在帕克菲尔德的圣安德烈亚斯断层沿线的地震后放松,来自连续的地震观测
F Brenguier1, M Campillo, C Hadziioannou
1Sismologie, Institut de Physique du Globe de Paris (IPGP) and CNRS, 4 Place Jussieu, 15252 Paris, France. fbrengui@ipgp.jussieu.fr
概括
大规模的地震改变了圣安德烈亚斯断层沿线的地特性,导致地震速度的变化和非火山性震动. 这些效应持续多年,表明断层区域的长期扰动.
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:
- 大规模的地震可以显著改变断层区域的物理特性.
- 了解这些扰动对于地震危险评估至关重要.
研究的目的:
- 调查大地震对圣安德烈亚斯断层区域地物质的长期影响.
- 为了将地震速度变化与非火山震动活动相关联.
主要方法:
- 使用环境地震噪声相关性对地震速度变化的分析.
- 监测非火山震动活动.
- 与全球定位系统 (GPS) 获得的滑后数据进行比较.
主要成果:
- 2003年圣西门和2004年帕克菲尔德地震降低了地震速度.
- 在地震后的圣安德烈亚斯断层上观察到非火山性震动活动的增加.
- 帕克菲尔德地震发生后,减速和震动活动在帕克菲尔德地震发生后的3年内仍然很高,随着时间的推移而衰减.
结论:
- 地震速度的变化与浅层的共地震损伤和深层应力变化/放松有关.
- 非火山震动活动是断层区域地震后过程的敏感指标.
- 地震会对圣安德烈亚斯断层区的机械性能产生持久的改变.
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