在主要热点下面的地球地幔底部植根于宽的羽毛
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Updated: Apr 4, 2026

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Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
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Scott W French1, Barbara Romanowicz1,2,3
1Department of Earth and Planetary Science, Berkeley Seismological Laboratory, University of California at Berkeley, California 94720, USA.
Nature
|September 4, 2015
概括
层中的深层, 作为火点火山的潜在来源, 显示为宽的, 准垂直的管道, 而不是薄的热尾. 这些结构连接到深处的超低速度区域,
科学领域:
- 地质学
- 地震学
- 地幔动力学
背景情况:
- 热点火山的起源是有争议的,热点火山被提出但难以检测.
- 地力学模型表明,纯粹的热应该是薄而难以捉摸的
研究的目的:
- 使用先进的地震技术, 拍摄热点下的深层地幔结构.
- 调查地幔羽毛的物理特征和起源.
主要方法:
- 使用全地幔地震成像技术,结合精确的波场计算和完整的地震波形分析.
- 通过这种方法, 揭示了突出的热点下面的宽, 准垂直管道.
主要成果:
- 已确定从核心-地幔边界延伸到~1,000公里的宽 (非薄) 管道.
- 发现这些管道植根于超低速度区域 (如夏威夷,冰岛,萨摩亚),建立了连接.
- 导管比热模型更宽,表明热化学起源和缓慢的深层地幔循环.
结论:
- 覆盖层的羽毛很宽,寿命很长,而且很可能是热化学的,而不是纯热的.
- 建立了深度超低速度区域和地幔羽毛之间的直接联系.
- 这些发现限制了地幔粘度分层和热化学对流研究.
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