2023年2月6日の東トルコの地震のシーケンスの表面変形
Jiannan Meng1,2, Timothy Kusky1,2,3, Walter D Mooney4
1State Key Laboratory of Geological Processes and Mineral Resources, Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China.
まとめ
2023年2月6日にトルコで起こった2つの大きな地震は,複雑な破裂ダイナミクスを示した. この研究は,死海と東アナトリアの断層地帯の間の表面変形と滑り移転を記録しています.
科学分野:
- 地震学
- 構造学
- 地理学
背景:
- 2023年2月6日,トルコでマグニチュード (Mw) 7.8とMw 7.5の2つの強力な地震が発生した.
- 地震は死海断層地帯から始まり,破裂は東アナトリア断層地帯 (EAFZ) に移った.
- 2番目の大きな地震はMw 4.5の余震が先行し,因果関係を示唆しました.
研究 の 目的:
- 滑り落ちた断層の表面の偏移と動力学を定量的に記録する.
- 大規模な大陸衝突地震の表面変形を分析する.
- 複雑な断層システム間の断裂伝播機構と滑り移転を調査する.
主な方法:
- 地面の偏移の量的な地上および空間のドキュメントの収集.
- 断層動力学と表面変形の分析
- 破裂の拡散と移転を理解するために地震データ分析.
主要な成果:
- 表面の偏移と故障動力学の詳細なドキュメントを取得しました.
- 東アナトリア断層地帯 (EAFZ) で最大の移転とエネルギー放出が発生した.
- 余震と第2の大地震の間の因果関係が示唆されています.
結論:
- 大規模な大陸の地震の表面変形に関する重要なデータを提供しています.
- 複雑な故障システム間の滑り移転メカニズムが解明されました.
- リンクされた断層系が地球板の動きに対応する方法についての洞察が得られた.
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