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Vol 64 Iss. 2
Pages:
77-82
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RUS
Article

Sulfur as an indicator for sulfide ores in lithochemical surveying

Authors:
N. F. Mayorov
Date submitted:
1973-08-19
Date accepted:
1973-10-17
Date published:
1974-02-01

Abstract

When searching for sulfide ores, sulfur is usually not determined in lithochemical samples. Meanwhile, at clark values in the lithosphere of 0.047%, its content in sulfide ores reaches tens of percent. Thus, in samples of sulfide copper-nickel ores of Allarechensky and Monchegorsk districts of the Kola Peninsula up to 27-33% of sulfur was found, in .samples of pyrrhotite ores of Allarechensky district 20-26%.

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References

  1. Dreimanis A. Geochemical prospecting for copper, lead and zinc in the glaciated areas of Eastern Canada. Proc. XXI International Geol. Congress. Vol. III. World, 1964.
  2. Garrels R.M. Rates of chemical reactions at low temperatures and pressures. In the proceedings: Geochemical Investigations, IL, 1961.
  3. Perelman A.I. Geochemistry of Epigenetic Processes (Hypergenesis Zone). Nedra, 1968.
  4. Sveshnikov G. B. Electrochemical Processes at Sulfide Deposits. LSU, 1967.
  5. Sokolov V. A. Geochemistry of Earth Crust and Atmosphere Gases. Nedra, 1966.
  6. Каurаnnе L. K. Geologi, 1957, No. 2.

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