概括
石中高同位素比率表明-87的"孤儿"成分. 这种成分源于带有破碎粘土的低温海水透,而不是来自地幔内的放射性衰变.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 海洋学 海洋学 海洋学
背景情况:
- 在深和高山矿石中,较高的同位素比率 (87) Sr/ (86) Sr) 超过了从简单的地幔和海水混合中预期的比率.
- 过量或"孤儿" (87) Sr的存在,看似与其放射性母体脱,通常归因于分析错误.
研究的目的:
- 在石样本中调查"孤儿" (87) Sr 的起源和位置.
- 确定将放射性引入海洋地的机制.
主要方法:
- 对大量深和高山矿样本的分析.
- 微观和化学检查矿变化产品,特别关注奥利文和恩斯塔.
- 在已识别的成分中对的同位素分析.
主要成果:
- "孤儿" (87) Sr成分位于奥利文和恩斯塔的变化产物中,位于深层的岩石中.
- 有证据表明,通过低温 (<200°C) 海水透来引入.
- 相关的破碎颗粒,包括来自大陆的粘土,具有高度的放射性.
结论:
- "孤儿" (87) 矿中的Sr不是一种分析工件,而是海水驱动的变化的结果.
- 带有放射性破碎物质的低温海水透是这种过量的的主要来源.
- 像"孤儿" (87) Sr这样的放射性同位素可以作为低温海水透到海洋地的有价值的标记物.
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