古代的上层地从地转变为地板构造的开始
Ming Tang1, Kang Chen2, Roberta L Rudnick3
1Department of Geology, University of Maryland, College Park, MD 20742, USA. Corresponding author.
概括
在阿基亚时代,早期的大陆地从地变为地. 这种由地质量增加的变化表明全球板块构造大约在30亿年前开始.
科学领域:
- 地质学
- 地质化学
- 早期的地球科学
背景情况:
- 古代时代 (4.02.5亿年前) 对早期大陆地的形成和生命的出现至关重要.
- 由于随后的地质过程,大陆地的初始组成尚不清楚.
- 了解早期地的演化是解读地球早期历史的关键.
研究的目的:
- 重建大陆上层的MgO组成.
- 确定早期大陆地的组成变化的时间.
- 研究地的演变与板块构造的开始之间的关系.
主要方法:
- 在古土壤沉积岩中分析Ni/Co和Cr/Zn的比率.
- 考古火岩和火岩岩的分析.
- 在上大陆地中大量MgO组成的地化学跟踪.
主要成果:
- 在30亿至25亿年前,古老的上层大陆地从地形变为体.
- 在这个时期,上大陆地的质量增加了五倍.
- 增加的花岩石有助于地质量的增加.
结论:
- 古代地的组成演变表明了岩过程的重大变化.
- 表面质量的大幅增加表明地生成率有所提高.
- 这些发现支持全球板块构造大约在30亿年前开始的假设.
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