大陆地在早期地球上的起源
1State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, China.
National science review
|September 12, 2025
概括
早期的地球地球.
科学领域:
- 地质科学 地质科学
- 早期地球的地质学
- 构造学领域 构造学领域
背景情况:
- 大陆地的起源与早期地球上的构造学领域有关.
- 仅从中的微量元素推断地岩的主要元素组成是有问题的.
- 哈迪纪时期很可能出现了非板块构造,用于形成地.
研究的目的:
- 研究构造学领域在早期大陆地形成中的作用.
- 为了解决使用的微量元素来推断地组成的局限性.
- 为了了解地球早期历史中地从状到状地的过渡.
主要方法:
- 分析的微量元素组成.
- 地质化学建模地的演变.
- 对哈迪纪和阿基纪的构造体制进行比较研究.
主要成果:
- 仅仅对的微量元素分析不足以确定地岩的主要元素组成.
- 非板块构造学可能在海底纪期间主导了岩地的形成.
- 板块构造学对于将哈地亚黄岩地转化为阿凯亚黄岩地至关重要.
结论:
- 构造领域的演化对于理解早期大陆地的起源至关重要.
- 从非板块到板块构造的转变标志着地组成的显著变化.
- 在阿尔盖时代,变化为状地是由板块构造过程驱动的.
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