表面の折りたたみによって明らかになった地震の可能性:1983年 コリンガ,カリフォルニア,地震
まとめ
1983年のコアリンガ地震は,地表を破裂させるのではなく,地殻の層を弾性的に折りたたんだ. 地震学,地質学,地質学的データの分析により,地下の断層滑り率と地震再発の間隔が明らかになりました.
科学分野:
- * 地震学とテクトニクス
背景:
- * 1983年のコアリンガ地震 (Mw 6.5) は,地表の堆積物が破裂しなかった.
- * それどころか,上層地殻の弾性折りたたみを引き起こした.
研究 の 目的:
- * 地下断層滑り率を推定するために.
- * コアリンガ地域における地震の繰り返しの時間を決定する.
- * 隠された逆断層と活発な折りたたみとの関係を調査する.
主な方法:
- * 地震データの統合.
- * ジオデシカル測定の活用.
- *地質学的証拠の分析. 地質学的証拠の分析.
主要な成果:
- * 地震の結果,浅い地殻の弾性折りたたみが発生した.
- * 地下断層滑り率と地震再発の間隔を推定した.
- *過去20年間に発生した3つのより大きな地震 (最大7.5MW) は,活発な折りたたみの下の盲目逆断層で発生しました.
結論:
- * 地震は,表面の折りたたみの下に隠された断層で発生することがあります.
- * 弾性地殻変形は地震の発生において重要な役割を果たします.
- * ブラインド・フォールティングの理解は,地震リスクの評価に不可欠です.
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