全球表面波断层扫描使用地震声
Kiwamu Nishida1, Jean-Paul Montagner, Hitoshi Kawakatsu
1Earthquake Research Institute (ERI), The University of Tokyo, 1-1-1, Yayoi, Bunkyo-ku, Tokyo, Japan. knishida@eri.u-tokyo.ac.jp
概括
地震声,地球的背景振动,提供了一种新的方法,用于在没有地震的情况下进行上层地幔断层扫描. 这项技术绘制了3D S波速度结构,推进了行星内部探索.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 行星科学 行星科学
背景情况:
- 全球表面波断层扫描传统上依赖于大型地震来探测地球的深层内部.
- 长期的地震波是深层地球探索所必需的,以前人们认为这些地震波是主要的地震事件所产生的.
- 发现地震,地球从海洋/大气来源的连续自由振荡,提出了一个替代的地震波源.
研究的目的:
- 开发和呈现使用地震声的全球上层地幔地震断层扫描,独立于地震数据.
- 测量雷利波在100到400秒的周期中的相速异常.
- 为了逆转这些异常,为上层地幔的三维S波速度结构.
主要方法:
- 利用地震声作为地震波生成的来源.
- 模拟了54个分布在全球的地震站对之间的交叉相关函数.
- 执行相速异常的反转,以导出3D S波速度结构.
主要成果:
- 通过使用地震气成功生成了全球上层地幔地震断层扫描.
- 映射了雷利波的相位速度异常,跨越了长时间 (100-400秒) 的范围.
- 获得了上层地幔的详细的三维S波速度模型.
结论:
- 地震声为全球地震断层扫描提供了一种可行且新的地震替代方案.
- 开发的技术可以探索陆地行星的三维内部结构.
- 这种方法特别适用于有大气和/或海洋的行星,包括火星.
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