地震断裂被一个沉降的断裂区域所阻碍
D P Robinson1, S Das, A B Watts
1Department of Earth Sciences, University of Oxford, Parks Road, Oxford, OX1 3PR, UK. David.Robinson@earth.ox.ac.uk
概括
2001年秘鲁地震的发生.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 2001年秘鲁地震 (Mw 8.4) 为了解地震破裂动态提供了一个独特的案例研究.
- 俯冲区地震是主要的地震危险,它们的破裂行为很复杂.
研究的目的:
- 调查断层屏障在控制2001年秘鲁地震破裂传播中的作用.
- 分析屏障的特征及其与地震破裂前线的相互作用.
主要方法:
- 分析地震数据,绘制破裂传播的地图.
- 断层区属性和地震活动的表征.
- 断裂动态与地质特征的相关性.
主要成果:
- 破裂在遇到6000平方公里的断层障碍之前传播了70公里.
- 屏障延迟破裂30秒,然后破裂.
- 与周围地区相比,该屏障的破裂速度,滑动和余震密度较低.
结论:
- 潜水板上的断裂区域可能成为破裂的重要障碍.
- 屏障破裂与主要能量释放相吻合,影响了地震的整体大小和持续时间.
- 了解这些障碍对于在俯冲区的地震危险评估至关重要.
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