新马德里地震的触发是普莱斯托纪晚期的侵蚀
E Calais1, A M Freed, R Van Arsdale
1Purdue University, Department of Earth and Atmospheric Sciences, West Lafayette, Indiana 47907, USA. ecalais@purdue.edu
Nature
|July 31, 2010
概括
密西西比海域气候驱动的侵蚀影响了中部大陆的地震. 来自河流切口的卸载减少了地压力,揭开了接近故障的断层,并在新马德里地震区集中了大地震.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 四年纪地质学四年纪地质学
背景情况:
- 大陆板内部和板边界之间的地震行为不同.
- 中大陆断层激活和地震活动持续时间的了解很少.
- 自从最后一个冰河时代以来,新马德里地震区经历了集中的大地震.
研究的目的:
- 为了调查在新马德里地震区集中的大型地震的原因.
- 将中大陆的地震性与气候控制的侵蚀历史联系起来.
- 了解控制断层激活和地震活动持续时间的因素.
主要方法:
- 分析密西西比州北部海湾的侵蚀历史.
- 由于沉积物卸载而导致的石质层曲的建模.
- 模拟上层地和断层行为的应力变化.
主要成果:
- 最近,密西西比河流域的气候控制侵蚀与地震度有关.
- 来自河流切口的石质层曲 (16,00010,000年前) 降低了上层地的正常应力.
- 这种压力减轻揭示了先前存在的故障,使它们接近故障平衡.
结论:
- 密西西比河堤的侵蚀历史是新马德里地震性的关键因素.
- 靠近故障平衡的断片容易发生断裂.
- 卸载和过去的地震造成的压力变化可能会在附近的未被破坏的段落中引发未来的断裂.
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