1999年のMW 7.6のイズミット地震の拡張核化
Michel Bouchon1, Hayrullah Karabulut, Mustafa Aktar
1Centre National de la Recherche Scientifique and Université Joseph Fourier, Grenoble, France. Michel.Bouchon@ujf-grenoble.fr
まとめ
大規模な地震は,ゆっくりと滑り落ちる現象が先行する可能性があります. 1999年のイズミット地震では,地震信号が44分間加速し,動的断裂の前に断層がゆっくりと滑り落ちることを示した.
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
- 地震科学 地震科学 地震科学
背景:
- 実験室と理論の研究では,地震はゆっくりと滑り落ちる不安定性から始まると示唆されています.
- 地震前のプロセスを理解することは,地震の危険性評価に不可欠です.
研究 の 目的:
- 1999年のイズミット地震の前の地震信号を調査するために.
- 動的破裂前にゆっくりと滑る段階の証拠を特定するために.
主な方法:
- 1999年のイズミット地震の地震データ分析.
- 低中心部から発する地震信号の調査,繰り返し発生する爆発と低周波ノイズを含む.
主要な成果:
- 久しぶりの地震信号は,イズミット地震より44分前に発生した.
- 信号は,加速した地震爆発と低周波の地震騒音の増大から構成された.
- これは,脆い地殻の底部でゆっくりと滑る段階を示し,時間の経過とともに加速します.
結論:
- 1999年のイズミット地震は,44分間のスロースリップ・フェーズが先行した.
- このスロースリップは加速し,メインの断裂の前の最後の2分間で急速な加速に終わった.
- 観測は,大規模な地震の前にゆっくりと滑り落ちるという仮説を裏付けている.
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