津波発生の巨大地震を調査する
Shuichi Kodaira1, Takeshi Iinuma2, Kentaro Imai2
1Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan kodaira@jamstec.go.jp.
まとめ
2011年の東北大震災は,予期せぬ浅い断層滑落を示した. 地震後の地震活動と変形は継続しており,すぐに別の大きな地震が発生する可能性は低い.
科学分野:
- 地球科学
- 地震学
- 地理学
背景:
- 日本溝は 破壊的な地震と津波で知られる 沈殿地です
- この地域では太平洋プレートが北米プレートの下に沈む.
- 2011年の東北大震災は重大な結果をもたらした大きな出来事でした.
研究 の 目的:
- 2011年の東北大震災の地震,地質学,津波データを分析するためです.
- コセイズミック断層の特徴,特にその浅い範囲を調査する.
- 東日本における継続的な地震活動と地殻の変形を理解するために
主な方法:
- 密集した地震,地質学,津波観測ネットワークを利用した.
- 詳細に記録するための海底観測.
- フォールトスリップの変動を分析するために海洋地質学の研究を適用しました.
主要な成果:
- 大規模なコセイズム断層が 予期せぬ形で 浅いメガスラスト断層に広がった
- 溝の近くで 強い横向きの変動を記録した
- 地震後の東日本における継続的な高い地震活動と地殻変形を観測した.
結論:
- 2011年の東北大震災の浅い滑落は,この出来事の重要な特徴でした.
- 斜面の滑り方によって 溝の近くの地質学的な制御が 示唆されています
- 近いうちにマグニチュード9の地震は起こりそうにないが,海底の正常な断層地震は将来の潜在的な危険である.
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