从早期进化地形的石地化学记录了同期的停滞和移动盖的构造体制
Emily E Mixon1, Ann M Bauer1, Tyler B Blum1
1Department of Geoscience, University of Wisconsin-Madison, WI.
概括
早期的地球地球.
科学领域:
- 地质科学,地质化学和石油学.
- 了解早期地球的过程和地的演变.
背景情况:
- 早期大陆地的产生和重新加工是地球进化的关键.
- 40亿年前的板块构造设置被地循环覆盖.
- 的微量元素共变 (U,Nb,Sc,Yb) 作为可靠的板块构造学代理.
研究的目的:
- 应用的微量元素代码来解读早期的阿尔凯时构造学设置.
- 为了研究来自阿卡斯塔·格内斯和萨格勒克-希伯伦综合体的岩石石.
- 了解地球早期历史上的地生成和重制机制.
主要方法:
- 在磁性石的微量元素和氧同位素分析.
- 来自加拿大的阿卡斯塔·格尼斯综合体和萨格勒克-希伯伦综合体的晶体地岩的分析.
- 与全岩石地质化学和的U-Pb,Hf和O同位素数据的整合.
主要成果:
- 的U-Nb-Sc-Yb结果表明,水合玄武岩的融化早在3.9亿年前就发生了.
- 水性融参与了海底原地的重新加工和青少年地的产生.
- 的微量元素数据显示,在具有不同地质化学和同位素的环境中存在水性化.
结论:
- 水性玄武岩融化不仅仅局限于古代的一个构造磁体过程.
- 早期的阿凯时构造学设置包括停滞盖 (海洋高原) 和移动盖 (弧形) 两种制度.
- 这些发现为早期地球的复杂地力学条件提供了洞察力.
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