Sulfur as an indicator for sulfide ores in lithochemical surveying
Authors:
Abstract
When searching for sulfide ores, sulfur is usually not determined in lithochemical samples. Meanwhile, with 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 the Allarechensky and Monchegorsk districts of the Kola Peninsula, up to 27–33% of sulfur was found, and in samples of pyrrhotite ores of the Allarechensky district, 20–26%.
Область исследования:
(Archived) Without section
Funding:
None
References
- Dreimanis A. Geochemical prospecting for copper, lead and zinc in the glaciated areas of Eastern Canada. Tr. XXI Mezhdunarodn. geol. kongr. Issue III. Mir, 1964 (in Russian)
- Garrels R. M. Rates of chemical reactions at low temperatures and pressures. Sb.: Geokhimicheskie issledovaniya , IL, 1961 (in Russian)
- Perelman A. I. Geochemistry of Epigenetic Processes (Hypergenesis Zone). Nedra, 1968 (in Russian)
- Sveshnikov G. B. Electrochemical Processes at Sulfide Deposits. LGU, 1967 (in Russian)
- Sokolov V. A. Geochemistry of Gases of the Earth's Crust and Atmosphere. Nedra, 1966 (in Russian)
- Kauranne L. K. Geologi, 1957, No. 2
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