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远程触发的地震能力由7.3级的Landers,加利福尼亚,地震触发
概括
1992年兰德斯地震在美国西部引发了广泛的地震活动. 与地液的非线性相互作用,而不是静态应力,可能解释了这种远程地震触发.
科学领域:
- 地震学 地震学
- 地震科学 地震科学 地震科学
- 地质物理学 地质物理学
背景情况:
- 1992年兰德斯地震 (Mw 7.3) 导致远离震中心的地震活动显著.
- 触发的地震发生在距离1250公里的地区,在现有地震和特定断层风格的地区.
研究的目的:
- 调查Landers主震后引发的广泛地震背后的机制.
- 评估静态应力变化与动态应力相互作用在触发远程地震中的作用.
主要方法:
- 在Landers事件发生后,对地震分布和特征的分析.
- 使用弹性脱位模型计算静态应力变化.
- 考虑动态应变效应和地液相互作用.
主要成果:
- 在Landers地震之后,美国西部的地震活动突然和广泛地增加.
- 被触发的地震集中在地震活跃的区域,通常靠近地热或火山区域.
- 仅仅静态应力变化不足以解释观察到的触发.
结论:
- 兰德斯主震引发远程地震并不能仅仅通过静态应力变化来充分解释.
- 地震波动力应变和地液体 (可能包括岩) 之间的非线性相互作用为广泛触发提供了更合理的解释.
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