日本,関東盆地における地震地運動の拡散,日本
1Earthquake Research Institute, University of Tokyo, Tokyo 113-0032, Japan. inquiry@taro.eri.u-tokyo.ac.jp
まとめ
マグニチュード5.7の地震は,地震波が関東盆地を通過する方法を明らかにした. 地表波は,盆地端で折れ,盆地内の速度が遅くなり,波の伝播パターンに影響を与えます.
科学分野:
- 地震学 地震学とは
- 地震工学は,地震工学である.
- 地質物理学 地質物理学とは地質物理学です.
背景:
- 地震波の伝播を理解することは,地震の危険性評価に不可欠です.
- 沈殿盆地では,地震の際に地表運動の特徴を大幅に変化させることができます.
研究 の 目的:
- 関東堆積盆地内の長期地運動の伝播を分析する.
- 盆地縁の表面波折れ現象を調査する.
主な方法:
- 384個の強度の地面運動測定器から得られたデータを利用した.
- 東京近郊で起きたマグニチュード5.7の地震による地上の動きを記録した.
- 関東盆地における地震波の伝播パターンを視覚化しました.
主要な成果:
- 関東盆地の縁の表面波の折射を観測した.
- 折れた波は震源から直接ではなく,斜めに移動することを示した.
- 周辺地域と比較して,盆地内の表面波の伝播速度が遅いことを特定しました.
- 折れた波が,盆地と周辺地域の速度差を調和させる方法を示した.
結論:
- この研究は,堆積層の盆地における複雑な地震波の振る舞いを視覚化しています.
- 盆地辺の表面波折れは,地面運動に影響を与える重要な要因です.
- 折れた到着は,特に関東盆地の縁の近くで優勢です.
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