潜水 巨大地震 の 隠された 単純さ
M-A Meier1, J P Ampuero2, T H Heaton2
1Seismological Laboratory, California Institute of Technology, Pasadena, CA, USA mmeier@caltech.edu.
まとめ
大規模な潜水地域地震は,明らかな変動にもかかわらず,普遍的な破裂行動を示す. この発見は,地震の大きさを 破裂の始まりの特徴だけで予測できないことを示しています.
科学分野:
- 地理学
- 地震学
- 地震科学
背景:
- 潜水界面での巨大地震は最大で最も破壊的なものです.
- 物理と早期警告システムにとって 破裂の振る舞いを理解することは 極めて重要です
- 単純で統一的なモデルを阻害していました
研究 の 目的:
- 大規模な潜水地帯の地震破裂の普遍的な行動を調査する.
- メガトラストの変動を 統一モデルで説明できるかどうかを判断する.
主な方法:
- 3つのソース時間関数 (STF) データセットの分析.
- 震度 (Mw) ≥7の潜水地域地震に注目する.
主要な成果:
- 典型的な,普遍的な行動は,大きな潜水地帯の地震で特定されました.
- 中央のSTFはスケーラブルで 線形に成長し ほぼ三角形です
- 平均行動からの偏差は,事件の大きさに比例し,掛け算であり,ガウス型です.
結論:
- 明らかな違いにもかかわらず 大規模なメガストラストの破裂は 共通の基本的な行動を共有しています
- 地震の大きさは,この普遍的な行動に基づいた断裂発生の特徴から予測できません.
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