チ・チ地震のシーケンス: 台湾で活発でシーケンス外推力断層が発生
1Institute of Earth Sciences, Academia Sinica, Nankang, Taipei, Taiwan 115, Republic of China. Department of Geology and Mid-America Earthquake (MAE) Center, University of Illinois, Urbana, IL 61801, USA.
まとめ
1999年のチ・チ地震のシーケンスは,主に中等に低下する推力断層によって発生した. より深い地震地帯が存在し,無地震の基礎脱皮と正常な断層を示唆しています.
科学分野:
- 地震学 地震学とは
- テクトニクス (地質学) とは
- 地質学 地質学 地質学
背景:
- 台湾の1999年のチチ地震は,大きな地震の出来事でした.
- 原因となる断層構造を理解することは,地震リスクの評価に不可欠です.
研究 の 目的:
- 1999年9月20日のチチ地震の発生に起因する主要な断層構造を特定する.
- 台湾中部の地下地質と地震地帯を調査する.
主な方法:
- 40以上の地震の正確な焦点深さと断層平面の解を組み合わせた.
- 合成された地下地質データ.
主要な成果:
- 主要で中等に沈む推力断層 (20〜30度) を特定し,変形フロントから離れて地震を生成しました.
- 2つ目のサブパラレル地震地帯が,主推力の約15km下に発見されました.
- 基礎脱皮とリリカ正常断層の両方がアセイミックであるように見える.
結論:
- 特定された地震帯は,台湾の構造構造の以前のモデルとは異なる.
- この研究は,アセイミックな基礎脱皮と正常な断層が地域の地震構造に役割を果たしていることを示唆しています.
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