概括
在变态石榴石中,氧同位素区分揭示了变态过程中的液体透和脱水反应. 氧同位素值 (delta(18) O) 的这些变化为地质过程提供了洞察力.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 变态石器学 变态石器学
背景情况:
- 石榴石是变态岩石中的一个关键矿物,保留了关于P-T条件的信息.
- 氧同位素分析是追踪流体岩石相互作用的强大工具.
研究的目的:
- 为了研究氧同位素在变态石榴石中的划分.
- 了解变态过程对石榴石地质化学的影响.
主要方法:
- 稳定同位素激光探针分析氧同位素 (delta(18) O).
- 对来自佛蒙特州和犹他州的四颗石榴石进行了检查.
主要成果:
- 在所有检查的石榴石中观察到集中的氧同位素区分 (delta(18) O).
- 区域变态石榴石显示出最大的变化 (从核心到边缘高达3每毫米).
结论:
- 石榴石中的氧同位素区分反映了成长过程中岩石三角洲的变化.
- 液体透和脱水反应是转化过程中这些同位素变化的关键驱动因素.
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