来自环境地震噪声的高分辨率表面波断层扫描
Nikolai M Shapiro1, Michel Campillo, Laurent Stehly
1Center for Imaging the Earth's Interior, Department of Physics, University of Colorado at Boulder, Boulder, CO, USA. nshapiro@ciei.colorado.edu
概括
地震噪声分析揭示了加利福尼亚州的地震噪声.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地球科学 地球科学 地球科学
背景情况:
- 了解地球地的结构对于地质和地震危险评估至关重要.
- 传统的地震成像方法在分辨率和数据采集方面可能受到限制.
研究的目的:
- 开发和应用一种新的方法来成像加利福尼亚的地结构.
- 为了利用环境地震噪声进行高分辨率的地质物理成像.
主要方法:
- 加利福尼亚州USArray站记录的环境地震噪声与交叉相关.
- 对于站间路径,获得了表面波群速度测量.
- 加利福尼亚的地质单位的断层图像是使用这些测量来构建的.
主要成果:
- 产生了数百个短时间的表面波群速度测量结果.
- 断层图像清楚地划出了主要的地质单位.
- 低速异常与沉积盆相关;高速异常与山脉核心相关.
结论:
- 环境地震噪声的交叉相关性为地成像提供了有效的表面波数据.
- 与传统方法相比,这种技术提高了地图像的分辨率和真实性.
- 该研究成功地利用地震噪声绘制了加利福尼亚州的主要地质单位的地图.
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