2004年苏门答腊-安达曼地震后,GRACE观察到的地扩张
Shin-Chan Han1, C K Shum, Michael Bevis
1Geodetic Science, Department of Geological Sciences, Ohio State University, 275 Mendenhall Laboratory, 125 South Oval Mall, Columbus, OH 43210-1398, USA.
重力恢复和气候实验 (GRACE) 卫星检测到地震引起的重力变化. 这种基于太空的测量提供了2004年苏门答腊-安达曼地震对地扩张的证据.
科学领域:
- 地质物理学 地质物理学
- 卫星地质测量是如何实现的
- 地震学 地震学
背景情况:
- 地震造成显著的变形,改变地球的重力场.
- 基于太空的地质测量测量为地震事件提供了全球视角.
研究的目的:
- 报道了第一次基于太空的地震引力变化的探测.
- 用卫星数据分析2004年苏门答腊-安达曼地震造成的重力场变化.
主要方法:
- 利用来自重力恢复和气候实验 (GRACE) 卫星的数据.
- 分析了地震后观察到的+/-15-microgalileo重力变化.
主要成果:
- 检测到显著的重力异常,归因于co-seismic变形.
- 观察到垂直移位和膨胀效应的贡献大致相同.
- 提供了海底地震导致地扩张的证据.
结论:
- 基于太空的重力测量对于检测地震引起的变形是有效的.
- 格雷斯 (GRACE) 数据揭示了在大海底地震中发生的复杂物理过程的洞察力.
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