2004年苏门答腊 - 安达曼地震的破裂过程
Charles J Ammon1, Chen Ji, Hong-Kie Thio
1Department of Geosciences, Pennsylvania State University, 440 Deike Building, University Park, PA 16802, USA. cammon@geosc.psu.edu
2004年苏门答腊-安达曼地震开始缓慢,然后迅速向北-西北方向破裂,超过1200公里. 这次巨大的海底地震造成了海底的巨大变迁,造成了广泛的破坏.
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:
- 2004年苏门答腊-安达曼地震是一个具有重大全球影响的重大地震事件.
- 了解这么大的地震的断裂动态对于危险评估至关重要.
研究的目的:
- 分析2004年苏门答腊-安达曼地震的发起和传播特征.
- 量化沿板边界的滑动分布和破裂速度.
主要方法:
- 分析地震数据以确定断裂速度和持续时间.
- 对地震波的建模以估计滑动分布和位移.
- 检查余震模式以推断断裂的复杂性.
主要成果:
- 地震以缓慢的破裂阶段 (40-60秒) 开始,然后加速到~2.5公里/秒.
- 断裂沿着安达曼峡谷延伸了1200-1300公里.
- 沿着600公里的段落,峰值滑坡达到了15米,北部部分滑坡减少.
结论:
- 苏门答腊-安达曼地震表现出复杂的断裂行为,开始缓慢,然后迅速传播.
- 沿断层发生了显著的滑动变化,表明异质的破裂过程.
- 一些滑动可能发生在传统的地震频段之外,这表明了复杂的故障机制.
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