同位素对矿石金属回收在潜水区的限制
1Commonwealth Scientific and Industrial Research Organization Exploration and Mining, Post Office Box 136, North Ryde, New South Wales 1670, Australia; Department of Earth Sciences, Monash University, Clayton, Victoria 3168, Australia;
概括
在拉多拉姆金矿下面的状地幔岩石显示出高度的铜,黄金,白金和. 这些金属很可能起源于地幔,通过构造过程聚焦.
科学领域:
- 地质化学 地质化学
- 经济地质学 地质学
- 地幔石化学地幔石化学
背景情况:
- 带有静脉的矿石 (peridotite xenoliths) 在巴布亚新几内亚利希尔岛的拉多拉姆金矿下面的地幔中被发现.
- 与周围的枯竭弧相比,这些异石的铜,金,白金和的度显著更高.
研究的目的:
- 为了调查Ladolam黄金矿藏中的金属的起源.
- 了解地幔在合金-表热性铜-金沉积物的形成中的作用.
主要方法:
- 在桃石异石中主要和微量元素的分析.
- 黄金矿石和地幔矿石的同位素分析.
主要成果:
- 与周围地幔相比,矿的矿含量是Cu,Au,Pt和Pd的2至800倍.
- 黄金矿石的同位素组成与潜伏修饰的地幔矿石来源相匹配.
- 地幔是拉多拉姆矿床金属的主要来源.
结论:
- 地幔是拉多拉姆黄金矿藏的主要金属来源.
- 凝聚可溶于液体的金属的构造过程对于形成酸盐-高热性铜-金沉积物至关重要.
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