由于地的快速生长而形成的1.88亿年前铁层的沉积
Birger Rasmussen1, Ian R Fletcher, Andrey Bekker
1Department of Applied Geology, Curtin University, Kent Street, Bentley, Western Australia 6102, Australia.
Nature
|April 28, 2012
概括
大约188亿年前铁层的重新出现与地幔活动和火山活动的增加有关. 这释放了铁,尽管大气氧气水平上升,但暂时创造了铁质的海洋条件.
科学领域:
- 地质化学 地质化学
- 沉积物学的沉积物学
- 古代海洋学 古代海洋学 古代海洋学
背景情况:
- 铁的形成 (化学沉积岩) 需要无氧的,富含铁的海水.
- 它们的沉积在大气中的氧气增加后停止了,大约在232亿年前.
- 5亿年后的再现是一个科学难题.
研究的目的:
- 为了调查晚期古新生代铁形成沉积的原因.
- 为了确定澳大利亚的铁结构是否与北美铁结构同时代.
- 将铁形成沉积与全球地质事件联系起来.
主要方法:
- 在西澳大利亚的弗雷雷岩层内,岩层的石约会.
- 岩层的地化学分析.
- 与全球地质和地幔活动数据的相关性.
主要成果:
- 约会证实澳大利亚的铁矿形成有约1.88亿年的历史,与北美形成的同时代.
- 这种同期沉积表明全球海洋化学影响了铁的形成.
- 这一事件与地幔活动,地形成和火山性大硫化物形成的高峰相吻合.
结论:
- 增强的海底火山活动和热水活动释放了铁,压倒了海洋氧化剂.
- 这导致了铁质条件的暂时回归,使大气和海洋的氧化还原状态脱.
- 随后的铁矿形成的下降,很可能反映了地幔活动的减弱和水热铁流.
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