在现代新马德里地震区的断层滑坡率
1Department of Geological Sciences, University of Colorado, Boulder, CO 80309-0399, USA. Department of Geology, University of Arkansas, Fayetteville, AR 72701, USA. William Lettis and Associates, 1777 Botelho Drive, Suite 262, Walnut Creek, CA 945.
概括
晚期Holocene沉积物揭示了位于新马德里地震区的Reelfoot推力断层上方的断层相关折叠. 这项研究量化了滑动率,这对于了解该地区的地震危险至关重要.
科学领域:
- 地质地质地质地质地质地
- 地震学 地震学
- 地质物理学 地质物理学
背景情况:
- 新马德里地震区是美国中部一个具有重大地震危险的地区.
- 了解盲断层活动对于地震风险评估至关重要.
研究的目的:
- 分析湖县地区的晚期Holocene沉积物,以了解Reelfoot推力断层上方的变形.
- 量化Reelfoot推力断层和新马德里地震区的滑动率.
主要方法:
- 晚期Holocene沉积物的结构和地形分析.
- 模拟Reelfoot痕作为断层曲折叠的前肢,使用沟暴露的曲折带宽度.
- 使用结构缓解和估计的断层深度计算滑动率.
主要成果:
- 沉积物因盲目Reelfoot推力断层上方的断层相关折叠而变形.
- 在盲目推力上的滑动率估计在过去的2300年+/- 100年中为6.1+/- 0.7mm/年.
- 对盲目推力的替代滑动率计算产生了4.8 +/- 0.2 mm/年.
- 据估计,新马德里地震区的右侧滑动率为每年1.8至2.0毫米.
结论:
- 里尔脚推力断层活跃,并导致新马德里地震区的变形.
- 滑动率数据为该地区的地震潜力提供了关键的见解.
- 几何关系表明右侧滑动对整体地震区域活动的具体贡献.
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