まとめ
地震のエネルギー放出パターンは,深さによって異なります. 深い地震は,中間地震とは異なり,対称的なエネルギー放出を示し,断層破裂のスタイルの変化を示唆しています.
科学分野:
- 地震学 地震学とは
- 地震の断裂のダイナミクス
背景:
- 地震のエネルギー放出パターンは,故障の故障プロセスに関する洞察を提供します.
- 地震の深さ (100 km 以下の) を理解することは依然として困難です.
研究 の 目的:
- 中級地震と深度地震における地震エネルギー放出の時間的なパターンを調査する.
- 破裂行動の系統的な変化を深度が増加するにつれて識別する.
主な方法:
- 地域地震配列から積み重ねられたテレシーミック記録の分析.
- 122の中間 (100~350km) と深 (350~700km) の地震を研究した.
主要な成果:
- 中程度の深さの地震は,断裂の初期により多くのエネルギーを放出します.
- 深い地震は,突然の始まりと終わりで,対称的なエネルギー放出を示します.
- 短期の地震放射線パターンが深さによって体系的に変化することが観察されました.
結論:
- 破裂のスタイルは,深さによって大きく異なります.
- 断層のヘテロゲニティが深さと共に減少することは,地震の断裂行動に影響を与える可能性が高い.
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