哈夫尼同位素证据表明,大陆生长动态的转变发生在3.2 Gyr前
T Næraa1, A Scherstén, M T Rosing
1Geological Survey of Denmark and Greenland, GEUS, Øster Voldgade 10, 1350 Copenhagen K, Denmark. tomn@geus.dk
Nature
|June 5, 2012
概括
早期的地球地球.
科学领域:
- 地质化学 地质化学
- 构造学 构造学 构造学 构造学
- 同位素地质学的同位素.
背景情况:
- 地球的石化层由于地幔温度变化而演变为现代板块构造学.
- 大陆地的生长随着时间的推移而下降,大部分被阿基亚纪时期提取出来.
- 超级大陆周期影响了地的生长和经过30亿年前的重新加工.
研究的目的:
- 调查地球早期地中类似于现代的构造体制的启动.
- 分析了来自格陵兰西南部地下岩石的同位素数据.
- 确定石质层动态中的过渡的时间.
主要方法:
- 在的同位素分析.
- 在石的海同位素分析.
- 在石的位置氧同位素分析.
主要成果:
- 哈夫同位素时间模式揭示了岩石原石特征的变化.
- 岩石年龄为39亿至35亿年 (Gyr),来源于一个带状或枯竭的源.
- 年龄小于3.2 Gyr的岩石显示出年轻枯竭物质的添加,类似于Phanerozoic orogens.
结论:
- 一个过渡时期 (3.5-3.2 Gyr ago) 标志着从古代地进化转向现代板块构造学的转变.
- 早期地 (3.9-3.5 Gyr) 在与现代板块构造学不同的模式下形成.
- 在3.2 Gyr之后,地的形成涉及板块构造过程和青少年地的形成.
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