古磁场强度的变化表明中原生代内核形成
A J Biggin1, E J Piispa2, L J Pesonen3
1Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool L69 7ZE, UK.
Nature
|October 10, 2015
概括
地球的内核大约在15亿年前开始生长,这标志着行星进化的关键时刻. 这一发现基于古磁数据, 支持地球热史的简单模型.
科学领域:
- 地质学
- 星球科学
- 古磁论
背景情况:
- 地球的内核通过液体铁的固化而成长.
- 由于导热值不同,内核核形成的时间估计差异很大 (0.5到20亿年前).
- 内核核形成对行星的热进化和地气动力产生重大影响.
研究的目的:
- 精确地球内核核形成的时间.
- 研究地磁场强度的长期变化.
- 提供支持地球热演变的具体模型的证据.
主要方法:
- 一个扩展的前剑桥古磁强度数据库的分析.
- 采用新的可靠性标准来选择古磁数据.
- 对地磁场强度和地质时间尺度上的变化进行检查.
主要成果:
- 这项研究提供了基于强度的支持,
- 发现了地磁强度长期变化的确证据.
- 平均场强度和变异性在10亿至15亿年前显著增加.
结论:
- 观察到的地磁场强度的转变强烈地表明内核核形成发生在10亿至15亿年前.
- 这种计时支持温和的核心导热值.
- 这些发现与地球的简单热进化模型一致.
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