パンチボウル断層の断裂表面エネルギー,サンアンドレアス系
Judith S Chester1, Frederick M Chester, Andreas K Kronenberg
1Center for Tectonophysics, Department of Geology & Geophysics, Texas A&M University, College Station, Texas 77843-3115, USA. chesterj@geo.tamu.edu
Nature
|September 2, 2005
まとめ
地震の断裂エネルギーは,地震学的データによって著しく過小評価されています. パンチボウル断層の構造分析は,断層の表面の形成は,これまで考えられていたよりもはるかに多くのエネルギーを要求し,追加の滑り弱化のプロセスを示唆しています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 構造地質学 構造地質学
- 地震学 地震学とは
背景:
- 地震の断裂ダイナミクスの構成要素である断裂エネルギーは,その大きさと断裂表面形成と滑り弱化のメカニズムについてほとんど理解されていません.
- 地震学および実験データに基づく既存の推定は,地震破裂のエネルギー予算を完全に説明することはできません.
研究 の 目的:
- 大面積の掘り起こされた断層における断層表面の形成に必要なエネルギーを定量化するために.
- これらの定量化されたエネルギー需要を,地震の断裂エネルギーに関する地震学的推定値と比較する.
- 破裂表面の生成が地震中の全体的な滑り弱化に与える影響を調査する.
主な方法:
- サンアンドレアス断層システムの主要な発掘された断層であるパンチボウル断層の構造分析.
- 観測された断層構造に基づいて,断層表面積と関連するエネルギー需要の定量化.
主要な成果:
- パンチボウル断層の断裂表面面積を生成するのに必要なエネルギーは,地震学者が1つの大きな地震について推定するエネルギーの約300倍です.
- すべての断裂エネルギーを断裂表面の生成にのみ帰属すると,1km未満の地震の移動が観測された表面面積を説明できると示唆されます.
結論:
- 地震の断裂エネルギーに対する地震学的見積もりは,実際のエネルギー予算を大幅に過小評価している可能性があります.
- 断層表面の生成だけでは,大規模な地震における滑り弱化の際に散らばるエネルギーの総量を説明することはできません.
- 表面破裂を超えた追加の物理的プロセスは,地震破裂イベントの際に滑り落ちの弱まりに大きく寄与する可能性があります.
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