作为压力变化的信标,地震是变化的信号
1Lamont-Doherty Earth Observatory, Palisades, New York 10964, USA. nano@ldeo.columbia.edu
Nature
|September 19, 2000
概括
小地震可以充当信标,揭示地的机械状态. 从Landers地震分析压力变化有助于理解断层相互作用,并预测未来的地震事件.
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:
- 由于应力变化,地震会在附近断层引发余震.
- 断层相互作用,影响地震事件的时间和发生.
- 了解地的机械状态对于地震危险评估至关重要.
研究的目的:
- 探索小地震作为地机械状态指标的潜力.
- 为了研究1992年兰德斯地震造成的静态应力变化.
- 使用地震性来确定主要破裂的滑动分布.
主要方法:
- 开发了一种新技术来分析Landers地震的区域地震反应.
- 应用了反向方法来估计主冲击滑动分布的地震性.
- 使用静态应力变化计算.
主要成果:
- 成功测量了对Landers事件的区域地震反应.
- 推导出可信的滑动形状,与来自Landers主震器的直接测量相匹配.
- 证明了静态应力变化与余震模式之间的联系.
结论:
- 小地震可以作为有效的"信标"来监测地的机械状况.
- 该研究提供了一种方法来调查导致故障失效的过程.
- 结果提高了对地震相互作用和断层系统行为的理解.
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