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Doklady Earth Sciences

, Volume 481, Issue 1, pp 877–878 | Cite as

Energy Parameters of Ore-Forming Deep Fluid Systems

  • F. A. Letnikov
  • B. S. Danilov
  • A. F. Letnikova
Geology
  • 5 Downloads

Abstract

The energy parameters of ore-forming deep fluid systems (enthalpy and Gibbs free energy) for compounds of S, Cl, and B have been estimated by thermodynamic methods at a lithosphere depth of 1000–20 km. At a depth of 1000 km, ore-forming fluids are dominated by BF3. With a decrease in a depth to 100–20 km, the range of fluid ore-forming systems becomes wider due to the B, F, Cl, and S compounds providing a real basis for development of the voluminous ore-forming fluid systems at the top of the lithosphere.

References

  1. 1.
    F. A. Letnikov, A. F. Letnikova, and B. S. Danilov, Dokl. Earth Sci. 453 (2), 1234–1237 (2013).CrossRefGoogle Scholar
  2. 2.
    F. A. Letnikov, B. S. Danilov, and P. I. Dorogokupets, Dokl. Earth Sci. 437 (2), 548–551 (2011).CrossRefGoogle Scholar

Copyright information

© Pleiades Publishing, Ltd. 2018

Authors and Affiliations

  • F. A. Letnikov
    • 1
  • B. S. Danilov
    • 1
  • A. F. Letnikova
    • 2
  1. 1.Institute of the Earth’s Crust, Siberian BranchRussian Academy of SciencesIrkutskRussia
  2. 2.Irkutsk State UniversityIrkutskRussia

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