在夏威夷Kīlauea火山的无声滑动事件引发的地震,夏威夷
Paul Segall1, Emily K Desmarais, David Shelly
1Geophysics Department, Stanford University, Stanford, California 94305, USA.
Nature
|July 11, 2006
概括
伴随Kīlauea火山缓慢滑动事件的高频地震表明引发了地震活动. 这一发现有助于限制静音地震的深度,并评估相关的危险.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 火山学 火山学是一门学科.
背景情况:
- 缓慢滑动事件,或"静音地震",发生在俯冲区,但它们的深度很难确定.
- 与高频地震相关,易于定位,很少见,阻碍了深度限制.
- 非火山性震动有时伴随着缓慢的滑动,但很难准确地定位.
研究的目的:
- 为了研究缓慢滑动事件和高频地震之间的关系.
- 通过分析伴随的地震性来确定缓慢滑动事件的深度.
- 了解与缓慢滑动事件相关的触发机制和潜在危险.
主要方法:
- 对伴随Kīlauea火山缓慢滑动事件的地震群的分析.
- 地震活动与缓慢滑动事件进展的相关性,特别是2005年1月事件.
- 应用库伦应力变化原理来推断地震触发.
主要成果:
- 观察到大量的高频地震伴随着Kīlauea的缓慢滑落.
- 2005年1月的缓慢滑动事件在地震性增加之前发生,这表明引发了地震.
- 在7-8公里深的地震限制了缓慢滑落到可比的深度.
结论:
- 高频地震可以由缓慢滑动事件触发,提供深度限制.
- 检测触发的地震性对于了解缓慢滑动事件深度和危险至关重要.
- 这种关联为量化缓慢滑动事件期间增加的地震危险提供了一个潜在的方法.
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