ゆっくりとした地震と巨大な地震を結びつける
Kazushige Obara1, Aitaro Kato2
1Earthquake Research Institute, University of Tokyo, Bunkyo, Tokyo 113-0032, Japan. obara@eri.u-tokyo.ac.jp.
まとめ
ゆっくりとした地震は 伝統的な地震とは違って 巨大地震の物理学の洞察を与えてくれます これらの出来事の監視は 重要なストレスメーターとして機能し 大規模な地震を予測する可能性があります
科学分野:
- 地震学
- 地震物理学
背景:
- 遅い地震は,伝統的な地震とは異なる様々な断層滑り行動と地震放射線を示します.
- 震源地帯の内にある巨大地震と 滑り込みメカニズムを共有しています
研究 の 目的:
- 巨大地震の物理を理解するために ゆっくりとした地震を模倣する.
- 地震発生地における 感度計として 遅い地震の可能性を調査する.
主な方法:
- 断層の滑り方と地震放射線パターンの比較分析
- 遅い地震の発生とそのストレス変化のモニタリング
主要な成果:
- ゆっくりとした地震は,巨大地震を研究するための貴重な類似点として機能します.
- ストレスの変化に対する高い感受性により 効果的なストレスの計測器として機能します
結論:
- 頻繁に起こるゆっくりとした地震は 巨大地震の物理的性質を 明らかにするかもしれません
- 遅い地震の監視は,ストレスの移転を追跡することによって,迫り来る大きな地震の予測を高めることができます.
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