ゆっくりとした地震は,エピソード的な震動とゆっくりとした滑りイベントと一致します
Yoshihiro Ito1, Kazushige Obara, Katsuhiko Shiomi
1National Research Institute for Earth Science and Disaster Prevention, 3-1 Tennodai, Tsukuba 305-0006, Japan. yito@bosai.go.jp
まとめ
日本では,非常に低周波の地震が発生しました.
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
- プレート・テクトニクス (プレート・テクトニクス)
背景:
- 日本南西部のナンカイ潜水地域は,地震活動が顕著な地域です.
- 遅い地震の理解は,地震の危険性を評価するために不可欠です.
研究 の 目的:
- ナンカイ潜水地帯における非常に低周波地震 (VLFE) を調査する.
- VLFE,深度の低周波震動,およびゆっくりと滑り落ちる出来事の間の関係を分析するために.
主な方法:
- VLFEからの地震波の分析.
- 地震データと深い低周波震動とゆっくりと滑り落ちる現象の相関.
主要な成果:
- VLFEは,約20秒の支配的な周期を持つ地震波を発現します.
- VLFEの地震性は,深い低周波震動やゆっくりと滑り落ちる出来事と密接に関連しており,それと移行します.
結論:
- VLFE,震動,およびスロースリップイベントの同時発生は,遅い地震の検出と特徴付けに役立ちます.
- これらの遅い地震現象は,隣接するメガスラスト地震の断裂地帯のストレスを増加させる可能性があります.
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