Ore-Bearing Fluids of the Blagodatnoye Gold Deposit (Yenisei Ridge, Russia): Results of Fluid Inclusion and Isotopic Analyses

被引:8
作者
Shaparenko, Elena [1 ]
Gibsher, Nadezhda [1 ]
Tomilenko, Anatoly [1 ]
Sazonov, Anatoly [2 ]
Bul'bak, Taras [1 ]
Ryabukha, Maria [1 ]
Khomenko, Margarita [1 ]
Silyanov, Sergey [2 ]
Nekrasova, Natalya [2 ]
Petrova, Marina [1 ]
机构
[1] Russian Acad Sci, Siberian Branch, Sobolev Inst Geol & Mineral, Novosibirsk 630090, Russia
[2] Siberian Fed Univ, Dept Geol Mineral & Petrog, Krasnoyarsk 660041, Russia
关键词
Yenisei Ridge; Blagodatnoye deposit; gold; fluid inclusions; gas chromatography-mass spectrometry; FORMING FLUIDS; PHYSICOCHEMICAL PARAMETERS; HYDROTHERMAL FLUIDS; QUARTZ VEINS; AGE; TEMPERATURE; EVOLUTION; GEOCHEMISTRY; HYDROCARBONS; TECTONICS;
D O I
10.3390/min11101090
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Blagodatnoye deposit with 340 t gold reserves is one of the most productive mines in Russia. Modern methods of studying fluid inclusions were used to determine the properties of fluids that formed this deposit. A comprehensive study revealed that the Blagodatnoye gold deposit was formed between 120 and 350 degrees C and at 0.2-2.6 kbar, and from fluids with salinities ranging from 0.5 to 30 wt.% (NaCl-eq.). These fluids are: 1-water-carbon dioxide; 2-carbon dioxide-hydrocarbon; 3-highly saline aqueous. According to Raman spectroscopy and gas chromatography-mass spectrometry, ore-forming fluids contained H2O, CO2, hydrocarbons and oxygenated organic compounds, sulfonated, nitrogenated and halogenated compounds. Early oxidized water-carbon dioxide fluids formed barren associations of the deposit. Later reduced carbon dioxide-hydrocarbon fluids had a key role in the formation of gold-bearing quartz veins. The stable isotope data (delta S-34 = 0.8 to 21.3 parts per thousand, delta C-13 = -2.8 to -20.9 parts per thousand, He-3/He-4 = 0.14 +/- 0.3 x 10(-6)) suggest the ore-forming fluids have a crustal source.
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页数:20
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