巨型矿铜沉积物的最佳岩氧化条件
Dian-Zhong Wang1, Jing-Jing Zhu1, Ruizhong Hu2
1State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.
Science bulletin
|January 17, 2025
概括
适度氧化的岩石 (大约 ΔFMQ +1) 是形成巨型矿铜沉积物 (PCD) 的最佳条件. 较高的氧化水平显著降低了铜沉效率,与此前的假设相反.
科学领域:
- 经济地质学 地质学
- 岩石地质化学 岩石地质化学
- 矿产沉积物的形成
背景情况:
- 矿铜沉积物 (PCDs) 的形成与中度至高度氧化的岩石有关.
- 有限的研究存在于磁性氧气流动性 (fO) 对PCD起源的具体影响.
- 巨型PCD通常在氧气流动度在 ΔFMQ -0.5 和 ΔFMQ +2.5.5 之间的 magma 中形成.
研究的目的:
- 为了研究可变的岩氧气流动性对铜沉效率的定量影响.
- 为了确定形成巨型PCD的最佳岩氧化状态.
主要方法:
- 与氧气流失性相关的硫种的数值建模.
- 石矿学建模以评估不同FO2条件下的铜沉效率.
主要成果:
- 铜沉效率在较高的氧气流动性值 (ΔFMQ +2和ΔFMQ +3) 与ΔFMQ +1.0相比大幅下降.
- 硫化硫 (S2-) 变异,对于铜沉至关重要,在高度氧化的岩石中显著减少.
- 最大的铜沉效率,因此潜在的赋予,发生在 ΔFMQ +1.1 左右.
结论:
- 适度氧化的岩 (大约 ΔFMQ +1) 是巨型PCD形成的最佳条件.
- 高氧化 (ΔFMQ > +2) 不太适合大量的铜沉和沉积物形成.
- 这一发现完善了对岩氧化状态在控制铜矿化中的关键作用的理解.
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