概括
基元素 (PGE) 在岩硫化物中的度与原始岩有关.
科学领域:
- 经济地质学 地质学
- 地质化学 地质化学
- 矿产矿产储备矿产储备矿产储备矿产储备矿产储备矿产储备矿产储备矿产储备
背景情况:
- 组元素 (PGE) 是重要的工业金属.
- PGE沉积物主要由分离的铁铜硫化物融物形成.
- 硫化物中PGE度的差异很大,不同于其他基元素.
研究的目的:
- 为了解释岩石硫化物中PGE度的变化.
- 为了确定PGE比例和母岩特征之间的关系.
- 研究控制矿石矿床中PGE分布的地质过程.
主要方法:
- 在各种沉积物中分析岩硫化物中PGE度.
- PGE相对比例与原始岩组成的相关性.
- 模拟部分化,批量平衡和分数分离过程.
主要成果:
- 硫化物中的PGE度跨越五个数量级.
- 相对PGE比例系统地与原始岩类型相关.
- 地幔部分化和硫化物分离过程的程度解释了观察到的度.
结论:
- 富含PGE的岩硫化物沉积物的形成是由地幔融度和硫化物分离控制的.
- 了解这些过程是探索新的PGE资源的关键.
- 存在大量未开发的PGE资源,特别是在北美 (例如,Stillwater综合体).
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