非火山性震动的演变以及加利福尼亚州圣西缅和帕克菲尔德地区的地震
Robert M Nadeau1, Aurélie Guilhem
1Berkeley Seismological Laboratory, University of California, Berkeley, CA 94720, USA.
概括
在锁定断层附近的非火山震动可能会在地震之前发生. 在两次大地震之后,圣安德烈亚斯断层的震动活动多年来一直保持在高位,这表明累积的压力.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地震科学 地震科学
背景情况:
- 非火山震动是发生在锁定断层附近的地震信号.
- 假设这些震动与地震生成过程有关.
- 了解震动行为对于地震危险评估至关重要.
研究的目的:
- 为了研究大地震与非火山震动活动之间的关系.
- 在圣安德烈亚斯断层发生地震事件后,分析震动模式的变化.
- 为了评估从震行为推断出的压力积累率.
主要方法:
- 持续地对帕克菲尔德地区的圣安德烈亚斯断层进行地震监测.
- 在两次强烈地震之前和之后,对震动速率和周期性的分析.
- 静态剪切和库伦应力变化的计算.
主要成果:
- 两次强烈的地震引发了地震活动的显著增加.
- 震动活动变得升高和周期性,持续超过四年.
- 静态剪切和库伦应力增加与突然震率增加相关.
结论:
- 持续的震动变化表明在圣安德烈亚斯断层的研究部分下方加速的压力积累.
- 这一地区可能会为未来的大型地震积累压力,类似于1857年福特·泰事件.
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