矿类矿石矿床中Cu/Au比率的起源
Werner E Halter1, Thomas Pettke, Christoph A Heinrich
1Isotope Geochemistry and Mineral Resources, Department of Earth Sciences, Swiss Federal Institute of Technology (ETH), ETH Zentrum NO, 8092 Zürich, Switzerland. halter@erdw.ethz.ch
概括
磁性硫化物液体通过缩铜和黄金等关键金属,直接影响矿矿床的组成. 这些金属后来被释放到热水流体中,控制矿石的比率.
科学领域:
- 地质化学 地质化学
- 经济地质学 地质学
- 石化学 石化学是一门学科.
背景情况:
- 矿类型矿石矿床是铜和黄金等金属的重要来源.
- 这些矿床中的金属的确切起源和演变仍然是积极研究的领域.
- 了解岩过程的作用对于勘探和资源评估至关重要.
研究的目的:
- 调查岩石硫化物液体与类矿石矿床元素组成之间的直接联系.
- 为了确定金属 (Cu,Au,Fe) 度和释放在岩演变过程中的机制.
- 评估岩石硫化物融演变对矿石矿床中经济金属比率的影响.
主要方法:
- 硫化物和酸盐融物中主要元素和微量元素的微分析.
- 使用激光剥离感应合等离子体质谱法 (LA-ICP-MS).
主要成果:
- 在岩石硫化物液体组成和矿类型矿石矿床特征之间建立了直接的相关性.
- 铜,黄金和铁在岩石进化过程中被发现集中在硫化物化物中.
- 这些金属随后在岩石历史的晚期释放到热水流体中.
- 岩硫化物液体的组成受岩源和地演变的影响.
结论:
- 岩石硫化物液体在控制矿类矿石矿床的经济金属比率方面发挥着关键作用.
- 岩和相关的硫化物化的演变直接决定了矿石形成的潜力.
- 这项研究为主要金属资源的起源提供了关键的见解.
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