Sulfur isotopic composition of sulfides at the Mangazeya silver deposit, Eastern Sakha-Yakutia, Russia

• Published in: Geology of ore deposits 2010-12, Vol.52 (6), p.479-495
• Main Authors: Anikina, E. Yu, Gamyanin, G. N., Bortnikov, N. S.
• Format: Article
• Language: English
• Subjects: Earth and Environmental Science; Earth Sciences; Mineral Resources
• ISSN: 1075-7015; 1555-6476
• DOI: 10.1134/S1075701510060048

The succession of the formation of ore zones and sulfur isotope ratio of sulfides at the Mangazeya Ag deposit have been studied. The deposit is located in the Nyuektame Fault Zone in the eastern limb of the Endybal Anticline. The ore zones are hosted in the Middle Carboniferous to Middle Jurassic terrigenous sequences of the Verkhoyansk Complex intruded by the Endybal subvolcanic stock and felsic and mafic dikes. Three ore stages are distinguished: (I) gold-rare metal, (II) cassiterite-sulfide, and (III) silver-base-metal. Products of these stages are spatially isolated. The δ 34 S of sulfides ranges from −6.4 to +8.0‰. In the sulfides of the gold-rare metal assemblage, this value varies from −1.8 to +4.7‰; in the sulfides of the cassiterite-sulfide stage, −6.4 to +6.6‰; and in the sulfides of the silver-base-metal assemblage, -5.6 to +8.0‰. A sulfur isotope thermometer indicates the temperature of mineral deposition at 315–415°C for the first stage and 125–280°C for the third stage. Possible causes of variable sulfur isotopic composition in sulfides are discussed. The data on the sulfur isotope ratio is interpreted in terms of involvement of magmatic fluid (δ 34 S ∼ 0) in the mineralizing process along with low-temperature fluid taking sulfur from host rocks (δ 34 S ≫ 0). Boiling and mixing of magmatic fluid with heated meteoric water were important at the last stage of the deposit formation.