在苏门答腊地震之后,在阿拉斯加的兰格尔山 (Mount Wrangell) 定期触发地震
Michael West1, John J Sánchez, Stephen R McNutt
1Alaska Volcano Observatory, Geophysical Institute, University of Alaska, Fairbanks, AK 99775, USA. west@gi.alaska.edu
概括
来自遥远地震的地表波引发了在万雷格尔山附近的局部地震. 这种地震群发生在雷利波地面运动的相位上,这表明在正常断层上出现了简单的剪切故障.
科学领域:
- 地震学 地震学
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
背景情况:
- 2004年苏门答腊地震产生了强大的地表波.
- 温格尔山附近的地震站提供了关键数据.
研究的目的:
- 为了研究遥远的地表波引发局部地震的原因.
- 了解表面波动与当地地震活动之间的关系.
主要方法:
- 分析了Wrangell山的地震数据.
- 当地地震发生与雷利波移动的相关性.
- 计算水平延伸应力.
主要成果:
- 在温格尔山附近引发了11分钟的14个地方事件的地震群.
- 地震发生时与雷利波的正垂直地面移位相一致.
- 雷利波运动表现出高达25千帕斯卡尔的水平延伸应力.
结论:
- 遥远的地表波可以触发局部地震.
- 触发机制涉及正常故障的简单剪切故障.
- 观测突出了大规模地震事件对当地构造学的影响.
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