黄金含量是马菲克到的酸岩
Jia Chang1, Andreas Audétat2, Thomas Pettke3
1Bavarian Geoinstitute, University of Bayreuth, Bayreuth, 95440, Germany. Jia.Chang@uni-bayreuth.de.
Nature communications
|August 14, 2024
概括
岩岩本身并不是富含黄金的. 这项研究发现,它们的黄金度与性岩相似,这表明水热过程,而不是岩组成,驱动黄金沉积物的形成.
科学领域:
- 经济地质学 地质学
- 岩石岩石学 岩石岩石学
- 地质化学 地质化学
背景情况:
- 表面热性黄金和类型的沉积物通常与性岩石有关.
- 之前的假设表明,性岩异常富含金 (Au) 或具有高的Au/铜 (Cu) 比率.
- 这些假设缺乏严格的测试.
研究的目的:
- 为了测试岩岩是相关矿石矿床中异常高的黄金度的来源的假设.
- 在全球范围内分析酸盐岩石融含物中的黄金度和Au/Cu比率.
主要方法:
- 在化物融中分析黄金 (Au) 度.
- 在这些含量中确定Au/铜 (Cu) 的比率.
- 全球对岩进行采样.
主要成果:
- 马菲石岩含有低金 (Au) 度 (27 ng/g),即使在地幔化过程中硫化物耗尽.
- 性岩石中的绝对Au度和Au/Cu比率都与性岩石相比较.
- 岩分化显示Au/Cu比率的变化很小,这是由于单硫化物固体溶液的沉,Au和Cu的含量很低.
结论:
- 富含黄金的矿床与岩的联系并不是由于富含岩的组成.
- 在热水阶段的选择性黄金 (Au) 沉是丰富矿石矿床的可能原因.
- 这挑战了以前关于岩在黄金矿化中的作用的假设.
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