在帕克菲尔德的圣安德烈亚斯断层上远程触发断层强度变化
Taka'aki Taira1, Paul G Silver, Fenglin Niu
1Department of Terrestrial Magnetism, Carnegie Institution of Washington, District of Columbia 20015, USA. taira@dtm.ciw.edu
Nature
|October 2, 2009
概括
科学家们开发了一种新的方法来使用圣安德烈亚斯断层的地震数据来监测断层强度. 像2004年苏门答腊-安达曼地震这样的大规模地震,可以远程改变全球断层的强度,可能引发更多的地震活动.
科学领域:
- 地震学 地震学
- 地质物理学 地质物理学
- 地震科学 地震科学 地震科学
背景情况:
- 断层强度对于了解地震的可能性和触发至关重要.
- 在现场监测断层强度变化一直是一个重大挑战.
- 远程触发地震性表明可能对断层行为产生外部影响.
研究的目的:
- 介绍一种用于监测断裂强度的时间变化的新方法.
- 调查大型远程地震对当地断层强度的影响.
- 探索断层强度扰动的全球影响.
主要方法:
- 分析了来自帕克菲尔德地区,圣安德烈亚斯断层的约20年的观测数据 (1987-2008).
- 识别地震散射器属性的时间变化,表明流体迁移.
- 检查重复地震序列的系统变化,以推断断裂强度变化.
主要成果:
- 确定了两种可能的远程断层强度变化的情况,与1992年的登陆者和2004年的苏门答腊-安达曼地震有关.
- 观察到的变化包括地震散射器的变化和重复的地震特征.
- 1992年兰德斯地震可能减少了断层强度,引发了帕克菲尔德随后的地震事件.
结论:
- 大规模地震可能会导致断层强度的显著,长期变化.
- 这些变化可能是由流体迁移驱动的,可以影响地震性.
- 这些发现表明,大地震可能对断层系统产生全球影响,可能导致集群地震.
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