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The Isotope Composition and Geochemical Features of Ores of the Dzhusa Pyrite–Polymetallic Deposit (Southern Urals)

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Abstract

The sulfur isotope composition was measured in the main morphological types and generations of sulfides composing the ores of the Dzhusa deposit and the contents of trace elements were measured using highly sensitive laser ablation-inductively coupled plasma-mass spectrometry (LA–ICP–MS) for the first time. According to the sulfur isotope geochemistry, we assume that a deep magmatic source made a predominant contribution to the ore-forming fluid. Using the STATISTICA software modules, correlation analysis was performed and the trace element distribution patterns in sulfides were revealed.

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ACKNOWLEDGMENTS

Analytical studies were performed at the Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of Russian Academy of Sciences (Moscow).

Funding

This work was supported by the Russian Science Foundation (project no. 14-17-00693-P).

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Authors and Affiliations

  1. Department of Geology, Moscow State University, 119991, Moscow, Russia

    E. I. Yartsev & N. I. Eremin

  2. Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences, Staromonetny per. 35, 119017, Moscow, Russia

    E. I. Yartsev & I. V. Vikentyev

Authors
  1. E. I. Yartsev
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  2. I. V. Vikentyev
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  3. N. I. Eremin
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Correspondence to E. I. Yartsev, I. V. Vikentyev or N. I. Eremin.

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Translated by D. Voroshchuk

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Yartsev, E.I., Vikentyev, I.V. & Eremin, N.I. The Isotope Composition and Geochemical Features of Ores of the Dzhusa Pyrite–Polymetallic Deposit (Southern Urals). Moscow Univ. Geol. Bull. 74, 504–509 (2019). https://doi.org/10.3103/S0145875219050144

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  • DOI: https://doi.org/10.3103/S0145875219050144

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