冰川的地震 冰川的地震
Göran Ekström1, Meredith Nettles, Geoffrey A Abers
1Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA. ekstrom@seismology.harvard.edu
概括
科学家们在冰川下发现了中度地震,由于低高频地震辐射,以前没有被检测到. 这些冰川地震涉及缓慢的冰滑,持续时间比构造地震要长得多.
科学领域:
- 地质物理学 地质物理学
- 冰川学的冰川学
- 地震学 地震学
背景情况:
- 在冰川下方发生的中度地震基本上没有被发现.
- 由于独特的地震辐射模式,传统的地震方法经常错过这些事件.
研究的目的:
- 报告检测到以前未知的中度地震发生在大型冰川下面.
- 描述这些冰川地震的地震源和行为.
主要方法:
- 使用先进的地震波形分析检测地震事件.
- 从一个记录良好的事件中对长期地震波形进行反向建模.
主要成果:
- 在冰川下发现了数十次以前未知的中度地震.
- 这些事件的地震辐射在高频率下被耗尽.
- 源机制被确定为冰川冰的滑动,下坡滑动.
- 冰川地震的持续时间 (30-60秒) 是类似规模的构造地震的15-30倍.
结论:
- 冰川地震是一个独特的地震现象.
- 缓慢滑动的机制解释了它们以前的难以捉摸性.
- 对冰川地震性的进一步研究是有必要的.
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