まとめ
1975年のオロビルの地震.
科学分野:
- 地震学 地震学とは
- 構造地質学 構造地質学
背景:
- 1975年8月1日のカリフォルニア州オロビル地震は,多くの余震を引き起こした.
- 原因の断層を理解することは,この地域の地震リスクの評価に不可欠です.
研究 の 目的:
- 1975年のオロビル地震の断層平面の幾何学と動力学を特徴づける.
- 欠陥と現地インフラストラクチャの関係を決定する.
主な方法:
- 断層平面の寸法と向きを定義するために,余震分布の分析.
- P波の最初の動きを使用して焦点機構の決定.
主要な成果:
- 断層平面は南北方向に衝突し,西60度沈み,10kmの深さまで落ちる.
- 正常な断層が特定され,西ブロック (グレートバレー) は東ブロック (シエラネバダ) に比べて倒れた.
- 断層平面の北の範囲は,オロビルダムと貯水池の下に位置しています.
結論:
- 1975年のオロヴィル地震は,西に沈む断層の正常な断層によるものだった.
- この断層がオロビルダムに近いことは,重要なインフラストラクチャに対する潜在的な地震リスクを強調しています.
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