在地球内核顶部地震速度的半球变化
1Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road NW, Washington DC 20015, USA. niu@dtm.ciw.edu
Nature
|April 27, 2001
概括
地球上的地震速度变化.
科学领域:
- 地质物理学,地震学,地球科学
背景情况:
- 了解地球内核的地震速度结构对于阐明内核生长过程至关重要.
- 之前的地震研究主要研究了深度超过100公里的结构,对内核最上层100公里的数据有限.
研究的目的:
- 为了限制直接在内核边界下方的地震速度变化.
- 为了研究最上层内核内的地震速度的区域差异.
主要方法:
- 在内核边界反射和通过内核边界传输的地震波之间的旅行时间差异的分析.
- 利用来自全球地震仪站和区域地震网络的数据.
- 检查了波浪的旅行时间余量,采样了内核的不同半球区域.
主要成果:
- 观察到的系统旅行时间余量大约为0.8秒,对于采样"东半球"的波浪,与内核的"西半球"相比.
- 没有发现残余和波穿越角度之间的相关性,这表明该地区的地震异性极小.
- 确定东部内核的同otropic地震速度大约比西部内核高0.8%.
结论:
- 地球最上层的内核表现出显著的区域速度异质性.
- 内核的东半球具有比西半球更高的同位带地震速度.
- 这些发现为控制内核生长和结构的物理过程提供了新的见解.
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