移動する震動は,地震発生性のサンアンドレアス断層の下にある複雑な変形を明るくする
1US Geological Survey, 345 Middlefield Road, MS 977, Menlo Park, California 94025, USA. dshelly@usgs.gov
Nature
|February 5, 2010
まとめ
構造的震動は,深いサンアンドレアス断層が活発であり,地殻に構造化されていることを明らかにします.
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:
- サンアンドレアス断層の深い構造と変形は,まだ十分に理解されていない.
- 構造的震動は,深い断層の振る舞いに新しい洞察をもたらします.
研究 の 目的:
- 深いサンアンドレアス断層の物理的性質と変形を調査する.
- カリフォルニア州パークフィールドの近くの地形震動を分析するために.
主な方法:
- 2001年から2008年までの連続的な地震データの分析.
- 構造的震動信号の識別と分解.
- 波形特性に基づいて震動活動の区分.
主要な成果:
- 複雑な震動パターンと断層に沿って観察されたほぼ連続した移住.
- 震動エピソードは,時速15-80kmで20km以上に広がった.
- 地震後の震動の変化は,異質な断層特性とストレス崩壊を示した.
結論:
- サンアンドレアス断層は,地殻の底まで広がる局所的な構造です.
- 震動の再発は,深い断層変形を監視する可能性を示唆しています.
- 深い断層変形は,より浅い地震発生地帯を不安定に負荷する可能性があります.
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