钻石中的硫同位素揭示了大陆结构的不同
Karen V Smit1, Steven B Shirey2, Erik H Hauri2
1Gemological Institute of America, 50 West 47th Street, New York, NY 10036, USA. ksmit@gia.edu.
概括
新生代的钻石揭示了地球表面的古老的硫痕迹. 这表明早期的构造过程,包括沉积,在数十亿年前形成大陆石中发挥了关键作用.
科学领域:
- 地质化学
- 同位素地质学
- 构造学
背景情况:
- 来自西非的新新生代钻石含有具有独特硫同位素特征的硫化物含量.
- 这些含量中的硫同位素的质量独立分离 (MIF) 表明与阿尔盖表面过程的联系.
研究的目的:
- 调查西非钻石中MIF同位素的来源.
- 了解构造过程在地幔表面的作用.
- 为了将钻石形成和硫同位素记录与克拉顿进化相关联.
主要方法:
- 在新生代钻石中的硫化物含量分析.
- 对含有钻石的石坑进行地质和地时间研究 (西非,斯拉夫,卡普瓦尔,津巴布韦).
主要成果:
- 西非钻石含有MIF同位素,可以追溯到地幔的古老表面特征.
- 记录了两个不同的沉积事件:大约30亿年前 (石质层加厚) 和大约6.5亿年前 (重新加工和钻石生长).
- 来自卡普瓦尔,津巴布韦和西非克拉顿的年轻钻石含有MIF硫,与较老的奴隶克拉顿钻石不同.
结论:
- 钻石内含的硫同位素记录反映了阿克海大陆岩层形成期间的构造过程的变化.
- 克拉结构,特别是通过地层岩层通过沉积增厚,与MIF硫的存在有关.
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