概括
岩混合在形成斯蒂尔沃特综合体组元素 (PGE) 沉积物中发挥了关键作用. 同位素数据揭示了不同的岩来源,而非质岩为矿石地平线贡献了像米这样的基本元素.
科学领域:
- 地质化学 地质化学
- 经济地质学 地质学
- 同位素地球化学 同位素地球化学
背景情况:
- 蒙大拿州的静水综合体形成于大约2.7亿年前.
- 了解这个复杂的石化过程对于探索基元素 (PGE) 沉积物至关重要.
研究的目的:
- 调查岩混合在形成战略性PGE矿石矿床中的作用.
- 为了分析参与静水复合物入侵的岩石的同位素特征.
主要方法:
- 获取和分析 (Nd) 和 (Os) 的同位素数据.
- 超岩 (U型) 和无岩 (A型) 岩石地质化学特征的表征.
主要成果:
- 同位素数据表明,静水综合体起源于至少两个不同的岩石:U型和A型.
- U型岩显示了有回收地的岩层地幔来源,而A型岩则表明地污染或下层地融化.
- 矿石地平线 (例如,J-M礁) 中的和可能的其他PGEs起源于A型岩石.
- Nd和Os的同位素异质性表明A型岩多次注入U型岩室.
结论:
- 岩混合是形成静水综合体及其相关PGE沉积物的关键过程.
- U型和A型岩的不同同位素组成为它们的来源和进化途径提供了洞察力.
- 在J-M Reef矿石矿床内,A型岩是PGEs的主要来源,包括.
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