子温度计揭示了最早的地球上最小的融化条件
1Department of Earth and Environmental Sciences, Rensselaer Polytechnic Institute, Troy, NY 12180, USA. watsoe@rpi.edu
概括
古代的圆表明,早期地球已经调节了温度和海洋. 这些发现表明,一个令人惊的稳定的Hadean Eon,地的形成和循环开始比以前认为的要早得多.
科学领域:
- 地质地质地质地质地质地
- 行星科学 行星科学
- 地球科学 地球科学 地球科学
背景情况:
- 纪 (4.0至4.5亿年前) 传统上被视为一个地力学上暴力的时期.
- 最近的解释表明一个更温和的Hadean,可能有类似地球的海洋.
- 了解哈第安石结晶温度对于这个辩论至关重要.
研究的目的:
- 为了确定来自西澳大利亚杰克山脉的古代石的结晶温度.
- 使用这些温度来推断早期地球在哈第安纪期间的条件.
主要方法:
- 使用专门的温度计分析古代石中含量的分析.
- 哈迪时代石温度与现代花状石生长温度的比较.
主要成果:
- 哈第安石呈现出强烈的结晶温度集群,结晶温度在700°C左右.
- 这些温度与现代花状石生长的温度无法区分.
- 这些发现支持了早期地球上存在潮湿,最低融化的条件的存在.
结论:
- 在哈地亚纪期间,生产含的岩石的规范机制已经存在.
- 在太阳系形成的2亿年内,存在着潮湿的,最低融化的条件.
- 地球可能早在43.5亿年前就已经建立了地形成,侵蚀和沉积物回收过程.
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