概括
在新马德里地震区检测到的快速地压力积累表明,未来内部板块地震的风险增加. 这一发现对于地震活跃地区的地震危险评估至关重要.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地质测量是指地质测量.
背景情况:
- 新马德里地震区 (NMSZ) 具有重要的历史地震性,包括1811年至1812年发生的三次大地震.
- 内部板块地震区对危险评估构成独特的挑战,原因是很少发生大型事件.
研究的目的:
- 评估目前在南NMSZ的地菌株积累情况.
- 评估未来在该地区造成破坏性的板内地震的可能性.
主要方法:
- 使用全球定位系统 (GPS) 重新测量历史三角网络.
- 对地质测量数据进行分析,以检测地变形模式.
主要成果:
- 自20世纪50年代以来,人们已经观察到显著而快速的地菌株积累.
- 观察到的应变与沿着东北趋势的断层的右侧冲击滑动运动一致.
- 当前的地震性模式与推断的断层方向保持一致.
结论:
- 地应变检测是识别未来内板地震风险区域的宝贵工具.
- 即使没有最近的大型历史地震,NMSZ也表现出持续的变形,表明潜在的地震危险.
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