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首页> 外文期刊>Doklady Earth Sciences >Formation Stages of the Large-Scale Noble Metal Mineralization in the Sukhoi Log Deposit, East Siberia: Results of Isotope-Geochronological Study
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Formation Stages of the Large-Scale Noble Metal Mineralization in the Sukhoi Log Deposit, East Siberia: Results of Isotope-Geochronological Study

机译:西伯利亚东部苏霍伊测井矿床中大规模贵金属矿化的形成阶段:同位素-年代学研究结果

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摘要

This paper presents results of the Rb-Sr and K-Ar isotope-geochronological study of the Sukhoi Log deposit, one of the world's largest noble metal deposits localized among metasedimentary black shales. The deposits of this type (Muruntau, Uzbekistan; Nezhda-ninskoe, Russia; Ashanti, Gana; and others) account for a considerable part in the balance of mined gold and its potential reserves. The significance of these deposits and, primarily, the Sukhoi Log deposit became even higher with the discovery of Pt mineralization in some of them. However, the origin and especially age of the noble metal mineralization in the Sukhoi Log deposit remain controversial.
机译:本文介绍了Sukhoi测井矿床的Rb-Sr和K-Ar同位素-年代学研究结果,该矿床是世界上最大的贵金属矿床之一,位于准沉积黑色页岩中。这种类型的矿床(乌兹别克斯坦的穆伦陶;俄罗斯的涅日达宁斯科;加纳的阿散蒂;及其他)的矿藏在矿山黄金及其潜在储量中占相当大的比例。随着其中一些铂矿床的发现,这些矿床的重要性以及主要是苏霍伊原木矿床的重要性变得更高。然而,苏霍伊原木矿床中贵金属矿化的成因,特别是年龄尚有争议。

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