Native Gold from Alluvial Sediments of the Kyvvozh Region and Its Possible Sources (Vol–Vym Uplift, Central Timan)

IF 0.8 4区 地球科学 Q3 GEOLOGY Geology of Ore Deposits Pub Date : 2024-08-28 DOI:10.1134/s1075701524600178
K. G. Parkhacheva, Yu. V. Glukhov, M. Yu. Sokerin, S. K. Kuznetsov, R. I. Shaibekov
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Abstract

The most possible genetic types of primary sources are determined on the basis of study of typomorphic features of gold from alluvial sediments of the Kyvvozh region of Central Timan, including economic placers. The size of gold particles widely varies, reaching small nuggets; there are rounded, weakly rounded, and nonrounded particles. Many of them underwent recurrent deformations in form of envelope curves, pits, and fractures. Most gold grains have high-fineness rims. Native gold always contains Ag and, locally, Cu, Pd, and Hg. There are frequent blocky gold particles with high-Ag veinlet zones. Native gold is intergrown with and contains inclusions of pyrite and galena and rarely minerals of the cobaltite–gersdorffite series, ankerite, galenobismuthite, native bismuth, and aurostibite, as well as sudovikovite PtSe2, which is identified for the first time in the region. Three types of native gold are recognized: (1) homogenous Ag-bearing, (2) blocky with high-Ag veinlet zones, and (3) rare Ag-bearing with Cu and Pd. The morphology, composition, and structure of placer gold indicate its contribution from various (including proximal) sources. The NW-oriented zones of hydrothermal stringer-disseminated sulfide mineralization, which are partly exposed during placer exploitation, are most interesting. Native gold with Cu and Pd is most likely related to the derivatives of basic magmatism. The Vol–Vym, Tsil’ma, and Chetlas uplifts of Central Timan can be considered the promising for primary gold and deserve further study and searching works.

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基伏沃日地区冲积沉积物中的原生金及其可能的来源(伏尔维姆隆起,中蒂曼地区)
摘要 根据对中提曼省基辅沃日地区冲积沉积物(包括经济堆积物)中金的类型特征的研究,确定了原生矿源最可能的遗传类型。金颗粒的大小差异很大,甚至有小金块;有圆形、弱圆形和非圆形颗粒。其中许多颗粒经历了反复变形,形成了包络曲线、凹坑和裂缝。大多数金粒都有高细度的边缘。原生金总是含有银,局部还含有铜、钯和汞。经常出现块状金颗粒,并伴有高银细脉带。原生金与黄铁矿和方铅矿相互交错,并含有黄铁矿和方铅矿的包裹体,很少有钴铁矿-格斯多佛铁矿系列、黝帘石、方铋矿、原生铋、黝帘石,以及在该地区首次发现的苏多维可夫石 PtSe2。原生金有三种类型:(1) 均质含 Ag,(2) 块状含高金细脉带,(3) 含铜和钯的稀有含 Ag。块状金的形态、成分和结构表明它来自不同的(包括近端)来源。最令人感兴趣的是西北向热液串状浸蚀硫化物矿化带,这些矿化带在块金开采过程中部分暴露出来。含铜和钯的原生金很可能与碱性岩浆岩的衍生物有关。中提曼的沃尔维姆(Vol-Vym)、齐勒马(Tsil'ma)和切特拉斯(Chetlas)隆起带可被视为原生金的宝地,值得进一步研究和勘探。
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来源期刊
Geology of Ore Deposits
Geology of Ore Deposits 地学-地质学
CiteScore
1.10
自引率
14.30%
发文量
24
审稿时长
6-12 weeks
期刊介绍: Geology of Ore Deposits is a periodical covering the topic of metallic and nonmetallic mineral deposits, their formation conditions, and spatial and temporal distribution. The journal publishes original scientific articles and reviews on a wide range of problems in theoretical and applied geology. The journal focuses on the following problems: deep geological structure and geodynamic environment of ore formation; distribution pattern of metallogenic zones and mineral deposits; geology and formation environment of large and unique metallic and nonmetallic deposits; mineralogy of metallic and nonmetallic deposits; physicochemical and isotopic characteristics and geochemical environment of ore deposition; evolution of ore-forming systems; radiogeology and radioecology, economic problems in exploring, developing, and mining of ore commodities.
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