Optical cathodoluminescence petrography, combined with SEM and LA-ICP-MS analyses: a case study from the Elatsite porphyry Cu-Au deposit

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Elitsa Stefanova, M. Kadiyski, S. Georgiev, A. Hikov, Sylvina Georgieva, I. Peytcheva
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引用次数: 0

Abstract

In the present research, we have applied a combination of Cold-CL petrography with two in-situ techniques (SEM-EDS and LA-ICP-MS) to study quartz-pyrite-sericite veins with some carbonates from the Elatsite porphyry Cu-Au deposit. Based on Cold-CL images, we found out that these veins are formed during two stages: quartz-pyrite with sericite and later quartz-carbonate with chlorite. Together with the quartz and carbonates small amount of arsenian pyrite, hematite, chalcopyrite, sphalerite, galena and apatite are precipitated. SEM-EDS and LA-ICP-MS allowed determining that the observed zoning of the pyrite from Q-Py stage is due to a variable Co and Ni content. Similarly, the zonal growth of calcite is due to variable Mn content. Pyrite and arsenian pyrite have different trace element composition. Arsenian pyrite has elevated Au, Ag, Cu, Pb, Sb and Tl contents compared to the pyrite. The combination of the three techniques was essential for resolving temporal relationships between the minerals within quartz-pyrite-carbonate veins and changes of the composition of the pyrite from the quartz-pyrite-sericite to the later quartz-carbonate stage.
光学阴极发光岩相学与SEM和LA-ICP-MS分析相结合:以黄铜矿斑岩型铜金矿为例
在本研究中,我们应用Cold-CL岩相学与两种原位技术(SEM-EDS和LA-ICP-MS)相结合的方法,研究了榴辉斑岩型铜金矿床中含有部分碳酸盐的石英-黄铁矿-绢云母脉。通过Cold-CL成像,我们发现这些矿脉形成于石英-黄铁矿-绢云母和石英-碳酸盐-绿泥石两个阶段。除石英和碳酸盐外,还析出少量砷黄铁矿、赤铁矿、黄铜矿、闪锌矿、方铅矿和磷灰石。SEM-EDS和LA-ICP-MS可以确定从Q-Py阶段观察到的黄铁矿的分带是由于Co和Ni含量的变化。同样,方解石的带状生长是由于Mn含量的变化。黄铁矿和砷黄铁矿的微量元素组成不同。砷黄铁矿中Au、Ag、Cu、Pb、Sb和Tl的含量高于黄铁矿。这三种技术的结合对于解决石英-黄铁矿-碳酸盐脉内矿物与黄铁矿组成从石英-黄铁矿-绢云母到后期石英-碳酸盐阶段变化的时间关系至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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