日本南西部の沈殿に関連した非火山深い震動
1National Research Institute for Earth Science and Disaster Prevention, Tenno-dai 3-1, Tsukuba, Ibaraki, 305-0006, Japan. obara@bosai.go.jp
まとめ
日本の非火山地帯では,フィリピンの海プレートに沿って深い震動が起こりました.
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
背景:
- 深い震えは,地殻の大きな深さで発生する地震現象です.
- 震動発生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:
- 日本の南西部の非火山地帯で,深い,長期の震動を特定し,位置づけること.
- 震動の分布とフィリピン海板の沈下との関係を調査する.
主な方法:
- 地震データ分析により,深い地震を検知し,その位置を特定します.
- 潜水板の幾何学と深さの地球物理的マッピング.
主要な成果:
- フィリピンの海板の600キロメートルの範囲で,深い長期震動が確認されました.
- 地震はモホロビッチ断絶点の近く,平均30キロの深さで発生した.
- 個々の震えは数週間続いた.
結論:
- 震動の空間的分布は,潜水板とのつながりを示唆しています.
- スラブ内の脱水プロセスからの液体生成は,これらの深い震動の潜在的な原因です.
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