直接地震波之前的弹性重力信号的观测和建模
Martin Vallée1, Jean Paul Ampuero2, Kévin Juhel3
1Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, CNRS, France. vallee@ipgp.fr.
概括
早期的地震信号是通过重力变化而不是地震波探测到的. 这种新方法可以使用宽带地震计快速估计大规模地震.
科学领域:
- 地震学
- 地质学
- 重力测量
背景情况:
- 地震预警系统通常依赖于地震波 (P波).
- 引力场的变化发生在光速上,
- 之前对地震引力扰动的检测不够准确.
研究的目的:
- 调查重力扰动作为早期地震信号的可能性.
- 准确地模拟重力变化和相关的运动,用于地震分析.
- 探索使用这些信号来快速确定地震的强度.
主要方法:
- 使用宽带地震仪检测微妙的重力扰动.
- 分析2011年东北地震的数据 (9.1级).
- 开发一种新的形式主义来模拟重力变化和重力诱导的运动.
主要成果:
- 在距离东北地震中心1000-2000公里的宽带地震仪有效地观察到重力扰动.
- 一种新的建模方法准确地捕获了这些迅速的弹性重力信号.
- 这些发现表明使用这些信号进行地震分析的可行性.
结论:
- 迅速的弹性重力信号为了解地震动态提供了新的途径.
- 这项研究为分钟时间尺度大地震的大小确定提供了可能性.
- 重力扰动分析可以显著提高早期地震检测和特征.
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