,破裂が完了する前に地震の大きさを推定することができます.
結論:
- 地震の破裂は,ある程度の決定論を示している.
- 初期の地震データは,地震の最終的な大きさを推定するために使用され,非決定的カスケードモデルに挑戦することができます.
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