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Bryolithochemical studies in the search for and evaluation of gold-silver mineralization based on stream sediments (northeastern Russia)

机译:基于流沉积物(东北俄罗斯东北部)的金银矿化搜索和评价的浅黑摩尔化学研究

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The first bryolithochemical studies have been carried out within the Dukat ore field (Balygychan-Sugoi trough, northeastern Russia), in its northeast (Dukat Au-Ag deposit, Chaika site) and on its eastern flank (Au-Ag ore occurrence, Piritovyi site). Sampling was made along primary water streams draining Au-Ag ore zones, because the headstreams localized in the permafrost zone are poor in alluvial sediments or lack them, whereas the stream banks and beds are overgrown with aquatic and semiaquatic mosses. We examined samples of moss cushions with loose sediments (fine silt suspension and sand-silt material). The study has shown that moss cushions are an effective natural trap extracting finely dispersed, ultradisperse, and colloid-dispersed particles, including ore ones, from water stream suspension. The contents of major elements indicating Au-Ag mineralization (Au, Ag, Hg, Sb, As, Pb, and Zn) in the bryolithochemical and lithochemical samples were compared. The highest contents of these elements have been revealed in the bryolithochemical samples. Scintillation analysis shows a predominance of finely dispersed Au and Ag particles. The chemical composition of lithoparticles and probable species of elements indicating mineralization were studied by energy-dispersive X-ray microanalysis. It has been concluded that the bryolithochemical stream sediments are an integral part of the lithochemical ones and can also be effectively used to reveal geochemical anomalies and identify the corresponding ores. It is shown that the bryolithochemical sediment streams bear important information about the chemical composition of primary ores, as they have the same major indicator elements (Au, Ag, Hg, Sb, As, Pb, and Zn) and nearly the same mineral composition (finely dispersed gold and silver, electrum, silver sulfosalts, and simple sulfides). The proposed bryolithochemical research is promising not only for northeastern Russia but also for other areas with similar landscapes, primar
机译:第一个浅黑摩尔化学研究已经在Dukat Ore领域(Balygychan-Sugoi,东北俄罗斯),东北(Dukat Au-Ag押金,Chaika网站)和东部侧翼(Au-Ag矿石,Piritovyi网站)。取样沿着初级水流排出Au-Ag矿石区的原发性水流,因为Puxafrost区局部局部的脑脊在冲积沉积物中差,而溪流银行和床覆盖着水生和半苔藓覆盖。我们检查了松散沉积物(精细淤泥悬架和砂淤泥材料)的苔垫的样品。该研究表明,苔垫是一种有效的自然陷阱,从水流悬浮液中萃取精细分散的,超接和胶体分散的颗粒,包括矿石。比较了溴化细胞化学和岩石化学样品中的Au-Ag矿化(Au,Ag,Hg,Sb,Sb,Sb,Zn)的主要元素的含量。在溴二摩尔化学样品中揭示了这些元素的最高内容物。闪烁分析显示精细分散的Au和Ag颗粒的主要分析。通过能量分散X射线微基分析研究了表明矿化的岩石颗粒的化学成分和表明矿化的可能性。已经得出结论,溴罗地理流沉积物是岩石化学沉积物的一种组成部分,也可以有效地用于揭示地球化学异常并鉴定相应的矿石。结果表明,溴罗地理沉积物流具有关于初级矿石化学成分的重要信息,因为它们具有相同的主要指示剂元素(Au,Ag,Hg,Sb,As,Pb和Zn)和几乎相同的矿物组合物(精细分散的金银,电,硫磺,硫磺和简单的硫化物)。拟议的Broomithochemical研究不仅是俄罗斯东北部的承诺,而且很有适用于其他有景观的其他地区,Primar

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