イタリア中部で発生した地震の群れによるゆっくりとした地震の動態に対する制約
1Dipartimento di Scienze della Terra, Universita di Camerino, Camerino (MC), Italy. Istituto Nazionale di Fision Nucleare-Laboratori Nazionali del Gran Sasso (LNGS), L'Aquila, Italy. Dipartimento di Fisica, Universita di L'Aqui.
まとめ
研究者らはイタリアでゆっくりとした地震を観測した. これらのイベントの地震モメントは,上昇時間の平方根でスケールされ,熱拡散に似た緩やかな破裂伝播を示唆しています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
背景:
- 遅い地震は,長期にわたる破裂期間によって特徴づけられる地震現象です.
- そのメカニズムを理解することは,地震の危険性評価に不可欠です.
研究 の 目的:
- イタリア中部で集結した遅い地震の特徴を分析する.
- これらのイベントの地震瞬間と上昇時間との関係を調査する.
主な方法:
- 地質学的干渉計を用いて地震データを記録した.
- 記録されたイベントのストレスの上昇時間と地震の瞬間を分析した.
主要な成果:
- 数回の集結したゆっくりとした地震が記録されました.
- 地震モメントのスケールは,上昇時間の平方根に等しいことが観察されました.
- ストレンの上昇時間は,数十秒から数千秒まで変化しました.
結論:
- 観測されたスケーリング法則は,従来の故障モデリングの仮定に異議を唱える.
- この結果は,熱拡散に類似した緩慢な破裂伝播モデルを支持している.
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