从海底地构建的古老地
Jonathan O'Neil1, Richard W Carlson2
1Department of Earth and Environmental Sciences, University of Ottawa, Ottawa, Canada. jonathan.oneil@uottawa.ca.
概括
古老的加拿大岩石揭示了早期的地球过程. 哈德逊湾的新古时期状地是由较古老的状地形成的,这挑战了关于早期地生存的先前观点.
科学领域:
- 地质化学
- 早期地球地质
- 同位素地质学
背景情况:
- 地球表面的过程已经消除了地球最初的地的大部分证据.
- 加拿大东北部的哈德逊湾地层包含新古时期的皮,是东北部高级省份的一部分.
- 了解早期地形成是解读地球历史的关键.
研究的目的:
- 研究新古哈德逊湾土壤的起源和演变.
- 为了确定这个地区的古老地的年龄和来源.
- 使用同位素数据重建早期的地球地过程.
主要方法:
- 分析新-142 (142Nd) 和新-143 (143Nd) 的同位素.
- 使用-146 (146Sm) 和-147 (147Sm) 的同位素数据.
- 地质年代测定约27亿年前的岩石.
主要成果:
- 哈德逊湾土壤中的岩石 (约27亿年) 显示出最年轻的142Nd变异性.
- 结合的Sm-Nd同位素数据表明,这个古老的地是由超过42亿年的地重新加工而形成的.
- 在地球早期的15亿年间,
结论:
- 早期地球上的马菲克地可以存活超过10亿年.
- 这种古老的地是古老地起源的重要来源岩石.
- 这些发现为地球早期地的形成和演变提供了新的见解.
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