古磁证据证明了新古纪的板块运动
Jikai Ding1,2, Chris Rogers3, Ulf Söderlund4,5
1Department of Earth & Planetary Sciences, Yale University, New Haven, CT, USA. djikai@126.com.
Nature communications
|December 31, 2024
概括
地球板块构造学可能比以前认为的更早开始. 来自怀俄明克拉顿的新古磁数据表明,大约248亿年前发生了显著的地块运动,这表明早期的板块运动.
科学领域:
- 地质科学 地质科学
- 古磁力学是一种古磁学.
- 构造学 构造学 构造学 构造学
背景情况:
- 地球上板块构造的开始受到高度辩论,提出的开始时间差异很大.
- 古磁数据对于理解地球地块的大规模横向运动至关重要.
- 以前的古磁证据将最古老的相对水平运动限制在27亿到217亿年前.
研究的目的:
- 使用古磁数据调查最早板块构造的时间.
- 为了确定怀俄明和高级石坑的组装和并置的时间.
- 为了提供关于新古时代地块之间的相对水平运动的证据.
主要方法:
- 收购一个古磁极从怀俄明克拉顿.
- 对怀俄明和高级石坑的明显极地流浪路径的分析.
- 古磁学结果与构造层地图数据和地质代理数据的整合.
主要成果:
- 一个强大的古磁极可追溯到大约248亿年前,从怀俄明克拉顿中获得.
- 怀俄明和高级石坑可能在27亿至25亿年前组装在一起,直到21亿年前才相邻.
- 怀俄明和高级石坑之间的碰撞被认为是大约26亿年前的,由地质证据支持.
结论:
- 这项研究提供了强有力的证据,表明在新古时代,地块之间存在显著的相对水平运动.
- 这些发现表明,在25亿年前之前,板块流动在地球上是活跃的.
- 这项研究有助于解决围绕板块构造开始的争议.
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