大气中的硫在阿尔盖亚科马提石宿主沉积物中的大气硫
Andrey Bekker1, Mark E Barley, Marco L Fiorentini
1Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch Road, NW, Washington, DC 20015, USA. bekker@cc.umanitoba.ca
概括
古代铁硫化物沉积中的硫是来自大气处理和海洋底积累的. 由地幔衍生的岩石将这种硫结合起来,在海洋缺乏硫时形成沉积物.
科学领域:
- 地质化学 地质化学
- 经济地质学 地质学
- 前坎布里亚时期的古生物学.
背景情况:
- 大规模的铁 (Fe-Ni) 硫化物矿石矿床是在阿纪和早期原生纪时代形成的.
- 了解金属和硫的来源是它们形成的关键.
- 古代海洋的特点是硫度低.
研究的目的:
- 为了调查硫的起源在阿尔盖亚komatiite托管的Fe-Ni硫化物沉积物.
- 阐明涉及这些重要的矿石体起源的过程.
主要方法:
- 分析了来自阿克海科马岩托管的Fe-Ni硫化物沉积物的多重硫同位素数据.
- 从大气到海洋环境的硫循环路径的重建.
主要成果:
- 硫同位素数据表明先前的大气处理和随后的海洋底积累.
- 有证据表明,硫是从海底的水热硫化物和硫化页岩中获取的.
- 由地幔衍生的科马岩岩吸收了这种加工的硫.
结论:
- 古代Fe-Ni硫化物沉积物中的硫黄起源于大气和海洋储库.
- 科马岩岩在将这种硫融入矿石矿床中起到了至关重要的作用.
- 这项研究揭示了早期地球海洋中硫含量有限的矿石形成过程.
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