Boiling assemblages in the Kupel occurrence, Krumovgrad goldfield, SE Bulgaria

I. Marinova, E. Tacheva
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引用次数: 1

Abstract

This paper presents a study on boiling assemblages in the Kupel occurrence, as boiling was evidenced by the presence of vein adularia and platy calcite. Fluid inclusion evidence is not available since the present fluid inclusions are very small in size for investigation under optical microscope. Boiling assemblages occur in two types of auriferous mineralization hosted by supradetachment, grey fine-grained arkosic sandstones and presented by (i) veinlets of quartz-adularia and (ii) veinlets of platy calcite. In quartz-adularia veinlets micron-sized electrum aggregates form globular shapes, which reach 800 µm across and are arranged along the veinlet length. In cross-sections electrum aggregates display abundant silicate-filled pores of a few microns in size. Globular geometry of the electrum aggregates and their arrangement along the veinlet length suggest collectively that these globules were flowing particles - flocs but not colloidal particles since the latter are much smaller. In these veinlets electrum is intergrown with micron-sized chalcopyrite, galena, hessite and greenockite. The auriferous calcite veinlets are formed later than the auriferous quartz-adularia ones, since the first clearly has intersected or brecciated the latter. Electrum in the calcite veinlets forms accumulations only in portions of sharp thickness expansions after throttle portions, which are barren. This suggests that electrum has been transported by a flowing fluid, in a particulate form and deposited due to pressure drop during hydrofracturing, as the electrum particles have been arrested in low velocity (expanded) portions of ore conduits. The auriferous assemblages in the Kupel occurrence indicate high effectiveness of boiling for deposition of Au, Ag, Cu, Pb, Cd and Te through collective loss of H2, CO2, H2S and H2Te what is in complete accord with recent studies on modern terrestrial geothermal fields. Methods used comprise observations under binocular, optical and scanning electron microscope, and electron microprobe analysis.
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保加利亚东南部克鲁莫夫格勒金矿库佩尔产层的沸腾组合
本文介绍了Kupel产状中沸腾组合的研究,因为沸腾的证据是存在静脉状的adularia和板状方解石。由于目前的流体包裹体尺寸很小,在光学显微镜下无法观察,因此没有流体包裹体的证据。沸水组合出现在两种含金矿化类型中,由上离脱岩、灰色细粒黑质砂岩赋存,表现为(i)石英-阿胶脉和(ii)板状方解石脉。在石英-紫砂脉中,微米大小的电晶体聚集体形成球状,其直径达到800微米,并沿着脉长排列。在横截面上,电极聚集体显示出大量的几微米大小的硅酸盐填充孔。电极聚集物的球状几何形状及其沿静脉长度的排列表明,这些小球是流动的颗粒-絮凝体,而不是胶体颗粒,因为后者要小得多。在这些细脉中,银与微米级的黄铜矿、方铅矿、海绢石和绿绿石共生。含金方解石脉脉的形成要晚于含金石英脉脉,因为前者明显与后者相交或角化。方解石脉脉中的银镁只在节流阀后厚度急剧膨胀的部分形成堆积,这些部分是贫瘠的。这表明,在水力压裂过程中,由于电解液颗粒在矿石管道的低速(膨胀)部分被截留,电解液以颗粒形式被流动的流体输送,并由于压降而沉积。Kupel产状的含金组合表明,沸腾通过H2、CO2、H2S和H2Te的集体损失沉积Au、Ag、Cu、Pb、Cd和Te具有较高的效率,这与现代陆地地热田的最新研究结果完全一致。使用的方法包括在双目,光学和扫描电子显微镜下观察,以及电子显微探针分析。
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