カリフォルニア州パークフィールド近くの地震: 1934年と1966年のシーケンスを比較する
まとめ
サンアンドレアス断層のパークフィールド付近で発生する中程度の地震は,繰り返されるパターンを示しています. 1966年の地震は1934年のシーケンスとよく似ており,予測可能なストレスと故障の振る舞いを示しています.
科学分野:
- 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.
- 地震科学 地震科学 地震科学
背景:
- カリフォルニア州パークフィールドの近くでは,今世紀で4回,中規模地震 (リヒター級M・L,51/2) が発生しました.
- これらの出来事は,主要な構造的境界であるサンアンドレアス断層で起こった.
研究 の 目的:
- パークフィールド近くのサンアンドレアス断層で発生する中規模地震のパターンを分析するために.
- 繰り返される地震の行動と断層地帯のダイナミクスの可能性を調査する.
主な方法:
- 歴史的な地震のシーケンスの比較分析.
- 1901年,1922年,1934年,そして1966年の地震データを調査した.
主要な成果:
- 1966年の地震のシーケンスには,1934年のシーケンスと多くの点で似ている.
- この繰り返しは,断層に沿ってストレスの蓄積と放出の予測可能なパターンを示唆しています.
結論:
- サンアンドレアス断層のパークフィールドセクションは,認識可能で繰り返される地震活動のパターンを示しています.
- これらのパターンを理解することで,地震の予測と危険性評価の改善に寄与できます.
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